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Substrates for sulfate reduction and methane production in intertidal sediments

Journal Article · · Appl. Environ. Microbiol.; (United States)
OSTI ID:5742712
The activity of and potential substrates for methane-producing bacteria and sulfate-reducing bacteria were examined in marsh, estuary, and beach intertidal sediments. Slow rates of methane production were detected in all sediments, although rates of sulfate reduction were 100- to 1,000-fold higher. After sulfate was depleted in sediments, the rates of methane production sharply increased. The addition of methylamine stimulated methanogenesis in the presence of sulfate, and (/sup 14/C)methylamine was rapidly converted to /sup 14/CH/sub 4/ and /sup 14/CO/sub 2/ in freshly collected marsh sediment. Acetate, hydrogen, or methionine additions did not stimulate methanogenesis. (methyl-/sup 14/C)methionine and (2-/sup 14/C)acetate were converted to /sup 14/CO/sub 2/ and not to /sup 14/CH/sub 4/ in fresh sediment. No reduction of /sup 14/CO/sub 2/ to /sup 14/CH/sub 4/ occurred in fresh sediment. Molybdate, an inhibitor of sulfate reduction, inhibited (2-/sup 14/C)acetate metabolism by 98.5%. Fluoracetate, an inhibitor of acetate metabolism, inhibited sulfate reduction by 61%. These results suggest that acetate is a major electron donor for sulfate reduction in marine sediments. In the presence of high concentrations of sulfate, methane may be derived from novel substrates such as methylamine.
Research Organization:
Montana State Univ., Bozeman
OSTI ID:
5742712
Journal Information:
Appl. Environ. Microbiol.; (United States), Journal Name: Appl. Environ. Microbiol.; (United States) Vol. 45:1; ISSN AEMID
Country of Publication:
United States
Language:
English