<?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>Hydroclimatic variability record from the Cabo Frio coast (Rio de Janeiro, Brazil) during the last 6500 yr</dc:title>
  <dc:creator>/Laslandes, B&#xE9;rang&#xE8;re</dc:creator>
  <dc:creator>/Sylvestre, Florence</dc:creator>
  <dc:creator>/Sifeddine, Abdelfettah</dc:creator>
  <dc:creator>/Turcq, Bruno</dc:creator>
  <dc:creator>Albuquerque, A.L.S.</dc:creator>
  <dc:creator>Abrao, J.</dc:creator>
  <dc:subject>holocene</dc:subject>
  <dc:subject>Brazilian coast</dc:subject>
  <dc:subject>sedimentology</dc:subject>
  <dc:subject>isotopes</dc:subject>
  <dc:subject>diatoms</dc:subject>
  <dc:subject>palaeoclimate</dc:subject>
  <dc:subject>El Nino</dc:subject>
  <dc:description>This study concerns a core collected in Brejo do Espinho's lagoon from Cabo Frio littoral (Brazil) submitted to dry influence of local upwelling controlled by north-cast trade winds from the South Atlantic and particularly strengthened during El Nino events. Diatoms study supported by sedimentological and isotopic analyses shows dry phases infrequent before 4000 yr, a highly variable climatic phase between 3600 and 2900 yr and from 2400 yr onward a dryness enhancement.</dc:description>
  <dc:date>2006</dc:date>
  <dc:type>text</dc:type>
  <dc:identifier>https://www.documentation.ird.fr/hor/fdi:010035756</dc:identifier>
  <dc:identifier>fdi:010035756</dc:identifier>
  <dc:identifier>Laslandes B&#xE9;rang&#xE8;re, Sylvestre Florence, Sifeddine Abdelfettah, Turcq Bruno, Albuquerque A.L.S., Abrao J.. Hydroclimatic variability record from the Cabo Frio coast (Rio de Janeiro, Brazil) during the last 6500 yr. 2006, 338 (10),  667-675</dc:identifier>
  <dc:language>EN</dc:language>
</oai_dc:dc>
