Anaerobic oxidation of ethane by archaea from a marine hydrocarbon seep
Song-Can Chen,
Niculina Musat,
Oliver J. Lechtenfeld,
Heidrun Paschke,
Matthias Schmidt,
Nedal Said,
Denny Popp,
Federica Calabrese,
Hryhoriy Stryhanyuk,
Ulrike Jaekel,
Yong-Guan Zhu,
Samantha B. Joye,
Hans-Hermann Richnow,
Friedrich Widdel and
Florin Musat ()
Additional contact information
Song-Can Chen: Helmholtz Centre for Environmental Research – UFZ
Niculina Musat: Helmholtz Centre for Environmental Research – UFZ
Oliver J. Lechtenfeld: Helmholtz Centre for Environmental Research – UFZ
Heidrun Paschke: Helmholtz Centre for Environmental Research – UFZ
Matthias Schmidt: Helmholtz Centre for Environmental Research – UFZ
Nedal Said: Helmholtz Centre for Environmental Research – UFZ
Denny Popp: Helmholtz Centre for Environmental Research – UFZ
Federica Calabrese: Helmholtz Centre for Environmental Research – UFZ
Hryhoriy Stryhanyuk: Helmholtz Centre for Environmental Research – UFZ
Ulrike Jaekel: Max Planck Institute for Marine Microbiology
Yong-Guan Zhu: Chinese Academy of Sciences
Samantha B. Joye: University of Georgia
Hans-Hermann Richnow: Helmholtz Centre for Environmental Research – UFZ
Friedrich Widdel: Max Planck Institute for Marine Microbiology
Florin Musat: Helmholtz Centre for Environmental Research – UFZ
Nature, 2019, vol. 568, issue 7750, 108-111
Abstract:
Abstract Ethane is the second most abundant component of natural gas in addition to methane, and—similar to methane—is chemically unreactive. The biological consumption of ethane under anoxic conditions was suggested by geochemical profiles at marine hydrocarbon seeps1–3, and through ethane-dependent sulfate reduction in slurries4–7. Nevertheless, the microorganisms and reactions that catalyse this process have to date remained unknown8. Here we describe ethane-oxidizing archaea that were obtained by specific enrichment over ten years, and analyse these archaea using phylogeny-based fluorescence analyses, proteogenomics and metabolite studies. The co-culture, which oxidized ethane completely while reducing sulfate to sulfide, was dominated by an archaeon that we name ‘Candidatus Argoarchaeum ethanivorans’; other members were sulfate-reducing Deltaproteobacteria. The genome of Ca. Argoarchaeum contains all of the genes that are necessary for a functional methyl-coenzyme M reductase, and all subunits were detected in protein extracts. Accordingly, ethyl-coenzyme M (ethyl-CoM) was identified as an intermediate by liquid chromatography–tandem mass spectrometry. This indicated that Ca. Argoarchaeum initiates ethane oxidation by ethyl-CoM formation, analogous to the recently described butane activation by ‘Candidatus Syntrophoarchaeum’9. Proteogenomics further suggests that oxidation of intermediary acetyl-CoA to CO2 occurs through the oxidative Wood–Ljungdahl pathway. The identification of an archaeon that uses ethane (C2H6) fills a gap in our knowledge of microorganisms that specifically oxidize members of the homologous alkane series (CnH2n+2) without oxygen. Detection of phylogenetic and functional gene markers related to those of Ca. Argoarchaeum at deep-sea gas seeps10–12 suggests that archaea that are able to oxidize ethane through ethyl-CoM are widespread members of the local communities fostered by venting gaseous alkanes around these seeps.
Date: 2019
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DOI: 10.1038/s41586-019-1063-0
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