WorldWideScience

Sample records for ka cal bp

  1. Sediment record of environmental change at Lake Lop Nur (Xinjiang, NW China) from 13.0 to 5.6 cal ka BP

    Science.gov (United States)

    Wang, Jingzhong; Jia, Hongjuan

    2016-09-01

    Lake Lop Nur is located in the eastern part of the Tarim Basin in Xinjiang, northwestern China. A 220-cm-long sediment core was collected from the center of the ear-shaped depression forming the basin and dated with AMS14C. Grain size, total organic matter (TOC), total nitrogen (TN), and TOC/TN (C/N) analyses were used to reconstruct climatic conditions from 13.0 to 5.6 cal ka BP. The results showed five main climatic stages. Zone I (13.0-11.3 cal ka BP) was a wet-dry environment, whereas Zone II (11.3-8.9 cal ka BP) consisted of a primarily wet environment. Zone III (8.9-7.7 cal ka BP) was subdivided into Zone IIIa (8.9-8.2 cal ka BP) that indicated lake constriction and dry climate, and Zone IIIb (8.2-7.7 cal ka BP) in which the proxies indicated wet conditions. In Zone IV (7.7-6.6 cal ka BP), the climate presented a bit wet conditions. In Zone V (6.6-5.6 cal ka BP), abundant glauberite is present in the sediment and silt dominates the lithology; these results indicate the lake shrank and the overall climate was dry. Abrupt environmental events were also identified, including six dry events at 11.0, 10.5, 9.3, 8.6, 8.2, and 7.6 cal ka BP and one flood event from 7.8 to 7.7 cal ka BP in the Early-Middle Holocene.

  2. Sediment record of environmental change at Lake Lop Nur (Xinjiang, NW China) from 13.0 to 5.6 cal ka BP

    Science.gov (United States)

    Wang, Jingzhong; Jia, Hongjuan

    2017-09-01

    Lake Lop Nur is located in the eastern part of the Tarim Basin in Xinjiang, northwestern China. A 220-cm-long sediment core was collected from the center of the ear-shaped depression forming the basin and dated with AMS14C. Grain size, total organic matter (TOC), total nitrogen (TN), and TOC/TN (C/N) analyses were used to reconstruct climatic conditions from 13.0 to 5.6 cal ka BP. The results showed five main climatic stages. Zone I (13.0-11.3 cal ka BP) was a wet-dry environment, whereas Zone II (11.3-8.9 cal ka BP) consisted of a primarily wet environment. Zone III (8.9-7.7 cal ka BP) was subdivided into Zone IIIa (8.9-8.2 cal ka BP) that indicated lake constriction and dry climate, and Zone IIIb (8.2-7.7 cal ka BP) in which the proxies indicated wet conditions. In Zone IV (7.7-6.6 cal ka BP), the climate presented a bit wet conditions. In Zone V (6.6-5.6 cal ka BP), abundant glauberite is present in the sediment and silt dominates the lithology; these results indicate the lake shrank and the overall climate was dry. Abrupt environmental events were also identified, including six dry events at 11.0, 10.5, 9.3, 8.6, 8.2, and 7.6 cal ka BP and one flood event from 7.8 to 7.7 cal ka BP in the Early-Middle Holocene.

  3. Glacial to paraglacial history and forest recovery in the Oglio glacier system (Italian Alps) between 26 and 15 ka cal BP

    Science.gov (United States)

    Ravazzi, Cesare; Badino, Federica; Marsetti, Diego; Patera, Glauco; Reimer, Paula J.

    2012-12-01

    The integrated stratigraphic, radiocarbon and palynological record from an end-moraine system of the Oglio valley glacier (Italian Alps), propagating a lobe upstream in a lateral reach, provided evidence for a complete cycle of glacial advance, culmination and withdrawal during the Last Glacial Maximum and early Lateglacial. The glacier culminated in the end moraine shortly after 25.8 ± 0.8 ka cal BP, and cleared the valley floor 18.3-17.2 ± 0.3 ka cal BP. A primary paraglacial phase is then recorded by fast progradation of the valley floor. As early as 16.7 ± 0.3 ka cal BP, early stabilization of alluvial fans and lake filling promoted expansion of cembran pine. This is an unprecedented evidence of direct tree response to depletion of paraglacial activity during the early Lateglacial, and also documents the cembran pine survival in the mountain belt of the Italian Alps during the last glaciation. Between 16.1 and 14.6 ± 0.5 ka cal BP, debris cones emplacement points to a moisture increase favouring tree Betula and Pinus sylvestris-mugo. A climate perturbation renewed paraglacial activity. According to cosmogenic ages on glacial deposits and AMS radiocarbon ages from lake records in South-Eastern Alps such phase compares favourably with the Gschnitz stadial and with the oscillations recorded at lakes Ragogna, Längsee and Jeserzersee, most probably forced by the latest freshening phases of the Heinrich Event 1. A further sharp pine rise marks the subsequent onset of Bølling interstadial. The chronology of the Oglio glacier compares closely with major piedmont glaciers on the Central and Eastern Alpine forelands. On the other hand, the results of the present study imply a chronostratigraphic re-assessment of the recent geological mapping of the Central Italian Alps.

  4. Post-glacial flooding of the Bering Land Bridge dated to 11 cal ka BP based on new geophysical and sediment records

    Science.gov (United States)

    Jakobsson, Martin; Pearce, Christof; Cronin, Thomas M.; Backman, Jan; Anderson, Leif G.; Barrientos, Natalia; Björk, Göran; Coxall, Helen; de Boer, Agatha; Mayer, Larry A.; Mörth, Carl-Magnus; Nilsson, Johan; Rattray, Jayne E.; Stranne, Christian; Semiletov, Igor; O'Regan, Matt

    2017-08-01

    The Bering Strait connects the Arctic and Pacific oceans and separates the North American and Asian landmasses. The presently shallow ( ˜ 53 m) strait was exposed during the sea level lowstand of the last glacial period, which permitted human migration across a land bridge today referred to as the Bering Land Bridge. Proxy studies (stable isotope composition of foraminifera, whale migration into the Arctic Ocean, mollusc and insect fossils and paleobotanical data) have suggested a range of ages for the Bering Strait reopening, mainly falling within the Younger Dryas stadial (12.9-11.7 cal ka BP). Here we provide new information on the deglacial and post-glacial evolution of the Arctic-Pacific connection through the Bering Strait based on analyses of geological and geophysical data from Herald Canyon, located north of the Bering Strait on the Chukchi Sea shelf region in the western Arctic Ocean. Our results suggest an initial opening at about 11 cal ka BP in the earliest Holocene, which is later than in several previous studies. Our key evidence is based on a well-dated core from Herald Canyon, in which a shift from a near-shore environment to a Pacific-influenced open marine setting at around 11 cal ka BP is observed. The shift corresponds to meltwater pulse 1b (MWP1b) and is interpreted to signify relatively rapid breaching of the Bering Strait and the submergence of the large Bering Land Bridge. Although the precise rates of sea level rise cannot be quantified, our new results suggest that the late deglacial sea level rise was rapid and occurred after the end of the Younger Dryas stadial.

  5. Landscape transformations at the dawn of agriculture in southern Syria (10.7-9.9 ka cal. BP): Plant-specific responses to the impact of human activities and climate change

    Science.gov (United States)

    Arranz-Otaegui, Amaia; López-Sáez, José Antonio; Araus, José Luis; Portillo, Marta; Balbo, Andrea; Iriarte, Eneko; Gourichon, Lionel; Braemer, Frank; Zapata, Lydia; Ibáñez, Juan José

    2017-02-01

    In southwest Asia, the accelerated impact of human activities on the landscape has often been linked to the development of fully agricultural societies during the middle and late Pre-Pottery Neolithic B (PPNB) period (around 10.2-7.9 ka cal. BP). This work contributes to the debate on the environmental impact of the so-called Neolitisation process by identifying the climatic and anthropogenic factors that contributed to change local and regional vegetation at the time when domesticated plants appeared and developed in southern Syria (around 10.7-9.9 ka cal. BP). In this work a multidisciplinary analysis of plant microremains (pollen and phytoliths) and macroremains (wood charcoal) is carried out along with stable carbon isotope discrimination of wood charcoals in an early PPNB site (Tell Qarassa North, west of the Jabal al-Arab area). Prior to 10.5 ka cal. BP, the results indicate a dynamic equilibrium in the local and regional vegetation, which comprised woodland-steppe, Mediterranean evergreen oak-woodlands, wetland vegetation and coniferous forests. Around 10.5-9.9 ka cal. BP, the elements that regulated the vegetation system changed, resulting in reduced proportions of arboreal cover and the spread of cold-tolerant and wetlands species. Our data show that reinforcing interaction between the elements of the anthropogenic (e.g. herding, fire-related activities) and climatic systems (e.g. temperature, rainfall) contributed to the transformation of early Holocene vegetation during the emergence of fully agricultural societies in southern Syria.

  6. Millennial-Scale Climate Variability during the Last 28 cal. ka BP in the Tyrrhenian Sea (central Sector of Mediterranean Sea)

    Science.gov (United States)

    Amore, F. Ornella; Palumbo, Eliana; Elderfield, Henry; Perugia, Carmen; Emanuele, Dario; Petrillo, Zaccaria

    2014-05-01

    High resolution reconstructions of coccolithophore assemblages and plankton carbon and oxygen stable isotope data from Ocean Drilling Project (ODP) Hole 974D have been studied to investigate climate variability in the Tyrrhenian Sea (Western Mediterranean) during the last 28 cal. ka BP. The main climatic signal is showed by coccolithophore assemblages and isotopic records at glacial/interglacial timescale. Through the application of statistical analyses, a possible role of half and fourth precession cycles was hypothesised, more likely linked to the influence of the Equator insolation on central sector of Western Mediterranean circulation. The occurrence of abrupt coolings, more likely connected to Northern Hemisphere global climatic changes, was hypothesised also in the Tyrrhenian Sea during the Last Glacial (LG) and the Holocene, highlighted by the occurrence of the subpolar species Coccolithus pelagicus pelagicus. The events of the LG occurred in correspondence of the Dansgaard/Oeschger (D/O) stadial at 28 cal. ka BP and Heinrich event 2. The Holocene events were quite synchronous with several Bond Cycles and Rapid Climate Changes. In addition, marine warm phases, coincident with the D/O interstadial 2 and the Bølling-Allerød interval, were recognised at ODP Hole 974D by increases of warm species. Furthermore, during the Younger Dryas, oxygen stable isotope record indicates the occurrence of a cooling while coccolithophore assemblages testify increased nutrient conditions, highlighted by the group of small Gephyrocapsa. During the transition to the Holocene a latitudinal warming was observed, through the comparison of available data from coccolithophore assemblages of other sites of the Tyrrhenian Sea (Sbaffi et al., 2001; Buccheri et al., 2002; Amore et al., 2004). The latitudinal warming moved northward versus the central part of the basin, reaching the maximum amplitude in correspondence of Tyrrhenian Holocene Climatic Optimum (Buccheri et al., 2002). Other

  7. Marine04 Marine radiocarbon age calibration, 26 ? 0 ka BP

    Energy Technology Data Exchange (ETDEWEB)

    Hughen, K; Baille, M; Bard, E; Beck, J; Bertrand, C; Blackwell, P; Buck, C; Burr, G; Cutler, K; Damon, P; Edwards, R; Fairbanks, R; Friedrich, M; Guilderson, T; Kromer, B; McCormac, F; Manning, S; Bronk-Ramsey, C; Reimer, P; Reimer, R; Remmele, S; Southon, J; Stuiver, M; Talamo, S; Taylor, F; der Plicht, J v; Weyhenmeyer, C

    2004-11-01

    New radiocarbon calibration curves, IntCal04 and Marine04, have been constructed and internationally ratified to replace the terrestrial and marine components of IntCal98. The new calibration datasets extend an additional 2000 years, from 0-26 ka cal BP (Before Present, 0 cal BP = AD 1950), and provide much higher resolution, greater precision and more detailed structure than IntCal98. For the Marine04 curve, dendrochronologically dated tree-ring samples, converted with a box-diffusion model to marine mixed-layer ages, cover the period from 0-10.5 ka cal BP. Beyond 10.5 ka cal BP, high-resolution marine data become available from foraminifera in varved sediments and U/Th-dated corals. The marine records are corrected with site-specific {sup 14}C reservoir age information to provide a single global marine mixed-layer calibration from 10.5-26.0 ka cal BP. A substantial enhancement relative to IntCal98 is the introduction of a random walk model, which takes into account the uncertainty in both the calendar age and the radiocarbon age to calculate the underlying calibration curve. The marine datasets and calibration curve for marine samples from the surface mixed layer (Marine04) are discussed here. The tree-ring datasets, sources of uncertainty, and regional offsets are presented in detail in a companion paper by Reimer et al.

  8. Advection of Atlantic Water to the Western and Northern Svalbard Shelves Through the Last 17.5 ka cal yr BP

    Science.gov (United States)

    Slubowska, M. A.; Rasmussen, T. L.; Koc, N.; Kristensen, D. K.; Nilsen, F.; Solheim, A.

    2005-12-01

    We have studied the distribution of benthic foraminifera species together with planktonic and benthic foraminifera abundances, stable oxygen isotopes and lithology in two cores: JM02-440 from the western (77° 22' N, 12° 48' E, 240 m water depth) and NP94-51 from the northern (80° 21' N and 16 ° 17' E, 400 m water depth) shelf of Svalbard. The purpose of the study was to reconstruct the changes in flow and character of the relatively warm Atlantic Water through the last 17.5 ka cal yr BP. The results from these two sites were compared with previously published records from the eastern Nordic Seas in order to follow the history of the advection of Atlantic Water as it moved northwards along the Norwegian coast and into the Arctic Ocean. Our results indicate that synchronous oceanographic changes occurred at the western and northern Svalbard shelves. The benthic foraminifera and oxygen isotope records indicate almost continuous presence of the Atlantic Water at the shelf areas since the deglaciation. The Bolling-Allerod period stands out as the warmest period in our records with the highest bottom waters temperatures indicating strong inflow of Atlantic Water. However, the warm Atlantic Water was isolated below cold and probably sea ice covered surface waters in contrast to the surface waters along the Norwegian coast, which experienced enhanced temperatures. During the Younger Dryas a freshening of the bottom waters occurred and the Polar Front was located in a proximal position to both sites. The strong inflow of saline, but chilled Atlantic Water happened during the Early Holocene. A distinct cooling and freshening of the bottom water masses occurred during the Mid- and Late Holocene, and was accompanied by glacier re-advances leading to the present-day conditions. During the last millennium, the inflow of Atlantic Water appears to increase, but the conditions turned unstable. The development of the paleoceanographic conditions at the western and northern

  9. Norwegian Sea warm pulses during Dansgaard-Oeschger stadials: Zooming in on these anomalies over the 35-41 ka cal BP interval and their impacts on proximal European ice-sheet dynamics

    Science.gov (United States)

    Wary, Mélanie; Eynaud, Frédérique; Rossignol, Linda; Lapuyade, Joanna; Gasparotto, Marie-Camille; Londeix, Laurent; Malaizé, Bruno; Castéra, Marie-Hélène; Charlier, Karine

    2016-11-01

    The last glacial millennial climatic events (i.e. Dansgaard-Oeschger and Heinrich events) constitute outstanding case studies of coupled atmosphere-ocean-cryosphere interactions. Here, we investigate the evolution of sea-surface and subsurface conditions, in terms of temperature, salinity and sea ice cover, at very high-resolution (mean resolution between 55 and 155 years depending on proxies) during the 35-41 ka cal BP interval covering three Dansgaard-Oeschger cycles and including Heinrich event 4, in a new unpublished marine record, i.e. the MD99-2285 core (62.69°N; -3.57s°E). We use a large panel of complementary tools, which notably includes dinocyst-derived sea-ice cover duration quantifications. The high temporal resolution and multiproxy approach of this work allows us to identify the sequence of processes and to assess ocean-cryosphere interactions occurring during these periodic ice-sheet collapse events. Our results evidence a paradoxical hydrological scheme where (i) Greenland interstadials are marked by a homogeneous and cold upper water column, with intensive winter sea ice formation and summer sea ice melting, and (ii) Greenland and Heinrich stadials are characterized by a very warm and low saline surface layer with iceberg calving and reduced sea ice formation, separated by a strong halocline from a less warm and saltier subsurface layer. Our work also suggests that this stadial surface/subsurface warming started before massive iceberg release, in relation with warm Atlantic water advection. These findings thus support the theory that upper ocean warming might have triggered European ice-sheet destabilization. Besides, previous paleoceanographic studies conducted along the Atlantic inflow pathways close to the edge of European ice-sheets suggest that such a feature might have occurred in this whole area. Nonetheless, additional high resolution paleoreconstructions are required to confirm such a regional scheme.

  10. NotCal04 - Comparison / Calibration 14C records 26-50 cal kBP

    Energy Technology Data Exchange (ETDEWEB)

    der Plicht, J v; Beck, J; Bard, E; Baille, M

    2004-11-11

    The radiocarbon calibration curve, IntCal04, extends back to 26 cal kBP. While several high resolution records exist beyond this limit, these data sets exhibit discrepancies one to another of up to several millennia. As a result, no calibration curve for the time range 26-50 cal kBP can be recommended as yet, but in this paper the IntCal04 working group compares the available data sets and offers a discussion of the information that they hold.

  11. 12 kaBP lake environment on the Tibetan Plateau

    Institute of Scientific and Technical Information of China (English)

    李炳元; 王苏民; 朱立平; 李元芳

    2001-01-01

    The systemic analyses have been carried out in this paper to the paleolake shorelines, paleolake sediments and paleoclimatic proxies of 20 lakes, in which there were 12 kaBP dating data on the Tibetan Plateau. The results showed that the paleolake level had apparently risen during 14-11 kaBP, the glaciers melting period, in the Tibetan area and Northwest China. Especially, much more increasing amplitude supplied by thawy glaciers water occurred than in the best period of Holocene. The temperate-humid climate around 12 kaBP appeared in the Tibetan area and even in the whole China. This event may be compared with the Bolling/Allerod warm period which was reflected by Europe and Greenland ice core records. It showed that the B/A event was not a regional one in the North Atlantic area.

  12. 18 Ka BP records of climatic changes, Bay of Bengal: Isotopic and sedimentological evidences

    Digital Repository Service at National Institute of Oceanography (India)

    Chauhan, O.S.; Suneethi, J.

    arid climate between 18 and 15 14C Ka BP, a variable climate between 15 and 13 Ka BP, and again an arid climate at 12.5 Ka BP. The negative d18O, reduced C/I and higher smectite document a humid phase culminating at 12 Ka BP. Arid climate phases...

  13. Lake-expanding events in the Tibetan Plateau since 40 kaBP

    Institute of Scientific and Technical Information of China (English)

    贾玉连; 施雅风; 王苏民; 蒋雪中; 李世杰; 王爱军; 李徐生

    2001-01-01

    Since 40 kaBP, the current endorheism on the Tibetan Plateau had experienced at least four lake-expanding events, at 40-28 kaBP, 19-15 kaBP, 13-11 kaBP, 9.0-5.0 kaBP, respectively. The 40-28 kaBP and 9.0-5.0 kaBP lake-expanding events, corresponding to the global warming periods, were mainly determined by the abundant summer monsoon rainfall brought by strong Indian monsoon, aroused by enhanced solar radiation at earth orbital precessional cycle. The 40-28 kaBP lake-expanding event, also called the great lake period or the pan-lake period, for several great lake groups had come into being by the interconnection of the presently isolated and closed lake catchments. The total lake area over the Tibetan Plateau was estimated at least up to 150000 km2, 3.8 times of the present, and the lake supply coefficients were about 3-10. The 9.0-5.0 kaBP lake-expanding, with a total lake area of 68000 km2, less than the above mentioned reflected the Indian monsoon rainfall less than that of 40-28 kaBP. The expanded lak

  14. The Terrestrial NPP Simulation in China since 6ka BP

    Institute of Scientific and Technical Information of China (English)

    HE Yong; DONG Wenjie; JI Jinjun; DAN Li

    2005-01-01

    A better understanding of the long-term global carbon cycle required estimate of the changes in terrestrial carbon storage after the last glacial period. The results of simulation at mid-Holocene (MH) from PMIP (Paleoclimate Modeling Intercomparison Project) and the modern data from CRU (Climate Research Unit,East Anglia University, UK) allow us to use the Atmosphere-Vegetation Interaction Model (AVIM) to simulate the Chinese terrestrial net primary productivity (NPP) at 6ka BP and present time. The change of NPP and total NPP in China from now to mid-Holocene are about 54 g m-2yr-1 and 0.63 Pg yr-1,respectively, mainly due to the build-up of temperate forest and tropical rainforest. Chinese terrestrial NPP variation from MH to now is closely related to the variation in intensity of Asian monsoon, which controlled the climate-vegetation pattern change.

  15. A multi-proxy warm season temperature reconstruction (3400 cal yr BP - 1500 cal yr BP) from the varved sediments of Lake Silvaplana

    Science.gov (United States)

    Stewart, Monique; Larocque, Isabelle; Grosjean, Martin

    2010-05-01

    A multi-proxy analysis of a nine-meter sediment core from Lake Silvaplana (1791 m a.s.l., 46°24'N, 9°42'E - 46°30'N, 9°52'E), including an innovative application of Spectrolino (380 - 730 nm) data, provides a decadal warm season temperature reconstruction (3400 cal yr BP - 1500 cal yr BP). The climate of this region has been shown to be representative of continental Europe (Trachsel et al., 2009). Consequently, we offer one of the first high-resolution multi-proxy records of European climate for this time period. The sediment of Silvaplana contains annual (‘varved') layers. Therefore, a chronology has been based on varve counts, 210Pb, 137Cs, documented flood layers and radiocarbon dates (Blass et al., 2007a;b). These varves enable high-resolution (sub-decadal) sampling and measurement of geochemical (Spectrolino, Biogenic Silica [BSi], varve thickness) and biological (chironomids) parameters. Spectrolino and BSi Flux measurements of the upper three meters of the core have been used to develop two independent calibrations-in-time and warm season (JJAS) temperature reconstructions back to AD 1177 (Spectrolino calibration period = 1864 - 1949; r = 0.92; pcorr = 0.001; BSi calibration period = 1864 - 1949; r = 0.67; pcorr = 0.03) (Trachsel et al., in review a;b; Blass et al., 2007b). A third warm season (July) temperature reconstruction to AD 1177 has been developed from chironomids (Larocque et al., 2009; Larocque-Tobler et al., 2009; accepted). Finally, Leemann and Niessen (1994), Ohlendorf et al. (1997), Nussbaumer et al. (in prep.) and Blass et al. (2007a) have shown a close relationship between local glacial activity and mean summer temperature. Here, the laboratory methods and calibrations-in-time previously used to reconstruct temperatures to AD 1177 are applied to the lower six meters of sediments (Spectrolino and varve thickness: 3400 cal yr BP - 1500 cal yr BP; BSi and chironomids: 2550 cal yr BP - 1810 cal yr BP). Both the BSi and chironomid based

  16. Evidence and modeling study of droughts in China during 4 - 2 ka BP

    Institute of Scientific and Technical Information of China (English)

    WANG ShaoWu; HUANG JianBin; WEN XinYu; ZHU JinHong

    2008-01-01

    Four periods with predominated droughts are identified in 4-2 ka BP according to documentary data, namely 3.6-3.5, 3.1-3.0, 2.8-2.7, and 2.45-2.35 ka BP. Palaeo-environmental data indicated that droughts were predominated in 4-2 ka BP in the south of Northeast China, Inner-Mongolia, east of Qinghai-Tibetan Plateau, and South China. Modeling study shows that precession may be responsible for the occurrence of droughts in 4-2 ka BP, integrating the GCM with forcing of insolation.

  17. Did Lake Bonneville Experience A Major Water-Budget Shift At 17.4 cal ka?

    Science.gov (United States)

    Oviatt, C.

    2009-12-01

    Lake Bonneville, in western Utah, had transgressed to its highest level by 18.3 cal ka, overflowed into the Snake River drainage basin until 17.4 cal ka, then catastrophically dropped 100 m as its overflow threshold was washed out. This event, which is referred to as the “Bonneville flood,” is well documented geomorphically, stratigraphically, and geochronologically. At the same time the Bonneville flood was occurring, the level of Lake Estancia in central New Mexico dropped over 30 m then returned to its previous high level in an event caused by climate change in that basin. The question is: “did Lake Bonneville experience a correlative climate-induced shift in its water budget (a decrease in the ratio of input to output), even while it continuously overflowed before, during, and after the Bonneville flood?” The answer to this question has a bearing on the global effects of the climate change that is well documented in the Estancia basin. Data from sediment cores from the Bonneville basin are providing a means to address the question. Data include: ostracode faunal changes, total inorganic carbon, stable isotopes, detrital sand, and mineralogy. The challenge is to identify the measurable characteristics of the sediment core that can be used to clearly separate the effects of water-budget change from those caused by the catastrophic (essentially instantaneous) 100-m lowering of Lake Bonneville.

  18. Environmental change in the Limfjord, Denmark (ca 7500-1500 cal yrs BP): A multiproxy study

    DEFF Research Database (Denmark)

    Lewis, J. P.; Ryves, D.B.; Rasmussen, P.

    2013-01-01

    , foraminifera, sedimentary pigments, C and O stable isotopes and plant macrofossils) has been adopted to assess environmental change over the period ca 7500–1500 cal yrs BP at Kilen, a coastal fjord (before AD 1856) situated in the Western Limfjord. A diatom-based salinity transfer function based on a pan...... (and high productivity) between ca 7500–5000 BP, followed by a gradual transition to a shallow benthic system with more oceanic conditions (i.e. higher salinity, lower productivity, slower sedimentary accumulation rate and poorer fossil preservation) after ca 5000 BP and no stratification after ca 4400...

  19. The quantitative reconstruction of the palaeoclimate between 5200 and 4300 cal yr BP in the Tianshui Basin, NW China

    Directory of Open Access Journals (Sweden)

    N. Sun

    2012-03-01

    Full Text Available The quantitative reconstruction of the palaeoclimate is a prerequisite for understanding climate processes at time scales of centuries and millennia. Here, the coexistence approach (CA was applied to reconstruct climatic factors quantitatively based on the fossil charcoal records between 5200 and 4300 cal yr BP in the Tianshui Basin, NW China. The CA analysis showed that the climate of the Tianshui Basin belonged to the northern subtropical zone between 5200 and 4300 cal yr BP. The mean annual temperature (MAT was approximately 13.2 °C, and the mean annual precipitation (MAP was approximately 778 mm between 5200 and 4900 cal yr BP. The MAT was approximately 13.2 °C, and the MAP was approximately 688 mm between 4800 and 4300 cal yr BP. The MAT was approximately 2.2 °C higher than today, and the MAP was approximately 280 mm higher than today from 5200 to 4900 cal yr BP. The MAT was also approximately 2.2 °C higher than today from 4800 to 4300 cal yr BP, while the MAP was approximately 196 mm higher than today. No abrupt cold event occurred between 5200 and 4300 cal yr BP; however, a drought tendency appeared after around 4800 cal yr BP.

  20. Impact of climate variability on terrestrial environment in Western Europe between 45 and 9 kyr cal. BP: vegetation dynamics recorded by the Bergsee Lake (Black Forest, Germany).

    Science.gov (United States)

    Duprat-Oualid, Fanny; Begeot, Carole; Rius, Damien; Millet, Laurent; Magny, Michel

    2016-04-01

    changes at millennial/pluri-millennial scale. The well-known afforestation of the Late-Glacial interstadial and the Holocene (with pine and hazel-dominated forests respectively) are recorded. Our results also reveal a three-phase sequence in the Last-Glacial. The persistence of very cold conditions between 24 and 30 kyr cal. BP favored a drastic steppe grassland. In contrast, trees proportion increased during the two other periods (14.7-24 and 30-45 kyr cal. BP) in correlation with a relative favorable climate. Second, the respons of vegetation to centennial scale climatic events is characterized by the successive rapid establishment of two different landscapes. GS are dominated by steppic taxa (Artemisia, Helianthemum), whereas more or less complete ecological successions Juniperus-Betula-Pinus seem to occur for most GIs when edaphic conditions became more favorable. Therefore, we suggest a global forcing defined by the strong impact of the climate variability on vegetation changes. We also propose the contribution of local characteristics (latitude, topography) which favored flora migration and long distance pollen inputs from refuge areas. Heiri O., Koinig K.A., Spötl C., Barrett S, Brauer A., Drescher-Schneider R., Gaar D., Ivy-Ochs S., Kerschner H., Luetscher M., Moran A., Nicolussi K., Preusser F., Schmidt R., Schoeneich P., Schwörer C., Sprafke T., Terhorst B., Tinner W. -2014- "Palaeoclimate records 60-8 ka in the Austrian and Swiss Alps and their forelands", Quaternary Science Review, 106 : 186-205.

  1. Pollen record and environmental evolution of Caotanhu wetland in Xinjiang since 4550 cal. a BP

    Institute of Scientific and Technical Information of China (English)

    ZHANG Yun; KONG ZhaoChen; NI Jian; YAN Shun; YANG ZhenJing

    2008-01-01

    This paper presents a multi-proxy reconstruction of the climate change in Caotanhu wetland using pollen, phytolith and charcoal records, and the data of loss of ignition (LOI), grain size analysis, and susceptibility. Results reveal that between 4550 and 2500 cal. a BP, a dry climatic condition was not favorable for the accumulation of peat. Since 2500 cal. a BP, the climate became humid and the wetland developed with abundant freshwater aquatic plants, which contributed to peat accumulation. Never-theless, alternate periods of rain and dry climate occurred during that period. Between 2500 and 1810 cal. a BP (550 BC-140 AD), the climate was more humid than at present. A lot of emerged plants, such as Phragmites, Typha and Sparganium, and freshwater green algae grew in the wetland which was sur-rounded by desert-steppe vegetation composed mainly of Chenopodiaceae, Arternisia, Compositae and Thalictrum. However, from 1810 to 1160 cal. a BP (140-790 AD), the water level started to decrease and hydrophyte species reduced greatly, but some Phragmites still grew in the wetland and around it was desert vegetation with high proportion of Chenopodiaceae and Artemisia. Then from 1160 to 650 a BP (790-1300 AD), it entered a period of desert-steppe with abundant mesic and xerophytic plants. And a lot of aquatic plants prevailed in the wetland. Here, what is noticeable is that percentages of arboreal pollen, consisting mainly of Betula and Picea, increased greatly and reached a maximal value of 27.2%, in which, Betula percentages rose to 23.2%. Hence, it is reasonable to conclude that Betula grew in the highland of the wetland, or Picea timberline shifted downward resulting in the increase of percentages of Betula and Picea pollen, which were transported into the wetland by flood or wind. But since 650 cal. a BP, desert vegetation prevailed around the wetland again with dominant Chenopodiaceae and Ar-temisia, and the climate was similar to modern one. Despite some aquatic

  2. The 8200 calBP ‘climate event’ and the process of neolithisation in south-eastern Europe

    Directory of Open Access Journals (Sweden)

    Mihael Budja

    2007-12-01

    Full Text Available Climate anomalies between 8247–8086 calBP are discussed in relation to the process of transition farming and to demographic dynamics and population trajectories in south-eastern Europe.

  3. The WAIS Divide deep ice core WD2014 chronology - Part 2: Annual-layer counting (0-31 ka BP)

    Science.gov (United States)

    Sigl, Michael; Fudge, Tyler J.; Winstrup, Mai; Cole-Dai, Jihong; Ferris, David; McConnell, Joseph R.; Taylor, Ken C.; Welten, Kees C.; Woodruff, Thomas E.; Adolphi, Florian; Bisiaux, Marion; Brook, Edward J.; Buizert, Christo; Caffee, Marc W.; Dunbar, Nelia W.; Edwards, Ross; Geng, Lei; Iverson, Nels; Koffman, Bess; Layman, Lawrence; Maselli, Olivia J.; McGwire, Kenneth; Muscheler, Raimund; Nishiizumi, Kunihiko; Pasteris, Daniel R.; Rhodes, Rachael H.; Sowers, Todd A.

    2016-03-01

    We present the WD2014 chronology for the upper part (0-2850 m; 31.2 ka BP) of the West Antarctic Ice Sheet (WAIS) Divide (WD) ice core. The chronology is based on counting of annual layers observed in the chemical, dust and electrical conductivity records. These layers are caused by seasonal changes in the source, transport, and deposition of aerosols. The measurements were interpreted manually and with the aid of two automated methods. We validated the chronology by comparing to two high-accuracy, absolutely dated chronologies. For the Holocene, the cosmogenic isotope records of 10Be from WAIS Divide and 14C for IntCal13 demonstrated that WD2014 was consistently accurate to better than 0.5 % of the age. For the glacial period, comparisons to the Hulu Cave chronology demonstrated that WD2014 had an accuracy of better than 1 % of the age at three abrupt climate change events between 27 and 31 ka. WD2014 has consistently younger ages than Greenland ice core chronologies during most of the Holocene. For the Younger Dryas-Preboreal transition (11.595 ka; 24 years younger) and the Bølling-Allerød Warming (14.621 ka; 7 years younger), WD2014 ages are within the combined uncertainties of the timescales. Given its high accuracy, WD2014 can become a reference chronology for the Southern Hemisphere, with synchronization to other chronologies feasible using high-quality proxies of volcanism, solar activity, atmospheric mineral dust, and atmospheric methane concentrations.

  4. Morphological and vegetation changes on tidal flats of the Amazon Coast during the last 5000 cal. yr BP

    OpenAIRE

    2013-01-01

    The analysis of morphology, sedimentary facies, palynology, carbon and nitrogen isotopes, C/N ratio and radiocarbon data from tidal flats sediments influenced by the Amazon River indicates that vegetation development during the last 5000 cal. yr BP was controlled by morphological changes associated with marine and fluvial process. The proximal portion of the tidal flat corresponds to abandoned channels surrounded by terrest rial vegetation since 5280–5160 cal. yr BP. Du...

  5. Vegetation and Climate Variations at Taibai, Qinling Mountains in Central China for the Last 3 500 cal BP

    Institute of Scientific and Technical Information of China (English)

    Xiao-Qiang LI; John DODSON; Jie ZHOU; Su-Min WANG; Qian-Li SUN

    2005-01-01

    Pollen records of two swamp sections, located at Taibai Mountain, the highest peak in the Qinling Mountains of central China, show variations of vegetation and climate for the last 3 500 cal BP. The pollen assemblage at the Foyechi and Sanqingchi sections and the surface soil pollen allowed us to reconstruct a high-altitude vegetation history at Taibai Mountain for the first time. The data indicated that there was a cold-dry climate interval between 3 500 and 3 080 cal BP and a relatively warm and wet period compared with the present from 3 080 to 1 860 cal BP. The warmest period in the late Holocene on Taibai Mountain was from 1 430 to 730 cal BP, with an approximate 2℃ increase in mean annual temperature compared with today.There was a relatively cool-dry climate interval from 730 to 310 cal BP. After 310 cal BP, a mountain tundra vegetation developed again and the position of the modern tree line was established.

  6. Reconstruction of climatic and environmental changes in NW Romania during the early part of the last deglaciation (˜15,000-13,600 cal yr BP)

    Science.gov (United States)

    Wohlfarth, Barbara; Hannon, Gina; Feurdean, Angelica; Ghergari, Lucretia; Onac, Bogdan P.; Possnert, Göran

    2001-12-01

    High resolution pollen, plant macrofossil, charcoal, mineral magnetic and sedimentary analyses, combined with AMS 14C measurements, were performed on multiple sediment sequences along a transect through the former crater lake Preluca Ţiganului in northwestern Romania in order to reconstruct the climatic and environmental changes during the early part of the Last Termination. Lake sediments started to accumulate at ˜14,700 cal yr BP. Initially the upland vegetation consisted of an open forest with mainly Betula and Salix and few Pinus sp., but from 14,500 cal yr BP onwards, Pinus mugo, P. sylvestris and Populus and later on also Larix became established around the lake. Between 14,150 and 13,950 cal yr BP, Pinus cembra seems to have replaced P. mugo and P. sylvestris. At ˜13,950 cal yr BP the tree cover increased and Picea appeared for the first time, together with Pinus cembra, P. mugo and Larix. From ˜13,750 cal yr BP onwards, a Picea forest developed around the site. Based on the combined proxy data the following climatic development may be inferred: 14,700-14,500 cal yr BP, cooler and wet/humid; 14,500-14,400 cal yr BP: gradually warmer temperatures, wet/humid with dry summers; 14,400-14,320 cal yr BP: warm and dry; 14,320-14,150 cal yr BP: cooler and wet/humid; 14,150-14,100 cal yr BP: warm and dry; 14,100-13,850 cal yr BP: warmer and wet/humid; 14,700 cal yr could correspond to GS-2a, the time span between 14,700 and 14,320 to GI-1e, the phase between 14,320 and 14,150 cal yr BP to GI-1d and the time frame between 14,150 and 13,600 cal yr BP to the lower part of GI-1c.

  7. 35 ka BP climate simulations in East Asia and probing the mechanisms of climate changes

    Institute of Scientific and Technical Information of China (English)

    YU Ge; ZHENG Yiqun; KE Xiankun

    2005-01-01

    Paleoclimate modeling has become an important tool to detect the future climate of the global warming that is difficult to be validated. The paleoclimate modeling has to be evaluated by regionally geological data in order to determine if it is able to reproduce a reality of climate states. Geological evidence shows that there was a warm-wet interstadial at 35000±3000 a BP in China, which provides an important climate period to be historical analogue for the future climate changes induced by greenhouse gas emissions. Integrated geological records of later phase of the MSI3 from China also provide basements for evaluation of 35 ka BP climate modeling. This paper reports the paleoclimate experiments applied by various forces, and validates the outputs by geological data, consequently improving the boundary conditions in the experiments and making the paleoclimates more approach the reality. The simulations show an increased temperature in the mid-low latitudes and an extended rain-belt northwards in East Asia, while a decreased temperature in high latitudes and a strong exchange of the N-S atmospheric circulation. As there is only ca. 10-15 ka from 35 ka BP to the LGM (21 ka BP) during which climate rapidly changed from a warm-wet interstadial to a typical ice age, this simulation provides scientific basis to recognize the criteria of global warming and trends of natural climate development.

  8. Desert evolution and climatic changes in the Tarim River basin since 12 ka BP

    Institute of Scientific and Technical Information of China (English)

    冯起; 苏志珠; 金会军

    1999-01-01

    Climatic changes in the Tarim River basin since 12 kaBP were divided into four stages based on the analyses of sedimentary phase, the features of some climatic and environmental biomarks in the sedimentary strata and desert evolution. During the Holocene, cool-dry and temperate-dry climates resulted in apparent alluvial-fluvial and weak aeolian activities. During 10—8 kaBP, the climate was dry and cold, large-scale sand dunes activities led to regional desert expansion. During the hypsithermal (8—3 kaBP), the climate was dry and warm, shifting sand areas decreased and a lot of sand dunes were fixed along the banks of the Tarim River and its tributaries, lowlands and lakes. As a result, fluvial-alluvial areas increased. Since 3 kaBP, the aeolian activity and sandstorms have been enhancing due to the combined influences of climatic warming and illogical exploitation of land and water resources. The climate in the Tarim River basin have been persistently dry and alternated by warm and cold periods. Conse

  9. The 3000-4000 cal. BP anthropogenic shift in fire regime in the French Pyrenees.

    Science.gov (United States)

    Rius, D.; Vannière, B.; Galop, D.; Richard, H.

    2009-04-01

    Fire is a key disturbing agent in a wide range of ecosystems: boreal biome (Pitkanen, 2000), Mediterranean area (Colombaroli et al., 2008) as well as temperate European mountain zones (Tinner et al., 1999). During the Holocene, climate may control fire regime by both ignition and fire spread-favouring conditions (i.e. composition, structure and moisture of biomass) whereas man may change charcoal accumulation patterns through type and intensity of agro-pastoral activities. In western and Mediterranean Europe, single sites charcoal analysis recorded the anthropogenic forcing over fire regime broadly between the mid and the late-Holocene. Turner et al (2008) showed that climate and fire had been disconnected since 1700 cal. BP in Turkey. In central Swiss, Mean Fire Interval decreased by two times 2000 years ago due to increasing human impact (Stahli et al., 2006). In Italy, climate and man have had a combined influence on fire-hazard since ca 4000 cal. BP (Vannière et al., 2008). In the Pyrenees Mountains, the linkage between agro-pastoral practices and fire could be dated back to ca 4000-3000 cal. BP with a clear succession of a clearance phase (high fire frequency) followed by a quite linear trend throughout Middle Ages and Modern times corresponding to a change in fire use (Vanniere et al., 2001; Galop et al., 2002, Rius et al., in press). The quantification of fire regimes parameters such as frequency with robust methodological tools (Inferred Fire Frequency, Mean Fire Interval) is needed to understand and characterise such shifts. Here we present two sequences from the Lourdes basin (col d'Ech peat bog) and from the occidental Pyrenees (Gabarn peat bog), which cover the last 9000 years with high temporal resolution. The main goals of this study were to (1) assess control factors of fire regime throughout the lateglacial and Holocene (climate and/or man) on the local scale, (2) evidence the local/regional significance of these control factors , (3) discuss the

  10. Vesetation and climate changes during the last 8660 cal. a BP in central Mongolia, based on a high-resolution pollen record from Lake Ugii Nuur

    Institute of Scientific and Technical Information of China (English)

    WANG Wei; MA YuZhen; FENG ZhaoDong; MENG HongWei; SANG YanLi; ZHAI XinWei

    2009-01-01

    Based on modern pollen studies and reliable chronology of nine AMS 14C dates, a detailed history of vegetation and climate changes during the past 8660 cal. a BP was reconstructed by a high-resolution pollen record from Ugii Nuur in central Mongolia. Poaceae-steppe dominated the study area and the climate was mild and semi-humid before 7800 cal. a BP with a noticeable cool and humid interval at 8350-8250 cal. a BP. Xerophytic plant increased and the climate became warm and dry gradually since 7800 cal. a BP. From 6860 to 3170 cal. a BP, semi-desert steppe expanded, suggesting a prolonged warm and dry climate. Between 3170 and 2340 cal. a BP, regional forest steppe expanded whereas semi-desert steppe retreated, indicating the climate became cool and wet gradually and the humidity reached the maximum at the end of this stage. From 2340 to 1600 cal. a BP, a general cool and wet climate prevailed. And the climatic instability increased after 1600 cal. a BP. Review of regional pub-lished palaeoclimaUc records implies that the mid-Holocene dry climate might have prevailed in vast areas from central Mongolia to arid areas of northwest China. Pollen-based climate reconstruction for UG04 core was well correlated with the result of climate model on Central Asia by Bush. In addition, several abrupt climatic events (cool and wet) were found and some could be broadly compared with the cool events in Atlantic.

  11. Grain-size cycles in Salawusu River valley since 150 ka BP

    Institute of Scientific and Technical Information of China (English)

    2001-01-01

    The palaeo-mobile dune sands and fluvio-lacustrine facies with palaeosols in Milanggouwan stratigraphic section of the Salawusu River valley situated at the southeast of the Mu Us Desert experienced abundant remarkable alternative changes of coarse and fine rhythms in grainsize since 150 ka BP, and the grain-size parameters - Mz, σ, Sk, Kg and SC/I also respond to the situation of multi-fluctuational alternations between peak and valley values. Simultaneity the grainsize eigenvalues - Ф5, Ф16, P25, Ф50, Ф75, Ф84 and Ф95 are respondingly manifested as greatly cadent jumpiness. Hereby, the Milanggouwan section can be divided into 27 grain-size coarse and fine sedimentary cycles, which can be regarded as a real and integreted record of climate-geological process of desert vicissitude resulted from the alternative evolvement of the ancient winter and summer monsoons of East Asia since 150 ka BP.

  12. Sedimentary Evidence for a Rapid Sea Level Rise at 7,600 cal yr BP from North-Central Cuba

    Science.gov (United States)

    Peros, M. C.; Agosta G'meiner, A. M.; Collins, S.

    2016-12-01

    A lack of high-resolution relative sea level (RSL) proxy data has meant that the pattern of early Holocene RSL change in the Caribbean is poorly understood. A RSL curve published by Toscano and Macintyre (2003) using inter-tidal mangrove peats and submerged corals suggests RSL underwent a relatively fast and `smooth' curvilinear increase during the Holocene. However, others, such as Blanchon and Shaw (1995), suggest that RSL increased rapidly at around 7600 cal yr BP, in response to the final stages of the melting of the Laurentide Ice Sheet (melt water pulse 1C or catastrophic rise event 3). We investigated this question using multi-proxy data from a flooded sinkhole (Cenote Jennifer) on the north coast of central Cuba. Cenote Jennifer is located 7 m above mean sea level and 2 km from the Bahamas Channel and appears to have a high degree of connectivity with the ocean through a network of underground caverns. The water depth is 13 m and the bottommost 5 m is anoxic. A sediment core collected from Cenote Jennifer was studied using loss-on-ignition, pollen analysis, high-resolution XRF core-scanning, and grain size analysis. An age-depth model was generated for the core by AMS dating. The results show that the bottommost stratigraphic unit ( 9000 to 7600 cal yr BP) is a fine-grained carbonate-rich mud (i.e., marl). This unit abruptly transitions into finely laminated organic-rich sediment from 7600 cal yr BP to the present. The pollen analysis shows that the sinkhole supported a cattail (Typha) community until 7600 cal yr BP, indicating low water levels ( 1 m). At 7600 cal yr BP, the cattail community disappeared and the vegetation of the surrounding bedrock became dominated by a thorny coastal scrubland. In addition, a 3 cm thick fining-upward siliciclastic unit is present immediately above the marl-organic contact, suggesting: 1) a marine sediment source given the limestone-dominated nature of the region, and 2) the presence of a short-duration, high

  13. Robust date for the Bronze Age Avellino eruption (Somma-Vesuvius): 3945 ± 10 calBP (1995 ± 10 calBC)

    Science.gov (United States)

    Sevink, Jan; van Bergen, Manfred J.; van der Plicht, Johannes; Feiken, Hendrik; Anastasia, Carmela; Huizinga, Annika

    2011-05-01

    We found Bronze Age lake sediments from the Agro Pontino graben (Central Italy) to contain a thin (2-3 cm) continuous tephra layer composed of lithics, crystals and minor volcanic glass. Tephrochronological and compositional constraints strongly suggest that this layer represents the Avellino pumice eruption, which has also been identified in Central Italian lake cores. Its provenance is corroborated by electron-microprobe analyses performed on juvenile pumice grains, showing that the tephra layer is probably the distal equivalent of the EU2 event of the Avellino eruption. We used multiple 14C age estimations of two lacustrine sequences with intercalated tephra layer, from the western border zone (Migliara 44.5) and the centre of the former lake (Campo Inferiore), for in tandem dating of this eruption, employing the OxCal code, which yielded a robust age of 3945 ± 10 calBP (1995 ± 10 calBC). To date, this is the only study providing both a terminus post and terminus ante quem of this precision, also demonstrating the advantage of dating distal tephra layers in a clear stratigraphic context over proximal deposits in sequences with major stratigraphic hiatuses. Our new results underscore the importance of the Avellino tephra layer as a precise time marker for studies on the Early Bronze Age of Central Italy.

  14. Dietary shift after 3600 cal yr BP and its influencing factors in northwestern China: Evidence from stable isotopes

    Science.gov (United States)

    Ma, Minmin; Dong, Guanghui; Jia, Xin; Wang, Hui; Cui, Yifu; Chen, Fahu

    2016-08-01

    Human diets rely on natural resource availability and can reflect social and cultural values. When environments, societies, and cultures change, diets may also shift. This study traced the extent of dietary change and the factors influencing such change. Through stable carbon and nitrogen isotopic analysis of late Neolithic and early Bronze Age human and animal bone collagen, we found that significant shifts in human diets were closely associated with intercontinental cultural exchanges in Eurasia and climate change in northwestern China. The isotopic evidence indicated that human diets mainly consisted of C4 foodstuffs (presumably millet and/or animals fed with C4 foods) around 4000 calibrated years before the present (cal yr BP), corresponding to the flourishing of millet agriculture in the context of the optimal climate conditions of the mid-Holocene. Subsequently, more C3 foods (probably wheat, barley, and animals fed with C3 foods) were added to human diets post-3600 cal yr BP when the climate became cooler and drier. Such dietary variation is also consistent with the increasing intensity of long-distance exchange after 4000 cal yr BP. While many factors can lead to human dietary shifts (e.g. climate change, population growth, cultural factors, and human migration), climate may have been a key factor in Gansu and Qinghai.

  15. Dietary shift after 3600 cal yr BP and its influencing factors in northwestern China: Evidence from stable isotopes

    Science.gov (United States)

    Ma, Minmin; Dong, Guanghui; Jia, Xin; Wang, Hui; Cui, Yifu; Chen, Fahu

    2017-04-01

    :Human diets rely on natural resource availability and can reflect social and cultural values. When environments, societies, and cultures change, diets may also shift. This study traced the extent of dietary change and the factors influencing such change. Through stable carbon and nitrogen isotopic analysis of late Neolithic and early Bronze Age human and animal bone collagen, we found that significant shifts in human diets were closely associated with intercontinental cultural exchanges in Eurasia and climate change in northwestern China. The isotopic evidence indicated that human diets mainly consisted of C4 foodstuffs (presumably millet and/or animals fed with C4 foods) around 4000 calibrated years before the present (cal yr BP), corresponding to the flourishing of millet agriculture in the context of the optimal climate conditions of the mid-Holocene. Subsequently, more C3 foods (probably wheat, barley, and animals fed with C3 foods) were added to human diets post-3600 cal yr BP when the climate became cooler and drier. Such dietary variation is also consistent with the increasing intensity of long-distance exchange after 4000 cal yr BP. While many factors can lead to human dietary shifts (e.g. climate change, population growth, cultural factors, and human migration), climate may have been a key factor in Gansu and Qinghai.

  16. A high-resolution temporal record of environmental changes in the Eastern Caribbean (Guadeloupe) from 40 to 10 ka BP

    Science.gov (United States)

    Royer, Aurélien; Malaizé, Bruno; Lécuyer, Christophe; Queffelec, Alain; Charlier, Karine; Caley, Thibaut; Lenoble, Arnaud

    2017-01-01

    In neotropical regions, fossil bat guano accumulated over time as laminated layers in caves, hence providing a high-resolution temporal record of terrestrial environmental changes. Additionally, cave settings have the property to preserve such organic sediments from processes triggered by winds (deflation, abrasion and sandblasting) and intense rainfall (leaching away). This study reports both stable carbon and nitrogen isotope compositions of frugivorous bat guano deposited in a well-preserved stratigraphic succession of Blanchard Cave on Marie-Galante, Guadeloupe. These isotopic data are discussed with regard to climate changes and its specific impact on Eastern Caribbean vegetation during the Late Pleistocene from 40 to 10 ka cal. BP. Guano δ13C values are higher than modern ones, suggesting noticeable vegetation changes. This provides also evidence for overall drier environmental conditions during the Pleistocene compared to today. Meanwhile, within this generally drier climate, shifts between wetter and drier conditions can be observed. Large temporal amplitudes in both δ13C and δ15N variations reaching up to 5.9‰ and 16.8‰, respectively, also indicate these oceanic tropical environments have been highly sensitive to regional or global climatic forcing. Stable isotope compositions of bat guano deposited from 40 to 35 ka BP, the Last Glacial Maximum and the Younger-Dryas reveal relatively wet environmental conditions whereas, at least from the end of the Heinrich event 1 and the Bølling period the region experienced drier environmental conditions. Nevertheless, when considering uncertainties in the model age, the isotopic record of Blanchard Cave show relatively similar variations with known proxy records from the northern South America and Central America, suggesting thus that the Blanchard Cave record is a robust proxy of past ITCZ migration. Teleconnections through global atmospheric pattern suggest that islands of the eastern Caribbean Basin could

  17. Sedimentary cycles of trace elements in Salawusu River Valley since 150 ka BP

    Institute of Scientific and Technical Information of China (English)

    2002-01-01

    The paper makes some analyses on 11 trace elements in the Milanggouwan stratigraphical section in the Salawusu River valley, which is regarded as a prototype geology-palaeoclimate record since 150 ka BP. The results show that the content and variation of trace elements has experienced remarkably regular changes in the pace with coarse and fine sedimentary cycles of palaeo-aeolian sands to its overlying fluvio-lacustrine facies or/and palaeosols. The trace elements with chemical properties of relatively active (V, Sr, Cu, Ni, As) and relatively stable (P, Pb, Rb, Mn, Nb, Zr) are a manifestation of the corresponding 27 changeable cycles between peak and valley values, appearing a multi-fluctuational process line of relative gathering and migration since then. The low numerical value distribution of these two types of trace elements in the aeolian sand facies represents erosion and accumulation under wind force during the cold-dry climate. Whereas their enrichments in both fluvio-lacustrine facies and palaeosols are related to the valley's special low-lying physiognomic position between the Ordos Plateau and the Loess Plateau under the warm and humid climate conditions. The above relatively migrated and gathered change of the trace elements is the result of 27 climatic cycles of cold-dry and warm-humid, which is probably caused by repeated alternations of winter monsoon and summer monsoon in the Mu Us Sandy Land influenced by the climate vicissitudes in northern hemisphere during glacial and interglacial periods since 150 ka BP.

  18. Desert-steppe migration on the Loess Plateau at about 450 kaBP

    Institute of Scientific and Technical Information of China (English)

    ZHAOJingbo

    2005-01-01

    According to the field investigation, observation by an electronic microscope and x-ray identification and chemical analysis, desert-steppe migration in the Loess Plateau at about 450 kaBP was studied. The data show that gypsum illuvial horizon indicating the desert-steppe environment developed in the early stage of the formation of the fifth layer loess in Shaoling tableland in Chang'an and Bailu tableland in Xran of Shaanxi are situated in the southern Loess Plateau. This indicates that remarkable drying occurred, a large-scope migration of desert steppe took place toward south and the climate zone migrated 5 degrees in latitude to south which is the largest migration range indicated by geochemical indexes. The desert-steppe and more wild environment distributed widely on the Loess Plateau at that time. The development of gypsum also indicates that the climate changed at 450 kaBP from monsoon climate to nonmonsoon climate in the Loess Plateau, and the region was not affected by summer monsoon and was in the cold and dry environment of nonmonsoon climate. Annual mean nrecinitation was about 200 rnm. 400 mm less at that time than at oresent.

  19. Sedimentary Characteristics and Paleoenvironmental Records of Zabuye Salt Lake, Tibetan Plateau, since 128 ka BP

    Institute of Scientific and Technical Information of China (English)

    2007-01-01

    This paper for the first time reveals high-resolution core records of Zabuye Salt Lake in the interior of the Qinghai-Tibet Plateau. According to 1346 samples taken continuously, relatively accurate 14C, U-series disequilibrium and ESR ages have been obtained, thus revealing that the lake core ages from 0 to 83.63 m of hole SZK02 are ~800 to over 128 ka. In the paper, the lake core sedimentary characteristics (including the lithologies and mineral assemblages) are analyzed in detail and correlated with ostracod assemblages Ⅰ to ⅩⅩ and sporopollen zones A to I, and on the basis of an integrated analysis of the δ18O values of authigenic calcium-magnesium carbonate and environmental proxies of minerals, sporopollen and microfossils in the lake core, a correlation has been made of oxygen isotope change between this lake core and the Greenland GISP2 and GRIP and Guliya ice cores, and the climate of Zabuye Salt Lake since 128 ka BP is divided into the last interglacial stage (including substages e, d, c, b and a) of oxygen isotope stage (OIS) 5, early glacial stadial of the last glacial stage of OIS 4, interglacial stadial of the last glacial stage of OIS 3, late glacial stadial of the last glacial stage or Last Glacial Maximum of OIS 2 and postglacial state of OIS 1; in addition, 6 Heinrich (H6-H1) events, Younger Dryas event and 8.2 ka BP cold event have been recognized.

  20. Abrupt Climate Change around 4 ka BP:Role of the Thermohaline Circulation as Indicated by a GCM Experiment

    Institute of Scientific and Technical Information of China (English)

    王绍武; 周天军; 蔡静宁; 朱锦红; 谢志辉; 龚道溢

    2004-01-01

    A great deal of palaeoenvironmental and palaeoclimatic evidence suggests that a predominant temperature drop and an aridification occurred at ca. 4.0 ka BP. Palaeoclimate studies in China support this dedution. The collapse of ancient civilizations at ca. 4.0 ka BP in the Nile Valley and Mesopotamia has been attributed to climate-induced aridification. A widespread alternation of the ancient cultures was also found in China at ca. 4.0 ka BP in concert with the collapse of the civilizations in the Old World. Palaeoclimatic studies indicate that the abrupt climate change at 4.0 ka BP is one of the realizations of the cold phase in millennial scale climate oscillations, which may be related to the modulation of the Thermohaline Circulation (THC) over the Atlantic Ocean. Therefore, this study conducts a numerical experiment of a GCM with SST forcing to simulate the impact of the weakening of the THC. Results show a drop in temperature from North Europe, the northern middle East Asia, and northern East Asia and a significant reduction of precipitation in East Africa, the Middle East, the Indian Peninsula, and the Yellow River Valley. This seems to support the idea that coldness and aridification at ca. 4.0 ka BP was caused by the weakening of the THC.

  1. 5 ka BP event in monsoonal China%我国季风区5 ka BP气候事件

    Institute of Scientific and Technical Information of China (English)

    李东; 谭亮成; 安芷生

    2016-01-01

    Background, aim, and scope A lot of studies suggested the Holocene climate change had played an important role in the evolution of the Neolithic cultures around the world. During the Holocene, there were a series of abrupt climate changes. One of the abrupt events occurred around~5 ka BP, which signiifcantly changed the environment of many regions over the world. Because this event occurred before the dawn of civilization, it had caused important inlfuences on human society. In this paper, we reviewed the recently published high-resolution, absolutely-dated speleothem and limnological records from different regions of monsoonal China, which had recorded hydrological changes during the 5 ka BP event period. We further discussed its impacts on the Neolithic culture of China, as well as the driving mechanisms.Materials and methods We divided the monsoonal China into Northeast China, North China, Central China, East China, South China, Southwest China and the Tibetan Plateau. We compared the hydrological changes in different regions of monsoonal China, by using recent published high-resolution, absoluted dated records.Results We suggested the monsoonal China, from the north to the south, had experienced dry climate during this event. The dry event was most signiifcantly recorded in North China, Northeast China and Tibetan Plateau. It began at 5.6—5.5 ka BP, reaching to the driest at ~5.0 ka BP, and then the precipitation rapidly recovered. Stalagmite record from Central China also showed similar result with North China. There was also cold and dry climate in Southwest China during the period of 5.5—4.8 ka BP. In South China, notably dry climate was observed in 5.5—5.0 ka BP. It seems there was imprint of 5 ka BP event in East China, although it’s hard to determine the exact timing, because of low resolutions and poor age controls of the published records. The extreme dry climate had played an important role on the evolution of Chinese Neolithic culture. The

  2. Quantification of southwest China rainfall during the 8.2 ka BP event with response to North Atlantic cooling

    Science.gov (United States)

    Liu, Yuhui; Hu, Chaoyong

    2016-07-01

    The 8.2 ka BP event could provide important information for predicting abrupt climate change in the future. Although published records show that the East Asian monsoon area responded to the 8.2 ka BP event, there is no high-resolution quantitative reconstructed climate record in this area. In this study, a reconstructed 10-year moving average annual rainfall record in southwest China during the 8.2 ka BP event is presented by comparing two high-resolution stalagmite δ18O records from Dongge cave and Heshang cave. This decade-scale rainfall reconstruction is based on a central-scale model and is confirmed by inter-annual monitoring records, which show a significant positive correlation between the regional mean annual rainfall and the drip water annual average δ18O difference from two caves along the same monsoon moisture transport pathway from May 2011 to April 2014. Similar trends between the reconstructed rainfall and the stalagmite Mg / Ca record, another proxy of rainfall, during the 8.2 ka BP period further increase the confidence of the quantification of the rainfall record. The reconstructed record shows that the mean annual rainfall in southwest China during the central 8.2 ka BP event is less than that of present (1950-1990) by ˜ 200 mm and decreased by ˜ 350 mm in ˜ 70 years experiencing an extreme drying period lasting for ˜ 50 years. Comparison of the reconstructed rainfall record in southwest China with Greenland ice core δ18O and δ15N records suggests that the reduced rainfall in southwest China during the 8.2 ka BP period was coupled with Greenland cooling with a possible response rate of 110 ± 30 mm °C-1.

  3. Using data assimilation to investigate the causes of Southern Hemisphere high latitude cooling from 10 to 8 ka BP

    NARCIS (Netherlands)

    P. Mathiot; H. Goosse; X. Crosta; B. Stenni; M. Braida; A. Mairesse; S. Dubinkina (Svetlana)

    2013-01-01

    htmlabstractFrom 10 to 8 ka BP (thousand years before present), paleoclimate records show an atmospheric and oceanic cooling in the high latitudes of the Southern Hemisphere. During this interval, temperatures estimated from proxy data decrease by 0.8 °C over Antarctica and 1.2 °C over the Southern

  4. Study of the varve record from Erlongwan maar lake,NE China, over the last 13 ka BP

    Institute of Scientific and Technical Information of China (English)

    2008-01-01

    In a sediment sequence from Erlongwan maar lake that spans the last 13 ka BP, two main varve types can be recognized: biogenic varves (from the present to ~11.2 ka BP, 0-632 cm) and clastic varves (from ~11.2 to ~12.7 ka BP, 632-700 cm). Based on the dominant types of algae contained in the sediment, the biogenic varves can be classified into dinocyst-biogenic varves (0-63 cm) and mixed (dinocyst and diatom)-biogenic varves (214-632 cm). In this paper, the formation process and components of the varve are described, the possible reason for the types of varve changing throughout the record is discussed and a high-resolution varve chronology is established spanning the last 13 ka BP.Although further varve counting and error assessment are needed, the results presented here represent a solid foundation for studying the palaeoclimate record of Erlongwan maar lake.

  5. Pollen-recorded climate changes between 13.0 and 7.0 14C ka BP in southern Ningxia, China

    Institute of Scientific and Technical Information of China (English)

    SUN AiZhi; MA YuZhen; FENG ZhaoDong; LI Fei; WU HuiNing

    2007-01-01

    A pollen record from Haiyuan section in the southern part of Ningxia revealed a detailed history of vegetation variation and associated climate changes during the period from ~13.0 to ~7.0 14C ka BP. A steppe landscape under a moderately dry (and probably cool) condition (~12.7-~12.1 14C ka BP) was replaced by a coniferous forest dominating the landscape under a generally wet climate from ~12.1 to ~11.0 14C ka BP. This generally wet period, corresponding to the European B(o)lling/All(e)rod period, can be divided into three stages: a cool and wet stage between ~12.1 and ~11.4 14C ka BP, a mild and relatively dry stage between ~11.4 and ~11.2 14C ka BP, and a mild and wet stage between ~11.2 and ~11.0 14C ka BP. The coniferous forest-dominated landscape was then deteriorated into steppe landscape (~11.0-~10.6 14C ka BP) and further into a desert steppe landscape from ~10.6 to ~9.8 14C ka BP, being correspondent to the European Younger Dryas period. After a brief episode of a cool and wet climate (~9.8-~9.6 14C ka BP), a relatively mild and dry condition prevailed during the early Holocene (~9.6-~7.6 14C ka BP) and then a warm and humid climate started the mid-Holocene (~7.6-~7.2 14C ka BP).

  6. Advection of Atlantic Water to the western and northern Svalbard shelf since 17,500 cal yr BP

    Science.gov (United States)

    Ślubowska-Woldengen, Marta; Rasmussen, Tine L.; Koç, Nalân; Klitgaard-Kristensen, Dorthe; Nilsen, Frank; Solheim, Anders

    2007-02-01

    The changes in flow and character of the warm Atlantic Water through the last 17,500 cal yr are reconstructed from the distribution of benthic foraminifera species, planktonic and benthic foraminifera abundances, stable oxygen isotopes and lithology in two cores from the western and northern shelf of Svalbard. The results show almost continuous presence of Atlantic Water at the shelf areas since >14,500 cal yr BP. The Bølling and Allerød intervals stand out as periods of highest bottom waters temperatures. The strong inflow of saline, but chilled Atlantic Water during the early Holocene was followed by cooling and freshening of the bottom waters during the mid- and late Holocene. The two records reveal synchronous oceanographic changes that are closely tied to changes in the flow of Atlantic Water recorded further south in the Nordic seas. The early Holocene warming was not just an effect of higher solar insolation, but was also due to increased heat flux from the stronger Atlantic Water inflow driven by wind force and/or thermohaline circulation.

  7. The paleoclimatic events and cause in the Okinawa Trough during 50 kaBP

    Institute of Scientific and Technical Information of China (English)

    2001-01-01

    Planktonic foraminiferal d18O record for core DGKS9603 from the Okinawa Trough shows a series of climatic fluctuations and sudden cooling events in short time scale during 50 kaBP, which appear to correlate closely to the Younger Dryas and Heinrich events H1-5 recorded in Chine-se loess, the South China Sea, the North Atlantic cores and the Greenland ice cores. Three polarity reversal events, cor-relating to Gothenburg, Mungo and Laschamp events, ap-proximately correspond to Heinrich events H1, H3 and H5 respectively, which could be a cause of global climate changes. The d18O curve of the Okinawa Trough is well asso-ciated with the grain size record of the Lijiayuan loess profile in northwestern China and is somewhat different from the climate fluctuations documented in the Greenland ice cores. These correlation results indicate that regional factors play an important role in controlling the climate changes in the East Asia, and the East Asian Monsoon could be the promi-nent regional controlling factor.

  8. AN AGCM +SSiB MODEL SIMULATION ON CHANGES IN PALAEOMONSOON CLIMATE AT 21 KA BP IN CHINA

    Institute of Scientific and Technical Information of China (English)

    陈星; 于革; 刘健

    2001-01-01

    The numerical simulation experiment of climate at Last Glacial Maximum (LGM, 21 ka BP)in China is made by using an atmospheric general circulation model (AGCM) coupled with land surface processes (AGCM+SSiB) and earth orbital parameters and boundary forcing conditions at 21 ka. The modeled climate features are compared with reconstructed conditions at 21 ka from palco-lake data and pollen data. The results show that the simulated climate conditions at 21 ka in China are fairly comparable with palco-climatological data. The climate features at 21 ka in China from the experiment are characterized by a drier in the east and a wetter in the west and in the Tibetan Plateau as well. According to the analysis of distribution of pressure and precipitation, as well as the intensity of atmospheric circulation at 21 ka, monsoon circulation in eastern Asia was significantly weak comparing with the present. In the Tibetan Plateau, the intensity of summer monsoon circulation was strengthened, and winter monsoon was a little stronger than the present.The simulation with given forcing boundary conditions, especially the different vegetation coverage, can reproduce the climate condition at the LGM in China, and therefore provides dynamical mechanisms on the climate changes at 21 ka.

  9. Are Avellino (4365 cal BP) and Pompeii twin plinian eruptions? Pre-eruptive constraints and degassing history

    Science.gov (United States)

    Boudon, Georges; Balcone-Boissard, Hélène; Villemant, Benoît.; Ucciani, Guillaume; Cioni, Raffaello

    2010-05-01

    Somma-Vesuvius activity started 35 ky ago and is characterized by numerous eruptions of variable composition and eruptive style, sometimes interrupted by long periods of unrest. The main explosive eruptions are represented by four plinian eruptions: Pomici di Base eruption (22 cal ky), Mercato (~8900 cal BP), Avellino (4365 cal BP) and Pompeii (79 AD). The 79 AD eruption embodies the most famous eruption since it's responsible of the destruction of Pompeii and Herculanum and it's the first described eruption. The Avellino eruption represents the last plinian event that preceded the Pompeii eruption. The eruptive sequence is similar to the 79 AD plinian eruption, with an opening phase preceding a main plinian fallout activity which ended by a phreatomagmatic phase. The fallout deposit displays a sharp colour contrast from white to grey pumice, corresponding to a magma composition evolution. We focus our study on the main fallout deposit that we sampled in detail in the Traianello quarry, 9 km North-North East of the crater, to investigate the degassing processes during the eruption, using volatile content and textural observations. Density and vesicularity measurements were obtained on a minimum of 100 pumice clasts sampled in 10 stratigraphic levels in the fallout deposit. On the basis of the density distribution, bulk geochemical data, point analytical measurements on glasses (melt inclusions and residual glass) and textural observations were obtained simultaneously on a minimum of 5 pumice clasts per eruptive unit. The glass composition, in particular the Na/K ratio, evolves from Na-rich phonolite for white pumices to a more K-rich phonolite for grey pumices. The pre-eruptive conditions are constrained by systematic Cl measurements in melt inclusions and matrix glass of pumice clasts. The entire magma was saturated relative to sub-critical fluids (a Cl-rich H2O vapour phase and a brine), with a Cl melt content buffered at ~6000 ppm, and a mean pre-eruptive H2O

  10. Direct linking of Greenland and Antarctic ice cores at the Toba eruption (74 ka BP

    Directory of Open Access Journals (Sweden)

    A. Svensson

    2013-03-01

    Full Text Available The Toba eruption that occurred some 74 ka ago in Sumatra, Indonesia, is among the largest volcanic events on Earth over the last 2 million years. Tephra from this eruption has been spread over vast areas in Asia, where it constitutes a major time marker close to the Marine Isotope Stage 4/5 boundary. As yet, no tephra associated with Toba has been identified in Greenland or Antarctic ice cores. Based on new accurate dating of Toba tephra and on accurately dated European stalagmites, the Toba event is known to occur between the onsets of Greenland interstadials (GI 19 and 20. Furthermore, the existing linking of Greenland and Antarctic ice cores by gas records and by the bipolar seesaw hypothesis suggests that the Antarctic counterpart is situated between Antarctic Isotope Maxima (AIM 19 and 20. In this work we suggest a direct synchronization of Greenland (NGRIP and Antarctic (EDML ice cores at the Toba eruption based on matching of a pattern of bipolar volcanic spikes. Annual layer counting between volcanic spikes in both cores allows for a unique match. We first demonstrate this bipolar matching technique at the already synchronized Laschamp geomagnetic excursion (41 ka BP before we apply it to the suggested Toba interval. The Toba synchronization pattern covers some 2000 yr in GI-20 and AIM-19/20 and includes nine acidity peaks that are recognized in both ice cores. The suggested bipolar Toba synchronization has decadal precision. It thus allows a determination of the exact phasing of inter-hemispheric climate in a time interval of poorly constrained ice core records, and it allows for a discussion of the climatic impact of the Toba eruption in a global perspective. The bipolar linking gives no support for a long-term global cooling caused by the Toba eruption as Antarctica experiences a major warming shortly after the event. Furthermore, our bipolar match provides a way to place palaeo-environmental records other than ice cores into a

  11. Direct linking of Greenland and Antarctic ice cores at the Toba eruption (74 ka BP)

    Science.gov (United States)

    Svensson, A.; Bigler, M.; Fischer, H.; Johnsen, S. J.; Kipfstuhl, S.; Parrenin, F.; Rasmussen, S. O.; Steffensen, J. P.; Vinther, B. M.; Wegner, A.

    2012-04-01

    The Toba eruption that occurred some 74 ka ago in Sumatra, Indonesia, is among the largest volcanic events on Earth over the last 2 million years. Tephra from this eruption has been spread over vast areas in Asia where it constitutes a major reference horizon close to the Marine Isotope Stage 3/4 (MIS 3/4) boundary. Up to now, no tephra has been associated with Toba neither in Greenland nor in Antarctic ice cores, but based on Toba tephra identified in marine records from the Arabian Sea it is very likely that Greenland ice core acidity spikes related to Toba occur towards the end of Greenland Interstadial 20 (GI-20). Furthermore, the linking of Greenland and Antarctic ice cores by gas records suggests that the Antarctica counterpart should be situated between Antarctic Isotope Maxima (AIM) 19 and 20. In this work we suggest a direct synchronization of Greenland (NGRIP) and Antarctic (EDML) ice cores based on matching of a pattern of bi-polar volcanic spikes and annual layer counting in both cores around 74 ka BP. The synchronization pattern covers some 2000 years in GI-20 and AIM 19/20 and includes 5 major and several minor acidity peaks that are recognized in both ice cores. The most prominent acidity spikes in this time interval that occur towards the end of GI-20, are those thought to originate from Toba, but the proposed linking is independent of the source of the volcanic spikes. Although the linking of Greenland and Antarctic ice cores around Toba is already quite well constrained by matching of gas records, the relative phasing between ice cores from the two hemispheres still has some uncertainty related to the offset in the age of ice and air bubbles in the ice cores (delta-gas age). The identification of a direct Toba synchronization may help to determine the exact phasing of inter-hemispheric climate during this period and to constrain delta-gas ages. It also provides a way to place paleo-environmental records other than ice cores into a precise climatic

  12. Using data assimilation to investigate the causes of Southern Hemisphere high latitude cooling from 10 to 8 ka BP

    Directory of Open Access Journals (Sweden)

    P. Mathiot

    2012-11-01

    Full Text Available Paleoclimate records show an atmospheric and oceanic cooling in the high latitudes of the Southern Hemisphere from 10 to 8 ka BP. In order to study the causes of this cooling, simulations covering the early Holocene period have been performed with the climate model of intermediate complexity LOVECLIM constrained to follow the signal recorded in climate proxies using a data assimilation method based on a particle filtering. The selected proxies represent oceanic and atmospheric surface temperature in the Southern Hemisphere derived from terrestrial, marine and glaciological records. Using our modeling framework, two mechanisms potentially explaining the 10–8 ka BP cooling pattern are investigated. The first hypothesis is a change in atmospheric circulation. The state obtained by data assimilation displays a modification of the meridional atmospheric circulation around Antarctica, producing a 0.6 °C drop in atmospheric temperatures over Antarctica from 10 to 8 ka BP without congruent cooling of the atmospheric and sea-surface temperature in the Southern Ocean. The second hypothesis is a cooling of the sea surface temperature in the Southern Ocean, simulated here as the response to a higher West Antarctic Ice Sheet melting rate. Using data assimilation, we constrain the fresh water flux to increase by 100 mSv from 10 to 8 ka BP. This perturbation leads to an oceanic cooling of 0.5 °C and a strengthening of Southern Hemisphere westerlies (+6%. However, the observed cooling in Antarctic and the Southern Ocean proxy records can only be reconciled with the combination of a modified atmospheric circulation and an enhanced freshwater flux.

  13. Using data assimilation to investigate the causes of Southern Hemisphere high latitude cooling from 10 to 8 ka BP

    Directory of Open Access Journals (Sweden)

    P. Mathiot

    2013-04-01

    Full Text Available From 10 to 8 ka BP (thousand years before present, paleoclimate records show an atmospheric and oceanic cooling in the high latitudes of the Southern Hemisphere. During this interval, temperatures estimated from proxy data decrease by 0.8 °C over Antarctica and 1.2 °C over the Southern Ocean. In order to study the causes of this cooling, simulations covering the early Holocene have been performed with the climate model of intermediate complexity LOVECLIM constrained to follow the signal recorded in climate proxies using a data assimilation method based on a particle filtering approach. The selected proxies represent oceanic and atmospheric surface temperature in the Southern Hemisphere derived from terrestrial, marine and glaciological records. Two mechanisms previously suggested to explain the 10–8 ka BP cooling pattern are investigated using the data assimilation approach in our model. The first hypothesis is a change in atmospheric circulation, and the second one is a cooling of the sea surface temperature in the Southern Ocean, driven in our experimental setup by the impact of an increased West Antarctic melting rate on ocean circulation. For the atmosphere hypothesis, the climate state obtained by data assimilation produces a modification of the meridional atmospheric circulation leading to a 0.5 °C Antarctic cooling from 10 to 8 ka BP compared to the simulation without data assimilation, without congruent cooling of the atmospheric and sea surface temperature in the Southern Ocean. For the ocean hypothesis, the increased West Antarctic freshwater flux constrainted by data assimilation (+100 mSv from 10 to 8 ka BP leads to an oceanic cooling of 0.7 °C and a strengthening of Southern Hemisphere westerlies (+6%. Thus, according to our experiments, the observed cooling in Antarctic and the Southern Ocean proxy records can only be reconciled with the reconstructions by the combination of a modified atmospheric circulation and an enhanced

  14. The late Holocene dry period: multiproxy evidence for an extended drought between 2800 and 1850 cal yr BP across the central Great Basin, USA

    Science.gov (United States)

    Mensing, Scott A.; Sharpe, Saxon E.; Tunno, Irene; Sada, Don W.; Thomas, Jim M.; Starratt, Scott W.; Smith, Jeremy

    2013-01-01

    Evidence of a multi-centennial scale dry period between ∼2800 and 1850 cal yr BP is documented by pollen, mollusks, diatoms, and sediment in spring sediments from Stonehouse Meadow in Spring Valley, eastern central Nevada, U.S. We refer to this period as the Late Holocene Dry Period. Based on sediment recovered, Stonehouse Meadow was either absent or severely restricted in size at ∼8000 cal yr BP. Beginning ∼7500 cal yr BP, the meadow became established and persisted to ∼3000 cal yr BP when it began to dry. Comparison of the timing of this late Holocene drought record to multiple records extending from the eastern Sierra Nevada across the central Great Basin to the Great Salt Lake support the interpretation that this dry period was regional. The beginning and ending dates vary among sites, but all sites record multiple centuries of dry climate between 2500 and 1900 cal yr BP. This duration makes it the longest persistent dry period within the late Holocene. In contrast, sites in the northern Great Basin record either no clear evidence of drought, or have wetter than average climate during this period, suggesting that the northern boundary between wet and dry climates may have been between about 40° and 42° N latitude. This dry in the southwest and wet in the northwest precipitation pattern across the Great Basin is supported by large-scale spatial climate pattern hypotheses involving ENSO, PDO, AMO, and the position of the Aleutian Low and North Pacific High, particularly during winter.

  15. Agriculture, Settlement, and Abrupt Climate Change: The 4.2ka BP event in Northern Mesopotamia

    Science.gov (United States)

    Ristvet, L.

    2003-12-01

    attendant villages. The survey records an 80% decline in settled hectares from the previous period. The only agricultural villages that remained occupied during this crisis were either concentrated along perennial wadis or located in areas with ample groundwater. Otherwise, the survey recorded the presence of a few temporary sites, probably camps belonging to semi-nomadic pastoralists, a lifestyle which may have begun in response to this event. The precipitation regime stabilized at approximately 1900 BC, allowing for a massive resettlement of the area. This resettlement did not, however, lead to a resumption of third millennium agricultural practices; instead, these villages embraced a flexible economic regime, which emphasized a reliance on pastoral as well as agricultural products, and as such, was well-adapted to the more marginal conditions of the early second millennium BC. This paper, therefore, attempts to quantify the effects of the 4.2 ka BP abrupt climate change event on ancient agricultural systems, settlement patterns, and societies through archaeological survey in northern Mesopotamia.

  16. Multistep food plant processing at Grotta Paglicci (Southern Italy) around 32,600 cal B.P.

    Science.gov (United States)

    Mariotti Lippi, Marta; Foggi, Bruno; Aranguren, Biancamaria; Ronchitelli, Annamaria; Revedin, Anna

    2015-09-29

    Residue analyses on a grinding tool recovered at Grotta Paglicci sublayer 23A [32,614 ± 429 calibrated (cal) B.P.], Southern Italy, have demonstrated that early modern humans collected and processed various plants. The recording of starch grains attributable to Avena (oat) caryopses expands our information about the food plants used for producing flour in Europe during the Paleolithic and about the origins of a food tradition persisting up to the present in the Mediterranean basin. The quantitative distribution of the starch grains on the surface of the grinding stone furnished information about the tool handling, confirming its use as a pestle-grinder, as suggested by the wear-trace analysis. The particular state of preservation of the starch grains suggests the use of a thermal treatment before grinding, possibly to accelerate drying of the plants, making the following process easier and faster. The study clearly indicates that the exploitation of plant resources was very important for hunter-gatherer populations, to the point that the Early Gravettian inhabitants of Paglicci were able to process food plants and already possessed a wealth of knowledge that was to become widespread after the dawn of agriculture.

  17. Palaeolake and palaeoenvironment between 42 and 18 kaBP in Tengger Desert, NW China

    Institute of Scientific and Technical Information of China (English)

    2002-01-01

    Comprehensive field investigations and laboratory analyses show that palaeolakes, including fresh- mesohaline water Megalake Tengger and other semi-con- nected, isolated water bodies, during late Pleistocene covered an area of more than 20000 km2, which is more than half of the Tengger Desert in NW China. Stratigraphic correlation and chronological evidence indicate that before ca. 42000 aBP the area was more arid. The palaeolakes started to develop around 40000 uncal. 14C aBP but until 37000 14C aBP their scope was limited. High water levels established from 35000 14C aBP lasted until 22000 14C aBP. Lake levels regressed between 22000 and 20000 14C aBP but transgressed from 20000 to 18600 14C aBP. Subsequently, water level declined further and the Megalake Tengger finally desiccated at around 18000 14C aBP. Megalake Tengger possessed a fresh-mesohaline water property, implying that the regional precipitation increased significantly. During the period of Megalake Tengger, the climate was warmer-humid than present. The annual rainfall was 250 to 350 mm more than that of today and the temperature was 1.5 to 3.0℃ higher.

  18. Interpreting the seasonality of precipitation in northern Baja California for the last ~45,000 cal yr BP

    Science.gov (United States)

    Chavez, V.; Brunelle, A.; Brewer, S.

    2014-12-01

    The Sierra de Juarez of Northern Baja California lies in a region that is heavily influenced by the El Niño Southern Oscillation (ENSO), which brings winter precipitation and the North American Monsoon (NAM), which brings summer precipitation to the region. Little is known about the impacts that the seasonality of precipitation have had on fire and vegetation throughout the region, especially extending into the early Holocene and Pleistocene. Fire regimes and ciénega processes, as indicate by loss on ignition, magnetic susceptibility, and charcoal data, appear to be controlled by the amount of precipitation to the region and groundwater levels. This study will analyze seasonality of precipitation based on certain taxa that are associated with summer wet or winter wet moisture patterns. Preliminary pollen analysis shows that when summer-wet taxa are more prevalent on the landscape, winter-wet taxa declines. Based on existing ENSO and NAM data, we know that the influences of both phenomena have changed in their intensities and spatial boundaries throughout time. Our study sites (Ciénega Chimeneas, 32o 14' N and 116 o 06' W, and Ciénega San Faustino, 32° 12' 30.4" N 116° 09' 55" W, spanning the last ~45,000 cal yrs BP) are located in a region that can help define when and where changes in the seasonality of precipitation have occurred since the late Pleistocene. Additional dating and pollen analysis will allow us to further validate the relationships between ENSO and NAM like activity and ecosystem processes for this site.

  19. Climate warming and vegetation response at the end of Heinrich event 1 (16 700–16 000 cal yr BP in Europe south of the Alps

    Directory of Open Access Journals (Sweden)

    S. Samartin

    2012-05-01

    Full Text Available Chironomids preserved in a sediment core from Lago di Origlio (416 m a.s.l., a lake in the foreland of the Southern Swiss Alps, allowed quantitative reconstruction of Late Glacial and early Holocene temperatures using a combined Swiss-Norwegian temperature inference model based on chironomid assemblages from 274 lakes. We reconstruct July air temperatures of ca. 10 °C between 17 300 and 16 000 cal yr BP, a rather abrupt warming to ca. 12.0 °C at ca. 16 500–16 000 cal yr BP, and a strong temperature increase at the transition to the Bølling/Allerød Interstadial with average temperatures of about 14 °C. During the Younger Dryas and earliest Holocene very similar temperatures are reconstructed as for the interstadial. The rather abrupt warming at 16 500–16 000 cal yr BP is consistent with sea-surface temperature as well as speleotherm records, which indicate a marked Pre-Bølling warming after the end of Heinrich event 1 in southern Europe and the Mediterranean Sea. The pollen record of Origlio and other sites from southern Switzerland and northern Italy indicate an early reforestation of the lowlands prior to the large-scale afforestation at the onset of the Bølling period at 14 700 cal yr BP in Central Europe. Our results suggest that these afforestation processes in the formerly glaciated areas of southern Switzerland and Northern Italy have been promoted by increasing temperatures.

  20. Climate warming and vegetation response after Heinrich event 1 (16 700–16 000 cal yr BP in Europe south of the Alps

    Directory of Open Access Journals (Sweden)

    W. Tinner

    2012-11-01

    Full Text Available Chironomids preserved in a sediment core from Lago di Origlio (416 m a.s.l., a lake in the foreland of the Southern Swiss Alps, allowed quantitative reconstruction of Late Glacial and Early Holocene summer temperatures using a combined Swiss–Norwegian temperature inference model based on chironomid assemblages from 274 lakes. We reconstruct July air temperatures of ca. 10 °C between 17 300 and 16 000 cal yr BP, a rather abrupt warming to ca. 12.0 °C at ca. 16 500–16 000 cal yr BP, and a strong temperature increase at the transition to the Bølling/Allerød interstadial with average temperatures of about 14 °C. During the Younger Dryas and earliest Holocene similar temperatures are reconstructed as for the interstadial. The rather abrupt warming at 16 500–16 000 cal yr BP is consistent with sea-surface temperature as well as speleothem records, which indicate a warming after the end of Heinrich event 1 (sensu stricto and before the Bølling/Allerød interstadial in southern Europe and the Mediterranean Sea. Pollen records from Origlio and other sites in southern Switzerland and northern Italy indicate an early reforestation of the lowlands 2000–1500 yr prior to the large-scale afforestation of Central Europe at the onset of the Bølling/Allerød period at ca. 14 700–14 600 cal yr BP. Our results suggest that these early afforestation processes in the formerly glaciated areas of northern Italy and southern Switzerland have been promoted by increasing temperatures.

  1. Past environmental and climatic changes during the last 7200 cal yrs BP in Adamawa Plateau (Northern-Cameroun based on fossil diatoms and sedimentary 13C isotopic records from Lake Mbalang

    Directory of Open Access Journals (Sweden)

    C. Martin

    2011-01-01

    Full Text Available Past limnological conditions of Lake Mbalang (7°19´ N, 13°44´ E, alt: 1130 m and vegetation type were reconstructed from diatoms and sedimentary stable carbon isotope records (δ13C since 7200 cal yrs BP. The data showed that before 3600 yrs cal BP the water column was preferentially cold and stable except around 5000–5300 cal yrs BP where diatom evidenced mixed upper water layer, δ13C data suggest more forested vegetation in the landscape. These stable conditions can be explained by a strong monsoonal flux and correlatively northern position of the ITCZ that entailed high/low rainfall well distributed over the year to allow the development mountainous forest taxa. The decreasing trend of the monsoonal flux towards mid-Holocene was however affected by several centennial to millennial time scale abrupt weakening at 6700, 5800–6000, 5000–5300, 4500 and 3600 cal yrs BP although their impact on vegetation is not visible probably because rainfall distribution was favourable to forest maintenance or extension. After 3600 cal yrs BP, water column became very mixed as a result of more intense NE trade winds (Harmattan that led at ~3000 cal yrs BP to the instalment of savana in the vegetation landscape. At that time, rainfall was probably reduced following the southwards shift of the ITCZ and the distribution of yearly rainfall was no more favourable to forest development. Thus a strong seasonality with a well marked dry season was established, conditions that maintained the savana vegetation till today. Diatom data suggest the lake did not dried during the last 7200 cal yrs BP, however, a low lake level observed at 2400–2100 cal yrs BP is contemporaneous to a climatic event evidenced in several areas of tropical Africa and could correspond to the southernmost position of the ITCZ. Other low lake levels are observed at 1800 and 1400 cal yrs BP, after which lake rose to its present level.

  2. Gavdos/West Crete Cal-Val Site: Over a Decade Calibrations for Jason Series, SARAL/AltiKa, Cryosat-2, Sentinel-3 and Hy-2 Altimeter Satellites

    Science.gov (United States)

    Mertikas, Stelios; DonLon, Craig; Mavrochordatos, Constantin; Tziavos, Ilias; Galanakis, Demitris; Vergos, George; Baltazar Andersen, Ole; Tripolitsiotis, Achilles; Frantzis, Xenofon; Lin, Mingsen; Qiao, Fangli

    2016-08-01

    This work presents and compares the latest altimeter calibration results for Jason series, the SARAL/AltiKa the Chinese HY-2 missions and the ESA missions of CryoSat-2 and Sentinel-3, conducted at the Gavdos/Crete calibration/validation facilities. At first, the Jason altimeter calibration values will be given for the ascending Pass No.109 and the descending Pass No.18, based on the GDR-E (Jason-1), GDR-D (Jason- 2) and GDR-T (Jason-3) products. Secondly, these values will be cross-examined against the altimeter bias for the SARAL/AltiKa (GDR-T) satellite at Gavdos Cal/Val using its reference ascending orbit No. 571. The Chinese HY-2 satellite altimeter bias will be presented using the CRS1 permanent site in southwest Crete for the descending HY-2 Pass No. 280, at 20 Hz based on SGDR data products. Finally, values will be compared against the Sentinel-3 altimeter. Additionally, altimeter biases as determined by locally developed Mean Sea Surface models, will be presented and compared with the conventional sea-surface calibration methodology.

  3. The evolution of deserts with climatic changes in China since 150 ka B.P.

    Institute of Scientific and Technical Information of China (English)

    董光荣; 陈惠忠; 王贵勇; 李孝泽; 邵亚军; 金炯

    1997-01-01

    According to the bioclimatic zones, dune mobility and the fabric characteristics of stratigraphic sedimentary facies, the deserts in China are divided into Eastern, Western, Central and Northwestern deserts. Based on the records of stratigraphical facies, climatic proxies, historical data, etc. in each desert region, the evolution of deserts with climatic changes in time and space since 150 ka B. P. in China are dealt with; then the evolution of deserts in relation to the glacial climatic fluctuations caused by solar radiation changes, underlying surface variation and their feedback mechanism is discussed through comparison with global records; finally, in consideration of global wanning due to increasing of greenhouse gases such as CO2, the possible tendency of the evolution of deserts and the climatic changes is discussed.

  4. Chronological reconstruction of eolianites and transversal mobile dunes of northwest coast of Ceará State - Brazil, in the last 3000 cal yrs BP

    Science.gov (United States)

    Castro, João Wagner Alencar; Malta, Julia Varella; Miguel, Lucas Lavo Antonio Jimo; Cabral, Caique Lima; Passemilio, Alvaro Balmant

    2017-10-01

    Dunefields are very common in the northern coastal zone of northeast Brazil. They have the potential to yield important information about paleoclimate, paleo-winds and regional winds and their response to sea-level fluctuations during the Holocene. We reconstructed the coastal dunes geochronological evolution of northwest Ceará State - Brazil, in the last 3000 cal yrs BP, using detailed analyses of lithostratigraphy, microfossil (foraminifera), wind regime, dune monitoring and 8 radiocarbon dates. The chronology was based on 14C dating in eolianites and monitoring transversal mobile dunes movement processes. Radiocarbon date results indicated that the dunes corresponding to eolianites revealed ages between 2760-2480 and 980-750 cal yrs BP, suggesting that the vast transversal mobile dunefields were formed after this period in similar condition to the current sea-level. We considered that the material transportation by the prevailing east winds towards the transversal dunes is estimated in the order of 11.0 m/year, thus the current aeolian system is less than 1000 yrs BP.

  5. Paleotemperature reconstructions from speleothem fluid inclusions between 14 - 10 ka BP in Milandre cave (NW Switzerland)

    Science.gov (United States)

    Affolter, Stéphane; Häuselmann, Anamaria; Fleitmann, Dominik; Leuenberger, Markus

    2016-04-01

    In cave environments, speleothems constitute a well preserved and precisely dated continental climate archive that record past environmental changes such as paleotemperature or moisture source, namely through oxygen and hydrogen isotopes variations. Fluid inclusions are common in speleothems and they correspond to micrometric voids that often contain fossil liquid water representing past precipitation falling above the cave nearly at the time the inclusions were sealed. To measure the δD and δ18O isotopic composition of speleothem fluid inclusions, we extracted submicrolitre amounts of water from stalagmites (old and recent) coming from Milandre cave (Switzerland) using a new online method developed at the University of Bern (Affolter et al., 2014). The released water is then flushed directly to a Picarro L1102-i or L2140-i laser based instrument that allows to simultaneously monitor hydrogen and oxygen isotopes. At Milandre cave site, a two year isotope monitoring campaign has confirmed that isotopes in precipitation for northwestern Switzerland are principally controlled by air temperature (Affolter et al., 2015). Therefore, when combined with calcite δ18O, the fluid inclusion water isotopes can be used to calculate paleotemperatures. We reconstructed a cold season biased (roughly autumn - winter - spring) paleotemperature trend for the time interval covering the Allerød, the Younger Dryas cold interval and the early Holocene (13'900 - 9'900 BP). References: Affolter S., Fleitmann D., and Leuenberger M.: New online method for water isotope analysis of speleothem fluid inclusions using laser absorption spectroscopy (WS-CRDS), Clim. Past, 10, 1291-1304, doi:10.5194/cp-10-1291-2014, 2014. Affolter S., Häuselmann A.D., Fleitmann D., Häuselmann P., Leuenberger M.: Triple isotope (δD, δ17O, δ18O) study on precipitation, drip water and speleothem fluid inclusions for a Western Central European cave (NW Switzerland), Quat. Sci. Rev., 127, pp. 73-89, 2015.

  6. Magnetic parameters and their palaeoclimatic implications—the sediment record of the last 15 500 cal. BP from Laguna Potrok Aike (Argentina)

    Science.gov (United States)

    Irurzun, M. A.; Orgeira, M. J.; Gogorza, C. S. G.; Sinito, A. M.; Compagnucci, R.; Zolitschka, B.

    2014-08-01

    Lake sediments are excellent sources of palaeoenvironmental and palaeoclimatic information because they provide continuous and high-resolution records. South America is of particular interest because it is the only landmass that stretches southward into the Pacific and Atlantic Oceans towards Antarctica. The aim of this study is to explore the relationship of magnetic parameters with elemental and palaeobiological data of Laguna Potrok Aike to develop a model of lake-level changes and related hydrological and climatic fluctuations. Magnetic measurements were performed on subsamples from 15 500 cal. BP to the present, and associated rock magnetic parameters were calculated to infer magnetic mineralogy, concentration and grain size. According to the model, parameters dependent on magnetic concentration and grain size are directly related to lake-level changes. During dry periods, the remanent coercivity displays high values, whereas the proportion of magnetite is relatively low. Low percentages of greigite are observed, indicating that the water of the lake was stratified at least four times during the studied period, at approximately 10 300, 8900, 8500 and 8300 cal. BP. The preservation of greigite by inhibiting its complete transformation into pyrite is associated with a rapid burial that occurs with high sedimentation rates. Thermal stratification could be caused by a slight cooling in the area triggered by a weakening of the Westerlies and/or low activity of the sun, sum to the effect of a flood of melt water in the North Atlantic.

  7. Work More? The 8.2 kaBP Abrupt Climate Change Event and the Origins of Irrigation Agriculture and Surplus Agro-Production in Mesopotamia

    Science.gov (United States)

    Weiss, H.

    2003-12-01

    The West Asian archaeological record is of sufficient transparency and resolution to permit observation of the social responses to the major Holocene abrupt climate change events at 8.2, 5.2 and 4.2 kaBP. The 8.2kaBP abrupt climate change event in West Asia was a three hundred year aridification and cooling episode. During this period rain-fed agriculture, established for over a millennium in northern Mesopotamia, suddenly collapsed. Irrigation agriculture, pastoral nomadism, or migration were the only subsistence alternatives for populations previously supported by cereal dry-farming. Irrigation agriculture was not, however, possible along the northern alluvial plains of the Tigris and Euphrates Rivers, where incised riverbeds were several meters below plain level. Exploitable plain-level levees were only accessible in southern-most alluvial plain, at the head of the present-day Persian Gulf. The archaeological data from this region documents the first irrigation agriculture settlement of the plain during the 8.2 kaBP event. Irrigation agriculture provides about twice the yield of dry-farming in Mesopotamia, but at considerable labor costs relative to dry-farming. With irrigation agriculture surplus production was now available for deployment. But why work more? The 8.2 kaBP event provided the natural force for Mesopotamian irrigation agriculture and surplus production that were essential for the earliest class-formation and urban life.

  8. The reconstruction of paleo wind directions for the Eifel region (Central Europe during the period 40.3–12.9 ka BP

    Directory of Open Access Journals (Sweden)

    K. Seelos

    2009-09-01

    Full Text Available A continuous reconstruction of last glacial wind directions is based on provenance analysis of eolian sediments in a sediment core from the Dehner dry Maar in the Eifel region (Germany. This Maar is suitable to archive paleo wind directions due to its location west of the Devonian carbonate basins of the Eifel-North-South-Zone. Thus, eolian sediments with high clastic carbonate content can be interpreted as an east wind signal. The detection of such east wind sediments is applied by a new module of the RADIUS grain size analyze technique. Increased frequencies of east wind occur during the time intervals corresponding with the Heinrich events H1 and H2. The unusual H3 show no higher east wind frequency but so do its former and subsequent Greenland stadials. The LGM (21–18 ka BP is characterized by a slightly elevated east wind activity. The investigated time period from 40.3–12.9 ka BP can be subclassified in three units: The first time period during Marine Isotope Stage 3 (40.3–36 ka BP is controlled by relative warm climate leading to an enriched content of organic matter in the sediment. Thus, there is only little accumulation of dust in the Eifel region and Heinrich 4 is not recorded in the archive by our dust proxy. The second time slice (36–24 ka BP has an increased content of dust accumulation and a high amount of east winds layers (up to 19% of the dust storms per century came from the east. In comparison, the subsequent period (24–12.9 ka BP is characterized by lower east winds sediments again.

  9. Evidence for natural fire and climate history since 37 ka BP in the northern part of the South China Sea

    Institute of Scientific and Technical Information of China (English)

    孙湘君[1; 李逊[2; 陈怀成[3

    2000-01-01

    The history of natural fire since 37 kaBP and its relationship to climate for the northern part of the South China Sea are revealed from the statistic study of charcoal particles and associated pollen data from deep sea core 17940 (20° 07’N, 117° 23’E, 1 727 m in water depth). Our study indicates that, during the last glaciation, the concentration of charcoal and the ratio of concentration between charcoal and terrestrial pollen are much higher than that of the Holocene. This can be explained as the relatively high strength and frequency of natural fire during glaciation which is probably due to the drier climate; during the Last Glacial Maximum (LGM), the substantial rising of the concentration of large and medium charcoal particles probably suggests the local source area of the natural fires, i.e. the exposed continental shelf; moreover, the correlation between charcoal concentration with different size and pollen percentage may elucidate different transport dynamics. During the glacial time, almost

  10. The application of Flow Cytometry to the study of ancient agriculture: Evidence for Mesolithic farming in Northern Britain 7200 Cal yr BP.

    Science.gov (United States)

    Jones, Richard; Tennant, Richard; Hatton, Jackie; Lee, Rob; Love, John

    2017-04-01

    The onset of agriculture in the UK, (the Mesolithic-Neolithic transition 6000 - 5500 Cal yr BP), has commonly been viewed as the end point of a cultural and technological wave that began in Eastern Europe on the Hungarian Plain 7500 Cal yr BP. This view is not without its critics, due in part to the uncertainty regarding the timing and rate of expansion and the difficulty in identifying the point at which agriculture first arrived in a particular location. Evidence for potential 'episodes' of Mesolithic agricultural activity in the UK has been identified in the UK pollen record, but this data is very tentative. Cereal pollen is typically present in very low concentrations (requiring very large, time consuming counts) and differentiating early cereal pollen from local grasses is very problematic, particularly in areas where the local grasses were domesticated. We present a multi-proxy record from Mere Tarn (54°8'12.09" N 3°7'24.28"W), 2km from the Morecambe Bay coast in South Cumbria, UK; a region with a long history of human occupation extending back into the Palaeolithic. A lacustrine core spanning the Mesolithic and Neolithic has been analysed using a combination of 'traditional' pollen analysis, Flow Cytometry and ancient DNA (aDNA). Flow Cytometry is employed to increase the concentration of cereal type grains in a sample, whilst also providing a more 'targeted' sample for aDNA analysis. The results so far provide clear evidence for an early phase of 'Mesolithic' agriculture in the catchment, spanning only two centuries ( 7300 to 7100 Cal yr BP). This phase is characterised by the occurrence of large cereal type grains (> 38µm), evidence for woodland clearance and the expansion of key anthropogenic indicators such as P. lanceolata. It occurred over 1600 years before the main transition into permanent and intensive agriculture in the catchment, at a time of significant changes in regional climate and sea-level. The results from Mere Tarn provide the earliest

  11. Environmental change and cultural response around 4200 cal. yr BP in the Yishu River Basin, Shandong%山东沂沭河流域2000BC前后古文化兴衰的环境考古

    Institute of Scientific and Technical Information of China (English)

    高华中; 朱诚; 徐伟峰

    2007-01-01

    Neolithic culture series in the Yishu River Basin developed in the order of Beixin culture-Dawenkou culture-Longshan culture-Yueshi culture. During the early and middle stage of Longshan culture (4600-4300 cal. yr BP), the climate in the Yishu River Basin was warm and wet. Paddy-oriented agriculture planted paddy was very developed. The society was flourishing with great amount of archaeological sites. The cooling starting in 4200 cal. yr BP made the paddies shortfall in output or even no seeds were gathered. This situation intensified the discrepancy between population and resource. The scarcity in natural resource led to substantial decrease in population and subsequent drop in archaeological sites. About 4000 cal. yr BP Longshan culture was displaced by Yueshi culture which was relatively underdeveloped, simple and unsophisticated.

  12. Sporo-pollen Assemblage and Paleoclimate Events in Shelf Area of the Southern Yellow Sea Since 15 ka B.P.

    Institute of Scientific and Technical Information of China (English)

    孟广兰; 韩有松; 王少青; 王珍岩

    2004-01-01

    Based on the authors'1986 to 1994 sporo-pollen assemblage analysis in the southern Yellow Sea area, data from 3 main cores were studied in combination with 14C, palaeomagnetic and thermoluminescence data. The evolution of the paleoclimate environments in the southern Yellow Sea since 15ka B.P. was revealed that, in deglaciation of the last glacial period, the climate of late glaciation transformed into that of postglaciation, accompanied by a series of violent climate fluctuations. These evolution events happened in a global climate background and related to the geographic changes in eastern China. We distinguished three short-term cooling events and two warming events. Among them, the sporo-pollen assemblage of subzone A1 showed some cold climate features indicating that a cooling event occurred at about 15-14ka. B.P. in early deglaciation. This subzone corresponds to the Oldest Dryas. In subzone A3, many drought-enduring herbal pollens and some few pollens of cold-resistant Picea, Abies, etc. were found, which indicated that a cooling event, with cold and arid climate, occurred at about 12-11ka. B.P. in late deglaciation. This subzone corresponds to the Younger Dryas. The sporo-pollen assemblage of zone B showed warm and arid climate features in postglaciation. Although the assemblage of subzone B2 indicated a cold and arid climate environment, the development of flora in subzone B2 climate was less cold than that in A3. Subzone B2 indicated a cooling event which occurred at about 9ka B.P. in early Holocene. Subzone A2, with some distinct differences from subzone A1 and A3, indicated a warming event which occurred at 14-13ka. B.P. and should correspond to a warming fluctuation. The sporo-pollen assemblage of zone C showed features of warm-moist flora and climate, and indicated a warming event which universally occurred along the coast of eastern China at 8-3ka B.P. in middle Holocene, and its duration was longer than that of any climate events mentioned above

  13. A Detailed Radiometric Chronological Framework for Nordic Seas Ocean-Ice Sheet Interactions Spanning 50-150 Ka BP

    Science.gov (United States)

    Brendryen, J.; Edwards, R. L.; Haflidason, H.; Cheng, H.; Grasmo, K. J.; Sejrup, H. P.

    2014-12-01

    Chronological control of sedimentary deposits is a key to do paleoclimatic interpretations of proxy records and to compare them with records from other archives. Beyond the reach of radiocarbon dating there are however few options for developing chronological control. We present a detailed radiometrical-based chronological framework of a Norwegian Sea core archive that records ocean-ice sheet interactions in the Nordic Seas covering the time span 50-150 ka BP. The chronology is based on a detailed multi-proxy and multi-archive alignment of high resolution records from the Norwegian Sea and precisely radiometric dated speleothem δ18O record from both China and the Alps. This approach utilizes the close and well documented millennial and multi-centennial scale coupling between the North Atlantic climate variability (recorded in the Norwegian Sea records, the Greenland ice cores and in the Alpine speleothems) and the Asian Monsoon system recorded in the Chinese speleothem δ18O. One intriguing feature of the Norwegian Sea record is that it often is more similar to the Chinese speleothem records than to the Greenland ice core records. The alignment is aided by a tephrostratigraphic link to the Greenland ice cores which provide an independent test of the age model and alignment. Uncertainties are addressed by Bayesian age-depth modeling. The radiometric-based age model and the quantified uncertainties enable an independent comparison between the Nordic Seas ocean-ice sheet interaction and other absolutely dated records such as U/Th dated sea-level indices and orbital parameters. This improves our ability to interpret the ocean-ice sheet interactions of the polar north in a global context over this time span that comprises a glacial-interglacial cycle.

  14. Evidence for natural fire and climate history since 37 ka BP in the northern part of the South China Sea

    Institute of Scientific and Technical Information of China (English)

    2000-01-01

    The history of natural fire since 37 kaBP and its relationship to climate for the northern part of the South China Sea are revealed from the statistic study of charcoal particles and associated pollen data from deep sea core 17940 (20°07′N, 117°23′E, 1 727 m in water depth). Our study indicates that, during the last glaciation, the concentration of charcoal and the ratio of concentration between charcoal and terrestrial pollen are much higher than that of the Holocene. This can be explained as the relatively high strength and frequency of natural fire during glaciation which is probably due to the drier climate; during the Last Glacial Maximum (LGM), the substantial rising of the concentration of large and medium charcoal particles probably suggests the local source area of the natural fires, i.e. the exposed continental shelf; moreover, the correlation between charcoal concentration with different size and pollen percentage may elucidate different transport dynamics. During the glacial time, almost all the peak concentrations of small particles correspond with the peak pollen percentage of Artemisia, an indicator of comparatively dry climate, while for large particles, their concentrations always lag behind small particles and thus change with pollen percentage of montane conifers implying relatively cold and humid climate. So, it is possible to assume that small particles reflect regional emissions under drier climate and were brought over by strengthened winter monsoon. When the climate became relatively humid, the increasing precipitation carried the large particles accumulated on continental shelf before under arid condition to the studied area.

  15. Climatic changes documented by stable isotopes of sedimentary carbonate in Lake Sugan, northeastern Tibetan Plateau of China, since 2 kaBP

    Institute of Scientific and Technical Information of China (English)

    QIANG Mingrui; CHEN Fahu; ZHANG Jiawu; GAO Shangyu; ZHOU Aifeng

    2005-01-01

    Lake Sugan at the northern edge of the Qaidam Basin was selected as the research object. The temporal sequence of sedimentary cores retrieved from Lake Sugan since 2 kaBP was reconstructed using the 210Pb, AMS 14C and conventional 14C dating methods. Carbon and oxygen isotopes of carbonate in the fine-grained lake sediments were analysed. Combined with the changes of δ18O values of surface water and air temperature observation data in the study area, it might be thought that theδ18O value of the carbonate indicates effective moisture, and the changes in δ13C values are related to annual freeze-up duration of the lake and indirectly indicate air temperature changes in winter half year. From the above, the sequence of climatic changes in the region since 2 kaBP was established. The climatic changes experienced five stages: Warm-dry climate during 0-190 AD; cold-dry climate during 190-580 AD; warm-dry climate during 580-1200 AD (MWP); cold-wet climate during 1200-1880 AD (LIA); cold-dry climate during 1880-1950 AD; and climate warming since 1950s. The air temperature changes in winter half year reflected by carbon isotope since 2 kaBP are in good agreement with the historical literature records and other geologic records, which shows that the climate changes recorded by the stable isotopes from Lake Sugan since 2 kaBP are of universal significance.

  16. The WAIS Divide deep ice core WD2014 chronology – Part 2: Annual-layer counting (0–31 ka BP

    Directory of Open Access Journals (Sweden)

    M. Sigl

    2015-07-01

    Full Text Available We present the WD2014 chronology for the upper part (0–2850 m, 31.2 ka BP of the West Antarctic Ice Sheet (WAIS Divide ice core. The chronology is based on counting of annual layers observed in the chemical, dust and electrical conductivity records. These layers are caused by seasonal changes in the source, transport, and deposition of aerosols. The measurements were interpreted manually and with the aid of two automated methods. We validated the chronology by comparing to two high-accuracy, absolutely dated chronologies. For the Holocene, the cosmogenic isotope records of 10Be from WAIS Divide and 14C for Intcal13 demonstrated WD2014 was consistently accurate to better than 0.5 % of the age. For the glacial period, comparisons to the Hulu Cave chronology demonstrated WD2014 had an accuracy of better than 1 % of the age at three abrupt climate change events between 27 and 31 ka. WD2014 has consistently younger ages than Greenland ice-core chronologies during most of the Holocene. For the Younger Dryas-Preboreal transition (11 546 ka BP, 24 years younger and the Bølling-Allerød Warming (14 576 ka, 7 years younger WD2014 ages are within the combined uncertainties of the timescales. Given its high accuracy, WD2014 can become a reference chronology for the Southern Hemisphere, with synchronization to other chronologies feasible using high quality proxies of volcanism, solar activity, atmospheric mineral dust, and atmospheric methane concentrations.

  17. An exceptionally strengthened East Asian summer monsoon event between 19.9 and 17.1 ka BP recorded in a Hulu stalagmite

    Institute of Scientific and Technical Information of China (English)

    L.; R.; EDWARDS

    2009-01-01

    A stalagmite-based isotope record (No. H82) from Nanjing Hulu Cave, spanning from 16.5 to 10.3 ka BP, provided strong evidence for a coherence relation between the East Asian summer monsoon (EASM) and the North Atlantic climates on millennial time scales. Here we extend the high-resolution δ 18O time series back to 22.1 ka BP with additional 7 230Th dates and 573 stable isotope measurements on the lower part of that sample. The new record with a decadal resolution, piecing together with the previous data, provides a detailed, complete Last Glacial Maximum (LGM)/deglacial history of the EASM. Two centennial-scale weak monsoon events are detected within the analogue H1 event, and can be corre- lated to corresponding Greenland temperature shifts. This suggests a rapid re-organization of atmos- pheric and oceanic circulations during the ice-rafted debris (IRD) event in North Atlantic. A strength- ened EASM event spanning from 19.9 to 17.1 ka BP, firstly reported here, reaches on average a half of the monsoon intensity of B?lling warming with its peak close to the full level. Taking all available evi- dence from continental and oceanic sediments into consideration, we suggest that a forcing mecha- nism behind the event would be a positive feedback of the tropical Pacific Super-ENSO cycles in re- sponse to precessional changes in solar irradiation.

  18. An exceptionally strensthened East Asian summer monsoon event between 19.9 and 1 7.1 ka BP recorded in a Hulu stalagmite

    Institute of Scientific and Technical Information of China (English)

    WU JiangYing; WANG YongJin; CHENG Hai; L.R.EDWARDS

    2009-01-01

    A stalagmite-based isotope record (No.H82)from Nanjing Hulu Cave,spanning from 16.5 to 10.3 ka BP,provided strong evidence for a coherence relation between the East Asian summer monsoon (EASM) and the North Atlantic climates on millennial time scales.Here we extend the high-resolution δ18O time series back to 22.1 ka BP with additional 7 230 Th dates and 573 stable isotope measurements on the lower part of that sample.The new record with a decadal resolution,piecing together with the previous data,provides a detailed,complete Last Glacial Maximum (LGM)/deglacial history of the EASM.Two centennial-scale weak monsoon events are detected within the analogue H1 event,and can be correlated to corresponding Greenland temperature shifts.This suggests a rapid re-organization of atmospheric and oceanic circulations during the ice-rafted debris (IRD) event in North Atlantic.A strengthened EASM event spanning from 19.9 to 17.1 ka BP,firstly reported here,reaches on average a half of the monsoon intensity of B(Φ)iling warming with its peak close to the full level.Taking all available evidence from continental and oceanic sediments into consideration,we suggest that a forcing mechanism behind the event would be a positive feedback of the tropical Pacific Super-ENSO cycles in response to precessional changes in solar irradiation.

  19. Multiproxy evidence for terrestrial and aquatic ecosystem responses during the 8.2 ka cold event as recorded at Højby Sø, Denmark

    DEFF Research Database (Denmark)

    Hede, Mikkel Ulfeldt; Rasmussen, Peter; Noe-Nygaard, Nanna;

    2010-01-01

    .2 ka cold event as registered in the Greenland ice cores. At Højby Sø, the climate anomaly appears to have started 200–250 yr earlier than the 8.2 ka cold event as the lake proxy data provide strong evidence for a precipitation-induced distinct increase in catchment soil erosion beginning around 8500...... cal yr BP. Alteration of the terrestrial environment then resulted in a major aquatic ecosystem change with nutrient enrichment of the lake and enhanced productivity, which lasted until c. 7900 cal yr BP. Keywords: 8.2 ka cold event; Lake sediments; Palaeoclimate; Pollen; Macrofossils; Geochemistry...

  20. Landscape dynamics and fire activity since 6740 cal yr BP in the Cantabrian region (La Molina peat bog, Puente Viesgo, Spain)

    Science.gov (United States)

    Pérez-Obiol, R.; García-Codron, J. C.; Pèlachs, A.; Pérez-Haase, A.; Soriano, J. M.

    2016-03-01

    A lack of paleobotanic studies with adequate resolution and multiproxy approaches has limited proper discussion of vegetation dynamics in Cantabria and of the role of fires in the configuration of the plant landscape during the Holocene in the northwest part of the Iberian peninsula. The pollen diagram of La Molina peat bog in Puente Viesgo (43°15‧38″ N-3°58‧37″ W; ETRS89), located at 484 m.a.s.l., and the study of its sedimentary charcoals allowed the acquisition of a continuous and thorough fire sequence for the last 6700 cal yr BP and an understanding of its relationship to the forest. The results show the importance of human influence on the incidence and characteristics of fire activity during the different phases studied: the Neolithic, Bronze Age, Iron Age, Roman period, and Middle Ages. A synergy seems to exist between dry climate periods (especially during Bond events 3 and 4) and a greater presence of biomass. As the Holocene advances, vegetation coverage clearly tends to decrease. This study provides key elements for understanding the role of fire activity in the forest dynamics of deciduous and evergreen Quercus, Corylus, Pinus, Fagus, and Alnus and demonstrates the strongly artificialized character of the present landscape.

  1. CALS Mapping

    DEFF Research Database (Denmark)

    Collin, Ib; Nielsen, Povl Holm; Larsen, Michael Holm

    1998-01-01

    To enhance the industrial applications of CALS, CALS Center Danmark has developed a cost efficient and transparent assessment, CALS Mapping, to uncover the potential of CALS - primarily dedicated to small and medium sized enterprises. The idea behind CALS Mapping is that the CALS State...... enterprise is, when applied in a given organisation modified with respect to the industry regarded, hence irrelevant measure parameters are eliminated to avoid redundancy. This assessment of CALS Mapping, quantify the CALS potential of an organisation with the purpose of providing decision support to the top...

  2. 秦岭地区15 ka BP以来的植被与环境%The vegetational and environmental history in Qinling Mountain since 15 ka BP

    Institute of Scientific and Technical Information of China (English)

    赵先贵; 肖玲

    2003-01-01

    通过对秦岭海拔2 200 m一山间盆地沼泽沉积剖面的花粉分析和14C年代测定,结合对该区植被与表土花粉的研究,认为秦岭的暗针叶林带15 ka BP以来植被和环境经历了4个发展阶段:(1) 约15 450~6 760 a BP,植被为冷杉(Abies)-云杉(Picea)林,气候寒冷潮湿;(2) 约6 760~2 940 a BP,沉积物中花粉稀少,以冷杉、云杉、桦(Betula)、栎(Quercus)为主,出现了喜暖型植物桤木(Alnus),气候暖湿;(3) 2 940~40 a BP,植被为冷杉林,气候冷湿;(4) 0~40 a BP,植被为桦、栎、榛(Corylus)、桤木、铁杉(Tsuga)和小片状分布的冷杉,松(Pinus)的数量极少,气候向暖干方向发展,这是近期人为活动干扰的结果.

  3. Beringian Megafaunal Extinctions at ~37 ka B.P.: Do Micrometeorites Embedded in Fossil Tusks and Skulls Indicate an Extraterrestial Precursor to the Younger Dryas Event?

    Science.gov (United States)

    Hagstrum, J. T.; Firestone, R. B.; West, A.

    2009-12-01

    Studies of Late Pleistocene megafaunal fossils and their ancient DNA from Beringia (eastern Siberia, Alaska, and the emerged Bering Strait) indicate sharp declines in steppe bison population diversity and horse body size, extinction of the Alaskan wild ass, and local extinctions of brown bear and woolly mammoth genetic lines beginning at about 37 ka B.P. Beringia is also well known for its remarkably preserved Late Pleistocene frozen animal mummies. 14C ages of these mummies are bimodally distributed, having peaks coincident with the earlier ~37 ka B.P., and ~13 ka B.P. Younger Dryas, onset extinction events. Associated with the ~37 ka B.P. event are, for example, the Berezovka mammoth, headless Selerikan horse, steppe bison “Blue Babe”, and baby mammoths “Dima” and “Lyuba”. Analyses of these and other mummies indicate that they died instantly, in mostly healthy condition, with gut contents and high fat reserves indicative of a late summer to autumn season. An assortment of uneaten limbs and other body parts from a variety of species have also been found. Uniformitarian death scenarios inadequately account for the lack of evidence of normal predation and scavenging. Extensive internal injuries (e.g. large bone fractures, hemorrhaging) and apparent rapid burial of the mummies also indicate that something truly unusual happened at the time of these extinction events. We have discovered what appear to be micrometeorites embedded in seven Alaskan mammoth tusks and a Siberian bison skull acquired from commercial sources. 14C ages for five of these fossils have a weighted mean age of 33 ± 2 ka B.P. Laser ablation ICP-MS and XRF analyses of the particles indicate high Fe contents with compositions enriched in Ni and depleted in Ti, similar to Fe meteorites and unlike any natural terrestrial sources. Microprobe analyses of a Fe-Ni sulfide grain from tusk 2 also show that it contains between 3 and 20 weight percent Ni. SEM images and XRF analyses of a bison

  4. 柴达木盆地大浪滩130ka BP以来的孢粉组合与古气候%Sporo-pollen assemblage and palaeoenvironment since 130 ka BP in Dalangtan Lake of Qaidarn Basin

    Institute of Scientific and Technical Information of China (English)

    侯献华; 郑绵平; 杨振京; 杨庆华; 毕志伟

    2011-01-01

    This paper obtained the data of the cores based on U-series age from ZK02 borehole at ridge of Dalangtan in the western Qaidam basin, where 34 samples from the sludge containing gypsum silt were selected of select for 130 ka BP (90.5 m and above) and the pollen analysis was done. Based on the pollen characteristics, the assemblage of the pollen from the bottom upwards can be divided into six zones to analyze the ancient vegetation succession in the last interglacial (130 ka BP) state in this area. The results showed as follows: in the period of 130 ka BP (the last interglacial period), the vegetation in the western Qaidam basin obviously changed compared with the very significant environment. Overall, the spruce, fir and pine trees consisted of some cold temperate coniferous forest had expanded for five times to the surrounded Zhongshan area, and even extends towards the basin. But thegrass of Gramineae, Compositae, Artemisia as the main component occupied the basin, which showed the climate that was mild climate controlled by the summer monsoon flow from the East Asia to the West, while vegetation flourished, the enhanced soil expanded, water being desalinized, the lake larger in the interstadial period, particularly that in the first pollen assemblage I ( 130 -92 ka BP) and the pollen assemblage IV (56.2 -49 ka BP) in the duration of sedimentation when the plant diversity increased. In addition to the grassland vegetation in the basin, on the wetlands around the lake the plant was growing quite flonrishing, which demonstrated that the two periods were the most enhanced summer monsoon circulation with more adequate rainfall and the forest expanding fast in the mountains. The river flow was incresing and salt lake became desaltinized. The emergent grasses were growing at the edge of the marsh in the lake area. In particular in 49 ka BP ago or so, coniferous forest was growing associated with mountain cedar. Thus it suggested that the place was affected by the

  5. Desert-steppe migration on the Loess Plateau at about 450 kaBP%黄土高原450kaBP前后荒漠草原大迁移研究

    Institute of Scientific and Technical Information of China (English)

    赵景波

    2005-01-01

    According to the field investigation, observation by an electronic microscope and x-ray identification and chemical analysis, desert-steppe migration in the Loess Plateau at about 450 kaBP was studied. The data show that gypsum illuvial horizon indicating the desert-steppe environment developed in the early stage of the formation of the fifth layer loess in Shaoling tableland in Chang'an and Bailu tableland in Xi'an of Shaanxi are situated in the southern Loess Plateau. This indicates that remarkable drying occurred, a large-scope migration of desert steppe took place toward south and the climate zone migrated 5 degrees in latitude to south which is the largest migration range indicated by geochemical indexes. The desert-steppe and more wild environment distributed widely on the Loess Plateau at that time. The development of gypsum also indicates that the climate changed at 450 kaBP from monsoon climate to nonmonsoon climate in the Loess Plateau, and the region was not affected by summer monsoon and was in the cold and dry environment of nonmonsoon climate. Annual mean precipitation was about 200 mm, 400 mm less at that time than at present.

  6. First calibration results of Jason-2 and SARAL/AltiKa satellite altimeters from the Qianli Yan permanent Cal/Val facilities, China

    Science.gov (United States)

    Yang, Lei; Zhou, Xinghua; Mertikas, S. P.; Zhu, Lin; Yang, Long; Lei, Ning

    2017-06-01

    This work presents the first calibration results for the Jason-2 and the SARAL/AltiKa altimetric missions by using the permanent calibration facilities on the Qianli Yan islet (China). Qianli Yan is located in the Yellow Sea and only ∼3 km from the Jason-2 and SARAL/AltiKa crossover point. Analysis of the Jason-2 and SARAL/AltiKa waveform data and geophysical data over the Qianli Yan calibration area has proven that the altimeters and microwave radiometers are not contaminated by the mainland or the islet. The accuracies of the regional geoid model, provided by the First Institute of Oceanography (FIO), State Oceanic Administration of China, and the DTU10 MSS model were assessed by a GNSS buoy experiment. The results indicated that the FIO model is suitable for altimeter calibration in the Qianli Yan area. From the observations and the geoid model, the absolute biases for the Jason-2 and SARAL/AltiKa altimeters (2013-2014) were determined as 21.0 ± 5.9 and -44.0 ± 7.3 mm, respectively. The 2 years' results indicated that the Jason-2 bias had no trend. However, the SARAL/AltiKa bias presented a downward trend that was more stable in 2014 than in 2013. The Qianli Yan results are consistent with those determined by other international dedicated calibration sites and crossover analysis.

  7. The WAIS-Divide deep ice core WD2014 chronology – Part 2: Methane synchronization (68–31 ka BP and the gas age-ice age difference

    Directory of Open Access Journals (Sweden)

    C. Buizert

    2014-08-01

    Full Text Available The West Antarctic Ice Sheet (WAIS-Divide ice core (WAIS-D is a newly drilled, high-accumulation deep ice core that provides Antarctic climate records of the past ∼68 ka at unprecedented temporal resolution. The upper 2850 m (back to 31.2 ka BP have been dated using annual-layer counting. Here we present a chronology for the deep part of the core (67.8–31.2 ka BP, which is based on stratigraphic matching to annual-layer-counted Greenland ice cores using globally well-mixed atmospheric methane. We calculate the WAIS-D gas age-ice age difference (Δage using a combination of firn densification modeling, ice flow modeling, and a dataset of δ15N-N2, a proxy for past firn column thickness. The largest Δage at WAIS-D occurs during the last glacial maximum, and is 525 ± 100 years. Internally consistent solutions can only be found when assuming little-to-no influence of impurity content on densification rates, contrary to a recently proposed hypothesis. We synchronize the WAIS-D chronology to a linearly scaled version of the layer-counted Greenland Ice Core Chronology (GICC05, which brings the age of Dansgaard-Oeschger (DO events into agreement with the U/Th absolutely dated Hulu speleothem record. The small Δage at WAIS-D provides valuable opportunities to investigate the timing of atmospheric greenhouse gas variations relative to Antarctic climate, as well as the interhemispheric phasing of the bipolar "seesaw".

  8. Precise dating of East-Asian-Monsoon D/O events during 95―56 ka BP: Based on stalagmite data from Shanbao Cave at Shennongjia, China

    Institute of Scientific and Technical Information of China (English)

    XIA ZhiFeng; KONG XingGong; JIANG XiuYang; CHENG Hai

    2007-01-01

    Based on 23 U/Th analyses and 532 oxygen isotopic data, an averaged 80-a stalagmite oxygen isotopic composition series was established through 95 to 56 thousand years before present (ka BP) from two speleothems in Shanbao Cave, Shennongjia, central China. Shanbao Cave record (referred to as SB record) replicates well with Hulu Cave record, extending the characteristics of millennial oscillations in East-Asian-Summer-Monsoon (EASM) to the past 95 ka. The trend of the SB record generally follows mid-July solar insolation at 65°N, suggesting that mid-high northern latitude insolation, in the first order, controls changes of EASM intensity. Millennial oscillations of EASM recorded in the stalagmites are well related to the Greenland interstadials referred to as Dansgaard/Oeschger (D/O) events from 1 to 22, indicating that rapid ocean-atmosphere reorganization in North Atlantic has a remote effect in EASM. The well-dated D/O events by stalagmites probably provide an absolute calibration for chronologies of Greenland ice cores. The timings of D/O events in the SB record are different variously from those in Greenland ice cores. For D/O 19 and 20, the age offsets between the stalagmites' and the Greenland ice cores' record are significant, larger than the uncertainties of uranium-series dating. The two events in the SB record are younger than those in North GRIP time scale by 1―2 ka, and older than the counterparts in GISP2 by approximately 3―4 ka. A comparison between the SB and Brazil stalagmite record shows an anti-phase relation in millennial-scale monsoon precipitation between the two localities. This supports a mode for the coupled ocean-atmosphere "See-saw".

  9. Precise dating of East-Asian-Monsoon D/O events during 95―56 ka BP: Based on stalagmite data from Shanbao Cave at Shennongjia, China

    Institute of Scientific and Technical Information of China (English)

    2007-01-01

    Based on 23 U/Th analyses and 532 oxygen isotopic data, an averaged 80-a stalagmite oxygen isotopic composition series was established through 95 to 56 thousand years before present (ka BP) from two speleothems in Shanbao Cave, Shennongjia, central China. Shanbao Cave record (referred to as SB record) replicates well with Hulu Cave record, extending the characteristics of millennial oscillations in East-Asian-Summer-Monsoon (EASM) to the past 95 ka. The trend of the SB record generally follows mid-July solar insolation at 65°N, suggesting that mid-high northern latitude insolation, in the first or- der, controls changes of EASM intensity. Millennial oscillations of EASM recorded in the stalagmites are well related to the Greenland interstadials referred to as Dansgaard/Oeschger (D/O) events from 1 to 22, indicating that rapid ocean-atmosphere reorganization in North Atlantic has a remote effect in EASM. The well-dated D/O events by stalagmites probably provide an absolute calibration for chro- nologies of Greenland ice cores. The timings of D/O events in the SB record are different variously from those in Greenland ice cores. For D/O 19 and 20, the age offsets between the stalagmites’ and the Greenland ice cores’ record are significant, larger than the uncertainties of uranium-series dating. The two events in the SB record are younger than those in North GRIP time scale by 1―2 ka, and older than the counterparts in GISP2 by approximately 3―4 ka. A comparison between the SB and Brazil stalag- mite record shows an anti-phase relation in millennial-scale monsoon precipitation between the two localities. This supports a mode for the coupled ocean-atmosphere "See-saw".

  10. 天山乌鲁木齐河源区3.6 ka BP以来的植被变化和环境变迁:以大西沟剖面为例%Vegetation Changes and Environmental Evolution in the Urumqi River Head,Central Tianshan Mountains Since 3.6 ka BP:a Case Study of Daxigou Profile

    Institute of Scientific and Technical Information of China (English)

    张芸; 孔昭宸; 杨振京; 阎顺; 倪健

    2004-01-01

    A relatively high resolution pollen record and data of loss of ignition (LOI), grain size and susceptibility of the Daxigou profile in the head area of the Urumqi River, central Tianshan Mountains,revealed new information about vegetation changes and environmental evolution since 3.6 ka BP. Results showed that from 3.6 ka BP to present, climate was unstable with multi-changes of warming-cooling and wetting-drying. From ca. 3.6 to 3.2 ka BP, climate was warmer and more humid than today. Climate changed to cooler and drier between ca. 3.2 and 2.0 ka BP, coinciding with a glacier advance in the head area of the Urumqi River. From ca. 2.0 to 1.4 ka BP, climate became warmer and more humid again. From ca. 1.4 to 0.5 ka BP temperature and humidity went on increasing and a period of Climatic Optimum since 3.6 ka BP might occur. A few limnetic hydrophytes pollen are counted for all zones, indicating a freshwater habitat since 3.6 ka BP in this region. Based on synthetically analysis of ecological characteristics and dispersal of spruce pollen, the abundance of Picea is influenced by treeline moving upward, valley wind and glacier ablation. Statistics of charcoal concentration and susceptibility further suggest that fires may have occurred in this region since 0.5 ka BP and the peak value of charcoal might be related to human activities.%天山乌鲁木齐河源区大西沟剖面孢粉鉴定结果表明:在3.6~3.2 ka BP,该区气候较今温暖湿润;在3.2~2.0 ka BP,气候变为寒冷干燥,这一时期乌鲁木齐河源地区曾出现一次冰进;在2.0~1.4 ka BP,气候又转为暖湿;在1.4~0.5 ka BP,出现了3.6 ka BP以来气候最适宜的时期.整个剖面自下而上都有一定量的淡水水生植物出现,这反映了该剖面3 ka BP以来一直处于淡水沼泽的环境中.通过对云杉属生态习性、传播特性等综合分析,认为剖面中的云杉丰值可能与林线上移、山谷风搬运以及冰川退缩等有一定的相关性.通过

  11. Vegetation and Climate Changes in Patagonia (46°S) during the Last 20 kyr cal. BP from South East Pacific MD 07 3088 Core

    Science.gov (United States)

    Montade, V.; Combourieu Nebout, N.; Siani, G.; Michel, E.; Kissel, C.; Carel, M.; Mulsow, S.

    2010-12-01

    The Chilean Patagonia (41°S to 56°S) crossed by the Andes from north to south represents a critical topographic constraint on atmospheric and oceanic systems, and the only continental landmass intercepting the entire Southern Westerlies Wind (SHW) belt in southern hemisphere. Therefore, the southern Chile is a key-area to study the paleoclimate changes and, to understand the synoptic scale ocean-atmospheric circulation systems of the mid to high southern latitudes. However, several questions remain partly unsolved: Is there abrupt reversal event during the Last Glacial-Interglacial transition (LGIT)? Is there a shift or an intensification of the SHW? When begin the Holocene onset? What are the inter or intra hemispheric climatic links? In this aim, we present here a detailed pollen record from the deep-sea core MD 07 3088 (46°04’S; 76°05’W, 1536 m) near Taitao peninsula, taken during the “Pachiderme” cruise (MD 159) within the IMAGES (International MArine Global changES) program (Kissel et al., 2007). The age model (Siani et al., in press) is based upon stable oxygen isotopes of planktonic foraminifera G. bulloïdes coupled to ten AMS 14C measurements performed on planktonic foraminifera and four tephrochronological markers attributed to the Hudson volcano (Haberle and Lumley, 1998). The pollen record expresses vegetation changes and thus climate variations during the last 20 kyr cal. BP. Several vegetation phases are observed during the LGIT and the Holocene onset: Before 18 kyr, the low diversity and pollen influx show the reduced vegetation due to the Patagonian Ice Cap extension and cold temperature. From 17.5 to 14.5 kyr, the diversity and pollen influx increase mark the vegetation development linked to the ice cap melting and temperature increase. From 14.5 to 12 kyr, the Astelia development illustrates the Magellanic Moorland extension and humid conditions linked to the SHW. Later 11.5 kyr, the forest diversification expresses the Holocene onset

  12. Evidence of the Pan-Lake Stage in the Period of 40- 28 ka B.P. on the Qinghai-Tibet Plateau

    Institute of Scientific and Technical Information of China (English)

    2000-01-01

    The Qinghai-Tibet plateau is one of major saline lake regions in China, where saline lakes are widespread and constitute an important object of researches on the palaeoclimatic change in the region. On the basis of comprehensive investigations of the evolution of the lake's surface and sediments on the plateau, the authors have further demonstrated the existence of a pan-lake stage (river and lake flooding stage) on the Qinghai-Tibet plateau during the period of about 40+- 28 ka B.P. and analyzed the palaeoclimatic characteristics of the pan-lake period and relationships between the ancient monsoons and the uplift of the plateau since the beginning of the Quaternary.

  13. The 9.2 ka event in Asian summer monsoon area: the strongest millennial scale collapse of the monsoon during the Holocene

    Science.gov (United States)

    Zhang, Wenchao; Yan, Hong; Dodson, John; Cheng, Peng; Liu, Chengcheng; Li, Jianyong; Lu, Fengyan; Zhou, Weijian; An, Zhisheng

    2017-06-01

    Numerous Holocene paleo-proxy records exhibit a series of centennial-millennial scale rapid climatic events. Unlike the widely acknowledged 8.2 ka climate anomaly, the likelihood of a significant climate excursion at around 9.2 cal ka BP, which has been notably recognized in some studies, remains to be fully clarified in terms of its magnitude and intensity, as well as its characteristics and spatial distributions in a range of paleoclimatic records. In this study, a peat sediment profile from the Dajiuhu Basin in central China was collected with several geochemical proxies and a pollen analysis carried out to help improve understanding of the climate changes around 9.2 cal ka BP. The results show that the peat development was interrupted abruptly at around 9.2 cal ka BP, when the chemical weathering strength decreased and the tree-pollen declined. This suggests that a strong drier regional climatic event occurred at around 9.2 cal ka BP in central China, which was, in turn, probably connected to the rapid 9.2 ka climate event co-developing worldwide. In addition, based on the synthesis of our peat records and the other Holocene hydrological records from Asian summer monsoon (ASM) region, we further found that the 9.2 ka event probably constituted the strongest abrupt collapse of the Asian monsoon system during the full Holocene interval. The correlations between ASM and the atmospheric 14C production rate, the North Atlantic drift ice records and Greenland temperature indicated that the weakened ASM event at around 9.2 cal ka BP could be interpreted by the co-influence of external and internal factors, related to the changes of the solar activity and the Atlantic Meridional Overturning Circulation (AMOC).

  14. Abrupt climate change of East Asian Monsoon at 130 kaBP inferred from a high resolution stalagmite δ18O record

    Institute of Scientific and Technical Information of China (English)

    JIANG Xiuyang; WANG Yongjin; KONG Xinggong; WU Jiangying; SHAO Xiaohua; XIA Zhifeng; CHENG Hai

    2005-01-01

    230Th ages and oxygen isotope data of a stalagmite from Shanbao Cave in Hubei Province characterize the East Asian Monsoon precipitation from 133 to127 ka. The decadal-scale high-resolution δ18O record reveals a detailed transitional process from the Penultimate Glaciation to the Last Interglaciation. As established with 230Th dates, the age of the Termination II is determined to be 129.5±1.0 kaBP, which supports the Northern Hemisphere insolation as the triggers for the ice-age cycles. In our δ18O record, the glacial/ interglacial fluctuation reaches about 4‰, almost the same level as in other Asian Monsoon cave stalagmite δ18O records. The transition of the glacial/interglacial period in our record can be recognized as four stepwise stages, among which, a rapid rise of monsoon precipitation follows the stage of "Termination II pause". The rapid rise is synchronous with the abrupt change of global methane concentration, which reflects that an increase in both Asian Monsoon precipitation and tropical wetland plays an important role in the global climate changes.

  15. Insights from a synthesis of old and new climate-proxy data from the Pyramid and Winnemucca lake basins for the period 48 to 11.5 cal ka

    Science.gov (United States)

    Benson, Larry; Smoot, J.P.; Lund, S.P.; Mensing, S.A.; Foit, F.F.; Rye, R.O.

    2013-01-01

    A synthesis of old and new paleoclimatic data from the Pyramid and Winnemucca lake basins indicates that, between 48.0 and 11.5·103 calibrated years BP (hereafter ka), the climate of the western Great Basin was, to a degree, linked with the climate of the North Atlantic. Paleomagnetic secular variation (PSV) records from Pyramid Lake core PLC08-1 were tied to the GISP2 ice-core record via PSV matches to North Atlantic sediment cores whose isotopic and(or) carbonate records could be linked to the GISP2 δ18O record. Relatively dry intervals in the western Great Basin were associated with cold Heinrich events and relatively wet intervals were associated with warm Dansgaard-Oeschger (DO) oscillations. The association of western Great Basin dry events with North Atlantic cold events (and vice versa) switched sometime after the Laurentide Ice Sheet (LIS) reached its maximum extent. For example, the Lahontan highstand, which culminated at 15.5 ka, and a period of elevated lake level between 13.1 and 11.7 ka were associated with cold North Atlantic conditions, the latter period with the Youngest Dryas event. Relatively dry periods were associated with the Bølling and Allerød warm events. A large percentage of the LIS may have been lost to the North Atlantic during Heinrich events 1 and 2 and may have resulted in the repositioning of the Polar Jet Stream over North America. The Trego Hot Springs, Wono, Carson Sink, and Marble Bluff tephras found in core PLC08-1 have been assigned GISP2 calendar ages of respectively, 29.9, 33.7, 34.1, and 43.2 ka. Given its unique trace-element chemistry, the Carson Sink Bed is the same as Wilson Creek Ash 15 in the Mono Lake Basin. This implies that the Mono Lake magnetic excursion occurred at approximately 34 ka and it is not the Laschamp magnetic excursion. The entrance of the First Americans into the northern Great Basin is dated to approximately 14.4 ka, a time when the climate was relatively dry. Evidence for human occupation of

  16. A compilation of Western European terrestrial records 60-8 ka BP: towards an understanding of latitudinal climatic gradients

    Science.gov (United States)

    Moreno, Ana; Svensson, Anders; Brooks, Stephen J.; Connor, Simon; Engels, Stefan; Fletcher, William; Genty, Dominique; Heiri, Oliver; Labuhn, Inga; Perşoiu, Aurel; Peyron, Odile; Sadori, Laura; Valero-Garcés, Blas; Wulf, Sabine; Zanchetta, Giovanni

    2014-12-01

    Terrestrial records of past climatic conditions, such as lake sediments and speleothems, provide data of great importance for understanding environmental changes. However, unlike marine and ice core records, terrestrial palaeodata are often not available in databases or in a format that is easily accessible to the non-specialist. As a consequence, many excellent terrestrial records are unknown to the broader palaeoclimate community and are not included in compilations, comparisons, or modelling exercises. Here we present a compilation of Western European terrestrial palaeo-records covering, entirely or partially, the 60-8-ka INTIMATE time period. The compilation contains 56 natural archives, including lake records, speleothems, ice cores, and terrestrial proxies in marine records. The compilation is limited to include records of high temporal resolution and/or records that provide climate proxies or quantitative reconstructions of environmental parameters, such as temperature or precipitation, and that are of relevance and interest to a broader community. We briefly review the different types of terrestrial archives, their respective proxies, their interpretation and their application for palaeoclimatic reconstructions. We also discuss the importance of independent chronologies and the issue of record synchronization. The aim of this exercise is to provide the wider palaeo-community with a consistent compilation of high-quality terrestrial records, to facilitate model-data comparisons, and to identify key areas of interest for future investigations. We use the compilation to investigate Western European latitudinal climate gradients during the deglacial period and, despite of poorly constrained chronologies for the older records, we summarize the main results obtained from NW and SW European terrestrial records before the LGM.

  17. 北半球72ka BP气候突变事件及其与Toba火山的关系%The Relation between the 72 ka BP Event and the Toba Super-eruption

    Institute of Scientific and Technical Information of China (English)

    吴帅男; 陈仕涛; 段福才

    2012-01-01

    The abrupt cooling event occurred about 72(the 72 ka Event) is the largest climate change during the last glacial period.At the same time a super-eruption of Toba volcano,the largest explosive eruption over the past two million years,erupted in northern Sumatra,with a Volcanic Explosivity Index of magnitude 8.It always deserves special attention for the relation between the 72 ka Event and the Toba Super-eruption.Therefore,an in-depth study of the 72 ka Event should be useful for further evaluating the environment effect of the eruption and refining the mechanism of the abrupt events during the last glacial period.Here,we make a systematic rewiew about the research achievements from different fields such as marine cores,ice cores,stalagmites,loess,lakes and so on.These records showed different expressions on the cold event occurred about 72 ka BP and/or the Toba eruption and their relations.Based on the timing of this cold event and the Toba eruption,and the operating mechanism of the volcanic eruption on climate,the eruption has substantial impact on climate.This impact is well documented by Greenland ice core records,and further supported by climate models.Nevertheless,marine core records in low latitudes did not exhibit an obvious climate change around the super eruption,and,at least,the amplitude of the variation is not strong as one in the high latitude.Also,paleontological evidences show that the Toba eruption did not make a catastrophic effect on the living environment.So,the relation between the 72 ka Event and the Toba Super-eruption is still being hotly debated.The further progress depends not only on developing resolution and chronological precision of climate records,but also on detecting the evidence of volcanic eruptions as well.%72 ka BP左右的强降温事件是末次冰期最大的气候突变事件,且同时期发生了第四纪以来最强的火山喷发———Toba火山喷发,后者在此次强降温事件中扮演着什么角色一直

  18. The northernmost and latest occurrence of the fossil porcupine (Hystrix brachyura vinogradovi Argyropulo, 1941) in the Altai Mountains in the Late Pleistocene (ca. 32,000-41,000 cal BP)

    Science.gov (United States)

    Kuzmin, Yaroslav V.; Kosintsev, Pavel A.; Vasiliev, Sergei K.; Fadeeva, Tatyana V.; Hodgins, Gregory W. L.

    2017-04-01

    Several new finds of the Late Pleistocene porcupine (Hystrix brachyura vinogradovi) in the Altai Mountains of southern Siberia and the Urals occur far north of previously assigned range for porcupine. These finds have necessitated a renewed study of this species's chronology and spatial distribution. We conclude that the oldest records of this porcupine in the Ural Mountains date to MIS 5e, and its geographic range possibly included also the Altai at that time. Directly radiocarbon-dated porcupine bones in the Altai fall in MIS 3 (ca. 32,000-41,000 cal BP). It is the northernmost record of this species and the youngest find outside its current geographic range.

  19. A high-resolution 14C chronology from the Cormor alluvial megafan (Tagliamento glacier, NE Italy) for the reconstruction of Alpine glacier activity during 50-20 ka BP

    Science.gov (United States)

    Hippe, Kristina; Fontana, Alessandro; Hajdas, Irka; Ivy-Ochs, Susan

    2016-04-01

    During the Last Glacial Maximum (LGM), the Cormor alluvial megafan was delivering large amounts of glacial sediment from the Alpine Tagliamento glacier onto the southern Alpine foreland basin. Rate and character of sedimentation were primarily controlled by the glacier activity and, thus, by variations in climate. To gain a better understanding of the late-Pleistocene sedimentary processes in the Alpine foreland alluvial megafans and their response to climate changes, we have performed high-resolution radiocarbon dating of a drilling core (PNC1, 65 m deep) located in the distal sector of the Cormor alluvial megafan, near the Marano Lagoon [1]. The stratigraphic sequence of the core is characterized by an alternation of silt and clay deposits with the intercalation of several peaty and humic horizons. These organic layers (5-40 cm thick) correspond to phases of locally inactive fluvioglacial sedimentation, allowing plant remains to be accumulated at the surface. A series of about 55 peat samples between 33 to 4 m of depth with sample distances of few cm-dm were dated with radiocarbon. Half of these samples were separated into various fractions in order to check for systematic age differences with regard to the size and/or type of the organic particles. Additionally, the influence of sample pre-treatment was evaluated by using the ABA treatment as well as two different ABOX treatment protocols for each sample fraction. While no systematic age differences with size and/or type of the organic particles was observed, some samples indicate a shift towards younger ages after ABOX treatment. Moreover, deposits containing old carbon (too old ages) were observed suggesting that a careful approach and high-resolution sampling is an imperative in obtaining accurate chronologies. Radiocarbon ages obtained for the PNC1 record range from ~50-20 cal ka BP and provide a detailed chronology of the pre-LGM and LGM fluvioglacial sequence. Due to the immediate connection of the Cormor

  20. 最近12 000年来青藏高原植被的时空分布%Temporal-Spatial Distribution of Vegetation in the Qinghai-Xizang Plateau During the Past 12 ka BP

    Institute of Scientific and Technical Information of China (English)

    唐领余

    2002-01-01

    青藏高原30个点湖泊的孢粉记录综合研究显示: 在进入全新世之前(12 ka BP以前),除最东南部外,高原从东到西均发育为荒漠草原植被.全新世早期(12.0-9.0 ka BP)高原东南部(104°-98° E)为落叶阔叶林/针阔叶混交林; 中部(98°-92° E)为草甸或灌丛草甸,再向西至80° E左右为草原植被; 全新世中期(9.0-3.2 ka BP)高原由东向西古植被依次发育为针阔混交林和硬叶阔叶林(104°-98° E)→针阔混交林(98°-94° E)→灌丛草甸(94°-92° E)→草原(92°-80° E);全新世晚期(3.2 ka BP以后)由东向西古植被依次为硬叶阔叶林→针阔混交林→草甸→草原→荒漠.%Comprehensive studies on the basis of pollen records from lake cores at 30 sites in the Qinghai-Xizang Plateau have been used to reconstruct temporal-spatial distributions of Holocene vegetations. Before the Holocene (prior to 12.0 ka BP) desert steppe vegetation was developed from the east to the west in the most parts of the Plateau, with a few exceptions in the extreme southeastern appeared. During the early Holocene (12.0-9.0 ka BP),deciduous broad-leaved forest/conifer and broad-leaved deciduous mixed forest were distributed in the east of Plateau (104°-98° E). Meadows or shrub meadow appeared in the middle of the Plateau (98°-92° E). Farther west to about 80° E, a steppe landscape was present. During the middle Holocene (9.0-3.2 ka BP), the palaeovegetations were sequentially conifer and broad-leaved deciduous mixed forest and sclerophyllous broad-leaved forest (104°-98° E)-conifer and broad-leaved deciduous mixed forest (98°-94° E)-shrub meadow (94°-92° E)-steppe (92°-80° E). During the late Holocene (after 3.2 ka BP), the palaeovegetations were sequentially sclerophyllous broad-leaved forest-conifer and broad-leaved deciduous mixed forest-meadow-steppe-desert from east to west of the Plateau.

  1. Climate-driven changes in water level: a decadal scale multiproxy study recording the 8.2-ka event and ecosystem responses in Lake Sarup (Denmark)

    DEFF Research Database (Denmark)

    Hansen, Rikke Bjerring; Olsen, Jesper; Jeppesen, Erik

    2013-01-01

    A two-stage change in lake level during the 8.2-ka event was identified in Lake Sarup, Denmark (55A degrees N), using a multiproxy approach on precise radiocarbon wiggle-matched annually laminated sediments deposited 8740-8060 cal. yr BP. Changes in delta C-13 and delta O-18 indicated closed lake...... hydrology driven by precipitation. The isotopic, sedimentary and plant macrofossil records suggested that the lake level started to decrease around 8400 cal. yr BP, the decrease accelerating during 8350-8260 before an abrupt increase during 8260-8210. This pattern shows that the climate anomaly started...

  2. Paleopathological description and diagnosis of metastatic carcinoma in an Early Bronze Age (4588+34 Cal. BP) forager from the Cis-Baikal region of Eastern Siberia.

    Science.gov (United States)

    Lieverse, Angela R; Temple, Daniel H; Bazaliiskii, Vladimir I

    2014-01-01

    Extensive osteolytic and osteoblastic lesions were observed on the skeletal remains of an adult male excavated from an Early Bronze Age cemetery dated to 4556+32 years BP, located in the Cis-Baikal region of Siberia (Russian Federation). Lytic lesions ranged in size from several mm to over 60 mm in diameter and had irregular, moth-eaten borders. Many of these lesions destroyed trabecular bone, though a hollowed shell of cortical bone often remained observable. Radiographic analysis revealed numerous lytic lesions within trabecular bone that had not yet affected the cortex. Blastic lesions were identified as spiculated lines, bands, or nodules of mostly immature (woven) bone formed at irregular intervals. Anatomical elements with the greatest involvement included those of the axial skeleton (skull, vertebrae, sacrum, ribs, and sternum) as well as proximal appendicular elements (ossa coxae, proximal femora, clavicles, scapulae, and proximal humeri). Osteocoalescence of destructive foci was observed on the ilium and frontal bone, with the largest lesion found on the right ilium. Differential diagnoses include metastatic carcinoma, mycotic infections, tuberculosis, Langerhan's cell histiocytosis, and multiple myeloma. Based on lesion appearance and distribution, age and sex of the individual, as well as pathogen endemism, the most likely diagnostic option for this set of lesions is metastatic carcinoma. The age and sex of this individual and appearance of the lesions may reflect carcinoma of the lung or, possibly, prostate. This represents one of the earliest cases of metastatic carcinoma worldwide and the oldest case documented thus far from Northeast Asia.

  3. Timing of wet episodes in Atacama Desert over the last 15 ka. The Groundwater Discharge Deposits (GWD) from Domeyko Range at 25°S.

    Science.gov (United States)

    Sáez, Alberto; Godfrey, Linda V.; Herrera, Christian; Chong, Guillermo; Pueyo, Juan J.

    2016-08-01

    A chronologically robust reconstruction of timing and dynamics of millennial time scale wet episodes encompassing the entire Atacama Desert during the last 15 ka has been constructed. To accomplish this, a new composite paleoclimatic record from Groundwater Discharge Deposits (GWD) in the Sierra de Varas (Domeyko Range, southern Atacama in Chile at 25°S) has been compiled and compared with other published paleohydrologic records from the Atacama region. In Sierra de Varas (SV), three millennial timescale wet climate phases have been characterized: around 14.5 ka cal BP, 12.2-9.8 ka cal BP, and 4.7 ka cal BP to the present day. These wet phases are interpreted from intervals of GWD facies formed during periods when the springs were active. GWD facies include: (1) black organic peat, rooted mudstones and sandstones formed in local wetland environments, and (2) gypsum-carbonate rich layers formed by interstitial growth. GWD intervals alternate with gravelly alluvial material deposited during arid phases. A trend towards less humid conditions during the Late Holocene wet episode characterizes GWD sedimentary series in Sierra the Varas, suggesting the onset of a dry episode over the last few centuries. Around 0.7 ka BP a very short wet episode is recorded in the central part of the desert suggesting this was the time of maximum humidity for the entire late Holocene wet period. A brief arid phase occurred between 1.5 and 2.0 ka BP indicated by the absence of GWD in the Domeyko Range. The paleoclimatic reconstruction encompassing the entire Atacama region shows that both the intensity and occurrence of wetter conditions were governed mainly by the distance to the source of moisture, and secondarily by the elevation of the sites. In the northern Atacama (16-20°S), four wet phases fed by N-NE summer monsoon precipitations have been proposed: Tauca phase (18-14 ka cal BP) and Coipasa phase (13-10 ka cal BP) during the Late Glacial, followed by Early Holocene and Late

  4. A coccolithophore based view on paleoenvironmental changes in the open ocean mid-latitude North Atlantic between 130 and 48ka BP with special emphasis on MIS 5e

    DEFF Research Database (Denmark)

    Schwab, C.; Kinkel, Hanno; Weinelt, M.

    2013-01-01

    past changes in productivity and hydrography from a new sediment core (MD08-3179Cq) taken in the open ocean mid-latitude North Atlantic in the vicinity of the Azores Current System. Concomitant to the reorganizations of environmental conditions in the North Atlantic between 130 and 48ka BP, changes......As oceanographic changes in the North Atlantic are known to modulate global climate, they are key to the understanding of past and future climate changes. Especially the mid-latitudes of the open ocean North Atlantic may be of interest, regarding the large area covered. We therefore reconstructed...

  5. Evolution of Jilantai Salt Lake, Inner Mongolia in the last 13.8 ka%13.8ka以来内蒙古吉兰泰盐湖的演化过程

    Institute of Scientific and Technical Information of China (English)

    于志同; 刘兴起; 王永; 葛兆帅; 潘存峰; 杨波

    2012-01-01

    Evolution of Jilantai Salt Lake in the last 13.8 ka was reconstructed based on the analysis of evaporate minerals, carbonate minerals and detrital minerals from the core JLT-20I0. The lake water was fresh or slightly salty between 13.8 and 11.7 cal ka BP. The lake began to shrink between 11.7 and 10.2 cal ka BP, and then it entered into the lagoon stage. Sulfate deposition occurred in Jilantai Salt Lake between 10.2 and 5.5 cal ka BP, meanwhile, from 9.0 to 8.2 cal ka BP there existed a significant desalination process. The lake reached full chloride deposition stage between 3.7 and 2.0 cal ka BP, and a short and obvious desalt period occurred between 2.0 and 1.7 cal ka BP. Overall, evaporate minerals appeared just at the beginning of the Holocene when temperature increased relative to the late glacial. As the regional arid climate continually affecting the area, Jilantai Salt Lake gradually shrank and salinized.%通过系统分析吉兰泰盐湖JLT-2010孔蒸发盐类矿物、碳酸盐矿物、碎屑岩矿物等,结合AMS14C测年获得的年代序列,研究该湖13.8 ka以来的演化过程.结果表明:吉兰泰盐湖13.8-11.7 calka BP期间水体较淡;11.7-10.2 calkaBP期间湖泊开始萎缩、咸化,进入咸水湖阶段;10.2-5.5 cal ka BP期间湖泊进入硫酸盐沉积阶段,其中9.0-8.2 cal kaBP经历了一个明显的淡化过程;5.5 cal ka BP以来,湖泊成盐作用进一步加强,由前期的硫酸盐沉积转变为氯化物沉积,其中3.7-2.0 cal ka BP达到全面氯化物沉积阶段,2.0- 1.7 cal ka BP又经历了一个短暂而明显的淡化过程;目前,该盐湖已进入干盐湖发展阶段.总体而言,吉兰泰盐湖蒸发盐类矿物主要是在全新世增温的背景条件下逐步萎缩形成的,由于区域性干旱气候的持续影响,吉兰泰盐湖逐步萎缩、咸化,进而析盐.

  6. Discovery of a large area of ice-wedge networks in Ordos:Implications for the southern boundary of permafrost in the north of China as well as for the environment in the latest 20 kaBP

    Institute of Scientific and Technical Information of China (English)

    CUI Zhijiu; YANG Jianqiang; ZHANG Wei; ZHAO Liang; XIE Youyu

    2004-01-01

    The delineation of the southern boundary of the latitudinal permafrost in the north of China in the period of late Pleistocene, i.e. the last glaciation maximum (LGM), has been hampered for two reasons. Firstly, previous studies were limited to the eastern part of the north of China, and, secondly, the ages of the permafrost had not been determined systematically. In this paper, we suggest that the southern boundary of the high latitudinal permafrost in the north of China is bounded by approximately 38-40°N (eastern part) and 37-39°N (western part) lines of latitude based on our interpretation of periglacial phenomena and their implication to the environment during the late Pleistocene, and this southern boundary is plotted for the first time. Also, we reconstruct the migration of the southern latitudinal permafrost boundary and the environment after LGM. It is proposed that two cold stages occurred in the LGM at 26 kaBP and 23-13 kaBP, when the annual mean temperature was 8-12℃ lower than at present.

  7. 南海低纬地区15kaBP以来高分辨率孢粉记录及植被、气候演变%High-resolution palynological record and evolution of vegetation and climate in the low latitude of the South China Sea since 15 kaBP

    Institute of Scientific and Technical Information of China (English)

    张玉兰; 彭学超; 赵晶

    2011-01-01

    本文依据南海低纬地区SA09-090孔高分辨率的孢粉记录,从下至上划分了4个孢粉组合带,从孢粉成分的变化,重建了15kaBP以来的植被和气候变化历史.研究结果发现:15.0-12.5kaBP期间研究区花粉主要来自当地出露的陆架,揭示出出露的陆架植被类型是以热带低山雨林和低地雨林为主.海滨地区生长着茂盛的红树林,当时气温比现在低一些,但无明显变干现象.12-10kaBP期间植被中低山雨林花粉增多,红树植物花粉减少,这说明此时海平面上升,气温也回升,花粉源区变远.全新世时(10kaBP至今),花粉主要来源于加里曼丹岛和周围岛屿,植被以低山雨林和海滨红树植物为主,但花粉浓度大幅降低,这种花粉浓度降低说明海平面继续上升,研究区距离花粉源区越来越远.全新世中期时为热、湿的气候环境,后期与现今相近.%Based on the high resolution pollen record at the Core SA09-090, which was in the low latitude of the South China Sea, four pollen zones are distinguished in an ascending order. According to the pollen composition in each zone, the vegeta-tion evolution and climate change since lSkaBP is reconstructed. The research shows that at the stage of 15.0-12.5kaBP, the pollen in the research area mainly came from the continental shelf when it was above the sea level. This indicates that the vegetation on the continental shelf that was above the sea level was mainly tropical low-mountain rainforest and lowland rainforest. Many mangroves lived in the coastal area. The temperature was a little lower than today's, but there was no clear evidence of aridity. At the stage of 12-10kaBP, the amount of pollen from lowland rainforest increased, and the amount of pollen from the mangroves decreased. This indicates that the sea level rose in that period, and the temperature rose, too. The pollen source became far away. At the Holocene (10kaBP to now), the pollen mainly came from Borneo and the

  8. Introduktion til CALS

    DEFF Research Database (Denmark)

    Kirkby, Phillip; Larsen, Michael Holm; Langer, Gilad

    1997-01-01

    Denne rapport er udarbejdet af CALS Center Danmark og er en generel introduktion til CALS. Rapportenbeskriver indholdet i CALS ud fra fire synsvinkler: visionen i CALS, principper i CALS, det tekniske indhold,og organiseringen af CALS internationalt og i Danmark. Der redegøres for historien bag...... CALS, hvorfor der er behov for CALS og hvordan CALS standarderne ermed til at gøre information uafhængig af den teknologi, som benyttes. Forskellen mellem syntaktisk ogsemantisk standard defineres, og det beskrives, hvorledes CALS kan fungere som en "enabler" forrestrukturering af forretningsprocesser....... Endelig uddybes de videre perspektiver for CALS, hvordan CALSkan føre til nye dynamiske organisationsformer, som fungerer fuldstændig virtuelt på tværs af geografi og tid.Nye begreber som "Extended Enterprise", "Agile manufacturing" og "Virtuelle virksomheder" introduceres. Dokumentet afsluttes med...

  9. Consolidating BPR with CALS

    DEFF Research Database (Denmark)

    Larsen, Michael Holm; Leinsdorff, Torben; Madsen, Claus;

    1999-01-01

    the likelihood of BPR success. Firstly, CALS contributes to process orientation and process organising in a BPR project. This is partly because CALS satisfies the increased information need of the process team members and partly because CALS breaks down information-based barriers. Secondly, CALS contributes...

  10. Palaeoenvironmental changes from pollen record in deep sea core PC-1 from northern Okinawa Trough, East China Sea during the past 24 ka

    Institute of Scientific and Technical Information of China (English)

    XU HongYan; CHANG FengMing; LUO YunLi; SUN XiangJun

    2009-01-01

    A pollen record of core PC-1 from the northern Okinawa Trough, East China Sea (ECS), provides in-formation on vegetation and climate changes since 24 cal. kaBP. A total of 103 samples were palyno-logically analyzed at 8 cm intervals with a time resolution of 230 a. Four pollen zones are recognized: zone I (812-715 cm, 24.2-21.1 cal. kaBP), zone II (715-451 cm, 21.1 -15.2 cal. kaBP), zone Ⅲ (451 -251 cm, 15.2-10.8 cal. kaBP), zone Ⅳ (251-0 cm, 10.8-0.3 cal. kaBP), corresponding to Late MIS 3, Last Glacial Maximum (LGM), deglaciation and Holocene, respectively. The LGM is characterized by the dominance of herbs, mainly Artemisia, and high pollen influx, implying an open vegetation on the ex-posed continental shelf and e cool and dry climate. The deglaciation is a climate warming stage with Pinus percentage increased and Artemisia percentage decreased and a rapid sea-level rise. The Holo-cene is characterized by predominance of tree pollen with rapid increase in Castanea-Castanopsis in-dicating the development of mixed evergreen and deciduous broad-leaved forest and a warm, humid climate. Low pollen influx during the Holocene probably implies submergence of the continental shelf and retreat of the pollen source area. The vegetation indicated by pollen assemblage found in this up-per zone is consistent with the present vegetation found in Kyushu, Japan. Originating from the humid mountain area of North Luzon of the Philippines, Tasmania and New Zealand, Phyllocladus with spo-radic occurrence throughout PC-1 core probably suggests the influence of Palaeo-Kuroshio Current or intense summer monsoon. The observed changes in Pinus and Herbs percentage indicate fluctuations of the sea level, and high Pinus percentage corresponds to high sea level. Spectrum analysis of the pollen percentage record reveals many millennial-scale periodicities, such as periodicities of 6.8, 3.8, 2.2, 1.6 ka.

  11. Evolution Process of Land Desertification around Qinghai Lake since 32 ka BP Reflected by Sediment Grain-size Features%风成沉积物粒度特征及其反映的青海湖周边近32ka以来土地沙漠化演变过程

    Institute of Scientific and Technical Information of China (English)

    胡梦珺; 李森; 高尚玉; 张登山

    2012-01-01

    湖东地区是青海湖周边土地沙漠化面积最大、程度最为严重的区域。选取青海湖湖东种羊场附近高度约为10m的风蚀残丘(大水溏剖面)为研究对象,结合高密度采样和光释光测年,在对风成沉积物的粒度组成、粒度参数及粒度敏感指标进行分析的基础上,重建了32ka以来青海湖周边的土地沙漠化演变过程。结果表明,32kaBP以来青海湖周边土地沙漠化经历了末次冰期间冰阶(32~23.4kaBP)的固结成壤期、末次冰期冰盛期(23.4~15kaBP)的快速扩张期、末次冰期冰消期(15~10.4kaBP)的缓慢减小期和全新世(10.4kaBP至今)的快速缩小期4个阶段。%Land desertification in the east coast is the most serious and has the largest area among areas a- round the Qinghai Lake. in this paper we took an aeolian sediment section at Dashuitang (QDST section) in the east coast of the Qinghai Lake as the research object to reconstruct the evolution process of land deserti- fication around Qinghai Lake during the last 32 ka by the environment evolution information extracted from grain size composition, grain size parameters and grain size sensitive index. Results show that the evolution process of land desertification in the study area can be divided into four stages since 32 ka BP. In the inter- glacial period of the Last Glacial Stage from 32 ka BP to 23.4 ka BP, the climate was humid with weak wind, and sand dunes experienced being fixed and pedogenic process. So the area of land desertification land during this period was the smallest. From 23.4 ka BP to 15.2 ka BP, the climate was cold-dry with strong wind, and the intense aeolian activities activated sand dunes. Land desertification area during this period was the biggest in the past 32 ka. In 15-10.4 ka BP, land desertification area slowly decreased under the background of increasing temperature and humidity. Since 10.4 ka BP, aeolian activities weakened

  12. Black carbon record of the wildfire history of western Sichuan Province in China over the last 12.8 ka

    Science.gov (United States)

    Sun, Weiwei; Zhang, Enlou; Shen, Ji; Chen, Rong; Liu, Enfeng

    2016-01-01

    Wildfire is recognized as a critical Earth system process which affects the global carbon cycle, atmospheric chemistry, and ecosystem dynamics. Estimating the potential impact of future climate change on the incidence of fire requires an understanding of the long-term interactions of fire, climate, vegetation, and human activity. Accordingly, we analyzed the black carbon content and the pollen stratigraphy of sediments spanning the past 12.8 ka from Lake Muge Co, an alpine lake in western Sichuan Province, in order to determine the main factors influencing regional fire regimes. The results demonstrate that wildfires occurred frequently and intensively during the late deglaciation and the early Holocene when the regional vegetation was dominated by deciduous forests. Wildfire occurrence decreased significantly during the Holocene climatic optimum between 9.2 and 5.6 cal ka BP. Overall, the wildfire history of western Sichuan Province is similar to that of the Chinese Loess Plateau and of East Asia as a whole, suggesting that regional-scale fires depended mainly on changes in the intensity of the Asian summer monsoon. In addition, the fire regime of western Sichuan Province may have been influenced by the establishment of human settlement and agriculture in western Sichuan Province and the southeastern Tibetan Plateau after about 5.5 cal ka BP, and by an intensification of cereal cultivation coupled with population expansion in southwestern China during the last two millennia.

  13. Ecological Regime Shifts in Lake Kälksjön, Sweden, in Response to Abrupt Climate Change Around the 8.2 ka Cooling Event

    DEFF Research Database (Denmark)

    Randsalu-Wendrup, L.; Conley, D.J.; Snowball, I.;

    2012-01-01

    periphytic to planktonic diatom dominance over a 250-year period and a gradual diversification of the periphytic community that spanned c. 150 years. Rapid climate warming following the 8.2 ka event likely caused these changes and both regime shifts are examples of externally driven abrupt ecological change......A detailed diatom record from Lake Ka¨ lksjo¨ n, westcentral Sweden, reveals two periods of abrupt ecological change correlative with the 8.2 ka cooling event. Using a combination of abrupt step changes and piece-wise linear regressions, the diatom data were analyzed for change points over time...... increase in nutrient supply to the lake. The second event was characterized by a substantial shift within the planktonic diatom community from taxa indicative of colder conditions to those indicating warm over 5–10 years at c. 7850 cal. y BP. This event was superimposed on a successive change from...

  14. Pollen-inferred vegetation and environmental changes in the central Tibetan Plateau since 8200 yr BP

    Institute of Scientific and Technical Information of China (English)

    LIU; Kam-Biu; Carrie; MORRILL; Jonathan; T.; OVERPECK; Julia; E.; COLE

    2009-01-01

    The ecotone between alpine steppe and meadow in the central Tibetan Plateau is sensitive to climate changes. Here we used the pollen records from three lakes in this region to reconstruct the evolution of local vegetation and climate since 8200 cal. yr BP. The history of temperature and precipitation was reconstructed quantitatively with multi-bioclimatic indexes and a transfer function from pollen records. Results show that the steppe/meadow dominated during the period of 8200―6500 cal. yr BP, especially 8200―7200 cal. yr BP, indicating the central Tibetan Plateau was controlled by strong monsoon. The steppe dominated during the periods of 6000―4900, 4400―3900, and 2800―2400 cal. yr BP. The steppe decreased gradually and the meadow expanded during the period of 4900―4400 cal. yr BP. Three century-scale drought events occurred during 5800―4900, 4400―3900 and 2800 cal. yr BP, respectively. The first time when the regional climate shifted to the present level was at 6500 cal. yr BP in the central Plateau. Since 3000 cal. yr BP, the temperature and precipitation have decreased gradually to the present level. However, the cold climate between 700―300 cal. yr BP likely corresponds to the Little Ice Age.

  15. Pollen-inferred vegetation and environmental changes in the central Tibetan Plateau since 8200 yr BP

    Institute of Scientific and Technical Information of China (English)

    TANG LingYu; SHEN CaiMing; LI ChunHai; PENG JinLan; LIU Hui; LIU Kam-Biu; Carrie MORRILL; Jonathan T. OVERPECK; Julia E. COLE; YANG Bao

    2009-01-01

    The ecotone between alpine steppe and meadow in the central Tibetan Plateau is sensitive to climate changes. Here we used the pollen records from three lakes in this region to reconstruct the evolution of local vegetation and climate since 8200 cal. Yr BP. The history of temperature and precipitation was reconstructed quantitatively with multi-bioclimatic indexes and a transfer function from pollen records.Results show that the steppe/meadow dominated during the period of 8200-6500 cal. Yr BP, especially 8200-7200 cal. Yr BP, indicating the central Tibetan Plateau was controlled by strong monsoon. The steppe dominated during the periods of 6000--4900, 4400--3900, and 2800--2400 cal. Yr BP. The steppe decreased gradually and the meadow expended during the period of 4900-4400 cal. Yr BP. Three century-scale drought events occurred during 5800-4900, 4400-3900 and 2800 cal. Yr BP, respectively. The first time when the regional climate shifted to the present level was at 6500 cal. Yr BP in the central Plateau. Since 3000 cal. Yr BP, the temperature and precipitation have decreased gradually to the present level. However, the cold climate between 700--300 cal. Yr BP likely corresponds to the Little ice Age.

  16. Solar CalPoly

    Energy Technology Data Exchange (ETDEWEB)

    Stannard, Sandra [California Polytechnic State Univ., San Luis Obispo, CA (United States)

    2016-06-15

    The target budget of INhouse was about $650,000 for all materials and student expenses of the Solar Decathlon competition. In order to reach our goal, Cal Poly students and faculty worked with the College of Architecture and Environmental Design’s External Relations office to actively fundraise for INhouse. Students connected with Cal Poly alumni through phone calls, postal mail, email, and live presentations to reach as many alumni in the state of California as possible. Before construction begun, students and faculty met on a weekly basis to determine what brands of materials for the home to use and who would be responsible for reaching out to the company to seek a donation. Our College of Architecture and Environmental Design’s administration was essential in helping us fundraise. For some time, the college was hoping to depend on about half of our fundraising expenses to be covered through the sale of INhouse. However, plans to sell the home fell through during the design development phase; the college turned to the sale of a different asset in to help us meet our goal. If we were to do this project again, completing the design concept and securing a future location of our home sooner would have enhanced our fundraising activities.

  17. Geochemical properties and environmental impacts of seven Campanian tephra layers deposited between 40 and 38 ka BP in the varved lake sediments of Lago Grande di Monticchio, southern Italy

    Science.gov (United States)

    Wutke, Kristina; Wulf, Sabine; Tomlinson, Emma L.; Hardiman, Mark; Dulski, Peter; Luterbacher, Jürg; Brauer, Achim

    2015-06-01

    We present the results of new tephrostratigraphical and environmental impact studies of the 40-38 ka varved sediment section of Lago Grande di Monticchio (southern Italy). The sediments in this time zone are correlated with the Heinrich H4-stadial that occurred between Greenland Interstadials GI-9 and GI-8, and include the widespread Campanian Ignimbrite (CI, 39.3 ka) as a thick tephra layer in the middle of the H4 stadial. The CI in the Monticchio record is overlain by the Schiava tephra from Vesuvius, c. 1240 varve-years younger than the CI, and preceded by four tephras from small-scale eruptions of the Phlegrean Fields and by an Ischia-derived tephra. The four Phlegrean Field-derived tephras were deposited 600 varve-years or fewer prior to the deposition of the CI and show very similar major, minor, and trace element glass compositions to those of the CI. This close similarity in composition and age could compromise the accurate linking and synchronisation of palaeoenvironmental records in the central Mediterranean area. Microfacies analyses and μ-XRF core scanning were used to characterise primary and secondary depositional features of all seven tephra layers and to evaluate environmental and ecological responses after tephra deposition. Higher concentrations of tephra-derived material (mainly glass shards and pumices) in primary and reworked layers were detected by elevated K-counts in μ-XRF elemental core scans. Reworked tephra derives mainly from in-washing from the littoral zone and the catchment and occurs within five to 30 years, and up to 1240 varve years, after the deposition of thinner (1-5 mm) and thicker (5-230 mm) tephra fallout deposits, respectively. An obvious response of diatom population growth directly after the primary tephra deposition was observed for the thicker tephra layers (>1 mm) during the first 1-8 years after deposition of the primary deposit indicating that the additional input of potential nutrients (glass shards) temporarily

  18. Monsoon variability for the past 4 ka derived from high-resolution analyses of sediments from lake Nam Co, central Tibetan Plateau

    Science.gov (United States)

    Kasper, T.; Haberzettl, T.; Doberschütz, S.; Daut, G.; Mäusbacher, R.; Wang, J.; Zhu, L.; Wennrich, V.

    2010-12-01

    were used to perform a principle component analysis (PCA). This resulted in the derivation of monsoon variability during the last 4 ka based upon principle component 1 (PC1) which reflects the allochthonous, clastic input into the lake. PC 1 (Si, Ti, K, Fe, Rb) reaches maximum values between approximately 4000 cal BP and 1800 cal BP as well as between 1500 cal BP and 1200 cal BP. This pattern shows a very good correlation to the variability of the Indian Ocean Summer Monsoon as recorded in a peat bog in the north-eastern part of the Tibetan Plateau (Hong et al. 2005).

  19. CalCOFI Egg Counts

    Data.gov (United States)

    National Oceanic and Atmospheric Administration, Department of Commerce — Fish egg counts and standardized counts for eggs captured in CalCOFI icthyoplankton nets (primarily vertical [Calvet or Pairovet], oblique [bongo or ring nets], and...

  20. CalCOFI Egg Stages

    Data.gov (United States)

    National Oceanic and Atmospheric Administration, Department of Commerce — Egg morphological developmental stage for eggs of selected species captured in CalCOFI icthyoplankton nets. Sequential developmental stages are described by Moser...

  1. CalNex Observational Data

    Data.gov (United States)

    U.S. Environmental Protection Agency — Observations made during the 2010 CalNex measurement campaign. This dataset is associated with the following publication: Woody , M., K. Baker , P. Hayes, J....

  2. CalCOFI Larvae Stages

    Data.gov (United States)

    National Oceanic and Atmospheric Administration, Department of Commerce — Developmental stages (yolk sac, preflexion, flexion, postflexion, or transformation) of selected fish larvae captured in CalCOFI icthyoplankton nets.

  3. Kuulus dress ka Evelinile!

    Index Scriptorium Estoniae

    2009-01-01

    Proua Evelin Ilves kinkis Eestis esinenud popstaar Madonnale eesti rahvusmotiividega dressid. Sarnased spordirõivad tulevad müügile ka Tallinnas Viru keskuses Bastioni esinduskaupluses. Proua Evelin Ilvesele valmistatakse ainulaadsed valgest kangast dressid

  4. Kuulus dress ka Evelinile!

    Index Scriptorium Estoniae

    2009-01-01

    Proua Evelin Ilves kinkis Eestis esinenud popstaar Madonnale eesti rahvusmotiividega dressid. Sarnased spordirõivad tulevad müügile ka Tallinnas Viru keskuses Bastioni esinduskaupluses. Proua Evelin Ilvesele valmistatakse ainulaadsed valgest kangast dressid

  5. CALS - What are the Potentials for SMEs ?

    DEFF Research Database (Denmark)

    Bilberg, Arne; Larsen, Michael holm; Langer, Gilad

    1996-01-01

    The Danish CALS Center initiative, aims at making CALS operational in Danish industry. The center consists of three Danish companies, Bang & Olufsen, Odense Steel Shipyard, Nilfisk besides from the Technical University of Denmark and the Danish Technological Institute. The objective...... is to demonstrate the potentials for improving business processes by effective information management. The three companies involved will demonstrate practical and innovative applications of CALS solutions, that will serve as examples for a wide variety of SMEs.The paper will focus on the industrial results...... and the CALS engineering activities. It will summarize some actual results, e.g. discussion of CALS modeling and analysis techniques. One such technique is "CALS mapping", providing the possibility to plot an actual company’s CALS status in relation to an "ideal" CALS company. Thus, pointing at the central...

  6. Seasonal hypoxia was a natural feature of the coastal zone in the Little Belt, Denmark, during the past 8 ka

    NARCIS (Netherlands)

    van Helmond, N.A.G.M.; Krupinski, Nadine Quintana; Lougheed, Bryan; Obrochta, Stephen; Andrén, Thomas; Slomp, C.P.

    2017-01-01

    The extent of the hypoxic area in the Baltic Sea has rapidly expanded over the past century. Two previous phases of widespread hypoxia, coinciding with the Holocene Thermal Maximum (HTM; 8–4 ka before present; BP) and the Medieval Climate Anomaly (MCA; 2–0.8 ka BP), have been identified. Relatively

  7. Tephrochronology of a 70 ka-long marine record in the Marsili Basin (southern Tyrrhenian Sea)

    Science.gov (United States)

    Tamburrino, S.; Insinga, D. D.; Pelosi, N.; Kissel, C.; Laj, C.; Capotondi, L.; Sprovieri, M.

    2016-11-01

    A sequence of tephra layers is studied in a 13.9 m-long deep-sea core (MD01-2474G) from the southern Tyrrhenian Sea. The chronology of the succession is provided by a high-resolution age-depth model based on isotope stratigraphy and AMS radiocarbon dating, which place the succession of events in a time interval spanning the last 70 ka. Based on a precise chronological framework and proximal-distal correlations, the Y-1, Y-6 and Y-7 main marker tephras were identified. Compositional data on fresh micro-pumice or glass shards of selected tephras were correlated with the coeval volcanic activity of Aeolian Arc (Vulcano and Salina), Mt. Etna, Phlegrean Fields Pantelleria and Ischia. The tephra sequence contains a number of deposits documenting recurrent activity on Vulcano Island at ca. 6.9 ka BP (MD3), ca. 16.7 ka BP (MD11), ca. 23.2 ka BP (MD14), ca. 29.6 ka BP (MD15), ca. 36.9 ka BP (MD22) and ca. 42.5 ka BP (MD27). The results presented in this study improve the southern Tyrrhenian Sea tephrostratigraphic framework and provide new insights into chemistry and dispersal area of Aeolian Arc pyroclastic deposits in this sector of the Central Mediterranean.

  8. The Sharp Rise of Δ14C ca. 800 cal BC : Possible causes, related climatic teleconnections and the impact on human environments

    NARCIS (Netherlands)

    Geel, Bas van; Plicht, Johannes van der; Kilian, M.R.; Klaver, E.R.; Kouwenberg, J.H.M.; Renssen, H.; Reynaud-Farrera, I.; Waterbolk, H.T.

    1998-01-01

    In this study we report on accelerator mass spectrometry (AMS) wiggle-match dating of selected macrofossils from organic deposits ca. 800 cal BC (ca. 2650 BP). Based on paleological, archaeological and geological evidence, we found that the sharp rise of atmospheric 14C between 850 and 760 cal BC co

  9. Paleoenvironmental Changes in the Semiarid Coast of Chile (˜32°S) during the Last 6200 cal Years Inferred from a Swamp-Forest Pollen Record

    Science.gov (United States)

    Maldonado, Antonio; Villagrán, Carolina

    2002-09-01

    Pollen analysis of two sediment records from a coastal swamp forest site in the Chilean semiarid region (31°50'S; 71°28'W) shows an alternation of dry and wet phases during the past ˜6100 cal yr B.P. The most prominent vegetation changes occur at ˜4200 cal yr B.P., with the expansion of the swamp forest taxa Luma chequen and Escallonia sp., followed by a regression of the forest beginning at ˜3200 cal yr B.P. and ending with its replacement by a xerophytic scrub, between ˜1800 and 1300 cal yr B.P. The swamp forest reexpanded after ˜1300 cal yr B.P. and persisted, with minor variation, until the present. We interpret the establishment of the swamp forest at the study site to be the result of a rising watertable in response to increased rainfalls from ˜4200 cal yr B.P. onward. Our results indicate that in north-central Chile the second half of the Holocene was climatically more variable than previously thought, suggesting significant changes in the position and/or intensity of the westerlies wind belt and possibly in the frequency of El Niño-Southern Oscillation events.

  10. Vibrio parahaemolyticus CalR down regulates the thermostable direct hemolysin (TDH) gene transcription and thereby inhibits hemolytic activity.

    Science.gov (United States)

    Zhang, Yiquan; Zhang, Ying; Gao, He; Zhang, Lingyu; Yin, Zhe; Huang, Xinxiang; Zhou, Dongsheng; Yang, Huiying; Yang, Wenhui; Wang, Li

    2017-03-04

    TDH, encoded by tdh gene, is a major virulent determinant of V. parahaemolyticus that controls various biological activities, such as hemolytic activity, cytotoxicity, and enterotoxicity. The hemolytic activity on Wagatsuma agar ascribed to TDH is called Kanagawa phenomenon (KP). All KP positive strains contain tdh1 and tdh2 genes, but tdh2 is predominantly responsible for KP. CalR is a regulatory protein that was originally identified as a repressor of swarming motility and T3SS1 gene expression in V. parahaemolyticus. In the present study, the regulation of tdh2 by CalR was investigated using a set of experiments including qRT-PCR, primer extension, LacZ fusion, hemolytic phenotype, EMSA, and DNase I footprinting assays. The results showed that His-CalR protected a single region from 224bp to 318bp upstream of tdh2 against DNase I digestion, and a transcriptional start site located at 42bp upstream of tdh2 was detected and its transcribed activity was inhibited by CalR. Moreover, the KP test results showed that the hemolytic activity of V. parahaemolyticus is also under negative control of CalR. The data demonstrated that CalR is a repressor of the tdh2 transcription and thereby inhibits the hemolytic activity of V. parahaemolyticus.

  11. RELATIONSHIP BETWEEN PHYSICAL ACTIVITIES OF GIRLS AND THEIR PARENTS WITH GIRLS` ATTITUDES PHYSI CAL ACTIVITY

    Directory of Open Access Journals (Sweden)

    Nebojša Čokorilo

    2007-05-01

    Full Text Available The re se arch was con duc ted on the sam ple of 222 pa rents of ele men tary school - girls, aged 6-7 years from No vi Sad, Som bor, Srem ska Mi tro vi ca, Bač ka Pa lan ka and Zre nja nin. Physi cal ac ti vi ti es of ma le chil dren and the ir pa rents we re al so eva lu a ted by the ir pa rents. That is the ti me when chil dren can con sti tu te ha bits for physi cal exer ci ses. Pas si ve at ti tu de of fe ma le chil dren to wards physi cal exer ci ses are the con se qu en ces of the sa me at ti tu des sha red by pa rents. Wit hin re se arch it is fo und out that the re is a hu ge im por tan ce of pa rents’ par ti ci pa tion in chil dren’s ac ti vi ti es. That in clu des how much chil dren are physi cal ac ti ve per we ek.

  12. Quantitative estimation of Holocene surface salinity variation in the Black Sea using dinoflagellate cyst process length

    DEFF Research Database (Denmark)

    Mertens, Kenneth Neil; Bradley, Lee R.; Takano, Yoshihito

    2012-01-01

    ± 0.91 psu around 9.9 cal ka BP to a minimum ∼12.3 ± 0.91 psu around 8.5 cal ka BP, reaching current salinities of ∼17.1 ± 0.91 psu around 4.1 cal ka BP. The resolution of our sampling is about 250 years, and it fails to reveal a catastrophic salinization event at ∼9.14 cal ka BP advocated by other...

  13. CalCOFI Egg Counts Positive Tows

    Data.gov (United States)

    National Oceanic and Atmospheric Administration, Department of Commerce — Fish egg counts and standardized counts for eggs captured in CalCOFI icthyoplankton nets (primarily vertical [Calvet or Pairovet], oblique [bongo or ring nets], and...

  14. CalCOFI Larvae Counts Positive Tows

    Data.gov (United States)

    National Oceanic and Atmospheric Administration, Department of Commerce — Fish larvae counts and standardized counts for eggs captured in CalCOFI icthyoplankton nets (primarily vertical [Calvet or Pairovet], oblique [bongo or ring nets],...

  15. A 16 ka climate record deduced from δ13C and C/N ratio in Qinghai Lake sediments, northeastern Tibetan Plateau

    Institute of Scientific and Technical Information of China (English)

    2006-01-01

    On the basis of multi-proxy analysis on TOC, TN, C/N, organic δ13C and grain size, sediment record from Qinghai Lake provides evidences of stepwise-patterned climatic change since 16 ka BP.Results show that Qinghai Lake underwent six environmental stages. From 16.2 to 14.3 ka BP and from 4.0 to 2.1 ka BP, the organic δ13C value was controlled by the concentration of atmospheric CO2. Relative higher organic δ13C values occurred between 14.3 to 10.4 ka BP indicative of water hardness decrease resulted from melting ice water, corresponding to two intervals of C/N peak values to the Bo1ing and Allerod warm periods in Europe respectively. From 10.4 ka BP, Qinghai Lake entered the Holocene and the climate was warm and a little dry. The Megathermal appeared at about 6.7 ka BP when the vegetation around the lake transformed into a forest. Between 6.3 ka BP and 4.0 ka BP, the temperature decreased and δ13C value was controlled by the expansion of C3 plants and the retreat of C4 plants in river catchment.Since 4.0 ka BP, the climate gradually became cold and dry. From 2.1 ka BP, the cold-dry climate and human activity resulted in an abrupt increase in C/N with deceased δ13C value; meanwhile, many coarse grains appeared in sediments.

  16. Environment and paleoecology of a 12 ka mid-North American Younger Dryas forest chronicled in tree rings

    Science.gov (United States)

    Panyushkina, Irina P.; Leavitt, Steven W.; Thompson, Todd A.; Schneider, Allan F.; Lange, Todd

    2008-01-01

    Until now, availability of wood from the Younger Dryas abrupt cooling event (YDE) in N. America ca. 12.9 to 11.6 ka has been insufficient to develop high-resolution chronologies for refining our understanding of YDE conditions. Here we present a multi-proxy tree-ring chronology (ring widths, “events” evidenced by microanatomy and macro features, stable isotopes) from a buried black spruce forest in the Great Lakes area (Liverpool East site), spanning 116 yr at ca. 12,000 cal yr BP. During this largely cold and wet period, the proxies convey a coherent and precise forest history including frost events, tilting, drowning and burial in estuarine sands as the Laurentide Ice Sheet deteriorated. In the middle of the period, a short mild interval appears to have launched the final and largest episode of tree recruitment. Ultimately the tops of the trees were sheared off after death, perhaps by wind-driven ice floes, culminating an interval of rising water and sediment deposition around the base of the trees. Although relative influences of the continental ice sheet and local effects from ancestral Lake Michigan are indeterminate, the tree-ring proxies provide important insight into environment and ecology of a N. American YDE boreal forest stand.

  17. Developmental evolution of flowering plant pollen tube cell walls: callose synthase (CalS gene expression patterns

    Directory of Open Access Journals (Sweden)

    Abercrombie Jason M

    2011-07-01

    Full Text Available Abstract Background A number of innovations underlie the origin of rapid reproductive cycles in angiosperms. A critical early step involved the modification of an ancestrally short and slow-growing pollen tube for faster and longer distance transport of sperm to egg. Associated with this shift are the predominantly callose (1,3-β-glucan walls and septae (callose plugs of angiosperm pollen tubes. Callose synthesis is mediated by callose synthase (CalS. Of 12 CalS gene family members in Arabidopsis, only one (CalS5 has been directly linked to pollen tube callose. CalS5 orthologues are present in several monocot and eudicot genomes, but little is known about the evolutionary origin of CalS5 or what its ancestral function may have been. Results We investigated expression of CalS in pollen and pollen tubes of selected non-flowering seed plants (gymnosperms and angiosperms within lineages that diverged below the monocot/eudicot node. First, we determined the nearly full length coding sequence of a CalS5 orthologue from Cabomba caroliniana (CcCalS5 (Nymphaeales. Semi-quantitative RT-PCR demonstrated low CcCalS5 expression within several vegetative tissues, but strong expression in mature pollen. CalS transcripts were detected in pollen tubes of several species within Nymphaeales and Austrobaileyales, and comparative analyses with a phylogenetically diverse group of sequenced genomes indicated homology to CalS5. We also report in silico evidence of a putative CalS5 orthologue from Amborella. Among gymnosperms, CalS5 transcripts were recovered from germinating pollen of Gnetum and Ginkgo, but a novel CalS paralog was instead amplified from germinating pollen of Pinus taeda. Conclusion The finding that CalS5 is the predominant callose synthase in pollen tubes of both early-diverging and model system angiosperms is an indicator of the homology of their novel callosic pollen tube walls and callose plugs. The data suggest that CalS5 had transient expression

  18. Carbonate and carbon fluctuations in the Eastern Arabian Sea over 140 ka: Implications on productivity changes?

    Digital Repository Service at National Institute of Oceanography (India)

    Guptha, M.V.S.; Naidu, P.D.; Haake, B.G.; Schiebel, R.

    orientation. ARTICLE IN PRESS Table1 Core depth, age, stable oxygen isotope data, linear sedimenta- tion rate (LSR), and calcite and organic carbon concentration ofsedimentcoreSL-1 Depth (cm) Age (kaBP) d 18 O (%) LSR (cm/ka) CaCO 3 (%) C org (%) 1 0.49 47....96 0.50 225 44.00 30.85 0.38 230 45.00 C00.49 5.02 33.34 0.49 235 45.99 32.38 0.73 240 46.99 C00.24 5.02 38.10 0.56 Table1(continued) Depth (cm) Age (kaBP) d 18 O (%) LSR (cm/ka) CaCO 3 (%) C org (%) 245 47.98 45.24 0.48 250 48.98 C00.50 5.02 45.10 0...

  19. Oceanic Density Fronts Steering Bottom-Current Induced Sedimentation Deduced from a 50 ka Contourite-Drift Record and Numerical Modeling (off NW Spain)

    Science.gov (United States)

    Hanebuth, T. J. J.; Zhang, W.; Hofmann, A. L.; Lowemark, L. A.; Schwenk, T.

    2015-12-01

    How bottom-near hydrographic and sedimentary processes control the formation of bottom-current related confined deep-sea depocenters remains widely speculative. The geological approach of this study uses a transect of sediment cores and sediment echosounder profiles across a whole contourite system off NW Spain. This "mounded patch"-type contourite drift (18 km long, 20 km wide) with a 150-m deep moat has formed around an 800-m high structural obstacle. Past deposition was characterized by alternating calm and high-energy bottom-flow conditions. Calm conditions (Last Glacial period: 27-17 cal ka BP; late Holocene times: current-influenced deposition of fine-grained sediments (10 µm) over the entire basin. In contrast, waxing-and-waning high-energy conditions (D/O events during Marine Isotope Stage 3; the Deglacial/early Holocene time interval at 17-4 cal ka BP) resulted in coarse grained (70 µm) deposition. Process-based numerical modelling demonstrates that pulse-like oceanic density fronts travelling within the transition zone of two water masses (Labrador Sea Water, Mediterranean Outflow Water) provide a powerful mechanism for contouritic deposition, rather than the core of a water mass itself. These gravity-driven density fronts lead to local re-suspension of sand from the moat and to subsequent upward transport over the crest. Here, the oceanic density fronts produce additional km-scale eddies. These migrating eddies provide an efficient mechanism for further widespread sediment re-distribution. In comparison with paleoceanographic reconstructions, a downward migration or expansion of the Mediterranean Outflow Water by about 300 m led most probably to such temporary contouritic sand deposition. We finally propose a conceptual model to explain how seafloor obstacles redirect and perturbate bottom currents. This model proposes water mass transition zone as an important high-energy medium, for oceanic density fronts to travel. On the respective time scale, the

  20. Molecular Paleoclimate Reconstructions over the Last 9 ka from a Peat Sequence in South China.

    Science.gov (United States)

    Wang, Xinxin; Huang, Xianyu; Sachse, Dirk; Ding, Weihua; Xue, Jiantao

    2016-01-01

    To achieve a better understanding of Holocene climate change in the monsoon regions of China, we investigated the molecular distributions and carbon and hydrogen isotope compositions (δ13C and δD values) of long-chain n-alkanes in a peat core from the Shiwangutian (SWGT) peatland, south China over the last 9 ka. By comparisons with other climate records, we found that the δ13C values of the long-chain n-alkanes can be a proxy for humidity, while the δD values of the long-chain n-alkanes primarily recorded the moisture source δD signal during 9-1.8 ka BP and responded to the dry climate during 1.8-0.3 ka BP. Together with the average chain length (ACL) and the carbon preference index (CPI) data, the climate evolution over last 9 ka in the SWGT peatland can be divided into three stages. During the first stage (9-5 ka BP), the δ13C values were depleted and CPI and Paq values were low, while ACL values were high. They reveal a period of warm and wet climate, which is regarded as the Holocene optimum. The second stage (5-1.8 ka BP) witnessed a shift to relatively cool and dry climate, as indicated by the more positive δ13C values and lower ACL values. During the third stage (1.8-0.3 ka BP), the δ13C, δD, CPI and Paq values showed marked increase and ACL values varied greatly, implying an abrupt change to cold and dry conditions. This climate pattern corresponds to the broad decline in Asian monsoon intensity through the latter part of the Holocene. Our results do not support a later Holocene optimum in south China as suggested by previous studies.

  1. A Simple Acronym for Doing Calculus: CAL

    Science.gov (United States)

    Hathaway, Richard J.

    2008-01-01

    An acronym is presented that provides students a potentially useful, unifying view of the major topics covered in an elementary calculus sequence. The acronym (CAL) is based on viewing the calculus procedure for solving a calculus problem P* in three steps: (1) recognizing that the problem cannot be solved using simple (non-calculus) techniques;…

  2. Ostracod assemblages and their environmental significance from the lake core of the Nam Co on the Tibetan Plateau 8.4 kaBP%8.4 ka以来纳木错湖芯介形类组合的环境变化意义

    Institute of Scientific and Technical Information of China (English)

    谢曼平; 朱立平; 彭萍; 王君波; 汪勇; SCHWALB Antje

    2009-01-01

    A 332-cm long lacustrine core was drilled in the Nam Co in the central-southern part of the Tibetan Plateau. From the core, 15 species of ostracods (Crustacea: Ostracoda), which belong to 6 genera have been identified. According to the variations of the ostracod assem-blages and the ostracods ecological features, which are sensitive to the changing environ-ment, three main stages can be distinguished as follows: Stage I was from 8400 to 6800 a BP, during which the climate was cold-humid, and the lake depth changed from shallow to deep. Stage II was from 6400 to 2500 a BP, during which the climate changed from warm-humid to cold-humid, and then to cold-dry. The lake depth gradually became deep. The shifting of cli-mate, from wet-cold to dry-cold during this period, had constructed the basis of present en-vironment in the Nam Co. Stage III was from 2500 a BP to the present, which showed a trait of lake depth increasing. At the earlier period of this stage, the climate kept as cold-dry as that in the former stage, but the salinity of the lake increased. At the later period of this stage, the degree of cold-dry was enhanced, and the activities of land surface runoff tended to be weakened. Our research also found that the peak values of ostracods with black shell was coherent with the maximum production of the ostracods, and agreed with the increasing sedimentary water dynamics. This indicated that the ostracods with black shell was simulta-neous with the high prolificacy of ostracod, and transported from other places. The abun-dance of Candona juvenile shells reflected the high mortality of that kind of ostracods under an unfavorable condition. This was probably a result of the rapid change of water dynamics of sedimentary environment.

  3. CALS - what are the potentials for SME’s ?

    DEFF Research Database (Denmark)

    Bilberg, Arne; Thomsen, Finn Tang; Larsen, Michael Holm

    1997-01-01

    The DanishCALS Center initiative, aims at making CALS operational in Danish industry. The centerconsists of three Danish companies, Bang & Olufsen, Odense Steel Shipyard, Nilfiskbesides from the Technical University of Denmark and the Danish Technological Institute.The objective is to demonstrate...... the potentials for improvingbusiness processes by effective information management. The threecompanies involved will demonstrate practical and innovativeapplications of CALS solutions, that will serve as examples for awide variety of SMEs. The paper will focus on the industrial results and the CALSengineering...... activities. It will summarize some actual results, e.g.a discussion of CALS modeling and analysis techniques. One suchtechnique is "CALS mapping", providing the possibilityto plot an actual company’s CALS status in relation to an"ideal" CALS company. Thus, pointing at the centralareas where CALS can...

  4. Nonlinear waves in $\\cal PT$-symmetric systems

    OpenAIRE

    Konotop, Vladimir V.; Yang, Jianke; Zezyulin, Dmitry A.

    2016-01-01

    Recent progress on nonlinear properties of parity-time ($\\cal PT$-) symmetric systems is comprehensively reviewed in this article. $\\cal PT$ symmetry started out in non-Hermitian quantum mechanics, where complex potentials obeying $\\cal PT$ symmetry could exhibit all-real spectra. This concept later spread out to optics, Bose-Einstein condensates, electronic circuits, and many other physical fields, where a judicious balancing of gain and loss constitutes a $\\cal PT$-symmetric system. The nat...

  5. LumiCal alignment system - Status report

    CERN Document Server

    Daniluk, W.; Lesiak, T.; Moszczyński, A.; Pawlik, B.; Wojtoń, T.; Zawiejski, L.

    2015-01-01

    The paper describes the status of the laser-based alignment-system for the luminosity detector, LumiCal, taking into considerations the conditions of the International Large Detector in the International Linear Collider project. The design of the system comprises two parts: the first one containing semi-transparent silicon sensors used to deliver simultaneous position measurements in the X,Y directions of the monitored object, and the second one in which the interferometric technique, i.e. the Frequency Scanning Interferometry (FSI), is proposed. Two laboratory prototypes for both components of the system were built and the preliminary measurements of the DUT displacements demonstrated their utility in the design of the final alignment system. The alignment of the LumiCal detector will allow us to monitor the detector displacements and possible deformations in its internal structure. Lack of information of the displacements will introduce a systematic effect which will have an impact on the accuracy of the fi...

  6. Improving Supply Management: The CALS Connection

    Science.gov (United States)

    1992-02-01

    several data systems and presents the data online through prestructured reports and responses to ad hoc queries. Status: Operational. 12. 5-2 CALS...DLA Online Characteristics Search System DLA LOGRUN allows users to search for items by characteristics. After modernization, a much improved system...Committee SMR - source, maintenance, and recoverability (code) SPOC Ships Parts Control Center (Navy) SPS = Ships’ Provisioning System (Navy) SPTD

  7. Preliminary CALS Phase II Architecture. Volume 19

    Science.gov (United States)

    1989-07-03

    IDEF ICAM Definition Languages 5 IDEFO ICAM Definition Language: Activity Modeling IDEFIX ICAM Definition Language: Data Modeling 3 IDS Integrated Design...level. At the Conceptual Description level, data are defined by an integrated semantic data model, such as those produced using the IDEFIX modeling...Architecture with the dominate focus on the data dictionary for the IWSDB, represented by an IDEFIX semantic data model. It is at this level that CALS Phase II

  8. Prunskiene tahab lepet ka Keskerakonnaga

    Index Scriptorium Estoniae

    2011-01-01

    Leedu Rahvaerakonna (LLP) juht Kazimira Prunskeine käis Moskvas Ühtse Venemaa kongressil ning allkirjastas leppe oma erakonna ja Ühtse Venemaa vahel, samasuguse leppe kavatseb ta allkirjastada ka Eesti Keskerakonnaga, Kasahstanis võimul oleva Nur Otani partei ja Kreeka erakonnaga Uus Demokraatia

  9. Ajateenistust alustab ka viis neidu

    Index Scriptorium Estoniae

    2013-01-01

    Tuleval nädalal alustab ajateenistust üle 1600 noormehe, lisaks alustab juulis Kuperjanovi jala­väepataljonis vabatahtlikuna ajateenistust ka viis neidu. Juulikuise teenistusse kutsumisega alustavad teenistust ajateenijad, kelle ametikoht eeldab 11-kuulist ajateenistust ehk autojuhid, erialaspet­sialistid, allohvitserid ja reservrühmaülemad

  10. Partial ${\\cal N}=2 \\to {\\cal N}=1$ supersymmetry breaking and gravity deformed chiral rings

    CERN Document Server

    David, J R; Narain, K S; David, Justin R.; Gava, Edi

    2004-01-01

    We present a derivation of the chiral ring relations, arising in ${\\cal N}=1$ gauge theories in the presence of (anti-)self-dual background gravitational field $G_{\\alpha\\beta\\gamma}$ and graviphoton field strength $F_{\\alpha\\beta}$. These were previously considered in the literature in order to prove the relation between gravitational F-terms in the gauge theory and coefficients of the topological expansion of the related matrix integral. We consider the spontaneous breaking of ${\\cal N} =2$ to ${\\cal N} =1$ supergravity coupled to vector- and hyper-multiplets, and take a rigid limit which keeps a non-trivial $G_{\\alpha\\beta\\gamma}$ and $F_{\\alpha\\beta}$ with a finite supersymmetry breaking scale. We derive the resulting effective, global, ${\\cal N}=1$ theory and show that the chiral ring relations are just a consequence of the standard ${\\cal N}=2$ supergravity Bianchi identities . We can also obtain models with matter in different representations and in particular quiver theories. We also show that, in the...

  11. Nonlinear waves in $\\cal PT$-symmetric systems

    CERN Document Server

    Konotop, Vladimir V; Zezyulin, Dmitry A

    2016-01-01

    Recent progress on nonlinear properties of parity-time ($\\cal PT$-) symmetric systems is comprehensively reviewed in this article. $\\cal PT$ symmetry started out in non-Hermitian quantum mechanics, where complex potentials obeying $\\cal PT$ symmetry could exhibit all-real spectra. This concept later spread out to optics, Bose-Einstein condensates, electronic circuits, and many other physical fields, where a judicious balancing of gain and loss constitutes a $\\cal PT$-symmetric system. The natural inclusion of nonlinearity into these $\\cal PT$ systems then gave rise to a wide array of new phenomena which have no counterparts in traditional dissipative systems. Examples include the existence of continuous families of nonlinear modes and integrals of motion, stabilization of nonlinear modes above $\\cal PT$-symmetry phase transition, symmetry breaking of nonlinear modes, distinctive soliton dynamics, and many others. In this article, nonlinear $\\cal PT$-symmetric systems arising from various physical disciplines ...

  12. Coastal Meteorological Phenomena in CalNex

    Science.gov (United States)

    Angevine, W. M.; Brioude, J.

    2010-12-01

    Coastal meteorology plays an important role in air quality and climate in California. During the 2010 CalNex experiment, several phenomena affected the campaign observations. Among these were coastal eddies and outflow in Santa Monica Bay and the Los Angeles Bight; marine stratus and stratocumulus; and the land-sea breeze cycle on a variety of spatial scales, including transport from the San Francisco Bay Area into the Central Valley. In this presentation, we will describe these phenomena as they were seen in model forecasts and hindcast simulations, and compare those simulations to the relevant meteorological observations.

  13. A ˜25 ka Indian Ocean monsoon variability record from the Andaman Sea

    Science.gov (United States)

    Rashid, H.; Flower, B. P.; Poore, R. Z.; Quinn, T. M.

    2007-10-01

    Recent paleoclimatic work on terrestrial and marine deposits from Asia and the Indian Ocean has indicated abrupt changes in the strength of the Asian monsoon during the last deglaciation. Comparison of marine paleoclimate records that track salinity changes from Asian rivers can help evaluate the coherence of the Indian Ocean monsoon (IOM) with the larger Asian monsoon. Here we present paired Mg/Ca and δ 18O data on the planktic foraminifer Globigerinoides ruber (white) from Andaman Sea core RC12-344 that provide records of sea-surface temperature (SST) and δ 18O of seawater (δ 18O sw) over the past 25,000 years (ka) before present (BP). Age control is based on nine accelerator mass spectrometry (AMS) dates on mixed planktic foraminifera. Mg/Ca-SST data indicate that SST was ˜3 °C cooler during the last glacial maximum (LGM) than the late Holocene. Andaman Sea δ 18O sw exhibited higher than present values during the Lateglacial interval ca 19-15 ka BP and briefly during the Younger Dryas ca 12 ka BP. Lower than present δ 18O sw values during the BØlling/AllerØd ca 14.5-12.6 ka BP and during the early Holocene ca 10.8-5.5 ka BP are interpreted to indicate lower salinity, reflect some combination of decreased evaporation-precipitation (E-P) over the Andaman Sea and increased Irrawaddy River outflow. Our results are consistent with the suggestion that IOM intensity was stronger than present during the BØlling/AllerØd and early Holocene, and weaker during the late glaciation, Younger Dryas, and the late Holocene. These findings support the hypothesis that rapid climate change during the last deglaciation and Holocene included substantial hydrologic changes in the IOM system that were coherent with the larger Asian monsoon.

  14. Charting Class ${\\cal S}_k$ Territory

    CERN Document Server

    Franco, Sebastian; Uranga, Angel

    2015-01-01

    We extend the investigation of the recently introduced class ${\\cal S}_k$ of 4d $\\mathcal{N}=1$ SCFTs, by considering a large family of quiver gauge theories within it, which we denote $\\mathcal{S}^1_k$. These theories admit a realization in terms of $\\mathbb{Z}_k$ orbifolds of Type IIA configurations of D4-branes stretched among relatively rotated sets of NS-branes. This fact permits a systematic investigation of the full family, which exhibits new features such as non-trivial anomalous dimensions differing from free field values and novel ways of gluing theories. We relate these ingredients to properties of compactification of the 6d (1,0) superconformal ${\\cal T}_N^k$ theories on spheres with different kinds of punctures. We describe the structure of dualities in this class of theories upon exchange of punctures, including transformations that correspond to Seiberg dualities, and exploit the computation of the superconformal index to check the invariance of the theories under them.

  15. Dating North European mammoths (Mammuthus primigenius Blum.): a nearly continuous record from 53 ka to 11 ka

    Science.gov (United States)

    Ukkonen, P.; Aaris-Sørensen, K.; Arppe, L.; Clark, P. U.; Daugnora, L.; Lister, A.; Lõugas, L.; Seppä, H. A.; Stuart, A. J.; Wojtal, P.; Zupins, I.

    2010-05-01

    nearly continuously from 53 ka to 11 ka, completely disappearing from the area only during the Last Glacial Maximum (LGM). From the northern parts of the study area, mammoths disappeared ca. 27 ka ago. In the south they survived until the LGM, and occupied the area again during deglaciation. Mammoths survived in the eastern part of the study area until the end of Younger Dryas. References Weninger, B., Jöris, O., 2008. A 14C age calibration curve for the last 60 ka: the Greenland-Hulu U/Th timescale and its impact on understanding the Middle to Upper Paleolithic transition in Western Eurasia. Journal of Human Evolution 55,772-781. Weninger, B., Jöris, O., Danzeglocke, U., 2008. CalPal-2007. Cologne Radiocarbon Calibration & Palaeoclimate Research Package. http://www.calpal.de/ [2008-09-18].

  16. CALS Test Network Sacramento Air Logistics Center. CALS/EDI Transfer Test Number 2, Quick Short Test Report.

    Science.gov (United States)

    2007-11-02

    McClellan AFB , CA. The test required CALS data (MIL-R-28002A Raster) to be sent in an EDI (Electronic Data Interchange) envelope over a commercial VAN...Livermore National Laboratory EC/EDI (Electronic Commerce Through Electronic Data Interchange) Project, and the Sacramento Air Logistics Center (SM-ALC...Value Added Network). CALS Test Network Sacramento Air Logistics Center CALS/EDI Data Transfer Test Number 2 Quick Short Test Report.

  17. Environmental change of Gucheng Lake of Jiangsu in the past 15 ka and its relation to palaeomonsoon

    Institute of Scientific and Technical Information of China (English)

    王苏民; 羊向东; 马燕; 潘红玺; 童国榜; 吴锡浩

    1996-01-01

    The high-resolution and multi-proxy analysis of lacustrine sediments from the Gucheng Lake has revealed the palaeodimatic and palaeoenvironmental evolutionary process since 15 ka B.P. The formation, expansion and shrinkage of the lake is closely related to monsoon rain caused by strength change of monsoon circulation which is controlled by orbit forcing. An abrupt descending of temperature occurring from 11.3 to 11.0ka B.P. may be correlative to Younger Dryas event, which trancated the monsoon climate cycle. Through the correlation with adjacent regions, it can be known that there were twice north shifts and twice south migrations for polar front of monsoon.

  18. EST Table: BP182325 [KAIKOcDNA[Archive

    Lifescience Database Archive (English)

    Full Text Available BP182325 NRPG0442 10/09/28 77 %/149 aa ref|NP_001037470.1| protein ultraspiracle ho...molog [Bombyx mori] sp|P49700.1|USP_BOMMO RecName: Full=Protein ultraspiracle homolog; AltName: Full=Nuclear...8 low homology 10/09/10 low homology 10/09/10 39 %/168 aa gnl|Amel|GB16648-PA 10/09/10 48 %/109 aa gi|121308144|emb|CAL25729.1| ultra

  19. Finished Genome Sequence of Collimonas arenae Cal35

    NARCIS (Netherlands)

    Wu, Je-Jia; de Jager, Victor; Deng, Wen-ling; Leveau, Johan

    2015-01-01

    We announce the finished genome sequence of soil forest isolate Collimonas arenae Cal35, which comprises a 5.6-Mbp chromosome and 41-kb plasmid. The Cal35 genome is the second one published for the bacterial genus Collimonas and represents the first opportunity for high-resolution comparison of geno

  20. Finished Genome Sequence of Collimonas arenae Cal35

    NARCIS (Netherlands)

    Wu, Je-Jia; de Jager, Victor; Deng, Wen-ling; Leveau, Johan

    2015-01-01

    We announce the finished genome sequence of soil forest isolate Collimonas arenae Cal35, which comprises a 5.6-Mbp chromosome and 41-kb plasmid. The Cal35 genome is the second one published for the bacterial genus Collimonas and represents the first opportunity for high-resolution comparison of geno

  1. KaVA ESTEMA project

    Science.gov (United States)

    Oyadomari, Miyako; Imai, Hiroshi; Cho, Se-Hyung; Asaki, Yoshiharu; Choi, Yoon-Kyong; Kim, Jaeheon; Yun, Youngjoo; Matsumoto, Naoko; Min, Cheul-Hong; Oyama, Tomoaki; Yoon, Sung-Chul; Yoon, Dong-Hwan; Kim, Dong-Jin; Dodson, Richard; Rioja, Maria; Burns, Ross; Orosz, Gabor; Nakagawa, Akiharu; Chibueze O, James; Nakashima, Jun-ichi; Sobolev, Andrey

    2016-07-01

    The ESTEMA (Expanded Study on Stellar Masers) project is one of three Large Programs of the KaVA (the combined array of the Korean VLBI Network and Japanese VLBI Exploration of Radio Astrometry), and conducted in 2015-2016. It aims to publish a database of the largest sample of VLBI images of circumstellar water (H2O) and silicon-monoxide (SiO) maser sources towards circumstellar envelopes (CSEs) of 80 evolved stars in late AGB to early post-AGB phase. Here we present the specifications of the ESTEMA observations and the planned scientific goals in order to share the basic information of the ESTEMA with astronomical community and encourage future collaborations with the ESTEMA and future follow-up observations for the targeted stars.

  2. Fade Mitigation Techniques at Ka-Band

    Science.gov (United States)

    Dissanayake, Asoka (Editor)

    1996-01-01

    Rain fading is the dominant propagation impairment affecting Ka-band satellite links and rain fade mitigation is a key element in the design of Ka-band satellite networks. Some of the common fade mitigation techniques include: power control, diversity, adaptive coding, and resource sharing. The Advanced Communications Technology Satellite (ACTS) provides an excellent opportunity to develop and test Ka-band rain impairment amelioration techniques. Up-link power control and diversity are discussed in this paper.

  3. Noncommutative ${\\cal N}=2$ Chern-Simons-matter model

    CERN Document Server

    Bevilaqua, L Ibiapina

    2014-01-01

    In this work we study the three-dimensional ${\\cal N}=2$ supersymmetric Chern-Simons-matter model in a noncommutative space-time. We construct the action of the noncommutative $U(N)$ non-Abelian model in terms of explicit ${\\cal N}=2$ supervariables by dimensionally reducing a four-dimensional ${\\cal N}=1$ supermultiplet. We also obtain the on-shell ${\\cal N}=2$ supersymmetric model writing it in terms of ${\\cal N}=1$ superfields. In the noncommutative Abelian case, we show that linear UV divergences are cancelled in Feynman diagrams and logarithmic divergences are absent up to one-loop order, stating that our model is free of UV/IR mixing.

  4. Late Quaternary glaciation history of northernmost Greenland - Evidence of shelf-based ice

    DEFF Research Database (Denmark)

    Larsen, Nicolaj Krog; Kjær, Kurt H; Funder, Svend

    2010-01-01

    to retreat ca 16 ka to 10.3 cal ka BP before the final break-up, which took place ca 10.1 cal ka BP probably as a combined result of increased inflow of warm Atlantic water through the Fram Strait, a shallower halocline and higher summer temperatures, corresponding to orbital maximum solar insolation...

  5. Ka Band Parabolic Deployable Antenna (KaPDA) for Interplanetary CubeSat Communications Project

    Data.gov (United States)

    National Aeronautics and Space Administration — Ka Band Parabolic Deployable Antenna (KaPDA) for Interplanetary CubeSat Communications allowing moving up from UHF, S or X to get higher gain for a given diameter.

  6. Resonant scattering and recombination in cal 87

    Directory of Open Access Journals (Sweden)

    J. Greiner

    2004-01-01

    Full Text Available Se observ o la binaria eclipsante de rayos X supersuave CAL 87 con Chandra el 13/14 de agosto de 2001, durante casi 100 ksec, completando dos ciclos orbitales totales y tres eclipses. La forma de la curva de luz del eclipse derivada de los fotones de orden cero indica que el tama~no de la regi on de emisi on de rayos X es de alrededor de 1.5 R . El espectro ACIS/LETG est a dominado por completo por las l neas de emisi on sin ning un continuo apreciable. Las l neas de emisi on m as brillantes presentan un corrimiento al rojo signi cativo y dos picos, sugiriendo que se producen en un viento de 2000 km/s. Realizamos un modelo del espectro de rayos X mezclando la dispersi on de recombinaci on y resonancia. Esto nos permite deducir que la temperatura y la luminosidad de la fuente ionizante son kT 50 100 eV y LX 5 1037 erg/s, respectivamente.

  7. Minimal $\\cal N=4$ topologically massive supergravity

    CERN Document Server

    Kuzenko, Sergei M; Sachs, Ivo

    2016-01-01

    Using the superconformal framework, we construct a new off-shell model for topologically massive $\\cal N=4$ supergravity which is minimal in the sense that it makes use of a single compensating vector multiplet. Our theory provides a counterexample to the common lore that two compensating multiplets are required within the conformal approach to supergravity with eight supercharges in diverse dimensions. All solutions in this theory correspond to non-conformally flat superspaces. Its maximally supersymmetric solutions include the so-called critical (4,0) anti-de Sitter superspace introduced in arXiv:1205.4622. Other maximally supersymmetric solutions describe warped critical (4,0) anti-de Sitter superspaces. We also propose a dual formulation for the theory in which the vector multiplet is replaced with an off-shell hypermultiplet. Upon elimination of the auxiliary fields belonging to the hypermultiplet and imposing certain gauge conditions, the dual action reduces to the one introduced in arXiv:1605.00103.

  8. Response of mollusk assemblages from the Luochuan loess section to orbital forcing since the last 250 ka

    Institute of Scientific and Technical Information of China (English)

    2000-01-01

    This note presents a new result of terrestrial mollusk study from the Luochuan loess section since the last 250 ka. A total of 213 samples,taken at intervals of 10 cm in the S0-L3 portion,were analyzed for fossil mollusks. Generally,150 600 individuals were counted in each sample. According to the distribution of mollusk fossil assemblages in the loess section,11 mollusk fossil zones have been recognized,representing different climatic and ecological conditions. Three main ecological groups were identified according to the temperature and moisture requirements of each taxon. The cold-aridiphilous group shows maxima at about 240 220,190 182,150 140 and 74 66 ka BP. The thermo-humidiphilous set has high abundances for at least 6 times in the section at about 246 240,220 216,170 158,92 86,60 44 and 10 kaBP. Our results show that variations in mollusk ecological groups are related with changes in the Earth orbital parameters at the 41 and 20 ka frequencies. Maxima in thermo-humidiphilous taxa are in phase with accretion intervals of obliquity (41 ka period),reflecting the East Asian summer monsoon with 41 ka period in controlling variations in terrestrial mollusk ecological groups. In addition,maxima in thermo- humidiphilous taxa appearing at about 246 240,220 216,60 and 10 kaBP,are consistent with procession (20 ka period) maxima,indicating that the procession period also plays an important role in adjusting the ecological pattern of mollusk groups.

  9. Decadally resolved quantitative temperature reconstruction spanning 5.6 ka at Kurupa Lake, Arctic Alaska

    Science.gov (United States)

    Boldt, B. R.; Kaufman, D. S.; Briner, J. P.

    2012-12-01

    uncertainty estimate does not account for changes in the relation between temperature and pigment concentration through time (non-stationarity). Our chlorophyll-a-inferred temperature reconstruction (50-year smoothed) shows minimum summer temperature (ΔT -2.7 ± 0.8°C relative to the 1961-1990 reference period) at 660 AD and maximum summer temperature (ΔT = +2.3 ± 0.8°C) during the most recent decade. Despite the decrease in northern hemisphere insolation, there is no apparent overall cooling trend through the record. The middle and late Holocene temperatures were punctuated by warmer periods at 3390-2040 cal BP and 710-1060 AD (during the Medieval Climate Anomaly), and by colder temperatures 1110-1310 AD and 1660-1910 AD (a two-phase Little Ice Age). Our temperature reconstruction displays synchronous changes with independent paleoclimatic proxies from elsewhere in Arctic Alaska (e.g., Anderson and Abbott, 2001; Bird et al., 2009), and indicates that the last century was warmer than anytime during the last 5.6 ka.

  10. Cal-Adapt: California's Climate Data Resource and Interactive Toolkit

    Science.gov (United States)

    Thomas, N.; Mukhtyar, S.; Wilhelm, S.; Galey, B.; Lehmer, E.

    2016-12-01

    Cal-Adapt is a web-based application that provides an interactive toolkit and information clearinghouse to help agencies, communities, local planners, resource managers, and the public understand climate change risks and impacts at the local level. The website offers interactive, visually compelling, and useful data visualization tools that show how climate change might affect California using downscaled continental climate data. Cal-Adapt is supporting California's Fourth Climate Change Assessment through providing access to the wealth of modeled and observed data and adaption-related information produced by California's scientific community. The site has been developed by UC Berkeley's Geospatial Innovation Facility (GIF) in collaboration with the California Energy Commission's (CEC) Research Program. The Cal-Adapt website allows decision makers, scientists and residents of California to turn research results and climate projections into effective adaptation decisions and policies. Since its release to the public in June 2011, Cal-Adapt has been visited by more than 94,000 unique visitors from over 180 countries, all 50 U.S. states, and 689 California localities. We will present several key visualizations that have been employed by Cal-Adapt's users to support their efforts to understand local impacts of climate change, indicate the breadth of data available, and delineate specific use cases. Recently, CEC and GIF have been developing and releasing Cal-Adapt 2.0, which includes updates and enhancements that are increasing its ease of use, information value, visualization tools, and data accessibility. We showcase how Cal-Adapt is evolving in response to feedback from a variety of sources to present finer-resolution downscaled data, and offer an open API that allows other organization to access Cal-Adapt climate data and build domain specific visualization and planning tools. Through a combination of locally relevant information, visualization tools, and access to

  11. Ka-band MMIC subarray technology program (Ka-Mist)

    Science.gov (United States)

    Pottinger, W.

    1995-09-01

    Ka-band monolithic microwave integrated circuit (MMIC) arrays have been considered as having high potential for increasing the capability of space, aircraft, and land mobile communication systems in terms of scan performance, data rate, link margin, and flexibility while offering a significant reduction in size, weight, and power consumption. Insertion of MMIC technology into antenna systems, particularly at millimeter wave frequencies using low power and low noise amplifiers in closed proximity to the radiating elements, offers a significant improvement in the array transmit efficiency, receive system noise figure, and overall array reliability. Application of active array technology also leads to the use of advanced beamforming techniques that can improve beam agility, diversity, and adaptivity to complex signal environments. The objective of this program was to demonstrate the technical feasibility of the 'tile' array packaging architecture at EHF via the insertion of 1990 MMIC technology into a functional tile array or subarray module. The means test of this objective was to demonstrate and deliver to NASA a minimum of two 4 x 4 (16 radiating element) subarray modules operating in a transmit mode at 29.6 GHz. Available (1990) MMIC technology was chosen to focus the program effort on the novel interconnect schemes and packaging requirements rather than focusing on MMIC development. Major technical achievements of this program include the successful integration of two 4 x 4 subarray modules into a single antenna array. This 32 element array demonstrates a transmit EIRP of over 300 watts yielding an effective directive power gain in excess of 55 dB at 29.63 GHz. The array has been actively used as the transmit link in airborne/terrestrial mobile communication experiments accomplished via the ACTS satellite launched in August 1993.

  12. Ka-band InSAR Imaging and Analysis Based on IMU Data

    Directory of Open Access Journals (Sweden)

    Shi Jun

    2014-02-01

    Full Text Available Compared with other bands, the millimeter wave Interferometric Synthetic Aperture Radar (InSAR has high accuracy and small size, which is a hot topic in InSAR research. On the other hand, shorter wavelength causes difficulties in 2D imaging and interferometric phase extraction. In this study, the imaging and phase performance of the streaming Back Projection (BP method combined with IMU data are analyzed and discussed on the basis of actual Ka-band InSAR data. It is found that because the wavelength of the Ka-band is short, it is more sensitive to the antenna phase-center history. To ensure the phase-preserving capacity, the IMU data must be used with accurate motion error compensation. Furthermore, during data processing, we verify the flat-earth-removing capacity of the BP algorithm that calculates and compensates the master and slave antenna phase centers individually.

  13. The 100-133 ka record of Italian explosive volcanism and revised tephrochronology of Lago Grande di Monticchio

    Science.gov (United States)

    Wulf, Sabine; Keller, Jörg; Paterne, Martine; Mingram, Jens; Lauterbach, Stefan; Opitz, Stephan; Sottili, Gianluca; Giaccio, Biagio; Albert, Paul G.; Satow, Chris; Tomlinson, Emma L.; Viccaro, Marco; Brauer, Achim

    2012-12-01

    Laminated sediments of the maar lake Lago Grande di Monticchio in southern Italy exhibit a unique sequence of numerous primary tephra events that provide both insights into the Late Quaternary eruptive history of Italian volcanoes and an archive of essential marker horizons for dating and linking palaeoclimate records throughout the Central and Eastern Mediterranean. The acquisition of new sediment cores from this lake now extends the existing 100 ka-tephra record back to 133 ka BP, the end of the penultimate Glacial. The additional ca 30 m of sediments host a total number of 52 single tephra layers forming 21 tephra clusters that have been characterised on the basis of detailed geochemical and petrographical examinations. Tephras can be assigned to hitherto poorly known Plinian to sub-Plinian eruptive events of the nearby Campanian (Ischia Island, Phlegrean Fields), Roman (Sabatini volcanic district) and Aeolian-Sicilian volcanoes (Etna, Stromboli, Salina) and are dated according to the varve and sedimentation rate chronology of Monticchio sediments. The most prominent tephra layers within the interval of investigation - TM-25 and TM-27 - can be firmly correlated with Ionian Sea tephras X-5 (ca 105 ka BP) and X-6 (ca 108-110 ka BP). In addition, a further 26 tephra layers are correlated with radiometrically and radioisotopically dated volcanic events providing the basis for a robust revised tephrochronology of the entire Monticchio sediment sequence for the last 133 ka.

  14. Robust date for the Bronze Age Avellino eruption (Somma-Vesuvius) : 3945 +/- 10 calBP (1995 +/- 10 calBC)

    NARCIS (Netherlands)

    Sevink, Jan; van Bergen, Manfred J.; van der Plicht, Johannes; Feiken, Hendrik; Anastasia, Carmela; Huizinga, Annika; Maroto, Julià; Vaquero, Manuel; Arrizabalaga, Álvaro; Baena, Javier; Baquedano, Enrique; Jordá, Jesús; Julià, Ramon; Montes, Ramón; Rasines, Pedro; Wood, Rachel; Walsma, A.

    2011-01-01

    We found Bronze Age lake sediments from the Agro Pontino graben (Central Italy) to contain a thin (2-3 cm) continuous tephra layer composed of lithics, crystals and minor volcanic glass. Tephrochronological and compositional constraints strongly suggest that this layer represents the Avellino pumice

  15. Maximizing MST's inductive capability with a Bp programmable power supply

    Science.gov (United States)

    Chapman, B. E.; Holly, D. J.; Jacobson, C. M.; McCollam, K. J.; Morin, J. C.; Sarff, J. S.; Squitieri, A.

    2016-10-01

    A major goal of the MST program is the advancement of inductive control for the development of both the RFP's fusion potential and, synergistically, the predictive capability of fusion science. This entails programmable power supplies (PPS's) for the Bt and Bp circuits. A Bt PPS is already in place, allowing advanced RFP operation and the production of tokamak plasmas, and a Bp PPS prototype is under construction. To explore some of the new capabilities to be provided by the Bp PPS, the existing Bt PPS has been temporarily connected to the Bp circuit. One key result is new-found access to very low Ip (20 kA) and very low Lundquist number, S (104). At this low S, simulation of RFP plasmas with the MHD code NIMROD is readily achievable, and work toward validation of extended MHD models using NIMROD is underway with direct comparisons to these MST plasmas. The full Bp PPS will also provide higher Ip and S than presently possible, allowing MST to produce plasmas with S spanning as much as five orders of magnitude, a dramatic extension of MST's capability. In these initial tests, the PPS has also increased five-fold MST's Ip flattop duration, to about 100 ms. This, coupled with the recently demonstrated PPS ability to drive large-amplitude sinusoidal oscillations in Ip, will allow tests of extended-duration oscillating field current drive, the goal of which is ac sustainment of a quasi-dc plasma current. Work supported by US DOE.

  16. CalCOFI Larvae Counts, Scientific Names MB to MO

    Data.gov (United States)

    National Oceanic and Atmospheric Administration, Department of Commerce — Fish larvae counts and standardized counts for larvae captured in CalCOFI icthyoplankton nets (primarily vertical [Calvet or Pairovet], oblique [bongo or ring nets],...

  17. CalCOFI Larvae Counts, Scientific Names SU to TE

    Data.gov (United States)

    National Oceanic and Atmospheric Administration, Department of Commerce — Fish larvae counts and standardized counts for larvae captured in CalCOFI icthyoplankton nets (primarily vertical [Calvet or Pairovet], oblique [bongo or ring nets],...

  18. CalCOFI Larvae Counts, Scientific Names SB to SC

    Data.gov (United States)

    National Oceanic and Atmospheric Administration, Department of Commerce — Fish larvae counts and standardized counts for larvae captured in CalCOFI icthyoplankton nets (primarily vertical [Calvet or Pairovet], oblique [bongo or ring nets],...

  19. CalCOFI Larvae Counts, Scientific Names CD to CH

    Data.gov (United States)

    National Oceanic and Atmospheric Administration, Department of Commerce — Fish larvae counts and standardized counts for larvae captured in CalCOFI icthyoplankton nets (primarily vertical [Calvet or Pairovet], oblique [bongo or ring nets],...

  20. CalCOFI Larvae Counts, Scientific Names NB to OL

    Data.gov (United States)

    National Oceanic and Atmospheric Administration, Department of Commerce — Fish larvae counts and standardized counts for larvae captured in CalCOFI icthyoplankton nets (primarily vertical [Calvet or Pairovet], oblique [bongo or ring nets],...

  1. CalCOFI Larvae Counts, Scientific Names AS to BA

    Data.gov (United States)

    National Oceanic and Atmospheric Administration, Department of Commerce — Fish larvae counts and standardized counts for larvae captured in CalCOFI icthyoplankton nets (primarily vertical [Calvet or Pairovet], oblique [bongo or ring nets],...

  2. CalCOFI Larvae Counts, Scientific Names CP to DE

    Data.gov (United States)

    National Oceanic and Atmospheric Administration, Department of Commerce — Fish larvae counts and standardized counts for larvae captured in CalCOFI icthyoplankton nets (primarily vertical [Calvet or Pairovet], oblique [bongo or ring nets],...

  3. Development and Evaluation of a Computer-Aided Learning (CAL ...

    African Journals Online (AJOL)

    Development and Evaluation of a Computer-Aided Learning (CAL) Package on C++ ... Technology has created a great potential for borderless education. ... packages in the future, thus roviding additional resources for independent learning.

  4. CalCOFI Larvae Counts, Scientific Names C to CE

    Data.gov (United States)

    National Oceanic and Atmospheric Administration, Department of Commerce — Fish larvae counts and standardized counts for larvae captured in CalCOFI icthyoplankton nets (primarily vertical [Calvet or Pairovet], oblique [bongo or ring nets],...

  5. CalCOFI Larvae Counts, Scientific Names LB to LI

    Data.gov (United States)

    National Oceanic and Atmospheric Administration, Department of Commerce — Fish larvae counts and standardized counts for larvae captured in CalCOFI icthyoplankton nets (primarily vertical [Calvet or Pairovet], oblique [bongo or ring nets],...

  6. CalCOFI Larvae Counts, Scientific Names SJ to ST

    Data.gov (United States)

    National Oceanic and Atmospheric Administration, Department of Commerce — Fish larvae counts and standardized counts for larvae captured in CalCOFI icthyoplankton nets (primarily vertical [Calvet or Pairovet], oblique [bongo or ring nets],...

  7. CalCOFI Larvae Counts, Scientific Names OY to PI

    Data.gov (United States)

    National Oceanic and Atmospheric Administration, Department of Commerce — Fish larvae counts and standardized counts for larvae captured in CalCOFI icthyoplankton nets (primarily vertical [Calvet or Pairovet], oblique [bongo or ring nets],...

  8. CalCOFI Larvae Counts, Scientific Names V to Z

    Data.gov (United States)

    National Oceanic and Atmospheric Administration, Department of Commerce — Fish larvae counts and standardized counts for larvae captured in CalCOFI icthyoplankton nets (primarily vertical [Calvet or Pairovet], oblique [bongo or ring nets],...

  9. CalCOFI Larvae Counts, Scientific Names DH to EC

    Data.gov (United States)

    National Oceanic and Atmospheric Administration, Department of Commerce — Fish larvae counts and standardized counts for larvae captured in CalCOFI icthyoplankton nets (primarily vertical [Calvet or Pairovet], oblique [bongo or ring nets],...

  10. California Cooperative Oceanic Fisheries Investigations (CalCOFI)Database

    Data.gov (United States)

    National Oceanic and Atmospheric Administration, Department of Commerce — This database contains icthyoplankton data collected as part of the California Cooperative Oceanic Fisheries Investigations (CalCOFI) program and other cruises...

  11. CalCOFI Larvae Counts, Scientific Names BCE to BZ

    Data.gov (United States)

    National Oceanic and Atmospheric Administration, Department of Commerce — Fish larvae counts and standardized counts for larvae captured in CalCOFI icthyoplankton nets (primarily vertical [Calvet or Pairovet], oblique [bongo or ring nets],...

  12. CalCOFI Larvae Counts, Scientific Names SD to SI

    Data.gov (United States)

    National Oceanic and Atmospheric Administration, Department of Commerce — Fish larvae counts and standardized counts for larvae captured in CalCOFI icthyoplankton nets (primarily vertical [Calvet or Pairovet], oblique [bongo or ring nets],...

  13. CalCOFI Larvae Counts, Scientific Names CI to CO

    Data.gov (United States)

    National Oceanic and Atmospheric Administration, Department of Commerce — Fish larvae counts and standardized counts for larvae captured in CalCOFI icthyoplankton nets (primarily vertical [Calvet or Pairovet], oblique [bongo or ring nets],...

  14. CalCOFI Larvae Counts, Scientific Names LJ to MA

    Data.gov (United States)

    National Oceanic and Atmospheric Administration, Department of Commerce — Fish larvae counts and standardized counts for larvae captured in CalCOFI icthyoplankton nets (primarily vertical [Calvet or Pairovet], oblique [bongo or ring nets],...

  15. CalCOFI Larvae Counts, Scientific Names EV to GN

    Data.gov (United States)

    National Oceanic and Atmospheric Administration, Department of Commerce — Fish larvae counts and standardized counts for larvae captured in CalCOFI icthyoplankton nets (primarily vertical [Calvet or Pairovet], oblique [bongo or ring nets],...

  16. CalCOFI Larvae Counts, Scientific Names A to AM

    Data.gov (United States)

    National Oceanic and Atmospheric Administration, Department of Commerce — Fish larvae counts and standardized counts for larvae captured in CalCOFI icthyoplankton nets (primarily vertical [Calvet or Pairovet], oblique [bongo or ring nets],...

  17. CalCOFI Larvae Counts, Scientific Names Q to SA

    Data.gov (United States)

    National Oceanic and Atmospheric Administration, Department of Commerce — Fish larvae counts and standardized counts for larvae captured in CalCOFI icthyoplankton nets (primarily vertical [Calvet or Pairovet], oblique [bongo or ring nets],...

  18. CalCOFI Larvae Counts, Scientific Names HJ to ID

    Data.gov (United States)

    National Oceanic and Atmospheric Administration, Department of Commerce — Fish larvae counts and standardized counts for larvae captured in CalCOFI icthyoplankton nets (primarily vertical [Calvet or Pairovet], oblique [bongo or ring nets],...

  19. CalCOFI Larvae Counts, Scientific Names PP to PZ

    Data.gov (United States)

    National Oceanic and Atmospheric Administration, Department of Commerce — Fish larvae counts and standardized counts for larvae captured in CalCOFI icthyoplankton nets (primarily vertical [Calvet or Pairovet], oblique [bongo or ring nets],...

  20. CalCOFI Larvae Counts, Scientific Names ED to EU

    Data.gov (United States)

    National Oceanic and Atmospheric Administration, Department of Commerce — Fish larvae counts and standardized counts for larvae captured in CalCOFI icthyoplankton nets (primarily vertical [Calvet or Pairovet], oblique [bongo or ring nets],...

  1. CalCOFI Larvae Counts, Scientific Names PL to PO

    Data.gov (United States)

    National Oceanic and Atmospheric Administration, Department of Commerce — Fish larvae counts and standardized counts for larvae captured in CalCOFI icthyoplankton nets (primarily vertical [Calvet or Pairovet], oblique [bongo or ring nets],...

  2. CalCOFI Larvae Counts, Scientific Names HB to HI

    Data.gov (United States)

    National Oceanic and Atmospheric Administration, Department of Commerce — Fish larvae counts and standardized counts for larvae captured in CalCOFI icthyoplankton nets (primarily vertical [Calvet or Pairovet], oblique [bongo or ring nets],...

  3. CalCOFI Larvae Counts, Scientific Names AN to AR

    Data.gov (United States)

    National Oceanic and Atmospheric Administration, Department of Commerce — Fish larvae counts and standardized counts for larvae captured in CalCOFI icthyoplankton nets (primarily vertical [Calvet or Pairovet], oblique [bongo or ring nets],...

  4. CalCOFI Larvae Counts, Scientific Names MP to NA

    Data.gov (United States)

    National Oceanic and Atmospheric Administration, Department of Commerce — Fish larvae counts and standardized counts for larvae captured in CalCOFI icthyoplankton nets (primarily vertical [Calvet or Pairovet], oblique [bongo or ring nets],...

  5. Paleomagnetic secular variation at the Azores during the last 3 ka

    Science.gov (United States)

    Di Chiara, A.; Speranza, F.; Porreca, M.

    2012-12-01

    We report on 33 new paleomagnetic directions obtained from 16 lava flows emplaced in the last 3 ka on São Miguel, the largest island of the Azores. The data provide 27 directions from historical or 14C dated flows which, together with 6 directions previously gathered from the same flows by Johyson et al., (1998), yield the first paleomagnetic record of the last 3 ka from the Atlantic Ocean. Within-flow directions are consistent, suggesting that inclination swings from 60° to 25° and declination changes between -10° to 20° reflect variations in the geomagnetic field over the last 3 ka. To a first approximation, the declination record is consistent with predictions from CALS3k.4 and gufm1 global field models. Conversely, inclination values are lower than model predictions at two different ages: 1) four different sites from the 1652 AD flow yield I=48° instead of I=63° predicted by gufm1; 2) data from several flows nicely mimic the inclination minimum of 800-1400 AD, but inclination values are lower by ca. 10° than CALS3k.4 model predictions. By interpolating a cubic spline fit on declination / inclination versus age data, we tentatively infer the directional evolution of the geomagnetic field at the Azores from 1000 BC to 1600 AD.The obtained curve shows three tracks in virtual overlap during the 1000-800 BC, 800-500 BC, and 400-700 AD time spans; Cubic spline interpolation of flow mean declinations (a) and inclinations (b) versus respective calendar ages; c) directions derived every 100 years from cubic spline interpolation, superimposed on paleomagnetic directions (and relative confidence cones) from three loosely-dated flows (Fig. 1). For ages older than 750 AD the fit line is dashed, as it is constrained by a limited number of data. Vertical error bars for declination and inclination data are α95 /cos(I) and α95 values, respectively

  6. AltiKa in-flight performances

    Science.gov (United States)

    Boy, Francois; Desjonquères, Jean-Damien; Steunou, Nathalie

    2015-04-01

    The SARAL/AltiKa satellite has been launched the 25th of February 2013 from the launch pad of Sriharikota (India). Since this date, AltiKa provides measurements and affords the first altimetry results in Ka band. This paper recalls the instrument design and assesses the in-flight performance. The SARAL/AltiKa mission has been developed in the frame of a cooperation between CNES (French Space Agency) and ISRO (Indian Space Research Organization). AltiKa is a single frequency Ka-band altimeter with a bi-frequency radiometer embedded. Both altimeter and radiometer share the same antenna. Altimeter expertise and routine calibrations performed during assessment phase demonstrate the stability of the instrument. Moreover the performance assessed over ocean are noteworthy such as 0.9 cm on epoch 1 Hz noise for 2 m of SWH, which is fully consistent with simulations and ground pre-flight tests results. The data availability is also very good and very few altimeter measurements are lost due to rain attenuation. Radiometer data analysis shows that the instrument is very stable and its performances are consistent with pre-flight tests results.

  7. Ionization constants pKa of cardiolipin.

    Directory of Open Access Journals (Sweden)

    Gerd Olofsson

    Full Text Available Cardiolipin is a phospholipid found in the inner mitochondrial membrane and in bacteria, and it is associated with many physiological functions. Cardiolipin has a dimeric structure consisting of two phosphatidyl residues connected by a glycerol bridge and four acyl chains, and therefore it can carry two negative charges. The pKa values of the phosphate groups have previously been reported to differ widely with pKa1 = 2.8 and pKa2 = 7.5-9.5. Still, there are several examples of experimental observations from cardiolipin-containing systems that do not fit with this dissociation behavior. Therefore, we have carried out pH-titration and titration calorimetric experiments on two synthetic cardiolipins, 1,1',2,2'-tetradecanoyl cardiolipin, CL (C14:0, and 1,1',2,2'-tetraoctadecenoyl cardiolipin, CL (C18:1. Our results show that both behave as strong dibasic acids with pKa1 about the same as the first pKa of phosphoric acid, 2.15, and pKa2 about one unit larger. The characterization of the acidic properties of cardiolipin is crucial for the understanding of the molecular organization in self-assembled systems that contain cardiolipin, and for their biological function.

  8. Birth of the modern Chesapeake Bay estuary between 7.4 and 8.2 ka and implications for global seal-level rise

    Science.gov (United States)

    Bratton, J.F.; Colman, Steven M.; Thieler, E.R.; Seal, R.R.

    2003-01-01

    Two major pulses of sea-level rise are thought to have taken place since the last glacial maximum - meltwater pulses (mwp) 1A (12 cal ka) and 1B (9.5 cal ka). Between mwp 1B and about 6 cal ka, many of the complex coastal ecosystem which ring the world's oceans began to form. Here we report data for rhenium, carbon isotopes, total organic carbon, and fossil oysters from Chesapeake Bay which span the transition from fresh to brackish water conditions in the bay in the mid-Holocene. These data constrain sea-level change and resulting environmental change in the bay. They indicate that the transition was rapid, and that it was produced by (1) a third pulse of rapid eustatic sea-level rise, or (2) a geometry of the prehistoric Chesapeake Bay basin which predisposed it to a nonlinear response to a steadily rising sea level. Similar nonlinear changes in vulnerable coastal environments are likely to take place in the future due to polar warming, regardless of the timing or rate of sea-level rise.

  9. Birth of the modern Chesapeake Bay estuary between 7.4 and 8.2 ka and implications for global sea-level rise

    Science.gov (United States)

    Bratton, John F.; Colman, Steven M.; Thieler, E. Robert; Seal, Robert R.

    2002-12-01

    Two major pulses of sea-level rise are thought to have taken place since the last glacial maximum — meltwater pulses (mwp) 1A (12 cal ka) and 1B (9.5 cal ka). Between mwp 1B and about 6 cal ka, many of the complex coastal ecosystems which ring the world's oceans began to form. Here we report data for rhenium, carbon isotopes, total organic carbon, and fossil oysters from Chesapeake Bay which span the transition from fresh to brackish water conditions in the bay in the mid-Holocene. These data constrain sea-level change and resulting environmental change in the bay. They indicate that the transition was rapid, and that it was produced by (1) a third pulse of rapid eustatic sea-level rise, or (2) a geometry of the prehistoric Chesapeake Bay basin which predisposed it to a nonlinear response to a steadily rising sea level. Similar nonlinear changes in vulnerable coastal environments are likely to take place in the future due to polar warming, regardless of the timing or rate of sea-level rise.

  10. HORNO DE CAL [Material gráfico

    OpenAIRE

    Fundación para la Etnografía y el Desarrollo de la Artesanía Canaria

    1990-01-01

    ANTIGUO HORNO DE CAL QUE DISTRIBUIA SU PRODUCCION POR TODA LA ZONA SUR. CONSTA DE SEIS HORNOS, QUE EN SU DIA DESTINABAN LA PRODUCCIÓN DE CAL A TODA LA ISLA, SIENDO DE LOS HORNOS CON MAYOR PRODUCCIÓN. UNO DE SUS ULTIMOS EMPLEADOS FUE JUAN RAMOS ACOSTA, QUE RECUERDA QUE SIETE HOMBRES DEAMBULABAN DURANTE DOCE HORAS EN TORNO A UNOS HORNOS QUE NO SE APAGABAN NUNCA, LLEGÁNDOSE A LOS 7.000 GRADOS, Y CURÁNDOSE LAS QUEMADURAS CON ORINES. Antiguedad: SIGLO XX Calificación del suelo: URBANO NO CO...

  11. GAVDOS/west crete cal-val site: Over a decade calibrations for Jason series, SARAL/Altika, cryoSat-2, Sentinel-3 and HY-2 altimeter satellites

    DEFF Research Database (Denmark)

    Mertikas, Stelios; Tziavos, Ilias; Galanakis, Demitris

    for the ascending Pass No.109 and the descending Pass No.18, based on the the GDR-E (Jason-1) and GDR-D (Jason-2) products. Secondly, these values will be cross-examined against the altimeter bias for the SARAL/AltiKa (GDR-T) satellite at Gavdos Cal/Val using its reference ascending orbit No. 571. The Chinese HY-2...

  12. Data of evolutionary structure change: 1KA4A-1WGZA [Confc[Archive

    Lifescience Database Archive (English)

    Full Text Available 1KA4A-1WGZA 1KA4 1WGZ A A EVFQNETIKQILAKYRRIWAIGHAQSVLGWDLEVNMPKE...confEVID> 0 1KA4 A 1KA4A...tryChain> 1KA4 A 1KA4A FPLGTRARLD... CA 334 SER CA 255 1KA4 A 1KA4A LEEGKVPREHP HH

  13. Medi-Cal blamed for poor care in lawsuit

    Directory of Open Access Journals (Sweden)

    Robbins RA

    2017-07-01

    Full Text Available No abstract available. Article truncated at 150 words. Several sources are reporting a lawsuit filed in California alleging poor care in the state’s Medicaid program, Medi-Cal (1. The suit alleges that Medi-Cal failed to pay doctors enough to provide proper care. The suit was filed by five Latino residents on behalf of California’s 13 million lower-income residents, more than half of them Latinos. The suit alleges that "…California has created a separate and unequal system of health care, one for the insurance program with the largest proportion of Latinos (Medi-Cal, and one for the other principal insurance plans, whose recipients are disproportionately white.” The state budget includes $107 billion in state and federal funding for Medi-Cal this year, but the spending is not enough to restore reimbursement cuts made during the Great Recession of 2008. A proposal in the U.S. Senate to repeal the Affordable Health Care law (ACA, Obamacare could drastically reduce funding for Medicare and the …

  14. The 8.2 ka event in the northern Alps

    Science.gov (United States)

    Luetscher, M.; Hoffmann, D. L.; Müller, W.; Spötl, C.

    2012-04-01

    The 8.2 ka event has been identified as a widespread climate excursion affecting most of the Northern Hemisphere. High-resolution records from ice cores and speleothems constrain the chronology of this event to between 8.21±0.02 and 8.08±0.03 ka BP (Vinther et al. 2006, Cheng et al. 2009). A distinctive asymmetrical pattern in d18O is consistent with modelling results suggesting rapid input of freshwater into the northern Atlantic due to catastrophic drainage of ice-marginal lakes (LeGrande et al., 2008). Despite an increasing amount of data, the regional expression of this event is still poorly understood. Here, we present a new speleothem record from Gasselhöhle in the Northern Calcareous Alps, Austria. The 205 mm-long GAS19 stalagmite was analysed at high resolution for stable isotopes (100 µm) and trace elements (~10-15 µm; continuous LA-ICPMS profiles). Twelve individual MC-ICP-MS U/Th ages underline an annual growth rate of ca. 60 µm during the Early Holocene. The d18O averages -8.9‰, only slightly more depleted than modern carbonate precipitates from the same cave chamber. The 8.2 ka event is marked in GAS19 by a ca. 1‰ excursion with a minimum value of -9.9‰. Largely invariant trace element concentrations (e.g. Mg, U, Sr, Ba) indicate essentially no changes in the local hydrological regime and therefore support the hypothesis of a temperature-dominated signal. The proximity to the lacustrine isotope record from Mondsee (eg. Lauterbach et al. 2011) opens new perspectives for the interpretation of the oxygen isotope signal using two archives at different elevations. Moreover, several coeval speleothem records are available across the Eastern Alps fostering a spatial comparison of the proxy signals associated with this event. Cheng, H. et al. (2009), Geology, 37, 1007-1010 Lauterbach, S. et al. (2011), JQS, 26, 253-267 LeGrande, A.N., Schmidt, G.A. (2008), Paleoceanography, 23, doi: 10.1029/2008PA001610 Vinther, B. et al. (2006), JGR, 111, D13103

  15. A 20-ka reconstruction of a Sahelo-Sudanian paleoenvironment using multi-method dating on pedogenic carbonate

    Science.gov (United States)

    Diaz, Nathalie; Dietrich, Fabienne; King, Georgina E.; Valla, Pierre G.; Sebag, David; Herman, Frédéric; Verrecchia, Eric P.

    2016-04-01

    Soils can be precious environmental archives as they are open systems resulting from external persistent disturbance, or forcing (Jenny, 1941). Pedogenic carbonate nodules associated with clay-rich soils have been investigated in the Far North region of Cameroon in non-carbonate watersheds (Chad Basin). Nodule bearing soils have mima-like mound morphologies, within stream networks. Such settings raise questions on the processes leading to carbonate precipitation as well as landscape genesis. The mima-like mounds have been identified as degraded Vertisols, resulting from differential erosion induced by a former gilgai micro-relief (Diaz et al., 2016). Non-degraded Vertisols occur in waterlogged areas, located downstream from mima-like mound locations (Braband and Gavaud, 1985). Therefore during a former wetter period Vertisols may have been extended to the mima-like mound areas, followed by a shift toward drier conditions and erosion (Diaz et al., 2016). Consequently, mima-like mounds and associated carbonate nodules are inherited from climatic changes during the Late Pleistocene-Holocene period. The aim of this study is to validate the scenario above using the carbonate nodules collected in a mima-like mound as time archives. Optically stimulated luminescence (OSL) dating of K-feldspars trapped within the nodules is used to assess the deposition time of the soil parent material, composing the mima-like mounds. The carbonate and organic nodule parts have been radiocarbon dated with the aim of assessing the carbonate precipitation age and the age range of soil formation, respectively. Results show that the soil parent material was deposited between 18 ka and 12 ka BP and that the nodules precipitated between 7 ka and 5 ka BP. These results suggest that the deposition occurred during the arid climatic period of the Bossoumian (20 ka to 15 ka BP; Hervieu, 1970) and during the first drier part of the African Humid Period (14.8 ka to 11.5 ka BP; deMenocal et al., 2000

  16. The Mars Global Surveyor Ka-Band Link Experiment (MGS/KaBLE-II)

    Science.gov (United States)

    Morabito, D.; Butman, S.; Shambayati, S.

    1999-01-01

    The Mars Global Surveyor (MGS) spacecraft, launched on November 7, 1996, carries an experimental space-to-ground telecommunications link at Ka-band (32 GHz) along with the primary X-band (8.4-GHz) downlink. The signals are simultaneously transmitted from a 1.5-m-diameter parabolic antenna on MGS and received by a beam-waveguide (BWG) research and development (R&D) 34-meter a ntenna located in NASA's Goldstone Deep Space Network (DSN) complex near Barstow, California. This Ka-band link experiment (KaBLE-II) allows the performances of the Ka-band and X-band signals to be compared under nearly identical conditions. The two signals have been regularly tracked during the past 2 years. This article presents carrier-signal-level data (P_c/N_o) for both X-band and Ka-band acquired over a wide range of station elevation angles, weather conditions, and solar elongation angles. The cruise phase of the mission covered the period from launch (November 7, 1996) to Mars orbit capture (September 12, 1997). Since September 12, 1997, MGS has been in orbit around Mars. The measurements confirm that Ka-band could increase data capacity by at least a factor of three (5 dB) as compared with X-band. During May 1998, the solar corona experiment, in which the effects of solar plasma on the X-band and Ka-band links were studied, was conducted. In addition, frequency and difference frequency (f_x - f_(Ka)/3.8), ranging, and telemetry data results are presented. MGS/KaBLE-II measured signal strengths (for 54 percent of the experiments conducted) that were in reasonable agreement with predicted values based on preflight knowledge, and frequency residuals that agreed between bands and whose statistics were consistent with expected noise sources. For passes in which measured signal strengths disagreed with predicted values, the problems were traced to known deficiencies, for example, equipment operating under certain conditions, such as a cold Ka-band solid-state power amplifier (SSPA

  17. Paleointensities on 8 ka obsidian from Mayor Island, New Zealand

    Directory of Open Access Journals (Sweden)

    A. Ferk

    2011-11-01

    Full Text Available The 8 ka BP (6050 BCE pantelleritic obsidian flow on Mayor Island, Bay of Plenty, New Zealand, has been investigated using 30 samples from two sites. Due to a very high paramagnetic/ferromagnetic ratio, it was not possible to determine the remanence carriers. This is despite the fact that the samples were studied intensively at low, room, and high temperatures. We infer that a stable remanence within the samples is carried by single- or close to single-domain particles. Experiments to determine the anisotropy of thermoremanence tensor and the dependency on cooling rate were hampered due to alteration resulting from the repeated heating of the samples to temperatures just below the glass transition. Nonetheless, a well-defined mean paleointensity of 57.0 ± 1.0 μT, based on individual high quality paleointensity determinations, was obtained. This field value compares very well to a paleointensity of 58.1 ± 2.9 μT, which Tanaka et al. (2009 obtained for 5500 BCE at a site 100 km distant. Agreement with geomagnetic field models, however, is poor. Thus, gathering more high-quality paleointensity data for the Pacific region and for the southern hemisphere in general to better constrain global field models is very important.

  18. Logarithmic Corrections to the Black Hole Entropy Product of ${\\cal H}^{\\pm}$ via Cardy Formula

    CERN Document Server

    Pradhan, Parthapratim

    2016-01-01

    We compute the logarithmic corrections to the black hole (BH) entropy product of ${\\cal H}^{\\pm}$ \\footnote{ ${\\cal H}^{+}$ and ${\\cal H}^{-}$ denote outer (event) horizon and inner (Cauchy) horizons} by using \\emph{Cardy prescription}. We particularly apply this formula for BTZ BH. We show that logarithmic corrections to the entropy product of ${\\cal H}^{\\pm}$ when computed \\emph{via Cardy formula} it does not mass-independent (universal) nor does it quantized.

  19. Manifestations of CAL F-- and CAL EP--transients in radio emission based on "Zimenki" station data

    Science.gov (United States)

    Durasova, M. S.; Fridman, V. M.; Sheiner, O. A.

    The actual direction in the study of solar activity is the study of coronal mass ejection (CME). The onsets of CMEs associated with the flares are called in literature as cal F--transients. There are cases, when CME are not accompanied by flare phenomena in the optical range, although such processes have to associate the dynamical phenomena in the solar atmosphere. Such CMEs are called below cal EP--transients. It is assumed valid, that phenomena connected with formation of cal EP--transients must be manifested in radio emission, which reflects the processes at different levels of the solar atmosphere. We began our study with the examining the manifestations of cal EP--transients in radio emission, because of their lower energy levels than cal F--transients have, supposed that in that case there was the possibility to distinguish the typical features of these phenomenon. We considered the data of sixteen examples of observations made in 1980 and 1984--1989 connected with cal EP--transients. In the analysis we used the observational data of CME (Burkepile and Cyr 1993), the SGD data of the solar flares as well as the original records of observations of the solar radio emission fluxes at "Zimenki" station at six frequencies in the range of 9100--100 MHz. According to the data of optical observations during two--hour period before the registration of the transient, the flares either were not observed or weak flare events were observed but sufficiently far from the solar regions where the transient was formed. During the same time interval sufficiently bursts S and GRF types in the microwave emission were observed. As a rule, in the considered period of time, noise storms were registered at the meter wavelengths, the intensity of which decreased or fluctuated in the time interval preceding the registration of the transient at SMM. It allowed us to analyse radio spectra of manifestations and to give the estimation of appearance of several radio signs in CME-events on

  20. A comparison of the Greenland Ice-Core and IntCal timescales through the Laschamp geomagnetic excursion, utilising new 14c data from Tenaghi Philippon, Greece

    Science.gov (United States)

    Staff, Richard A.; Hardiman, Mark; Bronk Ramsey, Christopher; Koutsodendris, Andreas; Pross, Jörg

    2016-04-01

    Cosmogenic radionuclides, such as 10Be and 14C, share a common production signal, with their formation in the Earth's upper atmosphere modulated by changes to the geomagnetic field, as well as variations in the intensity of the solar wind. Here, we present 54 new 14C measurements from a terrestrial fen peat core extracted from the classical site of Tenaghi Philippon, NE Greece, contiguously spanning the time period between ~48,000 and 39,000 cal. BP. Utilising the most pronounced cosmogenic production peak of the last 100,000 years - that associated with the Laschamp geomagnetic excursion circa 41,000 years ago - we exploit this common production signal, comparing Greenland 10Be with our Tenaghi Philippon 14C record, thereby providing a means to assess the concordance between the radiocarbon (IntCal) and Greenland ice-core (GICC05) timescales themselves for this, the oldest portion of the radiocarbon technique.

  1. Modulation transfer functions at Ka band

    Science.gov (United States)

    Hesany, Vahid; Sistani, Bita; Salam, Asif; Haimov, Samuel; Gogineni, Prasad; Moore, Richard K.

    The modulation transfer function (MTF) is often used to describe the modulation of the radar signal by the long waves. MTFs were measured at 35 GHz (Ka band) with a switched-beam vector slope gauge/scatterometer on the research platform NORDSEE as part of the SAXON-FPN experiment. Three independent measurements of the scattering were available for each height measurement. This provided the opportunity to average the time series to reduce the effects of fading noise and sea spikes, or, alternatively, to append the time series to achieve more degrees of freedom in the spectral estimates. For upwind measurements, the phase of the VV-polarized Ka-band MTF was always positive, which implies that the maximum of the radar return originates from the forward face of the long-scale waves. This phase increases with increasing wind speed. The magnitude of the MTF decreases with increasing wind speed.

  2. [Enforcement of type M 20 cal. 4 mm cartridges].

    Science.gov (United States)

    Dobosz, Tadeusz; Jaworski, Ryszard; Kawecki, Jerzy; Semiczek, Wiesław; Trnka, Jakub

    2002-01-01

    The aim of the paper was to investigate and compare the speed and energy of a bullet from 4 mm cal. cartridges of central ignition type M20, both original and transformed by addition of different kinds of propellants. Original cartridges are characterized by an average speed of the bullet of 144 m/s and average energy of 4.8 J. After transformation by the addition of on an average 31.3 mg of smokeless powder from a cartridge type LR'22, a maximum bullet speed of 299 m/s (average) and maximum energy of 21.2 joule (average) were reached. Our test showed that shots using transformed ammunition type M 20 cal. 4 mm can be dangerous for both health and life. Multiple M20 shot wounds may be very similar to single shot wounds caused by a shotshell cartridge fired from a shotgun weapon.

  3. File list: ALL.Brs.20.AllAg.CAL-51 [Chip-atlas[Archive

    Lifescience Database Archive (English)

    Full Text Available ALL.Brs.20.AllAg.CAL-51 hg19 All antigens Breast CAL-51 ERX348279,ERX348278,ERX3482...8277,ERX348288,ERX348291,ERX348282,ERX348284,ERX348280,ERX348272 http://dbarchive.biosciencedbc.jp/kyushu-u/hg19/assembled/ALL.Brs.20.AllAg.CAL-51.bed ...

  4. File list: ALL.Bld.50.AllAg.CAL1 [Chip-atlas[Archive

    Lifescience Database Archive (English)

    Full Text Available ALL.Bld.50.AllAg.CAL1 hg19 All antigens Blood CAL1 SRX220960,SRX220958,SRX220959,SR...X471323,SRX471324 http://dbarchive.biosciencedbc.jp/kyushu-u/hg19/assembled/ALL.Bld.50.AllAg.CAL1.bed ...

  5. File list: ALL.Bld.20.AllAg.CAL1 [Chip-atlas[Archive

    Lifescience Database Archive (English)

    Full Text Available ALL.Bld.20.AllAg.CAL1 hg19 All antigens Blood CAL1 SRX220960,SRX220959,SRX471323,SR...X220958,SRX471324 http://dbarchive.biosciencedbc.jp/kyushu-u/hg19/assembled/ALL.Bld.20.AllAg.CAL1.bed ...

  6. File list: NoD.Brs.50.AllAg.CAL-51 [Chip-atlas[Archive

    Lifescience Database Archive (English)

    Full Text Available NoD.Brs.50.AllAg.CAL-51 hg19 No description Breast CAL-51 ERX348279,ERX348278,ERX34...348285,ERX348284,ERX348288,ERX348291,ERX348282,ERX348280,ERX348272 http://dbarchive.biosciencedbc.jp/kyushu-u/hg19/assembled/NoD.Brs.50.AllAg.CAL-51.bed ...

  7. File list: ALL.Brs.10.AllAg.CAL-51 [Chip-atlas[Archive

    Lifescience Database Archive (English)

    Full Text Available ALL.Brs.10.AllAg.CAL-51 hg19 All antigens Breast CAL-51 ERX348292,ERX348289,ERX3482...8272,ERX348280,ERX348283,ERX348285,ERX348288,ERX348291,ERX348282 http://dbarchive.biosciencedbc.jp/kyushu-u/hg19/assembled/ALL.Brs.10.AllAg.CAL-51.bed ...

  8. File list: ALL.Brs.05.AllAg.CAL-51 [Chip-atlas[Archive

    Lifescience Database Archive (English)

    Full Text Available ALL.Brs.05.AllAg.CAL-51 hg19 All antigens Breast CAL-51 ERX348277,ERX348289,ERX3482...8281,ERX348272,ERX348280,ERX348285,ERX348288,ERX348291,ERX348282 http://dbarchive.biosciencedbc.jp/kyushu-u/hg19/assembled/ALL.Brs.05.AllAg.CAL-51.bed ...

  9. File list: NoD.Brs.20.AllAg.CAL-51 [Chip-atlas[Archive

    Lifescience Database Archive (English)

    Full Text Available NoD.Brs.20.AllAg.CAL-51 hg19 No description Breast CAL-51 ERX348279,ERX348278,ERX34...348277,ERX348288,ERX348291,ERX348282,ERX348284,ERX348280,ERX348272 http://dbarchive.biosciencedbc.jp/kyushu-u/hg19/assembled/NoD.Brs.20.AllAg.CAL-51.bed ...

  10. File list: ALL.Bld.05.AllAg.CAL1 [Chip-atlas[Archive

    Lifescience Database Archive (English)

    Full Text Available ALL.Bld.05.AllAg.CAL1 hg19 All antigens Blood CAL1 SRX220960,SRX220959,SRX220958,SR...X471323,SRX471324 http://dbarchive.biosciencedbc.jp/kyushu-u/hg19/assembled/ALL.Bld.05.AllAg.CAL1.bed ...

  11. File list: NoD.Brs.05.AllAg.CAL-51 [Chip-atlas[Archive

    Lifescience Database Archive (English)

    Full Text Available NoD.Brs.05.AllAg.CAL-51 hg19 No description Breast CAL-51 ERX348277,ERX348289,ERX34...348281,ERX348272,ERX348280,ERX348285,ERX348288,ERX348291,ERX348282 http://dbarchive.biosciencedbc.jp/kyushu-u/hg19/assembled/NoD.Brs.05.AllAg.CAL-51.bed ...

  12. File list: ALL.Bld.10.AllAg.CAL1 [Chip-atlas[Archive

    Lifescience Database Archive (English)

    Full Text Available ALL.Bld.10.AllAg.CAL1 hg19 All antigens Blood CAL1 SRX220960,SRX220958,SRX220959,SR...X471323,SRX471324 http://dbarchive.biosciencedbc.jp/kyushu-u/hg19/assembled/ALL.Bld.10.AllAg.CAL1.bed ...

  13. File list: NoD.Brs.10.AllAg.CAL-51 [Chip-atlas[Archive

    Lifescience Database Archive (English)

    Full Text Available NoD.Brs.10.AllAg.CAL-51 hg19 No description Breast CAL-51 ERX348292,ERX348289,ERX34...348272,ERX348280,ERX348283,ERX348285,ERX348288,ERX348291,ERX348282 http://dbarchive.biosciencedbc.jp/kyushu-u/hg19/assembled/NoD.Brs.10.AllAg.CAL-51.bed ...

  14. File list: ALL.Brs.50.AllAg.CAL-51 [Chip-atlas[Archive

    Lifescience Database Archive (English)

    Full Text Available ALL.Brs.50.AllAg.CAL-51 hg19 All antigens Breast CAL-51 ERX348279,ERX348278,ERX3482...8285,ERX348284,ERX348288,ERX348291,ERX348282,ERX348280,ERX348272 http://dbarchive.biosciencedbc.jp/kyushu-u/hg19/assembled/ALL.Brs.50.AllAg.CAL-51.bed ...

  15. KaKa带你杀大网

    Institute of Scientific and Technical Information of China (English)

    昊月

    2005-01-01

    上期和大家一起漫步dust2,体会了其中的妙处,这期KaKa带你去inferno这张地图探个究竟。inferno是一张对于警匪都比较平衡的地图,攻守都有各自的优势,如何利用这些优势让自己在大网里的杀人数剧增,是KaKa这期要告诉大家的重点。上次KaKa教大家如果做匪徒在大网里杀人,这次咱做警察,练练如何在大网里防守,这次我们进一个开局金钱数16000的大网里,免得初期还要手枪肉搏。一切准备就绪,开局买上M4,炸宙,闪光再带把拆包器,可能会有人有疑问。”又不是打比赛,要买拆包器干吗?杀光敌人不就得了吗。”KaKa在这里还要提醒你一点.1.5版和1.6版其中的一个小区别就是如果警察成功拆除炸弹的话,可以增加3个杀人数,所以只要有机会就奋不顾身去抢拆包,这也算是提高自己在大网里杀人数一个“歪门邪道”,可比你和3个匪徒周旋半天划得来哦。

  16. Engineering wavefront caustics trajectories in ${\\cal PT}$-symmetric lattices

    CERN Document Server

    Bender, Nicholas; Kottos, Tsampikos

    2015-01-01

    We utilize caustic theory in ${\\cal PT}-$symmetric lattices to design focusing and curved beam dynamics. We show that the gain and loss parameter in these systems provides an addition degree of freedom which allows for the design of the same caustics trajectories with different intensity distribution in the individual waveguides. Moreover we can create aberration-free focal points at any paraxial distance $z_f$, with anomalously large focal intensity.

  17. On consistent truncations in ${\\cal N}=2^*$ holography

    CERN Document Server

    Balasubramanian, Venkat

    2013-01-01

    Although Pilch-Warner (PW) gravitational renormalization group flow [arXiv:hep-th/0004063] passes a number of important consistency checks to be identified as a holographic dual to a large-$N$ $SU(N)$ ${\\cal N}=2^*$ supersymmetric gauge theory, it fails to reproduce the free energy of the theory on $S^4$, computed with the localization techniques. This disagreement points to the existence of a larger dual gravitational consistent truncation, which in the gauge theory flat-space limit reduces to a PW flow. Such truncation was recently identified by Bobev-Elvang-Freedman-Pufu (BEFP) [arXiv:1311.1508]. Additional bulk scalars of the BEFP gravitation truncation might lead to destabilization of the finite-temperature deformed PW flows, and thus modify the low-temperature thermodynamics and hydrodynamics of ${\\cal N} =2^*$ plasma. We compute the quasinormal spectrum of these bulk scalar fields in the thermal PW flows and demonstrate that these modes do not condense, as long as the masses of the ${\\cal N}=2^*$ hyper...

  18. Pollen-based paleoenvironmental and paleoclimatic change at Lake Ohrid (SE Europe during the past 500 ka

    Directory of Open Access Journals (Sweden)

    L. Sadori

    2015-09-01

    Full Text Available Lake Ohrid is located at the border between FYROM and Albania and formed during the latest phases of Alpine orogenesis. It is the deepest, the largest and the oldest tectonic lake in Europe. To better understand the paleoclimatic and paleoenvironmental evolution of Lake Ohrid a deep drilling was carried out in 2013 within the framework of the Scientific Collaboration on Past Speciation Conditions (SCOPSCO project that was funded by the International Continental Drilling Program (ICDP. Preliminary results indicate that lacustrine sedimentation of Lake Ohrid started between 1.2 and 1.9 Ma ago. Here we present new pollen data (selected percentage and concentration taxa/groups of the uppermost ~200 m of the 569 m-long DEEP core drilled in the depocenter of Lake Ohrid. The study is the fruit of a cooperative work carried out in several European palynological laboratories. The age model is based on nine tephra layers and on tuning of biogeochemical proxy data to orbital parameters and to the global benthic isotope stack LR04. According to the age model the studied sequence covers the last ~500 000 years at a millennial-scale resolution (~1.6 ka and record the major vegetation and climate changes that occurred during the last 12 (13 only pro parte marine isotope stages (MIS. Our results indicate that there is a general good correspondence between forested/non-forested periods and glacial/interglacial cycles of marine isotope stratigraphy. Our record shows a progressive change from cooler and wetter to warmer and dryer interglacial conditions. This shift is visible also in glacial vegetation. The interglacial phase corresponding to MIS11 (pollen assemblage zone, PAZ OD-12, 488–455 ka BP and OD-19, 367–328 ka BP is dominated by montane trees such as conifers. The two younger interglacial periods, MIS5 (PAZ OD-3, 126–70 ka BP and MIS1 (PAZ OD-1, 12 ka BP to present are marked by dominance of mesophilous elements such as deciduous and semi

  19. Paleoseismic investigations at the Cal thrust fault, Mendoza, Argentina

    Science.gov (United States)

    Salomon, Eric; Schmidt, Silke; Hetzel, Ralf; Mingorance, Francisco

    2010-05-01

    Along the active mountain front of the Andean Precordillera between 30°S and 34°S in western Argentina several earthquakes occurred in recent times, including a 7.0 Ms event in 1861 which destroyed the city of Mendoza and killed two thirds of its population. The 1861 event and two other earthquakes (Ms = 5.7 in 1929 and Ms = 5.6 in 1967) were generated on the Cal thrust fault, which extends over a distance of 31 km north-south and runs straight through the center of Mendoza. In the city, which has now more than 1 million inhabitants, the fault forms a 3-m-high fault scarp. Although the Cal thrust fault poses a serious seismic hazard, the paleoseismologic history of this fault and its long-term slip rate remains largely unknown (Mingorance, 2006). We present the first results of an ongoing paleoseismologic study of the Cal thrust at a site located 5 km north of Mendoza. Here, the fault offsets Late Holocene alluvial fan sediments by 2.5 m vertically and exhibits a well developed fault scarp. A 15-m-long and 2-3-m-deep trench across the scarp reveals three east-vergent folds that we interpret to have formed during three earthquakes. Successive retrodeformation of the two youngest folds suggests that the most recent event (presumably the 1861 earthquake) caused ~1.1 m of vertical offset and ~1.8 m of horizontal shortening. For the penultimate event we obtain a vertical offset of ~0.7 m and a horizontal shortening of ~1.9 m. A vertical displacement of ~0.7 m observed on a steeply west-dipping fault may be associated with an older event. The cumulative vertical offset of 2.5 m for the three inferred events is in excellent agreement with the height of the scarp. Based on the retrodeformation of the trench deposits the fault plane dips ~25° to the west. In the deepest part of the trench evidence for even older seismic events is preserved beneath an angular unconformity that was formed during a period of erosion and pre-dates the present-day scarp. Dating of samples to

  20. Validation of GPM Ka-Radar Algorithm Using a Ground-based Ka-Radar System

    Science.gov (United States)

    Nakamura, Kenji; Kaneko, Yuki; Nakagawa, Katsuhiro; Furukawa, Kinji; Suzuki, Kenji

    2016-04-01

    GPM led by the Japan Aerospace Exploration Agency (JAXA) and the National Aeronautics and Space Administration of US (NASA) aims to observe global precipitation. The core satellite is equipped with a microwave radiometer (GMI) and a dual-frequency radar (DPR) which is the first spaceborne Ku/Ka-band dual-wavelength radar dedicated for precipitation measurement. In the DPR algorithm, measured radar reflectivity is converted to effective radar reflectivity by estimating the rain attenuation. Here, the scattering/attenuation characteristics of Ka-band radiowaves are crucial, particularly for wet snow. A melting layer observation using a dual Ka-band radar system developed by JAXA was conducted along the slope of Mt. Zao in Yamagata Prefecture, Japan. The dual Ka-band radar system consists of two nearly identical Ka-band FM-CW radars, and the precipitation systems between two radars were observed in opposite directions. From this experiment, equivalent radar reflectivity (Ze) and specific attenuation (k) were obtained. The experiments were conducted for two winter seasons. During the data analyses, it was found that k estimate easily fluctuates because the estimate is based on double difference calculation. With much temporal and spatial averaging, k-Ze relationship was obtained for melting layers. One of the results is that the height of the peak of k seems slightly higher than that of Ze. The results are compared with in-situ precipitation particle measurements.

  1. Språka och lek

    DEFF Research Database (Denmark)

    Bylander, Helle Iben; Thomsen, Inge Benn

    Språka och Lek innehåller mer än 100 språklekar och idéer. Bokens aktiviteter är noggrant beskrivna med tydliga mål och anvisningar, så att den pedagogiska personalen i förskolan kan erbjuda spännande och värdefulla språkliga upplevelser med hjälp av vardagsföremål och massor av fantasi. Boken är...

  2. Ka-band waveguide rotary joint

    KAUST Repository

    Yevdokymov, Anatoliy

    2013-04-11

    The authors present a design of a waveguide rotary joint operating in Ka-band with central frequency of 33 GHz, which also acts as an antenna mount. The main unit consists of two flanges with a clearance between them; one of the flanges has three circular choke grooves. Utilisation of three choke grooves allows larger operating clearance. Two prototypes of the rotary joint have been manufactured and experimentally studied. The observed loss is from 0.4 to 0.8 dB in 1.5 GHz band.

  3. CalSimHydro Tool - A Web-based interactive tool for the CalSim 3.0 Hydrology Prepropessor

    Science.gov (United States)

    Li, P.; Stough, T.; Vu, Q.; Granger, S. L.; Jones, D. J.; Ferreira, I.; Chen, Z.

    2011-12-01

    CalSimHydro, the CalSim 3.0 Hydrology Preprocessor, is an application designed to automate the various steps in the computation of hydrologic inputs for CalSim 3.0, a water resources planning model developed jointly by California State Department of Water Resources and United States Bureau of Reclamation, Mid-Pacific Region. CalSimHydro consists of a five-step FORTRAN based program that runs the individual models in succession passing information from one model to the next and aggregating data as required by each model. The final product of CalSimHydro is an updated CalSim 3.0 state variable (SV) DSS input file. CalSimHydro consists of (1) a Rainfall-Runoff Model to compute monthly infiltration, (2) a Soil moisture and demand calculator (IDC) that estimates surface runoff, deep percolation, and water demands for natural vegetation cover and various crops other than rice, (3) a Rice Water Use Model to compute the water demands, deep percolation, irrigation return flow, and runoff from precipitation for the rice fields, (4) a Refuge Water Use Model that simulates the ponding operations for managed wetlands, and (5) a Data Aggregation and Transfer Module to aggregate the outputs from the above modules and transfer them to the CalSim SV input file. In this presentation, we describe a web-based user interface for CalSimHydro using Google Earth Plug-In. The CalSimHydro tool allows users to - interact with geo-referenced layers of the Water Budget Areas (WBA) and Demand Units (DU) displayed over the Sacramento Valley, - view the input parameters of the hydrology preprocessor for a selected WBA or DU in a time series plot or a tabular form, - edit the values of the input parameters in the table or by downloading a spreadsheet of the selected parameter in a selected time range, - run the CalSimHydro modules in the backend server and notify the user when the job is done, - visualize the model output and compare it with a base run result, - download the output SV file to be

  4. Evidence for humid and arboreal environment in the Middle Lisan Basin, 45-39 ka (the Mughr el-Hamamah site, Jordan): Implications for Anatomically Modern Human Dispersal into Western Eurasia

    Science.gov (United States)

    Belmaker, M.; Stutz, A. J.

    2014-12-01

    The period between 50-30 kya in western Eurasia witnessed Neanderthal extinction, anatomically modern human (AMH) expansion, and a transition from Middle to Upper Paleolithic material culture. The prevailing hypothesis suggests a replacement of the Neanderthal populations by incoming AMH population, perhaps involving climatic fluctuations that favored AMH biology and habitat preferences. Yet, new evidence questions the role of climate as a forcing factor in AMH dispersal from Africa, raising the possibility that AMH populations in southern Arabia were responsible for the <50 ka expansion into western Eurasia. New excavations at Mughr el-Hamamah (MHM), Ajlun District, Jordan, uncovered a single well preserved occupational horizon. This horizon is dated by acid-base-wet oxidation/stepped combustion (ABOX-SC) AMS 14C assays to 45-39,000 cal BP and is associated with abundant diagnostic Early Upper Paleolithic (EUP) artifacts. The age of the site, combined with its excellent organic preservation, suggests that MHM can play a key role in testing hypotheses about the southern Levantine Rift Valley environment and EUP human adaptations to it. This paper presents a paleoecological reconstruction derived from micromammal remains associated with in situ archaeological deposits in MHM. The assemblage is highly dominated by the Syrian squirrel (Sciurus anomalus), typical of cool and humid climate. It is common in Late Glacial fauna of the Mediterranean of the Levant, in sites such as Kebara UP and Amud. Yet, today it is known only from high elevation in Turkey, Syria and Jordan. Other taxa include several genera of murids, further supporting the reconstruction of woodland habitats within a 1-3 km radius around the site. Additional archaeological data confirm that MHM was situated along an ecotone between the forested, temperate plateau and the Jordan Valley bottom grassland. Dead Sea speleothems and stromatolites in Dead Sea escarpment caves, indicating a high stand of Lake

  5. Climate changes in East China since the Late-glacial inferred from high-resolution mountain peat humification records

    Institute of Scientific and Technical Information of China (English)

    MA ChunMei; ZHU Cheng; ZHENG ChaoGui; YIN Qian; ZHAO ZhiPing

    2009-01-01

    High-resolution peat humification records were obtained from Dajiuhu of the Shennongjia Mountains and Qianmutian of the Tianmu Mountains to study climate changes in East China. The analyses of pollen, organic matters, TOC, and Rb/Sr indicate a high degree of peat humification and thus strong decomposition of organic matter when climate was dry. Conversely, when climate was humid, the de gree of humification is low because peat was preserved in a waterlogged condition. Peat humification from Dajiuhu occurred not only during the Younger Dryas (about 11.4-12.6 cal ka BP), the Bol ling-Allerφd Warm Period (12.6-15.2 cal ka BP), and the Oldest Dryas (about 15.2-16.0 cal ka BP), but also during the early Holocene (about 11.4-9.4 cal ka BP), the 8.2 cal ka BP cold event, and the Holo cene Optimum (about 7.0-4.2 cal ka BP). Both peat humification records since nearly 5 ka BP are consistent, showing that mountain peaUand has synchronous responses to the East Asia mon soon-induced precipitation. The LOI data confirm the above observation. The monsoon precipitation since nearly 5 ka BP recorded in these two peat profiles can be divided into three phases. During 4.9 3.5 ka BP, precipitation amount was high but fluctuated greatly. During 3.5-0.9 ka BP, precipitation amount was low. During 0.9-0 ka BP, degree of humification reduced gradually, indicating the increase of monsoon precipitation. Contrast to other high-resolution records from East China monsoon region shows that the monsoon precipitation records of the two peat profiles since nearly 16 ka BP are con trolled by a common forcing mechanism of summer solar radicalization in the Northern Hemisphere.

  6. Mass spectra in softly broken ${\\cal N}=2$ SQCD

    CERN Document Server

    Chernyak, Victor L

    2016-01-01

    Considered is ${\\cal N}=2\\,\\, SU(N_c)$ or $U(N_c)$ SQCD with $N_c+1cal N}=1$ by the mass term $\\mu_{\\rm x}{\\rm Tr} (X^2)$ of colored adjoint scalar partners of gluons, $\\mu_{\\rm x}\\ll\\Lambda_2$ ( $\\Lambda_2$ is the scale factor of the $SU(N_c)$ gauge coupling). There is a large number of different types of vacua in this theory with both unbroken and spontaneously broken global flavor symmetry $U(N_F)\\rightarrow U({\\rm n}_1)\\times U({\\rm n}_2)$. We consider in this paper the large subset of these vacua with the unbroken nontrivial $Z_{2N_c-N_F\\geq 2}$ discrete symmetry, at different hierarchies between the Lagrangian parameters $m\\gtrless\\Lambda_2,\\, \\mu_{\\rm x}\\gtrless m$. The forms of low energy Lagrangians, quantum numbers of light particles and mass spectra are described for all these vacua. Our results differ from corresponding results in recent papers arXiv:1304.0822; 1403.60...

  7. Nonabelian Superconductors: Vortices and Confinement in ${\\cal N}=2$ SQCD

    CERN Document Server

    Auzzi, R; Evslin, J; Konishi, K; Yung, A; Auzzi, Roberto; Bolognesi, Stefano; Evslin, Jarah; Konishi, Kenichi; Yung, Alexei

    2003-01-01

    We study nonabelian vortices (flux tubes) in SU(N) gauge theories, which are responsible for the confinement of (nonabelian) magnetic monopoles. In particular a detailed analysis is given of ${\\cal N}=2$ SQCD with gauge group SU(3) deformed by a small adjoint chiral multiplet mass. Tuning the bare quark masses (which we take to be large) to a common value $m$, we consider a particular vacuum of this theory in which an SU(2) subgroup of the gauge group remains unbroken. We consider $5 \\ge N_f \\ge 4$ flavors so that the SU(2) sub-sector remains non asymptotically free: the vortices carrying nonabelian fluxes may be reliably studied in a semi-classical regime. We show that the vortices indeed acquire exact zero modes which generate global rotations of the flux in an $SU(2)_{C+F}$ group. We study an effective world-sheet theory of these orientational zero modes which reduces to an ${\\cal N}=2$ O(3) sigma model in (1+1) dimensions. Mirror symmetry then teaches us that the dual SU(2) group is not dynamically broken...

  8. Application of genetic BP network to discriminating earthquakes and explosions

    Institute of Scientific and Technical Information of China (English)

    边银菊

    2002-01-01

    In this paper, we develop GA-BP algorithm by combining genetic algorithm (GA) with back propagation (BP) algorithm and establish genetic BP neural network. We also applied BP neural network based on BP algorithm and genetic BP neural network based on GA-BP algorithm to discriminate earthquakes and explosions. The obtained result shows that the discriminating performance of genetic BP network is slightly better than that of BP network.

  9. Origin and fate of sedimentary organic matter in the northern Bay of Bengal during the last 18 ka

    Science.gov (United States)

    Contreras-Rosales, L. A.; Schefuß, E.; Meyer, V.; Palamenghi, L.; Lückge, A.; Jennerjahn, T. C.

    2016-11-01

    The Northern Bay of Bengal (NBoB) is a globally important region for deep-sea organic matter (OM) deposition due to massive fluvial discharge from the Ganges-Brahmaputra-Meghna (G-B-M) rivers and moderate to high surface productivity. Previous studies have focused on carbon burial in turbiditic sediments of the Bengal Fan. However, little is known about the storage of carbon in pelagic and hemipelagic sediments of the Bay of Bengal over millennial time scales. This study presents a comprehensive history of OM origin and fate as well as a quantification of carbon sediment storage in the Eastern Bengal Slope (EBS) during the last 18 ka. Bulk organic proxies (TOC, TIC, TN, δ13CTOC, δ15NTN) and content and composition of total hydrolysable amino acids (THAA) in a sediment core (SO188-342KL) from the EBS were analyzed. Three periods of high OM accumulation were identified: the Late Glacial (LG), the Bölling/Alleröd (B/A), and the Early Holocene Climatic Optimum (EHCO). Lower eustatic sea level before 15 ka BP allowed a closer connection between the EBS and the fluvial debouch, favoring high terrestrial OM input to the core site. This connection was progressively lost between 15 and 7 ka BP as sea level rose to its present height and terrestrial OM input decreased considerably. Export and preservation of marine OM was stimulated during periods of summer monsoon intensification (B/A and EHCO) as a consequence of higher surface productivity enhanced by cyclonic-eddy nutrient pumping and fluvial nutrient delivery into the photic zone. Changes in the THAA composition indicate that the marine plankton community structure shifted from calcareous-dominated before 13 ka BP to siliceous-dominated afterwards. They also indicate that the relative proportion of marine versus terrestrial OM deposited at site 342KL was primarily driven by relative sea level and enlarged during the Holocene. The ballasting effect of lithogenic particles during periods of high coastal proximity and

  10. Extension of the Southern Hemisphere Atmospheric Radiocarbon Curve, 2120-850 years BP: Results from Tasmanian Huon Pine

    Energy Technology Data Exchange (ETDEWEB)

    Zimmerman, S R; P.Guilderson, T; Buckley, B M; Cook, E

    2010-02-12

    Decadal samples of dendrochronologically-dated pine (Lagorostrobos franklinii) from the Stanley River basin, Tasmania have been radiocarbon dated between 2120-850 yr BP. This data set overlaps and extends the current Southern Hemisphere record, which currently covers the period 110-995 yr BP. There is good agreement between the two records between 995-850 yr BP, between sample replicates and with consensus values for standards. As in the younger dataset, we find evidence for a distinct but variable offset between the southern hemisphere data and IntCal04; although this is likely due to real temporal variability in the interhemispheric offset, further work is planned to rule out possible laboratory or sample preparation differences.

  11. Precision Measurements of ${\\cal B}[\\psi(3686) \\to \\pi^+\\pi^- J/\\psi]$ and ${\\cal B}[J/\\psi\\to l^+l^-]$

    CERN Document Server

    Ablikim, M; Albayrak, O; Ambrose, D J; An, F F; An, Q; Bai, J Z; Ferroli, R Baldini; Ban, Y; Becker, J; Bennett, J V; Bertani, M; Bian, J M; Boger, E; Bondarenko, O; Boyko, I; Braun, S; Briere, R A; Bytev, V; Cai, H; Cai, X; Cakir, O; Calcaterra, A; Cao, G F; Cetin, S A; Chang, J F; Chelkov, G; Chen, G; Chen, H S; Chen, J C; Chen, M L; Chen, S J; Chen, X R; Chen, Y B; Cheng, H P; Chu, Y P; Cronin-Hennessy, D; Dai, H L; Dai, J P; Dedovich, D; Deng, Z Y; Denig, A; Denysenko, I; Destefanis, M; Ding, W M; Ding, Y; Dong, L Y; Dong, M Y; Du, S X; Fang, J; Fang, S S; Fava, L; Feng, C Q; Friedel, P; Fu, C D; Fu, J L; Fuks, O; Gao, Y; Geng, C; Goetzen, K; Gong, W X; Gradl, W; Greco, M; Gu, M H; Gu, Y T; Guan, Y H; Guo, A Q; Guo, L B; Guo, T; Guo, Y P; Han, Y L; Harris, F A; He, K L; He, M; He, Z Y; Held, T; Heng, Y K; Hou, Z L; Hu, C; Hu, H M; Hu, J F; Hu, T; Huang, G M; Huang, G S; Huang, J S; Huang, L; Huang, X T; Huang, Y; Hussain, T; Ji, C S; Ji, Q; Ji, Q P; Ji, X B; Ji, X L; Jiang, L L; Jiang, X S; Jiao, J B; Jiao, Z; Jin, D P; Jin, S; Jing, F F; Kalantar-Nayestanaki, N; Kavatsyuk, M; Kloss, B; Kopf, B; Kornicer, M; Kuehn, W; Lai, W; Lange, J S; Lara, M; Larin, P; Leyhe, M; Li, C H; Li, Cheng; Li, Cui; Li, D M; Li, F; Li, G; Li, H B; Li, J C; Li, K; Li, Lei; Li, Q J; Li, W D; Li, W G; Li, X L; Li, X N; Li, X Q; Li, X R; Li, Z B; Liang, H; Liang, Y F; Liang, Y T; Liao, G R; Liao, X T; Lin, D X; Liu, B J; Liu, C L; Liu, C X; Liu, F H; Liu, Fang; Liu, Feng; Liu, H; Liu, H B; Liu, H H; Liu, H M; Liu, H W; Liu, J P; Liu, K; Liu, K Y; Liu, P L; Liu, Q; Liu, S B; Liu, X; Liu, Y B; Liu, Z A; Liu, Zhiqiang; Liu, Zhiqing; Loehner, H; Lou, X C; Lu, G R; Lu, H J; Lu, J G; Lu, X R; Lu, Y P; Luo, C L; Luo, M X; Luo, T; Luo, X L; Lv, M; Ma, F C; Ma, H L; Ma, Q M; Ma, S; Ma, T; Ma, X Y; Maas, F E; Maggiora, M; Malik, Q A; Mao, Y J; Mao, Z P; Messchendorp, J G; Min, J; Min, T J; Mitchell, R E; Mo, X H; Moeini, H; Morales, C Morales; Moriya, K; Muchnoi, N Yu; Muramatsu, H; Nefedov, Y; Nikolaev, I B; Ning, Z; Olsen, S L; Ouyang, Q; Pacetti, S; Park, J W; Pelizaeus, M; Peng, H P; Peters, K; Ping, J L; Ping, R G; Poling, R; Prencipe, E; Qi, M; Qian, S; Qiao, C F; Qin, L Q; Qin, X S; Qin, Y; Qin, Z H; Qiu, J F; Rashid, K H; Redmer, C F; Rong, G; Ruan, X D; Sarantsev, A; Shao, M; Shen, C P; Shen, X Y; Sheng, H Y; Shepherd, M R; Song, W M; Song, X Y; Spataro, S; Spruck, B; Sun, D H; Sun, G X; Sun, J F; Sun, S S; Sun, Y J; Sun, Y Z; Sun, Z J; Sun, Z T; Tang, C J; Tang, X; Tapan, I; Thorndike, E H; Toth, D; Ullrich, M; Uman, I; Varner, G S; Wang, B; Wang, D; Wang, D Y; Wang, K; Wang, L L; Wang, L S; Wang, M; Wang, P; Wang, P L; Wang, Q J; Wang, S G; Wang, X F; Wang, X L; Wang, Y D; Wang, Y F; Wang, Y Q; Wang, Z; Wang, Z G; Wang, Z Y; Wei, D H; Wei, J B; Weidenkaff, P; Wen, Q G; Wen, S P; Werner, M; Wiedner, U; Wu, L H; Wu, N; Wu, S X; Wu, W; Wu, Z; Xia, L G; Xia, Y X; Xiao, Z J; Xie, Y G; Xiu, Q L; Xu, G F; Xu, Q J; Xu, Q N; Xu, X P; Xu, Z R; Xue, Z; Yan, L; Yan, W B; Yan, Y H; Yang, H X; Yang, Y; Yang, Y X; Ye, H; Ye, M; Ye, M H; Yu, B X; Yu, C X; Yu, H W; Yu, J S; Yu, S P; Yuan, C Z; Yuan, Y; Zafar, A A; Zallo, A; Zang, S L; Zeng, Y; Zhang, B X; Zhang, B Y; Zhang, C; Zhang, C C; Zhang, D H; Zhang, H H; Zhang, H Y; Zhang, J Q; Zhang, J W; Zhang, J Y; Zhang, J Z; Zhang, LiLi; Zhang, R; Zhang, S H; Zhang, X J; Zhang, X Y; Zhang, Y; Zhang, Y H; Zhang, Z P; Zhang, Z Y; Zhang, Zhenghao; Zhao, G; Zhao, H S; Zhao, J W; Zhao, Lei; Zhao, Ling; Zhao, M G; Zhao, Q; Zhao, S J; Zhao, T C; Zhao, X H; Zhao, Y B; Zhao, Z G; Zhemchugov, A; Zheng, B; Zheng, J P; Zheng, Y H; Zhong, B; Zhou, L; Zhou, X; Zhou, X K; Zhou, X R; Zhu, C; Zhu, K; Zhu, K J; Zhu, S H; Zhu, X L; Zhu, Y C; Zhu, Y S; Zhu, Z A; Zhuang, J; Zou, B S; Zou, J H

    2013-01-01

    Based on $(106.41 \\pm 0.86)\\times 10^{6}$ $\\psi(3686)$ events collected with the BESIII detector at the BEPCII collider, the branching fractions of $\\psi(3686) \\to \\pi^+\\pi^- J/\\psi$, $J/\\psi \\to e^+e^- $, and $J/\\psi \\to \\mu^+\\mu^-$ are measured. We obtain ${\\cal B}[\\psi(3686) \\to \\pi^+\\pi^-J/\\psi]=(34.98\\pm 0.02\\pm 0.45)%$, ${\\cal B}[J/\\psi \\to e^+e^-] = (5.983 \\pm 0.007 \\pm 0.037)%$ and ${\\cal B}[J/\\psi \\to \\mu^+\\mu^-] = (5.973 \\pm 0.007 \\pm 0.038)%$. The measurement of ${\\cal B}[\\psi(3686) \\to \\pi^{+}\\pi^{-}J/\\psi]$ confirms the CLEO-c measurement, and is apparently larger than the others. The measured $J/\\psi$ leptonic decay branching fractions agree with previous experiments within one standard deviation. These results lead to ${\\cal B}[J/\\psi \\to l^+l^-] = (5.978 \\pm 0.005 \\pm 0.040)%$ by averaging over the $e^{+}e^{-}$ and $\\mu^{+}\\mu^{-}$ channels and a ratio of ${\\cal B}[J/\\psi \\to e^+e^-] / {\\cal B}[J/\\psi \\to \\mu^+\\mu^-] = 1.0017 \\pm 0.0017 \\pm 0.0033$, which tests $e$-$\\mu$ universality at the fo...

  12. High Efficiency Ka-Band Spatial Combiner

    Directory of Open Access Journals (Sweden)

    D. Passi

    2014-12-01

    Full Text Available A Ka-Band, High Efficiency, Small Size Spatial Combiner (SPC is proposed in this paper, which uses an innovatively matched quadruple Fin Lines to microstrip (FLuS transitions. At the date of this paper and at the Author's best knowledge no such FLuS innovative transitions have been reported in literature before. These transitions are inserted into a WR28 waveguide T-junction, in order to allow the integration of 16 Monolithic Microwave Integrated Circuit (MMIC Solid State Power Amplifiers (SSPA's. A computational electromagnetic model using the finite elements method has been implemented. A mean insertion loss of 2 dB is achieved with a return loss better the 10 dB in the 31-37 GHz bandwidth.

  13. p Ka calculation of poliprotic acid: histamine

    Science.gov (United States)

    De Abreu, Heitor A.; De Almeida, Wagner B.; Duarte, Hélio A.

    2004-01-01

    Various theoretical studies have been reported addressing the performance of solvation models available to estimate p Ka values. However, no attention has been paid so far to the role played by the electronic, thermal and solvation energy individual contributions to the Gibbs free energy of the deprotonation process. In this work, we decompose the total Gibbs free energy into three distinct terms and then evaluate the dependence of each contribution on the level of theory employed for its determination using different levels of theory. The three possible p Kas of histamine have been estimated and compared with available experimental data. We found that the electronic energy term is sensitive to the level of theory and basis set, and, therefore, could be also a source of error in the theoretical calculation of p Kas.

  14. KaKa带你杀大网

    Institute of Scientific and Technical Information of China (English)

    昊月

    2005-01-01

    前两期的Dust2和Inferno相信大家杀得一定很过瘾吧?这期KaKa继续向大家介绍杀大网的奥妙,这次我们转战Train这张地图。这张地图的特点是阴人的特点是掩体多、整体的颜色比较暗,可以到处阴人。Train的空间感也比较强,上下移动的频率比较多,所以大家在玩这种地图的时候枪口上下移动会很频繁。对鼠标垫比较好的玩家来说,是比较耗损好的鼠标垫哦,希望大家不要心疼。

  15. Aeronautical applications of steerable K/Ka-band antennas

    Science.gov (United States)

    Helmken, Henry; Prather, Horton

    1995-01-01

    The expected growth of wideband data and video transmission via satellite will press existing satellite Ku-band services and push development of the Ka-band region. Isolated ground based K/Ka-band terminals can experience severe fading due to rain and weather phenomena. However, since aircraft generally fly above the severe weather, they are attractive platforms for developing commercial K/Ka-band communication links.

  16. Carrier Analysis Lab (CAL) – Aircraft/Weapons/Ship Compatibility Lab

    Data.gov (United States)

    Federal Laboratory Consortium — Purpose: The Carrier Analysis Lab (CAL) - Aircraft/Weapons/Ship Compatibility Lab located at the Naval Air Warfare Center Aircraft Division, Lakehurst, NJ provides...

  17. Palaeo-lakes and palaeo-climates in the circum western Indian ocean since 25 ka BP; Paleolacs et paleoclimats aux pourtours de l`ocean Indien occidental depuis 25 ka BP

    Energy Technology Data Exchange (ETDEWEB)

    Gasse, F.; Bergonzini, L.; Chalie, F.; Gibert, E.; Massault, M. [Paris-11 Univ., 91 - Orsay (France). Laboratoire d`Hydrologie et de Geochimie Isotopique; Melieres, F. [Centre National de la Recherche Scientifique (CNRS), 75 - Paris (France). Laboratoire de Geologie, MNHN

    1998-12-31

    Several lacustrine records from tropical regions of both Hemisphere (Tibet, Ethiopia, Tanganyika, Madagascar) illustrate the specificity of regional response to changes in the major forcing factors of the global climate system. Methodology and techniques are first briefly described. We then summarize major environmental changes recorded in the four regions considered. Hydro-climatic variations are partly explained by insolation forcing. All sites register a mean annual hydrological deficit during the Last Glacial Maximum, as expected from orbital forcing in the Northern Hemisphere, but not in he southern Hemisphere. Glacial climatic boundary conditions, i.e. lower tropical sea surface temperature and related availability in atmospheric moisture should be considered as the major cause. Other mechanisms have to be searched to account for short-term post-glacial variations that affect large geographical areas. (authors) 74 refs.

  18. A biomass burning record from the Lingtai Loess Section during the last 370 ka and implication for climate and environment

    Institute of Scientific and Technical Information of China (English)

    ZHOU Bin; SHEN Chengde; SUN Yanmin; YANG Ying; YI Weixi

    2006-01-01

    The history of natural fire and its relationship with climate and vegetation are revealed from the content of elemental carbon and associated pollen data and paleoclimatic substitutive indicators for the loess of Lingtai Section in the last 370 ka BP. The study indicates that intense episodes of vegetation fires occurred during the interim especially when the climate was changing from wet to drought. The average content of elemental carbon in the interglaciers is higher than that in the glaciers, which coincides with the biomass change locally (or globally). The content of elemental carbon increases in the stage around 130 ka BP, indicating that the vegetation and climate pattern have changed, which may contribute to the variation of CO2. As a whole, the content of elemental carbon increasing with the time reflects the increasing aridity trend to some degree. In addition, the occurrence of the maximum peak and the highest average content of elemental carbon in the Holocene reflects the occurrence of a rapid climate event in 5900 a BP and more frequent fires caused by anthropic activities.

  19. DARHT 2 kA Cathode Development

    Energy Technology Data Exchange (ETDEWEB)

    Henestroza, E.; Houck, T.; Kwan, J.W.; Leitner, M.; Miram, G.; Prichard, B.; Roy, P.K.; Waldron, W.; Westenskow, G.; Yu, S.; Bieniosek, F.M.

    2009-03-09

    In the campaign to achieve 2 kA of electron beam current, we have made several changes to the DARHT-II injector during 2006-2007. These changes resulted in a significant increase in the beam current, achieving the 2 kA milestone. Until recently (before 2007), the maximum beam current that was produced from the 6.5-inch diameter (612M) cathode was about 1300 A when the cathode was operating at a maximum temperature of 1140 C. At this temperature level, the heat loss was dominated by radiation which is proportional to temperature to the fourth power. The maximum operating temperature was limited by the damage threshold of the potted filament and the capacity of the filament heater power supply, as well as the shortening of the cathode life time. There were also signs of overheating at other components in the cathode assembly. Thus it was clear that our approach to increase beam current could not be simply trying to run at a higher temperature and the preferred way was to operate with a cathode that has a lower work function. The dispenser cathode initially used was the type 612M made by SpectraMat. According to the manufacturer's bulletin, this cathode should be able to produce more than 10 A/cm{sup 2} of current density (corresponding to 2 kA of total beam current) at our operating conditions. Instead the measured emission (space charge limited) was 6 A/cm{sup 2}. The result was similar even after we had revised the activation and handling procedures to adhere more closely to the recommend steps (taking longer time and nonstop to do the out-gassing). Vacuum was a major concern in considering the cathode's performance. Although the vacuum gauges at the injector vessel indicated 10{sup -8} Torr, the actual vacuum condition near the cathode in the central region of the vessel, where there might be significant out-gassing from the heater region, was never determined. Poor vacuum at the surface of the cathode degraded the emission (by raising the work function

  20. The HLD (CalMod) index and the index question.

    Science.gov (United States)

    Parker, W S

    1998-08-01

    The malocclusion index problem arises because of the need to identify which patient's treatments will be paid for with tax dollars. Both the civilian (Medicaid) and military (Champus) programs in the United States require that "need" be demonstrated. Need is defined as "medically necessary handicapping malocclusion" in Medicaid parlance. It is defined by Champus as "seriously handicapping malocclusion." The responsible specialty organization (the AAO) first approved the Salzmann Index in 1969 for this purpose and then reversed course in 1985 and took a formal position against the use of any index. Dentistry has historically chosen a state of occlusal perfection as ideal and normal and declared that variation was not normal hence abnormal and thus malocclusion. This "ideal" composes from 1% to 2% of the population and fails all statistical standards. Many indexes have been proposed based on variations from this "ideal" and fail for that reason. They are not logical. The HLD (CalMod) Index is a lawsuit-driven modification of some 1960 suggestions by Dr. Harry L. Draker. It proposes to identify the worst looking malocclusions as handicapping and offers a cut-off point to identify them. In addition, the modification includes two situations known to be destructive to tissue and structures. As of Jan. 1, 1998, the California program has had 135,655 patients screened by qualified orthodontists using this index. Of that number, 49,537 patients have had study models made and screened by qualified orthodontists using the index. Two separate studies have been performed to examine results and to identify problems. Necessary changes have been made and guidelines produced. The index problem has proven to be very dynamic in application. The HLD (CalMod) Index has been successfully applied and tested in very large numbers. This article is published as a factual review of the situation regarding the index question and one solution in the United States.

  1. AcEST: BP914941 [AcEST

    Lifescience Database Archive (English)

    Full Text Available ive uncharacterized protein OS=Oryza... 55 2e-06 tr|Q84KA5|Q84KA5_CUCME Selenium binding protein-like protei...007 >tr|Q84KA5|Q84KA5_CUCME Selenium binding protein-like protein OS=Cucumis melo GN=Sbp1 PE=4 SV=1 Length =

  2. Briti korruptsioonivastane seadus kehtib ka Eestis / Tõnis Tamme

    Index Scriptorium Estoniae

    Tamme, Tõnis, 1972-

    2011-01-01

    Suurbritannias jõustub 1. juulil 2011 uus korruptsioonivastane seadus (Bribery Act 2010), mis kehtib ühtmoodi nii Briti ettevõtetele kui ka mujal maailmas asutatud äriühingutele, kelle äritegevus või ka osa sellest omab puutumust Suurbritanniaga

  3. Assigning the pKa's of Polyprotic Acids.

    Science.gov (United States)

    Bodner, George M.

    1986-01-01

    Discusses (1) polyproptic acids for which the difference between K-a's is large; (2) the Henderson-Hasselbach equation; (3) polyprotic acids for which the difference between K-a's is small; (4) analysis of microscopic dissociation constants for cysteine; and (5) analysis of pK-a data. (JN)

  4. A compilation of Western European terrestrial records 60-8 ka BP: towards an understanding of latitudinal climatic gradients

    NARCIS (Netherlands)

    Moreno, A.; Svensson, A.; Brooks, S.J.; Connors, S.; Engels, S.; Fletcher, W.; Genty, D.; Heiri, O.; Labuhn, I.; Perşoiu, A.; Peyron, O.; Sadori, L.; Valero-Garcés, B.; Wulf, S.; Zanchetta, G; Data contributors, [Unknown

    2014-01-01

    Terrestrial records of past climatic conditions, such as lake sediments and speleothems, provide data of great importance for understanding environmental changes. However, unlike marine and ice core records, terrestrial palaeodata are often not available in databases or in a format that is easily ac

  5. CAL--ERDA program manual. [Building Design Language; LOADS, SYSTEMS, PLANT, ECONOMICS, REPORT, EXECUTIVE, CAL-ERDA

    Energy Technology Data Exchange (ETDEWEB)

    Hunn, B. D.; Diamond, S. C.; Bennett, G. A.; Tucker, E. F.; Roschke, M. A.

    1977-10-01

    A set of computer programs, called Cal-ERDA, is described that is capable of rapid and detailed analysis of energy consumption in buildings. A new user-oriented input language, named the Building Design Language (BDL), has been written to allow simplified manipulation of the many variables used to describe a building and its operation. This manual provides the user with information necessary to understand in detail the Cal-ERDA set of computer programs. The new computer programs described include: an EXECUTIVE Processor to create computer system control commands; a BDL Processor to analyze input instructions, execute computer system control commands, perform assignments and data retrieval, and control the operation of the LOADS, SYSTEMS, PLANT, ECONOMICS, and REPORT programs; a LOADS analysis program that calculates peak (design) zone and hourly loads and the effect of the ambient weather conditions, the internal occupancy, lighting, and equipment within the building, as well as variations in the size, location, orientation, construction, walls, roofs, floors, fenestrations, attachments (awnings, balconies), and shape of a building; a Heating, Ventilating, and Air-Conditioning (HVAC) SYSTEMS analysis program capable of modeling the operation of HVAC components including fans, coils, economizers, humidifiers, etc.; 16 standard configurations and operated according to various temperature and humidity control schedules. A plant equipment program models the operation of boilers, chillers, electrical generation equipment (diesel or turbines), heat storage apparatus (chilled or heated water), and solar heating and/or cooling systems. An ECONOMIC analysis program calculates life-cycle costs. A REPORT program produces tables of user-selected variables and arranges them according to user-specified formats. A set of WEATHER ANALYSIS programs manipulates, summarizes and plots weather data. Libraries of weather data, schedule data, and building data were prepared.

  6. High power Ka band TWT amplifier

    Energy Technology Data Exchange (ETDEWEB)

    Golkowski, C.; Ivers, J.D.; Nation, J.A.; Wang, P.; Schachter, L.

    1999-07-01

    Two high power 35 GHz TWT amplifiers driven by a relativistic pencil, 850 kV, 200A electron beam have been assembled and tested. The first had a dielectric slow wave structure and was primarily used to develop diagnostics, and to gain experience in working with high power systems in Ka band. The source of the input power for the amplifier was a magnetron producing a 30 kW, 200ns long pulse of which 10 kW as delivered to the experiment. The 30 cm long dielectric (Teflon) amplifier produced output power levels of about 1 MW with a gain of about 23 dB. These results are consistent with expectations from PIC code simulations for this arrangement. The second amplifier, which is a single stage disk loaded slow wave structure, has been designed. It consists of one hundred uniform cells with two sets of ten tapered calls at the ends to lower the reflection coefficient. The phase advance per cell is {pi}/2. The amplifier passband extends from 28 to 40 GHz. It is designed to increase the output power to about 20 MW. The amplifier is in construction and will be tested in the near future. Details of the design of both systems will be provided and initial results from the new amplifier presented.

  7. Elliptic Algebra and Integrable Models for Solitons on Noncommutative Torus ${\\cal T}$

    CERN Document Server

    Hou, B Y; Hou, Bo-Yu; Peng, Dan-Tao

    2002-01-01

    We study the algebra ${\\cal A}_n$ and the basis of the Hilbert space ${\\cal H}_n$ in terms of the $\\theta$ functions of the positions of $n$ solitons. Then we embed the Heisenberg group as the quantum operator factors in the representation of the transfer matrice of various integrable models. Finally we generalize our result to the generic $\\theta$ case.

  8. Data Management Standards in Computer-aided Acquisition and Logistic Support (CALS)

    Science.gov (United States)

    Jefferson, David K.

    1990-01-01

    Viewgraphs and discussion on data management standards in computer-aided acquisition and logistic support (CALS) are presented. CALS is intended to reduce cost, increase quality, and improve timeliness of weapon system acquisition and support by greatly improving the flow of technical information. The phase 2 standards, industrial environment, are discussed. The information resource dictionary system (IRDS) is described.

  9. Comparing Outcomes for Los Angeles County's HUD-Assisted and Unassisted CalWORKS Leavers.

    Science.gov (United States)

    Verma, Nandita; Hendra, Richard

    The impact of supplemental assistance from the U.S. Department of Housing and Urban Development (HUD) on CalWORKs leavers was examined in a study of CalWORKs recipients in Los Angeles County, California, who stopped receiving welfare benefits in the third quarter of 1998. Two groups received federal housing assistance at the time of exit from…

  10. Use of Modular Design in the Production of Portable CAL Software: A Case Study.

    Science.gov (United States)

    Wilson, R. N.; McCrum, E.

    1984-01-01

    Discusses difficulties of producing computer assisted learning (CAL) software economically. Proposed as a solution, modular programing is illustrated by describing production of a matrix algebra package. Use of special CAL modules and facilities provided by subroutine libraries are cited, and development of a package to teach matrix theory is…

  11. Evaluation of the SB 1041 Reforms to California's CalWORKs Program: Background and Study Design

    Science.gov (United States)

    Karoly, Lynn A.; Bozick, Robert; Davis, Lois M.; Kitmitto, Sami; Turk-Bicakci, Lori; Bos, Johannes M.; Holod, Aleksandra; Blankenship, Charles

    2015-01-01

    The California Budget Act of 2012, through a trailer bill known as Senate Bill (SB) 1041, contained significant reforms to the California Work Opportunity and Responsibility to Kids (CalWORKs) program. CalWORKs is California's Temporary Assistance for Needy Families (TANF) program, a central component of the safety net that provides cash aid for…

  12. Eruptive history of Sundoro volcano, Central Java, Indonesia since 34 ka

    Science.gov (United States)

    Prambada, Oktory; Arakawa, Yoji; Ikehata, Kei; Furukawa, Ryuta; Takada, Akira; Wibowo, Haryo Edi; Nakagawa, Mitsuhiro; Kartadinata, M. Nugraha

    2016-11-01

    Reconstruction of the eruptive history of Sundoro volcano is needed to forecast the probability of future eruptions and eruptive volumes. Sundoro volcano is located in Central Java (Indonesia), 65 km northwest of Yogyakarta, and in one of the most densely populated areas of Indonesia. On the basis of stratigraphy, radiocarbon dating, petrography, and whole-rock geochemistry, we recognize the following 12 eruptive groups: (1) Ngadirejo, (2) Bansari, (3) Arum, (4) Kembang, (5) Kekep, (6) Garung, (7) Kertek, (8) Watu, (9) Liyangan, (10) Kledung, (11) Summit, and (12) Sibajak. The Ngadirejo (34 ka BP) to Kledung (1 ka) eruptive groups are inferred to have been the stratovolcano building phase. Based on compositions of deposits, one or more magma reservoirs of intermediate chemical composition are inferred to have existed below the volcano during the periods of time represented by the eruptive groups. SiO2 of juvenile eruptive products ranges from 50 to 63 wt%, and K2O contents range from high K to medium K. The chemical composition and phenocryst content of eruptive products change with time. The lower SiO2 products contain mainly plagioclase, clinopyroxene, and olivine, whereas the more evolved rocks contain plagioclase, clinopyroxene, orthopyroxene, and rare hornblende and olivine. Our work has defined Sundoro's eruptive history for the period 1-34 ka, and this history helps us to forecast future activity. We estimated that the total amount of magma discharged since 34 ka is approximately 4.4 km3. The average eruption rate over this group ranges from 0.14 to 0.17 km3/kyr. The eruption rate and the frequency of individual eruptions indicate that the volcano has been very active since 34 ka, and this activity in combination with our petrological data suggest the presence of one or more magma reservoirs that have been repeatedly filled and then discharged as eruptions have taken place. Our data further suggest that the volume of the crustal reservoir system has

  13. The effects of multiple features of alternatively spliced exons on the KA/KS ratio test

    Directory of Open Access Journals (Sweden)

    Chen Feng-Chi

    2006-05-01

    Full Text Available Abstract Background The evolution of alternatively spliced exons (ASEs is of primary interest because these exons are suggested to be a major source of functional diversity of proteins. Many exon features have been suggested to affect the evolution of ASEs. However, previous studies have relied on the KA/KS ratio test without taking into consideration information sufficiency (i.e., exon length > 75 bp, cross-species divergence > 5% of the studied exons, leading to potentially biased interpretations. Furthermore, which exon feature dominates the results of the KA/KS ratio test and whether multiple exon features have additive effects have remained unexplored. Results In this study, we collect two different datasets for analysis – the ASE dataset (which includes lineage-specific ASEs and conserved ASEs and the ACE dataset (which includes only conserved ASEs. We first show that information sufficiency can significantly affect the interpretation of relationship between exons features and the KA/KS ratio test results. After discarding exons with insufficient information, we use a Boolean method to analyze the relationship between test results and four exon features (namely length, protein domain overlapping, inclusion level, and exonic splicing enhancer (ESE frequency for the ASE dataset. We demonstrate that length and protein domain overlapping are dominant factors, and they have similar impacts on test results of ASEs. In addition, despite the weak impacts of inclusion level and ESE motif frequency when considered individually, combination of these two factors still have minor additive effects on test results. However, the ACE dataset shows a slightly different result in that inclusion level has a marginally significant effect on test results. Lineage-specific ASEs may have contributed to the difference. Overall, in both ASEs and ACEs, protein domain overlapping is the most dominant exon feature while ESE frequency is the weakest one in affecting

  14. Mitotic protein kinase CDK1 phosphorylation of mRNA translation regulator 4E-BP1 Ser83 may contribute to cell transformation

    Energy Technology Data Exchange (ETDEWEB)

    Velásquez, Celestino; Cheng, Erdong; Shuda, Masahiro; Lee-Oesterreich, Paula J.; Pogge von Strandmann, Lisa; Gritsenko, Marina A.; Jacobs, Jon M.; Moore, Patrick S.; Chang, Yuan

    2016-07-11

    mTOR-directed 4E-BP1 phosphorylation promotes cap-dependent translation and tumorigen-esis. During mitosis, CDK1 substitutes for mTOR and fully phosphorylates 4E-BP1 at canoni-cal as well a non-canonical S83 site resulting in a mitosis-specific hyperphosphorylated δ isoform. Colocalization studies with a phospho-S83 specific antibody indicate that 4E-BP1 S83 phosphorylation accumulates at centrosomes during prophase, peaks at metaphase, and decreases through telophase. While S83 phosphorylation of 4E-BP1 does not affect in vitro cap-dependent translation, nor eIF4G/4E-BP1 cap-binding, expression of an alanine substitution mutant 4E-BP1.S83A partially reverses rodent cell transformation induced by Merkel cell polyomavirus (MCV) small T (sT) antigen viral oncoprotein. In contrast to inhibitory mTOR 4E-BP1 phosphorylation, these findings suggest that mitotic CDK1-directed phosphorylation of δ-4E-BP1 may yield a gain-of-function, distinct from translation regulation, that may be important in tumorigenesis and mitotic centrosome function.

  15. BP - bisnis põhjas? / Erik Aru

    Index Scriptorium Estoniae

    Aru, Erik

    2010-01-01

    Seoses Mehhiko lahe naftareostusega ootab BP-d kuni 21 mld. dollari suurune trahv, kahjude hüvitamiseks peab BP müüma osa oma varast. Ekspertide hinnangul tähendavad Mehhiko lahe sündmused suuri muutusi kogu naftaäris

  16. The sensitivity of the Late Saalian (140 ka) and LGM (21 ka) Eurasian ice sheets to sea surface conditions

    Energy Technology Data Exchange (ETDEWEB)

    Colleoni, Florence [Centro Euro-Mediterraneo per i Cambiamenti Climatici, Bologna (Italy); UJF, CNRS, Laboratoire de Glaciologie et Geophysique de l' Environnement, Saint Martin d' Heres Cedex (France); Stockholm University, Department of Geological Sciences, Stockhlom (Sweden); Liakka, Johan [Stockholm University, Department of Meteorology, Stockholm (Sweden); Krinner, Gerhard; Peyaud, Vincent [UJF, CNRS, Laboratoire de Glaciologie et Geophysique de l' Environnement, Saint Martin d' Heres Cedex (France); Jakobsson, Martin [Stockholm University, Department of Geological Sciences, Stockhlom (Sweden); Masina, Simona [Centro Euro-Mediterraneo per i Cambiamenti Climatici, Istituto Nazionale di Geofisica e Vulcanologia, Bologna (Italy)

    2011-08-15

    This work focuses on the Late Saalian (140 ka) Eurasian ice sheets' surface mass balance (SMB) sensitivity to changes in sea surface temperatures (SST). An Atmospheric General Circulation Model (AGCM), forced with two preexisting Last Glacial Maximum (LGM, 21 ka) SST reconstructions, is used to compute climate at 140 and 21 ka (reference glaciation). Contrary to the LGM, the ablation almost stopped at 140 ka due to the climatic cooling effect from the large ice sheet topography. Late Saalian SST are simulated using an AGCM coupled with a mixed layer ocean. Compared to the LGM, these 140 ka SST show an inter-hemispheric asymmetry caused by the larger ice-albedo feedback, cooling climate. The resulting Late Saalian ice sheet SMB is smaller due to the extensive simulated sea ice reducing the precipitation. In conclusion, SST are important for the stability and growth of the Late Saalian Eurasian ice sheet. (orig.)

  17. Terracotas del santuario de Calés (Calvi, Campania

    Directory of Open Access Journals (Sweden)

    J. M. BLÁZQUEZ

    2009-10-01

    Full Text Available El Museo Arqueológico Nacional de Madrid, entre sus magníficas colecciones, exhibe una compuesta por un numeroso conjunto de terracotas traídas de Italia en el siglo pasado por el Marqués de Salamanca. La colección Calvi, procedente del Santuario de Calés, en Campania, y así llamada del lugar de procedencia, ha sido repartida entre varios museos españoles, pero el grupo más numeroso es el depositado en el Museo Arqueológico Nacional que, a pesar de la alta calidad artística de las piezas y del buen estado de conservación de todas ellas, ha permanecido hasta el presente inédita. Tan sólo F. Benoit y nosotros, hemos publicado algunas terracotas de las que representan caballos. Otros investigadores, como Bianchi Bandinelli, han aludido a esta colección que, como las similares guardadas en los museos de Lecce, Capua, Louvre, Leide, British Museum, etc., se encuentra inédita. Particular interés ofrece el grupo conservado en la Glyptothek Ny Carlsberg, de Copenhague, algunos ejemplares se guardan en el Museo Universitario de Zurich y en el Museum f. ant. Kleinkunst de Munich. En Roma los conjuntos más numerosos de estas terracotas se encuentran depositados en los Museos Gregoriano Etrusco del Vaticano, Villa Giulia, y Nazionale Romano.

  18. Design de interface do ambiente virtual HyperCAL online

    Directory of Open Access Journals (Sweden)

    Jaire Passos

    2010-12-01

    Full Text Available A presente pesquisa objetiva propor uma metodologia que oriente o projeto de interface de ambiente virtual centrado no usuário que seja sistematizada como processo de produto com princípios de design de interação, considerando aspectos de usabilidade e ergonomia, de modo a favorecer o trabalho do usuário, permitindo a apropriação do conteúdo e a execução das tarefas através das funcionalidades do sistema. Para consecução do trabalho foram investigados: os elementos da experiência do usuário; as ferramentas de planejamento de produto; as técnicas engenharia de software; e os conceitos do design de interação. A validação da metodologia foi feita através do projeto de interface do módulo do desenvolvedor (professor/instrutor do HyperCalGD online. A interface projetada apresentou melhores condições para o desenvolvimento de materiais educacionais.

  19. Paleoclimatological and paleoenvironmental records since 4 000 a B.P. in sediments of alpine lakes in Taiwan

    Institute of Scientific and Technical Information of China (English)

    罗建育; 陈镇东

    1997-01-01

    The 3 310-m-high Chia-min Lake records the climatic history since 4 ka B. P. in Taiwan. The warm/wet period before 2.2 ka B.P. seemed to correspond to the later part of the Holocene Megathermal, and the cold/dry period during 0-2/2 ka B. P. corresponded to the Katathermal. Before the termination of the Megathermal, an especially warm and humid segment (2, 2-2. 4 ka B. P. ) emerged. The paleoclimatic records from Yuen-yang and Chi-tsai Lakes support the notion that the Megathermal in Taiwan terminated during 2-2. 3 ka B. P. A warm segment (820-1 320 AD) in the Katathermal could be considered the Medieval Warm Period. The climate turned cold and dry after 1 320 AD and this indicated the onset of the Little Ice Age. These paleoclimatic variations are also in good agreement with those recorded in Great Ghost Lake.

  20. Eastern Andean environmental and climate synthesis for the last 2000 years BP from terrestrial pollen and charcoal records of Patagonia

    Science.gov (United States)

    Sottile, G. D.; Echeverria, M. E.; Mancini, M. V.; Bianchi, M. M.; Marcos, M. A.; Bamonte, F. P.

    2015-06-01

    The Southern Hemisphere Westerly Winds (SWW) constitute an important zonal circulation system that dominates the dynamics of Southern Hemisphere mid-latitude climate. Little is known about climatic changes in the Southern South America in comparison to the Northern Hemisphere due to the low density of proxy records, and adequate chronology and sampling resolution to address environmental changes of the last 2000 years. Since 2009, new pollen and charcoal records from bog and lakes in northern and southern Patagonia at the east side of the Andes have been published with an adequate calibration of pollen assemblages related to modern vegetation and ecological behaviour. In this work we improve the chronological control of some eastern Andean previously published sequences and integrate pollen and charcoal dataset available east of the Andes to interpret possible environmental and SWW variability at centennial time scales. Through the analysis of modern and past hydric balance dynamics we compare these scenarios with other western Andean SWW sensitive proxy records for the last 2000 years. Due to the distinct precipitation regimes that exist between Northern (40-45° S) and Southern Patagonia (48-52° S) pollen sites locations, shifts on latitudinal and strength of the SWW results in large changes on hydric availability on forest and steppe communities. Therefore, we can interpret fossil pollen dataset as changes on paleohydric balance at every single site by the construction of paleohydric indices and comparison to charcoal records during the last 2000 cal yrs BP. Our composite pollen-based Northern and Southern Patagonia indices can be interpreted as changes in latitudinal variation and intensity of the SWW respectively. Dataset integration suggest poleward SWW between 2000 and 750 cal yrs BP and northward-weaker SWW during the Little Ice Age (750-200 cal yrs BP). These SWW variations are synchronous to Patagonian fire activity major shifts. We found an in phase

  1. NASA SCaN Overview and Ka-Band Actvities

    Science.gov (United States)

    Stegeman, James D.; Midon, Marco Mario; Davarian, Faramaz; Geldzahler, Barry

    2014-01-01

    The Ka- and Broadband Communications Conference is an international forum attended by worldwide experts in the area of Ka-Band Propagation and satellite communications. Since its inception, NASA has taken the initiative of organizing and leading technical sections on RF Propagation and satellite communications, solidifying its worldwide leadership in the aforementioned areas. Consequently, participation in this conference through the contributions described below will maintain NASA leadership in Ka- and above RF Propagation as it relates to enhancing current and future satellite communication systems supporting space exploration.

  2. Onboard Interferometric SAR Processor for the Ka-Band Radar Interferometer (KaRIn)

    Science.gov (United States)

    Esteban-Fernandez, Daniel; Rodriquez, Ernesto; Peral, Eva; Clark, Duane I.; Wu, Xiaoqing

    2011-01-01

    An interferometric synthetic aperture radar (SAR) onboard processor concept and algorithm has been developed for the Ka-band radar interferometer (KaRIn) instrument on the Surface and Ocean Topography (SWOT) mission. This is a mission- critical subsystem that will perform interferometric SAR processing and multi-look averaging over the oceans to decrease the data rate by three orders of magnitude, and therefore enable the downlink of the radar data to the ground. The onboard processor performs demodulation, range compression, coregistration, and re-sampling, and forms nine azimuth squinted beams. For each of them, an interferogram is generated, including common-band spectral filtering to improve correlation, followed by averaging to the final 1 1-km ground resolution pixel. The onboard processor has been prototyped on a custom FPGA-based cPCI board, which will be part of the radar s digital subsystem. The level of complexity of this technology, dictated by the implementation of interferometric SAR processing at high resolution, the extremely tight level of accuracy required, and its implementation on FPGAs are unprecedented at the time of this reporting for an onboard processor for flight applications.

  3. Interoperability of wearable cuffless BP measuring devices.

    Science.gov (United States)

    Liu, Jing; Zhang, Yuan-Ting

    2014-01-01

    While a traditional cuff-based Blood Pressure (BP) measuring device can only take a snap shot of BP, real-time and continuous measurement of BP without an occluding cuff is preferred which usually use the pulse transit time (PTT) in combination with other physiological parameters to estimate or track BP over a certain period of time after an initial calibration. This article discusses some perspectives of interoperability of wearable medical devices, based on IEEE P1708 draft standard that focuses on the objective performance evaluation of wearable cuffless BP measuring devices. The ISO/IEEE 11073 family of standards, supporting the plug-and play feature, is intended to enable medical devices to interconnect and interoperate with other medical devices and with computerized healthcare information systems in a manner suitable for the clinical environment. In this paper, the possible adoption of ISO/IEEE 11073 for the interoperability of wearable cuffless BP devices is proposed. In the consideration of the difference of the continuous and cuffless BP measuring methods from the conventional ones, the existing device specialization standards of ISO/IEEE 11073 cannot be directly followed when designing the cuffless BP device. Specifically, this paper discusses how the domain information model (DIM), in which vital sign information is abstracted as objects, is used to structure the information about the device and that generated from the device. Though attention should also be paid to adopt the communication standards for other parts for the communication system, applying communication standards that enable plug-and-play feature allows achieving the interoperability of different cuffless BP measuring devices with possible different configurations.

  4. CAl2Be3(2-) and its salt complex LiCAl2Be3-: anionic global minima with planar pentacoordinate carbon.

    Science.gov (United States)

    Wu, Yan-Bo; Duan, Yan; Lu, Hai-Gang; Li, Si-Dian

    2012-03-29

    Following the isoelectronic relationship in global minima planar pentacoordinate carbon (ppC) species (cationic CAl(5)(+), neutral CAl(4)Be, and monoanionic CAl(3)Be(2)(-)), we designed a dianionic ppC species C(2v) CAl(2)Be(3)(2-) (1a) and its salt complex C(2v) LiCAl(2)Be(3)(-) (2a) in this work. In combination with DFT and high-level ab initio calculations (CCSD(T)), the extensive exploration on their potential energy surfaces indicates that they are the global minima. Their kinetic stability was proved by two sets of 100 ps ab initio Born-Oppenheimer molecular dynamic simulations at the B3LYP/6-31+G(d) level. The detailed analyses indicate that the introduction of Li(+) into 1a only influences the electrovalent bonding (through changing of the charge distribution) and the σ aromaticity (through changing of the in-plane ring current), while the structures, the bonding properties, the π aromaticity, and so forth are almost unchanged. Nevertheless, the MO energy levels, the HOMO-LUMO gaps, and the values of vertical detachment energies (VDEs) all verify that the lithiation significantly improves the stability. We think the ppC dianion 1a is possible to detect directly in the gas-phase experiments, but it can be detected as its salt complex 2a more easily.

  5. 花粉记录的青藏高原中部中全新世以来植被与环境%Pollen-inferred vegetation and environmental changes in the central Tibetan Plateau since 8200 yr BP

    Institute of Scientific and Technical Information of China (English)

    唐领余; 杨保; 沈才明; 李春海; 彭金兰; 刘惠; Kam-Biu Liu; Carrie Morrill; Jonathan T.Overpeck; Jonathan E.Cole

    2009-01-01

    青藏高原中部的草甸/草原混合生态群落,对气候变化非常敏感.孢粉记录显示草原发育时期,莎草减少,区域气候是相对干旱的,在时间上对应季风相对弱的时期.依据唐古拉山垭口湖、阿洪错和错那3个淡水湖泊钻孔孢粉分析,定量重建的温度和降水指标.探讨该地区8200 cal a BP以来的植被与气候变化.8200~6500 cal aBP,尤其是8200~7200 cal a BP,植被以草甸/草原混合生态群落为主,显示强季风控制着青藏高原中部;6000~4900,4400~3900以及2800~2400 cal a BP时期区域植被以草原植被为主,应是3次百年尺度的干旱事件;4900~4400 cal a BP期间植被类型由草原向草甸转变:6500~5400和3000~1600 cal a BP出现两次大的变干事件;数值摸拟估计,高原中部接近于现今的环境,最早可能出现在6500 cal a BP,自3000 cal a BP以后高原中部季风性降水和湿度逐渐减少至现今水平,可能在700~300 cal a BP出现一次小冰期变冷事件.

  6. Proteomic Analysis of Anti-Tumor Effects of 11-Dehydrosinulariolide on CAL-27 Cells

    Directory of Open Access Journals (Sweden)

    Yu-Jen Wu

    2011-07-01

    Full Text Available The anti-tumor effects of 11-dehydrosinulariolide, an active ingredient isolated from soft coral Sinularia leptoclados, on CAL-27 cells were investigated in this study. In the MTT assay for cell proliferation, increasing concentrations of 11-dehydrosinulariolide decreased CAL-27 cell viability. When a concentration of 1.5 µg/mL of 11-dehydrosinulariolide was applied, the CAL-27 cells viability was reduced to a level of 70% of the control sample. The wound healing function decreased as the concentration of 11-dehydrosinulariolide increased. The results in this study indicated that treatment with 11-dehydrosinulariolide for 6 h significantly induced both early and late apoptosis of CAL-27 cells, observed by flow cytometric measurement and microscopic fluorescent observation. A comparative proteomic analysis was conducted to investigate the effects of 11-dehydrosinulariolide on CAL-27 cells at the molecular level by comparison between the protein profiling (revealed on a 2-DE map of CAL-27 cells treated with 11-dehydrosinulariolide and that of CAL-27 cells without the treatment. A total of 28 differential proteins (12 up-regulated and 16 down-regulated in CAL-27 cells treated with 11-dehydrosinulariolide have been identified by LC-MS/MS analysis. Some of the differential proteins are associated with cell proliferation, apoptosis, protein synthesis, protein folding, and energy metabolism. The results of this study provided clues for the investigation of biochemical mechanisms of the anti-tumor effects of 11-dehydrosinulariolide on CAL-27 cells and could be valuable information for drug development and progression monitoring of oral squamous cell carcinoma (OSCC.

  7. Under tõi kirjanduse juurde ka Ilvese / Jaanus Kulli

    Index Scriptorium Estoniae

    Kulli, Jaanus, 1955-

    2009-01-01

    Sirje Kiini raamatust "Marie Under : elu, luuletaja identiteet ja teoste vastuvõtt" (Tallinn : Tänapäev, 2009), mille esitlus toimus 10. dets. Kirjanike Majas Tallinnas. Sõnavõtuga esines ka president Toomas Hendrik Ilves

  8. NOAA Ship Ka'imimoana Underway Meteorological Data, Quality Controlled

    Data.gov (United States)

    National Oceanic and Atmospheric Administration, Department of Commerce — NOAA Ship Ka'imimoana Underway Meteorological Data (delayed ~10 days for quality control) are from the Shipboard Automated Meteorological and Oceanographic System...

  9. Key Science Observations of AGNs with KaVA Array

    CERN Document Server

    Kino, Motoki; Zhao, Guang-Yao; Sohn, Bong Won

    2015-01-01

    KaVA (KVN and VERA Array) is a new combined VLBI array with KVN (Korean VLBI Network) and VERA (VLBI Exploration of Radio Astrometry). First, we briefly review the imaging capabilities of KaVA array which actually achieves more than three times better dynamic range than that achieved by VERA alone. The KaVA images clearly show detailed structures of extended radio jets in AGNs. Next, we represent the key science program to be led by KaVA AGN sub working group. We will conduct the monitoring observations of Sgr A* and M87 because of the largeness of their central super-massive black hole angular sizes. The main science goals of the program are (i) testing magnetically-driven-jet paradigm by mapping velocity fields of the M87 jet, and (ii) obtaining tight constraints on physical properties of radio emitting region in Sgr A*.

  10. Autorid ja esitajad tahavad maksu ka mobiiltelefonidelt / Teele Tammeorg

    Index Scriptorium Estoniae

    Tammeorg, Teele

    2010-01-01

    Esitajate liidu arvates tuleks maksu alla minevate seadmete hulka arvata ka blu-ray plaadid, MP3-mängijad ja pleieriga mobiiltelefonid, millel on mälumahtu üle 128 MB. Elisa pressiesindaja Marika Raiski arvamus

  11. Rahvasaadik Pikhof toetab nii Tiibetit kui ka Hiinat / Mirko Ojakivi

    Index Scriptorium Estoniae

    Ojakivi, Mirko

    2007-01-01

    Riigikogu liige Heljo Pikhof on kirjas nii Riigikogu Tiibeti toetusrühmas kui ka Hiina parlamendirühmas, samuti Taiwani toetusrühmas. TÜ sinoloogiateaduri Märt Läänemetsa arvamus, H. Pikhofi selgitus

  12. Ka-Band MMIC T/R Module Project

    Data.gov (United States)

    National Aeronautics and Space Administration — This proposal is specifically written to address the need for improved Ka-band T/R modules. The solicitation calls for investigation and development of core...

  13. Under tõi kirjanduse juurde ka Ilvese / Jaanus Kulli

    Index Scriptorium Estoniae

    Kulli, Jaanus, 1955-

    2009-01-01

    Sirje Kiini raamatust "Marie Under : elu, luuletaja identiteet ja teoste vastuvõtt" (Tallinn : Tänapäev, 2009), mille esitlus toimus 10. dets. Kirjanike Majas Tallinnas. Sõnavõtuga esines ka president Toomas Hendrik Ilves

  14. Autorid ja esitajad tahavad maksu ka mobiiltelefonidelt / Teele Tammeorg

    Index Scriptorium Estoniae

    Tammeorg, Teele

    2010-01-01

    Esitajate liidu arvates tuleks maksu alla minevate seadmete hulka arvata ka blu-ray plaadid, MP3-mängijad ja pleieriga mobiiltelefonid, millel on mälumahtu üle 128 MB. Elisa pressiesindaja Marika Raiski arvamus

  15. Kindralpolkovnik Maiorov : "Teie mured on ka meie mured!" / Tiit Tambi

    Index Scriptorium Estoniae

    Tambi, Tiit

    1993-01-01

    President Lennart Meri kohtumine Venemaa relvajõudude loode väegrupi ülemjuhataja kindralpolkovnik Leonid Majoroviga, 9. veebruar 1993. Ka kindralpolkovniku kohtumistest Eestis elavate sõjaveteranidega

  16. Võitlus terrorismiga on ka meie kohus / Ando Leps

    Index Scriptorium Estoniae

    Leps, Ando, 1935-

    2002-01-01

    Ilmunud ka: Kesknädal 25. september lk. 4 (lühendatult). Septembri alguses Toledo Ülikoolis toimunud Euroopa Kriminoloogia Assotsiatsiooni II konverentsist. Autori ettekandest "Rahvusvaheline terrorism ja Eesti". Autor: Keskerakond. Parlamendisaadik

  17. Ka-Band MMIC T/R Module Project

    Data.gov (United States)

    National Aeronautics and Space Administration — This Phase II proposal is presented as the follow on to the Phase I SBIR contract number NNC06CB21C entitled "Ka-band MMIC T/R Module" For active microwave...

  18. Computer-aided acquisition and logistics support (CALS): Concept of Operations for Depot Maintenance

    Energy Technology Data Exchange (ETDEWEB)

    Bourgeois, N.C.; Greer, D.K.

    1993-04-01

    This CALS Concept of Operations for Depot Maintenance provides the foundation strategy and the near term tactical plan for CALS implementation in the depot maintenance environment. The user requirements enumerated and the overarching architecture outlined serve as the primary framework for implementation planning. The seamless integration of depot maintenance business processes and supporting information systems with the emerging global CALS environment will be critical to the efficient realization of depot user's information requirements, and as, such will be a fundamental theme in depot implementations.

  19. CalVR: an advanced open source virtual reality software framework

    Science.gov (United States)

    Schulze, Jürgen P.; Prudhomme, Andrew; Weber, Philip; DeFanti, Thomas A.

    2013-03-01

    We developed CalVR because none of the existing virtual reality software frameworks offered everything we needed, such as cluster-awareness, multi-GPU capability, Linux compatibility, multi-user support, collaborative session support, or custom menu widgets. CalVR combines features from multiple existing VR frameworks into an open-source system, which we use in our laboratory on a daily basis, and for which dozens of VR applications have already been written at UCSD but also other research laboratories world-wide. In this paper, we describe the philosophy behind CalVR, its standard and unique features and functions, its programming interface, and its inner workings.

  20. Implementació d'una Intranet pel Restaurant "Cal Fesu"

    OpenAIRE

    Maldonado Rubio, Lluís Manel

    2007-01-01

    Aquest projecte consisteix en el disseny i implementació d'una intranet amb zona privada pel restaurant "Cal Fesu", utilitzant una tecnologia puntera com és J2EE (struts). Este proyecto consiste en el diseño e implementación de una intranet con zona privada para el restaurante "Cal Fesu", utilizando una tecnología puntera como es J2EE (struts). This project consists of design and implementation of an intranet with a private area for the restaurant "Cal Fesu", using a leading technology ...

  1. A comparative study of RADAR Ka-band backscatter

    Science.gov (United States)

    Mapelli, D.; Pierdicca, N.; Guerriero, L.; Ferrazzoli, Paolo; Calleja, Eduardo; Rommen, B.; Giudici, D.; Monti Guarnieri, A.

    2014-10-01

    Ka-band RADAR frequency range has not yet been used for Synthetic Aperture Radar (SAR) from space so far, although this technology may lead to important applications for the next generation of SAR space sensors. Therefore, feasibility studies regarding a Ka-band SAR instrument have been started [1][2], for the next generation of SAR space sensors. In spite of this, the lack of trusted references on backscatter at Ka-band revealed to be the main limitation for the investigation of the potentialities of this technology. In the framework of the ESA project "Ka-band SAR backscatter analysis in support of future applications", this paper is aimed at the study of wave interaction at Ka-band for a wide range of targets in order to define a set of well calibrated and reliable Ka-band backscatter coefficients for different kinds of targets. We propose several examples of backscatter data resulting from a critical survey of available datasets at Ka-band, focusing on the most interesting cases and addressing both correspondences and differences. The reliability of the results will be assessed via a preliminary comparison with ElectroMagnetic (EM) theoretical models. Furthermore, in support of future technological applications, we have designed a prototypal software acting as a "library" of earth surface radar response. In our intention, the output of the study shall contribute to answer to the need of a trustworthy Ka-Band backscatter reference. It will be of great value for future technological applications, such as support to instrument analysis, design and requirements' definition (e.g.: Signal to Noise Ratio, Noise Equivalent Sigma Zero).

  2. BP Investment Exceeds $4 Bln in china

    Institute of Scientific and Technical Information of China (English)

    Wang Ping

    2008-01-01

    @@ British Petroleum (BP) recently signed a series of agreements with China including those in clean energy and wind power generation, during British Prime Minister Gordon Brown's visit to China in mid-January.

  3. The millimetre spectrum of BP Cru

    Science.gov (United States)

    Pestalozzi, Michele; Hobbs, George; Torkelsson, Ulf

    2010-04-01

    In this experiment we attempt to detect the millimetre emission from the high-mass X-ray binary BP Cru. This object is composed of a hypergiant (Wray 977) and a slow spinning X-ray pulsar (GX301-2). The recent ATCA observations of centimeter emission (Pestalozzi et al. 2009, this was the first detection of radio emission towards BP Cru) suggested that radio emission consists of two components, a transient non-thermal one and a persistent thermal one, probably arising from the large stellar wind of Wray 977. As stellar winds often show a positive spectral index, we ask to observe BP Cru at 13 and 7 mm, where we expect fluxes of around 1 mJy. Any detection will allow us to probe the inner parts of the wind and characterise the structure of the stellar wind of BP Cru. For this detection experiment we require 11 hours of observations with ATCA.

  4. The German SMOS project office - CAL/VAL activities

    Science.gov (United States)

    Tittebrand, A.; Stammer, D.; Dransfeld, S.

    2009-04-01

    The SMOS remote sensing mission planned to be launched in July 2009 is part of the opportunity missions of the European Space Agency's (ESA) Earth Explorer programme. The role of the German SMOS project office (funded by the BMBF/DLR) is to inform the scientific community and the public about the current mission status as well as to promote the use of the SMOS data products within Germany. Within the framework of the project office scientific studies for the calibration and validation (cal/val) of the SMOS data are also supported. Our work includes the analysis of model-, shiptrack- and climatology determined salinity data as well as satellite, drifter and float measurements. The first comprehensive in situ data set suitable for global investigations of SSS characteristics is that provided by ARGO temperature and salinity profiles since 2000. The global ARGO float system (Gould et al., 2004) consisting of 3000 floats that provide temperature and salinity profiles, globally, from the top 2000 m every 10 days on approximately a 3 degree global grid. For our study we extract the near-surface values from ARGO salinity and temperature profiles to form a data set of near-surface salinity and temperature covering the years 2002 until 2008. All those ARGO data points are located at a depth of 0 to 5 m. Of importance for the justification of the SMOS mission is the deviation of the Argo-Measurements from climatologies, based on the bulk of the past global in situ salt content measurements, which renders the temporal condition of world oceans. Additionally a deployment of 25 drifters is planned in parallel to the SMOS launch, collecting data of temperature and salinity in the GIN SEA and the western Pacific.

  5. New ${\\cal W}_{q,p}(sl(2))$ algebras from the elliptic algebra ${\\cal A}_{q,p}({\\hat sl}(2)_c)$

    CERN Document Server

    Avan, J; Rossi, M; Sorba, Paul

    1997-01-01

    We construct operators t(z) in the elliptic algebra introduced by Foda et al. ${\\cal A}_{q,p}({\\hat sl}(2)_c)$. They close an exchange algebra when p^m=q^{c+2} for m integer. In addition they commute when p=q^{2k} for k integer non-zero, and they belong to the center of ${\\cal A}_{q,p}({\\hat sl}(2)_c)$ when k is odd. The Poisson structures obtained for t(z) in these classical limits are identical to the q-deformed Virasoro Poisson algebra, characterizing the exchange algebras at generic values of p, q and m as new ${\\cal W}_{q,p}(sl(2))$ algebras.

  6. Measurement of the ratio of branching fractions ${\\cal B}(B^0 \\to K^{\\ast 0} \\gamma)/{\\cal B}(B^0_s \\to \\phi \\gamma)$

    CERN Document Server

    Aaij, R; Adeva, B; Adinolfi, M; Adrover, C; Affolder, A; Ajaltouni, Z; Albrecht, J; Alessio, F; Alexander, M; Alkhazov, G; Alvarez Cartelle, P; Alves Jr, A A; Amato, S; Amhis, Y; Anderson, J; Appleby, R B; Aquines Gutierrez, O; Archilli, F; Arrabito, L; Artamonov, A; Artuso, M; Aslanides, E; Auriemma, G; Bachmann, S; Back, J J; Bailey, D S; Balagura, V; Baldini, W; Barlow, R J; Barschel, C; Barsuk, S; Barter, W; Bates, A; Bauer, C; Bauer, Th; Bay, A; Bediaga, I; Belogurov, S; Belous, K; Belyaev, I; Ben-Haim, E; Benayoun, M; Bencivenni, G; Benson, S; Benton, J; Bernet, R; Bettler, M -O; van Beuzekom, M; Bien, A; Bifani, S; Bird, T; Bizzeti, A; Bjørnstad, P M; Blake, T; Blanc, F; Blanks, C; Blouw, J; Blusk, S; Bobrov, A; Bocci, V; Bondar, A; Bondar, N; Bonivento, W; Borghi, S; Borgia, A; Bowcock, T J V; Bozzi, C; Brambach, T; van den Brand, J; Bressieux, J; Brett, D; Britsch, M; Britton, T; Brook, N H; Brown, H; Büchler-Germann, A; Burducea, I; Bursche, A; Buytaert, J; Cadeddu, S; Callot, O; Calvi, M; Calvo Gomez, M; Camboni, A; Campana, P; Carbone, A; Carboni, G; Cardinale, R; Cardini, A; Carson, L; Carvalho Akiba, K; Casse, G; Cattaneo, M; Cauet, Ch; Charles, M; Charpentier, Ph; Chiapolini, N; Ciba, K; Cid Vidal, X; Ciezarek, G; Clarke, P E L; Clemencic, M; Cliff, H V; Closier, J; Coca, C; Coco, V; Cogan, J; Collins, P; Comerma-Montells, A; Constantin, F; Contu, A; Cook, A; Coombes, M; Corti, G; Couturier, B; Cowan, G A; Currie, R; D'Ambrosio, C; David, P; David, P N Y; De Bonis, I; De Bruyn, K; De Capua, S; De Cian, M; De Lorenzi, F; De Miranda, J M; De Paula, L; De Simone, P; Decamp, D; Deckenhoff, M; Degaudenzi, H; Del Buono, L; Deplano, C; Derkach, D; Deschamps, O; Dettori, F; Dickens, J; Dijkstra, H; Diniz Batista, P; Domingo Bonal, F; Donleavy, S; Dordei, F; Dosil Suárez, A; Dossett, D; Dovbnya, A; Dupertuis, F; Dzhelyadin, R; Dziurda, A; Easo, S; Egede, U; Egorychev, V; Eidelman, S; van Eijk, D; Eisele, F; Eisenhardt, S; Ekelhof, R; Eklund, L; Elsasser, Ch; Elsby, D; Esperante Pereira, D; Falabella, A; Fanchini, E; Färber, C; Fardell, G; Farinelli, C; Farry, S; Fave, V; Fernandez Albor, V; Ferro-Luzzi, M; Filippov, S; Fitzpatrick, C; Fontana, M; Fontanelli, F; Forty, R; Francisco, O; Frank, M; Frei, C; Frosini, M; Furcas, S; Gallas Torreira, A; Galli, D; Gandelman, M; Gandini, P; Gao, Y; Garnier, J-C; Garofoli, J; Garra Tico, J; Garrido, L; Gascon, D; Gaspar, C; Gauld, R; Gauvin, N; Gersabeck, M; Gershon, T; Ghez, Ph; Gibson, V; Gligorov, V V; Göbel, C; Golubkov, D; Golutvin, A; Gomes, A; Gordon, H; Grabalosa Gándara, M; Graciani Diaz, R; Granado Cardoso, L A; Graugés, E; Graziani, G; Grecu, A; Greening, E; Gregson, S; Gui, B; Gushchin, E; Guz, Yu; Gys, T; Hadjivasiliou, C; Haefeli, G; Haen, C; Haines, S C; Hampson, T; Hansmann-Menzemer, S; Harji, R; Harnew, N; Harrison, J; Harrison, P F; Hartmann, T; He, J; Heijne, V; Hennessy, K; Henrard, P; Hernando Morata, J A; van Herwijnen, E; Hicks, E; Holubyev, K; Hopchev, P; Hulsbergen, W; Hunt, P; Huse, T; Huston, R S; Hutchcroft, D; Hynds, D; Iakovenko, V; Ilten, P; Imong, J; Jacobsson, R; Jaeger, A; Jahjah Hussein, M; Jans, E; Jansen, F; Jaton, P; Jean-Marie, B; Jing, F; John, M; Johnson, D; Jones, C R; Jost, B; Kaballo, M; Kandybei, S; Karacson, M; Karbach, T M; Keaveney, J; Kenyon, I R; Kerzel, U; Ketel, T; Keune, A; Khanji, B; Kim, Y M; Knecht, M; Koopman, R F; Koppenburg, P; Korolev, M; Kozlinskiy, A; Kravchuk, L; Kreplin, K; Kreps, M; Krocker, G; Krokovny, P; Kruse, F; Kruzelecki, K; Kucharczyk, M; Kvaratskheliya, T; La Thi, V N; Lacarrere, D; Lafferty, G; Lai, A; Lambert, D; Lambert, R W; Lanciotti, E; Lanfranchi, G; Langenbruch, C; Latham, T; Lazzeroni, C; Le Gac, R; van Leerdam, J; Lees, J -P; Lefèvre, R; Leflat, A; Lefrançois, J; Leroy, O; Lesiak, T; Li, L; Li Gioi, L; Lieng, M; Liles, M; Lindner, R; Linn, C; Liu, B; Liu, G; von Loeben, J; Lopes, J H; Lopez Asamar, E; Lopez-March, N; Lu, H; Luisier, J; Mac Raighne, A; Machefert, F; Machikhiliyan, I V; Maciuc, F; Maev, O; Magnin, J; Malde, S; Mamunur, R M D; Manca, G; Mancinelli, G; Mangiafave, N; Marconi, U; Märki, R; Marks, J; Martellotti, G; Martens, A; Martin, L; Martín Sánchez, A; Martinez Santos, D; Massafferri, A; Mathe, Z; Matteuzzi, C; Matveev, M; Maurice, E; Maynard, B; Mazurov, A; McGregor, G; McNulty, R; Meissner, M; Merk, M; Merkel, J; Messi, R; Miglioranzi, S; Milanes, D A; Minard, M -N; Molina Rodriguez, J; Monteil, S; Moran, D; Morawski, P; Mountain, R; Mous, I; Muheim, F; Müller, K; Muresan, R; Muryn, B; Muster, B; Musy, M; Mylroie-Smith, J; Naik, P; Nakada, T; Nandakumar, R; Nasteva, I; Nedos, M; Needham, M; Neufeld, N; Nguyen, A D; Nguyen-Mau, C; Nicol, M; Niess, V; Nikitin, N; Nikodem, T; Nomerotski, A; Novoselov, A; Oblakowska-Mucha, A; Obraztsov, V; Oggero, S; Ogilvy, S; Okhrimenko, O; Oldeman, R; Orlandea, M; Otalora Goicochea, J M; Owen, P; Pal, B K; Palacios, J; Palano, A; Palutan, M; Panman, J; Papanestis, A; Pappagallo, M; Parkes, C; Parkinson, C J; Passaleva, G; Patel, G D; Patel, M; Paterson, S K; Patrick, G N; Patrignani, C; Pavel-Nicorescu, C; Pazos Alvarez, A; Pellegrino, A; Penso, G; Pepe Altarelli, M; Perazzini, S; Perego, D L; Perez Trigo, E; Pérez-Calero Yzquierdo, A; Perret, P; Perrin-Terrin, M; Pessina, G; Petrella, A; Petrolini, A; Phan, A; Picatoste Olloqui, E; Pie Valls, B; Pietrzyk, B; Pilař, T; Pinci, D; Plackett, R; Playfer, S; Plo Casasus, M; Polok, G; Poluektov, A; Polycarpo, E; Popov, D; Popovici, B; Potterat, C; Powell, A; Prisciandaro, J; Pugatch, V; Puig Navarro, A; Qian, W; Rademacker, J H; Rakotomiaramanana, B; Rangel, M S; Raniuk, I; Raven, G; Redford, S; Reid, M M; dos Reis, A C; Ricciardi, S; Richards, A; Rinnert, K; Roa Romero, D A; Robbe, P; Rodrigues, E; Rodrigues, F; Rodriguez Perez, P; Rogers, G J; Roiser, S; Romanovsky, V; Rosello, M; Rouvinet, J; Ruf, T; Ruiz, H; Sabatino, G; Saborido Silva, J J; Sagidova, N; Sail, P; Saitta, B; Salzmann, C; Sannino, M; Santacesaria, R; Santamarina Rios, C; Santinelli, R; Santovetti, E; Sapunov, M; Sarti, A; Satriano, C; Satta, A; Savrie, M; Savrina, D; Schaack, P; Schiller, M; Schleich, S; Schlupp, M; Schmelling, M; Schmidt, B; Schneider, O; Schopper, A; Schune, M -H; Schwemmer, R; Sciascia, B; Sciubba, A; Seco, M; Semennikov, A; Senderowska, K; Sepp, I; Serra, N; Serrano, J; Seyfert, P; Shapkin, M; Shapoval, I; Shatalov, P; Shcheglov, Y; Shears, T; Shekhtman, L; Shevchenko, O; Shevchenko, V; Shires, A; Silva Coutinho, R; Skwarnicki, T; Smith, N A; Smith, E; Sobczak, K; Soler, F J P; Solomin, A; Soomro, F; Souza De Paula, B; Spaan, B; Sparkes, A; Spradlin, P; Stagni, F; Stahl, S; Steinkamp, O; Stoica, S; Stone, S; Storaci, B; Straticiuc, M; Straumann, U; Subbiah, V K; Swientek, S; Szczekowski, M; Szczypka, P; Szumlak, T; T'Jampens, S; Teodorescu, E; Teubert, F; Thomas, C; Thomas, E; van Tilburg, J; Tisserand, V; Tobin, M; Tolk, S; Topp-Joergensen, S; Torr, N; Tournefier, E; Tourneur, S; Tran, M T; Tsaregorodtsev, A; Tuning, N; Ubeda Garcia, M; Ukleja, A; Urquijo, P; Uwer, U; Vagnoni, V; Valenti, G; Vazquez Gomez, R; Vazquez Regueiro, P; Vecchi, S; Velthuis, J J; Veltri, M; Viaud, B; Videau, I; Vieira, D; Vilasis-Cardona, X; Visniakov, J; Vollhardt, A; Volyanskyy, D; Voong, D; Vorobyev, A; Voss, H; Wandernoth, S; Wang, J; Ward, D R; Watson, N K; Webber, A D; Websdale, D; Whitehead, M; Wiedner, D; Wiggers, L; Wilkinson, G; Williams, M P; Williams, M; Wilson, F F; Wishahi, J; Witek, M; Witzeling, W; Wotton, S A; Wyllie, K; Xie, Y; Xing, F; Xing, Z; Yang, Z; Young, R; Yushchenko, O; Zangoli, M; Zavertyaev, M; Zhang, F; Zhang, L; Zhang, W C; Zhang, Y; Zhelezov, A; Zhong, L; Zvyagin, A

    2012-01-01

    The ratio of branching fractions of the radiative $B$ decays $B^0\\to K^{*0}\\gamma$ and $B^0_s\\to \\phi\\gamma$ has been measured using $0.37\\,$fb$^{-1}$ of $pp$ collisions at a centre of mass energy of $\\sqrt{s}=7\\,$TeV, collected by the LHCb experiment. The value obtained is \\begin{equation} \\frac{{\\cal B}(B^0\\to K^{*0}\\gamma)}{{\\cal B}(B^0_s\\to \\phi\\gamma)} = 1.12 \\pm 0.08^{+0.06}_{-0.04}\\phantom{.}^{+0.09}_{-0.08},\

  7. ARCHAEOLOGICAL AND ENVIRONMENTAL CHANGES BETWEEN 9500 BP AND 4500 BP: A CONTRIBUTION FROM THE SAHARA TO UNDERSTAND EXPANDING DROUGHTS IN THE “GREAT MEDITERRANEAN”

    Directory of Open Access Journals (Sweden)

    E. A.A. Garcea

    2013-03-01

    Full Text Available The Sahara is more connected to the Mediterranean than often assumed and palynology, in particular, has provided evidence of past interrelations between the Mediterranean and the Sahara with pollen spectra from prehistoric Saharan deposits including Mediterranean taxa. In order to show human-environment relationships and populations’ strategies in response to changing environments, this paper presents a case study from the southern Sahara. This region offered a natural laboratory for the study of human/climate interaction as the range of environmental change extended from flood to drought, forcing people to cope with periodic environmental instability. When the tropical rainfall belt migrated northward, watertable outcropped in interdunal depressions and formed permanent lakes, which alternated with severe arid spells. As a case study, this paper presents the results of interdisciplinary investigations on climate changes, human adaptations and subsistence strategies at Gobero, in the southern Sahara of Niger. Gobero is a restricted archaeological area comprising 8 sites that surround the shores of a palaeolake. It was intermittently occupied between about 9500 cal years BP and 4500 BP. Due to alternating environmental conditions it could only be occupied at the beginning and at the end of the most humid periods.

  8. Conformal kernel for NLO BFKL equation in ${\\cal N}$=4 SYM

    Energy Technology Data Exchange (ETDEWEB)

    Balitsky, Ian; Chirilli, Giovanni

    2009-01-01

    Using the requirement of M\\"{o}bius invariance of ${\\cal N}$=4 SYM amplitudes in the Regge limit we restore the conformal NLO BFKL kernel out of the eigenvalues known from the forward NLO BFKL result.

  9. TileCal Beam Test Simulation Application in the FADS/Goofy Framework (GEANT4)

    CERN Document Server

    Solodkov, A A

    2003-01-01

    A new application for the Tile Calorimeter (TileCal) beam test simulation has been developed in GEANT4 within the FADS/Goofy framework. The geometry and readout systems for all the different TileCal modules have been implemented in a quite detailed way. This application allows to simulate all the TileCal beam test setup configurations existing so far. Details of the development as well as instructions to install and run the program are presented. The first tests have been performed for a beam test setup consisting of five prototype modules using negative pions with different energies and results of comparison to the experimental data from TileCal TDR are presented as well.

  10. A Complete Set of Firmware for the TileCal Read-Out Driver

    CERN Document Server

    Valero, A; Cuenca, C; Ferrer, A; Fullana, E; González, V; Higón, E; Poveda, J; Ruiz-Martinez, A; Salvachúa, B; Sanchís, E; Solans, C; Torres, J; Valls, J A

    2007-01-01

    TileCal is the hadronic tile calorimeter of the ATLAS experiment at LHC/CERN. The Read-Out Driver (ROD) is the main component of the TileCal back-end electronics. The ROD is a VME 64x 9u board with multiple programmable devices which requires a complete set of firmware. This paper describes the firmware and functionalities of all these programmable devices, especially the DSP Processing Units daughterboards where the data processing takes place.

  11. Fusion Rules of the ${\\cal W}_{p,q}$ Triplet Models

    CERN Document Server

    Wood, Simon

    2009-01-01

    In this paper we determine the fusion rules of the logarithmic ${\\calW}_{p,q}$ triplet theory and construct the Grothendieck group with subgroups for which consistent product structures can be defined. The fusion rules are then used to determine projective covers. This allows us also to write down a candidate for a modular invariant partition function. Our results demonstrate that recent work on the ${\\cal W}_{2,3}$ model generalises naturally to arbitrary (p,q).

  12. Malnutrition: role of the TwoCal HN Med Pass program.

    Science.gov (United States)

    Bender, S; Pusateri, M; Cook, A; Ferguson, M; Hall, J C

    2000-12-01

    Malnutrition is common in older adults and is associated with poor outcomes. The causes and outcomes of malnutrition are discussed, and the TwoCal HN Med Pass program, designed to overcome poor dietary intake, is described. Benefits of the program, role of the pharmacist, identification of candidates for the TwoCal HN Med Pass program, and health care team roles and responsibilities are reviewed.

  13. Practical Aspects of CALS in Design and Manufacturing of Sheet Metal Products

    DEFF Research Database (Denmark)

    Shpitalni, Moshe; Alting, Leo; Bilberg, Arne

    1998-01-01

    the CALS approach. This approach requires global observation and allows actual and current information to flow both forward and backward. This information, regardless of the specific process in which it has been generated, is used to improve the entire global process. This paper is concerned...... with the design and manufacture of sheet metal parts. It is demonstrated that through implementation of the CALS approach, the overall process can be optimised and products can be manufactured significantly more accurately, faster and less expensively....

  14. Equipment Design for Oxidation of 1BP/2BP Using NO_x

    Institute of Scientific and Technical Information of China (English)

    ZHOU; Xian-ming; CHANG; Shang-wen; LI; Gao-liang; LAN; Tian; LIU; Jin-ping; TANG; Hong-bin; HE; Hui

    2013-01-01

    NOx can Oxidize the reductants in 1BP and 2BP feed of Purex process,and can adjust the oxidation state of plutonium as Pu(Ⅳ)to meet the need of 2AF feed.Using NOx in Purex process can reduce the volumn of solid waste effectively,and attract more and more interest of researchers.In this work the oxidation of reductants in 1BP/2BP feed were investigated in glass column as the same-current mode,in

  15. Optical Reciprocity Induced Symmetry of the Scattering Eigenstates in Non-$\\cal PT$-Symmetric Heterostructures

    CERN Document Server

    Ge, Li

    2016-01-01

    The scattering matrix $S$ obeys the unitary relation $S^\\dagger S=1$ in a Hermitian system and the symmetry property ${\\cal PT}S{\\cal PT}=S^{-1}$ in a Parity-Time (${\\cal PT}$) symmetric system. Here we report a different symmetry relation of the $S$ matrix in a one-dimensional heterostructure, which is given by the amplitude ratio of the incident waves in the scattering eigenstates. It originates from the optical reciprocity and holds independent of the Hermiticity or $\\cal PT$ symmetry of the system. Using this symmetry relation, we probe a quasi-transition that is reminiscent of the spontaneous symmetry breaking of a $\\cal PT$-symmetric $S$ matrix, now with unbalanced gain and loss and even in the absence of gain. We show that the additional symmetry relation provides a clear evidence of an exceptional point, even when all other signatures of the $\\cal PT$ symmetry breaking are completely erased. We also discuss the existence of a final exceptional point in this correspondence, which is attributed to asymm...

  16. ${\\cal{KK}}\\text{MC-hh}$: Resummed Exact ${\\cal O}(\\alpha^2L)$ EW Corrections in a Hadronic MC Event Generator

    CERN Document Server

    Jadach, S; Was, Z A; Yost, S A

    2016-01-01

    We present an improvement of the MC event generator Herwiri2, where we recall the latter MC was a prototype for the inclusion of CEEX resummed EW corrections in hadron-hadron scattering at high cms energies. In this improvement the new exact ${\\cal O}(\\alpha^2L)$ resummed EW generator ${\\cal{KK}}$ MC 4.22, featuring as it does the CEEX realization of resummation in the EW sector, is put in union with the Herwig parton shower environment. The {\\rm LHE} format of the attendant output event file means that all other conventional parton shower environments are available to the would-be user of the resulting new MC. For this reason (and others -- see the text) we henceforth refer to the new improvement of the Herwiri2 MC as ${\\cal{KK}}\\text{MC-hh}$. Since this new MC features exact ${\\cal O}(\\alpha)$ pure weak corrections from the DIZET EW library and features the CEEX and the EEX YFS-style resummation of large multiple photon effects, it provides already the concrete path to 0.05\\% precision on such effects if we...

  17. Structural and functional characterization of CalS11, a TDP-rhamnose 3′-O-methyltransferase involved in calicheamicin biosynthesis

    Science.gov (United States)

    Singh, Shanteri; Chang, Aram; Helmich, Kate E.; Bingman, Craig A.; Wrobel, Russel L.; Beebe, Emily T.; Makino, Shin-Ichi; Aceti, David J.; Dyer, Kevin; Hura, Greg L.; Sunkara, Manjula; Morris, Andrew J.; Phillips, George N.; Thorson, Jon S.

    2013-01-01

    Sugar methyltransferases (MTs) are an important class of tailoring enzymes which catalyze the transfer of a methyl group from S-adenosyl-L-methionine to sugar-based N-, C- and O- nucleophiles. While sugar N- and C-MTs involved in natural product biosynthesis have been found to act on sugar nucleotide substrates prior to a subsequent glycosyltransferase reaction, corresponding sugar O-methylation reactions studied thus far occur after the glycosyltransfer reaction. Herein we report the first in vitro characterization using 1H-13C-gHSQC with isotopically-labeled substrates and the X-ray structure determination at 1.55 Å resolution of the TDP-3′-O-rhamnose-methyltransferase CalS11 from Micromonospora echinospora. This study highlights a unique NMR-based methyltransferase assay, implicates CalS11 to be a metal and general acid/base-dependent O-methyltransferase and, as a first crystal structure for a TDP-hexose-O-methyltransferase, presents a new template for mechanistic studies and/or engineering. PMID:23662776

  18. Structural and functional characterization of CalS11, a TDP-rhamnose 3'-O-methyltransferase involved in calicheamicin biosynthesis.

    Science.gov (United States)

    Singh, Shanteri; Chang, Aram; Helmich, Kate E; Bingman, Craig A; Wrobel, Russell L; Beebe, Emily T; Makino, Shin-Ichi; Aceti, David J; Dyer, Kevin; Hura, Greg L; Sunkara, Manjula; Morris, Andrew J; Phillips, George N; Thorson, Jon S

    2013-07-19

    Sugar methyltransferases (MTs) are an important class of tailoring enzymes that catalyze the transfer of a methyl group from S-adenosyl-l-methionine to sugar-based N-, C- and O-nucleophiles. While sugar N- and C-MTs involved in natural product biosynthesis have been found to act on sugar nucleotide substrates prior to a subsequent glycosyltransferase reaction, corresponding sugar O-methylation reactions studied thus far occur after the glycosyltransfer reaction. Herein we report the first in vitro characterization using (1)H-(13)C-gHSQC with isotopically labeled substrates and the X-ray structure determination at 1.55 Å resolution of the TDP-3'-O-rhamnose-methyltransferase CalS11 from Micromonospora echinospora. This study highlights a unique NMR-based methyltransferase assay, implicates CalS11 to be a metal- and general acid/base-dependent O-methyltransferase, and as a first crystal structure for a TDP-hexose-O-methyltransferase, presents a new template for mechanistic studies and/or engineering.

  19. Human (Clovis)-gomphothere (Cuvieronius sp.) association ∼13,390 calibrated yBP in Sonora, Mexico

    Science.gov (United States)

    Sanchez, Guadalupe; Holliday, Vance T.; Gaines, Edmund P.; Arroyo-Cabrales, Joaquín; Martínez-Tagüeña, Natalia; Kowler, Andrew; Lange, Todd; Hodgins, Gregory W. L.; Mentzer, Susan M.; Sanchez-Morales, Ismael

    2014-07-01

    The earliest known foragers to populate most of North America south of the glaciers [∼11,500 to ≥ ∼10,800 14C yBP; ∼13,300 to ∼12,800 calibrated (Cal) years] made distinctive "Clovis" artifacts. They are stereotypically characterized as hunters of Pleistocene megamammals (mostly mammoth) who entered the continent via Beringia and an ice-free corridor in Canada. The origins of Clovis technology are unclear, however, with no obvious evidence of a predecessor to the north. Here we present evidence for Clovis hunting and habitation ∼11,550 yBP (∼13,390 Cal years) at "El Fin del Mundo," an archaeological site in Sonora, northwestern Mexico. The site also includes the first evidence to our knowledge for gomphothere (Cuvieronius sp.) as Clovis prey, otherwise unknown in the North American archaeological record and terminal Pleistocene paleontological record. These data (i) broaden the age and geographic range for Clovis, establishing El Fin del Mundo as one of the oldest and southernmost in situ Clovis sites, supporting the hypothesis that Clovis had its origins well south of the gateways into the continent, and (ii) expand the make-up of the North American megafauna community just before extinction.

  20. Human (Clovis)–gomphothere (Cuvieronius sp.) association ∼13,390 calibrated yBP in Sonora, Mexico

    Science.gov (United States)

    Sanchez, Guadalupe; Holliday, Vance T.; Gaines, Edmund P.; Arroyo-Cabrales, Joaquín; Martínez-Tagüeña, Natalia; Kowler, Andrew; Lange, Todd; Hodgins, Gregory W. L.; Mentzer, Susan M.; Sanchez-Morales, Ismael

    2014-01-01

    The earliest known foragers to populate most of North America south of the glaciers [∼11,500 to ≥ ∼10,800 14C yBP; ∼13,300 to ∼12,800 calibrated (Cal) years] made distinctive “Clovis” artifacts. They are stereotypically characterized as hunters of Pleistocene megamammals (mostly mammoth) who entered the continent via Beringia and an ice-free corridor in Canada. The origins of Clovis technology are unclear, however, with no obvious evidence of a predecessor to the north. Here we present evidence for Clovis hunting and habitation ∼11,550 yBP (∼13,390 Cal years) at “El Fin del Mundo,” an archaeological site in Sonora, northwestern Mexico. The site also includes the first evidence to our knowledge for gomphothere (Cuvieronius sp.) as Clovis prey, otherwise unknown in the North American archaeological record and terminal Pleistocene paleontological record. These data (i) broaden the age and geographic range for Clovis, establishing El Fin del Mundo as one of the oldest and southernmost in situ Clovis sites, supporting the hypothesis that Clovis had its origins well south of the gateways into the continent, and (ii) expand the make-up of the North American megafauna community just before extinction. PMID:25024193

  1. Human (Clovis)-gomphothere (Cuvieronius sp.) association ∼ 13,390 calibrated yBP in Sonora, Mexico.

    Science.gov (United States)

    Sanchez, Guadalupe; Holliday, Vance T; Gaines, Edmund P; Arroyo-Cabrales, Joaquín; Martínez-Tagüeña, Natalia; Kowler, Andrew; Lange, Todd; Hodgins, Gregory W L; Mentzer, Susan M; Sanchez-Morales, Ismael

    2014-07-29

    The earliest known foragers to populate most of North America south of the glaciers [∼ 11,500 to ≥ ∼ 10,800 (14)C yBP; ∼ 13,300 to ∼ 12,800 calibrated (Cal) years] made distinctive "Clovis" artifacts. They are stereotypically characterized as hunters of Pleistocene megamammals (mostly mammoth) who entered the continent via Beringia and an ice-free corridor in Canada. The origins of Clovis technology are unclear, however, with no obvious evidence of a predecessor to the north. Here we present evidence for Clovis hunting and habitation ∼ 11,550 yBP (∼ 13,390 Cal years) at "El Fin del Mundo," an archaeological site in Sonora, northwestern Mexico. The site also includes the first evidence to our knowledge for gomphothere (Cuvieronius sp.) as Clovis prey, otherwise unknown in the North American archaeological record and terminal Pleistocene paleontological record. These data (i) broaden the age and geographic range for Clovis, establishing El Fin del Mundo as one of the oldest and southernmost in situ Clovis sites, supporting the hypothesis that Clovis had its origins well south of the gateways into the continent, and (ii) expand the make-up of the North American megafauna community just before extinction.

  2. Phytolith records of the climate change since the past 15000 years in the middle reach of the Yangtze River in China

    Institute of Scientific and Technical Information of China (English)

    Yansheng GU; Hanlin WANG; Xianyu HUANG; Hongxia PENG; Junhua HUANG

    2012-01-01

    Based on 14C dating and core sediments survey,phytolith records are employed to reconstruct paleovegetation and paleoclimate in the Jianghan Plain in the middle reach of the Yangtze River.Phytoliths identified are assigned into 21well-described morphotypes and divided into four groups (Poaceae,fern,coniferous and broad-leaved).The phytolith assemblages together with warmth index (Iw) are divided into 18 ecological zones,which reflect a complete vegetation history related to climate change in the middle reach of the Yangtze River during the past 15000 years.On the basis of the correlation ofphytolith records with the paleoclimatic indicators from stalagmite,peatland,North Atlantic deep-sea sediments,Loess Plateau of Central China,and Arabic Sea sediments,eight climatic phases are identified included Last Glacial Maximum (LGM) (20-14.8 cal kaBP),Last Deglaciation (LDG) (14.8-11.9cal kaBP),low-temperature phase in the Early Holocene (11.9-8 cal kaBP),Holocene Optimum (8-4.9cal kaBP),Holocene Katathermal (4.9-1.1cal kaBP),Medieval Warmth Period (MWP) (1.1-0.7 cal kaBP),Little Ice Age (LIA) (0.7-0.15 cal kaBP),and Modem Warming (0.15 cal kaBP-present).Climatic events such as Bolling-Allerod warm intervals,Older Dryas,Inter-Allerod Cold Period,and Younger Dryas,and eight Holocene Bond events (B1-8) have been identified since the LDG.Our results demonstrate that the evolution of the climate in the research area has a strong link with the Indian Summer Monsoon (SW Monsoon),Asian Summer Monsoon (SE Monsoon),and Holocene events in North Atlantic simultaneously,which might indicate that solar variability affects the Earth surface climate system at the centennial and millennial scales.

  3. Phytolith records of the climate change since the past 15000 years in the middle reach of the Yangtze River in China

    Science.gov (United States)

    Gu, Yansheng; Wang, Hanlin; Huang, Xianyu; Peng, Hongxia; Huang, Junhua

    2012-03-01

    Based on 14C dating and core sediments survey, phytolith records are employed to reconstruct paleovegetation and paleoclimate in the Jianghan Plain in the middle reach of the Yangtze River. Phytoliths identified are assigned into 21 well-described morphotypes and divided into four groups (Poaceae, fern, coniferous and broad-leaved). The phytolith assemblages together with warmth index ( I w) are divided into 18 ecological zones, which reflect a complete vegetation history related to climate change in the middle reach of the Yangtze River during the past 15000 years. On the basis of the correlation of phytolith records with the paleoclimatic indicators from stalagmite, peatland, North Atlantic deep-sea sediments, Loess Plateau of Central China, and Arabic Sea sediments, eight climatic phases are identified included Last Glacial Maximum (LGM) (20-14.8 cal kaBP), Last Deglaciation (LDG) (14.8-11.9 cal kaBP), low-temperature phase in the Early Holocene (11.9-8 cal kaBP), Holocene Optimum (8-4.9 cal kaBP), Holocene Katathermal (4.9-1.1 cal kaBP), Medieval Warmth Period (MWP) (1.1-0.7 cal kaBP), Little Ice Age (LIA) (0.7-0.15 cal kaBP), and Modern Warming (0.15 cal kaBP — present). Climatic events such as Bolling-Allerod warm intervals, Older Dryas, Inter-Allerod Cold Period, and Younger Dryas, and eight Holocene Bond events (B1-8) have been identified since the LDG. Our results demonstrate that the evolution of the climate in the research area has a strong link with the Indian Summer Monsoon (SW Monsoon), Asian Summer Monsoon (SE Monsoon), and Holocene events in North Atlantic simultaneously, which might indicate that solar variability affects the Earth surface climate system at the centennial and millennial scales.

  4. Sea surface temperatures in the North Atlantic Ocean from 30ka to 10ka

    Science.gov (United States)

    Barrack, Kerr; Greenop, Rosanna; Burke, Andrea; Barker, Stephen; Chalk, Thomas; Crocker, Anya

    2016-04-01

    Some of the most striking features of the Late Pleistocene interval are the rapid changes in climate between warmer interstadial and cold stadial periods which, when coupled, are termed Dansgaard-Oeschger (D-O) events. This shift between warm and cold climates has been interpreted to result from changes in the thermohaline circulation (Broecker et al., 1985) triggered by, for instance, freshwater input from the collapse of the Laurentide ice sheet (Zahn et al., 1997). However, a recent study suggests that major ice rafting events cannot be the 'trigger' for the centennial to millennial scale cooling events identified over the past 500kyr (Barker at al., 2015). Polar planktic foraminiferal and lithogenic/terrigenous grain counts reveal that the southward migration of the polar front occurs before the deposition of ice rafted debris and therefore the rafting of ice during stadial periods. Based upon this evidence, Barker et al. suggest that the transition to a stadial state is a non-linear response to gradual cooling in the region. In order to test this hypothesis, our study reconstructs sea surface temperature across D-O events and the deglaciation in the North Atlantic between 30ka and 10ka using Mg/ Ca paleothermometry in Globigerina bulloides at ODP Sites 980 and 983 (the same sites as used in Barker et al., 2015) with an average sampling resolution of 300 years. With our new record we evaluate the timing of surface ocean temperature change, frontal shift movement, and ice rafting to investigate variations in the temperature gradient across the polar front over D-O events. References: Barker, S., Chen, J., Gong, X., Jonkers, L., Knorr, G., Thornalley, D., 2015. Icebergs not the trigger for North Atlantic cold events. Nature, 520(7547), pp.333-336. Broecker, W.S., Peteer, D.M., Rind, D., 1985. Does the ocean-atmosphere system have more than one stable mode of operation? Nature, 315 (6014), pp.21-26. Zahn, R., Schönfeld, J., Kudrass, H.-R., Park, M

  5. THE CURRENT STAR FORMATION RATE OF K+A GALAXIES

    Energy Technology Data Exchange (ETDEWEB)

    Nielsen, Danielle M. [Department of Astronomy, University of Wisconsin-Madison, 475 North Charter Street, Madison, WI 53706 (United States); Ridgway, Susan E.; De Propris, Roberto [Cerro Tololo Inter-American Observatory Casilla 603, La Serena (Chile); Goto, Tomotsugu, E-mail: nielsen@astro.wisc.edu [Dark Cosmology Center, Niels Bohr Institute, University of Copenhagen, Juliane Maries Vej 30, 2100 Copenhagen O (Denmark)

    2012-12-20

    We derive the stacked 1.4 GHz flux from the FIRST survey for 811 K+A galaxies selected from the Sloan Digital Sky Survey Data Release 7. For these objects we find a mean flux density of 56 {+-} 9 {mu}Jy. A similar stack of radio-quiet white dwarfs yields an upper limit of 43 {mu}Jy at a 5{sigma} significance to the flux in blank regions of the sky. This implies an average star formation rate of 1.6 {+-} 0.3 M{sub Sun} yr{sup -1} for K+A galaxies. However, the majority of the signal comes from {approx}4% of K+A fields that have aperture fluxes above the 5{sigma} noise level of the FIRST survey. A stack of the remaining galaxies shows little residual flux consistent with an upper limit on star formation of 1.3 M{sub Sun} yr{sup -1}. Even for a subset of 456 'young' (spectral ages <250 Myr) K+A galaxies, we find that the stacked 1.4 GHz flux is consistent with no current star formation. Our data suggest that the original starburst has been terminated in the majority of K+A galaxies, but that this may represent part of a duty cycle where a fraction of these galaxies may be active at a given moment with dusty starbursts and active galactic nuclei being present.

  6. The Efficiency of Delone Coverings of the Canonical Tilings MATH {cal T}(*(A_4)) -> T^*(A4) and MATH {cal T}(*(D_6)) -> T^*(D6)

    Science.gov (United States)

    Papadopolos, Zorka; Kasner, Gerald

    This chapter is devoted to the coverings of the two quasiperiodic canonical tilings MATH {cal T}(*(A_4)) -> T^*(A4) and MATH {cal T}(*(D_6)) equiv {cal T}(*(2F)) -> T^*(D6) T^*(2F), obtained by projection from the root lattices A4 and D6, respectively. In the first major part of this chapter, in Sect. 5.2, we shall introduce a Delone covering MATH {cal C}(s_{{cal) T}(*(A_4)}) -> C^sT^*(A4) of the 2-dimensional decagonal tiling MATH {cal T}(*(A_4)) -> T^*(A4). In the second major part of this chapter, Sect. 5.3, we summarize the results related to the Delone covering of the icosahedral tiling MATH {cal T}(*(D_6)) -> T^*(D6), MATH {cal C}_{{cal T}(*(D_6)}) -> CT^*(D6) and determine the zero-, single-, and double- deckings and the resulting thickness of the covering. In the conclusions section, we give some suggestions as to how the definition of the Delone covering might be changed in order to reach some real (full) covering of the icosahedral tiling MATH {cal T}(*(D_6)) -> T^*(D6). In Section 5.2 the definition of the Delone covering is also changed in order to avoid an unnecessary large thickness of the covering.

  7. BP to Increase Production Capacity of PTA at BP Zhuhai Chemical

    Institute of Scientific and Technical Information of China (English)

    2011-01-01

    BP has announced a strategic plan for its substantial development in China. It is actively proceeding with its project to increase its production capacity of purified terephthalic acid, or PTA, at the BP Zhuhai Chemical Company Limited facility i n Guangdong, China.

  8. Sporo-pollen assemblage and paleoclimate events in shelf area of the southern Yellow Sea since 15 ka B. P.

    Science.gov (United States)

    Meng, Guanglan; Han, Yousong; Wang, Shaoqing; Wang, Zhenyan

    2004-03-01

    Based on the authors’ 1986 to 1994 sporo-pollen assemblage analysis in the southern Yellow Sea area, data from 3 main cores were studied in combination with14C, palaeomagnetic and thermoluminescence data. The evolution of the paleoclimate environments in the southern Yellow Sea since 15ka B. P. was revealed that, in deglaciation of the last glacial period, the climate of late glaciation transformed into that of postglaciation, accompanied by a series of violent climate fluctuations. These evolution events happened in a global climate background and related to the geographic changes in eastern China. We distinguished three short-term cooling events and two warming events. Among them, the sporo-pollen assemblage of subzone A1 showed some cold climate features indicating that a cooling event occurred at about 15-14ka. B. P. in early deglaciation. This subzone corresponds to the Oldest Dryas. In subzone A3, many drought-enduring herbal pollens and some few pollens of cold-resistant Picea, Abies, etc. were found, which indicated that a cooling event, with cold and arid climate, occurred at about 12-11ka. B. P. in late deglaciation. This subzone corresponds to the Younger Dryas. The sporo-pollen assemblage of zone B showed warm and arid climate features in postglaciation. Although the assemblage of subzone B2 indicated a cold and arid climate environment, the development of flora in subzone B2 climate was less cold than that in A3. Subzone B2 indicated a cooling event which occurred at about 9ka B. P. in early olocene. Subzone A2, with some distinct differences from subzone A1 and A3, indicated a warming event which occurred at 14-13ka. B.P. and should correspond to a warming fluctuation. The sporo-pollen assemblage of zone C showed features of warn-moist flora and climate, and indicated a warming event which universally occurred along the coast of eastern China at 8-3 ka B. P. in middle Holocene, and its duration was longer than that of any climate events mentioned

  9. Distribution of tetraether lipids in the 25-ka sedimentary record of Lake Challa: extracting reliable TEX86 and MBT/CBT palaeotemperatures from an equatorial African lake

    Science.gov (United States)

    Sinninghe Damsté, Jaap S.; Ossebaar, Jort; Schouten, Stefan; Verschuren, Dirk

    2012-09-01

    The distribution of isoprenoid and branched glycerol dialkyl glycerol tetraether (GDGT) lipids was studied in the sedimentary record of Lake Challa, a permanently stratified, partly anoxic crater lake on the southeastern slope of Mt. Kilimanjaro (Kenya/Tanzania), to examine if the GDGTs could be used to reconstruct past variation in regional temperature. The study material comprised 230 samples from a continuous sediment sequence spanning the last 25 ka with excellent age control based on high-resolution AMS 14C dating. The distribution of GDGTs showed large variation through time. In some time intervals (i.e., from 20.4 to 15.9 ka BP and during the Younger Dryas, 12.9-11.7 ka BP) crenarchaeol was the most abundant GDGT, whereas at other times (i.e., during the Early Holocene) branched GDGTs and GDGT-0 were the major GDGT constituents. In some intervals of the sequence the relative abundance of GDGT-0 and GDGT-2 was too high to be derived exclusively from lacustrine Thaumarchaeota, suggesting a sizable contribution from methanogens and other archaea. This severely complicated application of TEX86 palaeothermometry in this lake, and limited reliable reconstruction of lake water temperature to the time interval 25-13 ka BP, i.e. the Last Glacial Maximum and the period of post-glacial warming. The TEX86-inferred timing of this warming is similar to that recorded previously in two of the large African rift lakes, while its magnitude is slightly or much higher than that recorded at these other sites, depending on which lake-based TEX86 calibration is used. Application of calibration models based on distributions of branched GDGTs developed for lakes inferred temperatures of 15-18 °C for the Last Glacial Maximum and 19-22 °C for the Holocene. However, the MBT/CBT palaeothermometer reconstructs temperatures as low as 12 °C for a Lateglacial period centred on 15 ka BP. Variation in down-core values of the BIT index are mainly determined by the varying production rate of

  10. ATLAS distributed computing operations in the GridKa cloud

    Energy Technology Data Exchange (ETDEWEB)

    Duckeck, Guenter; Serfon, Cedric; Walker, Rodney [Ludwig-Maximilians-Universitaet, Garching (Germany); Harenberg, Torsten; Kalinin, Sergey; Schultes, Joachim [Bergische Universitaet, Wuppertal (Germany); Kawamura, Gen [Johannes-Gutenberg-Universitaet, Mainz (Germany); Leffhalm, Kai [DESY, Zeuthen (Germany); Meyer, Joerg [Georg-August-Universitaet, Goettingen (Germany); Petzold, Andreas [Karlsruher Institut fuer Technologie (Germany); Sundermann, Jan Erik [Albert-Ludwigs-Universitaet, Freiburg (Germany)

    2011-07-01

    The ATLAS Grid Computing resources in Germany, Poland, the Czech Republic, Austria, and Switzerland consist of a cloud of 12 Tier-2 computing centers grouped around the Tier-1 center GridKa at the Steinbuch Centre for Computing at KIT. While the Tier-1 center serves as a hub for data management in the cloud and is the principal resource for reprocessing and custodial storage of raw ATLAS data, the Tier-2 centers provide the resources for user analysis and production of simulated events. During the first full year of data taking at the LHC, the GridKa cloud has successfully contributed to the overall ATLAS computing effort, enabling physicists to quickly analyze the large volume of new incoming data and the corresponding simulated events. This talk covers the computing operations in the GridKa cloud with focus on performance and experiences at both the Tier-1 and Tier-2 centers.

  11. Ka-band MMIC microstrip array for high rate communications

    Science.gov (United States)

    Lee, R. Q.; Raquet, C. A.; Tolleson, J. B.; Sanzgiri, S. M.

    1991-01-01

    In a recent technology assessment of alternative communication systems for the space exploration initiative (SEI), Ka-band (18 to 40 GHz) communication technology was identified to meet the mission requirements of telecommunication, navigation, and information management. Compared to the lower frequency bands, Ka-band antennas offer higher gain and broader bandwidths; thus, they are more suitable for high data rate communications. Over the years, NASA has played an important role in monolithic microwave integrated circuit (MMIC) phased array technology development, and currently, has an ongoing contract with Texas Instrument (TI) to develop a modular Ka-band MMIC microstrip subarray (NAS3-25718). The TI contract emphasizes MMIC integration technology development and stipulates using existing MMIC devices to minimize the array development cost. The objective of this paper is to present array component technologies and integration techniques used to construct the subarray modules.

  12. Kažun kao prepoznatljiv element identiteta Istre

    OpenAIRE

    2013-01-01

    Temeljem terenskih istraživanja provedenih posljednjih desetljeća te prikupljene literature u članku se analizira pojam, funkcija i značaj građevine koja se u Istri označava najčešće imenom kažun, također casita (u nekoliko lokaliteta istroromanskoga govornog područja) te hižica, hiška, koča, kućica na sjevernom dijelu poluotoka. Konstrukcija kažuna podrazumijeva način građenja suhozidom na kružnoj osnovi: kameni prstenovi podižu se u kružni zid, a zatim sužavaju u „lažni svod“ koji se zasipa...

  13. Predicting pKa for proteins using COSMO-RS

    DEFF Research Database (Denmark)

    Andersson, Martin Peter; Jensen, Jan Halborg; Stipp, Susan Louise Svane

    2013-01-01

    We have used the COSMO-RS implicit solvation method to calculate the equilibrium constants, pKa, for deprotonation of the acidic residues of the ovomucoid inhibitor protein, OMTKY3. The root mean square error for comparison with experimental data is only 0.5 pH units and the maximum error 0.8 p......H units. The results show that the accuracy of pKa prediction using COSMO-RS is as good for large biomolecules as it is for smaller inorganic and organic acids and that the method compares very well to previous pKa predictions of the OMTKY3 protein using Quantum Mechanics/Molecular Mechanics. Our approach...

  14. Mid-Holocene mangrove succession and its response to sea-level change in the upper Mekong River delta, Cambodia

    Science.gov (United States)

    Li, Zhen; Saito, Yoshiki; Mao, Limi; Tamura, Toru; Li, Zhen; Song, Bing; Zhang, Yulan; Lu, Anqing; Sieng, Sotham; Li, Jie

    2012-09-01

    Middle Holocene vegetation and mangrove successions are clearly evident in the palynological records of two cores from the upper Mekong River delta in Cambodia. Spanning from ~ 9.4 to 6.3 cal ka BP, the cores mainly record a transgressive sequence from floodplain freshwater marsh to tidal flat, which was overlain by mangrove. Corresponding to the decelerated sea-level rise at ~ 8.3 cal ka BP, pioneer mangrove species Sonneratia alba and Sonneratia caseolaris appeared in the sediments, and then was replaced by regressive mangrove succession containing upward-increasing abundances of Rhizophora apiculata and Bruguiera spp. High salinity- and flooding-tolerant community S. alba was developed at the western core site PSG at ~ 8.2 cal ka BP, and the eastern core site PK at ~ 7.5 cal ka BP. The time difference of S. alba appearance between the two sites might be resulted from the complexity of sedimentary environment, where a higher sediment supply was provided to the western floodplain than to the eastern floodplain. After 7.5 cal ka BP, aggradational stacking of intertidal sediments, of which the thickness is larger than the present maximum tidal range, may have resulted from continuous sea-level rise during 7.5-7.0 cal ka BP.

  15. Southwest monsoon changes indicated by oxygen isotope of ostracode shells from sediments in Qinghai Lake since the late Glacial

    Institute of Scientific and Technical Information of China (English)

    LIU XingQi; SHEN Ji; WANG SuMin; WANG YongBo; LIU WeiGuo

    2007-01-01

    The δ18O records of ostracode shells in sediments of core QH-2000 from Qinghai Lake can be used as a better proxy to reflect monsoon changes. Low monsoon precipitation between 17.5 and 11 cal. Ka BP is indicated by positive δ18O values averaging 2.37‰. A fast shift in δ18O from positive at 11 cal. Ka BP to negative at 10 cal. Ka BP indicates sharp increase of monsoon precipitation. An interval of generally high monsoon precipitation is observed between 10 and 6 cal. Ka BP with δ18O values averaging -2.15‰. Decrease of monsoon precipitation between 6 and 2.5 cal. Ka BP is indicated by positive δ18O values. δ18O keeps positive values averaging 3.0‰ between 2.5 and 0 cal. Ka BP suggesting low high monsoon precipitation. The climatic changes indicated by δ18O records of ostracode shells in sediments of core QH-2000 from Qinghai Lake and our broader regional comparison show that the climate in Qinghai Lake since the late Glacial is probably controlled by southwest monsoon other than southeast monsoon.

  16. X-/Ka-band dichroic plate noise temperature reduction

    Science.gov (United States)

    Veruttipong, W.; Lee, P.

    1994-11-01

    The X-/Ka-band (8.4 GHz/32.0 GHz) dichroic plate installed as DSS 13 contributes an estimated 3 K to the system noise temperature at 32.0 GHz. Approximately 1 percent of the Ka-band incident field is reflected by the plate into the 300-K environment of the DSS-13 pedestal room. A low-cost, easily implemented method of reducing the noise temperature is presented. Using a curved reflector, the reflected field can be re-focused into an 80-K cold load, reducing the noise temperature contribution of the dichroic plate by about 2 K.

  17. Identiteto paieška šeimos fotografijose

    OpenAIRE

    Kniškaitė, Kristina

    2012-01-01

    Darbe nagrinėjamas identitetas ir jo paieška šeimos fotografijose. Keliamas tikslas išanalizuoti identitetą ir jo vizualumą formuojančius faktorius. Kadangi darbo tema susijusi su savęs paieška, analizės objektu tampa tapatumas, o šeima pasirinkta kaip priemonė jam atskleisti. Albuminės fotografijos šiame darbe naudojamos kaip giminės istorinis šaltinis, kaip paveldas, kurio pagalba ne tik vizualiai atkuriamas šeimos genealoginis medis, bet ir pereinama prie interpretacinio požiūrio į albumi...

  18. Pollen-climate relationships in time (9 ka, 6 ka, 0 ka) and space (upland vs. lowland) in eastern continental Asia

    Science.gov (United States)

    Tian, Fang; Cao, Xianyong; Dallmeyer, Anne; Zhao, Yan; Ni, Jian; Herzschuh, Ulrike

    2017-01-01

    Temporal and spatial stability of the vegetation-climate relationship is a basic ecological assumption for pollen-based quantitative inferences of past climate change and for predicting future vegetation. We explore this assumption for the Holocene in eastern continental Asia (China, Mongolia). Boosted regression trees (BRT) between fossil pollen taxa percentages (Abies, Artemisia, Betula, Chenopodiaceae, Cyperaceae, Ephedra, Picea, Pinus, Poaceae and Quercus) and climate model outputs of mean annual precipitation (Pann) and mean temperature of the warmest month (Mtwa) for 9 and 6 ka (ka = thousand years before present) were set up and results compared to those obtained from relating modern pollen to modern climate. Overall, our results reveal only slight temporal differences in the pollen-climate relationships. Our analyses suggest that the importance of Pann compared with Mtwa for taxa distribution is higher today than it was at 6 ka and 9 ka. In particular, the relevance of Pann for Picea and Pinus increases and has become the main determinant. This change in the climate-tree pollen relationship parallels a widespread tree pollen decrease in north-central China and the eastern Tibetan Plateau. We assume that this is at least partly related to vegetation-climate disequilibrium originating from human impact. Increased atmospheric CO2 concentration may have permitted the expansion of moisture-loving herb taxa (Cyperaceae and Poaceae) during the late Holocene into arid/semi-arid areas. We furthermore find that the pollen-climate relationship between north-central China and the eastern Tibetan Plateau is generally similar, but that regional differences are larger than temporal differences. In summary, vegetation-climate relationships in China are generally stable in space and time, and pollen-based climate reconstructions can be applied to the Holocene. Regional differences imply the calibration-set should be restricted spatially.

  19. CaCO3 CYCLES IN SALAWUSU RIVER BASIN SINCE 150KA B. P.

    Institute of Scientific and Technical Information of China (English)

    2001-01-01

    This paper, with Milanggouwan stratigraphic section as a typical section of the Salawusu River Basin,explores the relation between CaCO3 content distribution and climate change since 150 ka B.P. and concludes that: 1) The low-high changes of CaCO3 content in the section has a remarkable corresponding relation with the sedimentary cycles of ancient aeolian sand and overlying fluviolacustrine facies or palaeosols. 2) CaCO3 distribution in aeolian sand is relatively meagre, ranging from 0. 8% -7.18%, or on an average 2. 50% but relatively enriches in the fluviolacustrine faceis and palaeosols, ranging from 2. 20% - 14. 9%, or on an average 5.74%. This implies that they have different climatic backgrounds. The former was the product of erosion, transport and deposition by wind under arid and cold climatic conditions, whereas the latter was related to its special low-lying geomorphic position between the Ordos Plateau and Loess Plateau and warm-humid climatic environment. When the climatic became warm and humid, fluviola custrine and swamp facies developed, soil-forming action strengthened, and low-lying catchment condition was favor able to CaCO3 accumulation. 3) The basic cause responsible for the multicycie of CaCO3 migration and accumulation in the Milanggouwan section may be the multiple alterations of winter and summer monsoons over the Mu Us Desert under the influences of climatic fluctuation of glacial and interglacial periods in the Northern Hemisphere since 150ka B. P..

  20. CAMPARE and Cal-Bridge: Two Institutional Networks Increasing Diversity in Astronomy

    Science.gov (United States)

    Rudolph, Alexander L.; Smecker-Hane, Tammy A.

    2017-01-01

    We describe two programs, CAMPARE and Cal-Bridge, with the common mission of increasing participation of groups traditionally underrepresented in astronomy, through summer research opportunities, in the case of CAMPARE, scholarships in the case of Cal-Bridge, and significant mentoring in both programs, creating a national impact on their numbers successfully pursuing a PhD in the field.In 7 years, the CAMPARE program has sent 80 students, >80% from underrepresented groups, to conduct summer research at one of 14 major research institutions throughout the country. The graduation rate among CAMPARE scholars is 98%, and of the CAMPARE scholars who have graduated with a Bachelor’s degree, more than 60% have completed or are pursuing graduate education in astronomy or a related field, at institutions including UCLA, UC Riverside, UC Irvine, UC Santa Barbara, USC, Stanford, Univ. of Arizona, Univ. of Washington, and the Fisk-Vanderbilt Master’s-to-PhD program.Now entering its third year, the Cal-Bridge program is a CSU-UC Bridge program comprised of over 75 physics and astronomy faculty from 5 University of California (UC), 9 California State University (CSU), and 14 California Community College (CCC) campuses in Southern California. In the first three years, 22 Cal-Bridge Scholars have been selected, including 11 Hispanic, 3 African-American and 8 female students, 5 of whom are from URM groups. Nineteen (19) of the 22 Cal-Bridge Scholars are first-generation college students. The entire first cohort of 4 Cal-Bridge scholars was accepted to one or more PhD programs in astronomy or physics, including UC Irvine, UC Santa Cruz, UC Davis, Michigan State, and Georgia State Universities. The second cohort of 8 Cal-Bridge scholars is applying to graduate schools this fall.Cal-Bridge provides much deeper mentoring and professional development experiences over the last two years of undergraduate and first year of graduate school to students from this diverse network of higher

  1. 2000 Johnston Site 3B-P

    Data.gov (United States)

    US Fish and Wildlife Service, Department of the Interior — Underwater Site 3B-P was established at Johnston Atoll by Dr. James Maragos, U.S. Fish & Wildlife Service, on July 3, 2000. With a start point (meter 0) at...

  2. 2000 Johnston Site 1B-P

    Data.gov (United States)

    US Fish and Wildlife Service, Department of the Interior — Underwater Site 1B-P was established at Johnston Atoll by Dr. James Maragos, U.S. Fish & Wildlife Service, on June 29, 2000. With a start point (meter 0) at...

  3. 2000 Johnston Site 2B-P

    Data.gov (United States)

    US Fish and Wildlife Service, Department of the Interior — Underwater Site 2B-P was established at Johnston Atoll by Dr. James Maragos, U.S. Fish & Wildlife Service, on June 30, 2000. With a start point (meter 0) at...

  4. The Golden Point of No-Scale and No-Parameter ${\\cal F}$-$SU(5)$

    CERN Document Server

    Li, Tianjun; Nanopoulos, Dimitri V; Walker, Joel W

    2010-01-01

    The ${\\cal F}$-lipped $SU(5)\\times U(1)_X$ Grand Unified Theory (GUT) supplemented by TeV-scale vector-like particles from ${\\cal F}$-theory, together dubbed ${\\cal F}$-$SU(5)$, offers a natural multi-phase unification process which suggests an elegant implementation of the No-Scale Supergravity boundary conditions at the unification scale $M_{\\cal F} \\simeq 7 \\times 10^{17}$~GeV. Enforcing the No-Scale boundary conditions, including $B_\\mu(M_{\\cal F})=0$ on the Higgs bilinear soft term, with the precision 7-year WMAP value on the dark matter relic density isolates a highly constrained ``golden point'' located near $M_{1/2} = 455$~GeV and $\\tan \\beta = 15$ in the $\\tan\\beta-M_{1/2}$ plane, which simultaneously satisfies all known experiments, and moreover corresponds to an imminently observable proton decay rate. Because the universal gaugino mass is actually determined from established low energy data via Renormalization Group Equation (RGE) running, there are no surviving arbitrary scale parameters in the p...

  5. AcEST: BP919856 [AcEST

    Lifescience Database Archive (English)

    Full Text Available YMU001_000130_A02 514 Adiantum capillus-veneris mRNA. clone: YMU001_000130_A02. BP919856 - Show BP91985...is mRNA. clone: YMU001_000130_A02. Accession BP919856 Tissue type prothallium Developmental stage - Contig I...protein database search programs, Nucleic Acids Res. 25:3389-3402. Query= BP91985... generation of protein database search programs, Nucleic Acids Res. 25:3389-3402. Query= BP919856|Adiantum c

  6. AcEST: BP919841 [AcEST

    Lifescience Database Archive (English)

    Full Text Available YMU001_000129_G06 496 Adiantum capillus-veneris mRNA. clone: YMU001_000129_G06. BP919841 - Show BP91984...is mRNA. clone: YMU001_000129_G06. Accession BP919841 Tissue type prothallium Developmental stage - Contig I...ase search programs, Nucleic Acids Res. 25:3389-3402. Query= BP919841|Adiantum ca...e search programs, Nucleic Acids Res. 25:3389-3402. Query= BP919841|Adiantum capi

  7. AcEST: BP919150 [AcEST

    Lifescience Database Archive (English)

    Full Text Available YMU001_000121_G08 485 Adiantum capillus-veneris mRNA. clone: YMU001_000121_G08. BP919150 - Show BP91915...is mRNA. clone: YMU001_000121_G08. Accession BP919150 Tissue type prothallium Developmental stage - Contig I...n of protein database search programs, Nucleic Acids Res. 25:3389-3402. Query= BP91915... of protein database search programs, Nucleic Acids Res. 25:3389-3402. Query= BP91915

  8. AcEST: BP920131 [AcEST

    Lifescience Database Archive (English)

    Full Text Available YMU001_000133_D06 495 Adiantum capillus-veneris mRNA. clone: YMU001_000133_D06. BP920131 - Show BP92013...is mRNA. clone: YMU001_000133_D06. Accession BP920131 Tissue type prothallium Developmental stage - Contig I..., Nucleic Acids Res. 25:3389-3402. Query= BP920131|Adiantum capillus-veneris mRNA...base search programs, Nucleic Acids Res. 25:3389-3402. Query= BP920131|Adiantum c

  9. AcEST: BP919887 [AcEST

    Lifescience Database Archive (English)

    Full Text Available YMU001_000130_C10 511 Adiantum capillus-veneris mRNA. clone: YMU001_000130_C10. BP919887 - Show BP91988...is mRNA. clone: YMU001_000130_C10. Accession BP919887 Tissue type prothallium Developmental stage - Contig I...generation of protein database search programs, Nucleic Acids Res. 25:3389-3402. Query= BP91988...on of protein database search programs, Nucleic Acids Res. 25:3389-3402. Query= BP91988

  10. AcEST: BP920154 [AcEST

    Lifescience Database Archive (English)

    Full Text Available YMU001_000133_F09 487 Adiantum capillus-veneris mRNA. clone: YMU001_000133_F09. BP920154 - Show BP92015...is mRNA. clone: YMU001_000133_F09. Accession BP920154 Tissue type prothallium Developmental stage - Contig I...n database search programs, Nucleic Acids Res. 25:3389-3402. Query= BP920154|Adia...abase search programs, Nucleic Acids Res. 25:3389-3402. Query= BP920154|Adiantum

  11. AcEST: BP921101 [AcEST

    Lifescience Database Archive (English)

    Full Text Available YMU001_000145_F04 489 Adiantum capillus-veneris mRNA. clone: YMU001_000145_F04. BP921101 - Show BP921101...is mRNA. clone: YMU001_000145_F04. Accession BP921101 Tissue type prothallium Developmental stage - Contig I...se search programs, Nucleic Acids Res. 25:3389-3402. Query= BP921101|Adiantum cap... protein database search programs, Nucleic Acids Res. 25:3389-3402. Query= BP921101

  12. AcEST: BP914001 [AcEST

    Lifescience Database Archive (English)

    Full Text Available YMU001_000038_G04 493 Adiantum capillus-veneris mRNA. clone: YMU001_000038_G04. BP914001 - Show BP91400...is mRNA. clone: YMU001_000038_G04. Accession BP914001 Tissue type prothallium Developmental stage - Contig I...otein database search programs, Nucleic Acids Res. 25:3389-3402. Query= BP914001|...ic Acids Res. 25:3389-3402. Query= BP914001|Adiantum capillus-veneris mRNA, clone

  13. AcEST: BP919212 [AcEST

    Lifescience Database Archive (English)

    Full Text Available YMU001_000122_E05 508 Adiantum capillus-veneris mRNA. clone: YMU001_000122_E05. BP919212 - Show BP91921...is mRNA. clone: YMU001_000122_E05. Accession BP919212 Tissue type prothallium Developmental stage - Contig I... programs, Nucleic Acids Res. 25:3389-3402. Query= BP919212|Adiantum capillus-ven...ion of protein database search programs, Nucleic Acids Res. 25:3389-3402. Query= BP919212|Adiantum capillus-

  14. AcEST: BP920173 [AcEST

    Lifescience Database Archive (English)

    Full Text Available YMU001_000133_H07 454 Adiantum capillus-veneris mRNA. clone: YMU001_000133_H07. BP920173 - Show BP92017...is mRNA. clone: YMU001_000133_H07. Accession BP920173 Tissue type prothallium Developmental stage - Contig I...Res. 25:3389-3402. Query= BP920173|Adiantum capillus-veneris mRNA, clone: YMU001_...arch programs, Nucleic Acids Res. 25:3389-3402. Query= BP920173|Adiantum capillus

  15. Was the 12.1 ka Icelandic Vedde Ash one of a kind?

    Science.gov (United States)

    Lane, C. S.; Blockley, S. P. E.; Mangerud, J.; Smith, V. C.; Lohne, Ø. S.; Tomlinson, E. L.; Matthews, I. P.; Lotter, A. F.

    2012-02-01

    The Vedde Ash is the most important volcanic event marker layer for the correlation of Late Quaternary palaeoenvironmental archives in Europe and the North Atlantic. First defined from its type site localities near Ålesund, Western Norway, the Vedde Ash has now been traced across much of northern and central Europe, into northwest Russia, within North Atlantic marine sediments and into the Greenland ice cores. The Vedde Ash is thought to derive from an eruption of the Katla volcano in Iceland that occurred midway through the Younger Dryas/Greenland Stadial 1 (GS-1), ˜12.1 ka BP. Visible and cryptotephra deposits of the Vedde Ash have been found in numerous stratified sites with robust chronologies, which allow its age to be constrained and its dispersal to be mapped. The eruption must have been highly explosive, however few proximal outcrops have been confirmed and this crucial ash layer remains almost exclusively distally-described and characterised using major element glass compositions. The widespread distribution, stratigraphic associations and consistent major element glass chemistry have led the Quaternary tephrochronological community to see the Vedde Ash as a robust and unique chronological marker layer for the Last Glacial to Interglacial Transition (˜10-18 ka BP). Here we present new glass analyses of the Vedde Ash from multiple sites around the dispersal area, using a full suite of compositional analysis, including for the first time, single-grain trace element data. These data demonstrate the strong compositional coherence of Vedde Ash deposits. However, comparison with major, minor, and trace element compositional data from several other distally-described Icelandic tephras reveals that both before and after the Younger Dryas chronozone, there were eruptions that generated widespread tephra layers that have comparable glass shard compositions to the Vedde Ash. This implies that these numerous events not only hail from the same volcanic system, but

  16. Multi-Step Ka/Ka Dichroic Plate with Rounded Corners for NASA's 34m Beam Waveguide Antenna

    Science.gov (United States)

    Veruttipong, Watt; Khayatian, Behrouz; Hoppe, Daniel; Long, Ezra

    2013-01-01

    A multi-step Ka/Ka dichroic plate Frequency Selective Surface (FSS structure) is designed, manufactured and tested for use in NASA's Deep Space Network (DSN) 34m Beam Waveguide (BWG) antennas. The proposed design allows ease of manufacturing and ability to handle the increased transmit power (reflected off the FSS) of the DSN BWG antennas from 20kW to 100 kW. The dichroic is designed using HFSS and results agree well with measured data considering the manufacturing tolerances that could be achieved on the dichroic.

  17. Multi-Step Ka/Ka Dichroic Plate with Rounded Corners for NASA's 34m Beam Waveguide Antenna

    Science.gov (United States)

    Veruttipong, Watt; Khayatian, Behrouz; Hoppe, Daniel; Long, Ezra

    2013-01-01

    A multi-step Ka/Ka dichroic plate Frequency Selective Surface (FSS structure) is designed, manufactured and tested for use in NASA's Deep Space Network (DSN) 34m Beam Waveguide (BWG) antennas. The proposed design allows ease of manufacturing and ability to handle the increased transmit power (reflected off the FSS) of the DSN BWG antennas from 20kW to 100 kW. The dichroic is designed using HFSS and results agree well with measured data considering the manufacturing tolerances that could be achieved on the dichroic.

  18. 布鲁菌 bp26基因的原核表达及间接 ELISA方法的临床初步应用%Prokaryotic Expression of Brucella bp26 Gene and Preliminary Clinical Application of BP26-iELISA Assay

    Institute of Scientific and Technical Information of China (English)

    谷海峰; 郭港; 刘雪梅; 李天惠; 李鲁平

    2015-01-01

    构建诊断人布氏菌病的优势抗原BP26原核表达载体,并建立以该蛋白作为包被抗原的间接ELISA方法。人工合成bp26基因片段,构建原核表达载体pET30a-bp26,并转化入大肠埃希菌BL21(DE3)中,IPTG诱导表达,Ni柱亲和纯化BP26重组蛋白,间接ELISA检测其抗原活性,并优化间接ELISA方法的各个参数,检测临床大量样本,对该方法性能进行评价。 PCR鉴定及DNA测序证实pET30a-bp26重组质粒构建成功,并在0.8 mmol/L IPTG 20℃过夜诱导的条件下大量表达,经亲和纯化获得高纯度的可溶性BP26重组蛋白,间接ELISA结果显示该重组蛋白具有抗原活性,优化参数后,该方法的敏感度为70.00%,特异性为94.74%。成功获得高抗原活性的原核表达可溶性BP26重组蛋白,并建立用于临床特异性诊断人类布病的间接ELISA方法。%Prokaryotic expression vector of BP26, a predominant antigen for diagnosis of human brucellosis was con-structed, and established an indirect enzyme-linked immunosorbent assay ( i-ELISA) with the protein as encapsulated antigen.Gene fragment of bp26 was artificially synthesized and cloned into expression vector pET-30a to construct pro-caryotic vector pET30a-bp26 and transformed into competent E.coli BL21 ( DE3) cells and induced and expressed by IPTG, the recombinant BP26 protein was purified through Ni affinity chromatography.Antigenic activity of recombi-nant protein was tested by i-ELISA, and optimized each parameter of i-ELISA, and detecting a large number of clini-cal samples to evaluate the performance of the method.The results showed that PCR appraisal and DNA sequencing have confirmed that the recombinant plasmid pET30a-bp26 was successfully constructed.It was induced to express re-combinant protein BP26 in large number in 0.8 mmol/L IPTG at 20 ℃overnight, and obtained soluble protein BP26 with high purity through affinity chromatography.As demonstrated by

  19. Evidence for higher-than-average air temperatures after the 8.2 ka event provided by a Central European δ18O record

    Science.gov (United States)

    Andersen, Nils; Lauterbach, Stefan; Erlenkeuser, Helmut; Danielopol, Dan L.; Namiotko, Tadeusz; Hüls, Matthias; Belmecheri, Soumaya; Dulski, Peter; Nantke, Carla; Meyer, Hanno; Chapligin, Bernhard; von Grafenstein, Ulrich; Brauer, Achim

    2017-09-01

    The so-called 8.2 ka event represents one of the most prominent cold climate anomalies during the Holocene warm period. Accordingly, several studies have addressed its trigger mechanisms, absolute dating and regional characteristics so far. However, knowledge about subsequent climate recovery is still limited although this might be essential for the understanding of rapid climatic changes. Here we present a new sub-decadally resolved and precisely dated oxygen isotope (δ18O) record for the interval between 7.7 and 8.7 ka BP (103 calendar years before AD 1950), derived from the calcareous valves of benthic ostracods preserved in the varved lake sediments of pre-Alpine Mondsee (Austria). Besides a clear reflection of the 8.2 ka event, showing a good agreement in timing, duration and magnitude with other regional stable isotope records, the high-resolution Mondsee lake sediment record provides evidence for a 75-year-long interval of higher-than-average δ18O values directly after the 8.2 ka event, possibly reflecting increased air temperatures in Central Europe. This observation is consistent with evidence from other proxy records in the North Atlantic realm, thus most probably reflecting a hemispheric-scale climate signal rather than a local phenomenon. As a possible trigger we suggest an enhanced resumption of the Atlantic meridional overturning circulation (AMOC), supporting assumptions from climate model simulations.

  20. Planktonic Foraminifera as Sensitive Recorders of Climate Variability in the Eastern Mediterranean During the Last ~90 ka

    Science.gov (United States)

    Almogi-Labin, A.; Bar-Matthews, M.; Ayalon, A.; Paterne, M.

    2014-12-01

    Planktonic foraminifera (PF) are widely used in Quaternary paleoceanography as carriers of oxygen stable isotope signal. This signal is one of the main tools for establishing chronostratigraphy and determining the nature of global and local glacial and interglacial cycles. In this study, the focus is on the PF assemblages which are sensitive recorders of climate and water column properties including the degree of water column stratification and trophic levels. In order to reconstruct the climate variability of the last ~90 ka, core MDVAL9501 (980 m water depth), taken by R/V Marion Dufresnae, SE of Cyprus, was studied. A δ18O-Globigerinoides ruber stratigraphy was established and correlated with well-dated (U/Th) speleothem records of Soreq Cave and radiocarbon dates. The sedimentary record in this core covers the last ~90ka. Variations in PF assemblage composition indicate that conditions shifted between two main climatic scenarios. During the last glacial cooler, more aerated, less stratified and more mesotrophic water column persisted with distinct seasonality. This is evident from the occurrence of two deep water dwellers Globorotalia inflata being abundant from 75 to 50 ka BP and G. scitula from 55 to 15 ka BP (with respective SST of 15-16 ºC and 11-13 ºC) and accompanied continuously by the cold water species Neogloboqudrina pachyderma and Globigerina bulloides. Among the "warm" water species G. ruber is nearly the only "survivor" during the glacial period comprising 25-50% of the assemblage with lower values corresponding to minima in D-O events. During Holocene, water column was warmer, more stratified, mostly oligotrophic with reduced seasonality. The dominating species were G. ruber and other "warm" water species comprising >75% of the assemblage and occurring in low numbers. An exception are sapropel S1 (early Holocene) and S3 (MIS 5.1) periods, when lower δ18O and highest TOC values prevail with significantly increased numerical abundance of PF

  1. Improvisatsioonilised filmietendus-kontserdid "Kas kino ka saab?"

    Index Scriptorium Estoniae

    2006-01-01

    Eesti Ajaloomuuseumi ja Eesti Film 100 poolt Suurgildi hoones korraldatud koostöönäitust "Elavad ja laulvad pildid" täiendab filmietenduste-kontsertide sari "Kas kino ka saab?", kus täna on kinoklassiku Georges Meliesi (1861-1938) filmiprogramm Jaak Lõhmuse kommenteeriva sõnavõtuga

  2. Che legend elab ka 40 aastat hiljem / Evelyn Kaldoja

    Index Scriptorium Estoniae

    Kaldoja, Evelyn, 1980-

    2007-01-01

    Ilmunud ka: Postimees : na russkom jazõke 9. okt. lk. 10. Argentinas sündinud ja 1967. aastal hukatud revolutsionääri Ernesto Che Guevara poliitikukarjäärist, tema panusest Kuuba revolutsiooni ja poliitikasse. Ernesto Che Guevara mälestamisest Ladina-Ameeerika riikides. Lisa: Kuuba revolutsioon; Che Guevara elu

  3. Additive manufacturing of Ka-band antennas for wireless communications

    DEFF Research Database (Denmark)

    Armendariz, Unai; Rommel, Simon; Rodríguez Páez, Juan Sebastián

    2016-01-01

    This paper presents the design and fabrication of WR-28 waveguide horn antennas operating in the Ka-band frequency range between 26.5 GHz and 40 GHz through 3D printing. Three different antennas are fabricated from polylactide acid filaments in conductive and non-conductive variants; the latter...

  4. Aju rehkendab pingsalt ka unelemise ajal / Tiit Kändler

    Index Scriptorium Estoniae

    Kändler, Tiit, 1948-

    2011-01-01

    Siiani arvati, et kui inimene ei tegutse, siis ei tegutse ka aju. Nüüdseks on selge, et aju on aktiivne alati. Ja matemaatiliste ülesannete lahendamisega seotud ajupiirkonnad on ühed, mis inimese ajus alati valvel püsivad

  5. Eesti Energia emissioonis on koht ka rahvaaktsiatel / Raimo Poom

    Index Scriptorium Estoniae

    Poom, Raimo

    2010-01-01

    Eesti Energia võimaliku aktsiaemissiooni korral tagatakse võimalus soetada aktsiaid ka jaeinvestoritel. Majandus- ja kommunikatsiooniminister Juhan Partsi sõnul tugevdaks see Eesti inimeste huvi energeetika vastu, samuti võimaldaks see paigutada oma sääste Eesti arenguga seotud ettevõttesse

  6. Suhkruturu reform : [ka teiste toiduainete turu reformist] / Ants Laansalu

    Index Scriptorium Estoniae

    Laansalu, Ants, 1938-2011

    2005-01-01

    Ilmunud ka: Agriculture and the development of rural life : overview 2004/2005. - Tallinn, 2005, lk. 83-86. Euroopa Komisjon esitles 2004. a juuli keskel suhkruturu reformikava, mille eesmärgiks on muuta sektor konkurentsivõimelisemaks, turu nõudlustele vastavaks, tarbija- ja keskkonnasõbralikumaks ning lõpetada ületootmine

  7. Eesti Energia emissioonis on koht ka rahvaaktsiatel / Raimo Poom

    Index Scriptorium Estoniae

    Poom, Raimo

    2010-01-01

    Eesti Energia võimaliku aktsiaemissiooni korral tagatakse võimalus soetada aktsiaid ka jaeinvestoritel. Majandus- ja kommunikatsiooniminister Juhan Partsi sõnul tugevdaks see Eesti inimeste huvi energeetika vastu, samuti võimaldaks see paigutada oma sääste Eesti arenguga seotud ettevõttesse

  8. Ehitusala tõus jätkus ka mullu

    Index Scriptorium Estoniae

    2004-01-01

    Ilmunud ka: Delovõje Vedomosti, 3. nov. 2004, lk. 14-15. Ehitusfirmade TOP 95 aastal 2003. Kasumi TOP 40. Käibe TOP 40. TOP-i koostamise metoodika. Kasumi kasvu TOP 20. Käibe kasvu TOP 20. Omakapitali tootluse TOP 20. Rentaabluse TOP 20. Ehitusettevõtete üld- ja finantsandmed

  9. Ottis osales ka ise kahtlases riigihankes / Villy Paimets

    Index Scriptorium Estoniae

    Paimets, Villy, 1972-

    2005-01-01

    AS-i Riigi Kinnisvara juht Tiit Ottis palus 2005. aasta mais keskkriminaalpolitseil algatada Kärdla piirivalvekordoni hangete uurimiseks kriminaalasi. Antud hankel osales ka Ottise loodud AS Gustaf, mis pakkus küll odavaimat hinda, kuid konkursi võitis AS Pameron. Vt. samas: Kriminaalasi algatati teo suhtes

  10. Che legend elab ka 40 aastat hiljem / Evelyn Kaldoja

    Index Scriptorium Estoniae

    Kaldoja, Evelyn, 1980-

    2007-01-01

    Ilmunud ka: Postimees : na russkom jazõke 9. okt. lk. 10. Argentinas sündinud ja 1967. aastal hukatud revolutsionääri Ernesto Che Guevara poliitikukarjäärist, tema panusest Kuuba revolutsiooni ja poliitikasse. Ernesto Che Guevara mälestamisest Ladina-Ameeerika riikides. Lisa: Kuuba revolutsioon; Che Guevara elu

  11. Kas läheb ka Ruudi tapmiseks? / Kati Murutar

    Index Scriptorium Estoniae

    Murutar, Kati, 1967-

    2006-01-01

    Lastefilm "Ruudi" : stsenaristid Katrin Laur, Aare Toikka, Aarne Mägi : režissöör Katrin Laur : nimiosas lapsnäitleja Paul Oskar Soe : Allfilm - MRP Matila Röhr Productions - Schmidtz Katze Filmkollektiv 2006. Võetud kõne alla ka Peeter Simmi "Kõrini!" ja Peeter Urbla "Stiilipeo" arvustaja meelest teenimatult mahategevad retsensioonid

  12. Ehitusala tõus jätkus ka mullu

    Index Scriptorium Estoniae

    2004-01-01

    Ilmunud ka: Delovõje Vedomosti, 3. nov. 2004, lk. 14-15. Ehitusfirmade TOP 95 aastal 2003. Kasumi TOP 40. Käibe TOP 40. TOP-i koostamise metoodika. Kasumi kasvu TOP 20. Käibe kasvu TOP 20. Omakapitali tootluse TOP 20. Rentaabluse TOP 20. Ehitusettevõtete üld- ja finantsandmed

  13. Experimental radio frequency link for Ka-band communications applications

    Science.gov (United States)

    Fujikawa, Gene; Conray, Martin J.; Saunders, Alan L.; Pope, Dale E.

    1988-01-01

    An experimental radio frequency link has been demonstrated to provide two-way communication between a remote user ground terminal and a ground-based Ka-band transponder. Bit-error-rate performance and radio frequency characteristics of the communication link were investigated.

  14. High Througput pKa Prediction Using Semi Empirical Methods

    CERN Document Server

    Jensen, Jan H

    2015-01-01

    A large proportion of organic molecules relevant to medicine and biotechnology contain one or more ionizable groups, which means that fundamental physical and chemical properties (e.g. the charge of the molecule) depend on the pH of the surroundings via the corresponding pKa values of the molecules. As drug- and material design increasingly is being done through high throughput screens, fast - yet accurate - computational pKa prediction methods are becoming crucial to the design process. Current empirical pKa predictors are increasingly found to fail because they are being applied to parts of chemical space for which experimental parameterization data is lacking. We propose to develop a pKa predictor that, due its quantum mechanical foundation, is more generally applicable but still fast enough to be used in high throughput screening. The method has the potential to impact virtually any biotechnological design process involving organic molecules as we will demonstrate for metabolic engineering and organic bat...

  15. Tõnu Talve "Ka" tuuritab Kadrinas ja Rakveres / Ants Juske

    Index Scriptorium Estoniae

    Juske, Ants, 1956-

    2005-01-01

    Tõnu Talve maalidest. Kadrinas esitatud trio Fragile performance'st ja näitusest tsüklist "Ka" Rakveres. Rakvere näitusel Teele Tuuna ja kolmeaastase tütre Anneliise tööd. Trio Fragile koosseisus on kitarrist Robert Jürjendal, trummar Arvo Urb ja maalija Tõnu Talve

  16. Holland soovib Maailmapanga juhi kohale ka teisi kandidaate / Kalev Vilgats

    Index Scriptorium Estoniae

    Vilgats, Kalev

    2005-01-01

    USA president George W. Bush nimetas Iraagi sõja peamise planeerija Paul Wolfowitzi Maailmapanga presidendi kandidaadiks. See valik on Euroopas põhjustanud vastuolusid, kuna temast kardetakse Bushi senise välispoliitilise stiili jätkajat ka Maailmapangas. Bill Clintonit peetakse üheks võimalikuks kandidaadiks ÜRO peasekräri kohale

  17. Improvisatsioonilised filmietendus-kontserdid "Kas kino ka saab?"

    Index Scriptorium Estoniae

    2006-01-01

    Eesti Ajaloomuuseumi ja Eesti Film 100 poolt Suurgildi hoones korraldatud koostöönäitust "Elavad ja laulvad pildid" täiendab filmietenduste-kontsertide sari "Kas kino ka saab?", kus täna on kinoklassiku Georges Meliesi (1861-1938) filmiprogramm Jaak Lõhmuse kommenteeriva sõnavõtuga

  18. Aspects of screening and confinement in a topologically massive $U{\\left( 1 \\right)_{\\cal W}} \\times U{(1)_{\\cal Y}}$ Chern-Simons-Higgs theory

    CERN Document Server

    Gaete, Patricio

    2016-01-01

    By using the gauge-invariant but path-dependent, variables formalism, we consider a recently proposed topologically massive $U{\\left( 1 \\right)_{\\cal W}} \\times U{(1)_{\\cal Y}}$ Chern-Simons-Higgs theory in $2+1$ dimensions. In particular, we inspect the impact of a Chern-Simons mixing term between two Abelian gauge fields on physical observables. We pursue our investigation by analysing the model in two different situations. In the first case, where we integrate out the massive excitation and consider an effective model for the massless field, we show that the interaction energy contains a linear term leading to the confinement of static charge probes along with a screening contribution. The second situation, where the massless field can be exactly integrated over with its constraint duly taken into account, the interesting feature is that the resulting effective model describes a purely screening phase, without any trace of a confining regime.

  19. Faunal turnover in the Azraq Basin, eastern Jordan 28,000 to 9000 cal yr BP, signalling climate change and human impact

    Science.gov (United States)

    Martin, Louise; Edwards, Yvonne H.; Roe, Joe; Garrard, Andrew

    2016-09-01

    Recent zooarchaeological analyses of game exploitation in the Epipalaeolithic of the Southern Levant identify a decline in large game in the Natufian, with corresponding increase in small prey, interpreted as hunting pressure driven by population expansion. To date, studies focus on the Mediterranean zone. This paper adopts similar approaches to examine Epipalaeolithic to Neolithic faunal data from 16 sites in the steppic Jordanian Azraq Basin. Results here reveal very different trends. Large game, mainly equids, fluctuate throughout the Epipalaeolithic, due to climatic conditions and available water/vegetation. Cattle thrive in the Azraq oasis, showing no decline in the Late Epipalaeolithic. Gazelle exploitation is predominant and sustainable throughout the Epipalaeolithic, even at Kharaneh IV and Wadi Jilat 6 'megasites'. However, PPNB assemblages from the limestone steppe show intensive game exploitation resulting from longer-stay settlement. The focused gazelle-hunting camp at Dhuweila in the basalt desert also shows pressure from indiscriminate culling impacting herd demography, interpreted as providing meat for onwards exchange. Human impacts on steppe fauna appear both local and in many cases short-term, unlike the large-game suppression reported from west of the Rift Valley. Resource pressures and game over-kill, whether population-driven or otherwise, are not currently apparent east of the Jordan River.

  20. Completando el mapa de la Cuenca del Ebro: el Mesolítico del IX milenio cal BP de Espantalobos (Huesca, España

    Directory of Open Access Journals (Sweden)

    Montes, L., Domingo, R., Cuchí, J.A., Alcolea, M., Sola, C.

    2015-01-01

    Full Text Available Se presentan los resultados de la primera campaña de excavación de un nuevo yacimiento mesolítico, Espantalobos, en la Cuenca del Ebro. Localizado en las proximidades de la ciudad de Huesca, se trata de un abrigo de arenisca que conserva restos de dos ocupaciones humanas de las que la más reciente se relaciona con el Mesolítico Geométrico. Los escasos materiales del nivel más antiguo, sin embargo, no permiten de momento decidir su adscripción a esta fase o a su predecesora de Muescas y Denticulados, y tampoco su datación, bisagra entre ambas etapas. Pese al pobre estado de conservación del sitio fuertemente afectado por tareas de cantería y por la erosión, se han recuperado, además de los habituales materiales líticos, algunos restos de fauna y un interesante lote de carbones cuyo análisis antracológico permite paliar en parte la ausencia de datos de polen, que no se ha conservado.

  1. Bayesian chronological analyses consistent with synchronous age of 12,835-12,735 Cal BP for Younger Dryas boundary on four continents

    DEFF Research Database (Denmark)

    Kennett, James P.; Kennett, Douglas J.; Culleton, Brendan J.

    2015-01-01

    The Younger Dryas impact hypothesis posits that a cosmic impact across much of the Northern Hemisphere deposited the Younger Dryas boundary (YDB) layer, containing peak abundances in a variable assemblage of proxies, including magnetic and glassy impact-related spherules, high-temperature mineral...

  2. A deadly cocktail: How a drought around 4200 cal. yr BP caused mass mortality events at the infamous ‘dodo swamp’in Mauritius

    NARCIS (Netherlands)

    de Boer, E.J.; Vélez, M.I.; Rijsdijk, K.F.; de Louw, P.G.B.; Vernimmen, T.J.J.; Visser, P.M.; Tjallingii, R.; Hooghiemstra, H.

    2015-01-01

    Analyses of pollen, diatoms, XRF geochemistry, and pigments provide a unique window into how an insular ecosystem in Mauritius responded to an extreme drought event 4200 years ago. We provide a reconstruction of regional vegetation change and local wetland development under influence of sea level ri

  3. Geomagnetic Secular Variation in Texas over the Last 17,000 Years: High-Intensity Geomagnetic Field 'Spike' Observed at ca. 3000 cal BP

    Science.gov (United States)

    Bourne, M. D.; Feinberg, J. M.; Waters, M. R.; Stafford, T. W., Jr.; Forman, S. L.; Lundelius, E. L.

    2015-12-01

    By observing the fluctuations in direction and intensity of the Earth's magnetic field through time, we increase our understanding of the fluid motions in the Earth's outer core that sustain the geomagnetic field, the geodynamo. Recent archaeomagnetic studies in the Near East have proposed extremely rapid increases - 'spikes' - in geomagnetic field intensity ca. 3000 years ago that have proved problematic for our current understanding of core-flow. However, until now, these geomagnetic spikes had not been observed outside of the Near East, where they have been found in metallurgical slag and mud brick walls. We present a new fully-oriented, geomagnetic secular variation and relative palaeointensity (RPI) record for the last 17,000 years from Hall's Cave, Texas. Sediment washed into the cave has formed a continuous stratigraphic sequence that is at least 3.5 m thick. Within the stable, cool climate of the cave, pedogenic and bioturbation processes are almost non-existent, thereby limiting post-depositional physical and geochemical alteration of the magnetic record. The sub-aerial and subterranean setting of the sedimentary sequence in Hall's Cave enabled us to collect oriented palaeomagnetic cubes from an excavated section through the sequence. The palaeomagnetic samples yielded high-quality vectors. An age model for the sequence, determined using 57 AMS 14C-dates on individual bones from microvertebrate, was combined with the palaeomagnetic data to construct a secular variation record. The record is in broad agreement with predictions by Holocene field models for the site's location. However, at ca. 3000 years ago, the RPI data indicate an almost four-fold increase in geomagnetic field intensity lasting several hundred years and contemporaneous with the more short-lived, decadal-scale spikes reported from the Near East. Evidence for this extreme intensity event outside of the Near East has major implications for our current understanding of core-dynamics.

  4. A palaeolithic map from 13,660 calBP: engraved stone blocks from the Late Magdalenian in Abauntz Cave (Navarra, Spain).

    Science.gov (United States)

    Utrilla, P; Mazo, C; Sopena, M C; Martínez-Bea, M; Domingo, R

    2009-08-01

    An engraved block from the cave of Abauntz is interpreted as a Magdalenian map in which the actual surrounding landscape, including mountains, rivers, and ponds, is represented. Some possible routes or avenues of access to different parts of the geography are also engraved on the landscape. The engraving seems to reproduce the meandering course of a river crossing the upper part of side A of the block, joined by two tributaries near two mountains. One of these is identical to the mountain that can be seen from the cave, with herds of ibex depicted on its hillsides, on both sides of the gorge in front of which the cave of Abauntz is strategically located. In the southern part of the gorge, there is a completely flat area where the watercourses slow down, forming meanders and flooding in springtime. The following elements are also represented on the block: tangles of concentric strokes and bundles of lines forming very marked meanders. In short, all of these engravings could be a sketch or a simple map of the area around the cave. It could represent the plan for a coming hunt or perhaps a narrative story of one that had already happened. This paper is provided in the context of recent discussions on early modern human capacities of spatial awareness, planning, and organized hunting.

  5. the sub-Plinian Greenish Pumice eruption (19,065±105 yr cal BP) of Mount Somma - Vesuvius. Geochemical and textural constrains.

    Science.gov (United States)

    Zdanowicz, Géraldine; Boudon, Georges; Balcone-Boissard, Hélène; Cioni, Raffaello; Mundula, Filippo; Orsi, Giovanni; Civetta, Lucia

    2016-04-01

    Researches are currently focused on large intensity and stable eruptive columns as for Plinian event. But the large variability in deposits issued from sub-Plinian eruptions needs more observations, theoretical and experimental investigations to be better described and enhances criteria of classification and the knowledge on processes at the origin of this unsteadiness of various timescales. Here, we focus on the well-known example of sub-Plinian eruption exhibiting by Mount Somma-Vesuvius: the Greenish Pumice eruption (GP). On the basis of coupled geochemical and textural analyses we investigate the volatile behavior (H2O, CO2 and halogen (F, Cl)) to better constrain (1) the magma reservoir location and pre-eruptive state and (2) the sub-Plinian eruptive style through a detailed study of the degassing processes in relation with the dynamic of the eruptive column. Results evidence that Cl act as a geobarometer for the trachytic-phonolitic melt involved during the eruption indicating that magma reservoir was at 100 MPa (Cl buffer value: 5300 ±130 ppm) and wholly H2O-saturated (pre-eruptive H2O content between 3.8 and 5.2 wt%). The eruption dynamic is clearly explained by open-system degassing processes responsible of the eruptive column instability, correlated to textural heterogeneities of the eruptive products reflecting conduit heterogeneity (smaller diameter and higher horizontal gradient in magma ascent velocity).

  6. CALS and the Product State Model - Methodology and Supporting Schools and Paradigms

    DEFF Research Database (Denmark)

    Larsen, Michael Holm

    1998-01-01

    This paper address the preliminary considerations in a research project, initiated February 1997, regarding Continuous Acquisition and Life-cycle Support (CALS) which is a part of the activities in CALS Center Denmark. The CALS concept is presented focusing on the Product State Model (PSM). The PSM...... incorporates relevant information about each stage of the production process.The paper will describe the research object, the model object and discuss a part of the methodology in developing a Product State Model. The project is primarily technological, however, organisational and human aspects...... will be considered, as the intentions are that a prototype should be implemented in the production line at Odense Steel Shipyard. Hence, a Multiview approach will be considered incorporating the informational need of many actors/machines. Parameter identification, i.e. describing the parameters which PSM...

  7. L’Observatoire numérique Nouvelle-Calédonie

    Directory of Open Access Journals (Sweden)

    Charlotte Ullmann

    2013-06-01

    Full Text Available Ses missions consistent à observer le développement numérique et favoriser l’animation territoriale des acteurs en Nouvelle-Calédonie. Parrainée par l’association calédonienne pour les technologies de l’information et de la communication (ACTIC et le ministère en charge de l’économie numérique du Gouvernement de Nouvelle-Calédonie nommé depuis mai 2009, une mission d’étude a été menée depuis juin 2010 pour définir les contours d’un Observatoire numérique. A travers cette étude, il s’agissai...

  8. CalFUSE v3: A Data-Reduction Pipeline for the Far Ultraviolet Spectroscopic Explorer

    CERN Document Server

    Dixon, W V; Barrett, P E; Civeit, T; Dupuis, J; Fullerton, A W; Godard, B; Hsu, J C; Kaiser, M E; Kruk, J W; Lacour, S; Lindler, D J; Massa, D; Robinson, R D; Romelfanger, M L; Sonnentrucker, P

    2007-01-01

    Since its launch in 1999, the Far Ultraviolet Spectroscopic Explorer (FUSE) has made over 4600 observations of some 2500 individual targets. The data are reduced by the Principal Investigator team at the Johns Hopkins University and archived at the Multimission Archive at Space Telescope (MAST). The data-reduction software package, called CalFUSE, has evolved considerably over the lifetime of the mission. The entire FUSE data set has recently been reprocessed with CalFUSE v3.2, the latest version of this software. This paper describes CalFUSE v3.2, the instrument calibrations upon which it is based, and the format of the resulting calibrated data files.

  9. Anomalies, counterterms and the ${\\cal N} =0$ Polchinski-Strassler solutions

    CERN Document Server

    Taylor-Robinson, M M

    2001-01-01

    The singularity structure of many IIB supergravity solutions asymptotic to $AdS_5 \\times S^5$ becomes clearer when one considers the full ten dimensional solution rather than the dimensionally reduced solution of gauged supergravity. It has been shown that all divergences in the gravitational action of the dimensionally reduced spacetime can be removed by the addition of local counterterms on the boundary. Here we attempt to formulate the counterterm action directly in ten dimensions for a particular class of solutions, the ${\\cal N} = 0$ Polchinski-Strassler solutions, which are dual to an ${\\cal N} =4$ SYM theory perturbed by mass terms for all scalars and spinors. This involves constructing the solution perturbatively near the boundary. There is a contribution to the Weyl anomaly from the mass terms (which break the classical conformal invariance of the action). The coefficient of this anomaly is reproduced by a free field calculation indicating a non-renormalisation theorem inherited from the ${\\cal N} =4...

  10. The Framework Model of Supply-Chain Process in CALS Environment

    Institute of Scientific and Technical Information of China (English)

    2002-01-01

    E-supply chain is the trend of the supply chain ma na gement. However, building E-supply chain depends on business process improvemen t and re-engineering, which becomes one of the important aspects in supply chai n management. However, the supply chain process re-engineering and improvement is constrained because of lack of integrating operation framework and standards based on information management. We find that the idea of CALS origins from DoD of USA can solve the problems very well. CALS is the abb...

  11. QIE12: A New High-Performance ASIC for the ATLAS TileCal Upgrade

    CERN Document Server

    Drake, Gary; The ATLAS collaboration; Proudfoot, James; Stanek, Robert; Chekanov, Sergei

    2015-01-01

    We present results on the QIE12, a custom ASIC, being developed for the ATLAS TileCal Phase 2 Upgrade. The design features 1.5 fC sensitivity, more than 17 bits of dynamic range with logarithmic response, and an on-chip TDC with one nanosecond resolution. It has a programmable shunt output for monitoring the integrated current. The device operates with no dead-time at 40 MHz, making it ideal for calorimetry at the LHC. We present bench measurements and integration studies that characterize the performance, radiation tolerance measurements, and the design for the ATLAS TileCal detector for the Phase 2 Upgrade.

  12. Comportamiento de una pista experimental de pavimento flexible con base estabilizada con cal

    OpenAIRE

    Hidalgo Montoya, César Augusto; Pandales, Carlos Arturo; Pedroza Valdés, Boris Andrés; Rodríguez Moreno, Mario Alberto

    2011-01-01

    En este trabajo se presentan resultados de una investigación realizada para determinar las propiedades de deformabilidad de bases estabilizadas con cal a partir de ensayos de campo no destructivos. Se realizaron ensayos de placa estática y viga Benkelman en un tramo de prueba de pavimento flexible de 70m de longitud. Se usaron diferentes mezclas de suelo-cal y varios espesores de la estructura para evaluar el comportamiento del pavimento. A partir de los resultados de estos ensayos fuer...

  13. Altimetry, bathymetry and geoid variations at the Gavdos permanent Cal/Val facility

    DEFF Research Database (Denmark)

    Mertikas, Stelios P.; Daskalakis, Antonis; Tziavos, Ilias N.

    2013-01-01

    The aim of this work has been to examine the relationship of steep bathymetry in the coastal areas around the permanent Cal/Val facility of Gavdos, and their influence on the produced calibration values for the Jason-2 satellite altimeter. The paper describes how changes in seafloor topography...... calibration data and careful data analysis, certain features and variations, with permanent signatures at some locations south of Gavdos, have been found in the altimeter bias values. Causes of these variations have been interpreted. Some of these features, for example, at 12km south of the Cal/Val site seem...

  14. Las fuentes clásicas de Calígula de Albert Camus

    OpenAIRE

    Toledano Muñoz, Sara

    2017-01-01

    Este trabajo pretende rastrear las fuentes clásicas que aparecen en la obra Calígula de Albert Camus. Para ello, hemos recurrido a la perspectiva de la recepción, de tal manera que, en primer lugar, mostraremos los paralelos con las fuentes de las que se sirve (Suetonio y Dión Casio), para luego analizar la relectura que hace Camus de ellas, dando como resultado una visión nueva de la figura de Calígula, que trataremos de explicar partiendo de las propias reflexiones de C...

  15. Frontline CALS - Extranet Enabled Support of Customer Relations Based on Product State Information

    DEFF Research Database (Denmark)

    Larsen, Michael Holm; Franck, Lesley Robert; Pedersen, Mogens Kühn

    1999-01-01

    The electronic economy has proliferated during the past decade. Many initiatives are launched in order to support customer's interaction with the company, however, often fragmented. A more holistic approach is provided in this article. The article suggests a business model in the era of electronic...... commerce called Frontline CALS. Frontline CALS integrate three bodies of knowledge, i.e. Continuous Acquisition and Lifecycle Support, Electronic Commerce, and the Customer Consumption Chain in order to construct a concept that enhances the service quality for customers with time critical operations...

  16. The new Ford Ka: a design for the future; Der neue Ford Ka: Ein Konzept fuer die Zukunftt

    Energy Technology Data Exchange (ETDEWEB)

    Becker, K.; Bietz, T.; Castro, P.; Cole, S.; Jansen, K.H.; McColm, A.

    1996-09-01

    One of the factors of success in the competitive world of today`s automotive industry is the ability to adapt quickly to changing customer requirements. Surveys in all European countries indicate an increasing demand for cars that are below the established small cars in terms of size and price. Ford is offering with the new Ford Ka a product in the Sub-B class, which gains new ground by a fascinating design as well as matches the B-class for safety and noise comfort. The Ka is fun-to-drive with lively, safe handling to `best in class` standard at an outstanding price/performance ratio. (orig.) [Deutsch] Befragungen in ganz Europa signalisieren einen steigenden Bedarf an Fahrzeugen, die in Groesse und Preis unterhalb der etablierten Kleinwagen positioniert sind. Ford bietet mit dem neuen Ka in der Sub-B-Klasse ein Produkt, das nicht nur durch wegweisendes Design besticht, sondern gleichzeitig Fahrvergnuegen durch agiles und sicheres Handling garantiert. Der Ka bietet Sicherheit und Geraeuschkomfort auf dem Niveau der naechsthoeheren Klasse und dies bei einem guten Preis-Leistungsverhaeltnis. (orig.)

  17. The 15q11.2 BP1–BP2 Microdeletion Syndrome: A Review

    Directory of Open Access Journals (Sweden)

    Devin M. Cox

    2015-02-01

    Full Text Available Patients with the 15q11.2 BP1–BP2 microdeletion can present with developmental and language delay, neurobehavioral disturbances and psychiatric problems. Autism, seizures, schizophrenia and mild dysmorphic features are less commonly seen. The 15q11.2 BP1–BP2 microdeletion involving four genes (i.e., TUBGCP5, CYFIP1, NIPA1, NIPA2 is emerging as a recognized syndrome with a prevalence ranging from 0.57%–1.27% of patients presenting for microarray analysis which is a two to four fold increase compared with controls. Review of clinical features from about 200 individuals were grouped into five categories and included developmental (73% and speech (67% delays; dysmorphic ears (46% and palatal anomalies (46%; writing (60% and reading (57% difficulties, memory problems (60% and verbal IQ scores ≤75 (50%; general behavioral problems, unspecified (55% and abnormal brain imaging (43%. Other clinical features noted but not considered as common were seizures/epilepsy (26%, autism spectrum disorder (27%, attention deficit disorder (ADD/attention deficit hyperactivity disorder (ADHD (35%, schizophrenia/paranoid psychosis (20% and motor delay (42%. Not all individuals with the deletion are clinically affected, yet the collection of findings appear to share biological pathways and presumed genetic mechanisms. Neuropsychiatric and behavior disturbances and mild dysmorphic features are associated with genomic imbalances of the 15q11.2 BP1–BP2 region, including microdeletions, but with an apparent incomplete penetrance and variable expressivity.

  18. Mars Global Surveyor Ka-Band Frequency Data Analysis

    Science.gov (United States)

    Morabito, D.; Butman, S.; Shambayati, S.

    2000-01-01

    The Mars Global Surveyor (MGS) spacecraft, launched on November 7, 1996, carries an experimental space-to-ground telecommunications link at Ka-band (32 GHz) along with the primary X-band (8.4 GHz) downlink. The signals are simultaneously transmitted from a 1.5-in diameter parabolic high gain antenna (HGA) on MGS and received by a beam-waveguide (BWG) R&D 34-meter antenna located in NASA's Goldstone Deep Space Network (DSN) complex near Barstow, California. The projected 5-dB link advantage of Ka-band relative to X-band was confirmed in previous reports using measurements of MGS signal strength data acquired during the first two years of the link experiment from December 1996 to December 1998. Analysis of X-band and Ka-band frequency data and difference frequency (fx-fka)/3.8 data will be presented here. On board the spacecraft, a low-power sample of the X-band downlink from the transponder is upconverted to 32 GHz, the Ka-band frequency, amplified to I-W using a Solid State Power Amplifier, and radiated from the dual X/Ka HGA. The X-band signal is amplified by one of two 25 W TWTAs. An upconverter first downconverts the 8.42 GHz X-band signal to 8 GHz and then multiplies using a X4 multiplier producing the 32 GHz Ka-band frequency. The frequency source selection is performed by an RF switch which can be commanded to select a VCO (Voltage Controlled Oscillator) or USO (Ultra-Stable Oscillator) reference. The Ka-band frequency can be either coherent with the X-band downlink reference or a hybrid combination of the USO and VCO derived frequencies. The data in this study were chosen such that the Ka-band signal is purely coherent with the X-band signal, that is the downconverter is driven by the same frequency source as the X-band downlink). The ground station used to acquire the data is DSS-13, a 34-meter BWG antenna which incorporates a series of mirrors inside beam waveguide tubes which guide the energy to a subterranean pedestal room, providing a stable environment

  19. Hidrólise da cana-de-açúcar com cal virgem ou cal hidratada Hydrolysis of cane sugar with lime or hydrated lime

    Directory of Open Access Journals (Sweden)

    Diego Azevedo Mota

    2010-06-01

    Full Text Available Objetivou-se estudar o efeito do tratamento alcalino da cana-de-açúcar com cal virgem ou cal hidratada sobre a composição bromatológica e a digestibilidade in vitro da matéria seca, da fibra em detergente neutro e da fibra em detergente ácido. Utilizou-se um delineamento inteiramente casualizado em esquema fatorial 3 × 3, composto de três formas de processamento da cana (in natura; cana hidrolisada com 0,5% de cal virgem; e cana hidrolisada com 0,5% de cal hidratada e três tempos de armazenamento (12, 36 e 60 horas. As formas de processamento influenciaram os teores de matéria orgânica, matéria mineral, carboidratos totais e hemicelulose, assim como os teores de fibra em detergente neutro e nutrientes digestíveis totais. Os tempos de armazenamento influenciaram os teores de proteína bruta, matéria orgânica, carboidratos totais e hemicelulose. Entre os minerais, somente o teor de cálcio teve aumento com a inclusão de ambos os tipos de cal em relação à cana-de-açúcar, que não sofreu o processo de hidrólise. Os coeficientes de digestibilidade da matéria seca e da fibra em detergente neutro aumentaram com a hidrólise da cana em comparação à cana in natura. A hidrólise com cal hidratada ou com cal virgem mantém o valor nutricional da cana-de-açúcar, permitindo que possa ser utilizada depois de até 60 horas de armazenamento.The objective of the present work was to evaluate the effect of the alkaline treatment of sugarcane with virgin lime or hydrated lime on the bromatologic composition and in vitro digestibility of dry matter, neutral detergent fiber, and acid detergent fiber. It was used a complete random design with a 3 × 3 factorial scheme composed by three forms of of sugarcane processing (in natura sugarcane; hydrolyzed sugarcane with 0.5% virgin lime; and hydrolyzed sugarcane with 0.5% hydrated lime and three storage times (12, 36 and 60 hours. The forms of processing changed the contents of organic matter

  20. Past climate variability between 97 and 7 ka reconstructed from a multi proxy speleothem record from Western Cuba

    Science.gov (United States)

    Winterhalder, Sophie; Scholz, Denis; Mangini, Augusto; Spötl, Christoph; Jochum, Klaus Peter; Pajón, Jesús M.

    2016-04-01

    The tropical hydrological cycle plays a key role in regulating global climate, mainly through the export of heat and moisture to higher latitudes, and is highly sensitive to climate change, for instance due to changes in the position of the Intertropical Convergence Zone (ITCZ). Previous work on Caribbean stalagmites suggests a strong connection of precipitation variability to North Atlantic (NA) sea surface temperatures on multidecadal to millenial timescales (Fensterer et al., 2012; Fensterer et al., 2013; Winter et al., 2011). Cold phases in the NA potentially lead to a southward shift of the ITCZ and thus drier conditions in Cuba. On orbital timescales, Cuban stalagmites suggest a relation of speleothem δ18O values with the δ18O value of Caribbean surface waters (Fensterer et al., 2013). Here we present an expansion of the Cuban speleothem record covering the whole last glacial period from the end of MIS5c (97 ka BP) until 7 ka with hiatuses between 93-80 ka, 37-35 ka and 13-10 ka. Stalagmite Cuba medio (CM) has been precisely dated with 60 230Th/U-ages, mainly performed by the MC-ICPMS technique. The δ18O and δ13C records are completed by a continuous, high resolution LA-ICPMS trace element profile. These data allow for the first time to establish a multi-proxy climate reconstruction for the North Western Caribbean at decadal to centennial resolution for this period. The long-term variability of the δ18O values probably reflects rainfall amount in Cuba. The response to some Dansgaard/Oeschger and Heinrich stadials confirms the previously observed correlation between Caribbean and NA climate variability. However, this connection is not clearly imprinted throughout the record. Furthermore, trace elements, such as Mg, do not proof without ambiguity drier conditions in Cuba during NA cold events, such as the Heinrich stadials. This suggests that climate variability in Cuba was more complex during the last 100ka, and that the NA was not the only driving factor

  1. Hydrological variability in northern Levant over the past 250 ka

    Directory of Open Access Journals (Sweden)

    F. Gasse

    2011-05-01

    Full Text Available The Levant features sharp climatic gradients from North to South and from West to East resulting in a large environmental diversity. The lack of long-term record from the northern Levant limits our understanding of the regional response to glacial-interglacial boundary conditions in this key area. The 250 ka paleoenvironmental reconstruction presented here is a first step to fill this geographical gap.

    The record comes from a 36 m lacustrine-palustrine sequence cored in the small intra-mountainous karstic basin of Yammoûneh (northern Lebanon. The paper combines times series of sediment properties, paleovegetation, and carbonate oxygen isotopes, to yield a comprehensive view of paleohydrologic-paleoclimatic fluctuations in the basin over the two last glacial-interglacial cycles. Efficient moisture was higher than today during interglacial peaks around 240, 215–220, ~130–120 ka and 11–9 ka (although under different Precipitation minus Evaporation balance. Moderate wetting events took place around 170, 150, 105–100, 85–75, 60–55 and 35 ka. The penultimate glacial period was generally wetter than the last glacial stage. Local aridity culminated from the LGM to 15 ka, possibly linked to water storage as ice in the surrounding highlands. An overall decrease in local water availability is observed from the profile base to top. Fluctuations in available water seem to be primarily governed by changes in local summer insolation controlled by the orbital eccentricity modulated by the precession cycle, and by changes in precipitation and temperature seasonality.

    Our record is roughly consistent with long-term climatic fluctuations in northeastern Mediterranean lands, except during the penultimate glacial phase. It shares some features with speleothem records of western Israel. Conversely, after 130 ka, it is clearly out of phase with hydrological changes in the Dead Sea basin. Potential causes of these spatial heterogeneities

  2. 基于 BP 神经网络的光伏发电预测模型设计%Design of Photovoltaic Power Forecasting Model Based on BP Neutral Network

    Institute of Scientific and Technical Information of China (English)

    王思睿; 薛云灿; 李彬; 邓立华; 顾菁

    2016-01-01

    结合历史发电量和气象数据分析了影响光伏系统发电功率的各项因素,针对传统光伏发电预测模型预测精度不高的问题,加入了电池板温度信息作为光伏发电预测模型的输入参考量;针对传统 BP 神经网络易陷入局部极值的缺陷,提出了基于改进学习率和权值的弹性自适应规则的 BP 神经网络。采用光伏监控系统历史发电量和气象数据建立了弹性自适应 BP 神经网络预测模型,对训练好的模型进行了测试和评估。预测结果表明,该预测方法较好地解决了传统 BP 算法易陷入局部极值的问题,提高了系统预测结果精度。%Combined with historical power and weather data,all factors which influence the power generation of photovoltaic system are discussed,and the temperature information from the solar panels is added to the forecasting model as the reference input to solve the problems of low prediction accuracy of the traditional forecasting model.Aiming at the defects of the traditional BP neutral network into a local extreme value,this paper proposes the BP neutral network based on the improved learning rate and elastic adaptive rule.The BP neural network forecasting module of elastic adaptive method is trained by histori-cal power and weather data of photovoltaic monitoring system.The trained module is tested and evaluated.The forecasted results show that the prediction method can effectively solve problems of the traditional BP algorithm into a local extreme value and improve the system precision of forecast results.

  3. 13 kA Superconducting Busbars Manufacturing Process

    CERN Document Server

    Principe, R; Fornasiere, E

    2012-01-01

    In the LHC, the superconducting Main Bending magnets and Quadrupole magnets are series-connected electrically in different excitation circuits by means of superconducting busbars, carrying a maximum current of 13 kA. These superconducting busbars consist of a superconducting Rutherford cable thermally and electrically coupled to a copper section all along the length. The function of the copper section is essentially to provide an alternative path for the magnet current in case of resistive transition. The production of these components was originally outsourced. The decision to import the technology at CERN led to a global re-engineering of the standard process. Although based on the procedures adopted during the LHC construction, a few modifications and improvements have been implemented, profiting of the experience gained in the last few years. This document details the manufacturing process of the 13 kA busbars as it is actually performed at CERN, emphasizing the new solutions adopted during the first mon...

  4. NOVEL MLANTJARAN KA SASAK: FROM DILLEMATIC TEACHERS TO HUMOROUS ONES

    Directory of Open Access Journals (Sweden)

    I Nyoman Tingkat

    2015-07-01

    Full Text Available This article discusses the representation of the image of teachers in the novel entitled Mlantjaran ka Sasak written by Gde Srawana. Using the theory of literary sociology and the theory of representation as the basis of analysis, it was found that teachers were  imaged of being dilemmatic, humanistic idealistic, caring about the Balinese culture, and being humorous. Sociologically, the novel entitled Mlantjaran ka Sasak pictured the life background of the Balinese society during 1930s, indicated by the critical attitude of the intellectuals through I Made Sarati and Ida Ayu Priya, the characters who played a role as teachers, towards the caste feudalism in marriage. Such a critical attitude was expressed in such an inciting way that the ethic and aesthetic values needed to educate society were not neglected.

  5. An Approach to ${\\cal N}=4$ ADE Gauge Theory on K3

    CERN Document Server

    Jinzenji, M; Jinzenji, Masao; Sasaki, Toru

    2002-01-01

    We propose a recipe for determination of the partition function of ${\\cal N}=4$ $ADE$ gauge theory on $K3$ by generalizing our previous results of the SU(N) case. The resulting partition function satisfies Montonen-Olive duality for $ADE $ gauge group.

  6. Setup, tests and results for the ATLAS TileCal Read Out Driver production

    CERN Document Server

    Valero, Alberto; Castillo, V; Cuenca, C; Ferrer, A; Fullana, E; González, V; Higón, E; Munar, A; Poveda, J; Ruiz-Martínez, A; Salvachúa, B; Sanchís, E; Solans, C; Soret, J; Torres, J; Valls, J A

    2007-01-01

    In this paper we describe the performance and test results of the production of the 38 ATLAS TileCal Read Out Drivers (RODs). We first describe the basic hardware specifications and firmware functionality of the modules, the test-bench setup used for production and the test procedure to qualify the boards. We then finally show and discuss the performance results.

  7. Comparison of multi-media transport and transformation models: Regional fugacity model vs. CalTOX

    Energy Technology Data Exchange (ETDEWEB)

    Maddalena, R.L.; McKone, T.E.; Layton, D.W.; Hsieh, D.P.H. [Univ. of California, Davis, CA (United States). Dept. of Environmental Toxicology

    1994-12-31

    Two multimedia fugacity based environmental transport and transformation models are summarized and compared. The regional fugacity model published by Mackay and Paterson (1991), termed Fug3ONT, is a four compartment steady-state model designed to simulate the relative distribution of nonionic in a multimedia system. CalTOX is a seven compartment multimedia total exposure model for hazardous waste sites. Both models are based on the principles of fugacity. CalTOX, however, separates the soil into three layers and uses a new approach to estimate the diffusive mass transfer rate in soil. These differences result in lower estimates of the steady-state contaminant concentrations of six different chemicals in the root soil of CalTOX as compared to the bulk soil of Fug3ONT. The difference is greatest for compounds such as 2,3,7,8-Tetrachlorodibenzo-p-dioxin and Benzo(a)pyrene where estimates from CalTOX and Fug3ONT differ by more than 3 orders of magnitude. The models provide similar estimates, however, for the distribution of six environmentally relevant chemicals among the air, water, sediment and surface soil.

  8. Comparison of multi-media transport and transformation models: regional fugacity model vs. CalTOX.

    Science.gov (United States)

    Maddalena, R L; McKone, T E; Layton, D W; Hsieh, D P

    1995-03-01

    Two multimedia environmental transport and transformation computer models are summarized and compared. The regional fugacity model published by Mackay and Paterson (1991), termed Fug3ONT, is a four compartment steady-state model designed to simulate the relative distribution of nonionic organic chemicals in a multimedia system. CalTOX is a seven compartment multimedia total exposure model for hazardous waste sites. Both models are based on the principles of fugacity. CalTOX, however, separates the soil into three layers (surface, root, and vadose) and uses a different approach to estimate the diffusive mass transfer rate in soil. These differences result in lower estimates of the steady-state contaminant concentrations of six environmentally relevant chemicals in the root soil of CalTOX as compared to the bulk soil of Fug3ONT. The difference is greatest for compounds with low mobility in soil such as 2,3,7,8-Tetrachlorodibenzo-p-dioxin and Benzo(a)pyrene where estimates from CalTOX and Fug3ONT differ by more than 3 orders of magnitude. Otherwise, the models provide similar estimates for the distribution of the six chemicals among the air, water, sediment and surface soil.

  9. The location of cemento enamel junction for CAL measurement: A clinical crisis.

    Science.gov (United States)

    Vandana, K L; Gupta, Ira

    2009-01-01

    We face various problems while measuring the Clinical attachment level (CAL) from Cemento-enamel junction (CEJ). This study aims to record and compare the CEJ location measurements using a xed reference point (FRP) [Custom made stent] before and after ap elevation. A custom made stent and UNC-15 probe were used. Recording of CEJ location was made using a UNC-15 (Hu-Friedy) probe, before (close CEJ) and after (Open CEJ) the reflection of the flap from the lower edge of the stent in those subjects who were indicated for flap surgery, at baseline. We used statistical analysis involving intra-group comparison done by Paired-'t' test. The close and the open CEJ measurements demonstrated a, statistically, non-significant difference. The equi-measurements of close and open CEJ numerical data were remarkably lower than the under and overestimation of measurements. Thus, despite certain disadvantages of stent, the FRP provides a simple solution for CAL measurement. The results of this study confirms the objective of the study and strongly suggests that CAL measurements done without FRP is subjected to great variation and the diagnostic and prognostic interpretation of CAL should be viewed seriously in periodontics.

  10. Parallel implementation of a hyperspectral image linear SVM classifier using RVC-CAL

    Science.gov (United States)

    Madroñal, D.; Fabelo, H.; Lazcano, R.; Callicó, G. M.; Juárez, E.; Sanz, C.

    2016-10-01

    Hyperspectral Imaging (HI) collects high resolution spectral information consisting of hundreds of bands across the electromagnetic spectrum -from the ultraviolet to the infrared range-. Thanks to this huge amount of information, an identification of the different elements that compound the hyperspectral image is feasible. Initially, HI was developed for remote sensing applications and, nowadays, its use has been spread to research fields such as security and medicine. In all of them, new applications that demand the specific requirement of real-time processing have appear. In order to fulfill this requirement, the intrinsic parallelism of the algorithms needs to be explicitly exploited. In this paper, a Support Vector Machine (SVM) classifier with a linear kernel has been implemented using a dataflow language called RVC-CAL. Specifically, RVC-CAL allows the scheduling of functional actors onto the target platform cores. Once the parallelism of the classifier has been extracted, a comparison of the SVM classifier implementation using LibSVM -a specific library for SVM applications- and RVC-CAL has been performed. The speedup results obtained for the image classifier depends on the number of blocks in which the image is divided; concretely, when 3 image blocks are processed in parallel, an average speed up above 2.50, with regard to the RVC-CAL sequential version, is achieved.

  11. Nonlinear modal interactions in parity-time (${\\cal PT}$) symmetric lasers

    CERN Document Server

    Ge, Li

    2016-01-01

    Parity-time ($\\cal PT$) symmetric lasers have attracted considerable attention lately due to their promising applications and intriguing properties, such as free spectral range doubling and single-mode lasing. In this work we discuss nonlinear modal interactions in these laser systems under steady state conditions, and we demonstrate that several gain clamping scenarios can occur for lasing operation in the $\\cal PT$-symmetric and $\\cal PT$-broken phases. In particular, we show that, depending on the system's design and the external pump profile, its operation in the nonlinear regime falls into two different categories: in one the system is frozen in the $\\cal PT$ phase space as the applied gain increases, while in the other the system is pulled towards its exceptional point. These features are first illustrated by a coupled mode formalism and later verified by employing the Steady-state Ab-initio Laser Theory (SALT). Our findings shine light on the robustness of single-mode operation in these lasers against ...

  12. The Evolution and Redefining of "CAL": A Reflection on the Interplay of Theory and Practice

    Science.gov (United States)

    Hartley, R.

    2010-01-01

    This article comments on how the core idea of the computer as an assistant to teaching and learning became reconfigured through changing technologies, pedagogies and educational cultures. Early influential researchers in computer assisted learning (CAL) made strong but differing links to theories and representations of learning, showing a…

  13. Windows Calorimeter Control (WinCal) program computer software configuration management plan

    Energy Technology Data Exchange (ETDEWEB)

    NONE

    1997-03-26

    This document describes the system configuration management activities performed in support of the Windows Calorimeter Control (WinCal) system, in accordance with Site procedures based on Institute of Electrical and Electronic Engineers (IEEE) Standard 828-1990, Standard for Software Configuration Management Plans (IEEE 1990) and IEEE Standard 1042-1987, Guide to Software Configuration Management (IEEE 1987).

  14. New Fuzzy Extra Dimensions from $SU({\\cal N})$ Gauge Theories

    CERN Document Server

    Kurkcuoglu, Seckin

    2015-01-01

    We start with an $SU(\\cal {N})$ Yang-Mills theory on a manifold ${\\cal M}$, suitably coupled to two distinct set of scalar fields in the adjoint representation of $SU({\\cal N})$, which are forming a doublet and a triplet, respectively under a global $SU(2)$ symmetry. We show that a direct sum of fuzzy spheres $S_F^{2 \\, Int} := S_F^2(\\ell) \\oplus S_F^2 (\\ell) \\oplus S_F^2 \\left ( \\ell + \\frac{1}{2} \\right ) \\oplus S_F^2 \\left ( \\ell - \\frac{1}{2} \\right )$ emerges as the vacuum solution after the spontaneous breaking of the gauge symmetry and lay the way for us to interpret the spontaneously broken model as a $U(n)$ gauge theory over ${\\cal M} \\times S_F^{2 \\, Int}$. Focusing on a $U(2)$ gauge theory we present complete parameterizations of the $SU(2)$-equivariant, scalar, spinor and vector fields characterizing the effective low energy features of this model. Next, we direct our attention to the monopole bundles $S_F^{2 \\, \\pm} := S_F^2 (\\ell) \\oplus S_F^2 \\left ( \\ell \\mp \\frac{1}{2} \\right )$ over $S_F^2 (...

  15. Organic Aerosol Composition and Sources in Pasadena, California during the 2010 CalNex Campaign

    Science.gov (United States)

    Organic aerosols (OA) in Pasadena are characterized using multiple measurements from the California Research at the Nexus of Air Quality and Climate Change (CalNex) campaign. Five OA components are identified using positive matrix factorization including hydrocarbon-like OA (HOA) ...

  16. The location of cemento enamel junction for CAL measurement: A clinical crisis

    Directory of Open Access Journals (Sweden)

    Vandana K

    2009-01-01

    Full Text Available Background: We face various problems while measuring the Clinical attachment level (CAL from Cemento-enamel junction (CEJ. This study aims to record and compare the CEJ location measurements using a xed reference point (FRP [Custom made stent] before and after ap elevation. Materials and Methods: A custom made stent and UNC-15 probe were used. Recording of CEJ location was made using a UNC-15 (Hu-Friedy probe, before (close CEJ and after (Open CEJ the reflection of the flap from the lower edge of the stent in those subjects who were indicated for flap surgery, at baseline. Results: We used statistical analysis involving intra-group comparison done by Paired-′t′ test. The close and the open CEJ measurements demonstrated a, statistically, non-significant difference. The equi-measurements of close and open CEJ numerical data were remarkably lower than the under and overestimation of measurements. Thus, despite certain disadvantages of stent, the FRP provides a simple solution for CAL measurement. Conclusion: The results of this study confirms the objective of the study and strongly suggests that CAL measurements done without FRP is subjected to great variation and the diagnostic and prognostic interpretation of CAL should be viewed seriously in periodontics.

  17. A double copy for ${\\cal N}=2$ supergravity: a linearised tale told on-shell

    CERN Document Server

    Cardoso, G L; Nampuri, Suresh

    2016-01-01

    We construct the on-shell double copy for linearised four-dimensional ${\\cal N}=2$ supergravity coupled to one vector multiplet with a quadratic prepotential. We apply this dictionary to the weak-field approximation of dyonic BPS black holes in this theory.

  18. Tests with beam setup of the TileCal Phase-II upgrade electronics

    CERN Document Server

    Hlaluku, Dingane Reward; The ATLAS collaboration

    2017-01-01

    The LHC has planned a series of upgrades culminating in the High Luminosity LHC (HL-LHC) which will have an average luminosity 5-7 times larger than the nominal Run-2 value. The ATLAS Tile Calorimeter (TileCal) will undergo an upgrade to accommodate to the HL-LHC parameters. The TileCal electronics both on- and off-detector will be completely redesigned and a new readout architecture will be adopted. The photomultiplier signals will be digitised and transferred to the TileCal PreProcessors (PPr) located off-detector for every bunch crossing. Then, the PPr will provide preprocessed digital data to the first level trigger with improved spatial granularity and energy resolution with respect to the current analog trigger signals. We plan to insert one TileCal module instrumented with the new electronics in the real detector to evaluate and qualify the new readout and trigger concepts in the overall ATLAS data acquisition system. This new drawer, so-called Hybrid Demonstrator, must provide analog trigger signal fo...

  19. In silico screening of 393 mutants facilitates enzyme engineering of amidase activity in CalB

    DEFF Research Database (Denmark)

    Hediger, Martin Robert; De Vico, Luca; Rannes, Julie Bille

    2013-01-01

    Our previously presented method for high throughput computational screening of mutant activity (Hediger et al., 2012) is benchmarked against experimentally measured amidase activity for 22 mutants of Candida antarctica lipase B (CalB). Using an appropriate cutoff criterion for the computed barriers...

  20. Anatomically modern human in Southeast Asia (Laos) by 46 ka

    OpenAIRE

    Demeter, Fabrice; Shackelford, Laura L.; Bacon, Anne-Marie; Duringer, Philippe; Westaway, Kira; Sayavongkhamdy, Thongsa; Braga, José; Sichanthongtip, Phonephanh; Khamdalavong, Phimmasaeng; Ponche, Jean-Luc; wang, Hong; Lundstrom, Craig; Patole-Edoumba, Elise; Karpoff, Anne-marie

    2012-01-01

    Uncertainties surround the timing of modern human emergence and occupation in East and Southeast Asia. Although genetic and archeological data indicate a rapid migration out of Africa and into Southeast Asia by at least 60 ka, mainland Southeast Asia is notable for its absence of fossil evidence for early modern human occupation. Here we report on a modern human cranium from Tam Pa Ling, Laos, which was recovered from a secure stratigraphic context. Radiocarbon and luminescence dating of the ...

  1. Riigikogus tehakse ka tööd / Vilja Savisaar

    Index Scriptorium Estoniae

    Savisaar, Vilja, 1962-

    2007-01-01

    Ilmunud ka: Sakala, 13. juuni 2007, lk. 2; Lääne Elu, 14. juuni 2007, lk. 2; Põhjarannik, 14. juuni 2007, lk. 2; Severnoje Poberezhje, 14. juuni 2007, lk. 2; Vooremaa, 14. juuni 2007, lk. 2; Harju Ekspress, 15. juuni 2007, lk. 8; Järva Teataja, 16. juuni 2007, lk. 2; Koit, 21. juuni 2007, lk. 6. Parlamendiliige Keskerakonna fraktsiooni poolt parlamendis algatatud eelnõudest

  2. Kui suudab Steve, suudab ka Apple / Tarvo Vaarmets

    Index Scriptorium Estoniae

    Vaarmets, Tarvo

    2008-01-01

    Ehkki Apple'i kolmanda kvartali kasum kasvas kolmandiku võrra ja oli oodatust kümnendiku jagu suurem, langes ettevõtte aktsia hind börsil. Investoreid teeb rahutuks nii ettevõtte juhi Steve Jobsi tervis kui ka Apple'i majandusprognoos neljandaks kvartaliks. Lisa: Analüütikud on aktsia suhtes üksmeelel. Diagramm: Aktsia hinnal taas suund alla

  3. Euroopa Liit toetab ka väiketalupidajaid / Rein Aidma

    Index Scriptorium Estoniae

    Aidma, Rein, 1950-

    2003-01-01

    Ilmunud ka: Vali Uudised 12. nov. lk. 4, Harjumaa, Hiiu Leht, Sakala 14. nov. lk. 3,2,2, Koit 18. nov. lk. 6, Põhjarannik, Severnoje Poberezhje 21. nov. lk. 4, Järva Teataja 25. nov. lk. 2. Väiksematel põllumajandusega tegelevatel ettevõtetel on võimalus saada ajutist abi paremaks toimetulekuks võimalike muutuste korral, mis leiavad aset liitumisjärgsel perioodil

  4. Ka omavalitsus vastutab palkade eest / Aivar Õun

    Index Scriptorium Estoniae

    Õun, Aivar, 1959-

    2003-01-01

    Ilmunud ka: Nädaline, Koit 11. nov. lk.4,6, Põhjarannik, Severnoje Poberezhje, Hiiumaa, Järva Teataja 11. nov. lk. 2, Pärnu Postimees 12. nov. lk. 15, Vali Uudised 14. nov. lk. 2, Valgamaalane 18. nov. lk. 2, Vooremaa 25. nov. lk. 2. Kohalike omavalitsuste võimalustest õpetajate ja kultuuritöötajate palkade täiendavaks tõstmiseks 2004. aastal

  5. Riigikogus tehakse ka tööd / Vilja Savisaar

    Index Scriptorium Estoniae

    Savisaar, Vilja, 1962-

    2007-01-01

    Ilmunud ka: Sakala, 13. juuni 2007, lk. 2; Lääne Elu, 14. juuni 2007, lk. 2; Põhjarannik, 14. juuni 2007, lk. 2; Severnoje Poberezhje, 14. juuni 2007, lk. 2; Vooremaa, 14. juuni 2007, lk. 2; Harju Ekspress, 15. juuni 2007, lk. 8; Järva Teataja, 16. juuni 2007, lk. 2; Koit, 21. juuni 2007, lk. 6. Parlamendiliige Keskerakonna fraktsiooni poolt parlamendis algatatud eelnõudest

  6. Ka omavalitsus vastutab palkade eest / Aivar Õun

    Index Scriptorium Estoniae

    Õun, Aivar, 1959-

    2003-01-01

    Ilmunud ka: Nädaline, Koit 11. nov. lk.4,6, Põhjarannik, Severnoje Poberezhje, Hiiumaa, Järva Teataja 11. nov. lk. 2, Pärnu Postimees 12. nov. lk. 15, Vali Uudised 14. nov. lk. 2, Valgamaalane 18. nov. lk. 2, Vooremaa 25. nov. lk. 2. Kohalike omavalitsuste võimalustest õpetajate ja kultuuritöötajate palkade täiendavaks tõstmiseks 2004. aastal

  7. Eestil on Euroopas ka oma tee / Jürgen Ligi

    Index Scriptorium Estoniae

    Ligi, Jürgen, 1959-

    2004-01-01

    Ilmunud ka: Põhjarannik, 17. apr. 2004, lk. 2; Severnoje Poberezhje, 17. apr. 2004, lk. 2; Koit,17. apr. 2004, lk. 6; Meie Maa, 17. apr. 2004, lk. 2; Hiiu Leht, 20. apr. 2004, lk. 2; Virumaa Nädalaleht, 23. apr. 2004, lk. 2; Sakala, 23. apr. 2004, lk. 2; Valgamaalane, 8. mai 2004, lk. 2. Maksu- ja sotsiaalpoliitika otsustusõigusest ning kaitsmisest EL-i riikides

  8. Kui suudab Steve, suudab ka Apple / Tarvo Vaarmets

    Index Scriptorium Estoniae

    Vaarmets, Tarvo

    2008-01-01

    Ehkki Apple'i kolmanda kvartali kasum kasvas kolmandiku võrra ja oli oodatust kümnendiku jagu suurem, langes ettevõtte aktsia hind börsil. Investoreid teeb rahutuks nii ettevõtte juhi Steve Jobsi tervis kui ka Apple'i majandusprognoos neljandaks kvartaliks. Lisa: Analüütikud on aktsia suhtes üksmeelel. Diagramm: Aktsia hinnal taas suund alla

  9. Apoptosis of human tongue squamous cell carcinoma cell (CAL-27 induced by Lactobacillus sp. A-2 metabolites

    Directory of Open Access Journals (Sweden)

    Guoliang ZHANG

    2014-07-01

    Full Text Available Objective: To study the effect of Lactobacillus sp. A-2 metabolites on viability of CAL-27 cells and apoptosis in CAL-27 cells. Methods: Lactobacillus sp. A-2 metabolites 1 and 2 (LM1 and LM2 were obtained by culturing Lactobacillus sp. A-2 in reconstituted whey medium and whey-inulin medium; the cultured CAL-27 cells were treated with different concentrations of LM1 and LM2 (0, 3, 6, 12, 24, 48 mg/mL and assayed by methyl thiazolyltetrazolium (MTT method; morphological changes of apoptotic cell were observed under fluorescence microscopy by acridine orange (Ao fluorescent staining; flow cytometry method (FCM and agarose gel electrophoresis were used to detect the apoptosis of CAL-27 cells treated LM1 and LM2. Results: The different concentrations of LM1 and LM2 could restrain the growth of CAL-27 cells, and in a dose-dependent manner; the apoptosis of CAL-27 cells was obviously induced and was time-dependent. Conclusions: Viability of CAL-27 cells was inhibited by Lactobacillus sp. A-2 metabolites; Lactobacillus sp. A-2 metabolites could induce CAL-27 cells apoptosis; study on the bioactive compounds in the Lactobacillus sp. A-2 metabolites and their molecular mechanism is in progress.

  10. Precision Deployable Mast for the SWOT KaRIn Instrument Project

    Data.gov (United States)

    National Aeronautics and Space Administration — Design and prototype a lightweight, precision-deployable mast for the Ka-band Radar Interferometer (KaRIn) antennas in the Surface Water and Ocean Topography (SWOT)...

  11. Air Monitoring Data for BP Spill/Deepwater Horizon

    Data.gov (United States)

    U.S. Environmental Protection Agency — The Deepwater Horizon oil spill (also referred to as the BP oil spill) began on 20 April 2010 in the Gulf of Mexico on the BP-operated Macondo Prospect. Following...

  12. Air Sampling Data for BP Spill/Deepwater Horizon

    Data.gov (United States)

    U.S. Environmental Protection Agency — The Deepwater Horizon oil spill (also referred to as the BP oil spill) began on 20 April 2010 in the Gulf of Mexico on the BP-operated Macondo Prospect. Following...

  13. Waste Sampling Data for BP Spill/Deepwater Horizon

    Data.gov (United States)

    U.S. Environmental Protection Agency — The Deepwater Horizon oil spill (also referred to as the BP oil spill) began on 20 April 2010 in the Gulf of Mexico on the BP-operated Macondo Prospect. Following...

  14. Water Sampling Data for BP Spill/Deepwater Horizon

    Data.gov (United States)

    U.S. Environmental Protection Agency — The Deepwater Horizon oil spill (also referred to as the BP oil spill) began on 20 April 2010 in the Gulf of Mexico on the BP-operated Macondo Prospect. Following...

  15. Sediment Sampling Data for BP Spill/Deepwater Horizon

    Data.gov (United States)

    U.S. Environmental Protection Agency — The Deepwater Horizon oil spill (also referred to as the BP oil spill) began on 20 April 2010 in the Gulf of Mexico on the BP-operated Macondo Prospect. Following...

  16. Surface Water Sampling Data for BP Spill/Deepwater Horizon

    Data.gov (United States)

    U.S. Environmental Protection Agency — The Deepwater Horizon oil spill (also referred to as the BP oil spill) began on 20 April 2010 in the Gulf of Mexico on the BP-operated Macondo Prospect. Following...

  17. Use of Roud Wood in Kaingáng Houses

    Directory of Open Access Journals (Sweden)

    Ricardo Dias Silva

    2002-01-01

    Full Text Available This work has the purpose of describing and analyzing the evolutionary habitation process of the Kaingáng. Its main focus is the typological reading of the shelters as well as the registration of the wooden building system used in the construction of the houses in the “Äpucaraninha” Reserve, located in a district of Londrina. The research proceeds with the elaboration of the genealogy of the kaingáng’s habitation through the consultation to the published historical reports and their chronological organization. The data collection within the group was accomplished through informal interviews, photographic survey and in loco observations. Aspects related to the use of the round wood as well as the other elements that are part of the construction, were verified at this stage. The raw material used in every building system is obtained in the Reserve itself, being the wood used not only in the structure but also in the sealing. The connections are made through fittings and fastenings with liana. In spite of the mixture of values and meanings that the Kaingáng community experiences through the contact with other cultures, traditional aspects related to the building of the “traditional house” are preserved, with no domain of other techniques by most of the group. The registration intends to contribute towards the identification and understanding of important issues related to the spaces built by the man.

  18. Rain Fade Compensation Alternatives for Ka Band Communication Satellites

    Science.gov (United States)

    Acosta, Roberto J.

    1997-01-01

    Future satellite communications systems operating in Ka-band frequency band are subject to degradation produced by the troposphere which is much more severe than those found at lower frequency bands. These impairments include signal absorption by rain, clouds and gases, and amplitude scintillation's arising from refractive index irregularities. For example, rain attenuation at 20 GHz is almost three times that at 11 GHz. Although some of these impairments can be overcome by oversizing the ground station antennas and high power amplifiers, the current trend is using small (less than 20 inches apertures), low-cost ground stations (less than $1000) that can be easily deployed at user premises. As a consequence, most Ka-band systems are expected to employ different forms of fade mitigation that can be implemented relatively easily and at modest cost. The rain fade mitigation approaches are defined by three types of Ka-band communications systems - a low service rate (less than 1.5 Mb/s), a moderate service rate (1.5 to 6 Mb/s) system and a high service rate (greater than 43 Mb/s) system. The ACTS VSAT network, which includes an adaptive rain fade technique, is an example of a moderate service rate.

  19. ATLAS computing operations within the GridKa Cloud

    Energy Technology Data Exchange (ETDEWEB)

    Kennedy, J; Walker, R [LMU Munich (Germany); Olszewski, A [Institute of Nuclear Physics Krakow (Poland); Nderitu, S [University of Bonn (Germany); Serfon, C; Duckeck, G

    2010-04-01

    The organisation and operations model of the ATLAS T1-T2 federation/Cloud associated to the GridKa T1 in Karlsruhe is described. Attention is paid to Cloud level services and the experience gained during the last years of operation. The ATLAS GridKa Cloud is large and divers spanning 5 countries, 2 ROC's and is currently comprised of 13 core sites. A well defined and tested operations model in such a Cloud is of the utmost importance. We have defined the core Cloud services required by the ATLAS experiment and ensured that they are performed in a managed and sustainable manner. Services such as Distributed Data Management involving data replication,deletion and consistency checks, Monte Carlo Production, software installation and data reprocessing are described in greater detail. In addition to providing these central services we have undertaken several Cloud level stress tests and developed monitoring tools to aid with Cloud diagnostics. Furthermore we have defined good channels of communication between ATLAS, the T1 and the T2's and have pro-active contributions from the T2 manpower. A brief introduction to the GridKa Cloud is provided followed by a more detailed discussion of the operations model and ATLAS services within the Cloud.

  20. Utjecaj materijala za pakiranje na kvalitetu Kačkavalja

    Directory of Open Access Journals (Sweden)

    Goce Talevski

    2017-02-01

    Full Text Available U ovom radu ispitivan je utjecaj različitog ambalažnog materijala (A - kontrolni uzorak, B - polimerna emulzija, C - vosak i D - polimerna folija na kvalitetu Kačkavalja. Najnižu pH vrijednost imao je uzorak zaštićen voskom, što je rezultat zadržavanja nastalih organskih kiselina i plinova od strane ambalažnog materijala. Statistički značajan utjecaj ambalažnih materijala (p<0.01 bio je utvrđen kod sadržaja suhe tvari, proteina i pepela, dok statistička značajnost nije bila utvrđena kod sadržaja masti kod Kačkavalja. Proteolitički procesi bili su izraženiji kod uzorka zaštićenog voskom i polimernom folijom, s višim razinama topljivog dušika, primarnih i sekundarnih dušičnih spojeva i koeficijenta zrelosti u odnosu na kontrolni uzorak i uzorak zaštićen polimernom emulzijom.

  1. AltiKa: a Ka-band Altimetry Payload and System for Operational Altimetry during the GMES Period

    Science.gov (United States)

    Vincent, Patrick; Steunou, Nathalie; Caubet, Eric; Phalippou, Laurent; Rey, Laurent; Thouvenot, Eric; Verron, Jacques

    2006-01-01

    This paper describes the Ka-band altimetry payload and system that has been studied for several years by CNES, ALCATEL SPACE and some science laboratories. Altimetry is one of the major elements of the ocean observing system to be made sustainable through the GEOSS (Global Earth Observation System of Systems) and GMES (Global Monitoring of the Environment and Security) programs. A short review of some mission objectives to be fulfilled in terms of mesoscale oceanography in the frame of the GEOSS and GMES programs is performed. To answer the corresponding requirements, the approach consisting in a constellation of nadir altimeter is discussed. A coupled Ka-band altimeter-radiometer payload is then described; technical items are detailed to explain how this payload shall meet the science and operational requirements, and expected performances are displayed. The current status of the payload development and flight perspectives are given.

  2. AltiKa: a Ka-band Altimetry Payload and System for Operational Altimetry during the GMES Period

    Directory of Open Access Journals (Sweden)

    Jacques Verron

    2006-03-01

    Full Text Available This paper describes the Ka-band altimetry payload and system that has beenstudied for several years by CNES, ALCATEL SPACE and some science laboratories.Altimetry is one of the major elements of the ocean observing system to be madesustainable through the GEOSS (Global Earth Observation System of Systems and GMES(Global Monitoring of the Environment and Security programs. A short review of somemission objectives to be fulfilled in terms of mesoscale oceanography in the frame of theGEOSS and GMES programs is performed. To answer the corresponding requirements, theapproach consisting in a constellation of nadir altimeter is discussed. A coupled Ka-bandaltimeter-radiometer payload is then described; technical items are detailed to explain howthis payload shall meet the science and operational requirements, and expectedperformances are displayed. The current status of the payload development and flightperspectives are given.

  3. AcEST: BP917073 [AcEST

    Lifescience Database Archive (English)

    Full Text Available YMU001_000095_E10 67 Adiantum capillus-veneris mRNA. clone: YMU001_000095_E10. BP917073 - Show BP91707... mRNA. clone: YMU001_000095_E10. Accession BP917073 Tissue type prothallium Developmental stage - Contig ID

  4. AcEST: BP919848 [AcEST

    Lifescience Database Archive (English)

    Full Text Available YMU001_000129_H02 84 Adiantum capillus-veneris mRNA. clone: YMU001_000129_H02. BP919848 - Show BP91984... mRNA. clone: YMU001_000129_H02. Accession BP919848 Tissue type prothallium Developmental stage - Contig ID

  5. AcEST: BP912001 [AcEST

    Lifescience Database Archive (English)

    Full Text Available YMU001_000011_H05 68 Adiantum capillus-veneris mRNA. clone: YMU001_000011_H05. BP912001 - Show BP9120... mRNA. clone: YMU001_000011_H05. Accession BP912001 Tissue type prothallium Developmental stage - Contig ID

  6. AcEST: BP920096 [AcEST

    Lifescience Database Archive (English)

    Full Text Available YMU001_000132_H11 24 Adiantum capillus-veneris mRNA. clone: YMU001_000132_H11. BP920096 - Show BP9200... mRNA. clone: YMU001_000132_H11. Accession BP920096 Tissue type prothallium Developmental stage - Contig ID

  7. AcEST: BP915983 [AcEST

    Lifescience Database Archive (English)

    Full Text Available YMU001_000081_D10 68 Adiantum capillus-veneris mRNA. clone: YMU001_000081_D10. BP915983 - Show BP9159... mRNA. clone: YMU001_000081_D10. Accession BP915983 Tissue type prothallium Developmental stage - Contig ID

  8. AcEST: BP915976 [AcEST

    Lifescience Database Archive (English)

    Full Text Available YMU001_000081_C10 41 Adiantum capillus-veneris mRNA. clone: YMU001_000081_C10. BP915976 - Show BP9159... mRNA. clone: YMU001_000081_C10. Accession BP915976 Tissue type prothallium Developmental stage - Contig ID

  9. AcEST: BP915990 [AcEST

    Lifescience Database Archive (English)

    Full Text Available YMU001_000081_E12 98 Adiantum capillus-veneris mRNA. clone: YMU001_000081_E12. BP915990 - Show BP9159... mRNA. clone: YMU001_000081_E12. Accession BP915990 Tissue type prothallium Developmental stage - Contig ID

  10. AcEST: BP915963 [AcEST

    Lifescience Database Archive (English)

    Full Text Available YMU001_000081_B02 67 Adiantum capillus-veneris mRNA. clone: YMU001_000081_B02. BP915963 - Show BP9159... mRNA. clone: YMU001_000081_B02. Accession BP915963 Tissue type prothallium Developmental stage - Contig ID

  11. AcEST: BP915998 [AcEST

    Lifescience Database Archive (English)

    Full Text Available YMU001_000081_F12 46 Adiantum capillus-veneris mRNA. clone: YMU001_000081_F12. BP915998 - Show BP9159... mRNA. clone: YMU001_000081_F12. Accession BP915998 Tissue type prothallium Developmental stage - Contig ID

  12. AcEST: BP915935 [AcEST

    Lifescience Database Archive (English)

    Full Text Available YMU001_000079_F11 64 Adiantum capillus-veneris mRNA. clone: YMU001_000079_F11. BP915935 - Show BP9159... mRNA. clone: YMU001_000079_F11. Accession BP915935 Tissue type prothallium Developmental stage - Contig ID

  13. AcEST: BP911835 [AcEST

    Lifescience Database Archive (English)

    Full Text Available YMU001_000009_G02 27 Adiantum capillus-veneris mRNA. clone: YMU001_000009_G02. BP911835 - Show BP91183... mRNA. clone: YMU001_000009_G02. Accession BP911835 Tissue type prothallium Developmental stage - Contig ID

  14. AcEST: BP911839 [AcEST

    Lifescience Database Archive (English)

    Full Text Available YMU001_000009_G06 76 Adiantum capillus-veneris mRNA. clone: YMU001_000009_G06. BP911839 - Show BP91183... mRNA. clone: YMU001_000009_G06. Accession BP911839 Tissue type prothallium Developmental stage - Contig ID

  15. AcEST: BP919947 [AcEST

    Lifescience Database Archive (English)

    Full Text Available YMU001_000131_A11 35 Adiantum capillus-veneris mRNA. clone: YMU001_000131_A11. BP919947 - Show BP91994... mRNA. clone: YMU001_000131_A11. Accession BP919947 Tissue type prothallium Developmental stage - Contig ID

  16. AcEST: BP915006 [AcEST

    Lifescience Database Archive (English)

    Full Text Available YMU001_000065_D07 96 Adiantum capillus-veneris mRNA. clone: YMU001_000065_D07. BP915006 - Show BP91500... mRNA. clone: YMU001_000065_D07. Accession BP915006 Tissue type prothallium Developmental stage - Contig ID

  17. AcEST: BP920020 [AcEST

    Lifescience Database Archive (English)

    Full Text Available YMU001_000132_B05 91 Adiantum capillus-veneris mRNA. clone: YMU001_000132_B05. BP920020 - Show BP920020... mRNA. clone: YMU001_000132_B05. Accession BP920020 Tissue type prothallium Developmental stage - Contig ID

  18. AcEST: BP915916 [AcEST

    Lifescience Database Archive (English)

    Full Text Available YMU001_000079_D12 73 Adiantum capillus-veneris mRNA. clone: YMU001_000079_D12. BP915916 - Show BP91591... mRNA. clone: YMU001_000079_D12. Accession BP915916 Tissue type prothallium Developmental stage - Contig ID

  19. Study on the Characters of the Geochemical Elements and Changes of Paleoclimate since about 4 000 a B.P. in Niya Section%南疆尼雅地区4 000 a来的地化元素分布特征 与古气候环境演化的初步研究

    Institute of Scientific and Technical Information of China (English)

    舒强; 钟巍; 熊黑钢; 塔西甫拉提; 高村宏毅

    2001-01-01

    通过应用因子分析法对尼雅剖面中的多种地化元素和氧化物的分析,在R、Q型因子分析的基础上,提取出古气候信息。初步的研究表明:近4 000 a来,尼雅地区气候环境仍以干旱化为主,但此期间出现过多次不同程度的干湿变化,大致可分为5个气候期:4.0~3.0 ka B.P.相对暖干期;3.0~2.2 ka B.P. 相对冷湿期;2.2~1.6 ka B.P. 相对暖干期;1.6~1.0 ka B.P. 相对冷湿期;1.0 ka B.P.左右之后的相对暖干期。%Niya relics lie in south Xinjiang, north of Kunlun Mountains and in south edge of Taklimakan desert, 100 km north away from county town. It was the important post of south route of ancient “Silk Road”. In the article, we select about 300 cm natural profile on the right bank of Niya river, collect 22 samples, and analyze them with radiocarbon 14C dating and X fluorescent spectrum analysis of geochemical elements. By applying the factor analyzing method to deal with various geochemical elements and oxides in section of Niya, the results of Q-type factors and R-type factors are obtained, which we use as a proxy to extract the information of paleoclimate and resume the features of paleoclimate in Niya. Since 4 000 a B.P., climate in Niya region has a trend of drought, although the area of Niya has experienced alternations of relative cold-moisture and warm-dry period. The pattern of paleoclimatic evolution of this area not only has its regional characters and coincides with that of others areas in Xinjiang, but also corresponds to the global climatic changes. During the period, the history of paleoclimatic changes is reconstructed as follows:   (1) 4.0~3.0 ka B.P., it was dry in climate mainly, although several little cold-moisture and warm-dry fluctuation appeared, showing no difference with the results obtained in Aibi Lake in north Xinjiang (that is, in 6.4~3.5 ka B.P.,drier in climate and fluctuating frequently). In 3.5 ka B.P., a warm peak

  20. Deficiency in Either 4E-BP1 or 4E-BP2 Augments Innate Antiviral Immune Responses

    Science.gov (United States)

    Nehdi, Atef; Sean, Polen; Linares, Izzar; Colina, Rodney; Jaramillo, Maritza; Alain, Tommy

    2014-01-01

    Genetic deletion of both 4E-BP1 and 4E-BP2 was found to protect cells against viral infections. Here we demonstrate that the individual loss of either 4E-BP1 or 4E-BP2 in mouse embryonic fibroblasts (MEFs) is sufficient to confer viral resistance. shRNA-mediated silencing of 4E-BP1 or 4E-BP2 renders MEFs resistant to viruses, and compared to wild type cells, MEFs knockout for either 4E-BP1 or 4E-BP2 exhibit enhanced translation of Irf-7 and consequently increased innate immune response to viruses. Accordingly, the replication of vesicular stomatitis virus, encephalomyocarditis virus, influenza virus and Sindbis virus is markedly suppressed in these cells. Importantly, expression of either 4E-BP1 or 4E-BP2 in double knockout or respective single knockout cells diminishes their resistance to viral infection. Our data show that loss of 4E-BP1 or 4E-BP2 potentiates innate antiviral immunity. These results provide further evidence for translational control of innate immunity and support targeting translational effectors as an antiviral strategy. PMID:25531441

  1. AcEST: BP912479 [AcEST

    Lifescience Database Archive (English)

    Full Text Available YMU001_000019_H10 595 Adiantum capillus-veneris mRNA. clone: YMU001_000019_H10. BP912479 - Show BP91247...is mRNA. clone: YMU001_000019_H10. Accession BP912479 Tissue type prothallium Developmental stage - Contig I...T and PSI-BLAST: a new generation of protein database search programs, Nucleic Acids Res. 25:3389-3402. Query= BP91247...PSVNQRCLGG 325 + + + E+ KVPSV + G Sbjct: 2452 STTFVSD---RSLEKHPKVPSVEAVTVNG 2477 ...h programs, Nucleic Acids Res. 25:3389-3402. Query= BP912479|Adiantum capillus-veneris mRNA, clone: YMU001_0

  2. AcEST: BP912472 [AcEST

    Lifescience Database Archive (English)

    Full Text Available YMU001_000019_H03 369 Adiantum capillus-veneris mRNA. clone: YMU001_000019_H03. BP912472 - Show BP91247...is mRNA. clone: YMU001_000019_H03. Accession BP912472 Tissue type prothallium Developmental stage - Contig I...abase search programs, Nucleic Acids Res. 25:3389-3402. Query= BP912472|Adiantum capillus-veneris mRNA, clon...ams, Nucleic Acids Res. 25:3389-3402. Query= BP912472|Adiantum capillus-veneris mRNA, clone: YMU001_000019_H

  3. AcEST: BP912470 [AcEST

    Lifescience Database Archive (English)

    Full Text Available YMU001_000019_H01 466 Adiantum capillus-veneris mRNA. clone: YMU001_000019_H01. BP91247...0 CL266Contig1 Show BP912470 Clone id YMU001_000019_H01 Library YMU01 Length 466 Definition Adiantum cap...illus-veneris mRNA. clone: YMU001_000019_H01. Accession BP912470 Tissue type prothallium Developmental stage...programs, Nucleic Acids Res. 25:3389-3402. Query= BP912470|Adiantum capillus-vene... BLAST and PSI-BLAST: a new generation of protein database search programs, Nucleic Acids Res. 25:3389-3402. Query= BP91247

  4. AcEST: BP921247 [AcEST

    Lifescience Database Archive (English)

    Full Text Available YMU001_000147_D10 328 Adiantum capillus-veneris mRNA. clone: YMU001_000147_D10. BP921247... CL2844Contig1 Show BP921247 Clone id YMU001_000147_D10 Library YMU01 Length 328 Definition Adiantum ca...pillus-veneris mRNA. clone: YMU001_000147_D10. Accession BP921247 Tissue type prothallium Developmental stag...25:3389-3402. Query= BP921247|Adiantum capillus-veneris mRNA, clone: YMU001_000147_D10. (311 letters) Databa...generation of protein database search programs, Nucleic Acids Res. 25:3389-3402. Query= BP921247|Adiantum ca

  5. AcEST: BP912471 [AcEST

    Lifescience Database Archive (English)

    Full Text Available YMU001_000019_H02 517 Adiantum capillus-veneris mRNA. clone: YMU001_000019_H02. BP912471 - Show BP91247...is mRNA. clone: YMU001_000019_H02. Accession BP912471 Tissue type prothallium Developmental stage - Contig I... of protein database search programs, Nucleic Acids Res. 25:3389-3402. Query= BP91247...(34%), Positives = 38/78 (48%), Gaps = 6/78 (7%) Frame = -1 Query: 247 KDNAITDDSLKRFESQQKN-IFDWFRKKGAPEA---V...ase search programs, Nucleic Acids Res. 25:3389-3402. Query= BP912471|Adiantum ca

  6. AcEST: BP913247 [AcEST

    Lifescience Database Archive (English)

    Full Text Available YMU001_000028_B06 567 Adiantum capillus-veneris mRNA. clone: YMU001_000028_B06. BP913247 - Show BP913247...is mRNA. clone: YMU001_000028_B06. Accession BP913247 Tissue type prothallium Developmental stage - Contig I...se search programs, Nucleic Acids Res. 25:3389-3402. Query= BP913247|Adiantum capillus-veneris mRNA, clone: ...ucleic Acids Res. 25:3389-3402. Query= BP913247|Adiantum capillus-veneris mRNA, c

  7. AcEST: BP912474 [AcEST

    Lifescience Database Archive (English)

    Full Text Available YMU001_000019_H05 367 Adiantum capillus-veneris mRNA. clone: YMU001_000019_H05. BP91247...4 CL2087Contig1 Show BP912474 Clone id YMU001_000019_H05 Library YMU01 Length 367 Definition Adiantum ca...pillus-veneris mRNA. clone: YMU001_000019_H05. Accession BP912474 Tissue type prothallium Developmental stag... generation of protein database search programs, Nucleic Acids Res. 25:3389-3402. Query= BP912474|Adiantum c...eration of protein database search programs, Nucleic Acids Res. 25:3389-3402. Query= BP912474|Adiantum capil

  8. AcEST: BP920247 [AcEST

    Lifescience Database Archive (English)

    Full Text Available YMU001_000134_G05 431 Adiantum capillus-veneris mRNA. clone: YMU001_000134_G05. BP920247 - Show BP920247...is mRNA. clone: YMU001_000134_G05. Accession BP920247 Tissue type prothallium Developmental stage - Contig I...AST and PSI-BLAST: a new generation of protein database search programs, Nucleic Acids Res. 25:3389-3402. Query= BP920247...ped BLAST and PSI-BLAST: a new generation of protein database search programs, Nucleic Acids Res. 25:3389-3402. Query= BP920247

  9. AcEST: BP918247 [AcEST

    Lifescience Database Archive (English)

    Full Text Available YMU001_000111_C03 349 Adiantum capillus-veneris mRNA. clone: YMU001_000111_C03. BP918247 - Show BP918247...is mRNA. clone: YMU001_000111_C03. Accession BP918247 Tissue type prothallium Developmental stage - Contig I... Nucleic Acids Res. 25:3389-3402. Query= BP918247|Adiantum capillus-veneris mRNA, clone: YMU001_000111_C03. ...I-BLAST: a new generation of protein database search programs, Nucleic Acids Res. 25:3389-3402. Query= BP918247

  10. AcEST: BP912247 [AcEST

    Lifescience Database Archive (English)

    Full Text Available YMU001_000016_G11 467 Adiantum capillus-veneris mRNA. clone: YMU001_000016_G11. BP912247 - Show BP912247...is mRNA. clone: YMU001_000016_G11. Accession BP912247 Tissue type prothallium Developmental stage - Contig I...f protein database search programs, Nucleic Acids Res. 25:3389-3402. Query= BP912247...ein database search programs, Nucleic Acids Res. 25:3389-3402. Query= BP912247|Adiantum capillus-veneris mRN

  11. AcEST: BP915247 [AcEST

    Lifescience Database Archive (English)

    Full Text Available YMU001_000069_C06 538 Adiantum capillus-veneris mRNA. clone: YMU001_000069_C06. BP915247... CL4212Contig1 Show BP915247 Clone id YMU001_000069_C06 Library YMU01 Length 538 Definition Adiantum ca...pillus-veneris mRNA. clone: YMU001_000069_C06. Accession BP915247 Tissue type prothallium Developmental stag...otein database search programs, Nucleic Acids Res. 25:3389-3402. Query= BP915247|Adiantum capillus-veneris m... PSI-BLAST: a new generation of protein database search programs, Nucleic Acids Res. 25:3389-3402. Query= BP915247

  12. AcEST: BP919684 [AcEST

    Lifescience Database Archive (English)

    Full Text Available YMU001_000127_H09 516 Adiantum capillus-veneris mRNA. clone: YMU001_000127_H09. BP919684 - Show BP91968...is mRNA. clone: YMU001_000127_H09. Accession BP919684 Tissue type prothallium Developmental stage - Contig I...rotein database search programs, Nucleic Acids Res. 25:3389-3402. Query= BP919684...BLAST and PSI-BLAST: a new generation of protein database search programs, Nucleic Acids Res. 25:3389-3402. Query= BP91968

  13. AcEST: BP919685 [AcEST

    Lifescience Database Archive (English)

    Full Text Available YMU001_000127_H10 544 Adiantum capillus-veneris mRNA. clone: YMU001_000127_H10. BP919685 - Show BP91968...is mRNA. clone: YMU001_000127_H10. Accession BP919685 Tissue type prothallium Developmental stage - Contig I... Res. 25:3389-3402. Query= BP919685|Adiantum capillus-veneris mRNA, clone: YMU001_000127_H10. (544 letters) ...eneration of protein database search programs, Nucleic Acids Res. 25:3389-3402. Query= BP91968

  14. AcEST: BP919687 [AcEST

    Lifescience Database Archive (English)

    Full Text Available YMU001_000128_A01 517 Adiantum capillus-veneris mRNA. clone: YMU001_000128_A01. BP919687 - Show BP91968...is mRNA. clone: YMU001_000128_A01. Accession BP919687 Tissue type prothallium Developmental stage - Contig I...AST: a new generation of protein database search programs, Nucleic Acids Res. 25:3389-3402. Query= BP91968...PSI-BLAST: a new generation of protein database search programs, Nucleic Acids Res. 25:3389-3402. Query= BP91968

  15. AcEST: BP919681 [AcEST

    Lifescience Database Archive (English)

    Full Text Available YMU001_000127_H06 556 Adiantum capillus-veneris mRNA. clone: YMU001_000127_H06. BP919681 - Show BP91968...is mRNA. clone: YMU001_000127_H06. Accession BP919681 Tissue type prothallium Developmental stage - Contig I...otein database search programs, Nucleic Acids Res. 25:3389-3402. Query= BP919681|Adiantum capillus-veneris m...ucleic Acids Res. 25:3389-3402. Query= BP919681|Adiantum capillus-veneris mRNA, clone: YMU001_000127_H06. (5

  16. AcEST: BP919683 [AcEST

    Lifescience Database Archive (English)

    Full Text Available YMU001_000127_H08 545 Adiantum capillus-veneris mRNA. clone: YMU001_000127_H08. BP919683 - Show BP91968...is mRNA. clone: YMU001_000127_H08. Accession BP919683 Tissue type prothallium Developmental stage - Contig I...Acids Res. 25:3389-3402. Query= BP919683|Adiantum capillus-veneris mRNA, clone: YMU001_000127_H08. (545 lett... protein database search programs, Nucleic Acids Res. 25:3389-3402. Query= BP919683|Adiantum capillus-veneri

  17. AcEST: BP912209 [AcEST

    Lifescience Database Archive (English)

    Full Text Available YMU001_000016_D06 540 Adiantum capillus-veneris mRNA. clone: YMU001_000016_D06. BP912209 - Show BP91220...is mRNA. clone: YMU001_000016_D06. Accession BP912209 Tissue type prothallium Developmental stage - Contig I...protein database search programs, Nucleic Acids Res. 25:3389-3402. Query= BP912209|Adiantum capillus-veneris... programs, Nucleic Acids Res. 25:3389-3402. Query= BP912209|Adiantum capillus-veneris mRNA, clone: YMU001_00

  18. AcEST: BP919858 [AcEST

    Lifescience Database Archive (English)

    Full Text Available YMU001_000130_A04 328 Adiantum capillus-veneris mRNA. clone: YMU001_000130_A04. BP919858 - Show BP91985...is mRNA. clone: YMU001_000130_A04. Accession BP919858 Tissue type prothallium Developmental stage - Contig I...AST and PSI-BLAST: a new generation of protein database search programs, Nucleic Acids Res. 25:3389-3402. Query= BP91985...ation of protein database search programs, Nucleic Acids Res. 25:3389-3402. Query= BP919858|Adiantum capillu

  19. AcEST: BP919857 [AcEST

    Lifescience Database Archive (English)

    Full Text Available YMU001_000130_A03 501 Adiantum capillus-veneris mRNA. clone: YMU001_000130_A03. BP91985...7 CL3173Contig1 Show BP919857 Clone id YMU001_000130_A03 Library YMU01 Length 501 Definition Adiantum ca...pillus-veneris mRNA. clone: YMU001_000130_A03. Accession BP919857 Tissue type prothallium Developmental stag...eration of protein database search programs, Nucleic Acids Res. 25:3389-3402. Query= BP91985...T: a new generation of protein database search programs, Nucleic Acids Res. 25:3389-3402. Query= BP919857|Ad

  20. AcEST: BP919852 [AcEST

    Lifescience Database Archive (English)

    Full Text Available YMU001_000129_H07 499 Adiantum capillus-veneris mRNA. clone: YMU001_000129_H07. BP919852 - Show BP91985...is mRNA. clone: YMU001_000129_H07. Accession BP919852 Tissue type prothallium Developmental stage - Contig I..., Nucleic Acids Res. 25:3389-3402. Query= BP919852|Adiantum capillus-veneris mRNA...tabase search programs, Nucleic Acids Res. 25:3389-3402. Query= BP919852|Adiantum capillus-veneris mRNA, clo

  1. AcEST: BP911985 [AcEST

    Lifescience Database Archive (English)

    Full Text Available YMU001_000011_F08 421 Adiantum capillus-veneris mRNA. clone: YMU001_000011_F08. BP911985 - Show BP911985...is mRNA. clone: YMU001_000011_F08. Accession BP911985 Tissue type prothallium Developmental stage - Contig I...7), Gapped BLAST and PSI-BLAST: a new generation of protein database search programs, Nucleic Acids Res. 25:3389-3402. Query= BP91198...rams, Nucleic Acids Res. 25:3389-3402. Query= BP911985|Adiantum capillus-veneris

  2. AcEST: BP917474 [AcEST

    Lifescience Database Archive (English)

    Full Text Available YMU001_000101_C07 287 Adiantum capillus-veneris mRNA. clone: YMU001_000101_C07. BP917474... CL2332Contig1 Show BP917474 Clone id YMU001_000101_C07 Library YMU01 Length 287 Definition Adiantum ca...pillus-veneris mRNA. clone: YMU001_000101_C07. Accession BP917474 Tissue type prothallium Developmental stag...eration of protein database search programs, Nucleic Acids Res. 25:3389-3402. Query= BP917474|Adiantum capil...ch programs, Nucleic Acids Res. 25:3389-3402. Query= BP917474|Adiantum capillus-veneris mRNA, clone: YMU001_

  3. AcEST: BP921003 [AcEST

    Lifescience Database Archive (English)

    Full Text Available YMU001_000144_D08 457 Adiantum capillus-veneris mRNA. clone: YMU001_000144_D08. BP92100...3 CL1992Contig1 Show BP921003 Clone id YMU001_000144_D08 Library YMU01 Length 457 Definition Adiantum ca...pillus-veneris mRNA. clone: YMU001_000144_D08. Accession BP921003 Tissue type prothallium Developmental stag...ds Res. 25:3389-3402. Query= BP921003|Adiantum capillus-veneris mRNA, clone: YMU0...f protein database search programs, Nucleic Acids Res. 25:3389-3402. Query= BP921003|Adiantum capillus-vener

  4. AcEST: BP921008 [AcEST

    Lifescience Database Archive (English)

    Full Text Available YMU001_000144_E02 477 Adiantum capillus-veneris mRNA. clone: YMU001_000144_E02. BP921008 - Show BP92100...is mRNA. clone: YMU001_000144_E02. Accession BP921008 Tissue type prothallium Developmental stage - Contig I...c Acids Res. 25:3389-3402. Query= BP921008|Adiantum capillus-veneris mRNA, clone:...ion of protein database search programs, Nucleic Acids Res. 25:3389-3402. Query= BP921008|Adiantum capillus-

  5. AcEST: BP921007 [AcEST

    Lifescience Database Archive (English)

    Full Text Available YMU001_000144_E01 460 Adiantum capillus-veneris mRNA. clone: YMU001_000144_E01. BP92100...7 CL57Contig1 Show BP921007 Clone id YMU001_000144_E01 Library YMU01 Length 460 Definition Adiantum capi...llus-veneris mRNA. clone: YMU001_000144_E01. Accession BP921007 Tissue type prothallium Developmental stage ...search programs, Nucleic Acids Res. 25:3389-3402. Query= BP921007|Adiantum capill... protein database search programs, Nucleic Acids Res. 25:3389-3402. Query= BP921007|Adiantum capillus-veneri

  6. AcEST: BP916167 [AcEST

    Lifescience Database Archive (English)

    Full Text Available YMU001_000084_A11 268 Adiantum capillus-veneris mRNA. clone: YMU001_000084_A11. BP916167 - Show BP91616...is mRNA. clone: YMU001_000084_A11. Accession BP916167 Tissue type prothallium Developmental stage - Contig I... database search programs, Nucleic Acids Res. 25:3389-3402. Query= BP916167|Adiantum capillus-veneris mRNA, ...ds Res. 25:3389-3402. Query= BP916167|Adiantum capillus-veneris mRNA, clone: YMU001_000084_A11. (253 letters

  7. AcEST: BP911616 [AcEST

    Lifescience Database Archive (English)

    Full Text Available YMU001_000007_B05 303 Adiantum capillus-veneris mRNA. clone: YMU001_000007_B05. BP911616 - Show BP911616...is mRNA. clone: YMU001_000007_B05. Accession BP911616 Tissue type prothallium Developmental stage - Contig I...ion of protein database search programs, Nucleic Acids Res. 25:3389-3402. Query= BP911616|Adiantum capillus-... and PSI-BLAST: a new generation of protein database search programs, Nucleic Acids Res. 25:3389-3402. Query= BP911616...132 PE=4 SV=1 Length = 278 Score = 69.7 bits (169), Expect = 7e-11 Identities = 2

  8. AcEST: BP920305 [AcEST

    Lifescience Database Archive (English)

    Full Text Available YMU001_000135_E03 413 Adiantum capillus-veneris mRNA. clone: YMU001_000135_E03. BP920305 - Show BP92030...is mRNA. clone: YMU001_000135_E03. Accession BP920305 Tissue type prothallium Developmental stage - Contig I...rotein database search programs, Nucleic Acids Res. 25:3389-3402. Query= BP920305|Adiantum capillus-veneris ... new generation of protein database search programs, Nucleic Acids Res. 25:3389-3402. Query= BP920305|Adiant

  9. AcEST: BP920306 [AcEST

    Lifescience Database Archive (English)

    Full Text Available YMU001_000135_E04 480 Adiantum capillus-veneris mRNA. clone: YMU001_000135_E04. BP920306 - Show BP92030...is mRNA. clone: YMU001_000135_E04. Accession BP920306 Tissue type prothallium Developmental stage - Contig I...n of protein database search programs, Nucleic Acids Res. 25:3389-3402. Query= BP92030...ST and PSI-BLAST: a new generation of protein database search programs, Nucleic Acids Res. 25:3389-3402. Query= BP92030

  10. AcEST: BP920303 [AcEST

    Lifescience Database Archive (English)

    Full Text Available YMU001_000135_E01 493 Adiantum capillus-veneris mRNA. clone: YMU001_000135_E01. BP920303 - Show BP92030...is mRNA. clone: YMU001_000135_E01. Accession BP920303 Tissue type prothallium Developmental stage - Contig I...f protein database search programs, Nucleic Acids Res. 25:3389-3402. Query= BP92030...ion of protein database search programs, Nucleic Acids Res. 25:3389-3402. Query= BP920303|Adiantum capillus-

  11. AcEST: BP920307 [AcEST

    Lifescience Database Archive (English)

    Full Text Available YMU001_000135_E05 493 Adiantum capillus-veneris mRNA. clone: YMU001_000135_E05. BP920307 - Show BP92030...is mRNA. clone: YMU001_000135_E05. Accession BP920307 Tissue type prothallium Developmental stage - Contig I...arch programs, Nucleic Acids Res. 25:3389-3402. Query= BP920307|Adiantum capillus...-BLAST: a new generation of protein database search programs, Nucleic Acids Res. 25:3389-3402. Query= BP92030

  12. AcEST: BP920309 [AcEST

    Lifescience Database Archive (English)

    Full Text Available YMU001_000135_E07 488 Adiantum capillus-veneris mRNA. clone: YMU001_000135_E07. BP920309 - Show BP92030...is mRNA. clone: YMU001_000135_E07. Accession BP920309 Tissue type prothallium Developmental stage - Contig I...tabase search programs, Nucleic Acids Res. 25:3389-3402. Query= BP920309|Adiantum... a new generation of protein database search programs, Nucleic Acids Res. 25:3389-3402. Query= BP920309|Adia

  13. AcEST: BP914147 [AcEST

    Lifescience Database Archive (English)

    Full Text Available YMU001_000042_D12 534 Adiantum capillus-veneris mRNA. clone: YMU001_000042_D12. BP914147 - Show BP91414...is mRNA. clone: YMU001_000042_D12. Accession BP914147 Tissue type prothallium Developmental stage - Contig I...T: a new generation of protein database search programs, Nucleic Acids Res. 25:3389-3402. Query= BP91414...niprot_sprot.fasta 412,525 sequences; 148,809,765 total letters Searching......................................ids Res. 25:3389-3402. Query= BP914147|Adiantum capillus-veneris mRNA, clone: YMU001_000042_D12. (534 letter

  14. AcEST: BP917072 [AcEST

    Lifescience Database Archive (English)

    Full Text Available YMU001_000095_E09 516 Adiantum capillus-veneris mRNA. clone: YMU001_000095_E09. BP917072 - Show BP91707...is mRNA. clone: YMU001_000095_E09. Accession BP917072 Tissue type prothallium Developmental stage - Contig I... Acids Res. 25:3389-3402. Query= BP917072|Adiantum capillus-veneris mRNA, clone: YMU001_000095_E09. (516 let...LAST and PSI-BLAST: a new generation of protein database search programs, Nucleic Acids Res. 25:3389-3402. Query= BP91707

  15. AcEST: BP917078 [AcEST

    Lifescience Database Archive (English)

    Full Text Available YMU001_000095_F03 438 Adiantum capillus-veneris mRNA. clone: YMU001_000095_F03. BP91707...8 CL4266Contig1 Show BP917078 Clone id YMU001_000095_F03 Library YMU01 Length 438 Definition Adiantum ca...pillus-veneris mRNA. clone: YMU001_000095_F03. Accession BP917078 Tissue type prothallium Developmental stag...Gapped BLAST and PSI-BLAST: a new generation of protein database search programs, Nucleic Acids Res. 25:3389-3402. Query= BP91707...programs, Nucleic Acids Res. 25:3389-3402. Query= BP917078|Adiantum capillus-vene

  16. AcEST: BP917071 [AcEST

    Lifescience Database Archive (English)

    Full Text Available YMU001_000095_E08 525 Adiantum capillus-veneris mRNA. clone: YMU001_000095_E08. BP917071 - Show BP91707...is mRNA. clone: YMU001_000095_E08. Accession BP917071 Tissue type prothallium Developmental stage - Contig I...ew generation of protein database search programs, Nucleic Acids Res. 25:3389-3402. Query= BP91707...earch programs, Nucleic Acids Res. 25:3389-3402. Query= BP917071|Adiantum capillus-veneris mRNA, clone: YMU0

  17. AcEST: BP917077 [AcEST

    Lifescience Database Archive (English)

    Full Text Available YMU001_000095_F02 487 Adiantum capillus-veneris mRNA. clone: YMU001_000095_F02. BP91707...7 CL10Contig1 Show BP917077 Clone id YMU001_000095_F02 Library YMU01 Length 487 Definition Adiantum capi...llus-veneris mRNA. clone: YMU001_000095_F02. Accession BP917077 Tissue type prothallium Developmental stage ... protein database search programs, Nucleic Acids Res. 25:3389-3402. Query= BP91707...AST: a new generation of protein database search programs, Nucleic Acids Res. 25:3389-3402. Query= BP917077|

  18. AcEST: BP917074 [AcEST

    Lifescience Database Archive (English)

    Full Text Available YMU001_000095_E11 418 Adiantum capillus-veneris mRNA. clone: YMU001_000095_E11. BP91707...4 CL413Contig1 Show BP917074 Clone id YMU001_000095_E11 Library YMU01 Length 418 Definition Adiantum cap...illus-veneris mRNA. clone: YMU001_000095_E11. Accession BP917074 Tissue type prothallium Developmental stage...w generation of protein database search programs, Nucleic Acids Res. 25:3389-3402. Query= BP917074|Adiantum ...ograms, Nucleic Acids Res. 25:3389-3402. Query= BP917074|Adiantum capillus-veneri

  19. AcEST: BP917070 [AcEST

    Lifescience Database Archive (English)

    Full Text Available YMU001_000095_E07 451 Adiantum capillus-veneris mRNA. clone: YMU001_000095_E07. BP917070 - Show BP91707...is mRNA. clone: YMU001_000095_E07. Accession BP917070 Tissue type prothallium Developmental stage - Contig I...Gapped BLAST and PSI-BLAST: a new generation of protein database search programs, Nucleic Acids Res. 25:3389-3402. Query= BP91707...s. 25:3389-3402. Query= BP917070|Adiantum capillus-veneris mRNA, clone: YMU001_000095_E07. (451 letters) Dat

  20. AcEST: BP920002 [AcEST

    Lifescience Database Archive (English)

    Full Text Available YMU001_000131_G12 513 Adiantum capillus-veneris mRNA. clone: YMU001_000131_G12. BP92000...2 CL642Contig1 Show BP920002 Clone id YMU001_000131_G12 Library YMU01 Length 513 Definition Adiantum cap...illus-veneris mRNA. clone: YMU001_000131_G12. Accession BP920002 Tissue type prothallium Developmental stage...on of protein database search programs, Nucleic Acids Res. 25:3389-3402. Query= BP92000...new generation of protein database search programs, Nucleic Acids Res. 25:3389-3402. Query= BP920002|Adiantu