Methanogenesis in marine sediments.
The anaerobic conversion of complex organic matter to CH(4) is an essential link in the global carbon cycle. In freshwater anaerobic environments, the organic matter is decomposed to CH(4) and CO(2) by a microbial food chain that terminates with methanogens that produce methane primarily by reduction of the methyl group of acetate and also reduction of CO(2). The process also occurs in marine environments, particularly those receiving large loads of organic matter, such as coastal sediments. The great majority of research on methanogens has focused on marine and freshwater CO(2)-reducing species, and freshwater acetate-utilizing species. Recent molecular, biochemical, bioinformatic, proteomic, and microarray analyses of the marine isolate Methanosarcina acetivorans has revealed that the pathway for acetate conversion to methane differs significantly from that in freshwater methanogens. Similar experimental approaches have also revealed striking contrasts with freshwater species for the pathway of CO-dependent CO(2) reduction to methane by M. acetivorans. The differences in both pathways reflect an adaptation by M. acetivorans to the marine environment.
Ferry
James G
JG
Department of Biochemistry and Molecular Biology, The Pennsylvania State University, University Park, PA 16802, USA. jgf3@psu.edu
Lessner
Daniel J
DJ
D000085:Acetates / Q000378:metabolism*; D000693:Anaerobiosis; D019015:Geologic Sediments / Q000382:microbiology*; D008697:Methane / Q000378:metabolism*; D017020:Methanosarcina / Q000378:metabolism*; D008954:Models, Biological; D012623:Seawater / Q000382:microbiology*
D000085:Acetates; D008697:Methane