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...
Main Authors: | , |
---|---|
Other Authors: | |
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 |
id |
ftunivmilanobic:oai:boa.unimib.it:10281/184621 |
---|---|
record_format |
openpolar |
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 |
_version_ |
1790597353392046080 |