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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%">Cauvy-Fraunie, S.</style>
          </author>
          <author>
            <style face="normal" font="default" size="100%">Andino, P.</style>
          </author>
          <author>
            <style face="normal" font="default" size="100%">Espinosa, R.</style>
          </author>
          <author>
            <style face="bold" font="default" size="100%">Calvez, Roger</style>
          </author>
          <author>
            <style face="normal" font="default" size="100%">Jacobsen, D.</style>
          </author>
          <author>
            <style face="bold" font="default" size="100%">Dangles, Olivier</style>
          </author>
        </authors>
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      <titles>
        <title>Ecological responses to experimental glacier-runoff reduction in alpine rivers</title>
        <secondary-title>Nature Communications</secondary-title>
      </titles>
      <pages>art. 12025 [7 p.]</pages>
      <keywords>
        <keyword>EQUATEUR</keyword>
        <keyword>ANDES</keyword>
        <keyword>ANTISANA GLACIER</keyword>
        <keyword>ZONE TROPICALE</keyword>
      </keywords>
      <dates>
        <year>2016</year>
      </dates>
      <call-num>fdi:010067655</call-num>
      <language>ENG</language>
      <periodical>
        <full-title>Nature Communications</full-title>
      </periodical>
      <isbn>2041-1723</isbn>
      <accession-num>ISI:000379091500001</accession-num>
      <electronic-resource-num>10.1038/ncomms12025</electronic-resource-num>
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      <volume>7</volume>
      <remote-database-provider>Horizon (IRD)</remote-database-provider>
      <abstract>Glacier retreat is a worldwide phenomenon with important consequences for the hydrological cycle and downstream ecosystem structure and functioning. To determine the effects of glacier retreat on aquatic communities, we conducted a 4-year flow manipulation in a tropical glacier-fed stream. Compared with an adjacent reference stream, meltwater flow reduction induces significant changes in benthic fauna community composition in less than 2 weeks. Also, both algal and herbivore biomass significantly increase in the manipulated stream as a response to flow reduction. After the flow reduction ceased, the system requires 14-16 months to return to its pre-perturbation state. These results are supported by a multi-stream survey of sites varying in glacial influence, showing an abrupt increase in algal and herbivore biomass below 11% glacier cover in the catchment. This study shows that flow reduction strongly affects glacier-fed stream biota, prefiguring profound ecological effects of ongoing glacier retreat on aquatic systems.</abstract>
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      <custom7>Équateur</custom7>
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