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      <source-app name="Horizon">Horizon</source-app>
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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%">Dekaezemacker, J.</style>
          </author>
          <author>
            <style face="bold" font="default" size="100%">Bonnet, Sophie</style>
          </author>
          <author>
            <style face="normal" font="default" size="100%">Grosso, O.</style>
          </author>
          <author>
            <style face="normal" font="default" size="100%">Moutin, T.</style>
          </author>
          <author>
            <style face="normal" font="default" size="100%">Bressac, M.</style>
          </author>
          <author>
            <style face="normal" font="default" size="100%">Capone, D.G.</style>
          </author>
        </authors>
      </contributors>
      <titles>
        <title>Evidence of active dinitrogen fixation in surface waters of the eastern tropical South Pacific during El Niño and La Niña events and evaluation of its potential nutrient controls</title>
        <secondary-title>Global Biogeochemical Cycles</secondary-title>
      </titles>
      <pages>768-779</pages>
      <keywords>
        <keyword>MILIEU MARIN</keyword>
        <keyword>EAU DE SURFACE</keyword>
        <keyword>EL NINO</keyword>
        <keyword>FIXATION BIOLOGIQUE DE L'AZOTE</keyword>
        <keyword>PRODUCTION PRIMAIRE</keyword>
        <keyword>FACTEUR LIMITANT</keyword>
        <keyword>CHLOROPHYLLE</keyword>
        <keyword>NUTRIMENT</keyword>
        <keyword>OXYGENE</keyword>
        <keyword>OLIGOTROPHIE</keyword>
        <keyword>LA NINA</keyword>
        <keyword>N2 fixation</keyword>
        <keyword>ETSP</keyword>
        <keyword>oligotrophic</keyword>
        <keyword>HNLC</keyword>
        <keyword>oxygen minimum zones</keyword>
        <keyword>nutrient</keyword>
        <keyword>limitation</keyword>
        <keyword>ZONE TROPICALE</keyword>
        <keyword>PACIFIQUE SUD</keyword>
      </keywords>
      <dates>
        <year>2013</year>
      </dates>
      <call-num>fdi:010061267</call-num>
      <language>ENG</language>
      <periodical>
        <full-title>Global Biogeochemical Cycles</full-title>
      </periodical>
      <isbn>0886-6236</isbn>
      <accession-num>ISI:000325488600014</accession-num>
      <number>3</number>
      <electronic-resource-num>10.1002/gbc.20063</electronic-resource-num>
      <urls>
        <related-urls>
          <url>https://www.documentation.ird.fr/hor/fdi:010061267</url>
        </related-urls>
        <pdf-urls>
          <url>https://www.documentation.ird.fr/intranet/publi/2013/11/010061267.pdf</url>
        </pdf-urls>
      </urls>
      <volume>27</volume>
      <remote-database-provider>Horizon (IRD)</remote-database-provider>
      <abstract>Biological N-2 fixation rates were quantified in the Eastern Tropical South Pacific (ETSP) during both El Nino (February 2010) and La Nina (March-April 2011) conditions, and from Low-Nutrient, Low-Chlorophyll (20 degrees S) to High-Nutrient, Low-Chlorophyll (HNLC) (10 degrees S) conditions. N-2 fixation was detected at all stations with rates ranging from 0.01 to 0.88nmolNL(-1) d(-1), with higher rates measured during El Nino conditions compared to La Nina. High N-2 fixations rates were reported at northern stations (HNLC conditions) at the oxycline and in the oxygen minimum zone (OMZ), despite nitrate concentrations up to 30 mu molL(-1), indicating that inputs of new N can occur in parallel with N loss processes in OMZs. Water-column integrated N-2 fixation rates ranged from 4 to 53 mu molNm(-2) d(-1) at northern stations, and from 0 to 148 mu molm(-2) d(-1) at southern stations, which are of the same order of magnitude as N-2 fixation rates measured in the oligotrophic ocean. N-2 fixation rates responded significantly to Fe and organic carbon additions in the surface HNLC waters, and surprisingly by concomitant Fe and N additions in surface waters at the edge of the subtropical gyre. Recent studies have highlighted the predominance of heterotrophic diazotrophs in this area, and we hypothesize that N-2 fixation could be directly limited by inorganic nutrient availability, or indirectly through the stimulation of primary production and the subsequent excretion of dissolved organic matter and/or the formation of micro-environments favorable for heterotrophic N-2 fixation.</abstract>
      <custom6>032MILPHY</custom6>
      <custom1>UR235</custom1>
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