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Temperature limitation of methanogenesis in aquatic sediments

Journal Article · · Appl. Environ. Microbiol.; (United States)
OSTI ID:5277811

Microbial methane formation in Lake Mendota (southern Wisconsin) is greatly influenced by temperature, according to an investigation of the microbial ecology of methanogenesis in the lake. The results support other findings that bacterial decomposition processes in aquatic sediments are temperature-limited. Sediments were taken at depths of 5, 10, and 18 m. Methanogenesis varied with respect to sediment site and depth, sampling date, in situ temperatures and number of methanogens. Increased numbers of methanogenic bacteria and rates of methanogenesis correlated with increased sediment temperature during seasonal change, with the greatest methanogenic activity observed for 18-m sediments throughout the sampling year. As compared with shallower sediments, 18-m was removed from oxygenation effects and contained higher amounts of ammonia, carbonate and methanogenic bacteria, and the population density of methanogens fluctuated less during seasonal change. It is thought that in any future comparative studies that aim to establish the rates of anaerobic carbon decomposition or to define in situ carbon precursors and mirobial interactions associated with methanogenesis must employ sediments nearly identical with respect to sample site and depth, to date of collection and processing, and to in vitro experimental conditions including anaeobiosis and length and temperature of incubation.

OSTI ID:
5277811
Journal Information:
Appl. Environ. Microbiol.; (United States), Journal Name: Appl. Environ. Microbiol.; (United States) Vol. 31:1; ISSN AEMID
Country of Publication:
United States
Language:
English