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

High Mg, Fe, heavy metals, 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 biologic...

Full description

Bibliographic Details
Main Authors: Michele D'Amico, Franco Previtali
Other Authors: M.E. D'Amico, F. Previtali
Format: Conference Object
Language:English
Published: 2011
Subjects:
Online Access:http://hdl.handle.net/2434/874627
id ftunivmilanoair:oai:air.unimi.it:2434/874627
record_format openpolar
spelling ftunivmilanoair:oai:air.unimi.it:2434/874627 2024-01-28T10:04:04+01:00 Biogeochemistry of high altitude soils on ophiolites in the Western Italian Alps Michele D'Amico Franco Previtali M.E. D'Amico F. Previtali 2011-06 http://hdl.handle.net/2434/874627 eng eng International Conference on Serpentine Ecology http://hdl.handle.net/2434/874627 Settore AGR/14 - Pedologia info:eu-repo/semantics/conferenceObject 2011 ftunivmilanoair 2024-01-02T23:53:06Z High Mg, Fe, heavy metals, 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 The University of Milan: Archivio Istituzionale della Ricerca (AIR) Arctic
institution Open Polar
collection The University of Milan: Archivio Istituzionale della Ricerca (AIR)
op_collection_id ftunivmilanoair
language English
topic Settore AGR/14 - Pedologia
spellingShingle Settore AGR/14 - Pedologia
Michele D'Amico
Franco Previtali
Biogeochemistry of high altitude soils on ophiolites in the Western Italian Alps
topic_facet Settore AGR/14 - Pedologia
description High Mg, Fe, heavy metals, 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 M.E. D'Amico
F. Previtali
format Conference Object
author Michele D'Amico
Franco Previtali
author_facet Michele D'Amico
Franco Previtali
author_sort Michele D'Amico
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
publishDate 2011
url http://hdl.handle.net/2434/874627
geographic Arctic
geographic_facet Arctic
genre Arctic
genre_facet Arctic
op_relation International Conference on Serpentine Ecology
http://hdl.handle.net/2434/874627
_version_ 1789329647001927680