<?xml version="1.0"?>
<oai_dc:dc xmlns:oai_dc="http://www.openarchives.org/OAI/2.0/oai_dc/" xmlns:dc="http://purl.org/dc/elements/1.1/" xmlns:xsi="http://www.w3.org/2001/XMLSchema-instance" xsi:schemaLocation="http://www.openarchives.org/OAI/2.0/oai_dc/ http://www.openarchives.org/OAI/2.0/oai_dc.xsd">
  <dc:title>Paleohydrological changes during the last deglaciation in Northern Brazil</dc:title>
  <dc:creator>Jacob, J.</dc:creator>
  <dc:creator>Huang, Y. S.</dc:creator>
  <dc:creator>Disnar, J. R.</dc:creator>
  <dc:creator>/Sifeddine, Abdelfettah</dc:creator>
  <dc:creator>Boussafir, M.</dc:creator>
  <dc:creator>Albuquerque, A. L. S.</dc:creator>
  <dc:creator>/Turcq, Bruno</dc:creator>
  <dc:description>We here report a reconstruction of hydrological balance variations in Northern Brazil for the last 20 ka deduced from the delta D values of aquatic and land plant molecules extracted from the sediment infill of Lake Caco. Our reconstructed precipitation, lake water isotope ratio and evaporation-evapotranspiration isotope effect allows us to obtain an estimate of moisture balance, and, to a lesser extent, precipitation amount and seasonality changes. During the end of the Last Glacial Maximum (LGM, between ca 20 and 17.3 ka), high delta D values and smaller fractionation of leaf waxes indicate an and to semi-arid climate with a long lasting dry season. An abrupt change towards much wetter conditions occurred within ca 500 years from 17.3 to 16.8 ka, as shown by a 50 parts per thousand decrease in D/H ratios and a marked increase in H isotopic fractionation of leaf waxes. This abrupt isotopic change coincides with a major transformation from savanna-dominated vegetation to humid rain forest around the lake, based on pollen data. Comparisons with other paleo-precipitation records from South American sites indicate that Lateglacial humid conditions were controlled by intensification of the ITCZ and/or a southward shift of its mean position across our study site. Our isotope data show only a small rise in aridity during Younger Dryas event (13-11.5 ka). Although the Holocene was not screened in details, D/H ratios of terrestrial and aquatic compounds show near constant offsets, suggesting stable and relatively humid climate conditions during this period.</dc:description>
  <dc:date>2007</dc:date>
  <dc:type>text</dc:type>
  <dc:identifier>https://www.documentation.ird.fr/hor/fdi:010040777</dc:identifier>
  <dc:identifier>fdi:010040777</dc:identifier>
  <dc:identifier>Jacob J., Huang Y. S., Disnar J. R., Sifeddine Abdelfettah, Boussafir M., Albuquerque A. L. S., Turcq Bruno. Paleohydrological changes during the last deglaciation in Northern Brazil. 2007, 26 (7-8),  1004-1015</dc:identifier>
  <dc:language>EN</dc:language>
  <dc:coverage>BRESIL</dc:coverage>
  <dc:coverage>AMAZONIE</dc:coverage>
</oai_dc:dc>
