Aerobic bacterial methane synthesis

Reports of biogenic methane (CH₄) synthesis associated with a range of organisms have steadily accumulated in the literature. This has not happened without controversy and in most cases the process is poorly understood at the gene and enzyme levels. In marine and freshwater environments, CH₄ supersa...

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Veröffentlicht in:Proceedings of the National Academy of Sciences - PNAS 2021-07, Vol.118 (27), p.1-9
Hauptverfasser: Wang, Qian, Alowaifeer, Abdullah, Kerner, Patricia, Balasubramanian, Narayanaganesh, Patterson, Angela, Christian, William, Tarver, Angela, Dore, John E., Hatzenpichler, Roland, Bothner, Brian, McDermott, Timothy R.
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Sprache:eng
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Zusammenfassung:Reports of biogenic methane (CH₄) synthesis associated with a range of organisms have steadily accumulated in the literature. This has not happened without controversy and in most cases the process is poorly understood at the gene and enzyme levels. In marine and freshwater environments, CH₄ supersaturation of oxic surface waters has been termed the “methane paradox” because biological CH₄ synthesis is viewed to be a strictly anaerobic process carried out by O₂-sensitive methanogens. Interest in this phenomenon has surged within the past decade because of the importance of understanding sources and sinks of this potent greenhouse gas. In our work on Yellowstone Lake in Yellowstone National Park, we demonstrate microbiological conversion of methylamine to CH₄ and isolate and characterize an Acidovorax sp. capable of this activity. Furthermore, we identify and clone a gene critical to this process (encodes pyridoxylamine phosphate-dependent aspartate aminotransferase) and demonstrate that this property can be transferred to Escherichia coli with this gene and will occur as a purified enzyme. This previously unrecognized process sheds light on environmental cycling of CH₄, suggesting that O₂-insensitive, ecologically relevant aerobic CH₄ synthesis is likely of widespread distribution in the environment and should be considered in CH₄ modeling efforts.
ISSN:0027-8424
1091-6490
DOI:10.1073/pnas.2019229118