Low photolability of yedoma permafrost dissolved organic carbon

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Degradation potentials of dissolved organic carbon (DOC) from thawed permafrost peat

Global warming can substantially affect the export of dissolved organic carbon (DOC) from peat-permafrost to aquatic systems. The direct degradability of such peat-derived DOC, however, is poorly constrained because previous permafrost thaw studies have mainly addressed mineral soil catchments or DOC pools that have already been processed in surface waters. We incubated peat cores from a palsa ...

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Uranium isotopes and dissolved organic carbon in loess permafrost: modeling the age of ancient ice

The residence time of ice in permafrost is an indicator of past climate history, and of the resilience and vulnerability of high-latitude ecosystems to global change. Development of geochemical indicators of ground-ice residence times in permafrost will advance understanding of the circumstances and evidence of permafrost formation, preservation, and thaw in response to climate warming and othe...

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The deep permafrost carbon pool of the Yedoma region in Siberia and Alaska

[1] Estimates for circumpolar permafrost organic carbon (OC) storage suggest that this pool contains twice the amount of current atmospheric carbon. The Yedoma region sequestered substantial quantities of OC and is unique because its deep OC, which was incorporated into permafrost during ice age conditions. Rapid inclusion of labile organic matter into permafrost halted decomposition and result...

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ژورنال

عنوان ژورنال: Journal of Geophysical Research: Biogeosciences

سال: 2017

ISSN: 2169-8953

DOI: 10.1002/2016jg003688