Project description:The purple sulfur bacterium Allochromatium vinosum DSM 180T is one of the best studied sulfur-oxidizing anoxygenic phototrophic bacteria and has been developed into a model organism for laboratory-based studies of oxidative sulfur metabolism. Here, we took advantage of the organismM-bM-^@M-^Ys high metabolic versatility and performed whole-genome transcriptional profiling to investigate the response of A. vinosum cells upon exposure to sulfide, thiosulfate, elemental sulfur or sulfite as compared to photoorganoheterotrophic growth on malate. Differential expression (at least twofold) of 1149 genes was observed, corresponding to 30% of the A. vinosum genome. A total of 549 genes were identified for which relative transcription increased at least twofold during growth on one of the different sulfur sources while relative transcription of 599 genes decreased. A significant number of genes that were strongly induced have documented sulfur-metabolism-related functions. Among these are the dsr genes including dsrAB for dissimilatory sulfite reductase and the sgp genes for the proteins of the sulfur globule envelope thus confirming former results. In addition we were able to identify new genes encoding proteins with appropriate subcellular localization and properties to participate in oxidative dissimilatory sulfur metabolism. Two of these were chosen for inactivation and phenotypic analyses of the respective mutant strains. This approach verified the importance of the encoded proteins for the oxidation of sulfide and thereby also documented the suitability of comparative transcriptomics for the identification of new sulfur-related genes in anoxygenic phototrophic sulfur bacteria. In this study, the relative genomic expression profiles of A. vinosum DSM 180T growing photolithoautotrophically on different reduced sulfur compounds were determined in comparison to those of cells grown photoorganoheterothrophically on malate (RCV medium) at exactly the same light intensity. The malate-containing medium was supplied with 0.815 mM sulfate in order to satisfy the sulfur-requirement for biosynthesis of sulfur-containing cell constituents. Three independent photolithoautotrophic cultures each, grown on sulfide, thiosulfate or sulfite were harvested 1 h, 2 h or 7 h, respectively, after inoculation. When elemental sulfur was the substrate, four independent cultures were harvested 3 h after inoculation.

Project description:Haloalkaliphilic microorganisms are double extremophiles functioning optimally at high salinity and pH. Their typical habitats are soda lakes, representing geologically ancient ecosystems which are still widespread on Earth and supposedly harbor relict microbial communities. We compared metabolic features and their genomic determinants in two strains of a single natronophilic species Dethiobacter alkaliphilus, the only cultured representative of “Dethiobacteria” class within Bacillota phylum. The strains of D. alkaliphilus were previously isolated from geographically remote Mongolian and Kenyan soda lakes. The type strain AHT1T was described as a facultatively chemolithoautotrophic sulfidogen reducing or disproportionating sulfur or thiosulfate, while strain Z-1002 was isolated as a chemolithoautotrophic iron reducer. Here, we uncovered iron reducing ability of strain AHT1T, as well as the capability of strain Z-1002 for thiosulfate reduction and anaerobic Fe(II) oxidation. Key catabolic processes sustaining the growth of both strains appeared to fit the geochemical settings of two contrasting natural alkaline environments, sulfur-enriched soda lakes and iron-enriched serpentinites. This assumption was supported by meta-analysis of publicly available Dethiobacterial metagenomes, as well as by the enrichment of a novel phylotype from a deep subsurface non-serpentinizing slightly alkaline water after its amendment with an Fe(III) mineral. Genome analysis of D. alkaliphilus strains revealed that the most probable determinants of iron and sulfur redox transformations in the organism are multiheme c-type cytochromes. Their phylogeny reconstruction showed that sulfur and thiosulfate respiration is most probably provided by evolutionary early forms of unconventional octaheme tetrathionate and sulfite reductases sharing a root with structurally similar group of OmhA/OcwA Fe(III)-reductases. Large sets of other multihemes are likely to provide Fe(III) reduction in both strains. Also, several different, yet phylogenetically related, determinants of anaerobic Fe(II) oxidation were identified in Z-1002 genome, and the oxidation process was further experimentally proven. Considering these results and phylogenetic relatedness of D. alkaliphilus’s sulfur reductases with Fe(III) reducing cytochromes, but not with archetypal bacterial sulfur/thiosulfate reductases, we suggest that sustaining high variation of multiheme cytochromes is an effective adaptive strategy to occupy geochemically contrasting alkaline anaerobic environments. We further propose that sulfur-enriched soda lakes are secondary habitats for D. alkaliphilus comparing to Fe-rich serpentinites, and discuss the evolutionary traits which might occur in prokaryotes on a crucial junction of the biosphere’s history, when intensification of the sulfur cycle outweighed the global significance of the iron cycle.

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Thiosulfate oxidation in Erythrobacter flavus 21-3 provides novel clues to the source of element sulfur in the deep-sea cold seep

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A novel bacterial thiosulfate oxidation pathway provides a new clue about the formation of zero-valent sulfur in deep sea.

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