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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%">Aumont, Olivier</style>
          </author>
          <author>
            <style face="normal" font="default" size="100%">Bopp, L.</style>
          </author>
        </authors>
      </contributors>
      <titles>
        <title>Globalizing results from ocean in situ iron fertilization studies</title>
        <secondary-title>Global Biogeochemical Cycles</secondary-title>
      </titles>
      <pages>art. no. GB2017 - NIL_32-NIL_46</pages>
      <keywords>
        <keyword>MONDE</keyword>
      </keywords>
      <dates>
        <year>2006</year>
      </dates>
      <call-num>PAR00001000</call-num>
      <language>ENG</language>
      <periodical>
        <full-title>Global Biogeochemical Cycles</full-title>
      </periodical>
      <isbn>0886-6236</isbn>
      <accession-num>CC:0002385702-0002</accession-num>
      <number>2</number>
      <electronic-resource-num>10.1029/2005GB002591</electronic-resource-num>
      <urls>
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          <url>https://www.documentation.ird.fr/hor/PAR00001000</url>
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          <url>https://horizon.documentation.ird.fr/exl-doc/pleins_textes/divers20-09/010078685.pdf</url>
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      <volume>20</volume>
      <remote-database-provider>Horizon (IRD)</remote-database-provider>
      <abstract>Despite the growing number of in situ iron fertilization experiments, the efficiency of such fertilization to sequester atmospheric CO2 remains largely unknown. For the first time, a global ocean biogeochemical model has been evaluated against those experiments and then used to estimate the effect of a long-term and large-scale iron addition on atmospheric CO2. The model reproduces the observed timing and amplitude in chlorophyll, the shift in ecosystem composition, and the pCO(2) drawdown; it also proves to be of utility in interpreting the observations. However, a full ocean fertilization during 100 years results in a 33 mu atm decrease in atmospheric CO2, that is 2 to 3 times smaller than found previously.</abstract>
      <custom6>032 ; 066 ; 064</custom6>
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