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: |
Copernicus Publications
2017
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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 |