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

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Direct and indirect effects of glaciers on aquatic biodiversity in high Andean peatlands. / Quenta, Estefania; Molina-Rodriguez, Jorge; Gonzales, Karina; Rebaudo, François; Casas, Jérôme; Jacobsen, Dean; Dangles, Olivier.

In: Global Change Biology, 2016, p. 3196-3205.

Research output: Contribution to journalJournal articleResearchpeer-review

Harvard

Quenta, E, Molina-Rodriguez, J, Gonzales, K, Rebaudo, F, Casas, J, Jacobsen, D & Dangles, O 2016, 'Direct and indirect effects of glaciers on aquatic biodiversity in high Andean peatlands', Global Change Biology, pp. 3196-3205. https://doi.org/10.1111/gcb.13310

APA

Quenta, E., Molina-Rodriguez, J., Gonzales, K., Rebaudo, F., Casas, J., Jacobsen, D., & Dangles, O. (2016). Direct and indirect effects of glaciers on aquatic biodiversity in high Andean peatlands. Global Change Biology, 3196-3205. https://doi.org/10.1111/gcb.13310

Vancouver

Quenta E, Molina-Rodriguez J, Gonzales K, Rebaudo F, Casas J, Jacobsen D et al. Direct and indirect effects of glaciers on aquatic biodiversity in high Andean peatlands. Global Change Biology. 2016;3196-3205. https://doi.org/10.1111/gcb.13310

Author

Quenta, Estefania ; Molina-Rodriguez, Jorge ; Gonzales, Karina ; Rebaudo, François ; Casas, Jérôme ; Jacobsen, Dean ; Dangles, Olivier. / Direct and indirect effects of glaciers on aquatic biodiversity in high Andean peatlands. In: Global Change Biology. 2016 ; pp. 3196-3205.

Bibtex

@article{025c8744abc044849e3d716b9da71d69,
title = "Direct and indirect effects of glaciers on aquatic biodiversity in high Andean peatlands",
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.",
keywords = "Aquatic biodiversity, Environmental heterogeneity, Glacial influence, High Andean peatlands, Peatland area, Tropical Andes",
author = "Estefania Quenta and Jorge Molina-Rodriguez and Karina Gonzales and Fran{\c c}ois Rebaudo and J{\'e}r{\^o}me Casas and Dean Jacobsen and Olivier Dangles",
year = "2016",
doi = "10.1111/gcb.13310",
language = "English",
pages = "3196--3205",
journal = "Global Change Biology",
issn = "1354-1013",
publisher = "Wiley-Blackwell",

}

RIS

TY - JOUR

T1 - Direct and indirect effects of glaciers on aquatic biodiversity in high Andean peatlands

AU - Quenta, Estefania

AU - Molina-Rodriguez, Jorge

AU - Gonzales, Karina

AU - Rebaudo, François

AU - Casas, Jérôme

AU - Jacobsen, Dean

AU - Dangles, Olivier

PY - 2016

Y1 - 2016

N2 - 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.

AB - 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.

KW - Aquatic biodiversity

KW - Environmental heterogeneity

KW - Glacial influence

KW - High Andean peatlands

KW - Peatland area

KW - Tropical Andes

U2 - 10.1111/gcb.13310

DO - 10.1111/gcb.13310

M3 - Journal article

C2 - 27058991

SP - 3196

EP - 3205

JO - Global Change Biology

JF - Global Change Biology

SN - 1354-1013

ER -

ID: 162751218