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    <titleInfo>
      <title>Off Congo waters (Angola Basin, Atlantic Ocean) : a hot spot for cadmium-phosphate fractionation</title>
    </titleInfo>
    <name type="personnal">
      <namePart type="family">Waeles</namePart>
      <namePart type="given">M.</namePart>
      <role>
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    <name type="personnal">
      <namePart type="family">Maguer</namePart>
      <namePart type="given">J. F.</namePart>
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    <name type="personnal">
      <namePart type="family">Baurand</namePart>
      <namePart type="given">François</namePart>
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    <name type="personnal">
      <namePart type="family">Riso</namePart>
      <namePart type="given">R. D.</namePart>
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    <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>
    <targetAudience authority="marctarget">specialized</targetAudience>
    <subject authority="local">
      <geographic>OCEAN ATLANTIQUE</geographic>
      <geographic>ANGOLA BASSIN</geographic>
    </subject>
    <classification authority="local">032</classification>
    <relatedItem type="host">
      <titleInfo>
        <title>Limnology and Oceanography</title>
      </titleInfo>
      <part>
        <detail type="volume">
          <number>58</number>
        </detail>
        <detail type="volume">
          <number>4</number>
        </detail>
        <extent unit="pages">
          <list> 1481-1490</list>
        </extent>
      </part>
      <originInfo>
        <dateIssued>2013</dateIssued>
      </originInfo>
      <identifier type="issn">0024-3590</identifier>
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    <identifier type="uri">https://www.documentation.ird.fr/hor/fdi:010060621</identifier>
    <identifier type="doi">10.4319/lo.2013.58.4.1481</identifier>
    <identifier type="issn">0024-3590</identifier>
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      <url usage="primary display" access="object in context">https://www.documentation.ird.fr/hor/fdi:010060621</url>
      <url access="row object">https://www.documentation.ird.fr/intranet/publi/2013/09/010060621.pdf</url>
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      <recordCreationDate encoding="w3cdtf">2013-10-02</recordCreationDate>
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      <recordIdentifier>fdi:010060621</recordIdentifier>
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        <languageTerm authority="iso639-2b">fre</languageTerm>
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