Proceedings of the National Academy of Sciences · 2023 · 25 citations · 28 references
Life SciencesMarine BiologyMicrobiologyMarine MicrobiologyMetagenomicsMicrobial EcologyAnaerobic MetabolismGreenhouse Gas ProductionMarine Microbial MetabolismMarine Microbial PhysiologyMicrobial GrowthMicrobial RespirationAnaerobic MethanogenesisBiochemical CharacterizationMethanogenesisMethanogenesis PathwaysMethanotrophic SymbiosisMethanotrophySulfate-reducing BacteriaSulfate-reducing Microorganisms
Anaerobic marine environments are the third largest producer of the greenhouse gas methane. The release to the atmosphere is prevented by anaerobic ‘methanotrophic archaea (ANME) dependent on a symbiotic association with sulfate-reducing bacteria or direct reduction of metal oxides. Metagenomic analyses of ANME are consistent with a reverse methanogenesis pathway, although no wild-type isolates have been available for validation and biochemical investigation. Herein is reported the characterization of methanotrophic growth for the diverse marine methanogens Methanosarcina acetivorans C2A and Methanococcoides orientis sp. nov. Growth was dependent on reduction of either ferrihydrite or humic acids revealing a respiratory mode of energy conservation. Acetate and/or formate were end products. Reversal of the well-characterized methanogenic pathways is remarkably like the consensus pathways for uncultured ANME based on extensive metagenomic analyses.
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Manganese- and Iron-Dependent Marine Methane Oxidation
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Artificial electron acceptors decouple archaeal methane oxidation from sulfate reduction
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