Consistent microbial responses during the aerobic thaw of Alaskan permafrost soils.

ABSTRACT: Arctic systems are warming at four times the global average, causing permafrost-permanently frozen soil, ice, organic matter, and bedrock-to thaw. Permafrost thaw exposes previously unavailable soil carbon and nutrients to decomposition-a process mediated by microbes-which releases greenhouse gases such as carbon dioxide and methane into the atmosphere. While it is well established that thaw alters the composition and function of the permafrost microbiome, patterns revealing common responses to thaw across different permafrost soil types have not yet emerged. In this study, we address how permafrost thaw impacts microbiome diversity, alters species abundance, and contributes to carbon flux in the Arctic. We sampled peat-like, mineral, and organic-mineral permafrost from three locations in

SUBMITTER: O'Brien JM 

PROVIDER: S-EPMC12643468 | biostudies-literature | 2025

REPOSITORIES: biostudies-literature