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      <rec-number>1</rec-number>
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      <ref-type name="Journal Article">17</ref-type>
      <work-type>ACL : Articles dans des revues avec comité de lecture répertoriées par l'AERES</work-type>
      <contributors>
        <authors>
          <author>
            <style face="normal" font="default" size="100%">Fersi, W.</style>
          </author>
          <author>
            <style face="normal" font="default" size="100%">Bassinot, F.</style>
          </author>
          <author>
            <style face="normal" font="default" size="100%">Lezine, Anne-Marie</style>
          </author>
        </authors>
      </contributors>
      <titles>
        <title>Past productivity variations and organic carbon burial in the Gulf of Aden since the last glacial maximum</title>
        <secondary-title>Quaternaire</secondary-title>
      </titles>
      <pages>213-226</pages>
      <keywords>
        <keyword>Gulf of Aden</keyword>
        <keyword>dinoflagellate cysts</keyword>
        <keyword>productivity</keyword>
        <keyword>organic carbon</keyword>
        <keyword>monsoon</keyword>
        <keyword>ADEN GOLFE</keyword>
        <keyword>OMAN</keyword>
      </keywords>
      <dates>
        <year>2016</year>
      </dates>
      <call-num>PAR00015364</call-num>
      <language>ENG</language>
      <periodical>
        <full-title>Quaternaire</full-title>
      </periodical>
      <isbn>1142-2904</isbn>
      <accession-num>ISI:000388370700003</accession-num>
      <number>3</number>
      <urls>
        <related-urls>
          <url>https://www.documentation.ird.fr/hor/PAR00015364</url>
        </related-urls>
      </urls>
      <volume>27</volume>
      <remote-database-provider>Horizon (IRD)</remote-database-provider>
      <abstract>We reconstructed the evolution of marine primary productivity across the last deglaciation in the Gulf of Aden based on micro-paleontological and sedimentological data from marine core MD92-1002. Dinoflagellate cysts analysis suggests that the glacial period was characterized by weakened upwellings and well ventilated bottom water. Primary productivity increased from 14.5 ka with a maximum between 12.6 and 10.8 ka, then declined during the Holocene. Maximum of primary productivity in the Gulf of Aden took place about 3 ka earlier than the maximum of upwelling intensity off the Oman margin, and was not phase-locked with the maximum of boreal summer insolation. XRF-derived bromine contents mimic the variations of Total Organic Carbon (TOC) in core MD92-1002. Both records show a strong glacial/interglacial signal that is largely decoupled from our reconstruction of surface productivity, suggesting that total organic content in core MD92-1002 is mainly controlled by preservation at the sea floor.</abstract>
      <custom6>064 ; 021 ; 036</custom6>
      <custom1>UR182</custom1>
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