Zn isotope fractionation in a pristine larch forest on permafrost-dominated soils in Central Siberia

Stable Zn isotopes fractionation was studied in main biogeochemical compartments of a pristine larch forest of Central Siberia developed over continuous permafrost basalt rocks. Two north- and south-oriented watershed slopes having distinctly different vegetation biomass and active layer depth were...

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Published in:Geochemical Transactions
Main Authors: Viers, Jerome, Prokushkin, Anatoly S, Pokrovsky, Oleg S, Kirdyanov, Alexander V, Zouiten, Cyril, Chmeleff, Jerome, Meheut, Merlin, Chabaux, Francois, Oliva, Priscia, Dupré, Bernard
Format: Text
Language:English
Published: Springer International Publishing 2015
Subjects:
Online Access:http://www.ncbi.nlm.nih.gov/pmc/articles/PMC4415248/
https://doi.org/10.1186/s12932-015-0018-0
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spelling ftpubmed:oai:pubmedcentral.nih.gov:4415248 2023-05-15T17:56:46+02:00 Zn isotope fractionation in a pristine larch forest on permafrost-dominated soils in Central Siberia Viers, Jerome Prokushkin, Anatoly S Pokrovsky, Oleg S Kirdyanov, Alexander V Zouiten, Cyril Chmeleff, Jerome Meheut, Merlin Chabaux, Francois Oliva, Priscia Dupré, Bernard 2015-04-16 http://www.ncbi.nlm.nih.gov/pmc/articles/PMC4415248/ https://doi.org/10.1186/s12932-015-0018-0 en eng Springer International Publishing http://www.ncbi.nlm.nih.gov/pmc/articles/PMC4415248/ http://dx.doi.org/10.1186/s12932-015-0018-0 © Viers et al.; licensee Springer. 2015 This is an Open Access article distributed under the terms of the Creative Commons Attribution License (http://creativecommons.org/licenses/by/4.0), which permits unrestricted use, distribution, and reproduction in any medium, provided the original work is properly credited. CC-BY Research Article Text 2015 ftpubmed https://doi.org/10.1186/s12932-015-0018-0 2015-05-03T00:26:28Z Stable Zn isotopes fractionation was studied in main biogeochemical compartments of a pristine larch forest of Central Siberia developed over continuous permafrost basalt rocks. Two north- and south-oriented watershed slopes having distinctly different vegetation biomass and active layer depth were used as natural proxy for predicting possible future climate changes occurring in this region. In addition, peat bog zone exhibiting totally different vegetation, hydrology and soil temperature regime has been studied. Text permafrost Siberia PubMed Central (PMC) Geochemical Transactions 16 1
institution Open Polar
collection PubMed Central (PMC)
op_collection_id ftpubmed
language English
topic Research Article
spellingShingle Research Article
Viers, Jerome
Prokushkin, Anatoly S
Pokrovsky, Oleg S
Kirdyanov, Alexander V
Zouiten, Cyril
Chmeleff, Jerome
Meheut, Merlin
Chabaux, Francois
Oliva, Priscia
Dupré, Bernard
Zn isotope fractionation in a pristine larch forest on permafrost-dominated soils in Central Siberia
topic_facet Research Article
description Stable Zn isotopes fractionation was studied in main biogeochemical compartments of a pristine larch forest of Central Siberia developed over continuous permafrost basalt rocks. Two north- and south-oriented watershed slopes having distinctly different vegetation biomass and active layer depth were used as natural proxy for predicting possible future climate changes occurring in this region. In addition, peat bog zone exhibiting totally different vegetation, hydrology and soil temperature regime has been studied.
format Text
author Viers, Jerome
Prokushkin, Anatoly S
Pokrovsky, Oleg S
Kirdyanov, Alexander V
Zouiten, Cyril
Chmeleff, Jerome
Meheut, Merlin
Chabaux, Francois
Oliva, Priscia
Dupré, Bernard
author_facet Viers, Jerome
Prokushkin, Anatoly S
Pokrovsky, Oleg S
Kirdyanov, Alexander V
Zouiten, Cyril
Chmeleff, Jerome
Meheut, Merlin
Chabaux, Francois
Oliva, Priscia
Dupré, Bernard
author_sort Viers, Jerome
title Zn isotope fractionation in a pristine larch forest on permafrost-dominated soils in Central Siberia
title_short Zn isotope fractionation in a pristine larch forest on permafrost-dominated soils in Central Siberia
title_full Zn isotope fractionation in a pristine larch forest on permafrost-dominated soils in Central Siberia
title_fullStr Zn isotope fractionation in a pristine larch forest on permafrost-dominated soils in Central Siberia
title_full_unstemmed Zn isotope fractionation in a pristine larch forest on permafrost-dominated soils in Central Siberia
title_sort zn isotope fractionation in a pristine larch forest on permafrost-dominated soils in central siberia
publisher Springer International Publishing
publishDate 2015
url http://www.ncbi.nlm.nih.gov/pmc/articles/PMC4415248/
https://doi.org/10.1186/s12932-015-0018-0
genre permafrost
Siberia
genre_facet permafrost
Siberia
op_relation http://www.ncbi.nlm.nih.gov/pmc/articles/PMC4415248/
http://dx.doi.org/10.1186/s12932-015-0018-0
op_rights © Viers et al.; licensee Springer. 2015
This is an Open Access article distributed under the terms of the Creative Commons Attribution License (http://creativecommons.org/licenses/by/4.0), which permits unrestricted use, distribution, and reproduction in any medium, provided the original work is properly credited.
op_rightsnorm CC-BY
op_doi https://doi.org/10.1186/s12932-015-0018-0
container_title Geochemical Transactions
container_volume 16
container_issue 1
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