Isotopic compositions of ground ice in near-surface permafrost in relation to vegetation and microtopography at the Taiga-Tundra boundary in the Indigirka River lowlands, northeastern Siberia.


Journal

PloS one
ISSN: 1932-6203
Titre abrégé: PLoS One
Pays: United States
ID NLM: 101285081

Informations de publication

Date de publication:
2019
Historique:
received: 27 03 2019
accepted: 26 09 2019
entrez: 11 10 2019
pubmed: 11 10 2019
medline: 12 3 2020
Statut: epublish

Résumé

The warming trend in the Arctic region is expected to cause drastic changes including permafrost degradation and vegetation shifts. We investigated the spatial distribution of ice content and stable isotopic compositions of water in near-surface permafrost down to a depth of 1 m in the Indigirka River lowlands of northeastern Siberia to examine how the permafrost conditions control vegetation and microtopography in the Taiga-Tundra boundary ecosystem. The gravimetric water content (GWC) in the frozen soil layer was significantly higher at microtopographically high elevations with growing larch trees (i.e., tree mounds) than at low elevations with wetland vegetation (i.e., wet areas). The observed ground ice (ice-rich layer) with a high GWC in the tree mounds suggests that the relatively elevated microtopography of the land surface, which was formed by frost heave, strongly affects the survival of larch trees. The isotopic composition of the ground ice indicated that equilibrium isotopic fractionation occurred during ice segregation at the tree mounds, which implies that the ice formed with sufficient time for the migration of unfrozen soil water to the freezing front. In contrast, the isotopic data for the wet areas indicated that rapid freezing occurred under relatively non-equilibrium conditions, implying that there was insufficient time for ice segregation to occur. The freezing rate of the tree mounds was slower than that of the wet areas due to the difference of such as soil moisture and snow cover depends on vegetation and microtopography. These results indicate that future changes in snow cover, soil moisture, and organic layer, which control underground thermal conductivity, will have significant impacts on the freezing environment of the ground ice at the Taiga-Tundra boundary in northeastern Siberia. Such changes in the freezing environment will then affect vegetation due to changes in the microtopography of the ground surface.

Identifiants

pubmed: 31600327
doi: 10.1371/journal.pone.0223720
pii: PONE-D-19-08723
pmc: PMC6786563
doi:

Substances chimiques

Ice 0
Oxygen Isotopes 0
Soil 0
Water 059QF0KO0R

Types de publication

Journal Article Research Support, Non-U.S. Gov't

Langues

eng

Sous-ensembles de citation

IM

Pagination

e0223720

Déclaration de conflit d'intérêts

The authors have declared that no competing interests exist.

Références

Glob Chang Biol. 2018 Sep;24(9):4225-4237
pubmed: 29569800
PeerJ. 2018 Sep 20;6:e5374
pubmed: 30258705
Glob Chang Biol. 2017 Dec;23(12):5179-5188
pubmed: 28585765
Glob Chang Biol. 2014 Apr;20(4):1264-77
pubmed: 24115456
Science. 1961 May 26;133(3465):1702-3
pubmed: 17814749
Proc Natl Acad Sci U S A. 2011 Sep 6;108(36):14769-74
pubmed: 21852573

Auteurs

Shinya Takano (S)

Graduate School of Environmental Science, Hokkaido University, Sapporo, Japan.

Atsuko Sugimoto (A)

Faculty of Environmental Earth Science, Hokkaido University, Sapporo, Japan.
Arctic Research Center, Hokkaido University, Sapporo, Japan.
Global Station for Arctic Research, Hokkaido University, Sapporo, Japan.
North-Eastern Federal University in Yakutsk, Yakutsk, Sakha, Russia.

Shunsuke Tei (S)

Faculty of Environmental Earth Science, Hokkaido University, Sapporo, Japan.
Arctic Research Center, Hokkaido University, Sapporo, Japan.

Maochang Liang (M)

Graduate School of Environmental Science, Hokkaido University, Sapporo, Japan.

Ryo Shingubara (R)

Graduate School of Environmental Science, Hokkaido University, Sapporo, Japan.

Tomoki Morozumi (T)

Graduate School of Environmental Science, Hokkaido University, Sapporo, Japan.

Trofim C Maximov (TC)

North-Eastern Federal University in Yakutsk, Yakutsk, Sakha, Russia.
Institute for Biological Problems of Cryolithozone, Siberian Branch of the Russian Academy of Sciences, Yakutsk, Sakha, Russia.

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Classifications MeSH