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This document summarizes a research article that studied how alternative electron acceptors (EAs) like sulfate, nitrate, ferric iron, manganic iron, and oxygen affect methane-producing and methane-consuming microbes in sediments from two boreal lakes. The study found that populations of archaea and bacteria capable of anaerobic methane oxidation were low, likely due to the shallow depths of the lakes. As a result, rates of potential anaerobic methane oxidation were low and not enhanced by EAs. Instead, incr

Author

Kniat Taink

Language

EN