Author
Listed:
- Rafael Laso-Pérez
(Max-Planck Institute for Marine Microbiology
Alfred Wegener Institute Helmholtz Center for Polar and Marine Research)
- Gunter Wegener
(Max-Planck Institute for Marine Microbiology
Alfred Wegener Institute Helmholtz Center for Polar and Marine Research
MARUM, Center for Marine Environmental Sciences, University Bremen)
- Katrin Knittel
(Max-Planck Institute for Marine Microbiology)
- Friedrich Widdel
(Max-Planck Institute for Marine Microbiology)
- Katie J. Harding
(Max-Planck Institute for Marine Microbiology
†Present address: University of California at Santa Cruz, Ocean Sciences Department, Santa Cruz, California 95064, USA.)
- Viola Krukenberg
(Max-Planck Institute for Marine Microbiology
Alfred Wegener Institute Helmholtz Center for Polar and Marine Research)
- Dimitri V. Meier
(Max-Planck Institute for Marine Microbiology)
- Michael Richter
(Max-Planck Institute for Marine Microbiology)
- Halina E. Tegetmeyer
(Alfred Wegener Institute Helmholtz Center for Polar and Marine Research
Center for Biotechnology, Bielefeld University)
- Dietmar Riedel
(Max Planck Institute for Biophysical Chemistry)
- Hans-Hermann Richnow
(Helmholtz Centre for Environmental Research − UFZ)
- Lorenz Adrian
(Helmholtz Centre for Environmental Research − UFZ)
- Thorsten Reemtsma
(Helmholtz Centre for Environmental Research − UFZ)
- Oliver J. Lechtenfeld
(Helmholtz Centre for Environmental Research − UFZ)
- Florin Musat
(Max-Planck Institute for Marine Microbiology
Helmholtz Centre for Environmental Research − UFZ)
Abstract
The anaerobic formation and oxidation of methane involve unique enzymatic mechanisms and cofactors, all of which are believed to be specific for C1-compounds. Here we show that an anaerobic thermophilic enrichment culture composed of dense consortia of archaea and bacteria apparently uses partly similar pathways to oxidize the C4 hydrocarbon butane. The archaea, proposed genus ‘Candidatus Syntrophoarchaeum’, show the characteristic autofluorescence of methanogens, and contain highly expressed genes encoding enzymes similar to methyl-coenzyme M reductase. We detect butyl-coenzyme M, indicating archaeal butane activation analogous to the first step in anaerobic methane oxidation. In addition, Ca. Syntrophoarchaeum expresses the genes encoding β-oxidation enzymes, carbon monoxide dehydrogenase and reversible C1 methanogenesis enzymes. This allows for the complete oxidation of butane. Reducing equivalents are seemingly channelled to HotSeep-1, a thermophilic sulfate-reducing partner bacterium known from the anaerobic oxidation of methane. Genes encoding 16S rRNA and methyl-coenzyme M reductase similar to those identifying Ca. Syntrophoarchaeum were repeatedly retrieved from marine subsurface sediments, suggesting that the presented activation mechanism is naturally widespread in the anaerobic oxidation of short-chain hydrocarbons.
Suggested Citation
Rafael Laso-Pérez & Gunter Wegener & Katrin Knittel & Friedrich Widdel & Katie J. Harding & Viola Krukenberg & Dimitri V. Meier & Michael Richter & Halina E. Tegetmeyer & Dietmar Riedel & Hans-Hermann, 2016.
"Thermophilic archaea activate butane via alkyl-coenzyme M formation,"
Nature, Nature, vol. 539(7629), pages 396-401, November.
Handle:
RePEc:nat:nature:v:539:y:2016:i:7629:d:10.1038_nature20152
DOI: 10.1038/nature20152
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