Direct and indirect effects of glaciers on aquatic biodiversity in high Andean peatlands
| dc.contributor.author | Estefania Quenta | |
| dc.contributor.author | Jorge Molina‐Rodriguez | |
| dc.contributor.author | Karina Gonzales | |
| dc.contributor.author | François Rebaudo | |
| dc.contributor.author | Jérôme Casas | |
| dc.contributor.author | Dean Jacobsen | |
| dc.contributor.author | Olivier Dangles | |
| dc.coverage.spatial | Bolivia | |
| dc.date.accessioned | 2026-03-22T14:13:14Z | |
| dc.date.available | 2026-03-22T14:13:14Z | |
| dc.date.issued | 2016 | |
| dc.description | Citaciones: 28 | |
| dc.description.abstract | 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 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.doi | 10.1111/gcb.13310 | |
| dc.identifier.uri | https://doi.org/10.1111/gcb.13310 | |
| dc.identifier.uri | https://andeanlibrary.org/handle/123456789/45240 | |
| dc.language.iso | en | |
| dc.publisher | Wiley | |
| dc.relation.ispartof | Global Change Biology | |
| dc.source | Université de Tours | |
| dc.subject | Biodiversity | |
| dc.subject | Glacier | |
| dc.subject | Ecology | |
| dc.subject | Glacial period | |
| dc.subject | Peat | |
| dc.subject | Beta diversity | |
| dc.subject | Environmental science | |
| dc.subject | Alpha diversity | |
| dc.subject | Zooplankton | |
| dc.subject | Physical geography | |
| dc.title | Direct and indirect effects of glaciers on aquatic biodiversity in high Andean peatlands | |
| dc.type | article |