Our newly designed primers were evaluated for the molecular analysis of specific groups of the sqr gene encoding sulfide : quinone reductase (SQR) in sediment environments. Based on the phylogenetic analysis, we classified the sqr sequences into six groups. PCR primers specific for each group were developed. We successfully amplified sqr-like gene sequences related to groups 1, 2 and 4 from diverse sediments including a marine sediment (SW), a tidal flat (TS), a river sediment (RS) and a lake sediment (FW). We recovered a total of 82 unique phylotypes (based on a 95 % amino acid sequence similarity cutoff) from 243 individual sqr-like gene sequences. Phylotype richness varied widely among the groups of sqr-like gene sequences (group 1.group 2.group 4) and sediments (SW.TS.RS.FW). Most of the sqr-like gene sequences were affiliated with the Proteobacteria clade and were distantly related to the reference sqr gene sequences from cultivated strains (less than~80 % amino acid sequence similarity). Unique sqr-like gene sequences were associated with individual sediment samples in groups 1 and 2. This molecular tool has also enabled us to detect sqr-like genes in a sulfuroxidizing enrichment from marine sediments. Collectively, our results support the presence of previously unrecognized sqr gene-containing micro-organisms that play important roles in the global biogeochemical cycle of sulfur.
INTRODUCTIONSulfide, the most reduced form of inorganic sulfur, occurs in sediment environments, where it is generated from anaerobic sulfate-reducing bacteria (Detmers et al., 2001;Sorensen et al., 1981). Besides chemical oxidation, microorganisms are involved in the oxidation of sulfide at oxicanoxic interfaces; this reaction initiates the first step of the sulfur oxidation process (Cytryn et al., 2005;Jorgensen, 1982) and produces sulfate or sulfur as the major oxidation product (Friedrich, 1998;Ruepp et al., 2000;She et al., 2001;Theissen et al., 2003).The oxidation of sulfide to sulfate is mediated by membrane-bound electron-transport systems. Two main enzymic systems participating in the initial step have been intensively studied to understand the mechanism of sulfide oxidation. The electrons from sulfide enter the electrontransport chain either at the level of c-type cytochromes, via a sulfide : cytochrome c reductase (FCC) (Kusai & Yamanaka, 1973a, b, c; Lyric & Suzuki, 1970a, b, c), or at the level of quinone via a sulfide : quinone reductase (SQR) (Nubel et al., 2000;Schutz et al., 1997Schutz et al., , 1998Schutz et al., , 1999. FCC was suggested to play an essential role in sulfide oxidation in vivo, and found in a number of chemotrophic and phototrophic sulfide-oxidizing bacteria (Griesbeck et al., 2000;Schutz et al., 1999). However, it is not obligatory in sulfide oxidation since FCC does not occur in a variety of sulfide-oxidizing bacteria, and appears to be dispensable in the micro-organisms in which it is present (Brune, 1995). For example, disruption of the fcc gene in Chromatium vinosum did not have any signifi...