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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Библиографические подробности
Опубликовано в: :Global Biogeochem Cycles
Главные авторы: 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
Формат: Artigo
Язык:Inglês
Опубликовано: John Wiley and Sons Inc. 2019
Предметы:
Research Articles
Online-ссылка:https://ncbi.nlm.nih.gov/pmc/articles/PMC6472570/
https://ncbi.nlm.nih.gov/pubmed/31007381
https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1029/2018GB005969
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