Permafrost-carbon mobilization in Beringia caused by deglacial meltwater runoff, sea-level rise and warming

During the last deglaciation (18–8 kyr BP), shelf flooding and warming presumably led to a large-scale decomposition of permafrost soils in the mid-to-high latitudes of the Northern Hemisphere. Microbial degradation of old organic matter released from the decomposing permafrost potentially contribut...

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Detalles Bibliográficos

Principais autores:	Vera D Meyer, Jens Hefter, Peter Köhler, Ralf Tiedemann, Rainer Gersonde, Lukas Wacker, Gesine Mollenhauer
Formato:	Artigo
Idioma:	Inglês
Publicado:	IOP Publishing 2019-01-01
Series:	Environmental Research Letters
Assuntos:	deglaciation permafrost decomposition Beringia Bering Sea biomarker atmospheric CO2 open climate campaign
Acceso en liña:	https://doi.org/10.1088/1748-9326/ab2653
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