Direct and indirect effects of glaciers on aquatic biodiversity in high Andean peatlands

dc.contributor.authorEstefania Quenta
dc.contributor.authorJorge Molina‐Rodriguez
dc.contributor.authorKarina Gonzales
dc.contributor.authorFrançois Rebaudo
dc.contributor.authorJérôme Casas
dc.contributor.authorDean Jacobsen
dc.contributor.authorOlivier Dangles
dc.coverage.spatialBolivia
dc.date.accessioned2026-03-22T14:13:14Z
dc.date.available2026-03-22T14:13:14Z
dc.date.issued2016
dc.descriptionCitaciones: 28
dc.description.abstractThe 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 α-diversity at intermediate levels of glacial influence due to the high degree of environmental heterogeneity caused by glacier water. This α-diversity pattern generates high levels of between-site aquatic community variation (high β diversity) and increases regional diversity (γ-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 (α, β and γ-diversity) of four aquatic groups (zooplankton, macroinvertebrates, algae and macrophytes) living in high-elevation peatlands (>4500 m above sea level). We sampled 200 pools from 20 peatlands along a glacier gradient in the Cordillera Real of Bolivia. We performed structural equation modeling (SEM) to analyze the potential mechanisms underlying the observed diversity patterns. Intermediate levels of glacial influence (15-20% cover) resulted in high heterogeneity, but α-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 α-diversity. Peatland area had a strong positive effect on heterogeneity and diversity. β-diversity was significantly associated with glacier gradient, and 12.9% of the total regional diversity (γ-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.identifier.doi10.1111/gcb.13310
dc.identifier.urihttps://doi.org/10.1111/gcb.13310
dc.identifier.urihttps://andeanlibrary.org/handle/123456789/45240
dc.language.isoen
dc.publisherWiley
dc.relation.ispartofGlobal Change Biology
dc.sourceUniversité de Tours
dc.subjectBiodiversity
dc.subjectGlacier
dc.subjectEcology
dc.subjectGlacial period
dc.subjectPeat
dc.subjectBeta diversity
dc.subjectEnvironmental science
dc.subjectAlpha diversity
dc.subjectZooplankton
dc.subjectPhysical geography
dc.titleDirect and indirect effects of glaciers on aquatic biodiversity in high Andean peatlands
dc.typearticle

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