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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%">Waeles, M.</style>
          </author>
          <author>
            <style face="normal" font="default" size="100%">Maguer, J. F.</style>
          </author>
          <author>
            <style face="bold" font="default" size="100%">Baurand, François</style>
          </author>
          <author>
            <style face="normal" font="default" size="100%">Riso, R. D.</style>
          </author>
        </authors>
      </contributors>
      <titles>
        <title>Off Congo waters (Angola Basin, Atlantic Ocean) : a hot spot for cadmium-phosphate fractionation</title>
        <secondary-title>Limnology and Oceanography</secondary-title>
      </titles>
      <pages>1481-1490</pages>
      <keywords>
        <keyword>OCEAN ATLANTIQUE</keyword>
        <keyword>ANGOLA BASSIN</keyword>
      </keywords>
      <dates>
        <year>2013</year>
      </dates>
      <call-num>fdi:010060621</call-num>
      <language>ENG</language>
      <periodical>
        <full-title>Limnology and Oceanography</full-title>
      </periodical>
      <isbn>0024-3590</isbn>
      <accession-num>ISI:000322514600026</accession-num>
      <number>4</number>
      <electronic-resource-num>10.4319/lo.2013.58.4.1481</electronic-resource-num>
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          <url>https://www.documentation.ird.fr/hor/fdi:010060621</url>
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      <volume>58</volume>
      <remote-database-provider>Horizon (IRD)</remote-database-provider>
      <abstract>We report the distribution of cadmium at 13 stations along 5.83 degrees S in the Angola Basin. The studied area (which is influenced by the plume of the Congo River, doming, and relatively high primary production) is characterized by relatively low-circulation regime, which results in a strong oxygen minimum. In subsurface, very low cadmium : phosphate (Cd : P) ratios (0.05-0.10 nmol L-1 : mu mol L-1) were observed below the euphotic zone (depth range = 50-200 m), indicating that mineralization is the main process explaining the Cd-P fractionation. Cd-P decoupling is not restricted to subsurface waters, but occurs also throughout the oxygen minimum zone. An isopycnal analysis of the Cd : P ratio throughout the Atlantic Ocean shows that upper and intermediate waters in the South-east Atlantic are highly altered in terms of Cd-P properties. Benthic inputs at 4000 m were associated with degradation of organic matter with an important siliceous component, but were not accompanied by substantial changes in the Cd : P ratio.</abstract>
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