INTRODUCTIONAnaerobic microorganisms play a major role in the global carbon cycle by remineralizing the large quantities of organic matter which enter anoxic marine and freshwater environments. Methane and CO2 are the end products of anaerobic decomposition, which occurs in a diversity of habitats, such as the rumens of ruminant animals, the lower intestinal tracts of humans, sewage digesters, landfills, rice paddies, and the sediments of freshwater lakes and rivers. Most of the methane released is oxidized to CO2 by the strictly aerobic methanotrophs; however, a significant proportion escapes into the upper atmosphere where methane has a major role in the greenhouse effect.The methanogenic decomposition of organic matter requires microbial consortia composed of at least three interacting metabolic groups of anaerobes. The fermentative bacteria degrade polymers to H2, CO2, formate, acetate, and higher volatile carboxylic acids. The acetogenic bacteria then oxidize the higher acids to acetate and either H2 or formate. The strictly anaerobic methane-producing microorganisms are the final group in the consortia and utilize H2, formate, and acetate as substrates for growth. Methane producers represent the largest and most diverse group within the Archaea domain (57). The reader is referred to reviews that describe general aspects of the methanogenic members of the Archaea domain (32, 56).About two-thirds of the methane produced in nature originates from the methyl group of acetate, and about one-third originates from the reduction of CO2 with electrons derived from the oxidation of H2 or formate. Two independent pathways exist for the conversion of acetate and reduction of CO2. The pathway of CO2 reduction to methane has been studied extensively over the past 20 years and is the subject of several reviews (9,34,51,55); however, a fundamental understanding of methanogenesis from acetate has emerged only recently.Most acetate-utilizing anaerobes from the Bacteria domain cleave acetyl coenzyme A (acetyl-CoA) and oxidize the methyl and carbonyl groups completely to CO2, reducing a variety of electron acceptors (52). In contrast, the methanogenic members of the Archaea domain carry out a fermentation of acetate in which the molecule is cleaved and the methyl group is reduced to methane with electrons derived from oxidation of the carbonyl group to CO2 (reaction 1).