Massive remobilization of permafrost carbon during post-glacial warming
T. Tesi (),
F. Muschitiello,
R. H. Smittenberg,
M. Jakobsson,
J. E. Vonk,
P. Hill,
A. Andersson,
N. Kirchner,
R. Noormets,
O. Dudarev,
I. Semiletov and
Ö Gustafsson
Additional contact information
T. Tesi: Stockholm University
F. Muschitiello: Bolin Centre for Climate Research, Stockholm University
R. H. Smittenberg: Bolin Centre for Climate Research, Stockholm University
M. Jakobsson: Bolin Centre for Climate Research, Stockholm University
J. E. Vonk: Faculty of Earth and Life Sciences, VU University Amsterdam
P. Hill: University Centre in Svalbard (UNIS)
A. Andersson: Stockholm University
N. Kirchner: Bolin Centre for Climate Research, Stockholm University
R. Noormets: University Centre in Svalbard (UNIS)
O. Dudarev: Pacific Oceanological Institute FEB RAS
I. Semiletov: Pacific Oceanological Institute FEB RAS
Ö Gustafsson: Stockholm University
Nature Communications, 2016, vol. 7, issue 1, 1-10
Abstract:
Abstract Recent hypotheses, based on atmospheric records and models, suggest that permafrost carbon (PF-C) accumulated during the last glaciation may have been an important source for the atmospheric CO2 rise during post-glacial warming. However, direct physical indications for such PF-C release have so far been absent. Here we use the Laptev Sea (Arctic Ocean) as an archive to investigate PF-C destabilization during the last glacial–interglacial period. Our results show evidence for massive supply of PF-C from Siberian soils as a result of severe active layer deepening in response to the warming. Thawing of PF-C must also have brought about an enhanced organic matter respiration and, thus, these findings suggest that PF-C may indeed have been an important source of CO2 across the extensive permafrost domain. The results challenge current paradigms on the post-glacial CO2 rise and, at the same time, serve as a harbinger for possible consequences of the present-day warming of PF-C soils.
Date: 2016
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Persistent link: https://EconPapers.repec.org/RePEc:nat:natcom:v:7:y:2016:i:1:d:10.1038_ncomms13653
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DOI: 10.1038/ncomms13653
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