Zn isotope fractionation in a pristine larch forest on permafrost-dominated soils in Central Siberia
Abstract 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 de...
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ftbiomed:oai:biomedcentral.com:s12932-015-0018-0 2023-05-15T17:57:46+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.geochemicaltransactions.com/content/16/1/3 en eng BioMed Central Ltd. http://www.geochemicaltransactions.com/content/16/1/3 Copyright 2015 Viers et al.; licensee Springer. Tree Soil Bog Moss Seasons Larix Transport Translocation Uptake Research article 2015 ftbiomed 2015-05-02T23:56:20Z Abstract 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. The isotopic composition of soil profile from Central Siberia is rather constant with a δ 66 Zn value around 0.2‰ close to the value of various basalts. Zn isotopic composition in mosses ( Sphagnum fuscum and Pleurozium schreberi ) exhibits differences between surface layers presenting values from 0.14 to 0.2‰ and bottom layers presenting significantly higher values (0.5 – 0.7‰) than the underlain mineral surface. The humification of both dead moss and larch needles leads to retain the fraction where Zn bound most strongly thus releasing the lighter isotopes in solution and preserving the heavy isotopes in the humification products, in general accord with previous experimental and modeling works [GCA 75:7632–7643, 2011]. The larch (Larix gmelinii ) from North and South-facing slopes is enriched in heavy isotopes compared to soil reservoir while larch from Sphagnum peatbog is enriched in light isotopes. This difference may result from stronger complexation of Zn by organic ligands and humification products in the peat bog compared to mineral surfaces in North- and South-facing slope. During the course of the growing period, Zn followed the behavior of macronutrients with a decrease of concentration from June to September. During this period, an enrichment of larch needles by heavier Zn isotopes is observed in the various habitats. We suggest that the increase of the depth of rooting zone, and the decrease of DOC and Zn concentration in soil solution from the root uptake zone with progressively thawing soil could provoke heavy isotopes to become more available for the larch roots at the end of the vegetative season compared to the beginning of the season, because the decrease of DOC will facilitate the uptake of heavy isotope as it will be less retained in strong organic complexes. Article in Journal/Newspaper permafrost Siberia BioMed Central |
institution |
Open Polar |
collection |
BioMed Central |
op_collection_id |
ftbiomed |
language |
English |
topic |
Tree Soil Bog Moss Seasons Larix Transport Translocation Uptake |
spellingShingle |
Tree Soil Bog Moss Seasons Larix Transport Translocation Uptake 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 |
Tree Soil Bog Moss Seasons Larix Transport Translocation Uptake |
description |
Abstract 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. The isotopic composition of soil profile from Central Siberia is rather constant with a δ 66 Zn value around 0.2‰ close to the value of various basalts. Zn isotopic composition in mosses ( Sphagnum fuscum and Pleurozium schreberi ) exhibits differences between surface layers presenting values from 0.14 to 0.2‰ and bottom layers presenting significantly higher values (0.5 – 0.7‰) than the underlain mineral surface. The humification of both dead moss and larch needles leads to retain the fraction where Zn bound most strongly thus releasing the lighter isotopes in solution and preserving the heavy isotopes in the humification products, in general accord with previous experimental and modeling works [GCA 75:7632–7643, 2011]. The larch (Larix gmelinii ) from North and South-facing slopes is enriched in heavy isotopes compared to soil reservoir while larch from Sphagnum peatbog is enriched in light isotopes. This difference may result from stronger complexation of Zn by organic ligands and humification products in the peat bog compared to mineral surfaces in North- and South-facing slope. During the course of the growing period, Zn followed the behavior of macronutrients with a decrease of concentration from June to September. During this period, an enrichment of larch needles by heavier Zn isotopes is observed in the various habitats. We suggest that the increase of the depth of rooting zone, and the decrease of DOC and Zn concentration in soil solution from the root uptake zone with progressively thawing soil could provoke heavy isotopes to become more available for the larch roots at the end of the vegetative season compared to the beginning of the season, because the decrease of DOC will facilitate the uptake of heavy isotope as it will be less retained in strong organic complexes. |
format |
Article in Journal/Newspaper |
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 |
BioMed Central Ltd. |
publishDate |
2015 |
url |
http://www.geochemicaltransactions.com/content/16/1/3 |
genre |
permafrost Siberia |
genre_facet |
permafrost Siberia |
op_relation |
http://www.geochemicaltransactions.com/content/16/1/3 |
op_rights |
Copyright 2015 Viers et al.; licensee Springer. |
_version_ |
1766166261620801536 |