| Autor: |
Su G; Department of Environmental Sciences, University of Basel, Basel, Switzerland., Zopfi J; Department of Environmental Sciences, University of Basel, Basel, Switzerland., Niemann H; Department of Environmental Sciences, University of Basel, Basel, Switzerland.; Department of Marine Microbiology and Biogeochemistry, NIOZ Royal Institute for Sea Research, Texel, Netherlands.; Department of Earth Sciences, Faculty of Geosciences, Utrecht University, Utrecht, Netherlands., Lehmann MF; Department of Environmental Sciences, University of Basel, Basel, Switzerland. |
| Jazyk: |
angličtina |
| Zdroj: |
Frontiers in microbiology [Front Microbiol] 2022 May 09; Vol. 13, pp. 864630. Date of Electronic Publication: 2022 May 09 (Print Publication: 2022). |
| DOI: |
10.3389/fmicb.2022.864630 |
| Abstrakt: |
Freshwater lakes represent an important source of the potent greenhouse gas methane (CH 4 ) to the atmosphere. Methane emissions are regulated to large parts by aerobic (MOx) and anaerobic (AOM) oxidation of methane, which are important CH 4 sinks in lakes. In contrast to marine benthic environments, our knowledge about the modes of AOM and the related methanotrophic microorganisms in anoxic lake sediments is still rudimentary. Here, we demonstrate the occurrence of AOM in the anoxic sediments of Lake Sempach (Switzerland), with maximum in situ AOM rates observed within the surface sediment layers in presence of multiple groups of methanotrophic bacteria and various oxidants known to support AOM. However, substrate-amended incubations (with NO 2 - , NO 3 - , SO 4 2- , Fe-, and Mn-oxides) revealed that none of the electron acceptors previously reported to support AOM enhanced methane turnover in Lake Sempach sediments under anoxic conditions. In contrast, the addition of oxygen to the anoxic sediments resulted in an approximately 10-fold increase in methane oxidation relative to the anoxic incubations. Phylogenetic and isotopic evidence indicate that both Type I and Type II aerobic methanotrophs were growing on methane under both oxic and anoxic conditions, although methane assimilation rates were an order of magnitude higher under oxic conditions. While the anaerobic electron acceptor responsible for AOM could not be identified, these findings expand our understanding of the metabolic versatility of canonically aerobic methanotrophs under anoxic conditions, with important implications for future investigations to identify methane oxidation processes. Bacterial AOM by facultative aerobic methane oxidizers might be of much larger environmental significance in reducing methane emissions than previously thought.
Competing Interests: The authors declare that the research was conducted in the absence of any commercial or financial relationships that could be construed as a potential conflict of interest.
(Copyright © 2022 Su, Zopfi, Niemann and Lehmann.) |
| Databáze: |
MEDLINE |
| Externí odkaz: |
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