Abstract
The role of anaerobic CH
4 oxidation in controlling lake sediment CH
4 emissions remains unclear. Therefore, we tested how relevant EAs (SO
42−, NO
3−, Fe
3+, Mn
4+, O
2) affect CH
4 production and oxidation in the sediments of two shallow boreal lakes. The changes induced to microbial communities by the addition of Fe
3+ and Mn
4+ were studied using next-generation sequencing targeting the 16S rRNA and methyl-coenzyme M reductase (
mcrA) genes and
mcrA transcripts. Putative anaerobic CH
4 oxidizing archaea (ANME-2D) and bacteria (
NC 10) were scarce (up to 3.4% and 0.5% of archaeal and bacterial 16S rRNA genes, respectively), likely due to the low environmental stability associated with shallow depths. Consequently, the potential anaerobic CH
4 oxidation (0–2.1 nmol g
−1dry weight (DW)d
−1) was not enhanced by the addition of EAs, nor important in consuming the produced CH
4 (0.6–82.5 nmol g
−1DWd
−1). Instead, the increased EA availability suppressed CH
4 production via the outcompetition of methanogens by anaerobically respiring bacteria and via the increased protection of organic matter from microbial degradation induced by Fe
3+ and Mn
4+. Future studies could particularly assess whether anaerobic CH
4 oxidation has any ecological relevance in reducing CH
4 emissions from the numerous CH
4-emitting shallow lakes in boreal and tundra landscapes.
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