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      <title>Aphotic N-2 fixation in the Eastern Tropical South Pacific Ocean</title>
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    <abstract>We examined rates of N-2 fixation from the surface to 2000 m depth in the Eastern Tropical South Pacific (ETSP) during El Niño (2010) and La Niña (2011). Replicated vertical profiles performed under oxygen-free conditions show that N-2 fixation takes place both in euphotic and aphotic waters, with rates reaching 155 to 509 mu mol N m(-2) d(-1) in 2010 and 24 +/- 14 to 118 +/- 87 mu mol N m(-2) d(-1) in 2011. In the aphotic layers, volumetric N-2 fixation rates were relatively low (&lt; 1.00 nmol N L-1 d(-1)), but when integrated over the whole aphotic layer, they accounted for 87-90% of total rates (euphotic+ aphotic) for the two cruises. Phylogenetic studies performed in microcosms experiments confirm the presence of diazotrophs in the deep waters of the Oxygen Minimum Zone (OMZ), which were comprised of non-cyanobacterial diazotrophs affiliated with nifH clusters 1K (predominantly comprised of alpha-proteobacteria), 1G (predominantly comprised of gamma-proteobacteria), and 3 (sulfate reducing genera of the delta-proteobacteria and Clostridium spp., Vibrio spp.). Organic and inorganic nutrient addition bioassays revealed that amino acids significantly stimulated N-2 fixation in the core of the OMZ at all stations tested and as did simple carbohydrates at stations located nearest the coast of Peru/Chile. The episodic supply of these substrates from upper layers are hypothesized to explain the observed variability of N-2 fixation in the ETSP.</abstract>
    <targetAudience authority="marctarget">specialized</targetAudience>
    <subject authority="local">
      <topic>MILIEU MARIN</topic>
      <topic>EL NINO</topic>
      <topic>COUCHE EUPHOTIQUE</topic>
      <topic>FIXATION BIOLOGIQUE DE L'AZOTE</topic>
      <topic>OXYGENE</topic>
      <topic>MICROORGANISME</topic>
      <topic>ANALYSE QUANTITATIVE</topic>
      <topic>PROFIL VERTICAL</topic>
      <topic>PROFONDEUR</topic>
    </subject>
    <subject>
      <topic>LA NINA</topic>
      <topic>COUCHE APHOTIQUE</topic>
      <topic>OMZ.OXYGENE MINIMUM ZONE</topic>
    </subject>
    <subject authority="local">
      <geographic>ZONE TROPICALE</geographic>
    </subject>
    <classification authority="local">032MILPHY</classification>
    <classification authority="local">034MIORG</classification>
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      <titleInfo>
        <title>Plos One</title>
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      <part>
        <detail type="volume">
          <number>8</number>
        </detail>
        <detail type="volume">
          <number>12</number>
        </detail>
        <extent unit="pages">
          <list>e81265 [14 ]</list>
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      </part>
      <originInfo>
        <dateIssued>2013</dateIssued>
      </originInfo>
      <identifier type="issn">1932-6203</identifier>
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    <identifier type="uri">https://www.documentation.ird.fr/hor/fdi:010061449</identifier>
    <identifier type="doi">10.1371/journal.pone.0081265</identifier>
    <identifier type="issn">1932-6203</identifier>
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      <recordCreationDate encoding="w3cdtf">2014-03-03</recordCreationDate>
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