High biolability of ancient permafrost carbon upon thaw
Ongoing climate warming in the Arctic will thaw permafrost and remobilize substantial terrestrial organic carbon (OC) pools. Around a quarter of northern permafrost OC resides in Siberian Yedoma deposits, the oldest form of permafrost carbon. However, our understanding of the degradation and fate of...
Published in: | Geophysical Research Letters |
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Main Authors: | , , , , , , , , , , , |
Format: | Article in Journal/Newspaper |
Language: | English |
Published: |
2013
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Subjects: | |
Online Access: | https://research.vu.nl/en/publications/74139c22-20c0-4742-8c13-69af259dd233 https://doi.org/10.1002/grl.50348 https://hdl.handle.net/1871.1/74139c22-20c0-4742-8c13-69af259dd233 http://www.scopus.com/inward/record.url?scp=84879969370&partnerID=8YFLogxK http://www.scopus.com/inward/citedby.url?scp=84879969370&partnerID=8YFLogxK |