A novel sulfate-reducing bacterium was isolated from pristine sediments of Lake Stechlin, Germany. This strain, STP12 T , was found to contain predominantly c-type cytochromes and to reduce sulfate, sulfite and thiosulfate using lactate as an electron donor. Although STP12 T could not utilize elemental sulfur as an electron acceptor, it could support growth by dissimilatory Fe(III) reduction. In a comparison of 16S rRNA gene sequences, STP12 T was 96?7 % similar to Desulfosporosinus auripigmenti DSM 13351 T , 96?5 % similar to Desulfosporosinus meridiei DSM 13257 T and 96?4 % similar to Desulfosporosinus orientis DSM 765 T . DNA-DNA hybridization experiments revealed that strain STP12 T shows only 32 % reassociation with the type strain of the type species of the genus, D. orientis DSM 765 T . These data, considered in conjunction with strain-specific differences in heavy metal tolerance, cell-wall chemotaxonomy and riboprint patterns, support recognition of strain STP12 T (=DSM 15449 T =JCM 12239 T ) as the type strain of a distinct and novel species within the genus Desulfosporosinus, Desulfosporosinus lacus sp. nov.The genus Desulfosporosinus currently contains three species with validly published names, Desulfosporosinus orientis (Stackebrandt et al., 1997), Desulfosporosinus auripigmenti (Stackebrandt et al., 2003) and Desulfosporosinus meridiei (Robertson et al., 2001). Isolates from locales separated by thousands of kilometres exist for some of these species (e.g. DSM 8344; Vainshtein et al., 1994). Culture-and nonculture-based studies have revealed the existence of Desulfosporosinus-like organisms in environmental settings as diverse as permafrost (Vainshtein et al., 1994), pristine aquifers (Detmers et al., 2004), municipal drinking water (Bade, 2000) and rice plant roots (Scheid et al., 2004).Multiple lines of evidence suggest that members of the genus also commonly inhabit industrially impacted soils and sediments. D. auripigmenti was isolated from an arseniccontaminated watershed, and is one of a limited number of bacteria known to respire arsenate (Newman et al., 1997). Recently, another arsenic-reducing Desulfosporosinus strain was isolated from arsenic-contaminated sediments; this organism has the capacity to metabolize a wide variety of aromatic compounds (Liu et al., 2004). Kusel et al. (2001) reported the isolation of Desulfosporosinus-like organisms from a coal-mining-impacted lake, while Robertson et al. (2000) isolated eight Desulfosporosinus strains from a hydrocarbon-contaminated soil. Two of these were later described as D. meridiei (Robertson et al., 2001) and their activity was linked to toluene mineralization (Robertson et al., 2000;Franzmann et al., 2002 et al., 2003), and uranium mine tailings in Shiprock, NM (Nevin et al., 2003). Significantly, enrichment of Desulfosporosinus-like microbes has been associated with stimulated removal of solution-phase uranium (Nevin et al., 2003). In such contexts, uranium precipitation may occur secondarily to sulfidogenesis or as a primary resul...