Back flux during anaerobic oxidation of butane supports archaea-mediated alkanogenesis

Microbial formation and oxidation of volatile alkanes in anoxic environments significantly impacts biogeochemical cycles on Earth. The discovery of archaea oxidizing volatile alkanes via deeply branching methyl-coenzyme M reductase variants, dubbed alkyl-CoM reductases (ACR), prompted the hypothesis of archaea-catalysed alkane formation in nature (alkanogenesis). A combination of metabolic modelling, anaerobic physiology assays, and isotope labeling of Candidatus Syntrophoarchaeum archaea catalyzing the anaerobic oxidation of butane (AOB) show a back flux of CO<sub>2</sub> to butane, demonstrating reversibility of the entire AOB pathway. Back fluxes correlate with thermodynamics and kinetics of the archaeal catabolic system. AOB reversibility supports a biological formation of butane, and generally of higher volatile alkanes, helping to explain the presence of isotopically light alkanes and deeply branching ACR genes in sedimentary basins isolated from gas reservoirs.

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Publication Details

Journal
Nature Communications
Published
2024-11-07
DOI
https://doi.org/10.1038/s41467-024-53932-9
Citations
3
Primary Topic
Microbial Community Ecology and Physiology
Type
article
Field-Weighted Citation Impact
1.38

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article

Back flux during anaerobic oxidation of butane supports archaea-mediated alkanogenesis

Hans H. Richnow, Song‐Can Chen, Oliver Jens Lechtenfeld, Steffen Kümmel et al.
3 citations
Nature Communications
Microbial Community Ecology and Physiology
1.38
article

Back flux during anaerobic oxidation of butane supports archaea-mediated alkanogenesis

Hans H. Richnow, Song‐Can Chen, Oliver Jens Lechtenfeld, Steffen Kümmel, Niculina Musat, Florin Musat, Alexis Gilbert, Jiaheng Ji, M. Lund, Sheng Chen
article en
3 citations

Abstract

Microbial formation and oxidation of volatile alkanes in anoxic environments significantly impacts biogeochemical cycles on Earth. The discovery of archaea oxidizing volatile alkanes via deeply branching methyl-coenzyme M reductase variants, dubbed alkyl-CoM reductases (ACR), prompted the hypothesis of archaea-catalysed alkane formation in nature (alkanogenesis). A combination of metabolic modelling, anaerobic physiology assays, and isotope labeling of Candidatus Syntrophoarchaeum archaea catalyzing the anaerobic oxidation of butane (AOB) show a back flux of CO<sub>2</sub> to butane, demonstrating reversibility of the entire AOB pathway. Back fluxes correlate with thermodynamics and kinetics of the archaeal catabolic system. AOB reversibility supports a biological formation of butane, and generally of higher volatile alkanes, helping to explain the presence of isotopically light alkanes and deeply branching ACR genes in sedimentary basins isolated from gas reservoirs.

Nature CommunicationsVol. 15(1)
Tokyo Institute of Technology (JP), University of Vienna (AT), Helmholtz Centre for Environmental Research (DE), Aarhus University (DK), Beijing Normal University (CN), Babeș-Bolyai University (RO), Zhejiang University (CN)
European Commission, National Natural Science Foundation of China, Beijing Normal University, Novo Nordisk, Helmholtz-Zentrum für Umweltforschung, Novo Nordisk Fonden, European Regional Development Fund, H2020 Marie Skłodowska-Curie Actions
Life below water
Openalex Percentile: Top 18%
Microbial Community Ecology and Physiology
1.38
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