Massive remobilization of permafrost carbon during post-glacial warming
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 CO 2 rise during post-glacial warming. However, direct physical indications for such PF-C release have so far...
Published in: | Nature Communications |
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Main Authors: | , , , , , , , , , , , |
Format: | Article in Journal/Newspaper |
Language: | English |
Published: |
2016
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Subjects: | |
Online Access: | https://research.vu.nl/en/publications/e0dfa8b0-9cc9-416c-95ba-06a84346bda5 https://doi.org/10.1038/ncomms13653 https://hdl.handle.net/1871.1/e0dfa8b0-9cc9-416c-95ba-06a84346bda5 http://www.scopus.com/inward/record.url?scp=84999836703&partnerID=8YFLogxK http://www.scopus.com/inward/citedby.url?scp=84999836703&partnerID=8YFLogxK |
Summary: | 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 CO 2 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 CO 2 across the extensive permafrost domain. The results challenge current paradigms on the post-glacial CO 2 rise and, at the same time, serve as a harbinger for possible consequences of the present-day warming of PF-C soils. |
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