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Dissimilatory adenosine-5'-phosphosulfate (APS) reductase (AprBA) is a key enzyme of the dissimilatory sulfate-reduction pathway. Homologues have been found in photo- and chemotrophic sulfur-oxidizing prokaryotes (SOP), in which they are postulated to operate in the reverse direction, oxidizing sulfite to APS. Newly developed PCR assays allowed the amplification of 92-93% (2.1-2.3 kb) of the APS reductase locus aprBA. PCR-based screening of t 16 taxonomically divergent SOP reference strains revealed a distribution of aprBA restricted to photo- and chemotrophs with strict anaerobic or at least facultative anaerobic lifestyles, including Chlorobiaceae, Chromatiaceae, Thiobacillus, Thiothrix and invertebrate symbionts. In the AprBA-based tree, the SOP diverge into two distantly related phylogenetic lineages, Apr lineages I and II, with the proteins of lineage II (Chlorobiaceae and others) in closer affiliation to the enzymes of the sulfate-reducing prokaryotes (SRP). This clustering is discordant with the dissimilatory sulfite reductase (DsrAB) phylogeny and indicates putative lateral aprBA gene transfer from SRP to the respective SOB lineages. In support of lateral gene transfer (LGT), several beta- and gammaproteobacterial species harbour both aprBA homologues, the DsrAB-congruent 'authentic' and the SRP-related, LGT-derived gene loci, while some relatives possess exclusively the SRP-related apr genes as a possible result of resident gene displacement by the xenologue. The two-gene state might be an intermediate in the replacement of the resident essential gene. Collected genome data demonstrate the correlation between the AprBA tree topology and the composition/arrangement of the apr gene loci (occurrence of qmoABC or aprM genes) from SRP and SOP of lineages I and II. The putative functional role of the SRP-related APS reductases in photo- and chemotrophic SOP is discussed.

Newly developed PCR assays were used to PCR-amplify and sequence fragments of the dissimilatory adenosine-5'-phosphosulfate (APS) reductase genes (aprBA) comprising nearly the entire gene locus (2.2-2-4 kb, equal to 92-94% of the protein coding sequence) from 75 sulfate-reducing prokaryotes (SRP) of a taxonomically wide range. Comparative phylogenetic analysis included all determined and publicly available AprBA sequences from SRP and selected homologous sequences of sulfur-oxidizing bacteria (SOB). The almost identical AprB and AprA tree topologies indicated a shared evolutionary path for the aprBA among the investigated SRP by vertical inheritance and concomitant lateral gene transfer (LGT). The topological comparison of AprB/A- and 16S rRNA gene-based phylogenetic trees revealed novel LGT events across the SRP divisions. Compositional gene analysis confirmed Thermacetogenium phaeum to be the first validated strain affected by a recent lateral transfer of aprBA as a putative effect of long-term co-cultivation with a Thermodesulfovibrio species. Interestingly, the Apr proteins of SRP and SOB diverged into two phylogenetic lineages, with the SRP affiliated with the green sulfur bacteria, e.g. Chlorobaculum tepidum, while the Aflochromatium vinosum-related sequences formed a distinct group. Analysis of genome data indicated that this phylogenetic separation is also reflected in the differing presence of the putative proteins functionally associated with Apr, QmoABC complex (quinone-interacting membrane-bound oxidoreductase) and AprM (transmembrane protein). Scenarios for the origin and evolution of the dissimilatory APS reductase are discussed within the context of the dissimilatory sulfite reductase (DsrAB) phylogeny, the appearance of QmoABC and AprM in the SRP and SOB genomes, and the geochemical setting of Archean Earth.

The diversity of bacterial endosymbionts in Inanidrilus leukodermatus from Bermuda and Inanidrilus makropetalos from Bahamas was studied using comparative sequence analysis of 16S rRNA gene and fluorescence in situ hybridization. The findings show that stable coexistence of multiple endosymbionts is not limited to single species but appears to be a common feature in oligochaete symbioses.

The dissimilatory reduction of sulfate is an ancient metabolic process central to today's biogeochemical cycling of sulfur and carbon in marine sediments. Until now its polyphyletic distribution was most parsimoniously explained by multiple horizontal transfers of single genes rather than by a not-yet-identified 'metabolic island.' Here we provide evidence that the horizontal transfer of a gene cluster may indeed be responsible for the patchy distribution of sulfate-reducing prokaryotes (SRP) in the phylogenetic tree. We isolated three DNA fragments (32 to 41 kb) from uncultured, closely related SRP from DNA directly extracted from two distinct marine sediments. Fosmid ws39f7, and partially also fosmids ws7f8 and hr42c9, harbored a core set of essential genes for the dissimilatory reduction of sulfate, including enzymes for the reduction of sulfur intermediates and synthesis of the prosthetic group of the dissimilatory sulfite reductase. Genome comparisons suggest that encoded membrane proteins universally present among SRP are critical for electron transfer to cytoplasmic enzymes. In addition, novel, conserved hypothetical proteins that are likely involved in dissimilatory sulfate reduction were identified. Based on comparative genomics and previously published experimental evidence, a more comprehensive model of dissimilatory sulfate reduction is presented. The observed clustering of genes involved in dissimilatory sulfate reduction has not been previously found. These findings strongly support the hypothesis that genes responsible for dissimilatory sulfate reduction were concomitantly transferred in a single event among prokaryotes. The acquisition of an optimized gene set would enormously facilitate a successful implementation of a novel pathway.

Author(s): Hang T. Dinh [1]; Jan Kuever [1, 2]; Marc Mußmann [1]; Achim W. Hassel [3]; Martin Stratmann [3]; Friedrich Widdel (corresponding author) [1] Corrosion of iron presents a serious [...]

Researchers have tested sulfur isotope enrichment during sulfate reduction in 32 sulfate-reducing prokaryotes, over the total microbial temperature range, a variety of substrates, and differing salinities and pH values. Under these conditions, isotope fractionation factors ranged from 2% to 42%.