The project “ROCK-ME: geochemical response of Alpine Rock Glaciers to global warming: hydroecological consequences of trace element Export”

ROCK-ME is a 3-year project funded by the 4th Call of the EUREGIO Interregional Project Networks framework, including the Alpine regions North Tyrol (A), South Tyrol and Trentino (I). The project, started in April 2022, addresses the effects of climate warming on the degradation of mountain permafro...

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Main Authors: Monica Tolotti, Stefano Brighenti, Lorenzo Brusetti, Francesco Comiti, Andrea Fisher, Maria Cristina Bruno
Other Authors: José M. Fernández-Fernández, Josep Bonsoms, Julia Garcia-Oteyza, Marc Oliva, Tolotti, M., Brighenti, S., Brusetti, L., Comiti, F., Fisher, A., Bruno, M.C.
Format: Conference Object
Language:English
Published: country:ES 2023
Subjects:
Online Access:https://hdl.handle.net/10449/80175
https://doi.org/10.52381/EUCOP6.abstracts.1
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author Monica Tolotti
Stefano Brighenti
Lorenzo Brusetti
Francesco Comiti
Andrea Fisher
Maria Cristina Bruno
author2 José M. Fernández-Fernández, Josep Bonsoms, Julia Garcia-Oteyza, Marc Oliva
Tolotti, M.
Brighenti, S.
Brusetti, L.
Comiti, F.
Fisher, A.
Bruno, M.C.
author_facet Monica Tolotti
Stefano Brighenti
Lorenzo Brusetti
Francesco Comiti
Andrea Fisher
Maria Cristina Bruno
author_sort Monica Tolotti
collection Fondazione Edmund Mach: IRIS-OpenPub
description ROCK-ME is a 3-year project funded by the 4th Call of the EUREGIO Interregional Project Networks framework, including the Alpine regions North Tyrol (A), South Tyrol and Trentino (I). The project, started in April 2022, addresses the effects of climate warming on the degradation of mountain permafrost. Thawing rock glaciers (RG) are becoming key hydroecological drivers in numerous deglaciating Alpine catchments, as they export cold waters often enriched in trace elements (TE). However, both the hydrological dynamics and the ecological effects of TE enrichment on water quality and ecology of RG and the downstream river networks are almost entirely unknown. The research questions investigated by ROCK-ME are: 1) Do thawing RGs export higher loads of TE than glaciers, relict RGs and groundwater springs? 2) Do TE in RG-streams mainly originate from bedrock weathering, while only a smaller amount derives from past/present atmospheric deposition? 3) Do TE export and its ecological effects vary at multiple timescales in relation to seasonal and long-term dynamics of permafrost thawing; 4) Do TE bioaccumulate in the stream foodweb? 5) Do RG microbial communities modulate TE bioavailability? 6) Do thawing RGs release trace metal resistance genes? Three Alpine catchments with different proportions of glaciers and RG cover - Futschöl in Jamtal (North Tyrol, A), Lazaun in Schnalstal/Val Senales and Madritsch in Martelltal/ Val Martello (South Tyrol, I) - have been investigated during the Alpine summer 2022 following an integrated approach combining geomorphological/geochemical analysis, hydrological monitoring and modelling, ecological and genomic characterization. Field activities are going to be completed within autumn 2023.
format Conference Object
genre permafrost
genre_facet permafrost
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institution Open Polar
language English
op_collection_id ftiasma
op_doi https://doi.org/10.52381/EUCOP6.abstracts.1
op_relation ispartofbook:6th European Conference on Permafrost (EUCOP 2023), Puigcerdà, Catalonia, Spain, 18-22 June, 2023
6th European Conference on Permafrost (EUCOP 2023)
firstpage:113
alleditors:José M. Fernández-Fernández, Josep Bonsoms, Julia Garcia-Oteyza, Marc Oliva
https://hdl.handle.net/10449/80175
doi:10.52381/EUCOP6.abstracts.1
op_rights info:eu-repo/semantics/openAccess
publishDate 2023
publisher country:ES
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spelling ftiasma:oai:openpub.fmach.it:10449/80175 2025-01-17T00:16:13+00:00 The project “ROCK-ME: geochemical response of Alpine Rock Glaciers to global warming: hydroecological consequences of trace element Export” Monica Tolotti Stefano Brighenti Lorenzo Brusetti Francesco Comiti Andrea Fisher Maria Cristina Bruno José M. Fernández-Fernández, Josep Bonsoms, Julia Garcia-Oteyza, Marc Oliva Tolotti, M. Brighenti, S. Brusetti, L. Comiti, F. Fisher, A. Bruno, M.C. 2023 https://hdl.handle.net/10449/80175 https://doi.org/10.52381/EUCOP6.abstracts.1 eng eng country:ES ispartofbook:6th European Conference on Permafrost (EUCOP 2023), Puigcerdà, Catalonia, Spain, 18-22 June, 2023 6th European Conference on Permafrost (EUCOP 2023) firstpage:113 alleditors:José M. Fernández-Fernández, Josep Bonsoms, Julia Garcia-Oteyza, Marc Oliva https://hdl.handle.net/10449/80175 doi:10.52381/EUCOP6.abstracts.1 info:eu-repo/semantics/openAccess Rock glaciers Water resources Settore BIO/07 - ECOLOGIA info:eu-repo/semantics/conferenceObject 2023 ftiasma https://doi.org/10.52381/EUCOP6.abstracts.1 2023-10-17T22:26:04Z ROCK-ME is a 3-year project funded by the 4th Call of the EUREGIO Interregional Project Networks framework, including the Alpine regions North Tyrol (A), South Tyrol and Trentino (I). The project, started in April 2022, addresses the effects of climate warming on the degradation of mountain permafrost. Thawing rock glaciers (RG) are becoming key hydroecological drivers in numerous deglaciating Alpine catchments, as they export cold waters often enriched in trace elements (TE). However, both the hydrological dynamics and the ecological effects of TE enrichment on water quality and ecology of RG and the downstream river networks are almost entirely unknown. The research questions investigated by ROCK-ME are: 1) Do thawing RGs export higher loads of TE than glaciers, relict RGs and groundwater springs? 2) Do TE in RG-streams mainly originate from bedrock weathering, while only a smaller amount derives from past/present atmospheric deposition? 3) Do TE export and its ecological effects vary at multiple timescales in relation to seasonal and long-term dynamics of permafrost thawing; 4) Do TE bioaccumulate in the stream foodweb? 5) Do RG microbial communities modulate TE bioavailability? 6) Do thawing RGs release trace metal resistance genes? Three Alpine catchments with different proportions of glaciers and RG cover - Futschöl in Jamtal (North Tyrol, A), Lazaun in Schnalstal/Val Senales and Madritsch in Martelltal/ Val Martello (South Tyrol, I) - have been investigated during the Alpine summer 2022 following an integrated approach combining geomorphological/geochemical analysis, hydrological monitoring and modelling, ecological and genomic characterization. Field activities are going to be completed within autumn 2023. Conference Object permafrost Fondazione Edmund Mach: IRIS-OpenPub
spellingShingle Rock glaciers
Water resources
Settore BIO/07 - ECOLOGIA
Monica Tolotti
Stefano Brighenti
Lorenzo Brusetti
Francesco Comiti
Andrea Fisher
Maria Cristina Bruno
The project “ROCK-ME: geochemical response of Alpine Rock Glaciers to global warming: hydroecological consequences of trace element Export”
title The project “ROCK-ME: geochemical response of Alpine Rock Glaciers to global warming: hydroecological consequences of trace element Export”
title_full The project “ROCK-ME: geochemical response of Alpine Rock Glaciers to global warming: hydroecological consequences of trace element Export”
title_fullStr The project “ROCK-ME: geochemical response of Alpine Rock Glaciers to global warming: hydroecological consequences of trace element Export”
title_full_unstemmed The project “ROCK-ME: geochemical response of Alpine Rock Glaciers to global warming: hydroecological consequences of trace element Export”
title_short The project “ROCK-ME: geochemical response of Alpine Rock Glaciers to global warming: hydroecological consequences of trace element Export”
title_sort project “rock-me: geochemical response of alpine rock glaciers to global warming: hydroecological consequences of trace element export”
topic Rock glaciers
Water resources
Settore BIO/07 - ECOLOGIA
topic_facet Rock glaciers
Water resources
Settore BIO/07 - ECOLOGIA
url https://hdl.handle.net/10449/80175
https://doi.org/10.52381/EUCOP6.abstracts.1