<?xml version="1.0" encoding="UTF-8"?>
<xml>
  <records>
    <record>
      <source-app name="Horizon">Horizon</source-app>
      <rec-number>1</rec-number>
      <foreign-keys>
        <key app="Horizon" db-id="fdi:010077125">1</key>
      </foreign-keys>
      <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%">Lu, Y. Y.</style>
          </author>
          <author>
            <style face="normal" font="default" size="100%">Wen, Z. Z.</style>
          </author>
          <author>
            <style face="normal" font="default" size="100%">Shi, D. L.</style>
          </author>
          <author>
            <style face="normal" font="default" size="100%">Lin, W. F.</style>
          </author>
          <author>
            <style face="bold" font="default" size="100%">Bonnet, Sophie</style>
          </author>
          <author>
            <style face="normal" font="default" size="100%">Dai, M. H.</style>
          </author>
          <author>
            <style face="normal" font="default" size="100%">Kao, S. J.</style>
          </author>
        </authors>
      </contributors>
      <titles>
        <title>Biogeography of N-2 fixation influenced by the western boundary current intrusion in the South China Sea</title>
        <secondary-title>Journal of Geophysical Research : Oceans</secondary-title>
      </titles>
      <pages>6983-6996</pages>
      <keywords>
        <keyword>MER DE CHINE</keyword>
      </keywords>
      <dates>
        <year>2019</year>
      </dates>
      <call-num>fdi:010077125</call-num>
      <language>ENG</language>
      <periodical>
        <full-title>Journal of Geophysical Research : Oceans</full-title>
      </periodical>
      <isbn>2169-9275</isbn>
      <accession-num>ISI:000491809800001</accession-num>
      <number>10</number>
      <electronic-resource-num>10.1029/2018jc014781</electronic-resource-num>
      <urls>
        <related-urls>
          <url>https://www.documentation.ird.fr/hor/fdi:010077125</url>
        </related-urls>
        <pdf-urls>
          <url>https://www.documentation.ird.fr/intranet/publi/depot/2020-02-04/010077125.pdf</url>
        </pdf-urls>
      </urls>
      <volume>124</volume>
      <remote-database-provider>Horizon (IRD)</remote-database-provider>
      <abstract>The N-2 fixation and primary production rates were measured simultaneously using N-15(2) and C-13 incubation assays in the northern South China Sea influenced by the Kuroshio intrusion (KI) seasonally. The degree of KI (KI index, range from 0 to 1) was assessed by applying an isopycnal mixing model. The water column integrated N-2 fixation and primary production for stations with KI index larger than 0.5 were 463 +/- 260 mu mol N center dot m(-2)center dot day(-1) and 62 +/- 19 mmol C center dot m(-2)center dot day(-1), respectively, significantly higher than those for stations with KI index lower than 0.5 (50 +/- 10 mu mol N center dot m(-2)center dot day(-1) and 28 +/- 10 mmol C center dot m(-2)center dot day(-1), respectively). Trichodesmium was the dominant diazotroph at stations with KI index larger than 0.5, with 2 orders of magnitude higher nifH gene abundance than that at stations with KI index lower than 0.5. However, the highest N-2 fixation rates were found in waters with moderate KI index around 0.6, suggesting that frontal zone mixing might stimulate N-2 fixation. Our results demonstrated that diazotrophs (mainly Trichodesmium) were tightly associated with the KI, which modulated the biogeographic distribution of N-2 fixers. In summary, we found the transportation of Trichodesmium by KI, then, we quantified the fraction of KI and N-2 fixation rates in the northern South China Sea. The results suggested that KI generated a new biogeographic regime which could significantly influence the carbon and nitrogen cycles far away from the main stream.</abstract>
      <custom6>032 ; 034</custom6>
      <custom1>UR235</custom1>
      <custom7>Chine</custom7>
    </record>
  </records>
</xml>
