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Ecological responses to experimental glacier-runoff reduction in alpine rivers

Sophie Cauvy-Fraunié (), Patricio Andino, Rodrigo Espinosa, Roger Calvez, Dean Jacobsen and Olivier Dangles ()
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Sophie Cauvy-Fraunié: Institut de Recherche pour le Développement (IRD), UMR EGCE, IRD-247 CNRS-UP Sud-9191
Patricio Andino: Pontificia Universidad Católica del Ecuador, Escuela de Ciencias Biológicas
Rodrigo Espinosa: Pontificia Universidad Católica del Ecuador, Escuela de Ciencias Biológicas
Roger Calvez: Institut de Recherche pour le Développement (IRD), UMR G-EAU
Dean Jacobsen: Pontificia Universidad Católica del Ecuador, Escuela de Ciencias Biológicas
Olivier Dangles: Institut de Recherche pour le Développement (IRD), UMR EGCE, IRD-247 CNRS-UP Sud-9191

Nature Communications, 2016, vol. 7, issue 1, 1-7

Abstract: Abstract Glacier retreat is a worldwide phenomenon with important consequences for the hydrological cycle and downstream ecosystem structure and functioning. To determine the effects of glacier retreat on aquatic communities, we conducted a 4-year flow manipulation in a tropical glacier-fed stream. Compared with an adjacent reference stream, meltwater flow reduction induces significant changes in benthic fauna community composition in less than 2 weeks. Also, both algal and herbivore biomass significantly increase in the manipulated stream as a response to flow reduction. After the flow reduction ceased, the system requires 14–16 months to return to its pre-perturbation state. These results are supported by a multi-stream survey of sites varying in glacial influence, showing an abrupt increase in algal and herbivore biomass below 11% glacier cover in the catchment. This study shows that flow reduction strongly affects glacier-fed stream biota, prefiguring profound ecological effects of ongoing glacier retreat on aquatic systems.

Date: 2016
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Persistent link: https://EconPapers.repec.org/RePEc:nat:natcom:v:7:y:2016:i:1:d:10.1038_ncomms12025

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DOI: 10.1038/ncomms12025

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