Ecological responses to experimental glacier-runoff reduction in alpine rivers
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Ecological responses to experimental glacier-runoff reduction in alpine rivers. / Cauvy-Fraunié, Sophie; Andino, Patricio; Espinosa, Rodrigo; Calvez, Roger; Jacobsen, Dean; Dangles, Olivier.
In: Nature Communications, Vol. 7, 12025, 2016.Research output: Contribution to journal › Journal article › Research › peer-review
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T1 - Ecological responses to experimental glacier-runoff reduction in alpine rivers
AU - Cauvy-Fraunié, Sophie
AU - Andino, Patricio
AU - Espinosa, Rodrigo
AU - Calvez, Roger
AU - Jacobsen, Dean
AU - Dangles, Olivier
PY - 2016
Y1 - 2016
N2 - 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.
AB - 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.
U2 - 10.1038/ncomms12025
DO - 10.1038/ncomms12025
M3 - Journal article
C2 - 27338650
VL - 7
JO - Nature Communications
JF - Nature Communications
SN - 2041-1723
M1 - 12025
ER -
ID: 162905658