Direct and indirect effects of glaciers on aquatic biodiversity in high Andean peatlands
Autor: | Jérôme Casas, Karina Gonzales, Estefania Quenta, Dean Jacobsen, Olivier Dangles, Jorge Molina-Rodriguez, François Rebaudo |
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Rok vydání: | 2016 |
Předmět: |
0106 biological sciences
Aquatic Organisms Bolivia Peat 010504 meteorology & atmospheric sciences Climate Change Biodiversity Climate change Context (language use) 010603 evolutionary biology 01 natural sciences Animals Environmental Chemistry Ice Cover Ecosystem Glacial period 0105 earth and related environmental sciences General Environmental Science Global and Planetary Change geography geography.geographical_feature_category Ecology Glacier Macrophyte Environmental science |
Zdroj: | Global Change Biology. 22:3196-3205 |
ISSN: | 1354-1013 |
DOI: | 10.1111/gcb.13310 |
Popis: | 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. |
Databáze: | OpenAIRE |
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