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<oai_dc:dc xmlns:oai_dc="http://www.openarchives.org/OAI/2.0/oai_dc/" xmlns:dc="http://purl.org/dc/elements/1.1/" xmlns:xsi="http://www.w3.org/2001/XMLSchema-instance" xsi:schemaLocation="http://www.openarchives.org/OAI/2.0/oai_dc/ http://www.openarchives.org/OAI/2.0/oai_dc.xsd">
  <dc:title>Direct and indirect effects of glaciers on aquatic biodiversity in high Andean peatlands</dc:title>
  <dc:creator>Quenta, E.</dc:creator>
  <dc:creator>Molina-Rodriguez, J.</dc:creator>
  <dc:creator>Gonzales, K.</dc:creator>
  <dc:creator>/Rebaudo, Fran&#xE7;ois</dc:creator>
  <dc:creator>Casas, J.</dc:creator>
  <dc:creator>Jacobsen, D.</dc:creator>
  <dc:creator>/Dangles, Olivier</dc:creator>
  <dc:subject>aquatic biodiversity</dc:subject>
  <dc:subject>environmental heterogeneity</dc:subject>
  <dc:subject>glacial influence</dc:subject>
  <dc:subject>high Andean peatlands</dc:subject>
  <dc:subject>peatland area</dc:subject>
  <dc:subject>tropical Andes</dc:subject>
  <dc:description>The rapid melting of glacier cover is one of the most obvious impacts of climate change on alpine ecosystems and biodiversity. Our understanding of the impact of a decrease in glacier runoff on aquatic biodiversity is currently based on the glacier-heterogeneity-diversity' paradigm, according to which there is high -diversity at intermediate levels of glacial influence due to the high degree of environmental heterogeneity caused by glacier water. This -diversity pattern generates high levels of between-site aquatic community variation (high diversity) and increases regional diversity (-diversity). There is a rich conceptual background in favor of this paradigm, but empirical data supporting it are scarce. We investigated this paradigm by analyzing the different diversity patterns (, and -diversity) of four aquatic groups (zooplankton, macroinvertebrates, algae and macrophytes) living in high-elevation peatlands (&gt;4500m above sea level). We sampled 200 pools from 20 peatlands along a glacier gradient in the Cordillera Real of Bolivia. We performed structural equationmodeling (SEM) to analyze the potential mechanisms underlying the observed diversity patterns. Intermediate levels of glacial influence (15-20% cover) resulted in high heterogeneity, but -diversity responded to glacial influence only for the zooplankton group (Cladocera). Our SEM analysis did not identify environmental heterogeneity as a significant variable explaining the relationship between glacier and -diversity. Peatland area had a strong positive effect on heterogeneity and diversity. -diversity was significantly associated with glacier gradient, and 12.9% of the total regional diversity (-diversity) was restricted to peatlands with a high degree of glacial influence. These species might be lost in a context of glacial retreat. These findings provide new insight into the potential effects of glacial retreat on the aquatic environment and biodiversity in the peatlands of the tropical Andes.</dc:description>
  <dc:date>2016</dc:date>
  <dc:type>text</dc:type>
  <dc:identifier>https://www.documentation.ird.fr/hor/fdi:010067764</dc:identifier>
  <dc:identifier>fdi:010067764</dc:identifier>
  <dc:identifier>Quenta E., Molina-Rodriguez J., Gonzales K., Rebaudo Fran&#xE7;ois, Casas J., Jacobsen D., Dangles Olivier. Direct and indirect effects of glaciers on aquatic biodiversity in high Andean peatlands. 2016, 22 (9), 3196-3205</dc:identifier>
  <dc:language>EN</dc:language>
  <dc:coverage>BOLIVIE</dc:coverage>
  <dc:coverage>ANDES</dc:coverage>
  <dc:coverage>ZONE TROPICALE</dc:coverage>
</oai_dc:dc>
