Ubiquitous and significant anaerobic oxidation of methane in freshwater lake sediments.

Abstract Anaerobic oxidation of methane (AOM) is a microbial process that consumes dissolved methane (CH 4) in anoxic sediments and soils and mitigates CH 4 release to the atmosphere. The degree to which AOM limits global biospheric CH 4 emissions is not fully understood. In marine sediments, where the process was first described, AOM is responsible for oxidizing >90% of the CH 4 produced. More recently, AOM has been observed in soils, peatlands, and freshwater ecosystems. In lakes, where sediment anoxia, organic carbon turnover, and CH 4 production are common, AOM is not well studied but could represent a significant CH 4 sink and constraint on emissions. Here, we present evidence for the occurrence of AOM in the sediment of thirteen lakes that span a global climatic and trophic gradient. We further quantified and modeled AOM patterns and studied potential microbial controls of AOM using laboratory incubations of sediment and stable isotope measurements in three of the thirteen lakes. We demonstrate that AOM is widespread in freshwater lake sediments and accounts for 29%–34% (95% confidence interval) of the mean total CH 4 produced in surface and near-surface lake sediments. Graphical abstract Image 1 Highlights • Anaerobic oxidation of methane (AOM) was observed in 13 of 14 study lake sediments. • AOM profile was further established in the sediments of three lakes. • AOM ranged from 12 to 87% of the methane produced in the lake sediments. • We conclude that AOM is ubiquitous and reduces largely methane emissions from lakes. [ABSTRACT FROM AUTHOR]