Sources and characteristics of terrestrial carbon in Holocene-scale sediments of the East Siberian Sea
Thawing of permafrost carbon (PF-C) due to climate warming can remobilise considerable amounts of terrestrial carbon from its long-term storage to the marine environment. PF-C can be then be buried in sediments or remineralised to CO2 with implications for the carbon-climate feedback. Studying histo...
Published in: | Climate of the Past |
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Main Authors: | , , , , , , , , |
Format: | Article in Journal/Newspaper |
Language: | English |
Published: |
2017
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Subjects: | |
Online Access: | https://research.vu.nl/en/publications/20036252-e74b-4ae6-84cf-11c2bb89c50d https://doi.org/10.5194/cp-13-1213-2017 https://hdl.handle.net/1871.1/20036252-e74b-4ae6-84cf-11c2bb89c50d http://www.scopus.com/inward/record.url?scp=85029945259&partnerID=8YFLogxK http://www.scopus.com/inward/citedby.url?scp=85029945259&partnerID=8YFLogxK |