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: Copernicus Publications 2017
Subjects:
Online Access:https://doi.org/10.5194/cp-13-1213-2017
https://noa.gwlb.de/receive/cop_mods_00008644
https://noa.gwlb.de/servlets/MCRFileNodeServlet/cop_derivate_00008601/cp-13-1213-2017.pdf
https://cp.copernicus.org/articles/13/1213/2017/cp-13-1213-2017.pdf