Sample records for rio pilcomayo basin

  1. Reconnaissance of sedimentation in the Rio Pilcomayo Basin, May 1975, Argentina, Bolivia, and Paraguay

    Ritter, John R.


    The Rio Pilcomayo ' Alto ' (Bolivia) and ' Superior ' (Bolivia, Argentina, and Paraguay) transport large quantities of sediment for the size of the basin. The Rio Pilcomayo ' Inferior ' (Argentina and Paraguay) carries little sediment. The large loads of the ' Alto ' and ' Superior ' must be considered before dams or irrigation projects are started. The shifting channel and flooding of the Rio Pilcomayo ' Superior ' also are problems to be considered before development. The Rio Pilcomayo ' Alto ' basin has relatively little sediment deposition whereas the ' Superior ' basin has considerable deposition. A part of the ' Superior ' channel is filled with sediment to the top of its banks. The upstream limit of filling is moving farther upstream each year causing the place of overbank flooding to move upstream also. (Woodard-USGS)

  2. Simulations of Precipitation Variability over the Upper Rio Grande Basin

    Costigan, Keeley R.; Bossert, James E.; Langley, David L.


    In this research, we study Albuquerque`s water and how it may be affected by changes in the regional climate, as manifested by variations in Rio Grande water levels. To do this, we rely on the use of coupled atmospheric, runoff, and ground water models. Preliminary work on the project has focused on uncoupled simulations of the aquifer beneath Albuquerque and winter precipitation simulations of the upper Rio Grande Basin. The latter is discussed in this paper.

  3. A new species of Microglanis (Siluriformes: Pseudopimelodidae from upper rio Paraná basin, Brazil

    Oscar Akio Shibatta

    Full Text Available Microglanis garavelloi, new species, collected in tributaries of rio Paranapanema and rio Tietê, is the first species of the genus described from upper rio Paraná basin. The new species can be distinguished from other species of Microglanis on morphometric characters, color pattern, caudal-fin shape, pectoral-spine morphology and lateral line development. Characters used specifically to distinguish M. garavelloi from M. cottoides (laguna dos Patos and rio Uruguay basins and M. parahybae (rio Paraíba do Sul basin include morphometrics, color pattern and pectoral-spine serration.

  4. Metal exposure and reproductive disorders in indigenous communities living along the Pilcomayo River, Bolivia.

    Stassen, M.J.M.; Preeker, N.L.; Ragas, A.M.; Ven, M.W. van de; Smolders, A.J.P.; Roeleveld, N.


    BACKGROUND: The Pilcomayo River is polluted by tailings and effluents from upstream mining activities, which contain high levels of metals. The Weenhayek live along this river and are likely to have elevated exposure. OBJECTIVES: To assess whether the Weenhayek have increased risk of reproductive

  5. Metal exposure and reproductive disorders in indigenous communities living along the Pilcomayo River, Bolivia.

    Stassen, M.J.M.; Preeker, N.L.; Ragas, A.M.; Ven, M.W. van de; Smolders, A.J.P.; Roeleveld, N.


    BACKGROUND: The Pilcomayo River is polluted by tailings and effluents from upstream mining activities, which contain high levels of metals. The Weenhayek live along this river and are likely to have elevated exposure. OBJECTIVES: To assess whether the Weenhayek have increased risk of reproductive an

  6. Campano-Maastrichtian foraminifera from onshore sediments in the Rio del Rey Basin, Southwest Cameroon

    Njoh, Oliver Anoh; Victor, Obiosio; Christopher, Agyingi


    Campanian-Maastrichtian marine sediments outcrop in five genetically linked sedimentary basins along the West African coast in the Gulf of Guinea, from the Douala Basin in Cameroon to the Anambra Basin in Nigeria. These sediments in the more centrally located Rio del Rey Basin have been the least studied. Therefore, the geologic history of this region has merely been speculative. The Rio del Rey Basin like the adjacent Niger Delta is producing hydrocarbon from the offshore Tertiary sedimentary interval in which all studies have been focused, neglecting the onshore Cretaceous sediments. Outcrops in the basin are rare, small and highly weathered. Samples from some of these sediments have yielded a few Planktonic and dominantly benthonic foraminiferal assemblages. The long-ranging heterohelix and hedbergellids characterized the planktics while the species Afrobolivina afra which is a well known diagnostic taxon for Campanian-Maastrichtian sediments in West African basins clearly dominate the benthic assemblage. Its occurrence in association with other Upper Cretaceous forms such as Bolivina explicata, Praebulimina exiqua, Gabonita lata, Ammobaculites coprolithiformis amongst others, formed the basis on which this age was assigned to the sediments sampled from the Rio del Rey Basin. Hence, this work has undoubtedly established the much needed link in this regional geologic history and correlates these sediments with the Logbaba and Nkporo Formations in the Douala Basin in Cameroon and the southeastern Nigerian Sedimentary Basins. Thus, these units were all deposited during this same geologic period and probably controlled by the same geologic event.

  7. Redescription of Astyanax guaporensis Eigenmann, 1911 (Characiformes: Characidae), a small characid from the rio Madeira basin.

    Marinho, Manoela M F; Ohara, Willian M


    During recent expeditions to several localities in the rio Madeira basin, a poorly known species of Characidae described more than a century ago, Astyanax guaporensis Eigenmann, was collected. The species is herein redescribed based on the type material and many recently collected specimens. The species seems to occur only in the rio Madeira basin, rio Amazonas drainage. The species is mainly recognized among its congeners by having five to nine maxillary teeth, a series of V-shaped marks on the midlateral line of body, and the absence of a black mark on the caudal peduncle.

  8. Cenários ambientais na bacia do rio Atibaia Environmental scenarios in the Atibaia river basin

    Antonio Carlos Demanboro


    Full Text Available No presente artigo realizou-se uma análise integrada da bacia hidrográfica do rio Atibaia. Foi feito diagnóstico ambiental da área de estudo. Aplicou-se a metodologia desenvolvida pela Organisation for Economic Co-Operation and Development, em 2003, associada àquela aprimorada por Tricart e adaptada por Ross (1994. Foram selecionados 33 indicadores ambientais que permitiram as representações física e espacial da bacia e subsidiaram a elaboração de cenários. Foram elaborados três deles para a bacia hidrográfica do rio Atibaia, denominados tendencial, manejo e conservação. Avaliaram-se as potencialidades e fragilidades da bacia, o que gerou resultados que permitiram nortear a gestão adequada dos recursos hídricos e a conservação ambiental. Conclui-se que, no cenário conservação, foram observadas as melhores condições para ocorrer a restauração da qualidade ambiental da bacia.This paper presents an integrated analysis of the Atibaia river basin. An environmental diagnosis was performed in the study area. It was applied the methodology developed by the Organisation for Economic Co-Operation and Development, in 2003, coupled to that done by Tricart and adapted by Ross (1994. We selected 33 environmental indicators which allowed physical and spatial representations of the basin and supported the development of scenarios. Three of them were developed for the Atibaia river basin, called trend, management, and conservation. We evaluated the strengths and weaknesses of the basin, which generated results that allowed to manage water resources and environmental conservation. The main conclusion is that, in the conservationscenario, best conditions to restore the environmental quality of the basin were observed.

  9. Trace elements and organic compounds associated with riverbed sediments in the Rio Grande/Rio Bravo basin, Mexico and Texas

    Lee, R.W.; Wilson, J.T.


    In 1991, the Texas Natural Resource Conservation Commission (TNRCC) was mandated by the Texas Clean Rivers Act (Senate Bill 818) to assess water quality of rivers in Texas. Recent efforts to collect information for the assessment of water quality in the Rio Grande/Rio Bravo Basin have involved Federal agencies on both sides of the 1,248-mile U.S.-Mexico border?U.S. Environmental Protection Agency, U.S. Geological Survey (USGS), Secretaria de Desarollo Social (Secretary for Social Development, Mexico), National Water Commission of Mexico, and International Boundary and Water Commission?as well as State and local agencies in a spirit of international cooperation. Substantial efforts have been made to gather data needed to determine the quality of water and ecological status of the Rio Grande/Rio Bravo, especially at sites along the border (fig. 1). The purpose of this report is to assess selected historical data of trace elements and organic compounds in riverbed sediments of the Rio Grande/Rio Bravo, and of the Pecos River and the Arroyo Colorado in Texas.

  10. Hemiodus iratapuru, a new species of Hemiodontidae from the Rio Jari, Amazon Basin, Brazil (Teleostei, Characiformes).

    Langeani, F; Moreira, C R


    Hemiodus iratapuru, a new species of the Hemiodontidae from the Rio Iratapuru, a left bank tributary of the Rio Jari, Amazon Basin, Brazil, is described. The new species is diagnosed from other species of Hemiodus by modifications in the ectopterygoid, tooth form, scale counts, dorsal-fin form and colour pattern. The new species is proposed to be related to the Hemiodus quadrimaculatus species group.

  11. Research and management of soil, plant, animal, and human resources in the Middle Rio Grande Basin

    Deborah M. Finch


    The Rocky Mountain Forest and Range Experiment Station initiated a research program in 1994 called. "Ecology, diversity, and sustainability of soil, plant, animal, and human resources of the Rio Grande Basin". This program is funded by an Ecosystem Management grant from Forest Service Research. Its mission focuses on the development and application of new...

  12. Fishing resources in the rio Cuiabá basin, Pantanal do Mato Grosso, Brazil

    Lúcia. A. F. Mateus

    Full Text Available The rio Cuiabá is one of the most important tributaries of the upper rio Paraguay basin that form the Pantanal wetlands. The fishing resources of the rio Cuiabá basin were studied based on landing data obtained from the Fish Market of the city of Cuiabá, State of Mato grosso, Brazil. A description is given of the composition and origin of the 2000 and 2001 catch. The rio Cuiabá is the main source of fish for Cuiabá, although some fish sold locally comes from the rio Paraguay. The 2000-2001 catch consisted mainly of migratory species. The main landed species were the pimelodids pintado -Pseudoplatystoma corruscans, cachara -Pseudoplatystoma fasciatum, and jaú -Paulicea luetkeni, and the characiforms pacu -Piaractus mesopotamicus, piraputanga -Brycon microlepis, piavuçu -Leporinus macrocephalus, and dourado -Salminus brasiliensis. Large catfishes (Pimelodidae represented 70% of the landed fish, among which pintado was the most abundant. The data indicate that current catches are smaller than those recorded in the early 1980s and fish are caught far off the urban zone. Moreover, although the number and composition of species caught were similar to those of the 80s, the distribution of species abundance has changed. Currently, fisheries catch more carnivorous species than fish from lower trophic levels. These findings cannot be credited solely to overfishing, but appear to result from a complex interaction of factors, i.e., environmental degradation, changes in market preferences, and restrictive legal fishing regulations.

  13. Introduction in New perspectives on Rio Grande rift basins: from tectonics to groundwater

    Hudson, Mark R.; Grauch, V.J.S.


    Basins of the Rio Grande rift have long been studied both for their record of rift development and for their potential as host of natural resources. Early workers described the basin geomorphology and the character of infilling sediments (e.g. Siebenthal, 1910; Bryan, 1938; Speigel and Baldwin, 1963), and subsequent research compilations provided general stratigraphic and tectonic overviews of rift basins and described their geophysical characteristics within the crust (Hawley, 1978; Riecker, 1979; Baldridge et al., 1984; Keller, 1986). Subsurface knowledge gained from hydrocarbon exploration activities coupled with detailed surface studies of basins and their flanking uplifts were presented in Geological Society of America (GSA) Special Paper 291, edited by Keller and Cather (1994a).

  14. IRBM for the Rio Conchos Basin as a Restoration and Conservation Tool

    Barrios, E.; Rodriguez, J. A.; de La Maza, M.


    The Rio Conchos basin is the main water supply for the people of the State of Chihuahua and the middle and lower Rio Bravo in northern Mexico. Flowing for about 850 km from the highlands of the Sierra Tarahumara towards the wide valleys of the Chihuahuan Desert, the river presents recurrent periods of water stress and its basin of 6.7 million of hectares experiences a wide spectrum of problems such us long drought periods, water over allocation and extraction, water pollution, severe soil use changes. Besides, drastic soil moisture reduction is forecasted by effects of climate change. These natural and anthropological harmful situations impose a serious stress for this important and beautiful river and the rest of the basin hydrological resources. The WWF-Gonzalo Rio Arronte Alliance and its partners USAID, The Coca Cola Company and RICOH are implementing since 2004 an Integrated River Basin Management (IRBM) strategy to recover the natural integrity of the Rio Conchos in the form of environmental flow. The strategy includes the five basic working lines: i) development of river basin scientific knowledge, ii) strengthen of local institutional capacities, iii) development of demonstrative projects, iv) strengthen of indigenous communities, v) education and communication. Although the implementation of the IRBM program is expected to show main results until the year 2050, some interesting results have been obtained. The strategy has provided i) new basic knowledge about the basin dynamic events such as soil change use rates, baseline values of biological integrity, water economic values, among others; ii) strong program acceptance by government and main water users (farmers), and the integration of a working group formed by government, academia and NGO's; iii) local acceptance and understanding of benefits about basin management (soil recovery, reforestation, ecological sanitation) through demonstrative projects; iv) social organization; v) few advances in education

  15. Water resources simulation in the Rio Grande basin using coupled models

    Springer, E.P.; Winter, C.L.; Bossert, J.E.


    Regional assessments of water resources under global climate change require models that can resolve management, land use, and climate effects. Los Alamos National Laboratory is developing a coupled model of water resources that places a river basin in its global context. The upper Rio Grande basin above El Paso, Texas is the testbed for this model. The model structure and computational approach are emphasize and issues such as nonlinear feedback between components and spatial and temporal scaling of processes are discussed. Using simulations of regional meteorology, the effects of high spatial resolution simulations on the distribution of precipitation are demonstrated.

  16. Existing opportunities to adapt the Rio Grande/Bravo Basin Water Resources Allocation Framework


    The study of the Rio Grande/Bravo (RGB) Basin water allocation demonstrates how the United States (U.S.) and Mexico have consolidated a transboundary framework based on water sharing. However, the water supply no longer meets the ever-increasing demand for water or the expectations of different stakeholders. This paper explores opportunities for an enhanced management regime that will address past problems and better examine how to balance demands for a precious resource and environmental nee...

  17. Hyphessobrycon lucenorum (Characiformes: Characidae), a new species from the rio Madeira basin, Rondônia State, Brazil.

    Ohara, Willian M; Lima, Flávio C T


    A new species of characid is described from the upper rio Machado, a tributary of the rio Madeira basin, Rondônia, Brazil. Hyphessobrycon lucenorum can be distinguished from all congeners by the unique combination of the presence of a conspicuous rounded humeral blotch and a broad and diffuse longitudinal stripe. The new species is included within the Hyphessobrycon agulha group. The high number of endemic species of fishes occurring in the headwater tributaries of three river systems (rio Madeira, rio Tapajós, and rio Paraguai) draining the watershed defined by the Chapada dos Parecis is discussed.

  18. Economic Value of Water in the Rio Bravo Basin (Mexico) : The Case of Bajo San Juan, Juarez and Saltillo


    This paper evaluates the economic value of water in three locations in the Rio Bravo Basin. Formally known as the Bravo-Conchos, this basin overlaps across five Mexican states, beneath the Rio Bravo in northeastern Mexico. The paper also estimates the level of economic output in terms of value added for the main economic activities, using official statistics. The evaluation of water use pr...

  19. Uncertainty in climate change impacts on water resources in the Rio Grande Basin, Brazil

    M. T. Nóbrega


    Full Text Available We quantify uncertainty in the impacts of climate change on the discharge of Rio Grande, a major tributary of the Paraná River in South America and one of the most important basins in Brazil for water supply and hydro-electric power generation. We consider uncertainty in climate projections associated with the greenhouse-gas emission scenarios (A1b, A2, B1, B2 and increases in global mean air temperature of 1 to 6° C for the HadCM3 GCM (Global Circulation Model as well as uncertainties related to GCM structure. For the latter, multimodel runs using 6 GCMs (CCCMA CGCM31, CSIRO Mk30, IPSL CM4, MPI ECHAM5, NCAR CCSM30, UKMO HadGEM1 and HadCM3 as baseline, for a +2° C increase in global mean temperature. Pattern-scaled GCM-outputs are applied to a large-scale hydrological model (MGB-IPH of Rio Grande Basin. Based on simulations using HadCM3, mean annual river discharge increases, relative to the baseline or control run period (1961–1990, by +5% to +10% under the SRES emissions scenarios and from +8% to +51% with prescribed increases in global mean air temperature of between 1 and 6° C. Substantial uncertainty in projected changes to mean river discharge (−28% to +13% under the 2° C warming scenario is, however, associated with the choice of GCM. We conclude that, in the case of Rio Grande Basin, the most important source of uncertainty derives from the GCM rather than the emission scenario or the magnitude of rise in mean global temperature.

  20. Uncertainty in climate change impacts on water resources in the Rio Grande Basin, Brazil

    M. T. Nóbrega


    Full Text Available We quantify uncertainty in the impacts of climate change on the discharge of the Rio Grande, a major tributary of the River Paraná in South America and one of the most important basins in Brazil for water supply and hydro-electric power generation. We consider uncertainty in climate projections associated with the SRES (greenhouse-gas emission scenarios (A1b, A2, B1, B2 and increases in global mean air temperature of 1 to 6 °C for the HadCM3 GCM as well as uncertainties related to GCM structure. For the latter, multimodel runs using 6 GCMs (CCCMA CGCM31, CSIRO Mk30, IPSL CM4, MPI ECHAM5, NCAR CCSM30, UKMO HadGEM1 and HadCM3 as baseline, for a + 2 °C increase in global mean temperature. Pattern-scaled GCM-outputs are applied to a large-scale hydrological model (MGB-IPH of the Rio Grande Basin. Based on simulations using HadCM3, mean annual river discharge increases, relative to the baseline period (1961–1990, by + 5% to + 10% under the SRES emissions scenarios and from + 8% to + 51% with prescribed increases in global mean air temperature of between 1 and 6 °C. Substantial uncertainty in projected changes to mean river discharge (− 28% to + 13% under the 2 °C warming scenario is, however, associated with the choice of GCM. We conclude that, in the case of the Rio Grande Basin, the most important source of uncertainty derives from the GCM rather than the emission scenario or the magnitude of rise in mean global temperature.

  1. A new species of Moenkhausia Eigenmann, 1903 (Characiformes, Characidae) from the rio Amazonas basin, Brazil.

    Oliveira, Gustavo D; Marinho, Manoela M F


    Moenkhausia abyss is herein described from the rio Amazonas basin lowlands. The new species can be distinguished from the congeners by presenting the combination of the following characters: a dark blotch located on the upper caudal-fin lobe and the lower lobe hyaline, 25-29 branched anal-fin rays, humeral spot rectangular, vertically oriented, extending horizontally through two or two and a half scales and located over the third to the fifth lateral line scales, five longitudinal scale rows above the lateral line, predorsal scales arranged in a single not interrupted median row and 30-34 perforated lateral line scales. Brief comments on Moenkhausia megalops are provided.

  2. Metal exposure and reproductive disorders in indigenous communities living along the Pilcomayo River, Bolivia

    Stassen, Marinke J.M., E-mail: [Department of Environmental Science, Institute for Water and Wetland Research, Radboud University Nijmegen, Heyendaalseweg 135, 6525 AJ Nijmegen (Netherlands); Foundation ' Los Amigos del Pilcomayo' , P.O. Box 47, Avenida Ayacucho entre Cap. Manchego y Avaroa, Villamontes - Departemento Tarija (Bolivia, Plurinational State of); Preeker, N. Louise, E-mail: [Department of Environmental Science, Institute for Water and Wetland Research, Radboud University Nijmegen, Heyendaalseweg 135, 6525 AJ Nijmegen (Netherlands); Foundation ' Los Amigos del Pilcomayo' , P.O. Box 47, Avenida Ayacucho entre Cap. Manchego y Avaroa, Villamontes - Departemento Tarija (Bolivia, Plurinational State of); Department of Epidemiology, Biostatistics and HTA, Radboud University Nijmegen Medical Centre, Nijmegen (Netherlands); Ragas, Ad M.J., E-mail: [Department of Environmental Science, Institute for Water and Wetland Research, Radboud University Nijmegen, Heyendaalseweg 135, 6525 AJ Nijmegen (Netherlands); School of Science, Open University, Heerlen (Netherlands); Ven, Max W.P.M. van de, E-mail: [Foundation ' Los Amigos del Pilcomayo' , P.O. Box 47, Avenida Ayacucho entre Cap. Manchego y Avaroa, Villamontes - Departemento Tarija (Bolivia, Plurinational State of); Smolders, Alfons J.P., E-mail: [Foundation ' Los Amigos del Pilcomayo' , P.O. Box 47, Avenida Ayacucho entre Cap. Manchego y Avaroa, Villamontes - Departemento Tarija (Bolivia, Plurinational State of); Department of Aquatic Ecology and Environmental Biology, Institute for Water and Wetland Research, Radboud University Nijmegen (Netherlands); and others


    Background: The Pilcomayo River is polluted by tailings and effluents from upstream mining activities, which contain high levels of metals. The Weenhayek live along this river and are likely to have elevated exposure. Objectives: To assess whether the Weenhayek have increased risk of reproductive and developmental disorders related to elevated metal exposure in comparison with a reference population. Methods: We assessed reproductive and developmental outcomes, i.e. fertility, fetal loss, congenital anomalies, and walking onset by means of structured interviews. We sampled hair, water and fish to assess the relative exposure of the Weenhayek. Samples were analyzed for Pb and Cd with ICP-MS techniques. Results: The Weenhayek communities studied had a higher prevalence of small families (OR 2.7, 95% CI 1.3-6.0) and delayed walking onset (OR 2.7, 95% CI 1.4-5.1) than the reference population. Median Pb levels in Weenhayek hair were 2-5 times higher than in the reference population, while Cd levels were not elevated. In water and fish, both Pb and Cd levels were increased in the Weenhayek area. Conclusions: We found indications for increased risks of small families and delayed walking onset among the Weenhayek living along the Pilcomayo River. Lactants form a high risk group for lead exposure. - Highlights: Black-Right-Pointing-Pointer We assessed selected disorders and metal exposure in two comparable populations. Black-Right-Pointing-Pointer Risks of small families and delayed walking onset were increased in the population with elevated lead levels in hair. Black-Right-Pointing-Pointer The population with increased risks lives along a river with increased lead and cadmium levels in water and fish.

  3. Petroleum geology of the deltaic sequence, Rio Del Rey basin, offshore Cameroon

    Coughlin, R.M.; Bement, W.O.; Maloney, W.V. (Pecten International Company, Houston, TX (United States))


    The Rio Del Rey Basin of offshore Cameroon comprises the easternmost portion of the Niger delta complex. In the delta flank setting, the overall package is thinner and stratigraphic correlation simpler than in the depocenter to the west so the distribution of reservoirs and seals is well defined. Productive reservoirs are shallow, typically less than 2000 m, and mostly hydropressured to slightly overpressured. Reservoir properties generally are excellent and seismic bright-spot technology has played a major role in exploration and development efforts. Rio Del Rey is characterized by three main structural styles from north to south: (1) detachment-based growth faults, (2) highly faulted, mobile shale cored domes and ridges, and (3) toe thrusts and folds. Virtually all individual traps are fault dependent and lack of sufficient internal seals in sand-rich wave-dominated deltaic sequences can limit the objective window. Most fields are downthrown fault traps in which hanging-wall reservoirs are effectively sealed against older prodelta and marine shales. All large oil fields are located in the dome and ridge province and are potential analogs for similar structures now being explored on the upper slope off Nigeria. The best quality source rocks identified thus far are Paleocene to Eocene marine shales. Oil vs. gas distribution in the basin is a function of variations in the kerogen type, organic richness, and maturity of these source rocks. A significant quantity of the gas found to date in Rio Del Rey is biogenic in origin. The Cameroon charge model may aid in better understanding hydrocarbon distribution on offshore Nigeria, where the Miocene deltaic section is much thicker and potential Paleocene-Eocene source rocks likely are unpenetrated. The shallow deltaic play in Cameroon is relatively mature. Future exploration likely will focus on identifying deeper, nonbright-spot-supported opportunities including potential stratigraphic traps.

  4. Existing Opportunities to Adapt the Rio Grande/Bravo Basin Water Resources Allocation Framework

    Luzma Fabiola Nava


    Full Text Available The study of the Rio Grande/Bravo (RGB Basin water allocation demonstrates how the United States (U.S. and Mexico have consolidated a transboundary framework based on water sharing. However, the water supply no longer meets the ever-increasing demand for water or the expectations of different stakeholders. This paper explores opportunities for an enhanced management regime that will address past problems and better examine how to balance demands for a precious resource and environmental needs. Based on an overview of the RGB Basin context and the water allocation framework, as well as a discussion on stakeholders’ ability to achieve solutions, this paper explores three key questions: (1 Does the current binational water allocation framework meet current and future human and environmental needs? (2 How can the U.S.-Mexico water allocation framework be adapted to balance social and environmental water demands so it can support and preserve the RGB Basin ecosystem? (3 What are the main opportunities to be explored for expanding the U.S.-Mexico water resources allocation framework? The U.S.-Mexico water resources framework is subject to broad interpretation and may be adapted to the circumstances taking the fullest advantage of its flexibility. Policy recommendations highlight the existing flexibility of the binational framework, the potential to move forward with an ad hoc institutional arrangement, and the creation of political will to achieve change through stakeholders recommendations.

  5. A Physical Assessment of the Opportunities for Improved Management of the Water Resources of the Bi-National Rio Grande/Rio Bravo Basin

    Aparicio, J.; McKinney, D.; Valdes, J.; Guitron, A.; Thomas, G.


    The hydro-physical opportunities for expanding the beneficial uses of the fixed water supply in the Rio Grande/Bravo Basin to better satisfy an array of water management goals are examined. These include making agriculture more resilient to periodic conditions of drought, improving the reliability of supplies to cities and towns, and restoring lost environmental functions in the river system. This is a comprehensive, outcome-neutral, model- based planning exercise performed by some 20 technical, primarily non-governmental institutions from both countries, aimed at proposing strategies that can reduce future conflicts over water throughout the entire basin. The second track consists in generating a set of future water management scenarios that respond to the needs and objectives of the basin stakeholders in each segment and each country. An array of scenarios for improved water management has been developed for the lower Rio Grande/Rio Bravo basin in Texas and the Mexican state of Tamaulipas. Another set under development will focus on the Rio Conchos and the El Paso/Juarez region. Eventually, scenarios will be generated such that will comprehend the entire basin on both sides of the border. These scenarios are the product of consultations with agricultural water districts, governmental organizations and environmental NGOs. They include strategies for reducing the physical losses of water in the system, conservation transfers, improvements in the operations of the Mexican and international reservoirs, improvements in environmental flow conditions, improvements in reliability of water supplies, and drought coping strategies.These scenarios will be evaluated for hydrologic feasibility by the basin-wide model and the gaming exercises. Modeling is necessary to understand how these options will affect the entire system and how they can be crafted to maximize the benefits and avoid unintended or uncompensated effects. The scenarios that have the potential to provide large

  6. Two new species of the Hypostomus cochliodon group (Siluriformes: Loricariidae from the rio Negro basin in Brazil

    Pedro Hollanda Carvalho

    Full Text Available Two new species of Hypostomus are described from the middle and upper rio Negro in Brazil. They are assigned to the Hypostomus cochliodon group (sensu Armbruster, 2003 by possessing few spoon-shaped teeth, and dentary angle averaging less than 80º. Hypostomus kopeyaka is described from the rio Tiquié, a tributary of the rio Uaupés, upper rio Negro basin, presents a unique color pattern among the Hypostomus species belonging to the Hypostomus cochliodon group, consisting of conspicuously horizontally elongated, closely-set black spots over the entire dorsal and lateral surfaces of the body. Hypostomus weberi is described from the middle rio Negro and can be distinguished from all remaining Hypostomus species belonging to the Hypostomus cochliodon group by possessing a unique color pattern consisting in large, rounded, widelyspaced black spots over body and fins.

  7. A new species of Hemigrammus Gill, 1858 (Characiformes: Characidae from the rio Madeira and rio Paraguai basins, with a redescription of H. lunatus

    Rafaela P. Ota

    Full Text Available A new Hemigrammusis described from the rio Paraguai and rio Madeira basins, Mato Grosso and Rondônia States, Brazil. The new species is characterized by possessing a wide dark horizontal stripe across the eye, a vertically elongated humeral blotch, and 4-5 gill-rakers on upper branch and 9-10 on lower. The new species can be easily diagnosed from H. lunatus, the sympatric and morphologically most similar congener, by the shape of humeral blotch and the number of gill rakers. Data of the type material of both Hemigrammus lunatus and H. maxillaris, as well as extensive examination of specimens, allowed us to conclude that H. maxillarisis a junior subjective synonym of H. lunatus. A redescription of H. lunatus, as well as a formal restriction of its type locality, is provided. A putative monophyletic group within Hemigrammus, composed by H. barrigonae, Hemigrammus lunatus, H. machadoi new species, and H. ulreyi, named Hemigrammus lunatus group, is proposed based on overall body morphology and color pattern. Additionally, a discussion on the biogeographical relationships between the rio Paraguai and rio Guaporé basins is provided.

  8. A new species of Moenkhausia Eigenmann (Characiformes: Characidae from the rio Xingu basin, Brazil

    Manoela M. F. Marinho

    Full Text Available A new species of Moenkhausia from the upper rio Xingu basin is described. Moenkhausia eurystaenia is distinguished from all congeners, except M. heikoi and M. phaeonota, by the presence of a dark, broad longitudinal stripe from the opercle to the end of caudal peduncle. The new species is distinguished from M. heikoi mainly by having 18-21 branched anal-fin rays (vs. 24-26 and the absence of a round blotch at the end of the caudal peduncle (vs. present. Moenkhausia eurystaenia can be distinguished from M. phaeonota mainly by the anterior portion of longitudinal band darker at horizontal septum (vs. darker below horizontal septum, the deep dark pigmentation along horizontal septum extending anteriorly up to humeral region (vs. extending up to vertical through pelvic-fin origin, number of vertebrae 34 (vs. 36-37, and others additional measurements.

  9. Mammal assemblage of the agroecosystem constituents of the Várzea River Basin, Rio Grande do Sul, Brazil

    Felipe Bortolotto Peters


    Full Text Available We provide recent information on the richness of mammals along the agroecosystems of the Rio da Várzea Basin, Rio Grande do Sul, Brazil. We used different field techniques to confirm the occurrence of 46 mammal species in this area. Nine species are threatened in at least one of the three “red lists” at state, national and global levels. Adding the up-to-date results obtained in the field to available data, mainly for conservation units, we present a richness of 85 species recorded for the basin. This number represents about 50% of mammals documented for Rio Grande do Sul state. The results suggest the importance of maintaining protected areas in altered regions, confirming the relevance of inventories of local fauna as a first approach to specific studies addressed to distribution, systematics, cytogenetics, physiology, population and community ecology.

  10. Factors affecting Hg (II adsorption in soils from the Rio Negro basin (Amazon

    Patricia Miretzky


    Full Text Available Mercury (II adsorption studies in top soils (top 10 cm from the Rio Negro basin show this process depends strongly on some selected parameters of the aqueous phase in contact with the soils. Maximum adsorption occurred in the pH range 3.0-5.0 (>90%. Dissolved organic matter shows an inhibitory effect on the availability of Hg (II to be adsorbed by the soils, whereas a higher chloride content of the solution resulted in a lower adsorption of Hg (II at pH 5.0. Soils with higher organic matter content were less affected by changes in the salinity. An increase in the initial Hg (II concentration increased the amount of Hg (II adsorbed by the soil and decreased the time needed to reach equilibrium. A Freundlich isotherm provided a good model for Hg (II adsorption in the two types of soil studied. The kinetics of Hg (II adsorption on Amazonian soils showed to be very fast and followed pseudo-second order kinetics. An environmental implication of these results is discussed under the real scenario present in the Negro River basin, where acidic waters are in contact with a soil naturally rich in mercury.

  11. Consumptive Water Use Analysis of Upper Rio Grande Basin in Southern Colorado.

    Dubinsky, Jonathan; Karunanithi, Arunprakash T


    Water resource management and governance at the river basin scale is critical for the sustainable development of rural agrarian regions in the West. This research applies a consumptive water use analysis, inspired by the Water Footprint methodology, to the Upper Rio Grande Basin (RGB) in south central Colorado. The region is characterized by water stress, high dessert conditions, declining land health, and a depleting water table. We utilize region specific data and models to analyze the consumptive water use of RGB. The study reveals that, on an average, RGB experiences three months of water shortage per year due to the unsustainable extraction of groundwater (GW). Our results show that agriculture accounts for 77% of overall water consumption and it relies heavily on an aquifer (about 50% of agricultural consumption) that is being depleted over time. We find that, even though potato cultivation provides the most efficient conversion of groundwater resources into economic value (m(3) GW/$) in this region, it relies predominantly (81%) on the aquifer for its water supply. However, cattle, another important agricultural commodity produced in the region, provides good economic value but also relies significantly less on the aquifer (30%) for water needs. The results from this paper are timely to the RGB community, which is currently in the process of developing strategies for sustainable water management.

  12. Evaluating the State of Water Management in the Rio Grande/Bravo Basin

    Ortiz Partida, Jose Pablo; Sandoval-Solis, Samuel; Diaz Gomez, Romina


    Water resource modeling tools have been developed for many different regions and sub-basins of the Rio Grande/Bravo (RGB). Each of these tools has specific objectives, whether it is to explore drought mitigation alternatives, conflict resolution, climate change evaluation, tradeoff and economic synergies, water allocation, reservoir operations, or collaborative planning. However, there has not been an effort to integrate different available tools, or to link models developed for specific reaches into a more holistic watershed decision-support tool. This project outlines promising next steps to meet long-term goals of improved decision support tools and modeling. We identify, describe, and synthesize water resources management practices in the RGB basin and available water resources models and decision support tools that represent the RGB and the distribution of water for human and environmental uses. The extent body of water resources modeling is examined from a perspective of environmental water needs and water resources management and thereby allows subsequent prioritization of future research and monitoring needs for the development of river system modeling tools. This work communicates the state of the RGB science to diverse stakeholders, researchers, and decision-makers. The products of this project represent a planning tool to support an integrated water resources management framework to maximize economic and social welfare without compromising vital ecosystems.

  13. Biodiversity and community structure of zooplankton in the Sub-basin of Rio Poxim, Sergipe, Brazil

    Eliane Maria de Souza Nogueira


    Full Text Available The zooplankton of aquatic environments is composed mostly of protozoans, rotifers, cladocerans and copepods, which play an important role in the food chain, transferring mass and energy from primary producers to higher trophic levels. This work was prepared with the objective of contributing to the knowledge of zooplankton biodiversity that occurs in the Sub-basin of Rio Poxim. Water samples were taken at monthly intervals at four sampling stations located along the sub-basin in the period August 2009 to July 2010. To obtain the zooplankton community, 100 L of water were filtered on nylon net with an aperture of 50 mm. Were identified 72 taxa distributed in the following taxonomic categories Rotifera, Protozoa, Porifera, Nematoda, Anellida, Cladocera, Copepoda, Ostracoda, Isopoda and Insecta. In terms of species richness, the phylum Rotifera followed by the Protoctista were the most relevant with forty and fifteen taxa, respectively. The most representative taxa in numerical terms were Arcella vulgaris, Notholca sp. Rotary sp. and nematodes. Regarding the community diversity index, the community was characterized as low diversity, but the taxa were distributed evenly in all monitoring points.

  14. Gravity and Seismic Investigations of the Santo Domingo Basin, Rio Grande Rift, New Mexico

    Braile, L. W.; Ferguson, J. F.; Boucher, C.; Novitsky, C. G.; O'Shea, P. M.; Daves, J.; Marzen, R.; Mendoza, K.; Rasmussen, T.; Wei, W.; Baldridge, W. S.; Biehler, S.; Claytor, J. M.; Bischoff, S. H.; Ranasinghe, N. R.; Corredor, A.


    The SAGE (Summer of Applied Geophysical Experience) program collected new gravity, seismic, electromagnetic and down-hole temperature data in 2014 in the Santo Domingo Basin and adjacent areas of the Rio Grande Rift (RGR) area of northern New Mexico. The SAGE 2014 data collection was part of an integrated geophysical study of the area initiated in 2010 and adds data and interpretations to a W to E transect of the RGR. The transect includes previous SAGE seismic refraction and CMP reflection profiles recorded in 2010 and 2011, some industry seismic reflection data, and detailed gravity observations. Seismic data consisted of a 4.8 km NW to SE profile (120 three-component stations in four overlapping deployments, 20 m station spacing, using a Vibroseis source - 20 m spacing for reflection VPs; 800 m spacing for refraction VPs) along the Borrego Canyon road with both refraction and CMP reflection coverage. About 50,000 seismograms were recorded. The surface conditions (dry unconsolidated sediments) increased surface wave energy and limited the signal-to-noise level of reflection arrivals although some wide-angle reflections with two-way times as great as 1.8 s were visible. The refraction data were modeled with first arrival travel time methods and mainly helped identify the velocity and minimum thickness of the Tertiary Santa Fe group sedimentary rocks in the Santo Domingo Basin. Interpretation of the seismic and gravity data along the transect was aided by refraction velocities, the existence of a nearby regional seismic reflection profile from industry, and lithologies and well-logs from a deep well. Gravity modeling, with significant control on depths of interfaces and densities from the seismic and drill hole data, indicates that the Santo Domingo sedimentary basin has a total depth of about 6 km.

  15. Seismic and Gravity Investigations of the Western Espanola Basin, Rio Grande Rift, New Mexico

    Braile, L. W.; Coldren, B. G.; Baca, A.; Fontana, J.; Olheiser, M.; Ziff, M.; Keske, A.; Rhode, A.; Martin-Short, R.; Allen, W.; Denton, K. M.; Harper, C.; Baldridge, W.; Biehler, S.; Ferguson, J. F.; McPhee, D.; Snelson, C. M.


    The SAGE (Summer of Applied Geophysical Experience) program collected new seismic, gravity, electromagnetic and down-hole temperature data in 2013 in the western Espanola basin of the Rio Grande rift area of northern New Mexico. The location, about 25 km NW of Santa Fe, has been identified as a potential geothermal resources area based on relatively high temperature gradients in drill holes. The SAGE 2013 data collection was part of an integrated geophysical study of the area initiated in 2011. Seismic data consisted of a 4.8 km W to E profile (120 three-component stations in four overlapping deployments, 20 m station spacing, using a Vibroseis source - 20 m spacing for reflection VPs; 800 m spacing for refraction VPs) with both refraction and CMP reflection coverage. About 55,000 seismograms were recorded. The surface conditions (dry unconsolidated sediments) increased surface wave energy and limited the signal-to-noise level of the refraction and reflection arrivals. Utilizing longer source-receiver offsets improved the shot-gather record sections by emphasizing wider angle reflections which are very strong and coherent. The refraction data were modeled with first arrival travel time methods. The reflection data were processed to produce a CMP stacked record section. Strong reflectors from basin-filling sedimentary rocks (mostly Tertiary in age) are visible above reflections from a thin section of Paleozoic rocks and the basement. The lower reflections have an apparent dip to the west of about 12 degrees. Eighty-one new gravity measurements (detailed data at 200 m spacing along the seismic profile, and regional stations) were collected and combined with existing regional data for modeling. Interpretation of the seismic and gravity data was aided by refraction velocities, the existence of a nearby regional seismic reflection profile from industry, and lithologies and well-logs from a deep well. The sedimentary basin interpreted from the seismic and gravity data

  16. Implementation of MAR within the Rio Grande Basin of Central New Mexico, USA

    Marley, Robert; Blandford, T. Neil; Ewing, Amy; Webb, Larry; Yuhas, Katherine


    The U.S. Bureau of Reclamation has identified the Rio Grande basin within Central New Mexico as one of several regions where water supplies are over-allocated and future conflicts over the inadequate resource are highly likely. Local water providers have consistently identified managed aquifer recharge (MAR) as an important tool to provide conjunctive management of surface-water, groundwater, and reclaimed water sources in order to extend the useful life of existing water sources. However, MAR projects have been slow to take root partly due to rigorous demonstration requirements, groundwater quality protection concerns, and ongoing water right uncertainties. At first glance the several thousand meters of unconsolidated basin-fill sediments hosting the regional aquifer appear to provide an ideal environment for the subsurface storage of surplus water. However, the basin has a complex structural and depositional history that impacts the siting and overall effectiveness of MAR systems. Several recharge projects are now in various stages of implementation and are overcoming site specific challenges including source water and ambient groundwater compatibility, low-permeability sediments and compartmentalization of the aquifer by extensive faulting, well clogging, and overall water quality management. This presentation will highlight ongoing efforts of these water providers to develop full-scale recharge facilities. The performance of natural in-channel infiltration, engineered infiltration galleries, and direct injection systems designed to introduce from 500 to 5,000 mega-liters per annum to target intervals present from 150 to 600 meters below ground surface will be described. Source waters for recharge operations include inter-basin transferred surface water and highly treated reclaimed water sources requiring from minor to extensive treatment pre-recharge and post-recovery. Operational complexities have raised concerns related to long-term operation and maintenance

  17. Wrapped in flames: Corydoras hephaestus, a new remarkably colored species from the Rio Madeira basin (Teleostei: Callichthyidae).

    Ohara, Willian Massaharu; Tencatt, Luiz F C; Britto, Marcelo R


    A new species of Corydoras is described from the upper Rio Machado, Rio Madeira basin, Rondônia State, Brazil. The new species can be distinguished from its congeners by the absence of contact between the posterior process of the parieto-supraoccipital and the nuchal plate; a ventral laminar expansion of the infraorbital 1 conspicuously developed; and the posterior margin of the pectoral-fin spine with serrations along almost of its entire length, only lacking in the distal portion. Additionally, Corydoras hephaestus possesses dorsal and pectoral spines short, and exhibits an unusual color pattern in life. The conservation status of the new species and other endemic species are briefly commented.

  18. Hyphessobrycon petricolus, a new species of tetra (Characiformes: Characidae) from the rio Madeira basin, Mato Grosso, Brazil.

    Ohara, Willian M; Lima, Flávio C T; Barros, Bruno S


    A new species of Hyphessobrycon is described from the rio Roosevelt, rio Madeira basin, Mato Grosso State, Brazil. Hyphessobrycon petricolus sp. n. can be distinguished from its congeners by the unique combination of the following features: a well-defined, relatively narrow dark midlateral stripe on body extending from immediately behind posterior margin of opercle to the middle caudal-fin rays, relatively conspicuous humeral blotch, and 16-20 branched anal-fin rays. Comments on the remaining Hyphessobrycon species presenting a conspicuous dark midlateral stripe are presented.

  19. Crenicichla chicha, a new species of pike cichlid (Teleostei: Cichlidae from the rio Papagaio, upper rio Tapajós basin, Mato Grosso, Brazil

    Henrique R. Varella

    Full Text Available Crenicichla chicha, new species, occurs in clear, fast-running waters with rocky substrates in the rio Papagaio and tributaries. It is distinguished from all other Crenicichla species by the combination of two character states: infraorbitals 3 and 4 co-ossified (vs. separated and 66-75 scales in the row immediately above to that containing the lower lateral line (E1 row scales. Crenicichla chicha shares a smooth preopercular margin, co-ossification of infraorbitals 3 and 4, and some color features with C. hemera from the adjacent rio Aripuanã drainage, rio Madeira basin. It differs from Crenicichla hemera in more E1 scales (66-75 vs. 58-65 and presence of a conspicuous black narrow stripe running from infraorbital 3 obliquely caudoventrad toward the preopercular margin vs. a rounded and faint suborbital marking present on infraorbitals 3-4. Examination of the type series and additional material from the rio Aripuanã confirms that Crenicichla guentheri Ploeg, 1991 is a junior subjective synonym of C. hemera Kullander, 1990.

  20. AMS-{sup 14}C measurements for the carbonate platform of the offshore Campos Basin, Rio de Janeiro State, Brazil

    Coimbra, Melayne M. E-mail:; Barbosa, Catia F.; Soares-Gomes, Abilio; Silva, Cleverson G.; Rios-Netto, Aristoteles; Mueller, Ken A


    As part of our accelerator mass spectrometry (AMS) program in Brazil we prepared and measured some red algae carbonate crust samples from Campos Basin, Rio de Janeiro, Brazil. The measurements were performed at Purdue Rare Isotope Measurement Laboratory (PRIME Lab), Purdue University, IN, USA. This carbonate material is interlaminated with foraminiferal lime mud reflecting recurrent intervals of carbonate development, which might be linked to outer-shelf oceanographic circulation.

  1. Endocrine disruptors in water filters used in the Rio dos Sinos Basin region, Southern Brazil.

    Furtado, C M; von Mühlen, C


    The activated carbon filter is used in residences as another step in the treatment of drinking water, based on a physical-chemical process to absorb pollutants that are not removed in conventional treatment. Endocrine disruptors (EDCs) are exogenous substances or mixtures of substances that acts on the endocrine system similarly to the endogenously produced hormones, triggering malfunctions and harmful changes to human and animal health. The objective of the present work was to study EDCs through semi-quantitative analysis of residential water filters collected in the region of Rio dos Sinos basin, focusing on two specific classes: hormones and phenols. The solid phase extraction principle was used for the extraction of compounds and gas chromatography coupled with mass spectrometry for the separation and characterization of EDCs. Four samples of residential filters collected from public water distribution and artesian wells, from the cities of Novo Hamburgo and São Leopoldo were analysed. Using the developed methodology, it was possible to detect and comparatively quantify selected EDCs in all studied samples, which indicates the presence of these contaminants in drinking water from different sources.

  2. Hydrochemical tracers in the middle Rio Grande Basin, USA: 1. Conceptualization of groundwater flow

    Plummer, L. Niel; Bexfield, Laura M.; Anderholm, Scott K.; Sanford, Ward E.; Busenberg, Eurybiades

    Chemical and isotopic data for groundwater from throughout the Middle Rio Grande Basin, central New Mexico, USA, were used to identify and map groundwater flow from 12 sources of water to the basin, evaluate radiocarbon ages, and refine the conceptual model of the Santa Fe Group aquifer system. Hydrochemical zones, representing groundwater flow over thousands to tens of thousands of years, can be traced over large distances through the primarily siliciclastic aquifer system. The locations of the hydrochemical zones mostly reflect the ``modern'' predevelopment hydraulic-head distribution, but are inconsistent with a trough in predevelopment water levels in the west-central part of the basin, indicating that this trough is a transient rather than a long-term feature of the aquifer system. Radiocarbon ages adjusted for geochemical reactions, mixing, and evapotranspiration/dilution processes in the aquifer system were nearly identical to the unadjusted radiocarbon ages, and ranged from modern to more than 30 ka. Age gradients from piezometer nests ranged from 0.1 to 2 year cm-1 and indicate a recharge rate of about 3 cm year-1 for recharge along the eastern mountain front and infiltration from the Rio Grande near Albuquerque. There has been appreciably less recharge along the eastern mountain front north and south of Albuquerque. Des données sur les éléments chimiques et les isotopes présents dans l'eau souterraine prélevée à divers endroits dans le bassin moyen du Rio Grande, au centre du Nouveau-Mexique (É-U), ont permis de déterminer l'existence et l'étendue de douze sources d'eau régionales dans le bassin, d'évaluer les âges radiocarbones et de raffiner le modèle conceptuel du système aquifère du groupe de Santa Fe. Des zones hydro-chimiques qui représentent l'écoulement de l'eau souterraine depuis des dizaines de milliers d'années peuvent être suivies sur de longues distances à travers l'aquifère principalement siliclastique. La position des

  3. Significant Cenozoic faulting, east margin of the Española Basin, Rio Grande rift, New Mexico

    Vernon, James H.; Riecker, Robert E.


    Tectonic interpretation of the east margin of the Española Basin, Rio Grande rift, New Mexico, has been controversial. Previous authors have disagreed as to whether significant faulting defines the boundary between the basin and the Sangre de Cristo Mountains. A more recent geophysical basin transect that suggests no significant faulting and held observation of faceted spurs along the western Sangre de Cristo Mountain front indicating a faulted margin motivate our study. The east margin of the Española Basin for about 37 km north of Santa Fe, New Mexico, is marked by a complex array of significant, late Cenozoic high-angle faults. Locally, three parallel, north-trending, high-angle faults cut Precambrian basement and Tertiary basin-fill rocks along the basin margin. Elsewhere along the margin, tilted fault blocks and intersecting faults occur. Fault area, fault attitude with depth, magnitude of fault motion, and timing of fault motion remain uncertain. However, faults studied in detail are 1-2 km long, have minimum dip-slip motion of 33-100 m, and underwent movement during the late Cenozoic. Potentially significant tectonic and seismic hazard implications arise from the possibility of post-150 ka fault motion.

  4. Data collection for cooperative water resources modeling in the Lower Rio Grande Basin, Fort Quitman to the Gulf of Mexico.

    Passell, Howard David; Pallachula, Kiran (GRAM, Inc., Albuquerque, NM); Tidwell, Vincent Carroll; Villalobos, Joshua (Texas A& M University); Piccinni, Giovanni (Texas A& M University); Brainard, James Robert; Gerik, Thomas (Texas A& M University); Morrison, Wendy (Texas A& M University); Serrat-Capdevila, Aleix (University of Arizona); Valdes, Juan (University of Arizona); Sheng, Zhuping (Texas A& M University); Lovato, Rene (Instituto Mexicano de Tecnologia del Agua); Guitron, Alberto (Instituto Mexicano de Tecnologia del Agua); Ennis, Martha Lee; Aparicio, Javier (Instituto Mexicano de Tecnologia del Agua); Newman, Gretchen Carr (GRAM, Inc., Albuquerque, NM); Michelsen, Ari M. (Texas A& M University)


    Water resource scarcity around the world is driving the need for the development of simulation models that can assist in water resources management. Transboundary water resources are receiving special attention because of the potential for conflict over scarce shared water resources. The Rio Grande/Rio Bravo along the U.S./Mexican border is an example of a scarce, transboundary water resource over which conflict has already begun. The data collection and modeling effort described in this report aims at developing methods for international collaboration, data collection, data integration and modeling for simulating geographically large and diverse international watersheds, with a special focus on the Rio Grande/Rio Bravo. This report describes the basin, and the data collected. This data collection effort was spatially aggregated across five reaches consisting of Fort Quitman to Presidio, the Rio Conchos, Presidio to Amistad Dam, Amistad Dam to Falcon Dam, and Falcon Dam to the Gulf of Mexico. This report represents a nine-month effort made in FY04, during which time the model was not completed.

  5. A Conceptual Framework for SAHRA Integrated Multi-resolution Modeling in the Rio Grande Basin

    Liu, Y.; Gupta, H.; Springer, E.; Wagener, T.; Brookshire, D.; Duffy, C.


    The sustainable management of water resources in a river basin requires an integrated analysis of the social, economic, environmental and institutional dimensions of the problem. Numerical models are commonly used for integration of these dimensions and for communication of the analysis results to stakeholders and policy makers. The National Science Foundation Science and Technology Center for Sustainability of semi-Arid Hydrology and Riparian Areas (SAHRA) has been developing integrated multi-resolution models to assess impacts of climate variability and land use change on water resources in the Rio Grande Basin. These models not only couple natural systems such as surface and ground waters, but will also include engineering, economic and social components that may be involved in water resources decision-making processes. This presentation will describe the conceptual framework being developed by SAHRA to guide and focus the multiple modeling efforts and to assist the modeling team in planning, data collection and interpretation, communication, evaluation, etc. One of the major components of this conceptual framework is a Conceptual Site Model (CSM), which describes the basin and its environment based on existing knowledge and identifies what additional information must be collected to develop technically sound models at various resolutions. The initial CSM is based on analyses of basin profile information that has been collected, including a physical profile (e.g., topographic and vegetative features), a man-made facility profile (e.g., dams, diversions, and pumping stations), and a land use and ecological profile (e.g., demographics, natural habitats, and endangered species). Based on the initial CSM, a Conceptual Physical Model (CPM) is developed to guide and evaluate the selection of a model code (or numerical model) for each resolution to conduct simulations and predictions. A CPM identifies, conceptually, all the physical processes and engineering and socio

  6. A new species of Moenkhausia Eigenmann (Characiformes: Characidae from the rio Xingu basin, Brazil

    Manoela M. F. Marinho


    Full Text Available A new species of Moenkhausia from the upper rio Xingu basin is described. Moenkhausia eurystaenia is distinguished from all congeners, except M. heikoi and M. phaeonota, by the presence of a dark, broad longitudinal stripe from the opercle to the end of caudal peduncle. The new species is distinguished from M. heikoi mainly by having 18-21 branched anal-fin rays (vs. 24-26 and the absence of a round blotch at the end of the caudal peduncle (vs. present. Moenkhausia eurystaenia can be distinguished from M. phaeonota mainly by the anterior portion of longitudinal band darker at horizontal septum (vs. darker below horizontal septum, the deep dark pigmentation along horizontal septum extending anteriorly up to humeral region (vs. extending up to vertical through pelvic-fin origin, number of vertebrae 34 (vs. 36-37, and others additional measurements.Uma espécie nova de Moenkhausia da bacia do alto rio Xingu é descrita. Moenkhausia eurystaenia distingue-se de todas as congêneres, exceto M. heikoi e M. phaeonota, pela presença de uma faixa longitudinal larga e escura que se estende do opérculo ao pedúnculo caudal. A espécie nova distingue-se de Moenkhausia heikoi principalmente por apresentar 18-21 raios ramificados na nadadeira anal (vs. 24-26, e ausência de uma mácula circular no final do pedúnculo caudal (vs. presença. Moenkhausia eurystaenia distingue-se de M. phaeonota principalmente pela porção anterior da faixa longitudinal ser mais escura no septo horizontal (vs. mais escura abaixo do septo horizontal, pigmentação profunda e escura ao longo do septo horizontal se estendendo até a região umeral (vs. se estendendo até a vertical que passa pela origem da nadadeira pélvica, 34 vértebras (vs. 36-37, e outras medidas adicionais.

  7. A multi-tracer approach to delineate groundwater dynamics in the Rio Actopan Basin, Veracruz State, Mexico

    Pérez Quezadas, Juan; Heilweil, Victor M.; Cortés Silva, Alejandra; Araguas, Luis; Salas Ortega, María del Rocío


    Geochemistry and environmental tracers were used to understand groundwater resources, recharge processes, and potential sources of contamination in the Rio Actopan Basin, Veracruz State, Mexico. Total dissolved solids are lower in wells and springs located in the basin uplands compared with those closer to the coast, likely associated with rock/water interaction. Geochemical results also indicate some saltwater intrusion near the coast and increased nitrate near urban centers. Stable isotopes show that precipitation is the source of recharge to the groundwater system. Interestingly, some high-elevation springs are more isotopically enriched than average annual precipitation at higher elevations, indicating preferential recharge during the drier but cooler winter months when evapotranspiration is reduced. In contrast, groundwater below 1,200 m elevation is more isotopically depleted than average precipitation, indicating recharge occurring at much higher elevation than the sampling site. Relatively cool recharge temperatures, derived from noble gas measurements at four sites (11-20 °C), also suggest higher elevation recharge. Environmental tracers indicate that groundwater residence time in the basin ranges from 12,000 years to modern. While this large range shows varying groundwater flowpaths and travel times, ages using different tracer methods (14C, 3H/3He, CFCs) were generally consistent. Comparing multiple tracers such as CFC-12 with CFC-113 indicates piston-flow to some discharge points, yet binary mixing of young and older groundwater at other points. In summary, groundwater within the Rio Actopan Basin watershed is relatively young (Holocene) and the majority of recharge occurs in the basin uplands and moves towards the coast.

  8. A multi-tracer approach to delineate groundwater dynamics in the Rio Actopan Basin, Veracruz State, Mexico

    Pérez Quezadas, Juan; Heilweil, Victor M.; Cortés Silva, Alejandra; Araguas, Luis; Salas Ortega, María del Rocío


    Geochemistry and environmental tracers were used to understand groundwater resources, recharge processes, and potential sources of contamination in the Rio Actopan Basin, Veracruz State, Mexico. Total dissolved solids are lower in wells and springs located in the basin uplands compared with those closer to the coast, likely associated with rock/water interaction. Geochemical results also indicate some saltwater intrusion near the coast and increased nitrate near urban centers. Stable isotopes show that precipitation is the source of recharge to the groundwater system. Interestingly, some high-elevation springs are more isotopically enriched than average annual precipitation at higher elevations, indicating preferential recharge during the drier but cooler winter months when evapotranspiration is reduced. In contrast, groundwater below 1,200 m elevation is more isotopically depleted than average precipitation, indicating recharge occurring at much higher elevation than the sampling site. Relatively cool recharge temperatures, derived from noble gas measurements at four sites (11-20 °C), also suggest higher elevation recharge. Environmental tracers indicate that groundwater residence time in the basin ranges from 12,000 years to modern. While this large range shows varying groundwater flowpaths and travel times, ages using different tracer methods (14C, 3H/3He, CFCs) were generally consistent. Comparing multiple tracers such as CFC-12 with CFC-113 indicates piston-flow to some discharge points, yet binary mixing of young and older groundwater at other points. In summary, groundwater within the Rio Actopan Basin watershed is relatively young (Holocene) and the majority of recharge occurs in the basin uplands and moves towards the coast.

  9. Quantifying Salinization of the Upper-Middle Rio Grande Using a Basin-Scale Water and Chloride Mass Balance Model

    Mills, S. K.; Phillips, F. M.; Hogan, J. F.; Hendrickx, J. M.


    The Rio Grande is clearly undergoing salinization, manifested by a 50-fold increase in total dissolved solids content between its headwaters in Colorado and the U.S.-Mexico border. To elucidate the causes of this salinization, we conducted an eight-day synoptic sampling campaign in August 2001. This sampling included the river, its major tributaries, and major irrigation drain inflows. Along 1200 km between the river headwaters in Colorado and Fort Quitman, Texas, we collected 110 water samples with an average interval of ~10 km between sampling locales. In the laboratory, samples were analyzed for major constituents including chloride, as well as for bromide and the 36Cl/Cl ratio. Isotopic fingerprinting using the 36Cl/Cl ratio indicates that meteoric waters and deep sedimentary brines respectively account for most of the water and most of the salt inflow to the Rio Grande. The meteoric end member has a 36Cl/Cl ratio of 1100 and a Cl/Br ratio of 30; the brine end member has a 36Cl/Cl ratio of 35 and a Cl/Br ratio of 1150. Using these end member chemistries with USGS stream flow gauging data, we constructed a water- and salt- instantaneous mass balance model of the Rio Grande for the eight-day sampling interval. This model indicates that most water losses from the Rio Grande are due to evaporation from Elephant Butte reservoir, open water evaporation from irrigation ditches, and evapotranspiration of riparian and ditch-bank vegetation. The model also emphasizes the significance of salt input due to deep brine discharge to the river, particularly at the downstream ends of local sedimentary basins of the Rio Grande rift. The Rio Grande receives a smaller amount of salt from saline drains near El Paso, which may be acquiring salt from deep brine discharge as they cross over faults or other structural fluid conduits.

  10. A new species of Moenkhausia Eigenmann (Characiformes: Characidae) from the upper rio Juruena basin, Central Brazil.

    Dagosta, Fernando C P; Marinho, Manoela M F; Benine, Ricardo C


    Moenkhausia lineomaculata, new species, is described herein from the upper rio Juruena, upper rio Tapajós basin. The new species seems to be part of a monophyletic group formed by M. cosmops, M. cotinho, M. diktyota, M. forestii, M. oligolepis, M. sanctaefilomenae, and M. pyrophthalma, the Moenkhausia oligolepis/M. sanctaefilomenae complex, by sharing a reticulated color pattern on body and the presence of a light area preceding a wide, dark caudal-peduncle blotch. The new species is distinguished from these species, except M. cotinho, by the presence of longitudinal series of dark dots on body, and from M. cotinho by the humeral blotch evenly pigmented along its length and by having the dark line along horizontal septum starting approximately at the vertical through dorsal-fin origin. The new species presents intraspecific variation in lateral-line scales perforation, a feature often present in species of the aforementioned group.

  11. Palaeobotanical evidence of wildfires in the Late Palaeozoic of South America - Early Permian, Rio Bonito Formation, Paraná Basin, Rio Grande do Sul, Brazil

    Jasper, André; Uhl, Dieter; Guerra-Sommer, Margot; Mosbrugger, Volker


    Fossil charcoal, as direct evidence of palaeowildfires, has repeatedly been reported from several plant-bearing deposits from the Late Palaeozoic of the Northern Hemisphere. In contrast charcoal reports from the Late Palaeozoic deposits of the Southern Hemisphere are relatively rare in comparison to the Northern Hemisphere. Although the presence of pyrogenic coal macerals has repeatedly been reported from Late Palaeozoic coals from South America, no detailed anatomical investigations of such material have been published so far. Here is presented an anatomical analysis of charcoal originating from Early Permian sediments of the Quitéria Outcrop, Rio Bonito Formation, Paraná Basin, located in the central-eastern portion of Rio Grande do Sul, Brazil. This charcoal comes from two different coaly facies, and it was possible to scrutinize between three types, based on anatomical characters of the charcoal. Two of these charcoal types can be correlated to gymnosperm woods, and the other type corresponds to strongly permineralized bark with characteristic features of lycopsids. The presence of charcoal in different facies, ranging from parautochtonous to allochtonous origin, indicates that different vegetation types, i.e. plants which grew under wet conditions in the lowland as well as in the more dry hinterland, have experienced wildfires. Taking into account previous petrographic and lithological analyses from the facies in which the charcoal occurs and from the conditions of the wood and bark fragments, it was possible to speculate that the intensity of such wildfires most probably corresponds to forest-crown fires. Moreover, it is possible to state that wildfires have been a more or less common element in distinct Late Palaeozoic terrestrial ecosystems in the South American part of Gondwana. The data support previous assumptions on the occurrence of wildfires in the Early Permian of the Paraná Basin which were based solely on coal-petrographic data.

  12. Deep structure of the northern Rio Grande rift beneath the San Luis basin (Colorado) from a seismic reflection survey: implications for rift evolution

    Tandon, Kush; Brown, Larry; Hearn, Thomas


    A seismic reflection survey by Chevron across the San Luis basin (northern Rio Grande rift) and San Juan volcanic field of southern Colorado is reprocessed with extended correlation to search for basement structure. The trace of the main bounding fault of the basin, a high-angle normal fault against the Sangre de Cristo Range, can be correlated to a wide zone of dipping reflection fabric and soles out at lower crustal depths (26-28 km). The deeper reflection fabric represent either broad extensional strain or pre-existing structure, such as a Laramide thrust system. The Sangre de Cristo bounding fault in San Luis basin does not sole out at mid-crustal depths but continues into the lower crust with a shallower dip. The basin architecture in the northern Rio Grande rift (San Luis basin) provides little if any evidence that the Sangre de Cristo bounding fault should flatten in a shallow listric fashion. This fault geometry is quite similar to the high-angle bounding fault in the Espanola basin but contrasts with less deeply-rooted faults in the Albuquerque basin in the central Rio Grande rift. Deeper soling out of the Sangre de Cristo bounding fault could be due to less extension in the northern Rio Grande rift and/or greater strength of the lithosphere compared to the central Rio Grande rift. Unequivocal Moho reflections beneath the San Luis basin cannot be identified, probably due to limited signal penetration or a gradational nature of the Moho. The majority of rift-related movement observed on the Sangre de Cristo bounding fault is post-Eocene. Either the western margin of the basin is marked by a tight monocline or a low-angle normal fault.

  13. A new species of bumblebee catfish of the genus Microglanis (Siluriformes: Pseudopimelodidae from the upper rio Paraguay basin, Brazil

    Oscar Akio Shibatta

    Full Text Available ABSTRACT A new species of Microglanis from upper rio Paraguay basin is described. The species differs from congeners by the following combination of characters: deeply forked caudal fin with pointed lobes, bifurcated hook between antrorse and retrorse hooks on anterior margin of pectoral-fin spine, lateral line relatively long, surpassing the vertical through end of dorsal fin but not reaching adipose fin, color pattern of dorsal region of head dark brown with a restrict thin light area between anterior nostril and eye, broad light stripe on supraoccipital region.

  14. Description of a new species of Parotocinclus (Siluriformes, Hypoptopomatinae) from the rio Tapajós basin

    Roxo, Fábio F.; Silva, Gabriel S. C.; Oliveira, Claudio


    Abstract A new species of Parotocinclus is described from three small tributaries of the rio Tapajós basin, Mato Grosso State, Brazil. The new species can be distinguished from its congeners by presenting the following characters: (1) a triangular dark blotch at the anterior base of the dorsal fin, (2) the absence of an adipose fin but presence of one small platelet at typical adipose-fin region, (3) the abdomen completely covered by dermal plates, (4) a pectoral girdle totally exposed, (5) a single series of bicuspid teeth, and (6) the higher number of bicuspid premaxillary and dentary teeth. PMID:27917053

  15. Cooperation on Climate Services in the Binational Rio Grande/Bravo Basin

    Garfin, G. M.; Shafer, M. A.; Brown, D. P.


    The Rio Grande/Bravo River Basin (RGB) of the United States and México is exposed to tornadoes, severe storms, hurricanes, winter storms, wildfire, and drought. The combination of these weather and climate-related hazards has resulted in impacts, such as wildfire, crop loss, water supply reduction, and flooding, with exceedingly high economic costs ($13 billion in 2011). In order to contribute to increased binational information flow and knowledge exchange in the region, we have developed a prototype quarterly bilingual RGB Climate Outlook, in PDF, supplemented by Twitter messages and Facebook posts. The goal of the project is to improve coordination between institutions in the U.S. and Mexico, increase awareness about climate variations, their impacts and costs to society, and build capacity for enhanced hazard preparedness. The RGB Outlook features a synthesis of climate products, impact data and analysis, is expressed in user-friendly language, and relies substantially on visual communication in contrast to text. The RGB Outlook is co-produced with colleagues in the U.S. and Mexico, in conjunction with the North American Climate Services Partnership (NACSP) and NOAA's regional climate services program. NACSP is a tri-national initiative to develop and deliver drought-based climate services in order to assist water resource managers, agricultural interests, and other constituents as they prepare for future drought events and build capacity to respond to other climate extremes. The RGB Climate Outlook builds on lessons learned from the Climate Assessment for the Southwest (CLIMAS) Southwest Climate Outlook (PDF, html), La Niña Drought Tracker (PDF, html), the Southern Climate Impacts Policy Program (SCIPP) Managing Drought in the Southern Plains webinar series, the Border Climate Summary (PDF), and Transborder Climate newsletter (PDF) and webinar series. The latter two have been the only regularly occurring bilingual climate information products in the U

  16. Geochemical characterization of ground-water flow in the Santa Fe Group aquifer system, Middle Rio Grande Basin, New Mexico

    Plummer, L. Niel; Bexfield, Laura M.; Anderholm, Scott K.; Sanford, Ward E.; Busenberg, Eurybiades


    Chemical and isotopic data were obtained from ground water and surface water throughout the Middle Rio Grande Basin (MRGB), New Mexico, and supplemented with selected data from the U.S. Geological Survey (USGS) National Water Information System (NWIS) and City of Albuquerque water-quality database in an effort to refine the conceptual model of ground-water flow in the basin. The ground-water data collected as part of this study include major- and minor-element chemistry (30 elements), oxygen-18 and deuterium content of water, carbon-13 content and carbon-14 activity of dissolved inorganic carbon, sulfur-34 content of dissolved sulfate, tritium, and dissolved atmospheric gases including nitrogen, argon, helium, chlorofluorocarbons,

  17. Competing Interests and Concerns in the Rio Grande Basin: Mountain Hydrology, Desert Ecology, Climate Change, and Population Growth

    Rango, A.


    In the mountainous American Southwest, the Rio Grande basin is a prime example of how conflicts, misconceptions, and competition regarding water can arise in arid and semi-arid catchments. Much of the Rio Grande runoff originates from snow fields in the San Juan Mountains of southern Colorado and the Sangre De Cristo Mountains of northern New Mexico, far from population centers. Large and rapidly growing cities, like Albuquerque, Las Cruces, El Paso, and Juarez, are located along the Rio Grande where it flows through the Chihuahuan Desert, the largest desert in North America(two NSF Long Term Ecological Research sites are located in the desert portion of the basin). As a result, the importance of snowmelt, which makes up 50-75% or more of the total streamflow in sub-basins above Elephant Butte Reservoir(in south central New Mexico) is hardly known to the general public. Streamflow below Elephant Butte Reservoir is rainfall driven and very limited, with the lower basin receiving only 170-380 mm of precipitation annually, most of it occurring during the months of July-September. Extreme events, such as drought and flooding, are not unusual in arid basins, and they are of increasing concern with regard to changes in frequency of such events under the impending conditions of climate change. Current water demands in the basin already exceed the water supply by 15% or more, so streamflow forecasts(especially from snowmelt runoff) are extremely valuable for efficient water management as well as for proper apportionment of water between Colorado, New Mexico, and Texas under the Rio Grande Compact of 1938 and between the U.S. and Mexico under the Treaty of 1906. Other demands on the water supply include Indian water rights, flood regulation, irrigated agriculture, municipal and industrial demands, water quality, riverine and riparian habitat protection, endangered and threatened species protection, recreation, and hydropower. To assess snow accumulation and cover and to

  18. A new Xenacanthiformes shark (Chondrichthyes, Elasmobranchii from the Late Paleozoic Rio do Rasto Formation (Paraná Basin, Southern Brazil



    Full Text Available The Brazilian records on Xenacanthiformes include teeth and cephalic spines from the Parnaíba, Amazonas and Paraná basins. This work describes a new species of Xenacanthidae, collected in an outcrop of Serrinha Member of Rio do Rasto Formation (Wordian to Wuchiapingian, Paraná Basin, municipality of Jacarezinho, State of Paraná. The teeth of the new species are two or three-cuspidated and the aboral surface show a smooth concavity and one rounded basal tubercle. The coronal surface presents one semi-spherical and subcircular coronal button, and also two lateral main cusps and one central (when present with less than one fifth of the size of the lateral cusps in the labial portion. The lateral cusps are asymmetric or symmetric, rounded in transversal section, lanceolate in longitudinal section, devoid of lateral carinae and lateral serrations, and with few smooth cristae of enameloid. In optical microscope the teeth show a trabecular dentine (osteodentine base, while the cusps are composed by orthodentine, and the pulp cavities are non-obliterated by trabecular dentine. The fossil assemblage in the same stratigraphical level and in the whole Rio do Rasto Formation indicates another freshwater record for xenacanthid sharks.

  19. A new Xenacanthiformes shark (Chondrichthyes, Elasmobranchii) from the Late Paleozoic Rio do Rasto Formation (Paraná Basin), Southern Brazil.

    Pauliv, Victor E; Dias, Eliseu V; Sedor, Fernando A; Ribeiro, Ana Maria


    The Brazilian records on Xenacanthiformes include teeth and cephalic spines from the Parnaíba, Amazonas and Paraná basins. This work describes a new species of Xenacanthidae, collected in an outcrop of Serrinha Member of Rio do Rasto Formation (Wordian to Wuchiapingian), Paraná Basin, municipality of Jacarezinho, State of Paraná. The teeth of the new species are two or three-cuspidated and the aboral surface show a smooth concavity and one rounded basal tubercle. The coronal surface presents one semi-spherical and subcircular coronal button, and also two lateral main cusps and one central (when present) with less than one fifth of the size of the lateral cusps in the labial portion. The lateral cusps are asymmetric or symmetric, rounded in transversal section, lanceolate in longitudinal section, devoid of lateral carinae and lateral serrations, and with few smooth cristae of enameloid. In optical microscope the teeth show a trabecular dentine (osteodentine) base, while the cusps are composed by orthodentine, and the pulp cavities are non-obliterated by trabecular dentine. The fossil assemblage in the same stratigraphical level and in the whole Rio do Rasto Formation indicates another freshwater record for xenacanthid sharks.

  20. Relationship between the inorganic chemical composition of water, precipitation and evaporation in the basin of Rio Grande, Chone, Ecuador

    David Carrera


    Full Text Available (Received: 2015/01/19 - Accepted: 2015/03/25In the Rio Grande basin, the Chone Multi-Purpose dam (PMCH is built with an investment of approximately $66 million, to irrigate over 7000ha. The marked differences in precipitation could impair the quality of water; therefore the aim of this study was to establish the relationship between the ions and their location in the graph: relationship of ions and mechanisms of chemical processes, water behavior and trend setting. The study was a non-experimental, cross-sectional and descriptive research. 111 samples were collected in the group of channels that form the Rio Grande basin, in 2013 and 2014 during times of drought and rain. The parameters were measured in the sample anions and cations. The processes that control the chemistry of surface water in the studied area during the rainy season have a predisposition to mineralization in equilibrium with rocks. However, in the time of drought, water movement was observed towards the area where evaporation with respect to precipitation predominates, increasing the inorganic chemistry of the waters that, in time, could be extended.

  1. Progress on the palynostratigraphy of the Permian strata in Rio Grande do Sul State, Paraná Basin, Brazil

    Souza Paulo A.


    Full Text Available A review of published papers and results of analysis of new material have allowed improvements on the palynostratigraphy of the Permian strata of the Paraná Basin in Rio Grande do Sul State. Based on first and last occurrences of certain species of pollen taxa, two palynozones are formalized, these are the Vittatina costabilis and Lueckisporites virkkiae Interval Zones, in ascending order. The Vittatina costabilis Interval Zone is subdivided into two units, in ascending order the Protohaploxypinus goraiensis and the Hamiapollenites karrooensis Subzones, and is recognized from the glacial (Itararé Group and post-glacial sequence (Rio Bonito Formation and the base of the Palermo Formation. The Lueckisporites virkkiae Interval Zone occurs from the uppermost Rio Bonito Formation, through the Palermo and Irati formations, and into the Serra Alta and Teresina formations. The main characteristics and reference sections are established, as well as additional criteria to recognize biostratigraphical units, in accordance with the International Stratigraphic Guide. Palynostratigraphical correlation suggests that the Vittatina costabilis Zone concerns the Early Permian (early Cisuralian, while the Lueckisporites virkkiae is regarded as late Early Permian to early Middle Permian (late Cisularian to early Guadalupian.

  2. A new species of Eigenmannia Jordan and Evermann (Gymnotiformes: Sternopygidae) from the upper rio Paraguai basin.

    Campos-DA-Paz, Ricardo; Queiroz, Igor Raposo


    Eigenmannia correntes, a new species belonging to the Eigenmannia trilineata species-group, is described from tributaries of rio Correntes, a major affluent of the rio Piquiri system, upper rio Paraguai basin (Mato Grosso and Mato Grosso do Sul states, Brazil). Eigenmannia correntes is included in the currently poorly defined sternopygid genus Eigenmannia (Ostariophysi: Gymnotiformes) by presenting characters that are either primitive or of uncertain polarity, such as eyes covered by skin, scales present over entire postcranial portion of body, teeth absent from oral valve, infraorbital bones 1+2 with enlarged posterodorsal expansion, and gill rakers short and unossified. The new species is distinguished from all congeners, except those species included in the Eigenmannia trilineata species-group, by the presence of a conspicuous superior midlateral stripe (synapomorphy of this clade). Eigenmannia correntes can be differentiated from all members of the Eigenmannia trilineata species-group, except E. vicentespelaea, E. waiwai and E. besouro, by its subterminal mouth (vs. terminal in remaining species of that group). Further, it differs from these aforementioned species by a number of meristic and morphometric characters, including number of premaxillary and dentary teeth, number of longitudinal series of scales above lateral line, number of pectoral-fin and anal-fin rays, eye diameter, postorbital distance, and snout length. Finally, notes on reproduction and parasitism for E. correntes are presented.

  3. Water resources during drought conditions and postfire water quality in the upper Rio Hondo Basin, Lincoln County, New Mexico, 2010-13

    Sherson, Lauren R.; Rice, Steven E.


    Stakeholders and water-resource managers in Lincoln County, New Mexico, have had long-standing concerns over the impact of population growth and groundwater withdrawals. These concerns have been exacerbated in recent years by extreme drought conditions and two major wildfires in the upper Rio Hondo Basin, located in south-central New Mexico. The U.S. Geological Survey (USGS), in cooperation with Lincoln County, initiated a study in 2006 to assess and characterize water resources in the upper Rio Hondo Basin. Data collected during water years 2010–13 are presented and interpreted in this report. All data presented in this report are described in water years unless stated otherwise.

  4. Petrography and diagenesis of Gomo member sandstones - Candeias Formation (lower cretaceous) Rio do Buoil field, Reconcavo Basin; Petrografia e diagenese dos arenitos do Membro Gomo - Formacao Candeias (Cretaceo Inferior) no Campo de Rio do Bu, Bacia do Reconcavo

    Mato, Luiz F.; Souza, Edson M. [PETROBRAS, BA (Brazil). Distrito de Exploracao


    Characteristics, textural and compositional aspects, analyse the provenance and diagenetic evolution of the Gomo Member/Candeias Formation sandstones (Lower Cretaceous) in the Rio do Bu oil field, Reconcavo Basin, are discussed. Studies of sandstone petrography, shales and carbonates associated, diagenetic sequence, rifts fractures and cementation characterization, are also analyzed. 17 figs., 2 tabs., 19 refs

  5. Magnetotelluric data collected near geophysically logged boreholes in the Espa?ola and Middle Rio Grande basins, New Mexico

    Williams, Jackie M.; Rodriguez, Brian D.


    The Santa Fe region is growing rapidly. The Santa Fe Group aquifer in the Espa?ola Basin is the main source of municipal water for the region, and water shortfalls could have serious consequences. Future growth and land management in the region depend on accurate assessment and protection of the region's ground-water resources. An important issue in managing the ground-water resources is a better understanding of the hydrogeology of the Tertiary Santa Fe Group. The Santa Fe Group includes the sedimentary deposits that fill the Rio Grande rift and contain the principal ground-water aquifers. The U.S. Geological Survey (USGS) is conducting a series of multidisciplinary studies of the Espa?ola Basin in northern New Mexico. Detailed geologic mapping, high-resolution airborne magnetic surveys, electromagnetic surveys, and hydrologic, lithologic, and hydro-geochemical data are being used to better understand the aquifer systems. Magnetotelluric (MT) surveys were completed as part of these studies. The primary purpose of the MT surveys was to map changes in electrical resistivity with depth that are related to differences in various rock types that help control the properties of aquifers in the region. Resistivity modeling of the MT data can be used to investigate buried structures related to the basic geologic framework of the study area. The purpose of this report is to release MT sounding data collected near geophysically logged boreholes in the study area, including the nearby Middle Rio Grande Basin. This MT data can be used in subsequent resistivity modeling. No interpretation of the data is included in this report.

  6. Hydrology, water quality, and potential alternatives for water-resources development in the Rio Majada and Rio Lapa basins near the Albergue Olimpico, southern Puerto Rico

    Ramos-Gines, Orlando


    A water-resources investigation was conducted during 1989 in the Rio Lapa mountain basins in southern Puerto Rico, to define the hydrology, water quality, and to describe alternatives for additional water- resources supply. The total water budget for both surface- and ground-water resources in the study area was estimated to be 7,530 acre-feet per year for 1989. The water budget for the ground-water system, from which water needs are supplied in the study area, was estimated to be 2,760 acre-feet per year for 1989. Concentration of dissolved solids and fecal bacteria increased during the dry season as both streamflow and ground-water levels decreased. Water samples collected at two stream sites exceeded the recommended U.S. Environmental Protection Agency fecal bacteria concentration for natural water of 2,000 colonies per 100 milliliters during June to November 1989. Water samples obtained from a well in the Rio Lapa Valley exceeded the secondary drinking-water standard for dissolved solids of 500 milligrams per liter during four dry months. In addition, fecal bacteria concentrations at this water-supply well exceeded the primary fecal- bacteria drinking-water standard of 1 colony per 100 milliliter during June to October 1989. Existing water resources can probably be developed to meet additional demands of 110 acre-feet per year pro- jected for 1995. Storage of the surface-water runoff during the wet season and its gradual release to the study area could offset ground-water declines during the dry season. Ground-water withdrawals can be increased by the construction and use of low- capacity wells to reduce the amount of water lowing out of the study area.

  7. Assessing Water Availability in the Rio Grande Basin using NOAH Land Surface Model and NLDAS2 Forcing Data

    Khedun, C. P.; Giardino, J. R.; Singh, V. P.; Bolten, J. D.


    The Rio Grande/Río Bravo basin is a transboundary basin shared between several states in the United States and trends along part of the border between the United States and Mexico. The basin has a varied climatology - desert with high temperature and low water resources in the northern part and a tropical climate in the southern part. The surface water in the basin is over allocated, and some cities already rely solely on ground water to meet municipal water needs. The population and urban water demand are expected to double in the next 50 years. Climate variability and change, along with persistent long-term droughts, exacerbate the problem of meeting water demands. Uncertainty in the ways these climatic phenomena will affect the water availability in the coming decades will impact the effective long-term policies and management of water resources in the basin in the United States and Mexico, and this can lead to tensions over water allocation across the border. In order to study the impact of demographic changes and climate variability and change on future water availability, it is important to develop a model that can assess the current water availability and evaluate the effect of projected climate change, based on IPCC’s scenarios, on the hydrology of the basin. For this study we developed a model based on the community NOAH land surface model (LSM) within NASA’s GSFC Land Information System. The LSM is a 1-D column model that runs in coupled or uncoupled mode, and it simulates soil moisture, soil temperature, skin temperature, snowpack depth, snow water equivalent, canopy water content, and energy flux and water flux of the surface energy and water balance. The North American Land Data Assimilation Scheme (NLDAS2) is used to drive the model. The NLDAS2 datasets extends back to 1979, thereby allowing the model to be run retrospectively for a period of 30 years. Additional model parameters include seasonal maximum snow free albedo maps, monthly greenness

  8. Use of System Thinking Software for Determining Climate Change Impacts in Water Balance for the Rio Yaqui Basin, Sonora, Mexico

    Tapia, E. M.; Minjarez, J. I.; Espinoza, I. G.; Sosa, C. M.


    Climate change in Northwestern Mexico and its hydrological impact on water balance, water scarcity and flooding events, has become a matter of increasing concern over the past several decades due to the region's semiarid conditions. Changes in temperature, precipitation, and sea level will affect agriculture, farming, and aquaculture, in addition to compromising the quality of water resources for human consumption. According to the Fourth Assessment Report of the Intergovernmental Panel on Climate Change (IPCC, 2007), Global Circulation Models (GCMs) can provide reliable estimations of future climate conditions in addition to atmospheric processes that cause them, based on different input scenarios such as A2 (higher emission of greenhouse gases) and B1 (lower emission of GHG), among others. However, GCM`s resolution results to coarse in regions which have high space and time climate variability. To remediate this, several methods based on dynamical, statistical and empirical analysis have been proposed for downcaling. In this study, we evaluate possible changes in precipitation and temperature for the "Rio Yaqui Basin" in Sonora, Mexico and assess the impact of such changes on runoff, evapotranspiration and aquifer recharge for the 2010-2099 period of time. For this purpose, we analyzed the results of a Bias Corrected and Downscaled Climate Projection from the World Climate Research Programme's (WCRP's) Coupled Model Intercomparison Project phase 3 (CMIP3) multi-model dataset: UKMO-HADCM3 from the Hadley Centre for Climate Prediction. Northwest Mexico is under the influence of the North American Monsoon (NAM), a system affecting the states of Sinaloa and Sonora where the precipitation regimes change drastically during the summer months of June, July and August. It is associated to the sharp variations of topography, precipitation and temperature regimes in the region, so the importance of analyzing the downscaled climate projections. The Rio Yaqui Basin is one of

  9. A new species of the catfish genus Centromochlus (Siluriformes: Auchenipteridae: Centromochlinae from the upper rio Paraná basin, Brazil

    Luisa Maria Sarmento-Soares

    Full Text Available Centromochlus comprises twelve species, distributed in the main inland watersheds of South America, including the Orinoco, Essequibo, coastal rivers of Suriname, Amazon, upper Paraná and São Francisco basins. The new species is described from the upper rio Paraná based on material collected in 1965 during the construction of the UHE Ilha Solteira, São Paulo, Brazil. The new species is easily distinguished from all congeners due to absence of adipose fin, a condition otherwise restricted to Gelanoglanis nanonocticolus, among centromochlin catfishes. The new species comprises small catfishes (adults ranging from 35 to 39 mm SL, in which modified anal fin of males is devoid of denticulations or spines, and most posterior rays reduced in length. In addition, Tatia simplex Mees is transferred to Centromochlus and its generic reassignment discussed.

  10. Description of a new species of Ituglanis (Siluriformes: Trichomycteridae from Serra dos Carajás, rio Tocantins basin

    Wolmar B. Wosiacki

    Full Text Available A new species of Ituglanis is described from the rio Tocantins basin, State of Pará, Brazil. Ituglanis ina, new species, is distinguished from its congeners by the presence of a dark vertical bar over the base of the caudal-fin rays (vs. no bars over caudal-fin base; and by the presence of a middle trunk line of tiny neuromasts extending along the flank until the vertical through the dorsal fin, or near the caudal-fin base (vs. no middle trunk line of tiny neuromasts. Ituglanis ina can be further distinguished by a combination of characters related to color pattern and morphology. Comments on the relationship between Ituglanis species are presented.

  11. Two new species of Hypostomus Lacépède (Teleostei: Loricariidae from the upper rio Paraná basin, Central Brazil

    Cláudio H. Zawadzki

    Full Text Available Two new species of Hypostomus Lacépède (Teleostei: Loricariidae from the rio Paranaíba and rio Grande basins, both in the upper rio Paraná basin, central Brazil, are described herein. One of them is distinguished from all congeners, except H. albopunctatus, by having the pectoral-fin spine length equal to or smaller than the pelvic-fin spine. From H. albopunctatus, it is distinguished by having round dark spots (vs. pale on body and fins. The second species is distinguished from all congeners, except H. multidens and H. ternetzi, by having more than 115 teeth (vs. less than 109 per ramus on dentary and premaxilla. It is distinguished most readily from H. ternetzi by having teeth with two symmetrical (vs. asymmetrical cusps. It is distinguished from H. multidens by having round dark spots (vs. pale over body and fins.

  12. A new species of the Hypostomus cochliodongroup (Siluriformes: Loricariidae from the rio Aripuanã basin in Brazil

    Cláudio H. Zawadzki

    Full Text Available A new species of Hypostomus, H. dardanelos, is described from the rio Aripuanã basin, a southern tributary to the rio Madeira, in northern Mato Grosso State, Brazil. The new species is assigned to the Hypostomus cochliodon group by the possession of few teeth, spoon-shaped teeth, angle between dentaries usually less than 80°, and by the absence of a notch between hyomandibular and the metapterygoid. The new species can be diagnosed from its congeners by its unique color pattern of yellowish-brown ground color covered by well-defined dark spots of relatively equal size, evenly spaced and moderately set along the dorsal region of the body and fins, except on the ventrolateral region of the caudal peduncle and proximal region of anal and caudal fins, which are devoid of spots. The new species is further diagnosed by having teeth with very small lateral cusp, fused to the mesial one and almost imperceptible; by the absence of medial buccal papillae, and by nuptial odontodes all along the body (odontodes more pronounced in some few larger specimens.

  13. Development of Semi-distributed ecohydrological model in the Rio Grande De Manati River Basin, Puerto Rico

    Setegn, S. G.; Ortiz, J.; Melendez, J.; Barreto, M.; Torres-Perez, J. L.; Guild, L. S.


    There are limited studies in Puerto Rico that shows the water resources availability and variability with respect to changing climates and land use. The main goal of the HICE-PR (Human Impacts to Coastal Ecosystems in Puerto Rico (HICE-PR): the Río Loco Watershed (southwest coast PR) project which was funded by NASA is to evaluate the impacts of land use/land cover changes on the quality and extent of coastal and marine ecosystems (CMEs) in two priority watersheds in Puerto Rico (Manatí and Guánica).The main objective of this study is to set up a physically based spatially distributed hydrological model, Soil and Water Assessment Tool (SWAT) for the analysis of hydrological processes in the Rio Grande de Manati river basin. SWAT (soil and water assessment tool) is a spatially distributed watershed model developed to predict the impact of land management practices on water, sediment and agricultural chemical yields in large complex watersheds. For efficient use of distributed models for hydrological and scenario analysis, it is important that these models pass through a careful calibration and uncertainty analysis. The model was calibrated and validated using Sequential Uncertainty Fitting (SUFI-2) calibration and uncertainty analysis algorithms. The model evaluation statistics for streamflows prediction shows that there is a good agreement between the measured and simulated flows that was verified by coefficients of determination and Nash Sutcliffe efficiency greater than 0.5. Keywords: Hydrological Modeling; SWAT; SUFI-2; Rio Grande De Manati; Puerto Rico

  14. Application of a Distributed, Physically Based, Hydrologic Model to Improve Streamflow Forecasts in the Upper Rio Grande Basin

    Gorham, T. A.; Boyle, D. P.; McConnell, J. R.; Lamorey, G. W.; Markstrom, S.; Viger, R.; Leavesley, G.


    Approximately two-thirds of the runoff in the Rio Grande begins as seasonal snowpack in the headwaters above the USGS stream gaging stations at several points (nodes) above Albuquerque, New Mexico. Resource managers in the Rio Grande Basin rely on accurate short and long term forecasts of water availability and flow at these nodes to make important decisions aimed at achieving a balance among many different and competing water uses such as municipal, fish and wildlife, agricultural, and water quality. In this study, a distributed, physically based hydrologic model is used to investigate the degree of spatial and temporal distribution of snow and the processes that control snowmelt necessary to accurately simulate streamflow at seven of these nodes. Specifically, snow distribution and surface runoff are estimated using a combination of the USGS Modular Modeling System (MMS), GIS Weasel, Precipitation-Runoff Modeling System (PRMS), and XYZ snow distribution model. This highly collaborative work between researchers at the Desert Research Institute and the USGS is an important part of SAHRA (Sustainability of semi-Arid Hydrology and Riparian Areas) efforts aimed at improving models of snow distribution and snowmelt processes.

  15. Description of a new species of Ituglanis (Siluriformes: Trichomycteridae from Serra dos Carajás, rio Tocantins basin

    Wolmar B. Wosiacki


    Full Text Available A new species of Ituglanis is described from the rio Tocantins basin, State of Pará, Brazil. Ituglanis ina, new species, is distinguished from its congeners by the presence of a dark vertical bar over the base of the caudal-fin rays (vs. no bars over caudal-fin base; and by the presence of a middle trunk line of tiny neuromasts extending along the flank until the vertical through the dorsal fin, or near the caudal-fin base (vs. no middle trunk line of tiny neuromasts. Ituglanis ina can be further distinguished by a combination of characters related to color pattern and morphology. Comments on the relationship between Ituglanis species are presented.Uma espécie nova de Ituglanis é descrita da bacia do rio Tocantins, Pará, Brasil. Ituglanis ina, espécie nova, é facilmente diferenciada das congêneres por apresentar uma barra vertical escura sobre a base dos raios da nadadeira caudal (vs. sem barras na base da nadadeira caudal; e por apresentar linha lateral seguida por uma linha de diminutos neuromastos até a região do flanco, abaixo da nadadeira dorsal, ou até o pedúnculo caudal (vs. sem neuromastos após a linha lateral. Ituglanis ina distingue-se, também, por uma combinação de caracteres relacionados ao padrão de coloração e morfologia. Comentários sobre o relacionamento das espécies e grupos de espécies de Ituglanis são apresentados

  16. Availability of water resources in the rio Bermudez micro-basin. Central Region of Costa Rica; Disponibilidad del recurso hidrico en la microcuenca del rio Bermudez. Region Central de Costa Rica

    Hernando Echevarria, L.; Orozco Montoya, R.


    The Rio Bermudez micro-basin makes up part of the principal hydrological resource area in the Central Region of Costa Rica. For this reason a study was done to determine the availability of hydrological resources in said micro-basin to identify areas with potential water availability problems. A monthly water balance was calculated using land use, geomorphology and climate parameters. From these water balance studies, the amount of available water was calculated and classified into four categories, however, in this micro-basin, only three categories were identified: high, medium and moderate water availability. No areas were identified with low water availability, indicating availability is sufficient; however, there is increasing demand on water resources because over half of the micro-basin area is classified as having moderate water availability. (Author)


    Adilson Ben da Costa


    Full Text Available The aim of this research was to evaluate the quality of groundwater in areas of permanent preservation (Guarani Aquifer System – GAS in the Rio Pardo Hydrographical Basin, RS, Brazil, using physical, chemical and microbiological variables, based on resolution no. 396/2008 of the National Council on the Environment - CONAMA. Nine sampling points were distributed throughout the basin, where groundwater was classified as the major ions through the Piper diagram. The results indicated that most of the wells evaluated were classified in Class 4, accounting for water uses less restrictive. However, it should be considered that the aquifers are characterize by different geological conditions, having intrinsical physical, chemical and biological variables with hydrogeochemical variations, requiring that their quality levels are often based on these characteristics, as noted in diagram Piper, where the samples P1, P2, P3, P5 and P9 were classified as calcium bicarbonate, the waters of the points P4, P6, P7 as sodium bicarbonate and P8 as sulfated. It was found that the quality of water from wells with depths less than 6 m are becoming more vulnerable due to anthropogenic activities, as showing by the concentration of nitrate, total and thermotolerant coliforms, while the quality of water from deeper wells basically depends on their hydrogeological and hydrogeochemical characteristics based on the concentration of sodium and sulfate variables. However, they also showed contamination by human activities, mainly by the nitrate variable.

  18. Miocene sediment dispersal in the central Española basin, Rio Grande rift, New Mexico, U.S.A.

    Cavazza, William


    The central Española basin in north-central New Mexico represents one of the best opportunities to examine deposits related to the development of the Rio Grande rift. The Miocene Tesuque Formation represents the bulk of the Española basin fill. It is composed of a 2000-2500 m thick sequence of alluvial-fluvial and, subordinately, lacustrine deposits with numerous interbedded ash-fall tuff layers. The overall detrital composition of the Tesuque Formation is very similar throughout the central Española basin. Provenance is primarily from basement uplifts composed of Precambrian igneous and high-grade metamorphic rocks. Nevertheless, the combined use of paleocurrent analysis, and sandstone and conglomerate petrology allows a detailed reconstruction of the sediment paleodispersal system. Two sedimentary provinces are present within the Tesuque Formation: Province A, present in the eastern, central and southern portions of the study area, has a predominantly plutoniclastic and metamorphiclastic composition, and shows systematic paleocurrents toward the west. The sediments were derived from the Precambrian-cored Santa Fe block of the Sangre de Cristo Mountains, located directly to the east of the study area. Province B, present only in the northwestern portion of the study area, is characterized by a minor but significant amount of volcaniclastic and sedimentaclastic detritus, and shows consistent SSW-directed paleocurrents. The source area was possibly located in the area of the Taos Plateau and Latir volcanic fields. An intermediate narrow and discontinuous belt (province A + B) represents a hybrid province, where directional and compositional parameters are gradational.

  19. Effects of mining activities on heavy metal concentrations in water, sediment, and macroinvertebrates in different reaches of the Pilcomayo River, South America.

    Smolders, A J P; Lock, R A C; Van der Velde, G; Medina Hoyos, R I; Roelofs, J G M


    From 1997 until 1999 the extent and the ecological effects of zinc, copper, lead, and cadmium pollution were studied in different reaches of the South American Pilcomayo River. A comparison of metal concentrations in water, sediment, and chironomid larvae, as well as the diversity of macroinvertebrate species, was made between sites near the origin of the Pilcomayo River, with hardly any mining activities, sites in the Potosí region, with intensive mining, and sites located 500 km or further downstream of Potosí, in the Chaco plain. Samples were also collected in an unpolluted river (Cachi Mayu River) and in the Tarapaya River, which is strongly contaminated by mine tailings (1000 tons a day). The upper parts of the Pilcomayo River are strongly affected by the release of mine tailings from the Potosí mines where mean concentrations of lead, cadmium, copper, and zinc in water, filtered water, sediment, and chironomid larvae were up to a thousand times higher than the local background levels. The diversity of the benthic macroinvertebrate community was strongly reduced in the contaminated parts; 97% of the benthic macroinvertebrates consisted of chironomid larvae. The degree of contamination in the lower reaches of the river, however, was fairly low because of sedimentation processes and the strong dilution of mine tailings with enormous amounts of clean sediment from erosion processes. Analysis of sediment cores from the Ibibobo floodplain, however, reveal an increase of the heavy metal concentrations in the lower reaches since the introduction of the contaminating flotation process in the mine industry in 1985.

  20. Climate Change and the Snowmelt-runoff Relationship in the Upper Rio Grande Basin

    Chavarria, S. B.; Gutzler, D. S.


    Drought and rising temperatures have resulted in reduced snowpack and low flows in recent years for the Rio Grande, a vital source of surface water in three southwestern states and northern Mexico. We assess monthly and seasonal changes in streamflow volume on the upper Rio Grande (URG) near its headwaters in southern Colorado for water years 1958-2015. We use gage data from the U.S. Geological Survey, naturalized streamflows from the U.S. Natural Resources Conservation Service, and observed temperature, precipitation and snowpack data in the URG. Trends in discharge and downstream gains/losses are examined together with covariations in snow water equivalent, and surface climate variables. We test the hypothesis that climate change is already affecting the streamflow volume derived from snow accumulation in ways consistent with CMIP-based model projections of 21st Century streamflow, and we attempt to separate climate-related streamflow signals from variability due to reservoir releases or diversions. Preliminary results indicate that decreasing snowpack and resulting diminution of springtime streamflow in the URG are detectable in both observed and naturalized flow data beginning in the mid to late 1980s, despite the absence of significant decrease in total flow. Correlations between warm and cold season fluctuations in streamflow and temperature or precipitation are being evaluated and will be compared to model projections. Our study will provide information that may be useful for validating hydroclimatic models and improving seasonal water supply outlooks, essential tools for water management.

  1. A new long-finned Corydoras Lacépède, 1803 (Siluriformes: Callichthyidae from the lower rio Paraná basin, Brazil

    Luiz F. C. Tencatt

    Full Text Available A new species of Corydoras is described from the lower rio Paraná basin, just downstream from Itaipu Dam, Brazil, close to Paraguay boundary. The new species can be distinguished from most of its congeners by the infraorbital 2 with a posterior laminar expansion conspicuously reduced, first and second dorsal-fin branched rays conspicuously elongated in males, mesethmoid entirely covered by skin, and by the presence of four to six irregular black or brownish blotches on the midline of the flank. The probable occurrence of the new species in the floodplain of the upper portion of the rio Paraná drainage is discussed.

  2. Description and relationships of Otothyropsis marapoama, a new genus and species of hypoptopomatine catfish (Siluriformes: Loricariidae from rio Tietê basin, southeastern Brazil

    Alexandre C. Ribeiro

    Full Text Available Otothyropsis marapoama, a new genus and species, is described based on specimens recently collected in a headwater stream of the middle stretch of the rio Tietê, a river from the upper rio Paraná basin in southeastern Brazil. The new taxon belongs to a clade also encompassing the genera Schizolecis, Otothyris and Pseudotothyris. Otothyropsis marapoama is hypothesized to be the sister-group of Pseudotothyris and Otothyris based mainly on the presence of several derived characters of the swimbladder capsule and associated bones. Several paedomorphic characters shared by Pseudotothyris and Otothyris and their significance for the phylogenetic position of the new genus are discussed.

  3. Instream flow and water availability in the Rio das Pedras basin, Guarapuava-PR, Brazil

    Ederson Dias de Oliveira


    Full Text Available Knowledge of instream flow is of paramount importance to determine water availability for water resources management. This study estimated instream flow and evaluated water availability in the stretch of the Rio das Pedras, which supplies water to Guarapuava, a town in the mid-southern region of the state of Paraná, Brazil. Several different methods were employed to obtain instream flow, a reference discharge for water consumption permit, and the river regime. Methods comprised 7-day mean minimum with a 10-year return period, discharges associated to 95% and 90% permanence, yearly 7-day mean minimum discharge and basic water discharge. Discharge data were obtained from the meteorological station at the Water Station of Guarapuava (ETA. Results show that yearly river debit between 1985 and 2009 had a daily mean of 9.12 m³ s-1 and a median discharge of 9.16 m³ s-1. Estimated instream flow, measured by methods used for the Rio das Pedras stretch, ranged from 1.72 to 2.74 m³ s-1, with an average of 2.20 m³ s-1 and a coefficient of variation of 19.5%. Discharge for the stretch was estimated as 0.91 m³ s-1, following criteria used in the state of Paraná. The relationship of the evaluated stretch between daily flow and the intake volume granted by the government revealed the inefficiency of the applied methods for instream flow assessment. In fact, they failed to warrant a minimum water volume required for the conservation of the river ecosystem.

  4. Water quality and amphibian health in the Big Bend region of the Rio Grande Basin

    Sharma, Bibek; Hu, F.; Carr, J.A.; Patino, Reynaldo


    Male and female Rio Grande leopard frogs (Rana berlandieri) were collected in May 2005 from the main stem and tributaries of the Rio Grande in the Big Bend region of Texas. Frogs were examined for (1) incidence of testicular ovarian follicles in males; (2) thyroid epithelial cell height, a potential index of exposure to thyroid-disrupting contaminants; and (3) incidence of liver melanomacrophage aggregates, a general index of exposure to contaminants. Standard parameters of surface water quality and concentrations of selected elements, including heavy metals, were determined at each frog collection site. Heavy metals also were measured in whole-frog composite extracts. Water cadmium concentrations in most sites and chloride concentrations in the main stem exceeded federal criteria for freshwater aquatic life. Mercury was detected in frogs from the two collection sites in Terlingua Creek. There was a seventeen percent incidence of testicular ovarian follicles in male frogs. Mean thyroid epithelial cell height was greater in frogs from one of the Terlingua Creek sites (Terlingua Abajo). No differences were observed in the incidence of hepatic macrophage aggregates among sites. In conclusion, although potential cause-effect relationships between indices of habitat quality and amphibian health could not be established, the results of this study raise concerns about the general quality of the aquatic habitat and the potential long-term consequences to the aquatic biota of the Big Bend region. The presence of ovarian follicles in male frogs is noteworthy but further study is necessary to determine whether this phenomenon is natural or anthropogenically induced.

  5. Improvements in Snow Mapping of the Rio Grande Basin using MODIS Data

    G¢mez-Landesa, E.; Rango, A.


    Snow covered area data is valuable for assessing watershed condition. Additionally it is being used as an input for the Snowmelt Runoff Model (SRM), which provides simulations and forecasts of a basin's daily streamflow. A visible and a near infrared channel of the Moderate Resolution Imaging Spectroradiometer (MODIS) are being used to generate snow maps, replacing the traditional Advanced Very High Resolution Radiometer (AVHRR) data, and therefore improving the spatial resolution of the snow maps from 1 km to 250 m. In order to implement the MODIS data, a geometric correction algorithm was developed to remove the so called "Bowtie Effect" from the MODIS scenes. Radiances from pixels located on shaded slopes of the basin are strongly diminished because the two channels used in this method receive radiation from the solar reflective region of the spectrum. To correct this problem, an algorithm was developed to simulate the shaded areas on a Digital Elevation Model (DEM). This effect was found to be dependent on the altitude of the pixel, so an empirical second-order polynomial was applied. In order to make the snow mapping system as automated as possible, new methods were studied to retrieve snow albedo using bidirectional reflectance distribution functions (BRDF). Albedo retrieval can also be used as a criterium to infer the start of the snowmelt season, due to the decrease in reflectance of the snowpack as it ages.

  6. Trace-element accumulation by Hygrohypnum ochraceum in the upper Rio Grande Basin, Colorado and New Mexico, USA

    Carter, L.F. [Geological Survey, Albuquerque, NM (United States); Porter, S.D. [Geological Survey, Lakewood, CO (United States). Denver Federal Center


    Accumulation of 12 trace elements by transplanted aquatic bryophytes (Hygrohypnum ochraceum) was determined at 13 sites in the Rio Grande and tributary streams in southern Colorado and northern New Mexico as part of the US Geological Survey`s National Water-Quality Assessment Program. The purposes of the study were to determine the spatial distribution of trace elements in relation to land-use practices in the upper Rio Grande Basin, compare accumulation rates of metals in bryophytes at sites contaminated by trace elements, and evaluate transplanted aquatic bryophytes as a tool for examining the bioavailability of trace elements in relation to concentrations in water and bed sediment. Concentrations of Cd, Cu, Pb, and Zn in bryophytes, water, and bed sediment were significantly higher at sites that receive drainage from mining areas than at sites near agricultural or urban activities. Concentrations of most trace elements were lower in a tributary stream below an urban source than at sites near mining or agricultural use. Concentrations of Cu and Zn in bryophytes correlated with concentrations in water and bed sediment. In addition, bryophyte concentrations of As, Cd, and Pb correlated with concentrations in bed sediment. Transplanted bryophytes can provide an indication of bioavailability. Rates of accumulation were related to the magnitude of ambient trace-element concentrations; maximal uptake occurred during the first 10 d of exposure. Trace-element concentrations in transplanted bryophytes could potentially be used to predict water and sediment concentrations that represent an integration of conditions over short to intermediate lengths of time, rather than instantaneous conditions as measured using water samples.

  7. Resurrection of Pareiorhaphis Miranda Ribeiro, 1918 (Teleostei: Siluriformes: Loricariidae, and description of a new species from the rio Iguaçu basin, Brazil

    Edson H. Lopes Pereira

    Full Text Available A new species of the loricariid subfamily Neoplecostominae is described on the basis of specimens obtained from the headwaters of the rio Iguaçu basin in the State of Paraná, southern Brazil. Pareiorhaphis parmula is the first representative of the genus discovered from the rio Paraná basin and expands the geographic distribution of the genus. It is diagnosed from other Pareiorhaphis species by having one small plate on each side of the pectoral girdle, just posterior to the gill opening and the club-shaped pectoral-fin spine, broadening from base to tip in adult males. All species formerly included in Hemipsilichthys except H. gobio, H. papillatus, and H. nimius are transferred to the genus Pareiorhaphis, which is resurrected from the synonymy of Hemipsilichthys.

  8. Rock magnetic characterization of faulted sediments with associated magnetic anomalies in the Albuquerque Basin, Rio Grande rift, New Mexico

    Hudson, M.R.; Grauch, V.J.S.; Minor, S.A.


    Variations in rock magnetic properties are responsible for the many linear, short-wavelength, low-amplitude magnetic anomalies that are spatially associated with faults that cut Neogene basin sediments in the Rio Grande rift, including the San Ysidro normal fault, which is well exposed in the northern part of the Albuquerque Basin. Magnetic-susceptibility measurements from 310 sites distributed through a 1200-m-thick composite section of rift-filling sediments of the Santa Fe Group and prerift Eocene and Cretaceous sedimentary rocks document large variations of magnetic properties juxtaposed by the San Ysidro fault. Mean volume magnetic susceptibilities generally increase upsection through eight map units: from 1.7 to 2.2E-4 in the prerift Eocene and Cretaceous rocks to 9.9E-4-1.2E-3 in three members of the Miocene Zia Formation of the Santa Fe Group to 1.5E-3-3.5E-3 in three members of the Miocene-Pleistocene Arroyo Ojito Formation of the Santa Fe Group. Rock magnetic measurements and petrography indicate that the amount of detrital magnetite and its variable oxidation to maghemite and hematite within the Santa Fe Group sediments are the predominant controls of their magnetic property variations. Magnetic susceptibility increases progressively with sediment grain size within the members of the Arroyo Ojito Formation (deposited in fluvial environments) but within members of the Zia Formation (deposited in mostly eolian environments) reaches highest values in fine to medium sands. Partial oxidation of detrital magnetite is spatially associated with calcite cementation in the Santa Fe Group. Both oxidation and cementation probably reflect past flow of groundwater through permeable zones. Magnetic models for geologic cross sections that incorporate mean magnetic susceptibilities for the different stratigraphic units mimic the aeromagnetic profiles across the San Ysidro fault and demonstrate that the stratigraphic level of dominant magnetic contrast changes with

  9. Allozyme relationships in hypostomines (Teleostei: Loricariidae) from the Itaipu Reservoir, Upper Rio Paraná basin, Brazil.

    Zawadzki, Cláudio Henrique; Renesto, Erasmo; dos Reis, Roberto Esser; Moura, Maurício Osvaldo; Mateus, Rogério Pincela


    In an allozyme electrophoresis survey of 15 hypostomine species from the Itaipu Hydroelectric Reservoir, 25 loci from 14 enzyme systems were scored. Allozyme data allowed recording diagnostic genetic markers for all species analyzed and for some species groups within Hypostomus, a taxon which is taxonomically still unresolved in the Upper Rio Paraná basin. The mean expected heterozygosity of the species was considerably variable and hypotheses to tentatively explain this variation are discussed. A cladogram based upon the allelic frequencies of the species analyzed was produced by the continuous maximum likelihood method: Rhinelepis aspera and M. parananus were separated from the species of Hypostominae by a long branch length. Pterygoplichthys anisitsi was the sister of all the representatives of the genus Hypostomus. Within Hypostomus, two main clades were produced: in the first, H. cochliodon was the sister of the species comprising the H. plecostomus group, and in the second, the tree showed the following relationships: (H. albopunctatus (H. regani + Hypostomus sp. 3) + (H. margaritifer (H. microstomus (Hypostomus sp. 1 (H. ternetzi + Hypostomus sp. 2)). Hypostomus ternetzi and Hypostomus sp. 2 are referred to here as representatives of the H. ternetzi group.

  10. Dispersal syndromes of fossil seeds from the Lower Permian of Paraná Basin, Rio Grande do Sul, Brazil.

    Souza, Juliane M; Iannuzzi, Roberto


    The morphological analysis of seeds has been an important subject in modern ecological studies, once it provides evidence about the biology and adaptations of the parent plant. However, this kind of study has been restricted to the ecology of modern plants and is rarely used in interpretations of Paleozoic data. From the understanding of dispersal syndromes analysis as an important tool to paleoecological reconstruction, this study provides a first approach using this tool with seeds from the Lower Permian strata of southern Paraná Basin in Rio Grande do Sul. Based on previously classified seeds and using their biological and taphonomic data, the syndrome of dispersal was interpreted, and their placement in successional groups (pioneer, early-successional and later-successional) was suggested. Seven morphospecies were analyzed: Samaropsis gigas, representing a later-successional species living in water bodies with hydrochory as its dispersal syndrome; Samaropsis kurtzii, typical of early-successional species showing anemochory as its dispersal syndrome and living in distal areas in relation to water bodies; Samaropsis aff. S. millaniana, Cordaicarpus aff. C. brasilianus, Cordaicarpus cerronegrensis and Cordaicarpus truncata have typical characteristics of pioneer plants, exhibiting barochory as their primary dispersal syndrome with other syndromes associated.

  11. Immigration, science and health: risks control and expanding rights in the Rio de la Plata Basin (1873-1911

    Fernanda Rebelo-Pinto


    Full Text Available This paper analyzes how immigration process in the Rio de Plata Basin countries, specifically Brazil and Argentina, promoted inflexions in the sanitations agreements in the end of 19th century. The port is a device within in which are defined knowledge and standards and are established interventions on people in transit, particularly immigrants. The barriers in the agreements between these countries were not only related to controversies within medical and scientific communities but also to political and economics tensions linked to the labor immigrants disputes. In the beginning of 20th century, we can see a shift of interest and issues related to public health: epidemic control was not enough. The states must guarantee some benefits to the populations, especially heath care. This new view is analyzed according to the understanding and uses of the liberal ideology concerning risk self-regulations, collectivization of welfare and expanding of civil and social rights. This process is leveraged in parts by the inclusion of the immigrants in theses societies.

  12. Community-based transconjunctival marginal rotation for cicatricial trachoma in Indians from the Upper Rio Negro basin

    O.E. Soares


    Full Text Available The objective of the present study was to describe, for the first time in Brazil, the use by a non-ophthalmologist of a community-based marginal rotation procedure by a posterior approach in the indigenous population from the Upper Rio Negro basin. Seventy-three upper eyelids of 46 Indians (11 males and 35 females with cicatricial upper eyelid entropion and trichiasis were operated in the Indian communities using a marginal rotational procedure by a posterior approach by a non-ophthalmologist physician who had general surgery experience but only an extremely short period (one week of ophthalmic training. Subjects were reevaluated 6 months after surgery. Results were classified according to the presence and location of residual trichiasis and symptoms were assessed according to a three-level subjective scale (better, worse or no change. Fifty-six eyelids (76.7% were free from trichiasis, whereas residual trichiasis was observed in 17 eyelids (23.3% of 10 subjects. In these cases, trichiasis was either lateral or medial to the central portion of the lid. Of these 10 patients, only 4 reported that the surgery did not improve the irritative symptoms. We conclude that marginal rotation by a posterior approach is an effective and simple procedure with few complications, even when performed by non-specialists. Due to its simplicity the posterior approach is an excellent option for community-based upper eyelid entropion surgery.

  13. Climate model based consensus on the hydrologic impacts of climate change to the Rio Lempa basin of Central America

    E. P. Maurer


    Full Text Available Temperature and precipitation from 16 climate models each using two emissions scenarios (lower B1 and mid-high A2 were used to characterize the range of potential climate changes for the Rio Lempa basin of Central America during the middle (2040–2069 and end (2070–2099 of the 21st century. A land surface model was applied to investigate the hydrologic impacts of these changes, focusing on inflow to two major hydropower reservoirs. By 2070–2099 the median warming relative to 1961–1990 was 1.9°C and 3.4°C under B1 and A2 emissions, respectively. For the same periods, the models project median precipitation decreases of 5.0% (B1 and 10.4% (A2. Median changes by 2070–2099 in reservoir inflow were 13% (B1 and 24% (A2, with largest flow reductions during the rising limb of the seasonal hydrograph, from June through September. Frequency of low flow years increases, implying decreases in firm hydropower capacity of 33% to 53% by 2070–2099.

  14. Natural Landscapes and Optimal Resource Use at the Rio Grande Drainage Basin, Oaxaca, Mexico

    Marco Antonio Pablo Pablo


    Full Text Available Environmental conservation depends largely on the appropriate management and rational use of natural resources. The assessment of natural landscapes and their suitability for human occupation is key to ensure optimal resource use. The criteria for establishing land-use potentials vary according to the type of activity concerned. For example, in determining the most suitable areas for growing grapes in Cuyo, Argentina, Valpreda (2005 focused on topography, soil quality and water availability, whereas in their study on the oil-producing region of northern Chiapas, Mexico, Bollo et al. (2010 applied markedly different criteria. Soil components and their variability were key to the multi-purpose study of Ovalles and Núñez (1994, while morphometric criteria have been used by Bocco et al. (2010 on farming; for cattle raising, Travieso-Bello et al. (2013 added soil quality and moisture, similar to Rodríguez-Gallego, et al. (2012. In the state of Oaxaca, scientific studies on the feasibility of human activity in different natural landscapes are yet to be undertaken. This study assesses the natural landscapes and resources of the Río Grande drainage basin aimed at establishing optimal locations for agriculture, livestock farming, forestry, wildlife conservation and their combinations. Following the FAO studies (1976, 1993, geomorphological and morphoclimatic systems have been considered as landscape units for analysis. The methodology was adapted from the following studies: The Revised Universal Soil Loss Equation (Ouyang, 2002; an estimate of soil pH based on Landsat imagery (López-Granados et al., 2005; a calculation of potential livestock carrying capacity (LCC (Semarnat, 2003; Vergara and Ortiz-Espinoza, 2010; and a land use and vegetation cover analysis for forestry  suitability and the potential distribution of two cat species (Lynx rufus and Panthera onca (Chávez y Ceballos, 2006; Medellín-Legorreta and Bárcenas, 2009; Semarnat 2010

  15. A new species of Hemigrammus Gill, 1858 (Characiformes: Characidae) from the central and western Amazon and rio Paraná-Paraguai basins.

    Ota, Rafaela P; Lima, Flávio C T; Pavanelli, Carla S


    A new species of Hemigrammus is described from the middle rio Solimões/Amazonas and tributaries, upper and middle rio Madeira, and rio Paraná-Paraguai basins in Brazil and Paraguay. The new species is most similar among congeners with Hemigrammus marginatus, with which it shares similar caudal-fin pigmentation pattern. The new species can be distinguished from Hemigrammus marginatus by possessing two conspicuous dark patches of pigmentation on caudal fin, occupying most of caudal-fin lobes, except the tips, by having two dark narrow stripes along anal-fin base, and by possessing 5-8 pored lateral line scales. The new species differs from Hyphessobrycon diancistrus, which is similar in color pattern and general body shape, by the presence of small scales on caudal-fin lobes, occupying approximately its basal third, by the presence of two narrow stripes along anal fin base, and by the absence of bony hooks on analfin in mature males. The occurrence of the new species in both Amazon and rio Paraná-Paraguai basins is discussed in order to clarify and expand recent discussions on the biogeographical relationships between both river systems.

  16. Late Miocene-Pleistocene evolution of a Rio Grande rift subbasin, Sunshine Valley-Costilla Plain, San Luis Basin, New Mexico and Colorado

    Ruleman, C.A.; Thompson, R.A.; Shroba, R.R.; Anderson, M.; Drenth, B.J.; Rotzien, J.; Lyon, J.


    The Sunshine Valley–Costilla Plain, a structural subbasin of the greater San Luis Basin of the northern Rio Grande rift, is bounded to the north and south by the San Luis Hills and the Red River fault zone, respectively. Surficial mapping, neotectonic investigations, geochronology, and geophysics demonstrate that the structural, volcanic, and geomorphic evolution of the basin involves the intermingling of climatic cycles and spatially and temporally varying tectonic activity of the Rio Grande rift system. Tectonic activity has transferred between range-bounding and intrabasin faults creating relict landforms of higher tectonic-activity rates along the mountain-piedmont junction. Pliocene–Pleistocene average long-term slip rates along the southern Sangre de Cristo fault zone range between 0.1 and 0.2 mm/year with late Pleistocene slip rates approximately half (0.06 mm/year) of the longer Quaternary slip rate. During the late Pleistocene, climatic influences have been dominant over tectonic influences on mountain-front geomorphic processes. Geomorphic evidence suggests that this once-closed subbasin was integrated into the Rio Grande prior to the integration of the once-closed northern San Luis Basin, north of the San Luis Hills, Colorado; however, deep canyon incision, north of the Red River and south of the San Luis Hills, initiated relatively coeval to the integration of the northern San Luis Basin. Long-term projections of slip rates applied to a 1.6 km basin depth defined from geophysical modeling suggests that rifting initiated within this subbasin between 20 and 10 Ma. Geologic mapping and geophysical interpretations reveal a complex network of northwest-, northeast-, and north-south–trending faults. Northwest- and northeast-trending faults show dual polarity and are crosscut by north-south– trending faults. This structural model possibly provides an analog for how some intracontinental rift structures evolve through time.

  17. Structural and microstructural evolution of fault zones in Cretaceous poorly lithified sandstones of the Rio do Peixe basin, Paraiba, NE Brazil

    Balsamo, Fabrizio; Nogueira, Francisco; Storti, Fabrizio; Bezerra, Francisco H. R.; De Carvalho, Bruno R.; André De Souza, Jorge


    In this contribution we describe the structural architecture and microstructural features of fault zones developed in Cretaceous, poorly lithified sandstones of the Rio do Peixe basin, NE Brazil. The Rio do Peixe basin is an E-W-trending, intracontinental half-graben basin developed along the Precambrian Patos shear zone where it is abutted by the Porto Alegre shear zone. The basin formed during rifting between South America and Africa plates and was reactivated and inverted in a strike-slip setting during the Cenozoic. Sediments filling the basin consist of an heterolithic sequence of alternating sandstones, conglomerates, siltstone and clay-rich layers. These lithologies are generally poorly lithified far from the major fault zones. Deformational structures in the basin mostly consist of deformation band-dominated fault zones. Extensional and strike-slip fault zones, clusters of deformation bands, and single deformation bands are commonly well developed in the proximity of the basin-boundary fault systems. All deformation structures are generally in positive relief with respect to the host rocks. Extensional fault zones locally have growth strata in their hangingwall blocks and have displacement generally view, they are organized in anastomosed segments with high connectivity. They strike E-W to NE-SW, and typically consist of wide fault cores (narrow shear bands, in which bedding is transposed into foliation imparted by grain preferred orientation. Microstructural observations show negligible cataclasis and dominant non-destructive particulate flow, suggesting that extensional fault zones developed in soft-sediment conditions in a water-saturated environment. Strike-slip fault zones commonly overprint the extensional ones and have displacement values typically lower than about 2 m. They are arranged in conjugate system consisting of NNW-SSE- and WNW-ESE-trending fault zones with left-lateral and right-lateral kinematics, respectively. Compared to extensional

  18. Latest Miocene-earliest Pliocene evolution of the ancestral Rio Grande at the Española-San Luis Basin boundary, northern New Mexico

    Daniel J. Koning,; Scott Aby,; Grauch, V. J.; Matthew J. Zimmerer,


    We use stratigraphic relations, paleoflow data, and 40Ar/39Ar dating to interpret net aggradation, punctuated by at least two minor incisional events, along part of the upper ancestral Rio Grande fluvial system between 5.5 and 4.5 Ma (in northern New Mexico). The studied fluvial deposits, which we informally call the Sandlin unit of the Santa Fe Group, overlie a structural high between the San Luis and Española Basins. The Sandlin unit was deposited by two merging, west- to southwest-flowing, ancestral Rio Grande tributaries respectively sourced in the central Taos Mountains and southern Taos Mountains-northeastern Picuris Mountains. The river confluence progressively shifted southwestward (downstream) with time, and the integrated river (ancestral Rio Grande) flowed southwards into the Española Basin to merge with the ancestral Rio Chama. Just prior to the end of the Miocene, this fluvial system was incised in the southern part of the study area (resulting in an approximately 4–7 km wide paleovalley), and had sufficient competency to transport cobbles and boulders. Sometime between emplacement of two basalt flows dated at 5.54± 0.38 Ma and 4.82±0.20 Ma (groundmass 40Ar/39Ar ages), this fluvial system deposited 10–12 m of sandier sediment (lower Sandlin subunit) preserved in the northern part of this paleovalley. The fluvial system widened between 4.82±0.20 and 4.50±0.07 Ma, depositing coarse sand and fine gravel up to 14 km north of the present-day Rio Grande. This 10–25 m-thick sediment package (upper Sandlin unit) buried earlier south- to southeast-trending paleovalleys (500–800 m wide) inferred from aeromagnetic data. Two brief incisional events are recognized. The first was caused by the 4.82±0.20 Ma basalt flow impounding south-flowing paleodrainages, and the second occurred shortly after emplacement of a 4.69±0.09 Ma basalt flow in the northern study area. Drivers responsible for Sandlin unit aggradation may include climate

  19. Hydrochemical tracers in the middle Rio Grande Basin, USA: 2. Calibration of a groundwater-flow model

    Sanford, Ward E.; Plummer, L. Niel; McAda, Douglas P.; Bexfield, Laura M.; Anderholm, Scott K.

    The calibration of a groundwater model with the aid of hydrochemical data has demonstrated that low recharge rates in the Middle Rio Grande Basin may be responsible for a groundwater trough in the center of the basin and for a substantial amount of Rio Grande water in the regional flow system. Earlier models of the basin had difficulty reproducing these features without any hydrochemical data to constrain the rates and distribution of recharge. The objective of this study was to use the large quantity of available hydrochemical data to help calibrate the model parameters, including the recharge rates. The model was constructed using the US Geological Survey's software MODFLOW, MODPATH, and UCODE, and calibrated using 14C activities and the positions of certain flow zones defined by the hydrochemical data. Parameter estimation was performed using a combination of nonlinear regression techniques and a manual search for the minimum difference between field and simulated observations. The calibrated recharge values were substantially smaller than those used in previous models. Results from a 30,000-year transient simulation suggest that recharge was at a maximum about 20,000 years ago and at a minimum about 10,000 years ago. Le calibrage d'un modèle hydrogéologique avec l'aide de données hydrochimiques a démontré que la recharge relativement faible dans le Grand Bassin du Middle Rio est vraisemblablement responsable d'une dépression des eaux souterraines dans le centre du bassin et de la présence d'une quantité substantielle d'eau du Rio Grande dans l'aquifère du Groupe de Santa Fe. Les modèles antérieurs avaient des difficultés à reproduire ses conclusions sans l'aide de données hydrochimiques pour contraindre les taux et la distribution de la recharge. L'objectif de cette étude était d'utiliser une grande quantité de données hydrochimiques permettant de calibrer les paramètres du modèle, et notamment les taux de recharge. Le modèle a

  20. Modelagem hidrológica na bacia hidrográfica do Rio Aiuruoca, MG Hydrologic modeling in the Aiuruoca river basin, Minas Gerais State

    Marcelo R. Viola


    Full Text Available A simulação do comportamento hidrológico de bacias hidrográficas consiste em uma das principais ferramentas na gestão dos recursos hídricos, devido à possibilidade de predição do regime fluvial. A bacia em estudo está localizada na região Alto Rio Grande, Sul de Minas Gerais, com área de drenagem de 2.094 km², constituindo uma das bacias fundamentais de drenagem para o reservatório da Usina Hidrelétrica de Camargos (UHE - Camargos/CEMIG. Neste contexto se objetivou desenvolver e aplicar um modelo hidrológico semi-conceitual, na forma semi-distribuída, para simular o comportamento hidrológico da bacia do Rio Aiuruoca, com apoio dos SIGs e sensoriamento remoto, disponibilizando uma ferramenta útil para o gerenciamento e planejamento dos recursos hídricos na região. Os resultados do coeficiente estatístico de Nash-Sutcliffe (CNS foram de 0,87 e 0,92 para as etapas de calibração e verificação, respectivamente, o que, de acordo com a classificação proposta para modelos hidrológicos de simulação, permite qualificá-lo para simulação do comportamento hidrológico na bacia hidrográfica do Rio Aiuruoca.The hydrological simulation of watersheds is one of the most important tools for water resources management due to the possibility of flow regime prediction. The Aiuruoca river basin is located in the Alto Rio Grande Basin, southern Minas Gerais State, with 2,094 km² of drainage area, and is very important drainage basin into the Camargos Hydropower Plant Reservoir (UHE - Camargos/CEMIG. In this context, this work had the objective of developing and applying a semi-conceptual hydrologic model, in semi-distributed approach, for hydrologic simulation in the Aiuruoca river basin, based on GIS and Remote Sensing tools, thus creating an important tool for management and planning of water resources in the region. The Nash-Sutcliffe coefficients (CNS, respectively, for calibration and validation periods, were 0.87 and 0

  1. Mercury in sediments from shelf and continental slope at Campos Basin near Rio de Janeiro, Brazil

    Araujo, Beatriz; Hintelmann, Holger; Dimock, Brian; Gomes de Almeida, Marcelo; Falcão, Ana Paula; de Rezende, Carlos Eduardo


    Mercury (Hg) is a global pollutant due to its ability to undergo long-range transport from source regions to remote parts of the world, and its ubiquitous presence in aquatic ecosystems. The Hg isotope ratios could be an effective tool for tracing the sources and process of Hg in the environment. This study aimed to establish the distribution of mercury in surface sediments of three transects (25- 3000m water depth) in continental shelf and slope in Campos Basin-RJ-Brazil, using the Hg isotopes to understand the geochemical processes relating to Hg cycling that occur in a subtropical coastal environment. The study area was divided into three transects: A (located to the south and close to a upwelling area), D (located opposite the mouth of the Paraiba do Sul River) and I (located north near the top of Vitória-ES). Sampling isobaths were 25, 50, 75, 100, 150, 400, 700, 1000, 1300, 1900, 2500 and 3000m. The Total Hg, MMHg and Hg stable isotopes were determined based on EPA Method 1631, EPA method 1630 and Foucher and Hintelmann (2006), respectively. The silt/clay ranged from 0.05 to 95%, and the organic carbon (OC) from 0.07 to 1.43 % for all transects. THg and MMHg concentrations in the shelf were 11.9 ± 7.2 (1.7- 22.2) ng.g-1 and 0.15 ± 0.12 (0.02 - 0.40) ng.g-1; in the slope 30.3 ± 9.2 (11.6 - 51.6) ng.g-1 and 0.13 ± 0.06 (0.03 -0.29) ng.g-1 , respectively. The δ202Hg and Δ199Hg varied from -0.32 to -1.85 ‰ (-0.79 ± 0.44‰) and -0.41 to 0.09 ‰ (-0.03 ± 0.12 ‰) for all transects, respectively. The delta values between both regions are significantly different, the shelf region showed δ202Hg from -0.59 to -2.19 ‰ (mean: -1.52 ±0.65) and Δ199Hg from - 0.53 to 0.08 ‰ (mean: -0.27 ±0.55) and the slope region were observed δ202Hg values from -0.32 to -1.82 ‰ (mean: -0.73 ±0.39 ‰ n=18) and gΔ199Hg from -0.23 to 0.09‰ (mean: -0.02 ±0.08‰ n=5). The slope appears to be enriched with heavier isotopes compared to the shelf, however, in the

  2. Species diversity and distribution of freshwater crabs (Decapoda: Pseudothelphusidae inhabiting the basin of the Rio Grande de Térraba, Pacific slope of Costa Rica

    Luis Rólier Lara


    Full Text Available During the last decades, knowledge on biodiversity of freshwater decapods has increased considerably; however, information about ecology of these crustaceans is scarce. Currently, the freshwater decapod fauna of Costa Rica is comprised by representatives of three families (Caridea: Palaemonidae and Atyidae; Brachyura: Pseudothelphusidae. The present study aims to describe the species diversity and distribution of freshwater crabs inhabiting the basin of the Rio Grande de Térraba, Pacific slope of Costa Rica, where the Instituto Costarricense de Electricidad (ICE plans to implement one of the largest damming projects in the region. Samples were collected in 39 locations at an altitude ranging from 20 to 1,225 m. Sampling was carried out during several months in 2007, 2009 and 2010. We collected a total of 661 crabs, comprising eight species of Pseudothelphusidae of three genera, representing 53% of the 15 pseudothelphusid crab species currently recorded from Costa Rica. The most common species was Ptychophallus paraxanthusi followed by P. tristani. Freshwater crabs were more frequently encountered in the middle-low region of the basin (between 311 and 600 m and less frequently in the medium-high basin (between 601 and 1,225 m. Ptychophallus paraxanthusi showed the widest distribution and was collected in altitudes ranging from 20 to 700 m. The Rio Grande de Térraba region can be considered as a relatively small, but highly diverse system. Therefore, any alteration of the basin of Rio Grande de Térraba, and especially the possible construction of a hydroelectric power plant, needs to be carefully analyzed to mitigate the damaging effects of this project on the freshwater crabs. More ecological information about freshwater crabs from Costa Rica and the Central American region are needed to reach a first reasonable overview on the ecological role of these decapods in freshwater systems.

  3. Development of a Hydrologic Model to Assess the Feasibility of Water Leasing in the Middle Rio Grande Basin

    Garner, C. B.; Boyle, D. P.; Lamorey, G. W.; Bassett, S. D.


    The demand for water in the southwestern United States has increased in tandem with a rapid growth of population over the past 50 years. With ever increasing demands being placed on available water supplies, improving water management becomes crucial to the sustainability of the region's water resources. The National Science Foundation (NSF) Science and Technology Center (STC) for the Sustainability of semi-Arid Hydrology and Riparian Areas (SAHRA) is interested in the feasibility of water leasing as a method for more efficiently distributing water among competing users. Economists working on the project will run water leasing simulations in an auction-type environment to understand the pros and cons of water leasing in a free market system. To include hydrologic processes in the water leasing simulations, an MMS-PRMS hydrologic model was developed for a portion of the Middle Rio Grande Basin (MRGB) near Albuquerque, New Mexico. This portion of the MRGB contains a detailed network of diversions, canals, and drains that transport water through the system. In order to capture the complexity of the system, the model was developed using the highest resolution information available. In the model, each Hydrologic Response Unit (HRU) is represented as a trader. To achieve the 15 trader limit desired by economists, the model structure was simplified using two basic constraints; 1) HRUs having a common source and point of return to the river were lumped; and 2) HRUs with less than 20% agricultural land use were omitted from the auction simulations. A new Evapotranspiration (ET) module was implemented in the model to better estimate ET associated with different crops. Modules were also developed so that the end user has the flexibility to manipulate water deliveries based on crop type and land use. The MMS- PRMS model for the MRGB should help economists determine if the incentive to profit by selling or buying water can make more efficient use of the available water supply.

  4. New perspectives on the geometry of the Albuquerque Basin, Rio Grande rift, New Mexico: Insights from geophysical models of rift-fill thickness

    Grauch, V. J.; Connell, Sean D.


    Discrepancies among previous models of the geometry of the Albuquerque Basin motivated us to develop a new model using a comprehensive approach. Capitalizing on a natural separation between the densities of mainly Neogene basin fill (Santa Fe Group) and those of older rocks, we developed a three-dimensional (3D) geophysical model of syn-rift basin-fill thickness that incorporates well data, seismic-reflection data, geologic cross sections, and other geophysical data in a constrained gravity inversion. Although the resulting model does not show structures directly, it elucidates important aspects of basin geometry. The main features are three, 3–5-km-deep, interconnected structural depressions, which increase in size, complexity, and segmentation from north to south: the Santo Domingo, Calabacillas, and Belen subbasins. The increase in segmentation and complexity may reflect a transition of the Rio Grande rift from well-defined structural depressions in the north to multiple, segmented basins within a broader region of crustal extension to the south. The modeled geometry of the subbasins and their connections differs from a widely accepted structural model based primarily on seismic-reflection interpretations. Key elements of the previous model are an east-tilted half-graben block on the north separated from a west-tilted half-graben block on the south by a southwest-trending, scissor-like transfer zone. Instead, we find multiple subbasins with predominantly easterly tilts for much of the Albuquerque Basin, a restricted region of westward tilting in the southwestern part of the basin, and a northwesterly trending antiform dividing subbasins in the center of the basin instead of a major scissor-like transfer zone. The overall eastward tilt indicated by the 3D geophysical model generally conforms to stratal tilts observed for the syn-rift succession, implying a prolonged eastward tilting of the basin during Miocene time. An extensive north-south synform in the

  5. Review of the species of the genus Serrapinnus Malabarba, 1998 (Teleostei: Characidae: Cheirodontinae) from the rio Tocantins-Araguaia basin, with description of three new species.

    Malabarba, Luiz R; Jerep, Fernando C


    Species of the genus Serrapinnus from the rio Tocantins-Araguaia basin are revised and three new species are described. Serrapinnus aster new species is diagnosed by the presence of scimitar-shaped ventral procurrent caudal-fin rays of mature males forming a semicircle and by the presence of 7-9 cusps on the premaxillary teeth; S. lucindai new species is distinguished from its congeners by the presence of a higher number of ventral procurrent caudal-fin rays (17 to 19); and S. tocantinensis new species differs from the remaining species of the genus by the elongation of the unbranched dorsal and pelvic-fin rays into filaments in mature males. Serrapinnus sterbai is recognized as broadly distributed in the Tocantins-Araguaia basin and is redescribed based on specimens from across its entire distribution. A key for the cheirodontines occurring in the Atlantic drainages of northeastern Brazil, from the rio Tocantins-Araguaia to the rio Paraguaçú is provided.

  6. Web application to access U.S. Army Corps of Engineers Civil Works and Restoration Projects information for the Rio Grande Basin, southern Colorado, New Mexico, and Texas

    Archuleta, Christy-Ann M.; Eames, Deanna R.


    The Rio Grande Civil Works and Restoration Projects Web Application, developed by the U.S. Geological Survey in cooperation with the U.S. Army Corps of Engineers (USACE) Albuquerque District, is designed to provide publicly available information through the Internet about civil works and restoration projects in the Rio Grande Basin. Since 1942, USACE Albuquerque District responsibilities have included building facilities for the U.S. Army and U.S. Air Force, providing flood protection, supplying water for power and public recreation, participating in fire remediation, protecting and restoring wetlands and other natural resources, and supporting other government agencies with engineering, contracting, and project management services. In the process of conducting this vast array of engineering work, the need arose for easily tracking the locations of and providing information about projects to stakeholders and the public. This fact sheet introduces a Web application developed to enable users to visualize locations and search for information about USACE (and some other Federal, State, and local) projects in the Rio Grande Basin in southern Colorado, New Mexico, and Texas.

  7. A comprehensive survey of faults, breccias, and fractures in and flanking the eastern Española Basin, Rio Grande rift, New Mexico

    Caine, Jonathan S.; Minor, Scott A.; Grauch, V.J.S.; Budahn, James R.; Keren, Tucker T.


    A comprehensive survey of geologic structures formed in the Earth’s brittle regime in the eastern Española Basin and flank of the Rio Grande rift, New Mexico, reveals a complex and protracted record of multiple tectonic events. Data and analyses from this representative rift flank-basin pair include measurements from 53 individual fault zones and 22 other brittle structures, such as breccia zones, joints, and veins, investigated at a total of just over 100 sites. Structures were examined and compared in poorly lithified Tertiary sediments, as well as in Paleozoic sedimentary and Proterozoic crystalline rocks. Data and analyses include geologic maps; field observations and measurements; orientation, kinematic, and paleostress analyses; statistical examination of fault trace lengths derived from aeromagnetic data; mineralogy and chemistry of host and fault rocks; and investigation of fault versus bolide-impact hypotheses for the origin of enigmatic breccias found in the Proterozoic basement rocks. Fault kinematic and paleostress analyses suggest a record of transitional, and perhaps partitioned, strains from the Laramide orogeny through Rio Grande rifting. Normal faults within Tertiary basin-fill sediments are consistent with more typical WNW-ESE Rio Grande rift extension, perhaps decoupled from bedrock structures due to strength contrasts favoring the formation of new faults in the relatively weak sediments. Analyses of the fault-length data indicate power-law length distributions similar to those reported from many geologic settings globally. Mineralogy and chemistry in Proterozoic fault-related rocks reveal geochemical changes tied to hydrothermal alteration and nearly isochemical transformation of feldspars to clay minerals. In sediments, faulted minerals are characterized by mechanical entrainment with minor secondary chemical changes. Enigmatic breccias in rift-flanking Proterozoic rocks are autoclastic and isochemical with respect to their protoliths and

  8. A new species of Corydoras Lacépède (Siluriformes: Callichthyidae from the Rio Tapajós basin and its phylogenetic implications

    Vinicius C. Espíndola


    Full Text Available A new species of Corydoras is described from tributaries of the rio Arinos, rio Teles Pires and rio Preto, all in the rio Tapajós basin. The new species is a member of a group that includes 36 species with spots on the body. Within this group, the new species can be readily distinguished by having a smaller dorsal-fin spine than the first three subsequent soft dorsal-fin rays; pectoral, pelvic and anal fins hyaline; dorsal-fin interradial membrane hyaline; rounded spots on trunk restricted to dorsolateral body plates and dorsal portion of ventrolateral body plates, not reaching the base of pelvic and anal fins. The new species can be further distinguished from Corydoras xinguensis by having spots with diffuse edges, and from all other species of spotted Corydoras except C.multimaculatus, by the absence of ventral platelets. A phylogenetic analysis recovered the new species plus Corydoras metae and C.araguaiensis in a clade sharing the presence of a pointed process on the maxilla for insertion of the retractor tentaculi muscle. In addition, the presence in the new species of an elongated anterior portion of the mesethmoid and a triangular uncinate process of the epibranchial 3 suggests a close relationship with Corydoras metae.

  9. A new Hasemania Ellis from the upper rio Paraná basin, with the redescription of Hasemania crenuchoides Zarske & Géry (Characiformes: Characidae

    Jane Piton Serra

    Full Text Available A new Hasemania species is described from the headwaters of the rio Uberaba, rio Grande basin, State of Minas Gerais, Brazil. The new species is distinguished from its congeners by a combination of a black, vertically-elongate humeral spot, a single ossification in the position primitively occupied by infraorbitals four and five, four teeth on the inner series of premaxilla, and scales covering the anal-fin base. Hasemania crenuchoides is redescribed and its known geographic distribution is extended; it can be differentiated from other species of the genus by the combination of a black vertically-elongate humeral spot, ii,8 dorsal-fin rays, 11-14 branched anal-fin rays, the presence of separate infraorbitals four and five, and the presence of scales covering the anal-fin base. Phylogenetic relationships of H. crenuchoides and the new species within Hasemania are discussed.

  10. Phycocharax rasbora, a new genus and species of Brazilian tetra (Characiformes: Characidae) from Serra do Cachimbo, rio Tapajós basin.

    Ohara, Willian Massaharu; Mirande, Juan Marcos; de Lima, Flávio Cesar Thadeo


    A new genus and species of characid fish is described from rio Braço Norte, a tributary of rio Teles Pires, Tapajós basin, Mato Groso, Brazil. The new taxa can be diagnosed from the remaining characids by a unique combination of characters that includes the presence of a single row of relatively compressed premaxillary teeth, large teeth with four to nine cusps on premaxillary and dentary, absence of pseudotympanum, incomplete lateral line with 7-13 pored scales, sexually-dimorphic males with distal margin of anal fin approximately straight, and presence of a nearly triangular and horizontally elongated blotch from the posterior half of the body to caudal peduncle. The most parsimonious phylogenetic hypothesis, using morphological data, recovered the new genus and species in a clade including Paracheirodon axelrodi and Hyphessobrycon elachys.

  11. El elemento mitológico: uno de los factores intervinientes en las elecciones alimentarias. El caso de los matacos del pilcomayo. dto. Rivadavia, provincia de salta

    Graciela F. Torres


    Full Text Available En el presente artículo consideramos la influencia del horizonte mítico, en las elecciones y la perduración de las preferencias alimentarias en el grupo Mataco del Pilcomayo. Esta perduración se extiende, por lo menos, a lo largo de los últimos cuatrocientos años, pese a las múltiples influencias exógenas recibidas a lo largo de ese período. Utilizamos para el análisis la bibliografía etnográfica producida en los últimos veinticinco años, acerca de la mitología vinculada a los recursos alimenticios del grupo étnico que consideramos, y la información obtenida en nuestra investigación de campo durante 1998.

  12. Dispersal Syndromes of fossil Seeds from the Lower Permian of Paraná Basin, Rio Grande do Sul, Brazil

    Juliane M. Souza


    Full Text Available The morphological analysis of seeds has been an important subject in modern ecological studies, once it provides evidence about the biology and adaptations of the parent plant. However, this kind of study has been restricted to the ecology of modern plants and is rarely used in interpretations of Paleozoic data. From the understanding of dispersal syndromes analysis as an important tool to paleoecological reconstruction, this study provides a first approach using this tool with seeds from the Lower Permian strata of southern Paraná Basin in Rio Grande do Sul. Based on previously classified seeds and using their biological and taphonomic data, the syndrome of dispersal was interpreted, and their placement in successional groups (pioneer, early-successional and later-successional was suggested. Seven morphospecies were analyzed: Samaropsis gigas, representing a later-successional species living in water bodies with hydrochory as its dispersal syndrome; Samaropsis kurtzii, typical of early-successional species showing anemochory as its dispersal syndrome and living in distal areas in relation to water bodies; Samaropsis aff. S. millaniana, Cordaicarpus aff. C. brasilianus, Cordaicarpus cerronegrensis and Cordaicarpus truncata have typical characteristics of pioneer plants, exhibiting barochory as their primary dispersal syndrome with other syndromes associated.A Análise morfológica das sementes tem sido um importante objeto em estudos ecológicos modernos, uma vez que fornece evidências sobre a biologia e as adaptações das plantas-mãe de sementes. Entretanto, este tipo de estudo tem sido restrito a ecologia de plantas modernas e é raramente utilizado em interpretações de dados paleozóicos. A partir do entendimento da análise das sindromes de dispersão como uma importante ferramenta para reconstruções paleoecológicas, este estudo oferece uma primeira abordagem utilizando essa ferramenta com sementes do Permiano Inferior do Sul da

  13. New species of Bryconamericus Eigenmann (Characiformes: Characidae) from the rio Teles Pires, rio Tapajós basin, central Brazil.

    Dagosta, Fernando C P; Netto-Ferreira, André L


    A new species of Bryconamericus is described from the rio Teles Pires, a tributary of the rio Tapajós. The new taxon can be distinguished from its congeners by having a short anal fin with 11-13 branched rays, two maxillary teeth, four outer premaxillary teeth, and 34-38 perforated lateral-line scales. Other diagnostic characters of the species are the absence of a caudal-peduncle spot and the presence of a pigmented vertical band at the caudal-fin rays base. The phylogenetic position of the new species is inferred based in two available phylogenetic hypotheses, and a discussion on its generic placement is provided. 

  14. A new species of Rhinopetitia Géry 1964 (Ostariophysi: Characiformes: Characidae) from the Rio Teles Pires, Rio Tapajós basin, Brazil.

    Netto-Ferreira, A L; Birindelli, J L O; Sousa, L M; Menezes, N A


    A new species of Rhinopetitia is described from the Rio Teles Pires, a major tributary of the Rio Tapajós. The new taxon is distinguished from its only congener, Rhinopetitia myersi, by having all premaxillary teeth in both rows with seven to nine cusps, maxillary teeth with seven or eight cusps, a distinct dark midlateral stripe on the body and a round humeral blotch (v. outer series of premaxillary teeth with three cusps and inner series of premaxillary teeth with three to five cusps, maxillary teeth with three to five cusps, the absence of a dark midlateral stripe and humeral blotch). Putative characters suggesting a close relationship between Rhinopetitia, Bryconacidnus, Ceratobranchia, Monotocheirodon, Odontostoechus, Othonocheirodus and Rhinobrycon are presented. This putative clade is included in the Stevardiinae, a monophyletic group within the Characidae. © 2014 The Fisheries Society of the British Isles.

  15. A Conceptual Model to Link Anomalously High Temperature Gradients in the Cerros del Rio Volcanic Field to Regional Flow in the Espanola Basin, New Mexico

    Fillingham, E. J.; Keller, S. N.; McCullough, K. R.; Watters, J.; Weitering, B.; Wilce, A. M.; Folsom, M.; Kelley, S.; Pellerin, L.


    Temperature-depth well data along with electromagnetic (EM) data were collected by students of the Summer of Applied Geophysics Experience (SAGE) 2015 field season in the Espanola Basin, New Mexico. The data from this year, in addition to data acquired since 2013, were used to construct a conceptual east-west cross-section of the Espanola Basin and the adjacent highlands in order to evaluate the regional flow system. Vertical geothermal gradients from several monitoring wells were measured using a thermistor. Anomalously warm geothermal gradients were mapped in the Cerros del Rio volcanic field in the basin just east of the Rio Grande. Temperature gradients are up to 70℃/km, while the background geothermal gradients in the Rio Grande rift zone generally show 28℃-35℃/km. This anomaly extends to the Buckman well field, which supplies water to the city of Santa Fe. Overpumping of this well field has led to subsidence in the past. However, discharge temperature plots indicate that the temperature gradients of the Buckman field may be rebounding as pumping is reduced. Audiomagnetotelluric (AMT) and transient electromagnetic (TEM) data were acquired in the vicinity of three monitoring wells. TEM and AMT methods complement each other with the former having depths of investigation of less than ten to hundreds of meters and AMT having depths of investigation comparable to the wells deeper than 500m. These datasets were used collectively to image the subsurface stratigraphy and, more specifically, the hydrogeology related to shallow aquifers. The EM data collected at these wells showed a trend indicating a shallow aquifer with a shallower resistive layer of approximately 100 ohm-m at 70-100 meters depth. Beneath this resistive layer we resolved a more conductive, clay-rich layer of 10 ohm-m. These resistivity profiles compliment the electrical logs provided by Jet West, which indicate shallower sandstone interbedded with silt on top of more silt-dominant layers. Our

  16. Two new species of Hyphessobrycon (Teleostei: Characidae from upper rio Tapajós basin on Chapada dos Parecis, central Brazil

    Tiago Pinto Carvalho

    Full Text Available Two new species of Hyphessobrycon are described from the upper rio Tapajós basin, Mato Grosso, Brazil. Hyphessobrycon melanostichos is distinguished from its congeners by the combination of a conspicuous longitudinal broad black band beginning on the posterior margin of orbit and reaching the tip of middle caudal fin rays, a distinct vertically elongate humeral spot, and 16 to 18 branched anal-fin rays. Hyphessobrycon notidanos is distinguished from its congeners by the combination of an elongate dorsal fin in mature males, a vertically elongate humeral spot, 2-4 maxillary teeth, iii,8 dorsal-fin rays, and 16 to 21 branched anal-fin rays.

  17. Zinc and copper behaviour at the soil-river interface: New insights by Zn and Cu isotopes in the organic-rich Rio Negro basin

    Guinoiseau, Damien; Gélabert, Alexandre; Allard, Thierry; Louvat, Pascale; Moreira-Turcq, Patricia; Benedetti, Marc F.


    The complex behaviour of Zn and Cu at the soil-river interface was investigated in soil and riverine water samples from the Rio Negro basin, a secondary tributary of the Rio Amazonas, using their stable isotope compositions. This acidic and organic river drains two types of intensely weathered terrains: podzols in its upstream part, and lateritic soils downstream. Bulk soil particles, suspended particulate matter (SPM) as well as colloidal fractions were sampled across the whole basin during low and high water stages. In the basin, Zn and Cu are mostly exported from lateritic soils and transported by organic colloids where significant losses are observed in the downstream part of the river. The use of δ66Zn and δ65Cu measurements reveals distinct stories for these two metals in suspended sediments and colloids. In the colloids, the constant δ66Zncoll across the basin is induced by the same weak association mode between Zn and organic ligands, regardless of the origin of the water. By contrast, in SPM, the speciation of Zn and thus δ66ZnSPM differ according to the type of drained soils. Zn is associated with organic complexes in particles exported with water draining podzol whereas Zn2+ is incorporated in the structure of the remaining kaolinite clays in lateritic output. The stronger reactivity of Cu than Zn with organic ligands induces its complete complexation. Copper is controlled by refractory particulate organic matter (POM) and by reactive colloidal organic matter; the latter being enriched in 65Cu due to stronger binding interactions than in POM. While the Cu content remains constant in the upstream part of the Rio Negro, downstream, the decrease of SPM and colloidal Cu fluxes is associated with a constant δ65CuSPM and with an increase of δ65Cucoll at the Rio Negro outlet. Geochemical mass balance modelling, based on SPM, Cu and Zn fluxes in SPM and their associated isotopic signatures, confirms distinct host phases for Zn and Cu, and identifies the

  18. A new species of Microglanis(Siluriformes: Pseudopimelodidae from the upper rio Tocantins basin, Goiás State, Central Brazil

    Oscar Akio Shibatta

    Full Text Available A new species of Microglanis is described from the upper rio Tocantins basin, Barro Alto, Goiás State, Brazil. This species is distinguished from the others by presenting a unique color pattern, consisting of round spots in the flank between the larger dark brown blotches. Moreover, it can be distinguished by the combination of the following features: caudal fin emarginate, the upper lobe slightly larger than the lower, lateral line relatively long, reaching vertical through posterior margin of the pelvic fin, and light stripe on supra-occipital region absent or very narrow and with irregular shape.

  19. Groundwater vulnerability in the Arroyo Feliciano basin. Entre Rios. Argentina; Vulnerabilidad del agua subterranea en la cuenca del Arroyo Feliciano. Entre Rios. Argentina

    Diaz, E. L.; Romero, E. C.; Boschetti, N. G.; Duarte, O. C.


    The study area includes the basin of the Feliciano stream (Arroyo Feliciano) which increasing water resources are affected by the agriculturization rise and the change of soil usage. The 8.199,4 km{sup 2} basin is undergoing a sudden change in the soil usage that goes from an extensive cattle production to intensive rice soybean usage. It has an urban population of approximately 11,600 inhabitants and there are a low number of rural settlers. It is unknown if there is pollution produced by agricultural activity. The objective of this paper is to estimate the pollution vulnerability of the aquifers used for supplying water for human consumption to the towns within the basin; irrigation and watered of animals, fundamentally cattle. There are two internationally standard-considered methods that have been used, known as DRASTIC and GOD, in order to establish the capacity of attenuation of pollutants for elimination, delay and dilution, for agrochemical and fertilizers set in the surface. The outcomes of the application of both methodologies indicate that there is high vulnerability to pollution areas which are in the surroundings of the minor riverbeds and the main course of the Feliciano stream, where the depth to the aquifers is minimal. In the rest of the basin the effect that offers the thickness of the silts and clay of the Hernandarias formation, operates protecting the aquifer. (Author) 12 refs.

  20. Origin and evolution of phyllosilicate deformation bands in the poorly lithified sandstones of the Rio do Peixe Basin, NE Brazil

    Nogueira, Francisco; Nicchio, Matheus; Balsamo, Fabrizio; Bezerra, Francisco; Souza, Jorge; Carvalho, Bruno; Storti, Fabrizio


    In this work we describe the genetic processes and the microstructural evolution of phylossilicate deformation bands developed in poorly lithified, high porosity sandstones of the Rio do Peixe Basin, Northeast Brazil. The studied deformation bands occur in damage zones of NE-SW and NW-SE transtensional faults that exhibit well developed anastomosed clusters, with a thickness varying from tens of centimeters to 1 meter. The Host rocks are arkosic to lithic arkosic coarse sandstones to fine conglomerate and with less than 1% of clay content in the matrix. Based on (i) field observations, (ii) clay amount in deformation band cores and (iii) clay mineral arrangements in deformation bands cores, we identified two types of phyllosilicate deformation bands: (1) clay smearing deformation bands and (2) phyllosilicate deformation bands formed by clay authigenesis. The former occur only in fault zones that cut across clay-rich layers and are characterized by 45-50% of clay content. Single element chemical analysis indicates that the composition of clay minerals in clay smearing deformation bands is similar to that of clay-rich layers in the host rocks. The dominant deformation mechanism is particulate flow, which produces preferential alignments of grains and clay minerals. Only subordinate cataclasis occurs. Based on microstructural fabrics, three evolutionary stages can be identified for phyllosilicate deformation bands formed by clay authigenesis. The first one is characterized by preferentially cataclasis and weathering of feldspars. Clay concentration is relatively low, reaching 15-20%, with preferential concentration where crushed feldspar abundance is higher. The second stage is characterized by clay migration within deformation bands, to form continuous films with more than 20-25% of clay concentration. In the last stage clay mineral fabric re-organization occurs, forming well a developed S-C foliation. Clay concentration exceeds 35%. Single element chemical analysis

  1. Temporal and spatial constraints on the evolution of a Rio Grande rift sub-basin, Guadalupe Mountain area, northern New Mexico

    Thompson, R. A.; Turner, K. J.; Cosca, M. A.; Drenth, B.; Hudson, M. R.; Lee, J.


    The Taos Plateau volcanic field (TPVF) in the southern San Luis Valley of northern New Mexico is the most voluminous of the predominantly basaltic Neogene (6-1 Ma) volcanic fields of the Rio Grande rift. Volcanic deposits of the TPVF are intercalated with alluvial deposits of the Santa Fe Group and compose the N-S-trending San Luis Basin, the largest basin of the northern rift (13,500 km2 in area). Pliocene volcanic rocks of the Guadalupe Mountain area of northern New Mexico are underlain by the southern end of one of the larger sub-basins of the San Luis Valley, the Sunshine sub-basin (~ 450 km2 in area) juxtaposed against the down-to-west frontal fault of the Precambrian-cored Sangre de Cristo Range. The sub-basin plunges northward and extends to near the Colorado-New Mexico border. The western margin (~15 km west of the Sangre de Cristo fault) is constrained by outcrops of Oligocene to Miocene volcanic rocks of the Latir volcanic field, interpreted here as a broad pre-Pliocene intra-rift platform underlying much of the northern TPVF. The southern sub-basin border is derived, in part, from modeling of gravity and aeromagnetic data and is interpreted as a subsurface extension of this intra-rift platform that extends southeastward to nearly the Sangre de Cristo range front. Broadly coincident with this subsurface basement high is the northwest-trending, curvilinear terminus of the down-to-northeast Red River fault zone. South of the gravity high, basin-fill alluvium and ~3.84 Ma Servilleta basalt lava flows thicken along a poorly exposed, down-to-south, basin-bounding fault of the northern Taos graben, the largest of the San Luis Valley sub-basins. The uppermost, western sub-basin fill is exposed along steep canyon walls near the confluence of the Rio Grande and the Red River. Unconformity-bound, lava flow packages are intercalated with paleo Red River fan alluvium and define six eruptive sequences in the Guadalupe Mountain area: (1) Guadalupe Mtn. lavas (dacite ~5

  2. Combined land use and climate change impact on Surface and Ground water resources in the Rio Cobre and Great River basin, Jamaica

    Setegn, S. G.; Melesse, A. M.; Grey, O.; Webber, D.


    Possible adverse impacts of land use and climate change on one hand and population pressure, extended droughts, and environmental degradation on the other hand are major factors limiting water resources availability in the watersheds of Jamaica. The main objective of this study is to analyze the combined impact of land use/ land cover changes as well as climate change on the hydrological processes and water recourses availability in the Rio Cobre and Great River basins. A spatially distributed model SWAT was calibrated and validated in the basin and used for the study of land use and climate change impacts in the watersheds. Different land cover types were tested to analyze its impact on the hydrology of the watershed. The main land cover parameters considered within the Great and Rio Cobre River Watershed includes Agriculture, Tourism, Water, Road Infrastructure, Population, Forestry and land cover Information. The outputs of different Global climate model (GCM) were downscaled to the watershed level and used for assessing the impact of climate change on water resources availability in the area. The analysis of climate change impact on the surface and ground water resources of the basin indicated that the basin will experience a change in water balance due to changes in the major climate variables in the forthcoming decades. The direction of streamflow change follows mainly the direction of changes in rainfall. Many of the models show statistically-significant declines in mean annual streamflow (up to 60% reduction in streamflow) for the different time-periods and scenarios. The combined effect of climate and land-use/land-cover change on the hydrological processes and water recourses variability is an important step to develop sustainable adaptation strategy.


    Gabriela de Paula


    Full Text Available The aim of this paper is to evaluate the water availability of the Piracicaba river basin, comparing water consumption data, both actual and future, with the analyses of outflows (monthly average, minimum and maximum figures from the existing DAEE/CTH monitoring program. Extensive analysis was carried out of existing information, both in relation to consumption as well as of user profile, in scientific publications, technical reports, and water availability plans and the information was brought up-to-date with the help of the relevant government regulatory bodies and interviews with consumers. The Piracicaba river basin has a drainage area of 12,400 Km2, of which 90% is situated in the State of Sao Paulo, with the remaining 10% being in the States of Minas Gerais and Rio de Janeiro. The Piracicaba river basin’s population comes to a total of 3.1 million people (SEADE 1998. The average water availability in the basin is 165m3/s, dropping to 40 m3/s in periods of drought. The Cantareira System, which carries the waters of the basin to Sao Paulo’s Metropolitan Region, has not been maintaining the minimum outflow (40m3/s established for the Piracicaba River. Urban usage (11.2 m3/s and industrial usage (9.9 m3/s account for 81% of the water consumption in the Piracicaba Basin, while usage for irrigation purposes represents a further 19% (25m3/s. There is a trend towards stabilization in terms of industrial consumption and growth in urban consumption (+2% per year and in consumption for irrigation purposes (+1.34% per year, resulting in a yearly increase in demand of 0.35 m3/s. An examination of river surface discharge levels suggests that the Jaguari river sub basin has the highest discharge values available, 23.4 m3/s. During just 13% of the year, this river does not have a sufficient level of discharge to maintain an outflow rate of 40m3/s in the Piracicaba river, near the city bearing the same name. = O presente artigo visa avaliar a

  4. Corydoras tukano, a new species of corydoradine catfish from the rio Tiquié, upper rio Negro basin, Brazil (Ostariophysi: Siluriformes: Callichthyidae

    Marcelo R. Britto

    Full Text Available A new Corydoras species from the rio Tiquié, upper rio Negro system, Amazonas, Brazil, is described. This taxon was previously referred to as "Corydoras species 'Asher'", "Corydoras cf. reynoldsi", and "Corydoras aff. reynoldsi" in the aquarist literature. The new taxon can be distinguished from all its congeners, except Corydoras reynoldsi and C. weitzmani, by its color pattern, consisting of three large, dark blotches, the first one ("mask" on the head, across the eye; the second one on the trunk at the level of dorsal fin; and the third one on the trunk at the level of the adipose fin. It can be distinguished from Corydoras reynoldsi mainly by the development of trunk blotches; and from C. weitzmani by the presence of a dusky saddle between the dorsal and adipose fins, the second trunk blotch extending vertically from the adipose-fin base to the anal-fin base, and the presence of four dark stripes in the caudal fin.

  5. Quality of water and sediment in streams affected by historical mining, and quality of Mine Tailings, in the Rio Grande/Rio Bravo Basin, Big Bend Area of the United States and Mexico, August 2002

    Lambert, Rebecca B.; Kolbe, Christine M.; Belzer, Wayne


    The U.S. Geological Survey, in cooperation with the International Boundary and Water Commission - U.S. and Mexican Sections, the National Park Service, the Texas Commission on Environmental Quality, the Secretaria de Medio Ambiente y Recursos Naturales in Mexico, the Area de Proteccion de Flora y Fauna Canon de Santa Elena in Mexico, and the Area de Proteccion de Flora y Fauna Maderas del Carmen in Mexico, collected samples of stream water, streambed sediment, and mine tailings during August 2002 for a study to determine whether trace elements from abandoned mines in the area in and around Big Bend National Park have affected the water and sediment quality in the Rio Grande/Rio Bravo Basin of the United States and Mexico. Samples were collected from eight sites on the main stem of the Rio Grande/Rio Bravo, four Rio Grande/Rio Bravo tributary sites downstream from abandoned mines or mine-tailing sites, and 11 mine-tailing sites. Mines in the area were operated to produce fluorite, germanium, iron, lead, mercury, silver, and zinc during the late 1800s through at least the late 1970s. Moderate (relatively neutral) pHs in stream-water samples collected at the 12 Rio Grande/Rio Bravo main-stem and tributary sites indicate that water is well mixed, diluted, and buffered with respect to the solubility of trace elements. The highest sulfate concentrations were in water samples from tributaries draining the Terlingua mining district. Only the sample from the Rough Run Draw site exceeded the Texas Surface Water Quality Standards general-use protection criterion for sulfate. All chloride and dissolved solids concentrations in water samples were less than the general-use protection criteria. Aluminum, copper, mercury, nickel, selenium, and zinc were detected in all water samples for which each element was analyzed. Cadmium, chromium, and lead were detected in samples less frequently, and silver was not detected in any of the samples. None of the sample concentrations of

  6. Using cosmogenic nuclides to contrast rates of erosion and sediment yield in a semi-arid, arroyo-dominated landscape, Rio Puerco Basin, New Mexico

    Bierman, P.R.; Reuter, J.M.; Pavich, M.; Gellis, A.C.; Caffee, M.W.; Larsen, J.


    Analysis of in-situ-produced 10Be and 26Al in 52 fluvial sediment samples shows that millennial-scale rates of erosion vary widely (7 to 366 m Ma-1) through the lithologically and topographically complex Rio Puerco Basin of northern New Mexico. Using isotopic analysis of both headwater and downstream samples, we determined that the semi-arid, Rio Puerco Basin is eroding, on average, about 100 m Ma-1. This rapid rate of erosion is consistent with estimates made using other techniques and is likely to result from a combination of easily eroded lithologies, sparse vegetation, and monsoon-dominated rainfall. Data from 331 stream water samples collected by the US Geological Survey between 1960 and 1995 are consistent with basin-wide, average chemical denudation rates of only about 1??4 m Ma-1; thus, the erosion rates we calculate may be considered rates of sediment generation because physical weathering accounts for almost 99 per cent of mass loss. The isotopic data reveal that sediment is generally well mixed downstream with the area-weighted average sediment generation rate for 16 headwater samples (234 ton km-2 a-1 for basin area 170 to 1169 km2) matching well that estimated from a single sample collected far downstream (238 ton km-2 a-1, basin area = 14 225 km2). A series of 15 samples, collected from an arroyo wall and representing deposition through the late Holocene, indicates that 10Be concentration in sediment delivered by the fluvial system has not changed appreciably over the last 1200 years despite at least two cycles of arroyo cutting and filling. Other samples (n = 21) were collected along the drainage network. Rio Puerco erosion rates scale directly with a variety of metrics describing vegetation, precipitation, and rock erodibility. Using the headwater basins for calibration, the erosion rates for both the downstream samples and also the data set as a whole, are best modelled by considering a combination of relief and vegetation metrics, both of which co

  7. Design and Compilation of a Geodatabase of Existing Salinity Information for the Rio Grande Basin, from the Rio Arriba-Sandoval County Line, New Mexico, to Presidio, Texas, 2010

    Shah, Sachin D.; Maltby, David R.


    The U.S. Geological Survey, in cooperation with the U.S. Army Corps of Engineers, compiled salinity-related water-quality data and information in a geodatabase containing more than 6,000 sampling sites. The geodatabase was designed as a tool for water-resource management and includes readily available digital data sources from the U.S. Geological Survey, U.S. Environmental Protection Agency, New Mexico Interstate Stream Commission, Sustainability of semi-Arid Hydrology and Riparian Areas, Paso del Norte Watershed Council, numerous other State and local databases, and selected databases maintained by the University of Arizona and New Mexico State University. Salinity information was compiled for an approximately 26,000-square-mile area of the Rio Grande Basin from the Rio Arriba-Sandoval County line, New Mexico, to Presidio, Texas. The geodatabase relates the spatial location of sampling sites with salinity-related water-quality data reported by multiple agencies. The sampling sites are stored in a geodatabase feature class; each site is linked by a relationship class to the corresponding sample and results stored in data tables.

  8. Harttia absaberi, a new species of loricariid catfish (Siluriformes: Loricariidae: Loricariinae from the upper rio Paraná basin, Brazil

    Osvaldo Takeshi Oyakawa

    Full Text Available A new species of Harttia, tribe Harttiini, is described from tributaries of upper portions of rio Paraná drainage. The new species, the smallest known species of the genus, attaining up to 74.0 mm of standard length, can be distinguished from its congeners by the combination of the following characters: abdomen completely covered by plates, a single preanal plate, plates of the gular area in broad contact with the canal plate. Harttia absaberi is the second species of the genus known from the upper portion of rio Paraná drainage.

  9. Understanding Changes in Water Availability in the Rio Grande/Rio Bravo del Norte Basin Under the Influence of Large-Scale Circulation Indices Using the Noah Land Surface Model

    Khedun, C. Prakash; Mishra, Ashok K.; Bolten, John D.; Beaudoing, Hiroko K.; Kaiser, Ronald A.; Giardino, J. Richard; Singh, Vijay P.


    Water availability plays an important role in the socio-economic development of a region. It is however, subject to the influence of large-scale circulation indices, resulting in periodic excesses and deficits. An assessment of the degree of correlation between climate indices and water availability, and the quantification of changes with respect to major climate events is important for long-term water resources planning and management, especially in transboundary basins as it can help in conflict avoidance. In this study we first establish the correlation of the Pacific Decadal Oscillation (PDO) and El Nino-Southern Oscillation (ENSO) with gauged precipitation in the Rio Grande basin, and quantify the changes in water availability using runoff generated from the Noah land surface model. Both spatial and temporal variations are noted, with winter and spring being most influenced by conditions in the Pacific Ocean. Negative correlation is observed at the headwaters and positive correlation across the rest of the basin. The influence of individual ENSO events, classified using four different criteria, is also examined. El Ninos (La Ninas) generally cause an increase (decrease) in runoff, but the pattern is not consistent; percentage change in water availability varies across events. Further, positive PDO enhances the effect of El Nino and dampens that of La Nina, but during neutral/transitioning PDO, La Nina dominates meteorological conditions. Long El Ninos have more influence on water availability than short duration high intensity events. We also note that the percentage increase during El Ninos significantly offsets the drought-causing effect of La Ninas.

  10. Usage and administration manual for a geodatabase compendium of water-resources data-Rio Grande Basin from the Rio Arriba-Sandoval County line, New Mexico, to Presidio, Texas, 1889-2009

    Burley, Thomas E.


    The U.S. Geological Survey, in cooperation with the New Mexico Interstate Stream Commission, developed a geodatabase compendium (hereinafter referred to as the 'geodatabase') of available water-resources data for the reach of the Rio Grande from Rio Arriba-Sandoval County line, New Mexico, to Presidio, Texas. Since 1889, a wealth of water-resources data has been collected in the Rio Grande Basin from Rio Arriba-Sandoval County line, New Mexico, to Presidio, Texas, for a variety of purposes. Collecting agencies, researchers, and organizations have included the U.S. Geological Survey, Bureau of Reclamation, International Boundary and Water Commission, State agencies, irrigation districts, municipal water utilities, universities, and other entities. About 1,750 data records were recently (2010) evaluated to enhance their usability by compiling them into a single geospatial relational database (geodatabase). This report is intended as a user's manual and administration guide for the geodatabase. All data available, including water quality, water level, and discharge data (both instantaneous and daily) from January 1, 1889, through December 17, 2009, were compiled for the study area. A flexible and efficient geodatabase design was used, enhancing the ability of the geodatabase to handle data from diverse sources and helping to ensure sustainability of the geodatabase with long-term maintenance. Geodatabase tables include daily data values, site locations and information, sample event information, and parameters, as well as data sources and collecting agencies. The end products of this effort are a comprehensive water-resources geodatabase that enables the visualization of primary sampling sites for surface discharges, groundwater elevations, and water-quality and associated data for the study area. In addition, repeatable data processing scripts, Structured Query Language queries for loading prepared data sources, and a detailed process for refreshing all data in the

  11. Miniature catfishes of the genus Gelanoglanis (Siluriformes: Auchenipteridae: monophyly and the description of a new species from the upper rio Tapajós basin, Brazil

    Bárbara B. Calegari

    Full Text Available Previously proposed synapomorphies for the genus Gelanoglanis of the catfish family Auchenipteridae are evaluated and four additional features involving the relationship between the mesethmoid and premaxilla, the very fleshy anterior portion of the snout, the lack of ossification of the second through fourth infraorbitals, and the incomplete poring of the lateral line are hypothesized as synapomorphic for the members of the genus. A new species of Gelanoglanis is described based on a series of specimens collected in the rio Teles Pires, a tributary of the rio Tapajós in the southern reaches of the Amazon basin. The new species demonstrates a number of features unusual within Gelanoglanis including a fontanel bordered by the frontals, a particularly elongate gonopodium in mature males, reductions in the dentition on the premaxilla, and a shorter posterior extension of the maxilla inside the maxillary barbel. The new species is a miniature as evidenced both by its body size and the reductions of various ossifications of the head, the number of fin rays and of the laterosensory canal system on the head and body. Sinapomorfias propostas previamente para o gênero Gelanoglanisda família Auchenipteridae são avaliadas e quatro características adicionais que envolvem a relação entre o mesetmóide e a pré-maxila, a porção anterior do focinho carnosa, a perda de ossificação do segundo ao quarto infraorbital e linha lateral incompleta são hipotetizadas como sinapomórficas para os membros do gênero. Uma espécie nova de Gelanoglanis é descrita com base em uma série de exemplares coletados no rio Teles Pires, um tributário do rio Tapajós na porção sul da bacia Amazônica. A espécie nova possui várias características incomuns dentro de Gelanoglanis, incluindo uma fontanela bordeada pelos frontais, um gonopódio particularmente longo em machos maduros, redução da dentição na premaxila, e extensão posterior da maxila mais curta

  12. Calibration and Uncertainty of a Water Surface Model for a Large Basin in a Semiarid Region: The Rio Yaqui-Basin, Mexico.

    Munoz-Hernandez, A.; Mayer, A. S.


    This work consists of developing an integrated hydrologic-institutional water model of the Yaqui basin, to support decision-makers in managing developments as it relates to sustaining water supplies and minimizing impacts to the environment. The basin has an arid to semi-arid climate and consists of roughly 72,000 square kilometers of land, primarily in northwest Mexico. The first objective of this work is to develop a detailed surface water flow model. The model is based on a link- node concept, where each sub-basin is delineated using DEM data; runoff within each sub-basin is lumped into a single outflow point. The node-link network includes the three primary reservoirs within the basin, as well as the various canals of the main agricultural area in the Yaqui Valley. The network also includes nodes where all diversions occur. Most of these diversions are regulated by water rights. Precipitation data for the basin was interpolated using data collected from 43 weather stations on a monthly basis over 25 years. Distributions of static runoff coefficients were generated based on published regional maps. The product of the precipitation and runoff coefficients were determined using GIS on a pixel-by-pixel basis to determine the monthly hypothetical runoff. The monthly runoff data was merged into climatic seasons. The GIS-based seasonal runoff was further adjusted by calibrating against 25 years of seasonal inflow data collected at each of the three primary reservoirs along the river. The calibration involves fitting a simple empirical model that relates the GIS-based runoff to the reservoir inflows. The calibration is difficult due to the following factors: (a) the procedure involves merging sporadic, short-duration, and intense precipitation-runoff events to create seasonal estimates of runoff; (b) the seasonal precipitation varies significantly from year to year; and (c) potential errors in the historical reservoir inflow data. We assess the agreement between the

  13. Mammal assemblage of the agroecosystem constituents of the Várzea River Basin, Rio Grande do Sul, Brazil doi: 10.5007/2175-7925.2010v23n4p91

    Felipe Bortolotto Peters


    Full Text Available We provide recent information on the richness of mammals along the agroecosystems of the Rio da Várzea Basin, Rio Grande do Sul, Brazil. We used different fi eld techniques to confi rm the occurrence of 46 mammal species in this area. Nine species are threatened in at least one of the three "red lists" at state, national and global levels. Adding the up-to-date results obtained in the fi eld to available data, mainly for conservation units, we present a richness of 85 species recorded for the basin. This number represents about 50% of mammals documented for Rio Grande do Sul state. The results suggest the importance of maintaining protected areas in altered regions, confi rming the relevance of inventories of local fauna as a fi rst approach to specifi c studies addressed to distribution, systematics, cytogenetics, physiology, population and community ecology.

  14. Environmental evolution of the Rio Grande drainage basin and Nasca region (Peru) in 2003-2007 using ENVISAT ASAR and ASTER time series

    Cigna, Francesca; Tapete, Deodato; Lasaponara, Rosa; Masini, Nicola


    Recent palaeo-environmental studies and remote sensing investigations demonstrated that the Rio Grande drainage basin in Southern Peru is a still evolving landscape, and impacts due to its changes have implications for the preservation of both the natural and cultural features of the Nasca region, well-known for the evidences of the ancient Paracas and Nasca Civilizations, who flourished from the 4th century BC to the 6th century AD. To image the modifications occurred in the last decade, we exploited the entire 4year-long stack of ENVISAT ASAR C-band archive imagery available over the region, which was provided by the European Space Agency (ESA) via the Cat-1 project 11073. The latter supports the activities of the Italian mission of heritage Conservation and Archaeogeophysics (ITACA), which directly involve researchers from the Institute for Archaeological and Monumental Heritage (IBAM) and the Institute of Methodologies for Environmental Analysis (IMAA), National Research Council (CNR) of Italy. With the aim of reconstructing the temporal evolution of the Rio Grande drainage basin and its effects and implications for the heritage of the region, we processed 8 ASAR Image Mode IS2 scenes acquired in descending mode between 04/02/2003 and 15/11/2005 and 5 images in ascending mode between 24/07/2005 and 11/11/2007, and focused on SAR backscattering information, amplitude change detection methods and extraction of ASAR-derived time series of the backscattering coefficient over target areas of interest. The ASAR 2003-2007 analysis was coupled and integrated with NDVI-based soil moisture and vegetation change assessment performed by using ASTER multi-spectral data acquired during the same time frame of the ASAR stacks, on 30/05/2003, 01/06/2004 and 10/06/2007. The research was performed both at the regional scale over the entire Rio Grande drainage basin, with particular focus on its tributaries Rio Ingenio, Rio Nazca and Rio Taruga, and at the local scale over the

  15. NAA: metals in surface waters, margin sediments, forage and cattle hair in flood plains of the Rio Doce basin, Minas Gerais, Brazil

    Vasconcelos, Maria Adelaide R.V., E-mail: [Universidade Fundacao Mineira de Educacao e Cultura (FUMEC), Belo Horizonte, MG (Brazil). Mestrado em Construcao Civil, Meio Ambiente; Barbosa, Ana Flavia S.; Ruckert, Gabriela V., E-mail: [Centro Universitario do Leste de Minas Gerais (UnilesteMG), Coronel Fabriciano, MG (Brazil). Mestrado em Engenharia Industrial; Menezes, Maria Angela B.C.; Silva, Maria Aparecida, E-mail:, E-mail: [Centro de Desenvolvimento da Tecnologia Nuclear (CDTN/CNEN-MG), Belo Horizonte, MG (Brazil); Oliveira, Arno H. de, E-mail: [Universidade Federal de Minas Gerais (UFMG), Departamento de Engenharia Nuclear Belo Horizonte, MG (Brazil)


    Metals are toxic and can cause damage to human health when they accumulate in the food chain. The aim of this study was to determine Al, As, Ba, Br, Ca, Ce, Cl, Co, Cr, Cs, Eu, Fe, Hg, K, Mg, Mn, Na, Rb, Sb, Sc, Ta, Th, Ti, U, V and Zn in different samples: surface waters, margin sediments, forages and cattle hairs in the region of the Rio Doce basin. The metals were analyzed by Neutron Activation Analysis - NAA at the Centre for Development of Nuclear Technology of the National Commission of Nuclear Energy - CDTN / CNEN. The sampling sites were taken at two points: P1- (Pingo D'agua - city, Ponte Queimada, in a no industrial area) and P2 - (Santana do Paraiso city, industrial and pasture areas, subject to frequent floods). The samples were collected in different seasons: July 2009 (dry season - winter) and February 2010 (rainy season - summer). These points were strategically chosen because P1 is located into the Parque Estadual do Rio Doce, considered a no industrial pollution region. Contrariwise, P2 is located in a region of high concentration of industries. In (P2) the Doce River receives its most polluted affluent upstream the Piracicaba River which is charged of several pollutants of industries of Steel Valley region, Brazil. In general, the results showed higher concentrations of the elements in P2 riverside area of livestock production and subject to flood. (author)

  16. Holocene landscape evolution and geoarcheology of low-order streams in the Rio Grande basin, San Juan Mountains, Colorado, USA

    Carver, Daniel P.; Beeton, Jared M.


    This geoarcheological study investigates soil stratigraphy and geochronology of alluvial deposits to determine Holocene landscape evolution within the Hot Creek, La Jara Creek, and Alamosa River drainage basins in the San Juan Mountains of Colorado. Geomorphic mapping and radiocarbon dating indicate synchronicity in patterns of erosion, deposition, and stability between drainage basins. In all three basins, the maximum age of mapped alluvial terraces and fans is ~ 3300 cal yr BP. A depositional period seen at both Hot Creek and the Alamosa River begins ~ 3300 to 3200 cal yr BP. Based on soil development, short periods of stability followed by alluvial fan aggradation occur in the Alamosa River basin ~ 2200 cal yr BP. A period of landscape stability at Hot Creek before ~ 1100 cal yr BP is followed by a period of rapid aggradation within all three drainages between ~ 1100 and 850 cal yr BP. A final aggradation event occurred between ~ 630 and 520 cal yr BP at La Jara Creek. These patterns of landscape evolution over the past ~ 3300 yr provide the framework for an archeological model that predicts the potential for buried and surficial cultural materials in the research area.

  17. Natural and human forcing in recent geomorphic change; case studies in the Rio de la Plata basin.

    Bonachea, Jaime; Bruschi, Viola M; Hurtado, Martín A; Forte, Luis M; da Silva, Mario; Etcheverry, Ricardo; Cavallotto, José L; Dantas, Marcilene F; Pejon, Osni J; Zuquette, Lázaro V; Bezerra, Maria Angélica de O; Remondo, Juan; Rivas, Victoria; Gómez-Arozamena, José; Fernández, Gema; Cendrero, Antonio


    An analysis of geomorphic system's response to change in human and natural drivers in some areas within the Río de la Plata basin is presented. The aim is to determine whether an acceleration of geomorphic processes has taken place in recent years and, if so, to what extent it is due to natural (climate) or human (land-use) drivers. Study areas of different size, socio-economic and geomorphic conditions have been selected: the Río de la Plata estuary and three sub-basins within its watershed. Sediment cores were extracted and dated ((210)Pb) to determine sedimentation rates since the end of the 19th century. Rates were compared with time series on rainfall as well as human drivers such as population, GDP, livestock load, crop area, energy consumption or cement consumption, all of them related to human capacity to disturb land surface. Data on river discharge were also gathered. Results obtained indicate that sedimentation rates during the last century have remained essentially constant in a remote Andean basin, whereas they show important increases in the other two, particularly one located by the São Paulo metropolitan area. Rates in the estuary are somewhere in between. It appears that there is an intensification of denudation/sedimentation processes within the basin. Rainfall remained stable or varied very slightly during the period analysed and does not seem to explain increases of sedimentation rates observed. Human drivers, particularly those more directly related to capacity to disturb land surface (GDP, energy or cement consumption) show variations that suggest human forcing is a more likely explanation for the observed change in geomorphic processes. It appears that a marked increase in denudation, of a "technological" nature, is taking place in this basin and leading to an acceleration of sediment supply. This is coherent with similar increases observed in other regions.

  18. The Pilagá of the Argentine Chaco through an exoticizing and ethnographic lens: The Swedish documentary film Following Indian trails by the Pilcomayo River

    Anne Gustavsson


    Full Text Available In this article, we explore how traveling relates to image production and how transcultural filmic representations both uphold and are sustained by a “coloniality of seeing.” We pay special attention to the historical conditions of film making in an expedition context and the expectations associated with early film in Sweden. We discuss this through the study of the documentary film Following Indian Trails by the Pilcomayo River, which was recorded during a Swedish expedition to the Argentine Chaco in 1920 and later released in Stockholm in 1950 during a private screening organized by the Swedish Chaco Travellers Association. We argue that the film presents an account inspired by classic ethnography which rescues and puts into circulation images of indigenous people from the “impenetrable” and “savage” Chaco. The ethnographic emphasis in the narrative seems to have shifted with time as it was probably only partly present during the shooting of the footage. In the narrative mode of “monstration,” when bodies meet machines “in the field,” native performances are presented as an “unstaged” and realist spectacle. Later in the 1950 macro-“narration,” encompassing the final cutting and editing of the original footage, fragments of spectacle are systematized into an ethnographic description of primitive life.

  19. Measured Copper Toxicity to Cnesterodon decemmaculatus (Pisces: Poeciliidae and Predicted by Biotic Ligand Model in Pilcomayo River Water: A Step for a Cross-Fish-Species Extrapolation

    María Victoria Casares


    Full Text Available In order to determine copper toxicity (LC50 to a local species (Cnesterodon decemmaculatus in the South American Pilcomayo River water and evaluate a cross-fish-species extrapolation of Biotic Ligand Model, a 96 h acute copper toxicity test was performed. The dissolved copper concentrations tested were 0.05, 0.19, 0.39, 0.61, 0.73, 1.01, and 1.42 mg Cu L-1. The 96 h Cu LC50 calculated was 0.655 mg L-1 (0.823-0.488. 96-h Cu LC50 predicted by BLM for Pimephales promelas was 0.722 mg L-1. Analysis of the inter-seasonal variation of the main water quality parameters indicates that a higher protective effect of calcium, magnesium, sodium, sulphate, and chloride is expected during the dry season. The very high load of total suspended solids in this river might be a key factor in determining copper distribution between solid and solution phases. A cross-fish-species extrapolation of copper BLM is valid within the water quality parameters and experimental conditions of this toxicity test.

  20. Las relaciones interétnicas en el Pilcomayo medio: la guerra indígena y sus transformaciones (1882-1938.

    Federico Bossert


    Full Text Available Se aborda la conformación étnica y las relaciones interétnicas en el Pilcomayo medio a través del análisis de relatos de exploradores, militares y misione- ros, registrando los cambios acaecidos desde fi nes del XIX hasta la primera mitad del XX. Los propósitos centrales son dos: por un lado, introducir com- plejidad en el análisis de las categorías étnicas, especialmente confusas en los documentos de los exploradores; por el otro, discutir la lógica de la guerra indígena relacionándola con la venganza y las relaciones de amistad y ene- mistad. Se argumenta que la guerra obedecía a cambiantes estrategias políti- cas las cuales, en función del contexto histórico, podían trocar la hostilidad en alianza y viceversa.

  1. Evaluation of geothermal potential of Rio Grande rift and Basin and Range province, New Mexico. Final technical report, January 1, 1977-May 31, 1978

    Callender, J.F.


    A study was made of the geological, geochemical and geophysical characteristics of potential geothermal areas in the Rio Grande rift and Basin and Range province of New Mexico. Both regional and site-specific information is presented. Data was collected by: (1) reconnaissance and detailed geologic mapping, emphasizing Neogene stratigraphy and structure; (2) petrologic studies of Neogene igneous rocks; (3) radiometric age-dating; (4) geochemical surveying, including regional and site-specific water chemistry, stable isotopic analyses of thermal waters, whole-rock and mineral isotopic studies, and whole-rock chemical analyses; and (5) detailed geophysical surveys, using electrical, gravity and magnetic techniques, with electrical resistivity playing a major role. Regional geochemical water studies were conducted for the whole state. Integrated site-specific studies included the Animas Valley, Las Cruces area (Radium Springs and Las Alturas Estates), Truth or Consequences region, the Albuquerque basin, the San Ysidro area, and the Abiquiu-Ojo Caliente region. The Animas Valley and Las Cruces areas have the most significant geothermal potential of the areas studied. The Truth or Consequences and Albuquerque areas need further study. The San Ysidro and Abiquiu-Ojo Caliente regions have less significant geothermal potential. 78 figs., 16 tabs.

  2. Multi thematic geoprocessing and structural analysis on Irati - Rio Bonito Petroleum System, Parana Basin, Brazil; Geoprocessamento multitematico e analise estrutural no Sistema Petrolifero Irati - Rio Bonito, Bacia do Parana

    Freitas, Rafael Correia de [Universidade Federal do Parana (UFPR), Curitiba, PR (Brazil). Dept. de Geologia. Lab. de Analise de Bacias e Petrofisica], E-mail:; Rostirolla, Sidnei Pires; Ferreira, Francisco Jose Fonseca


    Structural features associated with aspects like migration routes, fluid convergence and/or barriers and seal integrity, among others, may be evaluated with the aid of information obtained by remote sensing and field data. This work is focused on the analysis of the geometry of tectonic structures and their relationship with essential elements of the Irati-Rio Bonito Petroleum System, inserted in the Parana Basin. The structural framework was outlined with satellite imagery, digital elevation models and geophysical maps. Several techniques relative to lineament analysis were reviewed and implemented by software programming. The description of structural styles, and kinematic and dynamic analysis were performed using field data obtained in key-areas. Another software was developed in order to calculate paleostress components. It computes maximum, intermediary and minor principal stress position based on Mohr-Coulomb criteria, for each fault individually. That aspect showed to be particularly important in this study due the several tectonic episodes that occurred in the Parana Basin. The relationships among features of different magnitudes and structural levels, interpreted by integrating several remote sensors, provided the understanding of the structural envelopment in the studied area. Based on the mapped structural elements, some accumulation controls were pointed out, such as the observed potential for the development of structural traps near regional structures, and the possibility of greater seals integrity associated with NE-SW oriented structural trends. Furthermore, N-S trending elements, generated in an extensional regime, could be associated with the rupture of the upper section, thus allowing leakage of hydrocarbon accumulations. (author)

  3. Space-based monitoring of land-use/land-cover in the Upper Rio Grande Basin: An opportunity for understanding urbanization trends in a water-scarce transboundary river basin.

    Mubako, S. T.; Hargrove, W. L.; Heyman, J. M.; Reyes, C. S.


    Urbanization is an area of growing interest in assessing the impact of human activities on water resources in arid regions. Remote sensing techniques provide an opportunity to analyze land cover change over time, and are useful in monitoring areas undergoing rapid urban growth. This case study for the water-scarce Upper Rio Grande River Basin uses a supervised classification algorithm to quantify the rate and evaluate the pattern of urban sprawl. A focus is made on the fast growing El-Paso-Juarez metropolitan area on the US-Mexico border and the City of Las Cruces in New Mexico, areas where environmental challenges and loss of agricultural and native land to urban development are major concerns. Preliminary results show that the land cover is dominantly native with some significant agriculture along the Rio Grande River valley. Urban development across the whole study area expanded from just under 3 percent in 1990, to more than 11 percent in 2015. The urban expansion is occurring mainly around the major urban areas of El Paso, Ciudad Juarez, and Las Cruces, although there is visible growth of smaller urban settlements scattered along the Rio Grande River valley during the same analysis period. The proportion of native land cover fluctuates slightly depending on how much land is under crops each analysis year, but there is a decreasing agricultural land cover trend suggesting that land from this sector is being lost to urban development. This analysis can be useful in planning to protect the environment, preparing for growth in infrastructure such as schools, increased traffic demands, and monitoring availability of resources such as groundwater as the urban population grows.

  4. Two new species of Hyphessobrycon (Teleostei: Characidae from upper rio Tapajós basin on Chapada dos Parecis, central Brazil

    Tiago Pinto Carvalho


    Full Text Available Two new species of Hyphessobrycon are described from the upper rio Tapajós basin, Mato Grosso, Brazil. Hyphessobrycon melanostichos is distinguished from its congeners by the combination of a conspicuous longitudinal broad black band beginning on the posterior margin of orbit and reaching the tip of middle caudal fin rays, a distinct vertically elongate humeral spot, and 16 to 18 branched anal-fin rays. Hyphessobrycon notidanos is distinguished from its congeners by the combination of an elongate dorsal fin in mature males, a vertically elongate humeral spot, 2-4 maxillary teeth, iii,8 dorsal-fin rays, and 16 to 21 branched anal-fin rays.Duas novas espécies do gênero Hyphessobrycon são descritas para a bacia do alto rio Tapajós, Mato Grosso, Brasil. Hyphessobrycon melanostichos distingue-se de seus congêneres pela combinação da presença de uma banda preta longitudinal larga entre a margem posterior da órbita até a ponta dos raios medianos da nadadeira caudal, de uma mancha umeral verticalmente alongada, e de 16 a 18 raios ramificados na nadadeira anal. Hyphessobrycon notidanos distingue-se de seus congêneres pela combinação da presença da nadadeira dorsal alongada nos machos maduros, de uma mancha umeral verticalmente alongada, 2-4 dentes no maxilar, iii,8 raios na nadadeira dorsal e 16 a 21 raios ramificados na nadadeira anal.

  5. Vascular epiphytes of the Atlantic Forest in the Sinos River basin, state of Rio Grande do Sul, Brazil: richness, floristic composition and community structure.

    Barbosa, M D; Becker, D F P; Cunha, S; Droste, A; Schmitt, J L


    The Atlantic Forest, which has a vast epiphytic richness, is a priority area for preservation, listed as one of the five most important world hotspots. Vascular epiphyte richness, composition and community structure were studied in two fragments, one of the ombrophilous (29º43'42"S and 50º22'00"W) and the other of the seasonal (29º40'54"S and 51º06'56"W) forest, both belonging to the Atlantic Forest biome in the Sinos River basin, Rio Grande do Sul, Brazil. In each fragment, 40 trees, divided into four ecological zones, were analyzed. In each zone, the occurrence of the species was recorded, and the importance value of each species was calculated according to the frequency of phorophytes and intervals, and cover scores. The Shannon index was calculated for the two communities. In the fragment of the ombrophilous forest (F1), 30 epiphytic species were recorded, and in the seasonal forest (F2), 25. The highest importance value was found for Microgramma squamulosa (Kaulf.) de la Sota in both fragments. The diversity indexes for F1 (H'=2.72) and F2 (H'=2.55) were similar and reflected the subtropical location of the areas. The decrease in mean richness in both fragments in zone 3 (internal crown) to zone 4 (external crown) may be associated with time and space availability for epiphyte occupation and microclimate variations. Exclusive species were found in the areas, which suggest that a greater number of preserved fragments may result in a greater number of preserved epiphytic species in the Sinos River basin.

  6. Controlling salinity in the river Llobregat basin; Control de la salinidad en la cuenca del rio Llobregat

    Gode, L. X.


    Few problems to do with water quality have required so many control measures over such a large area and such a prolonged period of time as the salinity in the river Llobregat basin. The technology and the methods used have undergone several major changes and the most significant periods in the history of the 20th century are reflected in the documents recording the evolution of salinity levels in the area. The interesting history of the salt and potassium mines, the natural and anthropic impacts, the vicissitudes of the brine collector and its positive effects, the evolution of the salinity and the systems for controlling it, and the prospects for the future are all discussed. (Author) 11 refs.

  7. Stratigraphic and structural analysis of the Rio do Peixe Basin, Northeastern Brazil: integration on the pioneer seismic survey 0295{sub R}IO{sub D}O{sub P}EIXE{sub 2}D; Analise estratigrafica e estrutural da Bacia do Rio do Peixe, Nordeste do Brasil: integracao a partir do levantamento sismico pioneiro 0295{sub R}IO{sub D}O{sub P}EIXE{sub 2}D

    Cordoba, Valeria Centurion; Antunes, Alex Francisco; Sa, Emanuel Ferraz Jardim de; Silva, Ajosenildo Nunes da; Sousa, Debora do Carmo; Lins, Fernando Antonio Pessoa Lira [Universidade Federal do Rio Grande do Norte (UFRN), Natal, RN (Brazil). Lab. de Geologia e Geofisica de Petroleo. Programa de Pos-Graduacao em Geodinamica e Geofisica


    The Northeast Brazil Interior Basins are the erosional remnants of a series of basins located south of he Potiguar Basin, overlying the crystalline basement of Precambrian Borborema Province . These basins were originated during the Early Cretaceous rifting that shaped the present continental margin of northeastern Brazil. Besides their exploration potential, the Interior Basins represent terrain analogues for better understanding of the continental margin basins, one of the objectives of the Interior Basins Project (agreement PETROBRAS/UFRN/PPGG), which supported the seismic survey in the Rio do Peixe Basin, subject to this paper. Combined with gravity and field data, the seismic sections allowed an improved view of the three-dimensional architecture of the Rio do Peixe Basin. In this basin, the combination of the current erosion level with the geometry of the main faults highlights the existence of different half-grabens (Pombal, Sousa, Brejo das Freiras), whose sedimentary filing (apart from cenozoic deposits) defines the Rio do Peixe Group, comprising the Antenor Navarro (alluvial fans/braided channels), Sousa (shallow lacustrine/floodplain) and Rio Piranhas (alluvial fans/braided channels). Structural data integration allows characterization of a NW-extension kinematics for the rifting event, responsible for fault nucleation controlled by basement structures, particularly the location and foliation dip of the Late Neoproterozoic, Brasiliano shear zones. Based on the structural style and petrographic-diagenetic features, one can infer larger original dimensions for this basin and similar counterparts in the region, which were reduced (with exposure of the crystalline highs) by the significant erosion that occurred in late to post-rift and subsequent evolutionary stages. (author)

  8. Modeling the transfer of land and water from agricultural to urban uses in the Middle Rio Grande Basin, New Mexico.

    Jarratt, Janet (Valencia County, NM); Passell, Howard David; Kelly, Susan (Utton Transboundary Resources Center, Albuquerque, NM); Malczynski, Leonard A.; Chermak, Janie (University of New Mexico, Albuquerque, NM); Van Bloeman Waanders, Paul (GRAM, Inc., Albuquerque, NM); McNamara, Laura A.; Tidwell, Vincent Carroll; Pallachula, Kiran (GRAM, Inc., Albuquerque, NM); Turnley, Jessica Glicken (Galisteo Consulting Group, Albuquerque, NM); Kobos, Peter Holmes; Newman, Gretchen Carr (GRAM, Inc., Albuquerque, NM)


    Social and ecological scientists emphasize that effective natural resource management depends in part on understanding the dynamic relationship between the physical and non-physical process associated with resource consumption. In this case, the physical processes include hydrological, climatological and ecological dynamics, and the non-physical process include social, economic and cultural dynamics among humans who do the resource consumption. This project represents a case study aimed at modeling coupled social and physical processes in a single decision support system. In central New Mexico, individual land use decisions over the past five decades have resulted in the gradual transformation of the Middle Rio Grande Valley from a primarily rural agricultural landscape to a largely urban one. In the arid southwestern U.S., the aggregate impact of individual decisions about land use is uniquely important to understand, because scarce hydrological resources will likely limit the viability of resulting growth and development trajectories. This decision support tool is intended to help planners in the area look forward in their efforts to create a collectively defined 'desired' social landscape in the Middle Rio Grande. Our research question explored the ways in which socio-cultural values impact decisions regarding that landscape and associated land use. Because of the constraints hydrological resources place on land use, we first assumed that water use, as embodied in water rights, was a reasonable surrogate for land use. We thought that modeling the movement of water rights over time and across water source types (surface and ground) would provide planners with insight into the possibilities for certain types of decisions regarding social landscapes, and the impact those same decisions would have on those landscapes. We found that water rights transfer data in New Mexico is too incomplete and inaccurate to use as the basis for the model. Furthermore

  9. Two new species of the Hypostomus cochliodon group (Siluriformes: Loricariidae from the rio Paraguay basin, with a redescription of Hypostomus cochliodonKner, 1854

    Luiz F. C. Tencatt

    Full Text Available Hypostomus cochliodon group is a monophyletic clade of 20 valid species of Neotropical armored catfishes that is widely distributed throughout South America. Recently, specimens identified as H. cochliodon from the type locality and nearby localities were examined, and found to include representatives of more than one species. A redescription of H. cochliodon is provided, with a description of two new species, one from the Bodoquena Plateau and another from several localities of the rio Paraguay basin. A lectotype for H. cochliodon is designated herein, since the previous designation is invalid. Hypostomus cochliodon is diagnosed from all other species of the H. cochliodon group by having the opercle almost completely covered laterally by thick layer of skin, the absence of buccal papilla, weak to moderately developed keels on the lateral plates of the body and by the color pattern of its body and fins. Hypostomus basilisko, new species, is distinguished from the remaining species of the H. cochliodon group by the absence of spots on the body, highly developed keels and spoon-shaped teeth. Hypostomus khimaera, new species, is distinguished from the other species of the H. cochliodon group by having a dark tan stripe along the midline of the flank, black spots on the body and/or fins and teeth with mesial cusp and not spoon-shaped.

  10. Diachronic aspects of land planning of the Alberche river basin; Aspectos diacrnicos de la ordenacion del territorio de la cuenca del rio Alberche

    Sotelo Perez, M.


    The planning scope of this study is a section of the edge of the metropolitan area southwest of Madrid, comprising the townships of Alamo, Navalcarnero, Villamanta and Sevilla la Nueva, which falls in the region of the Rio Alberche. The characteristics of the natural environment, the peculiar morphology of population settlements, together with the unique organization and economic dynamics, increased immigration in recent times and the seasonal residence, has resulted in a pattern of relationships and flows that interrelate to municipalities each other and manifested in population movements daily for work and labor, and important phenomena of outsourcing, which gives the most singular and main feature, along with the role of backbone of the region of Alberche river basin. Through the case study, questioning the methodology, we approach the study and research issues related to municipalities that are enrolled in spaces within the forms of protection (Regional Park of the middle river Guadarrama) and others not. All in all, after the previous analysis, we analyze the problem. (Author)

  11. Host-parasite interactions between the piranha Pygocentrus nattereri (Characiformes: Characidae and isopods and branchiurans (Crustacea in the rio Araguaia basin, Brazil

    Lucélia Nobre Carvalho

    Full Text Available In the tropics, studies on the ecology of host-parasite interactions are incipient and generally related to taxonomic aspects. The main objective of the present work was to analyze ecological aspects and identify the metazoan fauna of ectoparasites that infest the piranha, Pygocentrus nattereri. In May 2002, field samples were collected in the rio Araguaia basin, State of Goiás (Brazil. A total of 252 individuals of P. nattereri were caught with fishhooks and 32.14% were infested with ectoparasite crustaceans. The recorded ectoparasites were branchiurans, Argulus sp. and Dolops carvalhoi and the isopods Braga patagonica, Anphira branchialis and Asotana sp. The prevalence and mean intensity of branchiurans (16.6% and 1.5, respectively and isopods (15.5% and 1.0, respectively were similar. Isopods were observed in the gills of the host; branchiurans were more frequent where the skin was thinner, and facilitated attachment and feeding. The ventral area, the base of the pectoral fin and the gular area were the most infested areas. The correlations between the standard length of the host and the variables intensity and prevalence of crustaceans parasitism, were significant only for branchiurans (rs = 0.2397, p = 0.0001; chi2 = 7.97; C = 0.19. These results suggest that both feeding sites and body size probably play an important role in the distribution and abundance of ectoparasites.

  12. Radioactivity of rocks from the geological formations belonging to the Tibagi River hydrographic basin; Radioatividade de rochas provenientes das formacoes geologicas pertencentes a bacia hidrografica do Rio Tibagi

    Bastos, Rodrigo Oliveira


    This work is a study of the {sup 40}K and the {sup 238}U and {sup 232}Th series radioactivity in rocks measured with high resolution gamma ray spectrometry. The rocks were taken from the geologic formations in the region of the Tibagi river hydrographic basin. The course of this river cuts through the Paleozoic and Mesozoic stratigraphic sequences of the Parana sedimentary basin. In order to take into account the background radiation attenuation by the samples, a technique was developed that eliminated the need to measure a blank sample. The effects of the radiation's self-attenuation in the sample matrix were taken into account by using a gamma ray direct transmission method. The results for 87 rock samples, taken from 14 distinct formations, and their corresponding radioactivity variations are presented and discussed according to the possible geological processes from which they originated. Among the most discussed results are: an outcrop that profiles shale, limestone and rhythmite in the Irati Formation; a sandstone and siltstone sequence from the Rio do Rasto Formation; and a profile sampled in a coal mine located in the Rio Bonito Formation. The calculations of the rocks' contributions to the outdoor gamma radiation dose rate agree with the values presented by other authors for similar rocks. The highest dose values were obtained from felsic rocks (rhyolite of the Castro group, 129.8 {+-} 3.7 nGy.h{sup -1}, and Cunhaporanga granite, 167 {+-} 37 nGy.h{sup -1}). The other highest values correspond to the shale rocks from the Irati Formation (109 {+-} 16 nGy.h{sup -1}) and the siltic shale rocks from the Ponta Grossa Formation (107.9 {+-} 0.7 nGy.h{sup -1}). The most recent geological formations presented the lowest dose values (e.g. the Botucatu sandstone, 3.3 {+-} 0.6 nGy.h{sup -1}). The average value for sedimentary rocks from seven other formations is equal to 59 {+-} 26 nGy.h{sup -1}. The Rio Bonito Formation presented the highest dose value (334

  13. Geochemical behavior and dissolved species control in acid sand pit lakes, Sepetiba sedimentary basin, Rio de Janeiro, SE - Brazil

    Marques, Eduardo D.; Sella, Sílvia M.; Bidone, Edison D.; Silva-Filho, Emmanoel V.


    This work shows the influence of pluvial waters on dissolved components and mineral equilibrium of four sand pit lakes, located in the Sepetiba sedimentary basin, SE Brazil. The sand mining activities promote sediment oxidation, lowering pH and increasing SO 4 contents. The relatively high acidity of these waters, similar to ore pit lakes environment and associated acid mine drainage, increases weathering rate, especially of silicate minerals, which produces high Al concentrations, the limiting factor for fish aquaculture. During the dry season, basic cations (Ca, Mg, K and Na), SiO 2 and Al show their higher values due to evapoconcentration and pH are buffered. In the beginning of the wet season, the dilution factor by rainwater increases SO 4 and decreases pH values. The aluminum monomeric forms (Al(OH) 2+ and Al(OH) 2+), the most toxic species for aquatic organisms, occur during the dry season, while AlSO 4+ species predominate during the wet season. Gibbsite, allophane, alunite and jurbanite are the reactive mineral phases indicated by PHREEQC modeling. During the dry season, hydroxialuminosilicate allophane is the main phase in equilibrium with the solution, while the sulphate salts alunite and jurbanite predominate in the rainy season due to the increasing of SO 4 values. Gibbsite is also in equilibrium with sand pit lakes waters, pointing out that hydrolysis reaction is a constant process in the system. Comparing to SiO 2, sulphate is the main Al retriever in the pit waters because the most samples (alunite and jurbanite) are in equilibrium with the solution in both seasons. This Al hydrochemical control allied to some precaution, like pH correction and fertilization of these waters, allows the conditions for fishpond culture. Equilibrium of the majority samples with kaolinite (Ca, Mg, Na diagrams) and primary minerals (K diagram) points to moderate weathering rate in sand pit sediments, which cannot be considered for the whole basin due to the anomalous

  14. Analysis, diagnosis and proposal of protection measures to mitigate hydrological alterations in the basin "Rio Calandaima" derived from climate change

    Guerrero, Marcela B.; Corzo, Gerald; Varouchakis, Emmanouil; Taguas, Encarnación V.


    Climate change and its effects represent a challenge for decision makers and for scientific communities, given the complexity and uncertainty associated. Rainfall reduction and evapotranspiration increase are expected phenomena associated to the climate change which will affect water resources of Calandaima River Basin (Colombia), which implies the need of designing suitable mitigation measures based on the qualitative and quantitative diagnosis of water resources. The objectives of this work were: 1) hydrological characterization of the catchment to carry out a diagnosis of rainfall-runoff current patterns and availability of water resources; 2) to implement a water balance model to complete dataseries gaps as well as modeling future climate change scenarios; 3) risk assessment based on guarantee indicators to propose mitigation measures. Firstly, detailing characteristics such as climatic zonification, slope range, drainage network and land use were described. A simple water balance model was calibrated though the adjustment of 4 parameters with an efficiency coefficient of 0.51. The indicators of supply guarantee (demand-supply analyses) determined a high risk of water deficit in the catchment for the current conditions and for the studied scenarios. A dramatic rise in costs to provide water may be envisaged, given the reduction in supply associated with climatic scenarios where the phenomenon "El Niño" takes place. Thus, not only is more investment needed to monitor the dynamics of the alterations but it is also essential to promote, among farmers and owners, incentives to apply water harvesting techniques and at the same time, to control floods.


    Valtercides Cavalcante da Silva


    as the slope length factor (L factor, particularly in watersheds. The purpose of the present study was to apply the USLE, which was originally developed for individual slopes, to large watersheds. In order to achieve that, a methodology for automatic calculation of the L factor, was developed by Desmet and Govers (1996, using a geographic information system (GIS. This methodology was used to estimate the actual erosion. Existing thematic maps, in association with ancillary information about soil, land use, relief and climate, were used in order to obtain GIS coverages. These coverages were overlaid on the GIS and maps of actual erosion were generated. This study concludes that 67.2% of the total area of the Rio Paracatu basin is within the soil loss tolerance limit (less to 10 t.ha-1/year. In addition, the slope length factor, as developed by Desmet and Govers (1996, which accounts for accumulated flow, showed satisfactory results in a large watershed. The proposed methodology was validated with sedimentometric data in two sections of the watershed, and measured and calculated silting yield data agreed.

    KEY-WORDS: Erosion; USLE; L factor; GIS.

  16. A description of mercury in fishes from the Madeira River Basin, Amazon, Brazil Um estudo descritivo do mercúrio em peixes da bacia do Rio Madeira, Amazônia, Brasil

    Wanderley Rodrigues Bastos


    Full Text Available Over the last 20 years several projects carried on the Madeira River basin in the Amazon produced a great amount data on total Hg concentration in different fish species. In this paper we discuss temporal trends in Hg contamination and its relation to body weight in some of those fishes, showing that even within similar groups, such as carnivorous and non-migratory fish, the interspecies variability in Hg accumulation is considerable.Vários estudos têm sido desenvolvidos nos últimos 20 anos na bacia do Rio Madeira (Amazônia com o objetivo de diagnosticar a presença de mercúrio em peixes e compreender o ciclo deste elemento no meio ambiente tropical. Neste artigo são discutidas tendências temporais na concentração de Hg e sua relação com a massa corporal de algumas espécies de peixes com diferentes hábitos alimentares, coletadas no Rio Madeira e no reservatório da hidroelétrica de Samuel, no Rio Jamari, Estado de Rondônia. Foi avaliada uma amostragem de peixes de 14 anos (1987 - 2000 com 86 espécies e um total de 1100 espécimes.

  17. An integrated geological and geophysical study of the Uinta Mountains, Utah, Colorado and a geophysical study on Tamarix in the Rio Grande River basin, West Texas

    Khatun, Salma


    comprehensive picture of the structures in the study area. These models show that the Uinta uplift is a single sedimentary block with numerous thrust faults on the northern and southern flanks of the uplift. These models also reveal the fact that the thickness of the crust is quite variable in the study area. This is also supported by the crustal thickness map constructed for this study from seismic and receiver function information. Magnetic maps show that the Proterozoic sedimentary package known as Uinta Mountain Group extends into the Basin and Range and indicates its link with the ancient rift margin in the Western United States. Findings of this research are correlated to earlier studies and placed in a broader context. Finally an analogy is made between the Uinta aulacogen, the Southern Oklahoma aulacogen and the Dniepr-Donets aulacogen in Ukraine. This discussion focuses light on the mechanism that led to the Uinta's development from a failed rift to an uplift. Part two of this research examined the effect of saltcedar (Tamarix sp) on water and soil properties in the Rio Grande River valley in West Texas. Tamarix is a woody phreatophyte (water-loving plant) common in riparian habitats. The presence of Tamarix in a river system raises concerns about its effect on water quality because it can increase the salinity of water and surrounding soil and it reduces stream flow. Geophysical electrical techniques were used to track soil salinity and moisture changes caused by Tamarix, as well as to determine how soil salinity and moisture properties are altered when Tamarix is eradicated from the region. These techniques allowed more rapid in-situ assessment of the soil properties than the conventional method of removing soil and water samples for analysis. This study was focused on the influence of Tamarix on soil properties and hydrology at the subsurface at four sites in the Rio Bosque Wetlands Park, El Paso, Texas Two sites had flourishing Tamarix and two others were areas

  18. Patterns of species richness and composition of fish assemblages in streams of the Ivinhema River basin, Upper Paraná River Padrões de riqueza e composição de espécies das assembleias de peixes em riachos da bacia do rio Ivinhema, Alto Rio Paraná

    Yzel Rondon Súarez


    Full Text Available AIM: The present study analyzed the spatial variation in fish species richness and composition in streams of the Ivinhema River basin, Upper Paraná basin, determining the relationship between local and regional descriptors of the fish assemblage organization; METHOD: From 2001 to 2011 we sampled 200 stream stretches, using different sampling methods. Local species richness and composition were analyzed using univariate and multivariate methods to detect patterns of variation in the fish assemblage organization; RESULTS: We identified 111 fish species in the streams, and estimated the occurrence of 117 fish species (CIα0.05 = 111 to 123 with lower species richness in headwater streams compared to the lower parts of the basin. The fish species recorded were predominantly of small size, and the mean size increased from the headwaters to the river mouth. The four most common species are widely distributed in the basin. However, 24 species are allocthonous to the Upper Paraná basin, and two species (Chaetobranchopsis australis and Apistogramma commbrae are recorded here for the first time in the Upper Paraná basin. Altitude was the main determinant of local fish species richness and composition, and a discontinuity in assemblage organization (richness, composition, fish size was detected at approximately 430 m a.s.l.; CONCLUSION: Streams of the Ivinhema River basin are inhabited mainly by small-sized fishes; and longitudinal variation, interacting with local characteristics, determines the fish assemblage patterns.OBJETIVOS: O presente estudo tem como objetivo analisar a variação especial na riqueza e composição de espécies de peixes em riachos da bacia do rio Ivinhema, Alto Rio Paraná determinando a relação entre características locais e regionais na organização das assembleias de peixes; MÉTODOS: Amostramos 200 trechos de riachos entre 2001 e 2011 utilizando diferentes petrecho de pesca. A riqueza local e composição de esp

  19. Host-parasite interactions between the piranha Pygocentrus nattereri (Characiformes: Characidae and isopods and branchiurans (Crustacea in the rio Araguaia basin, Brazil

    Lucélia Nobre Carvalho


    Full Text Available In the tropics, studies on the ecology of host-parasite interactions are incipient and generally related to taxonomic aspects. The main objective of the present work was to analyze ecological aspects and identify the metazoan fauna of ectoparasites that infest the piranha, Pygocentrus nattereri. In May 2002, field samples were collected in the rio Araguaia basin, State of Goiás (Brazil. A total of 252 individuals of P. nattereri were caught with fishhooks and 32.14% were infested with ectoparasite crustaceans. The recorded ectoparasites were branchiurans, Argulus sp. and Dolops carvalhoi and the isopods Braga patagonica, Anphira branchialis and Asotana sp. The prevalence and mean intensity of branchiurans (16.6% and 1.5, respectively and isopods (15.5% and 1.0, respectively were similar. Isopods were observed in the gills of the host; branchiurans were more frequent where the skin was thinner, and facilitated attachment and feeding. The ventral area, the base of the pectoral fin and the gular area were the most infested areas. The correlations between the standard length of the host and the variables intensity and prevalence of crustaceans parasitism, were significant only for branchiurans (rs = 0.2397, p = 0.0001; chi2 = 7.97; C = 0.19. These results suggest that both feeding sites and body size probably play an important role in the distribution and abundance of ectoparasites.Nos trópicos, os estudos sobre a ecologia de interações parasito-hospedeiro são incipientes, sendo a maioria de cunho taxonômico. O principal objetivo do presente estudo foi identificar a fauna metazoária de ectoparasitas e analisar aspectos ecológicos da piranha Pygocentrus nattereri. As coletas foram realizadas em maio de 2002, na bacia do rio Araguaia, GO. Com o auxílio de linha e anzol foram capturados 252 exemplares de P. nattereri, dos quais 32,14% estavam infestados por crustáceos ectoparasitos. As espécies de ectoparasitas registradas foram Argulus sp

  20. The formation of early settled villages and the emergence of leadership: A test of three theoretical models in the Rio Ilave, Lake Titicaca Basin, southern Peru

    Craig, Nathan Mcdonald

    Despite obvious necessities for understanding later developments in the region, Preceramic cultures in the Titicaca Basin are poorly understood due to lacking empirical data. This dissertation focuses on examination of two processes occurring in the Rio Ilave drainage during the Late 5000--3100 B.C.E. (6000--4400 B.P.) and Terminal 3100--1500 B.C.E. Archaic (4400--3200 B.P.): the formation of settled villages and the emergence of leadership. These processes are tested against theoretical predictions derived from: population resource imbalance, human behavioral ecology, and agency theories. Resource imbalance theory predicts appearance of density dependent adaptive problems prior to major cultural transformations. Human behavioral ecology predicts increased dietary diversity and incorporation of greater processing costs occuring coincidentally with reduced residential mobility. Symbolic mate value advertising is a predicted leadership strategy. Agency theory predicts internal sources of social tension, potentially independent of external forces, as primary causes of cultural change. Feast hosting and the formation political economy are expected to be central to both social processes investigated from this perspective. Local paleoclimatic proxies suggest aridity from ca 4000--2000 B.C.E. Reanalysis of pedestrian survey data indicate population growth during the Late Archaic. Excavation and ground penetrating radar survey at Pirco and Jiskairumoko demonstrate reduced residential mobility and increased evidence for social differentiation appearing during the Late Archaic's (before 3000 B.C.E.) end. New cultural patterns include: pithouses, more groundstone, internal storage, costly non-local artifacts, domesticated plants and animals, costly grave goods, and use of ochre in symbolic contexts. No clear cut evidence for inter-community promotional feasting was identified but some finds suggest intra-community alliance feasts. By the end of the Terminal Archaic ca. 1500 B

  1. A water quality index model using stepwise regression and neural networks models for the Piabanha River basin in Rio de Janeiro, Brazil

    Villas Boas, M. D.; Olivera, F.; Azevedo, J. S.


    The evaluation of water quality through 'indexes' is widely used in environmental sciences. There are a number of methods available for calculating water quality indexes (WQI), usually based on site-specific parameters. In Brazil, WQI were initially used in the 1970s and were adapted from the methodology developed in association with the National Science Foundation (Brown et al, 1970). Specifically, the WQI 'IQA/SCQA', developed by the Institute of Water Management of Minas Gerais (IGAM), is estimated based on nine parameters: Temperature Range, Biochemical Oxygen Demand, Fecal Coliforms, Nitrate, Phosphate, Turbidity, Dissolved Oxygen, pH and Electrical Conductivity. The goal of this study was to develop a model for calculating the IQA/SCQA, for the Piabanha River basin in the State of Rio de Janeiro (Brazil), using only the parameters measurable by a Multiparameter Water Quality Sonde (MWQS) available in the study area. These parameters are: Dissolved Oxygen, pH and Electrical Conductivity. The use of this model will allow to further the water quality monitoring network in the basin, without requiring significant increases of resources. The water quality measurement with MWQS is less expensive than the laboratory analysis required for the other parameters. The water quality data used in the study were obtained by the Geological Survey of Brazil in partnership with other public institutions (i.e. universities and environmental institutes) as part of the project "Integrated Studies in Experimental and Representative Watersheds". Two models were developed to correlate the values of the three measured parameters and the IQA/SCQA values calculated based on all nine parameters. The results were evaluated according to the following validation statistics: coefficient of determination (R2), Root Mean Square Error (RMSE), Akaike information criterion (AIC) and Final Prediction Error (FPE). The first model was a linear stepwise regression between three independent variables

  2. Efeito das mudanças climáticas na disponibilidade hídrica da bacia hidrográfica do Rio Paracatu Effect of the climate change on the water availability in the Paracatu river basin

    Eloy L. de Mello


    Full Text Available O aumento da demanda pelo uso da água na bacia do Rio Paracatu vem ocasionando sérios problemas ambientais e conflitos entre os usuários. Para a gestão mais eficiente dos recursos hídricos, é importante o conhecimento do comportamento hidrológico da bacia hidrográfica, no presente e no futuro, devido às fortes evidências de mudanças climáticas no planeta. O objetivo deste trabalho foi estimar a tendência de variação da disponibilidade hídrica na bacia hidrográfica do Rio Paracatu, até o final deste século, considerando dois cenários contrastantes de mudanças climáticas, um para altas emissões de CO2 (A2 e outro para baixas (B2. Para atingir esse objetivo, foi realizado o downscaling das precipitações mensais para os anos de 2001 a 2099, simulados pelo modelo de circulação geral do Hadley Centre (HadCM3. As precipitações interpoladas serviram como entrada em modelo do tipo precipitação-vazão, que possibilitou a estimativa das vazões mínimas em 21 estações fluviométricas distribuídas na bacia. Para o cenário A2, verificou-se tendência de aumento na disponibilidade hídrica em todas as estações fluviométricas, variando de 31 a 131% até 2099. Para o cenário B2, não foi verificada nenhuma tendência significativa.The increase of water use in the Paracatu basin is leading to deep environmental problems and conflicts among the users. For a more efficient water resources management, the knowledge of the basin's hydrologic behavior is important, in the present and in the future, due to the strong climatic changes evidences in the planet. The aim of this work is to estimate the water availability variation trends in the Paracatu river basin, from the beginning until the end of this century, considering two contrasting climate change scenarios, the first one to take account of high CO2 emissions (A2 and the other one for low emissions (B2. To achieve this objective, the monthly precipitation downscaling was

  3. Determination of As, Co, Cr and Fe on sediments and soil of the region of middle and low courses of the Rio da Velhas basin, MB, Brazil; Determinacao de As, Co, Cr e Fe em sedimentos e solo na regiao do medio e baixo curso da bacia do Rio das Velhas, Minas Gerais

    Veado, Maria Adelaide R.V.; Trigueris, Giuliano de A.; Oliveira, Arno H. de; Carvalho, Fernando R. de [Minas Gerais Univ., Belo Horizonte, MG (Brazil). Dept. de Engenharia Nuclear]. E-mail: ,,; Veado, Julio Cesar C. [Minas Gerais Univ., Belo Horizonte, MG (Brazil). Escola de Veterinaria. Dept. de Clinica e Cirurgia Veterinarias]. E-mail:; Menezes, Maria Angela de B. C. [Centro de Desenvolvimento da Tecnologia Nuclear (CDTN), Belo Horizonte, MG (Brazil). Supervisao de Reator e Radioanalise. Setor de Radioquimica]. E-mail:


    The regions of the middle and low courses of the Rio das Velhas Basin are important under economical point of view for Minas Gerais State because of the agricultural production and high bovine population. In this work sediment and soil samples were analysed at monitoring points near the river established by FEAM-Fundacao Estadual do Meio Ambiente. As, Co, Cr and Fe were determined by means k{sub 0}-Neutron Activation Analysis. The sediment's and soil's results suggested metal contamination probably due to metals carried by high course water. (author)

  4. Enquadramento dos corpos d’água e cobrança pelo uso da água na bacia do rio Pirapama - PE Water body classification and raw water charges in the Pirapama River Basin

    Selma Cristina da Silva


    Full Text Available Neste artigo são apresentados os cenários de melhoria da qualidade da água para a bacia do rio Pirapama, localizada na Região Metropolitana do Recife, vinculados ao que dispõe o enquadramento dos corpos d’água segundo as Classes 1, 2 e 3 estipuladas pela Resolução CONAMA nº 357/05. Com base nesses cenários foram definidos os custos marginais de medida de redução da poluição que subsidiaram a concepção de um sistema de cobrança pelo lançamento de efluentes, o qual encontra respaldo legal na Lei nº 9.433/97 da Política Nacional de Recursos Hídricos. Os cenários foram simulados com o Sistema de Apoio à Decisão para o Controle Integrado de Poluição (SAD-CIP desenvolvido pelo Banco Mundial. Os resultados indicaram que para atender aos objetivos de qualidade (Classe 2, as fontes potencialmente poluidoras devem realizar o Tratamento Secundário e Terciário nas águas residuárias. O valor mais adequado a ser cobrado dos poluidores seria de US$ 320,00/ton de DBO lançada no rio.This paper establishes water quality improvement scenarios for an area of Pirapama River Basin in Recife Metropolitan Region, Brazil. This scenarios are related to Brazilian water body quality goals (defined by CONAMA Directive number 357/05. Based on those scenarios, pollution control marginal costs are calculated in order to simulate a water effluent system charge according to Brazilian Water Resources Policy (Law nº 9.433/97. The Decision Support System for Integrated Pollution Control (DSS-IPC, developed by the World Bank, was chosen for performing the simulations. The outcomes showed that in the studied area, the river does not comply with CONAMA Directive number 357/05, which establishes Class 2 for the main stream. Secondary and Tertiary treatments are needed to reach such Class and the water effluent system charge presents US$ 320.00/ton as a viable value to be charged.


    Eduardo Beraldo de Morais


    Full Text Available The hydric bodies in the Corumbataí basin have presented significant changes, resulted from land misuse by agricultural activities and domestic and industrial sewage discharge. Among the tributaries in this basin, the River ‘Head’ is located in areas occupied, principally, by pasture and sugar cane crops. This study aimed water quality in the River ‘Head’ micro basin, and possible pollution sources. During 24 months (April 2007 to March 2009 seven sampling stations were monitored, five in the River ‘Head’ and two in the river which receives its water, the Passa-Cinco River. According to Water Quality Index (WQI, the water quality is considered Good, but the values of parameters biochemical oxygen demand (BOD and Escherichia coli, using in calculating this index, were discordance with that established by CONAMA 357/2005 Resolution to class 2 hydric bodies. This indicates pollution by wastewater from rural village and/or breeding effluents. It was found during the rainy/warm season (October-March the runoff increased can influence the parameters values studied except for BOD. It is necessary the recovery the riparian forests in some places to reduce siltation and control of the dominant monoculture installed on slopes above 45 degrees and close to rivers and streams beds. = Os corpos hídricos na bacia do rio Corumbataí vêm apresentando alterações significativas devido ao mau uso das terras pelas atividades agropecuárias e lançamentos de efluentes domésticos e industriais. Dentre os tributários nessa bacia hidrográfica, o rio Cabeça situa-se em área explorada, principalmente, por pastagem e cultura de cana-de-açúcar. O presente estudo abordou a qualidade da água na microbacia do rio Cabeça e as possíveis fontes poluidoras. Durante 24 meses (abril de 2007 a março de 2009 sete pontos de amostragem foram monitorados, sendo cinco no rio Cabeça e dois no rio que recebe a suas águas, o rio Passa-Cinco. Segundo o

  6. Elements for an integrated resource planning in the framework of river basins: a study for the Cuiaba River Basin; Elementos para um planejamento integrado de recursos no ambito de bacias hidrograficas: um estudo para a bacia do rio Cuiaba

    Dorileo, Ivo Leandro; Bajay, Sergio Valdir [Universidade Estadual de Campinas (NIPE/UNICAMP), SP (Brazil). Nucleo Interdisciplinar de Planejamento Energetico. Dept. de Energia], e-mail:, e-mail:


    A new approach in energy planning in Brazil, IRP - Integrated Resources Planning for River Basins, gathers three main determinants of development: water, electricity and piped gas. This paper argues, briefly, the need of this planning, of indicative character, integrated with the River Basin Plans, and it presents a retrospective analysis concerning water, electricity and LPG demands of the economy sectors from Cuiaba River Basin region, priority elements to aid the prospective studies and to carry out process related to the IRP. (author)

  7. River basin planning as an instrument for the preservation and restoration of rivers. The case of the river Francoli; La planificacion de espacios fluviales como instrumento para la preservacion y restauracion de rios. Caso del rio Francoli

    Gode, L.; Gracia, A.; Garcia, E.; Borras, G.


    According to the Water Directive, River Basin Planning (RBP) is an instrument to be applied to ensure that water masses achieve a good ecological state. the instrument identifies flood able areas, risk maps and their management, and, in this case, takes into account the Regulations of the Catalan Town Planning Act governing the permitted uses of the river basins whose limits are set by the appropriate water administration board. These RBP projects are the results of interdisciplinary work integrating hydrological, hydraulic, morpho dynamic and environmental factors. Such projects have already been drawn up for various Catalan river basins (Tordera, Baix Llobregat and Anoia, Baix Ter, etc) or are under way in others (Muga, Foix, Gaia, Besos, Fluvia, Garona, Ondara, Ridaura-riera de Calonge, etc). This is the case of the one for the river Francoli which is described in this article. (Author) 10 refs.

  8. Estimativa de recarga da bacia do Rio das Fêmeas através de métodos manuais e automáticos Estimates of the recharge in the Femeas River basin by manual and automatic methods

    Ana C. L. S. Albuquerque


    Full Text Available Na região do oeste baiano, na qual se encontra a bacia do Rio das Fêmeas, a água subterrânea tem sido progressivamente procurada como fonte de abastecimento, haja vista a baixa densidade de drenagem da região e a crescente demanda por água, sobremaneira para projetos de irrigação. O objetivo do presente estudo é, a partir de dados de vazão, calcular a recarga da água subterrânea por meio de duas metodologias: Arnold & Allen (1999 e Rutledge & Daniel (1994, para o período de 1977 a 2007. A precipitação média anual para a bacia do Rio das Fêmeas foi de 1121,83 mm ano-1 e a vazão média anual igual a 50,28 m³ s-1, ambas apresentando tendência de queda significativa ao longo dos anos. As taxas de recarga foram de 4% da P total (Arnold & Allen, 1999 e de 17% (Rutledge & Daniel, 1994. Com referência ao escoamento de base (aproximadamente 250 mm ano-1, o último método mostrou-se melhor na estimação da recarga.In Western Bahia, where the Fêmeas River Basin is located, groundwater has been increasingly utilized, given the low density of drainage in the region and the growing demand for water, mainly irrigation projects. The objectives of this study are based on flow data to calculate the recharge of groundwater in the Femeas basin using two methods: Arnold & Allen (1999 and Rutledge & Daniel (1994, in the period of 1977 to 2007. The mean annual precipitation in the Fêmeas River Basin in the studied period was 1121.83 mm year-1 and the mean stream flow was 50.28 m³ s-1 year-1. Both showed a significant decreasing trend over the years. The mean base flow found for the basin was 257.41 mm year-1. The rates of recharge were 4% of total P (Arnold & Allen, 1999, and 17% (Rutledge & Daniel, 1994. Considering the basin discharge (around 250 mm year-1, the latter method seems to be better in estimating recharge.

  9. Comentários sobre a distribuição geográfica de Astyanax altiparanae Garutti & Britski, 2000 (Osteichthyes, Characidae na bacia do rio Iguaçu Astyanax altiparanae Garutti & Britski, 2000 (Osteichthyes, Characidae in the Iguaçu River basin

    Weferson Júnio da Graça


    Full Text Available Garutti (1995 fez a revisão de algumas espécies de Astyanax (Osteichthyes, Characidae e aquela, conhecida como “tambiú” na bacia do alto rio Paraná, anteriormente identificada como Astyanax bimaculatus, foi considerada nova e posteriormente descrita por Garutti & Britski (2000 como Astyanax altiparanae (Pisces, Characiformes. Naquela oportunidade, entretanto, não foram analisados exemplares da bacia do rio Iguaçu. Esse afluente do rio Paraná apresenta um alto grau de endemismo em sua ictiofauna devido ao isolamento geográfico causado pelas cataratas situadas próximo à sua foz. No entanto, muitas dúvidas relacionadas ao status específico da população da bacia do Iguaçu, também chamada de A. bimaculatus antes dos trabalhos de Garutti, permaneceram. Com o escopo de verificar se a população do Iguaçu era da espécie A. altiparanae, comparamos espécimes das duas bacias e concluímos que elas pertencem à mesma espécie, sendo, portanto, sua distribuição geográfica ampliada.Garutti (1995 made a revision of some Astyanax (Osteichthyes, Characidae species and the species called tambiú from the upper Paraná River basin, formerly identified as Astyanax bimaculatus, was considered new. Garutti & Britski (2000 later described it as Astyanax altiparanae (Pisces, Characiformes. However, they did not analyze specimens from the Iguaçu River basin at that time. The Iguaçu River, affluent to the Paraná River, has a high degree of endemism in its ichthyofauna because of the geographic isolation caused by the falls near its mouth. Thus, there were still many doubts regarding the specific status of the population from the Iguaçu River basin, also called A. bimaculatus before Garutti’s studies. To verify if the population from the Iguaçu River belongs to the A. altiparanae species, we compared specimens from both basins and concluded that they belong to the same species, widening their geographic distribution.

  10. Vazões máximas e mínimas para bacias hidrográficas da região alto Rio Grande, MG Maximum and minimum discharges for Alto Rio Grande region basins, Minas Gerais state, Brazil

    Carlos Rogério de Mello


    Full Text Available Vazões máximas são grandezas hidrológicas aplicadas a projetos de obras hidráulicas e vazões mínimas são utilizadas para a avaliação das disponibilidades hídricas em bacias hidrográficas e comportamento do escoamento subterrâneo. Neste estudo, objetivou-se à construção de intervalos de confiança estatísticos para vazões máximas e mínimas diárias anuais e sua relação com as características fisiográficas das 6 maiores bacias hidrográficas da região Alto Rio Grande à montante da represa da UHE-Camargos/CEMIG. As distribuições de probabilidades Gumbel e Gama foram aplicadas, respectivamente, para séries históricas de vazões máximas e mínimas, utilizando os estimadores de Máxima Verossimilhança. Os intervalos de confiança constituem-se em uma importante ferramenta para o melhor entendimento e estimativa das vazões, sendo influenciado pelas características geológicas das bacias. Com base nos mesmos, verificou-se que a região Alto Rio Grande possui duas áreas distintas: a primeira, abrangendo as bacias Aiuruoca, Carvalhos e Bom Jardim, que apresentaram as maiores vazões máximas e mínimas, significando potencialidade para cheias mais significativas e maiores disponibilidades hídricas; a segunda, associada às bacias F. Laranjeiras, Madre de Deus e Andrelândia, que apresentaram as menores disponibilidades hídricas.Maximum discharges are applied to hydraulic structure design and minimum discharges are used to characterize water availability in hydrographic basins and subterranean flow. This study is aimed at estimating the confidence statistical intervals for maximum and minimum annual discharges and their relationship wih the physical characteristics of basins in the Alto Rio Grande Region, State of Minas Gerais. The study was developed for the six (6 greatest Alto Rio Grande Region basins at upstream of the UHE-Camargos/CEMIG reservoir. Gumbel and Gama probability distribution models were applied to the

  11. A new Permian bivalve-dominated assemblage in the Rio do Rasto Formation, Paraná Basin, Brazil: Faunal turnover driven by regional-scale environmental changes in a vast epeiric sea

    Simões, Marcello Guimarães; Matos, Suzana Aparecida; Anelli, Luiz Eduardo; Rohn, Rosemarie; Warren, Lucas Veríssimo; David, Juliana Machado


    The basal portion of the Permian Rio do Rasto Formation (Serrinha Member), Passa Dois Group, Paraná Basin, Brazil, records an entirely new bivalve fauna intercalated between the underlying Pinzonella neotropica assemblage (uppermost portion of the Teresina Formation) and the overlying Leinzia similis assemblage (Rio do Rasto Formation). Mollusks of these assemblages lived in marginal shallow-water habitats of an immense epeiric sea and were dominated by endemic bivalve species. Taxonomic analysis revealed the presence of Terraia curvata (60.61%), Astartellopsis prosoclina (19.70%), Cowperesia emerita (10.61%), Leinzia curta (4.55%), Terraia bipleura (3.03%) and Beurlenella elongatella (1.52%), which are associated with conchostracans and plant remains. Species composition, abundance, and dominance in this novel assemblage differ notably from the preceding ones, suggesting a substantial evolutionary turnover. Regional-scale environmental changes recognized based on taphonomy, facies analysis, and geochemical data consist of progressive freshening of the marginal habitats of the Paraná Basin and taxic changes that include the following: (a) loss of genera, (b) decrease in bivalve abundance and ecological guilds, (c) disappearance of the dominant bivalve group (Pinzonellinae) and (d) diversification of Terrainae bivalves. The ecological signature also changed notably because only infaunal suspension-feeding bivalves are present, indicating a significant loss of functional diversity at the regional scale. Likely stressor factors (among others) are tied to freshening events, suggesting profound changes in (a) salinity, (b) primary productivity and (c) a lack of coarse, stable substrates coupled with high bioturbation rates. Hence, our regional example could offer valuable clues to benthic (bivalve) community responses in a habitat subjected to (a) rapid climate changes and (b) freshening events in shallow-water settings. Finally, the stratigraphic range of the

  12. La noción de trabajo en la construcción de la identidad: indígenas y criollos en el Pilcomayo salteño

    Catalina Buliubasich


    Full Text Available Con motivo de los reclamos por la propiedad de la tierra incoadas por comunidades indígenas chaquenses -mayoritariamente Wichí- aledañas al Pilcomayo salteño, el análisis se orientó a considerar qué factores intervinieron en la construcción de la identidad indígena, sobre todo frente a los criollos que ocupan esos mismos espacios. Estos, distribuidos en un patrón de asentamiento disperso, se ocupan del pastoreo de ganado, mientras que los indígenas desarrollan actividades de subsistencia, tanto las tradicionales, como la pesca en el río, caza, recolección de frutos silvestres y cultivos limitados, cuanto las no tan tradicionales de artesanías para el mercado o la venta temporaria de fuerza de trabajo. Tales diferencias en los usos del monte desembocaron en incompatibilidades y conflictos por la tierra entre las partes, que contribuyeron a la dinámica de la construcción de la identidad indígena, ocupando un lugar preponderante las visiones encontradas de lo que ambos grupos consideran trabajo.Due to the claim to own the land made by indigenous communities from Chaco -mostly Wichi- bordering the Salta 's Pilcomayo , this analysis was aimed to consider the factors that have intervened in the construction of the indigenous identity, especially in opposition to the criollos occupying the same area. The latter, distributed according to a pattern of scattered settlements, engage in cattle grazing, while indigenous people develop subsistence activities, both the traditional ones, such as fishing in the river, hunting, gathering wild fruits and limited farming and those not so traditional, such as craftmanship to be sold, or temporary workforce. Such differences in the use of the forest have provoked conflicts for the land between the parties. Those disagreements have contributed to the construction of the indigenous identity, and the different views on the concept of labor held by both groups have a relevant place in such construction.

  13. Medidas de controle de erosão em estradas rurais na bacia do rio das pedras, Guarapuava-PR / Erosion control measures of rural roads in the Rio das Pedras basin, Guarapuava, Paraná (Brazil

    Márcia Cristina da Cunha, ,


    Full Text Available O traçado das estradas que cortam grande número de rios e a drenagem lateral nas estradas faz com que as águas cheguem rapidamente à rede de drenagem aumentando a vazão. Disso resulta grande produção de sedimentos haja vista que algumas estradas e caminhos internos não possuem dissipadores de energia. Portanto o presente trabalho teve por objetivo analisar e discutir o sistema viário das estradas rurais da bacia do Rio das Pedras, Guarapuava-PR e a construção de caixas de contenção como medida preventiva para dissipar energia e conseqüentemente a entrada de sedimentos nos canais fluviais. No estudo utilizou-se de dados cartográficos e de campo para mensurar as estradas rurais e as caixas de contenção. Por meio da análise dos resultados constatou-se que o número de caminhos internos supera as estradas principais, que em grande parte não possui dissipadores de energia, potencializando a entrada de sedimentos nos cursos d‘água. Em dez pontos selecionados aleatoriamente verificou-se 792 cruzamentos de estradas rurais e cursos d’água. Nas estradas rurais com caixas de contenção verificou-se que em torno de 70% destas encontravam-se inativas, havendo uma deterioração em média de 10% do total de caixas de contenção mensuradas a cada dois anos.

  14. Zoneamento agroclimático da cultura do café para a Bacia do Rio Doce Agriculture-climatological zoning of coffee crop for the Rio Doce Basin

    Edson Luís Nunes


    Full Text Available Objetivou-se neste trabalho, através da geoespacialização, a identificação das regiões aptas, restritas e inaptas ao cultivo do café (Coffea arabica L. na Bacia do Rio Doce. Utilizou-se para tal, dados de temperatura e déficit hídrico de 50 estações meteorológicas instaladas na bacia e em bacias limítrofes. Os dados de déficit hídrico foram determinados utilizando o balanço hídrico segundo Thornthwaite & Mather (1955. Foram identificadas regiões equivalentes a um terço da bacia, localizadas na parte central e no nordeste da mesma, como sendo inaptas ao cultivo do café, conforme os critérios de produtividade relacionados com as exigências térmicas e hídricas da cultura.It was aimed in this work, through the geospatialization, the identification of the apt, restricted and inapt regions for cultivation of coffee (Coffea arabica L. in Rio Doce watershed. It was used for such, temperature and water deficit data of 50 meteorological stations installed in the watershed and in bordering watershed. The data of water deficit were determined using the water balance according to Thornthwaite & Mather (1955. They were identified equivalent regions the one third of the watershed, located in the central part and in the northeast of the same, as being inapt to the cultivation of coffee, according to the productivity criterions related with the thermal and hydric demands of culture.

  15. CONSIDERAÇÕES MORFOMÉTRICAS DA BACIA DO RIO UBERABINHA – MINAS GERAIS / Morphometric considerations of the Uberabinha river basin – Minas Gerais

    Antonio Feltran Filho


    Full Text Available The hydrographic basins demonstrate variables and attributes that make them unique. Themorphometric method that permits the utilization of techniques to obtain the indexes of existingnumber relations among the attributes of a drainage basin makes the knowledge of the variouslinear, area and hypsometric variables possible, which, added to the variable qualitatives,multiplies the possibilities for space analysis. The results obtained by this method serve as acomplement an aid to better explain the interaction that takes place among all the landscapeelements. This being the case, in this study, some basic morphometric surveys are sought in orderto obtain better knowledge of the hydrographic basin of the Uberabinha river, which will make itpossible to subsidize its planning. To reach this objective, cartographic maps from IBGE and theimage from the satellite TM/Landsat 5 from INPE to the scale of 1:100000 were used and computerprograms AutoCAD Map R13 and SPRING 4.2 were used to make the calculations. From theresults obtained, it was verified that the principal source of the Uberabinha river is, in realityfrom the Beija-Flor (Humming-bird creek and not from the Jacaré (Alligator stream. The greatdifference in the density of the rivers between the upper and lower thirds of the basin was alsoconfirmed. Another important geomorphological conclusion is the fact of its being a young basin.

  16. The expansion of the sugarcane in the hydrographic basin from Rio Brilhante, Mato Grosso do Sul state: the use of NDVI technique as an instrument for evidencing territorial dynamics

    Patricia Silva Ferreira


    Full Text Available The areas of sugarcane cultivation have expanding, often at the expense of the agricultural and pasture areas. Under this perspective, this manuscript aims to present a methodological guide in order to identify and to map up the areas of sugarcane cultivation, whose unity of analysis was located in the surrounding area of the Rio Brilhante hydrographic basin. We aimed to identify the changes through TM-Landsat5 and OLI-Landsat8 satellite pictures by comparing the scenarios from the years of 2001 and 2015, respectively. The classification of the vegetation was made through the technique of Normalized Difference Vegetation Index (NDVI. Thus, this study points that the use of some techniques and remote sensing tools, like NDVI, when used together with the field research, are extremely efficient for identifying the areas of the sugarcane cultivation.

  17. Georeferenced database generation with the purpose of hydrologic molding in reservoirs of the hydrographic basin of Jaguaribe river in the state of Ceará, Brazil Geração de base de dados georreferenciada com finalidade de modelagem hidrológica em reservatórios da bacia hidrográfica do rio Jaguaribe, Ceará, Brasil

    Raimundo A. de O. Leão


    Full Text Available The edafoclimatic conditions of the Brazilian semiarid region favor the water loss by surface runoff. The state of Ceará, almost completely covered by semiarid, has developed public policies for the construction of dams in order to attend the varied water demand. Several hydrological models were developed to support decisive processes in the complex management of reservoirs. This study aimed to establish a methodology for obtaining a georeferenced database suitable for use as input data in hydrological modeling in the semiarid of Ceará. It was used images of Landsat satellite and SRTM Mission, and soil maps of the state of Ceará. The Landsat images allowed the determination of the land cover and the SRTM Mission images, the automatic delineation of hydrographic basins. The soil type was obtained through the soil map. The database was obtained for Jaguaribe River hydrographic basin, in the state of Ceará, and is applicable to hydrological modeling based on the Curve Number method for estimating the surface runoff.As condições edafoclimáticas do semiárido brasileiro favorecem a perda de água por escoamento superficial. O Estado do Ceará,quase totalmente abrangido pelo semiárido, desenvolveu políticas públicas voltadas para a construção de açudes,a fim de atender à demanda hídrica diversificada. Vários modelos hidrológicos foram desenvolvidos para subsidiar os processos decisórios no complexo manejo dos reservatórios. Este trabalho teve como objetivo estabelecer uma metodologia para a obtenção de uma base de dados georreferenciada e adequada para uso como dados de entrada na modelagem hidrológica,no semiárido cearense. Foram utilizadas imagens de satélite Landsat e da missão SRTM, e mapa de solos do Estado do Ceará. As imagens Landsat possibilitaram determinar a cobertura do solo,e as imagens da missão SRTM, a delimitação automática das bacias hidrográficas. O tipo de solo foi obtido por meio do mapa de solos. A

  18. A rapid assessment of the decapod fauna in the Rio Tahuamanu and Rio Manuripi Basins, with new records of shrimps and crabs for Bolivia (Crustacea, Decapoda, Palaemonidae, Sergestidae, Trichodactylidae

    Célio Magalhães


    Full Text Available Results of a decapad fauna survey canducted during the AquaRAP expeditian to Río Tahuamanu and Río Manuripi Basins, in the Departmentaf Panda, Balivia, in September, 1996 are presented. Ten species of shrimps and crabs, representing three families and six genera were faund. New recards for Balivia were Macrobrachium depressimanum Pereira, 1993, Macrobrachium brasiliense (Heller, 1862, Acetes paraguayensis Hansen, 1919, Sylviocarcinus devillei H. Milne-Edwards, 1853, Sylviocarcinus maldonadoensis (Pretzmann, 1978, and valdivia serrata White, 1847.

  19. Fuzzy logic application for data correction of gamma ray profile and correlation with effective porosity of core from Resende Basin, Rio de Janeiro; Aplicacao da logica fuzzy para correcao de dados de perfil de raios gama e correlacao com porosidade efetiva de testemunhos da Bacia de Resende, Rio de Janeiro

    Souza, Francisco de Assis Leal de; Tunala, Leonardo Fernandes; Abreu, Carlos Jorge de; Lopes, Ricardo Tadeu, E-mail:, E-mail:, E-mail:, E-mail: [Universidade Federal do Rio de Janeiro (UFRJ/CCMN), RJ (Brazil). Centro de Ciencias Matematicas e da Natureza. Inst. de Geociencias. Dept. de Geologia; Rocha, Paula Lucia Ferrucio da, E-mail: [Universidade Federal do Rio de Janeiro (UFRJ), RJ (Brazil); Martins, Ricardo Rhomberg, E-mail: [Universidade Federal do Rio de Janeiro (UFRJ), RJ (Brazil). Escola Politenica de Engenharia; Lima, Inaya Correa Barbosa, E-mail: [Universidade Federal do Rio de Janeiro (UFRJ), RJ (Brazil). Centro de Tecnologia


    This work presents here a study on the porosity of cores from Resende Basin (Rio de Janeiro). The first step involved the selection, thinning of the material (core) and sample preparation for the use of porosimeter to obtain effective porosity. The material studied is sandstone, friable, coarse to very fine of three wells (GPR1, GPR2 and GPR3). The fuzzy logic (MatLab) was applied to the effective porosity data calculated from the gamma ray (GR) profile for the construction of a synthetic profile and from this we could identify the errors made in calculating the data. Then the results of porosity from the core were correlated with data from the corrected effective porosity (gamma ray profile) in order to prove the results obtained with both methods. The analysis of the synthetic porosity calculated by the fuzzy logic has shown that this is a promising method for assessing the quality of data and to obtain good fits. (author)

  20. Sequence stratigraphy of Taciba and Rio Bonito formations in Mafra, SC area, eastern Parana Basin, Brazil; Estratigrafia de sequencias das formacoes Taciba e Rio Bonito (Membro Triunfo) na regiao de Mafra/SC, leste da Bacia do Parana



    The Taciba and Rio Bonito ('lower' Triunfo Mbr) formations are divided into six depositional sequences based on cores, gamma-ray and electrical logs from shallow drillings from northern Santa Catarina State, Brazil. Each sequence is formed by two systems tracts, a lower one, sandy (low stand) and an upper one, shaly (high stand). The Taciba Formation has three sequences, S{sub 0} to S{sub 2}; sequence S{sub 0} has a thick turbidite sandstone at the base (Rio Segredo Member) that pinches out towards the eastern margin and even disappears in the Mafra outcrop area. Sequence S{sub 1} varies from a thin fluvial-estuarine system to a thick turbidite sandstone of a channelled fan system; S{sub 1} upper shaly system tract is marine in well PP-11, and it is glacially influenced in well PP-10. Sequence S{sub 2} is a thick sandstone body of shallow marine origin, but restricted to one well (PP-11); its upper shaly tract is dominated by massive siltstones intercalated with thin, distal tempestites. The 'lower' Triunfo Member (or 'Taciba- Triunfo transition') begins with the arrival of deltaic clastics of sequence S{sub 3} lower tract, coarsening-up from medial- to proximal delta front sandstones. Sequence S{sub 4} is quite similar to S{sub 3}, both showing sandstone pro gradation from north to south, as opposed to the southwest-sourced transgressive diamictites. Sequence S{sub 5} consists of fluvial deposits at well PP-12, and two transgressive cycles from wells PP-11 to PP-9, each one of them composed of fluvial-estuarine to marine systems. Well PP-10 is an exception, where the lower cycle presents de glaciation to marine deposits. (author)

  1. Sedimentary evolution of Rio do Rastro formation (permian-triassic of the Parana Basin) at central south portion of Santa Catarina State, Brazil; Evolucao sedimentar da Formacao Rio do Rastro (Permo-Triassico da Bacia do Parana) na porcao centro sul do estado de Santa Catarina, Brasil

    Warren, Lucas Verissimo; Roldan, Luis Fernando; Steiner, Samar dos Santos; Chamani, Marlei Antonio Carrari [Universidade de Sao Paulo (USP), SP (Brazil). Inst. de Geociencias. Programa de Pos Graduacao em Geoquimica e Geotectonica]. E-mail:; Almeida, Renato Paes de; Hachiro, Jorge; Machado, Romulo [Universidade de Sao Paulo (USP), SP (Brazil). Inst. de Geociencias. Dept. de Geologia Sedimentar e Ambiental


    Between the Late Carboniferous and the Early Triassic, the south portion of the Gondwana Supercontinent witnessed the development of intracratonic basins related with the coeval Sanrafaelic Orogeny. The continuous subsidence and consequent generation accommodation space resulted in the formation of a large confined water body and the accumulation of a transgressive regressive sequence between the Late Permian and the Early Triassic. The progradational nature of the upper portion of this sequence, represented by de Rio do Rasto e Piramboia formations, culminated with the complete filling of the water body. In the south-eastern portion of Santa Catarina State (Southern Brazil), the Rio do Rasto Formation overlies the Teresina formation and is overlain by the Piramboia formation, both contacts being characterized by lithological transition. The lower portion of the Rio do Rasto Formation is characterized by architectural elements deposited in offshore environments subject to storm action. A marked change of the color of the pelitic facies, from gray to red and purple occurs at the top of the unit. At this stratigraphic level, there is also a predominance of deltaic and eolian architectural elements. The intercalation of near shore and offshore architectural elements can be explained by the strong auto cyclic character expected in deltaic depositional systems and by the variation of relative rates of base-level rise. The occurrence of eolian architectural elements interbedded with subaquatically deposited sediments on the second third of the unit can be considered an evidence of continentalization to the top, materialized as the transition to the Piramboia desert system. (author)

  2. The paleozoic of Amazonas basin south edge: Tapajos river, Para state; O paleozoico da borda sul da bacia do Amazonas: rio Tapajos, estado do Para

    Matsuda, Nilo Siguehiko [Petrobras E e P, Rio de Janeiro, RJ (Brazil). Exploracao. Estratigrafia e Sedimentologia Geologia Aplicada a Exploracao], E-mail:; Winter, Wilson Rubem [Petrobras, Campoas dos Goytacases, RJ (Brazil). Exploracao. Sedimentologia e Estratigrafia], E-mail:; Wanderley Filho, Joaquim Ribeiro; Cacela, Alessandra Suzely Moda [Petrobras, Manaus, AM (Brazil). Exploracao. Unidade de Operacoes de Exploracao e Producao da Amazonia], Emails:,


    The intracratonic Amazonas Basin covers an area close to 500.000km{sup 2} shared between the Amazonas and Para states. The phanerozoic stratigraphic framework is up to 6.000m thick and may be subdivided into two, first order depositional sequences: the Paleozoic sequence, intruded by diabase dikes and sills and the Mesozoic-Cenozoic sequence. Analyzing the stratigraphic framework, the great tectonic influence on the basin development can be appreciated. The mainly NW-SE structural directions of the basement, which mark the boundaries of the geochronological provinces of the Amazonas, are clearly identified along the Tapajos River. The Paleozoic sequence outcrops on the southern border of the Amazonas Basin embraces potential source rocks, reservoirs and seal rocks. They can be subdivided in three, second order sequences, limited by regional unconformities, as: the Ordovician/Devonian, which corresponds to the Pitinga lithostratigraphic formation; the Devonian-Tournaisian, which corresponds to the Maecuru, Erere, Barreirinha and Curiri formations and, the Pensylvanian-Permian that are represented by the Monte Alegre and Itaituba formations. This field trip guide presents these classic lithostratigraphic outcrop units, together with a brief sedimentological description and an analysis of their positioning related to sequence stratigraphical concepts. (author)

  3. Diversidade de peixes do reservatório da UHE Escola Engenharia Mackenzie (Capivara, Rio Paranapanema, bacia do alto rio Paraná, Brasil, e a importância dos grandes tributários na sua manutenção Fish diversity in the UHE Escola Engenharia Mackenzie (Capivara reservoir, Paranapanema River, upper Rio Paraná basin, Brazil, and the importance of large tributaries in its maitenance

    Ana Cecília Hoffmann


    Full Text Available As espécies foram coletadas em quatro trechos ao longo de um gradiente formado pelo reservatório UHE Escola Engenharia Mackenzie (Capivara. A diversidade de espécies foi analisada pela constância, índice de Shannon-Wiener e similaridade da composição entre trechos através do coeficiente de Jaccard. O reservatório tem uma riqueza de peixes composta por 67 espécies incluídas em 5 ordens; 47% das espécies são constantes, 15 % são acessórias e 28% são acidentais. Os maiores índices de diversidade de Shannon-Wiener e similaridade de Jaccard foram obtidos em Cinzas e Tibagi, que são os trechos mais distantes da barragem e que apresentam grandes tributários. Os menores índices foram encontrados em Cruzália e Porecatu, os quais correspondem aos trechos com características, respectivamente, de ambientes lótico e semi-lótico. Este trabalho demonstra a extrema importância da presença dos tributários para a manutenção da diversidade das espécies em um reservatório, em função da preservação das características originais do sistema lótico naqueles trechos e conseqüente redução do impacto do represamento.Fish samples were taken in four stretches along a gradient formed by the UHE Escola Engenharia Mackenzie (Capivara reservoir. The diversity of species was analyzed by the constance, index of Shannon-Wiener and similarity of the composition among stretches through the Jaccard's coefficient. The reservoir presents a richness of fishes composed by 67 species distributed in 5 orders; 47% of the species are constant, 15% are accessory and 28% are accidental. The highest values of Shannon-Wiener diversity and Jaccard's similarity were obtained in Cinzas and Tibagi, wich are the most distant points from the dam and which present large tributaries. The lowest values were found in Cruzália and Porecatu, which respectively correspond to the stretches with lotic and semi-lotic environmental characteristics. This work demonstrates


    Sâmia Maria Tauk-Tornisielo


    Full Text Available This study was concerned to distinguish the main environmental and socio-economic aspects of 16 fee-fishing located in the Corumbataí river basin, São Paulo. Together, it verified the possibility of effluent treatment system with these units constructed wetlands system (CWS. Previously, it collected information on the number, location and diversity of activities of fee-fishing, as different government agencies and institutions did not have that information. Questionnaires were applied to collect information about the socio-economic and environmental aspects of fee-fishing units located in Corumbatai river basin. Were determinate abiotic and biotic factors present in water and effluent from the tanks of fee-fishing. It was applied a principal component analysis to the values of these factors monitored. The results showed that despite being a tourist attraction for the region and there is a considerable frequency of tourists on fee-fishing, it is still an activity that is economically unstable in Corumbataí River Basin. The results of the tests performed were compared with the limits for class 2 freshwater by CONAMA Resolution 357/05. These results showed that most of the values of the factors studied were above the limit established by this resolution, showing deterioration of water quality of the fee-fishing in this study. From an environmental standpoint, the fish-pay were considered potentially polluting sources, characterized by higher values of total nitrogen, ammonia, nitrite, nitrate, conductivity, turbidity, total phosphorus and microorganisms. The presence of excessive nutrients in the effluents in water is responsible for eutrophication and may indicate impairment of water quality of rivers in the basin study. Thus, the effluents from fish-you may pay in need of treatment, such as stabilization ponds and wastewater treatment systems using aquatic weeds before they are discarded into the environment. = Neste estudo preocupou

  5. Rio carnival

    Alex Miller


      With the Rio 2016 Olympic and Paralympic Games due to start in August, Brazil is hoping that a financial crisis and a dramatic cost-cutting of the Games budget will all be forgotten once the two-week...

  6. Rio+20

    Robert Horn


    Full Text Available This reflection on Rio+20 examines many of the major social institutions and how they fulfilled their functions during the United Nations Conference on Sustainable Development at Rio. The institutions are: 1. Nation-states as a collective. 2. Individual nation-states. 3. Vanguard institutions (some NGOs. 4. Action and convening NGOs. 5. Global media. 6. Governments of nation-states acting domestically 7. Individual governments in bilateral and multilateral situations. 8. Similar institutions in different countries acting together. 9. Businesses. 10. Global science. Each is considered within the assumptions of what the society expects them to deliver (in general, what is possible for them to deliver, and what they did deliver at Rio. In approaching Rio+20, our account differs considerably from much of the reportage by the mainstream media.

  7. Elementos traço na água e em vísceras de peixes da Bacia Hidrográfica Butuí-Icamaquã, Rio Grande do Sul, Brasil Trace elements in water and viscera of fish from Butuí-Icamaquã Basin, Rio Grande do Sul, Brazil

    Luiz Carlos Santos Porto


    Full Text Available Metais pesados, também denominados elementos traço, podem ser essenciais ao metabolismo de organismos vivos, e, ao mesmo tempo, dependendo de suas concentrações, altamente tóxicos. Com o objetivo de investigar a toxicidade da água da Bacia dos Rios Butuí-Icamaquã, na fronteira oeste do Rio Grande do Sul, foram analisados, através de espectrofotômetro de absorção atômica, os teores de alumínio, cádmio, chumbo, cobre, cromo, manganês, níquel e zinco em vísceras abdominais de peixes, coletados, entre junho de 2007 e fevereiro de 2008, em pontos determinados nos rios Butuí, Icamaquã e Uruguai. Mostraram-se acima do nível considerado seguro para consumo humano: alumínio, cádmio, manganês e níquel e teores próximos aos limites legais foram encontrados para cobre e cromo. A análise simultânea de amostras da água coletadas nos mesmos locais acusou em espectrofotômetro de luz visível, níveis superiores aos limites legais de bromo, chumbo, cianeto, cobre, cromato, fenóis, fosfato, manganês e sulfeto. Estes elementos, em tais concentrações na água e nos peixes, podem comprometer o ecossistema ou representar riscos à saúde humana.Heavy metals, also called trace elements, may be essential to the metabolism of living organisms, and at the same time, depending on their concentrations, highly toxic. With the objective to investigate the toxicity of water of the Butuí-Icamaquã Rivers Basin on the border west of Rio Grande do Sul, were analyzed by atomic absorption spectrophotometer, the contents of aluminum, cadmium, chromium, copper, lead, manganese, nickel and zinc in abdominal viscera of fish, collected between June 2007 and February 2008, at selected points in Butuí, Icamaquã and Uruguai rivers. Aluminum, cadmium, manganese and nickel were above the levels considered safe for human consumption and levels near the legal limit were found for chrome and copper. The simultaneous analysis of water samples collected in

  8. Soil and water losses in eucalyptus plantation and natural forest and determination of the USLE factors at a pilot sub-basin in Rio Grande do Sul, Brazil

    Bárbara Pereira Christofaro Silva

    Full Text Available ABSTRACT Monitoring water erosion and the factors that control soil and water loss are essential for soil conservation planning. The objective of this study was to evaluate soil and water losses by water erosion under natural rainfall in eucalyptus plantations established in 2001 (EF2, and 2004 (EF1, native forest (NF and bare soil (BS, during the period of 2007 to 2012; and to determine the USLE factors: rain erosivity (R, erodibility (K of a Red Argisol and the cover-management factor (C for EF1, EF2 and NF at a pilot sub-basin, in Eldorado do Sul, RS, Brazil. The R factor was estimated by the EI30 index, using rainfall data from a gauging station located at the sub-basin. The soil and water losses were monitored in erosion plots, providing consistent data for the estimation of the K and C factors. The sub-basin presented an average erosivity of 4,228.52 MJ mm ha-1 h-1 yr-1. The average annual soil losses em EF1 and EF2 (0.81 e 0.12 Mg ha-1 year-1, respectively were below of the limit of tolerance, 12.9 Mg ha-1 year-1. The percentage values of water loss relating to the total rainfall decreased annually, approaching the values observed at the NF. From the 5th year on after the implantation of the eucalyptus systems, soil losses values were similar to the ones from NF. The erodibility of the Red Argisol was of 0.0026 Mg ha h ha-1 MJ-1mm-1 and the C factor presented values of 0.121, 0.016 and 0.015 for EF1, EF2 and NF, respectively.

  9. Soil gamma ray spectrometry of the Buquira river basin, SP, Brazil; Gamametria de solos da bacia do rio Buquira, SP, Brazil

    Rivera, Alice


    Natural radioactivity found in rocks and its evaluation been frequently used for studies of environmental geochemistry, particularly those of detection and control of pollutants and the consequent changes in environment after antropic interferences. In this work natural radioactivity in forty nine soil samples in the basin of Buquira river, at the Northeast region of Sao Paulo State, has been analysed and measured with a Ge-HP gamma ray spectrometer. A table with the most relevant results found in rocks is shown and discussed. (author)

  10. Flora arbórea da bacia do rio Tibagi (Paraná, Brasil: Celastrales sensu Cronquist Tree flora of the Tibagi river basin (Paraná, Brazil: Celastrales sensu Cronquist

    Ricardo Augusto Gorne Viani


    Full Text Available Este trabalho estudou, por meio de coleções de herbários, os representantes arbóreos da ordem Celastrales sensu Cronquist, encontrados na bacia do rio Tibagi, estado do Paraná, Brasil. Esta bacia hidrográfica, subdividida em três zonas de norte para sul, baixo Tibagi (BT, médio Tibagi (MT e alto Tibagi (AT, apresenta diferentes condições ambientais e tipos de vegetação ao longo de sua extensão. A ordem Celastrales está representada na bacia estudada por 15 espécies arbóreas, pertencentes às famílias Aquifoliaceae, Celastraceae e Icacinaceae. Icacinaceae conta com apenas duas espécies, Citronella gongonha e C. paniculata, sendo a primeira distinta pelo ovário glabro e folhas geralmente com espinhos. Aquifoliaceae contém seis espécies: Ilex brasiliensis, I. brevicuspis, I. chamaedryfolia, I. dumosa, I. paraguariensis e I. theezans, que ocorrem preferencialmente no AT e MT e se distinguem pela dimensão, revestimento, ápice e margem da folha e pela morfologia das sépalas. Celastraceae está representada por sete espécies pertencentes a dois gêneros, Plenckia populnea, espécie de cerrado, encontrada apenas no MT e seis espécies de Maytenus (M. aquifolia, M. dasyclada, M. evonymoides, M. ilicifolia, M. robusta e M. salicifolia, com distinção baseada principalmente no tipo de margem e dimensão das folhas, forma do ramo e número de flores por inflorescência.A study of the tree species of the order Celastrales sensu Cronquist from the Tibagi river basin, Paraná state, Brazil, is presented, based on herbarium material. This basin is subdivided into three zones, from north to south: lower Tibagi (BT, mid Tibagi (MT and upper Tibagi (AT, each with different environmental conditions and vegetation types. The order Celastrales is represented in the basin by 15 tree species belonging to three families: Aquifoliaceae, Celastraceae and Icacinaceae. Icacinaceae has only two species, Citronella gongonha and C. paniculata. The

  11. Environmental isolation of Cryptococcus gattii VGII from indoor dust from typical wooden houses in the deep Amazonas of the Rio Negro basin.

    Brito-Santos, Fábio; Barbosa, Gláucia Gonçalves; Trilles, Luciana; Nishikawa, Marília Martins; Wanke, Bodo; Meyer, Wieland; Carvalho-Costa, Filipe Anibal; Lazéra, Márcia dos Santos


    Cryptococcosis is a human fungal infection of significant mortality and morbidity, especially in the meningoencephalitis form. Cryptococcosis is distributed worldwide and its agents, C. neoformans and C. gattii, present eight major molecular types-VNI-VNIV and VGI-VGIV respectively. The primary cryptococcosis caused by molecular type VGII (serotype B, MAT alpha) prevails in immunocompetent patients in the North and Northeast of Brazil, revealing an endemic regional pattern to this molecular type. Since 1999, C. gattii VGII has been involved in an ongoing outbreak in Canada, and is expanding to the Northwest of the United States, two temperate regions. Exposure to propagules dispersed in the environment, related to various organic substrates, mainly decomposing wood in and around dwellings, initiates the infection process. The present study investigated the presence of the agents of cryptococcosis in dust from dwellings in the upper Rio Negro, municipality of Santa Isabel do Rio Negro in Amazonas state. Indoor dust was collected from 51 houses, diluted and plated on bird seed agar. Dark brown colonies were identified phenotypically, and genotypically by URA5 restriction fragment length polymorphism analysis and multilocus sequence typing (MLST). The mating type was identified using pheromone-specific primers. Three of the 51 houses were positive for C. gattii molecular type VGII, MATα and MATa, showing a high prevalence of this agent. MLST studies identified eight subtypes, VGIIb (ST7), VGIIa (ST20), (ST5) and 5 new subtypes unique to the region. For the first time in the state of Amazonas, C. gattii VGII MATα and MATa were isolated from the environment and correlates with endemic cryptococcosis in this state. This is the first description of MLST subtypes on environmental isolates in the Brazilian Amazon, indicating domiciliary dust as a potential source for human infection with different subtypes of C. gattii VGII MATα and MATa.

  12. Environmental isolation of Cryptococcus gattii VGII from indoor dust from typical wooden houses in the deep Amazonas of the Rio Negro basin.

    Fábio Brito-Santos

    Full Text Available Cryptococcosis is a human fungal infection of significant mortality and morbidity, especially in the meningoencephalitis form. Cryptococcosis is distributed worldwide and its agents, C. neoformans and C. gattii, present eight major molecular types-VNI-VNIV and VGI-VGIV respectively. The primary cryptococcosis caused by molecular type VGII (serotype B, MAT alpha prevails in immunocompetent patients in the North and Northeast of Brazil, revealing an endemic regional pattern to this molecular type. Since 1999, C. gattii VGII has been involved in an ongoing outbreak in Canada, and is expanding to the Northwest of the United States, two temperate regions. Exposure to propagules dispersed in the environment, related to various organic substrates, mainly decomposing wood in and around dwellings, initiates the infection process. The present study investigated the presence of the agents of cryptococcosis in dust from dwellings in the upper Rio Negro, municipality of Santa Isabel do Rio Negro in Amazonas state. Indoor dust was collected from 51 houses, diluted and plated on bird seed agar. Dark brown colonies were identified phenotypically, and genotypically by URA5 restriction fragment length polymorphism analysis and multilocus sequence typing (MLST. The mating type was identified using pheromone-specific primers. Three of the 51 houses were positive for C. gattii molecular type VGII, MATα and MATa, showing a high prevalence of this agent. MLST studies identified eight subtypes, VGIIb (ST7, VGIIa (ST20, (ST5 and 5 new subtypes unique to the region. For the first time in the state of Amazonas, C. gattii VGII MATα and MATa were isolated from the environment and correlates with endemic cryptococcosis in this state. This is the first description of MLST subtypes on environmental isolates in the Brazilian Amazon, indicating domiciliary dust as a potential source for human infection with different subtypes of C. gattii VGII MATα and MATa.

  13. Resíduos Sólidos na Bacia do Rio Ivinhema-MS | Solid Waste in River Basin Ivinhema-MS

    Flávia Akemi Ikuta


    Full Text Available Normal 0 21 false false false PT-BR X-NONE X-NONE Introdução: O trabalho apresenta parte dos resultados da pesquisa intitulada “Geração e disposição de resíduos sólidos urbanos e as formas de organização dos trabalhadores catadores de resíduos recicláveis nos municípios localizados na bacia do rio Ivinhema-MS”, realizada com apoio do CNPq. A área estudada compreende um conjunto de 25 municípios, localizados na bacia do Rio Ivinhema, na região sudeste do Estado de Mato Grosso do Sul, com uma população total aproximada de 675.569 habitantes, sendo 81,92% urbana (IBGE, Censo 2010. Dentre os principais objetivos destacam-se: realizar um diagnóstico da situação da produção e destinação de resíduos sólidos; e contribuir para a identificação de ações prioritárias a serem desenvolvidas na área, tendo em vista o melhor gerenciamento dos resíduos sólidos. Metodologia/Desenvolvimento: O desenvolvimento da pesquisa apoiou-se em ampla revisão bibliográfica sobre as principais questões teórico-metodológicas ligadas ao tema escolhido, o que fundamentou sua melhor compreensão e orientação da pesquisa, bem como a coleta de dados de fontes secundárias. Os principais instrumentos utilizados para a coleta de dados foram: questionários, aplicados junto às prefeituras municipais, empresas envolvidas no manejo de resíduos e organizações de catadores (associações ou cooperativas; entrevistas não estruturadas, para esclarecimento de dúvidas sobre os questionários e complementação de informações; e observações realizadas em trabalho de campo nos locais de disposição dos diversos tipos de resíduos sólidos urbanos, para complementar dados, obter informações com registros fotográficos e confrontar os dados informados em questionários. Após a coleta, foi realizada a tabulação e sistematização, facilitando a verificação de semelhanças, diferenças, relações e inter-relações entre os dados. Em

  14. Toxicidad aguda por cinc en Cnesterodon decemmaculatus (Pisces: Poeciliidae y aplicación del Modelo de Ligando Biótico en agua del Río Pilcomayo (Sudamérica

    M. V. Casares


    (peces del BLM desarrollado para el zinc en agua del río Pilcomayo. Se llevó a cabo un ensayo de toxicidad aguda del zinc en el pez nativo Cnesterodon decemmaculatus. Las concentraciones de zinc disuelto aplicadas fueron: 0,13; 3,74; 9,2; 21,6 y 26,4 mg Zn L-1. La concentración letal media del zinc (CL50 96-h calculada para C. decemmaculatus fue 22,6 mg Zn L-1 (17,5 - 27,6 y la predicha por el BLM para Pimephales promelas en el agua experimental fue 1,71 mg L-1. Las concentraciones de zinc medidas excedían la solubilidad del metal lo que produjo la precipitación del mismo, derivando en una 96-h CL que muy probablemente incluyó tanto especies de zinc 50 disueltas como precipitadas. Sin embargo, las estimaciones de la especiación mostraron que la especie química del zinc más abundante en todos los tratamientos fue el ion libre. La mayor proporción de zinc en su forma iónica libre explicaría el bajo efecto protector de la elevada dureza del agua experimental. La diferencia entre la toxicidad del zinc observada y la predicha por el BLM podría deberse a la combinación de inexactitud en las mediciones de zinc disuelto y una menor sensibilidad de la especie experimental a la presencia de elevadas concentraciones de zinc.

  15. Ocorrência e ecologia trófica de quatro espécies de Astyanax (Characidae em diferentes rios da bacia do rio Tibagi, Paraná, Brasil Occurrence and trophic ecology of four species of Astyanax (Characidae in different rivers of the Tibagi River Basin, Paraná, Brazil

    Sirlei Terezinha Bennemann


    Full Text Available Na bacia do rio Tibagi, trechos dos rios Fortaleza, Iapó e Tibagi foram amostrados mensalmente, de maio de 2001 a abril de 2002, com tarrafas e redes de espera de diferentes malhagens. Foram capturados indivíduos de quatro espécies de Astyanax. Para conhecer como essas espécies utilizam o hábitat desses rios, foi calculada a constância, e as freqüências em número de exemplares foram comparadas pela análise de similaridade Bray-Curtis. A composição percentual dos alimentos consumidos foi ordenada usando-se a Análise de Componentes Principais (ACP. As proporções dos recursos alimentares foram avaliadas e classificadas quanto à natureza (animal ou material vegetal e origem (alóctone e autóctone. A constância e a baixa similaridade na abundância revelaram que as espécies têm preferências quanto ao porte do rio ou por determinado hábitat. Astyanax altiparanae Garutti & Britski, 2000 e A. fasciatus (Cuvier, 1819 ocorreram nos de maior porte, mas foram constantes somente no rio Tibagi. Astyanax eigenmanniorum (Cope, 1894 ocorreu em todos os rios, mas prefere hábitats próximos às desembocaduras de afluentes de grandes rios. Astyanax scabripinnis (Jenyns, 1842 esteve restrita ao Fortaleza, o rio de menor porte, subafluente do rio Tibagi. O número de itens alimentares consumidos variou de 11 a 23. Entre os alimentos principais, três itens foram comuns para as quatro espécies: restos de plantas (folhas e sementes de plantas terrestres, restos de insetos (de diferentes origens e não identificados e plantas aquáticas. Os vegetais e os insetos foram os principais alimentos para todas as espécies. A maior distinção na composição da dieta foi constatada para A. eigenmaniorum, devido à sua habilidade em explorar as plantas aquáticas, presentes em abundância, consumidas junto com carvão/sedimento, que estavam nas margens rochosas do rio Iapó. A similaridade quanto à origem e ao tipo de alimento consumido pelas quatro esp

  16. Taphonomy of Condensed Shell Storm beds of the Teresina Formation in Rio Preto (State of Paraná, Middle Permian, Paraná Basin: Paleoenvironmental Implications

    Jacqueline Peixoto Neves


    Full Text Available The deposits of the Permian Teresina Formation are mainly characterized by fi ne-grained siliciclastic rocks and centimetricintercalations of tempestites (bioclastic sandstones and coquinas. Despite the relevance of the bivalve-rich carbonate bedsof the Teresina Formation to paleoenvironmental studies, their taphonomy is still poorly studied. The fossil concentrationstudied in this work was found in a quarry in the city of Irati, Rio Preto district, Paraná State. The fossil concentration is locatedin the middle/upper portion of the unit, far from the top. The studied bed is a bioclastic, intraclastic, peloidal, grainstone/packstone, with abundant bivalve shell fragments, pelitic and micritic intraclasts, peloids, rare ooids and oncoids, as well aspermineralized of Lycophyta microphylles and fi sh scales. The grains of this carbonate concentration show: high degree oftime-averaging, variable degree of packing (dense to disperse, no sorting and chaotic orientation. Notably, the concentrationincludes a mixture of elements which are indicative of: a restrictive, low energy, carbonate environment (peloids, ooidsand oncoids; b subaerial environment surrounding the main body of water (Lycophyta microphylles and c quiet-waterenvironment punctuated by storm events, where the suspension-feeding bivalves thrived. At least four depositional eventscaused by storm fl ows were recorded. The amalgamated nature of the bed is a result of storm events in an intracratonic basinwith very low seafl oor slope and low rates of sedimentation and subsidence.

  17. Mapeamento do potencial de erosão laminar na bacia do rio Japaratuba, SE, via SIG Mapping the laminar erosion potential for the Japaratuba river basin, SE via GIS

    Ricardo de Aragão


    Full Text Available A erosão do solo é a principal causa do empobrecimento precoce de terras produtivas e dentre as suas formas está a erosão laminar. Esta se caracteriza não apenas pela remoção de uma camada relativamente uniforme da superfície, mas também por seus nutrientes, sendo intensificada, portanto, pelas ações antrópicas. Para evitar ou reduzir seus impactos, fazem-se necessárias diretrizes para a adequação do uso e da ocupação às condições de cobertura vegetal, tipo de solo e topografia, através de mapas do potencial erosivo laminar da região de interesse, obtidos via sistemas de informações geográficas (SIG. Neste trabalho foi desenvolvido o mapeamento do potencial erosivo laminar da bacia do rio Japaratuba, SE (1685 km²; trata-se de uma região sujeita a intensa atividade agrícola, pecuária e de mineração, onde só restam 6% da vegetação nativa. Os resultados mostram que 48,71% da área da bacia ficam nas classes de médio e alto potencial erosivo, indicando que a bacia está bastante impactada devido aos usos inadequados para as condições de solo e declividades.Soil erosion is a natural phenomenon that reduces soil fertility and causes a great impact on agricultural areas. Laminar erosion is characterized by the removal of the top soil fairly uniformly as well as its nutrients, which is accelerated by human activities. To minimize the impacts it is necessary to adopt an adequate soil management that takes into account the type of the soil, relief, and vegetation cover. The soil management can be aided by mapping the erosive potential of a region using GIS tools. In this work, the technique that was used for mapping the erosive potential in the Japaratuba River Basin (1685 km² located in the State of Sergipe is presented. The results show that 48.71% of the basin area lie within medium and high erosive potentials zones, suggesting the inadequate land use for the soil types and relief within the basin.

  18. New species of Cacatuocotyle (Monogenoidea, Dactylogyridae) parasitizing the anus and the gill lamellae of Astyanax aeneus (Pisces, Ostariophysi: Characidae) from the Rio Lacantún basin in the Biosphere Reserve of Montes Azules, Chiapas, Mexico.

    Franco, Edgar F Mendoza; Caspeta-Mandujano, J M; Salgado-Maldonado, G


    As part of a biological inventory of the Rio Lacantún basin in the Biosphere Reserve of Montes Azules from Chiapas State (southeastern, Mexico), the following monogenoid ectoparasites infecting the external surface of the anal opening and the gill lamellae of the freshwater fish Astyanax aeneus (Characidae) in ten streams were found: Cacatuocotyle chajuli sp. nov. (anus), Cacatuocotyle exiguum sp. nov., and Cacatuocotyle sp. (gill lamellae). C. chajuli is differentiated from its single congener, Cacatuocotyle paranaensis (Boeger et al. Syst Parasitol 36:75-78, 1997), from the gills of Characidium lanei (Characidae) from Paraná Brazil, in having a noticeably V-shaped haptoral bar and larger hooks and anchors. C. exiguum differs from these two latter species in the size of its anchors. Illustrations and data on morphological and biometric variability of individual specimens of C. chajuli and C. exiguum from different streams are provided. The present data support the statement about three species of Astyanax, which harbor the richest monogenoidean diversity in the Neotropics with a total of 18 species reported up to now. Occurrences of species of Cacatuocotyle on different sites of infection on three distant host species [including a Neotropical cichlid (Cichlidae) species] suggest that these monogenoideans switching to new hosts can result in the availability of potential hosts within the same habitat instead of showing signs of preferential switching between closely related hosts or on their respective microhabitats.

  19. Cladocerans from gut contents of fishes associated to macrophytes from Taquari River Basin, MS, Brazil Cladóceros do conteúdo estomacal de peixes associados a macrófitas da Bacia do Rio Taquari, MS, Brasil

    Adriana Maria Güntzel


    Full Text Available AIM: The aim of this study was to identify the cladocerans species from the gut contents of fishes sampled in an oxbow lake from Taquari River Basin, MS, with the specific view of investigating the importance of these crustaceans in the fishes diets; METHODS: Sampling was carried out in April and August of 2005 (dry season and January of 2006 (wet season. The fish were captured with a sieve. In the laboratory, individuals were identified and stomachs were removed and weighed. The stomach contents were identified, and a Feeding Index calculated; RESULTS: The items most consumed by fishes were filamentous algae, Cladocera and detritus. The Cladocera were especially important in the August and January samples, and consisted primarily of Chydoridae; cladocerans were most consumed by species of Serrapinnus and by Mesonauta festivus. Fish fed more in April, with decreases occurring in stomach fullness on the other two sampling dates. CONCLUSIONS: Cladocerans associated with macrophytes may be an important food source for small fish individuals in marginal lakes from Taquari River Basin. The relative importance of the Chydoridae in the guts may have been due to the high relative abundance and species richness of this group in the environment. A short discussion on fish feeding habits was included in the text.OBJETIVO: Este estudo teve por objetivo identificar as espécies de cladóceros presentes no conteúdo estomacal de peixes amostrados em uma lagoa marginal da Bacia do Rio Taquari, MS, visando avaliar a importância destes crustáceos na dieta dos peixes; MÉTODOS: A amostragem foi realizada em abril e agosto de 2005 (estação seca e janeiro de 2006 (estação chuvosa. Os peixes foram capturados com um peneirão. Em laboratório, os indivíduos foram identificados até o nível de espécie e os estômagos removidos e pesados. O conteúdo estomacal foi identificado e um Índice Alimentar calculado. RESULTADOS: Os itens mais consumidos pelos peixes

  20. Demanda de irrigação da cultura da uva na Bacia do Rio São Francisco Irrigation demand for grape crop in San Francisco River Basin

    Wallisson da S. Freitas


    Full Text Available Visando subsidiar o planejamento de projetos agrícolas para o dimensionamento de projetos de irrigação e a gestão de recursos hídricos, estimou-se e se espacializou a demanda de irrigação da videira (Vitis vinifera L., cv. Itália, na bacia do Rio São Francisco. Utilizaram-se séries históricas de dados de 81 estações climáticas distribuídas na bacia. Para cada estação calculou-se os valores, máximos diários e o total anual, da evapotranspiração de referência (ETo, da evapotranspiração da cultura (ETc, da demanda suplementar da cultura e da demanda suplementar de irrigação (este com eficiência de 70%. Com base nos resultados obtidos, concluiu-se que: (a a ETc máxima diária variou, em grande parte da bacia, de 4,5 a 5,7 mm d-1, tendo média anual de 943 mm; (b em média, a demanda anual suplementar da cultura foi 839,5 mm, equivalente a 103,5 mm inferior à ETc; (c o fato do sistema funcionar com 70% de eficiência, em vez de 90%, implica em acréscimo estimado de 18.808.755 m³ de água por ano, somente nas microrregiões de Juazeiro, BA e Petrolina, PE.The irrigation water demand of the grapevine (Vitis vinifera L. cv. Italy was estimated and spatialized in San Francisco River Basin, in order to subsidize the agricultural project planning and water resource management. Historical data series relative to 81 climatic stations distributed throughout the basin were used. The maximum daily values and the annual total values of the reference evapotranspiration (ETo, crop evapotranspiration (ETc, supplementary demand of the crop and the supplementary irrigation demand (70% efficiency were calculated for each station. According to the results, the following conclusions were drawn: (a in a large area of the basin, the maximum daily ETc varied from 4.5 to 5.7 mm d-1, with an annual mean of 943 mm; (b the supplementary annual demand of the crop averaged 839.5 mm, corresponding to 103.5 mm less than ETc; and (c the irrigation

  1. Stratigraphy sequence analysis application for multi scalar characterization of paralic reservoirs - an example in the Guata group (E O-Permian) of the Parana Basin, in the state of Rio Grande do Sul, Brazil; Aplicacao da estratigrafia de sequencias para caracterizacao multiescalar de reservatorios paralicos - um exemplo no Grupo Guata (EO-Permiano) da Bacia do Parana, no Rio Grande do Sul, Brasil

    Kuechle, Juliano [Rio Grande do Sul Univ., Porto Alegre, RS (Brazil). Inst. de Geociencias. Curso de Pos-graduacao em Geociencias]. E-mail:; Holz, Michael [Rio Grande do Sul Univ., Porto Alegre, RS (Brazil). Inst. de Geociencias]. E-mail:


    Detailed stratigraphic analysis of the Early Permian Rio Bonito and Palermo Formations of the Parana Basin in the region of Sao Gabriel County has been used for a study on reservoir characterization of paralic sandstones. Two main depositional systems were recognized, a fluvial-dominated delta system and a wave-dominated barrier island system. The succession is divided in two third-order depositional sequences, enclosing thirteen fourth-order para sequences. This high-resolution stratigraphic framework was the base for a multi scale approach on reservoir characterization of the sandstone bodies. Reservoir heterogeneities are discussed, staring from the scale of depositional sequence (heterogeneity level 1), passing down to heterogeneity at the scale of systems tracts (heterogeneity level 2) and finalizing with an approach at para sequence scale (heterogeneity level 3). Main control on heterogeneity at the first level is base-level variation as generating mechanism for un conformities at the sediment type and rate. At the second level, the reservoir heterogeneity is controlled by the lateral and vertical variations in thickness of particular systems within the different systems tracts, and at the third level, the heterogeneity occurs controlling reservoir continuity and connectivities between reservoirs. The study supplies a model which is useful as a predictive tool for similar geologic settings in producing oil fields. (author)

  2. Concentrations and isotope ratios of mercury in sediments from shelf and continental slope at Campos Basin near Rio de Janeiro, Brazil.

    Araujo, Beatriz Ferreira; Hintelmann, Holger; Dimock, Brian; Almeida, Marcelo Gomes; Rezende, Carlos Eduardo


    Mercury (Hg) may originate from both anthropogenic and natural sources. The measurement of spatial and temporal variations of Hg isotope ratios in sediments may enable source identification and tracking of environmental processes. In this study we establish the distribution of mercury concentrations and mercury isotope ratios in surface sediments of three transects along the continental shelf and slope in Campos Basin-RJ-Brazil. The shelf showed on average lower total Hg concentrations (9.2 ± 5.3 ng g(-1)) than the slope (24.6 ± 8.8 ng g(-1)). MMHg average concentrations of shelf 0.15 ± 0.12 ng g(-1) and slope 0.13 ± 0.06 ng g(-1) were not significantly different. Distinct differences in Hg isotope ratio signatures were observed, suggesting that the two regions were impacted by different sources of Hg. The shelf showed more negative δ(202)Hg and Δ(199)Hg values ranging from -0.59 to -2.19‰ and from -0.76 to 0.08‰, respectively. In contrast, the slope exhibited δ(202)Hg values from -0.29 to -1.82‰ and Δ(199)Hg values from -0.23 to 0.09‰. Mercury found on the shelf, especially along the "D" and "I" transects, is depleted in heavy isotopes resulting in more negative δ(202)Hg compared to the slope. Isotope ratios observed in the "D" and "I" shelf region are similar to Hg ratios commonly associated with plants and vegetation and very comparable to those detected in the estuary and adjoining mangrove forest, which suggests that Hg exported from rivers may be the dominating source of Hg in near coastal regions along the northern part of the shelf. Copyright © 2017 Elsevier Ltd. All rights reserved.

  3. A pesca comercial na bacia do rio Madeira no estado de Rondônia, Amazônia brasileira The Commercial fisheries of the Madeira river basin in the Rondônia state, brazilian Amazon

    Carolina Rodrigues da Costa Doria


    Full Text Available Este estudo caracteriza quali e quantitativamente a atividade pesqueira comercial na bacia do rio Madeira, afluente do rio Amazonas, no trecho entre Guajará-Mirim e Porto Velho, estado de Rondônia. No período de janeiro a dezembro/2004, foram registrados 460 t, correspondendo 935 viagens. A análise dos dados oriundos do monitoramento dos desembarques demonstrou que a pesca na região tem caráter artesanal de pequena escala, destacando a maior participação das canoas motorizadas (131 unidades do que barcos pesqueiros (45 unidades; capacidade média: 3.000kg na frota pesqueira. Os peixes migradores jaraqui (Semaprochilodus spp., dourada (Brachyplatystoma rousseauxii, sardinha (Triportheus spp., jatuarana/matrinxã (Brycon amazonicus e B. cephalus, curimatã (Prochilodus nigricans e filhote (Brachyplatystoma filamentosum se destacaram na composição das espécies desembarcadas. As informações técnicas geradas são importantes para subsidiar ações de ordenamento pesqueiro, bem como para avaliar futuras variações que possam ocorrer na atividade frente aos impactos dos empreendimentos hidrelétricos em construção na região.This study presents qualitative and quantitative information about commercial fishery in the basin of the Madeira River, tributary of the Amazon River, describing the fishing activity in the segment between Guajará-Mirim and Porto Velho, in Rondônia State. From January to December/2004, 219 fishermen and 935 trips were registered, corresponding to the capture of 460 t of fish. Data from fish landings demonstrate that fisheries in the region are small-scaled and point to a higher participation of small motorized canoes (130 units than of fishing boats (45 units; average capacity: 3000 kg in the fishing fleet. Migratory species like jaraqui (Semaprochilodus spp., dourada (Brachyplatystoma rousseauxii, sardinha (Triportheus spp., jatuarana/matrinxã (Brycon amazonicus e B. cephalus, curimatã (Prochilodus nigricans

  4. Presence of the walking catfish Clarias gariepinus (Burchell (Siluriformes, Clariidae in Minas Gerais state hydrographie basins, Brazil

    Carlos Bernardo Mascarenhas Alves


    Full Text Available The first official occurrence of the exotic species Clarias gariepinus (Burchell, 1822 in the Rio Paraopeba (São Francisco river basin, the Rio Grande (Paraná river basin, and the Rio Doce (Doce river basin, is reported, with comments on the possible ecological consequences and on the conservation of freshwater fish biodiversity due to non-native species introductions.

  5. Presence of the walking catfish Clarias gariepinus (Burchell) (Siluriformes, Clariidae) in Minas Gerais state hydrographie basins, Brazil

    Carlos Bernardo Mascarenhas Alves; Volney Vono; Fábio Vieira


    The first official occurrence of the exotic species Clarias gariepinus (Burchell, 1822) in the Rio Paraopeba (São Francisco river basin), the Rio Grande (Paraná river basin), and the Rio Doce (Doce river basin), is reported, with comments on the possible ecological consequences and on the conservation of freshwater fish biodiversity due to non-native species introductions.

  6. Epidemiología de la difilobotriasis en la cuenca del río Valdivia, Chile Epidemiologia de difílobotriase na bacia do rio Valdivia, Chile Epidemiology of diphyllobothriasis in the Valdivia River basin, Chile

    Patricio Torres


    por Diphyllobothrium latum nas áreas afetadas foi produzida pela ingestão de peixes defumados ou cozidos insuficientemente. A pesquisa realizada em l .450 peixes pertencentes a 4 espécies introduzidas e 11 autóctones capturadas na bacia do rio Valdivia mostrou a existência de plerocercoides de Diphyllobothrium latum e/ou D. dendriticum nas espécies introduzidas Salmo gairdneri e S. trutta além de outras autoctones. A prevalência ou intensidade média das infecções nos peixes bem como o grau de agregação das subpopulações variaram nos diferentes locais estudados. Na bacia do río Valdivia, alguns peixes atuaram como hospedeiros intermediários e outros como paratênicos das espécies de Diphyllobothrium encontradas. Como medidas de controle nos pontos de difilobotriase nas áreas estudadas sugere-se a melhoria das condições de saneamento básico, educação sanitária e tratamento das pessoas infectadas.In the Valdivia (Chile river basin 1,295 inhabitants of 6 riverside districts were examined between March and October 1987 and showed a 1.2% of prevalence by Diphyllobothrium in the districts of Riñihue and Las Huellas. Prevalence of 5.3% and 9.8% respectively were registered in dogs of the districts of Riñihue and Malihue. No cat or pig infection was observed in the different districts. The parasites recovered after the treatment were identified as Diphyllobothrium latum. Human infection by D. latum in the districts affected results from the consumption of smoked or insufficiently cooked fish. The investigation of 1,450 fish (4 exotic species and 11 autochthonous ones, caught in the Valdivia river basin in 1986 and 1987, showed the existence of plerocercoids of D. latum and/or Diphyllobothrium dendriticum in Salmo gairdneri and Salmo trutta among exotic fish and in some autochthonous species. Prevalence and mean intensity in the infection of fish as well as the degree of aggregation in the infrapopulations varied in the different districts. Some

  7. Reproductive biology of Leporinus taeniatus Lütken (Pisces, Anostomidae in Juramento Reservoir, São Francisco River basin, Minas Gerais, Brazil Biologia reprodutiva de Leporinus taeniatus Lütken (Pisces, Anostomidae do reservatório de Juramento, bacia do rio São Francisco, Minas Gerais, Brasil

    Ralph G. Thomé


    Full Text Available The reproductive biology of the piau-jejo Leporinus taeniatus Lütken, 1875, an endemic species from the São Francisco River basin, was studied by using macroscopical and histological techniques. A total of 121 males and 94 females were captured quarterly, between March 2002 and February 2003 in the Juramento Reservoir. Females were larger than males, indicating sexual dimorphism. Stages of gonadal maturation were defined from histological analyses and gonadosomatic index. Peaks of maturing/mature and spawned/spermiated fishes has occurred in period December-February. L. taeniatus presented total spawning and group-synchronic development of the oocytes. The gonadosomatic index accompanied gonad maturation in both sexes, and coelomic fat presented lower levels during maturing/mature stage, indicating fat consumption during the reproductive period. Stomach repletion index presented higher values during spawned and spermiated stages, indicating greater food ingestion after the reproductive period.A biologia reprodutiva do piau-jejo Leporinus taeniatus Lütken, 1875, espécie endêmica da bacia do rio São Francisco, foi estudada utilizando-se técnicas biométricas, macroscópicas e microscópicas. Capturaram-se no reservatório de Juramento, MG, em coletas trimestrais, 121 machos e 94 fêmeas, no período de março de 2002 a fevereiro de 2003. Observou-se que fêmeas são maiores do que os machos indicando dimorfismo sexual. Determinaram-se os estádios de maturação gonadal através de análise histológica e do índice gonado-somático. Os picos de maturação/maduro e de peixes desovados/espermiados ocorreram no trimestre dezembro/janeiro/fevereiro. L. taeniatus apresentou desova total e desenvolvimento grupo-sincrônico dos ovócitos. O índice gonadossomático acompanhou a maturação das gônadas e o índice de gordura celômica apresentou menores valores no estádio maturação/maduro, indicando consumo de reservas graxas no per

  8. Caracterização dos argilominerais usados em matéria-prima cerâmica, da formação Rio do Rasto, Bacia do Paraná, no município de Turvo, SC Characterization of clay minerals used in the ceramic industry, from Rio do Rasto formation, Paraná basin, exploitation in Turvo, SC, Brazil

    J. A. Costa


    Full Text Available No sudeste de Santa Catarina existem inúmeras minas de exploração de argilas destinadas à indústria cerâmica da região. Para o conhecimento desta matéria prima foi realizada a caracterização em detalhe de uma frente de lavra em atividade. A exploração é realizada em terrenos sedimentares da Formação Rio do Rasto (Permiano Superior na Bacia do Paraná que afloram como morros testemunho. Foram coletadas quatorze amostras representativas dos níveis desta mina composta de argilitos com intercalação de siltitos de pequena espessura. As amostras foram analisadas por difratometria de raios X pelo método do pó na rocha total e na fração In the southeastern part of Santa Catarina state, Brazil, many mines of clays used as raw material for the ceramic industry are found. A detail study of this material was developed in a mine in activity. The exploitation of clays is held in sedimentary rocks of Rio do Rasto Formation (Upper Permian in the Paraná Basin. The outcrops are in hills testimonies. Fourteen samples were collected and represent the levels of this mine which consisted of argillites with intercalation of slim siltite layer. These samples were analyzed by X-ray diffraction using the powder method and in the fraction < 4 µm. The chemical composition was determined by X-ray fluorescence spectrometer. Petrographic observations in thin section were also performed. Scanning electron microscope images was obtained in samples fragments by secondary electron method. Electron microprobe microanalysis was performed in one thin section. The results showed large vertical variation in the mineralogy and it has been identified three different levels. Up to 2.00 m there is a predominance of smectite. Between 5.50 m 2.00 m the smectite is the main clay mineral, but with significant amounts of illite/mica and above 5.50 m occurs large increase in K-feldspar and detrital mica. Studies in detail by X-ray diffraction (determination of the b

  9. Avaliação ecotoxicológica preliminar das águas das bacias hidrográficas dos rios Tarumã, São Raimundo e Educandos Preliminary evaluation of the toxicity in water of the Tarumã, São Raimundo and Educandos basins

    Déborah Oliveira Rodrigues


    Full Text Available As Bacias hidrográficas dos riosTarumã, São Raimundo e Educandos e seus afluentes estão sendo impactados, devido as influências antrópicas. Neste estudo foi realizada uma avaliação da toxicidade das águas destes ecossistemas, através de testes de toxicidade aguda com Daphnia similis e análises físico-químicas. Os resultados obtidos demostraram um maior efeito deletério sobre D. similis, nas amostras da microbacia Tarumã.The Tarumã, São Raimundo and Educandos basins, and their tributaries, are impacted by antropic influence. This study tried to evaluate the water toxicity of the hydrographic basins, through acute toxicity bioassay using Daphnia similis as test-organism and physical and chemical analysis. The results showed that, of the three basins, the water from Tarumã caused the most deleterious effect on D. similis.

  10. Diversity and distribution Patterns of the infralittoral green macroalgae from Potiguar basin, Rio Grande do Norte, Northeastern Brazil Diversidade e padrão de distribuição das macroalgas verdes da bacia Potiguar, Rio Grande do Norte, Nordeste do Brasil

    Adilma de Lourdes Montenegro Cocentino


    Full Text Available Diversity and distribution pattern of the infralittoral green macroalgae at Potiguar basin, Rio Grande do Norte, Northeastern Brazil were analyzed from material collected at depths varying from 2 to 100 m. Collections were carried out with two types of dredges during four campaigns: July 2002, May and November 2003 and May 2004 at 43 stations. Chlorophyta is represented by 54 species, five varieties and three forms. The most representative family is Caulerpaceae, and the most diverse genus is Caulerpa, with 11 species. The results showed that most taxa (89% are rare, and 10% are present at low frequencies. The most frequent species was Caulerpaprolifera (Forssk. J.V. Lamour. occurring at almost all coastal and inner shelf stations, recorded in all campaigns. Species distribution by depth range showed that higher species number occurred on the inner shelf from 10 to 20 m, and a wide vertical distribution pattern was registered for Anadyomenestellata (Wulfen in Jacq. C. Agardh,Chamaedoris peniculum (J. Ellis & Solander Kuntze, Codium isthmocladum Vickers, Microdictyon sp., Udoteaoccidentalis A. Gepp & E. Gepp and Ventricaria ventricosa (J. Agardh J.L. Olsen & J.A. West. Four species, Cladophoracoelothrix Kütz., C.ordinata (Børgensen C. Hoek, Caulerpellaambigua (Okamura Prud'homme & Lokhorst and Halimedasimulans M. Howe, were recorded for the first time in Rio Grande do Norte.Diversidade e padrão de distribuição das algas verdes do infralitoral da Bacia potiguar, RN, nordeste do Brasil foram analisados a partir de material coletado em profundidades que variaram de 2 a 100 m. As coletas foram feitas em dois tipos de dragas durante as quatro campanhas: julho de 2002, maio e novembro de 2003 e maio de 2004, em 43 estações. Chlorophyta está representada por 54 espécies, cinco variedades e três formas. A família mais representativa é Caulerpaceae e dentro da família, o gênero mais diverso é Caulerpa, com 11 espécies. Os resultados

  11. Inquérito do preservativo em ribeirinhos do Rio Acre: porte, acondicionamento, uso e risco para infecção pelas DSTs Inquerito del preservativo en la bacia fluvial del Rio Acre: porte, guarda, uso y el riesgo de infección por las EST Inquiry of the preservative in the basin of Rio Acre: carriage, package, use and the infection risk for DST

    Andréa Ramos da Silva


    prevención como grande/bueno.Descriptive-exploratory type study, carried with 168 inhabitants of the basin of Rio Acre - Brazil, which aimed to investigate preservative use and the risk for Sexually Transmited Diseases. For data collection it was used an application form with spontaneous participation and anonymate guaranty. As result, stands out the 64,3% masculine gender, 75,0% married/joined, 57,1% had incomplete first degree and 31,0% were illiterate. At that time 78,0% did not bring preservative when coming to the city, and 6,0% just came out seeking for sexual activity; 62,0% had already used the masculine preservative, with 67,2% of acceptance and 77,8% had kept it in the back pocket of the pants, with danger of damaging and infection risk and undesired pregnancy; 8,9% had had venereal disease, being 80,0% for the gonorrhea. Of these, 46,7% had negotiated respectively with pharmacist and doctor. Thus, 89,3% considered the prevention campaigns as great/good.

  12. Bottom water throughflows at the Rio de Janeiro and Rio Grande Fracture Zones

    Mercier, Herlé; Weatherly, Georges L.; Arhan, Michel


    Bottom water throughflows at the Rio de Janeiro Fracture Zone (22°S) and Rio Grande Fracture Zone (26°S) of the Mid-Atlantic Ridge are identified from hydrographic anomalies observed along 9°W in the Angola Basin. The throughflow water is supplied by a meridional band of cold and fresh water lying against the western flank of the Ridge.


    Claudinéia Raquel de Oliveira


    Full Text Available The presence of heavy metals in a sediment profile from the Rio das Pedras lagoon, located at the Moji-Guaçu river floodplain, São Paulo, was investigated. Samples were stratified at each 1 cm, sieved in 63 m m and digested in a strong acid solution (HNO3 + HF + HClO4 in PTFE bomb. The extracts were analyzed by emission plasma spectrometry (ICP-AES for Al, Cu, Mn, Cr and Ni contents. For Hg, the direct pyrolysis of samples and atomic fluorescence spectrometry detector AFS were employed. By using Al as a normalizer agent, an enrichment of metals concentration, with exception for Mn was observed. Average concentration for Cu (0.12 mg g-1 and Mn (1.12 mg g-1 were considered high in comparison to those concentrations in an unpolluted environment. Probably, these data are related to the agricultural activity (sugarcane plantation around the lagoon, or to the Moji-Guaçu river transport in the flood season. Hg, Cr and Niconcentrations were similar the those verified in unpolluted areas. The chronology inventigation, determined by the 210Pb technique, indicated that the 25 cm long sediment profile shows a 135 years of deposition history of the suspended material in this lagoon. = A presença de metais pesados em perfil de sedimento coletado na Lagoa Rio das Pedras, localizada na planície de inundação do rio Moji-Guaçu, São Paulo, foi investigada. Amostras estratificadas a cada 1 cm foram peneiradas a 63 m m e digeridas através de ataque ácido (HNO3 + HF + HClO4 em bombas de PTFE. Os extratos obtidos foram analisados quanto aos teores de Al, Cu, Mn, Cr e Ni por espectrometria de emissão de plasma (ICP-AES. Para Hg, empregou-se a pirólise direta da amostra e detecção por AFS. Utilizando-se Al como elemento normalizador, observou-se enriquecimento nos teores de metais pesados para anos recentes, exceto para Mn. As concentrações médias de Cu (0,12 mg g-1 e Mn (1,12 mg g-1 para amostras de sedimentos foram elevadas, em comparação

  14. Blastocistosis y otras infecciones por protozoos intetinales en comunidades humanas ribereñas de la cuenca del rio Valdivia, Chile Blastocystosis and other intestinal protozoan infections in human riverside communities from - Valdivia River Basin, Chile

    Patricio Torres


    Full Text Available Entre marzo y octubre de 1987 se examinaron muestras coprológicas de 970 personas (20, 9% de la población pertenecientes a 209 grupos familiares de las comunidades ribereñas de la cuenca del rio Valdivia, Chile; con el propósito de determinar las prevalencias de infección por Blastocystis hominis y otros protozoos intestinales para establecer relaciones con la edad y sexo de los hospedadores, saneamiento ambiental y porcentaje de individuos infectados por grupo familiar. Un 72, 5% de las personas presentó una o más especies de protozoos intestinales. La mayor prevalencia se registró para B. hominis (61, 8%, que se incrementó con la edad del hospedador al igual que en las infecciones por Endolimax nana y Entamoeba coli. No se demostró asociación entre el sexo del hospedador y la prevalencia de infección por B. hominis y otras especies de protozoos. La prevalencia de B. hominis fue mayor en individuos que habitaban viviendas cuya disposition de excrementos era no sanitaria. Más del 60% de los integrantes de los grupos familiares presentaron infección por B. hominis en el 53, 1% de las familias encuestadas en contraposición al 2,4%-21,8% observado en infecciones por otros protozoos. El examen de 45 muestras de excrementos de cerdos, reveló infección por Blastocystis en el 22,2% de estos animales.Between March and October 1987, the prevalence of infection by Blastocystis hominis and other intestinal protozoan, their relationship with the age and sex of the hosts, and the percentage of in fected persons in family groups were determined in riverside communities of Valdivia River Basin, Chile. One or more intestinal protozoan species were determined in 72.5% of the examined persons. The prevalence was greater for B. hominis (61.8%. The prevalences of B. hominis, Endolimax nana and Entamoeba coli were greater in relation to the age of the host. The sex of the host and prevalence of infections by B. hominis and other species of

  15. Population structure, feeding and reproductive aspects of Serrapinnus heterodon (Characidae, Cheirodontinae in a Mogi Guaçu reservoir (SP, upper Paraná River basin Estrutura populacional, alimentação e reprodução do lambari-prata Serrapinnus heterodon (Characidae, Cheirodontinae em um reservatório do rio Mogi Guaçu (SP, bacia do alto rio Paraná

    Cristina da Silva Gonçalves


    Full Text Available AIM: In this report, we describe the population structure, feeding and reproductive aspects of the cheirodontine Serrapinnus heterodon collected in a reservoir of a small hydro power of Mogi Guaçu River (SP; METHODS: Specimens were caught bimonthly between August 2005 and July 2006 near the marginal aquatic vegetation with four traps; RESULTS: A total of 38 specimens of S. heterodon were collected (mainly during the rainy season, comprising 16 males (32-47 mm SL, 18 females (32-49 mm SL and four individuals with indeterminate sex (33-45 mm SL. There were significant differences in length distribution between sexes, with males being smaller than females (_x males = 42 ± 4.3 mm and _x females = 45 ± 4.8 mm. Sex ratio was 1:1. Eight food items were identified in the diet, with a predominance of autochthonous items. The diet classified as omnivorous. Insects (fragments were the most consumed item, followed by microcrustaceans (Cladocera and Ostracoda, algae (mainly diatoms and immature insects (Diptera and Odonata. Comparing with other cheirodontines, S. heterodon has higher fecundity (mean = 1,231 ± 440 oocytes and smaller oocytes (61 to 793 µm. Moreover, the spawning was classified as total and occurred during the rainy season which is the breeding season for the majority of fish species from the upper Paraná River basin; CONCLUSIONS: The results seem to reflect the type of environment in which S. heterodon inhabit, because the lentic environment afforded by the dam provides relatively stable conditions to maintaining this species, which uses aquatic vegetation as shelter from predators and as feeding and breeding sites.OBJETIVO: Neste trabalho, a estrutura populacional e os aspectos alimentares e reprodutivos do queirodontíneo Serrapinnus heterodon são descritos, a partir de exemplares coletados no reservatório de uma pequena central hidrelétrica do rio Mogi Guaçu (SP; MÉTODOS: Os exemplares foram capturados bimensalmente entre agosto

  16. Comunidade arbórea de uma floresta estacional decídua sobre afloramento calcário na Bacia do rio Paraná Arboreal community of a seasonal deciduous forest on limestone outcrop in São Domingos - Goiás, Parana river Basin, Brazil

    Luciana Álvares da Silva


    Full Text Available A bacia do rio Paraná (GO e TO, com 5.940.382 ha, tem alta diversidade de fitofisionomias, com sua flora pouco conhecida. As atividades de extração de madeira e implantação de pastagem contribuíram decisivamente para a remoção da vegetação. Este estudo foi conduzido em uma floresta estacional decídua sobre afloramento calcário (aproximadamente 13º41'16"S e 46º44'20"W e 462 m de altitude - fazenda Canadá (São Domingos-GO. Foram demarcadas cinco linhas paralelas, a intervalos de 100 m, onde foram distribuídas aleatoriamente 25 parcelas de 20 x 20 m (total de 1 ha. Em cada parcela foram amostradas todas as árvores com diâmetro do caule a 1,3 m de altura do solo (DAP > 5 cm, nos quais foi medido o DAP, estimada a altura máxima e identificada a espécie. Foram amostrados 924 indivíduos de 48 espécies, 38 gêneros e 24 famílias e obtidos o índice de Shannon-Wienner de 2,99 nats/ind. e a equabilidade de 0,77. As espécies que apresentaram maior valor de importância (VI foram Myracrodruon urundeuva (36,09, Pseudobombax tomentosum (34,75, Dilodendron bipinnatum (26,61, Combretum duarteanum (22,19, Jacaranda brasiliana (21,57, Commiphora leptophloeos (19,18, Astronium fraxinifolium (13,84, Tabebuia impetiginosa (13,79, Pseudobombax longiflorum (11,64 e Machaerium scleroxylon (10,00, que juntas somaram 69,9% do VI total. A diversidade foi próxima à encontrada em outros trabalhos em floresta estacional decídua sobre solo e afloramento na região.The Parana River basin - an area of 5,940,382 ha located in Brazil- has a highly diverse phytophysiognomy and scarce flora information. Wood extraction and pasture activities have decisively contributed to the removal of vegetation in this area. This study was carried out in a seasonal deciduous forest on limestone outcrop (approximately 13º41'16" S and 46º44'20" W on Canada Farm (São Domingos-GO. Twenty -five plots of 20 m x 20m (1 ha were randomly allocated on parallel lines 100 m

  17. Fases larvais do mexilhão dourado Limnoperna fortunei (Dunker (Mollusca, Bivalvia, Mytilidae na Bacia do Guaíba, Rio Grande do Sul, Brasil Larval stages of the golden mussel Limnoperna fortunei (Dunker (Bivalvia, Mytilidae in Guaíba Basin, Rio Grande do Sul State, Brazil

    Cíntia P. dos Santos


    Full Text Available Desde o final de 1998, um pequeno bivalve invasor, o "mexilhão dourado", Limnoperna fortunei (Dunker, 1857, oriundo do sudeste asiático, está presente no sul do Brasil. Foi provavelmente transportado, não intencionalmente, através de água de lastro para a Bacia do Guaíba, Rio Grande do Sul, Brasil. Em nosso meio, este molusco vem causando problemas de "macrofouling" com grandes prejuízos econômicos e danos à fauna e flora. As coletas foram qualitativas e quantitativas quinzenais no período de um ano, no lago Guaíba, Praia do Veludo (30°12'35"S, 51°11'68"W, ao sul do município de Porto Alegre. Utilizou-se rede de plâncton com abertura de malha equivalente a 36 mm, filtrando-se a quantidade de 30 litros de água. Descrevem-se brevemente as diferentes fases larvais com parâmetros do comprimento. Primeiramente reconhece-se um estágio ciliado, desenvolvendo-se em trocófora (comprimento de 80 µm a 125 µm com quatro fases distintas, e valvadas com a larva "D" (120 µm a 150 µm, o veliger de charneira reta (150 µm a 190 µm, o veliger umbonado (190 µm a 220 µm e o pediveliger (220 µm a 250 µm. Quando pós-larvas ou plantígradas (comprimento em torno de 300 µm, começam a secretar o fio de bisso, permitindo a fixação ao substrato. Constatou-se a presença de larvas durante todos os meses amostrados, com picos nos meses de outubro a dezembro.Since the end of 1998 a small invasive bivalve, the golden mussel Limnoperna fortunei (Dunker, 1857, originating from Southeast Asia, is present in Southern Brazil. It was probably brought not intentionally in ballast water to the Guaíba Basin in Rio Grande do Sul State. In this environment, the golden mussel is causing macrofouling very rapidly with grate financial loss and damages to the native fauna and flora. Quali-quantitative samplings twice a month were performed during one year in the Guaíba lake, at Veludo Beach (30°12'35"S, 51°11'68"W southward of the municipality of Porto

  18. Análise de aspectos socioeconômicos e tecnológicos da agropecuária na Bacia Hidrográfica do Rio Mogi Guaçu Social-economic analyse and technologic aspects of the agriculture at the Mogi Guaçu River Hydrographic Basin

    Marianna S. Zibordi


    Full Text Available Atualmente, com a ocorrência de problemas ambientais e a necessidade de conservação e preservação, a gestão dos territórios de Bacias Hidrográficas apresenta extrema importância. O objetivo do trabalho é levantar e analisar dados socioeconômicos e tecnológicos da Bacia Hidrográfica do Rio Mogi Guaçu - SP, bem como fornecer subsídios para a gestão agropecuária, agrupando os municípios com características semelhantes para os dados levantados, o que poderá orientar ações conjuntas na gestão da Bacia Hidrográfica. Foram levantados dados primários e secundários, sendo utilizados os métodos da análise fatorial em componentes principais e da classificação automática hierárquica, bem como um Sistema de Informações Geográficas para representar os dados por meio de banco de dados georreferenciado. As principais características que contribuíram para o agrupamento dos municípios foram: área agrícola, presença efetiva de cultura semiperene nas unidades de produção agropecuária (upas, pecuária, concentração de upas com áreas de até 50 ha, número de tratores e valor total da produção agropecuária do município. Grupos relativamente homogêneos de municípios foram constituídos e, nesse sentido, reuniões de municípios com características e problemáticas similares podem ser efetuadas, buscando alternativas participativas e conjuntas para o desenvolvimento regional.Currently, owing to the occurrence of environmental problems, along with the need of environmental preservation, both the territory management of Hydrographic Basin and the conservation of natural resources have proven to have remarkable importance. Thus, the mean goal of the research is to raise and scrutinize social-economic and technologic data from the Mogi Guaçu River Hydrographic Basin (São Paulo, Brazil. The aim is to group municipalities with similar characteristics regarding the collected data, which may direct joint actions in the

  19. Time-variations of equivalent water heights'from Grace Mission and in-situ river stages in the Amazon basin Variações temporais do equivalente à altura d'água obtidas da Missão Grace e da altura d'água in-situ nos rios da bacia Amazônica

    Flavio Guilherme Vaz de Almeida


    Full Text Available Gravity Recovery and Climate Experiment (GRACE mission is dedicated to measuring temporal variations of the Earth's gravity field. In this study, the Stokes coefficients made available by Groupe de Recherche en Géodésie Spatiale (GRGS at a 10-day interval were converted into equivalent water height (EWH for a ~4-year period in the Amazon basin (from July-2002 to May-2006. The seasonal amplitudes of EWH signal are the largest on the surface of Earth and reach ~ 1250mm at that basin's center. Error budget represents ~130 mm of EWH, including formal errors on Stokes coefficient, leakage errors (12 ~ 21 mm and spectrum truncation (10 ~ 15 mm. Comparison between in situ river level time series measured at 233 ground-based hydrometric stations (HS in the Amazon basin and vertically-integrated EWH derived from GRACE is carried out in this paper. Although EWH and HS measure different water bodies, in most of the cases a high correlation (up to ~80% is detected between the HS series and EWH series at the same site. This correlation allows adjusting linear relationships between in situ and GRACE-based series for the major tributaries of the Amazon river. The regression coefficients decrease from up to down stream along the rivers reaching the theoretical value 1 at the Amazon's mouth in the Atlantic Ocean. The variation of the regression coefficients versus the distance from estuary is analysed for the largest rivers in the basin. In a second step, a classification of the proportionality between in situ and GRACE time-series is proposed.A missão espacial Gravity Recovery and Climate Experiment (GRACE é dedicada às medidas das variações temporais no campo gravitacional da Terra. Neste estudo, os coeficientes de Stokes disponibilizados pelo Groupe de Recherche en Géodésie Spatiale (GRGS com intervalos de 10 dias foram convertidos no equivalente à altura d'água (EWH para um período de 4 anos na bacia Amazônica (de julho de 2002 a maio de 2006

  20. Geochemical behavior of radionuclides and heavy metals in soils from Corumbatai River basin (SP), Brazil; Comportamento geoquimico de radionuclideos e metais pesados em solos da bacia do Rio Corumbatai (SP)

    Conceicao, Fabiano Tomazini da


    The purpose of this research was to study the geochemical behavior of radionuclides and heavy metals in soils of agricultural use at Corumbatai River basin (SP). The natural concentration and variability in sedimentary rocks at Corumbatai river basin follow the trend Ca > Mg > K > Na, with the concentration of heavy metals and radionuclides. The distribution of exposure rate in soils shows the occurrence of higher values towards south of the Corumbatai river basin, region where are applied phosphate fertilizers, amendments and 'vinhaca' in sugar cane crops. Heavy metals and radionuclides incorporated in phosphate fertilizers and amendments are annually added during the fertilization process in the sugar cane crops, but if they are utilized in accordance with the recommended rate, they do not rise the concentration levels in soils up to hazards levels. Thus, they are lower transferred from soils to sugar cane at Corumbatai river basin, not offering hazard to the ecosystem and animal or human health. (author)

  1. Avaliação socioambiental da bacia hidrográfica do rio Pequeno, São José dos Pinhais (PR / Socio-environmental evaluation of the Pequeno River hydrographic basin, São José dos Pinhais (PR

    Ariodari Francisco dos Santos


    Full Text Available ResumoExiste atualmente uma preocupação com o processo crescente de ocupação humana desordenada na bacia hidrográfica do rio Pequeno e a sua consequente degradação ambiental. Isso vem sendo demonstrado através de alertas e denúncias feitas por diversos segmentos da sociedade, as quais estão, frequentemente, sendo veiculadas pela mídia local e regional. Essa bacia merece atenção especial na medida em que o rio Pequeno desempenha um papel importante na disponibilização de água superficial para São José dos Pinhais na Região Metropolitana de Curitiba (PR. Diante desse cenário, faz-se mister investigar as atuais condições ambientais da bacia hidrográfica do rio Pequeno, visando avaliar qualitativamente as implicações ambientais decorrentes das diversas práticas agrícolas desenvolvidas pela agricultura familiar, pelo uso e ocupação do solo na bacia em tela. Na presente pesquisa, buscou-se evidenciar a problemática à luz de uma abordagem teórica que contemple o inter-relacionamento das variáveis ambientais, procurando caracterizar os relacionamentos entre os elementos naturais do meio e a dinâmica de uso e ocupação do solo atual. Constatou-se que esta é uma área ambientalmente frágil e, diante dos diversos usos e ocupação dos solos identificados, essa bacia vem passando por um processo de degradação ambiental acentuada, o que promove a deteorização da qualidade de suas águas, tornando assim, iminente o risco da sua perda como abastecimento público, pois a atividade agrícola na bacia, com o manejo intensivo dos solos, o uso de agroquímicos e a urbanização, geram impactos ambientais, tanto em termos de processos erosivos quanto em riscos de contaminação dos recursos hídricos.AbstractThere is, nowadays, a concern regarding the environmental consequences of the growing process of unordered human settlements at Pequeno River hydrographical basin, in São José dos Pinhais (Parana State, South Brazil

  2. Coscinodiscophyceae, Fragilariophyceae e Bacillariophyceae (Achnanthales dos rios Ivaí, São João e dos Patos, bacia hidrográfica do rio Ivaí, município de Prudentópolis, PR, Brasil Coscinodiscophyceae, Fragilariophyceae and Bacillariophyceae (Achnanthales of the Ivaí, São João and Patos rivers in the Ivaí basin, Prudentópolis, Paraná State, Brazil

    Fernanda Ferrari


    Full Text Available Realizou-se o levantamento florístico das Coscinodiscophyceae, Fragilariophyceae e Bacillariophyceae (Achnanthales dos rios Ivaí, São João e dos Patos, pertencentes à bacia hidrográfica do rio Ivaí, município de Prudentópolis, Paraná. Quarenta e uma amostras foram coletadas em março, junho e julho/2002 e janeiro/2003, e analisadas. As coletas fitoplanctônicas foram feitas através de arrasto superficial com rede de plâncton (25 µm e as perifíticas através da coleta de porções submersas de macrófitas aquáticas, rochas, cascalho, sedimento ou substrato arenoso. Foram identificados, nove táxons pertencentes à classe Coscinodiscophyceae, oito à classe Fragilariophyceae e quinze à ordem Achnanthales (Bacillariophyceae. Thalassiosira weissflogii (Grunow Fryxell & Hasle, Achnanthidium sp., Planothidium biporomum (Hohn & Hellerman Lange-Bertalot e Cocconeis placentula var. pseudolineata Geitler consistiram em novas citações para o estado do Paraná.A floristic study of Coscinodiscophyceae, Fragilariophyceae and Bacillariophyceae (Achnanthales in the Ivaí, São João and Patos rivers from the upper Ivaí river basin, located at Prudentópolis, Paraná State, Brazil is presented. Forty-one samples were collected in March, June and July/2002 and January/2003, and analysed. Phytoplankton samples were collected with a plankton net (25 µm mesh; periphyton was collected by removing the attached material from submerged portions of aquatic macrophytes, rocks, sediment or the sandy substratum. Nine species of the class Coscinodiscophyceae, eight of the class Fragilariophyceae and fourteen of the order Achnanthales were identified. Thalassiosira weissflogii (Grunow Fryxell & Hasle, Achnanthidium sp., Planothidium biporomum (Hohn & Hellerman Lange-Bertalot and Cocconeis placentula var. pseudolineata Geitler were new diatom records for Paraná State.


    Jean Berná Paim


    Full Text Available Adopt a basin as a hydrological unit to understand the physical processes related to the water and sediment production is important because its characteristics (area, shape and topography can determine its use in a sustainable manner. This study is aim in the test of the applicability of hydrologic model SWAT (Soil and Water Assessment Tool in the Tijucas River Basin to quantify the water and sediment production along it sub-basins. Together, geoprocessing techniques were applied with the creation of a database of geographical information to describe the region. On this database is included the daily precipitation an temperature data of the gauges distributed on the watershed, soil data, a land use map and the digital elevation model (DEM to create the Hydrologic Response Units (HRU’s. A time series with flow values and sediment concentration measured are very important to calibrate and validate the model output parameters. After the calibration of the initial results, the Flow Gauge number 102 presented a Nash and Sutcliffe Coefficient - COE = 0.6 indicating a good adjust of the model. The results were used to create a sediment production map for Tijucas River Basin, when the 10 years average ranged between 0.5 ton/ha and 9.0 ton/ha in some sub-basins.

  4. Avaliação dos estoques pesqueiros de quatro espécies de grandes bagres (Siluriformes, Pimelodidae na bacia do rio Cuiabá, Pantanal norte, Brasil, utilizando alguns Pontos de Referência Biológicos Fisheries stock assessment of four large catfish (Siluriformes, Pimelodidae in the Cuiaba River basin, north Pantanal, Brazil, using some Biological Reference Points

    Lúcia A. F. Mateus


    Full Text Available Os parâmetros de crescimento e mortalidade estimados a partir da estrutura em comprimento foram utilizados para avaliar o estado de explotação dos estoques de quatro espécies de grandes bagres da bacia do rio Cuiabá, Pantanal norte. As espécies estudadas foram o barbado, o cachara, o jaú e o pintado. As avaliações foram realizadas por meio do modelo de rendimento por recruta, considerando os Pontos de Referência Biológicos Fmax, F0,1, F = M e F BDR. As análises indicam que os estoques do pintado e do jaú estão bem conservados. Os estoques do cachara e, menos fortemente, o do barbado estão em iminente ameaça de sobrepesca na bacia do rio Cuiabá.The growth and mortality parameters estimated from length structure were used to evaluate the state of explotation of the stocks of four large catfish species from Cuiabá River basin, north Pantanal. The species studied were the Flatwhiskered catfish, the Jaú, the Barred sorubim, and the Spotted sorubim. The assessment were conducted with the yield per recruit model, and the Biological Reference Points Fmax, F0.1, F = M, and F BDR. The analysis indicates that the stocks of the Spotted sorubim, and of the Jaú are not overexploited. However, the stocks of the Barred sorubim, and, in lower degree, of the Flatwhiskered catfish of the Cuiabá River basin are in imminent threat of overfishing.

  5. Hydroelectric modelling of the Paraiba do Sul and Jequitinhonha rivers sub-basins by using the VALORAGUA computer program; Modelagem hidreletrica das sub bacias dos rios Paraiba do Sul e Jequitinhonha utilizando o programa VALORAGUA

    Ferreira, Vinicius Verna Magalhaes; Aronne, Ivan Dionysio [Centro de Desenvolvimento da Tecnologia Nuclear (CDTN), Belo Horizonte, MG (Brazil)]. E-mails:;; Martinez, Carlos Barreira; Versiani, Bruno Rabelo [Minas Gerais Univ., Belo Horizonte, MG (Brazil). Escola de Engenharia. Dept. de Engenharia Hidraulica e Recursos Hidricos]. E-mail:;


    This work presents a modelling of 50 hydroelectric power plants in the East Atlantica hydro graphic basin, operating, under construction or as basic projects. The simulations are performed by using the VALORAGUA computer code, developed by the EDP - Eletricidade de Portugal. The studies concentrate mostly on the sub basins of the Jequitinhonha and Paraiba do Sul rivers. The study includes the thermal power plants existent on the same geographical region. Some obtained results such as capacity factors and energy generation values are analysed. Some considerations are made on questions referring to the Brazilian energetic problems.

  6. Definition of the ecological status of Estanco River Basin (Antas de Ulla, Lugo, Spain) with Water Framework Directive; Definicion del estado ecologico de la cuenca del rio Estanco (Antas de Ulla, Lugo) segun la Directiva Marco del Agua

    Muno Fafian, D.; Cuesta Garcia, T. S.; Cancela Barrio, J. J.; Marin Lopez, A.; Carballo, R.; Marin Lopez, A.; Neira Seijo, X. X.


    The Water Framework Directiva (WFD) extends the scope of protection to all water uses. The WDF defines the ecological status of water bodies by characterizing each water body type and establishing reference conditions for the quality elements. This paper identifies indicators for defining the ecological status of Estanco river Basin (Antas de Ulla, Lugo) by using the methodology proposed in the WFD. In additions, this study highlights the obstacles for a correct application of the WFD in the study river basin. this study presents conclusions about the usefulness of the WFD in the development of specific programmes for improving the ecological status of rivers. (Author) 16 refs.

  7. Early development of Auchenipterus osteomystax (Osteichthyes, Auchenipteridae from the Paraná river basin, Brazil Caracterização do desenvolvimento inicial de Auchenipterus osteomystax (Osteichthyes, Auchenipteridae da bacia do rio Paraná, Brasil

    Maristela Cavicchioli Makrakis


    Full Text Available The aim of the present study was to characterize the early development of Auchenipterus osteomystax (Ribeiro, 1918 (Osteichthyes, Auchenipteridae. Specimens were taken from plankton samples in the Upper Paraná river, Ivaí river, Upper Ivinhema river and Itaipu Reservoir. Seventy-four larvae and seven juveniles (with standard length ranging from 5.25 mm to 39.0 mm were analyzed. Specimens were identified and separated according to their development and morphometric and meristic analyses were performed. The early development of A. osteomystax follows the pattern of other Siluriformes. However, individuals presented more pigmentation on the head and on fore part of the body. Number of myomeres ranged from 44 to 50O objetivo deste trabalho é caracterizar o desenvolvimento inicial de Auchenipterus osteomystax (Ribeiro, 1918 (Osteichthyes, Auchenipteridae. O material analisado é proveniente de amostras coletadas no plâncton no alto rio Paraná, rio Ivaí, alto rio Ivinhema e reservatório de Itaipu. Foram analisadas 74 larvas e 7 juvenis, entre 5,25 mm e 39 mm de comprimento padrão. Os espécimes foram identificados e separados em diferentes estágios, e foram obtidas as variáveis morfométricas e merísticas. As larvas de A. osteomystax apresentam o desenvolvimento inicial semelhante ao de outros Siluriformes, no entanto são caracterizadas principalmente por apresentar um aglomerado de pigmentos na cabeça e na região anterior do corpo e número de miômeros variando de 44 a 50

  8. Efeitos das mudanças do uso da terra na biogeoquímica dos corpos d'água da bacia do rio Ji-Paraná, Rondônia Effects of land use changes in the biogeochemistry of fluvial systems of the Ji-Paraná river basin, Rondônia

    Alex Vladimir Krusche


    Full Text Available Este trabalho discute os efeitos das mudanças do uso do solo na biogequímica dos rios da bacia de drenagem do rio Ji-Paraná (Rondônia. Nesta região, a distribuição espacial do desmatamento e das propriedades do solo resultam em sinais diferentes, possibilitando a divisão dos sistemas fluviais em três grupos: rios com águas pobres em íons e baixo impacto; rios com conteúdo iônico intermediário e impacto médio e rios com elevados conteúdo iônico e impacto antropogênico. As características biogeoquímicas dos rios têm relação significativa com a área de pasto, melhor parâmetro para prever a condutividade elétrica (r² = 0,87 e as concentrações de sódio (r² = 0,75, cloreto (r² = 0,69, potássio (r² = 0,63, fosfato (r² = 0.78, nitrogênio inorgânico (r² = 0.52, carbono inorgânico (r² = 0.81 e carbono orgânico (rain ² = 0.51 dissolvidos. Cálcio e magnésio tiveram sua variância explicada pelas características do solo e pastagem. Nossos resultados indicam que as mudanças observadas na micro-escala constituem "sinais biogeoquímicos" gerados pelo processamento do material nas margens dos rios. A medida em que os rios evoluem para ordens superiores, os sinais persistentes nos canais fluviais estão mais associdados às características da bacia de drenagem (solos e uso da terra. Apesar dos efeitos das mudanças observadas no uso do solo não serem ainda detectáveis na macro-escala (bacia amazônica, a disrupção da estrutura e funcionamento dos ecossistemas é detectável nas micro e meso escalas, com alterações significativas na ciclagem de nutrientes nos ecossistemas fluviais.In this article we present the results of the effects of land use change on the river biogeochemistry of the Ji-Paraná basin (Rondônia. In this region, the spatial distribution of deforestation and soil properties result in different biogeochemical signals, allowing the division of the fluvial systems into three groups: rivers with

  9. Análise Morfométrica da Rede de Drenagem da Bacia do Rio do Machado-MG / Morphometric Analisys of Machado Drainage Basin – Minas Gerais State

    Marli Carina Siqueira Ribeiro


    Full Text Available Este artigo visa analisar a rede de drenagem através da utilização das técnicas de indice Relação Declividade e Extensão do Curso de agua (RDE e análise do perfil longitudinal dos vales, numa região chave do Planalto Sul de Minas, a fim de contribuir com estudos sobre evolução da paisagem da região sudeste do Brasil. A pesquisa foi realizada na Bacia Hidrográfica do Rio do Machado (MG, afluente do Alto Rio Grande, e regiões adjacentes, localizadas no Planalto Sul de Minas. O Rio do Machado apresenta uma particularidade em seu curso, com uma mudança brusca de direção tomada por sua drenagem na área próxima ao seu médio curso. Com a aplicação das técnicas pretende-se compreender melhor a dinâmica do relevo na área, identificando áreas com indício de ação neotectônica e seu padrão de distribuição na bacia.


    Cristiane Compagnoni


    Full Text Available RESUMOA avaliação da bacia hidrográfica do rio Penso mapeou as áreas susceptíveis à risco de escorregamento e enchentes, relacionando estes problemas ambientais com o uso, cobertura do solo e as questões sociais. A partir da análise destas informações foram elaboradas propostas de medidas de controle de drenagem na nascente, as quais contribuem para o desenvolvimento sustentável. Como resultado deste trabalho, detectou-se que na referida bacia 50% da área de fundo de vale encontra-se com mata ciliar, identificou-se 10 áreas com inclinação superior a 30%.Palavras-chave: Cobertura do solo, Mata ciliar, Ocupação urbanaABSTRACTThe evaluation of the hydrographic basin of the Penso River mapping the risk of landslide and flood areas, relating these environmental problems with the use, the occupation of the soil and the social question. From the analysis of these information, proposals of draining control measures were elaborated, in the source which contributes for the sustainable development. As a result, it was detected that in the respective basin, 50% of the deep of valley area has reparian ecosystems, and 10 areas with inclination of more than 30% were identified. Key words: Use of the soil, Reparian ecosystems, Urban occupation

  11. Segundo registro de Sterrastrolepis brasiliensis Volkmer-Ribeiro & De Rosa-Barbosa (Demospongiae, Potamolepidae com descrição do habitat e de assembléia, Bacia do Rio Paraná, Brasil Second register of Sterrastrolepis brasiliensis Volkmer-Ribeiro & De Rosa-Barbosa (Demospongiae, Potamolepidae with description of the habitat and of assembly, Paraná Basin, Brazil

    Cecília Volkmer-Ribeiro


    Full Text Available A descoberta recente, no fundo rochoso do Rio Piquiri, Bacia do Paraná, Brasil, de Sterrastrolepis brasiliensis Volkmer-Ribeiro & De Rosa-Barbosa, 1978, uma espécie de esponja continental ameaçada, possibilitou o registro fotográfico de espécimes vivos, o aperfeiçoamento das ilustrações ao MEV e da descrição de algumas características, a descrição do habitat e o registro de uma assembléia de esponjas composta por S. brasiliensis, Oncosclera navicella (Carter, 1881 e Oncosclera tonolli (Bonetto & Ezcurra de Drago, 1968. Oncosclera tonolli tem seu primeiro registro para águas brasileiras e para a Bacia do Paraná. Gêmulas de O. navicella são tambem ilustradas ao MEV.The recent discovery of Sterrastrolepis brasiliensis Volkmer-Ribeiro & De Rosa-Barbosa, 1978, a brazilian endangered freshwater sponge, at the rocky bottom of River Piquiri, Paraná Basin, Brazil, enhanced the photographing of living specimens, the improving of SEM illustration and description for some characteristics, the description of the habitat and the register of an sponge assembly composed by S. brasiliensis, Oncosclera navicella (Carter, l881 and Oncosclera tonolli (Bonetto & Ezcurra de Drago, 1968. Oncosclera tonolli has its first register for Brazilian waters and for the Parana Basin. Gemmules of O. navicella are also SEM illustrated.

  12. Gradientes de diversidade nas comunidades de peixes da bacia do rio Iguatemi, Mato Grosso do Sul, Brasil Diversity gradients in fish communities of Iguatemi river basin, Mato Grosso do Sul, Brazil

    Yzel Rondon Súarez


    Full Text Available Com o objetivo de verificar a importância da variação longitudinal, sazonal e a influência das características físicas e químicas da água sobre a diversidade de espécies de peixes realizamos amostragens trimestrais, entre Novembro/1999 e Agosto/2000, em três pontos amostrais no rio Jogui e oito pontos amostrais no rio Iguatemi-MS. A variação longitudinal foi mais importante que a variação sazonal na determinação da riqueza e número de indivíduos no rio Jogui, no entanto, a equitabilidade não apresentou diferença significativa sazonal ou longitudinal. No rio Jogui 78,3% da variação na riqueza de espécies, 81,6% no número de indivíduos e 41,1% na equitabilidade foram explicadas pelas características físicas e químicas da água. No rio Iguatemi nós não detectamos diferenças estatisticamente significativas longitudinais ou sazonais nos descritores analisados das comunidades nem influência significativa dos fatores ambientais.In order to verify the importance of longitudinal and seasonal variations and the effect of physical and chemical water characteristics to fish species diversity we accomplished three-month samplings, between November/1999 and August/2000, in three selected points in the Jogui River and eight points in the Iguatemi River-MS. The longitudinal variation was more important than seasonal variation in determining richness and number of individuals in the Jogui River, however, evenness did not present statistically significant differences either longitudinal or seasonal. In the Jogui River 78.3% of species richness, 81.6% of number of individuals and 41.1% of evenness variation was explained by the water chemical and physical characteristics. In the Iguatemi River we did not detect longitudinal or seasonal statistically significant differences in the analyzed community descriptors nor significant influence of environmental factors.

  13. Associações de espécies de peixes em ambientes lóticos da bacia do rio Iguatemi, Estado do Mato Grosso do Sul - DOI: 10.4025/actascibiolsci.v25i2.2024 Fish species associations in lotic environments in Iguatemi river basin, State of Mato Grosso do Sul - DOI: 10.4025/actascibiolsci.v25i2.2024

    Miguel Petrere Junior


    Full Text Available Com o objetivo de descrever os padrões das associações entre espécies de peixes e sua distribuição nos ambientes lóticos ao nível da bacia, foram realizadas amostragens em 27 locais na bacia do rio Iguatemi-MS, distribuídas em quatro ambientes (rio Iguatemi, rio Jogui, rio Puitã e riachos. Os dados de presença/ausência das espécies que ocorreram em dois ou mais locais foram submetidos a métodos multivariados com o objetivo de descrever os principais padrões de associação entre espécies. A distribuição das espécies foi considerada determinística nessas comunidades (C-score = 17,33; P = 0,000, existindo diferença significativa entre os ambientes estudados (ANOSIM r = 0,082; P = 0,012, sendo constatada diferença entre rio Iguatemi e riachos (P = 0,001 e riachos e rio Jogui (P = 0,014. Constatamos uma clara segregação entre as espécies de riachos de cabeceiras e de trechos mais caudalosos dos rios ou mesmo de riachos com maior vazãoThe aim of this paper is to describe the patterns of associations between fish species and their distribution in lotic habitats at basin level. Samples were accomplished in 27 localities of Iguatemi river basin, distributed in four environments (Iguatemi river, Jogui river, Puitã river and streams. The presence/absence data of those species which occurred in 2 or more sites were submitted at multivariate methods with the aim to describe the major species associations. The species distribution was considered determinative in these communities (C-score = 17,33; P = 0,000, with significant difference among the studied environments (ANOSIM r = 0,082; P = 0,012, with verified difference between Iguatemi river and streams (P = 0,001 and also streams and Jogui river (P = 0,014. We verified a strong segregation among species from headstreams and more discharge river stretches or even larger streams

  14. Spar genetic analysis of two invasive species of Cichla (Tucunaré (Perciformes: Cichlidae in the Paraná river basin = Análise genética via spar, de duas espécies de Cichla (Tucunaré (Perciformes: Cichlidae introduzidas na Bacia do rio Paraná

    Giovanna Caputo Almeida-Ferreira


    Full Text Available The introduction of exotic species in lake ecosystems has been greatly highlighted in the literature worldwide. Since introduction may threaten diversity of native fish, the issue turns up to be of paramount importance. Ecological effects may be predation, competition, parasitism or genetic, that is, changes in the genetic pool of populations owing to the occurrence of hybrids. Although the Tucunaré fish (Cichla is native to the Amazon region, it can be foundin other hydrographic basins in which it has been introduced. RAPD molecular marker research showed that there are two species (Cichla kelberi and C. piquiti belonging to the genus Cichla in the rivers of the Paraná basin. Different morphotypes in the region may also be due to hybridization. Current research used SPAR molecular markers to confirm the presence of hybrids and the rupture of isolation mechanisms. Seventy-two specimens collected in several sites of the river Paraná and Amazon basins were analyzed. Since exclusive SPAR molecular markers were obtained for Cichla kelberi and C. piquiti populations, the introduction of the two species in the region has been confirmed. Identification of the markers in specimens of theParaná river basin confirmed hybridization between these exotic species.A introdução de espécies exóticas nos ecossistemas lacustres tem sido muito destacada na literatura mundial, pois ameaça a diversidade de peixes nativos, tornando-se uma questão de extrema importância. Os efeitos observados podem ser ecológicos, como predação, competição e parasitismo ou genéticos, como a ocorrência de híbridos. Apesar do peixe tucunaré (Cichla ser nativo da região amazônica, ele pode ser encontrado em outras bacias hidrográficas nas quais foram introduzidos. Estudos utilizando marcadores moleculares RAPD revelaram que existem duas espécies (Cichla kelberi e C. piquiti do gênero Cichla na bacia do alto rio Paraná e morfotipos diferentes que podem ser devido

  15. Avaliação multicriterial no mapeamento de risco de incêndios florestais, em ambiente sig, na bacia do Rio Corumbataí, SP Multi-criteria evaluation of a GIS environment in a forest fire hazard mapping for the Corumbataí River basin, SP, Brazil

    Hilton Luis Ferraz da Silveira


    Full Text Available Um dos agentes mais empregados na supressão de áreas florestais no Estado de São Paulo é o fogo, por meio de queimadas que, quando fora de controle, podem converter-se em incêndios responsáveis pela destruição de extensos ecossistemas. Na Bacia do Rio Corumbataí, SP, os incêndios são um dos causadores de fragmentação e degradação da cobertura florestal. Nesse contexto, este trabalho objetivou a realização do mapeamento de risco de incêndios florestais na Bacia do Rio Corumbataí, utilizando-se a avaliação multicriterial (Método da Média Ponderada Ordenada em um Sistema de Informações Geográficas. Os fatores importantes do estudo foram: declividade do terreno, face de exposição ao sol, pluviosidade, proximidade da malha viária, proximidade dos centros urbanos, proximidade da rede hidrográfica, vizinhança dos fragmentos e face de exposição aos ventos. A combinação dos mapas de fatores resultou no mapa de risco regional da bacia. Para a confecção do mapa de risco em nível de fragmento, determinou-se o risco associado a cada fragmento, a partir da análise de uma faixa de 30 m em seu entorno. O risco foi reclassificado em três classes: baixo, médio e alto. Com base no mapa final, verificou-se que: aproximadamente 20% dos fragmentos de mata nativa pertencem à classe de risco alto, 55% à classe de risco médio e 25% à classe de risco baixo. Nas condições atuais de uso e cobertura do solo, bem como de manejo das áreas agrícolas e pastagens, os remanescentes florestais da Bacia do Rio Corumbataí estão sob séria ameaça de degradação por incêndios florestais.Fire is one of the agents most used in the suppression of forest areas in the State of São Paulo, Brazil, and, when out of control, it can be responsible for the destruction of extensive ecosystems. In the case of the Corumbataí river basin, SP, fire is one of the main causes of forest fragmentation and degradation. The purpose of this study was

  16. Elementos traço na água e em vísceras de peixes da Bacia Hidrográfica Butuí-Icamaquã, Rio Grande do Sul, Brasil Trace elements in water and viscera of fish from Butuí-Icamaquã Basin, Rio Grande do Sul, Brazil

    Luiz Carlos Santos Porto; Eduardo Miranda Ethur


    Metais pesados, também denominados elementos traço, podem ser essenciais ao metabolismo de organismos vivos, e, ao mesmo tempo, dependendo de suas concentrações, altamente tóxicos. Com o objetivo de investigar a toxicidade da água da Bacia dos Rios Butuí-Icamaquã, na fronteira oeste do Rio Grande do Sul, foram analisados, através de espectrofotômetro de absorção atômica, os teores de alumínio, cádmio, chumbo, cobre, cromo, manganês, níquel e zinco em vísceras abdominais de peixes, coletados, ...

  17. Incorporação de indicadores de sustentabilidade na priorização de áreas para restauração florestal na bacia do rio Corumbataí, SP Incorporating sustainability indicators on site selection for forest restoration in the Corumbataí river basin

    Silvio Frosini de Barros Ferraz


    Full Text Available Na bacia do rio Corumbataí, a vegetação natural ocupa menos de 3% de sua área total, e a ausência dessa vegetação florestal tem levado ao aumento dos processos erosivos e ao desequilíbrio do regime hídrico de seus rios, causando diversos problemas no abastecimento de água de várias cidades, como Piracicaba e Rio Claro. Desse modo, existe a necessidade de um reflorestamento criterioso em áreas dessa bacia. No entanto, devido à limitação de recursos, é necessário que sejam realizados estudos de seleção de áreas prioritárias para que, com os recursos disponíveis, o ganho ambiental das áreas restauradas seja máximo. O objetivo deste trabalho foi desenvolver um método de priorização de áreas para restauração florestal baseado no uso de indicadores de sustentabilidade em microbacias. Cinco indicadores foram utilizados: porcentagem de mata nativa na APP; descontinuidade da vegetação nativa na bacia; diversidade da paisagem; variação média do uso da terra; e suscetibilidade à erosão. A seleção das microbacias para restauração das áreas de APP foi realizada por meio da ponderação linear dos indicadores e ordenamento das microbacias. Simulação inicial foi realizada para a seleção de 1.000 ha para restauração, e os resultados indicaram que os indicadores representam diferentes aspectos de sustentabilidade das microbacias. O método foi considerado útil na seleção de microbacias em condições extremas, diferenciando aquelas que necessitam de ações de conservação daquelas que necessitam de ações de restauração.In the Corumbataí river basin, State of São Paulo, forest remnants occupy less than 3% of the original total area, and the absence of this natural vegetation has been increasing erosion and disturbing hydrological regime of its streams, causing many problems on water supply in urban areas like Piracicaba and Rio Claro. This situation shows the need of a well planned reforestation in areas

  18. I.Quality of water in the Turia river basin. General quality index; I. Estudios hidraulicos y de calidad de la cuenca del rio Turia en el entorno de Teruel

    Lanaja, F.J.; Puebla, M.D.; Sarasa, M.D. [Escuela Universitaria de Ingenieria Tecnica Industrial de Zaragoza (Spain); Sanchez, M.D. [Instituto de Estudios Turolenses. Teruel (Spain)


    During four years (91-95) same campaigns of water sample taking are carried out in twenty points of the Turia River Basin in Teruel and physical, chemical parameters and bacteriological compounds, contamination indicators are determined in them. In order to interpret the analytical results a use is made of general quality index and the different contamination of the Turia river is evaluated. (Author) 6 refs.

  19. Aspectos Ecológicos dos Parasitos de Iheringichthys labrosus (Lütken, 1874 (Siluriformes: Pimelodidae em Reservatórios da Bacia do Rio Paraná e na Planície de Inundação do Alto Rio Paraná, Brasil - DOI: 10.4025/actascibiolsci.v27i4.1265 Ecological aspects of the parasites of Iheringichthys labrosus (Lütken, 1874 (Siluriformes: Pimelodidae in reservoirs of Paraná basin and upper Paraná floodplain, Brazil - DOI: 10.4025/actascibiolsci.v27i4.1265

    Gilberto Cezar Pavanelli


    Full Text Available Foram examinados 62 espécimes de Iheringichthys labrosus capturados nos reservatórios de Rosana, Taquaruçú, Salto Grande e Canoas I, localizados na bacia do Rio Paraná. Cinqüenta peixes (80,65% estavam parasitados por pelo menos uma espécie. Foram encontrados os seguintes parasitos: uma espécie de Dactylogyridae; uma espécie de Apocreadiidae; uma espécie de Proteocephalidea; Procamallanus (Spirocamallanus pimelodus Pinto, Fábio, Noronha e Rolas, 1974; Quadrigyrus sp.; e Ergasilus sp. Na planície de inundação do Alto rio Paraná, foram capturados 35 espécimes deste mesmo hospedeiro, sendo que 13 estavam parasitados por pelo menos uma espécie (37,14%. As espécies de parasitos encontradas foram: Herpetodiplostomum gymnoti larva; uma espécie de Proteocephalidea; Procamallanus (Spirocamallanus pimelodus; Contracaecum sp. Tipo 1 larva de Moravec, Kohn e Fernandes, 1993; e Quadrigyrus sp. Em ambos os locais de estudo, a prevalência e a abundância de parasitismo não estavam correlacionadas com o comprimento padrão dos hospedeiros. Houve diferenças significativas entre prevalência e abundância das espécies de parasitos de acordo com o sexo dos peixes somente na planície de inundação do Alto rio Paraná. Além disso, observou-se em ambas as localidades que a abundância de parasitismo não exerce influência sobre o fator de condição dos hospedeiros. A comparação das infracomunidades de parasitos presentes nos peixes de ambas as localidades apresentou uma similaridade de 54,54%Sixty-two specimens of Iheringichthys labrosus, captured in Rosana, Taquaruçú, Salto Grande and Canoas I reservoirs, located in the Paraná River basin, were necropsied. Fifty specimens were parasited by at least one species (80.65%. Six parasite species were recorded: one species of Dactylogyridae; one species of Apocreadiidae; one species of Proteocephalidea; Procamallanus (Spirocamallanus pimelodus Pinto, Fábio, Noronha e Rolas, 1974

  20. Modeling streamflow from snowmelt in the upper Rio Grande

    Annual snowpack in the high elevation snowsheds of the Upper Rio Grande (URG) Basin is a vital source of surface water for irrigated agriculture in New Mexico. Maximum streamflow from the annual snowpack usually occurs in early May for the southernmost snowsheds (e.g., Ojo Caliente) and at the end o...

  1. Composição florística e estrutura da comunidade arbórea em uma floresta estacional decidual em afloramento calcário (Fazenda São José, São Domingos, GO, bacia do rio Paranã Floristic composition and structure of the tree community in a deciduous forest on a limestone outcrop in São Domingos, Goiás, Paranã river basin, Brazil

    Luciana Álvares da Silva


    Full Text Available A bacia do rio Paranã (Goiás e Tocantins com 5.940.382ha, tem alta diversidade de fitofisionomias, incluindo a floresta estacional decidual sobre afloramento calcário, que ainda não foi estudada nesta região. Este trabalho objetivou o levantamento quantitativo da vegetação arbórea de uma floresta estacional decidual sobre afloramento calcário (13°49'34''S e 46º 41'55''W; 478m de altitude na fazenda São José, São Domingos, GO. Foram demarcadas cinco linhas a intervalos de 100m, onde foram aleatoriamente alocadas 25 parcelas permanentes de 20 × 20m (1,0 ha. Em cada parcela foram amostrados todos os indivíduos com diâmetro à altura do peito (DAP igual ou maior que 5cm, onde foram medidos o DAP e a altura, e identificadas as espécies. Foram amostrados 588 indivíduos (536 vivos e 52 mortos ainda em pé, pertencentes a 36 espécies, 31 gêneros e 21 famílias, com índice de Shannon 2,99 e Equabilidade 0,83. As principais espécies em valor de importância (VI, foram: Tabebuia impetiginosa (43,81, Aspidosperma pyrifolium (35,64, Luetzelburgia sp. (21,77, Commiphora leptophloeos (18,79, Myracrodruon urundeuva (15,79, Pseudobombax tomentosum (13,42, Combretum duarteanum (13,04, Luehea divaricata (12,24, Cabralea canjerana (11,99, Ficus pertusa (11,82, Jacaranda brasiliana (11,68 e Aspidosperma sp. (10,57 que juntas somaram 73,5% do VI total, enquanto as 24 espécies restantes somaram 26,5%. Esta floresta é similar, em termos de diversidade, a outras áreas de afloramentos na região.The Paranã river basin (States of Goiás and Tocantins, Brazil, with 5,940,382 ha, has many different plant physiognomies, including the deciduous forest on limestone outcrops which has not yet been studied in this region. In this paper we present the structure of the tree community of a deciduous forest on a limestone outcrop (13º49'34'' S; 46º 41'55'' W in São Domingos municipality, Goiás State, Brazil. Twenty-five plots of 20m × 20m (400m² were

  2. O Comitê da Bacia Hidrográfica do Rio São Francisco e a Gestão das Águas: O Conflito Exposto a Partir da Transposição do Rio São Francisco | The São Francisco River Basin Committee and Water Management Conflict Arising from the Transposition of The River

    Ana Paula Novais Pires


    Full Text Available Normal 0 21 false false false PT-BR X-NONE X-NONE Introduction: The São Francisco River Basin Committee (CBHSF was set up by presidential decree in 2001 with the aim of achieving decentralized and participatory management of its water. The São Francisco River flows overland for 2700 km from its source in the Serra da Canastra (MG to its mouth between Sergipe (SE and Alagoas (AL. The river passes through the states of Bahia (BA, Pernambuco (PE, Goiás (GO and the Federal District (DF. Central to the discussion in this research on the transposition of the São Francisco River is question of conflict concerning water management in the São Francisco River Basin Committee, making a nonsense of its power to function, contrary to the project, and the Federal Government which initiated the work and approved the budget. Hence, this study aims to analyze water management in the São Francisco river basin from the initiation of the CBHSF in order to understand how approval of the project and implementation of the work ran against the statutory representation of the committee. Methodology and Development: Having a qualitative approach, the study will be divided between theoretical research based on authors who study the topic of water and its transformation into a water resource and the major landowners of the north-east semi-arid zone in the context of transposition; the dynamics and politics of the river basin; as well as the role of the river basin committees in the process of decentralizing Brazilian water management, specifically concerning the São Francisco River and its state and interstate committees. Documentary research will take into account National Water Resources Law 9.433/1997; state water policies; documentary archives of the river basin committees (state and interstate, as well as the agencies participating in the integration project, such as the National Water Agency (ANA, the Integration Ministry (MI, and the Environment Ministry (MMA

  3. Space-Temporal evolution of climatic variables in the Basin Segura River in the period; Evolucion espacio-temporal de vairables climaticas en la Cuenca del Rio Segurida en el perido 1976-2007

    Gomariz Castillo, F.; Alonso Sarria, F.


    This work developed a methodology to analyse the spatio-temporal distribution of the must important climatic variable controlling environmental and socioeconomic processes in river Segura basin. A global multiple regression model is applied to interpolate climatic variables. Using as independent variables distances to sea, height aspect, easting and nothing. In cases where it is not possible to use a global model, local interpolation procedure will be used (krigging, IDW or splines). The methodology has six stages: 1) selection of stations, 2) data filtering and gep filling after an homogeneity test, 3) estimation of parameters for a regression model, 4) interpolation, 5) validation and 6) evolution analysis. (Author) 8 refs.

  4. Emissões naturais e antrópicas de metais e nutrientes para a bacia inferior do rio de contas, Bahia Natural and anthropogenic emissions of metals and nutrients to the lower contas river basin, Bahia state, Brazil

    Francisco C. F. de Paula


    Full Text Available Emission factors of anthropogenic activities and natural processes were used to estimate nutrients and metals loads to the Contas River lower basin, Southern Bahia, Brazil. Among natural sources, emission from soil leaching is larger for N, Cu and Pb. Atmospheric deposition is the major natural source of P, Zn, Cd and Hg. Among anthropogenic sources, agriculture is the major source of N, Cu and P. Urban sources are the major contributors to the other elements. Present anthropogenic land uses are already responsible for 78 and 99% of total N and P loads and about 50% of total Cu and Hg.

  5. Análise temporal da permeabilidade da superfície urbana da sub-bacia do córrego centenário em Lavras, MG Temporal analysis of permeability urban surfaces locaty of the Centenário sub-basin creek in Lavras, MG

    Marcelo Barbosa Furtini


    Full Text Available Nos últimos anos, séries de estudos têm sido realizadas por estudiosos de diferentes áreas para estabelecer os efeitos da urbanização na hidrologia de sub-bacias. O processo de urbanização freqüentemente produz alterações na drenagem da água pluvial. Um SIG com dados cadastrais planaltimétricos e fotografias aéreas permitiram estudar a ocupação em 3 diferentes períodos (1999, 1986 e 1971 na sub-bacia do Centenário, na cidade de Lavras, MG. Objetivou-se com este estudo realizar a análise temporal da permeabilidade da superfície na sub-bacia do Centenário comparando os 3 períodos. A permeabilidade da superfície urbana foi obtida pela análise da ocupação dos quarteirões por área construída ou pavimentada. Os resultados permitiram verificar que a permeabilidade da superfície decaiu de 1971 para 1999. Nestes anos a área urbana cresceu reduzindo a permeabilidade do solo da sub-bacia. Conclui-se que, sendo óbvio que a urbanização causou impactos na sub-bacia, as metodologias utilizadas para essas análises foram muito eficientes para determinar os impactos de superfícies impermeáveis.Over the past years, a series of studies have been undertaken by scientists of different areas, to assess the effects of urbanization on the hidrology of subbasins. The urbanization process has frequently been done alterations on the drainage of pluvial water. A GIS data base containing the cadastral planiltimetric charts and aerial photographies allowed to study the land occupation in three different periods (1999, 1986 and 1971 of the Centenário Subbasin in Lavras city, MG. So, the subject of this study was to realize a temporal analysis of the surface permeability of the Centenário subbasin comparing the three periods. The urban surface permeability was avaibled by the analysis of the city's squares occupation per builted or paved area. The results permitted verify that the surface permeability downed from 1971 to 1999 years. In

  6. Qualidade da água subterrânea para irrigação na bacia hidrográfica do Rio Piauí, em Sergipe Groundwater quality for irrigation purposes in Piauí River Basin in the State of Sergipe, Brazil

    Julio R. A. de Amorim


    Full Text Available O uso de água subterrânea para fins agrícolas tem-se intensificado no Estado de Sergipe, sobretudo na região de maior escassez de águas superficiais; no entanto, a irrigação ainda está restrita a pequenas áreas, como hortas familiares, justificado, em parte, pela ausência de estudos de caracterização hídrica, incluindo disponibilidade e qualidade das águas subterrâneas, que permitam o conhecimento da distribuição espacial das fontes de água viáveis para uso. Avaliaram-se os riscos potenciais relativos à salinização e sodificação de solos, à toxicidade de íons específicos às culturas e à obstrução em sistemas de irrigação localizada, a partir de dados secundários de 278 poços localizados na bacia hidrográfica do Rio Piauí, considerando-se os critérios de restrição ao uso da água para irrigação estabelecidos pela FAO. Mapas de risco foram gerados por procedimentos de krigagem ordinária, para as variáveis indicadoras de qualidade da água, que possibilitaram a visualização do comportamento espacial das águas na bacia. Verificou-se que as águas subterrâneas apresentam boas condições para uso na irrigação, principalmente na porção centro-litorânea da bacia, visto que houve tendência de aumento na concentração de sais das águas no sentido centro-cabeceiras.Groundwater use for agricultural purposes has been intensified in the State of Sergipe, mainly in the regions with more serious water shortage from surface sources. However, irrigation is still restricted to small areas like home gardens. In part, this problem is due to lack of studies on characterization of water resources, including availability and quality of groundwaters, detecting the spatial distribution of viable sources of groundwater for different uses. The potential hazards related to soil salinity and sodicity, toxicity of specific ions for crops, and clogging of components of microirrigation systems were evaluated

  7. Spatial variation of the length and humid weight of Limnoperna fortunei (Dunker, 1857 in Jacuí River Delta and Guaíba Lake Basin (Rio Grande do Sul State, Brazil

    Paulo Eduardo Aydos Bergonci


    Full Text Available Natural clusters of golden mussels (Limnoperna fortunei were sampled in January 2005, in four stations of the Jacuí River Delta (Garças Creek (DAG and Jacuí Channel (DCJ and Guaiba Lake (Veludo beach (GPV and Pombas Pier (GPP, in Rio Grande do Sul State, Brazil. Measurements of the length and humid weight of 180 collected specimens were tested based on Kruskal-Wallis (α = 0.05 followed by the SNK test of significance for the different populations. This test did not show any significant differences between stations GPV and GPP for the length (p = 0.247 or humid weight (p = 0.912. However, differences were found between DAG and DCJ for these parameters, which also differed from those found for other stations (p < 0.001. Environmental characteristics (water current, food support, etc. and the effects of predation possibly have some influence on the differences among populations found in this study.

  8. Hydrogeological and hydrochemical characterization of unconfined aquifer located in the alteration mantle of the Serra Geral Formation, in the Taquari-Antas river basin, northeast of Rio Grande do Sul State

    Gisele Cemin


    Full Text Available This paper presents the hydrogeological and hydrochemical characterization of the unconfined aquifer located in the alteration mantle in the volcanic rocks from Serra Geral Formation, in the northeast region of Rio Grande do Sul State. This aquifer is conditioned by the soil, topography, lithology and climate, being characterized by a saturated layer thinner than 1,7 m, static levels between 0 and 1 m and low flow (<0,5 m3/h. These waters are of calcium or magnesium bicarbonate type, and low alkalinity and electrical conductivity, low calcium, magnesium, sodium, potassium and chloride concentrations, and high iron and manganese concentrations. Additionally, these waters have high concentration of nitrates (mean above 10 mg/L and the presence of total coliforms. These characteristics evidence a quick circulation between the recharging and discharge zones in the aquifer.

  9. Temporal-space of charges in land use in the Segura River Basin; Analisis espacio-temporal de los cambios de usos del suelo en la Cuenca del Rio Segura

    Alonso Sarria, F.; Gomariz Castillo, F.; Canovas Garcia, F.; Moreno Brotons, J.


    Land use change is a dynamic process that affects heavily to different environmental processes. in this work, a GIS application is designed to analyse land use changes from Landsat imagery since 1976 to 2007, a period with important socioeconomic and land use changes in River Segura basin. This work describes the methodology used to obtain a yearly series of land cover maps of the Demarcation hidrografica del Segura (River Segura basin in South East Spain). In order to analyze this great amount of information for a large (more than 18,000 km{sup 2}) and heterogeneous area, a unified methodology has been developed. It has been used oa supervised classification improved by a previous not supervised classification using both spectral (4 or 6 Landsat solar spectrum bands depending on the sensor available, MSS or TM, ETM) and two textural variables. The las ones were obtained estimating the semi variogram function from the albedo and NDVI layers. having used two images from different seasons, the total number of variables included in the classification is 12 or 16 depending on the year. (Author) 7 refs.

  10. Influence of urbanisation on water quality in the basin of the upper Uruguay River in western Santa Catarina, Brazil Influência da urbanização sobre a qualidade da água na bacia do alto Rio Uruguai no oeste de Santa Catarina, Brasil

    Raquel Zeni Ternus


    Full Text Available AIM: The main objective of the study was to evaluate the limnological characteristics of rivers flowing through urban and rural areas in the upper Uruguay River basin in western Santa Catarina (SC, Brazil. METHODS: Sampling sites in the tributaries were selected along the longitudinal gradient and the different use of the soil in adjacent areas. Samples were collected bimonthly from March 2005 to August 2006. The following were analysed: depth, pH, electrical conductivity, dissolved oxygen concentration (DO, water temperature, chemical oxygen demand (COD, total alkalinity, ammonia, nitrite, nitrate and phosphorus were analysed. RESULTS: In most of the rivers analysed, we found a continuum from the spring to the river mouth that was characterised by a gradual increase in electrical conductivity, COD, phosphorus, alkalinity, nitrite and nitrate. However, an alteration from this pattern was found in rivers passing through urban areas. This deviation was due to high organic matter input poured into the rivers from these areas. CONCLUSIONS: Degraded riparian forest was observed along most of the bodies of water, which facilitates the entry of pollutants. Although the studied area suffers from intense farming activity (agriculture and livestock and has the highest concentration of swine livestock in the country, the rivers that were most altered from their natural state were those that were influenced by sewage and industrial effluents from urban development.OBJETIVO: O objetivo desta pesquisa foi avaliar as características limnológicas de rios que atravessam áreas rurais e urbanas na bacia do alto Rio Uruguai no oeste de Santa Catarina, Brasil. MÉTODOS: Foram selecionados pontos nos afluentes, obedecendo ao gradiente longitudinal e diferente uso do solo das áreas adjacentes. As amostragens foram bimestrais de março de 2005 a agosto de 2006. Foram analisadas as variáveis profundidade, pH, condutividade elétrica, oxigênio dissolvido (OD

  11. Determination of several elements in sediment samples from Nizao River basin, Dominican Republic by instrumental neutron activation analysis; Determinacao de diversos elementos em amostras de sedimento da bacia do Rio Nizao da Republica Dominicana por ativacao neutronica instrumental

    Kastner, Geraldo Frederico; Vilhena Schayer Sabino, Claudia de [Centro de Desenvolvimento da Tecnologia Nuclear (CDTN), Belo Horizonte, MG (Brazil)


    The Neutron Activation Laboratory at CDTN (Nuclear Technology Development Institute, Brazilian) (CNEN) has been acquiring through the years experience to determine several elements answering to analytical requests, including regional, national and international projects. Through neutron activation instrumental, gamma spectrometry and fission delayed neutron technique were analysed 50 samples of sediment from basin of Nizao River, Dominican Republic: Al, Fe, Mn, Na, Cr, Co, La, Sc, U and V with the objective to determine the concentration in both different parts: argil and sand. It was necessary to improve the irradiation conditions, delay time, counting, geometry and others proceedings due parameters like neutron flux, half life time of the radionuclide, gamma energies, all interfering in the procedures. The irradiations were carried about at IPR R1 TRIGA MARK I reactor. (author). 5 refs., 3 figs., 5 tabs.

  12. Rede neural artificial aplicada à previsão de vazão da Bacia Hidrográfica do Rio Piancó Artificial neural network applied to the forecast of streamflow in the Piancó River Basin

    Wanderson dos S. Sousa


    Full Text Available A previsão de vazão em um sistema hídrico não é apenas uma das técnicas utilizadas para minimizar o impacto das incertezas do clima sobre o gerenciamento dos recursos hídricos mas, também, um dos principais desafios relacionados ao conhecimento integrado da climatologia e da hidrologia de uma bacia hidrográfica. O objetivo deste trabalho foi modelar a relação não-linear entre chuva e vazão na bacia hidrográfica do rio Piancó, no semiárido paraibano, através da técnica de Redes Neurais Artificiais (RNA. Aqui se avaliou a capacidade da RNA modelar o processo chuva-vazão em base mensal e se considerou, durante o seu treinamento, a influência da arquitetura da rede e da inicialização dos pesos. No final do treinamento foi escolhida a melhor arquitetura para modelar vazões médias mensais na bacia estudada, com base no desempenho do modelo. A arquitetura de RNA que produziu melhor resultado foi a RC315L, com valores para o coeficiente de determinação, de eficiência e erro padrão da estimativa de 92,0, 77,0% e 8,29, respectivamente.Streamflow forecasting in a water system is one of the techniques used to reduce the impact of the uncertainties of the climate on administration of the water resources. That technique can be considered as one of the principal challenges related to the integrated knowledge of the climatology and of the hydrology of the river basin. The aim of this work was to model the non-linear relationship between rainfall and streamflow in the Piancó River Basin, in the Paraíba semiarid, using the technique of Artificial Neural Networks (ANN. Here the ability of ANN was evaluated to model the rainfall-runoff process on a monthly basis. During training of the ANN, the network architecture and weights initialization influence were considered. At the end of the training the best architecture was chosen, to model the streamflow monthly mean in the studied basin, based upon the performance of the model. The ANN

  13. Ecologia da ictiofauna de um córrego de cabeceira da bacia do alto rio Paraná, Brasil Ecology of the ichthyofauna of a headwater stream of the upper Paraná River basin, Brazil

    Elis Mara Lemes


    Full Text Available Ecological studies were conducted in the ichthyofauna of Cedro, a small headwater stream located in a degraded area of State of São Paulo, Brazil, situated in the upper Paraná River basin. These are the results of two non-consecutive years observations and collections in two biotopes of that stream: a pool and a rapid. The ecological characteristics studied change in space and time. The present richness of species is high (21 species, nine of which are constant, six accessory and six accidental. The diversity is low (0.69 to 2.38, and the numeric predominance, from one to three species, occurred in both biotopes. The most frequent species are Poecilia reticulata (Peters, 1859 (28.1%, Corydoras cf. aeneus (Gill, 1858 (20.3% and Hypostomus cf. ancistroides (Ihering, 1911 (19.8%. The density ranges from 0.7 to 19.8 specimens/m³. The similarity index indicates high similarity between the ichthyofauna (45.0% to 95.0% inside the same or contiguous biotopes. The evenness (0.46 to 1.0 is comparable to those found in similar studies carried out in other streams.

  14. Composição específica e abundância da ictiofauna do rio dos Padres, bacia do rio Iguaçu, Brasil = Specific composition and abundance of the ichthyofauna from Padres’ river, Iguaçu river basin, Brazil

    Alessandro Gasparetto Bifi


    Full Text Available A composição e estrutura das comunidades de peixes podem ser consideradas como indicadores ecológicos e ambientais, constituindo-se desta forma como ferramenta para o manejo de bacias hidrográficas. O presente estudo objetivou levantar informaçõessobre a composição específica e abundância da ictiofauna do rio dos Padres. Foram realizadas amostragens trimestrais pelo método da pesca elétrica em dois pontos de coleta, um próximo à nascente e outro nas proximidades da foz. As coletas resultaram na captura de 7.026 exemplares pertencentes a 12 espécies distribuídas em sete famílias. A nascente apresentou uma alta densidade em número de indivíduos e menores valores de diversidade, eqüitabilidade e riqueza de espécies em relação à foz. O levantamento da composição específica e abundância da ictiofauna de um rio é de grande importância, por fornecer subsídio a futuros manejos e monitoramentos, tanto da comunidade aquática quanto do ambiente.The composition and structure of fish community can be considered ecological and environmental indicators. The present study aimed to survey information about the specific composition and abundance of theichthyofauna from Padres’ River. Quarterly samplings were accomplished by the method of the electrofishing in two sample sites, one close to the headwater and another in the proximities of the mouth. The collections resulted in the capture of 7026 specimens belonging to 12 species, which, in turn, fit in seven different families. The headwater presented a high density in number of individuals and smaller values of diversity, evenness and richness of species in relation to the mouth. The raising of the specific composition and abundance of the ichthyofauna of a river is of great importance for supplying subsidy to future managements and accompaniment, as much of the aquatic community as of the environment.

  15. Inorganic carbon shortage may limit the development of submersed macrophytes in habitats of the Paraná River basin Baixas concentrações de carbono inorgânico podem limitar o desenvolvimento de macrófitas submersas em habitats do alto rio Paraná

    Aline de Freitas


    Full Text Available AIM: In this investigation we carried out an experiment to assess whether the growth of Egeria najas and E. densa (two rooted submersed Hydrocharitacea, native to South America are limited by inorganic carbon or not; METHODS: We measured the early plant growth in 3 L microcosms with alkalinities of 100 µM.L-1 and 500 µM.L-1. These alkalinites represent extremes which are typical of most waters in the Upper Paraná River basin and they represent low and high inorganic carbon (mainly bicarbonate availabilities, respectively; RESULTS: The elongation of E. densa, and the relative growth rates and root development of both species were significantly higher when they grew in the high alkalinity treatment; CONCLUSIONS: Our results strongly suggest that in several habitats and during certain periods of the year, inorganic carbon shortage may limit the growth of both species. In this sense, phosphorus and nitrogen may assume a secondary role as controlling factors of these plants, because they assimilate these nutrients from sediment, where they are usually found in high concentrations. Thus, controlling eutrofication as a strategy to reduce their biomass may not be successful.OBJETIVOS: Nesse trabalho nós realizamos um experimento para avaliar se o crescimento de Egeria najas e E. densa (duas espécies de macrófitas aquáticas submersas da família Hydrocharitaceae, nativas da América do Sul é limitado por carbono inorgânico; MÉTODOS: Nós medimos os estágios iniciais de crescimento de fragmentos em microcosmos de 3 L com alcalinidade de 100 µM.L-1 e 500 µM.L-1. Esses valores de alcalinidade foram escolhidos por representarem extremos típicos da maioria dos ecossistemas aquáticos da bacia do Alto rio Paraná e representaram baixa e alta disponibilidade de carbono (principalmente bicarbonato, respectivamente; RESULTADOS: O alongamento de E. densa e o crescimento relativo e desenvolvimento de raízes de ambas as espécies foram

  16. Spectral gamma-ray signature of fluvial deposits: a case study from the Late Permian Rio do Rasto Formation, Parana Basin, Brazil; Assinatura gamaespectrometrica de depositos fluviais: estudo de caso na Formacao do Rio do Rasto, Permiano Superior da Bacia do Parana

    Sowek, Guilherme Arruda, E-mail: [Universidade Federal do Parana (UFPR), Curitiba, PR (Brazil). Programa de Pos-graduacao em Geologia; Ferreira, Francisco Jose Fonseca; Vesely, Fernando Farias, E-mail:, E-mail: [Universidade Federal do Parana (UFPR), Curitiba, PR (Brazil). Dept. de Geologia. Setor de Ciencias da Terra; Berton, Fabio, E-mail: [Universidade Federal do Parana (UFPR), Curitiba, PR (Brazil)


    Fluvial channel-fill deposits form highly heterogeneous hydrocarbon reservoirs. The study of outcrop analogs can help in the characterization of these heterogeneities, which are usually not detected by subsurface geophysical methods. The aim of this research is to compare outcrop log signatures with grain size trends and depositional elements of the fluvial deposits of the Late Permian Rio do Rasto Formation. A series of vertical gamma-ray logs were assembled in two outcrops in order to: 1) characterize log-facies in a succession composed of alternated flood plain, channel fill and eolian strata; 2) define within-channel spectral gamma-ray variability of a mixed-load composite point bar deposit and its relationship with grain size trends and lithofacies; 3) correlate log signatures observed in the outcrop sections with deep exploratory wells drilled several tens of kilometers from the study area. The results of this study show that gamma-ray logs have good correlation with grain size trends and that different depositional elements have distinct signatures. On the other hand, point bar deposits exhibit strong lateral changes in log signature due variations in grain size and mud content within lateral accretion strata. Although frequent, the classic bell-shaped log motif was not always detected, which means that the amount of fluvial channel-fill deposits recognized in subsurface can be underestimated. Similar log signatures were detected in the boreholes, at least in the closest ones, helping in paleoenvironmental interpretation in the subsurface. (author)

  17. Mythical imaginary in rural agricultural practices on properties of La Vieja river basin, Colombia Imaginarios míticos en las prácticas agropecuarias rurales en fincas de la cuenca del rio La Vieja, Colombia

    Sebastián Ramírez Arias


    Full Text Available This work analyzes the mythological belief or superstitions associated with farming and conservation activities in nine rural productive units on the river basin La Vieja, Colombia. The elderly people recognize the influence of multiple stories over productive and environmental conditions that are an important part of success or fail on their rural activities. The beliefs were classified by their functionality and the activities they regulate. 14 myths that have any on the influence activities of cultivate, breeding, conservation and social regulation were described. The main element for discussion was the functionality, considering its relationship the distribution and application in the subsystems of productions in the farms with the age, the gender and the hierarchy position on the family structure. It was conclude that the flow of information between expert systems and systems of popular knowledge helps to construct an adapted system. An example is the use, in cattle farms, of different moon phases during the artificial insemination to ensure the pregnancy and sex of the breed.Este trabajo analiza las creencias mitológicas, agüeros o supersticiones asociadas con las actividades agropecuarias y de conservación en nueve unidades productivas rurales de la cuenca media del río La Vieja, Colombia. Plantea que las gentes de antaño reconocen la influencia de múltiples relatos sobre condiciones productivas y ambientales que redundan en el éxito o el fracaso de las actividades rurales. Las creencias se clasificaron según su funcionalidad y las actividades que regulan. Se describieron así 14 mitos que influyen en las actividades de cultivo, cría, conservación y regulación social. El principal elemento de discusión fue la funcionalidad, considerando la distribución y aplicación en los subsistemas de producción en la finca, la relación con la edad y el género y con la posición jerárquica en la estructura familiar. El flujo de

  18. ANÁLISE HISTÓRICA DAS TRANSFORMAÇÕES DA FLORESTA AMAZÔNICA EM ÁREAS AGRÍCOLAS NA BACIA DO RIO SUIA-MIÇU. - Historical Changes of the Amazonian Forest into Agricultural Lands in the Suia-Miçu River Basin.

    Antonio Roberto Formaggio


    Full Text Available Mudanças no uso e cobertura da terra, como as ocorridas nas áreas de expansão agrícola na AmazôniaLegal, geram uma série de impactos sociais, econômicos e ambientais. O entendimento destes processospode permitir um melhor planejamento de políticas públicas a fim de monitorar e mapear áreas maissuscetíveis a problemas ambientais. Sendo assim, este trabalho teve como objetivo analisar a dinâmicade ocupação da Bacia do Rio Suiá-Miçu, um dos afluentes do Rio Xingu localizado ao norte do estadodo Mato Grosso. Os mapas de uso e cobertura da terra para cada um dos períodos analisados (1973,1984 e 2005 foram confeccionados com o auxílio de imagens dos sensores MSS/Landsat-1, TM/Landsat-5 e do sensor MODIS/Terra. Os resultados mostraram que até 1984, 13% da vegetação natural dabacia havia sido desflorestada, enquanto que em 2005 as atividades agrícolas já ocupavam 40% daárea de estudo. Desta forma, tendo em vista as mudanças na paisagem observadas ao longo das últimasdécadas, torna-se notória a necessidade urgente de estudos mais aprofundados visando a avaliaçãodos impactos ambientais, bem como a preservação dos recursos naturais na regiãoLand use and land cover changes, as seen in the agricultural expansion areas in the Brazilian LegalAmazon, have as consequence several social, economic and environmental impacts. The understandingof these processes allows a better planning of public policies in order to monitor and map areas moresusceptible to environmental problems. Hence, this work had as objective to analyze the land use/landcover changes dynamics in the Suiá-Miçu River Basin, located in the north part of Mato Grosso state,Brazil. The land use/land cover maps for each of the analyzed periods (1973, 1984 and 2005 weremade using images from the MSS/Landsat-1, TM/Landsat-5 and the MODIS/Terra sensors. The resultsshowed that until 1984, 13% of the natural vegetation of the watershed was deforested, while in 2005the

  19. Espacialização da precipitação e erosividade na Bacia Hidrográfica do Rio Dourados - MS Rainfall and erosion spacializationin Dourados River Basin, MS, Brazil

    Fabiane K. Arai


    Full Text Available A distribuição da precipitação numa bacia hidrográfica durante o ano é um dos fatores determinantes para quantificar a necessidade de irrigação de culturas e de abastecimento de água doméstico e industrial, além de estudos para o controle de inundações e da erosão do solo. O potencial da chuva em causar erosão hídrica pode ser avaliado por meio de índices que se baseiam nas características físicas das chuvas de cada região, entre os quais se destacam índice de erosividade. Analisaram-se, neste trabalho, a espacialização da precipitação pluvial e o índice de erosividade médio anual e mensal na Bacia Hidrográfica do Rio Dourados. Analisando os resultados obtidos, foi possível concluir que: o regime de precipitação apresenta oscilação unimodal, com período chuvoso compreendido entre os meses de outubro e março; todos os meses da estação chuvosa apresentam drásticas reduções da precipitação média; a erosividade média anual variou de 3.192,0 a 4.977,0 MJ mm ha-1 h-1 ano-1; e os meses de dezembro a janeiro apresentam os maiores riscos de ocorrência de perdas de solo por erosão hídrica.The distribution of rainfall in a watershed bay during the year is one of the determining factors to quantify the need for irrigation of crops and domestic and industrial water supply, beyond studies to control flooding and soil erosion. The rain potency to cause erosion can be assessed by indices that are based on physical rainfall characteristics in each region, which erosion is an index. In this study it was analyzed the yearly and monthly indices of rainfall and erosion spacialization in Dourados Watershed Bay. According with the results it was possible to conclude: the rainfall presented a unimodal oscillation, the rainy season ranged from October to March, every month of the rainy season showed a dramatic reductions in the average rainfall, the yearly erosion ranged from 3.192,0 to 4.977,0 MJ mm ha-1 h-1 year-1, and


    Vladimir Souza


    Full Text Available Este trabalho tem como objetivo determinar o potencial natural à erosão (PNE na bacia do rio Jacaré Guaçú (SP com base nos fatores físicos da Equação Universal de Perdas de Solos (EUPS. Dados pedológicos, de precipitação pluviométrica e de Sensoriamento Remoto foram usados para determinar as variáveis naturais do referido modelo, ou seja, erosividade das chuvas (fator R, erodibilidade dos solos (fator K, comprimento de rampa (fator L e declividade do terreno (fator S. Técnicas de Geoprocessamento desenvolvidas em Sistema de Informação Geográfica (SIG foram utilizadas para a estruturação e execução do modelo ambiental. Os resultados demonstram que o fator R da área de estudo varia entre 6392 e 8015, o fator K está compreendido entre 0,0097 e 0,610 e o fator topográfico (LS predominante é menor que 4. Em relação ao PNE, dentre as classes definidas, destacam-se os locais classificados com alto, muito baixo, extremamente alto e muito alto potencial, com representatividade em mais de 90% da área de estudo. Os locais com PNE médio e baixo ocupam menos de 10% da bacia hidrográfica. Os resultados obtidos podem auxiliar no ordenamento territorial da área de estudo, sobretudo no que diz respeito ao gerenciamento e expansão das atividades agropecuárias. ABSTRACT This paper aims to determine the natural erosion potential in Jacaré Guaçú stream basin (São Paulo State - Brazil based in the physical factors of Universal Loss Soil Equation (ULSE. Pedological, rainfall and Remote Sensing data were used to define the natural variables of model, that is, rainfall erosivity (R factor, soil erodibility (K factor and topography (LS factor. Geoprocessing techniques developed in Geographic Information System (GIS were used to structure and execute the environmental model allowing determining areas with higher erosion risk. The results show that the areas classified as high, very low, extremely

  1. RIO Country Report 2015

    Grimpe, Christoph; Mitchell, Jessica

    The 2015 series of RIO Country Reports analyse and assess the policy and the national research and innovation system developments in relation to national policy priorities and the EU policy agenda with special focus on ERA and Innovation Union. The executive summaries of these reports put forward...

  2. RIO Country Report 2015

    Grimpe, Christoph; Mitchell, Jessica

    The 2015 series of RIO Country Reports analyse and assess the policy and the national research and innovation system developments in relation to national policy priorities and the EU policy agenda with special focus on ERA and Innovation Union. The executive summaries of these reports put forward...

  3. Levantamento florístico do componente arbustivo-arbóreo da vegetação ciliar na bacia do rio Taperoá, PB, Brasil Floristic survey of components of shrub-tree riparian vegetation in the Taperoá river basin, Paraíba State, Brasil

    Alecksandra Vieira de Lacerda


    Full Text Available Considerando o papel relevante e o nível de degradação presente nas áreas ciliares, a pesquisa objetivou estudar a composição florística do componente arbustivo-arbóreo da vegetação ciliar em diferentes ambientes hídricos do semi-árido paraibano na bacia do rio Taperoá. O levantamento florístico foi realizado no período de junho/2002 a fevereiro/2003 e abrangeu nove pontos distribuídos ao longo de rios, riachos, lagoa e açude. A definição das atividades apoiou-se em análise de cartas e mapas da vegetação em escala de 1:100.000 e caminhadas aleatórias que permitiram a realização de coleta de material vegetal, utilizado para identificação por meio de consultas a especialistas e de morfologia comparada, usando bibliografia especializada e análise das exsicatas depositadas no herbário Lauro Pires Xavier - JPB (UFPB, João Pessoa, PB. A vegetação arbustivo-arbórea da mata ciliar nos nove pontos amostrados foi representada por 43 espécies, das quais 41 são pertencentes a 19 famílias, e duas espécies permaneceram indeterminadas. As famílias que apresentaram o maior número de espécies foram Mimosaceae (sete, Caesalpiniaceae (cinco e Euphorbiaceae (cinco. Os resultados da análise de agrupamento indicaram que as áreas ciliares apresentaram certa particularização em termos de composição florística, o que se refletiu nos baixos índices de similaridades entre o conjunto de áreas amostradas.Considering the relevant role and the current level of degradation of riparian areas, this work aimed to study the floristic composition of shrub-tree riparian vegetation at different hydric environments in the Taperoá river basin, in the semi-arid region of the Paraíba State, Northeast Brazil. The survey was performed from June 2002 to February 2003. Nine sampling sites were distributed along rivers and streams, and around lagoon, and dam. The definition of activities was based on the analysis of charts and vegetation maps

  4. Ecohydromorphology of river environments of the das Velhas River upstream of Rio de Pedras hydroelectric reservoir, MG, Brazil

    Helena Lúcia Menezes Ferreira


    Full Text Available This paper presents the applicability of ecohydromorphology assessment in differentiating ecophysical structure of river habitats of Rio das Velhas river basin upward of Rio de Pedras reservoir, Minas Gerais,Brazil. It also presents the identification of the factors conditioning the ecophysical structure of river habitats. This review associated with biological and physico-chemical conditions of the waters aims to assess the ecological integrity of the river system and also validate the characterization of water bodies identified on a large scale in the Rio das Velhas basin.

  5. Avaliação da qualidade da água da bacia do rio Pirapó – Maringá, Estado do Paraná, por meio de parâmetros físicos, químicos e microbiológicos = Water quality evaluation of the Pirapó river basin – Maringá, Paraná State, through physical, chemical and microbiologic parameters

    Eliane Cristina Alves


    Full Text Available Este trabalho teve como objetivo monitorar a qualidade da água da bacia do rio Pirapó, principal fonte de abastecimento do município de Maringá, Estado do Paraná, e região. Foram estabelecidos cinco pontos de amostragem localizados à jusante dos principais ribeirões e córregos da bacia. A coleta das amostras foi realizada de forma pontual no ponto central da seção do rio, mensalmente, no período de abril/2005 a abril/2006. A qualidade da água foi avaliada por indicadores estabelecidos pela Resolução Conama nº 357/2005. Naavaliação dos parâmetros, foi possível indicar duas principais fontes poluidoras. A primeira é a exploração do solo, que se estende até às margens do rio, desprovida de mata ciliar, que ocasiona o transporte, principalmente, em períodos chuvosos, de sedimentos e nutrientes aocorpo d¢água. A segunda é o lançamento clandestino de esgoto doméstico, apontado como o responsável pelos elevados índices de matéria orgânica e coliforme encontrados no corpo receptor.This work had as objective to monitor water quality in the Pirapó River basin, which is the main supply source to the city of Maringá, Paraná State, and adjacent regions. Five sampling spots wereestablished downstream from the main creeks and streams of the basin. Sample collection was carried out periodically at the central point of the river section, collected monthly, during the period from April/2005 to April/2006. Water quality was evaluated usingindicators established by Conama Resolution no. 357/2005. During an evaluation of the parameters, it was possible to indicate that there are two main polluting sources. The first is soil exploitation extending until the river’s edges, which has no gallery forests, leading to sediments and nutrients fallout into the water body, mainly during the rainy periods. The second source is the dumping of domestic sewage, pointed as responsible for the elevated levels of organic matter and coliforms.

  6. Qualidade da água em região alterada pela mineração de carvão na microbacia do rio Fiorita (Siderópolis, Estado de Santa Catarina, Brasil - DOI: 10.4025/actascibiolsci.v26i2.1610 Water quality in disturbed area by coal mining, Fiorita river basin (Siderópolis, State of Santa Catarina, southern Brazil - DOI: 10.4025/actascibiolsci.v26i2.1610

    Eder Santo


    Full Text Available A mineração de carvão constitui importante atividade econômica na região sul catarinense. A área da bacia hidrográfica do rio Fiorita (Município de Siderópolis, SC foi intensamente minerada e atualmente apresenta inúmeros locais com rejeitos, estéreis de mineração e lagos ácidos. Este trabalho teve como principal objetivo verificar os efeitos da mineração de carvão na qualidade da água dos corpos de água na microbacia do rio Fiorita. As análises gráficas e multivariada (“cluster” sugerem que a microbacia apresenta um gradiente horizontal, com redução da qualidade da água em direção à parte baixa da bacia, com diminuição do pH e elevação nos valores de acidez total, condutividade elétrica, Eh e nos teores de sólidos totais, sulfato, alumínio, cálcio, ferro II e total, magnésio e manganês. Esses dados sugerem o efeito da concentração de metais. Como primeira aproximação, de acordo com a Resolução Conama 20 de 1986, as águas da microbacia do rio Fiorita apresentam-se com elevado grau de comprometimento de sua qualidade e de uso restrito. Também são apresentadas considerações visando contribuir com subsídios à recuperação ambiental da área em questãoCoal mining is an important economical activity in the south of Santa Catarina, Brazil. The em>Fiorita River basin (municipality of Siderópolis was heavily mined out and nowadays several places with mining spoils and sterile soil, as well as acid lakes, can be found in its area. This study aimed to carry out an environmental diagnosis on the water bodies quality in that region. Graphic and cluster analysis suggested that the Fiorita River basin was compartmented. It seemed that there was a deterioration gradient in water quality toward the lower portion of the basin, with pH decrease and a rise in values of total acidity, electric conductivity, Eh, total solids contents, sulphate, aluminium, calcium, iron II and totals, manganese and magnesium

  7. Geographic distribution of genetic diversity in populations of Rio Grande Chub Gila pandora

    Galindo, Rene; Wilson, Wade; Caldwell, Colleen A.


    In the southwestern United States (US), the Rio Grande chub (Gila pandora) is state-listed as a fish species of greatest conservation need and federally listed as sensitive due to habitat alterations and competition with non-native fishes. Characterizing genetic diversity, genetic population structure, and effective number of breeders will assist with conservation efforts by providing a baseline of genetic metrics. Genetic relatedness within and among G. pandora populations throughout New Mexico was characterized using 11 microsatellite loci among 15 populations in three drainage basins (Rio Grande, Pecos, Canadian). Observed heterozygosity (HO) ranged from 0.71–0.87 and was similar to expected heterozygosity (0.75–0.87). Rio Ojo Caliente (Rio Grande) had the highest allelic richness (AR = 15.09), while Upper Rio Bonito (Pecos) had the lowest allelic richness (AR = 6.75). Genetic differentiation existed among all populations with the lowest genetic variation occurring within the Pecos drainage. STRUCTURE analysis revealed seven genetic clusters. Populations of G. pandora within the upper Rio Grande drainage (Rio Ojo Caliente, Rio Vallecitos, Rio Pueblo de Taos) had high levels of admixture with Q-values ranging from 0.30–0.50. In contrast, populations within the Pecos drainage (Pecos River and Upper Rio Bonito) had low levels of admixture (Q = 0.94 and 0.87, respectively). Estimates of effective number of breeders (N b ) varied from 6.1 (Pecos: Upper Rio Bonito) to 109.7 (Rio Grande: Rio Peñasco) indicating that populations in the Pecos drainage are at risk of extirpation. In the event that management actions are deemed necessary to preserve or increase genetic diversity of G. pandora, consideration must be given as to which populations are selected for translocation.

  8. Two new species of Pseudancistrus (Siluriformes, Loricariidae) from the Amazon basin, northern Brazil

    Gabriel da Costa e Silva; Roxo, Fábio F; Claudio Oliveira


    Abstract Two new species of Pseudancistrus , a genus diagnosed by non-evertible cheek plates and hypertrophied odontodes along the snout margin, are described from two drainages of the Brazilian Shield: Pseudancistrus kayabi from the rio Teles Pires (rio Tapajós basin) and Pseudancistrus asurini from the rio Xingu. The new species are distinguished from congeners ( Pseudancistrus barbatus , Pseudancistrus corantijniensis , Pseudancistrus depressus , Pseudancistrus nigrescens , Pseudancistrus ...

  9. Variabilidade sazonal da relação entre a radiação fotossinteticamente ativa e a radiação global na bacia do rio Doce, Estado de Minas Gerais = Seasonal variability of the relationship between the photosynthetically active radiation and the global radiation at the river Doce basin, Minas Gerais State

    Antonio José Steidle Neto


    Full Text Available O conhecimento da Radiação Fotossinteticamente Ativa (RFA é importante para diferentes áreas relacionadas à fisiologia vegetal e ciências agrárias. Modelos de estimativa de RFA a partir da Radiação Global (Rg são extremamente úteis, visto que a Rg é convencionalmente medida nas estações meteorológicas. Assim, analisou-se a variabilidade sazonal da relação RFA/Rg em cinco áreas localizadas na bacia do rio Doce, Estado de Minas Gerais, considerando-se os períodos secos e chuvosos dos anos de 2001 a 2004. As relações RFA/Rg obtidas para os períodos secos e chuvosos, assim como para todos os dados, apresentaram concordância com as relações determinadas por diversos pesquisadores em diferentes áreas do mundo. Analisando-se os resultados, constatou-se que, de maneira geral,as relações RFA/Rg tendem a ser superiores durante os períodos chuvosos comparativamente aos secos. Por este estudo, pôde-se concluir que existe variação interanual desta relação, demonstrando assim a necessidade de se considerar esta variabilidade para estimaradequadamente a RFA a partir da Rg. The knowledge of the Photosynthetically Active Radiation (PAR is important to different areas of vegetal physiology and agricultural sciences. Estimation models of the PAR based on the Global Radiation (GR are extremely useful, since the GR is conventionally measured atthe meteorological stations. Thus, the seasonal variability of the relationship PAR/GR was analyzed in five areas located at the river Doce basin, Minas Gerais State, Brazil, considering the dry and wet periods of the years 2001 to 2004. The relationships PAR/GR obtained for the dry and wet periods, and also to all data, presented agreement with those ones determined by several researchers in different areas of the world. Results showed that the relationshipsPAR/GR generally tend to be greater during the wet periods when compared with the dry ones. By this work, it could be concluded that

  10. Análise de técnicas de interpolação para espacialização da precipitação pluvial na bacia do rio Itapemirim (ES / Analysis of interpolation techniques for spatial rainfall distribution in river basin Itapemirim (ES

    Benvindo Sirtoli Gardiman


    Full Text Available ResumoEste trabalho teve como objetivo comparar o desempenho de cinco métodos de interpolação: inverso da distância ponderada (IDW, Krigagem esférico, natural vizinho, Spline regularizada e Topo to Raster. Para tanto, utilizaram-se dados de precipitação pluviométrica média mensal de um período de trinta anos (1972 a 2002, obtidas junto ao Sistema de Informações Hidrológicas (HidroWEB da Agência Nacional de Águas (ANA, de estações localizadas dentro e fora da área da bacia hidrográfica do rio Itapemirim, sul do estado do Espírito Santo. Os resultados apontam que o interpolador de Krigagem esférica obteve o menor Erro Quadrado Médio (EQM, Percentual de Eficiência (EF%, Erro Médio Absoluto (MAE, Coeficiente de Determinação (r² e Estimativa do Erro Padrão (EEP, seguido por IDW, Spline regularizada, natural vizinho e, por último, Topo to Raster. A diferença entre os valores observados e estimados pelo método Krigagem esférico foi muito menor do que para os outros quatro métodos, indicando ser esse o interpolador que representa melhor a distribuição espacial da precipitação pluvial média mensal para os dados em estudo.AbstractThis work had the main objective to compare the performance of five methods of interpolation’s style, inverse of the distance’s weight (IDW, round Krigagem, natural neighbor , regularized Spline and Top to rater. Therefore, average monthly rainfall in a period 30 years (1972 the 2002, together with the results of Sytem Hidrological Information ( Hidroweb of National Water Agency (ANA were used around and next of Itapemirim hidrological basin river, southern state of Espirito Santo. The results showed the round Krigagem the lowst Medin Square Mistake (EQM, Efficient percent (EF%, Absolute Medium Mistake (MAE, Determination modulus (r2 and Standard Estimation Mistake (EEP, followed to IDW, regulated Spline, neighbor natural and for last Top to rater. Nonetheless, the difference between the


    Manuel Vazquez Vidal Jr.


    Full Text Available

    The aim of this article was evaluate de relationship among feeding index and reproductive cycle in male red-piau (Leporinus copelandii, in the low basin of paraiba do sul river. Fishes were collected monthly, from February 1998 to march 1999, and obtained the following param-eters: total condition factor (k1 and somatic (k2, stomach repletion index (SRI and stomach repletion stage (SRS, and gonadal maturation. in general, condition and gonadal parameters showed an inverse relation with nutritional parameters. during the spawning season (september to January, was observed low values of SRS and SRI, fol-lowing an increase of these parameters after spawning, and it seems to be a natural mechanism of corporal condition recovering.

    Key-Words: Leporinus, fish, reproduction, reproductive biology.

    Objetivou-se com este trabalho avaliar a relação entre índices de alimentação e ciclo reprodutivo de machos de piau-vermelho, na região do baixo rio Paraíba do Sul (latitude 21° 41’ 15” S e longitude 42° 03’ 45” W. amostras foram coletadas mensalmente, entre fevereiro de 1998 a janeiro de 1999, sendo obtidos os seguintes parâmetros: fator de condição total (k1 e somático (k2, índice gastro-somático (IGas e estádio de repleção estomacal (ERE, e estádios de maturação gonadal. em geral, parâmetros de condição corporal e gônadas apresentaram uma relação inversamente proporcional aos parâmetros de alimentação. durante a estação reprodutiva (setembro–janeiro, foram observados os menores valores de IGas e ERE, seguidos por um incremento desses parâmetros após a reprodução, mostrando ser um mecanismo natural de reposição da condição corporal.

    Palavras-chaves: biologia reprodutiva, Leporinus, peixe, reprodução.

  12. Evoluzione del paesaggio e insediamento nel bacino del Rio Posada. Indagini geoarcheologiche

    French, Charles; Sulas, Federica; Melis, Rita T.


    New geoarchaeological investigations provide the first local, environmental records concerning the long-term history of the Rio Posada basin in eastern Sardinia. In this article, we present some preliminary findings of field research and laboratory analyses and propose an environmental sequence a...

  13. 78 FR 5480 - Draft Candidate Conservation Agreement With Assurances and Draft Environmental Assessment; Rio...


    ... Grande cutthroat trout (Oncorhynchus clarkii virginalis) is native to the Rio Grande, Pecos River, and Canadian River basins in New Mexico and Colorado. It is the southernmost subspecies of cutthroat trout..., including fragmentation and isolation, small population size, presence of nonnative trout, whirling disease...

  14. Water resources data, Texas water year 1998, volume 3. Colorado River basin, Lavaca River basin, Guadalupe River basin, Nueces River basin, Rio Grande basin, and intervening coastal basins

    Gandara, S.C.; Gibbons, W.J.; Andrews, F.L.; Barbie, D.L.


    Water-resources data for the 1998 water year for Texas are presented in four volumes, and consist of records of stage, discharge, and water quality of streams and canals; stage, contents, and water-quality of lakes and reservoirs; and water levels and water quality of ground-water wells. Volume 3 contains records for water discharge at 126 gaging stations; stage only at 3 gaging stations; stage and contents at 15 lakes and reservoirs; water quality at 62 gaging stations; and data for 35 partial-record stations comprised of 8 flood-hydrograph, 14 low-flow, and 18 creststage, and 5 miscellaneous stations. Also included are lists of discontinued surface-water discharge or stage-only stations and discontinued surface-water-quality stations. Additional water data were collected at various sites, not part of the systematic data-collection program, and are published as miscellaneous measurements. These data represent that part of the National Water Data System operated by the U.S. Geological Survey and cooperating Federal, State, and local agencies in Texas. Records for a few pertinent stations in the bordering States also are included.

  15. Avaliação de risco ambiental por contaminação metálica e material orgânico em sedimentos da bacia do Rio Aurá, Região Metropolitana de Belém - PA Evaluation of environmental risk by metallic contamination and organic compounds in sediments of the Aurá River basin, Belém, Pará - Brazil

    Gilmar W. Siqueira


    Full Text Available A bacia do Rio Aurá está situada na região metropolitana de Belém, entre os municípios de Belém e Ananindeua, onde a taxa populacional tem aumentado sem qualquer medida de controle social ou ambiental. A região é intensamente explorada, sendo que os principais problemas ambientais são o desmatamento, erosão, inundação, poluição e contaminação das águas, especialmente por metais pesados e compostos orgânicos. O comportamento geoquímico dos elementos Al, Fe, Mn, Cr, Ni e Cu e os teores de compostos orgânicos foram avaliados em 30 pontos de amostragem no período entre 2008 e 2010 nos sedimentos fluviais. O aterro sanitário não controlado localizado nas proximidades da bacia do Rio Aurá é responsável, em parte, pela contaminação dos sedimentos. O estresse ambiental é resultado das atividades antrópicas locais, que contribuem no transporte de material clástico contendo metais para o rio. As variáveis estudadas foram classificadas segundo mecanismos de transporte e fonte (autóctone ou alóctone. Os resultados demonstraram que a principal contribuição de íons Al e Fe foi o aterro sanitário; Mn e Ni vieram principalmente dos solos adjacentes; Cr foi modificado (III/VI por processo alobioquímico e Cu por processo bioinduzido.The Aurá River basin is situated in the Belém Metropolitan region, between the municipalities of Belém and Ananindeua, where the rate of population growth has increased without any social and environmental control. The region is intensely exploited and the more frequent environmental problems are deforestation, erosion, flooding, water pollution and contamination, especially by heavy metals and organic compounds (OC. Geochemistry behavior (Al, Fe, Mn, Cr, Ni and Cu and OC levels were determined in the 30 sampling sites between 2008 and 2010 in the bottom sediments of the river. There is an uncontrolled sanitary landfill situated at the north of the Aurá River responsible, in part, by the

  16. The Temporal and Spatial Association of Faulting and Volcanism in the Cerros del Rio Volcanic Field - Rio Grande Rift, USA

    Thompson, R. A.; Hudson, M. R.; Minor, S. A.; McIntosh, W. C.; Miggins, D. P.; Grauch, V.


    The Plio-Pleistocene Cerros del Rio volcanic field (CdRVF) in northern New Mexico is one of the largest ( greater than 700 square kilometers) predominantly basaltic and andesitic volcanic centers of the Rio Grande rift; it records the late-stage, volcano-tectonic evolution of the SW part of the Espanola Basin. The CdRVF reflects both regional proclivity toward Pliocene basaltic volcanism following protracted Neogene extensional tectonism and localized eruptive response to migration of basin- bounding faults. Approximately 180 cubic kilometers of flat lying to gently dipping basalt, andesite, and minor dacite lava flows and pyroclastic deposits of the CdRVF were erupted from more than 50 exposed vents between 2.8 Ma and 1.14 Ma. Subsurface interpretations of drill hole data and incised canyon exposures of the Rio Grande show that volcanic deposits are interbedded with Santa Fe Group sediments deposited in actively subsiding sub-basins of the southernmost Espanola Basin. Major basin-bounding faults in this area strike north to northwest, dip basinward, and have mostly dip-slip and subordinate strike-slip displacement. Although major basin-bounding faults were active prior to the onset of volcanism in the CdRVF, protracted extension resulted in a westward migration of graben-bounding faults. Phases of coeval volcanism at 2.8-2.6 Ma, 2.5-2.2 Ma, and 1.5-1.1 Ma, decreased in eruptive volume through time and are delineated on the basis of mapped stratigraphy, argon geochronology, paleomagnetic and aeromagnetic properties, and record a syntectonic westward migration of eruptive centers. The alignment of vent areas with mapped faults strongly suggests deep magmatic sources utilized local structures as conduits (i.e. faults and fractures developed in response to regional stress). However, some near-surface feeder dikes associated with eroded cinder cones record orientations that are not typically correlative with regional fault patterns suggesting near-surface conduits are

  17. Rock in Rio: forever young

    Ricardo Ferreira Freitas


    Full Text Available The purpose of this article is to discuss the role of Rock in Rio: The Musical, as herald of megafestival Rock in Rio. Driven by the success that musicals have reached in Brazil, we believe that the design of this spectacle of music, dance and staging renews the brand of the rock festival, once it adds the force of young and healthy bodies to its concept. Moreover, the musical provides Rock in Rio with some distance from the controversal trilogy of sex, drugs and rock and roll, a strong mark of past festivals around the world. Thus, the musical expands the possibilities of growth for the brand.

  18. Rock in Rio: eternamente jovem

    Ricardo Ferreira Freitas; Flávio Lins Rodrigues


    The purpose of this article is to discuss the role of Rock in Rio: The Musical, as herald of megafestival Rock in Rio. Driven by the success that musicals have reached in Brazil, we believe that the design of this spectacle of music, dance and staging renews the brand of the rock festival, once it adds the force of young and healthy bodies to its concept. Moreover, the musical provides Rock in Rio with some distance from the controversal trilogy of sex, drugs and rock and roll, a strong mark ...

  19. The concentrations of heavy metals and the incidence of micronucleated erythrocytes and liver EROD activity in two edible-fish from the Paraíba do Sul river basin in Brazil | Concentração de metais pesados e incidência de eritrócitos micronucleados e atividade de EROD hepática em duas espécies de peixes comestíveis na bacia do Rio Paraíba do Sul, Brasil

    Thiago Estevam Martins Parente


    Full Text Available The Paraíba do Sul river (PSR basin crosses one of the most populated and industrialized regions of Brazil and receives effluent from the metallurgic, paper mill and agricultural industries. PSR water has multiple uses, including being a supply of potable water and riverine populations which consume some species of its fish. In the present study, we investigated the responses of two biomarkers of aquatic pollution, EROD activity in the liver and micronuclei frequency in peripheral blood, as well as the concentrations of seven heavy metals in the muscle tissue of two species of fish native to the PSR: Geophagus brasiliensis and Hypostomus sp. Sampling was performed in both the wet and dry seasons of 2003, with a total of 339 fish collected from 16 sites along the PSR basin. Fish collected at Levy Gasparian, Barra Mansa and Três Rios both had higher EROD activity and micronuclei frequency. The results also suggested a moderate induction of EROD activity in fish collected from S.L. Paraitinga and Sapucaia. Micronuclei frequency was elevated in fish from S.J. Campos, Além Paraíba, Campos and S.J. Barra. In all cases, heavy metal concentrations did not exceed the maximum considered safe for fish meat consumption. -------------------------------------------------------------------------------------------- A bacia do rio Paraíba do Sul (PSR atravessa uma das regiões mais povoadas e industrializadas do Brasil, recebendo efluentes de indústrias metalúrgicas, de papel e celulose e agrícolas. Os usos das águas do PSR são múltiplos, incluem o fornecimento de água potável, e as populações ribeirinhas consomem algumas de suas espécies de peixes. No presente trabalho foram investigadas as respostas de dois biomarcadores à poluição, a atividade hepática de EROD e a freqüência de micronúcleo em sangue periférico, e medidos os níveis de sete metais pesados no músculo de duas espécies de peixes nativas do PSR, Geophagus brasiliensis and

  20. Avaliação da contaminação do Igarapé do Sabino (Bacia do Rio Tibiri por metais pesados, originados dos resíduos e efluentes do Aterro da Ribeira, em São Luís, Maranhão Evaluation of contamination on Sabino streamlet (Basin Rio Tibiri by heavy metals originated from waste and effluents of the Ribeira landfill, in São Luis island, state of Maranhão, Brazil

    Antonio Eduardo Lopes Campos


    Full Text Available This work aimed to carry out an environmental monitoring in sabino narrow river (affluent of Tibiri Basin, in São Luís - MA, Brazil, in order to verify the main environmental impacts caused by effluent residues from Ribeira landfill. Chemical analysis and bibliographic and cartographic researches on this ecosystem were also carried out. In addition, heavy metals, such as Hg, Pb and Zn, were investigated in water samples by ICP-MS technique. It was observed that the contents of such heavy metals were above the tolerance limits established by the Brazilian legislation, showing a strong impact level on the evaluated ecosystem.

  1. Social-economic Analyse And Technologic Aspects Of The Agriculture At The Mogi Guaçu River Hydrographic Basin [análise De Aspectos Socioeconômicos E Tecnológicos Da Agropecuária Na Bacia Hidrográfica Do Rio Mogi Guaçu

    Zibordi M.S.; Cardoso J.L.; Vilela Filho L.R.


    Currently, owing to the occurrence of environmental problems, along with the need of environmental preservation, both the territory management of Hydrographic Basin and the conservation of natural resources have proven to have remarkable importance. Thus, the mean goal of the research is to raise and scrutinize social-economic and technologic data from the Mogi Guaçu River Hydrographic Basin (São Paulo, Brazil). The aim is to group municipalities with similar characteristics regarding the col...

  2. Sedimentation in Rio La Venta Canyon in Netzahualcoyotl Reservoir, Chiapas, Mexico

    de La Fuente, J. A.; Lisle, T.; Velasquez, J.; Allison, B. L.; Miller, A.


    Sedimentation of Rio La Venta as it enters the Netzahualcoyotl Reservoir in Chiapas, Mexico, threatens a unique part of the aquatic ecosystem. Rio La Venta enters the reservoir via a narrow canyon about 16 km long with spectacular, near-vertical limestone bluffs up to 320 m high and inhabited by the flora and fauna of a pristine tropical forest. Karst terrain underlies most of the Rio La Venta basin in the vicinity of the reservoir, while deeply weathered granitic terrain underlies the Rio Negro basin, and the headwaters of the Rio La Venta to the south. The Rio Negro joins Rio La Venta 3 km downstream of the upper limit of the reservoir and delivers the bulk of the total clastic sediment (mostly sand and finer material). The canyon and much of the contributing basin lie within the Reserva de la Biosfera, Selva El Ocote, administered by the Comision Nacional de Areas Naturales Protegidas, part of the Secretaria de Medioambiente y Recursos Naturales. The Klamath National Forest Forest has cooperated with its Mexican counterparts since 1993 in natural resource management, neo-tropical bird inventories, wildfire management, and more recently in watershed analyses. Rates of sedimentation are estimated from bathymetric surveys conducted in March, 2002. A longitudinal profile down the inundated canyon during a high reservoir level shows an inflection from a slope of 0.0017 to one of 0.0075 at 7.2 km downstream of the mouth of Rio Negro. The bed elevation at this point corresponds to the lowest reservoir level, suggesting that the gentler sloping bed upstream is formed by fluvial processes during drawdown and that downstream by pluvial processes. Using accounts that boats could access Rio Negro during low water levels in 1984, we estimate an annual sedimentation rate of roughly 3 million cubic meters per year. This suggests that boats might no longer be able to access the most spectacular section of canyon upstream of Rio Negro within a decade, depending on how the

  3. Water-level data for the Albuquerque Basin and adjacent areas, central New Mexico, period of record through September 30, 2014

    Beman, Joseph E.


    The Albuquerque Basin, located in central New Mexico, is about 100 miles long and 25–40 miles wide. The basin is hydrologically defined as the extent of consolidated and unconsolidated deposits of Tertiary and Quaternary age that encompasses the structural Rio Grande Rift. Drinking-water supplies throughout the basin were obtained solely from groundwater resources until December 2008, when treatment and distribution of surface water from the Rio Grande through the San Juan-Chama Drinking Water Project began. A 20-percent population increase in the basin from 1990 to 2000 and a 22-percent population increase from 2000 to 2010 resulted in an increased demand for water.

  4. Evapotranspiration seasonality across the Amazon Basin

    Eiji Maeda, Eduardo; Ma, Xuanlong; Wagner, Fabien Hubert; Kim, Hyungjun; Oki, Taikan; Eamus, Derek; Huete, Alfredo


    Evapotranspiration (ET) of Amazon forests is a main driver of regional climate patterns and an important indicator of ecosystem functioning. Despite its importance, the seasonal variability of ET over Amazon forests, and its relationship with environmental drivers, is still poorly understood. In this study, we carry out a water balance approach to analyse seasonal patterns in ET and their relationships with water and energy drivers over five sub-basins across the Amazon Basin. We used in situ measurements of river discharge, and remotely sensed estimates of terrestrial water storage, rainfall, and solar radiation. We show that the characteristics of ET seasonality in all sub-basins differ in timing and magnitude. The highest mean annual ET was found in the northern Rio Negro basin (˜ 1497 mm year-1) and the lowest values in the Solimões River basin (˜ 986 mm year-1). For the first time in a basin-scale study, using observational data, we show that factors limiting ET vary across climatic gradients in the Amazon, confirming local-scale eddy covariance studies. Both annual mean and seasonality in ET are driven by a combination of energy and water availability, as neither rainfall nor radiation alone could explain patterns in ET. In southern basins, despite seasonal rainfall deficits, deep root water uptake allows increasing rates of ET during the dry season, when radiation is usually higher than in the wet season. We demonstrate contrasting ET seasonality with satellite greenness across Amazon forests, with strong asynchronous relationships in ever-wet watersheds, and positive correlations observed in seasonally dry watersheds. Finally, we compared our results with estimates obtained by two ET models, and we conclude that neither of the two tested models could provide a consistent representation of ET seasonal patterns across the Amazon.

  5. Evolution of the central Rio Grande rift, New Mexico: New potassium-argon ages

    Baldridge, W. S.; Damon, P. E.; Shafiqullah, M.; Bridwell, R. J.


    New K sbnd Ar age determinations on mid-Oligocene to Pleistocene volcanic and shallow intrusive rocks from the central Rio Grande rift permit a more detailed understanding of the tectonic and magmatic history of the rift. Initial extension in the region of the central rift may have begun prior to 27 m.y. ago. By 25 m.y. ago broad basins existed and were filling with volcaniclastic sediments derived mainly from volcanic centers in the San Juan and Questa areas. Continued tectonic activity narrowed these basins by 21-19 m.y. ago, indicated in the Santa Fe area by tilting and faulting that immediately postdate 20-m.y.-old latite. Uplift of the Sangre de Cristo, Sandia, and Nacimiento Mountains shed clastic debris of the Santa Fe Group into these basins. Early rift magmatism is characterized by an overlap of mid-Tertiary intermediate intrusive and extrusive activity, extending to 20 m.y. ago, with mafic and ultramafic volcanism, ranging from 25 to 19 m.y. Both volcanism and tectonic activity were minimal during the middle Miocene. About 13 m.y. ago renewed volcanic activity began. Tectonism commenced in the late Miocene, resulting in the present, narrow grabens. The term "Rio Grande rift" should be restricted to these grabens formed during post-mid-Miocene deformation. Widespread eruption of tholeiitic and alkali olivine basalts occurred 3-2 m.y. ago. The Rio Grande drainage system was integrated 4.5-3 m.y. ago, leading to the present erosional regime. These intervals of deformation and magmatism correspond generally with a similar sequence of events in the Basin and Range province south of the Colorado Plateau. This similarity indicates that the Rio Grande rift is not a unique structure in the southwestern U.S., and must be related to the larger context of the entire Basin and Range province.

  6. Efeito do gradiente altitudinal/latitudinal sobre espécies de aves florestais da família Furnariidae na Bacia do Rio Tibagi, Paraná, Brasil Effect of altitudinal/latitudinal gradient about forest ovenbirds species (Aves: Furnariidae) in the Tibagi river basin, Paraná, Brazil

    Fernando de L. Fávaro; Luiz dos Anjos; Edson V. Lopes; Luciana B. Mendonça; Graziele H. Volpato


    Variações na riqueza e abundância de Furnariidae florestais foram analisadas ao longo do gradiente altitudinal/latitudinal da bacia do rio Tibagi (BRT), Paraná, Brasil. A Floresta Ombrófila Mista (1060 m a.n.m.) é...

  7. Composição específica e abundância da ictiofauna do rio dos Padres, bacia do rio Iguaçu, Brasil - DOI: 10.4025/actascibiolsci.v28i3.193 Specific composition and abundance of the ichthyofauna from Padres’ river, Iguaçu river basin, Brazil - DOI: 10.4025/actascibiolsci.v28i3.193

    Vitor André Frana


    Full Text Available A composição e estrutura das comunidades de peixes podem ser consideradas como indicadores ecológicos e ambientais, constituindo-se desta forma como ferramenta para o manejo de bacias hidrográficas. O presente estudo objetivou levantar informações sobre a composição específica e abundância da ictiofauna do rio dos Padres. Foram realizadas amostragens trimestrais pelo método da pesca elétrica em dois pontos de coleta, um próximo à nascente e outro nas proximidades da foz. As coletas resultaram na captura de 7.026 exemplares pertencentes a 12 espécies distribuídas em sete famílias. A nascente apresentou uma alta densidade em número de indivíduos e menores valores de diversidade, eqüitabilidade e riqueza de espécies em relação à foz. O levantamento da composição específica e abundância da ictiofauna de um rio é de grande importância, por fornecer subsídio a futuros manejos e monitoramentos, tanto da comunidade aquática quanto do ambiente.The composition and structure of fish community can be considered ecological and environmental indicators. The present study aimed to survey information about the specific composition and abundance of the ichthyofauna from Padres’ River. Quarterly samplings were accomplished by the method of the electrofishing in two sample sites, one close to the headwater and another in the proximities of the mouth. The collections resulted in the capture of 7026 specimens belonging to 12 species, which, in turn, fit in seven different families. The headwater presented a high density in number of individuals and smaller values of diversity, evenness and richness of species in relation to the mouth. The raising of the specific composition and abundance of the ichthyofauna of a river is of great importance for supplying subsidy to future managements and accompaniment, as much of the aquatic community as of the environment.

  8. Organização das assembléias de peixes em riachos da bacia do rio Iguatemi, Estado do Mato Grosso do Sul - DOI: 10.4025/actascibiolsci.v27i2.1350 Organization of the fish assemblages in streams of Iguatemi River basin, Mato Grosso do Sul State - DOI: 10.4025/actascibiolsci.v27i2.1350

    Miguel Petrere Junior


    Full Text Available Como o objetivo de descrever os padrões de organização das comunidades de peixes em riachos da bacia do rio Iguatemi amostramos riachos com redes de espera e de arrasto no período de novembro/1999 a agosto/2000. Coletamos 567 indivíduos distribuídos em 24 espécies. Constatamos influência significativa das características dos riachos sobre a diversidade de espécies. A composição de espécies foi pouco explicada pelas características dos riachos. Verificamos influência significativa da morfologia na distribuição em ocorrência das espécies (Mantel r = -0,34; P = 0,04, mas não na distribuição em sua abundância (Mantel r = -0,21; P = 0,07. Comprovamos através do índice de co-ocorrência (C-score das espécies que sua composição nos riachos estudados é estocásticaAiming to describe the patterns of the fish assemblages organization in streams of the Iguatemi River basin we sampled streams with seine nets and sieves from November/1999 to August/2000. We collected 567 individuals distributed in 24 species. We detected statistically significant influence of the streams characteristics upon species diversity. The species composition was hardly explained by the physical and chemical characteristics of the streams. Then we detected significant influence of the fish ecomorphology in the species occurrence (Mantel r = -0,34; P = 0,04, but not in the distribution of its abundance (Mantel r = -0,21; P = 0,07. We verified through the species co-occurrence index (C-score that its composition in the studied streams is stochastic

  9. Rio Grande Rift: History of Tectonic Opening and Magmatism

    van Wijk, J.; Axen, G. J.; Koning, D.


    We describe the mid-Miocene to present opening history of the Rio Grande rift from tectonic subsidence patterns, published Quaternary fault activity, and spatial, temporal and geochemical distributions of volcanism. Rift opening was quite fast until 8 Ma, with tectonic subsidence rates comparable to those of the pre-rupture phase of rifted continent margins, but post-8 Ma rates are slower in all studied localities. Integration of age control reveals that a rift-margin unconformity formed between 8.5 and 3.5 Ma, its exact duration varying depending on location. This partly coincides with uplift of the Ogallala formation in the western Great Plains. The widespread extent of the unconformity suggest that the unconformity records a region-wide dynamic uplift event, possibly resulting from mantle upwelling below the region. This is supported by geoid analyses. The unconformity postdates a change in relative plate motion between the North American and Pacific plates, which may account for the post-8 Ma decrease in subsidence rates. Distribution of Quaternary fault activity is concentrated on the border faults in the northern basins where the rift is in a juvenile stage, but distributed on intra-basin faults further south in the rift where the crust is thinned more. Our analyses show that volcanism in the Rio Grande rift has been of mainly basaltic composition since the Miocene; volcanism during early rifting ranged from basalt to rhyolite. Volcanism has not been evenly distributed in the rift, but concentrated in three large volcanic fields that were located outside of the main rift prior to rift opening, and along the Jemez Lineament which crosses the Rio Grande rift, with sporadic volcanic activity elsewhere. The southern portion of the rift has experienced less volcanic activity than the northern rift, perhaps because it is underlain by fast seismic wave velocity upper mantle that may be linked to colder or compositionally different (Farallon plate subduction related

  10. RIO Country Report 2015: Iceland



    The 2015 series of RIO Country Reports analyse and assess the policy and the national research and innovation system developments in relation to national policy priorities and the EU policy agenda with special focus on ERA and Innovation Union. The executive summaries of these reports put forward the main challenges of the research and innovation systems.

  11. ESD and the Rio Conventions

    Sarabhai, Kartikeya V.; Ravindranath, Shailaja; Schwarz, Rixa; Vyas, Purvi


    Chapter 36 of Agenda 21, a key document of the 1992 Earth Summit, emphasised reorienting education towards sustainable development. While two of the Rio conventions, the Convention on Biological Diversity (CBD) and the United Nations Framework Convention on Climate Change (UNFCCC), developed communication, education and public awareness (CEPA)…

  12. Travel to the Rio Olympics


    Learn how to stay healthy and safe when travelling to the 2016 Olympic Games in Rio de Janeiro.  Created: 7/21/2016 by National Center for Emerging and Zoonotic Infectious Diseases (NCEZID).   Date Released: 7/21/2016.

  13. New species of Cetopsidium (Siluriformes: Cetopsidae: Cetopsinae from the upper rio Branco system in Guyana

    Richard P. Vari

    Full Text Available Cetopsidium soniae, new species, is described from the Takutu River basin of southwestern Guyana, within the upper portions of the rio Branco of the Amazon basin. The new species differs from its congeners in details of pigmentation, the length of the pelvic fin, the form of the first rays of the dorsal and pectoral fins in mature males, the relative alignment of the dorsal and ventral profiles of the postdorsal portion of the body, the position of the anus, and the depth of the body. DNA barcodes were generated for the holotype and paratype. An examination of other samples of Cetopsidium from the rio Branco system extends the range of C. pemon into the Ireng River system of Guyana.

  14. Seven new species of the killifish genus Rivulus (Cyprinodontiformes: Rivulidae) from the Paraná, Paraguay and upperAraguaia river basins, central Brazil

    Wilson J. E. M. Costa


    ...., from the rio Inhanduí drainage, rio Paraná basin, is diagnosed by a unique color pattern of the caudal fin in males and a reduced number of gill rakers on the first branchial arch; R. litteratus n. sp...

  15. Variabilidade do vento na bacia hidrográfi ca do rio São Francisco durante a ocorrência da ZCAS / Variability of the wind in the hidrographic basin of the São Francisco river during ZCAS occurrence

    Djane Fonseca da Silva


    Full Text Available O rio São Francisco é um dos rios brasileiros mais extensos e sua importância também está no volume de água transportado por ele através da região semi-árida, na sua contribuição histórica e econômica para fi xação das populações ribeirinhas e na criação das cidades hoje plantadas ao longo do vale. O principal mecanismo produtor de chuvas sobre a bacia do rio São Francisco é a Zona de Convergência do Atlântico Sul (ZCAS. A intensidade e direção do vento são variáveis de grande interesse nos estudos de balanço de água. Portanto, o presente trabalho tem como objetivo estudar a climatologia do vento e sua variabilidade na bacia do rio São Francisco. Foram utilizados dados mensais de ventos, componentes zonal e meridional, oriundos da Reanálise do NCEP/NCAR no período de 1982-1994, em três faixas de longitude (40ºW, 42,5ºW e 45ºW entre as latitudes de 25ºS e 5ºS. Observou-se que nas longitudes de 42,5ºW e 45ºW, a posição média da ZCAS está em torno de 20º S. Também foi observado que a posição da ZCAS apresenta uma grande variabilidade interanual, pois, de dezembro/1982 a fevereiro/1983 a ZCAS posicionou-se ao sul de 25ºS, enquanto no período de dezembro/1988 a fevereiro/1989 estava em torno de 15ºS. O posicionamento médio meridional da ZCAS em torno de 20º é de fundamental importância para produção de chuva sobre a bacia do rio São Francisco.

  16. Structural analysis of the Rio Pardo Group - southeast of Bahia state

    Marcos Egydio-Silva


    Full Text Available The Meso- to Neoproterozoic Rio Pardo Group is located in the southeastern region of the Bahia State and consistsof low-grade metasedimentary rocks deposited on Paleoproterozoic to Archean basement. From the base to the top, themetasedimentary rocks are grouped into the following sequences: Panelinha Formation consisting of coarse-grainedimmature clastics; the overlying Itaimbé Subgroup which is made up of the Camacã Formation (metapelites with localcarbonates, the Água Preta Formation (fi ne-grained metapsamites and local carbonate lenses, Serra do Paraíso Formation(metacarbonates and quartzites and the Santa Maria Eterna Formation (metaconglomerates and metacarbonates. TheSalobro Formation was deposited unconformably on this sequence and consists of coarse-grained immature and local fi negrainedclastic rocks. The Rio Pardo Group was affected by three successive folding events, which were recorded in twolitho-structural units. The litho-structural unit 1 is located in the northeastern part of the basin, and the litho-structural unit2, in the southwestern part of the basin. These units are separated by the Rio Pardo-Água Preta inverse fault, trending NWSEand dipping SW. The fi rst unit is autochthonous and monophasic and displays open folds and slaty cleavage, changinggradually towards southwest into large overturned folds with axial plane schistosity. The second unit is polyphasic andshows large folds with NE vergence. A third folding is represented by folds and foliations present at the western marginof the basin. The NE vergence of the Rio Pardo Group can be explained by changes in the deformation regime and in thedirection of the principal axis of deformation in the north sector of the Araçuaí belt during the Brasiliano collision orogen.The tectonic transport to the north could be the cause of deformation of the Rio Pardo Group.

  17. Assessing recent declines in Upper Rio Grande runoff efficiency from a paleoclimate perspective

    Lehner, Flavio; Wahl, Eugene R.; Wood, Andrew W.; Blatchford, Douglas B.; Llewellyn, Dagmar


    Recent decades have seen strong trends in hydroclimate over the American Southwest, with major river basins such as the Rio Grande exhibiting intermittent drought and declining runoff efficiencies. The extent to which these observed trends are exceptional has implications for current water management and seasonal streamflow forecasting practices. We present a new reconstruction of runoff ratio for the Upper Rio Grande basin back to 1571 C.E., which provides evidence that the declining trend in runoff ratio from the 1980s to present day is unprecedented in context of the last 445 years. Though runoff ratio is found to vary primarily in proportion to precipitation, the reconstructions suggest a secondary influence of temperature. In years of low precipitation, very low runoff ratios are made 2.5-3 times more likely by high temperatures. This temperature sensitivity appears to have strengthened in recent decades, implying future water management vulnerability should recent warming trends in the region continue.type="synopsis">type="main">Plain Language SummarySince the 1980s, major river basins in the American Southwest such as the Rio Grande have experienced droughts, declining streamflow, and increasing temperatures. More importantly, runoff ratio—the portion of precipitation that ends up in the river each year, rather than evaporating—has been decreasing as well. For water managers, it is important to know whether these trends are exceptional or are merely patterns that have occurred throughout history. We use long reconstructions of historical climate based on tree rings to estimate, for the first time, the paleo runoff ratio of the Upper Rio Grande. This new record indicates that the recently observed trends in runoff ratio are unprecedented in the 445 year record. Together with precipitation, high temperatures have an important influence, making very low runoff ratios 2.5-3 times more likely. These findings suggest that runoff ratio could decrease further if

  18. The BDS iGMAS RIOS station at Observatório Nacional, Rio de Janeiro

    Humberto Andrei, Alexandre; Song, Shuli; Junqueira, Selma; Beauvalet, Laurene


    GNSS navigation satellites are currently being developed by all major players in the science and technology scene, to compete with the GPS system. Because their applications span many different areas, from traffic and cargo control, to geodesy and seismic monitoring, it is required to assess the coherence between the different constellations. BDS is the GNSS system currently developed in China. Its first generation of satellites consisted of 3 geostationnary satellites allowing geolocalisation in China only. In addition to these satellites, other satellites have been launched in geostationnary and geosynchronous orbits, as well as satellites orbiting with a classical GNSS semi-major axis. With these additions, the BDS system possesses 19 operating satellites, and though the system is mostly efficient for geolocalisation in Asia, the satellites are also visible in other parts of the globe. In parallel to the development of the BDS constellation, China has launched the iGMAS (International GNSS Monitoring and Assessment Service) project to develop a global tracking network of multi-GNSS geodetic receivers. One of the goals of this project is to evaluate the efficiency of the BDS constellation as well as the efficiency of the receivers developed by the Chinese laboratories. As part of the Brazilian program COSBAN leaded by the Foreign Affairs Ministry to foster up the science and technology partnership with China, materialized by the collaboration between the Shanghai Astronomical Observatory/CAS and the Observatório Nacional/MCTI, in Rio de Janeiro. Through it the RIOS-iGMAS station was installed at Observatório Nacional, where the RJEP GNSS station already operates as part of the Brazilian reference system. Thus at the Observatório Nacional can be observed satellites from any constellation with both systems of reception, leading to a direct, efficient way to compare the results obtained for each network. In this communication we focus on the determination of the

  19. Two new species of Pseudancistrus (Siluriformes, Loricariidae) from the Amazon basin, northern Brazil.

    Silva, Gabriel S C; Roxo, Fábio F; Oliveira, Claudio


    Two new species of Pseudancistrus, a genus diagnosed by non-evertible cheek plates and hypertrophied odontodes along the snout margin, are described from two drainages of the Brazilian Shield: Pseudancistruskayabi from the rio Teles Pires (rio Tapajós basin) and Pseudancistrusasurini from the rio Xingu. The new species are distinguished from congeners (Pseudancistrusbarbatus, Pseudancistruscorantijniensis, Pseudancistrusdepressus, Pseudancistrusnigrescens, Pseudancistrusreus, and Pseudancistruszawadzkii) by the coloration pattern. Pseudancistruskayabi has dark bars on the dorsal and caudal fins which are similar to that of Pseudancistrusreus from the Caroní River, Venezuela. Pseudancistrusasurini is unique among Pseudancistrus in having whitish tips of the dorsal and caudal fins in juveniles to medium-sized adults.

  20. Basin-scale recharge in the Southwestern United States

    Hogan, J. F.; Duffy, C.; Eastoe, C.; Ferre, T. P. A.; Goodrich, D.; Hendrickx, J.; Hibbs, B.; Phillips, F.; Small, E.; Wilson, J.


    The major domestic water source in the arid southwestern United States is groundwater from alluvial basin aquifers. Accurate estimates of basin-scale groundwater recharge rates are a critical need for developing sustainable or "safe yield" groundwater pumping. Basin-scale recharge rates are typically estimated using inverse hydrologic modeling or geochemical tracers (e.g. chloride mass balance). These methods, while useful, have a high level of uncertainty and provide no information about the mechanisms of groundwater recharge. SAHRA - an NSF Science and Technology Center focused on the Sustainability of semi-Arid Hydrology and Riparian Areas - has developed an integrated research plan to address this problem. Our approach is two-fold. First we are investigating the "input" components that comprise basin-scale recharge: basin floor recharge, alluvial channel recharge, mountain front recharge, and mountain block recharge. Each component has unique spatial and temporal scales and thus requires distinct methods. Our research is aimed at understanding the factors (e.g. vegetation type, bedrock lithology, soil structure) that control recharge rates in each of these locations. With such an understanding one could then scale from point measurements to the basin-scale using remote sensing data. Our second approach is to employ isotopic tracers to determine water sources, groundwater ages and residence times of the groundwater and surface water "outputs"; these values can then be used to better calibrate recharge rates in groundwater models. By focusing our studies on two basins, the San Pedro River Basin in Arizona and the Rio Grande in New Mexico, we hope to develop a better understanding of the importance of different recharge pathways for basin-scale recharge and which methods are best suited for estimating basin-scale recharge.

  1. An evaluation eMergetics of Itacoatiara's city in the central Amazon, their plywood, and cultivated plain of basin of Madeira's river; Uma avaliacao eMergetica da cidade de Itacoatiara na Amazonia Central, sua industria de compensado e laminado e a varzea da bacia do rio Madeira

    Comar, Vito


    The plywood production system of Itacoatiara's industry and the wooden extraction impact of cultivated plain of basin of Madeira's river are presented. The incorporated energy flows - eMergy are evaluated by the models mathematical simulation, which applies to specific indices derivation aiming at the comparison with other similar processes. Itacoatiara's city was going analyzed regarding the industry load energetics and of others urban components.

  2. Rio Grande do Sul, Brasil

    Charlote Wink


    Full Text Available The occurrence of Cryptophlebia carpophagoides Clarke, 1951, (Lepidoptera: Olethreutidae, in fruit of Enterolobium contortisiliquum (Vell. Morong, has bun first registered in the state of Rio Grande do Sul, Brazil. The damaged fruit was collected in the campus of National University of Santa Maria, Santa Maria, from May to June of 2003 and 2004. It was evidenced that the caterpillars damage the fruit of that specie affecting the integrety, the vigor and the germination of the seeds.


    Emmaneul Carneiro Leão


    Full Text Available ResumoQual a mútua referência existente entre homeme terceira margem? Pode-se tentar apontá-la no trabalho, no pensamento, na fi losofi a,ou, ainda no mistério, que engloba as três dimensõesanteriores. Assim, torna-se necessáriose perguntar pela identidade do mistérioe como esse se faz presente no trabalho, nafi losofi a e no pensamentoPalavras-chave: Terceira margem; mistério; fi losofi a; pensamento; verdade.AbstractWhat is the mutual reference between manand the third bank? One might try to outlineit in the spheres of work, thought, philosophyor even in mystery, which comprehendsthe previous spheres. As a result, one must fi -nally think about the identity of mystery itselfand how it relates to work, philosophy andthought.Keywords: Th ird bank; mystery; philosophy; thought; truth.Emmanuel Carneiro Leão Filósofo, ensaísta e tradutor, autor do livroAprendendo a pensar, entre outros. Ex-aluno de Martin Heideggerna Universidade de Freiburg, é hoje um de seus principais tradutoresbrasileiros. Atualmente é Professor Emérito da Universidade Federal doRio de Janeiro.

  4. Application of nonlinear-regression methods to a ground-water flow model of the Albuquerque Basin, New Mexico

    Tiedeman, C.R.; Kernodle, J.M.; McAda, D.P.


    This report documents the application of nonlinear-regression methods to a numerical model of ground-water flow in the Albuquerque Basin, New Mexico. In the Albuquerque Basin, ground water is the primary source for most water uses. Ground-water withdrawal has steadily increased since the 1940's, resulting in large declines in water levels in the Albuquerque area. A ground-water flow model was developed in 1994 and revised and updated in 1995 for the purpose of managing basin ground- water resources. In the work presented here, nonlinear-regression methods were applied to a modified version of the previous flow model. Goals of this work were to use regression methods to calibrate the model with each of six different configurations of the basin subsurface and to assess and compare optimal parameter estimates, model fit, and model error among the resulting calibrations. The Albuquerque Basin is one in a series of north trending structural basins within the Rio Grande Rift, a region of Cenozoic crustal extension. Mountains, uplifts, and fault zones bound the basin, and rock units within the basin include pre-Santa Fe Group deposits, Tertiary Santa Fe Group basin fill, and post-Santa Fe Group volcanics and sediments. The Santa Fe Group is greater than 14,000 feet (ft) thick in the central part of the basin. During deposition of the Santa Fe Group, crustal extension resulted in development of north trending normal faults with vertical displacements of as much as 30,000 ft. Ground-water flow in the Albuquerque Basin occurs primarily in the Santa Fe Group and post-Santa Fe Group deposits. Water flows between the ground-water system and surface-water bodies in the inner valley of the basin, where the Rio Grande, a network of interconnected canals and drains, and Cochiti Reservoir are located. Recharge to the ground-water flow system occurs as infiltration of precipitation along mountain fronts and infiltration of stream water along tributaries to the Rio Grande; subsurface

  5. Evaluation of the impact of farming activity in the water quality in surface catchment areas in hydrographic basin from Mogi-Guacu and Pardo Rivers, Sao Paulo; Avaliacao do impacto da atividade agropecuaria na qualidade da agua em areas de captacao superficial nas bacias hidrograficas dos Rios Mogi-Guacu e Pardo, Sao Paulo

    Katsuoka, Lidia


    This study was performed in 10 small basins located in the Mogi-Guacu and Pardo Rivers, in the Northeastern area of Sao Paulo State. The land belonging of these basins is used to grow row crops of potato, coffee and pasture areas. This study aimed to characterize small basins, to evaluate water and sediment quality and to correlate basic aspects of climatology, hydrology, toxicology and land uses to the physical, chemical and toxicological characteristics of the water in the streams. Geographic Information System (GIS) was used as a tool of evaluation of land uses and risk assessment was performed for a final evaluation. The samplings were carried out from June/1999 to June/2000 in the 13 collecting points. It was verified that water quality is dependent upon the rainy and dry periods and the harvest periods. In the beginning of rainy periods were found large concentrations of metals and traces of herbicides leachate from soil and, in the dry period the same event was verified, caused by concentration of the water. In August, September and October phosphorus concentrations were very low getting an improvement in the water quality. Al, Fe and Mn are majority elements of chemical compositions of rocks of the study area, and exceed the Brazilian Guidelines. The stream waters were classified as 44% oligotrophic, 42% mesotrophic and 14% eutrophic. Jaguari-Mirim River presented the largest values of Trophic Index (TI). Sediment analyses showed a great variety of organic compounds coming from anthropogenic activities (industrial and farming activity). Toxicity tests with hyalella azteca in the sediments presented toxicity for sediments from Sao Joao da Boa Vista and Divinolandia. A methodology was developed for organochlorinated pesticides by gas chromatography coupled to mass spectrometry (GCMS). The presence of organochlorinated pesticides was not verified. (author)


    Constança Marcondes Cesar


    Full Text Available O papel da imaginação na vida social é estudado por Ricoeur no âmbito de uma teoria geral da imaginação. Em sua filosofia, a ideologia e a utopia são focalizadas como duas expressões do imaginário social. Examinaremos, primeiro, o papel da imaginação, em seguida focalizaremos a questão da utopia e, finalmente, as relações entre ética e utopia.

  7. Electromagnetically Inferred Structure of the Caja del Rio Plateau, New Mexico

    Layton, M. E.; Speed, C.; Shukla, M.; Vila, A.; Chon, E.; Kitamikado, C.; Feucht, D. W.; Bedrosian, P.; Pellerin, L.


    Magnetotelluric (MT) and transient electromagnetic (TEM) data were acquired by students from the Summer of Applied Geophysical Experience (SAGE) to construct structural models in and around the Caja del Rio Plateau, New Mexico. The Caja del Rio is located on the La Bajada-Jemez constriction that separates the Española and Santa Domingo basins in the Rio Grande Rift. The Rio Grande Rift, the result of tectonic extensional forces, extends approximately north-south across northern New Mexico. MT data collected in 2016 were merged with that from previous years to make up an 11 km north line and a 16 km south line extending from the west side of the Caja Del Rio to the east off the plateau in the Old Buckman Road area. The resistivity distributions revealed in one-dimensional (1-D) and two-dimensional (2-D) inverse models show some robust features. Models of the north are interpreted as a top resistive layer (Cerros del Rio volcanic field, which, in turn, allow for the thickness of these basaltic and andesitic deposits to be mapped across the plateau. One-dimensional inverse models produced from the TEM data were aligned and interpreted geologically. A resistive ( 1000 ohm-m) unit, interpreted to represent the Cerros del Rio volcanics, thickens from 70m to 175m from southeast to northwest. The volcanics are overlain by a thin conductor, interpreted as weathered material. The resistive body is underlain by a thicker conductor, interpreted as sedimentary rocks of the Tertiary-aged Santa Fe Group.

  8. Social, political, and institutional setting: Water management problems of the Rio Grande

    Douglas, A.J.


    This paper discusses various water management issues facing federal, state, and local agencies charged with managing the water resources of the Rio Grande River Basin and its major tributaries. The Rio Grande - 3,058 km (=1,900 mi) long - is the fourth longest river in the United States. The river's basin is 870,236 km2 (=336,000 mi2) and for roughly two-thirds of its length it forms the United States-Mexican border. It is a major recreational resource providing world class trout fishing near its headwaters in Colorado's San Juan Mountains and shoreline, angling, and boating opportunities near the Colorado-New Mexico border. The Rio Grande is the principal tourist attraction of Big Bend National Park and flows through downtown Albuquerque and El Paso. Many reaches are wide and broad, but almost all are relatively shallow and not navigable by commercial ships. Nevertheless, it is one of the most important renewable water resources of the southwestern United States and North America. The issue of the "manageability" of the river in the face of social forces and disparate administrative jurisdictions that adversely impact Rio Grande flows is a thread linking various sections of the paper together. The length of the river; the fact that major reaches lie in Colorado, New Mexico, and Texas; and its unique role as an international boundary pose complex management problems. The allocation status quo formed by the complex nexus of existing river laws make it difficult to reshape Rio Grande management. ?? 2009 ASCE.

  9. Análise fitossociológica de um remanescente de vegetação na microbacia do Córrego Criminoso (Bacia do Rio Taquari, Coxim, MS, Brasil: subsídios para a recomposição da vegetação Phytosociological analysis of a vegetation remnant in the Córrego Criminoso Basin (Taquari River Basin, Coxim District, Mato Grosso do Sul, Brazil: data for vegetation recovery studies

    Adriana Maria Güntzel


    Full Text Available O objetivo deste estudo foi realizar a análise florística e fitossociológica preliminar em um remanescente de vegetação na área de entorno do Córrego Criminoso, visando subsidiar futuros projetos de recomposição da vegetação. A área total do remanescente foi determinada com o auxílio de GPS e dos programas Pathfinder e Autocad. Amostragens de indivíduos com CAP maior ou igual a 20 cm foram realizadas em 20 parcelas de 300 m² distribuídas na área. Foram encontradas 26 famílias botânicas contendo 36 gêneros e 49 espécies. A família Leguminosae foi a mais rica em espécies, seguida da família Annonaceae. A espécie Xylopia aromatica foi a mais freqüente, apresentando valores de IVI e IVC de 99,77 e 85,73, respectivamente. Observou-se que mais de 50% das espécies presentes na área são pioneiras ou secundárias, sendo cinco consideradas típicas de matas ciliares: Tapirira guianenses, Cecropia pachystachya, Terminalia argentea, Ocotea pulchellae e Luehea grandiflora. O remanescente de vegetação do entorno do Córrego Criminoso encontra-se fortemente degradado, necessitando de ações de manejo específicos nos fragmentos vegetados e nas áreas destituídas de vegetação, cujas recomendações são propostas.The aim of this study was to complete a preliminary, floristic, phytosociological analyses of a vegetation remnant in the Criminoso Stream Basin, in order to provide data for future projects focusing on vegetation recovery. The total area of the remnant was determined using a GPS and the software Pathfinder and Autocad. Samples of individuals larger or equal to 20 cm CBH were made in 20 quadrats that were 300 m². Thirty-six genera and 49 species, within 26 botanical families, were found. The family Leguminosae was the richest in species, followed by the Annonaceae. Xylopia aromatica was the most frequent species, presenting values of IVI and IVC of 99.77 and 85.73, respectively. More than 50% of the species present

  10. O batistério publicitário

    Nelly Carvalho


    Full Text Available

    O presente trabalho descreve o papel do léxico nos meios de comunicação, evidenciando a elaboração da mensagem publicitária. A necessidade de brevidade e clareza determina a escolha lexical, responsável pela informação e convencimento do receptor. Para nomear e qualificar o produto são utilizados substantivos, adjetivos e verbos por meio dos processos de formação de palavras, relações semânticas e recursos estilísticos. Os traços culturais também estão presentes no uso do vocabulário.

  11. Water Management for Competing Uses: Environmental Flows in the Transboundary Rio Grande/Rio Bravo

    Sandoval Solis, S.; McKinney, D. C.


    Introduction Due to high water demand, the scarcity of water, and the complexity of water allocation, environmental flows have not been considered as an integral part of the water management in the Rio Grande/Rio Bravo transboundary basin. The Big Bend reach is located between the cities of Presidio/Ojinaga to Amistad international reservoir, along the main stream (Fig. 1). Important environmental habitats such as the Big Bend National and State Park in the U.S., the Maderas del Carmen, Cañon de Santa Elena and Ocampo natural reserved areas in Mexico are ecologically threatened because of the lack of environmental water management policies. Several efforts have been undertaken by scientists, government agencies and NGOs to determine the environmental flows for this reach and water management policies that can provide these flows. Objective The objective of this research is to describe a water management policy that can conciliate environmental and human water uses in the Big Bend region. In other words, define a policy that can provide environmental flows without harming water supply for stakeholders or increasing flood risk, within legal and physical constraints of the system. Methodology First, the system was characterized identifying water users, hydraulic infrastructure, and water allocation according to state, federal and international regulations. Second, a hydrograph for environmental flows was proposed that mimics the hydrologic characteristics of the prior dam alteration. Third, a water planning model was constructed to evaluate alternative policies. Fourth, the water management is proposed to provide environmental restoration flows from Luis L. Leon reservoir. This policy considers mechanisms that reduce flooding and drought risks, while meting national and international water regulations. Results Three types of natural flow regimes are considered: (1) median flows aimed to provide the base flow in the region, (2) high flows to provide transversal

  12. Quantificação de fluxos de mercúrio gasoso na interface solo/atmosfera utilizando câmara de fluxo dinâmica: aplicação na bacia do Rio Negro Quantification of atmosphere - soil mercury fluxes by using a dynamic flux chamber: application at the Negro River basin, Amazon

    Gabriella Magarelli


    Full Text Available Gaseous mercury sampling conditions were optimized and a dynamic flux chamber was used to measure the air/surface exchange of mercury in some areas of the Negro river basin with different vegetal coverings. At the two forest sites (flooding and non-flooding, low mercury fluxes were observed: maximum of 3 pmol m-2 h-1 - day and minimum of -1 pmol m-2 h-1 - night. At the deforested site, the mercury fluxes were higher and always positive: maximum of 26 pmol m-2 h-1 - day and 17 pmol m-2 h-1 - night. Our results showed that deforestation could be responsible for significantly increasing soil Hg emissions, mainly because of the high soil temperatures reached at deforested sites.

  13. Reservoirs of the basin of Majaceite river (Hurones and Guadalcacin) in Cadiz; water quality and their influence with the drought; Influencia de la sequia en la calidad de las aguas de los embalses (Hurones y Guadalcacin) en la cuencia del rio Majaceite de la provincia de Cadiz

    Rodriguez Barroso, M. R.; Vidal Valderas, L.; Sales Marquez, D.; Quiroga Alonso, J. M.


    In this work the results of the limnological study of the two reservoirs of the basin of Majaceite river is presented: Guadalcacin and Hurones. These reservoirs are part of the hydrography net of the county of Cadiz (south of Spain) and it belongs to the Guadalquivir Hydrography Confederation. The study of physical chemical parameters, together with the data of the climate variations have allowed to know the quality of the dammed water, as well as, to predict certain behaviour rules in the adaptation of the water, in the drinking waters treatment plant for their final destination as water of supply. The results obtained in this study allow to conclude that the waters quality of the reservoirs of Hurones are biggest than the reservoir of Guadalcin makes then more appropriate for the public supply because present smaller saline content. (Author) 18 refs.

  14. A dinâmica atmosférica na vertente oriental da bacia do alto rio Paraná e a gênese das chuvas = The atmospheric dynamics on the eastern slope of the Paraná river basin and the genesis of rain

    Victor da Assunção Borsato


    Full Text Available O ritmo dos sistemas atmosféricos e a intensidade variam no tempo e noespaço. Por isso, para caracterizar a dinâmica climática de uma região é necessário estudar a dinâmica das massas de ar ao longo de uma série. Estudaram-se, por meio da dinâmica das massas de ar, a participação dos sistemas atmosféricos atuantes e as porcentagens das chuvas convectivas e frontais ao longo da vertente oriental da bacia do alto rio Paran��. Verificou-se que, nessa vertente, nos meses mais frios, predomina a atuação da massa tropical Atlântica e da polar Atlântica. Nos meses mais quentes, além de predominar a atuação dos sistemas de baixa pressão equatorial continental e tropical continental, têm-se as chuvas convectivas. Verificou-se, também, progressivo aumento na participação das chuvas convectivas, a partirda década de 1990, corroborando a teoria das mudanças climáticas.The rhythm and intensity of atmospheric systems vary intime and space. Therefore, it is necessary to study the dynamics of air masses over a temporal series in order to characterize the climate dynamics of a region or area. The participation of the active atmospheric systems and the percentage shared by convective andfrontal rains along the eastern slope of upper Paraná River were studied based on the dynamics of air masses. It was observed that, in such a slope, during the coldest months, the actions of the Atlantic tropical mass and polar Atlantic mass prevail. However, during thewarmer months, in addition to the predominance of the action of equatorial continental and tropical continental low atmospheric pressure systems, convective rains also take place. It was also noted that, from the 1990s onward, a progressive increase was observed in the participation of convective rains, strengthening the theory of climatic change.

  15. Climate Change Impacts in the Upper Rio Grande Catchment

    Heikkila, T.; Siegfried, T. U.; Sellars, S. L.; Schlager, E.


    In the US Southwest, evidence of increased future drought severity and duration in the context of climate change has been detected. Considering the already difficult water distribution and allocation strategies within the region, we are investigating the Costilla Creek, a tributary to the Rio Grande. The catchment is located in Costilla county in Colorado from where on runoff is crossing boundaries between Colorado and New Mexico three times before its confluence with the Rio Grande in New Mexico. Water allocation is governed by an interstate compact between Colorado and New Mexico. While the states have been relatively successful in complying with the compact’s allocation rules, the Costilla Creek catchment has experienced interstate upstream/downstream conflict, mainly during irrigation seasons. Whether or not the states will be able to avert conflict in the future and maintain compliance with the compact, is a critical question. The situation in the relatively small catchment is not unique. Various interstate watersheds, including the entire Rio Grande basin, the La Plata, Arkansas, and Colorado, are expected to face similar impacts from climate change, yet the water compacts that govern them may not be structured to adapt to these conditions. Looking at the Costilla Creek offers a valuable starting point for understanding how to model these effects across various basins. We have developed a lumped-parameter rainfall-runoff model including snow storage of the Costilla Creek watershed. Temperature and precipitation data from NCRS - SNOTEL stations together with USGS gauging station data were utilized for model calibration and validation. ISCCP solar radiation data and temperature data were used to estimate irrigation water demand in irrigated agriculture. The model is driven by the IPCC SRES A2 scenario. GCM ensemble averaged temperature / precipitation trends were extracted for the upper Rio Grande region. 50 year precipitation simulations were created using a

  16. Rio 2016 golf Olympic course: technical brief


    Through the RFP, Rio 2016™ seeks to identify the best concept design for the Olympic golf course, for both women’s and men’s competition at the Rio 2016™ Olympic Games as well as the best legacy solution for the future.

  17. Emissões naturais e antrópicas de nitrogênio, fósforo e metais para a bacia do Rio Macaé (Macaé, RJ, Brasil sob influência das atividades de exploração de petroleo e gás na Bacia de Campos Natural and anthropogenic emissions of nitrogen, phosphorous and metals into the Macaé river basin (Macaé, RJ, Brazil Influenced by oil and gas exploration in Campos Basin

    Mauricio Mussi Molisani


    Full Text Available Emission factors of natural processes and anthropogenic activities were used to estimate nutrients and metal loads for the lower Macaé river basin, which hosts the operational base for the offshore oil and gas exploration in the Campos Basin. The estimates indicated that emissions from anthropogenic activities are higher than natural emissions. Major contributing drivers include husbandry and urbanization, whose effluents receive no treatment. The increasing offshore oil exploration along the Brazilian littoral has resulted in rapid urbanization and, therefore might increase the inshore emission of anthropogenic chemicals in cases where effective residue control measures are not implemented in fluvial basins of the region.

  18. Reserves in western basins

    Caldwell, R.H.; Cotton, B.W. [Scotia Group, Dallas, TX (United States)


    The objective of this project is to investigate the reserves potential of tight gas reservoirs in three Rocky Mountain basins: the Greater Green River (GGRB), Uinta and Piceance basins. The basins contain vast gas resources that have been estimated in the thousands of Tcf hosted in low permeability clastic reservoirs. This study documents the productive characteristics of these tight reservoirs, requantifies gas in place resources, and characterizes the reserves potential of each basin. The purpose of this work is to promote understanding of the resource and to encourage its exploitation by private industry. At this point in time, the GGRB work has been completed and a final report published. Work is well underway in the Uinta and Piceance basins which are being handled concurrently, with reports on these basins being scheduled for the middle of this year. Since the GGRB portion of the project has been completed, this presentation win focus upon that basin. A key conclusion of this study was the subdivision of the resource, based upon economic and technological considerations, into groupings that have distinct properties with regard to potential for future producibility, economics and risk profile.

  19. Seepage investigation of the Rio Grande from below Leasburg Dam, Leasburg, New Mexico, to above American Dam, El Paso, Texas, 2015

    Briody, Alyse C.; Robertson, Andrew J.; Thomas, Nicole


    Seepage investigations have been conducted annually by the U.S. Geological Survey from 1988 to 1998 and from 2004 to the present (2015) along a 64-mile reach of the Rio Grande from below Leasburg Dam, Leasburg, New Mexico, to above American Dam, El Paso, Texas, as part of the Mesilla Basin monitoring program. Results of the investigation conducted in 2015 are presented in this report. The 2015 seepage investigation was conducted on February 10, 2015, during the low-flow conditions of the non-irrigation season. During the 2015 investigation, discharge was measured at 23 sites along the main-stem Rio Grande and 19 inflow sites within the study reach. Because of extended drought conditions affecting the basin, many sites along the Rio Grande (17 main-stem and 10 inflow) were observed to be dry in February 2015.

  20. Water resources data Texas water year 2001, volume 5. Guadalupe River basin, Nueces River basin, Rio Grande basin, and intervening coastal basins

    Gandara, Susan C.


    Water-resources data for the 2001 water year for Texas are presented in six volumes, and consist of records of stage, discharge, and water quality of streams and canals; stage, contents, and water-quality of lakes and reservoirs; and water levels and water quality of ground-water wells. Volume 5 contains records for water discharge at 77 gaging stations; stage only at 4 gaging stations; stage and contents at 5 lakes and reservoirs; water quality at 27 gaging stations; and data for 23 partial-record stations comprised of 3 flood-hydrograph, 8 low-flow, 4 crest-stage, and 3 miscellaneous stations. Also included are lists of discontinued surface-water discharge or stage-only stations and discontinued surface-water-quality stations. Additional water data were collected at various sites, not part of the systematic data-collection program, and are published as miscellaneous measurements. These data represent that part of the National Water Data System operated by the U.S. Geological Survey and cooperating Federal, State, and local agencies in Texas. Records for a few pertinent stations in the bordering States also are included.

  1. Water resources data Texas water year 2003, volume 5. Guadalupe River basin, Nueces River basin, Rio Grande basin, and intervening coastal basins

    Gandara, Susan C.


    Water-resources data for the 2003 water year for Texas are presented in six volumes, and consist of records of stage, discharge, and water quality of streams and canals; stage, contents, and water-quality of lakes and reservoirs; and water levels and water quality of ground-water wells. Volume 5 contains records for water discharge at 84 gaging stations; stage only at 6 gaging stations; stage and contents at 6 lakes and reservoirs; water quality at 28 gaging stations; and data for 18 partial-record stations comprised of 1 flood-hydrograph, 10 low-flow, 4 crest-stage, and 3 miscellaneous stations. Also included are lists of discontinued surface-water discharge or stage-only stations and discontinued surface-water-quality stations. Additional water data were collected at various sites, not part of the systematic data-collection program, and are published as miscellaneous measurements. These data represent that part of the National Water Data System operated by the U.S. Geological Survey and cooperating Federal, State, and local agencies in Texas. Records for a few pertinent stations in the bordering States also are included.

  2. Water resources data Texas water year 1999, volume 5. Guadalupe River basin, Nueces River basin, Rio Grande basin, and intervening coastal basins

    Gandara, S.C.; Gibbons, W.J.; Barbie, D.L.; Jones, R.E.


    Water-resources data for the 1999 water year for Texas are presented in six volumes, and consist of records of stage, discharge, and water quality of streams and canals; stage, contents, and water-quality of lakes and reservoirs; and water levels and water quality of ground-water wells. Volume 5 contains records for water discharge at 76 gaging stations; stage only at 1 gaging stations; stage and contents at 4 lakes and reservoirs; water quality at 38 gaging stations; and data for 30 partial-record stations comprised of 3 flood-hydrograph, 14 low-flow, and 8 crest-stage, and 5 miscellaneous stations. Also included are lists of discontinued surface-water discharge or stage-only stations and discontinued surface-water-quality stations. Additional water data were collected at various sites, not part of the systematic data-collection program, and are published as miscellaneous measurements. These data represent that part of the National Water Data System operated by the U.S. Geological Survey and cooperating Federal, State, and local agencies in Texas. Records for a few pertinent stations in the bordering States also are included.

  3. Water resources data Texas water year 2002, volume 5. Guadalupe River basin, Nueces River basin, Rio Grande basin, and intervening coastal basins

    Gandara, Susan C.


    Water-resources data for the 2002 water year for Texas are presented in six volumes and consist of records of stage, discharge, and water quality of streams and canals; stage, contents, and water quality of lakes and reservoirs; and water levels and water quality of ground-water wells. Volume 5 contains records for water discharge at 82 gaging stations; stage only at 6 gaging stations; stage and contents at 8 lakes and reservoirs; water quality at 25 gaging stations; and data for 30 partial-record stations comprised of 2 flood-hydrograph, 6 low-flow, 4 crest-stage, and 18 miscellaneous stations. Also included are lists of discontinued surface-water discharge or stage-only stations and discontinued surface-water-quality stations. Additional water data were collected at various sites, not part of the systematic data-collection program, and are published as miscellaneous measurements. These data represent that part of the National Water Data System operated by the U.S. Geological Survey and cooperating Federal, State, and local agencies in Texas. Records for a few pertinent stations in the bordering States also are included.

  4. Water resources data Texas water year 2000, volume 5. Guadalupe River basin, Nueces River basin, Rio Grande basin, and intervening coastal basins

    Gandara, S.C.; Gibbons, W.J.; Barbie, D.L.


    Water-resources data for the 2000 water year for Texas are presented in six volumes, and consist of records of stage, discharge, and water quality of streams and canals; stage, contents, and water-quality of lakes and reservoirs; and water levels and water quality of ground-water wells. Volume 5 contains records for water discharge at 71 gaging stations; stage only at 4 gaging stations; stage and contents at 4 lakes and reservoirs; water quality at 29 gaging stations; and data for 23 partial-record stations comprised of 3 flood-hydrograph, 10 low-flow, 6 crest-stage, and 4 miscellaneous stations. Also included are lists of discontinued surface-water discharge or stage-only stations and discontinued surface-water-quality stations. Additional water data were collected at various sites, not part of the systematic data-collection program, and are published as miscellaneous measurements. These data represent that part of the National Water Data System operated by the U.S. Geological Survey and cooperating Federal, State, and local agencies in Texas. Records for a few pertinent stations in the bordering States also are included.

  5. Water resources data Texas, water year 2004, volume 5. Guadalupe River basin, Nueces River basin, Rio Grande basin, and intervening coastal basins

    Long, Susan C. Aragon; Reece, Brian D.; Eames, Deanna R.


    Water-resources data for the 2004 water year for Texas are presented in six volumes, and consist of records of stage, discharge, and water quality of streams and canals; stage, contents, and water-quality of lakes and reservoirs; and water levels and water quality of ground-water wells. Volume 5 contains records for water discharge at 86 gaging stations; stage only at 5 gaging stations; elevation at 3 lakes and reservoirs; content at 4 lakes and reservoirs;and water quality at 24 gaging stations. Also included are data for 16 partial-record stations comprised of 1 flood-hydrograph, 11 low-flow, and 4 crest-stage stations. Also included are lists of discontinued surface-water discharge or stage-only stations and discontinued surface-water-quality stations. Additional water data were collected at various sites, not part of the systematic data-collection program, and are published as miscellaneous measurements. These data represent that part of the National Water Data System operated by the U.S. Geological Survey and cooperating Federal, State, and local agencies in Texas. Records for a few pertinent stations in the bordering States also are included.

  6. Estudo etnobotânico na comunidade de Conceição-Açu (alto da bacia do rio Aricá Açu, MT, Brasil Ethnobotany study in community of Conceição-Açu (on the upper basin of the River Aricá Açu, MT, Brazil

    Maria Corette Pasa


    Full Text Available O presente trabalho tem como objetivo realizar o levantamento etnobotânico de plantas classificadas em diferentes categorias de uso na comunidade de Conceição-Açu, no município de Cuiabá, MT, Brasil e estimar o valor de uso das espécies botânicas em matas de galeria. Entrevistas estruturadas e semi-estruturadas, o uso do questionário foram aplicados em 59 residentes adultos de ambos os sexos. Identificou-se as unidades de paisagem: quintais, roças e matas de galeria e o número total de espécies utilizadas foi de 180. A maioria das plantas foi coletada durante a entrevista e depositadas no Herbário da UFMT. Nos quintais das residências identificou-se 86 espécies, pertencentes a 43 famílias, a maioria cultivada e utilizada como alimento (48,1% e como remédio (44,5%. Nas roças os principais cultivos são: Manihot esculenta L. (100%, Carica papaya L. (76,2%, Musa paradisiaca L. (71,4%, Saccharum officinarum L. (57,1%. Na mata de galeria destacou-se a categoria medicinal (65%, com as espécies: Copaifera langsdorffii Desf. (2,5, Aspidosperma polyneuron Muell. Arg. (2,5, Hymenaea stignocarpa Mart. (2,33, Diptychandra aurantiaca Tul. (2,0, Cariniana rubra Gardner ex. Miers (20 e as famílias botânicas Mimosaceae, Bignoniaceae, Caesalpiniaceae, Fabaceae e Sapindaceae. Os resultados demonstram que a população possui vasto conhecimento das plantas e de suas propriedades de cura.This paper aims at doing the ethnobotany survey of plants classified in different categories of use in the community of Conceição-Açu, in the city of Cuiabá, MT, Brazil and estimate the value of use of the species botanic in the gallery forest. Structured and non-structured interviews and the questionnaire were used in 59 adult dwellers of both sexes. Were identified the landscape units: backyards, husbandry and gallery forest and the total number of used species is the 180. The majority of the plants was collected during the interview and is kept in the

  7. Reservoirs of the basin of Guadalete river (Zahara. El Gastor, Bornos and Arcos) in Cadiz; waters quality and their influence with the drought; Embalses de la cuencia del rio Guadalete (Zahara-El Gastor, Bornos y Arcos) de la provincia de Cadiz: calidad de las aguas y su influencia con la sequia

    Rodriguez Barroso, M. R.; Vidal Valderas, L.; Sales Marquez, D.; Quiroga Alonso, J. M.


    In this work the results of the limnological study of the reservoirs of the basin of Guadalete river is presented: Zahara-El Gastor, Bonos and Arcos. These reservoirs are part of the hydrography net of the county of Cadiz (south of Spain) and it belongs to the Guadalquivir Hydrography Confederation. The study of physical chemical parameters, together with the data of the climate variations have allowed to know the quality of the dammed water, as well as, to predict certain behaviour rules in the adaptation of the water, in the drinking waters treatment plant for their final destination ad water of supply. The results obtained show a similarity of the waters quality of the reservoirs of Bornos and Arcos, and different to the reservoirs of Zahara-El Gastor because are more saline content. It is showed a progressive decrees of the waters quality dammed during the drought period (1992-1995). In 1995 the water levels was alarmingly lowest. (Author) 19 refs.

  8. Mitigation : Closed Basin Project

    US Fish and Wildlife Service, Department of the Interior — The upcoming meeting on waterfowl mitigation for the Closed Basin Project will have several people talk about possible changes to the waterfowl mitigation program. A...

  9. Tulare Basin protection plan

    US Fish and Wildlife Service, Department of the Interior — The Tulare Basin Protection Plan has been initiated by The Nature Conservancy to elucidate the problems and opportunities of natural diversity protection....

  10. BASINS Framework and Features

    BASINS enables users to efficiently access nationwide environmental databases and local user-specified datasets, apply assessment and planning tools, and run a variety of proven nonpoint loading and water quality models within a single GIS format.

  11. California Air Basins

    California Department of Resources — Air ResourcesCalifornia Air Resources BoardThe following datasets are from the California Air Resources Board: * arb_california_airbasins - California Air BasinsThe...

  12. Watershed Planning Basins

    Vermont Center for Geographic Information — The Watershed Planning Basin layer is part of a larger dataset contains administrative boundaries for Vermont's Agency of Natural Resources. The dataset includes...

  13. Blog literário: alguns comentários

    Alamir Aquino Corrêa


    Full Text Available Se o conceito de literatura é marcado por discussões e reformulações ao longo da história, parece-nos importante partir da ideia que “as escritas de si” presentes na pós-modernidade apontam para a revisão de algumas noções a respeito do ficcional e da literariedade presentes em textos que são veiculados na internet, especificamente o blog. A escrita de autoria feminina, tradicional espaço de expressão subjetiva recolhida muitas vezes apenas em diários íntimos, encontrou na internet um meio para fazer ecoar vozes antes silenciadas devido à condição da mulher na sociedade e, portanto, também terá destaque dentre os assuntos aqui discutidos, ao lado de reflexões sobre a canonicidade de textos e da configuração do blog como espaço de autorreferencialidade e de publicidade da escrita literária.

  14. Water-quality trends in the Rio Grande/Rio Bravo Basin using sediment cores from reservoirs

    Van Metre, Peter C.; Mahler, B.J.; Callender, Edward C.


    Water-quality trends reflect the relation between water quality and human activities, chronicling changes in concentrations of environmental contaminants, introduction of new contaminants, and successful efforts in environmental pollution remediation. Historical data available for analyzing trends often have severe limitations, from questionable accuracy to unknown sampling and analytic methodologies. Where data are unavailable or have such limitations, water-quality trends sometimes can be reconstructed using sediment cores from lakes and reservoirs.

  15. K Basin Hazard Analysis

    PECH, S.H.


    This report describes the methodology used in conducting the K Basins Hazard Analysis, which provides the foundation for the K Basins Final Safety Analysis Report. This hazard analysis was performed in accordance with guidance provided by DOE-STD-3009-94, Preparation Guide for U. S. Department of Energy Nonreactor Nuclear Facility Safety Analysis Reports and implements the requirements of DOE Order 5480.23, Nuclear Safety Analysis Report.

  16. K Basins Hazard Analysis

    WEBB, R.H.


    This report describes the methodology used in conducting the K Basins Hazard Analysis, which provides the foundation for the K Basins Safety Analysis Report (HNF-SD-WM-SAR-062, Rev.4). This hazard analysis was performed in accordance with guidance provided by DOE-STD-3009-94, Preparation Guide for U. S. Department of Energy Nonreactor Nuclear Facility Safety Analysis Reports and implements the requirements of DOE Order 5480.23, Nuclear Safety Analysis Report.

  17. Irmã de índio, mulher de branco: perspectivas femininas no alto rio Negro

    Cristiane Lasmar


    Full Text Available A posição "deslocada" das mulheres é um traço constitutivo da experiência social feminina no alto rio Negro, em contraste com a masculina, esta fortemente centrada na noção de "pertencimento". Tomando isso por pressuposto, realiza-se, neste artigo, uma reflexão sobre a experiência social das mulheres indígenas que residem na cidade de São Gabriel da Cachoeira, principal pólo urbano da bacia do alto rio Negro. Com base em análise etnográfica, discute-se o modo como os casamentos com brancos na cidade contribuem para o processo de transformação da experiência social feminina.The "displaced" position of women is a constitutive feature of female social experience in the Upper Rio Negro, in contrast to the male position which is centred on the notion of "belonging". Starting from this premise, the article reflects on the social experience of Indigenous women who live in the city of São Gabriel da Cachoeira, the principal urban centre in the Upper Rio Negro basin. Through ethnographic analysis, it explores how marriages with white men in the city contribute to the process of transforming female social experience.

  18. Laimosemion leticia (Teleostei: Cyprinodontiformes: Rivulidae), a new species from the upper Rio Amazonas, Southern Colombia.

    Valdesalici, Stefano


    Laimosemion leticia is described from the Rio Tacana drainage, upper Rio Amazonas basin, Southern Colombia. The new species was found in a shallow swamp within a tropical rainforest in the vicinity of Leticia, capital of the department of Amazonas and southernmost municipality of Colombia. This miniature species is considered to be a member of the Owiyeye subgenus, which is diagnosed by a unique frontal squamation. Laimosemion leticia can be distinguished from all other species of the genus by the unique colour pattern on the unpaired fins. The new species appears related to L. jauaperi, L. uatuman and L. ubim due to the similar flank colour pattern in males, but is easy distinguished by coloration of the unpaired fins and morphological characters.

  19. The Aquitaine basin

    Biteau, J.-J.; Le Marrec, A.; Le Vot, M.; Masset, J.-M.


    The Aquitaine Basin is located in the southwest of France, between the Gironde Arch in the north and the Pyrenean Mountain Chain in the south. It is a triangular-shaped domain, extending over 35000km{sup 2}. From north to south, six main geological provinces can be identified: (1) the Medoc Platform located south of the Gironde Arch; (2) the Parentis sub-basin; (3) the Landes Saddle; (4) the North Aquitaine Platform; (5) the foreland of the Pyrenees (also known as the Adour, Arzacq and Comminges sub-basins); and (6) the Pyrenean fold-and-thrust belt. Only the Parentis sub-basin, the foreland of the Pyrenean Chain and a minor part of the fold-and-thrust belt itself are proven hydrocarbon provinces. The Aquitaine Basin, in turn, is subdivided into four sub-basins - the Parentis, Adour-Arzacq, Tarbes and Comminges areas. The lozenge shape of these depocentres is related to the Hercynian tectonic framework of the Palaeozoic basement, reactivated during Early Cretaceous rifting. This rift phase aborted at the end of the Albian (prior to the development of an oceanic crust) in response to the beginning of the subduction of the Iberian plate under the European plate. During the Upper Cretaceous, continued subduction led to the creation of northwards-migrating flexural basins. In the Eocene, a paroxysmal phase of compression was responsible for the uplift of the Pyrenean Mountain Chain and for the thin-skinned deformation of the foreland basin. The resulting structuration is limited to the south by the internal core of the chain and to the north by the leading edge of the fold-and-thrust belt, where the Lacq and Meillon gas fields are located. Four main petroleum provinces have been exploited since the Second World War: (1) the oil-prone Parentis sub-basin and (2) salt ridges surrounding the Arzacq and Tarbes sub-basins; and (3) the gas-prone southern Arzacq sub-basin (including the external Pyrenean fold-and-thrust belt and the proximal foreland sub-basin) and (4

  20. Disponibilidade de invertebrados aquáticos para peixes bentófagos de dois riachos da bacia do rio Iguaçu, Estado do Paraná, Brasil Aquatic invertebrates disponibility for bentophagous fishes in two streams at the Iguaçu River basin, state of Paraná, Brazil

    Anderson Ferreira


    Full Text Available Assumindo que os organismos que os peixes consomem refletem sua disponibilidade no ambiente, os objetivos deste trabalho foram verificar, através da dieta, quais os principais organismos que compõem a bentofauna disponível para peixes bentófagos, e analisar as variações espaço-temporais e ontogenéticas na dieta deste grupo de peixes. As coletas foram realizadas mensalmente de março/2000 a fevereiro/2001 através de pesca elétrica em dois riachos da bacia do rio Iguaçu e os estômagos (n=329 analisados pelo método volumétrico. A análise da dieta revelou uma grande diversidade de invertebrados bênticos, principalmente insetos de várias ordens, sendo as mais consumidas Ephemeroptera, representada por três famílias, Diptera por onze e Trichoptera por nove famílias, sendo esses, os organismos mais disponíveis para a alimentação, além de diversos organismos menos representativos. Os resultados de correlação de Spearman foram altamente significativos, revelando forte similaridade espacial, temporal e ontogenética. Essa grande disponibilidade de recursos aquáticos, provavelmente seja a maior responsável pela elevada abundância de indivíduos do gênero Trichomycterus (Siluriformes, Trichomyspteridae nos ambientes analisados.Analyzing aquatic organisms present in fish stomachs is a good way to determine their availability in the environment. This paper aims to determine aquatic organism availability (especially benthos for bentophagous fishes and to analyze spatial, temporal and ontogenetic changes in their diets. Samples were monthly taken from March 2000 to February 2001, through electrofishing, in two streams of the Iguaçu River. The stomachs were analyzed (329 units and the results expressed through volumetric method. The diet was composed of benthic invertebrates, especially insects from several orders, being Ephemeroptera (3 families, diptera (11 families and Trichoptera (9 families the most consumed ones. Therefore

  1. Long-term flow forecasts based on climate and hydrologic modeling: Uruguay River basin

    Tucci, Carlos Eduardo Morelli; Clarke, Robin Thomas; Collischonn, Walter; da Silva Dias, Pedro Leite; de Oliveira, Gilvan Sampaio


    This paper describes a procedure for predicting seasonal flow in the Rio Uruguay drainage basin (area 75,000 km2, lying in Brazilian territory), using sequences of future daily rainfall given by the global climate model (GCM) of the Brazilian agency for climate prediction (Centro de Previsão de Tempo e Clima, or CPTEC). Sequences of future daily rainfall given by this model were used as input to a rainfall-runoff model appropriate for large drainage basins. Forecasts of flow in the Rio Uruguay were made for the period 1995-2001 of the full record, which began in 1940. Analysis showed that GCM forecasts underestimated rainfall over almost all the basin, particularly in winter, although interannual variability in regional rainfall was reproduced relatively well. A statistical procedure was used to correct for the underestimation of rainfall. When the corrected rainfall sequences were transformed to flow by the hydrologic model, forecasts of flow in the Rio Uruguay basin were better than forecasts based on historic mean or median flows by 37% for monthly flows and by 54% for 3-monthly flows.

  2. Sumário/Editorial

    Irene Machado


    Full Text Available Nem sempre os temas candentes da investigação, numa determinada área do conhecimento, são colocados de maneira orgânica e organizada para o conjunto dos pesquisadores que sobre eles se debruçam. Quase nunca as edições cientí­cas, que se propõem a torná-los acessí­veis a seus leitores, conseguem harmonizá-los sem correr os riscos de aproximações indevidas. A única forma de não incorrer em equí­vocos perigosos é assumir a idiossincrasia do temário diversificado que constitui o campo em questão. O leitor que ora inicia seu diálogo com este sétimo número de Galáxia não deve tomar esse preâmbulo por alerta, mas sim como tentativa de a revista manter a coerência face a seu compromisso de ser porta-voz dos temas e problemas da comunicação e da cultura pelo prisma das teorias semióticas que orientam o olhar dos vários colaboradores que encontram neste espaço uma tribuna aberta ao trânsito das diferenças. Basta um relance pelo sumário desta edição para que tal armação possa ser confirmada. Os textos que constituem o Fórum, respeitadas as singularidades, tratam de temas que são caros para as abordagens da comunicação e da semiótica na cultura. Temos o privilégio de publicar o texto inédito em português de Jakob von Uexküll em que o autor apresenta sua teoria da Umwelt, caracterizando formulações da biossemiótica sobre o signi.cado do entorno ou do espaço circundante, que são valiosas para compreender a percepção, a interação, o contexto, a informação, os códigos em ambientes de semiose. De um outro lugar - aquele modulado pela lógica da linguagem - Lucrécia Ferrara perscruta o campo conceitual que entende o design não pelo viés da operatividade, mas como processo semiótico-cognitivo. A outra ponta deste que pode ser um triálogo nos é dado pela comunicologia de Vilém Flusser. Para Michael Hanke, Flusser foi um dos grandes teóricos a investigar a importância da mí­dia para os

  3. Subtle traps in Cretaceous, Archuleta, Conejos, Mineral, and Rio Grande counties, Colorado

    Brown, W.T. Jr. (Coastal Oil and Gas Corp., Denver, CO (USA))


    Regional interpretation of the stratigraphy, faulting, fracturing, and hydrodynamics in Archuleta, Conejos, Mineral, and Rio Grande Counties in southern Colorado indicates that significant reserves of hydrocarbons could exist in subtle trapping situations within the Cretaceous sequences. The presence of Price-Gramps field (7 million bbl of oil ultimate recoverable), which produces primarily from the Dakota Formation, is presently anomalous in this area but is indicative of existing hydrocarbon potential. Hydrocarbon shows from drilled wells and outcrops suggest that significant quantities of hydrocarbons are present in this area, sourced both from the San Juan basin to the south and west, and from more local areas for fractured reservoirs.

  4. EKA urbanistika osakond / Lilia del Rio

    Rio, Lilia del


    Lilia del Rio magistritöö "Beyond the player's manual / Mänguõpetus edasijõudnutele. Experiencing the world (and the city) as a playground / Kogedes maailma (ja linna) mänguväljakuna". Juhendaja Andres Kurg

  5. EKA urbanistika osakond / Lilia del Rio

    Rio, Lilia del


    Lilia del Rio magistritöö "Beyond the player's manual / Mänguõpetus edasijõudnutele. Experiencing the world (and the city) as a playground / Kogedes maailma (ja linna) mänguväljakuna". Juhendaja Andres Kurg

  6. Rio Grande Channel, El Paso Area, 1852

    Earth Data Analysis Center, University of New Mexico — Historical map of Rio Grande river between Texas and Mexico. U.S.-Mexican Boundary Survey.The original map is a Xerox of a Photolithographic Copy of Salazar...

  7. The Carnival of Rio de Janeiro

    Edson Farias


      According to historian Felipe Fer- reira civilization did arrive, but only to the degree that Rio's main streets of the urban center brimmed with parades of large allegorical floats upon which stood...

  8. Healthcare guide: Olympic Games Rio 2016


    This guide provides information on the medical services programme for the Rio 2016 Summer Olympic Games. It contains the map of the organisation, the IOC medical policies and procedures, and many more.

  9. Rio Grande Channel, Guadalupe Area, 1852

    Earth Data Analysis Center, University of New Mexico — Historical map of Rio Grande river between Texas and Mexico. U.S.- Mexican Boundary Survey. The original map is a xerox of a map entitled Boundary between the United...

  10. Complete Genome Sequence of Mayaro Virus Imported from the Amazon Basin to São Paulo State, Brazil.

    Mota, Mânlio Tasso Oliveira; Vedovello, Danila; Estofolete, Cassia; Malossi, Camila Dantas; Araújo, João Pessoa; Nogueira, Maurício Lacerda


    Mayaro (MAYV) is a neglected arbovirus from the tropical Americas. Here, we report the complete genome of an MAYV isolate from a patient returning from the Amazon basin and complaining of arthralgia, high fever, and headache, who was attended at an emergency service of São José do Rio Preto, São Paulo state, Brazil.

  11. An overview of mercury contamination research in the Amazon basin with an emphasis on Brazil Uma revisão das pesquisas sobre contaminação por mercúrio na Amazônia com ênfase no território brasileiro

    Sandra Hacon


    Full Text Available This article provides an overview of research on mercury contamination in the Amazon Basin and its evolution from 1990 to 2005. The assessment was based on an extensive and systematic review using bibliographic databases available online and a review of projects by research groups. Brazilian research groups were identified using the database of the Brazilian National Research Council (CNPq. A geographic information system was used to determine the location of the studies. Different aspects of mercury contamination were evaluated (environmental studies, impacts on human health, technological improvements. For 1990-2005, a total of 455 publications were identified. The main advances and remaining gaps in relation to environmental issues and human health were identified and discussed. Although the scientific output varied considerably over the period, there was a general increase in the total number of publications per year from the early 1990s (fewer than 20 until 2005 (more than 30, considering the articles published in indexed journals.Esta pesquisa apresenta uma visão geral dos estudos desenvolvidos sobre a contaminação por mercúrio na bacia Amazônica e a evolução destes estudos no período 1990-2005. O estudo baseou-se em extensiva e sistemática revisão utilizando bases de dados bibliográficas disponíveis na Internet e em uma revisão dos projetos de pesquisa realizados por grupos de pesquisa. Além disso, os grupos de pesquisa brasileiros foram identificados pela base de dados do Conselho Nacional de Desenvolvimento Científico e Tecnológico (CNPq. Um sistema de informação geográfica foi usado para localizar os estudos conduzidos. Diferentes aspectos da contaminação por mercúrio na Amazônia foram analisados (estudos ambientais, impactos na saúde humana, melhorias tecnológicas. No período de 1990-2005, foram identificadas 455 publicações. As principais realizações e as lacunas existentes em relação aos estudos

  12. A new Hyphessobrycon (Ostariophysi: Characiformes: Characidae) from the middle Amazon basin, Brazil.

    Lima, Flávio C T; Coutinho, Daniel P; Wosiacki, Wolmar B


    Hyphessobrycon montagi, new species, is described from tributaries of the Rio Arapiuns, a left margin affluent of the lower Rio Tapajós, Amazon basin, Pará, Brazil. The new species can be diagnosed from all its congeners by the possession of a combination of two well-defined humeral blotches, connected by a narrow stripe, and a caudal peduncle blotch. A putatively monophyletic Hyphessobrycon heterorhabdus species-group, restricted to H. heterorhabdus, H. amapaensis, and H. eschwartzae, is herein proposed based on shared derived features of color pattern. Alternative proposals of a "Hyphessobrycon heterorhabdus group" presented in the recent literature are evaluated and criticized.

  13. Subsurface recharge to the Tesuque aquifer system from selected drainage basins along the western side of the Sangre de Cristo Mountains near Santa Fe, New Mexico

    Wasiolek, Maryann


    Water budgets developed for basins of five streams draining the western side of the Sangre de Cristo Mountains in northern New Mexico indicate that subsurface inflow along the mountain front is recharging the Tesuque aquifer system of the Espanola Basin. Approximately 14,700 acre-feet of water per year, or 12.7 percent of average annual precipitation over the mountains, is calculated to leave the mountain block and enter the basin as subsurface recharge from the drainage basins of the Rio Nambe, Rio en Medio, Tesuque Creek, Little Tesuque Creek, and Santa Fe River. About 5,520 acre- feet per year, or about 12 percent of average annual precipitation, is calculated to enter from the Rio Nambe drainage basin; about 1,710 acre- feet per year, or about 15 percent of average annual precipitation, is calculated to enter from the Rio en Medio drainage basin; about 1,530 acre- feet, or about 10 percent of average annual precipi- tation, is calculated to enter from the Tesuque Creek drainage basin; about 1,790 acre-feet, or about 19 percent of average annual precipitation, is calculated to enter from the Little Tesuque Creek drainage basin; and about 4,170 acre-feet per year, or about 12 percent average annual precipitation, is calculated to enter from the Santa Fe River drainage basin. Calculated subsurface recharge values were used to define maximum fluxes permitted along the specified-flux boundary defining the mountain front of the Sangre De Cristo Mountains in a numerical computer model of the Tesuque aquifer system near Santa Fe, New Mexico.

  14. Water quality, discharge, and groundwater levels in the Palomas, Mesilla, and Hueco Basins in New Mexico and Texas from below Caballo Reservoir, New Mexico, to Fort Quitman, Texas, 1889-2013

    McKean, Sarah E.; Matherne, Anne Marie; Thomas, Nicole


    The U.S. Geological Survey, in cooperation with the New Mexico Environment Department, compiled data from various sources to develop a dataset that can be used to conduct an assessment of the total dissolved solids in surface water and groundwater of the Palomas, Mesilla, and Hueco Basins in New Mexico and Texas, from below Caballo Reservoir, N. Mex., to Fort Quitman, Tex. Data include continuous surface-water discharge records at various locations on the Rio Grande; surface-water-quality data for the Rio Grande collected at selected locations in the Palomas, Mesilla, and Hueco Basins; groundwater levels and groundwater-quality data collected from selected wells in the Palomas and Mesilla Basins; and data from several seepage investigations conducted on the Rio Grande and selected drains in the Mesilla Basin.

  15. Diverse mantle and crustal components in lavas of the NW Cerros del Rio volcanic field, Rio Grande Rift, New Mexico

    Duncker, K. E.; Wolff, J. A.; Harmon, R. S.; Leat, P. T.; Dickin, A. P.; Thompson, R. N.


    Products of Pliocene (2 4 Ma) mafic to intermediate volcanism in the northwestern Cerros del Rio, a dominantly mafic volcanic field in the Española Basin of the Rio Grande Rift (RGR), range from 49% to 63% SiO2 and exhibit diversity in silica saturation, trace-element patterns, and isotopic compositions. Tholeiites, which are largely confined to west of the Rio Grande, have trace-element abundances that resemble those of oceanic basalts, but with mild depletions in Nb and Ta, and high 87Sr/86Sr, low 143Nd/144Nd, and high δ18O compared to typical OIB. They are regarded as asthenospherically-derived magmas contaminated with continental crust. Alkali basalts and hawaiites erupted from vents east of the Rio Grande are geochemically distinct, having generally higher overall incompatible-element abundances, but with pronounced depletions in K, Rb, Nb and Ta with respect to Th and LREE. Spatially-associated benmoreites, mugearites and latites (collectively termed “evolved” lavas) have similar trace-element characteristics to the mafic mildly-alkaline compositions, but are typically not as depleted in K. Hawaiites and evolved lavas exhibit a good negative correlation of 143Nd/144Nd with SiO2, due to interaction with lower continental crust. The most silicic “evolved” lavas carry the highest proportions of crustal material, and consequently have higher K/Th than the related hawaiites. Several (mostly mafic) lavas contain abundant crustally-derived resorbed quartz xenocrysts in O-isotope disequilibrium with the host magma. The δ18O values of xenocrystic quartz range over 4‰, indicating a variety of quartz-bearing crustal contaminants beneath the Española Basin. The hawaiites, with their unusual combination of trace-element enrichments and depletions, cannot be generated by any process of fractionation or crustal contamination superposed on a common mantle source type (oceanic or arc-source). It is a regional mantle source type, inasmuch as it was also present

  16. Eruption History and Geochemical Evolution of Servilleta Basalt Along the Rio Grande Gorge, Colorado and New Mexico

    Cosca, M. A.; Thompson, R. A.; Turner, K. J.; Morgan, L. E.


    Subalkaline basalt to basaltic andesite lava flows formally known as Servilleta Basalt (SB) are the most voluminous rock type forming the Pliocene Taos Plateau volcanic field. Pleistocene incision by the Rio Grande into the bedrock-floored plateau has resulted in spectacular exposures of occasionally thick ( 240 m) accumulations of SB within the Rio Grande gorge. Incremental CO2 laser heating of individual rock fragments, the SB within and along the length of the Rio Grande gorge has been precisely dated by 40Ar/39Ar geochronology to between 5.3 Ma and 3.3 Ma. SB older than 4 Ma is restricted to some lava flows exposed between La Junta point, at the confluence of the Red River and Rio Grande, and the Gorge Bridge crossing northwest of Taos, NM. Vertical sampling through thick SB flow sequences within the gorge yields precise emplacement histories and also reveals small but systematic major and minor element concentration variations (including Si, Rb, Sr, Cu and Zn). 40Ar/39Ar data show that these trends developed over short (0-250 ka) timescales, and probably relate to partial assimilation of crust, possibly at multiple depths. Combined field, geochemical, and 40Ar/39Ar data consequently record short-lived changes in tholeiitic melt compositions in response to regional extension and development of the Rio Grande rift. The age, lateral extent, and thickness of exposed SB partially reflect the paleotopographic surface of the southern San Luis Basin prior to onset of Pliocene Taos Plateau volcanic field magmatism; paleotopographic highs diverted some flows while topographic lows were areas of infilling and accumulation. Heterogeneous basin paleotopography developed during contemporaneous or precursory andesitic to dacitic volcanism, extensional faulting and subsidence of sub-basins within the San Luis Basin, and deposition of prograding alluvial fans that originated in the Sangre de Cristo and Picuris Mountains. SB flowed into the southern San Luis Valley beginning 5

  17. Geologic and hydrogeologic framework of the Espa?ola basin -- Proceedings of the 5th annual Espa?ola basin workshop, Santa Fe, New Mexico, March 7-8, 2006

    McKinney, Kevin C.


    This report presents abstracts of technical studies that are focused on the hydrogeologic framework of the Espa?ola basin, a major subbasin of the Cenozoic Rio Grande rift. The Rio Grande, Rio Chama, Santa Fe River, and their tributaries carry important surface water in the Espa?ola basin. Sediments and interbedded volcanic rocks fill the Espa?ola basin and form extensive aquifer systems for ground water. Surface and ground water provide the principal sources of water for most residents of the basin, including people in the cities of Santa Fe, Espa?ola, and Los Alamos as well as Native Americans in several Pueblos. The abstracts describe results of technical studies that were presented either as poster exhibits or oral presentations at the fifth-annual Espa?ola basin workshop, held March 7-8 of 2006 in Santa Fe, New Mexico. The principal goal of this workshop was to share information about ongoing studies. The Espa?ola basin workshop was hosted by the Espa?ola basin technical advisory group (EBTAG) and sponsored by the U.S. Geological Survey, the New Mexico Bureau of Geology and Mineral Resources, and the Water Research Technical Assistance Office of Los Alamos National Laboratory. Abstracts in this report have been grouped into six information themes: Basic Water Data, Water Quality and Water Chemistry, Water Balance and Stream/Aquifer Interaction, Data Integration and Hydrologic Model Testing, Three-Dimensional Hydrogeological Architecture, and Geologic Framework. Abstracts submitted by U.S. Geological Survey authors in this report have had their technical content peer reviewed before they were included in the report. Technical reviews were not required for abstracts submitted by authors outside the USGS, although most did receive peer reviews within their originating agencies. Taken together, the abstracts in this report provide a view of the current status of hydrogeologic research within the Espa?ola basin.

  18. Modifed Great Basin Extent (Buffered)

    U.S. Geological Survey, Department of the Interior — Two different great basin perimeter files were intersected and dissolved using ArcGIS 10.2.2 to create the outer perimeter of the great basin for use modeling...

  19. Basin Hopping Graph

    Kucharik, Marcel; Hofacker, Ivo; Stadler, Peter


    Motivation RNA folding is a complicated kinetic process. The minimum free energy structure provides only a static view of the most stable conformational state of the system. It is insufficient to give detailed insights into the dynamic behavior of RNAs. A sufficiently sophisticated analysis...... of the folding free energy landscape, however, can provide the relevant information. Results We introduce the basin hopping graph (BHG) as a novel coarse-grained model of folding landscapes. Each vertex of the BHG is a local minimum, which represents the corresponding basin in the landscape. Its edges connect...

  20. Sumário/Editorial

    Irene Machado


    Full Text Available Um dos propósitos que tem orientado a edição de Galáxia é a publicação de trabalhos que provoquem discussões e sejam capazes de introduzir abordagens e metodologias de estudo na área de sua competência a partir, prioritariamente, de um ponto de vista semiótico. O que rege essa "carta de intenções" é a divulgação de temas e problemas atuais, inovadores e norteadores do pensamento. Até agora a sorte não nos deixou à deriva graças, sobretudo, à confiança que os colaboradores depositam na revista. Neste sexto número, Galáxia apresenta contribuições inéditas para se compreender a dimensão sensorial da imagem no cinema e nas artes, a semiótica da guerra, a dinâmica dos gêneros e formatos na comunicação mediada, a noção de design como intervenção cultural, a semiose dos gestos no discurso polí­tico veiculado pela mí­dia, o imaginário e o espaço na cibercultura. Esses são alguns dos temas de que o exercí­cio competente do pensamento sobre a comunicação na cultura não pode prescindir. Para a seção fórum, o incansável investigador da imagem Jacques Aumont nos ofertou uma de suas mais recentes pesquisas sobre a base sensorial da imagem. Em seu ensaio, examina o processo de superposição a partir da continuidade da imagem móvel e da descontinuidade da montagem. Esse é um tema que não apenas redimensiona as bases semióticas do cinema, como também revela a interferência que o processo cinematográfico continua exercendo na constituição da linguagem audiovisual como um todo. A abordagem de Aumont é surpreendente e, até agora, única, daí­ a decisão de dedicar a ela todo o espaço da seção. Trata-se de um trabalho que teve uma edição restrita no Les Cahiers du Musée National d'Art Modern (MNAM de Paris, uma publicação quadrimestral, editada por Jean-Pierre Criqui (historiador e crí­tico de arte, e voltada para a discussão da arte contemporânea na França. Vinculado ao Centre

  1. Relatório de Estágio Curricular - Dealpoint Mobiliário, Lda.

    Pinto, Sílvia


    O trabalho de estágio decorreu na empresa Dealpoint Mobiliário, empresa esta que se dedica á venda de mobiliário, através de uma loja on-line. Este estágio teve como objectivo a actualização do site e o tratamento de fotografia.


    Neide Coriolano, Luzia; Barbosa, Luciana Maciel


    A pesquisa estuda redes de territórios solidários, objetivando análise e compreensão do fenômeno turístico, sob o eixo do turismo comunitário, no estado do Ceará, localizado na região Nordeste do Brasil, é consolidado destino turístico nacional, pretensamente internacional. Esse eixo de turismo configura territórios solidários que produzem o turismo de base comunitária voltados às diretrizes da economia solidária. Ganha espaço em discussões de interesse do Estado, Organizações Não-Governament...


    selected satellite lakes and Mara River in Lake Victoria basin, during wet and dry seasons in. 2002. Samples ... The wet season recorded higher biomass in all satellite lakes than during the dry season (t = 2.476, DF ..... communication. Urbana ...

  4. Single-basined choice

    Bossert, W.; Peters, H.J.M.


    Single-basined preferences generalize single-dipped preferences by allowing for multiple worst elements. These preferences have played an important role in areas such as voting, strategy-proofness and matching problems. We examine the notion of single-basinedness in a choice-theoretic setting. In co

  5. Regional comparison of syn- and post-rift sequences in salt and salt-free basins offshore Brazil and Angola/Namibia, South Atlantic

    Strozyk, Frank; Back, Stefan; Kukla, Peter


    The large South Atlantic basins offshore South America and Africa record a highly variable syn- to post-breakup tectono-stratigraphic development. The present-day diversity in the structural and sedimentary architecture of the conjugate margins offshore southern Brazil, Namibia and Angola reflects variations in the interplay of a number of controlling factors, of which the most important are i) the structural configuration of each margin segment at the time of break-up, ii) the post break-up geodynamic history including tectonics and magmatism, and iii) variations in the type, quantity and distribution of sediment input to the respective margin segment. Particularly the basins around the Rio Grande Rise - Walvis Ridge volcanic complex show a pronounced tectono-stratigraphic asymmetry both along the respective continental margin and across the Atlantic. Only a few attempts exist to establish a regional tectono-stratigraphic correlation framework across the South Atlantic Ocean, mainly because of the lack of data across entire margin segments and limited resolution of basin wide geophysics. Still unresolved issues particularly concern the explanation of the basin-specific geological evolution of respective margin segments along the same continental margin, as well as the correlation of conjugate basins and margin segments across the Atlantic Ocean. In our study we present interpretations and first-pass restorations of regional 2D seismic-reflectivity data from the large basins offshore Brazil (Pelotas Basin, Santos Basin, Campos Basin, Espirito Santo Basin), and offshore Namibia and Angola (Walvis Basin, Namibe Basin, Benguela Basin, Kwanza Basin), which represent four adjacent pairs of conjugate basins on both sides of the South Atlantic. Results are used to document and compare on a basin-scale the contrasting styles of rift and post-rift settings during and after the continental breakup.

  6. Bransfield Basin and Cordilleran Orogenesis

    Dalziel, I. W.; Austin, J. A.; Barker, D. H.; Christensen, G. L.


    Tectonic uplift of the Andean Cordillera was initiated in the mid-Cretaceous with inversion of a composite marginal basin along 7500 km of the continental margin of South America, from Peru to Tierra del Fuego and the North Scotia Ridge. In the southernmost Andes, from 50-56 degrees S, the quasi-oceanic floor of this basin is preserved in the obducted ophiolitic rocks of the Rocas Verdes (Green Rocks) basin. We suggest that the basin beneath Bransfield Strait, 61-64 degrees S, separating the South Shetland Islands from the Antarctic Peninsula, constitutes a modern analog for the Rocas Verdes basin. Marine geophysical studies of Bransfield basin have been undertaken over the past 12 years by the Institute for Geophysics, University of Texas at Austin, under the auspices of the Ocean Sciences Division and United States Antarctic Program, National Science Foundation. These studies have elucidated the structure and evolution of Bransfield basin for comparison with the Rocas Verdes basin, with a view to eventual forward modeling of the evolution of a hypothetical cordilleran orogen by compression and inversion of the basin. These are the processes that can be observed in the tectonic transformation of the Rocas Verdes basin into the southernmost Andean cordillera, as South America moved rapidly westward in an Atlantic-Indian ocean hot-spot reference frame during the mid-Cretaceous. Multi-channel reflection seismic data from the Bransfield basin reveal an asymmetric structural architecture characterized by steeply-dipping normal faults flanking the South Shetlands island arc and gently dipping listric normal faults along the Antarctic Peninsula margin. Normal fault polarity reversals appear to be related to distributed loci of magmatic activity within the basin. This architecture is remarkably similar to that deduced from field structural studies of the Rocas Verdes basin. Notably, the oceanward-dipping, low angle normal faults along the Antarctic Peninsula margin

  7. Sumário/Editorial

    Comissão Editorial


    Full Text Available A revista Galáxia surgiu no cenário intelectual nacional para atestar que a vitalidade das múltiplas confluências entre Comunicação e Semiótica delimitava um campo de conhecimento maduro capaz de produzir a sua própria revista cientí­fica. Fiel ao seu nome - homenagem a Haroldo de Campos, que, em poema homônimo, sinalizava para o conví­vio entre fronteiras -, a revista assumiu sua vocação transdisciplinar. O Programa de Estudos Pós-Graduados em Comunicação e Semiótica da PUC/SP confiou o projeto inicial do periódico a Irene Machado, que respondeu, de forma notável, pela editoria cientí­fica dos sete primeiros números. A dedicação de Irene Machado contribuiu para consolidar a proposta dos trânsitos e fluxos de idéias como fatores de fomento da diversidade que marca a Comunicação como campo cientí­fico. Sem esse competente trabalho, a revista não teria alcançado o significativo patamar Nacional A na escala de avaliação do sistema Qualis/CAPES. Nessa esteira, feita em nome do Programa, os rigores de edição do presente volume ficaram a cargo de uma comissão composta por Lucrécia D'Aléssio Ferrara, Ana Claudia de Oliveira, Eugênio Trivinho e Helena Katz. Galáxia 8 apresenta uma dupla articulação na seção "Fórum". José Luiz Fiorin mostra as contribuições de uma teoria da significação para a compreensão dos fenômenos comunicacionais, que não se restringem ao âmbito da produção de massa. Eric Landowski, por sua vez, chama a atenção para um outro regime de interpretação das encenações do corpo numa detalhada análise ancorada em quatro dimensões especí­ficas do retrato (mimética, hermenêutica, cosmética e estética, na qual a fotografia dos homens polí­ticos na imprensa é tratada como componente de uma estratégia discursiva midiática global. A problematização dessas dimensões possibilita ao autor desenvolver uma teoria semiótica da visualidade midiática. Com essas duas

  8. Selamento coronário em Endodontia

    Oliveira, Rui Pedro Barra de Sá


    Introdução: A Endodontia é a especialidade da Medicina Dentária responsável pelo estudo e tratamento da câmara pulpar, de todo o sistema de canais radiculares e dos tecidos periapicais, bem como das doenças que os afetam. O selamento da porção coronária dos dentes alvo de tratamento endodôntico apresenta-se como um critério determinante no sucesso ou insucesso do tratamento. São vários os fatores que podem proporcionar um correto selamento coronário evitando assim a microinfiltração de ...

  9. Frontier petroleum basins of Colombia

    Keith, J.F. Jr.; Perez, V.E.


    The frontier basins of Colombia with hydrocarbon potential are numerous, have varying geological histories, and are in different stages of exploration development. In this paper, sedimentary or structural basins are classified as frontier petroleum basins if commercial discoveries of hydrocarbons are lacking, if the basin has not attained a high degree of exploration development, or if a new play concept has been perceived or developed for a portion of a mature exploration basin. Using these criteria for classification, the authors discuss the Cauca-Patia Choco-Pacifico, and Lower Magdalena basin complexes; the Cordillera Oriental foreland basin; and the Cesar-Rancheria, Sabana, and Amazonas basins. A comprehensive geological and structural setting of each of these frontier basins will be presented. The depositional and tectonic evolution of the basins will be highlighted, and the play concepts for each will be inventoried, catalogued, and categorized as to whether they are theoretical or established. The discussion of the available plays in each of these basins will include the main play concept elements of reservoirs traps, seals, source rocks, maturation, and timing. When detailed data permit, the reservoir and trap geometry will be presented.

  10. Natural frequency of regular basins

    Tjandra, Sugih S.; Pudjaprasetya, S. R.


    Similar to the vibration of a guitar string or an elastic membrane, water waves in an enclosed basin undergo standing oscillatory waves, also known as seiches. The resonant (eigen) periods of seiches are determined by water depth and geometry of the basin. For regular basins, explicit formulas are available. Resonance occurs when the dominant frequency of external force matches the eigen frequency of the basin. In this paper, we implement the conservative finite volume scheme to 2D shallow water equation to simulate resonance in closed basins. Further, we would like to use this scheme and utilizing energy spectra of the recorded signal to extract resonant periods of arbitrary basins. But here we first test the procedure for getting resonant periods of a square closed basin. The numerical resonant periods that we obtain are comparable with those from analytical formulas.

  11. Segunda Guerra Mundial, Rio de Janeiro

    Ricardo de Souza Rocha


    Full Text Available The purpose of this paper is to analyze the National Memorial to the World War II Dead (1956-60, a monument designed by Marcos Konder Netto and Hélio Ribas Marinho, and located in Flamengo Park, Rio de Janeiro. We start by commenting on the debates that were going on within the Modernist movement about the need for a new monumentality. Then, we examine the memorial against the urban landscape of Rio de Janeiro and its specific architectural language. Finally, we make an effort to explain the apparent paradox found in modern monuments.

  12. Relatório de atividade profissional

    Silva, Francisco Paulo Gomes da


    Relatório de atividade profissional de mestrado em Optometria Avançada Este relatório é constituído por duas partes: uma primeira em que tento descrever de forma mais ou menos sucinta o meu percurso pessoal e profissional desde que iniciei o estágio profissional em Outubro de 1994 até finais de 2015. Não sei números exatos, mas não devo errar por muito se afirmar que ao longo de mais de 20 anos já realizei mais de 20 000 exames o que, modéstia à parte, me permite afirmar sem...

  13. Solar astrometry with Rio Astrolabe and Heliometer

    Sigismondi, Costantino; Andrei, Alexandre Humberto; Reis-Neto, Eugenio; Penna, Jucira Lousada; D'Avila, Victor Amorim


    Monitoring the micro-variations of the solar diameter helps to better understand local and secular trends of solar activity and Earth climate. The instant measurements with the Reflecting Heliometer of Observatorio Nacional in Rio de Janeiro have minimized optical and thermal distortion, statistically reducing air turbulence effects down to 0.01 arcsec. Contrarily to satellites RHRJ has unlimited lifetime, and it bridges and extends the measures made with drift-scan timings across altitude circles with 0.1 arcsec rms with Astrolabes. The Astrolabe in Rio operated from 1998 to 2009 to measure the solar diameter and the detected variations have statistical significance.

  14. Perfil dos usuários do Arquivo Público do Estado do Rio Grande do Sul

    iviane Portella de Portella


    Full Text Available Este artigo trata sobre o perfil dos usuários do Arquivo Público do Estado do Rio Grande do Sul. A pesquisa caracteriza-se como descritiva, de cunho quantitativo e de natureza aplicada. Os dados foram recolhidos mediante levantamento, sendo realizada observação direta e análise de relatórios dos serviços prestados aos usuários referentes ao período de primeiro de janeiro a trinta e um de dezembro de 2010. Os resultados obtidos permitiram delinear o perfil dos usuários. Assim como, identificar os temas mais pesquisados, observar a existência de políticas e programas de treinamentos de usuários e atualização de funcionários. Através desta pesquisa foi possível quantificar os atendimentos prestados a sociedade, identificar a necessidade de ampliação do programa de difusão do APERS e comprovar a relevância de suas fontes documentais para a sociedade gaúcha.

  15. Two new species of Pseudancistrus (Siluriformes, Loricariidae from the Amazon basin, northern Brazil

    Gabriel da Costa e Silva


    Full Text Available Two new species of Pseudancistrus, a genus diagnosed by non-evertible cheek plates and hypertrophied odontodes along the snout margin, are described from two drainages of the Brazilian Shield: P. kayabi from the rio Teles Pires (rio Tapajós basin and P. asurini from the rio Xingu. The new species are distinguished from congeners (P. barbatus, P. corantijniensis, P. depressus, P. nigrescens, P. reus, and P. zawadzkii by the coloration pattern. Pseudancistrus kayabi has dark bars on the dorsal and caudal fins which are similar to that of P. reus from the Caroní River, Venezuela. Pseudancistrus asurini is unique among Pseudancistrus in having whitish tips of the dorsal and caudal fins in juveniles to medium-sized adults.

  16. Sumário/Editorial

    Comissão Editorial


    Full Text Available

    Galáxia: Revista Transdisciplinar de Comunicação, Semiótica, Cultura, editada pelo Programa de Estudos Pós-Graduados em Comunicação e Semiótica (PUC-SP, amplia, com a publicação deste número 9, a sua consolidação como periódico de divulgação científica de pesquisas e, sobretudo, como espaço incentivador do trânsito de idéias e do diálogo teórico entre investigadores nacionais e internacionais da área de Comunicação e afins. Procura propor paradigmas para a definição dos objetos científicos da área desafiada pelo desenvolvimento tecnológico da informação e pela crescente expansão da economia globalizada e da mundialização da cultura. O presente número confirma o projeto em que se aliam comunicação, semiótica, cultura, tecnologia e informação. Nessa integração, e dentre os temas do volume, destaca-se o espaço, que, lido em sua organização e mediação sígnica, permite compreender as dinâmicas culturais que lhe dão suporte. Na seção "Fórum", Manar Hammad, pesquisador francês da Falculté d'Architecture de Versailles, apresenta uma leitura semiótica do Santuário de Bel, conjunto religioso monumental da antiga Síria, situado na cidade de Tadmor-Palmira. Atualmente, o templo não é senão um complexo em ruínas ou pouco conservado, mas ainda oferece à leitura os alicerces de sua construção e os pilares de crenças que nortearam a civilização modelada por valores gregos que atestam um sincretismo básico para a compreensão da cultura do antigo oriente. A leitura da construção semiótica desse conjunto de relações sígnicas permite flagrar os procedimentos de enunciação que superam o âmbito do verbal para atingir a complexidade dos signos não-verbais e, notadamente, do espaço. Utilizando sua formação arquitetônica, mas superando os limites perceptivos de um espaço simplesmente físico ou tecnicamente edificado, Manar Hammad procura apreender o processo


    Jorge Antonio de Farias


    Full Text Available The present study aims to make a diagnosis of the forests planted in the basin of ‘Pardo’ river (Rio Pardo, in RS state, by contemplating the characterization of properties, of forestations, and of the availability and consumption of wood in the region. The area of reach of the study is in the central region of Rio Grande do Sul state, which main economy is the tobacco crop, enclosing 13 cities that compose the performance area of the Management Committee of Rio Pardo Hydrographic Basin. The data collect were conducted during year 2008. In order to determine the size of the sample, it was made a sampling with its probability proportional to the size, where the criterion of the sample unity distribution took in consideration the numbers of trees per city and, inside the cities, the number of trees per class of property size. The sampling method utilized on the forest inventory was by Prodan, in addition to interviews taken with the producers The region is characterized by small agricultural producers, and 61.4% of the firewood used in the cure of tobacco leaves is acquired from others, moreover, the majority of the forestation possess reduced spacing (2.26 m²/plant and low survival indices, in order of the 34.4% after 7 years of the plantation. The wooden current supply is of 2,781.069 m³, what guarantees a supplying for only 3.5 years. The collected data allow to evidence that the resources necessary to invest in the self-sufficiency of firewood for the crop tobacco, are of R$ 12,250,000,00, that could be placed annually, during seven years, equivalent the rotation in simple coppice, resulting in an area of 80 ha/year/city.

  18. Interaction of a river with an alluvial basin aquifer: Stable isotopes, salinity and water budgets

    Eastoe, Christopher J.; Hutchison, William R.; Hibbs, Barry J.; Hawley, John; Hogan, James F.


    SummaryDetailed sets of tracer data (isotopes, salinity) and the results of MODFLOW modeling of water budgets provide an unprecedented opportunity for comparing modeling with field data in the area where the Rio Grande enters the Hueco Bolson basin of Texas and Chihuahua. Water from the Rio Grande has recharged the Hueco Bolson aquifer to a depth of 300 m below the surface in the El Paso-Ciudad Juárez area, the depth of infiltration corresponding to the depth of ancestral Rio Grande fluvial sediments. Groundwater beneath the river exhibits complex isotope and salinity stratification. Post-dam (post -1916, type A) river water has infiltrated to depths up to 80 m. Pre-dam (type B) river water has infiltrated to 300 m depth near downtown El Paso, and has mixed with, or been displaced further downstream by high-salinity native Hueco Bolson groundwater (type C, present in the basin north of the river). Salinity and isotope boundaries do not correspond precisely. Isotope stratification corresponds to water residence time and (for type C) to degree of evaporation; the highest salinities are associated with the most evaporated water. Modeling of water budgets in the basin fill beneath the river predicts present-day mixing of water types B and C where changing rates of pumping have caused a reversal of groundwater flow direction between El Paso and Ciudad Juárez, and deep recharge of type B water under conditions prevailing in the 1960s.

  19. Hydrochemistry and weathering rates on Corumbataí River basin, São Paulo State, Brazil

    Bonotto, Daniel Marcos; Lima, Jorge Luis Nepomuceno de


    SummaryThis work was held at the Corumbataí River basin that is inserted within the giant Paraná sedimentary basin (Paleozoic-Cenozoic) in South America. The Corumbataí River is the major river draining the area and its water is extensively used by water supply systems in the basin. Its surface waters were collected at two sampling points, upstream and downstream from Rio Claro city, the principal municipality within the basin. We report chemical and radionuclides ( 222Rn and 210Po) analyses for rainwater and river water samples in order to estimate chemical weathering fluxes. All major chemical data indicated poorer conditions of the water quality in Corumbataí River after reaching Rio Claro city. However, one very important finding was that the weighted mean of the 210Po activity concentration is the same (0.21 dpm/L) upstream and downstream from Rio Claro city, indicating that 210Po is a conservative nuclide. The net output flux in Corumbataí River basin estimated from the difference between the total discharge flux and the input flux based on wet precipitation yielded a negative value for polonium as it is a very particle-reactive radionuclide, tending to accumulate into fluvial sediments. The chemical weathering rate (removed material quantity) corresponded to 76.5 t/km 2 yr when Po data in sediments and rocks were utilized in the calculations. This rate is compatible with others determined elsewhere, indicating the usefulness of Po in studies of weathering processes, even in areas characterized by anthropogenic inputs.

  20. The flora of Early Permian coal measures from the Parana Basin in Brazil: A review

    Iannuzzi, Roberto [Centro de Investigacoes do Gondwana, Instituto de Geociencias, Universidade Federal do Rio Grande do Sul, Av. Bento Goncalves, 9500, Porto Alegre, RS, 91.509-900 (Brazil)


    This paper presents an updated overview integrating both previous and newly published data on the most important floras found associated with Early Permian coal seams in the Parana Basin, Brazil. These floras occur within the Rio Bonito Formation and correspond to the Gondwana ''Glossopteris Flora.'' For this review, five floras are selected, in ascending stratigraphic order: the ''Sao Joao do Triunfo,'' ''Figueira,'' ''Quiteria,'' ''Morro do Papaleo'' and ''Irapua Bed'' floras. They are the best-known floras of the basin in terms of taxonomic composition, paleoecology and environments of deposition. An early-mid Sakmarian to earliest Artinskian age is indicated for the Rio Bonito Formation based on absolute radiometric and relative biostratigraphic ages. Integration of available information about the selected floras allows evaluation of taphonomic and paleoecological factors to provide a more comprehensive understanding of the Early Permian floral record in the Parana Basin. The variation observed in both the taxonomic composition of individual floras and in the frequency of occurrence of different plant groups is due to the broad range of environmental/edaphic conditions that prevailed in the many different depositional settings represented in the Rio Bonito Formation. A more precise age determination obtained for the plant-bearing deposits permits the establishment of a more confident correlation between the Early Permian floral succession in the Parana Basin and other Early Permian floral successions in other basins. The Sakmarian global warming favored the appearance of pecopterid and sphenopterid ferns amongst the spore-producing plants, and the glossopterids amongst the pollen-producing plants. (author)

  1. Basin Hopping Graph

    Kucharik, Marcel; Hofacker, Ivo; Stadler, Peter


    basins when the direct transitions between them are “energetically favorable”. Edge weights endcode the corresponding saddle heights and thus measure the difficulties of these favorable transitions. BHGs can be approximated accurately and efficiently for RNA molecules well beyond the length range...... accessible to enumerative algorithms. Availability The algorithms described here are implemented in C++ as standalone programs. Its source code and supplemental material can be freely downloaded from

  2. Substance Abuse in the Rio Grande Valley.

    Zavaleta, Anthony N.


    In the Mexican American barrios of Texas' Lower Rio Grande Valley, existence is complicated by the interactive forces of culture, society, and economy. These three factors act in unison to create an etiology of alcohol and drug use and abuse which is poorly understood by persons outside the barrio's grasp. (Author/NQ)

  3. Salinity management in the Rio Grande Bosque

    Jan M. H. Hendrickx; J. Bruce J. Harrison; Jelle Beekma; Graciela Rodriguez-Marin


    This paper discusses management options for salinity control in the Rio Grande Bosque. First, salt sources are identified and quantified. Capillary rise of ground water is the most important cause for soil salinization in the bosque. Next, a riparian salt balance is presented to explain the different mechanisms for soil salinization. Finally, the advantages and...

  4. Rio Branco, grand strategy and naval power

    João Paulo Alsina Jr.


    Full Text Available This article addresses Baron of Rio Branco's grand strategy and the role played by the naval reorganization program (1904-1910 in this context. The ensuing case study determined the domestic and international constraints that affected the program, as well as the worldview of the patron of Brazilian diplomacy regarding military power's instrumentality to foreign policy.

  5. 76 FR 80430 - Rio Tinto plc and Rio Tinto Limited; Notice of Application


    ... under the laws of Australia with shares listed on the Australian Securities Exchange and traded on the.... Rio Tinto is a dual-listed company (``DLC'') comprised of two distinct, commonly controlled corporate...\\ RTP is a foreign [[Page 80431

  6. A new dark-dotted species of Hypostomus Lacépède (Siluriformes: Loricariidae from rio Paraguaçu, Bahia State, Brazil

    Angela M. Zanata

    Full Text Available A new species of Hypostomus Lacépède is described from the rio Paraguaçu basin, Bahia State, Brazil. The new species is distinguished from its congeners by having black and conspicuous dots on a pale background, which are similar in size on the head, trunk, and fins, along with ventral surface of head and abdomen naked or the latter plated exclusively on its anterior portion, absence of ridges on head and trunk, and caudal-fin lobes relatively similar in length. The new species further differs from the sympatric H. chrysostiktos by having seven branched dorsal-fin rays instead of 10-11 and represents the eleventh siluriform species endemic to the rio Paraguaçu basin.

  7. Um Visitante do Rio de Janeiro Colonial

    Jean M. Carvalho França


    Full Text Available O texto que se segue é a tradução de um manuscrito francês, intitulado Relâche du Vaisseau L'Arc-en-ciel à Rio de Janeiro, 1748, que se encontra na Biblioteca da Ajuda, em Lisboa. Trata-se de um relato anônimo, que dá conta da passagem do navio francês L'Arc-en-ciel pelo porto carioca. Tal relato, um curioso documento para a história dos nossos costumes, contém uma descrição da baía da Guanabara e da cidade do Rio de Janeiro, uma pequena análise do caráter da gente portuguesa do Brasil, um perfil do Governador Dom Fernando Freire e algumas considerações gerais sobre a situação do porto local e sobre os víveres disponíveis na região.The following text is a translation of a French manuscript named Relachê du Vaisseau L'Arc-en-ciel à Rio de Janeiro, 1748, which is in Biblioteca da Ajuda (Ajuda Library in Lisbon. It is an anonymous report and relates the stay of the French ship L'Arc-en-ciel in Rio de Janeiro harbour. Such report, a curious document for the history of our customs, has a description of Guanabara bay and Rio de Janeiro city, a brief analysis of the character of the Portuguese people in Brazil, a prolife of Governor Dom Fernando Freire and some considerations of the situation of local harbour and on the provisions available in that region.

  8. ICLEI submission for Rio+20. Contribution to the Zero Draft of the Rio+20 outcome document



    ICLEI is an association of over 1200 local government Members who are committed to sustainable development. This document is ICLEI's submission to the zero draft document being developed for RIO+20, the United Nations Conference on Sustainable Development, scheduled for June 2012 in Rio de Janeiro, Brazil. In the paper, ICLEI calls for a UN Decade of Sustainable Urbanization to raise awareness, create synergies and to share solutions and good practices.

  9. O magistério dos bispos e o magistério dos doutores

    Zilles, Urbano


    Full Text Available Partindo de tensões recentes entre teólogos e bispos, de modo especial com a Cúria Romana, o autor expõe o papel do Magistério dos bispos e o dos teólogos na Igreja, defendendo a tese de que são dois serviços diferentes, mas complementares, ambos necessários para a vida da Igreja, como mostra a história

  10. Sumário/Editorial

    Irene Machado


    exterior à linguagem, mas a lingüí­stica cujo "foco principal é da ordem do processo". Se, no ensaio de Fiorin, essa é a porta de entrada para esmiuçar a teoria da linguagem de Hjelmslev, no fórum de Galáxia, tal noção é a contribuição para se pensar a epistemologia da semiose da comunicação extraposta ao lingüí­stico. Para isso temos o aval do mestre e da maturidade da própria investigação lingüí­stica que já passa de um século: "O objeto da teoria da linguagem é não somente a lí­ngua natural, mas toda e qualquer semiótica, ou seja, todo e qualquer objeto signi- ficante. A lí­ngua natural é apenas um caso particular desse objeto mais geral". É com Luiz Cláudio Martino que enfrentamos a discussão de natureza epistemológica no campo próprio da comunicação: em seu ensaio, ele discorre sobre a dificuldade de as teorias da comunicação fixarem minimamente os fundamentos dessa investigação. Não que o campo careça de publicações. Pelo contrário: "Ao problema da quantidade de publicações se sobrepõe o da qualidade da reflexão". Sua análise destaca, então, o próprio cepticismo que ronda os estudos na área. Porque entende que nenhuma epistemologia possa prescindir de encaminhamentos crí­tico-metodológicos, as demais seções da revista reúnem trabalhos de análise dentro do rigor crí­tico consolidado no interior de cada abordagem. Elisa de Sousa Martinez investiga duas exposições diferentes da obra do artista Cildo Meireles e mostra como "o significado da obra de arte é construí­do na relação que esta estabelece com o contexto em que é exposta e com as obras com as quais constitui um percurso perceptivo, sensí­vel e cognitivo". Mayra Rodrigues Gomes escolheu programas de televisão para operar com conceitos "palavra de ordem e dispositivo disciplinar formulados, respectivamente, por Deleuze e Foucault". Norma Discini busca compreender o "modo de presença da enunciação" em jornais de grande circula


    Edivaldo Lopes THOMAZ


    Full Text Available O objeto da Geomorfologia é o relevo e ele deve ser entendido quanto a sua forma, gênese, dinâmica entre outros elementos. Além disso, o relevo é o suporte para as atividades humanas e no caso da bacia do rio lratim a principal atividade é a agricultura. No entanto, a prática agrícola tem causado a degradação dos solos, que é o principal fator de produção e reprodução familiar no âmbito da bacia. O presente trabalho enfoca a importância da geomorfologia ambiental no entendimento da degradação da paisagem, bem como no planejamento do uso dos solos agrícolas. Enviromental geomorpholy and familiar agriculture on the river Iratim basin - Guarapuava - PR Abstract The object of the Geomorphology is the relief, and it must be understood in its form, genesis, and dynamic among others. Besides, the relief, is the support for human activities, and concerning to basin of Iratim river the main use is for agriculture. Nevertheless, the agricultural practice has been causing the degradation of the soils. The soil is the most important factor for production and reproduction of familial agriculture in the whole basin. The present work aims to show the importance of environmental geomorphology in the understanding of the landscape degradation, as well as in the planning for using agricultural soils.

  12. Solid Waste in Drainage Network of Rio do Meio Watershed, Florianópolis/SC

    Taiana Gava


    Full Text Available The urban drainage network is among the main pollution transport load factors. Researches on the identification of solid waste transported in the drainage network have been considered the allow evaluation of its impact. In this paper we analyze the main characteristics that influences the presence of solid wastes in the drainage network of the Rio do Meio basin, Florianópolis/SC. A metal net was installed in selected river section and monitored after each rain event. The results showed about 0.27 kg/ha.year of waste are carried in the drainage network. The majority being composed of plastics and building materials. Through the analysis of the data, it was possible to verify the presence of waste in the drainage network is due to poor packaging and to the lack of sweeping in some parts of the basin. It was also found that the total precipitation is directly proportional to the appearance of solid waste. It was concluded that the lack of an integrated management between the components of sanitary system leave unnoticed simple structural measures that ultimately decrease the amount of solid waste in the drainage basin, and that could eliminate this source of pollution.

  13. A construção de um programa de revitalização na bacia do Rio São Francisco The construction of a revitalization program for the São Francisco River watershed

    Antonio Thomaz da Mata Machado


    Full Text Available A construção de um Programa de Revitalização da bacia do Rio São Francisco está em curso. Um decreto presidencial de 2001 e os Planos de Recursos Hídricos das bacias dos rios São Francisco e Velhas introduziram critérios e conceitos inovadores na definição de propostas para a recuperação hidroambiental de bacias hidrográficas. A polêmica em torno das obras de transposição de águas do Rio São Francisco e da implementação da lei das águas na bacia determina o processo de construção do programa. Ações e obras centradas em coleta, interceptação e tratamento de esgotos sanitários estão em andamento e alcançam grande extensão da bacia.The construction of a Program for Rehabilitation of river basin San Francisco is underway. A presidential decree of 2001 and the Plans of Water Resources of the river basins of the San Francisco and Velhas, introduced innovative concepts and criteria in the definition of proposals for the hidroambiental recovery of basins. The controversy surrounding the translation of waters of river of San Francisco and the implementation of the law of water in the basin determines the process of the programme. Activities and works focusing on the collection, interception and treatment of sewage are in progress and achieve great extension of the basin.

  14. Intracontinental basins and strong earthquakes

    邓起东; 高孟潭; 赵新平; 吴建春


    The September 17, 1303 Hongtong M=8 earthquake occurred in Linfen basin of Shanxi down-faulted basin zone. It is the first recorded M=8 earthquake since the Chinese historical seismic records had started and is a great earthquake occurring in the active intracontinental basin. We had held a Meeting of the 700th Anniversary of the 1303 Hongtong M=8 Earthquake in Shanxi and a Symposium on Intracontinental Basins and Strong Earthquakes in Taiyuan City of Shanxi Province on September 17~18, 2003. The articles presented on the symposium discussed the relationships between active intracontinental basins of different properties, developed in different regions, including tensional graben and semi-graben basins in tensile tectonic regions, compression-depression basins and foreland basins in compressive tectonic regions and pull-apart basins in strike-slip tectonic zones, and strong earthquakes in China. In this article we make a brief summary of some problems. The articles published in this special issue are a part of the articles presented on the symposium.

  15. Estimated natural streamflow in the Rio San Jose upstream from the pueblos of Acoma and Laguna, New Mexico

    Risser, D.W.


    The development of surface and ground water, which began about 1870 in the upper Rio San Jose drainage basin, has decreased the flow of the Rio San Jose on the Pueblo of Acoma and the Pueblo of Laguna. The purpose of this study was to estimate the natural streamflow in the Rio San Jose that would have entered the pueblos if no upstream water development had taken place. Estimates of natural flow were based upon streamflow and precipitation records, historical accounts of streamflow, records of irrigated acreage, and empirically-derived estimates of the effects on streamflow of Bluewater Lake, groundwater withdrawals, and irrigation diversions. Natural streamflow in the Rio San Jose at the western boundary of the Pueblo of Acoma is estimated to be between 13,000 and 15,000 acre-feet per year, based on 55 years of recorded and reconstructed streamflow data from water years 1913 to 1972. Natural streamflow at the western boundary of the Pueblo of Laguna is estimated to be between 17 ,000 and 19,000 acre-feet per year for the same period. The error in these estimates of natural streamflow is difficult to assess accurately, but it probably is less than 25 percent. (USGS)

  16. A new species of Gladioglanis Ferraris & Mago-Leccia from rio Aripuanã, Amazonas, Brazil (Siluriformes: Heptapteridae

    Marcelo Salles Rocha

    Full Text Available A new species of Gladioglanis is described from a single locality on rio Aripuanã, rio Madeira basin, and can be distinguished from its congeners by the following characters: dorsal-fin spine and spinelet absent, first dorsal-fin ray flexible, unbranched, followed by five branched dorsal-fin rays, pectoral-fin spine short and with few (5 anterior-side, 4 posterior-side dentations, 22-25 anal-fin rays, round profile of the head in dorsal view, first dorsal-fin pterygiophore in contact with the neural spine of eighth vertebrae, 13 caudal-fin rays in both upper and lower lobes, and 60 total vertebrae. Some of its characters are discussed below and compared among the species of a small clade within Heptapteridae proposed by Bockmann (1998.

  17. The benthic macroinvertebrate fauna of highland streams in southern Brazil: composition, diversity and structure Fauna de macro-invertebrados bentônicos de rios de montanha no sul do Brasil: composição, diversidade e estrutura

    Ludwig Buckup


    Full Text Available Benthic macroinvertebrate in four rivers, three in the Pelotas River basin (Divisa, Marco and Silveira rivers, in the headwaters of the Uruguai River and one in the Taquari-Antas system (Antas River, a tributary in the Guaíba basin, in the state of Rio Grande do Sul, were identified. Two samples were collected in summer, autumn and spring, with one replicate in each river. The total of 28,961 specimens included members of Platyhelminthes, Annelida, Acarina, Insecta, Crustacea and Mollusca. The Silveira and Marco rivers showed significant differences in the indices of Shannon-Weaver (H’, Simpson’s Reciprocal (1/D, Margalef (DMg and Equitability (E. The Silveira River showed the highest means of diversity and the EPT index (Ephemeroptera, Plecoptera, Trichoptera. Comparison among the diversity indices, considered individually, were insufficient to show differences in community structure, for the purpose of ecological characterization of the rivers. The EPT values characterized the Divisa River as having the highest abundance (73%, followed by the Marco (71%, Antas (48% and Silveira (36%. These results suggest that the Silveira River is subject to moderate environmental stress, from human impact, although it showed the highest diversity of the major macrobenthic groups.Os macro-invertebrados bentônicos que ocorrem em quatro rios, três pertencentes à bacia do Rio Pelotas (Rios Divisa, Marco e Silveira nas cabeceiras do Rio Uruguai e um ao sistema Taquari-Antas (Rio Antas, tributário da bacia do Guaíba, no Estado do Rio Grande do Sul, foram identificados. Duas amostras foram coletadas no verão, outono e primavera, com uma réplica em cada rio. Foram coletados 28961 espécimes de macro-invertebrados compreendendo Platyhelminthes, Annelida, Acarina, Insecta, Crustacea e Mollusca. Na comparação entre os rios, Silveira e Marco mostraram diferenças significativas nos índices de Shannon-Weaver (H’, no Recíproco de Simpson (1/D, de

  18. Análise estratigráfica e distribuição do arsênio em depósitos sedimentares quaternários da porção sudeste do Quadrilátero Ferrífero, bacia do Ribeirão do Carmo, MG Stratigraphic analysis and distribution of arsenic in quaternary sedimentary deposits of the southeastern portion of the Quadrilátero Ferrífero, basin of the Ribeirão Carmo, MG

    Adivane Terezinha Costa


    Full Text Available A região do QF, em Minas Gerais, tornou-se internacionalmente conhecida pela exploração de ouro no século XVIII. Nesse artigo, serão apresentados valores de referência (background para o arsênio em sedimentos aluviais provenientes de áreas que foram intensamente afetadas pela exploração de ouro no passado, contidas na bacia do ribeirão do Carmo. A análise da sucessão faciológica dos perfis aluviais foi realizada em depósitos sedimentares de planícies de inundação, barrancos de rios (cutbank e terraços aluviais e foi o alicerce para a obtenção do valor de referência do arsênio em depósitos de fácies de canal e de planícies de inundação. A partir do conhecimento do valor de referência obtido pelo método estatístico, com base na confecção de curvas de freqüência acumulada em escala linear, foram gerados mapas geoquímicos no sistema SIG. A obtenção do valor de referência e do mapa geoquímico do arsênio, na bacia do ribeirão do Carmo, com representação das áreas com concentrações anômalas desse elemento, é fundamental para o diagnóstico e planejamento ambiental de um distrito mineiro potencialmente contaminado por arsênio.The Quadrilátero Ferrífero region, in the State of Minas Gerais, became internationally known due to the exploitation of gold in the eighteenth century. In this paper, we will present background values for arsenic in alluvial sediments from areas that were heavily affected by the exploitation of gold in the past, in the Carmo River Basin. The analyses of the facies succession of the alluvial profiles were carried out in the sedimentary deposits of flood plains, cutbank and alluvial terraces; this being the foundation for obtaining the arsenic background in the facies of the channel and flood plains. From the knowledge of the background obtained by the statistical method, and based on the construction of cumulative frequency curves on a linear scale, geochemical maps were generated

  19. Neopaleozoic biostratigraphy of the Parana Basin; Bioestratigrafia do neopaleozoico da Bacia do Parana

    Daemon, Roberto Ferreira; Quadros, Luiz Padilha de


    Surface samples and cores from 31 exploratory wells were chosen as being the most representative among those drilled by PETROBRAS across the Parana Sedimentary Basin, from Mato Grosso and Goias to Rio Grande do Sul. Their analysis yielded a large amount or Saccites, Monoletes and Monocolpates spores, in addition to representatives of Tasmanales. From the great number of identified forms, 40 species - characterized by their wide geographical distribution allied to a short vertical range - were selected and used as a basis for the biostratigraphical subdivision of the Gondwana section of this sedimentary basin. This biostratigraphic column was divided into six main intervals, designated by the letters G to L, some with further subdivisions. The comparison of the species with those described from other regions provided sufficient geochronological data for the dating of the different intervals. It also demonstrated that the Upper Paleozoic sedimentary sequence in the Parana Basin ranges from the Upper Pennsylvanian (Stephanian C) to the Upper Permian (Kazanian). To complete the paleogeologic data the previously established zonation of the Devonian section was also included. The correlation of the biostratigraphic intervals across the basin and their relationship with the rock-stratigraphic units are demonstrated in several sections. The interpretation of these sections and of the biostratigraphic interval isopachous maps provided important information on the paleogeographic development of the basin. Among the more significant results is evidence of the start of the Permo-Carboniferous sedimentation in the northern regional depression, of a subsequent southward tilting of the basin accompanied by the progressive advance of the deposits toward the Rio Grande do Sul shield and of a Lower Permian lacuna in eastern Parana indicating the beginning of the epeirogenic process which culminated with the rise of the Ponta Grossa arch. The paper also presents some paleoecological

  20. Endocrine disrupters in the Llobregat river basin; Disruptores endocrinos en la cuenca del rio Llobregat

    Romero, J.; Ventura, F.; Marti, I.; Cancho, B. [AGBAR Societat General d' Aigues de Barcelona S. A. (Spain)


    Endocrine disrupters are chemicals capable of modulating the endocrine system. These chemicals may have a natural or an anthropogenic origin. The latter are the most important to international organisms due to their potential hazardous effects on human health and wildlife. An important group of substances such as pesticides, surfactants, alkylphenols, phthalates and bisphenol A are considered as endocrine disrupters: adverse effects like cancer, infertility and alterations of sexual organs are related with their presence. Phthalates and alkylphenols (ethoxylated nonylphenols and their acidic metabolites) are the main endocrine disrupters identified in the Llobregat river water using different analytical techniques. No pesticides have been identified in significative concentrations due to the low agricultural activity in this area. The contamination levels, at the {mu} g/l values, are in agreement with those cited by other authors in the literature. Llobregat raw water is treated in the Sant Joan Despi plant with a complex treatment able to reduce and/or eliminate these compounds. Only phthalates and ethoxylated nonylphenols are identified in treated water (at sub-{mu}g/l levels). Brominated ethoxylated nonylphenols are formed in the water treatment plant due to the high bromide level in Llobregat raw water. (Author) 23 refs.

  1. Documentation and Testing of the WEAP Model for the Rio Grande/Bravo Basin


    border between Texas and the Mexican states of Coahuila, Nuevo Leon and Tamaulipas (Appendix B, Figure 32). There are four reservoirs of interest in this...Camargo - Ciudad Acuna - Ciudad Anhuac - Ciudad Juarez - Matamoros - Metropolitan Monterrey - Nuevo Laredo - Reynosa - Piedras Negras...Rivera, and Jorge A. Hidalgo. (2001). “Sistema de apoyo a la toma de decisions para el manejo integral del agua en cuencas.” IMTA/CNA, Proyecto

  2. Searching for an Acidic Aquifer in the Rio Tinto Basin: First Geobiology Results of MARTE Project

    Fernandez-Remolar, D. C.; Prieto-Ballesteros, O.; Stoker, C.


    Among the conceivable modern habitats to be explored for searching life on Mars are those potentially developed underground. Subsurface habitats are currently environments that, under certain physicochemical circumstances, have high thermal and hydrochemical stability [1, 2]. In planets like Mars lacking an atmospheric shield, such systems are obviously protected against radiation, which strongly alters the structure of biological macromolecules. Low porosity but fractured aquifers currently emplaced inside ancient volcano/sedimentary and hydrothermal systems act as excellent habitats [3] due to its thermal and geochemical properties. In these aquifers the temperature is controlled by a thermal balance between conduction and advection processes, which are driven by the rock composition, geological structure, water turnover of aquifers and heat generation from geothermal processes or chemical reactions [4]. Moreover, microbial communities based on chemolithotrophy can obtain energy by the oxidation of metallic ores that are currently associated to these environments. Such a community core may sustain a trophic web composed of non-autotrophic forms like heterotrophic bacteria, fungi and protozoa.

  3. Native aquatic vertebrates: Conservation and management in the Rio Sonoyta Basin, Sonora, Mexico

    C. Minckley; Izar Izaguirre Pompa; Doug Duncan; Ross Timmons; Dennis Caldwell; Jaime Lopez Mendez; Phil Rosen


    The Río Sonoyta in northern Sonora is an important aquatic ecosystem that is disappearing because of drought and groundwater withdrawal. Its native species are also threatened by introduced species. The only watered reach is an intermittent segment (

  4. Synthesis of national reports for Rio+20



    In the lead up to the United Nations Conference on Sustainable Development (Rio+20), which took place in Brazil in June 2012, there were numerous efforts in countries around the world to help governments, civil society organizations and individuals prepare for the event. One of the more significant efforts led by UNDP in collaboration with the United Nations Department of Economic and Social Affairs (UN DESA) was a support programme to 72 countries across all regions to build a consensus on national views around the themes and objectives of the Rio+20 Conference. This report highlights significant advances in sustainable development from almost 60 country reports and underscores the challenges and bottlenecks to moving beyond the economic-led growth strategies of the past 20 years.

  5. O falso documentário

    Emérito, Matheus Barbosa


    Este trabalho tem como propósito estudar um específico modo de representação: o falso documentário no suporte televisivo e no cinema. Dentre as hipóteses adotadas, o falso documentário é analisado como convenção anti-normativa , ao predominar a ficção no corpo (código discursivo) de não-ficção e, assim, incorporar a qualidade de crédito da linguagem documental. Seu processo de criação tende, por um lado, a desconstruir seu significante, mas, por outro, o celebra através da ...

  6. Dicionário de Arqueologia Portuguesa

    Encarnação, José d'


    Recensão a ALARCÃO (Jorge de) e BARROCA (Mário), Dicionário de Arqueologia Portuguesa, Livraria Figueirinhas, Porto, 2012 (ISBN: 978-972-661-219-3), publicada em Cyberjornal, edição de 6 de Fevereiro de 2013: Divulgado, na mesma data, em: Tecem-se considerações acerca das características do livro em análise e da relevância científica que detém....

  7. Vigilando la Calidad del Agua de los Grandes Rios de la Nacion: El Programa NASQAN del Rio Grande (Rio Bravo del Norte)

    Lurry, Dee L.; Reutter, David C.; Wells, Frank C.; Rivera, M.C.; Munoz, A.


    La Oficina del Estudio Geologico de los Estados Unidos (U.S. Geological Survey, 0 USGS) ha monitoreado la calidad del agua de la cuenca del Rio Grande (Rio Bravo del Norte) desde 1995 como parte de la rediseiiada Red Nacional para Contabilizar la Calidad del Agua de los Rios (National Stream Quality Accounting Network, o NASOAN) (Hooper and others, 1997). EI programa NASOAN fue diseiiado para caracterizar las concentraciones y el transporte de sedimento y constituyentes quimicos seleccionados, encontrados en los grandes rios de los Estados Unidos - incluyendo el Misisipi, el Colorado y el Columbia, ademas del Rio Grande. En estas cuatro cuencas, el USGS opera actualmente (1998) una red de 40 puntos de muestreo pertenecientes a NASOAN, con un enfasis en cuantificar el flujo en masa (la cantidad de material que pasa por la estacion, expresado en toneladas por dial para cada constituyente. Aplicacando un enfoque consistente, basado en la cuantificacion de flujos en la cuenca del Rio Grande, el programa NASOAN esta generando la informacion necesaria para identificar fuentes regionales de diversos contaminantes, incluyendo sustancias qui micas agricolas y trazas elementos en la cuenca. EI efecto de las grandes reservas en el Rio Grande se puede observar segun los flujos de constituyentes discurren a 10 largo del rio. EI analisis de los flujos de constituyentes a escala de la cuenca proveera los medios para evaluar la influencia de la actividad humana sobre las condiciones de calidad del agua del Rio Grande.

  8. Geologic map of the Rio Puerco quadrangle, Bernalillo and Valencia Counties, New Mexico

    Maldonado, Florian


    The Rio Puerco quadrangle is located southwest of Albuquerque in central New Mexico and covers part of the western part of the Isleta Reservation. The U.S. Geological Survey, the New Mexico Bureau of Geology and Mineral Resources, and the University of New Mexico have conducted geologic mapping on the Isleta Reservation and vicinity as part of the Middle Rio Grande Basin Project. The map area contains surficial deposits, calcic soils, fluvial deposits of the Rio Puerco, deposits of the Santa Fe Group, and three volcanic fields. The area is characterized by predominantly north-trending normal faults with generally down-to-the-east movement. Post-Santa Fe Group deposits are composed of surficial deposits (Pleistocene-Holocene) and fluvial deposits of the Rio Puerco (Pleistocene-Holocene). The surficial deposits are divided into eolian, alluvial, colluvial, and landslide deposits. The fluvial deposits of the Rio Puerco consist of four terrace and present channel deposits. The Santa Fe Group is divided into lower and upper parts. The lower part of the Santa Fe Group is exposed near the southwestern corner of the study area where deposits consist of reddish-brown mudstone and sandstone correlated to the Popotosa Formation (Unit 1) of Lozinsky and Tedford (1991). They interpreted deposition of the unit in a basin-floor playa setting. The Popotosa Formation is in fault contact to the east with deposits of the upper Santa Fe Group. The upper Santa Fe Group is derived from major tributary fluvial systems (ancestral Rio Puerco Puerco and possibly the Rio San Jose drainages) draining the adjacent Colorado Plateau and Sierra Nacimiento and correlated to parts of Kelley's (1977) Ceja Formation of the Santa Fe Group and equivalent to Machette's (1978) Sierra Ladrones Formation, Connell's Arroyo Ojito Formation (Connell and others, 1999, and Maldonado's lithofacies of the Isleta Reservation (Maldonado and Atencio,1998a, b). The group also locally includes a fine- grained unit

  9. Summary of the geology of the San Luis Basin, Colorado-New Mexico with emphasis on the geothermal potential for the Monte Vista Graben. Special Publication 17

    Burroughs, R.L.


    The known geologic data of the San Luis Basin are reviewed and related to an understanding of the hydrogeothermal potential of the Alamosa-Monte Vista area. The physiographic setting of the region, the structural framework of the basin, and its influence on the stratigraphic makeup of the rock sequence, which in turn control the occurrence of potential deep water reservoirs, are reviewed. It is suggested that the San Luis Basin was well-developed by Miocene time, and that although the basin was modified by Neogene faulting, it is essentially a late Laramide event having been produced during the Paleogene. Attention is also given to high heat flow along the Rio Grande Rift and to the geothermal gradient of the San Luis Basin. The confined aquifer is then considered in respect to its hydrogeology, water quality, and as to the legal aspects of the system. (LEW)

  10. A linguagem do imaginário

    Arruda, Francimar Duarte


    Full Text Available A linguagem do imaginário constitui, hoje, uma questão situada na arena de debates sobre as possibilidades da comunicação. É digna de reflexão essa busca tumultuada de pistas para compreender a forma como os seres lidam com a sua competência comunicativa e as suas frustrações pela não comunicação concreta. Admite-se atualmente, cada vez mais, a necessidade de se desvendarem os mistérios de uma linguagem com base ontológica, deixando antever o prenúncio de um novo paradigma. Este terá que incorporar novas regras num modelo mais amplo e generoso, onde a linguagem simbólica e, portanto, imaginária mostre sua importância e concretude. Este texto pretende percorrer os labirintos dessa proposta mostrando uma comunicação pelo imaginário como con-sentimento e esclarecer alguns de seus pressupostos

  11. Raptor Use of the Rio Grande Gorge

    Ponton, David A. [Los Alamos National Lab. (LANL), Los Alamos, NM (United States)


    The Rio Grande Gorge is a 115 km long river canyon located in Southern Colorado (15 km) and Northern New Mexico (100 km). The majority of the canyon is under the administration of the Bureau of Land Management {BLM), and 77 km of the canyon south of the Colorado/New Mexico border are designated Wild River under the National Wild and Scenic Rivers Act of 1968. Visits I have made to the Rio Grande Gorge over the past 15 .years disclosed some raptor utilization. As the Snake River Birds of Prey Natural Area gained publicity, its similarity to the Rio Grande Gorge became obvious, and I was intrigued by the possibility of a high raptor nesting density in the Gorge. A survey in 1979 of 20 km of the northern end of the canyon revealed a moderately high density of red-tailed hawks and prairie falcons. With the encouragement of that partial survey, and a need to assess the impact of river-running on nesting birds of prey, I made a more comprehensive survey in 1980. The results of my surveys, along with those of a 1978 helicopter survey by the BLM, are presented in this report, as well as general characterization of the area, winter use by raptors, and an assessment of factors influencing the raptor population.

  12. Environmental impact assessment, from Rio-92 to Rio+20 and beyond

    Luis E. Sánchez


    Full Text Available The 1992 Rio Earth Summit was of paramount importance in the consolidation and international dissemination of environmental impact assessment, officially recognized as a tool for informed decision-making towards sustainable development (Principle 17, Rio Declaration and for protection of biodiversity (Article 14, Convention on Biological Diversity. A significant development afterwards was the strengthening of strategic environmental assessment in the design of policies, plans and programs. Both forms of impact assessment can establish the necessary connections between one goal of the Rio+20 Conference - reaching an agreement on the transition to a green economy - and the underpinning decision making processes. Although the Rio+20 Summit has faced challenges to acknowledge its potential, impact assessment should be strengthened in support of both government and business decisions.La Cumbre de la Tierra de 1992 fue de la más grande importancia en la consolidación y diseminación de la evaluación de impacto ambiental, oficialmente reconocida como una herramienta para la toma de decisiones informada hacia el desarrollo sostenible (Principio 17, Declaración de Rio y para la protección de la biodiversidad (Artículo 14, Convención de la Diversidad Biológica. Un avanzo posterior importante fue el fortalecimiento de la evaluación ambiental estratégica en la preparación de políticas, planos y programas. Ambas formas de evaluación de impacto son capaces de establecer los necesarios vínculos entre un objetivo declarado de la Conferencia Rio+2- - llegar a un acuerdo sobre la transición para una economía verde - y los procesos decisorios subyacentes. Aunque la Cumbre Rio+20 tenga encontrado dificultades en reconocer su potencial, la evaluación de impactos debería ser fortalecida en soporte de decisiones gubernamentales y privadas.A Cúpula da Terra de 1992, no Rio de Janeiro, teve a maior importância na consolidação e dissemina

  13. Rio+20 ou Rio-20?: crônica de um fracasso anunciado

    Roberto Pereira Guimarães


    Full Text Available Passadas quatro décadas da Conferência de Estocolmo sobre o Meio Ambiente Humano, e decorridos apenas alguns meses da Rio+20, parece apropriado analisar o caminho percorrido a partir de Rio-92 e os desafios, em grande parte frustrados, da conferência recém concluída no Rio de Janeiro. Para tais propósitos, são analisados os avanços e retrocessos da agenda global de desenvolvimento sustentável, do processo preparatório e dos resultados alcançados no Rio em Junho de 2012, como também das ameaças provocadas pela nova agenda de segurança estratégica após os eventos de 11 Setembro de 2001 e pela crise econômica e financeira que já dura praticamente uma década. O artigo conclui com as perspectivas da agenda internacional nos próximos anos.Pasadas cuatro décadas desde la Conferencia de Estocolmo sobre Medio Ambiente Humano, y transcorridos tan solo algunos meses de la Rio+20, pareciera apropiado analisar el camino percorrido a partir de la Rio-92 y los desafíos, en grande parte frustrados, de la conferencia recien concluída en Rio de Janeiro. Para tales propósitos, serán analisados los avances e retrocesos en la agenda global de desarrollo sustentable, en el proceso preparatorio y en los resultados alcanzados en Rio en Junho de 2012, como también de las amenazas provocadas por la nueva agenda de segurida estratégica luego de los eventos de 11 Setembro de 2001 y por la crisis económica y financiera que ya dura prácticamente una década. El artículo concluye con las perspectivas de la agenda internacional em los próximos anos.After four decades since the Stockholm Conference on the Human Environment and after just a few months of Rio+20, it seems appropriate to assess the path followed since Rio+92 and the challenges, mostly frustrated, posed by Rio+20 . For this purpose, it is analyzed the advances and shortcomings of the global agenda of sustainable development, of the preparatory process and the results achieved in Rio

  14. Estancia Basin dynamic water budget.

    Thomas, Richard P.


    The Estancia Basin lies about 30 miles to the east of Albuquerque, NM. It is a closed basin in terms of surface water and is somewhat isolated in terms of groundwater. Historically, the primary natural outlet for both surface water and groundwater has been evaporation from the salt lakes in the southeastern portion of the basin. There are no significant watercourses that flow into this basin and groundwater recharge is minimal. During the 20th Century, agriculture grew to become the major user of groundwater in the basin. Significant declines in groundwater levels have accompanied this agricultural use. Domestic and municipal use of the basin groundwater is increasing as Albuquerque population continues to spill eastward into the basin, but this use is projected to be less than 1% of agricultural use well into the 21st Century. This Water Budget model keeps track of the water balance within the basin. The model considers the amount of water entering the basin and leaving the basin. Since there is no significant surface water component within this basin, the balance of water in the groundwater aquifer constitutes the primary component of this balance. Inflow is based on assumptions for recharge made by earlier researchers. Outflow from the basin is the summation of the depletion from all basin water uses. The model user can control future water use within the basin via slider bars that set values for population growth, water system per-capita use, agricultural acreage, and the types of agricultural diversion. The user can also adjust recharge and natural discharge within the limits of uncertainty for those parameters. The model runs for 100 years beginning in 1940 and ending in 2040. During the first 55 years model results can be compared to historical data and estimates of groundwater use. The last 45 years are predictive. The model was calibrated to match to New Mexico Office of State Engineer (NMOSE) estimates of aquifer storage during the historical period by

  15. Anthropogenic impact of mercury accumulation in fish from the Rio Madeira and Rio Negro rivers (Amazonia).

    Dórea, José G; Barbosa, Antonio C


    Fish is an important concentrator of mono-methyl mercury and the main route to human contamination. We compared fish Hg bioaccumulation (within similar weight ranges) in two Amazonian river habitats during high-water seasons. The Rio Madeira has been greatly impacted by agriculture, alluvial gold extraction, and a hydroelectric reservoir, whereas the Rio Negro is much less affected by these human activities. The species at the top of the food web, Hoplias malabaricus (piscivorous; 80-668 ng Hg/g) and Cichla spp. (piscivorous; 42-747 ng Hg/g) showed the highest range of Hg concentrations. Nonpiscivorous species with comparable weight range, such as Potamorhina latior (detritivorous; 20-157 ng Hg/g) and Myleus torquatus (herbivorous; 2-182 ng Hg/g), had lower Hg concentrations. Triportheus elongatus (omnivorous; 5-350 ng Hg/g), with the lowest weight range, also showed a low range of Hg concentrations. Despite the Rio Madeira's higher sediment load as well as environmental impacts (deforestation, agriculture, hydroelectric reservoir, and alluvial gold mining) on natural Hg release, fish Hg bioaccumulation was no different between the two river habitats for nonpiscivorous species. In this small observational study only the species at the top of the food web (M. torquatus, Cichla spp, T. elongatus) showed higher mean Hg concentrations in the Rio Madeira than the dominantly wilderness habitat of the Rio Negro.

  16. Environmental assessment of the area surrounding Dam Rio Verde - Parana/Brazil. An overview of environmental geomorphology.

    Garcia, Claudia Moreira; Carrijo, Beatriz Rodrigues; Sessegolo, Gisele; Passos, Everton


    This paper presents a brief essay on the situation in which the environment of the dam of the Rio Verde Basin-Parana, from the vision of environmental geomorphology. The area is located between the cities of Campo Magro and Campo Largo, Paraná plateau in the first part of theAlto Iguaçu basin. This study aims to raise the concepts relating to environmental geomorphology, to identify the anthropogenic impacts caused in the reservoir areas, identify the environmental compartments found around the dam and characterize the geologic and physiographic region. It was found that the area has intense anthropogenic influence, as urban growth is present in areas and wavy and rough terrain, subject to mass movements and floods. Besides these aspects, the use of land for agriculture contributes to fragility of the area.

  17. Relação entre fator de condição relativo (Kn e abundância de ectoparasitos de brânquias, em duas espécies de ciclídeos da bacia do rio Paraná, Brasil = Relation between the relative condition factor (Kn and the abundance of gill ectoparasites in two species of cichlids from the Paraná river basin, Brazil

    Fábio Hideki Yamada


    Full Text Available Foram analisados 33 espécimes de Satanoperca pappaterra, capturados entre março de 2004 e junho de 2005, na planície de inundação do alto rio Paraná e 33 espécimes de Crenicichla niederleinii, capturados entre novembro de 2005 e novembro de 2006, no reservatório de Itaipu. Ambos estavam parasitados por monogenéticos, pertencentes ao gênero Sciadicleithrum e por metacercárias de Ascocotyle sp. O fator de condição relativo (Kn não diferiu significativamente entre indivíduos parasitados e não-parasitados das duas espécies de hospedeiros. Apenas Sciadicleithrum sp.1 parasito de S. pappaterra apresentou correlação positiva e significativa entre o fator de condição relativo (Kn e a abundância de parasitismo. Por outro lado, Ascocotyle sp. de ambos os hospedeiros e Sciadicleithrum sp.2parasito de C. niederleinii não apresentaram correlações entre o Kn e a abundância de parasitismo.The study analyzed 33 specimens of Satanoperca pappaterra, captured from the Upper Paraná River floodplain between March 2004 and June of 2005, and 33 specimens of Crenicichla niederleinii captured from the Itaipu Reservoir between November 2005 and November 2006. Both were parasitized by monogeneans pertaining to the genus Sciadicleithrum and by metacercariae of Ascocotyle sp. The relative condition factor (Kn did not differ significantly between parasitized and unparasitized individuals from the two host species. Only Sciadicleithrum sp.1, parasite of S. pappaterra, presented positive and significant correlation between the relative condition factor (Kn and the abundance of parasitism. On the other hand, Ascocotyle sp. in both hosts and Sciadicleithrum sp.2 parasite of C. niederleiniidid not present correlations between the Kn and the abundance of parasitism.

  18. New species and records of the genus Aegla Leach, 1820 (Crustacea, Anomura, Aeglidae from the West-Central region of Rio Grande do Sul, Brazil

    Sandro Santos

    Full Text Available Aeglidae are anomuran freshwater "crabs" found only in southern South America. In Brazil, the greatest species diversity occurs in hydrographic basins of the state of Rio Grande do Sul. Two new species, Aegla georginae and Aegla ludwigi, are described from the Ibicuí and Ijuí Rivers, respectively (Uruguay River Basin. The new taxa can be distinguished from other Aegla species based on both morphological and molecular characters. The two new species have a very restricted distribution and are categorized as endangered (A. georginae and critically endangered (A. ludwigi using IUCN Red List criteria. We also summarize and present new records of the Aegla species occurring in the Uruguay River Basin.

  19. Simulation and Hydrologic Modeling of Urban Watershed for Flooding Forecast: The case of the Rio das Antas in the city of Anápolis-GO

    Eduardo Dourado Argolo


    Full Text Available The study area is located along the Rio das Antas basin in the city of Anápolis, Goiás. This study exemplifies an urban area exposed to flooding by rainwater. Decline in the permeability of the river basin area is result of significant real state development in recent years. This study proposes to simulate water flows and respective flooding areas along different sections of the River in response to different rainfall intensities. The simulated flow rates are the result of interpretation of land use scenarios and hydrologic modeling of the river basin area. The rational method and the Bernoulli equation were used in the hydraulic simulation model of the computer program HEC-RAS (Hydrologic Engineering Center's River Analysis System...

  20. Attributes for NHDPlus Catchments (Version 1.1): Basin Characteristics, 2002

    Wieczorek, Michael; LaMotte, Andrew E.


    -Red-Rainy River basins, contains NHDPlus Production Units 4, 5, 7 and 9. MRB4, covering the Missouri River basins, contains NHDPlus Production Units 10-lower and 10-upper. MRB5, covering the Lower Mississippi, Arkansas-White-Red, and Texas-Gulf River basins, contains NHDPlus Production Units 8, 11 and 12. MRB6, covering the Rio Grande, Colorado and Great Basin River basins, contains NHDPlus Production Units 13, 14, 15 and 16. MRB7, covering the Pacific Northwest River basins, contains NHDPlus Production Unit 17. MRB8, covering California River basins, contains NHDPlus Production Unit 18.

  1. Three new species of the armored catfish genus Loricaria (Siluriformes: Loricariidae from river channels of the Amazon basin

    Matthew R. Thomas

    Full Text Available Three new species of Loricaria are described from large white- and black-water river channels of the Amazon basin of Brazil, the upper rio Negro drainage of southern Venezuela, and clear waters of the lower rio Tocantins. Loricaria spinulifera and L. pumila differ from other species of Loricaria by having unique patterns of abdominal plate development and hypertrophied odontodes forming conspicuous crests on dorsal surfaces of the head and predorsal plates. Both are small species of Loricaria, reaching sexual maturity at less than 120 mm SL, and exhibiting sexually dimorphic characters consistent with members of the L. cataphracta complex. Loricaria spinulifera differs from L. pumila in having a unique arrangement of buccal papillae and large thorn-like odontodes on the dorsum of the head. Loricaria pumila is the smallest known Loricaria, reaching sexual maturity at less than 80 mm SL. Loricaria lundbergi differs from other Loricaria by having a unique abdominal plate pattern, broad head, and small basicaudal plate. Loricaria lundbergi is sympatric with L. spinulifera in the lower rio Negro drainage, but is also known from the rio Baria system of the Casiquiare drainage. Loricaria pumila occurs in the lower rio Amazonas and lower rio Tocantins. All three new species exhibit varying degrees of reduction in eye size and pigmentation seen in other fishes inhabiting deep river channels of South America.

  2. Silviculture of eucaliptus plantations in the Paraiba do Sul basin, Brazil, and its potential implication on the basin ecohydrology.

    Carriello, Felix; Andres Rodriguez, Daniel; Marques Neves, Otto; Vicens, Raul


    Silviculture of eucaliptus plantations is an important driver of the Mata Atlântica biome conversion into another land use in the Paraíba do Sul basin, in the southeastern of Brazil. This region is located in one of the most developed areas in Brazil, between Rio de Janeiro and São Paulo, the most important cities in Brazil, linked by Presidente Dutra highway. Between both cities there are another cities that produce a variety of goods - from meat to planes, cars and mobile phones. This area is, at the same time, one the most important hot spot for the Mata Atlântica biome. Here we have a large Mata Atlântica fragment protected by law and others fragments being conversed to pasture, agriculture, silviculture and urban areas. Paraiba do Sul river drains the region and runs into Rio de Janeiro State. The basin is highly anthropized, with multiple approaches of its waters resources. Its waters also serve Rio de Janeiro metropolitan area. Because land use and land cover changes impact the water yield in a basin, the study of its dynamic its of great importance for water resources management. We study the land use and land cover change in the region between 1986 and 2010, focusing in the development of silviculture of eucaliptus plantations. We used the HAND (Height Above Nearest Drainage) approach that uses the height above the nearest water body, acquired from SRTM Data and transformed into a Terrain Numeric Mode, to classify the landscape into three different ecohydrological environments: floodplain, mountain top and hillslope. This classes were intersected with 1986 and 2010 land use and cover change classification obtained from Landsat imagery. Results show that silviculture has increased in the region from 1986 to 2010. In both years, silviculture areas are mainly located at the hillslope (47%), while floodplain and mountain top share 28 % and 23 % respectively. Available census data from the Brazilian Institute of Geography and Statistics, IBGE, for 1995 and

  3. Erosion, storage, and transport of sediment in two subbasins of the Rio Puerco, New Mexico

    Gellis, A.C.; Pavich, M.J.; Ellwein, A.L.; Aby, S.; Clark, I.; Wieczorek, M.E.; Viger, R.


    Arroyos in the American Southwest proceed through cut-and-fill cycles that operate at centennial to millennial time scales. The geomorphic community has put much effort into understanding the causes of arroyo cutting in the late Quaternary and in the modern record (late 1800s), while little effort has gone into understanding how arroyos fill and the sources of this fill. Here, we successfully develop a geographic information system (GIS)-modeled sediment budget that is based on detailed field measurements of hillslope and channel erosion and deposition. Field measurements were made in two arroyo basins draining different lithologies and undergoing different land disturbance (Volcano Hill Wash, 9.30 km2; Arroyo Chavez, 2.11 km2) over a 3 yr period. Both basins have incised channels that formed in response to the late nineteenth-century incision of the Rio Puerco. Large volumes of sediment were generated during arroyo incision, equal to more than 100 yr of the current annual total sediment load (bed load + suspended load) in each basin. Downstream reaches in both arroyos are presently aggrading, and the main source of the sediment is from channel erosion in upstream reaches and first- and second-order tributaries. The sediment budget shows that channel erosion is the largest source of sediment in the current stage of the arroyo cycle: 98% and 80% of the sediment exported out of Volcano Hill Wash and Arroyo Chavez, respectively. The geomorphic surface most affected by arroyo incision and one of the most important sediment sources is the valley alluvium, where channel erosion, gullying, soil piping, and grazing all occur. Erosion rates calculated for the entire Volcano Hill Wash (-0.26 mm/yr) and Arroyo Chavez (-0.53 mm/yr) basins are higher than the modeled upland erosion rates in each basin, reflecting the large contributions from channel erosion. Erosion rates in each basin are affected by a combination of land disturbance (grazing) and lithology

  4. K-Basins design guidelines

    Roe, N.R.; Mills, W.C.


    The purpose of the design guidelines is to enable SNF and K Basin personnel to complete fuel and sludge removal, and basin water mitigation by providing engineering guidance for equipment design for the fuel basin, facility modifications (upgrades), remote tools, and new processes. It is not intended to be a purchase order reference for vendors. The document identifies materials, methods, and components that work at K Basins; it also Provides design input and a technical review process to facilitate project interfaces with operations in K Basins. This document is intended to compliment other engineering documentation used at K Basins and throughout the Spent Nuclear Fuel Project. Significant provisions, which are incorporated, include portions of the following: General Design Criteria (DOE 1989), Standard Engineering Practices (WHC-CM-6-1), Engineering Practices Guidelines (WHC 1994b), Hanford Plant Standards (DOE-RL 1989), Safety Analysis Manual (WHC-CM-4-46), and Radiological Design Guide (WHC 1994f). Documents (requirements) essential to the engineering design projects at K Basins are referenced in the guidelines.

  5. Geologic Basin Boundaries (Basins_GHGRP) GIS Layer

    U.S. Environmental Protection Agency — This is a coverage shapefile of geologic basin boundaries which are used by EPA's Greenhouse Gas Reporting Program. For onshore production, the "facility" includes...

  6. The Amazon basin in transition.

    Davidson, Eric A; de Araújo, Alessandro C; Artaxo, Paulo; Balch, Jennifer K; Brown, I Foster; C Bustamante, Mercedes M; Coe, Michael T; DeFries, Ruth S; Keller, Michael; Longo, Marcos; Munger, J William; Schroeder, Wilfrid; Soares-Filho, Britaldo S; Souza, Carlos M; Wofsy, Steven C


    Agricultural expansion and climate variability have become important agents of disturbance in the Amazon basin. Recent studies have demonstrated considerable resilience of Amazonian forests to moderate annual drought, but they also show that interactions between deforestation, fire and drought potentially lead to losses of carbon storage and changes in regional precipitation patterns and river discharge. Although the basin-wide impacts of land use and drought may not yet surpass the magnitude of natural variability of hydrologic and biogeochemical cycles, there are some signs of a transition to a disturbance-dominated regime. These signs include changing energy and water cycles in the southern and eastern portions of the Amazon basin.

  7. Hydrologic budget of the late Oligocene Lake Creede and the evolution of the upper Rio Grande drainage system

    Barton, Paul B.; Steven, Thomas A.; Hayba, Daniel O.


    The filling history, hydrologic budget, and geomorphic development of ancient Lake Creede and its tributary basin are evaluated to determine the factors that controlled its character. The lake filled the Creede caldera that formed in the late Oligocene as a consequence of the eruption of the Snowshoe Mountain Tuff. The caldera's sedimentary fill accumlated to a depth of about 1.26 km and had a volume of about 89 km3. The highest lake level was ~3300 m (10,800 ft) present altitude before it drained eastward across a broad volcanic plateau as the ancestral Rio Grande. A tributary canyon several hundred meters deep was cut into hard rhyolite in the north wall of the caldera before the lake was more than half full; its presence demonstrates that ancient Lake Creede filled slowly and thus occupied a long-lived, closed basin. The slow filling rate is incompatible with the present water flux through the Creede caldera basin, because such a flow would fill the basin geologically instantaneously. This mismatch, together with the recognition that the Oligocene climate was similar to that of today, forces the reexamination of the hydrologic and geomorphic history of the caldera. That appraisal shows that the caldera cannot have resurged rapidly immediately after caldera collapse, and that ancient watershed must have been lass than half as large as the present upper Rio Grande basin. The ancient lake had a more or less constant surface area of about 200 km2 that approximated a steady-state condition between inflow and evaporation. Although the lake level fluctuated with climatic variations, its surface elevation steadily climbed as sediment accumulated, accelerating as resurgance and dome growth usurped spacewithin the basin. It could have had one playa stage early in its development and another after the basin had nearly filled with sediment, but there is no direct evidence for either. At least the lower half of the sedimentary column (the part sampled by the scientific

  8. Cibercenários: Hekuras, Karuanas & Kurupiras

    Tânia Fraga


    O projeto apresenta a possibilidade de miscigenação do campo biológico com instrumentos tecnológicos computacionais em jornadas que utilizam a computação gráfica tridimensional interativa como cibercenários e que possibilitam a participação ativa dos intérpretes que com elas interagem. O intérprete provoca mudanças, em tempo real, nos nichos virtuais que compõem os cibermundos, pela manipulação de um mouse sem fio. As jornadas resultantes integram suas ações com aquel...

  9. Reconstruction of North American drainage basins and river discharge since the Last Glacial Maximum

    Wickert, Andrew D.


    Over the last glacial cycle, ice sheets and the resultant glacial isostatic adjustment (GIA) rearranged river systems. As these riverine threads that tied the ice sheets to the sea were stretched, severed, and restructured, they also shrank and swelled with the pulse of meltwater inputs and time-varying drainage basin areas, and sometimes delivered enough meltwater to the oceans in the right places to influence global climate. Here I present a general method to compute past river flow paths, drainage basin geometries, and river discharges, by combining models of past ice sheets, glacial isostatic adjustment, and climate. The result is a time series of synthetic paleohydrographs and drainage basin maps from the Last Glacial Maximum to present for nine major drainage basins - the Mississippi, Rio Grande, Colorado, Columbia, Mackenzie, Hudson Bay, Saint Lawrence, Hudson, and Susquehanna/Chesapeake Bay. These are based on five published reconstructions of the North American ice sheets. I compare these maps with drainage reconstructions and discharge histories based on a review of observational evidence, including river deposits and terraces, isotopic records, mineral provenance markers, glacial moraine histories, and evidence of ice stream and tunnel valley flow directions. The sharp boundaries of the reconstructed past drainage basins complement the flexurally smoothed GIA signal that is more often used to validate ice-sheet reconstructions, and provide a complementary framework to reduce nonuniqueness in model reconstructions of the North American ice-sheet complex.

  10. Ground-Water Temperature, Noble Gas, and Carbon Isotope Data from the Espanola Basin, New Mexico

    Manning, Andrew H.


    Ground-water samples were collected from 56 locations throughout the Espanola Basin and analyzed for general chemistry (major ions and trace elements), carbon isotopes (delta 13C and 14C activity) in dissolved inorganic carbon, noble gases (He, Ne, Ar, Kr, Xe, and 3He/4He ratio), and tritium. Temperature profiles were measured at six locations in the southeastern part of the basin. Temperature profiles suggest that ground water generally becomes warmer with distance from the mountains and that most ground-water flow occurs at depths 50 years old, consistent with the 14C ages. Terrigenic He (Heterr) concentrations in ground water are high (log Delta Heterr of 2 to 5) throughout much of the basin. High Heterr concentrations are probably caused by in situ production in the Tesuque Formation from locally high concentrations of U-bearing minerals (Northeast zone only), or by upward diffusive/advective transport of crustal- and mantle-sourced He possibly enhanced by basement piercing faults, or by both. The 3He/4He ratio of Heterr (Rterr) is commonly high (Rterr/Ra of 0.3-2.0, where Ra is the 3He/4He ratio in air) suggesting that Espanola Basin ground water commonly contains mantle-sourced He. The 3He/4He ratio of Heterr is generally the highest in the western and southern parts of the basin, closest to the western border fault system and the Quaternary to Miocene volcanics of the Jemez Mountains and Cerros del Rio.

  11. Influence of upwelling saline groundwater on iron and manganese cycling in the Rio Grande floodplain aquifer

    Kirk, Matthew F. [Department of Earth and Planetary Sciences, University of New Mexico, Albuquerque, NM 87131 (United States)], E-mail:; Crossey, Laura J. [Department of Earth and Planetary Sciences, University of New Mexico, Albuquerque, NM 87131 (United States); Takacs-Vesbach, Cristina [Department of Biology, University of New Mexico, Albuquerque, NM 87131 (United States); Newell, Dennis L. [Department of Earth and Planetary Sciences, University of New Mexico, Albuquerque, NM 87131 (United States); Bowman, Robert S. [Department of Earth and Environmental Science, New Mexico Tech, Socorro, NM 87801 (United States)


    Salinity contributions from upwelling groundwater significantly degrade water quality in the Rio Grande, a major source of water for the southwestern USA. This study considers the influence of this upwelling water on the geochemistry and microbiology of the Rio Grande floodplain alluvial aquifer. The composition of surface water, groundwater, and floodplain sediment samples collected from three transects in the Socorro Basin was examined. Terminal-restriction fragment length polymorphism (T-RFLP) was also used to examine microbial biomass samples. The distribution of salinity in the floodplain groundwater largely reflects the configuration of local groundwater flow and mixing of two major water sources, deeply-sourced saline groundwater and river water. Microbial populations in the shallow aquifer consume O{sub 2} and NO{sub 3}{sup -} and serve to redistribute metal oxides from the saturated zone to locations of groundwater discharge at the surface and possibly near the water table. The upwelling saline groundwater affects floodplain microbial processes by transporting reduced metals and organic electron donors to the alluvial aquifer system. This enhances metal reduction in the saturated zone and ultimately metal oxidation at or near the surface. Geochemical modeling suggests that mixing of the saline groundwater with more dilute water in the floodplain creates conditions more favorable for metal oxidation to occur and thereby influences the distribution of metal oxides.

  12. Paleomobility in the Tiwanaku diaspora: biogeochemical analyses at Rio Muerto, Moquegua, Peru.

    Knudson, Kelly J; Goldstein, Paul S; Dahlstedt, Allisen; Somerville, Andrew; Schoeninger, Margaret J


    Paleomobility has been a key element in the study of the expansion of ancient states and empires, including the Tiwanaku polity of the South Central Andes (AD 500-1000). We present radiogenic strontium and oxygen isotope data from human burials from three cemeteries in the Tiwanaku-affiliated Middle Horizon archaeological site complex of Rio Muerto in the Moquegua Valley of southern Peru. At Rio Muerto, archaeological human enamel and bone values range from (87) Sr/(86) Sr = 0.70657-0.72018, with a mean of (87) Sr/(86) Sr = 0.70804 ± 0.00207 (1σ, n = 55). For the subset of samples analyzed for oxygen isotope values (n = 48), the data ranges from δ(18) Ocarbonate(VSMOW)  = +18.1 to +27.0‰. When contextualized with other lines of archaeological evidence, we interpret these data as evidence for an archaeological population in which the majority of individuals had "local" origins, and were likely second-generation, or more, immigrants from the Tiwanaku heartland in the altiplano. Based on detailed life history data, we argue a smaller number of individuals came at different ages from various regions within the Tiwanaku polity. We consider whether these individuals with isotopic values consistent with "nonlocal" geographic origins could represent first-generation migrants, marriage exchange partners, or occupationally mobile herders, traders or other travelers. By combining isotopic life history studies with mortuary treatment data, we use a person-centered migration history approach to state integration and expansion. Isotopic analyses of paleomobility at the Rio Muerto site complex contribute to the role of diversity in ancient states by demonstrating the range of geographic origins rather than simply colonists from the Lake Titicaca Basin.

  13. Trip report Rainwater Basin Nebraska

    US Fish and Wildlife Service, Department of the Interior — This report is a summary a trip to Rainwater Basin Wetland Management District in 1991, and focuses on the hydrology and soil habitat types. It is part of the...

  14. Allegheny County Basin Outlines Map

    Allegheny County / City of Pittsburgh / Western PA Regional Data Center — This basins dataset was created to initiate regional watershed approaches with respect to sewer rehabilitation. If viewing this description on the Western...

  15. The ichthyofauna of upper rio Capivari: defining conservation strategies based on the composition and distribution of fish species

    Paulo dos Santos Pompeu

    Full Text Available Although the rio Capivari basin is recognized as an area of great importance for the ichthyofauna, it lacks virtually every basic requirement for the definition of appropriate conservation strategies, since not even its species composition is known. The objective of this work is to determine the composition and distribution of fish species in the upper rio Capivari basin, relating them to the local physical features, and to evaluate the effectiveness of proposed conservations units, delimited based on areas of native vegetation remains, on the conservation of local ichthyofauna. During 2007, 50 different watercourses were sampled with gillnets, cast nets and kick nets. A total of 1308 individuals belonging to 41 species were captured. Degree of conservation, altitude and width were the parameters that best explained fish species richness. Considering the recently proposed boundaries for potential conservation units in the region only 15 or 20 out of 41 species would be found in the State Park and Environmental Protection Area respectively. In practice, the proposed conservation units would not be effective tools for fish conservation, since it would be located in mountainous areas of high altitude, of headwaters streams and where few species are found. In such context, the conservation of specific stretches of larger rivers is critical.

  16. Phylogeography of the Neotropical catfish Pimelodus albicans (Siluriformes: Pimelodidae from río de la Plata basin, South America, and conservation remarks

    Julia Vergara


    Full Text Available Pimelodus albicans Valenciennes, 1840 (common name "moncholo" or "bagre blanco" is an endemic species of the family Pimelodidae in the río de la Plata basin. Phylogenetic approach based on cytochrome b sequences was performed to test the existence of a unique evolutionary lineage in P. albicans and to discriminate populations units or subpopulations related to a migration behavior of this taxon in the río de la Plata basin. This study included 34 samples of P. albicans of different collecting sites in the río de la Plata estuary and in the río Arrecifes belonging to the río Paraná basin. Among 614 base pairs in the cytochrome b sequence data set, 203 were variable and 120 were phylogenetically informative sites in P. albicans. A total of twenty haplotypes, nucleotide diversity (p = 0.032 and haplotype diversity = 0.941 were found. Tajima's test showed significant value D= -1.88 (pPimelodus albicans Valenciennes, 1840 (popularmente conhecida como moncholo ou bagre branco é uma espécie endêmica da família Pimelodidae na bacia do rio da Prata. Estudos filogeográficos baseados nas seqüências do citocromo b mitocondrial foram realizados para testar a existência de uma única linhagem evolutiva in P. albicans e para discriminar unidades populacionais relacionadas ao comportamento migratório desse táxon na bacia do rio da Prata. Um total de 34 amostras de P. albicans provenientes de diferentes lugares de coleta no estuário do rio da Prata e rio Arrecifes na bacia do rio Paraná foram analisados. Entre as 614 pares de bases do citocromo b no conjunto de dados, 203 deles variaram e 120 foram sítios filogeneticamente informativos para P. albicans. No presente estudo foi encontrado um total de vinte haplótipos, diversidade de nucleotídeos (p = 0,032 e diversidade de haplótipos = 0,941. O teste de Tajima mostrou valores significativos D= -1,88 (p<0,05 rejeitando a hipótese de mutação neutra para os dados de P. albicans. Todas as an

  17. 77 FR 45653 - Yakima River Basin Conservation Advisory Group; Yakima River Basin Water Enhancement Project...


    ... Bureau of Reclamation Yakima River Basin Conservation Advisory Group; Yakima River Basin Water... on the structure, implementation, and oversight of the Yakima River Basin Water Conservation Program... of the Water Conservation Program, including the applicable water conservation guidelines of...

  18. New Geological and Geophysical Data for the Geometric and Stratigraphic Characterization of the Alhandra Sub-basin (Southeast of Paraíba

    Benjamim Bley de Brito Neves


    Full Text Available Some recent geological and geophysical reconnaissance studies carried out in the Alhandra Sub-basin (southern segmentof the Paraíba Basin have revealed very interesting structural and stratigraphic behaviors that have not yet been described.Four different structural compartments with NNE-SSW trends were identifi ed, each characterized by a particularstratigraphic pile, as a result of vertical tectonic displacements, probably post-Pliocene in age: the Alto Rio MumbabaHigh (with widespread basement outcrops, the Rio Mamuaba Graben (the well-exposed Beberibe Formation with thicknessesfrom 100 m up to 300 m, the Rio Gramame High (a horst zone, with some basement outcrops, underlying the BeberibeFormation and the Alhandra-Guruji- Conde-Caaporã monoclinal zone, east of the BR-101, limited to the west bya fault line. The stratigraphic sequence of the Paraiba basin represented by the Paraíba Group is complete only along theeastern monoclinal zone, where the Barreiras Group is also preserved. Along the Rio Mamuaba graben, occurrences of theBarreiras Group were not found as would be expected, and this seems to be an indication that more than one phase of verticalmovement occurred, the second of which had probably removed the Barreiras Group. All these observations are preliminaryand demand further geological and geophysical studies, especially at scales greater than 1/50.000.

  19. Gravity and Magnetotelluric Modeling of the Santo Domingo Basin, Northern New Mexico

    Zamudio, K. D.; Keithline, N.; Blum, C.; Cunningham, E.; Fromont, A.; Jorgensen, M.; Lee, R.; McBride, K.; Saez Berrios, P.; Harper, C.; Pellerin, L.; McPhee, D.; Ferguson, J. F.


    The Santo Domingo Basin, one of a series of basins within the Rio Grande Rift, is located between Santa Fe and Albuquerque, NM, and has been the focus of research by the Summer of Geophysical Experience (SAGE) program since 2000. Gravity, magnetotelluric (MT), and seismic data have been collected throughout the region, although we are concentrating on gravity and MT data collected during SAGE 2014 and 2015. The study area is located in the center of the Santo Domingo basin, an extensional, Miocene age, rift basin, in an area that was minimally involved in the preceding local Laramide orogenic activity. Rift sediments (~3.5 km thick) are underlain by Eocene age sediments that were shed from adjacent uplifts. Up to 3 km of Mesozoic and Paleozoic sediments are preserved above the Precambrian basement. Geologic outcrop, borehole and seismic reflection data, and known density values were used in the construction of a ~100 km-long, generalized geologic cross section from which a gravity response was calculated. The modeled gravity response makes fairly definitive predictions about the geometry of the basin as well as the stratigraphy and faulting within and bounding the basin. MT data was collected at ten stations within the basin. The MT sounding curves exhibit one-dimensional behavior at short periods (1000 ohm-m) at ~ 3.5-4 km. Conductivities of the major stratigraphic units have been determined from well logs and previous MT modeling. Forward and inverse MT models constrained by the gravity-modeled geologic cross section are used to develop a conductivity model consistent with the geology, and are a step towards a better unified treatment of MT, seismic and gravity data.

  20. O Território usado e o uso atual do Território do Agreste Potiguar

    Diego Salomão Candido de Oliveira Salvador


    O trabalho em tela traz reflexões sobre o conceito de território usado, atentando para o uso que vem sendo feito, pelos diferentes agentes sociais, do território do Agreste Potiguar. Considera-se que o território é social, ou seja, guarda em si as marcas do trabalho humano, das relações de poder dos homens entre si e com o meio circundante. Além disso, acredita-se que o território usado também revela as ações estatais que são postas em tela em diferentes contextos, privilegiando, geralmente, ...

  1. Chemodiversity of dissolved organic matter in the Amazon Basin

    Gonsior, Michael; Valle, Juliana; Schmitt-Kopplin, Philippe; Hertkorn, Norbert; Bastviken, David; Luek, Jenna; Harir, Mourad; Bastos, Wanderley; Enrich-Prast, Alex


    Regions in the Amazon Basin have been associated with specific biogeochemical processes, but a detailed chemical classification of the abundant and ubiquitous dissolved organic matter (DOM), beyond specific indicator compounds and bulk measurements, has not yet been established. We sampled water from different locations in the Negro, Madeira/Jamari and Tapajós River areas to characterize the molecular DOM composition and distribution. Ultrahigh-resolution Fourier transform ion cyclotron resonance mass spectrometry (FT-ICR-MS) combined with excitation emission matrix (EEM) fluorescence spectroscopy and parallel factor analysis (PARAFAC) revealed a large proportion of ubiquitous DOM but also unique area-specific molecular signatures. Unique to the DOM of the Rio Negro area was the large abundance of high molecular weight, diverse hydrogen-deficient and highly oxidized molecular ions deviating from known lignin or tannin compositions, indicating substantial oxidative processing of these ultimately plant-derived polyphenols indicative of these black waters. In contrast, unique signatures in the Madeira/Jamari area were defined by presumably labile sulfur- and nitrogen-containing molecules in this white water river system. Waters from the Tapajós main stem did not show any substantial unique molecular signatures relative to those present in the Rio Madeira and Rio Negro, which implied a lower organic molecular complexity in this clear water tributary, even after mixing with the main stem of the Amazon River. Beside ubiquitous DOM at average H / C and O / C elemental ratios, a distinct and significant unique DOM pool prevailed in the black, white and clear water areas that were also highly correlated with EEM-PARAFAC components and define the frameworks for primary production and other aspects of aquatic life.

  2. Reduced Resolution Groundwater Modeling in the Rio Grande for Real Time Scenario Evaluation

    Roach, J. D.; Tidwell, V. C.


    As the finite, and often over-allocated water resources of the western United States are challenged by growing demands, computer based simulations can provide a powerful tool for evaluating potential water use scenarios in support of hydrologic decision making and water policy analysis. To represent the complexities of water resource management, a model should capture the salient behaviors and interactions between, the groundwater, surface water, and human behavioral systems, while to effectively connect science to the decision process, the model should run quickly enough to allow real time evaluation of a wide range of scenarios by stakeholders and decision makers themselves. As these potentially mutually exclusive objectives are pursued, the tradeoffs between resolution, run time, and the degree of coupling between modeled systems must be considered. In the Upper Rio Grande in New Mexico, three MODFLOW based, distributed groundwater models of the Espanola, Albuquerque, and Socorro groundwater basins have been used to calibrate a spatially simplified representation of the groundwater system in the region. The groundwater model is dynamically coupled to surface water and human behavioral systems as part of an integrated system dynamics based model which runs quickly enough to support rapid basin scale water policy scenario evaluation. This presentation will focus on development of the simplified groundwater model, and the performance tradeoffs and gains associated with spatial aggregation and dynamic coupling to the surface water system.

  3. Tectono-sedimentary evolution of the Neuquén basin (Argentina) between 39°S and 41°S during the Neogene

    Huyghe, D.; Bonnel, C.; Nivière, B.; Messager, G.; Dhont, D.; Fasentieux, B.; Hervouët, Y.; Xavier, J.-P.


    Sedimentary rocks deposited in foreland basins are of primary interest, because they record the interactions between the growth of the orogenic wedge, the isostatic readjustment of the lithosphere, the variations of base-level and earth surface process. The Neuquén basin (32°S - 41°S) is a triangular shape foreland basin located on the eastern flank of the Andes. Its filling began during the late Triassic, first as back arc basin context and as compressive foreland basin since the upper Cretaceous. The structural inheritance is thus important and old basement structures, like the Huincul Ridge, generate significant variations of both deformation and shortening. Its Mesozoic history is well constrained due to its hydrocarbon potential. In comparison, its Cenozoic history remains poorly documented. The modern configuration of this basin results from several successive compressive tectonic phases. The last one is dated from the Miocene (Quechua phase) and has conditioned the segmentation of the foreland basin in several intra-mountainous sub-basins, whose sedimentary filling could reach several hundred meters. In this work, we document the relative chronology of the geological events and the sedimentary processes that have governed the Cenozoic history of the southern part of the Neuquen basin, to discriminate the relative rules of climatic and structural controlling factors on the evolution of the depocentres. Several NNW-SSE oriented intra-mountainous basins exist in this part of the Andes (Collon Cura basin and Catan Lil basin). On the contrary the associated foreland basin (Picun Leufu basin) is relatively underformed and is bounded to the North by the Huincul ridge and the North Patagonian massif to the South. Fifteen sedimentary sections have been studied along the Rio Limay River in the southern border of the basin, from the range to the external part of the foreland. The sedimentation is discontinuous in time and important retrogradations of the depocentres

  4. Application of neutron activation analysis to the determination of total mercury and other elements of interest in soil and sediment samples from Serra do Navio and Vila Nova River Basin, Amapa, Brazil; Aplicacao do metodo de ativacao neutronica a determinacao do mercurio total e outros elementos de interesse em amostras de solo e sedimento da Serra do Navio e Bacia do Rio Vila Nova, Amapa

    Goncalves, Cristina


    In this work it is presented a survey on total mercury determination by a radiochemical method in sediment and soil samples from two regions, in the state of Amapa: Serra do Navio (background area) and Vila Nova river basin (gold mining area). The method consisted in leaching of the irradiated samples with acqua regia in a Parr bomb, and heating in microwave oven, for one minute. Then the solvent extraction technique was applied, using bismuth diethyldithiocarbamate (Bi(DDC){sub 3}) as extractant agent. The organic phase, containing {sup 197}Hg and {sup 203}Hg radioisotopes, was measured in a gamma spectrometer with hyper pure Ge detector. This method eliminated the interference of the 279.54 keV photopeak of {sup 75}Se on 279.2 keV photopeak of {sup 203}Hg, besides improving counting statistics of both Hg radioisotopes. The elements As, Ba, Br, Ce, Co, Cr, Cs, Eu, Fe, Hf, Ho, K, La, Lu, Mg, Mn, Na, Nd, Rb, Sb, Sc, Se, Sm, Ta, Tb, Th, Ti, U, V, W, Yb, Zn and Zr were also determined by the instrumental neutron activation analysis. Two irradiation series were carried out to quantify these elements in soil and sediment samples; a short term irradiation allowed to evaluate Mg, Mn, Na, Ti and V levels, and by long term irradiation, the other elements were determined. Precision and accuracy of radiochemical procedure were verified by means of analysis of the reference materials Buffalo River Sediment and Lake Sediment, for sediments and GXR-5, for soils. For the instrumental analysis, the reference materials Buffalo River Sediment, Soil 7, JB-1 and Oyster Tissue were used. The samples were also submitted to X ray diffraction, in Instituto de Geoscience-USP, to observe mercury behaviour with mineralogy. Aluminium concentration was determined by X ray fluorescence method, in the Department of Materials, IPEN/CNEN-SP, making possible enrichment factor calculation so that mercurial contamination in the gold mining area (Vila Nova river basin) could be evaluated. The mercury


    Robert Caldwell


    Vast quantities of natural gas are entrapped within various tight formations in the Rocky Mountain area. This report seeks to quantify what proportion of that resource can be considered recoverable under today's technological and economic conditions and discusses factors controlling recovery. The ultimate goal of this project is to encourage development of tight gas reserves by industry through reducing the technical and economic risks of locating, drilling and completing commercial tight gas wells. This report is the fourth in a series and focuses on the Wind River Basin located in west central Wyoming. The first three reports presented analyses of the tight gas reserves and resources in the Greater Green River Basin (Scotia, 1993), Piceance Basin (Scotia, 1995) and the Uinta Basin (Scotia, 1995). Since each report is a stand-alone document, duplication of language will exist where common aspects are discussed. This study, and the previous three, describe basin-centered gas deposits (Masters, 1979) which contain vast quantities of natural gas entrapped in low permeability (tight), overpressured sandstones occupying a central basin location. Such deposits are generally continuous and are not conventionally trapped by a structural or stratigraphic seal. Rather, the tight character of the reservoirs prevents rapid migration of the gas, and where rates of gas generation exceed rates of escape, an overpressured basin-centered gas deposit results (Spencer, 1987). Since the temperature is a primary controlling factor for the onset and rate of gas generation, these deposits exist in the deeper, central parts of a basin where temperatures generally exceed 200 F and drill depths exceed 8,000 feet. The abbreviation OPT (overpressured tight) is used when referring to sandstone reservoirs that comprise the basin-centered gas deposit. Because the gas resources trapped in this setting are so large, they represent an important source of future gas supply, prompting studies

  6. O diário do outro

    Nádia Battella Gotlib


    Full Text Available A produção literária de Simone de Beauvoir marca-se pelo seu caráter acentuadamente autobiográfico. E também por manter aí um constante diálogo com o seu companheiro Sartre. Sob esta perspectiva, A Cerimônia do Adeus (1981, que relata os dez últimos anos de vida de Sartre, apresenta uma estrutura narrativa curiosa: propõe-se como um diário, mas do outro, pois a narradora tenta anular-se em favor da reconstrução de um retrato de Sartre. No entanto, por injunção desta proposta, inviável, o texto acaba transformando-se num ponto de convergência de vários gêneros narrativos, tendo em vista o caráter múltiplo de personalidade do biografado. E este personalizado trabalho narrativo, à revelia da própria autora, acarreta o processo inverso: o texto transforma-se num retrato de Simone. Consuma-se, desta forma, no próprio corpo do texto, o movimento de sedução, em que ambos, homem e mulher, realizam-se como sujeitos necessários Um ao Outro.L'oeuvre de Simone de Beauvoir est marquée par son caractère fortemente autobiographique, aussi bien que par le dialogue constante avec son partenaire Sartre. Sous une telle optique, La Cérémonie des Adieux (1981, qui raconte les dix dernières années de la vie de Sartre, présente une structure narrative curieuse: le livre se présente comme un journal, mais le journal de l'autre, puisque la narratrice essaie de s'effacer face à la reconstruction d'un portrait de Sartre. Pourtant, à cause de cet objectif inacessible, le texte finit par devenir un point de convergence de plusieurs genres de récit, étant donné le caractère multiple de la personnalité du sujet de la biographie. Ce travail narratif personnalisé va entraîner le processus inverse, malgré son auteur même: le récit devient un portrait de Simone. Ainsi, c'est dans le corps même du texte qu'a lieu le mouvement de séduction où homme et femme se réalisent comme sujets indispensables l'Un à l'Autre.

  7. Memory effect triggered by exceptional event: the Rio Cordon study case

    Rainato, Riccardo; Mao, Luca; Picco, Lorenzo; Garcia-Rama, Adriana; Aristide Lenzi, Mario


    In the mountain environment, the steep channels play a key-role in the drainage networks. Notably, the sediment transport processes that here occur, can affect aspects as the geomorphic changes, channel evolution, reservoir management, infrastructure design and hazard assessment. Due to the complex and changeable hydraulic and morphological features that characterize the mountain environment, the steep channels can exhibit fluvial and/or debris-flow transport with magnitude of sediment delivery that, in the same basin, may strongly vary from event to event. In the light of these challenging conditions, appears clear as an accurate monitoring and investigation of sediment dynamics is of critical importance in the steep mountain channels. Such monitoring has even more significance if it is maintained over long-period, enabling to investigate even the role of high magnitude/low frequency events. Using a dataset 29 years-wide, this work aims to investigate the temporal trend of sediment dynamic in the Rio Cordon (Eastern Italian Alps). The Rio Cordon is a steep mountain channel (mean slope = 13%) characterized by step-pool and riffle-pool morphology. The basin (5 km2)exhibits a prevalent nivo-pluvial runoff regime. Since 1986, the catchment is equipped with a monitoring station, that continuously records water discharge, bedload and suspended load (at 1 hr intervals, and 5 min intervals during floods). In September 1994 an exceptional event (RI > 100 years) occurred in the study site, mobilizing about 4000 tons of material. Currently, the structure is managed by ARPA Veneto - Regional Department for Land Safety. In terms of magnitude, the 31 floods recorded by the monitoring station show a wide range of hydraulic forcing (i.e. peak discharge and effective runoff) and amount transported. Specifically, Qpeak ranges within one order of magnitude (1.02 - 10.42 m3 s-1), while the amount of bedload and suspended load varies by more than 3 orders (i.e. 0.9 t triggered a

  8. GO RIO: Achieving Universal Access to Mass Transit

    Martinez, Ted, Jr.; Castaneda-Calleros, Russell


    GO RIO is a universal access, mass-transit program that has been offered to all students who are registered full-time at Rio Hondo College. Through an agreement with five local transit agencies, full-time students can obtain a pass that provides full access seven days a week throughout the entire semester.

  9. Transshipment port in the Rio de la Plata

    Lemmens, D.; Smaling, H.; De Jong, J.; De Kloet, M.


    The predictions for the future foretell an increase of the amount of exported grain over the Rio Paraná/Rio de la Plata system of 63% in 2030. Besides this, the new Panama locks will be finished in 2015. Seeing as the current shipping standard is largely determined by the Panama locks, the general e

  10. Application of nuclear logging to porosity studies in Itaborai basin

    Oliveira, Milena F.S.; Lima, Inaya; Lopes, Ricardo Tadeu, E-mail:, E-mail:, E-mail: [Coordenacao dos Programas de Pos-Graduacao de Engenharia (COPPE/UFRJ), Rio de Janeiro, RJ (Brazil). Lab. de Instrumentacao Nuclear; Ferrucio, Paula Lucia; Borghi, Leonardo, E-mail:, E-mail: [Universidade Federal do Rio de Janeiro (UFRJ), RJ (Brazil). Inst. de Geociencias. Dept. de Geologia; Abreu, Carlos Jorge, E-mail: [Universidade de Brasilia (UnB), DF (Brazil). Inst. de Geociencias


    Nuclear logging provides information on bulk density and porosity variations by measuring the intensity of the scattered radiation induced on the formation by radioactive sources. In this study, nuclear logging was employed to analyze the pore-space system of the 2-ITAB-1-RJ well placed on the Itaborai limestone basin, in the state of Rio de Janeiro. This is one of the smallest sedimentary basin in Brazil and it is formed by clastic deposits and travertine limestone rocks which are fractured. Understanding the pore-space system of carbonate rocks has become important subject for the oil industry, specially in Brazil. A Density Gamma Probe (LSD) and a Neutron Probe (NEUT) were used for data acquisition, which nuclear logging was carried out in part of the well, with continuous detection for about 50 m of deep. The detection speed was 4 m/min for the LSD and 5 m/min for the NEUT. The results obtained by nuclear logging showed that the 2-ITAB-1-RJ well consists of three different intervals with rocks ranging from low to moderate porosity present in travertine, marls and gneisses. (author)

  11. Pastiche em Bastardos Inglórios

    Bruno Costa


    Full Text Available Este artigo tenta repensar o pastiche a partir das interações propostas, da relação com a história e do vai-e-vem entre mundos da ficção vistos no filme Bastardos Inglórios (2009 de Quentin Tarantino. Com o termo pastiche partimos em busca de valências da ficção cinematográfica contemporânea pesando, para tanto, algumas viragens tipicamente pós-modernas. Afastando-se da concepção marcadamente negativa do termo, o pastiche pode ser útil para compreendermos o reposicionamento das relações entre textos, destacando a produtividade da citação e da composição em busca de uma nova concepção de originalidade para além da arte aurática da modernidade.


    Desidério Murcho


    Full Text Available Chegamos ao quinto número da Prometeus. Como espaço para apresentação depesquisas acadêmicas de todos os âmbitos da Filosofia, nossa revista sempre seapresentou como um veículo eclético. Neste número, além dos artigos, comunicações edemais trabalhos, oferecemos aos leitores uma entrevista que realizamos com umpesquisador que vem se destacando por suas críticas em relação ao modo como seefetua a pesquisa filosófica em língua portuguesa, Desidério Murcho, professor daUFOP e diretor da revista eletrônica Crítica na Rede.

  13. Investigando o processo tradutório

    Heloísa Gonçalves Barbosa


    Full Text Available O presente trabalho descreve brevemente a evolução da pesquisa em tradução, abordando o deslocamento de seu foco do produto para o processo, até a adoção da metodologia empírica para acessar os processos mentais desenvolvidos durante o ato tradutório. Traça as origens desta metodologia a partir da psicolingüística voltada para a aprendizagem de línguas até sua aplicação no campo dos estudos da tradução. Finalmente, relata as investigações em curso no âmbito do Projeto PRONIT, que se utilizam de métodos introspectivos, apontando resultados e indicando caminhos a serem seguidos no futuro.

  14. Olympic Games Rio 2016: winners and losers

    Wagner Barbosa Matias


    Full Text Available This paper seeks to question the process of preparation of the Olympic Games in 2016. For that was done a literature review on the subject and their legacies as well as a document analysis of sports institutions, the Olympic Delivery Authority and the Federal Government about the mega event. In this sense , it was found that the preparation of the 2016 Games is prioritizing the actions of market interest, with measures establishing a state of emergency , which does not respect the constitutional laws, are linked to human rights, the environment, public property etc. The beneficiary groups are those who financed the Rio campaign headquarters of mega event and/ or are directly involved with members of all three government levels , as well as proprietary sports entities of the commodity Olympics.

  15. Thermo-tectonic evolution of the Purros Shear Zone and its implications in Walvis Basin, NW Namibia

    Fernandes, Fernanda M. [Rio Grande do Sul Univ., Porto Alegre, RS (Brazil)]|[Agencia Nacional do Petroleo, Rio de Janeiro, RJ (Brazil). Programa de Recursos Humanos]. E-mail:; Chemale Junior, Farid; Lelarge, Maria Lidia M.V. [Rio Grande do Sul Univ., Porto Alegre, RS (Brazil). Lab. de Geologia Isotopica e Tracos de Fissao]. E-mail:; Luft Junior, Joao Luiz [Rio Grande do Sul Univ., Porto Alegre, RS (Brazil). Programa de Pos-graduacao em Geociencias]. E-mail:


    The Namibian marginal basins record a long history of tectonic activity since the Proterozoic. The collision between the Congo and Rio de La Plata craton generated NNW-trend crustal weakness zones in the Kaoko mobile belt which became the preferential site to the Phanerozoic tectonic activity. The pre-existing structures reactivated in mobile belts are intimately related with the evolution of adjacent marginal basins. The Pre-Cambrian Purros Shear Zone is an important crustal discontinuity located in Kaoko mobile belt that put side by side basement rocks with basaltic lavas related to the South Atlantic opening. Apatite fission track thermo chronology could provide a better understanding about reactivation phases, denudation rates and paleotemperature data. Through all these information will be possible to make the correlation with the main unconformities in the stratigraphic record of the Walvis marginal basin. (author)

  16. Um imaginário ativo na cultura nacional

    Sodré, Muniz; UFRJ


    O texto aponta, dentre outras questões, que não há no Brasil ativos pesquisadores do imaginário. Talvez isso se deva à dificuldade em separar real de imaginário num país de longa tradição patrimonialista, pois, como bem se sabe, a cultura patrimonial apela fortemente para o imaginário da família ampliada em seu movimento de preservação e transmissão do capital. Ou esteja relacionado aos vários tipos de imaginário social que concorrem para constituir relações sociais originalíssimas no nível d...

  17. Para que servem os inventários de fauna?

    Luís Fábio Silveira; Beatriz de Mello Beisiegel; Felipe Franco Curcio; Paula Hanna Valdujo; Marianna Dixo; Vanessa Kruth Verdade; George Mendes Taliaferro Mattox; Patrícia Teresa Monteiro Cunningham


    Inventários de fauna acessam diretamente a diversidade de uma localidade, em um determinado espaço e tempo. Os dados primários gerados pelos inventários compõem uma das ferramentas mais importantes na tomada de decisões a respeito do manejo de áreas naturais. Entretanto, vários problemas têm sido observados em diversos níveis relacionados aos inventários de fauna no Brasil e vão desde a formação de recursos humanos até a ausência de padronização, de desenho experimental e de seleção de método...

  18. Léxico e vocabulário fundamental

    Maria Tereza Camargo Biderman


    Full Text Available

    O papel do léxico na estrutura e funcionamento da língua; seu lugar nos estudos da linguagem. Descrição de pesquisa realizada pela Universidade de Lisboa para obtenção de um vocabulário fundamental do português. Discussão dos conceitos e da terminologia técnica em Lexicologia. Procedimentos utilizados na identificação das unidades lexicais; será o dicionário um parâmetro confiável para a identificação dos lexemas? Comentários críticos sobre os resultados da pesquisa de Lisboa, particularmente dos dados do Inquérito da Disponibilidade. Considerações sobre a especificidade e o generalismo no vocabulário. Um vocabulário fundamental para o português do Brasil.

  19. Sigaud, operário da pintura

    Cristina Meneguello


    Full Text Available Até o presente momento, nenhuma biografia de fôlego foi produzida sobre Eugênio de Proença Sigaud. Em portais especializados em arte ou em dicionários de pintores, biografias concisas de uma lauda repetem as mesmas informações à exaustão. Este breve artigo não busca redimir Sigaud deste silêncio. Propõe, outrossim, entender por que persistem figuras consideradas "menores" na história da arte recente no País, bem como compreender os processos de perpetuação da memória e de valorização da obra de certos agentes históricos em detrimento de outros. Os cânones sobre o moderno no Brasil criam seus próprios critérios de narrativa do passado, em que a economia dos discursos da qualidade artística e o uso interessado e exclusivista de acervos criam invisibilidades e omissões, processo este do qual Sigaud, cuja obra visual eloquente não é secundada por textos, entrevistas e farta documentação, é exemplar. Na busca destes silêncios, este breve artigo elege a má recepção da obra de Sigaud, seu posicionamento político de esquerda e sua formação como arquiteto como seus fios condutores, buscando por meio destes aspectos pouco estudados até o momento guiar-se para lançar hipóteses que contribuam para a compreensão do trabalho deste pintor.

  20. Novos paradigmas literários

    Denise Azevedo Duarte Guimarães


    Full Text Available O artigo estuda a emergência de novos paradigmas literários, procurando refletir acerca das textualidades contemporâneas. Focaliza os hipertextos informatizados e a poesia multimídia, com o intuito de desvendar como estão sendo criados novos procedimentos expressivos e em que medida eles podem ser identificados com reflexões teóricas anteriores acerca do texto literário impresso. Remete a questões ligadas à leitura dos diferentes tipos de signos e aos modos como eles se integram para a constituição dessas novíssimas linguagens híbridas em novos suportes.El artículo estudia la emergencia de nuevos paradigmas literarios, procurando reflejar acerca de las textualidades contemporáneas. Enfoca los hipertextos informatizados y la poesía multimedia, intentando desvendar cómo están siendo creados nuevos procedimientos expresivos y en qué medida ellos pueden ser identificados a reflexiones teóricas anteriores acerca del texto literario impreso. Remite a cuestiones ligadas a la lectura de los diferentes tipos de signos y a los modos cómo ellos se interaccionan para la constitución de los novísimos lenguajes híbridos en nuevos supuestos.This article investigates the emergence of new literary paradigms as it tries to understand new contemporary textualities. It analyses some hypertexts and multimedia poetry trying to trace how new expressive procedures are being created. How can these new languages be identified and what are their relations to previous theories which dealt with the literary printed text? This study approaches questions linked to the reading of different types of signs and the modes they function towards the fabrication of these new hybrid languages.

  1. Simulation of a long-term aquifer test conducted near the Rio Grande, Albuquerque, New Mexico

    McAda, Douglas P.


    A long-term aquifer test was conducted near the Rio Grande in Albuquerque during January and February 1995 using 22 wells and piezometers at nine sites, with the City of Albuquerque Griegos 1 production well as the pumped well. Griegos 1 discharge averaged about 2,330 gallons per minute for 54.4 days. A three-dimensional finite-difference ground-water-flow model was used to estimate aquifer properties in the vicinity of the Griegos well field and the amount of infiltration induced into the aquifer system from the Rio Grande and riverside drains as a result of pumping during the test. The model was initially calibrated by trial-and-error adjustments of the aquifer properties. The model was recalibrated using a nonlinear least-squares regression technique. The aquifer system in the area includes the middle Tertiary to Quaternary Santa Fe Group and post-Santa Fe Group valley- and basin-fill deposits of the Albuquerque Basin. The Rio Grande and adjacent riverside drains are in hydraulic connection with the aquifer system. The hydraulic-conductivity values of the upper part of the Santa Fe Group resulting from the model calibrated by trial and error varied by zone in the model and ranged from 12 to 33 feet per day. The hydraulic conductivity of the inner-valley alluvium was 45 feet per day. The vertical to horizontal anisotropy ratio was 1:140. Specific storage was 4 x 10-6 per foot of aquifer thickness, and specific yield was 0.15 (dimensionless). The sum of squared errors between the observed and simulated drawdowns was 130 feet squared. Not all aquifer properties could be estimated using nonlinear regression because of model insensitivity to some aquifer properties at observation locations. Hydraulic conductivity of the inner-valley alluvium, middle part of the Santa Fe Group, and riverbed and riverside-drain bed and specific yield had low sensitivity values and therefore could not be estimated. Of the properties estimated, hydraulic conductivity of the upper part of

  2. Interactieve ontwerpmethodieken voor integrale duurzaamheid Toepassing van RIO in een aantal niet-veehouderij-gebonden cases

    Bos, A.P.; Annevelink, E.; Bos, H.L.; Keijsers, E.R.P.; Maas, van der M.P.; Poot, E.H.; Vermeulen, T.; Raaphorst, M.G.M.; Maas, van der A.A.; Schoorlemmer, H.B.; Dijk, van S.M.


    RIO (Reflexief Interactief Ontwerpen) bestaat uit drie hoofdonderdelen: de (systeem)analysefase, de ontwerpfase en de verankeringsfase. RIO is ontstaan in een veehouderijcontext. Die context heeft een aantal specifieke eigenschappen, die toepassing van RIO in andere sectoren niet volledig vanzelfspr

  3. Water Accounting from Ungauged Basins

    Bastiaanssen, W. G.; Savenije, H.


    Water scarcity is increasing globally. This requires a more accurate management of the water resources at river basin scale and understanding of withdrawals and return flows; both naturally and man-induced. Many basins and their tributaries are, however, ungauged or poorly gauged. This hampers sound planning and monitoring processes. While certain countries have developed clear guidelines and policies on data observatories and data sharing, other countries and their basin organization still have to start on developing data democracies. Water accounting quantifies flows, fluxes, stocks and consumptive use pertaining to every land use class in a river basin. The objective is to derive a knowledge base with certain minimum information that facilitates decision making. Water Accounting Plus (WA+) is a new method for water resources assessment reporting ( While the PUB framework has yielded several deterministic models for flow prediction, WA+ utilizes remote sensing data of rainfall, evaporation (including soil, water, vegetation and interception evaporation), soil moisture, water levels, land use and biomass production. Examples will be demonstrated that show how remote sensing and hydrological models can be smartly integrated for generating all the required input data into WA+. A standard water accounting system for all basins in the world - with a special emphasis on data scarce regions - is under development. First results of using remote sensing measurements and hydrological modeling as an alternative to expensive field data sets, will be presented and discussed.

  4. Geothermal resources of the northern gulf of Mexico basin

    Jones, P.H.


    Published geothermal gradient maps for the northern Gulf of Mexico basin indicate little or no potential for the development of geothermal resources. Results of deep drilling, from 4000 to 7000 meters or more, during the past decade however, define very sharp increases in geothermal gradient which are associated with the occurrence of abnormally high interstitial fluid pressure (geopressure). Bounded by regional growth faults along the landward margin of the Gulf Basin, the geopressured zone extends some 1300 km from the Rio Grande (at the boundary between the United States and Mexico) to the mouth of the Mississippi river. Gulfward, it extends to an unknown distance across the Continental Shelf. Within geopressured deposits, geothermal gradients range upwards to 100 ??C/km, being greatest within and immediately below the depth interval in which the maximum pressure gradient change occurs. The 120 ??C isogeotherm ranges from about 2500 to 5000 m below sea level, and conforms in a general way with depth of occurrence of the top of the geopressured zone. Measured geostatic ratios range upward to 0.97; the maximum observed temperature is 273 ??C, at a depth of 5859 m. Dehydration of montmorillonite, which comprises 60 to 80 percent of clay deposited in the northern Gulf Basin during the Neogene, occurs at depths where temperature exceeds about 80 ??C, and is generally complete at depths where temperature exceeds 120 ??C. This process converts intracrystalline and bound water to free pore water, the volume produced being roughly equivalent to half the volume of montmorillonite so altered. Produced water is fresh, and has low viscosity and density. Sand-bed aquifers of deltaic, longshore, or marine origin form excellent avenues for drainage of geopressured deposits by wells, each of which may yield 10,000 m3 or more of superheated water per day from reservoirs having pressures up to 1000 bars at depths greater than 5000 m. ?? 1971.

  5. Incentive pricing and cost recovery at the basin scale.

    Ward, Frank A; Pulido-Velazquez, Manuel


    Incentive pricing programs have potential to promote economically efficient water use patterns and provide a revenue source to compensate for environmental damages. However, incentive pricing may impose disproportionate costs and aggravate poverty where high prices are levied for basic human needs. This paper presents an analysis of a two-tiered water pricing system that sets a low price for subsistence needs, while charging a price equal to marginal cost, including environmental cost, for discretionary uses. This pricing arrangement can promote efficient and sustainable water use patterns, goals set by the European Water Framework Directive, while meeting subsistence needs of poor households. Using data from the Rio Grande Basin of North America, a dynamic nonlinear program, maximizes the basin's total net economic and environmental benefits subject to several hydrological and institutional constraints. Supply costs, environmental costs, and resource costs are integrated in a model of a river basin's hydrology, economics, and institutions. Three programs are compared: (1) Law of the River, in which water allocations and prices are determined by rules governing water transfers; (2) marginal cost pricing, in which households pay the full marginal cost of supplying treated water; (3) two-tiered pricing, in which households' subsistence water needs are priced cheaply, while discretionary uses are priced at efficient levels. Compared to the Law of the River and marginal cost pricing, two-tiered pricing performs well for efficiency and adequately for sustainability and equity. Findings provide a general framework for formulating water pricing programs that promote economically and environmentally efficient water use programs while also addressing other policy goals.

  6. The 'WaterWare' decision-support system for river-basin planning. 3. Example applications

    Jamieson, D. G.; Fedra, K.


    Having outlined the conceptual design and planning capability in the previous two papers, the final contribution in this trilogy describes the application of WaterWare to the River Thames basin in England and Rio Lerma in Mexico. Examples are given of the real-world problems that can be addressed using this system. These include water-resource assessment, reservoir site selection, decontamination of groundwater, estimation of sustainable irrigation abstractions and derivation of required effluent-quality standards. The requirement in both cases is to provide the analytical tools to be used by the agency staff themselves for planning purposes.

  7. Archaeozoology of marine mollusks from Sambaqui da Tarioba, Rio das Ostras, Rio de Janeiro, Brazil

    Rosa C. C. L. de Souza


    Full Text Available A reference inventory of prehistoric marine mollusks from the Rio das Ostras region was created based on an excavation carried out at the Sambaqui da Tarioba shellmound. Patterns of richness and biogeography were studied, and the representativeness of bivalve and gastropod diversities found at this archaeological site were inferred. A total of 47 taxa belonging to 28 families, most of which from unconsolidated substrates, was identified. The shellmound species composition does not differ from the present-day composition. All recorded species are characteristic of a wide transition zone between the south of the states of Espírito Santo (21°S and Rio Grande do Sul (32°S. Thus, the data show little evidence of evolution in the composition, richness,and biodiversity distribution patterns of mollusks in the Rio das Ostras region. Likewise, a reconstitution of the paleoenvironment from the functional characteristics of the shellmound species indicates that the locality's geomorphology and climate remained largely unchanged in the last 4,000 years BP.

  8. Um rio são muitos: de aventura e antropologia Rio São Francisco

    Roberto Lima


    Full Text Available Este artigo tenta trazer a noção de aventura de volta ao campo da antropologia por meio da análise de cinco narrativas sobre o Rio São Francisco - Burton, Pierson, Cavalcanti, Cappio e Tarsia (e companhia. Tenta-se entender como a mimesis e a sedução ligam esses atores ao rio e ao leitor, de tal maneira que, ao mesmo tempo em que os autores constroem-se nas narrativas, eles - narradores e rio - hermeneuticamente jogam suas redes sobre o leitor.This article tries to bring back the notion of adventure to the anthropological field, through the analyses of five narratives about the São Francisco river - Burton, Pierson, Cavalcanti, Cappio and Tarsia (& partners The article seeks to understand how mimesis and seduction join these actors to the river and to the reader, in such a way that, at the same time the authors construct themselves in the narrative, hermeneuticly they - storytellers and river - cast their nets over the reader.

  9. Numerical simulation of vertical ground-water flux of the Rio Grande from ground-water temperature profiles, central New Mexico

    Bartolino, James R.; Niswonger, Richard G.


    An important gap in the understanding of the hydrology of the Middle Rio Grande Basin, central New Mexico, is the rate at which water from the Rio Grande recharges the Santa Fe Group aquifer system. Several methodologies-including use of the Glover-Balmer equation, flood pulses, and channel permeameters- have been applied to this problem in the Middle Rio Grande Basin. In the work presented here, ground-water temperature profiles and ground-water levels beneath the Rio Grande were measured and numerically simulated at four sites. The direction and rate of vertical ground-water flux between the river and underlying aquifer was simulated and the effective vertical hydraulic conductivity of the sediments underlying the river was estimated through model calibration. Seven sets of nested piezometers were installed during July and August 1996 at four sites along the Rio Grande in the Albuquerque area, though only four of the piezometer nests were simulated. In downstream order, these four sites are (1) the Bernalillo site, upstream from the New Mexico State Highway 44 bridge in Bernalillo (piezometer nest BRN02); (2) the Corrales site, upstream from the Rio Rancho sewage treatment plant in Rio Rancho (COR01); (3) the Paseo del Norte site, upstream from the Paseo del Norte bridge in Albuquerque (PDN01); and (4) the Rio Bravo site, upstream from the Rio Bravo bridge in Albuquerque (RBR01). All piezometers were completed in the inner-valley alluvium of the Santa Fe Group aquifer system. Ground-water levels and temperatures were measured in the four piezometer nests a total of seven times in the 24-month period from September 1996 through August 1998. The flux between the surface- and ground-water systems at each of the field sites was quantified by one-dimensional numerical simulation of the water and heat exchange in the subsurface using the heat and water transport model VS2DH. Model calibration was aided by the use of PEST, a model-independent computer program that uses

  10. Exploration potential of offshore northern California basins

    Bachman, S.B.; Crouch, J.K.


    A series of exploratory wells was drilled in the northern California offshore basins in the 1960s following leasing of federal tracts off northern California, Oregon, and Washington. The drilling, although encountering numerous oil shows, was considered at the time to indicate low prospectivity in an area that extended as far south as the offshore Santa Maria basin. However, subsequent major discoveries in this decade in the offshore Santa Maria basin, such as the Point Arguello field, indicate that these offshore basins may be highly prospective exploration targets. Many of the key features of Monterey production in central and southern California are also present in the offshore basins of northern California. A new 5-year leasing plan has scheduled leasing in the northern California OCS starting in early 1989. The first basins on the schedule, the Point Arena and Eel River basins, differ in some respects. The Point Arena basin is more typical of a Monterey basin, with the potential for fractured chert reservoirs and organic-rich sections, deep burial of basinal sections to enhance the generation of higher gravity oils, and complex folding and faulting. The Eel River basin is more clastic-rich in its gas-producing, onshore extension. Key questions in the Eel River basin include whether the offshore, more distal stratigraphy will include Monterey-like biogenic sediments, and whether the basin has oil potential in addition to its proven gas potential. The Outer Santa Cruz basin shares a similar stratigraphy, structure, and hydrocarbon potential with the Point Arena basin. The Santa Cruz-Bodega basin, also with a similar stratigraphy, may have less exploration potential because erosion has thinned the Monterey section in parts of the basin.

  11. A new species of the armored catfish Parotocinclus (Loricariidae: Hypoptopomatinae, from the Amazon basin in Colombia

    Pablo Lehmann A.

    Full Text Available A new species of hypoptopomatine cascudinho is described from a creek tributary to the Amazon River in Leticia, Amazonas Departament, Colombia. The new species of Parotocinclus is distinguished from congeners from northeastern to southeastern Brazilian rivers in having the cheek canal plate elongated posteriorly on the ventral surface of head and contacting the cleithrum. It is diagnosed from P. collinsae (Essequibo River basin, Guiana and P. halbothi (rio Trombetas basin, Brazil and Marowijne River, Suriname, by having a triangular patch of dark pigmentation on the anterior portion of the dorsal-fin membrane, by the absence of unicuspid accessory teeth on both the premaxilla and dentary, and by having a Y-shaped light mark on the snout. The new species of Parotocinclus is distinguished from all remaining congeners by having a pigmentation pattern consisting of conspicuous dark dots smaller than a pupil diameter, broadly distributed dorsally and ventrally.

  12. Evaluation of geothermal potential of the basin and range province of New Mexico. Technical report

    Landis, G.P.; Callender, J.F.; Elston, W.E.; Jiracek, G.R.; Kudo, A.M.; Woodward, L.A.; Swanberg, C.A.


    This continuing research is designed to provide an integrated geological, geophysical, and geochemical study of the geothermal energy potential of promising thermal anomalies in the Rio Grande rift, Basin and Range province, the Mogollon--Datil volcanic field of New Mexico. Specific objectives undertaken in this study include the following: (a) reconnaissance and detailed geologic mapping (Animas Valley, Radium Springs, Alum Mountain, Truth or Consequences, Ojo Caliente, Albuquerque---Belene basin, and San Ysidro); (b) geochemical studies including reconnaissance water sampling (Animas Valley, Radium Springs and Alum Mountain); and (c) geophysical surveys using deep electric-resistivity, gravity, and magnetic techniques (Radium Springs, Animas Valley and Truth or Consequences). The results of one and one-half summer field seasons and approximately two years of analytical work, laboratory research, and development of research equipment and facilities are covered. Publications, communications, and public service resulting from the first years of U.S.G.S. and State funding are listed in Appendix A.

  13. Composição florística e estrutura do componente arbóreo de uma Floresta Paludosa na planície costeira da bacia do rio Itaguaré, Bertioga, SP, Brasil. Floristic composition andstructure of an arboreal component of the Paludal Forest in the coastal plain of the Itaguaré river basin, Bertioga (São Paulo state, Brazil

    Celia Regina de Gouveia SOUZA


    Full Text Available As Florestas Paludosas costeiras ou “caxetais” ocorrem no Domínio Atlântico, em geral associadas a depressões paleolagunares, cujos terrenos são permanentemente encharcados. Essas florestas se caracterizam por apresentar elevada densidade de indivíduos da espécie Tabebuia cassinoides (Lam. DC., conhecida popularmente por “caxeta”. O presente estudo foi desenvolvido em uma Floresta Paludosa situada na planície costeira do rio Itaguaré, município de Bertioga, Baixada Santista, Estado de São Paulo. A composição florística e a estrutura fitossociológica foram investigadas através da amostragem por parcelas, sendo incluídos todos os indivíduos com 10 cm ou mais de diâmetro a 1,3 m de altura do peito (DAP. Foram registradas 20 espécies e 11 famílias botânicas, resultando em uma densidade total de 450 ind./ha-1. A família com maior riqueza de espécies foi Myrtaceae, com quatro espécies. A análise de similaridade indicou dois grupos florísticos. Tabebuia cassinoides foi, de fato, a espécie mais importante, apresentando grande densidade e dominância de indivíduos, o que reforça sua posição de espécie indicadora deste tipo vegetacional, conforme difundido na literatura. The coastal Paludal Forest or “Caxetal” occurs on the Atlantic Domain, associated to wetlands within palaeolagoonal depressions. It is characterized by a high density of individuals of Tabebuia cassinoides (Lam. DC., which is popularly known as “caxeta”. A Paludal Forest located in the Itaguaré river coastal plain, in the municipality of Bertioga, Santos Lowland, São Paulo State, Brazil was studied. The floristic composition and phytossociological structure was investigated through a plot method including all individuals with diameter at 1.3 m (DBH ≥ 10 cm. A total of 20species and 11 botanic families were sampled, resulting in a total density of 450 ind./ha-1. Myrtaceae showed the highest species richness. The similarity index indicated

  14. Geology, exploration status of Uruguay's sedimentary basins

    Goso, C.; Santa Ana, H. de (Administracion Nacional de Combustibles, Alcohol y Portland (Uruguay))


    This article attempts to present the geological characteristics and tectonic and sedimentary evolution of Uruguayan basins and the extent to which they have been explored. Uruguay is on the Atlantic coast of South America. The country covers about 318,000 sq km, including offshore and onshore territories corresponding to more than 65% of the various sedimentary basins. Four basins underlie the country: the Norte basin, the Santa Lucia basin, the offshore Punta del Este basin, and the offshore-onshore Pelotas-Merin basin. The Norte basin is a Pale