Biogeochemistry of high altitude soils on ophiolites in the Western Italian Alps.

High Mg, Fe, and heavy metals content, pH values close to neutrality and high base status characterize “serpentine soils”; the low Ca/Mg ratios and the high metal contents can cause stress on biological communities: the vegetation often shows a low cover and a peculiar species composition. Chemical...

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Main Authors: D'Amico, ME, Previtali, F
Other Authors: D'Amico, M
Format: Conference Object
Language:English
Published: country:PT 2011
Subjects:
Online Access:http://hdl.handle.net/10281/184621
https://doi.org/10.13140/2.1.1409.0562
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spelling ftunivmilanobic:oai:boa.unimib.it:10281/184621 2024-02-11T10:01:33+01:00 Biogeochemistry of high altitude soils on ophiolites in the Western Italian Alps. D'Amico, ME Previtali, F D'Amico, ME Previtali, F D'Amico, M 2011 http://hdl.handle.net/10281/184621 https://doi.org/10.13140/2.1.1409.0562 eng eng country:PT place:Coimbra 7th International Conference on Serpentine Ecology firstpage:1 lastpage:21 numberofpages:21 http://hdl.handle.net/10281/184621 doi:10.13140/2.1.1409.0562 info:eu-repo/semantics/openAccess Soils ophilites Western Italian Alps AGR/14 - PEDOLOGIA info:eu-repo/semantics/conferenceObject 2011 ftunivmilanobic https://doi.org/10.13140/2.1.1409.0562 2024-01-16T23:22:50Z High Mg, Fe, and heavy metals content, pH values close to neutrality and high base status characterize “serpentine soils”; the low Ca/Mg ratios and the high metal contents can cause stress on biological communities: the vegetation often shows a low cover and a peculiar species composition. Chemical and biological properties of alpine and arctic “serpentine soils” have seldom been studied worldwide. 97 soil pits (associated with phytosociological surveys) were analyzed above the treeline in Mont Avic Natural Park (Val d’Aosta, north-western Italy). The aim was to recognize pedogenic processes, mobility and bioavailability of metals and nutrients, to statistically identify edaphic properties influencing vegetation and possible stress symptoms on microbial and arthropodal communities. On serpentinite, meta-gabbros and calcschists, in cold and wet high-altitude climates (annual temperatures below 2°C and rainfall below 1300mm/y), soils are acidic, with pH values increasing with altitude and cryogenic or erosive disturbances. Cryoturbation, erosion and deposition “rejuvenate” soils by adding unweathered material into surface horizons: the soil chemistry depends on substrate, and metal concentration is increased in biologically-active horizons on serpentinite. Despite the weak soil development, metal speciation shows a strong mobilization and bioavailability, caused by waterlogging at snowmelt and acidity. On serpentinite, high bioavailable Ni is related with the absence of some common acidophilous species, despite the low pH values, and with the presence of serpentine-endemic species. Ca/Mg ratios, nutrients and pH values are not statistically significant. Bioavailable metals don’t significantly influence micro-arthropod communities. Microbial activity and stress indices are not related either with substrate or metal content. Conference Object Arctic Università degli Studi di Milano-Bicocca: BOA (Bicocca Open Archive) Arctic
institution Open Polar
collection Università degli Studi di Milano-Bicocca: BOA (Bicocca Open Archive)
op_collection_id ftunivmilanobic
language English
topic Soils
ophilites
Western Italian Alps
AGR/14 - PEDOLOGIA
spellingShingle Soils
ophilites
Western Italian Alps
AGR/14 - PEDOLOGIA
D'Amico, ME
Previtali, F
Biogeochemistry of high altitude soils on ophiolites in the Western Italian Alps.
topic_facet Soils
ophilites
Western Italian Alps
AGR/14 - PEDOLOGIA
description High Mg, Fe, and heavy metals content, pH values close to neutrality and high base status characterize “serpentine soils”; the low Ca/Mg ratios and the high metal contents can cause stress on biological communities: the vegetation often shows a low cover and a peculiar species composition. Chemical and biological properties of alpine and arctic “serpentine soils” have seldom been studied worldwide. 97 soil pits (associated with phytosociological surveys) were analyzed above the treeline in Mont Avic Natural Park (Val d’Aosta, north-western Italy). The aim was to recognize pedogenic processes, mobility and bioavailability of metals and nutrients, to statistically identify edaphic properties influencing vegetation and possible stress symptoms on microbial and arthropodal communities. On serpentinite, meta-gabbros and calcschists, in cold and wet high-altitude climates (annual temperatures below 2°C and rainfall below 1300mm/y), soils are acidic, with pH values increasing with altitude and cryogenic or erosive disturbances. Cryoturbation, erosion and deposition “rejuvenate” soils by adding unweathered material into surface horizons: the soil chemistry depends on substrate, and metal concentration is increased in biologically-active horizons on serpentinite. Despite the weak soil development, metal speciation shows a strong mobilization and bioavailability, caused by waterlogging at snowmelt and acidity. On serpentinite, high bioavailable Ni is related with the absence of some common acidophilous species, despite the low pH values, and with the presence of serpentine-endemic species. Ca/Mg ratios, nutrients and pH values are not statistically significant. Bioavailable metals don’t significantly influence micro-arthropod communities. Microbial activity and stress indices are not related either with substrate or metal content.
author2 D'Amico, ME
Previtali, F
D'Amico, M
format Conference Object
author D'Amico, ME
Previtali, F
author_facet D'Amico, ME
Previtali, F
author_sort D'Amico, ME
title Biogeochemistry of high altitude soils on ophiolites in the Western Italian Alps.
title_short Biogeochemistry of high altitude soils on ophiolites in the Western Italian Alps.
title_full Biogeochemistry of high altitude soils on ophiolites in the Western Italian Alps.
title_fullStr Biogeochemistry of high altitude soils on ophiolites in the Western Italian Alps.
title_full_unstemmed Biogeochemistry of high altitude soils on ophiolites in the Western Italian Alps.
title_sort biogeochemistry of high altitude soils on ophiolites in the western italian alps.
publisher country:PT
publishDate 2011
url http://hdl.handle.net/10281/184621
https://doi.org/10.13140/2.1.1409.0562
geographic Arctic
geographic_facet Arctic
genre Arctic
genre_facet Arctic
op_relation 7th International Conference on Serpentine Ecology
firstpage:1
lastpage:21
numberofpages:21
http://hdl.handle.net/10281/184621
doi:10.13140/2.1.1409.0562
op_rights info:eu-repo/semantics/openAccess
op_doi https://doi.org/10.13140/2.1.1409.0562
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