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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="bold" font="default" size="100%">Bonnet, Sophie</style>
          </author>
          <author>
            <style face="normal" font="default" size="100%">Dekaezemacker, J.</style>
          </author>
          <author>
            <style face="normal" font="default" size="100%">Turk-Kubo, K. A.</style>
          </author>
          <author>
            <style face="normal" font="default" size="100%">Moutin, T.</style>
          </author>
          <author>
            <style face="normal" font="default" size="100%">Hamersley, R.M.</style>
          </author>
          <author>
            <style face="normal" font="default" size="100%">Grosso, O.</style>
          </author>
          <author>
            <style face="normal" font="default" size="100%">Zehr, J.P.</style>
          </author>
          <author>
            <style face="normal" font="default" size="100%">Capone, D.G.</style>
          </author>
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      <titles>
        <title>Aphotic N-2 fixation in the Eastern Tropical South Pacific Ocean</title>
        <secondary-title>Plos One</secondary-title>
      </titles>
      <pages>e81265 [14 ]</pages>
      <keywords>
        <keyword>MILIEU MARIN</keyword>
        <keyword>EL NINO</keyword>
        <keyword>COUCHE EUPHOTIQUE</keyword>
        <keyword>FIXATION BIOLOGIQUE DE L'AZOTE</keyword>
        <keyword>OXYGENE</keyword>
        <keyword>MICROORGANISME</keyword>
        <keyword>ANALYSE QUANTITATIVE</keyword>
        <keyword>PROFIL VERTICAL</keyword>
        <keyword>PROFONDEUR</keyword>
        <keyword>LA NINA</keyword>
        <keyword>COUCHE APHOTIQUE</keyword>
        <keyword>OMZ.OXYGENE MINIMUM ZONE</keyword>
        <keyword>ZONE TROPICALE</keyword>
        <keyword>PACIFIQUE SUD</keyword>
      </keywords>
      <dates>
        <year>2013</year>
      </dates>
      <call-num>fdi:010061449</call-num>
      <language>ENG</language>
      <periodical>
        <full-title>Plos One</full-title>
      </periodical>
      <isbn>1932-6203</isbn>
      <accession-num>ISI:000328731800014</accession-num>
      <number>12</number>
      <electronic-resource-num>10.1371/journal.pone.0081265</electronic-resource-num>
      <urls>
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          <url>https://www.documentation.ird.fr/hor/fdi:010061449</url>
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          <url>https://horizon.documentation.ird.fr/exl-doc/pleins_textes/divers17-10/010061449.pdf</url>
        </pdf-urls>
      </urls>
      <volume>8</volume>
      <remote-database-provider>Horizon (IRD)</remote-database-provider>
      <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>
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      <custom1>UR235</custom1>
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