Many anaerobic bacteria can completely oxidize organic matter to C 0 2 with either sulfur, sulfate, or protons as electron acceptor. The sulfur-reducing bacteria and one genus of sulfate reducers use a modified citric-acid cycle with a novel anaplerotic sequence as pathway of terminal respiration. All other anaerobes use an alternative pathway, in which carbon monoxide dehydrogenase is a key enzyme and in which acetyl-CoA is cleaved into two C1 units at the oxidation level of CH30H and CO. Thus almost 50 years after the discovery of the citric acid cycle by Hans Krebs in 1937, a second pathway for acetyl-CoA oxidation was found.1987 marked the 50th anniversary of the discovery of the citric acid cycle. In 1937 Hans Krebs summarized the evidence for a cyclic sequence of reactions that explained the complete oxidation, by pigeon breast muscle, of an unidentified 'triose' derived from glycolysis. The paper was entitled " [11][12][13][14], and intracellular organization [15, 161. The book contains excellent up-to-date treatises of these topics which therefore will not be dealt within the following review.Until recently it was believed that the citric acid cycle operates only in aerobic organisms in a few denitrifiers (reduce NO, to N,) [20, 211, and in some phototrophic purple non-sulfur bacteria [22, 231. Under anaerobic conditions all other known chemotrophic organisms, in pure culture, were incapable of complete oxidation of organic matter. And there was also a theory to explain this observation: the oxidation of succinate to fumarate in the citric-acid cycle requires a terminal electron acceptor with a redox potential (E"') more positive than that of the fumarate/ succinate couple (+32 mV). Only O2 ( 0 2 / H 2 0 : E" = f 8 1 8 mV), NO; (NO;/NO;: E"' = +433 mV) and NO; (NO;/N2: E"' = +970 mV), rather than the electron acceptors used by anaerobes, appeared to meet these conditions The above consideration ignored that there was, in the literature, evidence for a mineralization of organic matter in anaerobic biotopes. Hoppe-Seyler, already in 1886, described the complete oxidation of cellulose in anaerobic sediments supplemented with CaSO,. The reducing equivalents were quantitatively recovered as H2S [25]. Later Jerrgensen Martens and Berner [30], and Winfrey and Zeikus [31] reported that in marine sediments carbohydrates, proteins, and fatty acids were mineralized in the absence of O2 and that sulfate, elemental sulfur, and thiosulfate [29] were the major electron acceptors used. Sterilized sediments did not mediate the conversion. It was, therefore, evident that an anaerobic pathway of terminal respiration must exist.Pfennig and collaborators were then the first to isolate one of these organisms. In 1976 Pfennig and Biebl [32] described ~4 1 .