Calcite Twin Analysis in the Central Andes of Northern Argentina and Southern Bolivia

Science.gov (United States)

Hardesty, E.; Hindle, D.

2005-12-01

The use of calcite twinning to infer compression directions and strain axes patterns has been applied widely in both fold and thrust belts, and continental interiors. Calcite twinning is noted to be one of the most precise methods for determining the internal strain of deformed rocks. Until now, such data from the deformed plate boundary of the Central Andes were lacking. This study has examined twinning orientations along the deformed Andean foreland (southern Bolivia and northern Argentina) from -25 to -20 latitude. In the Central Andes, we find an abundance of calcite twins in intervals of the Cretaceous age Yacorite limestone. Twin samples were collected, measured for orientation and type (I and II can be best used for strain analysis), and processed using the Groshong method, to give resultant strain tensors. The orientations of the twin short axes trend mostly NE-SW, which is close to the plate convergence direction. However, in a limited number of samples from the north, adjacent to the southern culmination of the active Subandean fold thrust belt, they trend NW-SE. This difference may be related to the more active, or more recent, shortening of the southern portion of the Eastern Cordillera, south of the culmination of the Subandean belt. This implies that twin short axes vary consistently with respect to geographic location and local tectonic regime. NW-SE trends in the northern region match well with fault kinematic studies in rocks pre-dating the San Juan del Oro unconformity (9-10 Ma). NE-SW trends in the south could correspond to much younger (~1-3 Ma) fault kinematic trends. In the Eastern Cordillera, where there is present day tectonic activity, the plunges of the twin short axes are found to be almost horizontal. This suggests that the twins were formed after folding occurred.

Contenidos de uranio de lavas recientes en el sector sur de los Andes centrales

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Guerra, N.

1984-12-01

Full Text Available We have studied the distribution of U in modern lava -flows of the southern part from the Central Andes (16°-28° S. For a given SiO₂, content of the rocks, U abundance increases from west to east in a transects to the Andean Belt, while the depth of the subduction zone increases and the thickness of the continental curst decreases. Besides, U content tends to inerease steadly with the latitude, while the thick of the continental crust and the depth of the seismic zone decreases southward. Thus, on the basis of the available data, we are in a position to suggest that the U behavior in the studied lavas depends on the alkalanity and magmatic history of each volcanic center.

Se presenta un estudio de distribución de U en lavas modernas del sector sur de los Andes centrales (16°-28° S. Para rocas de contenidos similares en SiO₂ la abundancia de U crece de oeste a este en un perfil transversal al cordón andino, mientras que aumenta la profundidad de subducción, y disminuye la potencia de la corteza continental. Además, mientras la potencia de la corteza continental y la profundidad de la zona sísmica de Benioff disminuyen hacia el sur, U tiende a aumentar con la latitud. Así, y basado en los datos disponibles, estamos en posición de sugerir que el comportamiento de U en las rocas estudiadas, depende de la alcalinidad y de la historia magmática de cada centro volcánico.

Oroclinal Bending and Mountain Uplift in the Central Andes

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Mpodozis, C.; Arriagada, C.; Roperch, P.

2007-05-01

The large paleomagnetic database now available for the Central Andes permits a good understanding of the overall spatial and temporal variations of rotations. Mesozoic to Early Paleogene rocks along the forearc of northern Chile (23°-28°S) record significant clockwise rotations (>25°) [Arriagada et al., 2006, Tectonics, doi:10.1029/2005TC001923]. Along the forearc of southern Peru, counterclockwise rotations recorded within flat lying red-beds (Moquegua Formation) increase from about -30° at 17.5°S to - 45° at15.5°S and decrease through time from the late Eocene to the late Oligocene-early Miocene [Roperch et al., 2006, Tectonics, doi:10.1029/2005TC001882]. Recently published thermo-chronological studies show evidence for strong exhumation within Bolivian Eastern Cordillera and the Puna plateau starting in the Eocene while structural studies indicate that the majority of crustal shortening in the Eastern Cordillera occurred during the Eocene-Oligocene, although the final stages of deformation may have continued through the Early Miocene. Rotations in the Peruvian and north Chilean forearc thus occurred at the same time than deformation and exhumation/uplift within the Eastern Cordillera. In contrast Neogene forearc rocks in southern Peru and northern Chile do not show evidences of rotation but low magnitude (10°) counterclockwise rotations are usually found in mid to late Miocene rocks from the northern Altiplano. These Neogene rotations are concomitant with shortening in the Sub-Andean zone and sinistral strike-slip faulting along the eastern edge of the northern Altiplano. We interpret the rotation pattern along the southern Peru and north Chile forearc as a result of strong late Eocene- late Oligocene oroclinal bending of the Central Andes associated with shortening gradients along the Eastern Cordillera associated both with the Abancay deflection and the Arica bend. The amount and spatial distribution of pre-Neogene shortening needed to account for

Estrés y síntomas en personal de salud del Hospital Universitario de Los Andes.

OpenAIRE

Manzanilla, María D.; Molina de González Méndez, Tivizay; Caltagirone, Raimondo; Vera , Mariflor; Torres, Adrián R.

2007-01-01

Editorial. ¡Ya tenemos símbolo, ícono o logotipo!. Now we have symbol, icono or logo!. Salinas, Pedro José Accidentes domésticos en ancianos. Municipio Libertador. Mérida. 1993-1996. Domestics accidents in elderly people. Libertador County of Mérida State. 1993-1996. Salinas, Pedro José Rojas Márquez, Reina Estrés y síntomas en personal de salud del Hospital Universitario de Los Andes. Stress and symptoms in health staff of the Hospital Universitario de Los Andes. Méri...

Hydrological Modeling of Highly Glacierized Basins (Andes, Alps, and Central Asia

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Nina Omani

2017-02-01

Full Text Available The Soil and Water Assessment Tool (SWAT was used to simulate five glacierized river basins that are global in coverage and vary in climate. The river basins included the Narayani (Nepal, Vakhsh (Central Asia, Rhone (Switzerland, Mendoza (Central Andes, Argentina, and Central Dry Andes (Chile, with a total area of 85,000 km2. A modified SWAT snow algorithm was applied in order to consider spatial variation of associated snowmelt/accumulation by elevation band across each subbasin. In previous studies, melt rates varied as a function of elevation because of an air temperature gradient while the snow parameters were constant throughout the entire basin. A major improvement of the new snow algorithm is the separation of the glaciers from seasonal snow based on their characteristics. Two SWAT snow algorithms were evaluated in simulation of monthly runoff from the glaciered watersheds: (1 the snow parameters are lumped (constant throughout the entire basin and (2 the snow parameters are spatially variable based on elevation bands of a subbasin (modified snow algorithm. Applying the distributed SWAT snow algorithm improved the model performance in simulation of monthly runoff with snow-glacial regime, so that mean RSR decreased to 0.49 from 0.55 and NSE increased to 0.75 from 0.69. Improvement of model performance was negligible in simulations of monthly runoff from the basins with a monsoon runoff regime.

El tarwi o chocho: una de las principales fuentes de proteína vegetal de las comunidades indígenas de los Andes Centrales

OpenAIRE

Planchuelo, Ana M.; Fuentes, Esteban P.

2005-01-01

El lupino andino (Lupinus mutabilis Sweet) conocido también como tarwi o chocho, es una especie de leguminosa nativa de los Andes Centrales. Su domesticación se remonta a los principios de la cultura Nazca y desde ese entonces hasta la actualidad el cultivo está ampliamente difundido en las laderas montañosas y en los altos valles de Ecuador, Perú y Bolivia. La importancia del lupino para las comunidades andinas prehispánicas quedo documentada en pinturas de cerámicas y en tributos encontrado...

Facing unprecedented drying of the Central Andes? Precipitation variability over the period AD 1000–2100

International Nuclear Information System (INIS)

Neukom, Raphael; Salzmann, Nadine; Huggel, Christian; Rohrer, Mario; Calanca, Pierluigi; Acuña, Delia; Christie, Duncan A; Morales, Mariano S

2015-01-01

Projected future trends in water availability are associated with large uncertainties in many regions of the globe. In mountain areas with complex topography, climate models have often limited capabilities to adequately simulate the precipitation variability on small spatial scales. Also, their validation is hampered by typically very low station density. In the Central Andes of South America, a semi-arid high-mountain region with strong seasonality, zonal wind in the upper troposphere is a good proxy for interannual precipitation variability. Here, we combine instrumental measurements, reanalysis and paleoclimate data, and a 57-member ensemble of CMIP5 model simulations to assess changes in Central Andes precipitation over the period AD 1000–2100. This new database allows us to put future projections of precipitation into a previously missing multi-centennial and pre-industrial context. Our results confirm the relationship between regional summer precipitation and 200 hPa zonal wind in the Central Andes, with stronger Westerly winds leading to decreased precipitation. The period of instrumental coverage (1965–2010) is slightly dryer compared to pre-industrial times as represented by control simulations, simulations from the past Millennium, ice core data from Quelccaya ice cap and a tree-ring based precipitation reconstruction. The model ensemble identifies a clear reduction in precipitation already in the early 21st century: the 10 year running mean model uncertainty range (ensemble 16–84% spread) is continuously above the pre-industrial mean after AD 2023 (AD 2028) until the end of the 21st century in the RCP2.6 (RCP8.5) emission scenario. Average precipitation over AD 2071–2100 is outside the range of natural pre-industrial variability in 47 of the 57 model simulations for both emission scenarios. The ensemble median fraction of dry years (defined by the 5th percentile in pre-industrial conditions) is projected to increase by a factor of 4 until 2071�

Prediction of extreme floods in the Central Andes by means of Complex Networks

Science.gov (United States)

Boers, Niklas; Bookhagen, Bodo; Barbosa, Henrique; Marwan, Norbert; Kurths, Jürgen; Marengo, Jose

2014-05-01

Based on a non-linear synchronisation measure and complex network theory, we present a novel framework for the prediction of extreme events of spatially embedded, interrelated time series. This method is general in the sense that it can be applied to any type of spatially sampled time series with significant interrelations, ranging from climate observables to biological or stock market data. In this presentation, we apply our method to extreme rainfall in South America and show how this leads to the prediction of more than 60% (90% during El Niño conditions) of extreme rainfall events in the eastern Central Andes of Bolivia and northern Argentina, with only 1% false alarms. From paleoclimatic to decadal time scales, the Central Andes continue to be subject to pronounced changes in climatic conditions. In particular, our and past work shows that frequency as well as magnitudes of extreme rainfall events have increased significantly during past decades, calling for a better understanding of the involved climatic mechanisms. Due to their large spatial extend and occurrence at high elevations, these extreme events often lead to severe floods and landslides with disastrous socioeconomic impacts. They regularly affect tens of thousands of people and produce estimated costs of the order of several hundred million USD. Alongside with the societal value of predicting natural hazards, our study provides insights into the responsible climatic features and suggests interactions between Rossby waves in polar regions and large scale (sub-)tropical moisture transport as a driver of subseasonal variability of the South American monsoon system. Predictable extreme events result from the propagation of extreme rainfall from the region of Buenos Aires towards the Central Andes given characteristic atmospheric conditions. Our results indicate that the role of frontal systems originating from Rossby waves in polar latitudes is much more dominant for controlling extreme rainfall in

Aves y endemismo en los bosques relictos de la vertiente occidental andina del norte del Perú y sur del Ecuador

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Jeremy N. M. Flanagan

2013-05-01

Full Text Available Los bosques relictos de las vertientes occidentales de los Andes del norte del Perú y el sur del Ecuador forman parte de dos regiones, una la denominada región de endemismo tumbesina (caracterizada principalmente por bosques secos y otra, en altitudes mayores, la región de endemismo del sur de los Andes centrales (caracterizada por bosques nublados y páramo. La región tumbesina es reconocida por albergar gran cantidad de aves endémicas, muchas de las cuales están amenazadas, y también por el alto grado de deforestación y fragmentación de sus hábitats naturales. Este artículo presenta un resumen del estado de conservación de dichas aves y bosques, con recomendaciones para mejorar la conservación de los últimos bosques de la vertiente occidental.

El pH de la carne de cobayo (Cavia porcellus procedente del manejo deficiente del bienestar animal durante el sacrificio en la sierra central del Perú.

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LUCAS JR

2017-09-01

Full Text Available En la región andina del Perú es común observar el sacrificio de los cobayos sin aturdimiento ni descanso ante mortem. El objetivo del presente estudio fue evaluar el pH de la carne de cobayo (Cavia porcellus resultante de este manejo. Se evaluó el pH de 60 canales a las 0, 1, 6, 12, y 24 h posteriores al sacrificio sin descanso ante mortem ni aturdimiento. El pH fue de 6.79 ± 0.3, 6.74 ± 0.34, 6.59 ± 0.28, 6.45 ± 0.35 y 5.96 ± 0.11, a la 0, 1, 6, 12 y 24 horas post sacrificio respectivamente. La ecuación que representa la evolución del pH fue Y=6.7765-0.0231X-0.0005X2 (R2=0.996. SUMMARY. The pH of guinea pig (Cavia porcellus meat from the welfare-deficient slaughtering in the Peruvian central Andes. In Andean region of Peru is common to slaughter Guinea pig without lairage and stunning. The aim of this study was to evaluate the pH of meat of Guinea pig (Cavia porcellus from the unsuitable welfare practices during slaughtering in the Peruvian central Andes. The pH of 60 guinea pig carcasses were analyzed at 0, 1, 6, 12 and 24 hours after the end of the slaughter process. The pH was 6.79 ± 0.3, 6.74 ± 0.34, 6.59 ± 0.28, 6.45 ± 0.35 and 5.96 ± 0.11 for 0, 1, 6, 12 y 24 h post slaughtering. The equation that graphs pH evolution was Y=6.7765-0.0231X-0.0005X2 (R2=0.996.

Un réseau d'observation des glaciers dans les Andes tropicales

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1995-01-01

Full Text Available Par leur grande sensibilité au changement climatique, les glaciers tropicaux sont d’excellents indicateurs de l’évolution du climat et, en même temps, des objets hydrologiques susceptibles d’évoluer rapidement dans le futur. On montre que l’actuel recul accéléré des glaciers dans les Andes centrales et les conséquences qu’il peut avoir en matière hydrologique et de risques naturels rendent nécessaire un programme de surveillance de ces glaciers au niveau de toute la chaîne, ce que l’ORSTOM contribue à faire depuis 1991. UNA RED DE OBSERVACIÓN DE LOS GLACIARES EN LOS ANDES TROPICALES. Por su gran sensibilidad al cambio climático, los glaciares tropicales son excelentes indicadores de la evolución del clima, así como objectos hidrológicos susceptibles de una evolución rápida en el futuro. Considerando el actual retroceso acelerado de los glaciares en los Andes centrales y las consecuencias que puede tener a nivel hidrológico así como en el campo de los riesgos naturales, es necesario un programa de monitoreo de los glaciares a nivel de toda la cordillera, que es lo que ORSTOM contribuye a hacer desde 1991. A GLACIER MONITORING NETWORK IN THE TROPICAL ANDES. The high sensibility of Tropical glaciers to climatic forcing make it possible to use them as reliable indicators of climate evolution, as well as hydrological systems which could change rapidly in the future. Considering the present increase in glacier retreat in central Andes and the consequences induced by this evolution on water resources and natural hazards, a monitoring program at a large scale appears to be highly desirable. This has been the objective of ORSTOM since 1991.

Mio-Pliocene aridity in the south-central Andes associated with Southern Hemisphere cold periods.

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Amidon, William H; Fisher, G Burch; Burbank, Douglas W; Ciccioli, Patricia L; Alonso, Ricardo N; Gorin, Andrew L; Silverhart, Perri H; Kylander-Clark, Andrew R C; Christoffersen, Michael S

2017-06-20

Although Earth's climate history is best known through marine records, the corresponding continental climatic conditions drive the evolution of terrestrial life. Continental conditions during the latest Miocene are of particular interest because global faunal turnover is roughly synchronous with a period of global glaciation from ∼6.2-5.5 Ma and with the Messinian Salinity Crisis from ∼6.0-5.3 Ma. Despite the climatic and ecological significance of this period, the continental climatic conditions associated with it remain unclear. We address this question using erosion rates of ancient watersheds to constrain Mio-Pliocene climatic conditions in the south-central Andes near 30° S. Our results show two slowdowns in erosion rate, one from ∼6.1-5.2 Ma and another from 3.6 to 3.3 Ma, which we attribute to periods of continental aridity. This view is supported by synchrony with other regional proxies for aridity and with the timing of glacial ‟cold" periods as recorded by marine proxies, such as the M2 isotope excursion. We thus conclude that aridity in the south-central Andes is associated with cold periods at high southern latitudes, perhaps due to a northward migration of the Southern Hemisphere westerlies, which disrupted the South American Low Level Jet that delivers moisture to southeastern South America. Colder glacial periods, and possibly associated reductions in atmospheric CO 2 , thus seem to be an important driver of Mio-Pliocene ecological transitions in the central Andes. Finally, this study demonstrates that paleo-erosion rates can be a powerful proxy for ancient continental climates that lie beyond the reach of most lacustrine and glacial archives.

APROPIACIÓN INCA EN LA CORDILLERA DE CHILLA, SUROESTE DE LOS ANDES DEL ECUADOR: EL CASO DEL SITIO GUIÑAYZHU (Inca Appropriation in the Chilla Mountain Range, Southwest of the Andes of Ecuador: the Case of the Guiñayzhu Site

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Mary Jadán V.

2018-03-01

Full Text Available En este artículo se discuten los resultados del trabajo realizado en el sitio Guiñayzhu, al suroeste de los Andes del Ecuador. Esta investigación revela que el sitio, además de presentar evidencias de poblaciones locales, tiene colcas o qullcas para el almacenaje de productos, terrazas de pirca y caminos empedrados entre otras instalaciones. Se interpreta que Guiñayzhu es uno de los sitios de la cordillera de Chilla que refleja la expansión del incario y expresa una efectiva dominación de esta región como un enclave estratégico del imperio en su avance hacia el norte. ENGLISH: In this article, the results of research carried out in Guiñayzhu, located at the southwest of the Andes of Ecuador, are discussed. This work reveals that in addition to presenting evidence of local populations, the site has colcas or qullqas for the storage of products, terraces of pirca, and roads paved with stone, among other constructions. Guiñayzhu is interpreted as one of the sites of the Chilla mountain range that reflects the expansion of the Inca and expresses an effective domination of this region, representing a strategic enclave of the empire in its advance northward.

Crustal balance and crustal flux from shortening estimates in the Central Andes

Science.gov (United States)

Hindle, David; Kley, Jonas; Oncken, Onno; Sobolev, Stephan

2005-01-01

The Central Andes of South America form the second largest high elevation plateau on earth. Extreme elevations have formed on a noncollisional margin with abundant associated arc magmatism. It has long been thought that the crustal thickness necessary to support Andean topography was not accounted for by known crustal shortening alone. We show that this may in part be due to a two-dimensional treatment of the problem. A three-dimensional analysis of crustal shortening and crustal thickness shows that displacement of material towards the axis of the bend in the Central Andes has added a significant volume of crust not accounted for in previous comparisons. We find that present-day crustal thickness between 12°S and 25°S is accounted for (∼-10% to ∼+3%)with the same shortening estimates, and the same assumed initial crustal thickness as had previously led to the conclusion of a ∼25-35% deficit in shortening relative to volume of crustal material. We suggest that the present-day measured crustal thickness distribution may not match that predicted due to shortening, and substantial redistribution of crust may have occurred by both erosion and deposition at the surface and lower crustal flow in regions of the thermally weakened middle and lower crust.

Culture and landslide risk in the Central Andes of Bolivia and Peru

OpenAIRE

Nicholas Roberts

2009-01-01

Culture and its heritage play a major role in determining landslide risk in the Central Andes. Examples of some of these many possible influences are provided from natural and social science literature and from the author’s recent work in Bolivia. Landslide risk appears to have generally increased throughout the last millennium, due largely to anthropogenic modification of hazard, exposure, vulnerability and coping capacity. These changes result from both local and distant pressures and from ...

Surface uplift in the Central Andes driven by growth of the Altiplano Puna Magma Body.

Science.gov (United States)

Perkins, Jonathan P; Ward, Kevin M; de Silva, Shanaka L; Zandt, George; Beck, Susan L; Finnegan, Noah J

2016-10-25

The Altiplano-Puna Magma Body (APMB) in the Central Andes is the largest imaged magma reservoir on Earth, and is located within the second highest orogenic plateau on Earth, the Altiplano-Puna. Although the APMB is a first-order geologic feature similar to the Sierra Nevada batholith, its role in the surface uplift history of the Central Andes remains uncertain. Here we show that a long-wavelength topographic dome overlies the seismically measured extent of the APMB, and gravity data suggest that the uplift is isostatically compensated. Isostatic modelling of the magmatic contribution to dome growth yields melt volumes comparable to those estimated from tomography, and suggests that the APMB growth rate exceeds the peak Cretaceous magmatic flare-up in the Sierran batholith. Our analysis reveals that magmatic addition may provide a contribution to surface uplift on par with lithospheric removal, and illustrates that surface topography may help constrain the magnitude of pluton-scale melt production.

Rock Glacier Response to Climate Change in the Argentinian Andes

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Drewes, J.; Korup, O.; Moreiras, S.

2017-12-01

Rock glaciers are bodies of frozen debris and ice that move under the influence of gravity in permafrost areas. Rock glaciers may store a large amount of sediments and play an important role as prime movers of debris in the Andean sediment cascade. However, little is known about how much sediment and water rock glaciers may store at the mountain-belt scale, and the few existing estimates vary considerably. We address this question for the Argentinian Andes, for which a new glacial inventory containing more than 6500 rock glaciers gives us the opportunity to analyse their relevance within the sediment cascade. We examine the inventory for catchments in five sub-regions, i.e. the Desert Andes (22°-31°S); the Central Andes (31°-36°S); the Northern Andes of Patagonia (36°-45°S); the Southern Andes of Patagonia (45°-52°S); and Tierra del Fuego (52°-55°S), together with climate variables of the WorldClim datasets, and digital topographic data, to estimate how rock-glacier extents may change under different past and future climate scenarios. We observe for the northern Desert Andes that rock glacier toes are at 4000 to 5000 m a.s.l. and a mean annual temperature range of 3° and 8°C, though most rock glaciers are in areas with mean annual temperatures between -5 and 5°C, marking a distinct thermal niche. Rock glaciers are traditionally viewed as diagnostic of sporadic alpine permafrost and their toes are often near the annual mean 0°C isotherm. However, we find that only rock glaciers in the southern Desert Andes and Central Andes are located where annual mean temperature is -2°C. Future scenarios project an increase of > four degrees in these areas, which may further degrade ground ice and potentially change the rates at which rock glaciers advance. Where active rock glaciers become inactive their coarse material, which was formerly bound by ice, may be released into the sediment cascade, whereas accelerating or rapidly downwasting rock glaciers may either

Glacial lakes of the Central and Patagonian Andes

Science.gov (United States)

Wilson, Ryan; Glasser, Neil F.; Reynolds, John M.; Harrison, Stephan; Anacona, Pablo Iribarren; Schaefer, Marius; Shannon, Sarah

2018-03-01

The prevalence and increased frequency of high-magnitude Glacial Lake Outburst Floods (GLOFs) in the Chilean and Argentinean Andes suggests this region will be prone to similar events in the future as glaciers continue to retreat and thin under a warming climate. Despite this situation, monitoring of glacial lake development in this region has been limited, with past investigations only covering relatively small regions of Patagonia. This study presents new glacial lake inventories for 1986, 2000 and 2016, covering the Central Andes, Northern Patagonia and Southern Patagonia. Our aim was to characterise the physical attributes, spatial distribution and temporal development of glacial lakes in these three sub-regions using Landsat satellite imagery and image datasets available in Google Earth and Bing Maps. Glacial lake water volume was also estimated using an empirical area-volume scaling approach. Results reveal that glacial lakes across the study area have increased in number (43%) and areal extent (7%) between 1986 and 2016. Such changes equate to a glacial lake water volume increase of 65 km3 during the 30-year observation period. However, glacial lake growth and emergence was shown to vary sub-regionally according to localised topography, meteorology, climate change, rate of glacier change and the availability of low gradient ice areas. These and other factors are likely to influence the occurrence of GLOFs in the future. This analysis represents the first large-scale census of glacial lakes in Chile and Argentina and will allow for a better understanding of lake development in this region, as well as, providing a basis for future GLOF risk assessments.

Nurse effect in seedling establishment: facilitation and tolerance to damage in the Andes of central Chile Efecto nodriza en el establecimiento de plántulas: facilitación y tolerancia al daño en los Andes de Chile central

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IAN S ACUÑA-RODRÍGUEZ

2006-09-01

ás relevante en ambientes estresantes. Este efecto sería particularmente importante durante el periodo de establecimiento de las plántulas debido a su alta vulnerabilidad a factores bióticos y abióticos como herbivoría y desecación. La tolerancia a la herbivoría evidencia la capacidad de las plantas de recrecer y reproducirse después del daño, pero esta capacidad es recurso-dependiente. En los Andes de Chile central, la planta en cojín Laretia acaulis (Apiaceae atenúa el efecto del estrés ambiental, aumentando la supervivencia de diversas especies de plantas asociadas. Proponemos que las plántulas que se encuentren creciendo dentro de los cojines de L. acaulis deberían evidenciar niveles mayores de tolerancia en relación a aquellas plántulas creciendo fuera de los cojines. Para probar esta hipótesis se llevó a cabo un experimento de campo con dos especies nativas perennes: Hordeum comosum (Poaceae y Haplopappus anthylloides (Asteraceae. Plántulas de ambas especies fueron sembradas dentro y fuera de los cojines de L. acaulis, y la mitad de ellas recibieron daño manual (50 % tejido foliar removido. En general, las plántulas que se encontraron creciendo dentro del cojín evidenciaron una mayor supervivencia independientemente del tratamiento de daño. A pesar de que la ubicación de las plántulas no afectó la respuesta en tolerancia por parte de H. anthylloides, sí afectó significativamente la tolerancia de H. comosum. Por lo tanto, encontramos valores similares para la supervivencia de plántulas de H. comosum dentro de los cojines, pero la supervivencia de plántulas dañadas fuera de los cojines fue significativamente menor que la de plántulas control. Se pudo evidenciar la ocurrencia de efecto nodriza por parte de L. acaulis sobre el establecimiento de ambas especies y conjuntamente un aumento en la tolerancia al daño para H. comosum en este hábitat estresante

Constuccion social de comuninad y migración en Usibamba : un estudio sobre el impacto de los procesos de globalización en los Andes centrales del Perú

NARCIS (Netherlands)

Gilvonio Perez, J.M.

2009-01-01

The research for the thesis was conducted in the village of Usibamba, located in a high-Andean area called Alto Cunas east from the Mantaro Valley in the Peruvian Central Andes. Special attention was paid to the institutional context and the everyday life conditions in which the social construction

Pucarilla-Cerro Tipillas volcanic complex: the oldest recognized caldera in the southeastern portion of central volcanic zone of Central Andes?

Energy Technology Data Exchange (ETDEWEB)

Guzman, Silvina; Petrinovic, Ivan [CONICET -IBIGEO. Museo de Cs. Naturales, Universidad de Salta, Mendoza 2 (4400), Salta (Argentina)], E-mail: guzmansilvina@gmail.com

2008-10-01

We recognize the most eastern and oldest collapse caldera structure in the southern portion of the Central Volcanic Zone of the Andes. A description of Middle-Upper Miocene successions related to explosive- effusive events is presented. The location of this centre close to Cerro Galn Caldera attests a recurrence in the volcanism between 12 and 2 Ma in this portion of the Altiplano - Puna Plateau.

Cold Episodes, Their Precursors and Teleconnections in the Central Peruvian Andes (1958-2009)

Science.gov (United States)

Sulca, J. C.; Vuille, M. F.; Trasmonte, G.; Silva, Y.; Takahashi, K.

2014-12-01

The Mantaro valley (MV) is located in the central Peruvian Andes. Occasionally, cold episodes are observed during the austral summer (January-March), which strongly damage crops. However, little is known about the causes and impacts of such cold episodes in the MV. The main goal of this study is thus to characterize cold episodes in the MV and assess their large-scale circulation and teleconnections over South America (SA) during austral summer. To identify cold events in the MV daily minimum temperature for the period 1958-2009 from Huayao station, located within the MV was used. We defined a cold episode as the period when daily minimum temperature drops below the 10-percentile for at least one day. Several gridded reanalysis and satellite products were used to characterize the large-scale circulation, cloud cover and rainfall over SA associated with these events for same period. Cold episodes in the MV are associated with positive OLR anomalies, which extend over much of the central Andes, indicating reduced convective cloud cover during these extremes, but also affirm the large-scale nature of these events. At the same time, northeastern Brazil (NEB) registers negative OLR anomalies, strong convective activity and enhanced cloud cover because displacement of the South Atlantic Convergence Zone (SACZ) toward the northeast of its climatologic position. Further, it is associated with a weakening of the Bolivian High - Nordeste Low (BH-NL) system at upper levels, but also influenced by a low-level migratory high-pressure center develops at 30°S, 50°W; propagating from mid- to low latitudes as part of an extratropical Rossby wave train. In conclusion, cold episodes in the MV appear to be caused by radiative cooling associated with reduced cloudiness, rather than cold air advection. The reduced cloud cover in turn results from a robust large-scale pattern of westerly wind anomalies over central Peruvian Andes, inhibiting moisture influx, convective activity and

Intraseasonal variability of organized convective systems in the Central Andes: Relationship to Regional Dynamical Features

Science.gov (United States)

Mohr, K. I.; Slayback, D. A.; Nicholls, S.; Yager, K.

2013-12-01

The Andes extend from the west coast of Colombia (10N) to the southern tip of Chile (53S). In southern Peru and Bolivia, the Central Andes is split into separate eastern and western cordilleras, with a high plateau (≥ 3000 m), the Altiplano, between them. Because 90% of the Earth's tropical mountain glaciers are located in the Central Andes, our study focuses on this region, defining its zonal extent as 7S-21S and the meridional extent as the terrain 1000 m and greater. Although intense convection occurs during the wet season in the Altiplano, it is not included in the lists of regions with frequent or the most intense convection. The scarcity of in-situ observations with sufficient density and temporal resolution to resolve individual storms or even mesoscale-organized cloud systems and documented biases in microwave-based rainfall products in poorly gauged mountainous regions have impeded the development of an extensive literature on convection and convective systems in this region. With the tropical glaciers receding at unprecedented rates, leaving seasonal precipitation as an increasingly important input to the water balance in alpine valley ecosystems and streams, understanding the nature and characteristics of the seasonal precipitation becomes increasingly important for the rural economies in this region. Previous work in analyzing precipitation in the Central Andes has emphasized interannual variability with respect to ENSO, this is the first study to focus on shorter scale variability with respect to organized convection. The present study took advantage of the University of Utah's Precipitation Features database compiled from 14 years of TRMM observations (1998-2012), supplemented by field observations of rainfall and streamflow, historical gauge data, and long-term WRF-simulations, to analyze the intraseasonal variability of precipitating systems and their relationship regional dynamical features such as the Bolivian High. Through time series and

Compositional data supports decentralized model of production and circulation of artifacts in the pre-Columbian south-central Andes.

Science.gov (United States)

Lazzari, Marisa; Pereyra Domingorena, Lucas; Stoner, Wesley D; Scattolin, María Cristina; Korstanje, María Alejandra; Glascock, Michael D

2017-05-16

The circulation and exchange of goods and resources at various scales have long been considered central to the understanding of complex societies, and the Andes have provided a fertile ground for investigating this process. However, long-standing archaeological emphasis on typological analysis, although helpful to hypothesize the direction of contacts, has left important aspects of ancient exchange open to speculation. To improve understanding of ancient exchange practices and their potential role in structuring alliances, we examine material exchanges in northwest Argentina (part of the south-central Andes) during 400 BC to AD 1000 (part of the regional Formative Period), with a multianalytical approach (petrography, instrumental neutron activation analysis, laser ablation inductively coupled plasma mass spectrometry) to artifacts previously studied separately. We assess the standard centralized model of interaction vs. a decentralized model through the largest provenance database available to date in the region. The results show: ( i ) intervalley heterogeneity of clays and fabrics for ordinary wares; ( ii ) intervalley homogeneity of clays and fabrics for a wide range of decorated wares (e.g., painted Ciénaga); ( iii ) selective circulation of two distinct polychrome wares (Vaquerías and Condorhuasi); ( iv ) generalized access to obsidian from one major source and various minor sources; and ( v ) selective circulation of volcanic rock tools from a single source. These trends reflect the multiple and conflicting demands experienced by people in small-scale societies, which may be difficult to capitalize by aspiring elites. The study undermines centralized narratives of exchange for this period, offering a new platform for understanding ancient exchange based on actual material transfers, both in the Andes and beyond.

Estimation of slip scenarios of mega-thrust earthquakes and strong motion simulations for Central Andes, Peru

Science.gov (United States)

Pulido, N.; Tavera, H.; Aguilar, Z.; Chlieh, M.; Calderon, D.; Sekiguchi, T.; Nakai, S.; Yamazaki, F.

2012-12-01

We have developed a methodology for the estimation of slip scenarios for megathrust earthquakes based on a model of interseismic coupling (ISC) distribution in subduction margins obtained from geodetic data, as well as information of recurrence of historical earthquakes. This geodetic slip model (GSM) delineates the long wavelength asperities within the megathrust. For the simulation of strong ground motion it becomes necessary to introduce short wavelength heterogeneities to the source slip to be able to efficiently simulate high frequency ground motions. To achieve this purpose we elaborate "broadband" source models constructed by combining the GSM with several short wavelength slip distributions obtained from a Von Karman PSD function with random phases. Our application of the method to Central Andes in Peru, show that this region has presently the potential of generating an earthquake with moment magnitude of 8.9, with a peak slip of 17 m and a source area of approximately 500 km along strike and 165 km along dip. For the strong motion simulations we constructed 12 broadband slip models, and consider 9 possible hypocenter locations for each model. We performed strong motion simulations for the whole central Andes region (Peru), spanning an area from the Nazca ridge (16^o S) to the Mendana fracture (9^o S). For this purpose we use the hybrid strong motion simulation method of Pulido et al. (2004), improved to handle a general slip distribution. Our simulated PGA and PGV distributions indicate that a region of at least 500 km along the coast of central Andes is subjected to a MMI intensity of approximately 8, for the slip model that yielded the largest ground motions among the 12 slip models considered, averaged for all assumed hypocenter locations. This result is in agreement with the macroseismic intensity distribution estimated for the great 1746 earthquake (M~9) in central Andes (Dorbath et al. 1990). Our results indicate that the simulated PGA and PGV for

Características de uso de plaguicidas químicos y riesgos para la salud en agricultores de la sierra central del Perú

OpenAIRE

Ymelda Montoro; Rocío Moreno; Luis Gomero; Maria Reyes

2009-01-01

Con el objetivo de conocer las características sobre el uso e impactos en la salud de los plaguicidas químicos de uso agrícola en las provincias de Chupaca y Concepción en los andes centrales del Perú, se desarrolló un estudio descriptivo transversal entre abril y junio del año 2005, por medio de un cuestionario aplicado a 435 agricultores. Asimismo, se exploró la ubicación de los centros de expendio y la frecuencia de ventas de productos, además, se evaluó los casos de intoxicación reportado...

Andes 1997 Gravity Data

Data.gov (United States)

National Oceanic and Atmospheric Administration, Department of Commerce — The Central Andes gravity data (6,151 records) were compiled by Professor Gotze and the MIGRA Group. This data base was received in April, 1997. Principal gravity...

Culture and landslide risk in the Central Andes of Bolivia and Peru

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Nicholas Roberts

2009-06-01

Full Text Available Culture and its heritage play a major role in determining landslide risk in the Central Andes. Examples of some of these many possible influences are provided from natural and social science literature and from the author’s recent work in Bolivia. Landslide risk appears to have generally increased throughout the last millennium, due largely to anthropogenic modification of hazard, exposure, vulnerability and coping capacity. These changes result from both local and distant pressures and from contemporaneous and pervious cultural factors. Consequently, holistic examination of landslide risk necessitates consideration of culture and its heritage.

Genome of Plant Maca (Lepidium meyenii) Illuminates Genomic Basis for High-Altitude Adaptation in the Central Andes.

Science.gov (United States)

Zhang, Jing; Tian, Yang; Yan, Liang; Zhang, Guanghui; Wang, Xiao; Zeng, Yan; Zhang, Jiajin; Ma, Xiao; Tan, Yuntao; Long, Ni; Wang, Yangzi; Ma, Yujin; He, Yuqi; Xue, Yu; Hao, Shumei; Yang, Shengchao; Wang, Wen; Zhang, Liangsheng; Dong, Yang; Chen, Wei; Sheng, Jun

2016-07-06

Maca (Lepidium meyenii Walp, 2n = 8x = 64), belonging to the Brassicaceae family, is an economic plant cultivated in the central Andes sierra in Peru (4000-4500 m). Considering that the rapid uplift of the central Andes occurred 5-10 million years ago (Ma), an evolutionary question arises regarding how plants such as maca acquire high-altitude adaptation within a short geological period. Here, we report the high-quality genome assembly of maca, in which two closely spaced maca-specific whole-genome duplications (WGDs; ∼6.7 Ma) were identified. Comparative genomic analysis between maca and closely related Brassicaceae species revealed expansions of maca genes and gene families involved in abiotic stress response, hormone signaling pathway, and secondary metabolite biosynthesis via WGDs. The retention and subsequent functional divergence of many duplicated genes may account for the morphological and physiological changes (i.e., small leaf shape and self-fertility) in maca in a high-altitude environment. In addition, some duplicated maca genes were identified with functions in morphological adaptation (i.e., LEAF CURLING RESPONSIVENESS) and abiotic stress response (i.e., GLYCINE-RICH RNA-BINDING PROTEINS and DNA-DAMAGE-REPAIR/TOLERATION 2) under positive selection. Collectively, the maca genome provides useful information to understand the important roles of WGDs in the high-altitude adaptation of plants in the Andes. Copyright © 2016 The Authors. Published by Elsevier Inc. All rights reserved.

Caracterización química del material particulado atmosférico del centro urbano de Huancayo, Perú

OpenAIRE

Suárez-Salas, Luis; Álvarez Tolentino, Daniel; Bendezú, Yéssica; Pomalaya, José

2017-01-01

La ciudad de Huancayo, ubicada en los Andes centrales del Perú, presenta problemas de calidad del aire, siendo el principal contaminante el material particulado (MP). Por ello, el objetivo del presente artículo fue caracterizar la composición química del MP atmosférico colectados en una estación ubicada en el centro urbano de Huancayo. Se colectó MP en agosto del 2007, y enero, abril y mayo del 2008 con un equipo de bajo volumen (PARTISOL FRM 2000) y filtros de 47 mm. Se determinó la concentr...

Cronología, identidad, urbanismo y estado en los Andes Centrales y surcentrales entre los siglos V a X D.C.: algunas reflexiones finales

OpenAIRE

Kaulicke, Peter

2012-01-01

Chronology, Identity, Urbanism and State in the Central and South Central Andes between V and X Centuries AD: Some Final ConclusionsThe article doesn´t have an abstract El artículo no presenta resumen

Importance of water quality on plant abundance and diversity in high-alpine meadows of the Yerba Loca Natural Sanctuary at the Andes of north-central Chile Importancia de la calidad del agua sobre la abundancia y diversidad vegetal en vegas altoandinas del Santuario Natural Yerba Loca en los Andes de Chile centro-norte

Directory of Open Access Journals (Sweden)

ROSANNA GINOCCHIO

2008-12-01

Full Text Available Porphyry Cu-Mo deposits have influenced surface water quality in high-Andes of north-central Chile since the Miocene. Water anomalies may reduce species abundance and diversity in alpine meadows as acidic and metal-rich waters are highly toxic to plants The study assessed the importance of surface water quality on plant abundance and diversity in high-alpine meadows at the Yerba Loca Natural Santuary (YLNS, central Chile (33°15' S, 70°18' W. Hydrochemical and plant prospecting were carried out on Piedra Carvajal, Chorrillos del Plomo and La Lata meadows the growing seasons of 2006 and 2007. Direct gradient analysis was performed through canonical correspondence analysis (CCA to look for relationships among water chemistry and plant factors. High variability in water chemistry was found inside and among meadows, particularly for pH, sulphate, electric conductivity, hardness, and total dissolved Cu, Zn, Cd, Pb and Fe. Data on species abundance and water chemical factors suggests that pH and total dissolved Cu are very important factor determining changes in plant abundance and diversity in study meadows. For instance, Festuca purpurascens, Colobanthus quitensis, and Arenaria rivularis are abundant in habitals with Cu-rich waters while Festuca magellanica, Patosia clandestina, Plantago barbata, Werneria pygmea, and Erigeron andícola are abundant in habitals with dilute waters.Los megadepósitos de pórfidos de Cu-Mo han influido sobre la calidad de las aguas superficiales en las zonas altoandinas del centro-norte de Chile desde el Mioceno. Estas alteraciones en la calidad de las aguas podrían afectar negativamente a la vegetación presente en las vegas altoandinas, ya que las aguas acidas y ricas en metales son altamente tóxicas para las plantas. En este estudio se evaluó el efecto de la calidad de las aguas en la abundancia y diversidad florística de las vegas altoandinas del Santuario de la Naturaleza Yerba Loca (SNYL, en Chile central (33

Les Andes Centrales Tropicales vues par deux géographes: Isaiah Bowman et Carl Troll

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1978-01-01

Full Text Available Deux visions des Andes vues par deux géographes, Isaiah BOWMAN et Carl TROLL, au caractère et au milieu intellectuel différents. L'auteur étudie dans l'un et l'autre cas la méthode d'analyse de l'espace géographique et les conclusions tirées par chacun d'eux. I. BOWMAN, Américain, convaincu qu'une économie mercantiliste fondée sur l'exportation permettra aux Etats andins d'accéder à un modèle de développement, décrit les vastes contrées amazoniennes comme un futur El Dorado entre les mains de colons. L'aménagement des basses plaines selon des schémas nord-américains est le pilier de l'économie alors que les Andes abritant les communautés indigènes constituent un frein au développement. De ce fait il laisse de côté l'étude des paysanneries andines. Toute différente est la démarche de Carl TROLL dont la formation à la fois en sciences humaines et naturelles, lui permet de cerner l'espace géographique comme cadre de vie des sociétés. L'utilisation des étages écologiques, le développement de l'Empire Inca fondé sur l'étage des 'punas', la démarche historique des analyses minutieuses de Carl TROLL donne un éclairage nouveau aux relations des sociétés andines et des milieux naturels avec lesquels elles composent. Dos puntos de vista de los Andes por dos geógrafos, Isaiah BOWMAN y Carl TROLL con carácter y medio intelectual distintos. El autor estudia en ambos casos el método de análisis del espacio geográfico y las conclusiones sacadas por cada uno de ellos. I. BOWMAN, americano, convencido que una economía mercantil fundada sobre la exportación permitirá a los estados andinos acceder a un modelo de desarrollo, describe las extensas llanuras amazónicas como un El Dorado futuro entre las manos de los colonos. El desarrollo de las llanuras bajas según esquemas norteamericanos constituye el pilar de la economía mientras los Andes abrigando las comunidades indígenas se comportan como un freno al

Glacialmorphological reconstruction of glacier advances and glacial lake outburst floods at the Cachapoal glacier in the Dry Central Andes of Chile (34°S)

Science.gov (United States)

Iturrizaga, Lasafam; Charrier, Reynaldo

2013-04-01

Throughout the Andes Mountain range of South America a general trend of glacier shrinkage has taken place in the last century. Only a few glaciers have shown a rather non-continuous trend of glacier retreat and temporally advanced or even surged during the mid-19th to 20th century. One of the earliest assumed glacier surges has occurred in the upper Cachapoal catchment area at the homonymous glacier. In climatic respect the Cachapoal glacier is located in the transition zone from the most southern part of the Dry Central Andes of Chile to the more humid zone of the Wet Andes. The region is affected mainly by winter precipitation deriving from the Westerlies. The debris-covered, 12 km-long Cachapoal glacier represents one of the largest valley glaciers in the Central Andes. It is an avalanche-fed glacier with an almost 1500 m-high head wall in its upper catchment area flowing down from Picos del Barroso (5180 m) and terminates at an elevation of 2630 m a.s.l. with a bifurcated glacier tongue. A large moraine complex, almost 2 km in length and 500 m in width, separates the two glacier lobes. During times of advanced glacier tongue positions the Ríos Molina and Cachapoal may be have blocked independently at two distinct localities which are situated about 2300 m apart from each other. A blockage with temporal lake formation has occurred at least in the years 1848, 1955 and 1981 (cf. Plagemann 1887, Peña 1981), from which the rupture of the earliest glacier barrier has been the most devastating. This event is locally reminded as "la gran avenida en seco" in the historical record. Geomorphological evidence of the past historical and modern glacier expansions is given in the proglacial area by a fresh dead-ice hummocky topography and glacial trimlines at the valley flanks. More down valley broad outwash plains and boulder clusters indicate past high energy floods produced by glacier lake outbursts. Regarding the small size of the catchment area of the Río Molina

Climate in the Western Cordillera of the Central Andes over the last 4300 years

Science.gov (United States)

Engel, Zbyněk; Skrzypek, Grzegorz; Chuman, Tomáš; Šefrna, Luděk; Mihaljevič, Martin

2014-09-01

The Distichia peat core obtained in the Carhuasanta valley near Nevado Mismi, Cordillera Chila, provides information on climatic and environmental conditions over the last ˜4300 years. The relative changes in the stable carbon isotope composition of plant remains preserved in the core reflect major temperature fluctuations in the Western Cordillera of the southern Peruvian Andes. These temperature variations can be additionally linked with the changes in precipitation patterns by analysing C% and C/N ratio in the core. Relatively warm and moist conditions prevailed from 4280 to 3040 cal. yrs BP (BC 2330-1090) with a short colder dry episode around 3850 cal. yrs BP (BC 1900). The most prominent climate changes recorded in the peat occurred between 3040 and 2750 cal. yrs BP (BC 1090-800) when the initial warming turned to a rapid cooling to temperatures at least 2 °C lower than the mean for the Late Holocene. Initially drier conditions within this event turned to a short wet phase after 2780 cal. yrs BP (BC 830) when the temperature increased again. This event coincides with significant changes in peat and ice core records in the Central Andes matching the timing of the global climate event around 2.8 cal. ka BP. Climatic conditions in the study area became relatively dry and stable after the event for about 800 years. Highly variable temperatures and humidity prevailed during the last 2000 years when an extended warm and relatively humid period occurred between 640 and 155 cal. yrs BP (AD 1310-1795) followed by predominantly colder and drier conditions. The established δ13C peat record represents the first continuous proxy for the temperature in the southern Peruvian Andes dated by the AMS 14C. Distichia peat is wide spread in the Andes and the proposed approach can be applied elsewhere in high altitudes, where no other traditional climate proxies are available.

Impact of Santiago de Chile urban atmospheric pollution on anthropogenic trace elements enrichment in snow precipitation at Cerro Colorado, Central Andes

Science.gov (United States)

Cereceda-Balic, F.; Palomo-Marín, M. R.; Bernalte, E.; Vidal, V.; Christie, J.; Fadic, X.; Guevara, J. L.; Miro, C.; Pinilla Gil, E.

2012-02-01

Seasonal snow precipitation in the Andes mountain range is evaluated as an environmental indicator of the composition of atmospheric emissions in Santiago de Chile metropolitan area, by measuring a set of representative trace elements in snow samples by ICP-MS. Three late winter sampling campaigns (2003, 2008 and 2009) were conducted in three sampling areas around Cerro Colorado, a Central Andes mountain range sector NE of Santiago (36 km). Nevados de Chillán, a sector in The Andes located about 500 km south from the metropolitan area, was selected as a reference area. The experimental results at Cerro Colorado and Nevados de Chillán were compared with previously published data of fresh snow from remote and urban background sites. High snow concentrations of a range of anthropogenic marker elements were found at Cerro Colorado, probably derived from Santiago urban aerosol transport and deposition combined with the effect of mining and smelting activities in the area, whereas Nevados de Chillán levels roughly correspond to urban background areas. Enhanced concentrations in surface snow respect to deeper samples are discussed. Significant differences found between the 2003, 2008 and 2009 anthropogenic source markers profiles at Cerro Colorado sampling points were correlated with changes in emission sources at the city. The preliminary results obtained in this study, the first of this kind in the southern hemisphere, show promising use of snow precipitation in the Central Andes as a suitable matrix for receptor model studies aimed at identifying and quantifying pollution sources in Santiago de Chile.

Geografía, café y prosperidad en los andes occidentales de Colombia

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Juan Barón

2011-07-01

Full Text Available Compuesta por los departamentos de Antioquia, Caldas, Quindío, Risaralda y Valle del Cauca, los Andes Occidentales ha sido por mucho años una de las regiones más prósperas de Colombia. Esta prosperidad se ha traducido en condiciones de vida e infraestructura superiores a las del resto del país. El éxito y bienestar que presentan hoy en día los Andes Occidentales están estrechamente ligados a la concentración de la producción de café, que se dio allí durante gran parte del siglo XX. El arraigo del café en la región no sólo se dio debido a que la geografía ofrecía las condiciones ideales para el cultivo, sino también a las instituciones cafeteras creadas para organizar la industria del café. A pesar de esta prosperidad, el constante descenso del precio internacional del café después del rompimiento del pacto de cuotas de producción en 1989, sumado al estancamiento de la industria manufacturera en algunos departamentos de la región, han afectado las economías departamentales menos diversificadas. Es así como la región de los Andes Occidentales Colombianos presenta las tasas de desempleo más altas del país, tasas que se han visto afectadas aún más con la crisis financiera internacional a través del menor flujo de remesas que los trabajadores oriundos de la región, y residentes en el exterior envían a sus familias.

Novel Strain of Andes Virus Associated with Fatal Human Infection, Central Bolivia

Science.gov (United States)

Cruz, Cristhopher D.; Vallejo, Efrain; Agudo, Roberto; Vargas, Jorge; Blazes, David L.; Guevara, Carolina; Laguna-Torres, V. Alberto; Halsey, Eric S.; Kochel, Tadeusz J.

2012-01-01

To better describe the genetic diversity of hantaviruses associated with human illness in South America, we screened blood samples from febrile patients in Chapare Province in central Bolivia during 2008–2009 for recent hantavirus infection. Hantavirus RNA was detected in 3 patients, including 1 who died. Partial RNA sequences of small and medium segments from the 3 patients were most closely related to Andes virus lineages but distinct (1 hantaviruses; the highest prevalence was among agricultural workers. Because of the high level of human exposure to hantavirus strains and the severity of resulting disease, additional studies are warranted to determine the reservoirs, ecologic range, and public health effect of this novel strain of hantavirus. PMID:22515983

Spatio-Temporal Patterns of the 2010–2015 Extreme Hydrological Drought across the Central Andes, Argentina

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Juan Antonio Rivera

2017-08-01

Full Text Available During the period 2010–2015, the semi-arid Central Andes in Argentina (CAA experienced one of the most severe and long-lasting hydrological droughts on record. Since the snowmelt is the most important source of water, the reduced snowfall over the mountains propagated the drought signal through the streamflows in the adjacent foothills east of the Andes ranges. Motivated by the widespread impacts on the socio-economic activities in the region, this study aims to characterize the recent hydrological drought in terms of streamflow deficits. Based on streamflow data from 20 basins, we used the standardized streamflow index (SSI to characterize hydrological droughts during the period 1971–2016. We found that the regional extent of the 2010–2015 hydrological drought was limited to the basins located north of 38° S, with mean duration of 67 months and maximum drought severity exhibiting a heterogeneous pattern in terms of spatial distribution and time of occurrence. The drought event reached extreme conditions in 14 of the 15 basins in the CAA, being record-breaking drought in six of the basins. This condition was likely driven by a cooling in the tropical Pacific Ocean resembling La Niña conditions, which generated a decrease in snowfall over the Andes due to suppressed frontal activity.

Influence of spatial resolution on precipitation simulations for the central Andes Mountains

Science.gov (United States)

Trachte, Katja; Bendix, Jörg

2013-04-01

The climate of South America is highly influenced by the north-south oriented Andes Mountains. Their complex structure causes modifications of large-scale atmospheric circulations resulting in various mesoscale phenomena as well as a high variability in the local conditions. Due to their height and length the terrain generates distinctly climate conditions between the western and the eastern slopes. While in the tropical regions along the western flanks the conditions are cold and arid, the eastern slopes are dominated by warm-moist and rainy air coming from the Amazon basin. Below 35° S the situation reverses with rather semiarid conditions in the eastern part and temperate rainy climate along southern Chile. Generally, global circulation models (GCMs) describe the state of the global climate and its changes, but are disabled to capture regional or even local features due to their coarse resolution. This is particularly true in heterogeneous regions such as the Andes Mountains, where local driving features, e. g. local circulation systems, highly varies on small scales and thus, lead to a high variability of rainfall distributions. An appropriate technique to overcome this problem and to gain regional and local scale rainfall information is the dynamical downscaling of the global data using a regional climate model (RCM). The poster presents results of the evaluation of the performance of the Weather Research and Forecasting (WRF) model over South America with special focus on the central Andes Mountains of Ecuador. A sensitivity study regarding the cumulus parametrization, microphysics, boundary layer processes and the radiation budget is conducted. With 17 simulations consisting of 16 parametrization scheme combinations and 1 default run a suitable model set-up for climate research in this region is supposed to be evaluated. The simulations were conducted in a two-way nested mode i) to examine the best physics scheme combination for the target and ii) to

Tectonics, hydrothermal zoning, and uranium in the central Andes

Energy Technology Data Exchange (ETDEWEB)

Gabelman, J W

1961-01-01

The geological features of the Peruvian Andes are discussed in some detail. The geologic history of the Andrean tectonics was found to be virtually the same as that represented in both North and South American Cordillera. The study indicated that Andrean hydrothermal mineralization occurred intermittently but in close time relation with accompanying deformations from the late Cretaceous or early Tertiary up to the present. The mineralization cycle is discussed as it relates to several metals, particularly uranium. Uranium is believed to occupy the same several temperature--environmental positions in the Andes that it does throughout the rest of the western hemisphere Cordillera. Even though uranium is present in minor quantities in several high-to-moderate-temperature environments, the bulk of uranium present in the cycle is believed to precipitate in the subepithermal environment.

Extreme hydrometeorological events in the Peruvian Central Andes during austral summer and their relationship with the large-scale circulation

Science.gov (United States)

Sulca, Juan C.

In this Master's dissertation, atmospheric circulation patterns associated with extreme hydrometeorological events in the Mantaro Basin, Peruvian Central Andes, and their teleconnections during the austral summer (December-January-February-March) are addressed. Extreme rainfall events in the Mantaro basin are related to variations of the large-scale circulation as indicated by the changing strength of the Bolivian High-Nordeste Low (BH-NL) system. Dry (wet) spells are associated with a weakening (strengthening) of the BH-NL system and reduced (enhanced) influx of moist air from the lowlands to the east due to strengthened westerly (easterly) wind anomalies at mid- and upper-tropospheric levels. At the same time extreme rainfall events of the opposite sign occur over northeastern Brazil (NEB) due to enhanced (inhibited) convective activity in conjunction with a strengthened (weakened) Nordeste Low. Cold episodes in the Mantaro Basin are grouped in three types: weak, strong and extraordinary cold episodes. Weak and strong cold episodes in the MB are mainly associated with a weakening of the BH-NL system due to tropical-extratropical interactions. Both types of cold episodes are associated with westerly wind anomalies at mid- and upper-tropospheric levels aloft the Peruvian Central Andes, which inhibit the influx of humid air masses from the lowlands to the east and hence limit the potential for development of convective cloud cover. The resulting clear sky conditions cause nighttime temperatures to drop, leading to cold extremes below the 10-percentile. Extraordinary cold episodes in the MB are associated with cold and dry polar air advection at all tropospheric levels toward the central Peruvian Andes. Therefore, weak and strong cold episodes in the MB appear to be caused by radiative cooling associated with reduced cloudiness, rather than cold air advection, while the latter plays an important role for extraordinary cold episodes only.

Preliminary Results From the CAUGHT Experiment: Investigation of the North Central Andes Subsurface Using Receiver Functions and Ambient Noise Tomography

Science.gov (United States)

Ryan, J. C.; Ward, K. M.; Porter, R. C.; Beck, S. L.; Zandt, G.; Wagner, L. S.; Minaya, E.; Tavera, H.

2011-12-01

Jamie Ryan, Kevin M. Ward, Ryan Porter, Susan Beck, George Zandt, Lara Wagner, Estela Minaya, and Hernando Tavera The University of Arizona The University of North Carolina San Calixto Observatorio, La Paz, Bolivia IGP, Lima, Peru In order to investigate the interplay between crustal shortening, lithospheric removal, and surface uplift we have deployed 50 broadband seismometers in northwestern Bolivia and southern Peru as part of the interdisciplinary Central Andean Uplift and Geodynamics of High Topography (CAUGHT) project. The morphotectonic units of the central Andes from west to east, consist of the Western Cordillera, the active volcanic arc, the Altiplano, an internally drained basin (~4 km elevation), the Eastern Cordillera, the high peaks (~6 km elevation) of an older fold and thrust belt, the Subandean zone, the lower elevation active fold and thrust belt, and the foreland Beni basin. Between northwestern Bolivia and southern Peru, the Altiplano pinches out north of Lake Titicaca as the Andes narrow northward. The CAUGHT seismic instruments were deployed between 13° to 18° S latitudes to investigate the crust and mantle lithosphere of the central Andes in this transitional zone. In northwest Bolivia, perpendicular to the strike of the Andes, there is a total of 275 km of documented upper crustal shortening (15° to 17°S) (McQuarrie et al, 2008). Associated with the shortening is crustal thickening and possibly lithospheric removal as the thickening lithospheric root becomes unstable. An important first order study is to compare upper crustal shortening estimates with present day crustal thickness. To estimate crustal thickness, we have calculated receiver functions using an iterative deconvolution method and used common conversion point stacking along the same profile as the geologically based shortening estimates. In our preliminary results, we observed a strong P to S conversion corresponding to the Moho at approximately 60-65 km depth underneath the

Parasite loads and altitudinal distribution of Liolaemus lizards in the central Chilean Andes Cargas parasitarias y distribución de lagartijas Liolaemus en los Andes de Chile central

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JOHN H. CAROTHERS

2001-09-01

Full Text Available This study compared the distributions of ten species of Liolaemus lizards in the central Chilean Andes to the distributions of four types of parasites: malaria-causing Plasmodium, gut nematodes, ticks, and mites. We wanted to see if parasite numbers might be a factor in determining distributional limits of the lizards. We found that there was no evidence of malarial infestation of the lizards, that ticks were almost absent, that more often than not mite numbers decreased at the distributional limits of the lizards, and that gut nematodes confined to the herbivorous lizards in our sample may well be beneficial rather than detrimental. Rather than parasitism, other biotic interactions (e.g., predation or competition are more likely candidates as factors influencing lizard elevational distributions, as are abiotic characteristics such as microhabitat availabilities and thermal factorsEste estudio compara las distribuciones de diez especies de lagartijas Liolaemus en los Andes de Chile central, con las distribuciones de cuatro tipos de parásitos: Plasmodium causantes de malaria, nemátodos intestinales, garrapatas y ácaros. Quisimos verificar si los números de parásitos pudieran ser un factor determinante de los límites de distribución de las lagartijas. Encontramos que no había evidencia de infestación por malaria en las lagartijas; que las garrapatas estaban casi ausentes; que los números de ácaros más a menudo decrecían que aumentaban en los límites distribucionales de las lagartijas; y que los nemátodos intestinales confinados a las lagartijas herbívoras en nuestra muestra bien podían ser beneficiosos antes que dañinos. Más bien que parasitismo, otras interacciones bióticas (e.g., depredación o competencia son candidatos más probables como factores que influyen las distribuciones altitudinales de las lagartijas, además de características abióticas tales como la disponibilidad de microhábitats y los factores térmicos

Las puntas y rejas prehispánicas de metal en los Andes y su continuidad hasta el presente

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2005-01-01

Full Text Available Les pointes et les socs préhispaniques en métal dans les Andes et leur continuité jusqu’à aujourd’hui Résumé: Cet article tente de montrer la continuité entre les instruments à usages multiples composés de pointes et des socs en cuivre arsenical insérés sur des manches en bois qui ont été élaborés à partir de 900 d. C. par les Sicán de Batán Grande, département de Lambayeque (Pérou, et certains instruments en acier utilisés actuellement dans les Andes du nord du Pérou et du sud de l’Équateur : les barretas, barretillas, barretones et les petites pelles. Il s’agit d’indiquer, sur la base d’informations ethnographiques, la relation entre ces instruments et les allachus, kituchis et chaquitacllas dont se servent les paysans des hautes terres du centre et du sud du Pérou, ceci dans le but de contribuer à l’élaboration d’une histoire de la technologie andine. Este artículo intenta, por un lado, mostrar la continuidad entre las herramientas multiusos elaboradas a partir de 900 d.C. por los sicanes de Batán Grande, departamento de Lambayeque (Perú, compuestas por puntas y rejas de cobre arsenical insertadas en cabos de madera y algunos de los instrumentos de acero utilizados actualmente en los Andes del norte del Perú y del sur del Ecuador: barretas, barretillas, barretones y pequeñas lampas. Y por otro, indicar, en base a datos etnográficos, la relación entre estos instrumentos y los allachus, kituchis y chaquitacllas que emplean los campesinos de las tierras alto andinas del centro y el sur del Perú. Esto con la finalidad de abogar para la elaboración de una historia de la tecnología andina. Prehispanic metal points and ploughshares in the Andes and their continuity until the present Abstract: This article shows the continuity in the production of multiple use tools that where made beginning AD 900 by the Sicán people of Batán Grande, in the Department of Lambayeque, Peru. These tools are arsenical cooper

CARACTERIZACIÓN CLIMATICA DE LA ALTA CUENCA DEL RÍO NEUQUÉN, ANDES PATAGONICOS

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Griselda Ostertag

2005-12-01

Full Text Available En el desarrollo del presente documento se analizan las principales variables meteorológicas, temperatura y precipitación, que caracterizan y definen el clima de la Cordillera de los Andes en la Patagonia, provincia de Neuquén, particularmente en el área que ocupa la alta cuenca del río Neuquén. En esta etapa, de tipo descriptiva, el análisis estadístico refleja la situación de la climatología regional en el nivel medio histórico mediante la evaluación del comportamiento de las variables mencionadas durante los últimos 25 años. En este período se han registrado eventos extremadamente húmedos como así también situaciones de sequía. El objetivo es realizar una evaluación climática a partir de la información “in situ” de estaciones meteorológicas, información satelital y análisis estadístico para definir a posteriori, en cuál clasificación climática puede encuadrarse la zona de estudio, qué tipos climáticos pueden definirse en función de la bibliografía existente al respecto, y evaluar el grado de ajuste que presentan los climas determinados con los demás componentes del paisaje tales como vegetación y suelos.

Cold episodes in the Peruvian Central Andes: Composites, Types, and their Impacts over South America (1958-2014)

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Sulca, J. C.; Vuille, M. F.; Roundy, P. E.; Trasmonte, G.; Silva, Y.; Takahashi, K.

2015-12-01

The Mantaro basin (MB) is located in the central Peruvian Andes. Occasionally, cold episodes are observed during austral summer (January-March), that strongly damage crops. However, little is known about the causes and impacts of such cold episodes. The main goal of this study is thus to characterize cold episodes in the MB and assess their large-scale circulation and teleconnections over South America (SA) during austral summer. To identify cold events in the MB daily minimum temperature (Tmin) for the period 1958-2014 from Huayao station, located within the MB was used. A cold episode is defined when daily minimum temperature drops below its 10-percentile for at least one day. Additionally, to study the sensitivity between physical mechanisms associated with cold episodes and temperature, cold episodes are classified in three groups: Weak cold episodes (7.5 ≤ Tmin ≤ 10 percentile), strong cold episodes (Tmin ≤ 2.5 percentile), but excluding the 9 coldest events (Tmin ≤ 0 ͦ C), henceforth referred to as extraordinary cold episodes. Several gridded reanalysis were used to characterize the large-scale circulation, cloud cover and rainfall over SA associated with these events. Weak and strong cold episodes in the MB are mainly associated with a weakening of the Bolivian High-Nordeste Low system by tropical-extratropical interactions. Both types of cold episodes are associated with westerly wind anomalies at mid- and upper-tropospheric levels aloft the Peruvian Central Andes, which inhibit the influx of humid air masses from the lowlands to the east and hence limit the development of cloud cover (e.g., positive OLR anomalies over MB). The resulting clear sky conditions cause nighttime temperatures to drop, leading to cold extremes below 10-percentile. Simultaneously, northeastern Brazil (NEB) registers negative OLR anomalies, strong convection and enhanced cloud cover because displacement of the South Atlantic Convergence Zone (SACZ) toward the northeast of

Volcanic deformation in the Andes

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Riddick, S.; Fournier, T.; Pritchard, M.

2009-05-01

We present the results from an InSAR survey of volcanic activity in South America. We use data from the Japanese Space Agency's ALOS L-band radar satellite from 2006-2009. The L-band instrument provides better coherence in densely vegetated regions, compared to the shorter wave length C-band data. The survey reveals volcano related deformation in regions, north, central and southern, of the Andes volcanic arc. Since observations are limited to the austral summer, comprehensive coverage of all volcanoes is not possible. Yet, our combined observations reveal volcanic/hydrothermal deformation at Lonquimay, Llaima, Laguna del Maule, and Chaitén volcanoes, extend deformation measurements at Copahue, and illustrate temporal complexity to the previously described deformation at Cerro Hudson and Cordón Caulle. No precursory deformation is apparent before the large Chaitén eruption (VEI_5) of 2 May 2008, (at least before 16 April) suggesting rapid magma movement from depth at this long dormant volcano. Subsidence at Ticsani Volcano occurred coincident with an earthquake swarm in the same region.

Unraveling the diversification history of grasshoppers belonging to the “Trimerotropis pallidipennis” (Oedipodinae: Acrididae species group: a hotspot of biodiversity in the Central Andes

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Noelia Verónica Guzmán

2017-09-01

Full Text Available The Andean Mountain range has been recognized as one of the biodiversity hotspots of the world. The proposed mechanisms for such species diversification, among others, are due to the elevation processes occurring during the Miocene and the intensive glacial action during the Pleistocene. In this study we investigated the diversification history of the grasshopper Trimerotropis pallidipennis species complex which shows a particularly wide latitudinal and altitudinal distribution range across the northern, central and southern Andes in South America. Many genetic lineages of this complex have been so far discovered, making it an excellent model to investigate the role of the central Andes Mountains together with climatic fluctuations as drivers of speciation. Phylogenetics, biogeographic and molecular clock analyses using a multi-locus dataset revealed that in Peru there are at least two, and possibly four genetic lineages. Two different stocks originated from a common ancestor from North/Central America—would have dispersed toward southern latitudes favored by the closure of the Panama Isthmus giving rise to two lineages, the coastal and mountain lineages, which still coexist in Peru (i.e., T. pallidipennis and T. andeana. Subsequent vicariant and dispersal events continued the differentiation process, giving rise to three to six genetic lineages (i.e., clades detected in this study, which were geographically restricted to locations dispersed over the central Andes Mountains in South America. Our results provide another interesting example of “island diversification” motored by the topography plus unstable climatic conditions during the Pleistocene, pointing out the presence of a hotspot of diversification in the Andean region of Peru.

Palabras y silencios: la retórica del poder en los Andes

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1997-01-01

Full Text Available PAROLES ET SILENCES : LA RETHORIQUE DU POUVOIR DANS LES ANDES. La parole condense différents arguments et formes de pouvoir dans les sociétés andines. Le domaine social et le cadre cérémoniel appartiennent à ceux qui articulent bien les mots. La différenciation entre la valeur octroyée à la parole et celle correspondant aux silences implique diverses modalités de prestige de reconnaissance sociale et de pouvoir rituel dans les Andes. Les personnes, les vivants et les savants exercent une maîtrise subtile de la parole face aux étrangers, aux défunts et aux sots, qui demeurent socialement “muets”, silencieux. La palabra condensa diferentes argumentos y formas de poder en las sociedades andinas. El dominio social y el ámbito ceremonial pertenecen a los buenos articuladores de palabras. La diferenciación entre el valor otorgado a la palabra y el que corresponde a los silencios implica diferentes modalidades de prestigio, reconocimiento social y poder ritual en los Andes. Las personas, los vivos y los sabios ejercen un dominio exquisito de la palabra frente a los extraños, los difuntos y los “necios” que permanecen socialmente “mudos”, callados. WORDS AND SILENCES: THE RHETORIC OF POWER IN THE ANDES. Words have different meanings and means to exercise power in Andean societies. Social power and ceremonial environments belong people who are fluent in language. The difference between the value ascribed to the spoken word and that ascribed to silence implies several kinds of prestige, social recognition and ritual power in the Andes. “Ordinary”, alive and wise people exert an exquisite authority with words as compared with strange, dead and “stupid people” who remain socially 'dumb', silent.

Las sociedades anónimas cruzan los Andes: los inversores chilenos en Neuquén al comenzar el siglo XX

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Graciela Blanco

2012-08-01

Full Text Available El territorio de Neuquén, en el norte de la Patagonia, atrajo la mirada de diversos inversores privados a partir del avance militar que realizó el Estado nacional sobre los grupos indígenas y de la conquista de las tierras del sur argentino; tierras que fueron ofrecidas a particulares en propiedad o arrendamiento en condiciones muy beneficiosas. Este trabajo analiza la conformación en Chile, en los primeros años del siglo XX, de sociedades anónimas que explicitaban como objetivo central la intención de comprar tierras a ambos lados de la Cordillera de los Andes para la explotación agroganadera y la comercialización, y estudia específicamente el origen, itinerario y organización productiva de una de esas sociedades en Neuquén.Neuquen territory, in the north of the Patagonia, attracted the look of diverse investors after from the military advance that realized the national State on the indigenous groups and of the conquest of the lands of the Argentine's south, lands that were offered to individuals in property or lease in very beneficial conditions. This work analyzes the conformation in Chile, in the first years of the 20th century, of joint-stock companies that stated explicitly as central aim the intention of buying lands on both sides of the Mountain chain of the Andes for the agricultural and livestock exploitation and the commercialization, and there studies specifically the origin, itinerary and productive organization of one of these companies in Neuquen.

A millennium of metallurgy recorded by lake sediments from Morococha, Peruvian Andes.

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Cooke, Colin A; Abbott, Mark B; Wolfe, Alexander P; Kittleson, John L

2007-05-15

To date, information concerning pre-Colonial metallurgy in South America has largely been limited to the archaeological record of artifacts. Here, we reconstruct a millennium of smelting activity in the Peruvian Andes using the lake-sediment stratigraphy of atmospherically derived metals (Pb, Zn, Cu, Ag, Sb, Bi, and Ti) and lead isotopic ratios (206Pb/ 207Pb) associated with smelting from the Morococha mining region in the central Peruvian Andes. The earliest evidence for metallurgy occurs ca. 1000 A.D., coinciding with the fall of the Wari Empire and decentralization of local populations. Smelting during this interval appears to have been aimed at copper and copper alloys, because of large increases in Zn and Cu relative to Pb. A subsequent switch to silver metallurgy under Inca control (ca. 1450 to conquest, 1533 A.D.) is indicated by increases in Pb, Sb, and Bi, a conclusion supported by further increases of these metals during Colonial mining, which targeted silver extraction. Rapid development of the central Andes during the 20th century raised metal burdens by an order of magnitude above previous levels. Our results represent the first evidence for pre-Colonial smelting in the central Peruvian Andes, and corroborate the sensitivity of lake sediments to pre-Colonial metallurgical activity suggested by earlier findings from Bolivia.

Primer registro del ratón colombiano del bosque Chilomys instans (Cricetidae: Rodentia en Cajamarca: actualizando el listado de mamíferos del Perú

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César E. Medina

2016-12-01

Full Text Available El roedor Chilomys instans (Thomasomyini, Cricetidae es una especie común en la comunidad de mamíferos que habita los Andes del Norte en Sudamérica. Aquí presentamos el primer registro de la especie para el Perú, en base a la revisión morfológica de tres ejemplares colectados en el departamento de Cajamarca (Andes del Centro. Se presentan comentarios sobre la taxonomía de C. instans e información sobre su historia natural. La amplia distribución del género Chilomys en los Andes pone de manifiesto la necesidad de realizar la revisión taxonómica de éste género para esclarecer los límites de las especies que la conforman.

Influencia del fenómeno ENSO sobre la precipitación nival en el sector andino de Chile central durante el invierno

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1998-01-01

Full Text Available INFLUENCE DU PHÉNOMÈNE ENSO SUR LES PRÉCIPITATIONS NEIGEUSES DANS LE CENTRE DU CHILI ANDIN AU COURS DE L’HIVER AUSTRAL. On analyse l’influence du phénomène El Niño/Oscillation du Sud (ENSO sur les précipitations nivales dans les Andes du Chili central au cours de l’hiver. Pour cela, on a utilisé l’information obtenue sur des sites spécifiques (routes de neige situées entre 30° et 38° S et les anomalies de Température de Surface de la Mer (TSM du bloc Niño 3, comme indicateur de l’importance des événements chauds ou froids dans le Pacifique équatorial central. Au nord de 35°S, l’accumulation de neige tend à être supérieure à la normale quand l’anomalie moyenne de TSM dépasse +1°C au cours de la période mai-août. Dans ce même secteur, on enregistre une précipitation inférieure à la normale les hivers caractérisés par une anomalie de TSM inférieure à -0,5°C. Dans la zone située au sud de 35° S, l’influence du phénomène ENSO sur l’accumulation de neige n’est plus significative. Se analiza la influencia del fenómeno El Niño/Oscilación del Sur (ENSO sobre la precipitación nival en los Andes de Chile central durante el invierno. Para esto, se utiliza información de rutas de nieve localizadas entre 30° y 38° S, y de anomalías de temperatura superficial del mar (TSM en la región Niño 3 como un indicador de la magnitud de los eventos cálidos y fríos en el Pacífico ecuatorial central. En la región al norte de 35° S, la acumulación de nieve durante el invierno tiende a ser superior a lo normal cuando la magnitud de la anomalía media de TSM en el periodo mayo-agosto supera +1,0° C. En este mismo sector se verifica que durante los inviernos caracterizados por una anomalía de TSM inferior a -0,5° C, suele registrarse una precipitación nival inferior a lo normal. En el sector al sur de los 35° S, la influencia del fenómeno ENSO sobre la acumulación de nieve durante el invierno no es

Categorías conceptuales sobre la producción y gerencia del conocimiento en la Universidad de los Andes (ULA)

OpenAIRE

Rincón de Parra, Haydeé Cecilia; Briceño, Magally

2008-01-01

Esta investigación presenta como objetivo construir categorías conceptuales, a partir de lo expresado por un grupo de diez profesores-investigadores, sobre la forma en que se gerencia el proceso de producción de conocimiento en la Universidad de Los Andes. Para la recogida y análisis de los datos se consideraron algunos lineamientos de la Teoría Fundamentada. Se construyeron cinco categorías conceptuales: a) producción de conocimiento, b) filosofía del conocimiento como sustento, c) difusión ...

(Plio-)Pleistocene alluvial-lacustrine basin infill evolution in a strike-slip active zone (Northern Andes, Western-Central Cordilleras, Colombia)

OpenAIRE

SUTER, F.; NEUWERTH, R.; GORIN, G.; GUZMÁN, C.

2009-01-01

The (Plio)-Pleistocene Zarzal Formation was deposited in the Cauca Depression and Quindío-Risaralda Basin between the Western and Central Cordilleras (Northern Andes). This area is structurally located on the transcurrent Romeral Fault System (RFS). Because of the interaction between the Nazca plate and the Chocó-Panamá block (an active indenter), the RFS strike-slip component changes direction around the study zone (dextral in the south, senestral in the north). Zarzal sediments are the olde...

Linchamientos y conflicto político en Los Andes Lynchings and Political conflict in The Andes

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Carlos M. Vilas

2007-06-01

Full Text Available En 2004, los alcaldes de dos municipalidades de la región aimara de los Andes fueron linchados en la aparente culminación de agudos conflictos políticos internos y entre las respectivas comunidades y el Estado central. En este artículo se discuten ambos casos con el fin de ilustrar las transformaciones experimentadas en años recientes en la organización y la dinámica interna de las comunidades andinas, y de la articulación conflictiva de la política local en los procesos e instituciones de más amplio alcance. Precariedad social e incapacidad o renuencia del Estado para responder con eficacia a demandas básicas de determinados grupos de población configuran enmarcamientos socioeconómicos e institucionales de los linchamientos. En contraste con enfoques que enfatizan en factores culturales tradicionales o en un supuesto nacionalismo indígena, en el artículo se destaca la gravitación de fenómenos y procesos político- institucionales recientes en la transformación cultural y política de las comunidades, en el modo en que éstas procesan sus conflictos internos y con el Estado central.In 2004, two municipalitys mayors form the aimara Andes of Peru and Bolivia were subjected to mass lynchings as a result of the apparent culmination of violent political confrontations. This paper deals with these events as dramatic illustrations of the transformations the Andean communities experienced during recent decades in their internal dynamics, as well as in the articulation of local politics to processes and institutions beyond the communal limits. Structural precariousness combined with the state's inability or reluctance to come to terms with social or political demands from relevant segments of the people in the communities set the socioeconomic and institutional stage for lynchings. In contrast with approaches relating these events to an alleged indigenous cultural identity, the analysis points to the impact of the communities' political

Low-pressure evolution of arc magmas in thickened crust: The San Pedro-Linzor volcanic chain, Central Andes, Northern Chile

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Godoy, Benigno; Wörner, Gerhard; Kojima, Shoji; Aguilera, Felipe; Simon, Klaus; Hartmann, Gerald

2014-07-01

Magmatism at Andean Central Volcanic Zone (CVZ), or Central Andes, is strongly influenced by differentiation and assimilation at high pressures that occurred at lower levels of the thick continental crust. This is typically shown by high light to heavy rare earth element ratios (LREE/HREE) of the erupted lavas at this volcanic zone. Increase of these ratios with time is interpreted as a change to magma evolution in the presence of garnet during evolution of Central Andes. Such geochemical signals could be introduced into the magmas be high-pressure fractionation with garnet on the liquidus and/or assimilation from crustal rocks with a garnet-bearing residue. However, lavas erupted at San Pedro-Linzor volcanic chain show no evidence of garnet fractionation in their trace element patterns. This volcanic chain is located in the active volcanic arc, between 22°00‧S and 22°30‧S, over a continental crust ˜70 km thick. Sampled lavas show Sr/Y and Sm/Yb ratios Chile. We relate our geochemical observations to shallow crustal evolution of primitive magmas involving a high degree of assimilation of upper continental crust. We emphasize that low pressure AFC- (Assimilation Fractional Crystallization) type evolution of the San Pedro-Linzor volcanic chain reflects storage, fractionation, and contamination of mantle-derived magmas at the upper felsic crust (<40 km depth). The ascent of mantle-derived magmas to mid-crustal levels is related with the extensional regime that has existed in this zone of arc-front offset since Late-Miocene age, and the relatively thin portion of mafic lower crust observed below the volcanic chain.

Andes: An intelligent homework helper

Science.gov (United States)

van de Sande, Brett; Vanlehn, Kurt; Treacy, Don; Shelby, Bob; Wintersgill, Mary

2007-03-01

Andes (www.andes.pitt.edu) is an intelligent tutor homework system designed for use as the homework portion of an introductory physics course. It encourages students to use good problem solving techniques and provides immediate feedback on each step of a problem solution along with hints on request. I will discuss how Andes works, from a student perspective, and present research demonstrating its effectiveness as a pedagogical tool. Then, I will discuss using Andes as a tool for conducting education research, briefly reviewing several studies conducted using Andes. Finally, I will show how logs of student solutions to Andes problems can be used to develop cognitive models of student learning.

The role of climate in the accumulation of lithium-rich brine in the Central Andes

International Nuclear Information System (INIS)

Godfrey, L.V.; Chan, L.-H.; Alonso, R.N.; Lowenstein, T.K.; McDonough, W.F.; Houston, J.; Li, J.; Bobst, A.; Jordan, T.E.

2013-01-01

Highlights: • δ 7 Li of waters and rocks in the Central Andes were measured. • Halite/brine partition coefficients of lithium and δ 7 Li of halite were determined. • Li-rich brines have a high component of fluids of geothermal origin. • Removal of lithium by clays is minor relative to other regions of the world. • The weathering flux of lithium and sodium decouple according to climate state. - Abstract: Lithium-rich brine within the sub-surface of the Salar del Hombre Muerto (SHM) salt pan in the Andes of northwestern Argentina has a chemical and isotopic composition which is consistent with Li derived from several sources: the modern halite saturated lagoon, Li-rich salts and brines formed recently, and dissolution of halite which precipitated from ancient saline lakes. SHM lies in the closed basin that includes part of the massive Cerro Galán caldera which is drained by the Río los Patos, which is responsible for 90% of surface runoff into the salar. The low Li isotope composition, +3.4‰, of this river is consistent with significant contributions of geothermal spring water. As water drains through the volcaniclastic deposits which cover a large proportion of the basin, Li removal, as indicated by decreasing Li/Na, occurs but without significant isotope fractionation. This indicates a mechanism of surface sorption onto smectite or ferrihydrite rather than Li incorporation into octahedral structural sites of clays. These observations suggest that conditions in this high altitude desert have limited the dilution of hydrothermal spring water as well as the formation of clay minerals, which jointly have allowed the Li resource to accumulate rapidly. Changes in climate on a multi-millennial time scale, specifically in the hydrologic budget, have resulted in solute accumulation rates that have been variable through time, and decoupled Li and Na fluxes. Inflow to the salar under modern conditions has high Li/Na (7.9 × 10 −3 by wt) with δ 7 Li

Structural control on arc volcanism: The Caviahue Copahue complex, Central to Patagonian Andes transition (38°S)

Science.gov (United States)

Melnick, Daniel; Folguera, Andrés; Ramos, Victor A.

2006-11-01

This paper describes the volcanostratigraphy, structure, and tectonic implications of an arc volcanic complex in an oblique subduction setting: the Caviahue caldera Copahue volcano (CAC) of the Andean margin. The CAC is located in a first-order morphotectonic transitional zone, between the low and narrow Patagonian and the high and broad Central Andes. The evolution of the CAC started at approximately 4-3 Ma with the opening of the 20 × 15 km Caviahue pull-apart caldera; Las Mellizas volcano formed inside the caldera and collapsed at approximately 2.6 Ma; and the Copahue volcano evolved in three stages: (1) 1.2-0.7 Ma formed the approximately 1 km thick andesitic edifice, (2) 0.7-0.01 Ma erupted andesitic-dacitic subglacial pillow lavas, and (3) 0.01-0 Ma erupted basaltic-andesites and pyroclastic flows from fissures, aligned cones, and summit craters. Magma ascent has occurred along planes perpendicular to the least principal horizontal stress, whereas hydrothermal activity and hot springs also occur along parallel planes. At a regional scale, Quaternary volcanism concentrates along the NE-trending, 90 km long Callaqui-Copahue-Mandolegüe lineament, the longest of the southern volcanic zone, which is here interpreted as an inherited crustal-scale transfer zone from a Miocene rift basin. At a local scale within the CAC, effusions are controlled by local structures that formed at the intersection of regional fault systems. The Central to Patagonian Andes transition occurs at the Callaqui-Copahue-Mandolegüe lineament, which decouples active deformation from the intra-arc strike-slip Liquiñe-Ofqui fault zone to the south and the backarc Copahue-Antiñir thrust system.

Non-volant mammals in a protected area on the Central Andes of Colombia: new records for the Caldas department and the Chinchiná River basin

OpenAIRE

Ramírez-Mejía, Andrés; Sánchez, Francisco

2015-01-01

The Chinchiná River basin is located on the western slope of the Colombian Central Andes. This basin provides ecosystem services such as water provision for >500,000 people, but has suffered considerable ecosystem degradation, and the information on its biodiversity is limited. We inventoried the non-volant mammals in the Caldas' Central Hydroelectric (CHEC) Reserve in the Chinchiná River basin, in the Caldas department. We detected 18 species of mammals, present the first record of Puma ya...

The Influence of the Madden-Julian Oscillation (mjo) on Extreme Rainfall Over the Central and Southern Peruvian Andes

Science.gov (United States)

Heidinger, H.; Jones, C.; Carvalho, L. V.

2015-12-01

Extreme rainfall is important for the Andean region because of the large contribution of these events to the seasonal totals and consequent impacts on water resources for agriculture, water consumption, industry and hydropower generation, as well as the occurrence of floods and landslides. Over Central and Southern Peruvian Andes (CSPA), rainfall exceeding the 90th percentile contributed between 44 to 100% to the total Nov-Mar 1979-2010 rainfall. Additionally, precipitation from a large majority of stations in the CSPA exhibits statistically significant spectral peaks on intraseasonal time-scales (20 to 70 days). The Madden-Julian Oscillation (MJO) is the most important intraseasonal mode of atmospheric circulation and moist convection in the tropics and the occurrence of extreme weather events worldwide. Mechanisms explaining the relationships between the MJO and precipitation in the Peruvian Andes have not been properly described yet. The present study examines the relationships between the activity and phases of the MJO and the occurrence of extreme rainfall over the CSPA. We found that the frequency of extreme rainfall events increase in the CSPA when the MJO is active. MJO phases 5, 6 and 7 contribute to the overall occurrence of extreme rainfall events over the CSPA. However, how the MJO phases modulate extreme rainfall depends on the location of the stations. For instance, extreme precipitation (above the 90th percentile) in stations in the Amazon basin are slightly more sensitive to phases 2, 3 and 4; the frequency of extremes in stations in the Pacific basin increases in phases 5, 6 and 7 whereas phase 2, 3 and 7 modulates extreme precipitation in stations in the Titicaca basin. Greater variability among stations is observed when using the 95th and 99th percentiles to identify extremes. Among the main mechanisms that explain the increase in extreme rainfall events in the Peruvian Andes is the intensification of the easterly moisture flux anomalies, which

Low-grade metamorphism of Cambro-Ordovician successions in the Famatina belt, Southern-Central Andes: Burial-inversion history linked to the evolution of the proto-Andean Gondwana margin Metamorfismo de bajo grado de sucesiones cambro-ordovícicas en el cinturón del Famatina, Andes Centrales de Argentina: Historia de enterramiento-exhumación ligada a la evolución del margen proto-andino de Gondwana

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Gilda Collo

2011-07-01

.Las condiciones P-T del metamorfismo de las unidades de bajo grado del cinturón del Famatina, Andes Centrales de Argentina, fueron estimadas mediante petrografía, difracción de rayos-X y microscopía electrónica. La Formación Negro Peinado (Cámbrico Medio-Superior fue afectada por un evento tectono-metamórfico asociado con un plegamiento intrafoliar intenso, para el cual se estimaron temperaturas entre 290 y 400°C (IKcis: 0,16-0,27 A°29, blástesis de biotita y homogeneidad composicional en micas dioctaédricas y presiones intermedias (parámetro b de la mica blanca: 9,010 Á y 9,035 Á. La Formación Achavil (Cámbrico Medio-Superior presenta un evento metamórfico asociado con temperaturas entre 200 y 290°C (KIcis: 0,26-0,41A°29 y condiciones de presión intermedias-bajas (parámetro b de la mica blanca: 8,972Á-9,017Á. Para las sucesiones comprendidas entre el Cámbrico Superior y el Ordovícico Medio, se identificó un patrón metamórfico de soterramiento, con una disminución progresiva en el grado metamórfico desde la Formación Volcancito hasta el Grupo Cerro Morado (ca. 490-465 Ma; IKcis: 0,31-0,69 A°29 y ausencia de cambios de tendencia ligados a las discontinuidades estratigráficas. La mica blanca y la clorita son los principales filosilicatos en las unidades más antiguas, mientras los interestratificados Ilt/Sme (R3 son casi exclusivos en las más jóvenes. El parámetro b de la mica blanca indica condiciones de presión intermedia-baja para estas unidades. Este patrón metamórfico de soterramiento presenta un marcado quiebre hacia la unidad ordovícica más joven (Formación La Aguadita, posterior a los ca. 452 Ma con temperaturas estimadas entre 270 y 330°C (IKcis: 0,28-0,19A°29 y condiciones de presión intermedias. Nuestros resultados indican que los procesos relacionados con la contracción e inversión de la cuenca durante la orogenia Oclóyica involucran en esta región al menos dos episodios metamórficos bien diferenciados y no superpuestos.

Estructura y composición de las comunidades de macroinvertebrados acuáticos en ríos altoandinos del Ecuador y Perú. Diseño de un sistema de medida de la calidad del agua con índices multimétricos

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Villamarín Flores, Christian Patricio

2012-01-01

[spa] En la presente tesis se muestrearon ríos sobre los 2000 msnm (ríos altoandinos tropicales) que se distribuyen en la amplia región de los Andes del Norte (Ecuador) y los Andes Centrales (Perú) en Sudamérica. El muestreo de las 123 localidades se realizó en época seca, las cuales se seleccionaron tomando en cuenta su grado de alteración, que van desde sin o poca alteración (referencia) hasta muy alterados. En una primera instancia se analizaron las carácteristicas fisicoquímicas e hid...

Limitación de la conservación de variedades nativas por variedades mejoradas: Estudio de caso de la papa en los Andes centrales del Ecuador

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MSc. María Cecilia Dávila

2018-04-01

Full Text Available La conservación de la biodiversidad para la alimentación y la agricultura, es una actividad importante a nivel mundial para asegurar la seguridad alimentaria y nutricional, pero dicha actividad está siendo limitada por varios factores. Este estudio de caso analiza cómo la adopción de variedades mejoradas de papa limita la conservación de la diversidad de las variedades nativas a nivel de granja o chakra en seis comunidades indígenas en los Andes centrales ecuatorianos. Los resultados muestran que la adopción de variedades mejoradas ha desplazado una amplia gama de variedades locales tradicionales de los campos de agricultores que, junto con las condiciones socioeconómicas y ambientales que caracterizaron el sitio de estudio, han socavado la diversidad genética de variedades cultivadas de papa en las fincas. Palabras clave: Conservación en finca, diversidad de papa, variedades mejoradas, variedades nativas.

La implantación de la viruela en los Andes, la historia de un holocausto

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Uriel García Cáceres

2003-03-01

Full Text Available La historia de las epidemias de viruela en los Andes tiene el carácter tétrico del relato de un holocausto. Esta presentación está destinada a resaltar las etapas más importantes del proceso de la implantación de la viruela en las poblaciones andinas en general y, en particular, en el Perú, desde principio del siglo XVI hasta nuestros días.

Relationships between mineralization and silicic volcanism in the central Andes

Energy Technology Data Exchange (ETDEWEB)

Francis, P.W.; Halls, C.; Baker, M.C.W.

1983-10-01

Studies of late Tertiary silicic volcanic centers in the Western and Eastern Cordilleras of the Central Andes show that three volcanic environments are appropriate sites for mineralization: (1) ring-fracture extrusions post-dating large calderas; (2) similar extrusions within ignimbrite shields; and (3) isolated, small silicic volcanoes. Subvolcanic tin mineralization in the Eastern Cordillera is located in silicic stocks and associated breccias of Miocene age. The Cerro Rico stock, Potosi, Bolivia, contains tin and silver mineralization and has an intrusion age apparently millions of years younger than that of the associated Kari Kari caldera. Similar age relationships between mineralization and caldera formation have been described from the San Juan province, Colorado. The vein deposits of Chocaya, southern Bolivia, were emplaced in the lower part of an ignimbrite shield, a type of volcanic edifice as yet unrecognized in comparable areas of silicic volcanism. The El Salvador porphyry copper deposit, Chile, is related to silicic stocks which may have been intruded along a caldera ring fracture. Existing models for the genesis of porphyry copper deposits suggest that they formed in granodioritic stocks located in the infrastructure of andesitic stratovolcanoes. The dome of La Soufriere, Guadeloupe is proposed as a modern analog for the surface expression of subvolcanic mineralization processes, the phreatic eruptions there suggesting the formation of hydrothermal breccia bodies in depth.

Aproximaciones Biológicas y Fisicoquímicas en el tratamiento de contaminantes: un resumen del aporte de la Universidad de los Andes

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Jenny Dussan Garzón

2009-11-01

Full Text Available Este resumen pretende dar una visión global de los aportes de la Universidad de los Andes en el tratamiento de aguas y suelos con la presencia de compuestos de difícil degradación o tiempo de vida media prolongado, tales como fármacos (Ciclofosfamida, lodos aceitosos y derivados de la industria del petróleo (Tolueno, Xileno, Fenol derivados de la industria textil, química y pesticidas (Bisphenol A, AMBI, Glifosato, Isoproturon y Metobromuron, usando tecnologías ya sea basadas en procesos biológicos (biorremediación y bioadsorción o de oxidación avanzada (foto-Fenton. /This summary intends to give a global view of the Universidad de los Andes contributions related to the water and soil treatment in the presence of recalcitrant or long half-life aquatic pollutants such as drugs (Cyclophosphamide, oil sludge and petroleum (Toluene, Xylene and Phenol, textile, chemical (Bisphenol A, AMBI and pesticides (Glyphosate, Isoproturon, and Metobromuron industry derived products based on biological (bioremediation and bioadsortion and advanced oxidation (Photo-Fenton approaches.

A glassy lava flow from Toconce volcano and its relation with the Altiplano-Puna Magma Body in Central Andes

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Godoy, B.; Rodriguez, I.; Aguilera, F.

2012-12-01

Toconce is a composite stratovolcano located at the San Pedro - Linzor volcanic chain (SPLVC). This volcanic chain distributes within the Altiplano-Puna region (Central Andes) which is characterized by extensive rhyodacitic-to-rhyolitic ignimbritic fields, and voluminous domes of dacitic-to-rhyolitic composition (de Silva, 1989). The felsic melts that gave origin to ignimbrites and domes at this area were generated by mixing of mantle-derived magmas and anatectic melts assimilated during their ascent through the thick crust. Thus, partially molten layers exist in the upper crust below the APVC (de Silva et al., 2006). Evidence of large volumes of such melts has been also proposed by geophysical methods (i.e. the Altiplano-Puna Magma Body; Chmielowsky et al., 1999) In this work, petrography and whole rock, mineralogical and melt inclusions geochemistry of a glassy lava flow of Toconce volcano are presented. Petrographically, this lava flow shows a porphyric texture, with euhdral to subhedral plagioclase, ortho- and clino-pyroxene phenocrysts immersed in a glassy groundmass. Geochemically, the lava flow has 64.7% wt. SiO2. The glassy groundmass (~70% wt. SiO2) is more felsic than all the lavas in the volcanic chain (47-68% wt., Godoy et al., 2011). Analyzed orthopyroxene-hosted melt inclusions show an even higher SiO2 content (72-75% wt.), and a decreasing on Al2O3, Na2O, and CaO content with differentiation. Crystallization pressures of this lava flow, obtained using Putirka's two-pyroxene and clinopyroxene-liquid models (Putirka, 2008), range between 6 and 9 kbar. According to crystallization pressures, and major element composition, a felsic source located at shallow crustal pressures - where plagioclase is a stable mineralogical phase - originated the inclusions. This could be related to the presence of the Altiplano-Puna Magma Body (APMB) located below SPLVC. On the other hand, glassy groundmass, and disequilibrium textures in minerals of this lava flow could

The Mass Elevation Effect of the Central Andes and Its Implications for the Southern Hemisphere's Highest Treeline

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Wenhui He

2016-05-01

Full Text Available One of the highest treelines in the world is at 4810 m above sea level on the Sajama Volcano in the central Andes. The climatological cause of that exceptionally high treeline position is still unclear. Although it has been suggested that the mass elevation effect (MEE explains the upward shift of treelines in the Altiplano region, the magnitude of MEE has not yet been quantified for that region. This paper defines MEE as the air temperature difference in summer at the same elevation between the inner mountains/plateaus (Altiplano and the free atmosphere above the adjacent lowlands of the Andean Cordillera. The Altiplano air temperature was obtained from the Global Historical Climatology Network-Monthly temperature database, and the air temperature above the adjacent lowlands was interpolated based on the National Center for Environmental Prediction/National Center for Atmospheric Research Reanalysis 1 data set. We analyzed the mean air temperature differences for January, July, and the warm months from October to April. The air temperature was mostly higher on the Altiplano than over the neighboring lowlands at the same altitude. The air temperature difference increased from the outer Andean east-facing slope to the interior of the Altiplano in summer, and it increased from high latitudes to low latitudes in winter. The mean air temperature in the Altiplano in summer is approximately 5 K higher than it is above the adjacent lowlands at the same mean elevation, averaging about 3700 m above sea level. This upward shift of isotherms in the inner part of the Cordillera enables the treeline to climb to 4810 m, with shrub-size trees reaching even higher. Therefore, the MEE explains the occurrence of one of the world’s highest treelines in the central Andes.

Mixed bird flocks: patterns of activity and species composition in a region of the Central Andes of Colombia Bandadas mixtas de aves: patrones de actividad y composición de especies en una región de la Cordillera Central de los Andes de Colombia

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Enrique Arbeláez-Cortés

2011-06-01

Full Text Available Mixed bird flocks are groups of individuals from different species that travel and forage together. Such groups are common in several bird communities around the world. We present species composition and activity patterns of mixed bird flocks in a region of the Central Andes of Colombia. We compared the number of species per flock, as well as the number of flocks among 3 different habitats. We tested hypotheses concerning the flocks daily activity and the co-occurrences of species within them. We recorded 75 species, and the species number per flock varied from 4 to 21. Our data suggest that habitat affects the number of flocks but not their species number, and that the activity of flocks is similar throughout the day. In addition, the association of birds in flocks is affected by interspecific facilitation, with some species co-occurrences found more times than expected by chance. We hypothesize that some tanager species could have a role in flock cohesion. We witnessed 2 predator attacks upon flocks, a number of agonistic interactions among flock members, and squirrels following bird flocks. Our results meet some general patterns described for mixed bird flocks.Las bandadas mixtas de aves son grupos de individuos de diferentes especies que viajan y forrajean juntos, y son comunes en varias comunidades de aves alrededor del mundo. Presentamos la composición de especies y los patrones de actividad de las bandadas mixtas de aves en una región de la Cordillera Central de los Andes Colombianos. Comparamos el número de especies por bandada y el número de bandadas en 3 hábitats distintos. Evaluamos hipótesis relacionadas con la actividad de las bandadas durante el día y la presencia simultánea de especies en estos grupos. Observamos 75 especies, y el número de especies por bandada varió entre 4 y 21. Nuestros datos indican que el hábitat parece afectar el número de bandadas pero no su número de especies y que la actividad de las bandadas

A survey of volcano deformation in the central Andes using InSAR: Evidence for deep, slow inflation

Science.gov (United States)

Pritchard, M. E.; Simons, M.

2001-12-01

We use interferometric synthetic aperture radar (InSAR) to survey about 50 volcanos of the central Andes (15-27o S) for deformation during the 1992-2000 time interval. Because of the remote location of these volcanos, the activity of most are poorly constrained. Using the ERS-1/2 C-band radars (5.6 cm), we observe good interferometric correlation south of about 21o S, but poor correlation north of that latitude, especially in southern Peru. This variation is presumably related to regional climate variations. Our survey reveals broad (10's of km), roughly axisymmetric deformation at 2 volcanic centers with no previously documented deformation. At Uturuncu volcano, in southwestern Bolivia, the deformation rate can be constrained with radar data from several satellite tracks and is about 1 cm/year between 1992 and 2000. We find a second source of volcanic deformation located between Lastarria and Cordon del Azufre volcanos near the Chile/Argentina border. There is less radar data to constrain the deformation in this area, but the rate is also about 1 cm/yr between 1996 and 2000. While the spatial character of the deformation field appears to be affected by atmosphere at both locations, we do not think that the entire signal is atmospheric, because the signal is observed in several interferograms and nearby edifices do not show similar patterns. The deformation signal appears to be time-variable, although it is difficult to determine whether this is due to real variations in the deformation source or atmospheric effects. We model the deformation with both a uniform point-source source of inflation, and a tri-axial point-source ellipsoid, and compare both elastic half-space and layered-space models. We also explore the effects of local topography upon the deformation field using the method of Williams and Wadge (1998). We invert for source parameters using the global search Neighborhood Algorithm of Sambridge (1998). Preliminary results indicate that the sources at both

Glaciation in the Andes during the Lateglacial and Holocene

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Rodbell, Donald T.; Smith, Jacqueline A.; Mark, Bryan G.

2009-10-01

This review updates the chronology of Andean glaciation during the Lateglacial and the Holocene from the numerous articles and reviews published over the past three decades. The Andes, which include some of the world's wettest and driest mountainous regions, offer an unparalleled opportunity to elucidate spatial and temporal patterns of glaciation along a continuous 68-degree meridional transect. The geographic and altitudinal extent of modern glaciers and the sensitivity of both modern and former glaciers to respond to changes in specific climatic variables reflect broad-scale atmospheric circulation and consequent regional moisture patterns. Glaciers in the tropical Andes and in the mid-latitude Andes are likely to have been far more sensitive to changes in temperature than glaciers in the dry subtropical Andes. Broad-scale temporal and spatial patterns of glaciation during the Lateglacial are apparent. In the southernmost Andes, the Lateglacial chronology appears to have a strong Antarctic signature with the best-dated moraines correlating closely with the Antarctic Cold Reversal. The southernmost Andes do not appear to have experienced a significant ice advance coeval with the Younger Dryas (YD) climatic reversal. At the other end of the Andes, from ˜0 to 9°N, a stronger YD connection may exist, but critical stratigraphic and geochronologic work is required before a YD ice advance can be fully demonstrated. In the central Andes of Peru, well-dated moraines record a significant ice readvance at the onset of the YD, but ice was retreating during much of the remaining YD interval. The spatial-temporal pattern of Holocene glaciation exhibits tantalizing but incomplete evidence for an Early to Mid-Holocene ice advance(s) in many regions, but not in the arid subtropical Andes, where moraines deposited during or slightly prior to the Little Ice Age (LIA) record the most extensive advance of the Holocene. In many regions, there is strong evidence for Neoglacial

Population dynamics of the rat Microryzomys minutus (Rodentia: Muridae in the Venezuelan Andes

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Daniel R Cabello

2006-06-01

Full Text Available The population dynamics of the small forest rice rat Microryzomys minutus, a murid rodent that occurs in the high altitudes of the northern and central Andes, was studied in disturbed and primary environments in a cloud forest of the Venezuelan Andes (Juan Pablo Peñaloza National Park, 8º11’N, 71º49’W. We collected 121 animals (66♀♀ and 55♂♂ between 1995 and 1998, using pitfall traps with formalin. Adult males were heavier than adult females. Relative abundance was much greater in the disturbed environments (over 10 individuals in some periods than in the primary cloud forest: 4-8 individuals. In the disturbed environments, the rats were extremely abundant in the first sampling period, and less frequent afterwards. In the cropland, abundance showed some fluctuations during the study and displayed two small abundance peaks in March-June 1997 and 1998. In the mined area, the rats had irregular fluctuations until March-June 1997 and were not recorded in July-October 1997. The occurrence of this rat in both disturbed and natural habitats confirms the wide ecological tolerance of this species. Rev. Biol. Trop. 54(2: 651-. Epub 2006 Jun 01.Se analizó la dinámica poblacional de las pequeñas ratas silvestres del arroz Microryzomys minutus en ambientes alterados y primarios, en un bosque nublado de los Andes venezolanos. El estudio fue basado en 121 animales (66♀♀ y 55♂♂ recolectados entre 1995 y 1998, usando trampas que contenían formalina. Esta especie está presente en ambos hábitats lo que confirma su amplia tolerancia ecológica. La abundancia poblacional fue mayor en ambientes alterados que en los no alterados. M. minutus presenta dimorfismo sexual en el peso: los machos son más pesados que las hembras.

Linfoma no-Hodgkin del sistema nervioso central

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Iglesias Rozas, José Rafael, 1942-

2000-01-01

Diecisiete imágenes de un linfoma no-Hodgkin del sistema nervioso central en una paciente de 66 años. Seventeen pictures of a non-Hodgkin lymphoma of the central nervous system in a 66-year-old female patient.

De la complementariedad a la voluntad de Aplanar los Andes: representaciones de la naturaleza y pensamiento económico y político en el Perú del siglo XX

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2001-01-01

Full Text Available DE LA COMPLÉMENTARITÉ À LA VOLONTÉ D’APLANIR LES ANDES : REPRÉSENTATIONS DE LA NATURE ET PENSÉE ÉCONOMIQUE ET POLITIQUE AU PÉROU AU COURS DU XXÈME SIÈCLE. La représentation la plus courante du territoire péruvien à l’échelle nationale est celle qui le divise en trois régions dites “naturelles”, la costa, la sierra et la selva. Mais cette division et chacun de ses éléments peuvent prendre différents sens et ont orienté la réflexion politique tantôt vers l’idée d’une complémentarité entre ces trois ensembles et entre les “étages écologiques” qui les composent, tantôt vers celle d’une opposition insurmontable entre les Andes et leur piémont côtier - le piémont amazonien n’étant que plus rarement au centre des débats -. Cette seconde “traduction” de la nature semble aujourd’hui la plus influente et la représentation “négative” de la montagne comme espace de pauvreté et d’isolement tend dans le contexte du néolibéralisme à l’emporter sur celle, plus positive et tout aussi construite, qui présente les Andes comme un territoire ayant permis la conservation d’une culture indigène authentique. La representación más común del territorio peruano a nivel nacional es la división en tres regiones consideradas como “naturales”, la costa, la sierra y la selva. Pero esa división y cada uno de sus elementos pueden tener diversos significados, de tal forma que guiaron la reflexión política en ocasiones hacia la idea de una complementariedad entre las tres partes y entre los pisos ecológicos que las componen, y otras veces hacia la de una oposición insalvable entre los Andes y su piedemonte costeño (mientras el amazónico suscitaba menos interés. La segunda de estas “traducciones” de la naturaleza parece ser hoy en día la más influyente: la representación “negativa” de la sierra como espacio de pobreza y de aislamiento tiende, dentro del contexto del neoliberalismo, a prevalecer sobre aqu

LA FRECUENCIA DEL USO DEL USTED EN TRES ZONAS DEL DEPARTAMENTO DE ANTIOQUIA (COLOMBIA

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Ji Son Jang

2014-06-01

Full Text Available En este trabajo se presentan algunos resultados de una investigación sobre la selección pronominal acerca del uso del usted, llevada a cabo en tres municipios del departamento colombiano de Antioquia: la ciudad de Medellín (zona urbana; Carmen de Viboral (zona semirrural, y Andes (zona rural. La población estudiada está constituida por los informantes de edades entre 13 y 34 años. La variable social para este artículo es el lugar de la vivienda de los informantes (zona urbana, semirrural o rural. Para llevar a cabo la investigación, se aplicó un cuestionario, en el cual aparecen distintos tipos interaccionales, a los informantes en las zonas mencionadas; se obtuvieron 1940 informantes. La estadística muestra que, en la gran mayoría de relaciones interpersonales, en Andes se usa más el usted que en Carmen de Viboral y, en este último municipio, más que en Medellín.

Distribución de Stenocercus guentheri (Sauria: Iguanidae en el sur de los Andes de Colombia

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Castro Herrera Fernando

1993-12-01

Full Text Available The morphology of a population of Stenocercus guentherifrom Colombia is described in detail and compared to information from ecuadorean specimens. The range of the species is extended northward to include the colombian departments (provinces of Nariño and Cauca along the Andes. Some field observations about bahavior, habitat, and reproduction are included.El presente trabajo describe las características de Stenocercus guentheri, en las poblaciones del sur de Colombia y hace una comparación con la información del Ecuador. Se amplía su rango de distribución geográfica hacia el norte de Suramérica, incluyendo los departamentos de Nariño y Cauca en los Andes de Colombia. Se incluyen datos de campo sobre hábitat, hábitos y reproducción.

Migraciones en la puna: su relación con el uso de los recursos naturales del departamento Los Andes Migraciones en la puna: su relación con el uso de los recursos naturales del departamento Los Andes

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Francisco R. Barbarán

2009-12-01

Full Text Available From an historic and demographic perspective, as well as the use of natural resources, we analyzed the relationship between human migrations and the economic activities of Los Andes Department, West of the Salta Province, in NW Argentina. Using the residual method, we calculated migratory balances between Argentinean population censuses carried out in 1947,1960, 1970, 1980 and 2001. The migratory balances were negative for all the periods studied. When the train started to run through Ramal C-14, the workers who built it have to find jobs somewhere else. At the same time, the railway made easier for the natives, to find better economicopportunities out of the Puna. The close of mine La Casualidad by the end of the 70’s, the low creation of jobs by the remaining mining operations, focused in to hire qualified technicians no available in Los Andes and the privatization of the railway in early 90’s, were important factors of emigration. Despite of cattle rising as the main economic activity in rural areas, it is practiced without any technology of management. The overgrazing caused for that reason, has reduced almost to the half the quantity of sheep by inhabitant between 1947 and 2001. That is why the local people have to press more on the wildlife, trading illegally with vicuña (Vicugna vicugna fiber. Despite of a touristic development plan, a law promoting sheep rising and a census of vicuña population carried out by the provincial government, these recent actions should be part of a development project of regional scale, oriented to the sustainable use of the natural resources of Los Andes Department. That project would create jobs and discourage emigration.Desde una perspectiva histórica, demográfica y del uso de los recursos naturales, analizamos la relación existente entre las migraciones humanas y las actividades económicas en el departamento Los Andes, ubicado al W de la provincia de Salta, en el Noroeste Argentino. Usando el m

De Los ríos profundos a Lituma en los andes: La respuesta de Mario Vargas Llosa a José María Arguedas

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Marie-Madeleine Gladieu

2011-05-01

Full Text Available La novela de Mario Vargas Llosa Lituma en los Andes1 poco tiene que ver, aparentemente, con el mundo narrativo de José María Arguedas: las nuevas aventuras de un personaje ficticio bien conocido de los lectores, presente en varias obras anteriores de aquel autor, en nada se asemejan a las del niño Ernesto ni a las de otro protagonista arguediano. Los Andes sirven de decorado para los dos relatos, pero entre la naturaleza y los pueblos que se suceden en Los ríos profundos2en toda su diversidad, y los paisajes hoscos y siempre peligrosos por los que cruza Lituma, apenas reconoce el lector aquella parte del sur peruano. Algunos detalles, sin embargo, al examinar bien el texto y el contexto de Lituma en los Andes, llaman la atención.

Ausentismo laboral de causa médica en el Instituto Autónomo Hospital Universitario de Los Andes.

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Parada de Denis, María Eugenia; Rivas Padilla, Fernando; Moreno Barrios, Reyla; Rincón, Eglis; Mejía, Zurayma; Mora, Dania Margarita

2006-01-01

Editorial. ¡Ya tenemos símbolo, ícono o logotipo!. Now we have symbol, icono or logo!. Salinas, Pedro José Accidentes domésticos en ancianos. Municipio Libertador. Mérida. 1993-1996. Domestics accidents in elderly people. Libertador County of Mérida State. 1993-1996. Salinas, Pedro José Rojas Márquez, Reina Estrés y síntomas en personal de salud del Hospital Universitario de Los Andes. Stress and symptoms in health staff of the Hospital Universitario de Los Andes. Méri...

Barren Miocene granitoids in the Central Andean metallogenic belt, Chile: Geochemistry and Nd-Hf and U-Pb isotope systematics Granitoides estériles del Mioceno en la franja metalogénica de los Andes Centrales, Chile: geoquímica e isotopía de Nd-Hf y U-Pb

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Katja Deckart

2010-01-01

across the NE-SW-trending Yeso Valley transfer fault, assumed as coeval, which also explains the local lack of easterly magmatic are front migration.Cuatro complejos plutónicos del Mioceno Temprano a Medio que se encuentran ubicados entre los depósitos de pórfidos gigantes de cobre de los Andes chileno centrales fueron seleccionados para un estudio de geocronología U-Pb por LA-ICPMS y de isótopos de Hf en granos individuales de circón. Estudios geoquímicos de elementos mayores y trazas y los isótopos de Sr-Nd-Hf en roca permiten compararlos con rocas intrusivas ligeramente más jóvenes o coetáneas estériles y fértiles entre 32° y 34°S. Los granitoides estudiados muestran edades de cristalización de 11,3±0,1 Ma (masivo Cerro Mesón Alto, 10,3±0,2 Ma (plutón La Gloria, 14,9±0,2 Ma/14,9±0,l Ma (Yerba Loca stock y 11,2±0,1 Ma/14,7±0,l Ma (Batolito San Francisco. Elementos mayores y trazas excluyen una característica adakítica, como ha sido sugerido para los intrusivos porfídicos a los 32°S, los pórfidos mineralizados ligeramente más jóvenes de Río Blanco-Los Bronces y otras adakitas del Cenozoico. Las rocas volcánicas de caja son menos fraccionadas que las unidades de rocas intrusivas. La misma conclusión se obtiene con relación a los plutones de la zona norte comparados a los del sur. Valores isotópico iniciales Sr-Nd muestran una variación insignificante (0,703761-0,704118 y 0,512758-0,512882 en el campo del manto. El enriquecimiento de elementos traza puede ser explicado a través de una adición de fluidos de la placa subducida y/o por sedimentos terrígenos transportados hacia la cuña de manto y/o por un leve aporte cortical durante el ascenso del magma. Granos de circón separados de los intrusivos estériles del grupo más joven (10-12 Ma; 7,04-9,54 comparten valores iniciales de sHf, pero los intrusivos más antiguos (14-15 Ma; 8,50-15,34, en comparación, representan un rango más amplio; ambos rangos de valores se proyectan en la

Evidence of Teleconnections between the Peruvian central Andes and Northeast Brazil during extreme rainfall events

Science.gov (United States)

Sulca, J. C.; Vuille, M. F.; Silva, F. Y.; Takahashi, K.

2013-12-01

Knowledge about changes in regional circulation and physical processes associated with extreme rainfall events in South America is limited. Here we investigate such events over the Mantaro basin (MB) located at (10°S-13°S; 73°W-76°W) in the central Peruvian Andes and Northeastern Brazil (NEB), located at (9°S-15°S; 39°W-46°W). Occasional dry and wet spells can be observed in both areas during the austral summer season. The main goal of this study is to investigate potential teleconnections between extreme rainfall events in MB and NEB during austral summer. We define wet (dry) spells as periods that last for at least 3 (5) consecutive days with rainfall above (below) the 70 (30) percentile. To identify the dates of ocurrence of these events, we used daily accumulated rainfall data from 14 climate stations located in the Mantaro basin for the period 1965 to 2002. In NEB we defined a rainfall index which is based on average daily gridded rainfall data within the region for the same period. Dry (wet spells) in the MB are associated with positive (negative) OLR anomalies which extend over much of the tropical Andes, indicating the large-scale nature of these events. At 200 hPa anomalous easterly (westerly) zonal winds aloft accompany wet (dry) spells. Composite anomalies of dry spells in MB reveal significant contemporaneous precipitation anomalies of the opposite sign over NEB, which suggest that intraseasonal precipitation variability over the two regions may be dynamically linked. Indeed upper-tropospheric circulation anomalies over the central Andes extend across South America and appear to be tied to an adjustment in the Bolivian High-Nordeste Low system. Dry (wet) spells in NEB are equally associated with a large-scale pattern of positive (negative) OLR anomalies; however, there are no related significant OLR anomalies over the MB during these events. Dry (wet) spells are associated with robust patterns of anomalous wind fields at both low and upper

Historia, mito, memoria: armas del presente y pilares de identidad. La política de la memoria. Interpretación indigena de la historia de los Andes Colombianos

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Sonia M. Jaimes

2002-01-01

Full Text Available Historia, mito, memoria: armas del presente y pilares de identidad Joanne Rappaport, La Política de la Memoria. Interpretación Indígena de la Historia en los Andes Colombianos. Popayán: Editorial Universidad del Cauca-Serie Estudios Sociales, 2000. Traducción de José Ramón Martín. Pp: 260. Entre 1978 Y1982 la antropóloga norteamericana Joanne Rappaport visitó la región del Suroccidente colombiano con el propósito de llevar a cabo una investigación sobre la concepción del espacio sagrado de una comunidad indígena. Su objeto de estudio: los paeces, hoy conocidos como Nasa nombre que apela a una reivindicación identitaria ancestral. De acuerdo a Rappaport remitirse al estudio de una comunidad indígena, exige que el ejercicio se haga bajo una mirada de carácter «totalizante», en gran medida por la estructura misma del pensamiento y la cosmovisión indígena.

Modeling Soil Organic Carbon Variation Along Climatic and Topographic Trajectories in the Central Andes

Science.gov (United States)

Gavilan, C.; Grunwald, S.; Quiroz, R.; Zhu, L.

2015-12-01

The Andes represent the largest and highest mountain range in the tropics. Geological and climatic differentiation favored landscape and soil diversity, resulting in ecosystems adapted to very different climatic patterns. Although several studies support the fact that the Andes are a vast sink of soil organic carbon (SOC) only few have quantified this variable in situ. Estimating the spatial distribution of SOC stocks in data-poor and/or poorly accessible areas, like the Andean region, is challenging due to the lack of recent soil data at high spatial resolution and the wide range of coexistent ecosystems. Thus, the sampling strategy is vital in order to ensure the whole range of environmental covariates (EC) controlling SOC dynamics is represented. This approach allows grasping the variability of the area, which leads to more efficient statistical estimates and improves the modeling process. The objectives of this study were to i) characterize and model the spatial distribution of SOC stocks in the Central Andean region using soil-landscape modeling techniques, and to ii) validate and evaluate the model for predicting SOC content in the area. For that purpose, three representative study areas were identified and a suite of variables including elevation, mean annual temperature, annual precipitation and Normalized Difference Vegetation Index (NDVI), among others, was selected as EC. A stratified random sampling (namely conditioned Latin Hypercube) was implemented and a total of 400 sampling locations were identified. At all sites, four composite topsoil samples (0-30 cm) were collected within a 2 m radius. SOC content was measured using dry combustion and SOC stocks were estimated using bulk density measurements. Regression Kriging was used to map the spatial variation of SOC stocks. The accuracy, fit and bias of SOC models was assessed using a rigorous validation assessment. This study produced the first comprehensive, geospatial SOC stock assessment in this

Antecedentes geobotánicos de una cuenca andina de Chile Central

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Quintanilla Pérez, V.

2004-12-01

Hautes Andes; près de la ville de Santiago du Chili. [es] Como todos los ecosistemas de montaña; los Andes de Chile presentan una especificidad fitoecológica importante; que se expresa por la acción de condiciones ecológicas muy particulares y por la presencia de comunidades vegetales que se individualizan por sus caracteres estructurales y funcionales. Estos caracteres son el resultado de una adecuación entre las características biológicas de las plantas sometidas a los efectos de la altitud (largo periodo frío; pero que también se benefician de ciertas reservas de agua a pesar del rigor de las condiciones climáticas. Se establece una zonación altitudinal de la vegetación; determinándose tres pisos vegetales; montano; subandino y andino; resaltándose la similitud florística de las comunidades vegetales del piso montano inferior con las de los valles centrales del país. También se aportan datos sobre los procesos geomorfológicos de montaña; que afectan a la vida y a la distribución de las plantas de estos ambientes. Se presenta un estudio de un caso concreto en la Cordillera Andina; cerca de Santiago de Chile.

Kinematics, Exhumation, and Sedimentation of the North Central Andes (Bolivia): An Integrated Thermochronometer and Thermokinematic Modeling Approach

Science.gov (United States)

Rak, Adam J.; McQuarrie, Nadine; Ehlers, Todd A.

2017-11-01

Quantifying mountain building processes in convergent orogens requires determination of the timing and rate of deformation in the overriding plate. In the central Andes, large discrepancies in both timing and rate of deformation prevent evaluating the shortening history in light of internal or external forcing factors. Geologic map patterns, age and location of reset thermochronometer systems, and synorogenic sediment distribution are all a function of the geometry, kinematics, and rate of deformation in a fold-thrust-belt-foreland basin (FTB-FB) system. To determine the timing and rate of deformation in the northern Bolivian Andes, we link thermokinematic modeling to a sequentially forward modeled, balanced cross section isostatically accounting for thrust loads and erosion. Displacement vectors, in 10 km increments, are assigned variable ages to create velocity fields in a thermokinematic model for predicting thermochronometer ages. We match both the pattern of predicted cooling ages with the across strike pattern of measured zircon fission track, apatite fission track, and apatite (U-Th)/He cooling ages as well as the modeled age of FB formations to published sedimentary sections. Results indicate that northern Bolivian FTB deformation started at 50 Ma and may have begun as early as 55 Ma. Acceptable rates of shortening permit either a constant rate of shortening ( 4-5 mm/yr) or varying shortening rates with faster rates (7-10 mm/yr) at 45-50 Ma and 12-8 Ma, significantly slower rates (2-4 mm/yr) from 35 to 15 Ma and indicate the northern Bolivian Subandes started deforming between 19 and 14 Ma.

A new species of iguanid lizard, genus Stenocercus (Squamata, Iguania), from the Central Andes in Peru.

Science.gov (United States)

Venegas, Pablo J; Echevarría, Lourdes Y; García-Burneo, Karla; Koch, Claudia

2016-12-04

We describe a new species of Stenocercus from the montane forest of the right margin of the Marañón river in the northern portion of the Central Andes in northern Peru (Amazonas and La Libertad departments), at elevations ranging from 2300 to 3035 m. Stenocercus omari sp. nov. differs from other Stenocercus species, with the exception of S. amydrorhytus, S. chrysopygus, S. cupreus, S. johaberfellneri, S. latebrosus, S. melanopygus, S. modestus, S. ornatissimus, S. orientalis, and S. stigmosus, by having granular scales on the posterior surfaces of thighs, a conspicuous antehumeral fold and by lacking a vertebral crest. However, Stenocercus omari sp. nov. is easily distinguished from the aforementioned species, except S. orientalis, by the presence of prominently keeled dorsal head scales. The new species differs from S. orientalis by lacking a prominent oblique neck fold and by having a distinct deep postfemoral mite pocket.

Malformaciones del sistema nervioso central en una familia

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Elisa Dyce Gordon

1998-06-01

Full Text Available Se reporta la aparición de 3 malformaciones del sistema nervioso central (2 defectos del tubo neural y una hidrocefalia en la progenie de un matrimonio entre primos y se establece una posible relación entre la aparición de estos defectos y las herencias multifactorial y autosómica recesiva. Se recomienda evitar el matrimonio entre parientes, así como ofrecer asesoramiento genético y diagnóstico prenatal a todas las personas que han procreado un hijo con malformaciones del sistema nervioso centralIt is reported the appearance of 3 malformations of the central nervous system (2 defects of the neural tube and 1 hydrocephaly in the offspring of a marriage between cousins. A possible relationship between appearance of these defects and the multifactorial and recessive autosomal inheritances is established. It is recommended to avoid marriage between relatives, as well as to offer genetic counseling and prenatal diagnosis to all those persons who had procreated a child with malformations of the CNS

A 60,000-year record of hydrologic variability in the Central Andes from the hydrogen isotopic composition of leaf waxes in Lake Titicaca sediments

Science.gov (United States)

Fornace, Kyrstin L.; Hughen, Konrad A.; Shanahan, Timothy M.; Fritz, Sherilyn C.; Baker, Paul A.; Sylva, Sean P.

2014-12-01

A record of the hydrogen isotopic composition of terrestrial leaf waxes (δDwax) in sediment cores from Lake Titicaca provides new insight into the precipitation history of the Central Andes and controls of South American Summer Monsoon (SASM) variability since the last glacial period. Comparison of the δDwax record with a 19-kyr δD record from the nearby Illimani ice core supports the interpretation that precipitation δD is the primary control on δDwax with a lesser but significant role for local evapotranspiration and other secondary influences on δDwax. The Titicaca δDwax record confirms overall wetter conditions in the Central Andes during the last glacial period relative to a drier Holocene. During the last deglaciation, abrupt δDwax shifts correspond to millennial-scale events observed in the high-latitude North Atlantic, with dry conditions corresponding to the Bølling-Allerød and early Holocene periods and wetter conditions during late glacial and Younger Dryas intervals. We observe a trend of increasing monsoonal precipitation from the early to the late Holocene, consistent with summer insolation forcing of the SASM, but similar hydrologic variability on precessional timescales is not apparent during the last glacial period. Overall, this study demonstrates the relative importance of high-latitude versus tropical forcing as a dominant control on glacial SASM precipitation variability.

Evaluation of TRMM Multi-satellite Precipitation Analysis (TMPA performance in the Central Andes region and its dependency on spatial and temporal resolution

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M. L. M. Scheel

2011-08-01

Full Text Available Climate time series are of major importance for base line studies for climate change impact and adaptation projects. However, for instance, in mountain regions and in developing countries there exist significant gaps in ground based climate records in space and time. Specifically, in the Peruvian Andes spatially and temporally coherent precipitation information is a prerequisite for ongoing climate change adaptation projects in the fields of water resources, disasters and food security. The present work aims at evaluating the ability of Tropical Rainfall Measurement Mission (TRMM Multi-satellite Precipitation Analysis (TMPA to estimate precipitation rates at daily 0.25° × 0.25° scale in the Central Andes and the dependency of the estimate performance on changing spatial and temporal resolution. Comparison of the TMPA product with gauge measurements in the regions of Cuzco, Peru and La Paz, Bolivia were carried out and analysed statistically. Large biases are identified in both investigation areas in the estimation of daily precipitation amounts. The occurrence of strong precipitation events was well assessed, but their intensities were underestimated. TMPA estimates for La Paz show high false alarm ratio.

The dependency of the TMPA estimate quality with changing resolution was analysed by comparisons of 1-, 7-, 15- and 30-day sums for Cuzco, Peru. The correlation of TMPA estimates with ground data increases strongly and almost linearly with temporal aggregation. The spatial aggregation to 0.5°, 0.75° and 1° grid box averaged precipitation and its comparison to gauge data of the same areas revealed no significant change in correlation coefficients and estimate performance.

In order to profit from the TMPA combination product on a daily basis, a procedure to blend it with daily precipitation gauge measurements is proposed.

Different sources of errors and uncertainties introduced by the sensors, sensor

Andes: An Intelligent Homework System for Introductory Physics

Science.gov (United States)

van de Sande, Brett; VanLehn, K.; Hausmann, R.; Treacy, D.; Shelby, R.

2006-12-01

We know that students benefit from solving homework problems under the guidance of an expert (human) tutor. The Andes system (http://www.andes.pitt.edu) is designed for students to solve homework problems under the guidance of an expert computer tutor. Andes encourages students to use sound problem solving techniques and provides immediate right/wrong feedback on each step of a solution. On request, Andes also provides hints based on previous student actions. I will discuss how Andes works, from a student's perspective, and summarize research that demonstrates its effectiveness as a pedagogical tool. I will also discuss how Andes can function as a tool for conducting educational research, presenting an investigation of students' hint usage as an example.

Arquitectura precerámica en la cordillera de los Andes, Piruru frene a la diversidad de los datos

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Elisabeth Bonnier

1988-12-01

Full Text Available Los datos sobre la arquitectura precerámica en la cordilleraandina provienen de cinco sitios: La Galgada, Piruru, Huaricoto, Shillacotoy Kotosh. Contexto arqueológico y rasgos arquitectónicos específicos permitenidentificar la función ceremonial de esta arquitectura. La descripciónde las construcciones religiosas pone en evidencia un conjunto pertinente decaracteres comunes. El espacio ceremonial, construido y sin construir, se articulaalrededor del doble elemento arquitectónico fundamental, el fogón yel piso. Para analizar el piso a dos niveles, dos neologismos, pericausto y epicaustohan sido creados. El análisis arquitectónico muestra que el piso es elespacio sagrado por excelencia. Los fechados 14C de los sitios estudiadosdestacan la larga duración del Precerámico Final con arquitectura. A la luz delos últimos trabajos en Piruru y de los cambios arquitectónicos perceptiblesen este sitio, la hipótesis, formulada a principios de este decenio, sobre ·taexistencia de una tradición religiosa única propia de los Andes Centrales, seestá reconsiderando.

A review of the albidohirta group of Ptilothrix (Hymenoptera: Apidae: Emphorini Revisión del grupo albidohirta de Ptilothrix (Hymenoptera: Apidae: Emphorini

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Arturo Roig Alsina

2007-12-01

Full Text Available The albidohirta group of Ptilothrix Smith includes three species: Ptilothrix albidohirta Brèthes, P. concolor sp. nov., and P. nemoralis sp. nov. The group is known from northern and western Argentina and from central Bolivia. One of its species, P. albidohirta, reaches high altitudes in the Andes mountains, up to 3600 m a.s.l., while the other two species occur in the lowlands. A characterization of the group, descriptions of the species, and illustrations are provided.El grupo albidohirta de Ptilothrix Smith incluye tres especies: Ptilothrix albidohirta Brèthes, P. concolor sp. nov. y P. nemoralis sp. nov. Este grupo se conoce del oeste y norte de la Argentina y del centro de Bolivia. Una de sus especies, P. albidohirta, llega hasta los 3.600 m s.n.m. en la cordillera de los Andes, en tanto que las otras dos especies habitan en el llano. Se caracteriza el grupo y se describen e ilustran las especies.

El tarwi o chocho: una de las principales fuentes de proteína vegetal de las comunidades indígenas de los Andes Centrales

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Planchuelo, Ana M.

2005-01-01

Full Text Available El lupino andino (Lupinus mutabilis Sweet conocido también como tarwi o chocho, es una especie de leguminosa nativa de los Andes Centrales. Su domesticación se remonta a los principios de la cultura Nazca y desde ese entonces hasta la actualidad el cultivo está ampliamente difundido en las laderas montañosas y en los altos valles de Ecuador, Perú y Bolivia. La importancia del lupino para las comunidades andinas prehispánicas quedo documentada en pinturas de cerámicas y en tributos encontrados en tumbas de 100-150 años AC. Diversas técnicas de lavado y de mejoramiento vegetal fueron aplicadas desde la antigüedad para eliminar los alcaloides tóxicos que le confieren el sabor amargo a la planta y los granos. El tarwi, el maíz. los frijoles, los pseudocereales, quinoa y amaranto y la papa junto a otras raíces y tubérculos constituyen la comida básica de muchas culturas andinas. El objetivo de este trabajo fue determinar los componentes nutricionales de los granos del lupino andino para compararlos con los otros constituyentes de la dieta de las comunidades campesinas. Se analizaron por medio de técnicas fitoquímicas distintas variedades de tarwi. Se determinaron los contenidos de proteínas y grasas y los patrones de ácidos grasos. Los resultados muestran que la ingesta de lupinos, que provee un buen balance de proteínas y grasas en combinación con el maíz y los tubérculos, que aportan los hidratos de carbono, forman una dieta balanceada y de alto valor nutricional.

El impacto del cambio climático en los glaciares del complejo volcánico Nevado Coropuna, (Cordillera Occidental de los Andes Centrales)

OpenAIRE

Ubeda Palenque, José

2010-01-01

El objetivo de la investigación ha sido evaluar el impacto del cambio climático en los glaciares del Nevado Coropuna, que en la actualidad recubren el área de cumbres de ese complejo de edificios volcánicos alcanzando una superficie de casi medio centenar de km2. El interés del trabajo de investigación se debe a tres razones principales: 1) De esas masas de hielo depende el abastecimiento de varias decenas de miles de personas; 2) El escenario de riesgo que se deduce de la localización vulner...

MARIPOSAS PIERIDAE (LEPIDOPTERA: PAPILIONOIDEA) DE LA CUENCA DEL RÍO COELLO (TOLIMA), COLOMBIA

OpenAIRE

Ospina-López, Leonardo A.; García-Pérez, Jack F.; Villa-Navarro, Francisco A.; Reinoso-Flórez, Gladys

2010-01-01

Este estudio analiza la composición, riqueza, diversidad y estructura de la familia Pieridae en la cuenca del río Coello, cordillera Central de los Andes, departamento de Tolima (Colombia). Se establecieron 11 estaciones de muestreo localizadas entre los 433 y 3.600 m de altitud, que fueron muestreadas entre marzo y octubre de 2003, teniendo en cuenta tres tipos de hábitat (pradera, borde y bosque), mediante transectos de longitud no definida, entre las 08:00 y las 16:00 h, empleando para ell...

Seismicity, fault plane solutions, depth of faulting, and active tectonics of the Andes of Peru, Ecuador, and southern Colombia

Science.gov (United States)

Suarez, G.; Molnar, P.; Burchfiel, B. C.

1983-01-01

The long-period P waveforms observed for 17 earthquakes in the Peruvian Andes during 1963-1976 are compared with synthetic waveforms to obtain fault-plane solutions and focal depths. The morphological units of the Peruvian Andes are characterized: coastal plains, Cordillera Occidental, altiplano and central high plateau, Cordillera Oriental, and sub-Andes. The data base and analysis methodology are discussed, and the results are presented in tables, diagrams, graphs, maps, and photographs illustrating typical formations. Most of the earthquakes are shown to occur in the transition zone from the sub-Andes to the Cordillera Oriental under formations of about 1 km elevation at focal depths of 10-38 km. It is suggested that the sub-Andean earthquakes reflect hinterland deformation of a detached fold and thrust belt, perhaps like that which occurred in parts of the Canadian Rockies. From the total crustal shortening evident in Andean morphology and the shortening rate of the recent earthquakes it is estimated that the topography and crustal root of the Andes have been formed during the last 90-135 Myr.

Comunidad y desarrollo en los Andes Peruanos: una crítica etnográfica al programa de modernidad/colonialidad

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Pieter de Vries

2013-08-01

Full Text Available En las últimas décadas la desconstrucción del desarrollo, conocida como el 'postdesarrollismo', ha cobrado gran auge en las ciencias sociales. En Latino-américa el programa teórico denominado modernidad/colonialidad/descolonialidad (MCD se propone descolonizar el pensamiento moderno re-escribiendo la historia global a partir de la experiencia colonial. Arturo Escobar, uno de los mayores teóricos del paradigma postdevelopmentalista se apoya en el proyecto MCD para pensar 'alternativas a la modernidad'(o transmodernidad. En este artículo propongo someter la perspectiva postdesarrollista y el proyecto MCD a un test etnográfico. Para eso me centro en las visiones y experiencias de Usibamba, una comunidad en los Andes Centrales Peruanos. La etnografía gira alrededor de la siguiente pregunta: ¿porqué los usibambinos, a pesar de todas sus experiencias negativas con el aparato del desarrollo, insisten en reivindicar la promesa del desarrollo? El programa de MCD nos permite entender el impasse de la comunidad en Usibamba? ¿Conceptos como pluriverso y transmodernidad nos permiten entender los deseos y aspiraciones de los usibambinos? Para responder a estas preguntas me apoyo en un análisis Žižekian que distingue entre 'lo actual', 'lo virtual', y lo 'Real'de la comunidad.

Angiosperm flora and biogeography of the páramo region of Colombia, northern Andes

NARCIS (Netherlands)

Londoño, C.; Cleef, A.; Madriñan, S.

2014-01-01

Páramo is the neotropical high elevation ecosystem in the northern Andes and Central America consisting of multiple dissected open areas above 3000 m a.s.l. Complex evolutionary processes that occurred within these ecosystems gave rise to a unique tropical Andean flora. Previous phytogeographical

Recursos hídricos en los Andes: Lago Titicaca

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1995-01-01

Full Text Available RESSOURCES EN EAUX DANS LES ANDES : LAC TITICACA. Une analyse par régression a été menée entre les variations de niveau du Lac Titicaca et les entrées du système (apports des affluents et précipitations. Les coefficients de corrélation, quoique relativement faibles, montrent aux abords du lac un effet de persistance qui diminue lorsque les stations sont éloignées du plan d’eau. L’inertie du lac se manifeste l’année suivante pour les affluents du lac et évidemment pour le lac lui-même. Ces résultats confirment la présence d’un mécanisme de rétro alimentation (effet boomerang. Cela montre que le système du Lac Titicaca est fragile, face à une utilisation excessive de ses eaux. Las regresiones estudiadas de cambios de nivel en el lago Titicaca contra precipitaciones y aportes en su cuenca, aunque relativamente bajas, muestran un efecto de persistencia en las proximidades del lago que decrece conforme las estaciones se alejan de éste. Lo que evidencia que la inercia del lago se manifiesta en el período siguiente (lag uno en los afluentes del lago y obviamente en el propio lago, fenómeno que parece confirmar la presencia de un mecanismo de retroalimentación (efecto boomerang. Este comportamiento muestra la fragilidad del lago frente a un aprovechamiento consuntivo excesivo. WATER RESOURCES IN THE ANDES: LAKE TITICACA. The studied regressions of the level changes in the Lake Titicaca versus the rainfall and the runoff in the basin, even being relatively low, show an effect of persistence in the proximity of the lake which decreases as we go away from it. This makes evident that the lake inertia manifests itself the following period (lag one in the lake tributaries and obviously in the lake itself, phenomenon which seems to confirm the presence of a feedback mechanism (boomerang effect. This behaviour shows the fragility of the lake against the excessive consumptive uses of the waters in its basin.

Glaciers et évolution climatique dans les Andes boliviennes. Glacier de Zongo et glacier de Chacaltaya Cordillère Royale, 16°S

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1995-01-01

Full Text Available SEDIMENTOLOGY OF THE HUANCANE FORMATION (NEOCOMIAN OF THE CUSCO REGION AND ITS RELATION TO SEA LEVEL VARIATIONS. The Huancane formation (Neocomian of the Cusco region is mainly composed of quartz sandstones which are deposited in fluvial environments. The facies recognized are organized in a vertical sequence: fluvial sheet sandstones, oxidized or eroded surface, the shale facies of alluvial plain and unusual limestone facies of possible marine origin. These vertical facies sequences show that eustatic sea level variations controlled the fluvial sedimentation. The rivers came from the NE and were fed by the erosion of the Brazilian Shield. The sedimentation developed above the boundary of the SW edge of the Eastern basin, and the Cusco-Puno Swell which had locale horst and grabens inherited from pre-neocomian relief. GLACIARES Y EVOLUCIÓN CLIMÁTICA EN LOS ANDES BOLIVIANOS GLACIAR DE ZONGO Y GLACIAR DE CHACALTAYA, CORDILLERA REAL, 16°S. Por su sensibilidad y su plazo de respuesta breve, el glaciar es de un gran interés para analizar la evolución y la variabilidad actuales del clima entre los trópicos. Se presentan los métodos de determinación del balance de masas y del balance hidrológico, con una frecuencia de mediciones mensual. Los resultados recogidos durante tres años (1991-1994 muestran una grande variabilidad. Ésta es controlada sobre todo por la extensión del periodo de precipitaciones en medio de la temporada cálida que dura más o menos 6 meses. Los eventos ENSO (El Niño Southern Oscillation son asociados a balances netamente negativos, lo que es demostrado por la respuesta del glaciar al episodio de 1991-1992 y por la reconstrucción de los balances efectuados en base a los datos hidrológicos durante los dos últimos decenios. El retroceso acelerado de los glaciares tropicales desde los años 1980 es vinculado a la vez a una sucesión de eventos ENSO y al recalentamiento atmosférico. GLACIERS AND CLIMATIC EVOLUTION IN

Identificación, caracterización y dinámica de las geoformas glaciales y periglaciales en la Cordillera de los Andes a través de sensores remotos

OpenAIRE

Falaschi, Daniel

2015-01-01

El presente trabajo de Tesis Doctoral tuvo el objetivo de estudiar los glaciares y glaciares de escombros en tres regiones montañosas a lo largo de la Cordillera de los Andes Argentina: Monte San Lorenzo (Provincia de Santa Cruz), Volcán Domuyo (Provincia de Neuquén), y Nevados de Cachi (Provincia de Salta). Cada uno de estos sitios presenta características climáticas propias, representativas de tres porciones particulares de los Andes: Andes Patagónicos Meridionales, Andes Centrales Meridion...

Investigating Crustal Scale Fault Systems Controlling Volcanic and Hydrothermal Fluid Processes in the South-Central Andes, First Results from a Magnetotelluric Survey

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Pearce, R.; Mitchell, T. M.; Moorkamp, M.; Araya, J.; Cembrano, J. M.; Yanez, G. A.; Hammond, J. O. S.

2017-12-01

At convergent plate boundaries, volcanic orogeny is largely controlled by major thrust fault systems that act as magmatic and hydrothermal fluid conduits through the crust. In the south-central Andes, the volcanically and seismically active Tinguiririca and Planchon-Peteroa volcanoes are considered to be tectonically related to the major El Fierro thrust fault system. These large scale reverse faults are characterized by 500 - 1000m wide hydrothermally altered fault cores, which possess a distinct conductive signature relative to surrounding lithology. In order to establish the subsurface architecture of these fault systems, such conductivity contrasts can be detected using the magnetotelluric method. In this study, LEMI fluxgate-magnetometer long-period and Metronix broadband MT data were collected at 21 sites in a 40km2 survey grid that surrounds this fault system and associated volcanic complexes. Multi-remote referencing techniques is used together with robust processing to obtain reliable impedance estimates between 100 Hz and 1,000s. Our preliminary inversion results provide evidence of structures within the 10 - 20 km depth range that are attributed to this fault system. Further inversions will be conducted to determine the approximate depth extent of these features, and ultimately provide constraints for future geophysical studies aimed to deduce the role of these faults in volcanic orogeny and hydrothermal fluid migration processes in this region of the Andes.

Field guides for excursions to the Nevado del Ruiz Volcano and to the Romeral Fault System (Colombia, in the frame of the Neotectonics of arc-continent collision concepts

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Borrero Carlos

2011-06-01

Full Text Available Central Cordillera of Colombia near to the Nevado del Ruiz volcano, is a seismically active area above the subducting slab of the Nazca plate and deforming upper crust of the Andes. Buildings in the region require strengthening against the effects of both types of hazards: earthquakes and volcanoes. During these trips, we will discuss the 13
November, 1985, Nevado del Ruiz Volcano eruption that destroyed the Armero city with about 22,000 deceases, as well the 25 January, 1999, Armenia earthquake (M 6.2 that killed about 2000 people and injured 4000 largely as the result of older, poorly 3 constructed buildings. The economic impact of the quake on the region was significant with about 8000 coffee farms either completely or partially destroyed and over 13,000 structures either partially damaged or completely destroyed.
Both phenomena are associated to a large-transversal structure termed Caldas tear, which is controlling strong motion earthquakes and the Quaternary volcanism of the northern Andes.

Classification of debris-covered glaciers and rock glaciers in the Andes of central Chile

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Janke, Jason R.; Bellisario, Antonio C.; Ferrando, Francisco A.

2015-07-01

In the Dry Andes of Chile (17 to 35° S), debris-covered glaciers and rock glaciers are differentiated from true glaciers based on the percentage of surface debris cover, thickness of surface debris, and ice content. Internal ice is preserved by an insulating cover of thick debris, which acts as a storage reservoir to release water during the summer and early fall. These landforms are more numerous than glaciers in the central Andes; however, the existing legislation only recognizes uncovered or semicovered glaciers as a water resource. Glaciers, debris-covered glaciers, and rock glaciers are being altered or removed by mining operations to extract valuable minerals from the mountains. In addition, agricultural expansion and population growth in this region have placed additional demands on water resources. In a warmer climate, as glaciers recede and seasonal water availability becomes condensed over the course of a snowmelt season, rock glaciers and debris-covered glaciers contribute a larger component of base flow to rivers and streams. As a result, identifying and locating these features to implement sustainable regional planning for water resources is important. The objective of this study is to develop a classification system to identify debris-covered glaciers and rock glaciers based on the interpretation of satellite imagery and aerial photographs. The classification system is linked to field observations and measurements of ice content. Debris-covered glaciers have three subclasses: surface coverage of semi (class 1) and fully covered (class 2) glaciers differentiates the first two forms, whereas debris thickness is critical for class 3 when glaciers become buried with more than 3 m of surface debris. Based on field observations, the amount of ice decreases from more than 85%, to 65-85%, to 45-65% for semi, fully, and buried debris-covered glaciers, respectively. Rock glaciers are characterized by three stages. Class 4 rock glaciers have pronounced

Una nueva especie de Bolitoglossa (Caudata: Plethodontidae de las selvas del Magdalena Medio en Colombia

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Acosta Galvis Andrés R.

2001-12-01

Full Text Available Se describe una nueva especie del genero Bolitoglossa del grupo alfa (sensu Wake & Lynch, 1976 denominada Bolitoglossa lozanoi de las selvas húmedas relictuales del valle del Río Magdalena en La Cordillera Central de Colombia (loe. typ.: Río La Miel, Mpio. La Victoria, Departamento de Caldas, 500 m.s.n.m.; la nueva especie es reconocible por su cuerpo robusto, las palmeaduras manuales y pediales extensas, su patrón cromático ventral café con punteaduras café más oscuras y crema, ojos no protuberantes y la talla corporal relativamente grande entre las especies de salamandras del país. A new species of the genus Bolitoglossa, of the alpha group (sensu Wake & Lynch, 1976 named Bolitoglossa lozanoi from the relictual humid forest from the Magdalena Valley on the eastern slope ofthe central Andes Mountain range in Colombia (type locality: La Miel River, Mpio. La Victoria, Dept. of Caldas, 500 m.s.n.m.. The new species is mainly recognized by the presence of a robust body, extensively webbed hands and toes, a brownish ventral chromatic pattern with small darker brown and cream dots, non-protuberant eyes and a relatively large size.

An InSAR survey of the central Andes: Constraints on magma chamber geometry and mass balance in a volcanic arc

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Pritchard, M. E.; Simons, M.

2002-12-01

The central Andes (14-28o S) has a high density of volcanoes, but a sparse human population, such that the activity of most volcanoes is poorly constrained. We use InSAR to conduct the first systematic observations of deformation at nearly 900 volcanoes (about 50 of which are classified ``potentially active'') during the 1992-2002 time interval. We find volcanic deformation in four locations. Subsidence is seen at Robledo (or Cerro Blanco) caldera, Argentina. We observe inflation at the stratovolcano Uturuncu, Bolivia, near stratovolcano Hualca Hualca, Peru, and in a region not associated with any known edifice on the border between Chile and Argentina that we call ``Lazufre'' because it lies between volcanoes Lastarria and Cordon del Azufre. The deformation pattern can be well explained by a uniform point-source source of inflation or deflation, but we compare these model results with those from a tri-axial point-source ellipsoid to test the robustness of estimated source depth and source strength (inferred here to be volume change). We further explore the sensitivity of these parameters to elastic half-space and layered-space models of crustal structure, and the influence of local topography. Because only one satellite look direction is available for most time periods, a variety of models are consistent with our observations. If we assume that inflation is due solely to magmatic intrusion, we can compare the rate of magma intrusion to volcanic extrusion during the decade for which data is available and the longer-term geologic rate. For the last decade, the ratio of volume intruded to extruded is between about 1-10, which agrees with previous geologic estimates in this and other volcanic arcs. The combined rate of intrusion and extrusion is within an order of magnitude of the inferred geologic rate.

Problemas centrales del análisis de datos cualitativos

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Julio Mejía Navarrete

2011-04-01

Full Text Available El trabajo examina las operaciones prácticas y las decisiones concretas que enfrenta el trabajo de investigación cualitativa en la etapa del análisis de datos. Interesa subrayar los aspectos centrales del análisis de datos cualitativos que posibiliten abrir una discusión en la investigación metodológica de América Latina

High-Resolution ∂18O record of middle-late Holocene hydrologic variability from the central Peruvian Andes (Invited)

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Rodbell, D. T.; Abbott, M.; Bird, B. W.; Stansell, N.

2009-12-01

Laguna Yuraicocha in the western cordillera of the central Peruvian Andes (12.53°S; 75.50°W; 4460 masl) is dammed by late glacial moraines and is underlain and surrounded by Jurassic and Cretaceous limestone interbedded with siliciclastic rocks. A 6.9 meter-long sediment core from the distal end of the lake is dominated by authigenic calcite (marl) with a mean concentration of 82 weight percent that has accumulated at a rate of ~ 1 mm yr-1 for the past 6200 years. The age model for the core is based on a combination of 210Pb and AMS 14C ages from charcoal; modern lake water is ~1‰ evaporatively enriched from mean regional precipitation. Marl samples were taken with an average sampling interval of 8 years; samples were treated to remove organic matter, sieved to concentrate the clay fraction was removed by repeated pipette withdrawal. The Peru and Bolivia, are especially sensitive to changes in regional moisture balance.

The paradigm of paraglacial megafans of the San Juan river basin, Central Andes, Argentina

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Suvires, Graciela M.

2014-11-01

The spatial distribution and several morphometric characteristics of the Quaternary alluvial fans of the San Juan River, in the province of San Juan, at the Central and Western part of Argentina, have been studied to classify them as paraglacial megafans, as well to ratify its depositional environmental conditions. The high sedimentary load exported by San Juan river from the Central Andes to the foreland depressions is estimated about 3,682,200 hm3. The large alluvial fans of Ullum-Zonda and Tulum valleys were deposited into deep tectonic depressions, during the Upper Pleistocene deglaciation stages. The outcome of collecting remotely sensed data, map and DEM data, geophysical data and much fieldwork gave access to morphometric, morphographic and morphogenetic data of these alluvial fans. The main drainage network was mapped on processed images using QGis (vers.2.0.1). Several fan morphometric parameters were measured, such as the size, the shape, the thickness, the surface areas and the sedimentary volume of exported load. The analyzed fans were accumulated in deep tectonic depressions, where the alluvium fill reaches 700 to 1200 m thick. Such fans do not reach the large size that other world megafans have, and this is due to tectonic obstacles, although the sedimentary fill average volume surpasses 514,000 hm3. The author proposes to consider Ullum-Zonda and Tulum alluvial fans as paraglacial megafans. According to the stratigraphic relationships of the tropical South American Rivers, the author considers that the San Juan paraglacial megafans would have occurred in the period before 24 ka BP , possibly corresponding to Middle Pleniglacial (ca 65-24ka BP). They record colder and more humid conditions compared with the present arid and dry conditions.

Changing Student Attitudes using Andes, An Intelligent Homework System

Science.gov (United States)

van de Sande, Brett; Vanlehn, Kurt; Treacy, Don; Shelby, Bob; Wintersgill, Mary

2007-03-01

The size of introductory physics lectures often inhibits personal homework assistance and timely corrective feedback. Andes, an intelligent homework help system designed for two semesters of introductory physics, can fill this need by encouraging students to use sound problem solving techniques and providing immediate feedback on each step of a solution. On request, Andes provides principles-based hints based on previous student actions. A multi-year study at the U.S. Naval Academy demonstrates that students using Andes perform better than students working the same problems as graded pencil and paper homeworks. In addition, student attitude surveys show that Andes is preferred over other homework systems. These findings have implications for student attitudes toward, and mastery of, physics. See http://www.andes.pitt.edu for more information.

LA FRECUENCIA DEL TUTEO EN TRES ZONAS DEL DEPARTAMENTO DE ANTIOQUIA (COLOMBIA: INFLUENCIA DE LA ZONA URBANA/RURAL

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Ji Son Jang

2015-01-01

Full Text Available En este artículo se presentan algunos resultados acerca del uso de tú en el marco de una investigación sobre la selección pronominal llevada a cabo en tres municipios del departamento colombiano de Antioquia: 1 la ciudad de Medellín, capital del departamento; 2 Carmen de Viboral, ubicada a una hora de la capital en automóvil y 3 Andes, que se sitúa a unas tres horas de la capital en coche. Los informantes comprenden edades entre 13 y 34 años. La variable social para este artículo es el lugar de residencia de los informantes: zona urbana (Medellín, medio rural (Carmen de Viboral o rural (Andes. Para llevar a cabo esta investigación se aplicó a 1490 informantes un cuestionario que mostraba distintos tipos de interacción que se dan en dichas zonas. Tres técnicas estadísticas se aplicaron a estos datos: tamaño de muestra óptimo para distribuciones multinomiales; análisis de varianza con un solo factor (ANOVA; y prueba de hipótesis para proporciones. Se encontró que, en la gran mayoría de relaciones interpersonales solidarias, el tuteo se usa más en Medellín que en Carmen de Viboral y en este último municipio más que en Andes.

A Million-Year Record of Glaciation in the Tropical Andes

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Smith, J. A.; Seltzer, G. O.; Rodbell, D. T.; Farber, D. L.; Finkel, R. C.

2004-12-01

We present a longterm record of glaciation in the tropical Andes based on cosmogenic dating (10Be) of boulders on moraines. Well-preserved moraines in deglaciated valleys bordering the Junin Plain in central Peru ( ˜11° S, 76° W, 4000 m) were deposited during several glacial cycles extending back more than one million years before present (1 Myr BP). The presence of boulders with zero-erosion 10Be exposure ages >1 Myr constrains boulder erosion rates to relatively low values. For boulders at high altitudes, however, even low boulder erosion rates (0.3 to 0.5 m/Myr) make calculated old exposure ages markedly older [e.g., ˜20% older for a zero-erosion age of 400,000 10Be years (400 10Be kyr)]. Exposure ages recalculated with boulder erosion rates of 0.3 m/Myr straddle interglacial marine isotope stage (MIS) 11 ( ˜430-390 kyr BP), fall within glacial MIS 12 ( ˜480-430 kyr BP), but skip over glacial MIS 16 ( ˜670-630 kyr BP), perhaps the largest ice volume of the past 2 Myr. Increasing the erosion rate used in the calculations to 0.5 m/Myr moves ages into both MIS 11 and MIS 16. If we assume that the older Andean glaciations were indeed synchronous with global ice volume, our data suggest that boulder preservation cannot be treated as a simple linear process. Conversely, the data may be suggesting correctly that glaciation of the tropical Andes was not synchronous with the global glaciations as inferred from the marine isotope record. Our chronology for the last glacial maximum (LGM) in the region supports the idea of asynchrony between the global ice volume record and the terrestrial record of glaciation in the tropical Andes. The LGM in the Junin region of Peru and in the Cordillera Real of Bolivia (16° S 68° W) occurred ˜34 to 22 10Be kyr BP and was less extensive than older glaciations. Asynchrony between the LGM in the Northern Hemisphere ( ˜21 kyr BP) and the tropical Andes suggests that previous glaciations in the tropical Andes may have been

Ecuador y los objetivos del milenio : inversiones para la conservación del agua

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Fabián Rodríguez

2013-09-01

Full Text Available El presente estudio analiza si se justifica la inversión en la protección del Sistema Nacional de Áreas Protegidas (SNAP. El nivel de inversión del Estado ecuatoriano fue estimado a partir de las necesidades de financiamiento del SNAP. Los beneficios económicos fueron estimados a partir de la oferta de agua de las áreas protegidas que se encuentran a lo largo de la Cordillera de los Andes. La metodología para evaluar si es conveniente o no la inversión del Estado en la protección del SNAP fue la relación beneficio - costo (B/C. Los resultados del estudio demuestran que solo los valores piso de la relación B/C justifican la inversión del Estado.

EFECTO DE LA EXTRACCIÓN DE RAÍCES AÉREAS SOBRE LAS POBLACIONES DE “TRIPEPERRO” (PHILODENDRON LONGIRRHIZUM, ARACEAE EN LOS ANDES CENTRALES DE COLOMBIA

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García Nestor

2009-06-01

Full Text Available El "tripeperro" (Philodendron longirrhizum es una planta hemiepífi ta de ampliadistribución en Los Andes de Colombia. En la región del Eje Cafetero colombiano seemplean las raíces aéreas de esta especie como fi bra para elaborar canastos y artesanías.Esta actividad tiene una larga tradición en la región y se concentra en el municipiode Filandia (departamento del Quindío. En los últimos años se ha presentado unadisminución en la oferta de raíces adecuadas para la actividad artesanal en todas lasáreas donde tradicionalmente se obtiene el "tripeperro". Se evaluó el efecto de laextracción sobre la estructura de tamaños, la densidad y el rendimiento de las raíces,comparando poblaciones en áreas con extracción del recurso con poblaciones enáreas sin extracción. Los resultados indican que, aunque la extracción parece noafectar la densidad poblacional, sí tiene efectos signifi cativos sobre la estructura detamaños y, en consecuencia, sobre el rendimiento de las raíces. La disponibilidad deeste recurso en las áreas con extracción es hasta cinco o seis veces menor que en delas áreas sin extracción.

Lacustrine sedimentation in an altitude forest site, central Andes, Bolivia. Palaeo-climatic implications

International Nuclear Information System (INIS)

Sifeddine, A.; Bertaux, J.; Mourguiart, Ph.; Disnar, J.R.; Laggoun-Defarge, F.; Argollo, J.

1998-01-01

A sedimentological study of a 755 cm length core sampled in the middle of a marshy depression surrounded by a cloud forest in the central Andes reveals that this site has recorded important environmental variations during the last 50 000 years. For the most part (625 cm) the core is composed of detrital rich sediments deposited during the Upper Pleistocene. The highest amount of detrital influx underlines the Last Glacial Maximum which ranges from ca 29,000 14 C yr B.P. to ca 16,000 14 C yr B.P. (ca 18,500 cal yr B.P.), between two relatively humid phases. The sedimentation of the present Interglacial, starting at ca 12,500 14 C yr B.P. (14,500 cal yr B.P.), is mainly organic, as a consequence of the great development of soils and the forest vegetal cover the catchment area. The maximum extension of this vegetal cover ranging from 12,500 to ca 10,500 14 C yr B.P. (14,500 and 12,400 cal yr B.P.) is followed from 10,500 to 8,000 14 C yr B.P. (12,400 and 8,800 cal yr B.P.) by a drier period is revealed by the occurrence of micro-charcoals in the sediment. Between ca 8,000 and 4,000 14 C yr B.P. (8,800 and 4,500 cal yr B.P.), the sharp increase of micro-charcoals content, likely related to palaeo-fires, underlines an intensification of this dry trend. (authors)

Características de uso de plaguicidas químicos y riesgos para la salud en agricultores de la sierra central del Perú

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Ymelda Montoro

2009-10-01

Full Text Available Con el objetivo de conocer las características sobre el uso e impactos en la salud de los plaguicidas químicos de uso agrícola en las provincias de Chupaca y Concepción en los andes centrales del Perú, se desarrolló un estudio descriptivo transversal entre abril y junio del año 2005, por medio de un cuestionario aplicado a 435 agricultores. Asimismo, se exploró la ubicación de los centros de expendio y la frecuencia de ventas de productos, además, se evaluó los casos de intoxicación reportados en ambas provincias. Los agricultores no cuentan con ropa de protección y manipulan directamente los plaguicidas durante su preparación y aplicación; asimismo, muchas veces no toman medidas preventivas a pesar de conocer los riesgos relacionados. El comercio de los plaguicidas se ubica en los centros urbanos, cerca de restaurantes y tiendas de abarrotes, además, los plaguicidas más vendidos pertenecen a las categorías extremadamente y altamente peligrosos, tales como Tamaron® y Furadan®, esto representa un peligro para la salud de los agricultores. Los casos de intoxicación por estos productos en las provincias bajo estudio, se han incrementado entre los años 2001 a 2004.

Central Chile

Science.gov (United States)

2002-01-01

The beginning of spring in central Chile looked like this to SeaWiFS. The snow-covered Andes mark the country's eastern border, and phytoplankton blooms and river sediment plumes fill the waters off its west coast. A large eddy due west of Concepcion is highlighted by the phytoplankton it contains.

Una ruina habitada desde el presente: vestigios del horror, la resistencia y el duelo. A propósito de La Ilíada de Teatro de los Andes (2000

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María Gabriela Aimaretti

2016-12-01

Full Text Available Este trabajo describe y analiza la obra La Ilíada (2000 de Teatro de los Andes que, retomando el texto homérico desde el contexto boliviano y latinoamericano, ofrece una interpretación crítica del pasado reciente de las dictaduras cívico-militares y el presente neoliberal. Esa lectura es posible gracias al diseño de una compleja arquitectura discursiva, visual, lingüística —con apelación al quechua y español– y musical —combinando tradiciones vernáculas y europeas–, que reelabora numerosos y variados intertextos. Nutrido de los aportes de la crítica cultural latinoamericana y los estudios de la memoria, y considerando el marco socio-histórico en el que se inserta y con el que discute la obra; este ensayo reflexiona sobre las formas de representación del dolor y la violencia, y las prácticas de la resistencia y de duelo, a propósito de un espectáculo que se postula a sí mismo como la memoria de un pasado-presente traumático del cual es necesario aprender.

Mario Alberto Cajas Sarria (2015. La historia de la Corte Suprema de Justicia de Colombia, 1886-1991. Bogotá: Universidad de los Andes & Universidad ICESI

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Michael Cruz Rodríguez

2017-06-01

Full Text Available El libro del profesor Mario Alberto Cajas Sarria, que es resultado de su tesis doctoral en derecho en la Universidad de los Andes, realiza una narración de la historia de la Corte Suprema de Justicia de Colombia desde su creación en 1886 hasta su validación a la Asamblea Nacional Constituyente de 1991. Para ello toma como elemento central decisiones judiciales que efectuaron control constitucional en cuatro temas que sirven de hilos conductores: los estados de excepción, las leyes por vicios de trámite, los tratados internacionales y las reformas a la constitución. Así, el trabajo no sólo se detiene en las categorías jurídicas que orbitan alrededor de estos tópicos sino que, a partir de las decisiones judiciales, de la prensa y de fuentes secundarias, ilumina el contexto político y los ambientes institucionales en los que la Corte Suprema ejerció el control de constitucionalidad en algunas coyunturas en la trayectoria del régimen político colombiano.

Uplift sequence of the Andes at 30°S: Insights from sedimentology and U/Pb dating of synorogenic deposits

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Suriano, J.; Mardonez, D.; Mahoney, J. B.; Mescua, J. F.; Giambiagi, L. B.; Kimbrough, D.; Lossada, A.

2017-04-01

The South Central Andes at 30°S represent a key area to understand the Andes geodynamics as it is in the middle of the flat slab segment and all the morphotectonic units of the Central Andes are well developed. This work is focused in the proximal synorogenic deposits of the Western Precordillera, in the La Tranca valley, in order to unravel the uplift sequence of this belt. Nine facies associations were recognized; most of them represent piedmont facies with local provenance from Precordillera and were deposited in the wedge-top depozone, as is expected for proximal sinorogenic deposits. However there are intercalations of transference fluvial systems, which show mixed provenance indicating that Permo-Triassic igneous rocks were already exposed to the west (Frontal Cordillera). There are also lacustrine deposits which are interpreted as the result of damming by fault activity at east of the studied basin. Finally, two maximum depositional ages at ca. 11 Ma and 8 Ma of these deposits indicate that the onset of uplift of the Precordillera at 30°S is little older than 11 Ma. These data change two previous ideas about the evolution of the Precordillera: its uplift at 30° S is younger than proposed by previous works and it is nearly synchronous along strike.

Circulation, échange et production de poteries dans les Andes Centrales au deuxième millénaire AV. J.C

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1990-01-01

Full Text Available Sont présentés tout d’abord les quatre types céramiques définis pour la séquence Pirwa de Piruru (1600/1500 - 800/600 av. J.C.. Puis, après quelques réflexions méthodologiques à propos de la détermination de groupes céramiques pertinents, particulièrement durant le Formatif Initial, Piruru Pirwa est replacé dans le contexte culturel de la cordillère centre-andine, des changements significatifs étant constatés entre les phases Pirwa II et III. Les analyses céramologiques montrent que trois types sont importés et que le quatrième résulte d’une production locale. Les variations dans l’organisation globale de l’habitat Pirwa II et Pirwa III permettent de proposer l’hypothèse que l’activité céramique, c’est-à-dire la production de vaisselles, pourrait, dans l’exemple de Piruru, dépendre de la sédentarité. Circulación, intercambio y producción de cerámica en los Andes Centrales durante el segundo milenio a. C. En primer lugar, se presentan los cuatro tipos cerámicos definidos para la secuencia Pirwa de Piruru (1600/1500 - 800/600 a.C.. Luego, después de unas reflexiones metodológicas acerca de la determinación de grupos cerámicos pertinentes, especialmente durante el período Formativo Inicial, se sitúa Piruru Pirwa en el contexto cultural de la sierra central, notando cambios significativos entre las fases Pirwa II y Pirwa III. Los análisis ceramológicos muestran que tres tipos son importados, y que el cuarto es resultado de una producción local. Tomando en cuenta las variaciones en la organización general del asentamiento Pirwa II y Pirwa III, se plantea la hipótesis que la actividad cerámica, es decir la producción alfarera, en Piruru, podría vincularse al sedentarismo. Circulation, exchange and production of wares in the Central Highlands of Peru during the secund millenium B.C. In this paper, four ceramic types are defined and described for the Piruru Pirwa sequence (1600/1500 - 800/600 a C, and

Snakes of an urban-rural landscape in the central Andes of Colombia: species composition, distribution, and natural history

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Julián Andrés Rojas-Morales

2012-12-01

Full Text Available From 2005 to 2011, I studied the composition, distribution and natural history of an Andean urban-rural snake assemblage at the Cordillera Central of Colombia, based on three data sources: (1 examination of specimens in the MHN-UC [Museo de Historia Natural, Universidad de Caldas], (2 incidental encounters by author, and (3 collection of data by other researchers. Additionally, I provide natural history notes for the species involved. A total of 14 species, including two subspecies of snakes, belonging to 12 genera and four families, have been found in the studied area (municipality of Manizales, Caldas. Taking into account this total, 10 had atleast one record in the urban area, 13 in the rural area and 14 in forested areas. Only Liophis epinephelus bimaculatus was found exclusively in forest environment. Three species (21.4% are apparently endemic to the region, six species (42.8% correspond to afauna representative of the Tropical–Andean range of South America, four species (28.5% are distributed from Central America to the tropical Andes, and only one species is widely distributed in the whole continent. The snake assemblage in Manizales is mostly terrestrial, and in general, the species tend to be more active in the rainy periods of the year (mainly from October–December, and most of them may occasionally be found in urban areas, mainly close to areas of vegetation such as crops and pastures.

Disappearance of the glacier on Mama Cotacachi: ethnoecological research and climate change in the Ecuadorian Andes

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Rhoades, R.

2008-12-01

Full Text Available A first documented case study of a disappearing glacier in the snow capped volcano Cotacahi in Ecuador is presented with the studies belonging to the social sciences in relation to climate change and its impact on the population of the Equatorial Andes. With the use of multiple source methodology, including ethnographic analyzes, visual representations, repetitive photography, critical mapping by the local communities, longitudinal surveys, even archival research, as well as interviews to social actors and utilization of spatial data in a geographical information system (GIS. It is concluded that the documented disappearance of the glacier on the Cotacahi serves as an urgent call for action to the important dearth of social research related to global change from the ethnoecological perspective, with a cultural, local approach.

Se presenta el primer estudio documentado de la desaparición del glaciar del nevado Cotacachi en el Ecuador, con los estudios que corresponden a las ciencias sociales en relación con el cambio climático y su impacto en la población de los Andes ecuatoriales. Mediante el uso de una metodología que incluye análisis etnográficos, representaciones visuales, fotografía repetitiva, mapeo crítico por parte de las comunidades locales, encuestas longitudinales e incluso investigación de archivos, así como también entrevistas a actores sociales, y utilización de los datos espaciales en un sistema de información geográfica (SIG. Se concluye que la desaparición documentada del glaciar del Cotacachi sirve como una llamada de atención urgente a la importante falta de investigaciones sociales relacionadas con el cambio global desde el punto de vista etnoecológico, con un enfoque cultural local.

EL ROL DEL ANTICICLÓN PACÍFICO EN LA CAÍDA DE NIEVE EN LOS ANDES ÁRIDOS

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Arnobio G. Poblete

2016-12-01

Full Text Available This article aims to study in depth the role the anticyclone subtropical eastern South Pacific (ASPSO on the nival precipitation in the arid Andes, its seasonal variability, fluctuations in the long and medium scale and associations with snowfall. For this reason, the incidence on the ratio of precipitation, the SST in the South Pacific Ocean, precipitable water, wind zonal, Radiation in Outgoing Long Wave and Omega were analyzed. The methodology consisted in the evaluation of the ASPSO through the definition of an index, based on Santiago de Chile (PSGO measured surface atmospheric pressure. This would allow its surveillance and the processing of its temporal behavior in the statistical analysis. The results showed significant time - space associations within the involved variables, which confirmed in all cases the negative impact of ASPSO related to snowfall in the Andes mountains. period 1909-2015.

Aplicación de tres índices bióticos en el río San Juan, Andes, Colombia (Application of three biotic indexes in the river San Juan, Andes, Colombia

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Mailedt Paola Murillo Torrentes

2016-09-01

Full Text Available Durante los meses de febrero, mayo, agosto y octubre del año 2014, se evaluó la calidad del agua del río San Juan. Para tal fin se establecieron seis puntos de muestreo donde se recolectaron muestras de agua y macroinvertebrados acuáticos para los análisis fisicoquímicos e hidrobiológicos. Se aplicaron y modificaron los índices bióticos EPT (efemerópteros, plecópteros, tricópteros, BMWP/Col (Biological Monitoring Working Party y ASPT (Average Score per Taxon basados en las comunidades de macroinvertebrados acuáticos capturados. Los resultados de las variables fisicoquímicas y los índices bióticos indican que las estaciones E1 y E2 son las que presentan menor grado de contaminación, en las demás estaciones disminuye considerablemente la calidad del agua debido a las actividades económicas desarrolladas en el sector y a su cercanías con el casco urbano del municipio de Andes. De los tres índices analizados, el ASPT modificado y adaptado al río San Juan es el que mejor se relaciona con las condiciones ambientales del río en tanto las características de los macroinvertebrados acuáticos recolectados y analizados en el trayecto objeto de estudio. (Abstract. During the months of February, May, August and October 2014, the water quality of the San Juan River was assessed. To this aim, six sampling points were established, where water samples and macroinvertebrates for physical-chemical and hydrobiological analysis were collected. Three biotic indexes were applied and one modified: EPT (Ephemeroptera, Plecoptera, Trichoptera, BMWP / Col (Biological Monitoring Working Party and ASPT (Average Score per Taxon based on the captured communities of aquatic macroinvertebrates. The results of the physical-chemical variables and biotic indixes indicate that E1 and E2 stations are those with lower degree of contamination, other stations considerably decreased water quality due to economic activities around, and the short distance with the

Posibles efectos en la salud asociados con la metalurgia precolombina.

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Alvaro Javier Idrovo

2005-09-01

Full Text Available En el Viejo Mundo algunos investigadores piensan que los efectos adversos en la salud relacionados con la exposición a arsénico influyeron para que se cambiara de usar aleaciones de cobre con arsénico a otras menos tóxicas. En este artículo se evalúa esta hipótesis para las tres grandes tradiciones metalúrgicas precolombinas: Andes centrales, área intermedia y occidente mexicano. Los artefactos metálicos revelan que las concentraciones de arsénico en los Andes centrales fueron similares a las del Viejo Mundo (0,5% a 1%, en el área intermedia los valores eran muy inferiores, mientras en el occidente mexicano fueron muy superiores (7% a 25%. En los Andes centrales se observó inicialmente el uso de bronce arsenical, pero rápidamente se conocieron las aleaciones de cobre-estaño; estas últimas fueron cada vez más preferidas y difundidas por todo el imperio inca. Las evidencias, osteológicas y en objetos artísticos, de amputaciones de los pies entre individuos moches de los Andes centrales apoyan la idea de la presencia de la ?enfermedad del pie negro? entre las poblaciones precolombinas. En conclusión, es posible que los efectos nocivos del arsénico se hayan observado en el Nuevo Mundo, y favorecido el cambio hacia aleaciones menos tóxicas. Se requieren nuevos estudios específicos para verificar esta hipótesis.

Castrofroila: la representación del poder central en la ribera del Cea (siglos X-XII

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María PÉREZ RODRÍGUEZ

2016-03-01

Full Text Available Sin descartar la diversidad de funciones tradicionalmente atribuidas a castros y castillos, en los últimos años se ha incidido sobre todo en su papel como centros de representación del poder. El ejemplo que aquí presentamos viene caracterizado por la fuerte y continua vinculación que se establece entre Castro Froila–Mayorga, en la ribera del Cea, y la autoridad central. A través de las fuentes documentales y arqueológicas sabemos de la existencia de este enclave y de la importante función política que desde él se ejerció, intensificada tras la división del reino a la muerte de Alfonso VII y el recrudecimiento del conflicto entre León y Castilla.

CARACTERIZACIÓN FÍSIOGRÁFICA DE LA PUNA DE SAJAMA, CORDILLERA OCCIDENTAL DE LOS ANDES (BOLIVIA

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Fernando Javier Santa Cecilia Mateos

2015-01-01

Full Text Available Este artículo aproxima a la realidad física de la cordillera Occidental de los Andes. Un espacio geográfico donde los caracteres geológicos relacionados con el vulcanismo adquieren una relevancia especial en la configuración del paisaje andino. Los nevados y llanuras intermedias o altiplanos, son los dos elementos que constituyen la imagen de la puna andina, un territorio situado por encima de los 4.000 metros, ámbito intermedio entre los valles húmedos o yungas y las más altas cumbres de los Andes. A la singularidad volcánica habría que añadir la relacionada con el modelado glaciar, los aspectos hidrográficos y la biogeografia en esta área. El artículo toma como ejemplo de estudio la puna de Sajama en eldepartamento de Oruro, en la frontera boliviano-chilena.Abstract. This article approaches the physical reality of the Western Cordillera of the Andes. A geographical space where characters related geological volcanism are of particular importance in shaping the landscape Andean. The intermediate plains or mountains and plateaus, are the two elements that make up the image of the Andean puna, an area located above 4,000 meters, the middle ground between Yungas wet valley and the highest peaks of the Andes. A volcanic uniqueness should add that related to glacier modeling, hydrographic aspects and biogeography in this area. The article uses the example of the highlands of Sajama study in thedepartment of Oruro in Bolivian-Chilean border.

El represamiento y aluvión del río Santa Cruz, Andes Principales (31°40'S), provincia de San Juan

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Patricio E. D'odorico; Daniel J. Pérez; Nicolás Sequeira; Luis Fauqué

2009-01-01

En la región de los Andes Principales sanjuaninos, existe una alta concentración de deslizamientos, cuyos depósitos han originado represamientos naturales. El colapso de estos diques generados por movimientos de ladera es el proceso evolutivo más probable de estas geoformas. El análisis de imágenes satelitales y fotos aéreas permite reconstruir las características y el origen de los deslizamientos que formaron esos diques naturales. En esta región de los Andes Principales, el rápido levantami...

Calculated WIMP signals at the ANDES laboratory: comparison with northern and southern located dark matter detectors

Science.gov (United States)

Civitarese, O.; Fushimi, K. J.; Mosquera, M. E.

2016-12-01

Weakly interacting massive particles (WIMPs) are possible components of the Universe’s dark matter (DM). The detection of WIMPs is signaled by the recoil of the atomic nuclei which form a detector. CoGeNT at the Soudan Underground Laboratory (SUL) and DAMA at the Laboratori Nazionali del Gran Sasso (LNGS) have reported data on annual modulation of signals attributed to WIMPs. Both experiments are located in laboratories in the Northern Hemisphere. DM detectors are planned to operate (or already operate) in laboratories in the Southern Hemisphere, including SABRE at Stawell Underground Physics Laboratory (SUPL) in Australia, and DM-ICE in Antarctica. In this work we have analyzed the dependence of diurnal and annual modulation of signals, pertaining to the detection of WIMP, on the coordinates of the laboratory, for experiments which may be performed in the planned new Agua Negra Deep Experimental Site (ANDES) underground facility, to be built in San Juan, Argentina. We made predictions for NaI and Ge-type detectors placed in ANDES, to compare with DAMA, CoGeNT, SABRE and DM-ICE arrays, and found that the diurnal modulation of the signals, at the ANDES site, is amplified at its maximum value, both for NaI (Ge)-type detectors, while the annual modulation remains unaffected by the change in coordinates from north to south.

Calculated WIMP signals at the ANDES laboratory: comparison with northern and southern located dark matter detectors

International Nuclear Information System (INIS)

Civitarese, O; Mosquera, M E; Fushimi, K J

2016-01-01

Weakly interacting massive particles (WIMPs) are possible components of the Universe’s dark matter (DM). The detection of WIMPs is signaled by the recoil of the atomic nuclei which form a detector. CoGeNT at the Soudan Underground Laboratory (SUL) and DAMA at the Laboratori Nazionali del Gran Sasso (LNGS) have reported data on annual modulation of signals attributed to WIMPs. Both experiments are located in laboratories in the Northern Hemisphere. DM detectors are planned to operate (or already operate) in laboratories in the Southern Hemisphere, including SABRE at Stawell Underground Physics Laboratory (SUPL) in Australia, and DM-ICE in Antarctica. In this work we have analyzed the dependence of diurnal and annual modulation of signals, pertaining to the detection of WIMP, on the coordinates of the laboratory, for experiments which may be performed in the planned new Agua Negra Deep Experimental Site (ANDES) underground facility, to be built in San Juan, Argentina. We made predictions for NaI and Ge-type detectors placed in ANDES, to compare with DAMA, CoGeNT, SABRE and DM-ICE arrays, and found that the diurnal modulation of the signals, at the ANDES site, is amplified at its maximum value, both for NaI (Ge)-type detectors, while the annual modulation remains unaffected by the change in coordinates from north to south. (paper)

Estrés académico en estudiantes de la Facultad de Farmacia y Bioanálisis, Universidad de los Andes, Mérida-Venezuela

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Labrador Chacón, Carmen Zulay

2012-01-01

En esta tesis se ha tenido como objetivo, estudiar el estrés académico, así como algunos recursos psicosociales empleados, para su afrontamiento, en estudiantes de la Universidad de Los Andes, Mérida-Venezuela. La muestra estuvo constituida por 856 estudiantes del curso regular, de la Facultad de Farmacia y Bioanálisis. Para la medición del nivel de estrés académico se empleó el Cuestionario de Evaluación del Estrés Académico (CEEA) (Joan De Pablo, 2002). Para medir las variables sociodemográ...

Estimation de l'aléa sismique dans les Andes nord équatoriennes

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1996-01-01

Full Text Available Les Andes Nord équatoriennes ont connu de nombreux séismes historiques destructeurs. Pour caractériser l’aléa sismique de la région andine, nous avons fait une révision critique de la sismicité historique et de l’ensemble des failles actives de l’Équateur. Les deux sources majeures de l’aléa sismique sont respectivement la subduction superficielle pour la région côtière et le système transpressif des hautes Andes pour la région andine. Ce système est composé de failles décrochantes dextres d’orientation N30-35°E (failles du Rio Chingual-La Sofia et Pallatanga qui limitent respectivement au Nord et au Sud des failles inverses N-S du relais compressif de la vallée interandine (failles de Quito et de Latacunga. L’étude des mécanismes au foyer superficiels des Andes équatoriennes nous a permis de calculer une vitesse de raccourcissement crustal de 4.6 mm/a selon une direction N92°E et d’estimer des temps de récurrence et des périodes de retour. Un séisme de Mw = 5 pourrait se produire tous les 0.5 an, de Mw = 6 tous les 4.5 ans, de Mw = 7 tous les 45.4 ans. De même, sur une période de temps de 33 ans, 66 séismes de Mw=5 peuvent être attendus, 7 séismes de Mw=6 et 1 séisme de Mw=7. Enfin, nous avons estimé pour l’ensemble des sources sismogènes de la région andine des magnitudes maximales probables et des temps de récurrence. Un séisme de magnitude 7 à 7.5 peut se produire sur la faille du Rio Chingual tous les 400±440 ans et de magnitude 6.7 à 7.2 tous les 380±320 ans sur la faille de Pallatanga. Dans la vallée interandine, la faille de Quito est susceptible d’engendrer un séisme de magnitude 6.6 à 7.6 tous les 930±300 ans. LA AMENAZA SÍSMICA EN LOS ANDES ECUATORIANOS. Los Andes del Norte del Ecuador son una región sismogénica mayor, donde se puede contabilizar muchos terremotos históricos destructores. A fin de determinar la amenaza sísmica sobre la región andina, se hizo la asociaci

A paleolimnological perspective on industrial-era metal pollution in the central Andes, Peru.

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Cooke, Colin A; Abbott, Mark B

2008-04-15

To date, few studies have investigated the environmental legacy associated with industrialization in the South American Andes. Here, we present an environmental archive of industrial pollution from (210)Pb-dated lake cores recovered from Laguna Chipian, located near the Cerro de Pasco metallurgical region and Laguna Pirhuacocha, located near the Morococha mining region and the La Oroya smelting complex. At Laguna Chipian, trace metal concentrations increase beginning ~1900 AD, coincident with the construction of the central Peruvian railway, and the rapid industrial development of the Cerro de Pasco region. Trace metal concentrations and fluxes peak during the 1950s before subsequently declining up-core (though remaining well above background levels). While Colonial mining and smelting operations are known to have occurred at Cerro de Pasco since at least 1630 AD, our sediment record preserves no associated metal deposition. Based on our (14)C and (210)Pb data, we suggest that this is due to a depositional hiatus, rather than a lack of regional Colonial pollution. At Laguna Pirhuacocha, industrial trace metal deposition first begins ~1925 AD, rapidly increasing after ~1950 AD and peaking during either the 1970s or 1990s. Trace metal concentrations from these lakes are comparable to some of the most polluted lakes in North America and Europe. There appears to be little diagenetic alteration of the trace metal record at either lake, the exception being arsenic (As) accumulation at Laguna Pirhuacocha. There, a correlation between As and the redox-sensitive element manganese (Mn) suggests that the sedimentary As burden is undergoing diagenetic migration towards the sediment-water interface. This mobility has contributed to surface sediment As concentrations in excess of 1100 microg g(-1). The results presented here chronicle a rapidly changing Andean environment, and highlight a need for future research in the rate and magnitude of atmospheric metal pollution.

A paleolimnological perspective on industrial-era metal pollution in the central Andes, Peru

International Nuclear Information System (INIS)

Cooke, Colin A.; Abbott, Mark B.

2008-01-01

To date, few studies have investigated the environmental legacy associated with industrialization in the South American Andes. Here, we present an environmental archive of industrial pollution from 210 Pb-dated lake cores recovered from Laguna Chipian, located near the Cerro de Pasco metallurgical region and Laguna Pirhuacocha, located near the Morococha mining region and the La Oroya smelting complex. At Laguna Chipian, trace metal concentrations increase beginning ∼ 1900 AD, coincident with the construction of the central Peruvian railway, and the rapid industrial development of the Cerro de Pasco region. Trace metal concentrations and fluxes peak during the 1950s before subsequently declining up-core (though remaining well above background levels). While Colonial mining and smelting operations are known to have occurred at Cerro de Pasco since at least 1630 AD, our sediment record preserves no associated metal deposition. Based on our 14 C and 210 Pb data, we suggest that this is due to a depositional hiatus, rather than a lack of regional Colonial pollution. At Laguna Pirhuacocha, industrial trace metal deposition first begins ∼ 1925 AD, rapidly increasing after ∼ 1950 AD and peaking during either the 1970s or 1990s. Trace metal concentrations from these lakes are comparable to some of the most polluted lakes in North America and Europe. There appears to be little diagenetic alteration of the trace metal record at either lake, the exception being arsenic (As) accumulation at Laguna Pirhuacocha. There, a correlation between As and the redox-sensitive element manganese (Mn) suggests that the sedimentary As burden is undergoing diagenetic migration towards the sediment-water interface. This mobility has contributed to surface sediment As concentrations in excess of 1100 μg g -1 . The results presented here chronicle a rapidly changing Andean environment, and highlight a need for future research in the rate and magnitude of atmospheric metal pollution

Holocene compression in the Acequión valley (Andes Precordillera, San Juan province, Argentina): Geomorphic, tectonic, and paleoseismic evidence

Science.gov (United States)

Audemard, M.; Franck, A.; Perucca, L.; Laura, P.; Pantano, Ana; Avila, Carlos R.; Onorato, M. Romina; Vargas, Horacio N.; Alvarado, Patricia; Viete, Hewart

2016-04-01

The Matagusanos-Maradona-Acequión Valley sits within the Andes Precordillera fold-thrust belt of western Argentina. It is an elongated topographic depression bounded by the roughly N-S trending Precordillera Central and Oriental in the San Juan Province. Moreover, it is not a piggy-back basin as we could have expected between two ranges belonging to a fold-thrust belt, but a very active tectonic corridor coinciding with a thick-skinned triangular zone, squeezed between two different tectonic domains. The two domains converge, where the Precordillera Oriental has been incorporated to the Sierras Pampeanas province, becoming the western leading edge of the west-verging broken foreland Sierras Pampeanas domain. This latter province has been in turn incorporated into the active deformation framework of the Andes back-arc at these latitudes as a result of enhanced coupling between the converging plates due to the subduction of the Juan Fernández ridge that flattens the Nazca slab under the South American continent. This study focuses on the neotectonics of the southern tip of this N-S elongated depression, known as Acequión (from the homonym river that crosses the area), between the Del Agua and Los Pozos rivers. This depression dies out against the transversely oriented Precordillera Sur, which exhibits a similar tectonic style as Precordillera Occidental and Central (east-verging fold-thrust belt). This contribution brings supporting evidence of the ongoing deformation during the Late Pleistocene and Holocene of the triangular zone bounded between the two leading and converging edges of Precordillera Central and Oriental thrust fronts, recorded in a multi-episodic lake sequence of the Acequión and Nikes rivers. The herein gathered evidence comprise Late Pleistocene-Holocene landforms of active thrusting, fault kinematics (micro-tectonic) data and outcrop-scale (meso-tectonic) faulting and folding of recent lake and alluvial sequences. In addition, seismically

ANDES: An Underground Laboratory in South America

Science.gov (United States)

Dib, Claudio O.

ANDES (Agua Negra Deep Experiment Site) is an underground laboratory, proposed to be built inside the Agua Negra road tunnel that will connect Chile (IV Region) with Argentina (San Juan Province) under the Andes Mountains. The Laboratory will be 1750 meters under the rock, becoming the 3rd deepest underground laboratory of this kind in the world, and the first in the Southern Hemisphere. ANDES will be an international Laboratory, managed by a Latin American consortium. The laboratory will host experiments in Particle and Astroparticle Physics, such as Neutrino and Dark Matter searches, Seismology, Geology, Geophysics and Biology. It will also be used for the development of low background instrumentation and related services. Here we present the general features of the proposed laboratory, the current status of the proposal and some of its opportunities for science.

Diseño de la estrategia de Inglés con propósitos específicos en un contexto extracurricular para el aprendizaje del Inglés técnico médico en estudiantes de medicina de la Universidad Regional Autónoma de los Andes

OpenAIRE

Montes De Oca Sánchez, Irma Verónica

2017-01-01

1. Introducción. 2. Planteamiento de la propuesta de trabajo 3. Marco Teórico 4. Metodología 5. Resultados 6. Conclusiones y Recomendaciones. En el proceso de formación profesional del médico que realiza sus estudios en la Universidad Regional Autónoma de los Andes, se incluye la preparación en el dominio de competencias en inglés; misma que comprende el aprendizaje del inglés con propósitos generales (EGP) y no abarca el aprendizaje de aspectos específicos relacionados ...

Phytogeography of the vascular páramo flora of Ramal de Guaramacal (Andes, Venezuela) and its ties to other páramo floras

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Cuello, N.L.; Cleef, A.M.; Aymard, G.

2010-01-01

Ramal de Guaramacal is an outlier and lower elevation mountain range located at the northeastern end of the Venezuelan Andes. Phytogeographical patterns and affinities of the low altitude and wet vascular páramo flora of Ramal de Guaramacal, have been studied with emphasis in to the analysis of the floristic connections of the Guaramacal páramo flora with the neighboring dry páramos of the Sierra Nevada de Mérida and other páramo floras of the northern Andes and Central America. A total of 25...

Paleohidrología de los últimos 25000 años en los Andes bolivianos

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1995-01-01

Full Text Available PALÉOHYDROLOGIE DES DERNIÈRES 25 000 ANNÉES DANS LES ANDES BOLIVIENNES. Nous présentons une reconstruction climatique de haute résolution de l’Altiplano bolivien (Andes Centrales basée sur des données géomorphologiques, sédimentologiques, palynologiques et provenant de l’analyse des faunes d’ostracodes. Nous avons déterminé (1, de manière semi-quantitative, la température ainsi que (2 de façon quantitative, les variations des niveaux lacustres depuis la fin du Pléistocène (25 000 ans BP. Les principaux résultats obtenus sont les suivants: de 25 000 à 18 000 ans BP, les températures atmosphériques sont basses ainsi que les niveaux des lacs entre 18 000 et 15 000/14 000 ans BP, la présence d’une lacune de sédimentation est indicatrice d’une phase climatique sèche pendant le Tardi-Glaciaire (15 000/14 000 - 10 500, les lacs (phase Tauca et les glaciers se sont étendus de 10 500 à 8000 ans BP, les lacs et les glaciers reculent très rapidement pendant que la température globale moyenne augmente à l’Holocène moyen (8 000-3 900 ans BP, le climat régional est globalement de type sec autour de 3900 ans BP, le niveau du lac Titicaca monte fortement des conditions relativement humides s’installent alors et se maintiennent par la suite pendant le Petit âge de la Glace (16ème-19ème siècles, des conditions froides et humides prévalent. En base a datos geomorfológicos, sedimentológicos, palinológicos y el análisis de fauna de ostrácodos, se ha determinado (1, de manera semicuantitativa, la temperatura así como (2 los cambios cuantificados de las variaciones de los niveles lacustres desde el final del Pleistoceno (25 000 años BP. Los principales resultados obtenidos son los siguientes: de 25 000 a 18 000 años BP, las temperaturas atmosféricas son bajas así como los niveles de los lagos entre 18 000 y 15 000/14 000 años BP, una fase climática seca es definida por la presencia de una laguna de sedimentaci

Una escultura lítica del Formativo Temprano (1600-1000 AC) de Caraz, Callejón de Huaylas, Perú

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Gamboa, Jorge

2016-01-01

El Museo Arqueológico Municipal Hernán Osorio Herrera de la ciudad de Caraz, en la sierra de Ancash, alberga dos esculturas líticas del Período Formativo de los Andes centrales. Este artículo describe la iconografía de uno de esos relieves. Se presenta el estudio estilístico de esa escultura y su comparación con el arte lítico y en barro registrado en diversos asentamientos de la costa y sierra norte y norcentral de Perú. Este análisis permite asignar el relieve de Caraz al Formativo Temprano...

Factores de riesgo ambientales y alimentarios para la fluorosis dental, Andes, Antioquia, 2015

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Gustavo A. Posada-Jaramillo

2017-01-01

Full Text Available Objetivo: determinar los factores ambientales y alimentarios asociados a la fluorosis dental en la población de 12 a 15 años del municipio de Andes en el año 2015, para generar propuestas de intervención en salud bucal. Metodología: estudio de casos y controles, con un control por caso. Con una población de 206 adolescentes de 12 a 15 años. Criterios de selección: adolescentes con diagnóstico de fluorosis dental entre 2012 y 2014, reportados al Sistema de Vigilancia Epidemiológica; se excluyeron aquellas personas que no tuvieran dientes erupcionados en más de un 50%, restauraciones amplias o caries extensas, dientes fracturados y edentulos totales. Los casos fueron seleccionados por muestreo aleatorio simple, los controles a conveniencia. Se realizó examen clínico para clasificar según el Índice de Dean la presencia y nivel de fluorosis dental, se aplicó encuesta a los padres para indagar sobre hábitos de autocuidado, e identificar posibles fuentes de exposición a flúor. Se analizaron variables sociodemográficas, alimentarias y comportamentales, ambientales y clínicas, se utilizaron Chi2 de Pearson – or con intervalos de confianza del 95%. Se efectúo análisis de contenido de concentración de flúor en muestras de agroquímicos, alimentos, agua de consumo humano, sal, cremas dentales y suelos. Resultados: mediante regresión logística binaria usando el método stepwise los resultados mostraron una asociación entre manipulación de agroquímicos y fluorosis dental (or = 2,093; 95% 1,017 y 4,307. Conclusión: la manipulación de agroquímicos es un factor de riesgo para la aparición de la fluorosis dental en los adolescentes del municipio de Andes.

Photosynthetic performance of Colobanthus quitensis (Kunth Bartl. (Caryophyllaceae in a high-elevation site of the Andes of central Chile Desempeño fotosintético de Colobanthus quitensis (Kunth Bartl. (Caryophyllaceae en los Andes de Chile central

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M. ANGÉLICA CASANOVA-KATNY

2006-03-01

Full Text Available Photosynthesis of Colobanthus quitensis and mesoclimatic conditions of air temperature and light intensity during the growing season were investigated at 2,650 m in the central Chilean Andes. On three typical days of the growing period (January, March and May, CO2 exchange and chlorophyll fluorescence were measured. In addition, a series of fluorescence response curves with increasing light intensity at different temperatures were performed to estimate the propensity of Andean C. quitensis populations to be photoinhibited. Net Photosynthesis (Pn was low (ca. 2.0 mmol CO2 m-2s-1 during the morning and noon in days with high photosynthetic active radiation (PAR, above 1,800 mmol photons m-2s-1. Pn increased in the afternoon (3.5-4.8 mmol CO2 m-2s-1 when PAR decreased to ca. 1,400 mmol photons m-2s-1 and leaf temperature were ca. 20 °C. Fv/Fm in the diurnal periods was between 0.7-0.75 without evidence of photoinhibition. Leaves at 15 and 22 °C exhibited a slow decrease of F PSII with the increase in actinic light intensity, although the fraction of reaction centers open (expressed by qP remained higher at 22 °C. NPQ was saturated at light intensities close to 500 mmol photons m-2s-1 in leaves at 22 °C and at higher intensities at 15 °C, suggesting that NPQ could be a mechanism of energy dissipation at high light intensity and high leaf temperature in the field. Our results indicated that C. quitensis is not photodamaged during the diurnal cycle and that the low Pn registered during some diurnal periods are likely to be related with photorespiration, which has been suggested as an efficient protective mechanism for photoinhibition in alpine plants. Our results are also compared with the photosynthetic performance of C. quitensis populations from the maritime AntarcticSe estudió la fotosíntesis de Colobanthus quitensis y las condiciones mesoclimáticas de temperatura del aire e intensidad lumínica a 2.650 m en los Andes de Chile central. Se

The System Nobody Sees: Irrigated Wetland Management and Alpaca Herding in the Peruvian Andes

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Verzijl, A.; Guerrero Quispe, S.

2013-01-01

Increasingly, attention in regional, national, and international water governance arenas has focused on high-altitude wetlands. However, existing local water management practices in these wetlands are often overlooked. This article looks at the irrigation activities of alpaca herders in the community of Ccarhuancho in the Central Andes of Peru. For more than two centuries, they have been constructing small-scale irrigation canals to maintain and expand the local wetlands, called bofedales. Th...

Linfoma primario del sistema nervioso central en un paciente inmunocompetente

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José Málaga-Zenteno

2012-07-01

Full Text Available El linfoma primario del sistema nervioso central (LPSNC constituye el 2% de los linfomas extranodales y entre 0,3% y 1,5% de todas las neoplasias intracraneales en pacientes inmunocompetentes, siendo más frecuente a partir de los 60 años. Reportamos el caso de un paciente varón de 76 años, sin antecedentes médicos de importancia, que inició su enfermedad con inestabilidad en la marcha, dificultad para mover el hemicuerpo izquierdo, a predominio braquial, cefalea holocraneal y mareos. Ingresó a emergencia despierto, parcialmente desorientado, Glasgow 14 y ptosis palpebral derecha; además, hemiparesia e hipoestesia izquierda, a predominio crural. Por tomografía computarizada cerebral se evidenció imagen captadora de contraste en región frontoparietal derecha, intra y extra craneal, edema cerebral y desplazamiento de la línea media. Se realizó craneotomía y biopsia del tumor, diagnosticándose linfoma difuso de células grandes B del sistema nervioso central. Fue VIH negativo. Se descartó otro tumor primario y metástasis. Recibió esquema CHOD/BVAM y radioterapia. Evolucionó favorablemente. Según resonancia magnética cerebral postratamiento, desapareció el tumor.

DISPONIBILIDAD DEL RECURSO HÍDRICO EN LA MICROCUENCA DEL RÍO SEGUNDO. REGIÓN CENTRAL DE COSTA RICA

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Hernando-Echeverría, Ligia; Ruíz-Hernández, Amalia; Solís-Zamora, Kathya

2012-01-01

La microcuenca del río Segundo es parte de la principal zona de explotación hídrica, en la región Central de Costa Rica. Razón por la cual se realiza un diagnóstico de la disponibilidad del recur-so hídrico en  la microcuenca del río Segundo, e  identifcar  las áreas con mayor problemática de disponibilidad de recurso hídrico. Para ello se calculó un balance hídrico mensual, según uso del suelo, unidad geomorfológica y zona climática. Con base en este balance se calculó y clasifcó la disponib...

Compositional variations revealed by ASTER image analysis of the Viedma Volcano, southern Andes Volcanic Zone Variaciones composicionales reveladas mediante análisis de imágenes ASTER del volcán Viedma, Zona Volcánica Andina Austral

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Chiaki Kobayashi

2010-07-01

partes oscuras en el área del cráter central. La concentración de SiO2 se calculó a través del uso de las bandas en las regiones visibles e infrarrojo termal. Las partes oscura y brillante tienen un promedio aproximado de 51% y 63% de SiO2 en peso, respectivamente, lo que indica que el volcán Viedma expone una amplia diferenciación de las concentraciones de SiO2. Aunque, según otros autores, las muestras analizadas de material piroclástico del volcán Viedma tienen contenidos de 64-66% SiO2 y que otros aparatos de la ZVA son volcanes esencialmente monolitológicos dacíticos/andesíticos, el edificio del volcán Viedma estaría compuesto principalmente de basaltos o las rocas más antiguas de su basamento tienen un bajo contenido de sílice.

Flora y vegetación leñosa de los bosques de los Andes en la región de Madidi, La Paz (Bolivia)

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Fuentes Claros, Alfredo Fernando

2016-01-01

Introducción: La región del Madidi en el noroeste de Bolivia es una de las más biodiversas del mundo, por incluir un amplio rango altitudinal desde los 200 hasta más de 6000 m, y floras de los Andes y la Amazonía, dos de las regiones biogeográficas más diversas del mundo. Esta región comprende territorios de tres áreas protegidas de interés nacional (Madidi, Apolobamba y Pilón Lajas), superpuestas a comunidades indígenas, campesinas, y áreas de exploración hidrocarburífera, lo cual ha generad...

Morphologic evolution of the Central Andes of Peru

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Gonzalez, Laura; Pfiffner, O. Adrian

2012-01-01

In this paper, we analyze the morphology of the Andes of Peru and its evolution based on the geometry of river channels, their bedrock profiles, stream gradient indices and the relation between thrust faults and morphology. The rivers of the Pacific Basin incised Mesozoic sediments of the Marañon thrust belt, Cenozoic volcanics and the granitic rocks of the Coastal Batholith. They are mainly bedrock channels with convex upward shapes and show signs of active ongoing incision. The changes in lithology do not correlate with breaks in slope of the channels (or knick points) such that the high gradient indices (K) with values between 2,000-3,000 and higher than 3,000 suggest that incision is controlled by tectonic activity. Our analysis reveals that many of the ranges of the Western Cordillera were uplifted to the actual elevations where peaks reach to 6,000 m above sea level by thrusting along steeply dipping faults. We correlate this uplift with the Quechua Phase of Neogene age documented for the Subandean thrust belt. The rivers of the Amazonas Basin have steep slopes and high gradient indices of 2,000-3,000 and locally more than 3,000 in those segments where the rivers flow over the crystalline basement of the Eastern Cordillera affected by vertical faulting. Gradient indices decrease to 1,000-2,000 within the east-vergent thrust belt of the Subandean Zone. Here a correlation between breaks in river channel slopes and location of thrust faults can be established, suggesting that the young, Quechua Phase thrust faults of the Subandean thrust belt, which involve Neogene sediments, influenced the channel geometry. In the eastern lowlands, these rivers become meandering and flow parallel to anticlines that formed in the hanging wall of Quechua Phase thrust faults, suggesting that the river courses were actively displaced outward into the foreland.

Reabsorción de nitrógeno y fósforo foliar en árboles de bosques montanos en los Andes centrales de Colombia

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Miguel Vera

1999-06-01

Full Text Available Se determinaron las concentraciones y los porcentajes de reabsorción de nitrógeno y fósforo foliar en cinco especies de árboles de un bosque montano bajo (BMB a 1850 m.s.n.m. y en cinco de un bosque montano alto (BMA a 2800 m.s.n.m en la Cordillera Central colombiana, asi como la disponibilidad de nitrógeno y fósforo del suelo. Los porcentajes de reabsorción de N y P no fueron significativamente diferentes entre las especies de estos dos bosques. A pesar de esto, se observó que la reabsorción de P foliar tendió a ser mayor en las especies del BMB donde la concentración de P en el suelo fue significativamente más baja (3.2 ppm vs. 9.0 ppm. Cuando la reabsorción de P foliar se expresó como función de la concentración en hojas maduras en 12 tipos de bosques montanos tropicales, se encontró una correlación negativa y estadísticamente significativa. Estos resultados sugieren que los porcentajes de reabsorción de P foliar en bosques montanos estarían controlados parcialmente por la disponibilidad del elemento.Mature leaves and litterfall were collected between November 1992 and February 1993 from one to three individuals of five canopy tree species of a lower montane rain forest (LMRF at 1850 m. and five canopy tree species of an upper montane rain forest (UMRF at 2800 m. in the Central Andes of Colombia, to determine the concentrations and percentage retranslocation of nitrogen and phosphorus. The availability of these two nutrients was measured in the soils, by means of extracts of NH3-NH4, NO2-NO3 and PO4, and incubations of surface soil samples (0-10 cm to measure the rates of nitrogen mineralization and nitrification. In the species of the LMRF the average concentration of N in mature leaves (1.19 % dry weight and litterfall (0.87 % was significantly higher than in mature leaves (0.90 % and litterfall (0.59 % of the tree species of the UMRF. Percentage retranslocation of N and P were not significantly different between the

Body size, composition, and blood pressure of high-altitude Quechua from the Peruvian Central Andes (Huancavelica, 3,680 m).

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Toselli, S; Tarazona-Santos, E; Pettener, D

2001-01-01

Although much information is available about the effects of high altitude on physiological characteristics, less is know about its effect on body composition. In the present study, anthropometric and body composition variables were investigated in a sample of 77 adult Quechua males from the Peruvian Central Andes (Huancavelica, 3,680 m). The subjects are shorter in relation to body weight than other ethnic groups, whereas body proportions are macrocormic (indicating a long trunk relative to the lower extremities), with intermediate values of the acromial-iliac index. All skinfold thicknesses are low (approximately 15th percentiles of NHANES reference values for the triceps and subscapular skinfolds), but tend to be higher than in the other Quechua populations. Similar results are obtained when percentage fat is estimated. Somatotypes are dominant in mesomorphy with very low ectomorphy. Comparison with a sample of high-altitude Kirghiz (3,200 m), previously studied with the same methods, shows higher values in the Peruvian sample for all variables related to adiposity. The presence of low adiposity in the Quechua population could be associated with stresses of the high-altitude environment. Mean values of blood pressure are very low and there is no correlation with age.

Unexpected Climatological Behavior of MLT Gravity Wave Momentum Flux in the Lee of the Southern Andes Hot Spot

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DeWit, R. J.; Janches, D.; Fritts, D. C.; Stockwell, R. G.; Coy, L.

2017-01-01

The Southern Argentina Agile MEteor Radar (SAAMER), located at Tierra del Fuego (53.7degS, 67.7degW), has been providing near-continuous high-resolution measurements of winds and high-frequency gravity wave (GW) momentum fluxes of the mesopause region since May 2008. As SAAMER is located in the lee of the largest seasonal GW hot spot on Earth, this is a key location to study GWs and their interaction with large-scale motions. GW momentum flux climatologies are shown for the first time for this location and discussed in light of these unique dynamics. Particularly, the large eastward GW momentum fluxes during local winter are surprising, as these observations cannot be explained by the direct upward propagation of expected large-amplitude mountain waves (MWs) through the eastward stratospheric jet. Instead, these results are interpreted as secondary GWs propagating away from stratospheric sources over the Andes accompanying MW breaking over the Southern Andes.

L'enfant et le terroir. La construction de l'identité paysanne dans une communauté des Andes péruviennes

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1995-01-01

Full Text Available Cet article propose quelques pistes de travail sur l'identité et la notion de personne à partir de l'étude du statut de l'enfant. L'auteur montre notamment comment le lieu de naissance établit les bases de l'identité paysanne andine en inscrivant le nouveau-né dans un triple environnement (social, familial, mythique qui définit son appartenance à la lignée paternelle ou maternelle et, au-delà du groupe lignager, à la communauté. EL NIÑO Y LA TIERRA. LA CONSTRUCCIÓN DE LA IDENTITAD CAMPESINA EN UNA COMUNIDAD DE LOS ANDES PERUANOS. Este artículo propone algunas pistas de investigación sobre la identidad y la noción de persona a partir del estudio del estatus del niño. La autora muestra en particular cómo el lugar de nacimiento establece las bases de la identidad campesina andina al ubicar al recién nacido en un triple entorno (el grupo social, la familia y los mitos que define su pertenencia a la rama paterna y, más allá del linaje a la comunidad. THE CHILD AND THE LAND. THE CONSTRUCTION OF PEASANT’S IDENTITY IN A COMMUNITY OF THE PERUVIAN ANDES. This paper proposes a few lines of research about identity and the notion of the human being based on the study of the status of the infant. The author shows how birth-place establishes the basis of Andean peasant's identity by allowing the infant to fit into a triple environment (the social group, the extended family and the myths. This environment defines if infant belongs to the paternal or maternal line and, beyond the lineage, to the community.

Una nueva Armeria del Sistema Central (España: A. rivasmartinezii (Plumbaginaceae

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Sardinero, Santiago

1997-12-01

Full Text Available A new taxon from the central-western Sistema Central (Sierra de Béjar and Sierra de Tormantos, Spain, Armeria rivasmartinezii. is described and illustrated. lts morphological affinities and variability are discussed in concordance with its hypothetical hybrid origin.

Se describe e ilustra un nuevo taxon del centro-occidente del Sistema Central español. Armeria rivasmartinezii. Se discuten sus afinidades morfológicas y variabilidad en concordancia con su hipotético origen híbrido.

Use of high-resolution satellite images for detection of geological structures related to Central Andes geothermal field, Chile.

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Benavides-Rivas, C. L.; Soto-Pinto, C. A.; Arellano-Baeza, A. A.

2014-12-01

Central valley and the border with Argentina in the center, and in the fault system Liquiñe-Ofqui in the South of the country. High resolution images from the LANDSAT 8 satellite have been used to delineate the geological structures related to the potential geothermal reservoirs located at the northern end of the Southern Volcanic Zone of Chile. It was done by applying the lineament extraction technique, using the ADALGEO software, developed by [Soto et al., 2013]. These structures have been compared with the distribution of main geological structures obtained in the field. It was found that the lineament density increases in the areas of the major heat flux indicating that the lineament analysis could be a power tool for the detection of faults and joint zones associated to the geothermal fields. A lineament is generally defined as a straight or slightly curved feature in the landscape visible satellite image as an aligned sequence of pixel intensity contrast compared to the background. The system features extracted from satellite images is not identical to the geological lineaments that are generally determined by ground surveys, however, generally reflects the structure of faults and fractures in the crust. A temporal sequence of eight Landsat multispectral images of Central Andes geothermal field, located in VI region de Chile, was used to study changes in the configuration of the lineaments during 2011. The presence of minerals with silicification, epidotization, and albitization, which are typical for geothrmal reservoirs, was also identified, using their spectral characteristics, and subsequently corroborated in the field. Both lineament analysis and spectral analysis gave similar location of the reservoir, which increases reliability of the results.

TÉCNICAS DE LIQUENOMETRÍA BASADAS EN RHIZOCARPON SUBGÉNERO RHIZOCARPON PARA DATAR DEPÓSITOS GLACIARES EN LOS ANDES PATAGÓNICOS

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Irene Garibotti

2007-12-01

Full Text Available La liquenometría es una técnica de datación que estima la edad de exposición de una superficie a partir del diámetro de los líquenes que crecen en ella. El objetivo de este estudio es calibrar la curva de crecimiento de Rhizocarpon subgénero Rhizocarpon en los Andes Patagónicos, y aplicarla para reconstruir las fluctuaciones glaciares durante los últimos siglos. Para ello se investigaron seis glaciares, tres en el norte y tres en el sur de los Andes Patagónicos, en los cuales se realizaron mediciones del diámetro de ejemplares del subgénero Rhizocarpon en sitios de edad conocida (sitios control y sitios de edad desconocida. La edad de los sitios control se determinó fehacientemente a partir de información histórica. Los datos liquenométricos relevados en estos sitios control fueron utilizados para calibrar la curva de crecimiento. La relación entre el tamaño de los líquenes y la edad de la superficie (curva de crecimiento es lineal, indicando que los líquenes del subgénero Rhizocarpon tienen una tasa de crecimiento constante a lo largo del tiempo. Esta curva se extiende por 270 años. Aplicación de la curva a los datos liquenométricos relevados en las morenas de edad desconocida permitió establecer la cronología de la secuencia de morenas de los seis glaciares bajo estudio. Los datos liquenométricos fueron contrastados con datos dendrocronológicos, mostrando una gran concordancia entre los métodos. Los resultados obtenidos muestran dos períodos principales de formación de morenas. El primer período se extiende desde la mitad del siglo XVII hasta finales del siglo XIX, y está caracterizado por morenas muy prominentes. El segundo período se extiende desde mediados del siglo XIX hasta finales del siglo XX, y esta caracterizado por la formación de un gran número de morenas pequeñas.

Tectonic geomorphology of the Andes with SIR-A and SIR-B

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Bloom, Arthur L.; Fielding, Eric J.

1986-01-01

Data takes from SIR-A and SIR-B (Shuttle Imaging Radar) crossed all of the principal geomorphic provinces of the central Andes between 17 and 34 S latitude. In conjunction with Thematic Mapping images and photographs from hand-held cameras as well as from the Large Format Camera that was flown with SIR-B, the radar images give an excellent sampling of Andean geomorphology. In particular, the radar images show new details of volcanic rocks and landforms of late Cenozoic age in the Puna, and the exhumed surfaces of tilted blocks of Precambrian crystalline basement in the Sierras Pampeanas.

Caries dental en niños de 0-5 años del municipio de Andes, Colombia. Evaluación mediante el sistema internacional de detección y valoración de caries - ICDAS

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Blanca S. Ramírez-Puerta

2017-01-01

Full Text Available La falta de información de la situación de caries dental en la primera infancia en Andes, limita las acciones en el marco de la Alianza por un Futuro libre de Caries. Objetivo: establecer la situación de caries dental de los niños y niñas de 0 a 5 años del Municipio de Andes, Colombia. Metodología: fueron examinados 623 niños y niñas para evaluar la presencia y severidad de las lesiones de caries, con base en criterios del Sistema Internacional para la detección y evaluación de caries - icdas. Se calcularon las proporciones de experiencia y prevalencia de caries dental, y los índices cICDAS 5-6 opd y cICDAS 1-6 opd. Resultados: el 38,2% tenía experiencia de caries dental severa, cuando se incluyen las lesiones iniciales y moderadas de caries dental la experiencia fue 88,4%. Al año de edad, el 4,9% tenía lesiones severas de caries dental, y a los 5 años el 53,6% presentó este tipo de lesiones. El índice cICDAS 5-6 opd fue 0,15±0,8 al año de edad y 2,79±3,6 a los 5 años; el valor del indicador aumenta a 1,97±2,9 y 9,61±4,6 respectivamente, cuando se incluyen lesiones iniciales y moderadas de caries dental, cICDAS 1-6 opd. Discusión: la enfermedad está presente desde el primer año en el 58,8%, el doble de lo reportado en el país a esta edad (29,3%. Conclusión: los hallazgos resaltan la necesidad de diseñar estrategias integrales para el control de la enfermedad, que involucren la salud bucal en políticas y programas de primera infancia.

Finanzas de la Universidad de Los Andes

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Rosa Aura Casal de Altuve

2006-01-01

Full Text Available El objetivo primario de este artículo es el de fungir de base comparativa para otros estudios de países latinoamericanos que podrían estar considerando síntomas similares en el área de la investigación contable. El punto de partida lo representa un estudio de caso de los profesores del Departamento de Contabilidad y Finanzas de la Facultad de Ciencias Económicas y Sociales de la Universidad de los Andes. El artículo analiza la relación entre investigación y enseñanza y si el departamento está o no cumpliendo con sus objetivos. Un objetivo secundario consiste en la determinación de los posibles factores que han tenido una influencia significativa en el desempeño de la investigación y de la enseñanza por parte de los investigadores. Basándose en entrevistas y recolección directa de datos, se consideran las estrategias institucionales para fijar los objetivos de las actividades de investigación

Water and sediment quality of the Lake Andes and Choteau Creek basins, South Dakota, 1983-2000

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Sando, Steven Kent; Neitzert, Kathleen M.

2003-01-01

The Bureau of Reclamation has proposed construction of the Lake Andes/Wagner Irrigation Demonstration Project to investigate environmental effects of irrigation of glacial till soils substantially derived from marine shales. During 1983-2000, the U.S. Geological Survey collected hydrologic, water-quality, and sediment data in the Lake Andes and Choteau Creek Basins, and on the Missouri River upstream and downstream from Choteau Creek, to provide baseline information in support of the proposed demonstration project. Lake Andes has a drainage area of about 230 mi2 (square miles). Tributaries to Lake Andes are ephemeral. Water-level fluctuations in Lake Andes can be large, and the lake has been completely dry on several occasions. The outlet aqueduct from Lake Andes feeds into Garden Creek, which enters Lake Francis Case just upstream from Fort Randall Dam on the Missouri River. For Lake Andes tributary stations, calcium, magnesium, and sodium are approximately codominant among the cations, and sulfate is the dominant anion. Dissolved-solids concentrations typically range from about 1,000 mg/L (milligrams per liter) to about 1,700 mg/L. Major-ion concentrations for Lake Andes tend to be higher than the tributaries and generally increase downstream in Lake Andes. Proportions of major ions are similar among the different lake units (with the exception of Owens Bay), with calcium, magnesium, and sodium being approximately codominant among cations, and sulfate being the dominant anion. Owens Bay is characterized by a calcium sulfate water type. Dissolved-solids concentrations for Lake Andes typically range from about 1,400 to 2,000 mg/L. Whole-water nitrogen and phosphorus concentrations are similar among the Lake Andes tributaries, with median whole-water nitrogen concentrations ranging from about 1.6 to 2.4 mg/L, and median whole-water phosphorus concentrations ranging from about 0.5 to 0.7 mg/L. Whole-water nitrogen concentrations in Lake Andes are similar among the

EL CALENTAMIENTO GLOBAL Y SUS MANIFESTACIONES EN LA CRIÓSFERA DE LAS ALTAS MONTAÑAS DEL NORTE ARGENTINO.

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Ana Lía Ahumada

2007-12-01

Full Text Available Los efectos de el Cambio Climático Global afectan fuertemente los parámetros físicos que condicionan la estabilidad de la Criósfera del planeta. Las temperaturas del siglo XX se han incrementado en la Cordillera de los Andes en 0,62o C entre 1901-1997, incrementándose en 0,4o C por encima de lo esperado durante los 90 por efecto del Calentamiento Global. Por otro lado recientes evaluaciones de los glaciares de los Andes Centrales prevén una desaparición del 80% de los mismos en los próximos 15 años. La Criósfera se encuentra representada en las altas montañas del NW argentino por la presencia de permafrost de montaña, el que se manifiesta topoclimáticamente en el paisaje con glaciares de escombros y una asociación de geoformas menores generadas por el congelamiento permanente o estacional de los suelos. Los glaciares de escombros activos, indicadores de permafrost discontínuo, se encuentran ubicados de S a N en alturas desde 4000 a 4850 m s.n.m. en la región. Sus condiciones de estabilidad geoecológica son resilientes debido a las modificaciones de la temperatura en altura. Se han observado geoindicadores criosféricos de cambio climático global que pueden ser usados para el monitoreo y seguimiento de cambios geológicos en la región del NW de Argentina con permafrost andino. Se describen brevemente ejemplos de indicadores criosféricos. Los mismos pueden ser usados para el monitoreo y seguimiento de cambios geológicos en la región del NW de Argentina con permafrost andino. Como resultado del Calentamiento Global el hielo contenido en glaciares de escombros se está descongelando. Esto puede resultar en deslizamientos catastróficos, endicamientos y aluvionamientos en el curso de los ríos de montaña que provocan desastres significativos en las regiones pobladas de la zona de trabajo y el daño consecuente en la infraestructura vial y en instalaciones de energía eléctrica de costosa recuperación

Eocene extensional exhumation of basement and arc rocks along southwesternmost Peru, Central Andes.

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Noury, Mélanie; Bernet, Matthias; Sempéré, Thierry

2014-05-01

The overthickened crust of the current Central Andes is commonly viewed as the result of tectonic shortening. However, in the present-day terrestrial forearc and arc of southwesternmost Peru, crustal thickness increases from 30 km along the coastline to >60 km below the active arc, whereas the upper crust exhibits little to no evidence of crustal shortening and, in constrast, many extensional features. How (and when) crustal overthickness was acquired in this region is thus little understood. Because crustal overthickening often results in extensional collapse and/or significant erosion, here we address this issue through a regional-scale study of exhumation using fission-track thermochronology. The limited fission-track data previously available in the area suggested that exhumation began during the Mesozoic. In this study, we present new apatite and zircon fission-track data obtained along the current terrestrial forearc of southwesternmost Peru. This relatively restricted area presents the interest of providing extensive outcrops of Precambrian to Ordovician basement and Early Jurassic to Late Cretaceous arc plutons. In order to compare the chronology of exhumation of these units, we performed extensive sampling for fission-track dating, as well as structural mapping. Our results indicate that the basement rocks and Jurassic plutons that crop out in the Arequipa region, where the crust is now >50 km-thick, experienced a rapid cooling through the 240-110°C temperature range between ~65 and ~35 Ma. This period of rapid exhumation coincided in time with the accumulation of terrestrial forearc deposits (the Lower Moquegua Group), that exhibit many syn-sedimentary extensional features and are bounded by conspicuous normal faults, specifically along the region where intense activity of the main arc between ~90 and ~60 Ma had led to voluminous magma emplacement. This close succession of (1) intense magmatic activity and (2) regional-scale exhumation associated with

A paleolimnological perspective on industrial-era metal pollution in the central Andes, Peru

Energy Technology Data Exchange (ETDEWEB)

Cooke, Colin A. [Department of Geology, University of Pittsburgh, Pittsburgh, PA 15260 (United States); Earth and Atmospheric Sciences, University of Alberta, Edmonton, AB, T6G 2E3 (Canada)], E-mail: cacooke@ualberta.ca; Abbott, Mark B. [Earth and Atmospheric Sciences, University of Alberta, Edmonton, AB, T6G 2E3 (Canada); Section of Anthropology, Carnegie Museum of Natural History, Pittsburgh, PA 15206 (United States)

2008-04-15

To date, few studies have investigated the environmental legacy associated with industrialization in the South American Andes. Here, we present an environmental archive of industrial pollution from {sup 210}Pb-dated lake cores recovered from Laguna Chipian, located near the Cerro de Pasco metallurgical region and Laguna Pirhuacocha, located near the Morococha mining region and the La Oroya smelting complex. At Laguna Chipian, trace metal concentrations increase beginning {approx} 1900 AD, coincident with the construction of the central Peruvian railway, and the rapid industrial development of the Cerro de Pasco region. Trace metal concentrations and fluxes peak during the 1950s before subsequently declining up-core (though remaining well above background levels). While Colonial mining and smelting operations are known to have occurred at Cerro de Pasco since at least 1630 AD, our sediment record preserves no associated metal deposition. Based on our {sup 14}C and {sup 210}Pb data, we suggest that this is due to a depositional hiatus, rather than a lack of regional Colonial pollution. At Laguna Pirhuacocha, industrial trace metal deposition first begins {approx} 1925 AD, rapidly increasing after {approx} 1950 AD and peaking during either the 1970s or 1990s. Trace metal concentrations from these lakes are comparable to some of the most polluted lakes in North America and Europe. There appears to be little diagenetic alteration of the trace metal record at either lake, the exception being arsenic (As) accumulation at Laguna Pirhuacocha. There, a correlation between As and the redox-sensitive element manganese (Mn) suggests that the sedimentary As burden is undergoing diagenetic migration towards the sediment-water interface. This mobility has contributed to surface sediment As concentrations in excess of 1100 {mu}g g{sup -1}. The results presented here chronicle a rapidly changing Andean environment, and highlight a need for future research in the rate and magnitude

An InSAR-based survey of volcanic deformation in the central Andes

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Pritchard, M. E.; Simons, M.

2004-02-01

We extend an earlier interferometric synthetic aperture radar (InSAR) survey covering about 900 remote volcanos of the central Andes (14°-27°S) between the years 1992 and 2002. Our survey reveals broad (10s of km), roughly axisymmetric deformation at 4 volcanic centers: two stratovolcanoes are inflating (Uturuncu, Bolivia, and Hualca Hualca, Peru); another source of inflation on the border between Chile and Argentina is not obviously associated with a volcanic edifice (here called Lazufre); and a caldera (Cerro Blanco, also called Robledo) in northwest Argentina is subsiding. We explore the range of source depths and volumes allowed by our observations, using spherical, ellipsoidal and crack-like source geometries. We further examine the effects of local topography upon the deformation field and invert for a spherical point-source in both elastic half-space and layered-space crustal models. We use a global search algorithm, with gradient search methods used to further constrain best-fitting models. Inferred source depths are model-dependent, with differences in the assumed source geometry generating a larger range of accepted depths than variations in elastic structure. Source depths relative to sea level are: 8-18 km at Hualca Hualca; 12-25 km for Uturuncu; 5-13 km for Lazufre, and 5-10 km at Cerro Blanco. Deformation at all four volcanoes seems to be time-dependent, and only Uturuncu and Cerro Blanco were deforming during the entire time period of observation. Inflation at Hualca Hualca stopped in 1997, perhaps related to a large eruption of nearby Sabancaya volcano in May 1997, although there is no obvious relation between the rate of deformation and the eruptions of Sabancaya. We do not observe any deformation associated with eruptions of Lascar, Chile, at 16 other volcanoes that had recent small eruptions or fumarolic activity, or associated with a short-lived thermal anomaly at Chiliques volcano. We posit a hydrothermal system at Cerro Blanco to explain the

Mesozoic–Cenozoic Evolution of the Western Margin of South America: Case Study of the Peruvian Andes

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Laura Gonzalez

2013-06-01

Full Text Available Based on the structural style and physiographic criteria, the Central Andes of Peru can be divided into segments running parallel to the Pacific coast. The westernmost segment, the Coastal Belt, consists of a Late Jurassic–Cretaceous volcanic arc sequence that was accreted to the South American craton in Cretaceous times. The Mesozoic strata of the adjacent Western Cordillera represent an ENE-vergent fold-and-thrust belt that formed in Eocene times. Tight upright folds developed above a shallow detachment horizon in the West, while more open folds formed above a deeper detachment horizon towards the East and in the neighboring Central Highlands. A completely different style with steeply dipping reverse faults and open folds affecting the Neoproterozoic crystalline basement is typical for the Eastern Cordillera. The Subandean Zone is characterized by mainly NE-vergent imbricate thrusting which occurred in Neogene times. A quantitative estimate of the shortening of the orogen obtained from balanced cross-sections indicates a total shortening of 120–150 km (24%–27%. This shortening was coevel with the Neogene westward drift of South America, occurred at rates between 3 and 4.7 mm/year and was responsible for the high elevation of the Peruvian Andes.

Genetic structure of Quechua-speakers of the Central Andes and geographic patterns of gene frequencies in South Amerindian populations.

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Luiselli, D; Simoni, L; Tarazona-Santos, E; Pastor, S; Pettener, D

2000-09-01

A sample of 141 Quechua-speaking individuals of the population of Tayacaja, in the Peruvian Central Andes, was typed for the following 16 genetic systems: ABO, Rh, MNSs, P, Duffy, AcP1, EsD, GLOI, PGM1, AK, 6-PGD, Hp, Gc, Pi, C3, and Bf. The genetic structure of the population was analyzed in relation to the allele frequencies available for other South Amerindian populations, using a combination of multivariate and multivariable techniques. Spatial autocorrelation analysis was performed independently for 13 alleles to identify patterns of gene flow in South America as a whole and in more specific geographic regions. We found a longitudinal cline for the AcP1*a and EsD*1 alleles which we interpreted as the result of an ancient longitudinal expansion of a putative ancestral population of modern Amerindians. Monmonnier's algorithm, used to identify areas of sharp genetic discontinuity, suggested a clear east-west differentiation of native South American populations, which was confirmed by analysis of the distribution of genetic distances. We suggest that this pattern of genetic structures is the consequence of the independent peopling of western and eastern South America or to low levels of gene flow between these regions, related to different environmental and demographic histories. Copyright 2000 Wiley-Liss, Inc.

Una especie nueva de rana arbórea del género Hyloscirtus (Amphibia: Anura: Hylidae de la Cordillera del Cóndor

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Ana Almendáriz

2014-01-01

Full Text Available Las ranas ecuatorianas del género Hyloscirtus incluyen 16 especies descritas, de las cuales 11 pertenecen al grupo H. larinopygion. Su distribución se limita a los flancos de la Cordillera de los Andes, tanto al oriente como al occidente. Una evaluación de la herpetofauna en el sector meridional de la Cordillera del Cóndor (bosques montanos sobre mesetas de arenisca en la provincia de Zamora Chinchipe, Ecuador, condujo al descubrimiento de una especie nueva del grupo que describimos aquí como Hyloscirtus condor sp. nov.; se analizan los renacuajos, las llamadas de anuncio y se estima las relaciones filogenéticas de la especie nueva y de las especies relacionadas en base a nuevas secuencias de los genes mitocondriales 12S, tRNA Val y 16S, con un total de hasta 2508 bp. Los resultados muestran que el grupo H. larinopygion está conformado por dos clados, uno distribuido en los Andes norte y centro de Ecuador y el otro al sur. La nueva especie pertenece al clado sur y es hermana de H. tapichalaca y de una especie aparentemente no descrita de la Provincia Morona Santiago. La especie nueva difiere de sus congéneres por su patrón de coloración dorsal, que consiste de puntos amarillo obscuro en un fondo canela. Es la especie más grande del grupo H. larinopygion y comparte con H. tapichalaca la presencia de una espina prepólica grande y curvada y brazos hipertrofiados. La especie nueva habita un área remota y bien conservada de la Cordillera del Cóndor. El descubrimiento de ésta y otras especies nuevas del mismo lugar denota la importancia biológica del área y motivan al desarrollo de planes de conservación.

Los costos de la expedición militar a Chile, 1815-1818

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Beatriz Bragoni

2016-09-01

Full Text Available Este trabajo explora las estrategias utilizadas para financiar la creación y el sostenimiento del Ejército de los Andes y los instrumentos fiscales utilizados para conseguirlo. El análisis de los distintos rubros que integraban las cajas del ejército permite examinar el peso de los recursos aportados por el gobierno central y por la jurisdicción cuyana. Asimismo, analiza el destino de los fondos a través del estudio de los presupuestos del ejército, con el objetivo de ponderar el peso que tuvieron los salarios en el total de los gastos militares durante la etapa previa al cruce de los Andes, y en la posterior, cuando el ejército estaba en Chile bajo severas condiciones fiscales de los gobiernos patriotas.

Microdureza del esmalte dental en incisivos centrales permanentes de dos genotipos bovinos

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Jorge Cabrera A

2011-04-01

Full Text Available Objetivo. Evaluar la microdureza del esmalte dental de novillos criollos de origen patagónico y cruza índica criados en ambientes diferentes. Materiales y métodos. Se utilizaron dientes incisivos centrales derechos de novillos adultos: ocho Criollos Patagónicos (GCP y siete Cruzas Índicas (GCI. Para cada diente se definió una transecta central recorriendo el diente desde el borde externo del esmalte hacia la dentina y se midió la dureza en tres profundidades equidistantes: a 30 μ del borde exterior (P1, a 30 μ previos a la conexión amelodentinaria (P3 y P2 equidistante entre P1 y P3. Las mediciones de microdureza se realizaron con un microdurómetro Shimadzu modelo HMV-2 y se expresaron en unidades Vickers. Para el análisis se utilizó un modelo de regresión aleatoria. Se empleó el criterio de información de Akaike para la elección de la estructura de las matrices asociadas a los efectos aleatorios. Para el análisis estadístico se empleó el procedimiento PROC MIXED de SAS, y un nivel de significación del 5%. Resultados. No se detectó falta de paralelismo entre los grupos (p>0.05, con lo cual se ajustaron rectas de igual pendiente en cada grupo. La dureza media del esmalte disminuyó al aumentar la profundidad de la medición para ambos genotipos. Se observó heterogeneidad en la variabilidad de los grupos. Conclusiones. El GCP presentó mayor dureza pero fue el de mayor variabilidad. Se confirma la disminución de la dureza media con el aumento de la profundidad en el esmalte independientemente del genotipo y el ambiente.

Intervencion psicoeducativa en adolescentes con tumores del sistema nerviosos central

OpenAIRE

Grau Rubio, Claudia; Hernández Núñez-Polo, Mercedes

2002-01-01

Se describen los resultados de la evaluación neuropsicológica y de un programa de intervención psicoeducativa y apoyo emocional aplicados a 5 adolescentes afectados por un tumor del sistema nervioso central. Este programa se desarrolló en ASION (Asociación de padres de niños enfermos de cáncer de la Comunidad de Madrid).

Ethnobotany of the Sierra Nevada del Cocuy-Güicán

NARCIS (Netherlands)

Rodríguez, Mireia Alcántara; Angueyra, Andrea; Cleef, Antoine M.; Andel, van Tinde

2018-01-01

Background: The Sierra Nevada del Cocuy-Güicán in the Colombian Andes is protected as a National Natural Park since 1977 because of its fragile páramo ecosystems, extraordinary biodiversity, high plant endemism, and function as water reservoir. The vegetation on this mountain is threatened by

Diversification of clearwing butterflies with the rise of the Andes.

Science.gov (United States)

De-Silva, Donna Lisa; Elias, Marianne; Willmott, Keith; Mallet, James; Day, Julia J

2016-01-01

Despite the greatest butterfly diversity on Earth occurring in the Neotropical Andes and Amazonia, there is still keen debate about the origins of this exceptional biota. A densely sampled calibrated phylogeny for a widespread butterfly subtribe, Oleriina (Nymphalidae: Ithomiini) was used to estimate the origin, colonization history and diversification of this species-rich group. Neotropics. Ancestral elevation and biogeographical ranges were reconstructed using data generated from detailed range maps and applying the dispersal-extinction-cladogenesis model using stratified palaeogeographical time slice matrices. The pattern of diversification through time was examined by comparing constant and variable rate models. We also tested the hypothesis that a change in elevation is associated with speciation. The Oleriina likely originated in the Andes in the Early to Middle Miocene and rapidly diversified to include four genera all of which also originated in the Andes. These clades, together with four species groups, experienced varying spatial and temporal patterns of diversification. An overall early burst and decreasing diversification rate is identified, and this pattern is reflected for most subclades. Changes in the palaeogeological landscape, particularly the prolonged uplift of the Andes, had a profound impact on the diversification of the subtribe. The Oleriina mostly remained within the Andes and vicariant speciation resulted in some instances. Dynamic dispersal occurred with the disappearance of geological barriers such as the Acre System and the subtribe exploited newly available habitats. Our results confirm the role of the Andean uplift in the evolution of Neotropical biodiversity.

Evaluacion del factor central y periferico en fatiga muscular

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Marcela E. Panizza

1983-09-01

Full Text Available Se estúdio la fatiga muscular en 13 sujetos normales; para ello, fueron sometidos a un esfuerzo sostenido durante 10 minutos previo y posterior, al cual se realizo la medición de la onda M máxima. Durante el esfuerzo y cada 2 minutos, se obtuvieron cuantificaciones de la frecuencia y duración de las ondas positivas y negativas del EMG. Los resultados, mostraron diferencias significativas de estos valores, en función del tiempo de esfuerzo realizado, mientras que las mediciones de la onda M máxima inicial y final, no fueron diferentes, todo lo cual lleva a jerarquizar el factor central como el más importante en el desarrollo de fatiga, bajo nuestras condiciones de estudio, que son además de sencilla aplicación clínica.

Metodología para la identificación de características académicas a tener en cuenta en un sistema de alertas tempranas para la prevención del abandono

OpenAIRE

Gómez Sarmiento, Juliana; Ochoa, Antonio

2016-01-01

En este trabajo se diseñó y desarrolló una metodología para la identificación de características académicas que hacen parte del sistema de alertas tempranas para la prevención del abandono que se está construyendo en la Universidad de los Andes. Aunque la tasa de abandono de estudiantes de pregrado de la Universidad de los Andes es más baja que la de Colombia, existe una preocupación y un interés por prevenir y reducir este fenómeno. De acuerdo con cifras del Sistema para la Prevención de la ...

Parasitosis y Micosis del Sistema Central como Causa de Epilepsia en Adultos

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Alejandro Jiménez Arango

1987-12-01

Full Text Available

Nos corresponde hoy tratar el tema de las micosis y parasitosis del sistema nervioso central en relación con uno de los múltiples síntomas o complejos sindromáticos que pueden ocasionar: la epilepsia, se trata de uno de los síntomas más frecuentes en estas enfermedades y, en general, en las enfermedades encefálicas, y es el resultado de múltiples procesos fisiopatológicos que se producen en el cerebro. Puede la epilepsia ser síntoma de una enfermedad aguda o subaguda, o puede ser una de las secuelas, y a veces la única, de una enfermedad cuyo proceso activo ya ha terminado.

Con el objeto de buscar cierta coherencia en la presentación del tema, mencionaremos en primer lugar los procesos patológicos, síndromes y lesiones, varios de ellos comunes a muchas micosis y parasitosis, que pueden dar lugar al cuadro epiléptico. En seguida nos referiremos con mayor detalle a cuatro enfermedades o grupos de enfermedades que tienen particular importancia entre nosotros desde el punto de vista clínico y epidemiológico: las micosis, la toxoplasmosis del adulto, el paludismo cerebral y la cisticercosis.

Como ha sido ampliamente expuesto, las micosis y parasitosis del sistema nervioso central comprenden un gran número de entidades...

Caracterización de gneises glandulares del alto valle del Lozoya (Sistema Central Español) en base al quimismo de las biotitas y estado estructural del feldespato potásico

OpenAIRE

Tornos Arroyo, Fernando; Casquet, César

1982-01-01

En el presente trabajo se estudian las litologías gneísicas glandulares que afloran en la ladera este del Macizo de Peñalara (Sistema Central Español), en base a la interpretación del quimismo de las biotitas de glándulas y mesostasia y del estado estructural del feldespato potásico que forma la mayoría de estas glándulas. Se deduce a partir del estudio de las biotitas, que las glándulas se comportan como sistema cerrado para el Ti y abierto para el Al durante el metamorf...

Resilience and adaptations of rural communities and agricultural land use in the tropical Andes: Coping with environmental and socio-economic changes

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Stadel, Ch.

2008-12-01

Full Text Available In spite of a long settlement history of the tropical Andes, rural farming communities have always been exposed to conditions of ecological and economic vulnerability, risks, and even disasters. This has resulted, at certain times and in some regions, to a destabilization of livelihoods and to a manifestation of various forms of marginalization, to poverty or outmigration. However, Andean communities , over a long time, have given admirable testimonies of resilience and adaptations in the face of adverse conditions or new challenges. This paper examines the potentials and different facets of resilience and adaptation strategies of the rural campesinado in the tropical Andes. It emphasizes the proven traditional concepts of verticality, complementarity, reciprocity, and mutual community support, which to date support the feasibility and sustainability of Andean farming and community survival. In spite of this recognition, it is argued that Andean rural livelihoods always had to adapt to new developments, to threats and challenges, as well as to opportunities and alternative potentials. In the face of an almost ubiquitous penetration of modernization, new technologies, and economic and cultural globalization, the fundamental question arises, whether this can be considered as a path to progress and development, or as a threat to the survival of small-scale farming and rural community living. The paper concludes by formulating, albeit in a tentative form, some general suggestions for ‘development’ approaches and for research priorities in the rural Andes.

A pesar de una tradición muy extensa del asentamiento humano en los Andes tropicales, las comunidades campesinas siempre enfrentaron condiciones de vulnerabilidad ecológica y económica, con varios riesgos, y aun desastres. Eso ha resultado, en diversos tiempos y en algunas regiones, en una estabilización de la superviviencia humana y en varias manifestaciones de marginalización, de

The role of biomass in a pilot town of Venezuelan Andes

Energy Technology Data Exchange (ETDEWEB)

Padilla, A.; Sanchez, R.; Briceno, L.; Urbina, E. [Universidad de los Andes, Lab. de Bioenergia, Merida (Venezuela)

1999-01-01

This work analyses some factors of the energy crisis in a town of Venezuelan Andes (Llano del Hato, 3500 m.a.s.l.). The socioeconomics and climatic conditions in this region make the use of firewood as fuel mandatory. There are extensive desertified areas due to the extraction of plant species for firewood. It has been determined that there are diverse species in the area whose energy potential is superior to that reported in the literature, however, they are incorrectly used and are in danger of extinction. The absence of firewood drives peasants to use manure as a source of fuel. Parallel to the laboratory testing of different raw materials, a program of environmental education and optimisation of biomass to obtain energy is under way. It is hoped that pilot plans like this will expand to all of the Andean region. (Author)

PABLO PALACIO: LA VIOLENCIA CORPORAL SOBRE LAS IDENTIDADES IMPOSIBLES EN LA ZONA DE LOS ANDES

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Diego Falconí Travez

2014-10-01

Full Text Available Pablo Palacio, escritor ecuatoriano de la segunda década del siglo pasado, se encargó de construir en sus relatos un catálogo de cuerpos raros con sexualidades ambiguas e inquietantes que se alejan del canon andino al que él pertenece. No obstante, una de las cuestiones que más llama la atención es que varios de esos cuerpos son disciplinados por ciertos discursos de poder de un modo violento. Este trabajo explora desde la teoría literaria dichas vejaciones tomando en consideración la violencia sobre las identidades de mujeres y homosexuales en dos de sus relatos, e indaga sobre cuestiones como la economía de la representación, la  violencia, su relación con el texto literario y la vulnerabilidad, como requisito sine qua non de las vejaciones, en ciertos cuerpos en la zona de los Andes.

PROFUNDIZACIÓN DEL TOPE DE PERMAFROST Y TENDENCIAS EN LA DINÁMICA CRIOGÉNICA, A PARTIR DE 1989, EN EL GLACIAR DE ESCOMBROS COMPUESTO DEL VALLE DE MORENAS COLORADAS, MENDOZA, ARGENTINA.

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Darío Trombotto Liaudat

2007-12-01

Full Text Available Los glaciares de escombros (rockglaciers son las geoformas periglaciales con permafrost reptante más típicas e importantes, por su volumen en criosedimentos congelados y hielo, de los Andes Centrales. La presente contribución muestra ejemplos de la marcha de las temperaturas y la profundización del tope de permafrost en dos puntos de monitoreo (Balcón I y II del glaciar de escombros compuesto de Morenas Coloradas, Cordillera Frontal, en la provincia de Mendoza, Argentina. El engrosamiento de la capa activa en la lengua terminal, o límite inferior del creeping permafrost en este valle, de 4,9 m a 7,5 / 7,8 m en los últimos años, así como la tendencia de la dinámica criogénica desde 1992, y la geomorfología (termokarst inactivos en los frentes, expresan el fenómeno de calentamiento que se está detectando también en otros lugares del mundo. Estas variaciones térmicas sugieren cambios en la estructura interna de estas mesoformas. Asimismo, como otra situación geofísica paralela, el cálculo de difusividad térmica en Balcon II ( ̃ = 0.14 × 10-6 m2/s; Trombotto y Borzotta, 2007, a 3770 m de altura, permite correlacionar el bajo valor obtenido con una mejor y más larga conservación del hielo por debajo de los criorregolitos que son en este caso, principalmente, de origen volcánico. Los cambios térmicos detectados en esta zona piloto tendrían una consecuencia directa en el ambiente criogénico local y son un ejemplo para la situación regional del permafrost andino de los glaciares de escombros. Las variaciones descriptas se expresan a través de la profundización del tope de permafrost, formación de termokarst y reactivación de los más antiguos a lo largo del valle, y pérdida de movimiento, o de la criodinámica, en los taludes frontales (“narices” en la parte inferior y de menor altura de las geoformas investigadas. El trabajo promueve también a colocar mayor atención en la posible influencia que pueden tener estos

Evaluacion del componente central y periferico de fatiga muscular en pacientes neuropaticos y miopaticos

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L. G. Cohen

1983-09-01

Full Text Available Utilizando un método de cuantificación del electromiograma, se investigaron parte de los mecanismos centrales y periféricos responsables de la fatiga muscular en enfermos crónicamente denervados y en pacientes con compromiso muscular primitivo. Se observó en los denervados que los mecanismos de fatiga muscular, no difieren mayormente de los observados en el grupo de sujetos sanos, por el contrario, en los miopáticos a más del componente central, existen otros de orden periférico, tales como la pérdida de unidades motoras funcionantes durante el esfuerzo y el bloqueo temporario de la transmisión neuromuscular, que contribuye al desarrollo de la fatiga.

Sr and Nd isotopic and trace element compositions of Quaternary volcanic centers of the Southern Andes

Science.gov (United States)

Futa, K.; Stern, C.R.

1988-01-01

Isotopic compositions of samples from six Quaternary volcanoes located in the northern and southern extremities of the Southern Volcanic Zone (SVZ, 33-46??S) of the Andes and from four centers in the Austral Volcanic Zone (AVZ, 49-54??S) range for 87Sr 86Sr from 0.70280 to 0.70591 and for 143Nd 144Nd from 0.51314 to 0.51255. The ranges are significantly greater than previously reported from the southern Andes but are different from the isotopic compositions of volcanoes in the central and northern Andes. Basalts and basaltic andesites from three centers just north of the Chile Rise-Trench triple junction have 87Sr 86Sr, 143Nd 144Nd, La Yb, Ba La, and Hf Lu that lie within the relatively restricted ranges of the basic magmas erupted from the volcanic centers as far north as 35??S in the SVZ of the Andes. The trace element and Sr and Nd isotopic characteristics of these magmas may be explained by source region contamination of subarc asthenosphere, with contaminants derived from subducted pelagic sediments and seawater-altered basalts by dehydration of subducted oceanic lithosphere. In the northern extremity of the SVZ between 33?? and 34??S, basaltic andesites and andesites have higher 87Sr 86Sr, Rb Cs, and Hf Lu, and lower 143Nd 144Nd than basalts and basaltic andesites erupted farther south in the SVZ, which suggests involvement of components derived from the continental crust. In the AVZ, the most primitive sample, high-Mg andesite from the southernmost volcanic center in the Andes (54??S) has Sr and Nd isotopic compositions and K Rb and Ba La similar to MORB. The high La Yb of this sample suggests formation by small degrees of partial melting of subducted MORB with garnet as a residue. Samples from centers farther north in the AVZ show a regionally regular northward increase in SiO2, K2O, Rb, Ba, Ba La, and 87Sr 86Sr and decrease in MgO, Sr, K Rb, Rb Cs, and 143Nd 144Nd, suggesting increasingly greater degrees of fractional crystallization and associated intra

A new species of Telmatobius (Amphibia, Anura, Telmatobiidae from the Pacific slopes of the Andes, Peru

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Alessandro Catenazzi

2015-02-01

Full Text Available We describe a new species of Telmatobius from the Pacific slopes of the Andes in central Peru. Specimens were collected at 3900 m elevation near Huaytará, Huancavelica, in the upper drainage of the Pisco river. The new species has a snout–vent length of 52.5 ± 1.1 mm (49.3–55.7 mm, n = 6 in adult females, and 48.5 mm in the single adult male. The new species has bright yellow and orange coloration ventrally and is readily distinguished from all other central Peruvian Andean species of Telmatobius but T. intermedius by having vomerine teeth but lacking premaxillary and maxillary teeth, and by its slender body shape and long legs. The new species differs from T. intermedius by its larger size, flatter head, and the absence of cutaneous keratinized spicules (present even in immature females of T. intermedius, and in males by the presence of minute, densely packed nuptial spines on dorsal and medial surfaces of thumbs (large, sparsely packed nuptial spines in T. intermedius. The hyper-arid coastal valleys of Peru generally support low species richness, particularly for groups such as aquatic breeding amphibians. The discovery of a new species in this environment, and along a major highway crossing the Andes, shows that much remains to be done to document amphibian diversity in Peru.

El Picotudo o Taladrador del Platáno y del Abaca

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Gallego M. F. Luis

1956-12-01

Full Text Available El cultivo del plátano en el país, relativamente ha tenido pocos enemigos, pero desde hace algún tiempo, el producto se va haciendo más y más escaso y al mismo tiempo de mala clase, debido, fuera de otras causas, él la presencia en los campos de varios insectos, entre los cuales se encuentra el Cosmopolites. Entre nosotros suponemos pueda encontrarse desde hace muchos años pero solamente apenas en el año 1947 tuvimos la ocasión de obervarlo con características de daño en el occidente antioqueño desde Villa Arteaga hasta San Jerónimo y Ebéjico y en la región del Suroeste desde Angelópolis hasta Támesis, Valparaíso y Salgar de un lado, y Andes, Betania y Bolívar del otro; es de suponer que el insecto pueda encontrarse en otras secciones del país en donde los cultivos de plátano se encuentran bastante generalizados, pero carecemos de toda información sobre el particular.

Litterfall production under pine plantations in the southern Andes region of Ecuador

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Pablo Quichimbo

2016-09-01

Full Text Available Litterfall research is an interesting aspect in environmental studies due to its significance in nutrient cycling specially in regions like the Andes where the interactions between biomass production and its decomposition is poorly understood. This study is focusing in the litterfall biomass production under pine plantations in southern Ecuador. The litterfall production was studied for five months at two-week intervals in three pine forest sites located in the southern Andes region of Ecuador. Monthly litterfall production ranged between 1067-1907 kg ha-1, in comparison with other coniferous stands around the world, this study revealed a higher litterfall production for tropical areas and particularly the highest production under pine plantations in the Andes region. This high litterfall production highlights the upmost importance of this forest component as a potential nutrient reservoir involved in the global nutrient cycling under landscapes dominated by this exotic forest specie in the tropical Andes.

Centrales hidroeléctricas del Zemm – Austria

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Schmidt, W.

1972-11-01

Full Text Available In order to accommodate an increasing rate, doubled every ten years, of current consumption in this country, two hydroelectric power plants were constructed in the Zemm River. This type of power plant has the advantage of being able to produce energy at the time of consumption so as to be to handle peak energy production; while the normal power load requirement is covered by nuclear, petroleum and gas, and river power plants. These two plants have 517.500 kW, with a total annual yield of 648 GWh, or 778 GWh with pumping equipment. The gravity dam of the upper reservoir is 131 m high and 725 m long at the top. 960,000 m3 of concrete were used in its construction and it has an annual storage capacity of 127.4 millions m3. The earthen dam of the lower reservoir, which required 820,000 m3 to build, is about 28 m high and 480 m wide at the crown, with a capacity of 6,4 millions m3.Para poder hacer frente al aumento de consumo de corriente en el país, que se duplica cada 10 años, se construyeron dos centrales hidroeléctricas en el río Zemm. Este tipo de centrales tienen la ventaja de poder producir la energía en el mismo momento del consumo, por lo que se les confía la producción de energía de punta; mientras que la demanda de carga normal es cubierta por centrales de: energía nuclear; de petróleo y gas, y fluviales. Estas dos centrales tienen una potencia de 517.500 kW, con un rendimiento anual total de 648 GWh, ampliable en 130 GWh con el equipo de bombeo. La presa del embalse superior es de tipo gravedad, con 131 m de altura y una longitud de coronación de 725 m. Se emplearon 960.000 m3 de hormigón en su construcción. Tiene una capacidad de embalse anual de 127,4 millones de m3 En el embalse inferior, la presa es de tierra y se necesitaron 820.000 m3 para su construcción. Tiene una altura de unos 28 m, y una longitud de coronación de 480 m. Su capacidad es de 6,4 millones de m3.

Las concepciones centrales del liberalismo y del socialismo sobre la nación en Europa: 1850-1914

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Martha Lucía Quiroga Riviere

2015-07-01

Full Text Available El artículo presenta desde la historia del pensamiento político las reflexiones centrales alrededor del tema de la nación en Europa de las dos corrientes de pensamiento más importantes de la segunda mitad de siglo XIX, el liberalismo y el socialismo. Desde mediados del siglo las cuestiones de la nación aparecieron para estas dos corrientes como un problema complejo y difícil. Dentro de su contexto político y a través de literatura secundaria, pero sobre todo del estudio de los textos de los mismos autores, se exponen, desde el liberalismo, las reflexiones en su debate sobre la “nacionalidad” y el “principio de las nacionalidades” de Lord ACTON, así como la concepción de nación de Renán; y, desde el socialismo, los aportes alrededor de “la cuestión nacional” en Polonia e Irlanda de MARX y ENGELS, para luego entrar a exponer las expresiones más decantadas y sistemáticas sobre el concepto de nación poco antes de la Primera Guerra Mundial del liberal conservador FRIEDRICH MEINECKE y del austromarxista OTTO BAUER. El texto muestra una problemática que lleva muchas décadas y unos presupuestos teóricos que, desarrollados en su tiempo, aún hoy juegan un papel en la teoría y la práctica alrededor del problema de la nación. Por esto, al final el artículo evalúa de manera sintética la resonancia de dicho legado.

Charles Darwin in the Andes

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Bizzo, Nelio; Bizzo, Luis Eduardo Maestrelli

2006-01-01

Considering geological time as an important epistemological obstacle to the construction of ideas on biological evolution, a study was carried out on the so-called "Darwin Papers". The conclusion was that Charles Darwin's excursion in the Andes during March-April 1835 was a crucial step in this regard. An expedition was carried out in…

Influence of inherited structures on the growth of basement-cored ranges, basin inversion and foreland basin development in the Central Andes, from apatite fission-track and apatite Helium thermochronology.

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Zapata, S.; Sobel, E. R.; Del Papa, C.; Jelinek, A. R.; Muruaga, C.

2017-12-01

The Central Andes in NW of Argentina is part of a long-lived subduction zone, active since the Paleozoic. This region experienced several tectonic cycles; each of which created an unique set of structures and may have reactivated preexisting structures. These inherited structures may exert a first-order control over the different foreland deformational styles observed along the strike in the Central Andes. Our study area is located between 26°S and 28°S on the transition between the broken foreland (Santa Barbara system), which expresses a combination of thin-skin and thick-skin styles, and the Sierras Pampeanas, which is deform in a thick-skin style. The Cumbres Calchaquies range and the associated Choromoro Basin are located in the northern part of the study area, and are the southern expression of the Santa Barbara system. Published thermochronology data suggest that the rocks from the basement experienced Late Cretaceous and Late Miocene exhumation; the associated sedimentary rocks within the Choromoro basin experienced Paleogene and Late Miocene deformational phases. In contrast, the Sierra Aconquija range, located immediately south on the transition to the Sierras Pampeanas (thick skin) foreland basin, exhibit larger amounts of Miocene exhumation and lack of Cretaceous exhumation; the associated sedimentary rocks from the Tucuman basin have not been deformed since the Cretaceous. Our goal is to understand the evolution of the structural blocks and the structures responsible for the along strike changes in foreland basin deformational styles and their relation with inherited structures from previous tectonic cycles. We are obtaining new apatite U-Th/He and fission track data to reconstruct the thermal history of the basement, accompanied by U-Pb geochronology and stratigraphy to constrain the evolution of the associated sedimentary basins. Preliminary results combined with published data suggest that inherited structures within the study area have evolved

Les régimes thermiques et pluviométriques de Pachachaca (Andes Centrales du Pérou: contribution à la connaissance des rythmes saisonniers dans le climat de la Puna

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1983-01-01

Full Text Available A partir des données thermiques et pluviométriques fournies par la station de Pachachaca, on tente de définir les rythmes saisonniers du climat de la Puna vers 4000 m. d'altitude. Trois saisons s'individualisent nettement: une saison sèche de 4 mois, une saison de début des précipitations de septembre à décembre, et les mois très pluvieux (janvier à mars. La variabilité des températures tout au long de la série trentenaire, est due principalement à celle des minima une tendance au réchauffement des minima s'est dessinée récemment depuis les années 1965. La dispersion des totaux pluviométriques est forte depuis 1943 et des changements tendanciels peuvent intervenir la saison sèche est toujours très marquée relativement, par contre la saison humide peut connaître de fortes fluctuations, au niveau des totaux accumulés, mais aussi de la répartition mensuelle des précipitations: une tendance récente a vu l'accroissement sensible des chutes de début de saison humide, au détriment de celles du maximum des pluies. On s'interroge sur l'extension possible de ces remarques à l'ensemble des hautes Andes du Pérou. A partir de los datos térmicos y pluviométricos dados por la estación de Pachachaca, se trata de determinar los ritmos estacionales del clima de la Puna cerca de los 4000 metros s.n.m. Tres períodos se destacan de una manera clara: uno seco de cuatro meses, uno de principio de precipitaciones desde setiembre hasta diciembre, y finalmente los meses con mucha lluvia (enero-marzo. La variabilidad de las temperaturas durante toda la serie de treinta años es principalmente la consecuencia de las mínimas una tendencia al recalentamiento de las mínimas se ha destacado recientemente, desde los años 1965. La dispersión de los totales pluviométricos es fuerte desde 1943 (año de inicio de la serie y algunos cambios de tendencia pueden ocurrir la temporada seca es siempre relativamente muy marcada, pero al contrario la

Is tourism damaging ecosystems in the Andes? Current knowledge and an agenda for future research.

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Barros, Agustina; Monz, Christopher; Pickering, Catherine

2015-03-01

Despite the popularity of tourism and recreation in the Andes in South America and the regions conservation value, there is limited research on the ecological impacts of these types of anthropogenic use. Using a systematic quantitative literature review method, we found 47 recreation ecology studies from the Andes, 25 of which used an experimental design. Most of these were from the Southern Andes in Argentina (13 studies) or Chile (eight studies) with only four studies from the Northern Andes. These studies documented a range of impacts on vegetation, birds and mammals; including changes in plant species richness, composition and vegetation cover and the tolerance of wildlife of visitor use. There was little research on the impacts of visitors on soils and aquatic systems and for some ecoregions in the Andes. We identify research priorities across the region that will enhance management strategies to minimise visitor impacts in Andean ecosystems.

Neogene paleoelevation of intermontane basins in a narrow, compressional mountain range, southern Central Andes of Argentina

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Hoke, Gregory D.; Giambiagi, Laura B.; Garzione, Carmala N.; Mahoney, J. Brian; Strecker, Manfred R.

2014-11-01

The topographic growth of mountain ranges at convergent margins results from the complex interaction between the motion of lithospheric plates, crustal shortening, rock uplift and exhumation. Constraints on the timing and magnitude of elevation change gleaned from isotopic archives preserved in sedimentary sequences provide insight into how these processes interact over different timescales to create topography and potentially decipher the impact of topography on atmospheric circulation and superposed exhumation. This study uses stable isotope data from pedogenic carbonates collected from seven different stratigraphic sections spanning different tectonic and topographic positions in the range today, to examine the middle to late Miocene history of elevation change in the central Andes thrust belt, which is located immediately to the south of the Altiplano-Puna Plateau, the world's second largest orogenic plateau. Paleoelevations are calculated using previously published local isotope-elevation gradients observed in modern rainfall and carbonate-formation temperatures determined from clumped isotope studies in modern soils. Calculated Neogene basin paleoelevations are between 1 km and 1.9 km for basins that today are located between 1500 and 3400 m elevation. Considering the modern elevation and δ18O values of precipitation at the sampling sites, three of the intermontane basins experienced surface uplift between the end of deposition during the late Miocene and present. The timing of elevation change cannot be linked to any documented episodes of large-magnitude crustal shortening. Paradoxically, the maximum inferred surface uplift in the core of the range is greatest where the crust is thinnest. The spatial pattern of surface uplift is best explained by eastward migration of a crustal root via ductile deformation in the lower crust and is not related to flat-slab subduction.

Les flux de matières dissoutes et particulaires des Andes de Bolivie vers le rio Madeira en Amazonie brésilienne

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1995-01-01

Full Text Available Le Rio Madeira est le principal affluent méridional de l’Amazone et le deuxième tributaire andin du bassin. L’utilisation des données obtenues en Bolivie par le PHICAB (1, et au Brésil sur le réseau du DNAEE (2, a permis de suivre l’évolution des flux de matières dissoutes et particulaires, depuis les Andes jusqu’à l’Amazone. Les flux de matières en solution [36 106 t an-1 à Villabella (3] augmentent progressivement d’amont en aval avec les débits. Les flux de matières en suspension diminuent du piedmont andin jusqu’à Villabella (258 106 t an-1 du fait d’une forte sédimentation. Ensuite, les différences notables observées au Brésil posent clairement le problème des modes d’échantillonnage et de calcul des flux sédimentaires. LOS FLUJOS DE MATERIA DISUELTA Y PARTICULAR DESDE LOS ANDES DE BOLIVIA HASTA EL RÍO MADEIRA EN EL AMAZONAS DE BRASIL. El río Madeira es el principal afluente meridional del Amazonas, y el segundo tributario andino de la cuenca. La utilización de los datos obtenidos en Bolivia por el PHICAB (1, y en el Brasil sobre la red del DNAEE (2 permite conocer la evolución de los flujos de materia disuelta y particular, desde los Andes hasta el Amazonas. Los aportes en materia disuelta [36 106 t año-1 en Villabella (3] aumentan progresivamente de aguas arriba para aguas abajo, con el caudal. Los flujos de materias en suspensión disminuyen desde el Piedemonte hasta Villabella (258 106 t año-1 por causa de una fuerte sedimentación. Después, las diferencias notables observadas en el Brasil colocan claramente el problema de los tipos de muestreo y de cálculo de los flujos de sedimentos. THE DISSOLVED AND SEDIMENT YIELDS FROM THE ANDES OF BOLIVIA TO THE MADEIRA RIVER IN THE BRAZILIAN AMAZON. The Madeira river is the main Southern tributary of the Amazon, and the second Andean tributary of the drainage basin. The use of Bolivian data from the PHICAB (1, and Brazilian data from the DNAEE (2, allow to

Effects of diet and water supply on energy intake and water loss in a mygalomorph spider in a fluctuating environment of the central Andes.

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Canals, M; Figueroa, D; Alfaro, C; Kawamoto, T; Torres-Contreras, H; Sabat, P; Veloso, C

2011-11-01

The metabolic and water evaporation strategies in spiders may be part of a set of physiological adaptations to tolerate low or unpredictable food availability, buffering spiders against environmental fluctuations such as those of the high mountains of the central Andes. The aim of this study is to analyze experimentally the variations in metabolic rate and the rate of evaporative water with food and/or water restriction in a high mountain mygalomorph spider population (Paraphysa sp.). We found that the low metabolism of this spider was not affected by water restriction, but its metabolism was depressed after 3 weeks of food deprivation. The spider did not show seasonal metabolic changes but it presented seasonal changes in the rate of evaporative water loss at high temperatures. Females with egg sacs reduced their metabolic rate and evaporative water at high temperatures. These findings constitute a set of possible adaptations to a highly fluctuating Mediterranean environment, which is completely covered with snow for many months and then progresses rapidly to a very dry climate with high temperatures. Copyright © 2011 Elsevier Ltd. All rights reserved.

Multiproxy Holocene paleoclimate records from the southern Peruvian Andes - what new can we learn from the stable carbon isotope composition of high altitude organic matter deposits?

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Skrzypek, Grzegorz; Engel, Zbyněk

2015-04-01

Interpretation of the Central Andean paleoclimate over the last millennia still represents a research challenge demanding deeper studies [1,2]. Several high-resolution paleoclimate proxies for the last 10,000 years have been developed for the northern hemisphere. However, similar proxies are very limited for South America, particularly for high altitudes where, for example, tree-ring chronologies are not available and instrumental records are very limited. Consequently, our knowledge of high altitude climate changes in arid regions of the Peruvian Andes mainly relies on ice-core and lake deposit studies. In our study, we used a new alternative proxy for interpretation of palaeoclimate conditions based on a peat core taken from the Carhuasanta Valley at the foot of Nevado Mismi in the southern Peruvian Andes (15° 30'S, 71° 43'W, 4809m a.s.l.). The stable carbon isotope composition (δ13C) of Distichia peat reflects mainly the relative variation of the mean air temperature during subsequent growing seasons [3], and allows reconstructions of palaeotemperature changes. In contrast, peat organic carbon concentration (C % wt) records mainly wetness in the valley, directly corresponding to the changes in runoff in the upper part of the catchment. The most prominent climate changes recorded in the peat over last 4ka occurred between 3040 and 2750 cal. yrs BP. The initial warming turned to a very rapid cooling to temperatures at least 2° C lower than the mean for the Late Holocene. Initially drier conditions within this event turned to a short wet phase after 2780 cal. yrs BP, when the temperature increased again. This event coincides with significant changes in peat and ice core records in the Central Andes that match the timing of the global climate event around 2.8 cal. ka BP. Climatic conditions in the study area became relatively dry and stable after the event for about 800 years. Highly variable temperatures and humidity prevailed during the last 2000 years, when

Early Tertiary Exhumation, Erosion, and Sedimentation in the Central Andes, NW Argentina

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Carrapa, B.; Decelles, P. G.; Gerhels, G.; Mortimer, E.; Strecker, M. R.

2006-12-01

Timing of deformation and resulting sedimentation patterns in the Altiplano-Puna Plateau-Eastern Cordillera of the southern Central Andes are the subject of ongoing controversial debate. In the Bolivian Altiplano, sedimentation into a foreland basin system commenced during the Paleocene. Farther south in the Puna and Eastern Cordillera of NW Argentina, a lack of data has precluded a similar interpretation. Early Tertiary non-marine sedimentary rocks are preserved within the present day Puna Plateau and Eastern Cordillera of NW Argentina. The Salar de Pastos Grandes basin in the Puna Plateau contains more than 2 km of Eocene alluvial and fluvial strata in the Geste Formation, deposited in close proximity to orogenic source terrains. Sandstone and conglomerate petrographic data document Ordovician quartzites and minor phyllites and schists as the main source rocks. Detrital zircon U-Pb ages from both the Geste Formation and from underlying Ordovician quartzite cluster in the 900-1200 Ma (Grenville) and late Precambrian-Cambrian (Panafrican) ranges. Sparse late Eocene (~37-34 Ma) grains are also present; their large size, euhedral shape, and decreasing mean ages upsection suggest that these grains are volcanogenic (i.e. ash fall contamination), derived from an inferred magmatic arc to the west. The Eocene ages corroborate mammalian paleontological dates, defining the approximate begin of deposition of the Geste Formation. Alternatively, these young zircons could be of plutonic origin; however, no Eocene plutons are present in the surrounding source rocks and this interpretation is not likely. From W to E, fluvial rocks of the Quebrada de los Colorados Formation show similar sedimentological features as those observed for the Geste Formation, suggesting a genetic link between the two. Detrital zircon U-Pb data show mainly Panafrican ages, with sparse ages in the 860-935 Ma range and a few mid-Proterozoic ages. More importantly, a significant number of late Eocene

Surnames and genetic structure of a high-altitude Quechua community from the Ichu River Valley, Peruvian Central Andes, 1825-1914.

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Pettener, D; Pastor, S; Tarazona-Santos, E

1998-10-01

Changes in isolation, inbreeding, population subdivision, and isonymous relationships are examined in six Quechua communities from the upper valley of the Ichu River in the Peruvian Central Andes (3700 m). All marriages registered between 1825 and 1914 in the Parish of Santa Ana were analyzed. The data (1680 marriages) were divided into 2 periods (1825-1870 and 1871-1914) and into the 6 villages that constitute the parish. Endogamy rates are between 81% and 100%, indicating high levels of reproductive isolation. The inbreeding indicated by isonymy (Ft, Fr, and Fn) is lower than in other mountain populations studied. Isonymy values, calculated from the different surname combinations made possible by the Ibero-American Surnames System, indicate a strong rejection of consanguineous marriages, particularly between patrilineal relatives, in agreement with the parental structure typical of Andean populations. The comparison between observed and expected repeated-pair values reveals a moderate level of subdivision within populations, which could be related to cultural and socioeconomic factors. Nonmetric multidimensional scaling was used to investigate temporal changes in the isonymous relationships among the communities. The results reveal a decrease in the interpopulational variability measured by surnames, in agreement with an increase in exogamy. Surnames and data contained in historical and demographic records yield reliable information, and they can be used to reconstruct the biological history of Amerindian populations over the last few centuries.

Preliminary Depositional and Provenance Records of Mesozoic Basin Evolution and Cenozoic Shortening in the High Andes, La Ramada Fold-Thrust Belt, Southern-Central Andes (32-33°S)

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Mackaman-Lofland, C.; Horton, B. K.; Fuentes, F.; Constenius, K. N.; McKenzie, R.; Alvarado, P. M.

2015-12-01

The Argentinian Andes define key examples of retroarc shortening and basin evolution above a zone of active subduction. The La Ramada fold-thrust belt (RFTB) in the High Andes provides insights into the relative influence and temporal records of diverse convergent margin processes (e.g. flat-slab subduction, convergent wedge dynamics, structural inversion). The RFTB contains Mesozoic extensional basin strata deformed by later Andean shortening. New detrital zircon U-Pb analyses of Mesozoic rift sediments reveal: (1) a dominant Permo-Triassic age signature (220-280 Ma) associated with proximal sources of effective basement (Choiyoi Group) during Triassic synrift deposition; (2) upsection younging of maximum depositional ages from Late Triassic through Early Cretaceous (230 to 100 Ma) with the increasing influence of western Andean arc sources; and (3) a significant Late Cretaceous influx of Paleozoic (~350-550 Ma) and Proterozoic (~650-1300 Ma) populations during the earliest shift from back-arc post-extensional subsidence to upper-plate shortening. The Cenozoic detrital record of the Manantiales foreland basin (between the Frontal Cordillera and Precordillera) records RFTB deformation prior to flat-slab subduction. A Permo-Triassic Choiyoi age signature dominates the Miocene succession, consistent with sources in the proximal Espinacito range. Subordinate Mesozoic (~80-250 Ma) to Proterozoic (~850-1800 Ma) U-Pb populations record exhumation of the Andean magmatic arc and recycling of different structural levels in the RFTB during thrusting/inversion of Mesozoic rift basin strata and subjacent Paleozoic units. Whereas maximum depositional ages of sampled Manantiales units cluster at 18-20 Ma, the Estancia Uspallata basin (~50 km to the south) shows consistent upsection younging of Cenozoic populations attributed to proximal volcanic centers. Ongoing work will apply low-temperature thermochronology to pinpoint basin accumulation histories and thrust timing.

Histoplasmosis del sistema nervioso central en un paciente inmunocompetente

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Natalia Osorio

2014-12-01

Full Text Available La histoplasmosis es una afección polifacética producida por el hongo dimorfo Histoplasma capsulatum, cuyas esporas son inhaladas y llegan al pulmón, órgano primario de infección. La forma meníngea, considerada como una de las manifestaciones más graves de esta micosis, suele presentarse en individuos con alteraciones en la inmunidad celular: pacientes con síndrome de inmunodeficiencia humana adquirida, con lupus eritematoso sistémico o con trasplante de órgano sólido, así como en lactantes, debido a su inmadurez inmunológica. La forma de presentación más usual es de resolución espontánea y se observa en individuos inmunocompetentes que se han expuesto a altas concentraciones de conidias y fragmentos miceliares del hongo. En estas personas, la afección se manifiesta por trastornos pulmonares y por la posterior diseminación a otros órganos y sistemas. Se presenta un caso de histoplasmosis del sistema nervioso central en un niño inmunocompetente.

Late Pleistocene to Holocene tephrostratigraphy of the Lonquimay Volcano, South Central Chile

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Gilbert, D.; Freundt, A.; Kutterolf, S.; Burkert, C.

2010-12-01

The Lonquimay Volcanic Complex (LVC) in South Central Chile (38.38°S, 71.58°W) is part of the Southern Volcanic Zone of the Andes, which formed in response to the subduction of the Nazca Plate beneath the South American Plate. During the course of its magmatic evolution, the LVC produced explosive eruptions documented in the succession of widespread tephra deposits, as well as large lava flows that originated from the main edifice and several adjacent minor eruptive centers. The last eruptive phase in Lonquimays volcanic evolution occurred from 1988-1990. It led to the formation of the Navidad cinder cone with its associated 10.2 km long lava flow, and a widely distributed tephra blanket of andesitic composition (Moreno and Gardeweg, 1989). During recent field work we reinvestigated and complemented the LVC tephrostratigraphy as originally established by Polanco (1998)by detailed logging of 22 outcrops and collecting 126 stratigraphically controlled samples that were analyzed for their matrix glass, mineral and bulk rock compositions. This data set allows us to verify and extend the field-based correlations, and to establish a tephrostratigraphy for the LVC that comprises 15 stratigraphic units (LQA-LQO) and provides a framework for ongoing investigations of the petrogenetic evolution of the LVC. The stratigraphic record identifies at least 13 explosive eruptions of VEI > 3 that occurred since the last glaciation period (17150 a BP, McCulloch et al. 2000). Magmatic compositions of the tephra deposits range from basaltic scoriae (51wt% SiO2) to evolved dacitic pumice lapilli layers (67wt% SiO2), and thus have a wider compositional range than the chemically distinct andesitic lavas (57-63wt%) of the LVC. The vertical succession of tephra compositions reflects four periods of progressive magmatic differentiation, each successively tapped by several eruptions. The maximum degree of fractionation reached during these periods increases to younger ages. The

Los repositorios como herramienta para la recuperación del patrimonio bibliográfico: el caso de seis bibliotecas públicas municipales del departamento de Antioquia

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Wilson Castaño Muñoz

2016-01-01

Full Text Available El siguiente artículo tiene como objetivo principal evidenciar la importancia de implementar un repositorio digital en la investigaciones sobre la recuperación del patrimonio bibliográfico de seis bibliotecas públicas de los municipios de Andes, El Carmen de Viboral, Puerto Berrio, Sonsón, Turbo y Yarumal del departamento de Antioquia, Colombia. Se presenta brevemente el concepto de patrimonio-bibliográfico y se abordan los repositorios institucionales y digitales como categoría analítica y alternativa para la recuperación, organización y difusión de información patrimonial. The following article has as main objective to demonstrate the importance of implementing a digital repository in the research about the bibliographical patrimony recovery in six public libraries in municipalities located in the department of Antioquia, Colombia such as Andes, el Carmen de Viboral, Puerto Berrío, Sonsón, Turbo and Yarumal. The concept of bibliographical patrimony appears briefly in the article and the institutional and digital repositories are approached as an analytical and alternative category for the recovery, organization and dissemination of the patrimony information. .

Clima Organizacional y el Desempeño Laboral de los trabajadores de la Gerencia Central de Logística de la Sede Central del Ministerio Público – 2014

OpenAIRE

Arévalo Contreras, Niltón César; Arroyo Muñoz, Carol Liliana

2016-01-01

La presente investigación tuvo como objetivo general de determinar qué relación existe entre el Clima Organizacional y el Desempeño Laboral de los trabajadores de la Gerencia Central de Logística de la Sede Central del Ministerio Público – 2014, la población fue Constituida por 265 trabajadores del Ministerio Público, como muestra no probabilística por conveniencia se consideró a 114 trabajadores de la población, en los cuales se han empleado la variable: Clima Organizacional ...

Distribución y conservación de especies amenazadas en Mesoamérica, Chocó y Andes tropicales Distribution and conservation of endangered species in Mesoamerica, Chocó and Tropical Andes

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María Cecilia Londoño-Murcia

2011-09-01

Full Text Available En este estudio se modeló el nicho ecológico proyectado como distribución potencial de 313 especies amenazadas en Mesoamérica, Chocó y los Andes tropicales, según las listas de la UICN. De estas especies, 285 fueron plantas y 28 fueron vertebrados terrestres. La superposición de las distribuciones de las especies amenazadas cubrió prácticamente toda la región. Ecuador mostró cerca del 30% de su área con 50 especies. Colombia, Costa Rica, Guatemala, Nicaragua y Panamá mostraron > 50, aunque en 50% de su área. El Salvador y Honduras, de 11 a 20 en > 50% de su área y México de 1 a 5 especies en > 50% de su área. La distribución de estas especies en áreas transformadas (agricultura y áreas urbanas varió del 11al 30%; El Salvador, Panamá y Guatemala mostraron > 50% de la distribución; Colombia, Honduras y México This study modeled ecological niches projected as potential distributions for 313 endangered species listed in the IUCN for Mesoamerica, Chocó and Tropical Andes, of which 285 were plants, and 28 terrestrial vertebrates. Overlapping of endangered species distributions covered most of the region. Ecuador showed close to 30% of its area with 50 endangered species. Colombia, Costa Rica, Guatemala, Nicaragua y Panama showed more than 50 endangered species in 50% of its area with endangered species (21 to 50 species were Costa Rica, Ecuador, Nicaragua and Panama. El Salvador and Honduras showed > 50% of its area with 11 to 20 endangered species; Mexico showed 50% of endangered species in transformed areas; Colombia, Honduras and Mexico showed < 40%, and Belize and Ecuador showed < 25% of endangered species in transformed areas, respectively. El Salvador, Honduras, Panama, Nicaragua and Mexico showed a high proportion of endangered species in transformed areas for the Classes Amphibia, Liliopsida, Polipodiopsida, and the Orders Asterales, Fabales, Laurales, Myrtales, Scrophulariales and Rubiales. Less than 35% of endangered

Les effets de l’émigration paysanne dans les Andes équatoriennes : une lecture photographique

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Nasser Rebaï

2011-07-01

Full Text Available Dans les Andes équatoriennes, les effets de l’émigration paysanne sont partout visibles. Si dans la province de l’Azuay, on assiste à la diminution des superficies cultivées et à la réorganisation des tâches agricoles, on observe par ailleurs l’émergence d’une agriculture commerciale orientée vers le marché urbain régional. En procédant à la description de photographies prises à la campagne comme à la ville, nous chercherons à expliquer l’ensemble de ces mutations, avant de nous interroger plus largement sur l’avenir des exploitations familiales dans cette région.En los Andes ecuatorianos, los efectos de la migración campesina son visibles por todas partes. Si en la provincia del Azuay, se asiste a la disminución de las superficies cultivadas y a la reorganización de las tareas agrícolas, observamos por otro lado la emergencia de una agricultura comercial orientada hacia el mercado urbano regional. Procediendo a la descripción de fotografías tomadas en la campo como en la ciudad, procuraremos explicar el conjunto de estas mutaciones, antes de preguntarnos más ampliamente sobre el futuro de las explotaciones familiares en esta región.

Constraints on deformation of the Southern Andes since the Cretaceous from anisotropy of magnetic susceptibility

Science.gov (United States)

Maffione, Marco; Hernandez-Moreno, Catalina; Ghiglione, Matias C.; Speranza, Fabio; van Hinsbergen, Douwe J. J.; Lodolo, Emanuele

2015-12-01

The southernmost segment of the Andean Cordillera underwent a complex deformation history characterized by alternation of contractional, extensional, and strike-slip tectonics. Key elements of southern Andean deformation that remain poorly constrained, include the origin of the orogenic bend known as the Patagonian Orocline (here renamed as Patagonian Arc), and the exhumation mechanism of an upper amphibolite facies metamorphic complex currently exposed in Cordillera Darwin. Here, we present results of anisotropy of magnetic susceptibility (AMS) from 22 sites in Upper Cretaceous to upper Eocene sedimentary rocks within the internal structural domain of the Magallanes fold-and-thrust belt in Tierra del Fuego (Argentina). AMS parameters from most sites reveal a weak tectonic overprint of the original magnetic fabric, which was likely acquired upon layer-parallel shortening soon after sedimentation. Magnetic lineation from 17 sites is interpreted to have formed during compressive tectonic phases associated to a continuous N-S contraction. Our data, combined with the existing AMS database from adjacent areas, show that the Early Cretaceous-late Oligocene tectonic phases in the Southern Andes yielded continuous contraction, variable from E-W in the Patagonian Andes to N-S in the Fuegian Andes, which defined a radial strain field. A direct implication is that the exhumation of the Cordillera Darwin metamorphic complex occurred under compressive, rather than extensional or strike-slip tectonics, as alternatively proposed. If we agree with recent works considering the curved Magallanes fold-and-thrust belt as a primary arc (i.e., no relative vertical-axis rotation of the limbs occurs during its formation), then other mechanisms different from oroclinal bending should be invoked to explain the documented radial strain field. We tentatively propose a kinematic model in which reactivation of variably oriented Jurassic faults at the South American continental margin controlled

Glacial recession in the Tropical Andes from the Little Ice Age: the case of Ampato Volcanic Complex (Southern Peru

Science.gov (United States)

Alcalá, J.; Palacios, D.; Zamorano, J. J.

2010-03-01

Data published over the last decade reveal substantial glacial recession in the tropical Andes since the Little Ice Age (LIA), (Ramirez, et al., 2001; Rabatel, et al., 2005; Rabatel, et al., 2008; Vuille, et al., 2008; Hastenrath, 2009; Jomelli, et al., 2009), and a growing rate of recession since the 1980’s caused by global warming (Ramirez, et al., 2001; Vuille, et al., 2008). Today there is great interest in the evolution of these ice masses due to heightened awareness of climate change and of the strategic importance that glaciers have as a hydrologic resource for communities in arid climate zones in the tropical Andes (Mark, 2008; Vuille et al., 2008). Cordillera Blanca forms part of the Andes Mountains of northern Peru, and is a chosen site for many studies on glacier evolution. Vuille et al. 2008 determined that a considerable area of ice mass was lost at Huascarán-Chopicalqui glacier (18% from 1920-1970) and Astesonraju glacier (20% from 1962-2003). Studies at Coropuna volcano, which has the most extensive glacier field in the western range of southern Peru, also report a strong melting trend that began with only minimal recession from 1955-1986 (4%), but increased to 14% from 1986-2007 (Úbeda et al., 2009). Only a few of the Andes glaciers are consistently monitored, and the most comprehensive data are for Chacaltaya and Zongo glaciers (16º S) in Bolivia. Since the maximum LIA, Chacaltaya has lost 89% of its surface area, particularly in recent years. By 1983, the totaled loss was five times the shrinkage for the period 1940-1963 (Ramirez, et al., 2001). Zongo glacier maintained equilibrium from 1956-1975, but later experienced a period dominated by continuous recession (Soruco, et al., 2009). This study expands current knowledge of glacier evolution since the LIA in the Central Volcanic Zone (CVZ; 14º - 27º S) (Stern, 2004) of the Andes. The study site was chosen in an area that had never been used for preliminary research of this type, concretely

Biología reproductiva del águila Geranoaetus melanoleucus (Aves: Accipitridae) en Chile central Breeding biology of the black-chested eagle Geranoaetus melanoleucus (Aves: Accipitridae) in central Chile

OpenAIRE

EDUARDO F. PAVEZ

2001-01-01

Durante dos años (julio 1987­enero 1989) se estudió la biología reproductiva del águila (Geranoaetus melanoleucus) en San Carlos de Apoquindo, en Chile central. El inicio del período reproductivo se evidenció por un aumento del número de vuelos en pareja. Los cortejos incluyeron vuelos sincronizados de la pareja, capturas, transporte de material al nido y cópulas. Los traspasos de presas ocurrieron durante todo el año, aunque fuera del período reproductivo fueron escasos y forzados por la hem...

Corrales de piedra-pirkas- un patrimonio cultural del paisaje rural de Chile central

OpenAIRE

Tomic Jakas, Tonci Stipe

2016-01-01

Quisiéramos partir con este soliloquio, quizás el más famoso del drama español; ocurre al final del primer acto, cuando Segismundo piensa en la vida y en su suerte. No es el fatalismo lo que interesa si no que desde el inicio explicitar que se trata de una reflexión que lleva a configurar un visión –algo que anida en la mente-- que su fin central radica es tratar de poner en valor sobre la base de la importancia histórica, cultural y patrimonial de los muros de piedra o pirkas; en particular ...

Expanding Geophysical and Geochemical Investigation of Causes of Extraordinary Unrest at the Laguna del Maule (Rhyolitic) Volcanic Field, Southern Andes, Chile

Science.gov (United States)

Singer, B. S.

2014-12-01

The Laguna del Maule Volcanic Field, Chile, includes an unusually large and recent concentration of silicic eruptions. Since 2007 the crust here has been inflating at an astonishing rate of 25 cm/yr. Findings thus far lead to the hypothesis that the silicic vents have tapped an extensive layer of crystal-poor, rhyolitic melt that began to form atop a magmatic mush zone that was established by ~20 ka with a renewed phase of rhyolite eruptions during the Holocene. Modeling of surface deformation, magnetotelluric data, and gravity changes suggest that magma is currently intruding at a depth of ~5 km. Swarms of volcano-tectonic and long period earthquakes, mostly of M San Juan-Argentina, Nanyang Technological University-Singapore, SERNAGEOMIN, OVDAS, USGS, and SEGEMAR-Argentina. Team members will be introduced in this presentation. Our approach includes augmenting the OVDAS array of 6 permanent seisic stations with 40 additional instruments to conduct tomographic, receiver function and ambient noise studies. We continue to collect 4-D gravity data from 37 stations. Surface deformation is monitored via cGPS at 5 permanent receivers and InSAR data. A magnetotelluric survey across the Andes at 36o S is planned. Geochemical studies include mineral zoning and U-Th disequilibrium of zircons to constrain the timing of magma intrusion and mixing events prior to the current unrest. The overall aim is to integrate these observations and to construct numerical models of system dynamics. We are developing communications protocols and a web site to facilitate sharing of findings among the team members and with the public.

New ICT in the Peruvian Andes: Theoretical Foundation and Bibliographical Balance

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Mario Sánchez-Dávila

2016-04-01

Full Text Available On the one hand, this paper explains the theoretical foundations on which this proposal for digital anthropology in the Peruvian Andes is based (on the origins of digital anthropology, discussions on oral and written technology, and theories of digital technology as social practice. And, on the other hand, this paper presents a bibliographical balance of the studies on the new ICT in the Peruvian Andes (on identity expression, productive development and formal education in the Andean world.

Medición del conocimiento de los tsunamis en escuelas del pacífico central costarricense

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Fernández Arce, Mario

2017-12-01

Full Text Available A mediados de 2016 se investiga el conocimiento sobre tsunamis en cinco escuelas del Pacífico costarricense, a saber: la Escuela Central de Jacó, dos escuelas en Quepos, la escuela de Dominical y la Escuela Flor de Bahía en Uvita. La razón que impulsó a realizar este trabajo es que no se ha determinado el nivel de conocimiento del tema en la población de los centros educativos costeros. La investigación se realizó como un diagnóstico para iniciar un proceso de capacitación en manejo del riesgo en esas escuelas, cuyo fi n es aumentar la seguridad de la población estudiantil, prevenir desastres y reducir pérdidas humanas y materiales en caso de un eventual tsunami. Para lograr el objetivo se aplicó una encuesta de siete preguntas sobre el tema, con respuestas de escogencia única y luego se procesaron los datos manualmente. Se encontraron deficiencias de conocimiento, sin embargo, la población estudiada conoce ampliamente las reglas básicas para enfrentar un maremoto In the middle of 2016, we investigated the knowledge on tsunamis in five schools of the Costa Rican Pacific, whose names are: Escuela Central de Jacó, María Luisa Castro (Quepos, República de Corea (Quepos, Escuela de Dominical and Escuela Flor de Bahia (Uvita. We carried out this investigation because the subject is unknown in the in the population of coastal schools. The research was done to start a training process on risk management at these schools to increase the security of the students, prevent disasters and reduce deaths and material losses in the event of a possible tsunami. To achieve our objective we apply a seven questions poll about tsunamis, with single choice responses. The data were then processed manually. We found lack of knowledge in the students but they widely knows the basic rules to deal with a tsunami

Ecología y ocupación del espacio en los Andes Tropicales durante los últimos veinte milenios

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1973-01-01

Full Text Available Les Andes tropicales sont constituées par un ensemble de facettes écologiques dont le nombre est fonction du volume montagneux, du régime thermique a la base, de la diversité des modelés, du stock floristique, des effets de façade et d'abri, des modalités d'utilisation de l'espace. L'utilisation de ces facettes par les sociétés d'abord non agricoles, ensuite agricoles, a été très différente. Dans cette zone climatique les changements du climat au cours du Quaternaire ont moins affecté le milieu qu'aux latitudes moyennes, a l'exception des cotes touchées par les variations eustatiques. Aussi, une remarque importante est la constance de l'habitat au cours des 20 derniers millénaires, variant cependant en fonction des diverses facettes écologiques dont le comportement était différent suivant les modifications climatiques. Les glaciations dans les Andes sont relativement synchrones de celles des montagnes des latitudes moyennes, au moins pour le Quaternaire récent elles seraient dues a une meilleure distribution des précipitations au cours de l'année, a une nébulosité plus constante et a un abaissement des températures compris entre 5 et 9º. Les avancées glaciaires entre 20.000 et 16.000 et 14.000 et 10.000 ans BP ont eu des conséquences diverses suivant les milieux humides ou secs et les effets de dominance (en général glace au dessus de 4.000 m mais, jusque vers 2.900 m en Colombie et seulement 4.800 m dans les Andes sèches. Des processus périglaciaires se développent sur 1.000-1.500 m en contrebas dans les Andes sèches alors qu'ils n'affectent qu'une marge très étroite dans les Andes humides (500 m. L'englacement n'a jamais constitué une coupure dans la circulation N-S dans les Andes. Si la haute montagne entre 5 et 10º S était difficilement franchissable, les vallées et bassins intra andins situés entre 1.500 et 3.400 m étaient tièdes, avec une humidité mieux répartie durant l'année, moins secs qu

A remote sensing assessment of the impact of the 2010 Maule, Chile earthquake (Mw 8.8) on the volcanoes of the southern Andes

Science.gov (United States)

Pritchard, M. E.; Welch, M.; Jay, J.; Button, N.

2011-12-01

del Maule and Cordón Caulle (which began a major eruption in June, 2011). The deformation rate at Laguna del Maule continues through 2011 at a similar high rate, accumulating more than 60 cm of vertical deformation since 2007 -- making it one of the largest deformation signals without recent eruption yet observed. The rate of uplift at Laguna del Maule seems to be unchanged before and after the 2010 Maule earthquake. The spatial and temporal deformation at Cordón Caulle is complex as noted by Fournier et al., 2010, but does not appear to have been changed by the Maule earthquake either. The reasons that the 2010 Maule earthquake did not strongly affect the closest volcanic arc in the southern Andes remains a mystery. Comparison with the 2004 Sumatra (Mw 9.2) and the 2011 Japan (Mw 9.0) earthquakes and their closest volcanic arcs could provide clues to the elusive links between large earthquakes and volcanic unrest.

Overhaul of the generator of the hydroelectric central station Ingeniero Carlos Ramirez Ulloa; Rehabilitacion del generador de la unidad 2 de la central hidroelectrica ingeniero Carlos Ramirez Ulloa

Energy Technology Data Exchange (ETDEWEB)

Robles Pimentel, Edgar [Instituto de Investigaciones Electricas, Cuernavaca (Mexico); Garcia Hernandez, Javier [Comision Federal de Electricidad, Mexico, D. F. (Mexico)

1997-12-31

In November 1995, the failure of the Unit 2 generator at the hydroelectric central station Ingeniero Carlos Ramirez Ulloa, El Caracol, occurred. The accident forced to carry out its overhaul. Here are presented the technical problems faced during the overhaul of the generator and analyzed the implemented solutions. [Espanol] En noviembre de 1995 ocurrio la falla del generador de la unidad 2 de la central hidroelectrica Ing. Carlos Ramirez Ulloa, El Caracol. El accidente obligo a llevar a cabo su rehabilitacion. Se presentan los problemas tecnicos enfrentados durante la rehabilitacion del generador y se discuten las soluciones implementadas.

Overhaul of the generator of the hydroelectric central station Ingeniero Carlos Ramirez Ulloa; Rehabilitacion del generador de la unidad 2 de la central hidroelectrica ingeniero Carlos Ramirez Ulloa

Energy Technology Data Exchange (ETDEWEB)

Robles Pimentel, Edgar [Instituto de Investigaciones Electricas, Cuernavaca (Mexico); Garcia Hernandez, Javier [Comision Federal de Electricidad, Mexico, D. F. (Mexico)

1998-12-31

In November 1995, the failure of the Unit 2 generator at the hydroelectric central station Ingeniero Carlos Ramirez Ulloa, El Caracol, occurred. The accident forced to carry out its overhaul. Here are presented the technical problems faced during the overhaul of the generator and analyzed the implemented solutions. [Espanol] En noviembre de 1995 ocurrio la falla del generador de la unidad 2 de la central hidroelectrica Ing. Carlos Ramirez Ulloa, El Caracol. El accidente obligo a llevar a cabo su rehabilitacion. Se presentan los problemas tecnicos enfrentados durante la rehabilitacion del generador y se discuten las soluciones implementadas.

Cuando ya no se puede tomar trago ni chacchar coca. When alcohol can no longer be drunk or coca leaves chewed. the case of the “protestants” in the Peruvian central Andes

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Caroline Magny

2009-12-01

Full Text Available Desde hace mucho tiempo el alcohol y la coca ocupan un lugar central en las comunidades andinas. Hasta ahora en el distrito de Churcampa (Huancavelica, Perú, los católicos, mayoritarios, siguen explicando al visitante lo siguiente: “acá no se puede hacer nada sin trago ni coca”. No obstante, durante las ultimas décadas, muchas personas en este distrito – así como en muchos otros distritos de los Andes peruanos – se han convertido y siguen convirtiéndose al “protestantismo” (termino genérico usado por los católicos para referirse en forma general a las Iglesias evangélicas. Esta conversión implica, entre otras cosas, dejar completamente de masticar hojas de coca y de beber cualquier tipo de bebidas alcohólicas. En esta exposición proponemos analizar hasta qué punto y bajo qué modalidades estas restricciones alimenticias afectan a los conversos (quienes siguen siendo minoritarios en el distrito en su vida social cotidiana.Alcohol and coca have played a central role in Andean communities for many centuries. Nowadays, in the district of Churcampa (Huancavelica, Peru, the Catholic people, who are the majority, still explain to visitors that “here you can’t do anything without trago [alcohol] and coca”. Yet, over the past decades, many men and women in this district - as well as in many other districts of the Peruvian Andes - have been converting to “Protestantism” (a generic term used by Catholics to refer to the Evangelical Churches. This conversion implies, among other things, completely giving up chewing of coca leaves and drinking of any type of alcoholic drink. The aim of this article is to analyze to what extent and how these restrictions in the dietary habits affect converted people in their everyday social life.alcohol, coca leaves, religion, conversion, evangelic Churches, Peru

Variabilidad del ADN cloroplástico y su contribución al conocimiento del estado de conservación de Ulmus glabra en el Sistema Central

OpenAIRE

Martin del Puerto, Maria; Martinez Garcia, Felipe; Martin Clemente, Juan Pedro

2011-01-01

En el presente trabajo se ha analizado la diversidad existente en el ADN cloroplástico (ADNcp) de 16 poblaciones distribuidas a lo largo del Sistema Central. Para ello, se ha empleado la técnica de PCR-RFLP (amplificación de fragmentos específicos y posterior digestión con enzimas de restricción) sobre 38 regiones del ADNcp (Grivet et al., 2001).

El sistema de calidad del Instituto Central de Investigación Digital, la documentación de software y RUP

OpenAIRE

Nimia Olimpia Torres Gómez-Monte; Eugenia Genoveva Muñiz Lodos

2011-01-01

La calidad del proceso de desarrollo del software se ha convertido en uno de los aspectos más importantes en la Informática actualmente. Una metodología conocida internacionalmente para facilitar este proceso es Rational Unified Process (RUP) que cuenta con herramientas integradas. En el artículo se describen aspectos esenciales del RUP y del Sistema de Calidad del Instituto Central de Investigación Digital (ICID) basado en la norma ISO 9000:2000 (SGC ICID), proponiendo la forma de utilizar l...

Zeolites of the Valle Central of Costa Rica and its outskirts; Zeolitas del Valle Central de Costa Rica y sus alrededores

Energy Technology Data Exchange (ETDEWEB)

Zeledon, Luis Alonso [Moravia, San Jose, (Costa Rica)

2004-12-15

19 different species of zeolites have been found in 25 outcrops in the Valle Central of Costa Rica and in the Siquirres region. All the zeolites are secondary minerals and crystallized in little veins and vesicles of the basalts and pyroclastics rocks of the La Cruz and Grifo Alto formations, belonging to the Aguacate Group and the alkaline igneous rocks of Guayacan. The most frequent species of zeolites are stibnite, chabasite, laumontite, mesolite/mordenite, thomsonite, and analcime. Natrolite only was found near to Siquirres. (Author) [Spanish] Se describen 19 especies diferentes de zeolitas procedentes de 25 afloramientos en los alrededores del Valle Central de Costa Rica y en la region de Siquirres. Todas las zeolitas descritas son de origen secundario y se presentan en vetillas y vesiculas de los basaltos y rocas piroclasticas de las formaciones La Cruz y Grifo Alto del Grupo Aguacate y en las rocas igneas alcalinas de Guayacan. Las especies mas frecuentes son estilbita, chabasita, laumontita, mesolita/modernita, thomsonita y analcima. La natrolita solo se encontro en los alrededores de Siquirres. (Autor)

Phosphorus fractions and sorption dynamics in the sediments of two Ca-SO4 water reservoirs in the central Argentine Andes

Institute of Scientific and Technical Information of China (English)

José Gabriel León; Fernando Luis Pedrozo; Pedro Félix Temporetti

2017-01-01

Phosphorus (P) fractionation and sorption behavior were studied in the sediments of two calcium-sulfate (Ca-SO4:Ca2+170 mg L-1;SO42-400 mg L-1) water reservoirs in the southern central Argentine Andes-El Carrizal Reservoir (ECR),which stratifies in summer and El Nihuil Reservoir (ENR),which is vertically mixed throughout the year. Sediment size classes reflected the lithology of both basins and the reservoirs relative location:ECR (downstream from a valley adjacent to a mountain environment) had higher clay proportions while the sand fraction was more important in ENR (just next to a mountain environment). In both reservoirs, the chemical composition revealed low alteration and calcium enrichment. Total P content was relatively high (1.1–1.6 mg P kg-1 dry weight) as expected from the contribution of marine formations. P fractionation was dominated by Ca-P (ECR, 69%and ENR, 63%) followed by organic-P (23%) in summer-anoxic ECR and by iron/aluminum (Fe/Al)-P (27%) in oxic ENR. Batch experiments showed that sorption behavior in ECR had a typical Langmuir isotherm plot while in ENR that model fitted only at low dissolved P values (<5 mg P L-1) and co-precipitation evidence was observed at higher P con-centrations. It is proposed that lower Fe/Al-P content in anoxic (ECR) vs. oxic (ENR) sediments results from the P released from iron-bound phosphorus due to sulfate reduction-ferrous sulfide formation in an anoxic environment. This condition should enable ECR sediments to adsorb P into fresh oxidized iron, and ENR sediments to co-precipitate P with calcium due to Fe/Al-P saturation, as observed in batch experiments. This paper constitutes the first description of phosphorus content and dynamics in reser-voir sediments in arid central western Argentina, where water sulfate concentrations are naturally high due to basin lithology.

Perturbaciones del régimen de las lluvias y condiciones de tipo El Niño en América del sur tropical desde hace 7000 años

Directory of Open Access Journals (Sweden)

1995-01-01

Full Text Available PERTURBATIONS DU RÉGIME DES PLUIES ET CONDITIONS DE TYPE EL NIÑO EN AMÉRIQUE DU SUD TROPICALE DEPUIS 7 000 ANS. Des enregistrements sédimentaires provenant de trois régions d’Amérique du Sud, géographiquement et climatiquement très différentes, ont permis de reconstruire l’évolution du régime des pluies au cours des 7 000 dernières années. En Amazonie du sud-est, les analyses palynologiques et sédimentologiques de carottes prélevées dans des lacs de la région de Carajás (6° S ont permis de mettre en évidence l’existence de plusieurs périodes d’incendies de la forêt tropicale humide en liaison avec des phases sèches de courtes durées (quelques dizaines d’années. De même, dans le Brésil central, les analyses palynologiques et sédimentologiques de deux carottes prélevées dans la région de Salitre (19° S et de Boa Vista (27° S ont permis de mettre en évidence des variations synchrones mais de sens opposés de la végétation. Enfin, dans les Andes centrales, des reconstructions paléobathymétriques effectuées sur le lac Titicaca (14-17° S ont également permis de mettre en évidence des perturbations importantes du régime des précipitations en phase avec celles enregistrées à Carajás et à Salitre. Ces perturbations sont du même type que celles provoquées de nos jours par les importants événements El Niño. Algunos registros sedimentarios provenientes de tres regiones de América del Sur, geográfica y climáticamente diferentes, permitieron reconstruir la evolución del régimen, de las lluvias durante los últimos 7 000 años. En Amazonía del sudeste, los análisis palinológicos y sedimentológicos de testigos obtenidos de los lagos de la región de Carajás (6° S permitieron evidenciar la existencia de varios períodos de incendios del bosque tropical húmedo en relación con fases secas de corta duración (algunas decenas de años. Asimismo, en el Brasil central los análisis palinológicos y

Especie nueva de Scybalocanthon (Coleoptera: Scarabaeinae: Canthonini y descripción de la variación del órgano genital masculino A new species of Scybalocanthon (Coleoptera: Scarabaeinae: Canthonini and description of the variation of the male genitalia

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Fredy Molano Rendón

2010-12-01

Full Text Available Se describe Scybalocanthon arcabuquensis Molano y Medina, sp.nov. La distribución de esta especie se encuentra restringida a los bosques de roble del municipio de Arcabuco, Departamento de Boyacá, sobre la cordillera Oriental de los Andes en Colombia. El órgano genital del macho se describe e ilustra, se discute la variación de las estructuras del saco interno de varias especies del género, y se proponen algunas estructuras del órgano genital como posibles caracteres únicos que definen el género.Scybalocanthon arcabuquensis Molano y Medina, sp. nov. is described. The species is restricted to the oak forest at Arcabuco municipality, department of Boyacá, Eastern Cordillera of the Colombian Andes. The male genitalia is described and illustrated, the variation of structures of the internal sac is discussed for various species of the genus and some structures from the internal male genitalia are proposed as possible unique characters useful for defining the genus.

Asynchronous Glacial Chronologies in the Central Andes (15-40°S) and Paleoclimatic Implications

Science.gov (United States)

Zech, R.; Kull, C.; Kubik, P. W.; Veit, H.

2006-12-01

We have established glacial chronologies along a N-S transect over the Central Andes using 10Be surface exposure dating. Our results show that maximum glacial advances occurred asynchronously and reflect the varying influence and shifts of the major atmospheric circulation systems during the Late Quaternary: the tropical circulation in the north and the westerlies in the south. In Bolivia (three research areas in the Cordillera Real and the Cordillera Cochabamba, ~15°S) glacial advances could be dated to ~20 and 12 ka BP. This is in good agreement with published exposure age data from moraines in Bolivia and Peru (provided that all ages are calculated following the same scaling system). Accordingly, the maximum glaciation there probably occurred roughly synchronous to the temperature minimum of the global Last Glacial Maximum (LGM) and the lateglacial cold reversals. Strict correlation with neither the Younger Dryas in the northern hemisphere, nor the Antarctic Cold Reversal is possible due to the current systematic exposure age uncertainties (~10%). Glacier-Climate-Modelling corroborates the sensitivity of the reconstructed glaciers to temperature changes, rather than precipitation. On the contrary, there is good evidence for the dominant role of precipitation changes on the glacial chronologies in the lee of the Cordillera Occidental, i.e. on the Altiplano and further south. The pronounced lateglacial wet phase, which is well documented in lake transgression phases as far south as 28°S (-> tropical moisture source), seems to have caused glacial advances even at ~30°S. In two research areas in Chile at that latitude, we were able to date several lateglacial moraines. Besides, the maximum datable glaciation there occurred at ~30 ka BP. That is significantly earlier than the LGM (sensu strictu) and points to favourable climate conditions for glaciation at that time (particularly increased precipitation). We conclude that the westerlies were more intensive or

Glacier shrinkage and water resources in the Andes

Science.gov (United States)

Francou, Bernard; Coudrain, Anne

For more than a century glaciers around the world have been melting as air temperatures rise due to a combination of natural processes and human activity. The disappearance of these glaciers can have wide-ranging effects, such as the creation of new natural hazards or changes in stream flow that could threaten water suppliesSome of the most dramatic melting has occurred in the Andes mountain range in South America. To highlight the climatic and glacial change in the Andes and to encourage the scientific community to strengthen the glacier observation network that stretches from Colombia to the Patagonian ice fields, the Instituto Nacional de Recursos Naturales (INRENA), Perú, and the Institute of Research and Development (IRD), France, recently organized the second Symposium on Mass Balance of Andean Glaciers in Huaráz,Perú.

Una frontera casi invisible: los territorios al norte del Sistema Central en la Alta Edad Media (siglos VIII-XI

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Iñaki MARTÍN VISO

2009-12-01

Full Text Available RESUMEN: Los territorios al norte del Sistema Central no estuvieron sujetos a un dominio por parte de una autoridad centralizada entre los siglos VIII a XI. Los instrumentos del poder central, en especial la tributación y la organización episcopal, se descompusieron tras el siglo VIII y asumieron un papel determinante las estructuras de poder local, las cuales deben ser el principal objeto de estudio. A partir de su análisis, se descubre un espacio fronterizo abierto, con un dominio político informal, que es invisible para los poderes centrales. Palabras clave: Poderes Locales. Sitios de Altura. Necrópolis. Frontera. Tributación. Mozárabes.ABSTRACT: The territories at the North of the Iberian Central System were not ruled by any central authority between eighth and eleventh centuries. The main tools of the central power, especially the tribute and the episcopal organization, were broken down after the 8th century and the structures of local power, which must be studied particularly, got a very influential role. The analysis discover an opened frontier area, with an informal political control, that is invisible from the perspective of the central power

Dating the last Neanderthals in Central Iberia - New evidence from Abrigo del Molino, Segovia, Spain

Science.gov (United States)

Kehl, Martin; Álvarez-Alonso, David; de Andrés-Herrero, María; Díez-Herrero, Andrés; Klasen, Nicole; Rojo-Hernández, Julio; Weniger, Gerd-Christian

2017-04-01

The timing of Neanderthal disappearance in the Iberian Peninsula is a hotly debated subject in Palaeolithic archaeology. Several studies suggested a late survival in South and Central Iberia until about 32,000 year ago (ka), but were probably subject to significant age underestimation due to contamination of dating samples and/or lack of stratigraphic integrity. More recently, Late Neanderthal presence was dated to no later than 38 ka. In Central Iberia, few archaeological sites contain Mousterian levels attesting occupation by Neanderthals. The newly discovered rock shelter of Abrigo del Molino contains chronologically well-constraint Mousterian levels, which, according to radiocarbon dating on bone, place the latest Neanderthal occupation to around 42-44 ka and within Greenland interstadial 11. Accumulation of these levels took place after deposition of fluvial and slope sediments, dated to around 46 ± 3.5 ka using luminescence techniques, and probably correlating with Greenland stadial 13 including Heinrich event 5. Micromorphological evidence of banded sediment fabrics suggests frost dynamics pointing to cold climate conditions during that time in Central Spain. Abrigo del Molino thus provides a detailed and chronologically well-constrained record on Late Neanderthal presence and morphodynamic change in Central Iberia during times of millennial-scale climate changes. The site gives further evidence for an early rather than late disappearance of Neanderthals in Iberia.

Late Cenozoic basin evolution and fold-thrust deformation in the southern Central Andes: Initial constraints from synorogenic deposits of the Precordillera, Argentina

Science.gov (United States)

Levina, M.; Horton, B. K.; Fuentes, F.; Stockli, D. F.

2012-12-01

In the Precordillera region of the Argentine Andes, Cenozoic shortening associated with flattening of the Pampean segment of the subducting Nazca plate has resulted in a series of thin skinned fold-thrust systems that partitioned and uplifted Cenozoic foreland basin deposits. The kinematic and temporal evolution of the Andean Precordillera can be approached through detailed analyses of the sedimentary fill now preserved in intermontane regions and the bedrock low-temperature thermochronology of the fold-thrust belt. In this project, we focus on Neogene foreland basin fill exposed in the central and eastern Precordillera along the San Juan River (Quebrada Albarracín and Pachaco regions), on the western flank of the Sierra Talacasto, and in the Loma de las Tapias area near the Ullum dam. The sedimentary successions exposed in these regions record the hinterland development of the Frontal Cordillera (detrital zircon provenance and composition of sandstone and conglomeratic units), regional volcanism (pyroclastic flows and tuffaceous sandstone units), and initial construction of the Precordillera (fault cutoff relationships, growth strata, and paleocurrent changes). We investigate the development and subsequent partitioning and deformation of these synorogenic sections using sediment provenance (detrital zircon U-Pb geochronology, conglomerate clast counts, sandstone petrography, and paleocurrent measurements), facies analysis of measured stratigraphic successions, and initial apatite (U-Th)/He cooling histories to constrain the age of uplift-induced exhumation of successive thrust sheets in the Andean Precordillera.

Summer energy balance and ablation of high elevation glaciers in the central Chilean Andes

Science.gov (United States)

Brock, Benjamin; Rivera, Andres; Burger, Flavia; Bravo, Claudio

2014-05-01

Glaciers of the semi-arid central Chilean Andes are an important freshwater source for the populous Central Valley region of Chile, but have been shrinking in recent decades. The surface energy balance of these glaciers is of high scientific interest as summer ablation occurs through both sublimation and melt. During the 2012-13 Austral Summer a glacio-meteorological monitoring programme was established on Olivares Alfa (3.9 km2, 4130-4800 m elevation) and Beta (8.3 km2, 3620-4850 m elevation) Glaciers and their forelands in the Upper Olivares Valley, 33°00'-33°11' S, 70°05'-70°15' W, approximately 50 km north-east of Santiago. This included complete automatic weather stations (AWSs) with sonic rangers to record surface ablation on the ablation zones of the two glaciers, and one AWS in the proglacial area of Olivares Alfa Glacier including precipitation gauge. To complement these point data, daily images of the glaciers were captured with fixed cameras in order to calculate snow cover and albedo distributions. To calculate the surface energy balance and rates of melt and sublimation, a model was developed which uses direct AWS measurements of the radiative fluxes and calculates the turbulent fluxes of sensible and latent heat using the bulk aerodynamic approach. The model also calculates the subsurface heat flux and includes a simple scheme to estimate refreezing of melt water within surface snow or ice. Meteorological data and model results for the December to May period will be presented in this paper. Model calculations match closely the cumulative ablation curve of the sonic ranger at Olivares Alfa, with a slight overestimation, and overestimate cumulative ablation recorded by the sonic ranger at Olivares Beta, possibly due, at least in part, to uncertain snow density values. Modelled cumulative ablation in the December-April period is 2.2 m water equivalent (w.e.) at Olivares Alfa (0.10 m sublimation, 2.10 m melt) and 2.34 m w.e. at Olivares Beta (0.18 m

Floristic changes in alpine plant communities induced by the cushion plant Azorella madreporica (Apiaceae in the Andes of central Chile Cambios florísticos en comunidades de plantas alpinas inducidos por la planta en cojín Azorella madrepórica (Apiaceae en los Andes de Chile central

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CONSTANZA L QUIROZ

2009-06-01

Full Text Available It is well known that the number of plant species associated with nurse plants increases with elevation. However, studies conducted so far have largely ignored the effect of nurse plants on other community attributes, such as the species abundances, diversity and evenness. Moreover, changes in these community attributes along environmental gradients have also been seldom examined. The present study evaluates the effect of the cushion plant Azorella madrepórica (Apiaceae on species richness, species abundance, diversity and evenness of vascular plants at two elevations in the Andes of central Chile. Theoretically, the impact of this nurse cushion plant on these community attributes should be grater at a higher elevation. Results showed that the proportion of plant species associated with cushion plants increases with elevation, and the abundance of some species is also greater within cushions than on bare ground. Although the proportion of species growing within cushions increased with elevation, diversity and evenness were higher on bare ground. This is due to some few species that attained very high densities within cushions, generating assemblages highly dominated by some few species. Ordination analyses indicated differences in species assemblages within and outside A. madrepórica at the higher elevation. Therefore, the influence of cushion plants on community structure changes with elevation. Accordingly, we suggest that attributes other than species richness must be included in future studies in order to analyze the impact of nurse species on community structure along environmental gradients.Se sabe que el número de especies asociado a plantas nodrizas aumenta con la altitud. Sin embargo, el efecto de plantas nodrizas sobre otros atributos de las comunidades, como la abundancia de especies, diversidad y equidad, ha sido largamente ignorado. Más aún, cambios en estos atributos en gradientes ambientales han sido pocas veces examinados

Essential oils of medicinal plants from the central andes of Argentina: chemical composition, and antifungal, antibacterial, and insect-repellent activities.

Science.gov (United States)

Lima, Beatriz; López, Sandra; Luna, Lorena; Agüero, María B; Aragón, Liliana; Tapia, Alejandro; Zacchino, Susana; López, María L; Zygadlo, Julio; Feresin, Gabriela E

2011-05-01

The antifungal, antibacterial, and insect-repellent activities of the essential oils (EOs) of Acantholippia seriphioides, Artemisia mendozana, Gymnophyton polycephalum, Satureja parvifolia, Tagetes mendocina, and Lippia integrifolia, collected in the Central Andes area, province of San Juan, Argentina, were investigated. The dermatophytes Microsporum gypseum, Trichophyton mentagrophytes, and T. rubrum were inhibited by the EOs of G. polycephalum, L. integrifolia, and S. parvifolia, with minimum inhibitory concentrations (MICs) between 31.2 and 1000 μg/ml. Moreover, all EOs presented moderate activity against the bacteria tested, and the L. integrifolia and G. polycephalum EOs showed excellent repellent properties against Triatoma infestans, the Chagas disease vector, with repellency values between 60 and 100%. The A. seriphioides, G. polycephalum, and L. integrifolia EOs, obtained by hydrodistillation, were characterized by GC-FID and GC/MS analyses. The highest number of components (40) was identified in L. integrifolia EO, which, along with that of A. seriphioides, contained important amounts of oxygenated monoterpenes (44.35 and 29.72%, resp.). Thymol (27.61%) and carvacrol (13.24%) were the main components of A. seriphioides EO, and borneol, lippifoli-1(6)-en-5-one, and terpinen-4-ol (>8.5%) were the principal compounds of L. integrifolia EO. These results support the idea that oxygenated monoterpenes are the bioactive fractions of the EOs. Finally, the study shows that these Andean species might be used to treat superficial fungal infections and to improve the local Chagas disease situation by vector-control. Copyright © 2011 Verlag Helvetica Chimica Acta AG, Zürich.

Natural gas across the Andes : a case study of an international business venture

Energy Technology Data Exchange (ETDEWEB)

Figueroa, E.B.; Smith, B.

2002-07-01

This book describes the challenges and complexities of constructing the GasAndes pipeline from Argentinian gas fields across the Andes to Santiago in Chile. The project was a joint international effort between Canada's NOVA Corporation, Chile's Gasco and Gener, and Argentina's Compania General de Combustibles and Techint Compania Tecnica Internacional. The book relates how NOVA Gas International, together with its partners, accomplished the task of constructing the first major natural gas pipeline across the Andes mountains despite significant challenges such as steep mountain slopes, many river crossings, high altitude, high winds and bitter cold. It describes how the partnership developed and how political and socio-economic issues were dealt with. It demonstrates how business practices were modified to deal with local conditions and to ensure that the fragile environment of the Andean meadows was protected. It also describes how the builders of the pipeline addressed the concerns of communities along the pipeline route. The pipeline was constructed at a time when democracy was returning and market economies were shifting from a reduced role of government in the energy sector. The 463 km GasAndes pipeline has been in operation since August 7, 1997. refs., tabs., figs.

Gestión Técnica del Síndrome del Quemado por el Trabajo en la Central Metropolitana de Atención Ciudadana CMAC

OpenAIRE

Galarza Carrera, Oswaldo Arturo

2014-01-01

175 hojas : ilustraciones, 29 x 21 cm +CD-ROM 5526 El propósito del estudio fue aplicar el sistema de gestión técnica en seguridad industrial y salud ocupacional, sobre los factores de riesgo, y el síndrome del quemado por el trabajo (SQT), en los telefonistas de la Central Metropolitana de Atención Ciudadana (CMAC), se identificó, midió y evaluó los factores de riesgos psicosociales, para asesorar a la organización sobre las medidas de prevención y control a nivel individual, grupal, y ...

Gastrointestinal parasites of Lamas in the Bolivian Andes

DEFF Research Database (Denmark)

Nissen, Anne Malene; Nees, Ellinor Spörndly; Monrad, Jesper

A cross sectional study was conducted to determine prevalences and intensities of gastrointestinal (GIT) parasites in lamas in the Bolivian Andes. A quantitative and qualitative necro-copro-parasitlogical study was performed on 33 lamas between October and December 2007. At the time of necropsy t...

Una nueva especie de Lepidoblepharis (Sauria, Gekkonidae de la Cordillera Central de Colombia Una nueva especie de Lepidoblepharis (Sauria, Gekkonidae de la Cordillera Central de Colombia

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Ayala Stephen C.

1986-12-01

Full Text Available A third Lepidoblepharis is described from temperate elevations in the Colombian Andes. Unlike L. colombianus or L. duolepis, the new species from central Antioquia is a small, moderately short toed species, reaching about 30 mm snout-vent length. Most specimens have prominent rust colored dorsolateral stripes on the tail. Una tercera especie de Lepidoblepharis se describe de zonas templadas de los Andes de Colombia. A diferencia de L. colombianus o L. duolepis, la nueva especie de Antioquia es una especie de menor tamaño que alcanza unos 30 mm de longitud rostro-ano, y los dedos son moderadamente cortos. La mayoría de los ejemplares tiene franjas dorsolaterales muy notorias de color herrumbre en la cola.

Meteorological Conditions of Floods In The Chilean Andes Mountains

Science.gov (United States)

Vergara, J.

Catastrophic floods occurred on mountains River during 2000 and 2001. The meteo- rological conditions of flood during the last five years have analyzed. For example, the flood of June 29 of 2000 occurred after one of extremely wettest June of the last 40 years were snowfall was 991cm in the Aconcagua Valley. Infrequently storms activ- ity generated a huge snowfall and rainfall over the Andes mountains on June of 2000 (1525mm in El Maule Valley) and the end of the unusually period, the flood was trig- gered by rising temperatures on the mountains and heavy rain (199mm in 24 hours) fall over the fresh snow on the morning of June 29 and floods wave developed and moved down along of the all river located on Central part of Chile, the foods peak was 2970.5m3/s on the El Maule basin in the morning of June 29. The regional meteoro- logical models with the hydrological forecasting was used for alert of the floods.

Reflections on Andes' Goal-Free User Interface

Science.gov (United States)

VanLehn, Kurt

2016-01-01

Although the Andes project produced many results over its 18 years of activity, this commentary focuses on its contributions to understanding how a goal-free user interface impacts the overall design and performance of a step-based tutoring system. Whereas a goal-aligned user interface displays relevant goals as blank boxes or empty locations that…

Attenuation tomography in the western central Andes: A detailed insight into the structure of a magmatic arc

Science.gov (United States)

Haberland, Christian; Rietbrock, Andreas

2001-06-01

High-quality data from 1498 local earthquakes recorded by the PISCO '94 (Proyecto de Investigatión Sismológica de la Cordillera Occidental, 1994) and ANCORP '96 (Andean Continental Research Project, 1996) temporary seismological networks allowed the detailed determination of the three-dimensional (3-D) attenuation structure (Qp-1) beneath the recent magmatic arc in the western central Andes (20° to 24°S). Assuming a frequency-independent Qp-1 in a frequency band between 1 and 30 Hz, whole path attenuation (t*) was estimated from the amplitude spectra of the P waves using spectral ratios and a spectral inversion technique. The damped least squares inversion (tomography) of the data reveals a complex attenuation structure. Crust and mantle of the forearc and subducting slab are generally characterized by low attenuation (Qp > 1000). Crust and mantle beneath the magmatic arc show elevated attenuation. The strongest anomaly of extremely low Qp is found in the crust between 22° and 23°S beneath the recent volcanic arc (Qp < 100). N-S variations can be observed: The western flank of the crustal attenuation anomaly follows the curved course of the volcanic front. North of 21°S the attenuation is less developed. In the northern part of the study area the low-Qp zone penetrates in the forearc mantle down to the subducting slab. In the south a deeper zone of high attenuation is resolved between 23° and 24°S directly above the subducting slab. Low Qp in the mantle correlates with earthquake clusters. The strong crustal attenuation is confined to the distribution of young ignimbrites and silicic volcanism and is interpreted as a thermally weakened zone with partial melts. The attenuation pattern in the upper mantle might reflect the variable extent of the asthenosphere and maps variations of subduction-related hydration processes in the mantle wedge from slab-derived fluids.

Between Andes and Amazon: the genetic profile of the Arawak-speaking Yanesha.

Science.gov (United States)

Barbieri, Chiara; Heggarty, Paul; Yang Yao, Daniele; Ferri, Gianmarco; De Fanti, Sara; Sarno, Stefania; Ciani, Graziella; Boattini, Alessio; Luiselli, Donata; Pettener, Davide

2014-12-01

The Yanesha are a Peruvian population who inhabit an environment transitional between the Andes and Amazonia. They present cultural traits characteristic of both regions, including in the language they speak: Yanesha belongs to the Arawak language family (which very likely originated in the Amazon/Orinoco lowlands), but has been strongly influenced by Quechua, the most widespread language family of the Andes. Given their location and cultural make-up, the Yanesha make for an ideal case study for investigating language and population dynamics across the Andes-Amazonia divide. In this study, we analyze data from high and mid-altitude Yanesha villages, both Y chromosome (17 STRs and 16 SNPs diagnostic for assigning haplogroups) and mtDNA data (control region sequences and 3 SNPs and one INDEL diagnostic for assigning haplogroups). We uncover sex-biased genetic trends that probably arose in different stages: first, a male-biased gene flow from Andean regions, genetically consistent with highland Quechua-speakers and probably dating back to Inca expansion; and second, traces of European contact consistent with Y chromosome lineages from Italy and Tyrol, in line with historically documented migrations. Most research in the history, archaeology and linguistics of South America has long been characterized by perceptions of a sharp divide between the Andes and Amazonia; our results serve as a clear case-study confirming demographic flows across that 'divide'. © 2014 The Authors. American journal of physical Anthropology published by Wiley Periodocals, Inc.

Caracterización médico legal del feminicidio en la Morgue Central de Lima

OpenAIRE

Castro Pizarro, Hugo Vladimir

2013-01-01

Objetivo: Identificar las características médico legales del feminicidio, según los registros de la Morgue Central de Lima (MCL) para el período 2009 - 2010. Material y método: Se consignó la información de 2469 occisas registradas en la Morgue Central de Lima (MCL), durante el período 2009 - 2010. Los datos fueron analizados de forma cuantitativa y cualitativa. Resultados: La mayor causa de muerte fue natural (38,9%), seguida de causa por determinar (28,6%) y accidental (18,1%). El ...

Diseño del sistema de control y protección de una central hidráulica de 37 MVA

OpenAIRE

Feliz Juárez, Javier Fernando

2013-01-01

El presente Proyecto Fin de Carrera tiene como objetivo el estudio, diseño y valoración técnica y económica del Sistema de Control y Protección de Grupo de una central hidroeléctrica de 37 MVA. Este Sistema está compuesto por el conjunto de equipos eléctricos, electrónicos y mecánicos encargados del control y protección de los dispositivos e instalaciones existentes en la central y necesarias para el correcto funcionamiento de la unidad Turbina- Generador de la misma. Se han...

Diagnostic of annual cycle and effects of the ENSO about the maximum intensity of duration rains between 1 and 24 hours at the Andes of Colombia

International Nuclear Information System (INIS)

Poveda, German; Mesa, Oscar; Toro, Vladimir; Agudelo, Paula; Alvarez, Juan F; Arias, Paola; Moreno, Hernan; Salazar, Luis; Vieira, Sara

2002-01-01

We study the distribution of maximum rainfall events during the annual cycle, for storms ranging from 1 to 24-hour in duration; by using information over 51 rain gauges locate at the Colombian Andes. Also, the effects of both phases of ENSO (El Nino and La Nina) are quantified. We found that maximum rainfall intensity events occur during the rainy periods of march-may and September-November. There is a strong similarity between the annual cycle of mean total rainfall and that of the maximum intensities of rainfall over the tropical Andes. This result is quite consistent throughout the three ranges of the Colombian Andes. At inter annual timescales, we found that both phases of ENSO are associated with disturbances of maximum rainfall events; since during La Nina there are more intense precipitation events than during El Nino, overall, for durations longer than 3 hours, rainfall intensity gets reduced by one order of magnitude with respect to shorter durations (1-3 hours). The most extreme recorded rainfall events are apparently not associated with the annual and inter annual large scales forcing and appear to be randomly generated by the important role of the land surface atmosphere in the genesis and dynamics of intense storm over central Colombia

Nueva central del Oberbank Salzburgo Alta Austria

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Schmidt, W.

1983-03-01

Full Text Available This banking center has been constructed on a choice urban site, in accord with the most modern organizational and functional techniques, and with the latest studies on the forms of humanized work in administrative buildings. In its two basements and seven storeys above street level, of different surface areas — in accord with their different uses and requisites — all the annexes necessary in a building of this type have been distributed, with outstanding organization of great flexibility and function of the different spaces. Special mention should be made of the foundations and structure employed because of its proximity to the Danube: the treatment of the facades — given the urban site of the construction —, and of the security systems and installations for the specific function of the building.En un privilegiado enclave urbano se ha construido esta central bancaria, de acuerdo con las más modernas técnicas organizativas y funcionales, y los últimos estudios sobre las formas de trabajo humanizadas en edificios administrativos. En sus dos sótanos y siete plantas por encima de rasante, de distintas superficies —de acuerdo con sus diferentes usos y requisitos--, se han distribuido todas las dependencias necesarias en un edificio de este tipo, destacando en su organización la gran flexibilidad y funcionalidad de los diversos espacios conformados. Mención aparte merece la especial atención prestada a la cimentación y estructura empleadas por la proximidad del Danubio; al tratamiento de las fachadas —dada la situación urbana de la construcción—, y a los sistemas de seguridad e instalaciones por la función específica del edificio.

Ethnoecology of the tropical Andes avian indicators of landscape change in highland Ecuador.

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Sarmiento, F. O.

2005-12-01

reservas naturales absolutas, la ordenación del paisaje, las facilidades de conservación y los paisajes culturales deben considerarse escenarios conservacionistas para la supervivencia de la pluviisilva, que incluye sitios sagrados y dominios espirituales que merecen protegerse en los Andes tropicales.

Las cuencas cenozoicas y su control en el volcanismo de los Complejos Nevados de Chillan y Copahue-Callaqui (Andes del Sur, 36-39°S Cenozoic basins and their control on volcanism of Nevados de Chillan and Copahue-Callaqui complexes (36-39°S, Southern Andes

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Juan Pablo Radic

2010-01-01

Full Text Available La Cordillera Principal de los Andes entre los 36° y 39°S constituye un excelente lugar para el estudio de la relación entre volcanismo y tectónica. Por medio del análisis tectonoestratigráfico de las cuencas cenozoicas se ha podido reconocer una clara coincidencia espacial entre estructuras de primer orden pertenecientes a estas cuencas y la distribución del volcanismo plio-pleistocénico. Las cuencas cenozoicas comenzaron su desarrollo durante el Oligoceno-Mioceno como depresiones extensionales, conformando un sistema de al menos tres subcuencas orientadas N-S y conectadas por dos zonas de acomodación estructural. Posteriormente este sistema de cuencas fue tectónicamente invertido hacia finales del Mioceno y los antiguos depocentros fueron deformados y exhumados, reutilizando las fallas originalmente extensionales. Las zonas de acomodación estructural permanecieron como estructuras de primer orden a escala de cuenca y constituyeron zonas de debilidad que favorecieron el posterior desarrollo del volcanismo y magma-tismo en los complejos volcánicos Nevados de Chillan y Copahue-Callaqui. Cada uno de estos complejos volcánicos se caracteriza por una orientación de sus centros de emisión, morfología y depósitos volcánicos en forma subparalela a la orientación de las zonas de acomodación estructural inmediatamente por debajo.The Cordillera Principal at 36° to 39°S is an excellent place to address the relationship between tectonics and volcanism. Based on tectonostratigraphic analysis of the Cenozoic basins it has been possible to recognize a clear spatial coincidence between first order basin scale structures and Plio-Pleistocene volcanism. Cenozoic basins started in the Oligocene-Miocene as extensional depocenters, characterized by at least three north-south oriented sub-basins connected by two structural accommodation zones. Towards the Late Miocene this extensional system was tectonically inverted deforming and uplifting the

Determinantes del acceso a los productos financieros en los hogares colombianos

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Santiago Rodríguez-Raga

2016-01-01

Full Text Available Existe evidencia que establece una asociación positiva entre el acceso a productos financieros, la riqueza y calidad de vida de los hogares, en especial de los hogares pobres. En este ámbito, este estudio busca entender los determinantes del acceso a los diferentes productos financieros en los hogares de Colombia, utilizando un modelo econométrico con base en la información contenida en la Encuesta Longitudinal Colombiana (ELCA de la Universidad de los Andes. Como conclusión se encuentra que los principales determinantes del acceso a productos financieros son el nivel de ingreso o riqueza, la educación y la estabilidad en términos laborales.

Evidence for Cenozoic extensional basin development and tectonic inversion south of the flat-slab segment, southern Central Andes, Chile (33° 36°S.L.)

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Charrier, R.; Baeza, O.; Elgueta, S.; Flynn, J. J.; Gans, P.; Kay, S. M.; Muñoz, N.; Wyss, A. R.; Zurita, E.

2002-04-01

The mainly volcanic Cenozoic deposits that make up much of the western part of the Principal Cordillera in Central Chile are generally subdivided into two major units: an older Abanico or Coya-Machalí Formation and a younger Farellones Formation. Difficulty in differentiating these units has led to considerable debate. On the basis of the wide distribution, great thickness, and presence of sedimentary intercalations, it has been postulated that these arc volcanics were deposited in an intermontane basin; more recently, it has been proposed that this basin developed under extensional conditions and underwent subsequent tectonic inversion. We present field, geochronologic, geochemical, and thermal maturity data that support the latter interpretation. Collectively, this new information clarifies the stratigraphic, tectonic, and paleogeographic evolution of these deposits. The vast geographic extent of the Abanico Formation and lateral equivalents, which reach from at least 32°30' to 44°S along the Principal Cordillera, its great thickness, and the presence of repeated thick fluvial and lacustrine intercalations all indicate deposition in a large, strongly subsident, and probably north-south oriented basin, developed between middle to late Eocene and Oligocene. The unconformable contact with underlying Mesozoic units observed at several localities indicates that deposition followed a substantial erosional episode during late Cretaceous and/or early Cenozoic time. Basal deposits of the Abanico Formation near Termas del Flaco increase rapidly in thickness to the west. Still further to the west, a thick Abanico section contains, in its upper part, mammal fossils older than those found in the basal deposits near Termas. This evidence indicates a major space of deposition west of this locality, which had been filled before deposition took place at Termas. The east-vergent, high-angle El Fierro thrust fault on the east side of the westward-growing deposits is interpreted

Seasonal and elevational contrasts in temperature trends in Central Chile between 1979 and 2015

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Burger, F.; Brock, B.; Montecinos, A.

2018-03-01

We analyze trends in temperature from 18 temperature stations and one upper air sounding site at 30°-35° S in central Chile between 1979-2015, to explore geographical and season temperature trends and their controls, using regional ocean-atmosphere indices. Significant warming trends are widespread at inland stations, while trends are non-significant or negative at coastal sites, as found in previous studies. However, ubiquitous warming across the region in the past 8 years, suggests the recent period of coastal cooling has ended. Significant warming trends are largely restricted to austral spring, summer and autumn seasons, with very few significant positive or negative trends in winter identified. Autumn warming is notably strong in the Andes, which, together with significant warming in spring, could help to explain the negative mass balance of snow and glaciers in the region. A strong Pacific maritime influence on regional temperature trends is inferred through correlation with the Interdecadal Pacific Oscillation (IPO) index and coastal sea surface temperature, but the strength of this influence rapidly diminishes inland, and the majority of valley, and all Andes, sites are independent of the IPO index. Instead, valley and Andes sites, and mid-troposphere temperature in the coastal radiosonde profile, show correlation with the autumn Antarctic Oscillation which, in its current positive phase, promotes subsidence and warming at the latitude of central Chile.

Dos nuevas especies de cangrejos del género Neostrengeria Pretzmann, 1965, de Colombia (Crustacea: Decapoda: Pseudothelphusidae, con actualización de la clave de las especies del género

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MARTHA R. CAMPOS

2008-12-01

Full Text Available Se describen dos nuevas especies de Neostrengeria Pretzmann, 1965, N. bataensis, de Santa María, Departamento de Boyacá y N. celioi, de Aguazul, Departamento de Casanare, en la vertiente oriental de los Andes Orientales. Con la adición de las nuevas especies, el número de especies del género se incrementa a 23. Las nuevas especies se diferencian de las otras del género principalmente en la morfología del primer gonopodo del macho, particularmente en la forma de los lóbulos laterales y accesorios, el contorno del ápice, la proyección mesocaudal y el lóbulo mesial. El género Neostrengeria es endémico de Colombia y se distribuye en las dos vertientes y el altiplano de la Cordillera Oriental, en un rango de elevación de 470 a 3000 m. Se presenta una clave para la identificación de las especies basada esencialmente en la morfología del primer gonopodo del macho y de los pereopodos.

AEROMICROBIOLOGÍA DEL ARCHIVO CENTRAL DE LA UNIVERSIDAD PEDAGÓGICA Y TECNOLÓGICA DE COLOMBIA (TUNJA-BOYACÁ

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Deisy Lisseth Toloza Moreno

2011-01-01

Full Text Available La calidad del aire de los ambientes internos puede estar influenciada por distintas partículas suspendidas en la atmósfera (polvo, polen, bacterias, hongos, virus que pueden causar daños sobre los documentos y causar reacciones alérgicas sobre las personas que trabajan con éstos. Con este trabajo, se identificaron los microorganismos presentes en el ambiente del archivo central de la Universidad Pedagógica y Tecnológica de Colombia, que podrían causar alergias respiratorias en los trabajadores de esta área. Para las muestras de ambiente se empleó el método de sedimentación en placa utilizando Agar Papa Dextrosa, y se midió la temperatura y humedad relativa durante cada muestreo. Asimismo, se aplicó una encuesta a los trabajadores con el fin de conocer la sintomatología respiratoria sugestiva que podrían presentar por el manejo de los documentos y se tomaron muestras de fosas nasales a algunos de ellos. Se aislaron del ambiente 16 géneros entre hongos, levaduras y bacterias. Los géneros fúngicos predominantes fueron Mucor sp. y Penicillium sp., con un 36,6% y 27,5% respectivamente del total de colonias aisladas. Las formas levaduriformes y bacterianas fueron aisladas en menor proporción. No se encontró una correlación estadísticamente significativa entre el promedio de unidades formadoras de colonia con la temperatura y humedad relativa del ambiente. Además, en las muestras de fosas nasales solo se encontró flora normal de la nariz, lo cual indica que los síntomas respiratorios sugestivos que presentan los trabajadores no están influenciados directamente por la presencia de esporas de hongos en el ambiente del archivo central.

How do two Lupinus species respond to temperature along an altitudinal gradient in the Venezuelan Andes? ¿Cómo responden dos especies de Lupinus a la temperatura en un gradiente altitudinal en los Andes venezolanos?

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FERMÍN RADA

2008-09-01

Full Text Available Temperature determines plant formations and species distribution along altitudinal gradients. Plants in the tropical high Andes, through different physiological and morphological characteristics, respond to freezing night temperatures and high daytime energy inputs which occur anytime of the year. The main objective of this study was to characterize day and night temperature related responses of two Lupinus species with different altitudinal ranges (L. meridanus, 1,800-3,600 and L. eromonomos, 3,700-4,300 m of altitude. Are there differences in night low temperature resistance mechanisms between the species along the gradient? How do these species respond, in terms of optimum temperature for photosynthesis, to increasing altitude? Lupinus meridanus shows frost avoidance, in contrast to L. eromonomos, which tolerates freezing at higher altitudes. Optimum temperature for photosynthesis decreases along the gradient for both species. Maximum C0(2 assimilation rates were higher in L. meridanus, while L. eromonomos showed decreasing C0(2 assimilation rates at the higher altitude. In most cases, measured daily leaf temperature is always within the 80 % of optimum for photosynthesis. L. meridanus7 upper distribution limit seems to be restricted by cold resistance mechanisms, while L. eromonomos7 to a combination of both cold resistance and to C0(2 assimilation responses at higher altitudes.La temperatura determina las formaciones vegetales y la distribución de especies a lo largo de gradientes altitudinales. Las plantas en los altos Andes tropicales, a través de diferentes características morfológicas y fisiológicas, responden a temperaturas congelantes nocturnas y altas entradas energéticas durante el día en cualquier momento del año. El objetivo principal de este estudio fue caracterizar las respuestas relacionadas con temperaturas diurnas y nocturnas en dos especies de Lupinus con diferente distribución altitudinal (L. meridanus, 1

Distribución geográfica de Boeckella y Neoboeckella (Calanoida: Centropagidae en el Perú

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Iris Samanez

2014-12-01

Full Text Available El análisis de muestras de plancton colectadas en diferentes localidades a lo largo de los Andes peruanos, dieron como resultado el registro de siete especies de Boeckella (gracilis, gracilipes, calcaris, poopoensis, occidentalis, titicacae y palustris y dos de Neoboeckella (kinzeli y loffleri. Todas las especies citadas, exceptuando a las especies de Neoboeckella, fueron registradas en la cuenca del lago Titicaca (Puno. Además, B. palustris, B. gracilipes y B. calcaris fueron también reportadas en Moquegua, Apurímac y Pasco (Andes del sur y central. Boeckella titicacae parece estar restringida a la cuenca del lago Titicaca. Boeckella poopoensis ocurre en cuerpos de agua con elevada conductividad reportándose sólo en Las Salinas en Arequipa. Boeckella occidentalis fue la especie con mayor rango de distribución desde el sur en Puno hasta el norte en Cajamarca y se registra por primera vez para el país Neoboeckella loffleri. Las muestras están depositadas en la Colección de Plancton del Departamento de Limnología del Museo de Historia Natural de la Universidad Nacional Mayor de San Marcos, Lima-Perú.

Glacier loss and hydro-social risks in the Peruvian Andes

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Mark, Bryan G.; French, Adam; Baraer, Michel; Carey, Mark; Bury, Jeffrey; Young, Kenneth R.; Polk, Molly H.; Wigmore, Oliver; Lagos, Pablo; Crumley, Ryan; McKenzie, Jeffrey M.; Lautz, Laura

2017-12-01

Accelerating glacier recession in tropical highlands and in the Peruvian Andes specifically is a manifestation of global climate change that is influencing the hydrologic cycle and impacting water resources across a range of socio-environmental systems. Despite predictions regarding the negative effects of long-term glacier decline on water availability, many uncertainties remain regarding the timing and variability of hydrologic changes and their impacts. To improve context-specific understandings of the effects of climate change and glacial melt on water resources in the tropical Andes, this article synthesizes results from long-term transdisciplinary research with new findings from two glacierized Peruvian watersheds to develop and apply a multi-level conceptual framework focused on the coupled biophysical and social determinants of water access and hydro-social risks in these settings. The framework identifies several interacting variables-hydrologic transformation, land cover change, perceptions of water availability, water use and infrastructure in local and regional economies, and water rights and governance-to broadly assess how glacier change is embedded with social risks and vulnerability across diverse water uses and sectors. The primary focus is on the Santa River watershed draining the Cordillera Blanca to the Pacific. Additional analysis of hydrologic change and water access in the geographically distinct Shullcas River watershed draining the Huaytapallana massif towards the city of Huancayo further illuminates the heterogeneous character of hydrologic risk and vulnerability in the Andes.

Central Park y la producción del espacio público: el uso de la ciudad y la regulación del comportamiento urbano en la historia

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Álvaro Sevilla-Buitrago

2014-09-01

Full Text Available Los debates contemporáneos sobre el eclipse del espacio público suelen ofrecer una visión idealizada de su pasado, impidiendo una correcta reconsideración del papel que las técnicas urbanísticas han tenido en la producción y evolución del mismo. Contribuyendo al desarrollo de una historia crítica que subsane estas lagunas, Central Park se presenta aquí como un dispositivo gubernamental ideado para sustituir el régimen de uso del espacio público habitual en las calles de Manhattan a mediados del siglo XIX, por un nuevo conjunto de prácticas espaciales definidas y monitorizadas por el Estado. Tras una descripción de las formas de apropiación espontánea de la calle por parte de las clases populares, se analizan los distintos niveles proyectuales en los cuales se articulaba esta estrategia de domesticación del espacio público: del propio diseño espacial y concepción de la red de lugares del parque, a la regulación normativa del uso y comportamiento de los visitantes, al ejercicio activo de vigilancia y castigo de conductas y sujetos indeseables.

Craniofacial chronological microdifferentiation of human prehistoric populations of the Azapa valley, northern Chile Microdiferenciación cronológica craneofacial de poblaciones humanas prehistóricas del Valle de Azapa, norte de Chile

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FRANCISCO ROTHHAMMER

2002-03-01

Full Text Available Archeological evidence suggest that the cultural developments occurred in the highlands around lake Titicaca in the Central Andes, exerted influence on the cultural elaborations of the human groups that peopled the valley of Azapa, close to the city of Arica, and the Pacific coast of northern Chile. In this communication we show by means of a distance analysis, that a craniofacial differentiation accompanied the process of cultural evolution in the valley. The biological influence of Tiwanaku is partially reflected in craniofacial morphology, providing preliminary evidence that cultural changes were associated to intermittent gene flow from the highlands, specially during the Alto Ramírez and San Miguel phasesLos desarrollos culturales ocurridos en el altiplano en el área circumtiticaca en los Andes centrales, ejercieron influencia sobre las elaboraciones culturales de los grupos humanos que poblaban el Valle de Azapa cercano a la ciudad de Arica y la costa del norte de Chile. En esta comunicación presentamos un análisis de distancias que demostró que una diferenciación craniofacial acompaño en el valle el proceso de evolución cultural. La influencia biológica de Tiwanaku se refleja parcialmente en la morfología craniofacial, proporcionando evidencia preliminar de que los cambios culturales en el valle se realizaron acompañados de flujo génico intermitente desde el altiplano, especialmente durante las fases Alto Ramírez y San Miguel

Orden monetario y bancos centrales Monetary order and Central Banks

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Aglietta Michel

1996-06-01

Full Text Available Con el enfoque evolucionista e institucionalista de la economía de las convenciones francesa, este trabajo analiza el surgimiento histórico de la banca central y la creación institucional del 'arte de la banca central'. El artículo estudia los modelos formales del orden monetario, la banca libre y la banca central, y analiza los eventos históricos que llevaron a que el Banco de Inglaterra inventara el arte de manejar los bancos centrales en conjunción con el aprendizaje colectivo e institucional que lo hizo posible. Aglietta muestra que la banca central no es una creación del Estado sino una creación institucional endógena al sistema de mercado.With the evolutionist and institutionalist focus of the economics of the French conventions, this paper analyzes the historical rise of the central bank and the institutional creation of the 'art of the central bank'. The article studies formal models of the monetary order, free banking and the central bank, and analyzes the historie events that led to the Bank of England inventing the art of managing the central banks, in conjunction with the collective and institutional learning that made it possible. Aglietta shows that the central bank is not a creation of the State, but rather aninstitutional creation endogenous to the market system.

Dynamics of a Puelche foehn event in the Andes

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Lea Beusch

2018-01-01

Full Text Available In this numerical modelling study, we investigate a Puelche foehn event (25–26 March 2014 in the southern Andes – a region with sparse observations. The synoptic environment as well as the mesoscale structure and the dynamics of the easterly wind are examined with European Centre for Medium-Range Weather Forecasts (ECMWF analyses and a simulation with the mesoscale non-hydrostatic limited-area weather prediction model COSMO with a grid spacing of 2.2 km.The large-scale synoptic situation leading to this Puelche event is characterized by a mid-tropospheric cut-off low above the mountain range, the formation of a coastal surface low, as well as high pressure extending over the southern Andes. Easterly winds extend throughout the entire troposphere, indicative of a deep foehn flow. In the free troposphere, the easterlies are geostrophically balanced and develop in association with increasing pressure to the south. In contrast, within the planetary boundary layer, the easterly winds occur predominantly due to an increasing cross-range large-scale pressure gradient with only a weak geostrophic component. Kinematic trajectories indicate that a significant part of the Puelche air mass originates from above an inversion on the upstream side of the Andes. Some air parcels, however, ascend on the upstream side to crest height as the boundary layer deepens during daytime and/or flow through gaps across the mountain range. Hence, this Puelche event shares characteristics of both a blocked and a non-blocked foehn type.

Paleozoic evolution of active margin basins in the southern Central Andes (northwestern Argentina and northern Chile)

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Bahlburg, H.; Breitkreuz, C.

The geodynamic evolution of the Paleozoic continental margin of Gondwana in the region of the southern Central Andes is characterized by the westward progression of orogenic basin formation through time. The Ordovician basin in the northwest Argentinian Cordillera Oriental and Puna originated as an Early Ordovician back-arc basin. The contemporaneous magmatic arc of an east-dipping subduction zone was presumably located in northern Chile. In the back-arc basin, a ca. 3500 meter, fining-up volcaniclastic apron connected to the arc formed during the Arenigian. Increased subsidence in the late Arenigian allowed for the accomodation of large volumes of volcaniclastic turbidites during the Middle Ordovician. Subsidence and sedimentation were caused by the onset of collision between the para-autochthonous Arequipa Massif Terrane (AMT) and the South American margin at the Arenigian-Llanvirnian transition. This led to eastward thrusting of the arc complex over its back-arc basin and, consequently, to its transformation into a marine foreland basin. As a result of thrusting in the west, a flexural bulge formed in the east, leading to uplift and emergence of the Cordillera Oriental shelf during the Guandacol Event at the Arenigian-Llanvirnian transition. The basin fill was folded during the terminal collision of the AMT during the Oclóyic Orogeny (Ashgillian). The folded strata were intruded post-tectonically by the presumably Silurian granitoids of the "Faja Eruptiva de la Puna Oriental." The orogeny led to the formation of the positive area of the Arco Puneño. West of the Arco Puneño, a further marine basin developed during the Early Devonian, the eastern shelf of which occupied the area of the Cordillera Occidental, Depresión Preandina, and Precordillera. The corresponding deep marine turbidite basin was located in the region of the Cordillera de la Costa. Deposition continued until the basin fill was folded in the early Late Carboniferous Toco Orogeny. The basin

Tratamiento del dolor neuropático central; futuras terapias analgésicas: revisión sistemática

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R. Mora Moscoso; M. Guzmán Ruiz; A.M. Soriano Pérez; R. de Alba-Moreno

2014-01-01

Introducción: el dolor neuropático central (DNC) es aquel causado por una lesión primaria o disfunción del sistema nervioso central que genera una patología incapacitante, difícil de reconocer y tratar. Las causas más frecuentes son accidente cerebrovascular (ACV), esclerosis múltiple y lesión medular traumática. Objetivos: realizar revisión sistemática de las principales causas de dolor neuropático central, presentar evidencia de la efectividad y tolerabilidad de las opciones terapéuticas ac...

Ingeniería de Sistemas y Computación: Una utopía realizada en la Universidad de los Andes

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2010-12-01

Full Text Available Entre las tarjetas perforadas, las reglas de cálculo, los libros de Fortran y Cobol, y los cursos de algoritmos, sistemas de información y teoría de juegos, los jóvenes Alfredo Amore, Xavier Caicedo y Diego Escobar recibieron el 28 de agosto de 1970 su grado como los primeros Ingenieros de Sistemas y Computación del país. Por la celebración de su aniversario 40, la Revista de Ingeniería se propone hacer memoria sobre el proceso de creación de este programa y sus primeros egresados, pues constituyen un hito determinante en la historia de la ingeniería colombiana, gestado desde la Universidad de los Andes.

Tipos de vegetación del llano de Paletará. Cordillera Central Colombia Tipos de vegetación del llano de Paletará. Cordillera Central Colombia

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Restrepo Carla

1992-09-01

Full Text Available We studied the vegetation found in the Llano de Paletará, municipality of Coconuco, department of Cauca, Colombia. Based on the physiognomy and floristic composition of the vegetation we identified 8 paramo vegetation types. These units represent the most extensive azonal paramo vegetation types described up to now for the Cordillera Central. Four of the 8 vegetation types are herbaceous ("frailejonal-pajonal" with Espeletia, "chuscal abierto" with Chusquea,"swamp" with Carex, and "grassland" with Calamagrostis , three are bush tickets (thicket with Hypericum, thicket with Ageratina, and thicket with Diplostephium, and one is a forest of low stature (forest with Escallonia. We analyze some aspects of the ecology and distribution of the vegetation types and evaluate their degree of peril and value of conservation. Se estudiaron los tipos de vegetación del Llano de Paletará, municipio de Coconuco, departamento del Cauca, Colombia. Basados en la fisonomía y composición florística de la vegetación identificamos 8 tipos de vegetación, los cuales representan los tipos de vegetación paramunos de carácter azonal más extensos de la Cordillera Central registrados hasta el momento. De los 8 tipos de vegetación, cuatro son de porte herbáceo (''frailejonalpajonal'' con Espeletia. "chuscal abierto" con Chusquea. "pantano" con Carex y un "pajonal" con Calamagrostis, tres son de porte arbustivo (matorral con Hypericum, matorral con Ageratina y matorral con Diplostephium y uno es de porte arbóreo (bosque con Escallonia. Se analizan algunos aspectos de la ecología y distribución de los tipos de vegetación y se evalúa su grado de amenaza y valor de conservación.

Glosario selecto

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Lamb, Simon

2015-01-01

Roca acídica.- Roca ígnea que contiene más del 63% del peso en silicato -el granito o riolita son ejemplos típicos. Altiplano.- La ancha parte central de los Andes en Perú, Chile, Bolivia y Argentina, que forma una meseta con relieves a una altura general de 4 000 metros sobre el nivel del mar. Andesita.- Una roca volcánica de grano fino de feldespato, piroxina y a veces cuarzo, amfíbolo y olivina 45se define su composición como intermedia. Anomalía de aire libre.- La diferencia entre el valo...

Rapid Diversification and Time Explain Amphibian Richness at Different Scales in the Tropical Andes, Earth's Most Biodiverse Hotspot.

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Hutter, Carl R; Lambert, Shea M; Wiens, John J

2017-12-01

The Tropical Andes make up Earth's most species-rich biodiversity hotspot for both animals and plants. Nevertheless, the ecological and evolutionary processes underlying this extraordinary richness remain uncertain. Here, we examine the processes that generate high richness in the Tropical Andes relative to other regions in South America and across different elevations within the Andes, using frogs as a model system. We combine distributional data, a newly generated time-calibrated phylogeny for 2,318 frog species, and phylogenetic comparative methods to test the relative importance of diversification rates and colonization times for explaining Andean diversity at different scales. At larger scales (among regions and families), we find that faster diversification rates in Andean clades most likely explain high Andean richness. In contrast, at smaller temporal and spatial scales (within family-level clades within the Andes), diversification rates rarely explain richness patterns. Instead, we show that colonization times are important for shaping elevational richness patterns within the Andes, with more species found in habitats colonized earlier. We suggest that these scale-dependent patterns might apply to many other richness gradients. Recognition of this scale dependence may help to reconcile conflicting results among studies of richness patterns across habitats, regions, and organisms.

El deslizamiento de rocas y detritos sobre elrío Santa Cruz y el aluvión resultante por el colapso del dique natural, AndesCentrales de San Juan

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Laura Perucca; Yanina Esper

2009-01-01

Durante el verano de 2005 un gran deslizamiento derocas y detritos ubicado en la ladera occidental de la Cordillera de Santa Cruzobturó el valle del río Santa Cruz, en el sudeste de la provincia de San Juan(31º40'12''S; 70º16'18''O). Este deslizamiento originó una presa natural en laquebrada del río y formó un lago de volumen considerable. El 12 de noviembre de2005, probablemente por la enorme presión generada por la masa de agua contrala presa, se produjo el colapso parcial del dique natural...

Aspectos que influyen en las estrategias de marketing de distribución y publicidad en Huancayo, Perú

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José Maria Matas Castañeda

2013-06-01

Full Text Available El propósito de este artículo es analizar la situación actual de las principales estrategias de marketing en las variables de distribución y comunicación de Huancayo, capital del departamento de Junín, una de las más importantes zonas de los Andes Centrales del Perú. Esta región tiene como ciudad próxima de importancia a la ciudad de Lima, la capital peruana, que se encuentra a unas ocho horas con los medios de transporte actuales, después de atravesar los Andes y llegar hasta la costa. La mayoría de carreteras en los Andes y hasta la selva han sido sin asfaltar y complicadas aun los últimos años, por lo que el desplazamiento entre ciudades lo hacían pocas personas. Ello explica que tenga formas de distribución y comunicación propias. La llegada del primer centro comercial y la utilización de medios digitales están transformando las formas tradicionales de distribución y comunicación. El trabajo también analiza cómo se manifiesta la variable de comunicación en el marketing mix de las empresas huancaínas y cómo han influido la llegada de los medios digitales.

Viticultura tropical a gran altitud. Condiciones y expresiones del terroir

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Marco Quijano Rico

2009-01-01

Nuestro proyecto se inició en 1982 en la Loma de Puntalarga, entre 2500 y2600 metros de altitud, a 5,78 ºN y 72,98 ºW, en la cordillera oriental de los Andes. Las variedades más utilizadas actualmente son Pinot noir, Riesling y cruzamientos de Riesling x Silvaner. Desde 1984 se realizan trabajos de investigación sobre temas pertinentes. La baja latitud, la elevada altitud, el volumen de precipitación relativamente modesto y la transparencia del cielo, determinan el flujo de radiación solar in...

Developing services for climate impact and adaptation baseline information and methodologies for the Andes

Science.gov (United States)

Huggel, C.

2012-04-01

Impacts of climate change are observed and projected across a range of ecosystems and economic sectors, and mountain regions thereby rank among the hotspots of climate change. The Andes are considered particularly vulnerable to climate change, not only due to fragile ecosystems but also due to the high vulnerability of the population. Natural resources such as water systems play a critical role and are observed and projected to be seriously affected. Adaptation to climate change impacts is therefore crucial to contain the negative effects on the population. Adaptation projects require information on the climate and affected socio-environmental systems. There is, however, generally a lack of methodological guidelines how to generate the necessary scientific information and how to communicate to implementing governmental and non-governmental institutions. This is particularly important in view of the international funds for adaptation such as the Green Climate Fund established and set into process at the UNFCCC Conferences of the Parties in Cancun 2010 and Durban 2011. To facilitate this process international and regional organizations (World Bank and Andean Community) and a consortium of research institutions have joined forces to develop and define comprehensive methodologies for baseline and climate change impact assessments for the Andes, with an application potential to other mountain regions (AndesPlus project). Considered are the climatological baseline of a region, and the assessment of trends based on ground meteorological stations, reanalysis data, and satellite information. A challenge is the scarcity of climate information in the Andes, and the complex climatology of the mountain terrain. A climate data platform has been developed for the southern Peruvian Andes and is a key element for climate data service and exchange. Water resources are among the key livelihood components for the Andean population, and local and national economy, in particular for

Determinantes del acceso a los productos financieros en los hogares colombianos

OpenAIRE

Santiago Rodríguez-Raga; Félix Francisco Riaño Rodríguez

2016-01-01

Existe evidencia que establece una asociación positiva entre el acceso a productos financieros, la riqueza y calidad de vida de los hogares, en especial de los hogares pobres. En este ámbito, este estudio busca entender los determinantes del acceso a los diferentes productos financieros en los hogares de Colombia, utilizando un modelo econométrico con base en la información contenida en la Encuesta Longitudinal Colombiana (ELCA) de la Universidad de los Andes. Como conclusión se encuentra que...

La Cordillera de los Andes: presentación de los problemas geomorfológicos

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1974-01-01

érites sont souvent déblayées sur les pentes fortes par le ruissellement et les divers glissements et éboulements. El alzamiento en bóveda del Ponto-plioceno ha dado a los .Andes su volumen montañoso actual y ha llevado a más de 4000 m superficies de erosión elaboradas durante e! Terciario. Estas superficies o 'puna' son muy probablemente poligénicas y policíclicas. Están dominadas por grandes cordilleras que son generalmente horsts que delimitan los sectores de surrección máxima, horsts que son posteriores a la elaboración de la superficie de las mesetas. Esta superficie está deformada tanto sobre los bordes de las cuencas interiores como sobre los flancos de la montaña donde ella ha sido disectada y reducida a bandas. Algunas veces esta superficie ha podido desaparecer debido a su recorte en lo alto de los flancos de los grandes valles, sobretodo en los dos extremos de la cadena. A un nivel inferior, se desarrollaron aplanamientos menores durante el Plioceno y posiblemente durante el Cuaternario antiguo, en sectores que habían permanecido relativamente estables: son los 'glacis' de erosión en lazos del altiplano perú-boliviano o las superficies de abrasión retocadas en 'glacis' sobre los abombamientos costeros perú-chilenos. Algunos grandes valles están adaptados a las grandes direcciones estructurales consecutivas a los movimientos del fin de Terciario (la adaptación del conjunto va acompañada a menudo de numerosas inadaptaciones locales. Otros valles siguen antiguas direcciones estructurales, anteriores al alzamiento andino. El Cuaternario está marcado por una serie de períodos fríos acompañados de glaciaciones en la montaña. Se ha podido determinar lar existencia de cuatro glaciaciones distintas de las cuales una al menos remonta al Cuaternario antiguo. Las glaciaciones recientes son contemporáneas de las glaciaciones del Cuaternario reciente de Europa y de América del Norte. Sus causas hay que buscarlas, para las latitudes medias, en un

Black carbon and other light-absorbing impurities in the Andes of Northern Chile

Science.gov (United States)

Rowe, P. M.; Cordero, R.; Warren, S. G.; Pankow, A.; Jorquera, J.; Schrempf, M.; Doherty, S. J.; Cabellero, M.; Carrasco, J. F.; Neshyba, S.

2015-12-01

Black carbon (BC) and other light-absorbing impurities in snow absorb solar radiation and thus have the potential to accelerate glacial retreat and snowmelt. In Chile, glaciers and seasonal snow are important sources of water for irrigation and domestic uses. In July 2015 (Austral winter) we sampled snow in the western Andes in a north-south transect of Chile from 18 S to 34 S. Most of the sampled snow had fallen during a single synoptic event, during 11-13 July. The snow was melted and passed through 0.4 micrometer nuclepore filters. Preliminary estimates indicate that (1) the ratio of BC to dust in snow increases going south from Northern to Central Chile, and (2) in snow sampled during the two weeks following the snowstorm, the impurities were concentrated in the upper 5 cm of snow, indicating that the surface layer became polluted over time by dry deposition.

Colobanthus Quitensis (H.B.K. Bartl. (Caryophyllaceae en los Andes Colombianos

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Aguirre C. Jaime

1982-04-01

Full Text Available Colobantbus quitensis y Deschampsia antarctica son las dos únicas fanerogamas nativas presentes hoy dia en el continente antártico (Green, 1970. La primera tiene una distribución amplia en regiones templadas y frías de América Latina, desde la Tierra del Fuego hasta México (Moore, 1972.  En noviembre de 1978 se realizó una exploración geobotánica corta al Páramo Alto del Almorzadero en la Cordillera Oriental, Departamento de Santander; en el piso pantanoso de un vallecito a 3.900 m (El Tutal se encontraron algunas maticas dispersas de Colobanthus quitensis (biótipo laxa cerca de una corriente lenta de agua. El hallazgo anterior de Colobanthus quitensis en la región del Nevado del Ruiz en la Cordillera Central motivó la elaboración del presente trabajo, con el fin de dar a conocer los caracteres morfológicos, palinológicos y sociológicos de esta interesante especie.

Acceso y apropiación del agua en comunidades rurales pobres de Argentina central. Transformaciones y conflictos

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Daniel M. Cáceres

2014-01-01

Full Text Available Basado en un estudio de caso en Argentina central, esta investigación formula conceptualizaciones tendientes a comprender las estrategias de apropiación del agua rural; asimismo, analiza cómo las recientes transformaciones socioproductivas influyen en su apropiación y, finalmente, discute sus probables consecuencias sociales. Los resultados sugieren que el avance de la expansión del capitalismo agrario debilita la autonomía de los campesinos y pobladores pobres para acceder al agua con fines de consumo humano o productivo. Esto consolida la posición subordinada de los pobres rurales y la inequidad estructural de estos territorios, aumentando su vulnerabilidad ante prácticas clientelares. Por su parte, los productores capitalizados son más exitosos al apropiarse del agua rural.

Records of new or poorly known migratory birds from Laguna del Otun, Los Nevados National Natural Park, Risaralda, Colombia

International Nuclear Information System (INIS)

Acevedo Charry, Orlando; Matta Camacho, Nubia E; Moncada Alvarez, Ligia Ines

2013-01-01

Colombia is important for migratory birds. Despite this, we do not know where they are during their crossing or residency in the country, and which species use paramo. We registered new migratory bird species for Laguna Del Otun, immersed in a complex of wetlands declared a Ramsar site since 2008. The lagoon is located in the Los Nevados National Natural Park at 3932 m asl, in paramo ecosystems of the Central Andes of Colombia. During five field trips between 2010-2012 we recorded four new migratory bird species for the park: Anas acuta, Pandion haliaetus, Riparia riparia, and Dendroica petechia. We also registered an altitudinal range extension for two additional migratory species which had only been recorded below 3500 m: Tringa flavipes and Hirundo rustica. These findings suggest these species could tolerate high mountain conditions and use the paramo. It's needed inquiry about migratory dynamics and high mountain habitat use by migratory birds.

Germán Rodríguez Arias y el cine central de Chillán (1945. Una historia del exilio catalán en Chile

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David Caralt

2011-08-01

El presente artículo reivindica la figura de Rodríguez Arias y su aportación a la historia de la arquitectura chilena, explica su llegada a Chile y los motivos del encargo del Cine Central en base a una aproximación desde lo específico de la “arquitectura del exilio”. La parte final del texto se concentra en el discurrir del edificio y su estado actual de conservación.

Diversidad y dinámica de un bosque subandino de altitud en la región norte de los Andes colombianos

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Jesús Oswaldo Velásquez Restrepo

2012-06-01

Full Text Available Los bosques sub-Andinos poseen alta diversidad biológica, de los cuales poco se conoce sobre su dinámica natural. Se evaluaron patrones de diversidad y biomasa, tasas de mortalidad y reclutamiento en dos parcelas permanentes de una hectárea cada una, establecidas en bosques en altitudes entre los 2 000-2 200msnm, en la vertiente Oriental de la cordillera Occidental del norte de los Andes en Colombia. Se determino diversidad de especies mediante el índice alpha de Fisher, la dinámica del bosque se evaluó mediante tres censos durante nueve anos. En total, se hallaron 1 964 individuos con un diámetro a la altura del pecho DAP≥10cm. pertenecientes a 222 especies, 113 géneros y 60 familias. La riqueza media de especies fue de 156 especies por hectárea y un índice alpha medio de Fisher de 56.2/h. Las tasas de mortalidad y reclutamiento fueron de 0.88% y 1.16% respectivamente, lo cual no indica que se presente un efecto externo proveniente del calentamiento global sobre la dinámica del bosque. La biomasa aérea promedio fue de 243.44±9.82tn/ha con un incremento anual promedio de 2.9ton/ha, valor superior a los reportados, lo cual sugiere que el equilibrio para este bosque no se ha alcanzado. De acuerdo con las observaciones de campo, este bosque parece estar recuperándose de una alteración pasada.

Lineamientos de un plan estratégico para el mejoramiento de la calidad del servicio brindado en el Hospital Militar Central de Lima

OpenAIRE

Cabrera Rioja, Luis Alberto

2007-01-01

El presente estudio, realizado en el Hospital Militar Central (HMC) de Lima, está dirigido al diseño de los lineamientos de un plan estratégico que permita formular la misión y visión del HMC, analizar el entorno e intorno organizacional y formular objetivos estratégicos orientados al mejoramiento continuo de la calidad del servicio. A fin de superar las dificultades económicas, logísticas y de personal que afronta actualmente el Hospital Militar Central, debido a los recortes presupuestales ...

Distributional patterns of cecropia (Cecropiaceae: a panbiogeographic analysis

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Franco Rosselli Pilar

1997-06-01

Full Text Available A panbiogeographic analysis of the distributional patterns of 60 species of Cecropia was carried out. Based on the distributional ranges of 36 species, we found eight generalized tracks for Cecropia species. whereas distributional patterns of 24 species were uninformative for the analysis. The major concentration of species of Cecropia is in the Neotropical Andean region. where there are three generalized tracks and two nodes. The northern Andes in Colombia and Ecuador are richer than the Central Andes in Perú. they contain two generalized tracks; one to the west and another to the east, formed by individual tracks of eight species each. There are four generalized tracks outside the Andean region: two in the Amazonian region in Guayana-Pará and in Manaus. one in Roraima. one in Serra do Mar in the Atlantic forest of Brazil and one in Central America. Speciation in Cecropia may be related to the Andean first uplift.Con base en la distribución de 60 especies del género Cecropia, se hizo un análisis panbiogeográfico. Se construyeron 8 trazos generalizados con base en el patrón de distribución de 36 especies; la distribución de las demás especies no aportaba información para la definición de los trazos. La región andina tiene la mayor concentración de especies de Cecropia representada por la presencia de tres trazos generalizados y dos nodos; los dos trazos con mayor número de especies se localizan en su parte norte, en Colombia y Ecuador y el otro en los Andes centrales en Perú. Se encontraron además, cuatro trazos extrandinos: dos en la región amazónica, en Pará-Guayana y en Manaus, uno en Roraima, uno en Serra do Mar en la Selva Atlánfíca del Brasil y uno en Centro América. La especiación en Cecropia parece estar relacionada con el primer levantamiento de los Andes.

Hallazgos citogenéticos en los pacientes de la Unidad de Genética Médica de la Universidad de Los Andes en Mérida, Venezuela

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Dionora Araque

2013-09-01

Full Text Available El siguiente estudio tiene por finalidad identificar los hallazgos citogenéticos en los pacientes de la Unidad de Genética Médica de la Universidad de Los Andes, en Mérida, Venezuela, para determinar la prevalencia y tipo de alteraciones cromosómicas. Se realizó un estudio observacional, descriptivo y de corte transversal, en los pacientes evaluados desde enero de 2005 a enero de 2012. El estudio citogenético fue realizado por técnica convencional de banda G. De un total de 716 estudios citogenéticos realizados, 113 (15,78% presentaron algún tipo de alteración de los cromosomas autosómicos y la trisomía 21 fue la más frecuente con 95 (84,07%; 71 (9,92% de los cromosomas sexuales y la monosomía del X fue la más común con 67 (94,37%. La trisomía 21 constituye el principal tipo de alteración cromosómica en este estudio y los revisados, siendo la trisomía libre la forma más común. La monosomía del X constituye la segunda anormalidad cromosómica y la primera de los cromosomas sexuales, resaltando la alta frecuencia de mosaicismo con una línea celular con monosomía del X y otra línea celular normal. Es pertinente difundir la importancia del análisis citogenético en la práctica médica, como recurso útil en estudio de pacientes con alteraciones cromosómicas. Cytogenetic findings in the patients of the Unit of Medical Genetics University of Los Andes, in Mérida, Venezuela Abstract The following study aims to identify the cytogenetic findings in the patients of the Unit of Medical Genetics of the University of Los Andes in Merida, Venezuela to determine the prevalence and type of chromosomal abnormalities. An observational, descriptive and cross-sectional study was performed in the patients evaluated from january 2005 to january 2012. The cytogenetic study was realized by conventional technique G-banding. A total of 716 of cytogenetic studies performed, 113 (15,78% had some type of alteration of autosomal chromosomes and

Reproducción del pez erizo, Diodon holocanthus (Pisces: Diodontidae en la plataforma continental del Pacífico Central Mexicano

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Gabriela Lucano-Ramírez

2011-03-01

Full Text Available Diodon holocanthus es una especie con cierta importancia comercial y ecológica en la comunidad de peces que forma la fauna de acompañamiento del camarón en la plataforma continental del Pacífico central Mexicano, y de la cual no se conocen aspectos reproductivos. Por lo cual se obtuvieron el periodo de reproducción, la descripción macro y microscópica de las gónadas, además de variables poblacionales como: distribución de tallas, proporción sexual y talla de madurez. En total se capturaron alrededor de 400 organismos, los cuales presentaron una talla mínima de 5.0cm, máxima de 40.3cm y promedio de 18.4cm, y fueron capturados en la plataforma continental en el Pacífico central Mexicano, desde diciembre de 1995 a diciembre de 1998. La proporción sexual fue de 1:0.86 hembras por machos (n=253. La talla a la cual el 50% de individuos presentó gónadas maduras fue 19.7cm en las hembras y 20.1cm en los machos. Los organismos con las menores tallas que presentaron gónadas en fase de maduración midieron 12.2cm (hembras y 13cm (machos. En ambos sexos el desarrollo de la gónada se determinó con base en una escala de maduración de cuatro estadios. En el proceso de maduración de los ovocitos se identificaron cinco fases de desarrollo. El patrón de desarrollo de los ovocitos es de tipo asincrónico, lo que significa que la especie se puede reproducir varias veces al año. El desarrollo del testículo es de tipo lobular como en la mayoría de los peces teleósteos. El índice gonadosomático sugiere que el periodo de reproducción se concentra en los meses de junio, y de septiembre a diciembre.

Actividad microbiológica y biomasa microbiana en suelos cafetaleros de los Andes venezolanos

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Jorge E. Paolini Gómez

2018-01-01

Full Text Available En Venezuela el café (Coffea arabica L. ocupa un área aproximada de 200 000 ha, distribuidos principalmente en las zonas montañosas de Los Andes. Tradicionalmente, el café se cultiva con pocos insumos bajo la sombra de árboles de la familia de las leguminosas y de otros arbustos. En años recientes con la adopción de cultivares de alta productividad, notable precocidad y tamaño reducido se está produciendo café a plena exposición solar con fertilización mineral y uso de pesticidas. Las propiedades microbiológicas del suelo especialmente aquellas relacionadas con el flujo de energía y el reciclaje de nutrientes responden de forma rápida y sensible a los cambios de las condiciones del suelo mucho antes que por ejemplo el carbono orgánico, y de este modo, suministran una información anticipada sobre las alteraciones de la calidad del mismo. En este estudio se comparó la actividad microbiológica (respiración basal, la biomasa microbiana y los parámetros ecofisiológicos en suelos a nivel superficial (0-5 cm de ocho fincas cafetaleras en los municipios de Mérida y Trujillo donde se encuentran tres sistemas de producción: tradicional, convencional y orgánico. Las fincas con agricultura orgánica presentaron los mayores valores de carbono orgánico total, carbono hidrosoluble, respiración basal y biomasa microbiana en comparación con las de manejo tradicional y convencional; con lo cual la producción orgánica es un sistema de manejo más sostenible por la mayor conservación de los recursos naturales y la producción más amigable y armónica con el ambiente. En el caso del manejo convencional, la adición de fertilizantes y pesticidas afecta de forma negativa el bienestar de los microorganismos y los hace más ineficientes en el uso del carbono y la energía.

The Under-side of the Andes: Using Receiver Functions to Map the North Central Andean Subsurface

Science.gov (United States)

Ryan, J. C.; Beck, S. L.; Zandt, G.; Wagner, L. S.; Minaya, E.; Tavera, H.

2012-12-01

The Central Andean Uplift and Geodynamics of High Topography (CAUGHT) project is an interdisciplinary project to investigate connections between lithospheric removal, crustal shortening and surface uplift in the northern Bolivia and southern Peru region of the South American Andean orogen. The central Andes are defined by six major tectonomorphic provinces; the forearc, the volcanically active Western Cordillera (WC, ~6 km elevation), the internally drained Altiplano (~4 km elevation), an inactive fold and thrust belt in the Eastern Cordillera (EC, ~6 km elevation), a lower elevation active fold and thrust belt in the Subandean (SA) zone and the Beni, a foreland basin. Forty seismic stations installed for the CAUGHT project were deployed between 13° and 18° S latitude, covering the transition zone where the Altiplano region pinches out in southern Peru, in an effort to better constrain the changing character of the crust and mantle lithosphere. Geologic studies across the northern Bolivian portion of the eastern Andean margin (15-17° S) have documented a total of 275 km of upper crustal shortening (McQuarrie et al, Tectonics, v27, 2008), which may be associated with crustal thickening and/or the removal of lithospheric material as a thickened lithosphere root becomes unstable. For this receiver function (converted wave) study, we have little coverage in the forearc and foreland, ~75 km spacing in most of the array, and a relatively dense ~20 km spaced profile along the Charaña-La Paz-Yucumo transect, the eastern portion of which is nearly coincident with the balanced cross-section of McQuarrie et al. (2008). Using the first year of available data, more than 1200 receiver functions have been calculated using an iterative deconvolution method, and stacked using the common conversion point (CCP) method, along profiles parallel to and nearly coincident to those used for the geologic shortening estimates. We identified arrivals for the Moho and generated a 3D map of

Murciélagos de cola corta (Carollia: Phyllostomidae del Parque Nacional Natural Gorgona (Colombia y sus implicaciones biogeográficas

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Oscar E Murillo-García

2014-02-01

Full Text Available La identidad de la especie de Carollia (Chiroptera: Phyllostomidae en el Parque Nacional Natural Gorgona ha sido controvertida debido a la alta similitud entre C. perspicillata y C. brevicauda. C. perspicillata es la especie con mayor probabilidad de habitar en la isla debido a que actualmente se distribuye en las tierras bajas de la costa pacífica colombiana, mientras C. brevicauda es una especie predominantemente de tierras altas. Con el objetivo de resolver la controversia acerca de la especie del género Carollia que habita la isla, se realizaron análisis morfométricos con base en característica de cráneos y mandíbulas de especímenes de las dos especies y del PNN Gorgona. Los resultados evidenciaron que, contrario a lo esperado, esta población insular es morfológicamente más similar a C. brevicauda. Evidencia biológica para diferentes grupos de organismos sugiere que Gorgona puede haber estado conectada a los andes y las zonas bajas del pacífico del sur de Colombia-norte de Ecuador en el pasado. Por otra parte, existe evidencia geológica que muestra que Gorgona es la parte más alta de una cordillera (Cordillera de la Costa que se encuentra sumergida actualmente, pero que probablemente fue parte del continente durante el Pleistoceno. Por lo tanto, con base en esta evidencia biológica y geológica se plantea la hipótesis de una ruta de colonización de C. brevicauda a Gorgona desde los Andes a través de la Cordillera de la Costa. Este proceso pudo facilitarse por el descenso marino durante las glaciaciones del Pleistoceno.

Religiosidad popular y heterodoxia en los Andes: El caso del «niño compadrito»

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Fernández Juárez, Gerardo

1998-06-01

Full Text Available There are cults in Andean societies that are alien to the Catholic orthodoxy, yet assimilated as popular manifestations of Catholicism under the tutelage of the Church. The case of "Niño compadrito", venerated in Tambo del Montero, near Plaza de Armas in Cuzco, Perú, illustrates the personality and attributes with which devotees endow holy images in the country. This cult has the characteristic features of the indigenous and Mestizo context in Cuzco to which it belongs.Las sociedades andinas presentan formas de culto peculiares que no encajan con la ortodoxia católica, a pesar de ser tutelarmente asimiladas por aquella como manifestaciones populares de catolicismo. El caso del "niño compadrito", figura venerada en la zona de Tambo del Montero, cerca de la Plaza de Armas del Cuzco (Perú, es un ejemplo más de la personalidad y atribuciones que a las imágenes sagradas otorgan sus devotos. El "niño compadrito" esgrime cualidades propias del dominio mestizo e indígena en que se contextualiza su culto en la ciudad de Cuzco.

Andes hantavirus variant in rodents, southern Amazon Basin, Peru.

Science.gov (United States)

Razuri, Hugo; Tokarz, Rafal; Ghersi, Bruno M; Salmon-Mulanovich, Gabriela; Guezala, M Claudia; Albujar, Christian; Mendoza, A Patricia; Tinoco, Yeny O; Cruz, Christopher; Silva, Maria; Vasquez, Alicia; Pacheco, Víctor; Ströher, Ute; Guerrero, Lisa Wiggleton; Cannon, Deborah; Nichol, Stuart T; Hirschberg, David L; Lipkin, W Ian; Bausch, Daniel G; Montgomery, Joel M

2014-02-01

We investigated hantaviruses in rodents in the southern Amazon Basin of Peru and identified an Andes virus variant from Neacomys spinosus mice. This finding extends the known range of this virus in South America and the range of recognized hantaviruses in Peru. Further studies of the epizoology of hantaviruses in this region are warranted.

Andes Hantavirus Variant in Rodents, Southern Amazon Basin, Peru

OpenAIRE

Razuri, Hugo; Tokarz, Rafal; Ghersi, Bruno M.; Salmon-Mulanovich, Gabriela; Guezala, M. Claudia; Albujar, Christian; Mendoza, A. Patricia; Tinoco, Yeny O.; Cruz, Christopher; Silva, Maria; Vasquez, Alicia; Pacheco, Víctor; Ströher, Ute; Guerrero, Lisa Wiggleton; Cannon, Deborah

2014-01-01

We investigated hantaviruses in rodents in the southern Amazon Basin of Peru and identified an Andes virus variant from Neacomys spinosus mice. This finding extends the known range of this virus in South America and the range of recognized hantaviruses in Peru. Further studies of the epizoology of hantaviruses in this region are warranted.

100 kyr fluvial cut-and-fill terrace cycles since the Middle Pleistocene in the southern Central Andes, NW Argentina

Science.gov (United States)

Tofelde, Stefanie; Schildgen, Taylor F.; Savi, Sara; Pingel, Heiko; Wickert, Andrew D.; Bookhagen, Bodo; Wittmann, Hella; Alonso, Ricardo N.; Cottle, John; Strecker, Manfred R.

2017-09-01

Fluvial fill terraces in intermontane basins are valuable geomorphic archives that can record tectonically and/or climatically driven changes of the Earth-surface process system. However, often the preservation of fill terrace sequences is incomplete and/or they may form far away from their source areas, complicating the identification of causal links between forcing mechanisms and landscape response, especially over multi-millennial timescales. The intermontane Toro Basin in the southern Central Andes exhibits at least five generations of fluvial terraces that have been sculpted into several-hundred-meter-thick Quaternary valley-fill conglomerates. New surface-exposure dating using nine cosmogenic 10Be depth profiles reveals the successive abandonment of these terraces with a 100 kyr cyclicity between 75 ± 7 and 487 ± 34 ka. Depositional ages of the conglomerates, determined by four 26Al/10Be burial samples and U-Pb zircon ages of three intercalated volcanic ash beds, range from 18 ± 141 to 936 ± 170 ka, indicating that there were multiple cut-and-fill episodes. Although the initial onset of aggradation at ∼1 Ma and the overall net incision since ca. 500 ka can be linked to tectonic processes at the narrow basin outlet, the superimposed 100 kyr cycles of aggradation and incision are best explained by eccentricity-driven climate change. Within these cycles, the onset of river incision can be correlated with global cold periods and enhanced humid phases recorded in paleoclimate archives on the adjacent Bolivian Altiplano, whereas deposition occurred mainly during more arid phases on the Altiplano and global interglacial periods. We suggest that enhanced runoff during global cold phases - due to increased regional precipitation rates, reduced evapotranspiration, or both - resulted in an increased sediment-transport capacity in the Toro Basin, which outweighed any possible increases in upstream sediment supply and thus triggered incision. Compared with two

Role of maca (Lepidium meyenii) consumption on serum interleukin-6 levels and health status in populations living in the Peruvian Central Andes over 4000 m of altitude.

Science.gov (United States)

Gonzales, Gustavo F; Gasco, Manuel; Lozada-Requena, Ivan

2013-12-01

Lepidium meyenii (Maca) is a plant that grows at over 4,000 m above sea level in the central Peruvian Andes. The hypocotyls of this plant are traditionally consumed for their nutritional and medicinal properties. The aim of this study was to determine the health status based on a health related quality of life (HRQL) questionnaire (SF-20) and serum levels of interleukin 6 (IL-6) in subjects that are maca consumers. For this, a cross-sectional study was designed to be performed in 50 subjects from Junin (4,100 m): 27 subjects were maca consumers and 23 were non-consumers. The SF-20 survey is used to obtain a summary measure of health status. The stand up from a chair and sit down (SUCSD) test (to assess lower-extremity function), hemoglobin measurement, blood pressure, sexual hormone levels, serum IL-6 levels and the score of chronic mountain sickness (CMS) were evaluated. Testosterone/estradiol ratio (P maca consumers when compared to non-consumers (P maca consumers successfully completed the SUCSD test compared to non-consumers (P maca was associated with low serum IL-6 levels and in turn with better health status scores in the SF-20 survey and low chronic mountain sickness scores.

A further contribution to the knowledge of two inadequately known species of geophilid centipedes from the Andes of South-Central Chile, currently assigned to the genus Plateurytion Attems, 1909 (Chilopoda: Geophilomorpha).

Science.gov (United States)

Pereira, Luis Alberto

2015-10-06

Two poorly known species of geophilid centipedes from the Andes of South-Central Chile, i.e., Plateurytion mundus (Chamberlin, 1955) and Plateurytion zapallar (Chamberlin, 1955) (Myriapoda: Chilopoda: Geophilomorpha), are herein redescribed and illustrated after type specimens of both taxa and new material of the latter, rectifying the condition of the coxosternites of the second maxillae, which are medially joined through a narrow, hyaline and non-areolate membranous isthmus only (instead of "broadly fused as in Pachymerium", as stated by Chamberlin), this being consistent with the current generic assignment of these species under Plateurytion Attems, 1909. New data on many morphological features of specific value, until now unknown, are also given for both taxa. Plateurytion zapallar is reported for the first time from Coquimbo region, 11 Km N of Los Vilos (Elqui province), Valparaíso region, Quebrada Huaquén, Pichicuy (Petorca province), La Campana National Park (Quillota province), and Quebrada el Tigre, Cachagua (Valparíso province). A key for identification of the South American species currently included in Plateurytion is given.

Estudio geológico, estratigráfico y sedimentológico de la Cueva de Mamíferos del Pleistoceno de Santa Rosa (Perú: interpretación paleo-ambiental

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2002-01-01

Full Text Available ÉTUDE GÉOLOGIQUE, STRATIGRAPHIQUE ET SÉDIMENTOLOGIQUE DE LA GROTTE À MAMMIFÈRES PLÉISTOCÈNES DE SANTA ROSA (PÉROU : INTERPRÉTATION PALÉO-ENVIRONNEMENTALE. Les restes d’un spécimen de Megatheriinae (Mammalia: Xenarthra pléistocène (Lujanien viennent d’être mis à jour dans la grotte de Santa Rosa, située dans les Andes Nord-péruviennes. Cette découverte d’un squelette sub-complet de Gravigrade, fait exceptionnel dans les Andes, correspond à une nouvelle espèce du genre Megatherium. L’étude sédimentologique, pétrographique, stratigraphique et palynologique de la grotte montre que la cavité : - appartient à un système karstique (habituel dans cette région des Andes péruviennes creusée dans le calcaire de la formation Celendín (Coniacien - Santonien inférieur - a été soumise à des événements successifs : 1 le creusement de l’abri et le dépôt des sables calcaréo-argileux jaunes suite à la forte érosion du massif calcaire 2 le ravinement et l’érosion amenant des effondrements du toit de l’abri 3 le dépôt des sables calcaréo-argileux marrons où se trouvent les restes de mammifères (Megatheriidae, Camelidae, Cervidae et Muridae et de nombreux restes de flore et la présence locale de pollens. L’analyse pollinique semble indiquer l’existence d’une flore dominée par les fougères d’origine locale et parfois de spores coloniales indifférenciées d’origine vraisemblablement algaire. Ces observations suggèrent que les conditions climatiques étaient plus froides et humides que de nos jours. Restos de un espécimen de Megatheriinae (mammalia: Xenarthra del Pleistoceno superior [Lujanense] han sido descubiertos en la cueva de Santa Rosa, en el norte de los Andes del Perú. Este hallazgo de un esqueleto parcialmente completo de Gravigrado, hecho excepcional en los Andes, corresponde a una nueva especie del género Megatherium. El estudio sedimentológico, petrográfico, estratigráfico y palinol

Comparación de los valores del espesor corneal central según los equipos Lenstar, Galilei y Pentacam Comparative study of the central corneal thickness measurements taken by Lenstar, Gallilei and Pentacam equipment

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Iramis Miranda Hernández

2012-06-01

Full Text Available Objetivo: Comparar valores del espesor corneal central obtenidos mediante la paquimetría con el sistema de interferometria de coherencia parcial (Lenstar con los sistemas Scheimpflug (Pentacam; Oculus y Galilei (Ziemer, Suiza. Métodos: Se realizó un estudio prospectivo, comparativo en 120 ojos de 60 pacientes. Para la comparación se tomaron varias mediciones recomendadas por los fabricantes para probar la eficacia del equipo con el nuevo biómetro Lenstar LS 900 (Haag Streit AG y con los equipos Pentacam y Galilei. La comparación de los valores se realizó mediante el análisis de regresión lineal y correlación de Pearson. Resultados: El análisis reveló que existe una alta correspondencia en los valores del espesor corneal central entre Lenstar y los topógrafos Galilei y Pentacam. Conclusiones: Existe una alta correspondencia entre los valores del espesor corneal central obtenidos por los equipos Lenstar, Pentacam y Galilei. Por esto el equipo Lenstar es útil en la cirugía de catarata y la cirugía refractiva.Objective: To compare the central corneal thickness measurements taken by pachimetry with the partial coherence interferometry, Lenstar and with Scheimpflug systems (Pentacam; Oculus and Galilei (Ziemer, Switzerland. Methods: Comparative and prospective study of 120 eyes from 60 patients. Several recommended measurements were taken with the optical biometers LenstarLS 900 (Haag Streit AG and with Pentacam y Galilei topographers. The results were evaluated using the linear regresión analysis and Pearson´s correlation. Results: There is high correlation among the central corneal thickness measurements taken by the Lenstar equipment and topographers Pentacam and Galilei. Conclusion: The new biometer LENSTAR provided results that correlated very well with those of the Pentacam and Galilei systems. The Lenstar is a precise device that will be helpful for any cataract or refractive surgery.

Valoraciones del profesorado del área de Fresno (California Central sobre la influencia de la tecnología móvil en el aprendizaje de sus estudiantes

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Navaridas, Fermín

2013-10-01

Full Text Available En este artículo se presentan los resultados más relevantes de una investigación en la que se analizan las opiniones del profesorado del área de Fresno (California Central, EEUU respecto a los efectos que tiene el uso de los dispositivos móviles en los procesos de aprendizaje de los estudiantes. Entre otros objetivos, se ha tratado de reconocer la influencia del uso de los dispositivos móviles en tres dimensiones importantes del aprendizaje: la afectivo-emocional (motivación, la ético-social (habilidades sociales y la cognitiva (habilidades cognitivas. Para llevar a cabo el proceso de estudio se adoptó un enfoque metodológico de carácter descriptivo, considerando la técnica de encuesta como el procedimiento más adecuado para recoger la opinión del profesorado de una forma relativamente rápida y precisa. Los resultados obtenidos ponen de manifiesto un acuerdo bastante generalizado del profesorado sobre el potencial pedagógico de la tecnología móvil para mejorar la calidad del aprendizaje. En términos generales, las conclusiones vienen a corroborar un aumento del interés de los estudiantes por la tarea, el incremento de la actividad durante el estudio, un trabajo más colaborativo, así como la mejora de la creatividad y el proceso de adquisición de información de los estudiantes.

Luchas y defensas escondidas. Pluralismo legal y cultural como una práctica de resistencia creativa en la gestión local del agua en los Andes

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Boelens, R.A.

2011-01-01

En los Andes, los derechos de agua se materializan en procesos de lucha social. El artículo examina cómo la lucha por el agua de los colectivos locales no puede comprenderse sin su enraizamiento en subcorrientes dinámicas: los cimientos multicapas, a menudo ocultos, de los derechos de agua. Aquí se

La incorporación de los territorios nacionales en el proceso de consolidación del estado argentino. El caso del territorio de la Pampa Central

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Marisa Moroni

2005-01-01

Full Text Available En la mayoría de los escritos de la élite letrada argentina del XIX, se identificó a la civilización como una manifestación de la identidad nacional, supuesto que las llevó a legitimar su función civilizadora y a impulsar el proceso de consolidación del Estado que requería la ocupación total del territorio, aún en manos de los indígenas a los que se responsabilizaba, junto con los caudillos, del fracaso de la unificación nacional. Desde las estructuras del poder estatal, se definió a los nuevos territorios como espacios vírgenes con infinitas posibilidades y ventajas económicas para explotar. Este argumento político atrajo pobladores -nacionales y extranjeros- que ocuparon y encaminaron la organización productiva de las futuras provincias. En este trabajo se realiza una aproximación al proceso de incorporación y posterior organización institucional de las tierras fronterizas incorporadas con la "Conquista al Desierto". En particular, se analiza la estructura político-administrativa del Territorio Nacional de la Pampa Central, constituido como tal en 1884, con el establecimiento de las primeras autoridades militares destinadas a fundar poblaciones y administrarlas políticamente.

A new species of Trechisibus from Peruvian Andes (Coleoptera: Carabidae, Trechinae

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Pedro Delgado

2016-06-01

Full Text Available In this work the new species Trechisibus (s. str. delestali sp. n., is described from the southern Peruvian Andes. The morphological differences with the geographically closest species of the subgenus are also presented and discussed.

The Glaciation of the Ecuadorian Andes

Science.gov (United States)

Schubert, Carlos

This pleasing book fills the gap in the knowledge about Pleistocene and recent glaciation between Colombia and Peru. A significant amount of data exists already for Colombia and Venezuela and for Peru, Bolivia, and, particularly, Chile. Hastenrath has now given us a description of glaciers and glaciation underneath the equator in the Andes.The book begins with brief summaries of the physiography and the atmospheric circulation, which give the general setting of Ecuador. Then follow detailed descriptions of the glaciers and glacial morphology of all the important mountains of the Western and Eastern Cordilleras. These are well illustrated, and a particularly useful feature is the comparison of old photographs and paintings of glaciers with modern photographs, many taken by the author. All illustrate the spectacular retreat of the glaciers in the Ecuadorian Andes during the last century and correlate quite well with observations elsewhere. This retreat is snown quantitatively in Table 4, in terms of decrease in glacier-covered area since the glacial advance of moraine stage III. The area of present-day glaciers is about 10% of the area during that stage (compared with about 1.5% in the Sierra Nevada de Mérida, Venezuela). A series of maps show the glacial morphology of the mountains (unfortunately, some of the maps have been included within the binding, thus losing some information; they could have been reduced somewhat to fit a single page or, if too large, could have been included in the pocket, together with the map of Chimborazo-Carihuairazo).

Estabilización del sistema financiero alemán mediante la creación de la Banca Central, 1876-1914

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Momar Diop

2014-01-01

Full Text Available Sin una armonización monetaria y la presencia de un banco central, el imperio Alemán, representa la experiencia más larga de un sistema de banca libre en los países industrializados de Europa en el Siglo XIX. La "banca libre" en el Reich estuvo marcada por la inestabilidad financiera y la violencia producto de las crisis bancarias en tiempos de guerra. Este artículo hace un análisis retrospectivo de las condiciones de estabilización del sistema bancario alemán a través de la creación de un banco central cuyas principales funciones era ser un prestamista de última instancia, establecimiento de reservas estratégicas de oro así como estabilización de la especulación bancaria. Entre 1876 y 1914, la regulación bancaria en el Reich Alemán tuvo el efecto de limitar el número de bancos emisores y neutralizar las crisis financieras sistémicas. A través de este ejemplo, se pudo observar cómo el naciente Reichsbank fue capaz de adaptarse a su nuevo entorno y llevar a cabo su misión de constituirse como banco central. Originalmente diseñado de manera similar al Banco de Inglaterra en términos de cobertura en la emisión de billetes, el Reichsbank trató de ser más flexible en su respuesta. El fijar un nivel socialmente aceptable de tasas de interés fue para los banqueros del siglo XIX, una decisión en la que la interpretación y la aceptación por parte de la sociedad capitalista era difíciles de predecir. Por otra parte, muchos de los elementos que escapaban al control del Reichsbank que fue el caso, por ejemplo, del futuro de la balanza comercial, que depende tanto de la competitividad en los precios del país así como de otros factores complejos que afectan la producción nacionales. Traducción del francés Dra. Fernanda Vidal (Postdoctorando IIJ-UNAM-DGAPA

The role of changing geodynamics in the progressive contamination of Late Cretaceous to Late Miocene arc magmas in the southern Central Andes

Science.gov (United States)

Jones, Rosemary E.; Kirstein, Linda A.; Kasemann, Simone A.; Litvak, Vanesa D.; Poma, Stella; Alonso, Ricardo N.; Hinton, Richard; EIMF

2016-10-01

The tectonic and geodynamic setting of the southern Central Andean convergent margin changed significantly between the Late Cretaceous and the Late Miocene, influencing magmatic activity and its geochemical composition. Here we investigate how these changes, which include changing slab-dip angle and convergence angles and rates, have influenced the contamination of the arc magmas with crustal material. Whole rock geochemical data for a suite of Late Cretaceous to Late Miocene arc rocks from the Pampean flat-slab segment (29-31 °S) of the southern Central Andes is presented alongside petrographic observations and high resolution age dating. In-situ U-Pb dating of magmatic zircon, combined with Ar-Ar dating of plagioclase, has led to an improved regional stratigraphy and provides an accurate temporal constraint for the geochemical data. A generally higher content of incompatible trace elements (e.g. Nb/Zr ratios from 0.019 to 0.083 and Nb/Yb from 1.5 to 16.4) is observed between the Late Cretaceous ( 72 Ma), when the southern Central Andean margin is suggested to have been in extension, and the Miocene when the thickness of the continental crust increased and the angle of the subducting Nazca plate shallowed. Trace and rare earth element compositions obtained for the Late Cretaceous to Late Eocene arc magmatic rocks from the Principal Cordillera of Chile, combined with a lack of zircon inheritance, suggest limited assimilation of the overlying continental crust by arc magmas derived from the mantle wedge. A general increase in incompatible, fluid-mobile/immobile (e.g., Ba/Nb) and fluid-immobile/immobile (e.g., Nb/Zr) trace element ratios is attributed to the influence of the subducting slab on the melt source region and/or the influx of asthenospheric mantle. The Late Oligocene ( 26 Ma) to Early Miocene ( 17 Ma), and Late Miocene ( 6 Ma) arc magmatic rocks present in the Frontal Cordillera show evidence for the bulk assimilation of the Permian-Triassic (P

Privatizing Water in the Chilean Andes: The Case of Las Vegas de Chiu-Chiu

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Manuel Prieto

2015-08-01

Full Text Available The Chilean water model has been described as a textbook example of a free-market water system. This article contributes to the critiques of this model by showing the effect of its implementation in the Atacameño community of Chiu-Chiu, located in the Atacama Desert in the south-central Andes. In this community, the privatization of water rights ignored local water management practices that had produced a high-altitude wetland (known as a vega. This led to the inhabitants’ dispossession of crucial water rights and to wetland degradation. This process belies statements that the Chilean model relies on an unregulated market and instead highlights the state’s role in marginalizing local irrigation practices by reducing the water consumption of the indigenous population while keeping the copper mining industry (the main source of Chilean income and related growing urban populations supplied with water.

Tamaño y composición de la colonia de tres especies de hormigas del género Pogonomyrmex (Hymenoptera: Formicidae en la porción central del desierto del Monte, Argentina

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Beatriz E. NOBUA BEHRMANN

2010-01-01

Full Text Available El tamaño de la colonia es un atributo fundamental de la biología de las hormigas ya que está asociado a características ecológicamente relevantes, como sus estrategias de alimentación. Mientras que el tamaño de la colonia de varias especies de hormigas granívoras del género Pogonomyrmex de América del Norte se ha estudiado en detalle, no existe tal información para las especies de América del Sur. En este trabajo, se determinó el tamaño y la composición de la colonia y se describió la estructura del nido de tres especies de Pogonomyrmex que habitan la porción central del desierto del Monte en Argentina: P. mendozanus Cuezzo & Claver, P. inermis Forel y P. rastratus Mayr. Para ello, se excavaron dos nidos de cada especie y se recolectaron todos los individuos encontrados. Las tres especies tienen colonias pequeñas, compuestas por 300-1.100 individuos, de los cuales aproximadamente el 70% son obreras adultas. La estructura de sus nidos es relativamente simple, similar a la de la mayoría de las especies norteamericanas estudiadas, pero con un menor desarrollo en profundidad y un número menor de cámaras; probablemente se deba al menor número de obreras que poseen. Estas características (colonias pequeñas y nidos poco desarrollados son consideradas típicas para las especies del género Pogonomyrmex de América del Sur, lo que las diferencia de la mayoría de sus congéneres estudiados en América del Norte.

An elusive new species of Marsupial Frog (Anura: Hemiphractidae: Gastrotheca from the Andes of northern Peru

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William E. Duellman

2013-06-01

Full Text Available A new species of marsupial frog, genus Gastrotheca, is described from high-elevation grasslands in the Andes in Región Amazonas in northernPeru, where even calling males are well hidden in deep moss. The new species is distinguished from all congeners by its unique color pattern that includes a narrow, blackbordered, yellow middorsal stripe. The species apparently belongs to the Gastrotheca plumbea Group, which ranges in the Andes from northern Colombia to northern Peru.

Oscilaciones en la central hidroeléctrica Futaleufú : Diagnóstico y solución del problema

OpenAIRE

Molina Milyus, Roberto D.; Mastronardi, Jorge L.; Lo Giudice, G.; Belkenoff, P.; Beroqui, Mario César; Agüero, Jorge Luis

2007-01-01

La Central Hidroeléctrica Futaleufú (4 x 118 MW) constituye la Planta de generación más importante del Sistema Interconectado Patagónico (SIP). Se vincula a la E.T. Puerto Madryn mediante una doble terna de 330 kV de 550 km de longitud. El SIP es un sistema eléctrico radial dividido en dos áreas, norte y sur, interconectadas mediante una larga LAT de 132 kV de 300 km de longitud. En el pasado, con elevados flujos de potencia entre el norte y sur del SIP, era común observar oscilaciones en ...

Distribución y densidad de la trucha Oncorhynchus mykiss (Salmoniformes: Salmonidae en los Andes venezolanos

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Jaime E. Péfaur

1998-09-01

Full Text Available En el presente trabajo se informa acerca de la distribución espacial y la abundancia de las poblaciones de la trucha arcoiris silvestre en los Andes Venezolanos, con base en recolectas en 68 estaciones de muestreo durante un año. Ubicadas entre 500 y 4000 msnm en siete cuencas hidrográficas de los ríos más importantes de los Andes de Venezuela. Un total de 612 individuos fueron obtenidos en estaciones por encima de los 1700 m. La mayoría de los peces de recogieron en las cuencas de los ríos Chama (43%, Motatán (21% y Santo Domingo (32%, con sólo algunos ejemplares recolectados en los ríos Negro (1.75% y La Grita (0-33%, y con ausencia de capturas en los ríos Escalante y Mocotíes. Los machos adultos superan numéricamente a las hembras en una posición de 2.15: 1. Los juveniles conforman un 56.7% del total de capturas, con una proporción de 1.30 juveniles por adulto. El tamaño de los especímenes varió desde 2.0 a 21.8 cm. Con casi la mitad de ellos dentro del intervalo 5.1 - 10.0 cm. El peso de los ejemplares también presentó una amplia variación, con un máximo de 317.0g.Spatial distribution and relative abundance of wild rainbow trout populations were studied in 68 stations located between 500 and 4000 masl in seven hydrological basins of the most important Andean rivers of Venezuela during a year of sampling. A total of 612 individuals were obtained above 1700 m. Most fishes were obtained from the Chama ( 43%, Motatán (21% and Santo Domingo (32% rivers, very few in the Negro (1.75% and La Grita (0.33% rivers, and none in the Escalante and Mocotíes rivers basins. Adult males were more abundant than females in a 2.15:1 proportion. Juveniles made a 56.7% of captures, with a proportion of 1.30 juveniles per adult. Individual sizes varied from 2.0 to 21.8 cm, most within the interval 5.1 - 10.0 cm; the weight of specimens also showed an ample variation, with a maximum of 317.0 g.

Redefinición y tendencias del concepto de estrategia para el gerente colombiano

OpenAIRE

JAHIR ALEXANDER GUTIERREZ OSSA

2012-01-01

En Colombia son pocos los estudios especializados realizados sobre estrategia y pensamiento estratégico con referencia al empresario y las empresas. La indagación muestra algunas investigaciones realizadas sobre la materia en la Universidad del Rosario, en la Universidad de los Andes y en la Universidad Icesi, pioneras en este tipo de estudios; que buscan conocer un poco acerca de cómo piensan y actúan los gerentes colombianos. Ésta vez, la pregunta sobre el tema se traslada al grupo de gesti...

Different Phases of Earthquake Cycle Reflected in GPS Measured Crustal Deformations along the Andes

Science.gov (United States)

Khazaradze, G.; Klotz, J.

2001-12-01

The South American Geodynamic Activities (SAGA) project was initiated in 1993 by the GeoForschungsZentrum together with host organizations in Argentina and Chile with the main objective of studying the kinematics and dynamics of present-day deformation processes along the central and southern Andes. Currently the SAGA network consists of 230 geodetic markers spanning more than 2000 km long distance from Peru/Chile border in the north to Cape Horn in the south. The majority of the observed crustal deformation field is relatively homogenous: roughly parallel to the plate convergence direction and decreasing in magnitude away from the deformation front. This pattern is characteristic for the \\textit{inter-seismic} phase of earthquake deformation cycle and can be explained by the elastic strain accumulation due to locking of the thrust interface between the subducting Nazca and the overriding South America plates. However, in addition to the dominant inter-seismic signal, close examination of the observed velocity field also reveals significant spatial and temporal variations, contrary to the commonly used assumption of constant deformation rates. This variation is especially pronounced for the measurements in the vicinity of the 1995 Mw8.0 Antofagasta earthquake (22{° }S-26{° }S). Here, after capturing up to 1 meters of \\textit{co-seismic} displacements associated with this event, the analysis of data obtained during the three following field campaigns (1996-1999), reveals highly time dependent deformation pattern. This can be explained by the decreasing importance of \\textit{post-seismic} effects of the Antofagasta event relative to the increasing dominance of the inter-seismic phase of subduction. Perhaps, even more interesting time dependent observations have been detected in the southern part the SAGA network (38{° }S-43{° }S).Here, after 35 years of the occurrence of the 1960 Mw9.5 Chile earthquake, we still see the continuing post-seismic effects of this

A high-altitude peatland record of environmental changes in the NW Argentine Andes (24 ° S) over the last 2100 years

Science.gov (United States)

Schittek, Karsten; Kock, Sebastian T.; Lücke, Andreas; Hense, Jonathan; Ohlendorf, Christian; Kulemeyer, Julio J.; Lupo, Liliana C.; Schäbitz, Frank

2016-05-01

High-altitude cushion peatlands are versatile archives for high-resolution palaeoenvironmental studies, due to their high accumulation rates, range of proxies, and sensitivity to climatic and/or human-induced changes. Especially within the Central Andes, the knowledge about climate conditions during the Holocene is limited. In this study, we present the environmental and climatic history for the last 2100 years of Cerro Tuzgle peatland (CTP), located in the dry Puna of NW Argentina, based on a multi-proxy approach. X-ray fluorescence (XRF), stable isotope and element content analyses (δ13C, δ15N, TN and TOC) were conducted to analyse the inorganic geochemistry throughout the sequence, revealing changes in the peatlands' past redox conditions. Pollen assemblages give an insight into substantial environmental changes on a regional scale. The palaeoclimate varied significantly during the last 2100 years. The results reflect prominent late Holocene climate anomalies and provide evidence that in situ moisture changes were coupled to the migration of the Intertropical Convergence Zone (ITCZ). A period of sustained dry conditions prevailed from around 150 BC to around AD 150. A more humid phase dominated between AD 200 and AD 550. Afterwards, the climate was characterised by changes between drier and wetter conditions, with droughts at around AD 650-800 and AD 1000-1100. Volcanic forcing at the beginning of the 19th century (1815 Tambora eruption) seems to have had an impact on climatic settings in the Central Andes. In the past, the peatland recovered from climatic perturbations. Today, CTP is heavily degraded by human interventions, and the peat deposit is becoming increasingly susceptible to erosion and incision.

Trauma and violence in the Wari empire of the Peruvian Andes: warfare, raids, and ritual fights.

Science.gov (United States)

Tung, Tiffiny A

2007-07-01

This study examines bioarchaeological evidence for violence during the period of Wari imperialism in the Peruvian Andes through analysis of skeletal trauma from three populations dating to AD 650-800. The samples are from contemporaneous archaeological sites: Conchopata, a Wari heartland site in central highland Peru; Beringa, a community of commoners in the Majes valley of the southern Wari hinterland; and La Real, a high status mortuary site, also in the Majes valley. Given the expansionist nature of Wari and its military-related iconography and weaponry, it is hypothesized that Wari imperialism was concomitant with greater levels of violence relative to other prehispanic groups in the Andes. It is also hypothesized that differential articulation with the Wari empire (e.g., heartland vs. hinterland groups) affected the frequency and patterning of trauma. Results show that cranial trauma frequency of the three Wari era samples is significantly greater than several other Andean skeletal populations. This suggests that Wari rule was associated with high levels of violence, though it may not have always been related to militarism. The three adult samples show similar frequencies of cranial trauma (Conchopata = 26%; Beringa = 33%; La Real = 31%). This may suggest that differential positioning in the Wari empire had little effect on exposure to violence. Sex-based differences in cranial trauma frequencies are present only at La Real, but wound patterning differs between the sexes: females display more wounds on the posterior of the cranium, while males show more on the anterior. These data suggest that Wari rule may have contributed to violence. (c) 2007 Wiley-Liss, Inc.

Thermal analysis of the heat recuperator of a combined cycle thermoelectric central; Analisis termico del recuperador de calor de una central termoelectrica de ciclo combinado

Energy Technology Data Exchange (ETDEWEB)

Romero Paredes, Hernando; Sanchez, I; Lazcano, L C; Ambriz, Juan Jose; Alvarez, M [Universidad Autonoma Metropolitana-Iztapalapa, Mexico, D. F. (Mexico); Gonzalez, O [Comision Federal de Electricidad, Tula (Mexico)

1997-12-31

The thermoelectric centrals of the combined cycle type (Brayton Cycle and Rankine Cycle) present a series of opportunities to increase the efficiency of the combined cycle or of the generated power. This paper shows the methodology for the performance of energy balances in a heat recuperator (H. R.), typically employed in the combined cycle stations operating in Mexico, for the assessment of the energy harnessing in the different sections conforming a H. R. The effect of the installation of evaporative coolers and/or an absorption cooling system at the gas turbine compressor intake on the steam generation in the heat recuperator, is evaluated. This extra generation of steam is quantified for its potential use in the same absorption refrigeration system. From the assessment, it follows up that the steam generation in the H.R. is inversely proportional to the ambient temperature and that, although the increased amount of steam generated can not be harnessed in total by the steam turbine, the remaining fraction is good enough to cover the heat demand for the operation of the refrigeration system. [Espanol] Las centrales termoelectricas del tipo ciclo combinado (ciclo Brayton y ciclo Rankine) presentan un conjunto de oportunidades para incrementar la eficiencia del ciclo combinado o bien la potencia generada. En el presente trabajo se expone la metodologia para realizar los balances de energia en un recuperador de calor (R.C.) tipicamente utilizado en las Centrales de Ciclo Combinado (CCC) que operan en Mexico, para evaluar el aprovechamiento de la energia en las diferentes secciones que conforman un R.C. Se evalua el efecto que tiene la instalacion de enfriadores evaporativos y/o un sistema de enfriamiento por absorcion en la succion del compresor de la turbina de gas sobre la generacion de vapor en el recuperador de calor. Se cuantifica esta generacion extra de vapor para su posible utilizacion en el mismo sistema de refrigeracion por absorcion. De la evaluacion se

Thermal analysis of the heat recuperator of a combined cycle thermoelectric central; Analisis termico del recuperador de calor de una central termoelectrica de ciclo combinado

Energy Technology Data Exchange (ETDEWEB)

Romero Paredes, Hernando; Sanchez, I.; Lazcano, L. C.; Ambriz, Juan Jose; Alvarez, M. [Universidad Autonoma Metropolitana-Iztapalapa, Mexico, D. F. (Mexico); Gonzalez, O. [Comision Federal de Electricidad, Tula (Mexico)

1996-12-31

The thermoelectric centrals of the combined cycle type (Brayton Cycle and Rankine Cycle) present a series of opportunities to increase the efficiency of the combined cycle or of the generated power. This paper shows the methodology for the performance of energy balances in a heat recuperator (H. R.), typically employed in the combined cycle stations operating in Mexico, for the assessment of the energy harnessing in the different sections conforming a H. R. The effect of the installation of evaporative coolers and/or an absorption cooling system at the gas turbine compressor intake on the steam generation in the heat recuperator, is evaluated. This extra generation of steam is quantified for its potential use in the same absorption refrigeration system. From the assessment, it follows up that the steam generation in the H.R. is inversely proportional to the ambient temperature and that, although the increased amount of steam generated can not be harnessed in total by the steam turbine, the remaining fraction is good enough to cover the heat demand for the operation of the refrigeration system. [Espanol] Las centrales termoelectricas del tipo ciclo combinado (ciclo Brayton y ciclo Rankine) presentan un conjunto de oportunidades para incrementar la eficiencia del ciclo combinado o bien la potencia generada. En el presente trabajo se expone la metodologia para realizar los balances de energia en un recuperador de calor (R.C.) tipicamente utilizado en las Centrales de Ciclo Combinado (CCC) que operan en Mexico, para evaluar el aprovechamiento de la energia en las diferentes secciones que conforman un R.C. Se evalua el efecto que tiene la instalacion de enfriadores evaporativos y/o un sistema de enfriamiento por absorcion en la succion del compresor de la turbina de gas sobre la generacion de vapor en el recuperador de calor. Se cuantifica esta generacion extra de vapor para su posible utilizacion en el mismo sistema de refrigeracion por absorcion. De la evaluacion se

Actitudes lingüísticas en el Perú. Predominancia del castellano de la costa central y norte

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Ana Gloria Arias Torres

2014-11-01

Full Text Available Resumen Este artículo analiza las actitudes lingüísticas de los hablantes nativos de español de la ciudad de Lima hacia al español del Perú y hacia el español de los otros países hispanohablantes. El artículo es parte de los resultados del Proyecto LIAS (Linguistic Identity and Attitudes in Spanish-speaking Latin America, financiado por El Consejo Noruego de Investigación (RCN. La recolección de los datos se realizó en la capital del país, entrevistando a una muestra de 400 informantes previamente estratificada con las variables de edad, sexo y nivel socioeconómico. Como conclusión se ha comprobado que la mayoría de la población identifica su forma de hablar con las variedades de las zonas de la costa central y norte. Específicamente tienen valoración positiva las hablas de Lima y Trujillo; la valoración negativa se observa en algunas hablas de la capital, la sierra sur, la sierra central, y el oriente norte, por considerarlas formas muy diferentes, con acentos muy marcados. Abstract This article analyzes the linguistic attitudes of native Spanish speakers from Lima towards Spanish spoken in Peru and in the other Spanish-speaking countries. It is a result of the LIAS-Project (Linguistic Identity and Attitudes in Spanish-speaking Latin America, funded by The Research Council of Norway (RCN. The data were gathered in the capital of the country, interviewing a stratified sample of 400 respondents, based on the variables of age, sex and socioeconomic status. The results confirm that most of the population of the capital perceive their own speech to be very similar to the Spanish spoken in the central and northern regions of the country. The Spanish variety of Lima and Trujillo are valued positively, while some dialects of the capital, the southern and central sierras and the northeastern region are considered very different due to their strong accents.

Poder y sociedad en los Andes: Manuel Isidoro Belzu, un caudillo popular. Bolivia, 1848-1855

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Luis Javier Ortíz Mesa

1995-01-01

Full Text Available En este ensayo quiero referirme a un gobernante boliviano, Manuel Isidoro Belzu, presidente entre los años de 1848 y 1855. Con una larga carrera militar de casi 25 años, en un ambiente de permanente inestabilidad política y con una fascinante estrategia, Belzu ha sido percibido por algunos historiadores y literatos como un «Caudillo del Pueblo», otros lo calificaron como un demagogo y algunos más como el presidente para la Bolivia de entonces. Manuel Isidoro Belzu nació al tiempo que se vislumbraba la Bolivia Republicana en 1808. Fue un hombre pobre como muchos de sus conciudadanos, predominantemente indígenas. No obstante, Belzu fue un mestizo, expresión de los cambios raciales que desde la Colonia se produjeron en la población de la Audiencia de Charcas cuya sede y capital fue Chuquisaca o Sucre, donde tuvo asiento el emporio minero más importante y productivo de los Andes, el Cerro Rico de Potosí.

Conservación de los Bosques Relictos del NO de Perú

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Eric F. Rodríguez Rodríguez

2013-05-01

Full Text Available El presente documento resume las conclusiones obtenidas en el «Taller sobre Bosques Relictos de las Vertientes Occidentales Andinas del Norte del Perú y Sur del Ecuador», desarrollado en el marco del X Congreso Nacional de Botánica, Trujillo-Perú, el 04 de mayo del 2004. En este taller se llegaron a las siguientes conclusiones, dirigidas principalmente a los gobiernos regionales y concejos provinciales que incluyen a los departamentos de Cajamarca, Lambayeque, La Libertad y Piura: ·El Perú esta reconocido entre los países tropicales con mayor diversidad vegetal. La región norte del país incluye un porcentaje alto de esa diversidad. Entre los ecosistemas importantes que concentra la diversidad en esta región se encuentran los bosques relictos de la vertiente occidental de los Andes (Piura, Lambayeque, Cajamarca, La Libertad, considerados unos de los más altamente endémicos en todo el mundo. Estos bosques que se extienden hasta los 12°S, tienen tanto una diversidad muy elevada como un gran índice de endemismo. Muchas de estas especies están restringidas a bosques relictos individuales, tales como en los siguientes departamentos:

La tectónica alpina en el borde norte del Sistema Central español y su enlace con la cuenca del Duero

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Gómez Ortiz, D.

1997-12-01

Full Text Available This report is focused to describe the main alpine structures located in the northern edge of the Spanish Central System and the linking zone with the Tertiary Duero basin. A review of the main characteristics of the alpine tectonic phases is given. From these data, differences between the Gredos zone, dominated by N-S and E-W faults, and the Guadarrama zone, in which N 70° E reverse faults with N 140° E and N 10° E strike-slip faults are present, can be observed. The pattern of drainage of this area shows three main orientations, coincident with the alpine faults activated during the Guadarrama tectonic phase, which reveals the relationship between the present drainage pattern and the Alpine orogeny.En este trabajo se describen las principales estructuras alpinas del borde norte del Sistema Central y su enlace con la cuenca del Duero, así como las características de las principales fases tectónicas alpinas que han dado lugar a la actual estructura. Se pone de manifiesto las diferencias entre la zona de Gredos, dominada por fallas N-S y E-O principalmente, y la zona de Guadarrama en la que las fallas inversas son N 70° E acompañadas de desgarres N 140° E y N 10° E. El análisis de las direcciones de los ríos en este área permite definir tres zonas en función de su orientación, que coinciden con las definidas para las fallas alpinas, lo que refleja la relación entre la red de drenaje y la fase alpina Guadarrama principalmente.

Actions for the environmental adequateness and emissions control at the Martin del Corral power plant-Termozipa; Obras de adecuacion ambiental y control de emisiones para la central termoelectrica Martin del Corral - Termozipa

Energy Technology Data Exchange (ETDEWEB)

Arevalo Osorio, Luis [Empresa de Energia de Bogota, Bogota (Colombia)

1997-12-31

In this paper the general data on the Martin del Corral-Termozipa, of Colombia, fossil fueled power plant are exposed. The results of a study to determine the environmental impact originated in the influence zone of this Power Plant are presented, particularly on the Bogota River. The study was framed into the environmental policy driven by the Colombian sector. Different solutions addressed to the optimization of the handling, capacity and control of the emissions and counteract the pollution possibilities of the Bogota River are described [Espanol] En esta ponencia se exponen datos generales de la central termoelectrica Martin del Corral - Termozipa-, de Colombia. Se presentan los resultados de un estudio para determinar el impacto ambiental ocasionado en la zona de influencia de esta central, y en particular sobre el rio Bogota. El estudio se enmarco dentro de la politica ambiental impulsada por el sector colombiano. Se describen diversas soluciones encaminadas a optimizar el manejo, capacidad y control de las emisiones y contrarrestar las posibilidades de contaminacion del rio Bogota

Actions for the environmental adequateness and emissions control at the Martin del Corral power plant-Termozipa; Obras de adecuacion ambiental y control de emisiones para la central termoelectrica Martin del Corral - Termozipa

Energy Technology Data Exchange (ETDEWEB)

Arevalo Osorio, Luis [Empresa de Energia de Bogota, Bogota (Colombia)

1996-12-31

In this paper the general data on the Martin del Corral-Termozipa, of Colombia, fossil fueled power plant are exposed. The results of a study to determine the environmental impact originated in the influence zone of this Power Plant are presented, particularly on the Bogota River. The study was framed into the environmental policy driven by the Colombian sector. Different solutions addressed to the optimization of the handling, capacity and control of the emissions and counteract the pollution possibilities of the Bogota River are described [Espanol] En esta ponencia se exponen datos generales de la central termoelectrica Martin del Corral - Termozipa-, de Colombia. Se presentan los resultados de un estudio para determinar el impacto ambiental ocasionado en la zona de influencia de esta central, y en particular sobre el rio Bogota. El estudio se enmarco dentro de la politica ambiental impulsada por el sector colombiano. Se describen diversas soluciones encaminadas a optimizar el manejo, capacidad y control de las emisiones y contrarrestar las posibilidades de contaminacion del rio Bogota

Efecto del secado de las muestras sobre la extracción selectiva de Fe y A1 activos en Andisoles del norte de la cordillera central Colombiana.

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Jaramillo J. Daniel F.

2000-12-01

Full Text Available Muestras secadas al aire y sin secar de cinco perfiles de Andisoles del norte de la cordillera central colombiana fueron sometidas a extracción con oxalato ácido de amonio y con pirofosfato de sodio. En los extractos de oxalato se determinaron A1, Fe y Si y en los de pirofosfato A1 y Fe. El secado de las muestras redujo significativamente al 95% la cantidad de A1 y de Fe extraída con oxalato ácido, dificultando la clasificación de los suelos en el orden Andisol utilizando los parámetros de la taxonomía del USDA.

Manejo y conservación del suelo y agua en los Andes del Sur de Ecuador

OpenAIRE

Ochoa Cueva, Pablo Alejandro

2016-01-01

El manejo y la conservación de los recursos suelo y agua han sido y son motivo de gran preocupación para la sostenibilidad del Planeta en cuanto a la soberanía alimentaria y el desarrollo de la vida en general, esto se remarca en los países en vías de desarrollo que presentan fuertes contrastes, como lo es el Ecuador. Las limitaciones en la recolección de los datos climatológicos, de suelo, cobertura vegetal, entre otros; así como la aplicación de metodologías que se adapten a las realidades ...

Estado del Arte: El Banco Central de Estados Unidos a sus 100 años

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Jane D'Arista

2013-09-01

Full Text Available La creencia en la hipótesis de los mercados eficientes y la adopción de requerimientos de capital para los bancos como la mejor herramienta macroprudencial compatible con las fuerzas del mercado, reemplazó el compromiso previo de la Reserva Federal (Fed de emplear la conexión entre las operaciones de mercado abierto y los cambios en los requerimientos de reservas para limitar el crédito. Desde que se cortó esta palanca sobre la oferta crediticia, el banco central ha dependido de las operaciones de mercado abierto para lograr solamente un objetivo: influir sobre la demanda de crédito cambiando la tasa de referencia de corto plazo. La desequilibrada caja de herramientas contribuyó a un sesgo procíclico en los resultados de sus políticas que reflejó y exacerbó el sesgo procíclico del sistema financiero. El fracaso de evaluar y fortalecer sus herramientas monetarias ha socavado la habilidad de la Fed para restaurar el crecimiento económico y evitar otra crisis financiera. La traducción del inglés al español es de Wesley Marshall y Eugenia Correa.

Influencia de la hipoxia sobre el metabolismo óseo: rol central del factor inducible por hipoxia

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Elías Ernesto Aguirre Siancas

2013-10-01

Full Text Available El conocimiento de la influencia de la hipoxia sobre la fisiología humana dio un salto cualitativo cuando se descubrió al factor inducible por hipoxia (HIF. Las vías moleculares que este factor de transcripción regula son variadas y complejas, cuya comprensión continuamente se sigue profundizando. En la fisiología y en la fisiopatología del tejido óseo se desarrollan varios procesos característicos, como la osificación, la remodelación y la reparación. La disminución en la disposición de oxígeno determina la estabilización del HIF en muchos grupos celulares, entre los cuales destacan las células del linaje osteogénico. Este factor regula la expresión de múltiples genes, siendo, quizás, el más importante el que codifica al factor de crecimiento vascular del endotelio (VEGF, debido a su decisiva implicancia en el proceso de osteogénesis, directamente activando a las células osteoblásticas o indirectamente mediante su potente acción angiogénica. En este artículo, se hace una revisión actualizada sobre el rol central del HIF sobre la fisiología ósea, detallando la regulación de las principales vías moleculares dependientes de dicho factor de transcripción.

Genetic continuity after the collapse of the Wari empire: mitochondrial DNA profiles from Wari and post-Wari populations in the ancient Andes.

Science.gov (United States)

Kemp, Brian M; Tung, Tiffiny A; Summar, Marshall L

2009-09-01

The Wari empire flourished in the central, highland Peruvian Andes from AD 600-1000, and although the events that led to its demise are unknown, archaeological evidence indicates that Wari control waned at the end of the first millennium. Here, we test the hypothesis that, despite the major shift in social and political organization at the fall of the Wari empire, the mitochondrial DNA (mtDNA) composition of populations from the Ayacucho Basin, the former imperial heartland of the empire, remained essentially unchanged. Results show that mtDNA haplogroup frequencies among the Wari and post-Wari groups differ, but the difference is not statistically significant (chi2 = 5.886, df = 3, P = 0.1172). This is the first study in the Andes to use haplotypic data to evaluate the observed genetic distance between two temporally distinct prehispanic populations (F(ST) = 0.029) against modeled expectations of four possible evolutionary scenarios. None of these simulations allowed the rejection of continuity. In total, at both the haplogroup and haplotype levels these data do not allow us to reject the hypothesis that post-Wari individuals sampled in this study are the maternal descendants of those sampled from the Wari era site of Conchopata. However, genetic homogeneity in the mitochondrial gene pool, as seen in the late prehispanic southern Andes, may also characterize our study region. But, prior to this research, this was unknown. If our new data show mtDNA homogeneity, then this could limit the detection of female migration if, in fact, it occurred. Nonetheless, the novel mtDNA data presented here currently do not support the hypothesis that there was an influx of genetically distinct females into the former Wari heartland after the Wari collapse. Copyright 2009 Wiley-Liss, Inc.

Estatus ponderal y aptitud cardiorrespiratoria en escolares de la región central del Perú

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Alcibíades Bustamante

Full Text Available Objetivos. Determinar la frecuencia del sobrepeso y obesidad, en función a los niveles de aptitud cardiorrespiratoria (AptCR en escolares de cuatro distritos de la región central del Perú, y analizar la asociación entre estas variables. Materiales y métodos. El peso, altura y la AptCR fueron evaluados en 7841 escolares que residen en cuatro distritos ubicados en la costa, sierra y selva de la región central del Perú. El sobrepeso y la obesidad fueron clasificados según los criterios propuestos por Cole. La AptCR fue evaluada mediante la prueba de correr/caminar de doce minutos de la batería de la American Alliance for Health, Recreation and Dance. Se utilizó el ANOVA y la regresión logística para examinar las diferencias de las medias y asociaciones entre estas variables. Resultados. Escolares de ambos sexos presentan frecuencias semejantes de sobrepeso y obesidad (20,9% en mujeres y 20,1% en varones. Residentes en la costa (Barranco manifiestan elevadas frecuencias de sobrepeso y obesidad (37,8%. La edad, el sexo, área geográfica y la AptCR fueron predictores significativos para el sobrepeso y la obesidad. Escolares que viven en Barranco tienen cinco veces más probabilidades de ser obesos (OR=4,67; IC95%: 3,55-6,14; los que residen en la sierra (Junín tienen una menor probabilidad de ser obesos (OR=0,03; IC95%: 0,01-0,20; y quienes muestran una baja AptCR tienen una mayor probabilidad de ser obesos (OR=11 ,82; IC95%: 7,25-19,27, en comparación con aquellos con alta AptCR. Conclusiones. Los escolares que residen en Barranco presentan frecuencias de sobrepeso y obesidad elevados. Una baja AptCR está asociada al desarrollo del sobrepeso y la obesidad

Within plate seismicity analysis in the segment between the high Cordillera and the Precordillera of northern Mendoza (Southern Central Andes

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Julián Olivar

2018-01-01

Full Text Available Crustal seismicity in northwestern Mendoza Province in Argentina, corresponding to the transition zone between the Chilean-Pampean flat subduction zone (26.5–33.5°S and the Southern Central Andes normal subduction zone to the south, is studied in order to i identify its relationship with the mapped structure, ii determine deformational mechanisms and iii constrain the geometry of the fold and thrust belt in the lower crust. Through this, we aim to determine which are the structures that contribute to Andean construction, east of the Frontal Cordillera in Argentina and at the western Principal Cordillera in Chile. Data from a temporary local seismic network are reprocessed in order to achieve a precise location of hypocenters and, whenever possible, to build focal mechanisms. Results are interpreted and compared with previous seismic studies and structural models. Analyzed seismicity is grouped around the eastern front of Frontal Cordillera, with hypocenters mainly at depths of 25–40 km. Contrastingly, earthquakes in the Principal Cordillera to the west are located at the axial Andean sector and Chilean slope, with depths shallower than 15 km. Obtained focal mechanisms indicate mainly strike-slip displacements, left lateral at Frontal Cordillera and right lateral at Principal Cordillera. Based on these observations, new possible structural models are proposed, where seismogenic sources could be either associated with inherited basement structures from the Cuyania-Chilenia suture; or correspond to deep-blind thrusts linked with a deeper-than-previously-assumed decollement that could be shared between Frontal Cordillera and western Precordillera. This deeper decollement would coincide in turn with the one determined from receiver function analysis for the eastern Sierras Pampeanas in previous works, potentially implying a common decollement all through the fold and thrust belt configuration. Apart from this, a new interpretation of

Contribution to the Geology of the Central and Western Cordillera of Colombia in the sector between Ibagué and Cali

NARCIS (Netherlands)

Nelson, H.W.

1957-01-01

Het Westelijk gedeelte van de Republiek Columbia (Zuid Amerika) wordt ingenomen door de Cordilleras de los Andes, welke in genoemde republiek uit drie hoofdketens bestaat, t. w. de West Cordillera, de Centrale Cordillera en de Oost Cordillera. Een studie werd gemaakt van een centraal gelegen Strook

Elaboración y aplicación de una guía de técnicas plásticas fiorella para desarrollar las habilidades de motricidad fina en los niños y niñas del centro infantil del Buen Vivir “Aida Chávez” del barrio central de la parroquia matriz del cantón Guamote, provincia de Chimborazo en el período mayo-diciembre del 2013.

OpenAIRE

Cayán Moreno, Inés Yolanda

2015-01-01

El tema del presente trabajo de investigación es: Elaboración y aplicación de una Guía de Técnicas Plásticas “Fiorella” para desarrollar las habilidades de motricidad fina en los niños y niñas del Centro Infantil del Buen Vivir “Aida Chávez” del Barrio Central de la parroquia Matriz del cantón Guamote, provincia de Chimborazo en el período Mayo-Diciembre del 2013, con el objetivo de Demostrar, Evidenciar e Identificar cómo la elaboración y aplicación de la Guía de Técnicas Plásticas “Fiorel...

Variación espacio-temporal del nitrógeno y fósforo en el embalse del Neusa

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Juan Pablo Niño Garcia

2003-01-01

Full Text Available El Embalse del Neusa es un cuerpo de agua oligo-mesotrófico ubicado en la cordillera oriental de los Andes colombianos, utilizado en la regulación de caudales del río Neusa y en la distribución de agua para consumo. Allí se analizaron la variación espacial del nitrógeno y el fósforo y sus tasas de sedimentación, se indagó sobre su relación con la distribución de Egeria densa en el embalse. Para hacer una aproximación a la incidencia de las comunidades litorales sobre la variación del nitrógeno y fósforo se hicieron estimaciones de los porcentajes de nitrógeno y fósforo contenidos tanto en la biomasa como en la necromasa macrofíticas y se estudió su variación en el tiempo durante los procesos de descomposición in situ. En este trabajo se encontró que las diferencias temporales y espaciales en los contenidos de nitrógeno y fósforo en la columna de agua respondieron a las fluctuaciones estacionales de las afluencias y cambios de nivel del agua, así como a la distribución espacial de E. densa;. esta última se relacionó con el aumento en las tasas de sedimentación del seston, nitrógeno y fósforo. Durante la descomposición estos dos nutrientes se perdieron rápidamente en los primeros días, volviéndose limitantes para los microorganismos descomponedores en fases posteriores del proceso. Estos recurren a nutrientes disueltos, escasos en la columna de agua, que en consecuencia pueden ser limitantes para los procesos de descomposició.

Holocene tephra-fall deposits of southern and austral Andes volcanic zones (33-54oS): eruption recurrence

International Nuclear Information System (INIS)

Naranjo, J.A.; Polanco, E.; Lara, L; Moreno, H; Stern, C.R

2001-01-01

Radiometric 14 C dating is a very useful tool to study the chronostratigraphy of pyroclastic deposits. In addition, 14 C ages are essential parameters for the estimation of the recurrence time of the explosive volcanic activity. The origin, distribution and relative age of mappable Holocene tephra-fall deposits of the Southern Andes Volcanic Zone (SVZ) and Austral Andes Volcanic Zone (AVZ) from 33 o S-54 o S, were studied and their recurrence period is analysed (au)

Tamaño y composición de la colonia de tres especies de hormigas del género Pogonomyrmex (Hymenoptera: Formicidae en la porción central del desierto del Monte, Argentina Colony size and composition in three Pogonomyrmex ant species (Hymenoptera: Formicidae in the central Monte desert, Argentina

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Beatriz E. Nobua Behrmann

2010-06-01

Full Text Available El tamaño de la colonia es un atributo fundamental en la biología de las hormigas ya que está asociado a características ecológicamente relevantes, como sus estrategias de alimentación. Mientras que el tamaño de la colonia de varias especies de hormigas granívoras del género Pogonomyrmex de América del Norte se ha estudiado en detalle, no existe tal información para las especies de América del Sur. En este trabajo, se determinó el tamaño y la composición de la colonia y se describió la estructura del nido de tres especies de Pogonomyrmex que habitan la porción central del desierto del Monte en Argentina: P. mendozanus Cuezzo & Claver, P. inermis Forel y P. rastratus Mayr. Para ello, se excavaron dos nidos de cada especie y se recolectaron todos los individuos encontrados. Las tres especies tienen colonias pequeñas, compuestas por 300-1.100 individuos, de los cuales aproximadamente el 70% son obreras adultas. La estructura de sus nidos es relativamente simple, similar a la de la mayoría de las especies norteamericanas estudiadas, pero con un menor desarrollo en profundidad y un número menor de cámaras; probablemente se deba al menor número de obreras que poseen. Estas características (colonias pequeñas y nidos poco desarrollados son consideradas típicas para las especies del género Pogonomyrmex de América del Sur, lo que las diferencia de la mayoría de sus congéneres estudiados en América del Norte.Colony size in ants is associated with important ecological characteristics such as foraging strategy. Though colony size has been studied with some detail for several North American species of Pogonomyrmex harvester ants, it remains unknown for South American species. We studied colony size, composition, and nest structure of three species of Pogonomyrmex harvester ants inhabiting the central Monte desert in Argentina: P. mendozanus Cuezzo & Claver, P. inermis Forel and P. rastratus Mayr. We excavated two nests of each

Participación del consejo comunitario de la comunidad negra de Bellavista en la consulta previa para la formulación del plan de manejo ambiental de la central hidroeléctrica del bajo Anchicayá

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Nixon Arboleda Montaño

2016-01-01

Full Text Available El presente trabajo analiza el proceso de participación que se llevó a cabo en el marco de la consulta previa entre el Consejo Comunitario de la Comunidad Negra de Bellavista (CCCNB, situado en el distrito de Buenaventura y la Empresa de Energía del Pacífico (EPSA con motivo de la formulación del Plan de Manejo Ambiental para la actual operación y mantenimiento la Central Hidroeléctrica del Bajo Anchicayá (Colombia. Se presentan los antecedentes de la evaluación de impacto ambiental en el ámbito internacional y en Colombia, y se explica en qué consiste el proceso de la consulta previa en los proyectos que requieren licencia ambiental. Posteriormente se analizan las etapas del proceso (etapa previa; estudios ambientales y socioeconómicos; identificación y evaluación de impactos ambientales; y construcción de medidas de manejo ambiental y finalmente se analiza el proceso de consulta previa, identificando los valores agregados que pudo generar el proceso.

Abundancia y biomasa de macroinvertebrados edáficos en la temporada lluviosa, en tres usos de la tierra, en los Andes colombianos

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Pardo Luis C

2006-03-01

Full Text Available COMPENDIO los usos evaluados fueron pastizal, cafetal y bosque secundario (Vereda Villa del Rosario, Aprox. 3º 33' 16â€? Latitud Norte y 76º 36' 01â€? Longitud Oeste, altitud 1.500 a 1.820m., precipitación 960 a 1.050 mm/año, 19.8 a 21.2º C con la metodología TSBF. Se implementaron tres monolitos por uso y cada uno se subdividió en cuatro estratos (hojarasca, 0-10 cm, 10-20 cm, y 20-30 cm, las variables densidad y biomasa por parcela y estrato se examinaron a través de ANOVAS y Post-Anovas. En abundancia la supremacía fue de hormigas (25584 ejemplares, miriápodos (4808 ejemplares y lombrices (1984 ejemplares, la diferencia significativa la marcaron los miriápodos (F=4.84, P=0.014 asociados con bosque y cafetal con sombrío. En biomasa los grupos más importantes fueron miriápodos (701.05 g m-2, 58.71%, lombrices (90.64 g m-2; 7.59%, chisas (27.07 g m-2; 2.26% hor­migas (20.90 g m-2; 1.75% y arañas (15.71 g m-2 ; 1.31%, con diferencias significativas en hormigas (F=4.17, P=0.024 y arañas (F=3.43, P=0.4024; También hubo diferencias estadísticas significativas en la densidad y biomasa de macroinvertebrados y los estratos de los monolitos, los resultados indican que estos organismos expresan en su población y biomasa respuestas ambientales asociadas más con la estructura del agroecosistema que con la variación química, física o microbiológica del hábitat; se recomienda discriminar taxonómicamente los grupos funcionales y ampliar los muestreos a la temporada seca. Palabras clave: uso del suelo, macroinvertebrados edáficos, densidad, abundancia, agroecosistemas, Andes colombianos. ABSTRACT Abundance and biomass of soil macroinvertabrates during the rainy season in three land use systems in the Colombian Andes. Using the TSBF methodology, three land use systems—pastures, coffee plantation, and secondary forest— were evaluated in the rural community of Villa del Rosario, located in the

Crustal seismicity associated to rpid surface uplift at Laguna del Maule Volcanic Complex, Southern Volcanic Zone of the Andes

Science.gov (United States)

Cardona, Carlos; Tassara, Andrés; Gil-Cruz, Fernando; Lara, Luis; Morales, Sergio; Kohler, Paulina; Franco, Luis

2018-03-01

Laguna del Maule Volcanic Complex (LMVC, Southern Andes of Chile) has been experiencing large rates (ca. 30 cm/yr) of surface uplift as detected since 2008 by satellite geodetic measurements. Previous works have modeled the source of this deformation as an inflating rectangular sub-horizontal sill underlying LMVC at 5 km depth, which is supposedly related to an active process of magmatic replenishment of a shallow silicic reservoir. However little is known about the tectonic context on which this activity is taking place, particularly its relation with crustal seismicity that could help understanding and monitoring the current deformation process. Here we present the first detailed characterization of the seismic activity taking place at LMVC and integrate it with structural data acquired in the field in order to illuminate the possible connection between the ongoing process of surface uplift and the activation of crustal faults. Our main finding is the recognition of repetitive volcano-tectonic (VT) seismic swarms that occur periodically between 2011 and 2014 near the SW corner of the sill modeled by InSAR studies. A cross-correlation analysis of the waveforms recorded for these VT events allows identifying three different seismic families. Families F1 and F3 share some common features in the stacked waveform and its locations, which markedly differ from those of family F2. Swarms belonging to this later family are more energetic and its energy was increasing since 2011 to a peak in January 2013, which coincide with maximum vertical velocities detected by local GPS stations. This points to a common process relating both phenomena. The location of VT seismic swarms roughly coincides with the intersection of a NE-SW lineament with a WNW-ESE lineament. The former shows clear field evidences of dextral strike-slip that are fully consistent with one nodal plane of focal mechanism for well-recorded F2 events. The conjugate nodal plane of these focal mechanisms could

Sobre el significado del descubrimiento del gen FOXP2

OpenAIRE

Longa Martínez, Víctor Manuel

2006-01-01

El reciente descubrimiento del gen FOXP2 ha ofrecido la primera evidencia clara de la base genética del lenguaje, mostrando una correlación inequívoca desde la perspectiva genética entre una versión mutada de F0XP2 y los trastornos lingüísticos de diferente tipo sufridos por una familia inglesa, conocida como KE. El objetivo central del presente trabajo es discutir diferentes aspectos relacionados con tal descubrimiento; especialmente, la discusión del significado de FOXP2 con ...

Late Pleistocene glaciations of the arid subtropical Andes and new results from the Chajnantor Plateau, northern Chile

Science.gov (United States)

Ward, Dylan J.; Cesta, Jason M.; Galewsky, Joseph; Sagredo, Esteban

2015-11-01

The spatiotemporal pattern of glaciation along the Andes Mountains is an important proxy record reflecting the varying influence of global and regional circulation features on South American climate. However, the timing and extent of glaciation in key parts of the orogen, particularly the deglaciated arid Andes, are poorly constrained. We present new cosmogenic 10Be and 36Cl exposure ages for glacial features on and near the Chajnantor Plateau (23 °S). The new dates, although scattered due to cosmogenic inheritance, imply that the most recent extensive glacial occupation ended before or during the global Last Glacial Maximum (LGM). We discuss this new record in the context of published glacial chronologies from glacial features in Peru, Bolivia, and northern Chile rescaled using the latest cosmogenic 10Be production rate calibration for the tropical Andes. The results imply regionally synchronous moraine stabilization ca. 25-40 ka, 15-17 ka, and 12-14 ka, with the youngest of these moraines absent in records south of ∼20 °S, including in our new Chajnantor area chronology. This spatial pattern implicates easterly moisture in generating sufficient snowfall to glaciate the driest parts of the Andes, while allowing a role for westerly moisture, possibly modulated by the migration of the Southern Westerly Wind belt, in the regions near and south of the Atacama Desert.

Disminución del índice de consumo de agua por caña molida en el central "Cristino Naranjo"

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Luis Enrique Rodríguez González

2008-01-01

Full Text Available Se presenta un conjunto de medidas, ejecutadas, en el central "Cristino Naranjo Vázquez", en el período de zafras desde 1998 hasta 2002, lográndose una disminución del índice de consumo de agua por caña molida desde 1,21 hasta 0,30 kg agua / kg caña. Se logra la reducción del costo de producción de cada 1 000 kg de azúcar en $ 2.00 MN y se contribuye a la conservación del medio ambiente por reducción de tala de árboles como combustible adicional, menor consumo de aguas subterráneas en 524 643,29 m3, volumen que a su vez no se vierte como residual líquido, por lo que se evita la contaminación de la cuenca del río Cauto.

On the extension of the analytic nodal diffusion solver ANDES to sodium fast reactors

International Nuclear Information System (INIS)

Ochoa, R.; Herrero, J.J.; Garcia-Herranz, N.

2011-01-01

Within the framework of the Collaborative Project for a European Sodium Fast Reactor, the reactor physics group at UPM is working on the extension of its in-house multi-scale advanced deterministic code COBAYA3 to Sodium Fast Reactors (SFR). COBAYA3 is a 3D multigroup neutron kinetics diffusion code that can be used either as a pin-by-pin code or as a stand-alone nodal code by using the analytic nodal diffusion solver ANDES. It is coupled with thermal-hydraulics codes such as COBRA-TF and FLICA, allowing transient analysis of LWR at both fine-mesh and coarse-mesh scales. In order to enable also 3D pin-by-pin and nodal coupled NK-TH simulations of SFR, different developments are in progress. This paper presents the first steps towards the application of COBAYA3 to this type of reactors. ANDES solver, already extended to triangular-Z geometry, has been applied to fast reactor steady-state calculations. The required cross section libraries were generated with ERANOS code for several configurations. Here some of the limitations encountered when attempting to apply the Analytical Coarse Mesh Finite Difference (ACMFD) method - implemented inside ANDES - to fast reactor calculations are discussed and the sensitivity of the method to the energy-group structure is studied. In order to reinforce some of the conclusions obtained two calculations are presented. The first one involves a 3D mini-core model in 33 groups, where the ANDES solver presents several issues. And secondly, a benchmark from the NEA for a small 3D FBR in hexagonal-Z geometry in 4 energy groups is used to verify the good convergence of the code in a few-energy-group structure. (author)

The forest vegetation of Ramal de Guaramacal in the Venezuelan Andes

NARCIS (Netherlands)

Cuello, A.N.L.; Cleef, A.M.

2009-01-01

Montane forest community composition of Ranial de Guaramacal, Venezuelan Andes, was studied along the altitudinal gradient on both sides of the range with different slope expositions. Thirty five 0.1 ha plots were Surveyed, with variable intervals of 30 to 150 meters between 1350 in and 2890 in and

The forest vegetation of Ramal de Guaramacal in the Venezuelan Andes

NARCIS (Netherlands)

Cuello A., N.L.; Cleef, A.M.

2009-01-01

Montane forest community composition of Ramal de Guaramacal, Venezuelan Andes, was studied along the altitudinal gradient on both sides of the range with different slope expositions. Thirty five 0.1 ha plots were surveyed, with variable intervals of 30 to 150 meters between 1350 m and 2890 m and

Capacidad antioxidante in vitro y efecto hipoglucemiante de la maca negra (Lepidium meyenii) preparada tradicionalmente

OpenAIRE

Troya-Santos, Jhon; Ale-Borja, Neptalí; Suárez-Cunza, Silvia

2017-01-01

La maca (Lepidium meyenii) es una planta peruana nativa de los Andes centrales a la que se le atribuyen diversas propiedades, como mejorar la función sexual y la espermatogénesis, mejorar el aprendizaje, y la reducción del estrés; las mismas que podrían estar relacionadas con la variedad de este hipocótilo. Sin embargo, estas propiedades no sólo están basadas en el ecotipo o el color sino también en el tipo de prácticas del procesamiento de la maca. Tradicionalmente, la maca es preparada haci...

Santuarios, peregrinaciones y fiestas patronales en la cultura regional boyacense

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Cesar Moreno

2005-10-01

Full Text Available Este artículo muestra resultados parciales del estudio relacionado con la religiosidad católica de los campesinos de los Andes Orientales colombianos, particularmente de las partes altas del Departamento de Boyacá. El tema central se organiza en torno al simbolismo de los santuarios donde se efectúan peregrinaciones y fiestas patronales que son elementos de construcción de identidad cultural y de memoria colectiva entre estas sociedades a nivel local y regional.Este artículo hace parte de la tesis doctoral, en la Universidad de Paris 8 en marzo de 2005.

Landscape structure and live fences in Andes Colombian agrosystems: upper basin of the Cane-Iguaque River

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Javier Otero

2009-12-01

economic and ecological interest, decreasing the pressure on natural forest. Improving the network of live fences constitutes an important strategy for the sustainable management of the rural landscape of the Andino orobiome of Colombia and similar areas in the tropics. Rev. Biol. Trop. 57 (4: 1183-1192. Epub 2009 December 01.El cambio del uso del suelo ha generado una nueva configuración del paisaje en el Orobioma Andino de los Andes tropicales, dando lugar a un mosaico de cultivos y potreros interrumpidos por pequeños fragmentos de bosque y cercas vivas, con la disminución sobre la biodiversidad de este bioma. En la cuenca alta del río Cane- Iguaque (Boyaca-Colombia, ubicada entre 2 600-3 000 metros de altitud sobre la cordillera Oriental, se realizó un estudio de caracterización de estructura, patrones y evolución del paisaje y de las cercas vivas, en tres periodos 1960, 1984 y 2004, como herramienta para la conservación de la biodiversidad y alternativa en el manejo de los sistemas agrícolas. Se utilizó una metodología de interpretación de imágenes de satélite de alta resolución, bajo el enfoque de la ecología del paisaje y la utilización de métricas del paisaje. El bosque original esta altamente transformado por pastizales y cultivos, las cercas vivas ocupan apenas el 4.6% del área de estudio pero por su distribución se constituyen en elementos importantes para la biodiversidad. Se observa un incremento en las cercas vivas, entre los años 1960 y 1984. Sin embargo en este mismo período se da una disminución en la longitud, debido a la tendencia de aumento en el cultivo de papa y por la extracción de recursos de madera y leña. Para la zona de estudio es muy importante la producción agrícola y la conservación de la biodiversidad, y puede ser mejorada mediante la utilización de cercas vivas. Por tanto, las cercas deben considerarse como elementos multifuncionales del paisaje que contribuyen en el mantenimiento de la biodiversidad y aportan

The Iberian hamlet of L’Alt del Punxó: agricultural production and peasant settlement in central Contestania | La aldea ibérica de L’Alt del Punxó: producción agrícola y asentamiento campesino en el área central de la Contestania

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Israel Espí Pérez

2009-12-01

Full Text Available In this paper we describe an Iberian Iron Age village recently excavated as a result of the construction of a new motorway through Muro de l’Alcoi (El Comtat, Alicante province, Spain. The hamlet consists of huts, agricultural buildings and a paved road dating to between the seventh and fourth centuries BC. L’Alt del Punxó has significantly advanced our knowledge of Iberian settlement patterns and the organisation of economic activity in this area. An integrated analysis of the evidence furnished by the fieldwork increases our knowledge of different aspects of the social and economic organization of Iberian Iron Age populations in central Contestania. | En este trabajo damos a conocer un hábitat rural de época ibérica excavado con motivo de recientes obras de construcción de la Autovía del Mediterráneo a su paso por la localidad de Muro de l’Alcoi (El Comtat, Alacant. La aldea está conformada por cabañas, instalaciones de procesamiento agrícola y un camino empedrado que se datan entre los ss. VII y IV aC. L’Alt del Punxó ha permitido un considerable avance en el conocimiento de las formas de ocupación rural y articulación de la actividad económica de este territorio ibérico. La lectura integrada de la documentación permite abordar distintas cuestiones de la organización económica y social de los grupos ibéricos del área central de la Contestania.

Palm harvest impact in the western Amazon, Andes and Pacific lowlands

DEFF Research Database (Denmark)

Balslev, Henrik

2011-01-01

Palms are the most useful group of plants in tropical American forests and in this project we study the effect of extraction and trade of palms on forests in the western Amazon, Andes, and Pacific lowlands. We determine the size of the resource by making palm community studies in the different...

Reconstrucción espacial y temporal de la ocurrencia de avalanchas de nieve en los Andes patagónicos utilizando técnicas dendrocronológicas Dendrochronological reconstruction of spatial and temporal patterns of snow avalanches in the Patagonian Andes

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ALEJANDRO CASTELLER

2009-06-01

Full Text Available Las avalanchas de nieve representan un importante riesgo natural en diversas regiones montañosas alrededor del mundo. Daños a infraestructura y pérdidas de vidas humanas son reportados frecuentemente en relación a eventos catastróficos de avalanchas. En los Andes, numerosas obras de infraestructura se ubican en zonas vecinas a senderos de avalanchas, de las que poco se conoce sobre sus alcances máximos, periodos de retorno y presiones de impacto. A través de la implementación de técnicas dendrocronológicas hemos reconstruido las fechas de ocurrencia y áreas de influencia de eventos pasados de avalanchas de nieve. Ejemplares de Nothofagus pumilio con perturbaciones visibles de avalanchas fueron muestreados en sectores del canal, bordes y zonas de frenado de 11 senderos de avalanchas ubicados en Loma de las Pizarras, próximo a El Chaltén, Santa Cruz, Argentina. Además, áreas de control fueron muestreadas para determinar las condiciones de crecimiento en árboles no afectados por avalanchas. Nuestros análisis indican que las cicatrices, las variaciones de excentricidad en el leño, los cambios abruptos de crecimiento y la presencia de leño de tensión son los principales indicadores dendrocronológicos en N. pumilio asociados a la ocurrencia de avalanchas. Basados en una ponderación cuantitativa de los indicadores y en la profundidad de muestreo, calculamos un índice de ocurrencia de eventos, el cual nos permitió determinar para cada sendero los años con ocurrencia de avalanchas. Considerando de manera integral la actividad de avalanchas en los 11 senderos muestreados, los años con mayor ocurrencia de eventos fueron 1936, 1966, 1978 y 1995. Complementariamente, registros climáticos fueron analizados con el objetivo de determinar las relaciones entre los años con ocurrencia de avalanchas y las variaciones mensuales de precipitación y temperatura. Se observa que los años con gran frecuencia de avalanchas est

The effect of central contracts on the stability and performance of the England Test cricket team. [El efecto de contratos centrales sobre la estabilidad y el desempeño del equipo inglés de Test cricket].

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Steven Bullough

2014-01-01

Full Text Available In 1999 the England and Wales Cricket Board (ECB decided to implement central contracts for elite player management to give them control over a group of players to represent the England national team in Test cricket. The purpose of this paper is to investigate the impact that this change in policy has had on the stability and performance of the England Test team, and discuss implications thereof. Using a sample of 13 seasons pre-central contracts (1987-1999 and 13 seasons post-central contracts (2000-2012, the results, from secondary analysis of England’s Test match scorecards from both sample periods, allowed investigation of team performance and stability. To gain a greater understanding of how central contracts impacted on the England Test side, eight interviews were also organised with key stakeholders in English cricket. The results showed that both the stability and performance of the England Test side improved considerably in the sample period post-central contracts (2000-2012 with a much greater consistency of selection (fewer changes per match alongside an improvement in England’s on-field performance (better win ratio and points per match. The paper identifies two key challenges facing the current player management system in England from domestic and external sources. Resumen En 1999 El Consejo de Cricket en Inglaterra y Gales (ECB – England and Wales Cricket Board decidió implementar contratos centrales para la dirección de jugadores de élite, con el fin de darle control sobre el grupo de jugadores que representan el equipo nacional de Inglaterra de Test cricket. El objetivo de este artículo es investigar el impacto que este cambio ha tenido sobre la estabilidad y el desempeño del equipo inglés de Test cricket y considerar sus implicaciones. Tras emplear una muestra de 13 temporadas antes de la firma de los contratos centrales (entre 1987 y 1999 y otras 13 temporadas después de su implementación (entre 2000 y 2012, los

Variabilidad espacial y temporal de la temperatura del aire en la zona cafetera colombiana

OpenAIRE

Edna Paola Pérez Rendón; Víctor Hugo Ramírez Builes; Andrés Javier Peña Quiñones

2016-01-01

La zona cafetera colombiana está ubicada en- teramente en el hemisferio norte, entre los 1 y 11° grados de latitud, sobre la cordillera de los Andes. Esta condición (ecuatorial andina) ha hecho que se dé por sentado que la variación temporal de la temperatura es mínima y que por ello, en su mayor parte la variabilidad de este elemento es es- pacial, atribuible casi exclusivamente a los cambios en altura sobre el nivel del mar. En este estudio se exploran factores de variación al...

Evolution of the Chos Malal and Agrio fold and thrust belts, Andes of Neuquén: Insights from structural analysis and apatite fission track dating

Science.gov (United States)

Rojas Vera, E. A.; Mescua, J.; Folguera, A.; Becker, T. P.; Sagripanti, L.; Fennell, L.; Orts, D.; Ramos, V. A.

2015-12-01

The Chos Malal and Agrio fold and thrust belts are located in the western part of the Neuquén basin, an Andean retroarc basin of central-western Argentina. Both belts show evidence of tectonic inversion at the western part during Late Cretaceous times. The eastern part is dominated by late Miocene deformation which also partially reactivated the western structures. This work focuses on the study of the regional structure and the deformational event that shaped the relief of this part of the Andes. Based on new field work and structural data and previously published works a detailed map of the central part of the Neuquén basin is presented. Three regional structural cross sections were surveyed and balanced using the 2d Move™ software. In order to define a more accurate uplift history, new apatite fission track analyses were carried on selected structures. These data was used for new thermal history modeling of the inner part of the Agrio and Chos Malal fold and thrust belts. The results of the fission track analyses improve the knowledge of how these fold and thrust belts have grown trough time. Two main deformational events are defined in Late Cretaceous to Paleocene and Late Miocene times. Based on this regional structural analysis and the fission track data the precise location of the orogenic front for the Late Cretaceous-Paleocene times is reconstructed and it is proposed a structural evolution of this segment of the Andes. This new exhumation data show how the Late Cretaceous to Paleocene event was a continuous and uninterrupted deformational event.

Recherches préliminaires en laboratoire sur les céramiques de Piruru (Andes Centrales

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1985-01-01

Full Text Available A partir de l'analyse par fluorescence X de 44 tessons de céramique provenant de la fouille de Piruru, et de 11 prélèvements d'argile recueillis tant à Piruru que dans la vallée du Tantamayo, est proposée une classification du matériel qui est représentée par un dendro-gramme. Cette première étude en laboratoire permet de réfléchir sur la validité des types céramiques déjà définis, et d'émettre des hypothèses de travail sur les structures de production et l'origine des céramiques. A partir del análisis por fluorescencia X de 44 tiestos de cerámica procedentes de la excavación de Piruru, y de 11 muestras de arcilla recogidas tanto en Piruru como en el valle del Tantamayo, se propone una clasificación del material que está representada por un dendrograma. Este primer estudio en laboratorio permite reflexionar sobre la validez de los tipos cerámicos ya definidos, y plantear hipótesis de trabajo sobre las estructuras de producción y el origen de las cerámicas.

Recent increase in the distribution of the snail kite (Rostrhamus sociabilis along the central Pacific Coast of México Incrementos de la distribución del gavilán caracolero (Rostrhamus sociabilis en la costa del Pacífico central de México

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Salvador Hernández-Vázquez

2013-03-01

Full Text Available New records of the snail kite (Rostrhamus sociabilis are presented for the central Pacific Coast of Mexico. From April 2010 to August 2011, weekly or biweekly surveys were made through several wetlands of coastal Jalisco and Colima. We recorded 32 snail kites from October 2010 to August 2011. The recordings were in 8 wetlands. In all wetlands there was only 1 individual, except in the lagoons El Aguacate (June 2010 and El Tule (August 2012, where we recorded 3 and 5 individuals, respectively. Although we did not find any nests, we believe reproduction of snail kites is currently occurring because of the observed adult behavior (carrying small branches in its feet and the records of juveniles during the month of February to July, a time corresponding to the breeding season of the species in Florida. Our records expand the distribution of the snail kite in Mexico as much as 900 km northwest of the previously published distribution of the species.Presentamos nuevas observaciones del gavilán caracolero (Rostrhamus sociabilis para la costa del Pacífico central mexicano. De abril de 2010 a agosto de 2011 se realizaron visitas semanales o quincenales a varios humedales costeros de Jalisco y Colima. Se observaron 32 individuos entre octubre del 2010 y agosto del 2011 en 8 humedales. En todos los humedales se registró sólo 1 individuo, excepto en las lagunas El Aguacate (junio de 2011 y El Tule (agosto de 2012, donde se observaron 3 y 5 individuos, respectivamente. Aunque no se han registraron nidos, consideramos que es probable que la reproducción del gavilán caracolero está ocurriendo actualmente en la región debido a la conducta observada de algunos adultos (p. ej. llevando ramas pequeñas en sus patas y a la presencia de los juveniles durante los meses de febrero a julio, tiempo en el que ocurre la anidación de la especie en Florida. Nuestras observaciones incrementan la distribución del gavilán caracolero en México a cerca de 900 km al

Contrasting Climate Change Impact on River Flow from Glacierised Catchments in the Himalayan and Andes Mountains

Science.gov (United States)

Pellicciotti, F.; Ragettli, S.; Immerzeel, W. W. W.

2016-12-01

Glaciers and glacierised catchments in mountainous regions react to a changing climate in different manners depending on climate and glacier characteristics. Despite the key role of mountain ranges as natural water towers, their hydrological balance and future changes in glacier runoff associated with climate warming remain poorly understood because of high meteorological variability, physical inaccessibility and the complex interplay between climate, cryosphere and hydrological processes. We use a state-of-the art glacio-hydrological model informed by data from high altitude observations and the latest CMIP5 climate change scenarios to quantify the climate change impact on glaciers and runoff for two contrasting catchments vulnerable to changes in the cryosphere. The two catchments are located in the Central Andes of Chile and in the Nepalese Himalaya in close vicinity of densely populated areas. Although both sites are projected to experience a strong decrease in glacier area, they show remarkably different hydrological responses. Icemelt is on a rising limb in Langtang at least until 2041-2050 and starts to decrease afterwards, while in Juncal icemelt was already beyond its tipping point at the beginning of the 21st century. This contrasting response can be explained by differences in the elevation distribution of the glaciers in the two regions. In Juncal, many glaciers are melting up to the highest elevations already during the reference period (2000-2010) and increasing melt rates due to higher air temperatures cannot compensate the loss of glacier area. In Langtang, large sections of the glaciers at high elevations are currently not exposed to melt, but will be in the future, thus compensating for the loss of glacier area at lower elevations. As a result of these changes and projected changes in precipitation, in Juncal runoff will sharply decrease in the future and the runoff seasonality is sensitive to projected climatic changes. In Langtang, future water

BURMEISTERA DIAZII(CAMPANULACEAE: LOBELIOIDEAE, UNA ESPECIE NUEVA DE LOS ANDES DE ANTIOQUIA, Y NOTAS ACERCA DEL NUEVO REGISTRO DE B. LOEJTNANTII PARA COLOMBIA

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JAVIER GARZÓN VENEGAS

2014-12-01

Full Text Available Burmeistera diazii (Campanulaceae: Lobelioideae, de la Cordillera Central de Colombia, en la franja altitudinal entre 1,800 y 2,750 m en los municipios de Sonsón y Guatapé (Antioquia, es descrita como una especie nueva. Se discuten en detalle las semejanzas morfológicas con sus especies afines (B. obtusifolia, de Costa Rica y Panamá, B. killipii y B. serraniaguae, de Colombia y B. crassifolia y B. loejtnantii, de Colombia y Ecuador, las cuales se caracterizan por tener hojas ovadas a ovado-lanceoladas, pedúnculo ebracteado y lóbulos del cáliz largos. Se registra B. loejtnantii por primera vez para la flora de Colombia.

Estudio del sistema nervioso central en pacientes con anemia drepanocítica Study of the central nervous system in patients with drepanocytic anemia

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Edgardo Espinosa Martínez

2008-08-01

Full Text Available Se estudiaron 35 pacientes adultos con anemia drepanocítica. Se establecieron 2 grupos: grupo 1: 24 enfermos sin antecedentes de crisis del sistema nervioso central (15 hombres; 9 mujeres y grupo 2: 11 casos con antecedentes de crisis (6 hombres; 5 mujeres. El promedio de edad fue de 31 años en el sexo masculino y de 29 años en el femenino. Todos los enfermos estaban en condiciones basales. El tiempo transcurrido entre la crisis y el estudio fue de 4,7 años. No hubo diferencia significativa en las cifras de hemoglobina y los reticulocitos entre ambos grupos. Se encontró aumento significativo de la velocidad sanguínea cerebral en todos los pacientes del grupo 1 y del grupo 2 (p 35 adult patients with drepanocytic anemia were studied. They were divided into 2 groups: group 1 was composed of 24 patients without history of central nervous system crisis (15 males and 9 females, whereas group 2 included 11 cases with crisis history (6 males and 5 females. Average age was 31 years old for males and 29 for females. All the patients were under basal conditions. The time elapsed between the crisis and the study was 4.7 years. No significant differences were observed between the hemoglobin figures and the reticulocytes of both groups. A marked increase of the brain blood velocity was found in all the patients from group 1 and group 2 (p < 0.05 y p < 0.001, respectively. In 13 patients from group 1 (54.1 % the brain blood flow presented modifications, whereas it was altered in all patients from group 2. In 13 cases from group 1 (76.4 % the electroencephalogram was normal, but it was altered in 87.5 % of the patients from group 2. In 4 patients from group 1 (23.5 %, the brain electrical activity showed some modification. Computerized axial tomography was normal in 19 patients from group 1. Some alteration was detected in 3 cases from group 2 (37.5 %.

Evaluacion del factor central y periferico en fatiga muscular en pacientes com daño piramidal

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Carlos G. Schutz

1983-09-01

Full Text Available Para evaluar algunos de los componentes de la fatiga muscular en el daño piramidal, se seleccionó un grupo de 15 pacientes con hemiparesia faciobraquiocrural de severidad variable, los cuales fueron sometidos a un esfuerzo muscular, durante el cual se evaluaron los cambios de la frecuencia y duración de los potenciales positivos y negativos del EMG, asi como los sufridos por la onda M máxima al principio y fin del mismo. El estudio fue realizado en el lado parético, el contralateral y en un grupo control de voluntarios sanos, comparándose los resultados de los 3 grupos. Las curvas de frecuencia y duración del lado parético, el sano y el control mantuvieron las mismas tendencias, así como fue homologable el comportamiento de la onda M máxima en los 3 casos, lo cual indica que en la espasticidad, debido a daño de la vía piramidal, al igual que en la población normal, bajo las presentes condiciones de estudio, es el factor central el condicionante principal en el desarrollo de fatiga muscular.

Geology, petrology and geochemistry of the dome complex of Huequi volcano, southern Chile Geología, petrología y geoquímica de los domos volcánicos del volcán Huequi, Chile meridional

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Sebastian F.L Watt

2011-07-01

Full Text Available Huequi, a little-known volcano in the southern part of the Andean southern volcanic zone (SSVZ, shows a regionally unusual eruption style, mineralogy and geochemistry. The volcano comprises multiple highly-eroded lava domes. Past eruptions were accompanied by relatively minor explosive activity, most recently from 1890-1920. The rocks erupted by Huequi range from basaltic andesite to dacite, and are highly distinctive when compared to other volcanoes of the SSVZ, being K-poor and Al-rich, and containing euhedral hornblende phenocrysts. Overall compositions suggest a notably water-rich magma source, evolving through high levels of fractionation and subsequent degassing to produce highly porphyritic dome-forming andesites. The ultimate causes of water-rich magmas at this point in the arc remain unclear.El volcán Huequi es poco conocido, que se ubica en la provincia sur de la zona Volcánica Sur de los Andes (ZVSS. Sus tipos de erupción y características mineralógicas y geoquímicas son poco comunes a nivel regional. El volcán presenta múltiples domos poco erosionados. Las erupciones estuvieron acompañadas por una actividad explosiva secundaria, siendo las más recientes las ocurridas entre los años 1890 y 1920. Los magmas del Huequi son de composición andesítico-basáltica a dacítica. Si se las compara con rocas eruptadas por otros centros volcánicos de la ZVSS de los Andes, las del Huequi se caracterizan por ser pobres en K, ricas en Al y por presentar fenocristales euhedrales de anfíbola. Las composiciones totales sugieren una fuente magmática rica en H2O, que se desarrolla a través de niveles de cristalización fraccionada y desgasificación subsecuente, que producen domos volcánicos andesíticos altamente porfíricos. Sin embargo, la causa última que genera magmas ricos en H2O, en esta parte de los Andes, sigue aún sin explicación.

Caracterización de la circulación atmosférica y la temperatura superficial del mar asociadas a extremos de caudal de ríos andinos y su variabilidad en baja frecuencia

OpenAIRE

Araneo, Diego C.

2006-01-01

El objetivo principal del presente trabajo se centra en determinar los mecanismos asociados a la variabilidad de los caudales de los ríos andinos en relación con la circulación atmosférica y la Temperatura Superficial del Mar (TSM) como forzante del sistema climático. Para la circulación atmosférica el estudio se extiende desde la escala sinóptica a la climática. A lo largo de la Cordillera de los Andes se identifican dos zonas en las cuales el comportamiento de los caudales de los ríos muest...

Cómo los indígenas mejoran su calidad de vida a través del desistimiento. Protección de reservas de agua en Ecuador

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Oliver Hoelcke

2013-09-01

Full Text Available La gente en Los Andes lucha por cada gota de agua. De ese líquido vital dependen cientos de miles de personas que habitan en el valle. Sin embargo, cada año llega menos agua a los pequeños poblados. Garantizar el abastecimiento del recurso es la meta de El Plan de Manejo Páramo.

Imposex en Crassilabrum crassilabrum (Neogastropoda: Muricidae) en la costa central del Perú: Imposex in Crassilabrum crassilabrum (neogastropoda: muricidae) in the peruvian central coast

OpenAIRE

Rivas, Rolf; Pradel, Renzo; Hurtado, Soledad; Cornelio, Dayanne; Mendoza, Jorge; Guabloche, Angélica; Iannacone, José; Alvariño, Lorena; Castañeda, Luz

2017-01-01

El imposex es un fenómeno que consiste en el desarrollo de caracteres sexuales masculinos sobre el sistema reproductivo de las hembras de caracoles gasterópodos por la contaminación por compuestos organoestañosos (OTs), como el tributil estaño (TBT). En el presente trabajo se evaluó el imposex en Crassilabrum crassilabrum Sowerby, 1834 (Neogastropoda: Muricidae) proveniente de la costa central del Perú, para lo cual se analizaron individuos colectados de la zona intermareal de Pucusana y Ancó...

Concesión del monopolio de juegos de apuestas y azar en elvalle del cauca1

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Julio César Alonso Cifuentes, Ph.D

2010-07-01

Full Text Available La Beneficencia del Valle del Cauca (Colombia contrató con el CIENFI de la Universidad Icesi una consultoría que serviría como base para la licitación por la concesión de las apuestas permanentes en cinco zonas del Valle del Cauca. Uno de los resultados fundamentales del estudio era la proyección de las ventas brutas, que se basa, entre otras cosas, en una medida de tendencia central de la inversión en apuestas permanentes (chance de aquí en adelante por persona en el año. En el caso se presenta información relevante para la toma de decisión sobre la medida de tendencia central pertinente para la proyección de las ventas de chance y por lo tanto del valor de la concesión.

Imaging the lithospheric structure of the Central Andes from the joint inversion of multiple seismic data sets

Science.gov (United States)

Ward, Kevin Michael

A lingering question in Cordilleran tectonics is how high plateaus form in the absence of continental collision. The type example of an active Cordilleran high plateau is found in the Central Andes of Peru, Bolivia, Argentina, and Chile. Along this section of the South American Cordillera, tectonics are primarily driven by subduction of the oceanic Nazca Plate beneath the continental South American Plate. Extending over 1,800 km along the active continental margin, the Central Andean Plateau (CAP) reaches a maximum width of around 400 km with several peaks in excess of 6 km. Numerous morphotectonic subdivisions of the CAP highlight the complex along-strike variability of the Plateau providing a natural laboratory for investigating the relative contribution of tectonic processes involved in building and maintaining Cordilleran high plateaus. The scale of this problem extends far beyond the scope of any one geoscientific discipline requiring a multidisciplinary approach. Our contribution to this scientific problem and the focus of the work presented in this dissertation is to better understand the current lithospheric and uppermost mantle structure along the CAP. This is achieved by integrating recent advances in seismic imaging techniques with a growing availability of high-quality seismic data into three distinct studies across the South American continent. In the first study, we present a shear-wave velocity model for the crust below the Altiplano-Puna Volcanic Complex (APVC). The target of this study is to constrain the crustal volume of a large magma reservoir inferred to exist below the APVC. When combined with geological and petrological constraints, the large-volume magma reservoir imaged in this study suggests a significant magmatic contribution to the growth of the Plateau in excess of one kilometer over the last ten million years. In addition to the tectonic contributions of this work, we introduce a new method of jointly inverting surface-wave dispersion

On the generation of coastal lows in central Chile

International Nuclear Information System (INIS)

Rutllant, J.

1994-07-01

Previous studies of the coastal-low occurrences in central Chile have been aimed at the formulation of a conceptual model to explain observed features in connection with applied studies. The most prominent weather pattern associated with CL occurrences, (type A), coincides with the onset of a warm, middle-troposphere ridge over central Chile, and a surface high over northern Argentina. The synoptic forcing of the low is related to weak frontal disturbances that travel equatorwards. They result in a thickening of the marine layer that becomes blocked by the coastal escarpment, at the time of the onset of the ridge aloft. The blocking of the stable air above the subsidence inversion by the Andes is also hypothesized. The analysis of the subsidence inversion, the geometry of the coastal and Andes mountain ranges, and a scale analysis of the non-dimensional governing equations for the generation of the coastal lows, following the approach of Reason and Steyn (1990); leads to the conclusion that both blocking actions are strong and persistent in central Chile. An interactive mechanism between the upper and lower blocking effects is postulated to explain the cyclonic vorticity and the initial steering of the coastal lows. The scale analysis of the governing equations for the propagation stage of the low suggests that, departing for the South African case, non-linearity is important here, and that solitary Kelvin waves could be expected. Theoretical phase propagation speeds and Rossby radii are found to range between 8 and 15 m s-1 and 100-250 km, respectively. The importance of strong southerly winds ahead of the low and weak winds at its trailing edge is also stressed, as another major departure from the coastal-low behaviour elsewhere. (author). 17 refs, 4 figs, 4 tabs

Aproximación a un modelo de indicadores de alerta temprana considerando la función de pérdida del Banco Central

OpenAIRE

Armagno, Daniel; García Fronti, Javier; Rey, Sebastián

2004-01-01

Nuestro interés en este trabajo es estudiar las causas que llevan al debilitamiento de las entidades bancarias. Para ello incluiremos en el análisis, al responsable de la toma de decisiones del Banco Central que tiene en consideración una función de pérdida del tipo desarrollada en Dermirgüç–Kunt, A. and E. Detragiache (1999). Aplicando un modelo logit y evaluamos los resultados obtenidos.

Estimates of Carbon Reservoirs in High-Altitude Wetlands in the Colombian Andes

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Enrique Javier Peña

2009-10-01

Full Text Available The observed increase in emission of greenhouse gases, with attendant effects on global warming, have raised interests in identifying sources and sinks of carbon in the environment. Terrestrial carbon (C sequestration involves capture of atmospheric C through photosynthesis and storage in biota, soil and wetlands. Particularly, wetland systems function primarily as long-term reservoirs for atmospheric carbon dioxide (CO2 and as sources of atmospheric methane (CH4. The objective of this study was to evaluate the patterns of carbon reservoirs in two high-altitude wetlands in the central Andean mountain of Colombia. Carbon cycle in both systems is related mainly with the plant biomass dynamics from the littoral zone. Thus, total organic carbon concentrate an average up to 329 kg of N ha-1 and 125 kg of P ha-1 every year vs only 17 kg N ha-1 and 6 kg P ha-1 in the water column of the limnetic zone in the wetland, evidencing spatial differences in carbon concentrations for these types of ecosystems. Results revealed that these systems participate in the balance and sequestration of carbon in the Colombian Andes.

De estructuras, culturas y otros demonios: una revisión de las insurrecciones andinas de finales del siglo XVIII

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Hanni Jalil Paier

2011-07-01

Full Text Available Este ensayo observa las insurrecciones populares del siglo XVIII no como episodios casuales o aislados, sino como síntomas de un sentimiento generalizado de descontento social e intensificado conflicto. Sentimientos cuya intensidad se incrementó durante la segunda mitad del siglo XVIII y culminó con la Gran Rebelión de 1780-1783 en el sur de los Andes, el levantamiento en Quito de 1765 y la Rebelión de los Comuneros en la Nueva Granada de 1781. Este artículo examina los trabajos que hacen referencia a estas revueltas, reconociendo el hecho que la producción académica de las insurrecciones de finales del siglo XVIII en las colonias americanas forman parte de los amplios debates académicos que abordan las insurrecciones fuera del contexto Andino, e incorpora preguntas promulgadas por los estudiosos de las revueltas campesinas y el conflicto armado en otros campos y otros periodos.

Impact of glaciations on the long-term erosion in Southern Patagonian Andes

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Simon-Labric, Thibaud; Herman, Frederic; Baumgartner, Lukas; Shuster, David L.; Braun, Jean; Reiners, Pete W.; Valla, Pierre G.; Leuthold, Julien

2014-05-01

The Southern Patagonian Andes are an ideal setting to study the impact of Late-Cenozoic climate cooling and onset of glaciations impact on the erosional history of mountain belts. The lack of tectonic activity during the last ~12 Myr makes the denudation history mainly controlled by surface processes, not by tectonics. Moreover, the glaciations history of Patagonia shows the best-preserved records within the southern hemisphere (with the exception of Antarctica). Indeed, the dry climate on the leeward side of Patagonia and the presence of lava flows interbedded with glacial deposits has allowed an exceptional preservation of late Cenozoic moraines with precise dating using K-Ar analyses on lava flow. The chronology of moraines reveals a long history covering all the Quaternary, Pliocene, and up to the Upper Miocene. The early growth of large glaciers flowing on eastern foothills started at ~7-6 Myr, while the maximum ice-sheet extent dates from approximately 1.1 Myr. In order to quantify the erosion history of the Southern Patagonian Andes and compare it to the glaciations sediment record, we collected samples along an age-elevation profile for low-temperature thermochronology in the eastern side of the mountain belt (Torres del Paine massif). The (U-Th)/He age-elevation relationship shows a clear convex shape providing an apparent long-term exhumation rate of ~0.2 km/Myr followed by an exhumation rate increase at ~6 Myr. Preliminary results of 4He/3He thermochronometry for a subset of samples complete the erosion history for the Plio-Pleistocene epoch. We used inverse procedure predicting 4He distributions within an apatite grain using a radiation-damage and annealing model to quantify He-diffusion kinetics in apatite. The model also allows quantifying the impact of potential U-Th zonation throughout each apatite crystal. Inversion results reveal a denudation history composed by a pulse of denudation at ~6 Ma, as suggested by the age-elevation relationship

Hybrid Literacies: The Case of a Quechua Community in the Andes

Science.gov (United States)

de la Piedra, Maria Teresa

2009-01-01

Drawing on data from an ethnographic study in a Quechua rural community in the Peruvian Andes, this article examines hybrid literacy practices among bilingual rural speakers in the context of the household and the community. I examine the coexistence of two types of textual practices that operate side by side, at times integrated in the same…

Ilustración arqueológica en los Andes (1850-1890

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Joanne Pillsbury

Full Text Available Resumen En términos generales, es posible trazar en las publicaciones europeas sobre los Andes una trayectoria histórica en el curso de cuatro siglos, desde un sistema de representación que está íntimamente atado – y afiliado – a la palabra escrita, a uno donde las imágenes se convierten en la razón de ser de la publicación. Esta trayectoria refleja el campo de la arqueología en sí mismo, desde sus orígenes en una tradición de anticuarios dominada por las preocupaciones filológicas durante los siglos XVI y XVII, al siglo XIX, donde las evidencias fotográficas ganan fuerza frente a las escritas. Este documento se centra en el pico de esta trayectoria: los atlas arqueológicos creados entre 1850 y 1890, en particular el trabajo de Wilhelm Reiss y Alphons Stübel y su publicación en tres volúmenes titulada “The necropolis of Ancon in Peru” (“La necrópolis de Ancón en el Perú”. El presente estudio analiza el papel de la ilustración arqueológica en la iluminación, la difusión y comprensión de un pasado pre-inca durante el siglo XIX, y en última instancia, cómo las imágenes dan forma a la construcción del conocimiento.

ISOSTATICALLY DISTURBED TERRAIN OF NORTHWESTERN ANDES MOUNTAINS FROM SPECTRALLY CORRELATED FREE-AIR AND GRAVITY TERRAIN DATA

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Hernández P Orlando

2006-12-01

Full Text Available Recently revised models on global tectonics describe the convergence of the North Andes, Nazca, Caribbean and South American Plates and their seismicity, volcanism, active faulting and extreme
topography. The current plate boundaries of the area are mainly interpreted from volcanic and seismic datasets with variable confidence levels. New insights on the isostatic state and plate boundaries of
the northwestern Andes Mountains can be obtained from the spectral analysis of recently available gravity and topography data.
Isostatically disturbed terrain produces free-air anomalies that are highly correlated with the gravity effects of the terrain. The terrain gravity effects (TGE and free air gravity anomalies (FAGA of the
Andes mountains spectral correlation data confirms that these mountains are isostatically disturbed. Strong negative terrain-correlated FAGA along western South America and the Greater and Lesser Antilles are consistent with anomalously deepened mantle displaced by subducting oceanic plates.

Inversion of the compensated terrain gravity effects (CTGE reveals plate subduction systems with alternating shallower and steeper subduction angles. The gravity modeling highlights crustal
deformation from plate collision and subduction and other constraints on the tectonism of the plate boundary zones for the region.

Automated recognition of quasi-planar ignimbrite sheets and paleo-surfaces via robust segmentation of DTM - examples from the Western Cordillera of the Central Andes

Science.gov (United States)

Székely, B.; Karátson, D.; Koma, Zs.; Dorninger, P.; Wörner, G.; Brandmeier, M.; Nothegger, C.

2012-04-01

The Western slope of the Central Andes between 22° and 17°S is characterized by large, quasi-planar landforms with tilted ignimbrite surfaces and overlying younger sedimentary deposits (e.g. Nazca, Oxaya, Huaylillas ignimbrites). These surfaces were only modified by tectonic uplift and tilting of the Western Cordillera preserving minor now fossilized drainage systems. Several deep, canyons started to form from about 5 Ma ago. Due to tectonic oversteepening in a arid region of very low erosion rates, gravitational collapses and landslides additionally modified the Andean slope and valley flanks. Large areas of fossil surfaces, however, remain. The age of these surfaces has been dated between 11 Ma and 25 Ma at elevations of 3500 m in the Precordillera and at c. 1000 m near the coast. Due to their excellent preservation, our aim is to identify, delineate, and reconstruct these original ignimbrite and sediment surfaces via a sophisticated evaluation of SRTM DEMs. The technique we use here is a robust morphological segmentation method that is insensitive to a certain amount of outliers, even if they are spatially correlated. This paves the way to identify common local planar features and combine these into larger areas of a particular surface segment. Erosional dissection and faulting, tilting and folding define subdomains, and thus the original quasi-planar surfaces are modified. Additional processes may create younger surfaces, such as sedimentary floodplains and salt pans. The procedure is tuned to provide a distinction of these features. The technique is based on the evaluation of local normal vectors (perpendicular to the actual surface) that are obtained by determination of locally fitting planes. Then, this initial set of normal vectors are gradually classified into groups with similar properties providing candidate point clouds that are quasi co-planar. The quasi co-planar sets of points are analysed further against other criteria, such as number of minimum

A phytosociological analysis and synopsis of the dry woodlands and succulent vegetation of the Peruvian Andes

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ANTONIO GALÁN-DE-MERA

2016-01-01

Full Text Available ABSTRACT A phytosociological approach to dry forest and cactus communities on the occidental slopes of the Peruvian Andes is presented in base of 164 plots carried out following the Braun-Blanquet method. From them, 52 have been made recently, and the other 112 were taken from the literature. After a multivariate analysis, using a hierarchical clustering and a detendred correspondence analysis, the Acacio-Prosopidetea class (dry forest and cactus communities, developed on soils with some edaphic humidity or precipitations derived from El Niño Current, the Opuntietea sphaericae class (cactus communities of central and southern Peru, on few stabilized rocky or sandy soils and the Carico-Caesalpinietea class (dry forests of the Peruvian coastal desert, influenced by the maritime humidity of the cold Humboldt Current, are differentiated. Within the Acacio-Prosopidetea class, two alliances are commented: the Bursero-Prosopidion pallidae (with two new associations Loxopterygio huasanginis-Neoraimondietum arequipensis and Crotono ruiziani-Acacietum macracanthae, and the new alliance Baccharido-Jacarandion acutifoliae (with the new associations Armatocereo balsasensis-Cercidietum praecocis and Diplopterydo leiocarpae-Acacietum macracanthae. For the Opuntietea sphaericae class, the association Haageocereo versicoloris-Armatocereetum proceri (Espostoo-Neoraimondion is described on the basis of plots from hyperarid localities of central Peru. Finally, a typological classification of the studied plant communities is given.

A phytosociological analysis and synopsis of the dry woodlands and succulent vegetation of the Peruvian Andes.

Science.gov (United States)

Galán-DE-Mera, Antonio; Sánchez-Vega, Isidoro; Linares-Perea, Eliana; Campos, José; Montoya, Juan; Vicente-Orellana, José A

2016-01-01

A phytosociological approach to dry forest and cactus communities on the occidental slopes of the Peruvian Andes is presented in base of 164 plots carried out following the Braun-Blanquet method. From them, 52 have been made recently, and the other 112 were taken from the literature. After a multivariate analysis, using a hierarchical clustering and a detendred correspondence analysis, the Acacio-Prosopidetea class (dry forest and cactus communities, developed on soils with some edaphic humidity or precipitations derived from El Niño Current), the Opuntietea sphaericae class (cactus communities of central and southern Peru, on few stabilized rocky or sandy soils) and the Carico-Caesalpinietea class (dry forests of the Peruvian coastal desert, influenced by the maritime humidity of the cold Humboldt Current), are differentiated. Within the Acacio-Prosopidetea class, two alliances are commented: the Bursero-Prosopidion pallidae (with two new associations Loxopterygio huasanginis-Neoraimondietum arequipensis and Crotono ruiziani-Acacietum macracanthae), and the new alliance Baccharido-Jacarandion acutifoliae (with the new associations Armatocereo balsasensis-Cercidietum praecocis and Diplopterydo leiocarpae-Acacietum macracanthae). For the Opuntietea sphaericae class, the association Haageocereo versicoloris-Armatocereetum proceri (Espostoo-Neoraimondion) is described on the basis of plots from hyperarid localities of central Peru. Finally, a typological classification of the studied plant communities is given.

Patrones de diversidad alfa en tres fragmentos de bosques montanos en la región norte de los Andes, Colombia

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Wilson López

2010-03-01

Full Text Available En el presente trabajo se analizaron los patrones de diversidad alfa en tres áreas protegidas de bosque con base en información florística proveniente de seis parcelas permanentes de 1ha -dos en cada área protegida-. Las regiones de estudio están localizadas a lo largo de un gradiente altitudinal, en la parte norte de la cordillera central de los Andes, Colombia. Para los análisis, se generaron dos categorías de acuerdo al tamaño de los árboles: dosel (diámetro a la altura del pecho mayor o igual a 10cm y sotobosque (diámetro a la altura del pecho mayor o igual a un cm y menor a 10cm. Las curvas especies-área mostraron diferencias en riqueza para las dos categorías de tamaño en las tres regiones. Las curvas especies-individuos, en cambio, fueron independientes con respecto al tamaño de los individuos, excepto en la región de Belmira. La diversidad, medida con el índice alfa de Fisher, mostró una fuerte tendencia a la estabilización en muestras mayores a 1 000 individuos. Ni las curvas de especies-área ni las de especies-individuos fueron asintóticas; sin embargo, la tasa de acumulación de especies (z en Belmira alcanzó valores muy bajos (0.05 en comparación con Anorí y Angelópolis (0.25 en cada caso. El índice alfa de Fisher permitió además entender la magnitud de las diferencias relativas en diversidad entre regiones o tipos de bosque en gradientes altitudinales, aun cuando el tamaño de la muestra fue relativamente pequeño. Los resultados de este estudio soportan la limitación en dispersión como el principal mecanismo en estructurar las comunidades de especies a escalas muy finas, y un incremento continuo de procesos denso-dependientes en determinar la estructura de la comunidad en escalas espaciales más grandes. Igualmente, los resultados de este estudio proponen que la denso-dependencia tiende a aumentar positivamente con la altitud.Alpha diversity patterns in three fragmented forests of Northern Andes

The analytic nodal diffusion solver ANDES in multigroups for 3D rectangular geometry: Development and performance analysis

International Nuclear Information System (INIS)

Lozano, Juan-Andres; Garcia-Herranz, Nuria; Ahnert, Carol; Aragones, Jose-Maria

2008-01-01

In this work we address the development and implementation of the analytic coarse-mesh finite-difference (ACMFD) method in a nodal neutron diffusion solver called ANDES. The first version of the solver is implemented in any number of neutron energy groups, and in 3D Cartesian geometries; thus it mainly addresses PWR and BWR core simulations. The details about the generalization to multigroups and 3D, as well as the implementation of the method are given. The transverse integration procedure is the scheme chosen to extend the ACMFD formulation to multidimensional problems. The role of the transverse leakage treatment in the accuracy of the nodal solutions is analyzed in detail: the involved assumptions, the limitations of the method in terms of nodal width, the alternative approaches to implement the transverse leakage terms in nodal methods - implicit or explicit -, and the error assessment due to transverse integration. A new approach for solving the control rod 'cusping' problem, based on the direct application of the ACMFD method, is also developed and implemented in ANDES. The solver architecture turns ANDES into an user-friendly, modular and easily linkable tool, as required to be integrated into common software platforms for multi-scale and multi-physics simulations. ANDES can be used either as a stand-alone nodal code or as a solver to accelerate the convergence of whole core pin-by-pin code systems. The verification and performance of the solver are demonstrated using both proof-of-principle test cases and well-referenced international benchmarks

High-resolution paleoclimate records of Holocene hydroclimatic variability in the Eastern Colombian Andes from Lago de Tota

Science.gov (United States)

Ahmed, M. N.; Bird, B. W.; Escobar, J.; Polissar, P. J.

2017-12-01

The Northern Hemisphere (NH) South American Monsoon (SAM) is a significant source of precipitation for the North Andes (north of 0˚) and has major control over regional hydroclimate variability. Holocene-length histories of NH SAM variability are few compared to the Southern Hemisphere (SH), limiting understanding of how these systems are connected on orbital and shorter timescales. Here, we present multi-proxy lake-sediment-based paleoclimate and paleohydrologic reconstructions from Lago de Tota, Colombia, using sedimentological, geochemical and leaf-wax hydrogen isotopic indicators from radiometically dated cores. The results indicate periods of wet and dry climate phases during the past 9000 BP with an average Holocene sedimentation rate 33cm/kyr. An increase in total organic matter (TOM) content and finer grain-size distributions was observed from 8000 to 3200 BP, suggesting a period of high lake level. This was followed by lower TOM and coarser grain sizes, suggesting lower lake levels from 3200 BP to the present. Although Tota's lake level pattern is antiphased with other lake level reconstructions from the NH and SH Andes, it is consistent with hypothesized changes in atmospheric convection over the Andes during the Holocene and the way in which they would be modified by the so-called dry island effect in the Colombian Andes. This suggests that a common forcing mechanism can be invoked to explain differing millennial-scale Andean hydroclimate changes, namely atmospheric convection. Orbital and Pacific atmosphere-forcing are therefore likely to have played a significant role in driving pan-Andean hydroclimate variability based on their inter-hemispheric influence on Andean convection.

Caracterización citogenética del tinajo o borugo Agouti taczanowskii de Colombia

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Torres Olga María

2000-12-01

Full Text Available We describe the cytogenetics of the mountain paca, A. teczenowskii, which inhabits the mountains of Colombia. It was established that A. taczanowskií has a diploid number of 78 chromosomes with fairly large amounts of constitutive heterochromatin and remarkable C-band polymorphism. These results permit the differentiation of individuals and may shed light on the family status of the genus Agouti.Este trabajo presenta los cariotipos G, R Y C del tinajo o borugo A. taczanowskii que habita en los Andes de Colombia. A. taczanowskií posee 78 cromosomas, con una cantidad relativamente grande de heterocromatina constitutiva y un notable polimorfismo de bandas C, que permitió la identificación individual de los animales estudiados. Los resultados encontrados constituyen un punto de referencia importante para la taxonomía del género Agouti.

Ice-core evidence of earliest extensive copper metallurgy in the Andes 2700 years ago

Science.gov (United States)

Eichler, A.; Gramlich, G.; Kellerhals, T.; Tobler, L.; Rehren, Th.; Schwikowski, M.

2017-01-01

The importance of metallurgy for social and economic development is indisputable. Although copper (Cu) was essential for the wealth of pre- and post-colonial societies in the Andes, the onset of extensive Cu metallurgy in South America is still debated. Comprehensive archaeological findings point to first sophisticated Cu metallurgy during the Moche culture ~200-800 AD, whereas peat-bog records from southern South America suggest earliest pollution potentially from Cu smelting as far back as ~2000 BC. Here we present a 6500-years Cu emission history for the Andean Altiplano, based on ice-core records from Illimani glacier in Bolivia, providing the first complete history of large-scale Cu smelting activities in South America. We find earliest anthropogenic Cu pollution during the Early Horizon period ~700-50 BC, and attribute the onset of intensified Cu smelting in South America to the activities of the central Andean Chiripa and Chavin cultures ~2700 years ago. This study provides for the first time substantial evidence for extensive Cu metallurgy already during these early cultures.

Ice-core evidence of earliest extensive copper metallurgy in the Andes 2700 years ago.

Science.gov (United States)

Eichler, A; Gramlich, G; Kellerhals, T; Tobler, L; Rehren, Th; Schwikowski, M

2017-01-31

The importance of metallurgy for social and economic development is indisputable. Although copper (Cu) was essential for the wealth of pre- and post-colonial societies in the Andes, the onset of extensive Cu metallurgy in South America is still debated. Comprehensive archaeological findings point to first sophisticated Cu metallurgy during the Moche culture ~200-800 AD, whereas peat-bog records from southern South America suggest earliest pollution potentially from Cu smelting as far back as ~2000 BC. Here we present a 6500-years Cu emission history for the Andean Altiplano, based on ice-core records from Illimani glacier in Bolivia, providing the first complete history of large-scale Cu smelting activities in South America. We find earliest anthropogenic Cu pollution during the Early Horizon period ~700-50 BC, and attribute the onset of intensified Cu smelting in South America to the activities of the central Andean Chiripa and Chavin cultures ~2700 years ago. This study provides for the first time substantial evidence for extensive Cu metallurgy already during these early cultures.

VOCES EN EL BOSQUE: EL USO DE RECURSOS VEGETALES ENTRE CAZADORES-RECOLECTORES DE LA ZONA CENTRAL DE TIERRA DEL FUEGO

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Laura Caruso

2008-01-01

Full Text Available Se estudiaron las modalidades de aprovechamiento de las plantas entre los Selknam de Tierra del Fuego (Argentina y se presentan aquí los resultados obtenidos a partir del análisis de los restos de madera carbonizada y sin carbonizar del sitito Ewan, ocupado a principios del siglo XX para la realización de un ritual de iniciación. Los resultados permitieron una mejor comprensión de las estrategias de aprovechamiento de las plantas entre las sociedades cazadoras-recolectoras. La identificación de las especies empleadas y el registro de las principales características morfométricas permitió documentar el aprovechamiento del "ñire" (Nothofagus antarctica. Esta especie, dominante en el entorno, fue utilizada para la construcción de la vivienda y como combustible. En ambos casos se seleccionaron troncos de forma y tamaño adecuados. Los resultados del trabajo arqueobotánico y su confrontación con los datos etnográficos evidenciaron la importancia de los recursos vegetales dentro de la dinámica socioeconómica de este grupo humano. Los recursos vegetales, más allá de su rol alimentario, fueron relevantes en otros aspectos tales como la tecnología, la construcción, el combustible y debieron constituir una ventaja considerable en el ámbito de los bosques de la zona central de Tierra del Fuego.

Rentabilidad de la gestión del mantenimiento en los centrales azucareros cubanos. // Profitability of maintenance management in Cuban sugar cane factories.

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C. Batista Rodríguez

2001-10-01

Full Text Available Para evaluar de forma acertada la eficiencia de la gestión de mantenimiento en un central azucarero y a su personaldirectivo es necesario disponer de indicadores cuantitativos que reflejen los resultados y la evolución integral del trabajotécnico-organizativo y económico de la actividad. Actualmente existen gran cantidad de indicadores, pero se adolece de lano existencia de un indicador generalizador de la eficiencia de la gestión del mantenimiento, por lo cual es difícil valorarcorrectamente los resultados y la evolución integral de la actividad.En este trabajo se muestra la posibilidad de evaluar de forma integral la eficiencia de la gestión del mantenimiento en loscentrales azucareros cubanos, con el calculo del indicador Rentabilidad de la gestión del mantenimiento (Rgm.Palabras claves: Rentabilidad, gestión de mantenimiento, centrales azucareros, indicador de rentabilid__________________________________________________________________AbstractIn order to evaluate in a proper manner the efficiency of maintenance management in sugar cane factories and its directivepersonnel, it is necessary to have quantitative indicators that reflect the results and integral evolution of the technicalorganizationaland economic work of the activity. At the present a great amount of indicators exists, but it is sympathizedfrom the non-existence of a generalizing indicator of the maintenance management efficiency, thus it is difficult tocorrectly validate the results and integral evolution of the activity. In this paper is expose the possibility of integralevaluation of the maintenance management efficiency in Cuban sugar cane factories, with the computation of the indicatorof maintenance management profitability (Rgm.Key words: Profitability, maintenance management, sugar cane factories, profitability indicator.

Description of Lutzomyia velezi, a new species of phlebotomine sand fly (Diptera: Psychodidae) from the Department of Antioquia, Colombia

OpenAIRE

Bejarano, Eduar Elías; Vivero, Rafael José; Uribe, Sandra

2010-01-01

The phlebotomine sand fly Lutzomyia velezi sp.nov. was described and illustrated from male specimens collected by light trap in the Reserva Natural Cañon del Río Claro in the Central Cordillera of the Colombian Andes. The new species belongs to the series sanguinaria of the subgenus Helcocyrtomyia, which is represented in Colombia by Lutzomyia cirrita, Lutzomyia hartmanni, Lutzomyia sanguinaria, Lutzomyia scorzai, Lutzomyia sp. of Pichindé and Lutzomyia tortura. The new species can be differe...

Three new species of Pristimantis (Lissamphibia, Anura from montane forests of the Cordillera Yanachaga in Central Peru

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William E. Duellman

2007-12-01

Full Text Available We describe three additional new species of Pristimantis from the Cordillera Yanachaga, a part of the Andes in central Peru. Analyses of DNA sequences of the mitochondrial rRNA genes show that onespecies is a close relative of P. bipunctatus (P. conspicillatus Group, another is a close relative of P. stictogaster (P. peruvianus Group, and the third is related to several species in the P. unistrigatus Group. The first two species are morphologically similar to their closest relatives but occur at lower elevations. Twenty-nine species of Pristimantis and Phrynopus are known from the vicinity of the Cordillera Yanachaga. The number of species, especially of Pristimantis, is high in the humid montane forestin comparison with other sites in humid montane forests in Peru, but the number is lower than on the western slopes of the Andes in Ecuador.

DINÁMICA NUTRICIONAL EN CINCO PARRONES DE DIFERENTE PRODUCTIVIDAD DEL VALLE CENTRAL REGADO DE CHILE

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Ruiz S., Rafael

2000-01-01

Se efectuó un estudio comparativo de aspectos nutricionales del suelo y de la planta en 5 parronales de uva de mesa cv. Thompson Seedless con un historial muy diferente de productividad y vigor, en el valle central de Chile, durante 4 años. Durante este período se efectuaron análisis nutricionales mensuales, que incluyeron además de N, P y K total, fracciones de N de reserva como arginina y aminoácidos totales y carbohidratos de reserva en la parte aérea (sarmientos y brotes) y en raíces. El ...

INSATISFACCIÓN POR LA IMAGEN CORPORAL Y LA BAJA AUTOESTIMA POR LA APARIENCIA FÍSICA EN ESTUDIANTES DE LA FACULTAD DE MEDICINA DE LA UNIVERSIDAD DE LOS ANDES DEL ESTADO MERIDA VENEZUELA

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Pedro López Atencio

2008-07-01

Full Text Available La presente investigación tuvo como propósito central evaluar la insatisfacción por la imagen corporal y su relación con la baja autoestima por la apariencia física en estudiantes de la Facultad de Medicina de la Universidad de Los Andes en Mérida Venezuela. El estudio fue de tipo no experimental correlacional. La muestra estuvo constituida por 189 estudiantes, 27% masculino y 73% femenino, con una edad promedio de 19,58 años ± 1,57 (varones 19,81 años ± 1,74 y para las mujeres 20,24 años ± 1,76. Los participantes fueron seleccionados de los cursos del primer año de las carreras de: medicina, enfermería y nutrición, los cuales fueron seleccionados de forma intencional. El instrumento empleado para determinar la Insatisfacción por la Imagen Corporal fue el Body Shape Questionnaire (Cooper y Taylor, 1987. El método de Graffar Modificado fue utilizado para determinar el estrato socioeconómico de los participantes (Méndez y De Méndez, 1994. A los datos se les aplicó el análisis descriptivo (frecuencia, porcentajes, media e inferencial (ANOVA de un solo factor a través del paquete estadístico SPSS versión 9.0. Entre los principales hallazgos en el estudio se pudo determinar una asociación estadísticamente significativa entre la insatisfacción con la imagen corporal, la baja autoestima por la apariencia física con el género χ2 (2, N= 189 = 9,686, p=0,008. A través de ANOVA se pudo determinar que las diferencias en las medias para los niveles de insatisfacción y baja autoestima con la imagen corporal y el género son estadísticamente significativas, F=11,236; p=0,008, F=10,23; p=0,002 respectivamente. Conclusiones: los resultados obtenidos permiten sugerir sobre la relación que existe entre la insatisfacción y la baja autoestima por la apariencia física, existiendo un rechazo por la propia imagen corporal causada por la percepción distorsionada o no de la misma, lo que podría afectar la autoestima por la

Las flores del desierto. Opciones de vida en pueblos de la región central de Sonora

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Ma. Amalia Gracia

2014-01-01

Full Text Available Aunque la búsqueda de las localidades rurales por generar opciones de vida se observa en el esfuerzo de algunos pobladores, en México la política pública se restringe a ofrecer garantías sociales; le deja al mercado la creación de alternativas económicas, que no alcanzan para producir desarrollo local y regional. El presente artículo reflexiona sobre esto, a partir de una iniciativa de trabajo asociativo surgida hace más de seis años en pueblos de la región central del norte de Sonora, y muestra cómo se resuelven temporal y dinámicamente las tensiones entre prácticas de cooperación y reciprocidad y las de intercambio con el mercado utilizando postulados teóricos de distintas disciplinas, retomadas por las propuestas de economía solidaria. El caso ilustra las dificultades, riqueza y potencialidad de iniciativas como ésta, y la importancia del apoyo gubernamental en localidades a las que la baja capacidad económica y la generalización del narcotráfico las vuelve frágiles para contrarrestar procesos profundos de despoblamiento.

Evidence for an Early-Middle Miocene age of the Navidad Formation (central Chile: Paleontological, paleoclimatic and tectonic implications Evidencias de una edad miocena temprana-media de la Formación Navidad: Implicancias paleontológicas, paleoclimáticas y tectónicas

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Néstor M Gutiérrez

2013-01-01

Full Text Available The age of the Navidad Formation in central Chile has always been controversial, mainly due to the conflicting age ranges indicated by its macro- and microfossils. Macrofossils are generally interpreted as having been reworked from older, Early to Middle Miocene strata, whereas a Late Miocene-Pliocene age has been accepted on the basis of planktonic foraminifer index species. The results of this study, however, indicate that the macrofossils occur in situ, which necessitates a complete revision of the geochronological data. It is concluded that the evidence for an Early to Middle Miocene age is overwhelming, and that the planktonic foraminifer index species must have appeared in the SE Pacific earlier than elsewhere. These include Globoturborotalia apertura, Globorotalia puncticulata (Deshayes, Globorotalia spheriomizea (Walters, Neogloboquadrina pachyderma (Ehrenberg, and Neogloboquadrina acostaensis (Blow. An Early to Middle Miocene age for the Navidad Formation correlates well with a reinterpretation of its depo-sitional environment as a continental shelf instead of a deepwater continental slope, global and regional paleoclimatic events, and the tectonic development of the Andes Range.La edad de la Formación Navidad en Chile central siempre ha sido controversial, debido a los distintos rangos de edad indicados por los macro- y microfósiles. En general, se considera que los macro-fósiles han sido retrabajados de estratos del Mioceno Temprano a Medio, y se aceptó una edad miocena tardía para esta unidad sobre la base de especies indicadoras de foraminíferos planctónicos. Sin embargo, los resultados de este estudio indican que los macrofósiles ocurren in situ, lo cual hace necesario una revisión completa de los datos geocronológicos. Se concluye que la evidencia por una edad miocena temprana a media es contundente, y que los foraminíferos planctónicos que indicarían una edad miocena tardía aparecieron más temprano en el SE del oc

Innovación y competitividad del sistema lechero en Valles Centrales de Querétaro. Hacia un modelo de gobernanza territorial

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Javier Delgadillo Macías

2017-01-01

Full Text Available Los objetivos del trabajo consisten en analizar las formas de organización productiva del sistema de lácteos de la región Valles Centrales en Querétaro y reconocer las distintas modalidades de gobernanza que se han construido a partir de la interacción de agentes productivos y de sus incidencias organizativas territoriales. La metodología parte del enfoque milieux innovateurs que permite documentar los efectos del proceso de cambio tecnológico del sistema lácteo respecto del sistema lechero y analizar la competitividad territorial mediante la evaluación de los impactos en el nivel de eficiencia con el cual las empresas combinan sus recursos humanos, tecnológicos y de capital en el ámbito regional. El cuestionamiento general que rige la investigación es: ¿Qué concesiones (ventajas, privilegios, beneficios han construido los actores de este territorio para desplegar procesos de cambio tecnológico efectivos en la competitividad del sistema lácteo regional? Como resultado se encontró que la principal consecuencia de las interacciones locales en torno a la lechería en Querétaro responde a las estrategias del nivel global más que a una visión de desarrollo regional, no obstante poseer este territorio vocación cultural, natural y manifestarse como un medio innovador. La limitación principal se debió a la insuficiente información sobre la organización interna de las grandes empresas del conglomerado estudiado. Las conclusiones señalan cómo el aprovechamiento disímil de los recursos naturales y del potencial humano han redefinido los patrones de especialización lechera y han coadyuvado a concentrar la renta del suelo en un grupo selecto de actores del territorio en estudio.

Volcanic impediments in the progressive development of pre-Columbian civilizations in the Ecuadorian Andes

Science.gov (United States)

Hall, Minard L.; Mothes, Patricia A.

2008-10-01

Archaeological investigations in Ecuador have proposed that there appear to be hiatus or anomalous jumps in the progressive development of pre-Columbian indigenous cultures, based upon the fact that their ceramics and tools demonstrate abrupt advances in their sophistication at several horizons in the soil profile. Because some of these horizons are clearly associated with volcanic ash layers, archaeologists have sought a causal relation with volcanism, that is, the eruptive events or their products severely interfered with the early inhabitants, resulting in their abandonment of certain areas. Geological studies of the young volcanoes in the Ecuadorian Andes carried out during the past two decades now allow us to make a more thorough evaluation of the role of volcanism during the Holocene. This contribution briefly describes the principal Holocene volcanic events and the distribution of the corresponding eruptive products found along the InterAndean Valley, from southern Colombia to central Ecuador. Only those events that were sufficiently large that they could have had a detrimental effect on the valley's early residents are discussed. Dacitic and rhyolitic ash flows, as well as numerous debris flows (lahars) have occurred frequently and their deposits cover many valleys and floodplains, where early inhabitants probably settled. The enormous Chillos Valley lahar, associated with the 4500 yBP eruption of Cotopaxi volcano, buried soils containing ceramics of the early Formative Period. However, the greatest impact upon mankind was probably not these short-lived violent events, but rather the burying of settlements and agricultural fields by ash fallout, the effect of which may have lasted hundreds of years. Ash fall layers are observed in pre-Columbian cultural horizons in the soil profile, occurring in the InterAndean Valley, the lower flanks of the Andes, and along Ecuador's Pacific coast, the oldest corresponding to the 5800 yBP eruption of Cotopaxi. This brief

EFECTO DEL USO DE ADITIVOS EN DIETAS DE CODORNICES REPRODUCTORES (Coturnix coturnix japonica) BAJO CONDICIONES DE VERANO EN LA COSTA CENTRAL

OpenAIRE

Ciriaco Castañeda, Pedro; Facultad Zootecnia, Dpto. de Produccion Animal de la Universidad Nacional Agraria La Molina (Perú).; Roncal Ñañez, Henry David; Ing. Zootecnista (Perú).

2016-01-01

Se evaluaron los efectos de la adición en la dieta de 0.05% del Complejo B, 0.05% de Vitamina C, 0.2% de Bicarbonato de Sodio y 0.05% de Ácido Acetil Salicílico, sobre los parámetros productivos y reproductivos de codornices japonesas en época de verano en la costa central del Perú (Lima), con temperatura ambiental promedio de 25°C. Codornices reproductores (270 hembras y 90 machos) de 48 días de edad, fueron distribuidas en cinco tratamientos (4 con aditivos y una dieta control) con tres rep...

Temporal Analysis of Andes Virus and Sin Nombre Virus Infections of Syrian Hamsters

Science.gov (United States)

2007-05-01

Microbiology . All Rights Reserved. Temporal Analysis of Andes Virus and Sin Nombre Virus Infections of Syrian Hamsters Victoria Wahl-Jensen,1 Jennifer...Ye, C., J. Prescott , R. Nofchissey, D. Goade, and B. Hjelle. 2004. Neutralizing antibodies and Sin Nombre virus RNA after recovery from hantavirus

78 FR 64691 - Endangered and Threatened Wildlife and Plants; Listing Five Foreign Bird Species in Colombia and...

Science.gov (United States)

2013-10-29

... to establish new natural reserves for the blue-billed curassow in Cuchilla del Rio Minero and to... national plan to connect the East Andes, the West Andes, and the Pacific ports, including roadbuilding...

Interpretación fitosociológica de la vegetación de las lomas del desierto peruano

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Antonio Galán de Mera

2011-06-01

Full Text Available La vegetación de las lomas, causada sobre todo por las precipitaciones debidas a la influencia de la corriente fría de Humboldt, constituye la mayor originalidad del desierto peruano y chileno, con un alto número de endemismos que forman asociaciones geovicarias. En este trabajo, presentamos un estudio fitosociológico sobre la vegetación de los medios arenosos de las lomas del desierto costero peruano. De acuerdo con el método de Braun-Blanquet, hemos levantado 32 inventarios fitosociológicos a los que hemos añadido 138 procedentes de la bibliografía. En cada inventario, hemos analizado la composición florística y distintos parámetros ecológicos, como la altitud, el suelo y la geomorfología. Todos los inventarios fueron sintetizados en una tabla para deducir las asociaciones, las unidades fitosociológicas superiores y el origen de su flora. Como resultado, describimos dos nuevas asociaciones del sur del Perú -Nolanetum scaposo-spathulatae y Palauetum camanensis- weberbaueri, dos alianzas -Nolanion humifusae, del centro del Perú, y Nolanion spathulatae del sur del Perú-, y un nuevo orden -Tetragonio crystallinae-Plantaginetalia limensis-. También se presenta la vegetación de las quebradas en el contexto de las comunidades de riberas de la costa y su alteración por las dunas. Después de la aplicación del índice de Shannon-Wiener sobre las columnas de la tabla sintética, podemos deducir que el aumento de especies ruderales andinas y europeas en la costa central del Perú se ha visto favorecido por una actividad ganadera intensiva. La trashumancia entre los Andes y la costa, desde tiempos preincaicos hasta la actualidad, ha producido la dispersión zoócora de plantas altoandinas hacia la costa; la presencia de plantas europeas tuvo su origen en la colonización española de la costa del Perú.A phytosociological interpretation of vegetation from sandy hills of the Peruvian desert. The vegetation of the sandy hills (�

Staff Organization in Nuclear Power Stations; Organisation du personnel des centrales nucleaires; Organizatsiya personala na atomnykh ehlektrostantsiyakh; Organizacion del personal de las centrales nucleares

Energy Technology Data Exchange (ETDEWEB)

Scuricini, G. B. [Comitato Nazionale Energia Nucleare, Roma (Italy)

1963-10-15

This paper deals with the organization of operating and maintenance staff at nuclear power stations in Italy and manpower variations, either because the plants themselves differ or are organized in some special way. Staff doing jobs for which a specific training is required are given special consideration in the paper. (author) [French] Dans le memoire, on examine l'organisation du personnel d'exploitation et d'entretien des centrales nucleaires italiennes et les differences existant dans les effectifs, differences dues soit aux caracteristiques des centrales memes, soit aux particularites d'organisation des entreprises. Le personnel charge de fonctions determinees pour lesquelles un entrainement special est requis, fait l'objet d'une attention particuliere. (author) [Spanish] En la memoria se examina la organizacion del personal de explotacion y conservacion de las centrales nucleares italianas y las diferencias que existen entre sus efectivos, diferencias que se deben a las caracteristicas de las mismas centrales o a las particularidades de organizacion de las empresas. El autor dedica especial atencion al personal encargado de funciones que requieren una formacion profesional especial. (author) [Russian] Issleduyutsya voprosy organizatsii personala, zanimayushchegosya ehkspluatatsiej ital'yanskikh atomnykh ehlektrostantsij i ukhodom za nimi, a takkhe razlichiya v sostave personala, vytekayushchie libo iz kharakternykh osobennostej samikh stantsij, libo iz osobennostej organizatsii predpriyatij. Osoboe vnimanie udelyaetsya personalu, kotoromu porucheny opredelennye funktsii, trebuyushchie spetsial'noj pod go tovki. (author)

Evaluación del desarrollo del proceso de universalización en estomatología

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Daymi Vara Machín

2013-12-01

Full Text Available Introducción: la universalización es "la extensión de la universidad y de todos sus procesos a la sociedad a través de su presencia en los territorios, alcanzando mayores niveles de equidad y de justicia social. Objetivo: evaluar la satisfacción del proceso de universalización en la carrera de Estomatología en Pinar del Río. Material y método: se realizó una investigación descriptiva y trasversal, periodo enero-mayo de 2010. El universo estuvo constituido por la totalidad de los estudiantes de la carrera de Estomatología que comenzaron sus estudios en el curso 2007-2008, en Pinar del Río, tanto de la sede central como de las sedes municipales, y los profesores encargados del proceso docente educativo; la muestra incluyó la totalidad de los estudiantes y profesores de las sedes municipales; sede central 29 alumnos escogidos al azar del universo de estudiantes y 6 profesores; analizándose la accesibilidad a la información y la informatización, estabilidad y preparación del claustro profesoral, actualización y existencia de materiales impresos y digitales, categoría docente del claustro, satisfacción de estudiantes y profesores. Principales medidas frecuencias absolutas y relativas porcentuales, test estadístico ji cuadrado. Resultados: existía una estabilidad y preparación en el claustro profesoral en los diferentes escenarios, la minoría de estudiantes plantea la no existencia de una base material de estudio adecuada, la mayoría de los profesores de las sedes municipales son no categorizados o instructores mientras en la sede central la mitad son auxiliares. Conclusiones: es satisfactorio el desarrollo del proceso de universalización en la carrera de Estomatología en la provincia Pinar del Río.

Canyon incision chronology based on ignimbrite stratigraphy and cut-and-fill sediment sequences in SW Peru documents intermittent uplift of the western Central Andes

Science.gov (United States)

Thouret, Jean-Claude; Gunnell, Yanni; Jicha, Brian R.; Paquette, Jean-Louis; Braucher, Régis

2017-12-01

Based on an 40Ar/39Ar- and U/Pb-based chronostratigraphy of ignimbrite sheets and the geomorphological features of watersheds, river profiles and slope deposits in the Ocoña-Cotahuasi-Marán (OCM) and Colca valleys of southwest Peru, we reconstruct the valley incision history of the western Central Andes over the last c. 25 Myr. We further document the Pleistocene and Holocene evolution of deep valleys on the basis of 14 10Be surface-exposure ages obtained on debris-avalanche deposits and river straths. The data suggest that uplift was gradual over the past 25 Myr, but accelerated after c. 9 Ma. Valley incision started around 11-9 Ma and accelerated between 5 and 4 Ma. Incision was followed by several pulses of valley cut-and-fill after 2.3 Ma. Evidence presented suggest that the post-5 Ma sequence of accelerated canyon incision probably resulted from a combination of drainage piracy from the Cordilleran drainage divide towards the Altiplano, accentuated flexural tilting of the Western Cordillera towards the SE, and increased rainfall on the Altiplano after late Miocene uplift of the Eastern Cordillera. The valley deepening and slope steepening driven by tectonic uplift gave rise to large occurrences of rockslope failure. The collapsed rock masses periodically obstructed the canyons, thus causing abrupt changes in local base levels and interfering with the steadiness of fluvial incision. As a result, channel aggradation has prevailed in the lower-gradient, U-shaped Pacific-rim canyons, whereas re-incision through landslide deposits has occurred more rapidly across the steeper V-shaped, upper valleys. Existing canyon knickpoints are currently arrested at the boundary between the plutonic bedrock and widespread outcrops of middle Miocene ignimbritic caprock, where groundwater sapping favouring rock collapse may be the dominant process driving headward erosion.

Memoria de los Andes, memoria de la naturaleza

OpenAIRE

Usselmann, Pierre

2013-01-01

Hace más de 35 años, terminando su tesis (1965), OlivierDollfus destacó la importancia de los Andes, “inmenso ysuntuoso campo”, para futuras investigaciones. En ese entonces sus estudios trataban de la geomorfología; escribía que “una de sus razones de ser es justamente este vaivén constante entre la observación de los procesos actuales y el intento de explicación, es decir el análisis de las formas heredadas” (1964). Esta preocupación, esta noción de memoria de la naturaleza, complementaria ...

EL SUEÑO MINERO: UN ANÁLISIS DE LA NARRATIVA UTÓPICA DEL DESARROLLO

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Facundo Boccardi

2008-01-01

Full Text Available El presente trabajo forma parte de un proyecto de investigación en curso denominado “Cultura mediática, pasiones, política(s. El lazo social en la construcción de la actualidad (Argentina post-estallido 2001”. En este caso, el análisis intenta dar cuenta del funcionamiento de los dispositivos de construcción de consenso en torno a la implementación de proyectos de explotación minera transnacional situados en la Cordillera de los Andes. Por esta razón, indagamos los discursos provenientes de dos sedes autorizantes: el Estado y las empresas mineras, ya que consideramos que sus enunciadores son poseedores de una palabra con poder performativo por estar habilitados para hablar. Desde ese lugar, tanto el discurso empresarial como el estatal urden la narrativa utópica del desarrollo entendida como la articulación de ficciones, invenciones y construcciones que funcionan como estructuras constantes dentro del discurso hegemónico sobre la minería a cielo abierto.

Air temperature change in the northern and southern tropical Andes linked to North-Atlantic stadials and Greenland interstadials

Science.gov (United States)

Urrego, Dunia H.; Hooghiemstra, Henry

2016-04-01

We use eight pollen records reflecting climatic and environmental change from northern and southern sites in the tropical Andes. Our analysis focuses on the signature of millennial-scale climate variability during the last 30,000 years, in particular the Younger Dryas (YD), Heinrich stadials (HS) and Greenland interstadials (GI). We identify rapid responses of the vegetation to millennial-scale climate variability in the tropical Andes. The signature of HS and the YD are generally recorded as downslope migrations of the upper forest line (UFL), and are likely linked to air temperature cooling. The GI1 signal is overall comparable between northern and southern records and indicates upslope UFL migrations and warming in the tropical Andes. Our marker for lake level changes indicates a north to south difference that could be related to moisture availability. The direction of air temperature change recorded by the Andean vegetation is consistent with millennial-scale cryosphere and sea surface temperature records from the American tropics, but suggests a potential difference between the magnitude of temperature change in the ocean and the atmosphere.

Aridity changes in the temperate-Mediterranean transition of the Andes since ad 1346 reconstructed from tree-rings

Energy Technology Data Exchange (ETDEWEB)

Christie, Duncan A.; Quesne, Carlos le [Universidad Austral de Chile, Laboratorio de Dendrocronologia, Facultad de Ciencias Forestales y Recursos Naturales, Valdivia (Chile); Boninsegna, Jose A.; Morales, Mariano S.; Villalba, Ricardo [Instituto Argentino de Nivologia, Glaciologia y Ciencias Ambientales, IANIGLA, Departamento de Dendrocronologia e Historia Ambiental, Mendoza (Argentina); Cleaveland, Malcolm K.; Stahle, David W. [University of Arkansas Fayetteville, Tree-Ring Laboratory, Department of Geosciences, Fayetteville, AR (United States); Lara, Antonio [Universidad Austral de Chile, Laboratorio de Dendrocronologia, Facultad de Ciencias Forestales y Recursos Naturales, Valdivia (Chile); Universidad Austral de Chile, Forest Ecosystem Services under Climatic Fluctuations (Forecos), Valdivia (Chile); Mudelsee, Manfred [Climate Risk Analysis, Hanover (Germany); Alfred Wegener Institute for Polar and Marine Research, Bremerhaven (Germany)

2011-04-15

The Andes Cordillera acts as regional ''Water Towers'' for several countries and encompasses a wide range of ecosystems and climates. Several hydroclimatic changes have been described for portions of the Andes during recent years, including glacier retreat, negative precipitation trends, an elevation rise in the 0 isotherm, and changes in regional streamflow regimes. The Temperate-Mediterranean transition (TMT) zone of the Andes (35.5 -39.5 S) is particularly at risk to climate change because it is a biodiversity hotspot with heavy human population pressure on water resources. In this paper we utilize a new tree-ring network of Austrocedrus chilensis to reconstruct past variations in regional moisture in the TMT of the Andes by means of the Palmer Drought Severity Index (PDSI). The reconstruction covers the past 657 years and captures interannual to decadal scales of variability in late spring-early summer PDSI. These changes are related to the north-south oscillations in moisture conditions between the Mediterranean and Temperate climates of the Andes as a consequence of the latitudinal position of the storm tracks forced by large-scale circulation modes. Kernel estimation of occurrence rates reveals an unprecedented increment of severe and extreme drought events during the last century in the context of the previous six centuries. Moisture conditions in our study region are linked to tropical and high-latitude ocean-atmospheric forcing, with PDSI positively related to Nino-3.4 SST during spring and strongly negatively correlated with the Antarctic Oscillation (AAO) during summer. Geopotential anomaly maps at 500-hPa show that extreme dry years are tightly associated with negative height anomalies in the Ross-Amundsen Seas, in concordance with the strong negative relationship between PDSI and AAO. The twentieth century increase in extreme drought events in the TMT may not be related to ENSO but to the positive AAO trend during late-spring and

High altitude C4 grasslands in the northern Andes: relicts from glacial conditions?

NARCIS (Netherlands)

Boom, A.; Mora, G.; Cleef, A.M.; Hooghiemstra, H.

2001-01-01

The altitudinal vegetation distribution in the northern Andes during glacial time differed from the present-day conditions as a result of temperature and precipitation change. New evidence indicate that as a response to a reduced atmospheric partial CO2 pressure (pCO2), the competitive balance

Mammalian carnivore occupancy is inversely related to presence of domestic dogs in the high Andes of Ecuador.

Science.gov (United States)

Zapata-Ríos, Galo; Branch, Lyn C

2018-01-01

Although the Andes have long been occupied by people, habitat loss, fragmentation through deforestation, and other human activities such as introduction of invasive species have increased drastically during the past century. The Ecuadorian Andes are considered a biodiversity hotspot. However, the fauna and threats to the region are poorly studied, and understanding of factors that shape the distribution of species in habitats disturbed by human activities is needed to identify and mitigate region-wide threats to wildlife. We evaluated factors associated with patterns of occurrence of Andean carnivores in landscapes of the northern Ecuadorian Andes, particularly habitat loss, fragmentation, and occupancy of domestic dogs, and determined whether thresholds occurred for these factors beyond which carnivore occurrence declined markedly. Five study areas (each 20 x 20 km) were surveyed with a total effort of 2,800 camera trap nights. Occupancies of four of the eight carnivores known from the region were best predicted by occupancy of domestic dogs rather than measures of habitat loss and fragmentation [Andean fox (Pseudalopex culpaeus), puma (Puma concolor), striped hog-nosed skunk (Conepatus semistriatus), and Andean bear (Tremarctos ornatus)]. The two largest carnivores, puma and Andean bear, demonstrated significant threshold responses to the presence of domestic dogs at two sites. Four smaller carnivores were recorded too infrequently to model occupancy, and at least two of these species appear to be in decline. The magnitude of domestic dog impacts on native species in tropical areas like the Ecuadorian Andes currently are not recognized. Results of our study indicate that small and large carnivores are in urgent need of conservation and clearly point to dogs as a significant threat to a broad range of native species.

Setting practical conservation priorities for birds in the Western Andes of Colombia.

Science.gov (United States)

Ocampo-Peñuela, Natalia; Pimm, Stuart L

2014-10-01

We aspired to set conservation priorities in ways that lead to direct conservation actions. Very large-scale strategic mapping leads to familiar conservation priorities exemplified by biodiversity hotspots. In contrast, tactical conservation actions unfold on much smaller geographical extents and they need to reflect the habitat loss and fragmentation that have sharply restricted where species now live. Our aspirations for direct, practical actions were demanding. First, we identified the global, strategic conservation priorities and then downscaled to practical local actions within the selected priorities. In doing this, we recognized the limitations of incomplete information. We started such a process in Colombia and used the results presented here to implement reforestation of degraded land to prevent the isolation of a large area of cloud forest. We used existing range maps of 171 bird species to identify priority conservation areas that would conserve the greatest number of species at risk in Colombia. By at risk species, we mean those that are endemic and have small ranges. The Western Andes had the highest concentrations of such species-100 in total-but the lowest densities of national parks. We then adjusted the priorities for this region by refining these species ranges by selecting only areas of suitable elevation and remaining habitat. The estimated ranges of these species shrank by 18-100% after accounting for habitat and suitable elevation. Setting conservation priorities on the basis of currently available range maps excluded priority areas in the Western Andes and, by extension, likely elsewhere and for other taxa. By incorporating detailed maps of remaining natural habitats, we made practical recommendations for conservation actions. One recommendation was to restore forest connections to a patch of cloud forest about to become isolated from the main Andes. © 2014 Society for Conservation Biology.

Evaluation of Little Ice Age cooling in Western Central Andes, suggested by paleoELAs, in contrast with global warming since late 19th century deduced from instrumental records

Science.gov (United States)

Ubeda, Jose; Palacios, David; Campos, Néstor; Giraldez, Claudia; García, Eduardo; Quiros, Tatiana

2015-04-01

This paper attempts to evaluate climate cooling (°C) during the glacial expansion phases using the product GTV•ΔELA, where GTV is the vertical air temperature gradient (°C/m) and ΔELA (m) the difference in level observed between the Equilibrium Line Altitude (ELA) reconstructions for current and past glaciers. With this aim the Area x Altitude Balance Ratio-(AABR) method was used to produce reconstructions of present ELAs (2002-2010) and paleoELAs corresponding to the last glacier advance phase. The reconstructions were produced in three study areas located along a N-S transect of the western cordillera in the Central Andes: the south-western sector of the Nevado Hualcán (9°S, 77°W; Giráldez 2011); the southern slope of the Cordillera Pariaqaqa (12°S, 76°W; Quirós, 2013) and the NW, NE, SE and SW quadrants of the Nevado Coropuna (16°S, 72°W; García 2013; Úbeda 2011; Campos, 2012). The three mountains exceed 6000 m altitude, their summit areas are covered by glaciers, and on their slopes there are existing well-conserved moraines deposited by the last advances near the present front of the ice masses. Although there are no absolute dates to confirm this hypothesis, it has been assumed that the last glacial advances occurred during the Little Ice Age (LIA), which the oxygen isotopes of the Nevado Huascarán (9°S, 77°W) date to the period 1500-1890. For the Hualcán and Pariaqaqa the mean global value of the Earth's GTV (6.5°C/km) was used, considered valid for the Tropics. On the Coropuna a GTV=8.4°C/km was used, based on high resolution sensors installed in situ since 2007 (Úbeda 2011). This gradient is approaching the upper limit of the dry adiabatic gradient (9.8°C/km), as the Coropuna region is more arid than the other case study areas. The climate cooling estimates deduced from the product GTV•ΔELA were compared with the global warming shown by the 1880-2012 series, ΔT=0.85°C, and 1850/1900-2003/2012, ΔT=0.78°C. The differences are

Evaluación de las causas de los eventos adversos o incidentes que afectan la seguridad del paciente, en el hospital central de la policía de enero 2012 a diciembre 2013

OpenAIRE

Alarcon Ruiz, Diego Jesus; Gil Vargas, Luis Fabio

2016-01-01

TITULO DEL TRABAJO: Evaluación de las causas de los eventos adversos o incidentes que afectan la seguridad del paciente, en el hospital central de la policía de enero 2012 a diciembre 2013. OBJETIVO: Determinar y analizar la causa raíz de los principales factores de riesgo que afectan la seguridad del paciente que puedan ocasionar eventos adversos en la atención de los pacientes, con el uso de la teoría de restricciones TOC en el Hospital Central de la Policía HOCEN. MATERIALES Y METODO: Se r...

DE LA SOCIEDAD DEL CONOCIMIENTO A LA SOCIEDAD DEL RIESGO

OpenAIRE

Abdala Cardona, Alejandro

2013-01-01

El tiempo en el que vivimos: el siglo XXI, presenta a la vez, retos y exigencias al conjunto global de los habitantes del mundo, puesto que, no solo se nos presenta la actualidad como aquella coyuntura histórica en los que el cambio de los acontecimientos gira en torno al rol central del conocimiento, sino también, en torno al potencial que dicho conocimiento trae tras de sí; es decir, el presente siglo impone al conjunto de personas el rótulo de "sociedad del conocimiento" donde se puede enc...

Tumores del sistema nervioso central en población pediátrica entre 0 y 14 años

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Giselly Mayerly Nieves-Cuervo

2016-11-01

Full Text Available Introducción: Los tumores pediátricos primarios del sistema nervioso central (SNC, ocupan el segundo lugar en frecuencia, superados solamente por las neoplasias hematológicas. Objetivo: Realizar una revisión y análisis de la literatura médica existente sobre tumores del SNC en población entre los 0 y 14 años centrado en la epidemiologia, factores etiológicos, manifestaciones clínicas y diagnóstico. Metodología: Se realizó una búsqueda en las bases de datos PubMed, MedlinePlus, BIREME y red interna de trabajos de grados y tesis de la Universidad Industrial de Santander. Además, se realizó revisión de las páginas de los entes gubernamentales encargados del registro epidemiológico sobre cáncer nacional e internacional. Resultados: Los tumores de SNC en la población pediátrica son la segunda causa de muerte infantil solo superado por la leucemia; tienen una clínica y factores etiológicos bien establecidos. La epidemiología no difiere en el mundo. Los síntomas más frecuentes son vómito, cefalea, ataxia, síntomas visuales y alteraciones motoras. Los factores etiológicos más representativos son virus, síndromes genéticos, infecciones maternas y perinatales, exposición a radiación electromagnética e ionizante; algunos son muy discutidos como la presencia de trauma al momento del nacimiento. Además, existen documentados factores protectores tales como consumo de antioxidantes, frutas y verduras, e historia reportada de alergias. Conclusiones: El adecuado entrenamiento a los médicos de atención primaria en la identificación de los signos y síntomas para la sospecha y diagnóstico de los estadios iniciales de estos tumores pueden disminuir los índices de mortalidad. [Nieves-Cuervos GM, Manrique-Hernández EF, Ojeda-Rincón SA, Galvis-Pabón S. Tumores del sistema nervioso central en población pediátrica entre 0 y 14 años. MedUNAB 2016; 19 (2: 124-133

Composición química y actividad antibacteriana del aceite esencial de Peperomia acuminata de los Andes venezolanos

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Flor D. Mora-Vivas

2016-12-01

Full Text Available El género Peperomia (Piperaceae, es bien conocido por sus especies ornamentales y usos etnomedicinales. En el presente trabajo se describe la caracterización química y la actividad antibacteriana del aceite esencial de Peperomia acuminata Ruiz & Pav. proveniente del Estado Mérida Venezuela. El aceite esencial se obtuvo por hidrodestilación de las hojas y la separación de los componentes se realizó por Cromatografía de gases-Espectrometría de Masas (CG/EM. Se logró la elucidación de ocho compuestos (96,7%, siendo el 2E-dodecenal el componente mayoritario (65% seguido de dodecanal (14,8% y tetradecanal (9,2%. Esta investigación muestra el potencial del aceite esencial de P. acuminata frente a bacterias Gram positivas (Staphylococcus aureus ATCC 25923 y Enterococcus faecalis 29212, con un valor de Concentración inhibitoria mínima de 1μL/mL. Este es el primer reporte sobre la composición química del aceite esencial de esta especie, por lo tanto una contribución importante al estudio del género Peperomia.

EL SECUESTRO DE LAS HISTORIAS INDÍGENAS: ITENERARIO Y LIMITACIONES DEL TIEMPO LINEAL EN CHILE

OpenAIRE

MAXIMILIANO SALINAS CAMPOS

2015-01-01

La historia de Chile está cruzada por el conflicto entre la cultura moderna europea y las culturas indígenas. El tiempo lineal impuesto por el Estado nacional ha dejado al descubierto su irresponsabilidad con el tiempo indígena de los Andes. Esta temporalidad expresa una profunda y sustentable «ontología arcaica». Tras el fin de la Guerra Fría, y la postdictadura de Pinochet, esta propuesta se vuelve acuciante con las demandas políticas y los desafíos epistémicos indígenas del siglo XXI. En...

EL SECUESTRO DE LAS HISTORIAS INDÍGENAS: ITINERARIO Y LIMITACIONES DEL TIEMPO LINEAL EN CHILE

OpenAIRE

Salinas Campos, Maximiliano

2015-01-01

La historia de Chile está cruzada por el conflicto entre la cultura moderna europea y las culturas indígenas. El tiempo lineal impuesto por el Estado nacional ha dejado al descubierto su irresponsabilidad con el tiempo indígena de los Andes. Esta temporalidad expresa una profunda y sustentable «ontología arcaica». Tras el fin de la Guerra Fría, y la postdictadura de Pinochet, esta propuesta se vuelve acuciante con las demandas políticas y los desafíos epistémicos indígenas del siglo XXI. En e...

Mineralogía del perfil de «La Muela», terciario del sector central de la Depresion del Ebro (provincia Zaragoza

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López-Aguayo, F.

1988-08-01

Full Text Available The stratigraphic sequenre of «La Muela>., at the South (Central Sector of the Ebro basin, is studied. This profile presents two difIerentiated uoits. The first one gypsum-bearing and the second one carbonatic, which correspond to the gypsum of Zaragoza and Alcubierre Cormations respectively. 80th units present a different mineralogical assofiation. The first one is characterized by gypsum, carbonates (calcite/dolomite, clay minerals and quartz, whereas in the second one the association is carbonates (calcite and/or dolomite, clay minerals and quartz. The clay minerals systematically present are: illite, smectites, chlorite and kaolinite. However, it is possible to observe an important quantitative change between both units, with a variation in the average of smectites from 23% to 46%. The variation in the molar content of MgCO3 in the carbonates has loo to propase a model of the chemical evolution on the vertical, in agreement with the sedimentologic analysis of the materials, which correspond to playa and lacustrine deposits.El perfil estratigráfico de La Muela, sector Sur de la Depresión del Ebro. Consta de dos tramos diferenciados, el primero rico en yeso y el segundo carbonatado, que corresponden respectivamente a las Formaciones Yesos de Zaragoza y Alcubierre. Ambos tramos presentan una asociación mineralógica distinta: el primero está caracterizado por yeso, carbonatos (calcita/dolomita, minerales de la arcilla y cuarzo, mientras que el segundo la asociación consta de carbonatos (calcita y/o dolomita, minerales de la arcilla y cuarzo. Los minerales de la arcilla presentes sistemáticamente son: ilita, esmectitas, clorita y caolinita. No obstante, se observa un importante cambio cuantitativo entre ambos tramos con una variación notable en el contenido en esmectitas, que en términos medios, es del 23 al 46%. La variación del contenido molar en CO3 Mg de los carbonatos ha permitido proponer un modelo de evolución química en la

Control democrático sobre el manejo de la banca central. Un reto para la política del conocimiento económico

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Carlo Tognato

2004-07-01

Full Text Available La globalización económica ha acelerado la transformación de la racionalidad económica en racionalidad política. Durante esta transformación, la naturaleza de la pregunta del control democrático sobre las agencias económicas ha cambiado de forma radical. Lo que antes era puramente una cuestión institucional, hoy se ha convertido en una cuestión epistémica. Para reestablecer un control democrático efectivo sobre las agencias económicas, la democracia debe penetrar los fundamentos de la racionalidad económica misma, pilar sobre la cual la tecnocracia económica basa su operación. En otras palabras, es necesario practicar controles democráticos de carácter epistémico. Esta visión implica un giro Foucaultiano con respecto a la literatura tradicional sobre el diseño de las instituciones económicas. Además, llama al analista a mirar a la tecnocracia económica como una faceta organizacional de una formación discursiva, y a reconocer que un cambio en la operación de la tecnocracia económica requiere un cambio de otras facetas de su propia formación discursiva. Aquí daré cuenta de algunos de los cambios que implica la democratización de una de las tecnocracias económicas más impermeables al escrutinio democrático externo - la banca central independiente. En particular, mostraré que la democratización de la banca central independiente tiene implicaciones reflexivas importantes sobre la estructura argumentativa económica que la sostiene así como sobre la organización de la disciplina económica que articula dicha argumentación. En otras palabras, la democratización del objeto de análisis llama a una democratización del proceso de generación del conocimiento por medio del cual el objeto se constituye. PALABRAS CLAVES. Globalización banca central, control democrático.

Statistical analysis of the wind around a nuclear power plant; Analisis estadistico del viento alrededor de una central nucleoelectrica

Energy Technology Data Exchange (ETDEWEB)

Tejeda, A; Alvarez, Oscar; Contreras, A D; Jauregui, E [Universidad Veracruzana, (Mexico)

1997-12-31

In order to show an appropriate methodology for the climatic analysis of the wind, some of the recent results in the investigation of the field flow around the Laguna Verde Nuclear Power Station, at Veracruz State (Mexico,) through the angular correlation coefficients and contingency tables among the registered wind directions by a meteorological tower at the levels of 10 and 60 meters high are presented. Finally, by applying an objective analysis of the data some conclusions are obtained in connection with the local winds with the mesoscale systems. [Espanol] Con el objeto de mostrar una metodologia apropiada en el analisis climatico del viento, se presentan algunos resultados recientes en la investigacion del campo de flujo en los alrededores de la central nucleoelectrica de Laguna Verde, Veracruz (Mexico), a traves de los coeficientes de correlacion angulares y de tablas de contingencia entre las direcciones del viento registradas por una torre meteorologica en los niveles de 10 y 60 metros de altura. Finalmente, aplicando analisis objetivo de los datos, se obtienen algunas conclusiones sobre la conexion de los vientos locales con los sistemas de mesoescala.

Statistical analysis of the wind around a nuclear power plant; Analisis estadistico del viento alrededor de una central nucleoelectrica

Energy Technology Data Exchange (ETDEWEB)

Tejeda, A; Alvarez, Oscar; Contreras, A. D.; Jauregui, E. [Universidad Veracruzana, (Mexico)

1996-12-31

In order to show an appropriate methodology for the climatic analysis of the wind, some of the recent results in the investigation of the field flow around the Laguna Verde Nuclear Power Station, at Veracruz State (Mexico,) through the angular correlation coefficients and contingency tables among the registered wind directions by a meteorological tower at the levels of 10 and 60 meters high are presented. Finally, by applying an objective analysis of the data some conclusions are obtained in connection with the local winds with the mesoscale systems. [Espanol] Con el objeto de mostrar una metodologia apropiada en el analisis climatico del viento, se presentan algunos resultados recientes en la investigacion del campo de flujo en los alrededores de la central nucleoelectrica de Laguna Verde, Veracruz (Mexico), a traves de los coeficientes de correlacion angulares y de tablas de contingencia entre las direcciones del viento registradas por una torre meteorologica en los niveles de 10 y 60 metros de altura. Finalmente, aplicando analisis objetivo de los datos, se obtienen algunas conclusiones sobre la conexion de los vientos locales con los sistemas de mesoescala.

Viticultura tropical a gran altitud. Condiciones y expresiones del terroir

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Marco Quijano Rico

2009-10-01

Full Text Available Nuestro proyecto se inició en 1982 en la Loma de Puntalarga, entre 2500 y2600 metros de altitud, a 5,78 ºN y 72,98 ºW, en la cordillera oriental de los Andes. Las variedades más utilizadas actualmente son Pinot noir, Riesling y cruzamientos de Riesling x Silvaner. Desde 1984 se realizan trabajos de investigación sobre temas pertinentes. La baja latitud, la elevada altitud, el volumen de precipitación relativamente modesto y la transparencia del cielo, determinan el flujo de radiación solar incidente y su composición espectral, así como la amplitud del cambio de temperatura entre el día y la noche y las bajas temperaturas nocturnas, que son los rasgos del clima frío imperante en la región. El comportamiento de las cepas y las características del vino indican que las condiciones climáticas locales, pueden considerarse térmicamente equivalentesa las de ciertos territorios tradicionales renombrados. La coexistencia durante el año de todos los estadios de vegetación de la vid y la producción de vendimias con buen contenido de azúcar y niveles suficientes de acidez, hace posible la elaboración de vinos de calidad sobresaliente, de modo secuencial y continuo.En los viñedos del proyecto, las condiciones climáticas anuales son equivalentesa las otoñales, de maduración de las uvas en regiones septentrionales y australes. Al mismo tiempo, el flujo de radiación solar no sufre cambios notables y es rico en las longitudes de onda del ultravioleta B. Los dos factores pueden marcar las características de las uvas, haciendo parte así del efecto terroir.

Observaciones adicinales sobre la biogeografía de la zona de AmotapeHuancabamba en el norte del Perú: definiendo el límite suroriental

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Maximilian Weigend

2013-06-01

Full Text Available Observaciones de Loasaceae y Ribes (Grossulariaceae obtenidos durante estudios de campo en el Perú nos permiten definir el límite suroriental de la zona Amotape Huancabamba con gran precisión. El límite se encuentra entre la zona directamente al NE de Otuzco (departamento La Libertad, prov. Otuzco, sistema Río Chicama: 07° 50,315´ S, 078° 29,076´ W hacía el abra entre Parcoy y Buldibuyo (departamento La Libertad, provincia Pataz, N del Río Cajas: 08° 04,619´ S, 077° 25,457´ O. Los grupos de plantas típicas de la zona Amotape Huancabamba (grupo N. triphylla, N. ser. Alatae, grupo Ribes andicola, Nasa picta subsp. picta tienen sus límites suroriental de distribución en el Norte de la provincia de Pataz (La Libertad, y se encuentran reemplazadas por grupos de los Andes Centrales (grupo N. poissoniana, Ribes viscosum inmediatamente al sur de esta abra.

Tectonostratigraphic reconstruction Cretaceous volcano-sedimentary in the northwestern Andes: from extensional tectonics to arc accretion.

Science.gov (United States)

Zapata, S.; Patino, A. M.; Cardona, A.; Mejia, D.; Leon, S.; Jaramillo, J. S.; Valencia, V.; Parra, M.; Hincapie, S.

2014-12-01

Active continental margins characterized by continuous convergence experienced overimposed tectonic configurations that allowed the formation of volcanic arcs, back arc basins, transtensional divergent tectonics or the accretion of exotic volcanic terranes. Such record, particularly the extensional phases, can be partially destroyed and obscure by multiple deformational events, the accretion of exotic terranes and strike slip fragmentation along the margin. The tectonic evolution of the northern Andes during the Mesozoic is the result of post Pangea extension followed by the installation of a long-lived Jurassic volcanic arc (209 - 136 ma) that apparently stops between 136 Ma and 110 Ma. The Quebradagrande Complex has been define as a single Lower Cretaceous volcano-sedimentary unit exposed in the western flank of the Central Cordillera of the Colombian Andes that growth after the Late Jurassic to Early Cretaceous magmatic hiatus. The origin of this unit have been related either to an oceanic volcanic arc or a marginal basin environment. The existence of such contrasting models reflect the regional perspective followed in published studies and the paucity of detail analysis of the volcano-sedimentary sequences.We integrate multiple approaches including structural mapping, stratigraphy, geochemistry, U-Pb provenance and geochronology to improve the understanding of this unit and track the earlier phases of accumulation that are mask on the overimposed tectonic history. Our preliminary results suggest the existence of different volcano-sedimentary units that accumulated between 100 Ma and 82 Ma.The older Lower Cretaceous sequences was deposited over Triassic metamorphic continental crust and include a upward basin deepening record characterized by thick fan delta conglomerates, followed by distal turbidites and a syn-sedimentary volcanic record at 100 ma. The other sequence include a 85 - 82 Ma fringing arc that was also formed close to the continental margin or

Nuclear Data for Safe Operation and Waste Transmutation: ANDES (Accurate Nuclear Data for nuclear Energy Sustainability); Datos nucleares para la operacion segura y la transmutacion de residuos: Andes (Datos Nucleares Precisos para la Sostenibilidad de la Energia Nuclear)

Energy Technology Data Exchange (ETDEWEB)

Gonzalez, E. M.

2014-07-01

Nuclear research within the 7th Framework Program (FP7 and FP7+2) of EURATOM has devoted a significant fraction of its efforts to the development of advanced nuclear fuel cycles and reactor concepts, mainly fast reactors, aiming to improve the long term sustainability by reduction of the final wastes, optimal use of natural resources and improvement of safety in the present and future nuclear installations. The new design need more accurate basic nuclear data for isotopes, like minor actinides, potentially playing an important role in the operation, fuel concept, safety or final wastes of those reactors and fuel cycles. Four projects, ANDES, ERINDA, EUFRAT and CHANDA, supported by EURATOM within the FP7 and FP7+2, have put together most of the European Nuclear Data community to respond efficiently and in a coordinated way to those needs. This paper summarizes the objectives, and main achievements of ANDES, the project responsible for most of the measurements and technical achievements that was coordinated by CIEMAT. Indeed, CIEMAT has coordinated the nuclear data R and D projects within EURATOM during the last 7 years (NUDATRA domain of EUROTRANS, and ANDES) and will continue this coordination in the CHANDA project till 2017. (Author)

Mammalian carnivore occupancy is inversely related to presence of domestic dogs in the high Andes of Ecuador.

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Galo Zapata-Ríos

Full Text Available Although the Andes have long been occupied by people, habitat loss, fragmentation through deforestation, and other human activities such as introduction of invasive species have increased drastically during the past century. The Ecuadorian Andes are considered a biodiversity hotspot. However, the fauna and threats to the region are poorly studied, and understanding of factors that shape the distribution of species in habitats disturbed by human activities is needed to identify and mitigate region-wide threats to wildlife. We evaluated factors associated with patterns of occurrence of Andean carnivores in landscapes of the northern Ecuadorian Andes, particularly habitat loss, fragmentation, and occupancy of domestic dogs, and determined whether thresholds occurred for these factors beyond which carnivore occurrence declined markedly. Five study areas (each 20 x 20 km were surveyed with a total effort of 2,800 camera trap nights. Occupancies of four of the eight carnivores known from the region were best predicted by occupancy of domestic dogs rather than measures of habitat loss and fragmentation [Andean fox (Pseudalopex culpaeus, puma (Puma concolor, striped hog-nosed skunk (Conepatus semistriatus, and Andean bear (Tremarctos ornatus]. The two largest carnivores, puma and Andean bear, demonstrated significant threshold responses to the presence of domestic dogs at two sites. Four smaller carnivores were recorded too infrequently to model occupancy, and at least two of these species appear to be in decline. The magnitude of domestic dog impacts on native species in tropical areas like the Ecuadorian Andes currently are not recognized. Results of our study indicate that small and large carnivores are in urgent need of conservation and clearly point to dogs as a significant threat to a broad range of native species.

Apatite fission-track dating of erosion in the eastern Andes, Bolivia

International Nuclear Information System (INIS)

Crough, S.T.

1983-01-01

Three samples from a Triassic-age batholith in the eastern Andes northeast of La Paz, Bolivia yield apatitic fission-track ages of 11-13 Ma. Interpreting these young ages as due to uplift and erosion requires approximately 2.5-5.0 km of erosion in the past 12 Ma, an amount which is consistent with the known geology and which is typical of many active mountain ranges. (orig.)

Hidrodinámica bidimensional del canal de descarga de la central hidroeléctrica de Caruachi: correlación modelo matemático 2DH-Prototipo

OpenAIRE

Toscano Díaz, M.A.; Montilla Castro, G.A.

2007-01-01

La Central Hidroeléctrica de Caruachi está localizada en la zona Sur-Oriental de Venezuela en el Estado Bolívar sobre las aguas del río Caroní. Está equipada por 12 turbinas tipo Kaplan con 2196 MW de potencia instalada y un Aliviadero con una capacidad de 30000 m3/s. En este trabajo se presenta una correlación Modelo Matemático – Prototipo, cuyo objetivo es determinar la hidrodinámica del flujo del Canal de Descarga de Caruachi mediante el modelo matemático bidimensional SMS-FESWMS-2DH. El m...

Las redes de drenaje de los rios Alberche y Guadarrama como indicadores estructurales del Sistema Central Espanol

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Martín Escorza, C.

2003-08-01

Full Text Available The network of the Alberche and Guadarrama rivers, obtained by a semicuantitative method, shows that on the granitic and metamorphic rocks of the Spanish Central System exist circular alignments, until now detected by analysis of satellite image. Such alignments are located in the sub-geological system of the Sierra de Guadarrama, and they coexist with to already known rectilinear alignments. In the sub-westem system, Sierra de Gredos, are detected rectilinear alignments. The circular structures of Sierra de Guadarrarna would have a relationship to geological processes still unknown after the Hercynian Orogeny but before of the Oligocene.Utilizando una metodología semicuantitativa, las redes de drenaje de los ríos Alberche y Guadarrama ponen de manifiesto que existen alineaciones circulares sobre las rocas graníticas y metamórficas de la Cordillera Central, cuya presencia hasta ahora se había detectado por análisis de imagen de satélite. Tales alineaciones se sitúan en el subsistema geológico de la Sierra del Guadarrama, en donde coexisten con alineaciones rectas ya conocidas. En el subsistema occidental, la Sierra de Gredos, se detectan alineaciones rectas. Las estructuras circulares de la Sierra de Guadarrama tendrían su origen en relación con procesos geodinámicos todavía desconocidos, ocurridos con posterioridad a la Orogenia Hercínica, pero antes del Oligoceno.

Definição das trajetórias P-T-t em rochas metamórficas do flanco ocidental da Cordilheira Central da Colômbia, nas regiões de Caldas e El Retiro

OpenAIRE

Andres Bustamante Londoño

2003-01-01

Apesar da existência de vários estudos geológicos detalhados no segmento norte do Andes, muitos aspectos estão ainda por serem resolvidos, principalmente aqueles concernentes ao tipo, grau e evolução metamórfica, ambiente tectônico de formação e correlação com margem paleozóica do continente Gondwana e com os terrenos mesozóicos oceânicos. A Cordilheira Central dos Andes Colombianos, é representada por um complexo polimetamórfico com magmatismo associado e uma fina pilha de sedimentos supraja...

Caracterización morfométrica de la microcuenca de la quebrada los Andes, El Carmen de Viboral, Antioquia-Colombia Morphometrical characterization in los Andes watershed, El Carmen de Viboral, Antioquia-Colombia

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Yimmy Montoya Moreno

2009-07-01

Full Text Available Se evaluaron algunas características morfométricas básicas en la microcuenca de la quebrada Los Andes en el departamento de Antioquia (Colombia. La microcuenca tiene un área pequeña (Some morphometric characteristic were evaluated in the watershed of creek Los Andes department of Antioquia (Colombia. The headwater has a small area (<20km² with main direction in the axis S-N, with an elevation range between 2.700 and 2.200 m. asl. It presents a network of drainage well structured, for which presents a time of concentration of the water over 5 hours. The watershed is of class Kc2 with a high slope and a system of drainage subdendritic. This research permitted to identify the uses of the soil, being the adequate use the one that presented greater percentage (55% and the use is recommended conservationist in general for all headwater.

Infecciones del sistema nervioso central por enterovirus en niños atendidos en un hospital de Lima, Perú Enteroviral central nervous system infections in children treated at a hospital in Lima, Peru

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Iván O Espinoza

2011-12-01

Full Text Available Objetivos. Determinar la frecuencia y las características clínicas de las infecciones del sistema nervioso central por enterovirus en niños atendidos en el Hospital Nacional Cayetano Heredia de Lima, Perú. Materiales y métodos. Se realizó un estudio prospectivo y descriptivo desde abril 2008 hasta marzo 2010. Se enrolaron pacientes de un mes a 14 años con diagnóstico clínico de encefalitis o meningitis asépticas. Se investigó la presencia de enterovirus, virus herpes simple 1 (VHS-1, virus herpes simple 2 (VHS-2 y virus varicela-zoster (VZV mediante reacción en cadena de polimerasa (PCR. Resultados. Se enrolaron 97 pacientes de los cuales 69 % presentaron encefalitis aguda y 31 % meningitis aguda. Se identificó enterovirus en 52,6 % del total de infecciones agudas no bacterianas del sistema nervioso central; encontrándose en 83,3 % de las meningitis y en 38,8 % de las encefalitis. No hubo casos de infección por VHS-1, VHS-2 ni VZV. Las infecciones por enterovirus alcanzaron el 82,9 % en los meses cálidos de noviembre a enero y el 28,6 % en los meses fríos de mayo a julio. Conclusiones. Los enterovirus fueron los principales agentes etiológicos en las encefalitis y meningitis asépticas agudas en pacientes pediátricos de Lima, Perú. Los enterovirus tienen un comportamiento epidemiológico estacional con un claro aumento del número de casos en los meses de verano. Resulta útil tener disponible un método de diagnóstico rápido, como una ayuda para el manejo de las infecciones agudas del sistema nervioso.Objectives. To determine the frequency and clinical features of central nervous system infections caused by enterovirus in children treated at the Hospital Nacional Cayetano Heredia in Lima, Peru. Materials and methods. A prospective, descriptive study was performed from April 2008 to March 2010. Patients aged 1 month - 14 years with clinical diagnosis of encephalitis or aseptic meningitis were included. We investigated the

Millennial-scale vegetation changes in the tropical Andes using ecological grouping and ordination methods

NARCIS (Netherlands)

Urrego, D.H.; Hooghiemstra, H.; Rama-Corredor, O.; Martrat, B.; Grimalt, J.O.; Thompson, L.; Bush, M.B.; González-Carranza, Z.; Hanselman, J.; Valencia, B.; Velásquez-Ruiz, C.

2016-01-01

We compare eight pollen records reflecting climatic and environmental change from northern and southern sites in the tropical Andes. Our analysis focuses on the last 30 000 years, with particular emphasis on the Pleistocene to Holocene transition. We explore ecological grouping and downcore

DE LA DISCIPLINARIEDAD A LA TRANSDISCIPLINARIEDAD. UNA VISIÓN DESDE LA PERSPECTIVA DE LA FORMACIÓN DEL CONTADOR PÚBLICO

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Rosa Aura Casal de Altuve

2010-07-01

Full Text Available Los organismos internacionales exigen cambios en cuanto a la formación del contador público. Esta investigación busca presentar los criterios del tránsito disciplinar al transdisciplinar en la formación del contador público. El estudio es de tipo documental y analítico apoyado en discusiones grupales realizadas a los profesores del Departamento de Contabilidad y Finanzas de la Universidad de Los Andes – Venezuela. Como técnica interpretativa se utilizó la hermenéutica y se derivó que el contador público debido a su formación tan disciplinar, ha tenido como efecto una excesiva fragmentación y reducción de los problemas contables, pero por otra parte, no se habla de una formación sólida del contador público sin un estudio profundo de la disciplina contable. Por su parte, la formación del contador público desde la transdisciplinariedad, implica una concepción holística y amplia de los problemas contables, pero requiere no sólo de un cambio de planes de estudio, o de estructuras universitarias, sino un cambio del sujeto (estudiante-docente-autoridad y de la forma de ver al mundo.

CORVI,Corvus frugilegus L.,SVERNANTI NELLA VALPADANA CENTRALE E CONSERVAZIONE DEL PAESAGGIO AGRARIO TRADIZIONALE

Institute of Scientific and Technical Information of China (English)

RICCARDO GROPPALI

1993-01-01

<正> RIASSUNTO-Nel corso di tre inverni(1990-91,1991-92 e 1992-93)sono stati osservati,lungo differentipercorsi stradali della Valpadana centrale,10370 Corvi.Per ogni individuo sono stati rilevati tipo dicoltivazione sulla quale era posato,ampiezza del campo e presenza di filari/siepi.In anni singoli sonostati esaminati altri fattori(distanza da abitazioni,dalla strada e dai filari o loro uso come posatoio).Lungo un percorso di circa 70 km(Cremona-Pavia)è stata inoltre rilevata la posizione cartografica deiCorvi osservati.Dai dati raccolti si può dedurre che questa specie può svernare soltanto in aree consufficiente varietà colturale e paesaggio agrario tradizionale,e che modificazioni gestionali possono elimi-narne la presenza.Wintering Rooks,Corvus frugilegus L.,in the central Po Valley and conservation ofthe traditional agricultural landscape.During three winter seasons(1990-91,1991-92 and 1992-93)10370Rooks were observed,along roads of the central Po Valley.The kind of cultivation,the extension offield and the presence of tree rows/hedges was noted for every resting Rook.Other factors(distancefrom habitations,road and tree rows,and their use for resting)were examined during single years.Alonga 70 km road(Cremona-Pavia,Northern Italy)the geographic position of the observed Rooks was noted.According to the observations,it seems that Rooks can winter only in areas with sufficiently variouscultivations and a traditional agricultural landscape,and that variations in their management can elimina-te the presence of the species.

Natural dam failure in the eastern slope of the Central Andes of Argentina. Numerical modelling of the 2005 Santa Cruz river outburst flood

Science.gov (United States)

Penna, I.; Daicz, S.; Zlotnik, S.; Derron, M.-H.; Jaboyedoff, M.

2012-04-01

In the Central Andes of Argentina, ephemeral river blockage due to landslides deposition are common phenomena. During the first fortnight of January 2005, 11.5 * 106m3 of rock collapsed from the east slope of the Santa Cruz valley (San Juan province, Argentina). The rock mass displaced from 4300 m a.s.l., down to the valley bottom, at 2900 m a.s.l., and ran up the opposite flank of the valley. This produced the blockage of the Santa Cruz river and generated the Los Erizos lake. The rapid snow melting during the spring season caused the increase of the water level of the reservoir, leading to a process of overtopping on November 12th of 2005. 30 * 106m3 of water were released from the reservoir and the consequent outburst flood displaced along 250 km. From local reports of arrival times, we estimated that the outburst flood reduced its velocity from around 40 km/h near the source area to 6 km/h in its distal section. A road, bridges, and a mining post where destroyed. 75 tourists had to be rescued from the mountains using helicopters, and people from two localities had to be evacuated. Near its distal part, the flood damaged the facilities of the Caracoles power dam, which was under construction, and its inauguration had to be delayed one year due to the damage. The outburst flood produced changes in the morphology of the valley floor along almost all its path (erosion of alluvial fans, talus and terraces, and deposition of boulders). The most significant changes occurred in the first 70 km, especially upstream narrow sections, showing the importance of the backwater effects due to hydraulic ponding. In this work we carried out numerical simulations to obtain the velocity patterns of the flood, and compared them with those obtained from local reports. Furthermore, we analyze the relationship between the dynamics of the flood with the patterns of erosion and deposition near the source area.

Central catheter dressing in a simulator: the effects of tutor's assistance or self-learning tutorial Parche de catéter central en simulador: efecto de la presencia del tutor o del aprendizaje auto-instruccional Curativo de cateter central em simulador: efeito da presença do tutor ou da aprendizagem autoinstrucional

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Milene Thaís Marmol

2012-12-01

Full Text Available AIMS: to compare the performance of undergraduate students concerning semi-implanted central venous catheter dressing in a simulator, with the assistance of a tutor or of a self-learning tutorial. METHOD: Randomized controlled trial. The sample consisted of 35 undergraduate nursing students, who were divided into two groups after attending an open dialogue presentation class and watching a video. One group undertook the procedure practice with a tutor and the other with the assistance of a self-learning tutorial. RESULTS: in relation to cognitive knowledge, the two groups had lower performance in the pre-test than in the post-test. The group that received assistance from a tutor performed better in the practical assessment. CONCLUSION: the simulation undertaken with the assistance of a tutor showed to be the most effective learning strategy when compared to the simulation using a self-learning tutorial. Advances in nursing simulation technology are of upmost importance and the role of the tutor in the learning process should be highlighted, taking into consideration the role this professional plays in knowledge acquisition and in the development of critical-reflexive thoughts and attitudes. (ClinicalTrials.gov Identifier: NCT 01614314.OBJETIVO: comparar el desempeño de graduandos en la realización del parche del catéter venoso central semi-implantado, en simulador, con el auxilio del tutor o de un guía auto-instruccional. MÉTODO: estudio experimental controlado hecho aleatorio. La muestra fue compuesta por 35 alumnos de Graduación en Enfermería que fueron asignados en dos grupos después de asistir a una clase expositiva dialogada y a un vídeo. Un grupo realizó el entrenamiento del procedimiento con el tutor y el otro con el auxilio de un guía auto- instruccional. RESULTADOS: con relación al conocimiento cognoscitivo, los dos grupos presentaron desempeño menor en la pre-prueba comparada al pos-prueba. El grupo con presencia del tutor

Efectos de las anomalías climáticas en la cobertura de nieve de los glaciares centrales del Perú

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Jacinto Arroyo Aliaga

2015-06-01

Full Text Available Se definió como objetivo, identificar los efectos de anomalías climáticas en la cobertura de nieve de los glaciares centrales del Perú. Para el desarrollo de esta investigación se han utilizado los métodos del índice de precipitación estandarizada para el análisis de las anomalías climáticas; de la transformada rápida de Fourier para la identificación de la variabilidad climática, y el método de geoprocesamiento de imágenes satelitales Landsat. Algunos resultados son: Se identificaron cuatro anomalías negativas que corresponden a los años 1991 (extremadamente seco y 1986, 2005, 2009 (muy seco con tres anomalías positivas que corresponden a los años 1985, 2010 (extremadamente lluvioso; 1966 (muy lluvioso que influyeron en la pérdida y acumulación del manto de nieve del glaciar Huaytapallana. En el glaciar Pariaqaqa se encontró tres anomalías negativas de los años 1991 (Extremadamente seco; 1990, 2013 (muy seco y cuatro anomalías positivas de los años 1972 y 2010 (extremadamente lluvioso; 1966 y 2011 (muy lluvioso; que influyeron positivamente en la acumulación del manto de ieve. Se concluye que la pérdida neta corresponde a 5 km2 en el glaciar Huaytapallana y 7 km2 en el glaciar Pariaqaqa. El incremento del manto de nieve del glaciar Huaytapallana y Pariaqaqa en los ciclos hidrológicos del 2010, 2011 y 2012 se debe a un aumento en las intensidades de las precipitaciones registradas durante estos años por cambios en los patrones de circulación atmosférica por fenómenos de El Niño Oscilación del Sur.

El mundo del libro: [enero a diciembre] de 1980

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Agustín Rodríguez Garavito

1980-06-01

Full Text Available El documento presenta las siguientes reseñas de libros: -GUANO MALDITO-Por Joaquín Aguirre-Colección Andina-Bogotá-Ediciones Tercer Mundo-La Paz-Bogotá, Colombia. -El letrado español José María Alfaro y Polanco -FANTASMAS DE DOS MUNDOS-Por Arturo Uslar Pietri--Seix-Barral S. A. Barcelona- Caracas-México-Enero 1977-Avenida José Antonio-Madrid. -HOMENAJE A FERNANDO ANTONIO MARTÍNEZ-Estudios de Lingüística, filología, literatura e historia general-Publicaciones del Instituto Caro y Cuervo. LXVIII-Bogotá, 1979. -PROSAS-Por Jaime Barrera Parra- Empresa Colombiana de Petróleos - ECOPETROL - Editorial Andes, Bogotá. 1.347 páginas. -POESÍA-Por Rodolfo Moleiro -TENSO EN LA SOMBRA-Instituto de Cultura y Bellas Artes-Caracas, Venezuela. -REGRESO DEL VIENTO-Cuentos-Por Humberto Jaramillo Angel-Editorial Quin-Gráficas-Armenia, Colombia. -La poesía de Rafael Amaya -LA ÚLTIMA NOTICIA-Novela por Humberto Tafur Charry. -EL TRIUNFO DE LA MUERTE- Relatos-Por Gloria Nieto de Arias-Ediciones Tercer Mundo-Bogotá, Colombia. -COLOMBIA Y VENEZUELA-Integración-Por Manuel Roca Castellanos. -LOS ESPEJOS DEL TIEMPO-Por Eduardo Santa-Ediciones Príncipe-Bogotá, Colombia. -LOS OJOS DE LOS ENTERRADOS-Por Miguel Angel Asturias-Editorial Losada-Buenos Aires, Argentina. -APROXIMACIÓN A SIMÓN BOLÍVAR-Tema.

A modelling study of the seasonal snowpack energy balance at three sites along the Andes Cordillera. Regional climate and local effects.

Science.gov (United States)

McPhee, James; Mengual, Sebastian; MacDonell, Shelley

2017-04-01

Seasonal snowpack melt constitutes the main water source for large portions of extratropical South America, including central Chile and Western Argentina. The properties and distribution of snow in the Andes are threatened by rapid climate change, characterised by warming and drying. This study provides a first attempt at detailed description of the energy balance of the seasonal snowpack and its variability along a latitudinal gradient, which is also correlated with an elevation and precipitation gradient, in the Andes Cordillera. The Snowpack model was validated at semi-arid, Mediterranean and temperate humid sites, where meteorological and snowpack properties have been observed since year 2013. Site elevations decrease from north to south, whereas precipitation climatology increases with latitude. Results show that turbulent energy exchange becomes relatively more important in periods of low snow accumulation, with sensible heat fluxes having a greater effect in cooling the snowpack at the high-altitude, low latitude site. Likewise, daily melt-freeze cycles are important in maintaining positive cold contents throughout the accumulation season at this site, and contribute to extending the duration of snow cover despite low accumulation and high radiation loads. In contrast, the southernmost, lowest elevation site shows smaller daily temperature amplitude and a much more preponderant radiation component to the energy balance. This modelling exercise highlights the nonlinearities of snow dynamics at different geographical settings in a sparsely monitored mountain area of the world, as well as the need for further understanding in order to evaluate the sensitivity of snow-dominated watersheds to global warming and climate change.

Macroinvertebrate community response to acid mine drainage in rivers of the High Andes (Bolivia).

NARCIS (Netherlands)

Damme, P.A. van; Hamel, C.; Ayala, A.; Bervoets, L.

2008-01-01

Several High Andes Rivers are characterized by inorganic water pollution known as acid mine drainage (AMD). The aim of this study was to assess the relationship between metal concentrations in the sediments and the macroinvertebrate communities in two river basins affected by AMD. In general, the

Cenozoic basin thermal history reconstruction and petroleum systems in the eastern Colombian Andes

Science.gov (United States)

Parra, Mauricio; Mora, Andres; Ketcham, Richard A.; Stockli, Daniel F.; Almendral, Ariel

2017-04-01

Late Mesozoic-Cenozoic retro-arc foreland basins along the eastern margin of the Andes in South America host the world's best detrital record for the study of subduction orogenesis. There, the world's most prolific petroleum system occur in the northernmost of these foreland basin systems, in Ecuador, Colombia and Venezuela, yet over 90% of the discovered hydrocarbons there occur in one single province in norteastern Venezuela. A successful industry-academy collaboration applied a multidisciplinary approach to the study of the north Andes with the aim of investigating both, the driving mechanisms of orogenesis, and its impact on hydrocarbon accumulation in eastern Colombia. The Eastern Cordillera is an inversion orogen located at the leading edge of the northern Andes. Syn-rift subsidence favored the accumulation of km-thick organic matter rich shales in a back-arc basin in the early Cretaceous. Subsequent late Cretaceous thermal subsidence prompted the accumulation of shallow marine sandstones and shales, the latter including the Turonian-Cenomanian main hydrocarbon source-rock. Early Andean uplift since the Paleocene led to development of a flexural basin, filled with mainly non-marine strata. We have studied the Meso-Cenozoic thermal evolution of these basins through modeling of a large thermochronometric database including hundreds of apatite and zircon fission-track and (U-Th)/He data, as well as paleothermometric information based on vitrinite reflectance and present-day temperatures measured in boreholes. The detrital record of Andean construction was also investigated through detrital zircon U-Pb geochronometry in outcrop and borehole samples. A comprehensive burial/exhumation history has been accomplished through three main modeling strategies. First, one-dimensional subsidence was used to invert the pre-extensional lithospheric thicknesses, the magnitude of stretching, and the resulting heat flow associated to extension. The amount of eroded section and

The effect of heat and smoke on the emergence of exotic and native seedlings in a Mediterranean fire-free matorral of central Chile Efecto del calor y el humo sobre la emergencia de plántulas exóticas y nativas en un matorral mediterráneo libre de fuego en Chile central

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JAVIER A FIGUEROA

2012-03-01

Full Text Available We studied the effect of heat shock and wood-fueled smoke on the emergence of native and exotic plant species in soil samples obtained in an evergreen matorral of central Chile that has been free of fire for decades. It is located on the eastern foothills of the Andes Range in San Carlos de Apoquindo. Immediately after collection samples were dried and stored under laboratory conditions. For each two transect, ten samples were randomly chosen, and one of the following treatments was applied: (1 heat-shock treatment, (2 plant-produced smoke treatment, (3 combined heat-and-smoke treatment, and (4 control, corresponding to samples not subjected to treatment. Twenty-seven species, representing 13 families, emerged from the soil samples. The most abundant families were Asteraceae and Poaceae. All of the emerged species were herbaceous, and 18 species were exotic. Respect to general hypothesis, there is no evidence for the proposition that fire-free matorral has lower proportion of exotic and native species with fire-related cues than matorral with fires. Among the exotic and native, the mean number of species that emerged from soil samples did not change significantly with respect to the control for any of the treatments applied. Nevertheless, important species-specific responses were observed. Smoke and heat-smoke combination significantly increased the emergence of the exotic species Anthriscus caucalis. While smoke-related cues significantly increased the emergence of the exotic species Avena barbata, the emergence of the exotic Aphanes arvensis and the native Bromus berteroanus decreases. For several species our results showed inconsistent responses to fire-related cues compared to those reported in the literature. We suggest that these differences might be related with the fire-history in the populations, an important issue poorly acknowledge in the literature.Nosotros estudiamos el efecto del golpe de calor y del humo de la combustión de

Cuentos ashaninka del r??o Peren??

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Plasencia Soto, Rommel; S??nchez V??squez, Melisa

2009-01-01

La memoria ind??gena de los pueblos amaz??nicos del Per?? de hoy, es mostrada en cuatro relatos registrados en la comunidad de Mariscal C??ceres en el valle del r??o Peren?? de la selva central peruana.

A glacial record of the last termination in the southern tropical Andes

Science.gov (United States)

Bromley, G. R.; Schaefer, J. M.; Winckler, G.; Hall, B. L.; Todd, C. E.; Rademaker, K.

2012-12-01

The last glacial termination represents the highest-magnitude climate change of the last hundred thousand years. Accurate resolution of events during the termination is vital to our understanding of how - and why - the global climate system transitions from a full glacial to interglacial state, as well as the causes of abrupt climate change during the late-glacial period. Palaeoclimate data from low latitudes, though relatively sparse, are particularly valuable, since the tropical ocean and atmosphere likely play a crucial role in Quaternary climate variability on all timescales. We present a detailed glacier record from the Andes of southern Peru (15°S), resolved with 3He surface-exposure dating and spanning the last glacial maximum and termination. Our dataset reveals that glaciers in this part of the Southern Hemisphere maintained their Late Pleistocene maxima for several millennia and that the onset of the termination may have occurred relatively late. Deglaciation was punctuated by two major advances during the late-glacial period. Following the glacial-interglacial transition, our preliminary chronologic and morphologic data suggest that, in contrast to the Northern Hemisphere, glaciers in the southern tropical Andes have experienced overall shrinkage during the Holocene.

STRUCTURAL CHARACTERIZATION OF VOLCANIC ASH OF THE NEVADO DEL RUIZ: ZEOLITE PHASE IDENTIFICATION

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Heiddy P. Quiroz

2014-08-01

Full Text Available This paper presents a study of the structural properties obtained from volcanic ash from Nevado del Ruiz located in the Central Range of Andes - Colombia. The volcanic ash samples were subjected to hydration processes and heat treatments in situ during characterization stage material. During the hydration process, which consisted of introducing 2.4875 ± 0.0002g of volcanic ash in 20ml of water for 48 hours, the organic fraction present was removed from the particulate suspension in the aqueous medium. From measurements of X-ray diffraction (XRD, it was observed, that the temperature variations between 323 and 673 K influence the phase formation of zeolite with structures Heulandite -Ca, Stellerita and gmelinite. XRD measurements were performed in vacuum and atmospheric pressure. X'pert Highscore Plus program and simulation Rietveld refinement were used for to obtain the structures of each of the phases. It was found, using the Scherrer equation, that crystallite sizes (Δ (2θ are influenced by changes crystal-chemical caused by hydration, heat treatment and pressure conditions during the characterization. A variation of Δ ( 2θ between 37 and 106.9 nm from XRD measurements was found. It was determined that from 423K in the sample of un-hydrated volcanic ash, the formation of zeolite Stellerita presents with a stable phase up to 673 K.

Nueva especie de rana (Atelopus de Los Farallones de Cali, Cordillera Occidental de Colombia

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Kattan Gustavo

1986-06-01

Full Text Available Durante la realización de colecciones herpetológicas en el Departamento del Valle del Cauca, fue encontrada una especie no descrita de Atelopus (Anura: Bufonidae en los farallones de Cali, a 2600 m de altura. Esta es la primera especie en este género que se encuentra a elevaciones superiores a 2000 m en la Cordillera Occidental. Se conocen varias especies de Atelopus en las Cordilleras Central y Oriental de Colombia y en los Andes ecuatorianos (COCHRAN y GOIN 1970; PETERS 1973; RIVERO 1963 y probablemente futuras colecciones herpetológicas continuaran revelando nuevas especies en las partes altas de la Cordillera Occidental.

Influencia de la personalidad del cuidador/a, en los adolescentes que ejercen bullying, realizado en el nivel básico del Colegio Fiscal Mixto Central “La Inmaculada”

OpenAIRE

Cabrera Vélez, Marcela

2014-01-01

El bullying por sus características, es fundamental prevenirlo, siendo un papel importante el cual desenvuelven los cuidadores dentro del ambiente familiar, ya que según estadísticas, el Ecuador se encuentra en segundo lugar de incidencias en Sudamérica, presentándose en la Ciudad de Cuenca en un 16% a nivel escolar. El presente trabajo tiene como objetivo principal, analizar los rasgos de personalidad de los cuidadores de adolescentes que ejercen bullying pertenecientes al Colegio Central La...

Molecular identification of vectors of Leishmania in Colombia: mitochondrial introgression in the Lutzomyia townsendi series.

Science.gov (United States)

Testa, J M; Montoya-Lerma, J; Cadena, H; Oviedo, M; Ready, P D

2002-12-01

The identity of the sandfly vectors of Leishmania braziliensis in Valle del Cauca Department, Colombia, was originally given as Lutzomyia townsendi, but then changed to L. youngi, another member of the L. townsendi series (Verrucarum group) with isomorphic females. To identify members of this series in Valle del Cauca, we analyzed the nuclear gene elongation factor-alpha (EF-alpha) and the mitochondrial gene cytochrome b (Cyt b). DNA sequences from the L. verrucarum series (L. columbiana, L. evansi and L. ovallesi) were used as outgroups. Flies from two locations on the western cordillera of the Andes were identified as L. townsendi s.s., according to male morphology and distinctive gene lineages. In the third location, on the central cordillera of the Andes, most specimens were identified as belonging to a geographical population of L. youngi, according to male morphology, an EF-alpha lineage shared with L. youngi from the Venezuelan-type locality, and a distinctive Cyt b sub-lineage. All other specimens were identified as L. youngi with the introgressed Cyt b sequences of L. townsendi. Such interspecific introgression implies that vectorial traits and ecological associations may no longer be viewed as fixed properties of different morphospecies.

Design optimization of the Laguna Verde nuclear power station fuel recharge; Optimacion del diseno de recargas de combustible para la Central Laguna Verde

Energy Technology Data Exchange (ETDEWEB)

Cortes Campos, Carlos Cristobal [Instituto de Investigaciones Electricas, Cuernavaca (Mexico); Montes Tadeo, Jose Luis [Instituto Nacional de Investigaciones Nucleares (ININ), Salazar (Mexico)

1991-12-31

It is described, in general terms, the procedure that is followed to accomplish the optimization of the recharge design, and an example is shown where this procedure was applied for the analysis of the type BWR reactor of Unit No. 1 of the Laguna Verde Nuclear Power Station. [Espanol] Se describe en terminos generales el procedimiento que se sigue para realizar la optimacion del diseno de recargas, y se muestra un ejemplo en el que se utilizo dicho procedimiento para el analisis del reactor tipo BWR de la unidad 1, de la Central Laguna Verde (CLV).

Design optimization of the Laguna Verde nuclear power station fuel recharge; Optimacion del diseno de recargas de combustible para la Central Laguna Verde

Energy Technology Data Exchange (ETDEWEB)

Cortes Campos, Carlos Cristobal [Instituto de Investigaciones Electricas, Cuernavaca (Mexico); Montes Tadeo, Jose Luis [Instituto Nacional de Investigaciones Nucleares (ININ), Salazar (Mexico)

1992-12-31

It is described, in general terms, the procedure that is followed to accomplish the optimization of the recharge design, and an example is shown where this procedure was applied for the analysis of the type BWR reactor of Unit No. 1 of the Laguna Verde Nuclear Power Station. [Espanol] Se describe en terminos generales el procedimiento que se sigue para realizar la optimacion del diseno de recargas, y se muestra un ejemplo en el que se utilizo dicho procedimiento para el analisis del reactor tipo BWR de la unidad 1, de la Central Laguna Verde (CLV).