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Title: Terminal processes in the anaerobic degradation of an algal-bacterial mat in a high-sulfate hot spring

Journal Article · · Appl. Environ. Microbiol.; (United States)
OSTI ID:7001706

The algal-bacterial mat of a high-sulfate hot spring (Bath Lake) provided an environment in which to compare terminal processes involved in anaerobic decomposition. Sulfate reduction was found to dominate methane production, as indicated by comparison of initial electron flow through the two processes, rapid conversion of (2-/sup 14/C)acetate to /sup 14/CO/sub 2/ and not to /sup 14/CH/sub 4/, and the lack of rapid reduction of NaH/sup 14/CO/sub 3/ to /sup 14/CH/sub 4/. Sulfate reduction was the dominant process at all depth intervals, but a marked decrease of sulfate reduction and sulfate-reducing bacteria was observed with depth. Concurrent methanogenesis was indicated by the presence of viable methanogenic bacteria and very low but detectable rates of methane production. A marked increase in methane production was observed after sulfate depletion despite high concentrations of sulfide (>1.25 mM), indicating that methanogenesis was not inhibited by sulfide in the natural environment. Although a sulfate minimum and sulfide maximum occurred in the region of maximal sulfate reduction, the absence of sulfate depletion in interstitial water suggests that methanogenesis is always severely limited in Bath Lake sediments. Low initial methanogenesis was not due to anaerobic methane oxidation.

Research Organization:
Montana State Univ., Bozeman
OSTI ID:
7001706
Journal Information:
Appl. Environ. Microbiol.; (United States), Vol. 40:1
Country of Publication:
United States
Language:
English