Massive remobilization of permafrost carbon during post-glacial warming

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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 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 destabil...

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Effects of experimental warming of air, soil and permafrost on carbon balance in Alaskan tundra

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ژورنال

عنوان ژورنال: Nature Communications

سال: 2016

ISSN: 2041-1723

DOI: 10.1038/ncomms13653