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...

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Bibliographic Details
Published in:Climate of the Past
Main Authors: Keskitalo, Kirsi, Tesi, Tommaso, Bröder, Lisa, Andersson, August, Pearce, Christof, Sköld, Martin, Semiletov, Igor P., Dudarev, Oleg V., Gustafsson, Örjan
Format: Article in Journal/Newspaper
Language:English
Published: 2017
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
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