Biogenic volatile release from permafrost thaw is determined by the soil microbial sink

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Increased nitrous oxide emissions from Arctic peatlands after permafrost thaw.

Permafrost in the Arctic is thawing, exposing large carbon and nitrogen stocks for decomposition. Gaseous carbon release from Arctic soils due to permafrost thawing is known to be substantial, but growing evidence suggests that Arctic soils may also be relevant sources of nitrous oxide (N2O). Here we show that N2O emissions from subarctic peatlands increase as the permafrost thaws. In our study...

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ژورنال

عنوان ژورنال: Nature Communications

سال: 2018

ISSN: 2041-1723

DOI: 10.1038/s41467-018-05824-y