Methane production controls in a young thermokarst lake formed by abrupt permafrost thaw.

ABSTRACT: Methane (CH₄ ) release to the atmosphere from thawing permafrost contributes significantly to global CH₄ emissions. However, constraining the effects of thaw that control the production and emission of CH₄ is needed to anticipate future Arctic emissions. Here are presented robust rate measurements of CH₄ production and cycling in a region of rapidly degrading permafrost. Big Trail Lake, located in central Alaska, is a young, actively expanding thermokarst lake. The lake was investigated by taking two 1 m cores of sediment from different regions. Two independent methods of measuring microbial CH₄  production, long term (CH₄ accumulation) and short term (¹⁴ C tracer), produced similar average rates of 11 ± 3.5 and 9

SUBMITTER: Pellerin A 

PROVIDER: S-EPMC9310722 | biostudies-literature | 2022 May

REPOSITORIES: biostudies-literature