Sulfate-reducing bacteria, like Desulfovibrio vulgarisHildenborough, have developed a set of reactions allowing them to survive in oxic environments and even to reduce molecular oxygen to water. D. vulgaris contains a cytoplasmic superoxide reductase (SOR) and a periplasmic superoxide dismutase (SOD) involved in the elimination of superoxide anions. To assign the function of SOD, the periplasmic [Fe] hydrogenase activity was followed in both wild-type and sod deletant strains. This activity was lower in the strain lacking the SOD than in the wild-type when the cells were exposed to oxygen for a short time. The periplasmic SOD is thus involved in the protection of sensitive iron-sulfur-containing enzyme against superoxide-induced damages. Surprisingly, production of the periplasmic Microbial sulfate reduction has been reported to be an ancient process as old as 3.47 gigayears. Sulfate reduction thus represents an early specific metabolic pathway, allowing time calibration of a deep node on the tree of life (1). Sulfate-reducing bacteria (SRB) 1 are universally distributed in marine and microbial mats where sulfate reduction is the dominant anaerobic biomineralization pathway. They constitute a group of anaerobic prokaryotes, which are unified by sharing the capacity to carry out dissimilatory sulfate reduction to sulfide as a major component of their bioenergetic processes. Although sulfate reduction is generally considered to be an anaerobic process, the abundance and metabolic activity of SRB in oxic zones is frequently evaluated as higher than those in neighboring anoxic zones in numerous biotopes (2, 3). In situ detection of sulfate reducing activity and SRB populations in these biotopes showed that SRB species did not have the same capability of resisting oxygen. Analysis of the photooxic zone of cyanobacterial mats revealed a well-defined SRB distribution. Although Desulfobacter and Desulfobacterium were restricted to the deepest levels in the mats, Desulfococcus were predominant in the photooxic zone with Desulfovibrio also present. This distribution suggests that both groups contain oxygen-tolerant members (4). It is thus clear that SRB exhibit a differentiated set of reactions to oxygen: first, many SRB form aggregates (5), resulting in a higher tolerance to oxygen exposure; second, at least Desulfovibrio species migrate in response to the oxygen concentration in their environment (5); and third, many species respire with oxygen (6). However, although it has been demonstrated that aerobic respiration is coupled with proton translocation and ATP conservation, aerobic growth in pure culture has never been proved (7). The high respiration rate merely seems to have a protective function. In an oxygen gradient, bacteria form bands at the outer edge of the oxic zone, suggesting both negative and positive aerotaxis responses (8). The capability of SRB to move toward oxygen and reduce it might play an ecological role in the zone of transition from an oxic to an anoxic environment, protecting themselves and other...