Remobilization of Old Permafrost Carbon to Chukchi Sea Sediments During the End of the Last Deglaciation

Climate warming is expected to destabilize permafrost carbon (PF‐C) by thaw‐erosion and deepening of the seasonally thawed active layer and thereby promote PF‐C mineralization to CO(2) and CH(4). A similar PF‐C remobilization might have contributed to the increase in atmospheric CO(2) during deglaci...

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Detalles Bibliográficos
Autores principales: Martens, Jannik, Wild, Birgit, Pearce, Christof, Tesi, Tommaso, Andersson, August, Bröder, Lisa, O'Regan, Matt, Jakobsson, Martin, Sköld, Martin, Gemery, Laura, Cronin, Thomas M., Semiletov, Igor, Dudarev, Oleg V., Gustafsson, Örjan
Formato: Online Artículo Texto
Lenguaje:English
Publicado: John Wiley and Sons Inc. 2019
Materias:
Research Articles
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC6472570/
https://www.ncbi.nlm.nih.gov/pubmed/31007381
http://dx.doi.org/10.1029/2018GB005969

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC6472570/
https://www.ncbi.nlm.nih.gov/pubmed/31007381
http://dx.doi.org/10.1029/2018GB005969

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