Tetrachloroethene (PCE) dehalorespiration was investigated in a continuous coculture of the sulfatereducing bacterium Desulfovibrio fructosivorans and the dehalorespiring Desulfitobacterium frappieri TCE1 at different sulfate concentrations and in the absence of sulfate. Fructose (2.5 mM) was the single electron donor, which could be used only by the sulfate reducer. With 2.5 mM sulfate, the dehalogenating strain was outnumbered by the sulfate-reducing bacterium, sulfate reduction was the dominating process, and only trace amounts of PCE were dehalogenated by strain TCE1. With 1 mM sulfate in the medium, complete sulfate reduction and complete PCE dehalogenation to cis-dichloroethene (cis-DCE) occurred. In the absence of sulfate, PCE was also completely dehalogenated to cis-DCE, and the population size of strain TCE1 increased significantly. The results presented here describe for the first time dehalogenation of PCE by a dehalorespiring anaerobe in strict dependence on the activity of a sulfate-reducing bacterium with a substrate that is exclusively used by the sulfate reducer. This interaction was studied under strictly controlled and quantifiable conditions in continuous culture and shown to depend on interspecies hydrogen transfer under sulfate-depleted conditions. Interspecies hydrogen transfer was demonstrated by direct H 2 measurements of the gas phase and by the production of methane after the addition of a third organism, Methanobacterium formicicum.Some published results seem to indicate that dehalogenating and/or dehalorespiring bacteria and sulfate-reducing bacteria often share biotopes that are contaminated with chlorinated compounds. In this context for example, Gerritse et al. (23) reported on the isolation of a Desulfovibrio species (strain SULF1) and a Desulfitobacterium species (strain TCE1; now identified and deposited as Desulfitobacterium frappieri TCE1 [24]) from the same reactor, which was inoculated with a tetrachloroethene (PCE)-contaminated soil slurry. Both strains grew well in the presence of high concentrations of PCE (up to 30 mM) and sulfate (up to 20 mM) as electron acceptors. In another example, Drzyzga et al. (16) demonstrated dehalogenation of 2-and 4-fluorobenzoate by a freshwater coculture under sulfate-reducing conditions. One member of this coculture was identified as a Desulfotomaculum species, which was able to mineralize the aromatic intermediates, whereas the other unidentified strain was proposed to be responsible for the dehalogenation reaction. Because the authors of that study were not successful in separating both strains (only the sporeforming Desulfotomaculum species was obtained after pasteurization), they suggested that a symbiotic relationship between these two strains might have been essential when grown with halogenated compounds as the sole carbon source. Difficulties in separating dehalogenating and sulfate-reducing strains from a coculture were also reported by Mägli et al. (32), who isolated the dichloromethane-degrading Dehalobacterium formicoaceticum ...