Effects of deglaciation on Alpine freshwater ecosystems

Glaciers shrinkage and permafrost degradation are amongst the most evident and dramatic effects of human-driven climate change, and the loss of cryosphere is determining radical shifts in the hydrology and ecology of freshwaters also in the European Alps. A decreased water discharge from glaciers is...

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Main Authors: Brighenti, S., Bruno, M. C., Pusch, M., Tolotti, M., Wharton, G., Bertoldi, W.
Other Authors: Bruno, M.C.
Format: Conference Object
Language:English
Published: country:IT 2017
Subjects:
Online Access:http://hdl.handle.net/10449/43893
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author Brighenti, S.
Bruno, M. C.
Pusch, M.
Tolotti, M.
Wharton, G.
Bertoldi, W.
author2 Brighenti, S.
Bruno, M.C.
Pusch, M.
Tolotti, M.
Wharton, G.
Bertoldi, W.
author_facet Brighenti, S.
Bruno, M. C.
Pusch, M.
Tolotti, M.
Wharton, G.
Bertoldi, W.
author_sort Brighenti, S.
collection Fondazione Edmund Mach: IRIS-OpenPub
description Glaciers shrinkage and permafrost degradation are amongst the most evident and dramatic effects of human-driven climate change, and the loss of cryosphere is determining radical shifts in the hydrology and ecology of freshwaters also in the European Alps. A decreased water discharge from glaciers is foreseen in Alpine catchments, while thawing of rock glaciers (a common form of permafrost in the Alps) may become increasingly important for the hydroecology of headwaters. While a large amount of literature is available on the effects of glacier retreat on freshwater ecosystems, very little is known about the ecology of streams and lakes fed by rock glaciers. Nevertheless, there is evidence that permafrost degradation can have drastic effects on headwater physico-chemistry, which include increasing electrical conductivity, acidification, and contamination by heavy metals. The poster presents a PhD project, which aims at assessing the impacts of deglaciation on Alpine water ecosystems. A space by time substitution analysis will be undertaken in the Zay and Solda catchments (South Tyrol, Italy), where downstream changes in the contribution of different water sources (glaciers, rock glaciers, groundwater, snowmelt and rainfall) are considered as a proxy for temporal stages in the deglaciation process. In addition ecological shifts during different glaciation/deglaciation phases over the past centuries will be examined through the paleolimnological investigation of one high altitude lake within the study area.
format Conference Object
genre permafrost
genre_facet permafrost
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op_collection_id ftiasma
op_relation ispartofbook:International Meeting on the Conservation of High Mountain Lakes, July 6-8th, 2017, Ceresole Reale (TO), Italy
International Meeting on the Conservation of High Mountain Lakes
firstpage:51
http://hdl.handle.net/10449/43893
op_rights info:eu-repo/semantics/openAccess
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spelling ftiasma:oai:openpub.fmach.it:10449/43893 2025-01-17T00:15:31+00:00 Effects of deglaciation on Alpine freshwater ecosystems Brighenti, S. Bruno, M. C. Pusch, M. Tolotti, M. Wharton, G. Bertoldi, W. Brighenti, S. Bruno, M.C. Pusch, M. Tolotti, M. Wharton, G. Bertoldi, W. 2017 http://hdl.handle.net/10449/43893 eng eng country:IT ispartofbook:International Meeting on the Conservation of High Mountain Lakes, July 6-8th, 2017, Ceresole Reale (TO), Italy International Meeting on the Conservation of High Mountain Lakes firstpage:51 http://hdl.handle.net/10449/43893 info:eu-repo/semantics/openAccess Cryosphere Deglaciation Climate change Alpine headwaters Ecology Settore BIO/07 - ECOLOGIA info:eu-repo/semantics/conferenceObject 2017 ftiasma 2024-01-02T23:24:36Z Glaciers shrinkage and permafrost degradation are amongst the most evident and dramatic effects of human-driven climate change, and the loss of cryosphere is determining radical shifts in the hydrology and ecology of freshwaters also in the European Alps. A decreased water discharge from glaciers is foreseen in Alpine catchments, while thawing of rock glaciers (a common form of permafrost in the Alps) may become increasingly important for the hydroecology of headwaters. While a large amount of literature is available on the effects of glacier retreat on freshwater ecosystems, very little is known about the ecology of streams and lakes fed by rock glaciers. Nevertheless, there is evidence that permafrost degradation can have drastic effects on headwater physico-chemistry, which include increasing electrical conductivity, acidification, and contamination by heavy metals. The poster presents a PhD project, which aims at assessing the impacts of deglaciation on Alpine water ecosystems. A space by time substitution analysis will be undertaken in the Zay and Solda catchments (South Tyrol, Italy), where downstream changes in the contribution of different water sources (glaciers, rock glaciers, groundwater, snowmelt and rainfall) are considered as a proxy for temporal stages in the deglaciation process. In addition ecological shifts during different glaciation/deglaciation phases over the past centuries will be examined through the paleolimnological investigation of one high altitude lake within the study area. Conference Object permafrost Fondazione Edmund Mach: IRIS-OpenPub
spellingShingle Cryosphere
Deglaciation
Climate change
Alpine headwaters
Ecology
Settore BIO/07 - ECOLOGIA
Brighenti, S.
Bruno, M. C.
Pusch, M.
Tolotti, M.
Wharton, G.
Bertoldi, W.
Effects of deglaciation on Alpine freshwater ecosystems
title Effects of deglaciation on Alpine freshwater ecosystems
title_full Effects of deglaciation on Alpine freshwater ecosystems
title_fullStr Effects of deglaciation on Alpine freshwater ecosystems
title_full_unstemmed Effects of deglaciation on Alpine freshwater ecosystems
title_short Effects of deglaciation on Alpine freshwater ecosystems
title_sort effects of deglaciation on alpine freshwater ecosystems
topic Cryosphere
Deglaciation
Climate change
Alpine headwaters
Ecology
Settore BIO/07 - ECOLOGIA
topic_facet Cryosphere
Deglaciation
Climate change
Alpine headwaters
Ecology
Settore BIO/07 - ECOLOGIA
url http://hdl.handle.net/10449/43893