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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%">Mortillaro, J. M.</style>
          </author>
          <author>
            <style face="normal" font="default" size="100%">Passarelli, C.</style>
          </author>
          <author>
            <style face="bold" font="default" size="100%">Abril, Gwenaël</style>
          </author>
          <author>
            <style face="normal" font="default" size="100%">Hubas, C.</style>
          </author>
          <author>
            <style face="normal" font="default" size="100%">Alberic, P.</style>
          </author>
          <author>
            <style face="normal" font="default" size="100%">Artigas, L. F.</style>
          </author>
          <author>
            <style face="normal" font="default" size="100%">Benedetti, M. F.</style>
          </author>
          <author>
            <style face="normal" font="default" size="100%">Thiney, N.</style>
          </author>
          <author>
            <style face="bold" font="default" size="100%">Moreira Turcq, Patricia</style>
          </author>
          <author>
            <style face="normal" font="default" size="100%">Perez, M. A. P.</style>
          </author>
          <author>
            <style face="normal" font="default" size="100%">Vidal, L. O.</style>
          </author>
          <author>
            <style face="normal" font="default" size="100%">Meziane, T.</style>
          </author>
        </authors>
      </contributors>
      <titles>
        <title>The fate of C-4 and C-3 macrophyte carbon in central Amazon floodplain waters : insights from a batch experiment</title>
        <secondary-title>Limnologica</secondary-title>
      </titles>
      <pages>90-98</pages>
      <keywords>
        <keyword>Central amazon</keyword>
        <keyword>Floodplains</keyword>
        <keyword>Fatty acids</keyword>
        <keyword>Stables isotopes</keyword>
        <keyword>Macrophytes</keyword>
        <keyword>Degradation</keyword>
        <keyword>BRESIL</keyword>
        <keyword>AMAZONE BASSIN</keyword>
        <keyword>CAMALEAO LAC</keyword>
      </keywords>
      <dates>
        <year>2016</year>
      </dates>
      <call-num>fdi:010067718</call-num>
      <language>ENG</language>
      <periodical>
        <full-title>Limnologica</full-title>
      </periodical>
      <isbn>0075-9511</isbn>
      <accession-num>ISI:000380418300008</accession-num>
      <electronic-resource-num>10.1016/j.limno.2016.03.008</electronic-resource-num>
      <urls>
        <related-urls>
          <url>https://www.documentation.ird.fr/hor/fdi:010067718</url>
        </related-urls>
        <pdf-urls>
          <url>https://www.documentation.ird.fr/intranet/publi/2016/09/010067718.pdf</url>
        </pdf-urls>
      </urls>
      <volume>59</volume>
      <remote-database-provider>Horizon (IRD)</remote-database-provider>
      <abstract>The central Amazon floodplains are particularly productive ecosystems, where a large diversity of organic carbon sources are available for aquatic organisms. Despite the fact that C-4 macrophytes generally produce larger biomasses than C-3 macrophytes, food webs in the central Amazon floodplains appear dominantly based on a C-3 carbon source. In order to investigate the respective fate and degradation patterns of C-4 and C-3 aquatic plant-derived material in central Amazon floodplains, we developed a 23-days batch experiment. Fatty acid and carbon concentrations as well as stable isotope compositions were monitored over time in 60 L tanks. These tanks contained Amazon water, with different biomasses of C-3 and C-4 macrophyte, representative of in situ densities occurring in central Amazon floodplains. In the C-4 Paspalum repens treatments, organic (POC, DOC) and inorganic carbon (DIC) got rapidly enriched in C-13, whereas in the C-3 Salvinia auriculata treatments, POC and DOC showed little change in concentration and isotopic composition, and DIC got depleted in C-13. The contribution of P. repens to POC and DOC was estimated to reach up to 94.2 and 70.7%, respectively. In contrast, no differences were reported between the C-3 S. auriculata and control treatments, an observation attributed to the lower C-3 biomass encountered in the field, to a slower degradation rate of C-3 compared to C-4 compounds, and to similar isotopic compositions for river POC and DOC, and C-3 compounds. The C-13 enrichments of POC, DOC, and DIC from P. repens treatments were attributed to an enhanced bacterially-mediated hydrolysis and mineralization of C-4 material. Evolutions of bacterial abundance and branched fatty acid concentrations confirmed the role of heterotrophic microbial communities in the high P. repens decomposition rate. Our experiment highlights the predominant role of C-4 aquatic plants, as a large source of almost entirely biodegradable organic matter available for heterotrophic activity and CO2 outgassing to the atmosphere.</abstract>
      <custom6>036</custom6>
      <custom1>UR207 / UR219 / UR234 / UR226</custom1>
      <custom7>Brésil / Pérou</custom7>
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