The classDeltaproteobacteriacomprises an ecologically and metabolically diverse group of bacteria best known for dissimilatory sulphate reduction and predatory behaviour. Although this lineage is the fourth described class of the phylumProteobacteria, it rarely affiliates with other proteobacterial classes and is frequently not recovered as a monophyletic unit in phylogenetic analyses. Indeed, one branch of the classDeltaproteobacteriaencompassingBdellovibrio-like predators was recently reclassified into a separate proteobacterial class, theOligoflexia. Here we systematically explore the phylogeny of taxa currently assigned to these classes using 120 conserved single-copy marker genes as well as rRNA genes. The overwhelming majority of markers reject the inclusion of the classesDeltaproteobacteriaandOligoflexiain the phylumProteobacteria. Instead, the great majority of currently recognized members of the classDeltaproteobacteriaare better classified into four novel phylum-level lineages. We propose the namesDesulfobacterotaphyl. nov. andMyxococcotaphyl. nov. for two of these phyla, based on the oldest validly published names in each lineage, and retain the placeholder name SAR324 for the third phylum pending formal description of type material. Members of the classOligoflexiarepresent a separate phylum for which we propose the nameBdellovibrionotaphyl. nov. based on priority in the literature and general recognition of the genusBdellovibrio. Desulfobacterotaphyl. nov. includes the taxa previously classified in the phylumThermodesulfobacteria, and these reclassifications imply that the ability of sulphate reduction was vertically inherited in theThermodesulfobacteriarather than laterally acquired as previously inferred. Our analysis also indicates the independent acquisition of predatory behaviour in the phylaMyxococcotaandBdellovibrionota, which is consistent with their distinct modes of action. This work represents a stable reclassification of one of the most taxonomically challenging areas of the bacterial tree and provides a robust framework for future ecological and systematic studies.

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 Allochromatium 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 dissimilatory adenosine-5′-phosposulfate reductase is a key enzyme of the microbial sulfate reduction and sulfur oxidation processes. Because the alpha- and beta-subunit-encoding genes, aprBA , are highly conserved among sulfate-reducing and sulfur-oxidizing prokaryotes, they are most suitable for molecular profiling of the microbial community structure of the sulfur cycle in environment. In this study, a new aprA gene-targeting assay using a combination of PCR and denaturing gradient gel electrophoresis is presented. The screening of sulfate-reducing and sulfur-oxidizing reference strains as well as the analyses of environmental DNA from diverse habitats (e.g., microbial mats, invertebrate tissue, marine and estuarine sediments, and filtered hydrothermal water) by the new primer pair revealed an improved microbial diversity coverage and less-pronounced template-to-PCR product bias in direct comparison to those of the previously published primer set (B. Deplancke, K. R. Hristova, H. A. Oakley, V. J. McCracken, R. Aminov, R. I. Mackie, and H. R. Gaskins, Appl. Environ. Microbiol. 66:2166-2174, 2000). The concomitant molecular detection of sulfate-reducing and sulfur-oxidizing prokaryotes was confirmed. The new assay was applied in comparison with the 16S rRNA gene-based analysis to investigate the microbial diversity of the sulfur cycle in sediment, seawater, and manganese crust samples from four study sites in the area of the Lesser Antilles volcanic arc, Caribbean Sea (Caribflux project). The aprA gene-based approach revealed putative sulfur-oxidizing Alphaproteobacteria of chemolithoheterotrophic lifestyle to have been abundant in the nonhydrothermal sediment and water column. In contrast, the sulfur-based microbial community that inhabited the surface of the volcanic manganese crust was more complex, consisting predominantly of putative chemolithoautotrophic sulfur oxidizers of the Betaproteobacteria and Gammaproteobacteria .

Denaturing gradient gel electrophoresis (DGGE)-based analyses of 16S rRNA, aprA, and amoA genes demonstrated that a phylogenetically diverse and complex microbial community was associated with the Caribbean deep-water sponge Polymastia cf. corticata Ridley and Dendy, 1887. From the 38 archaeal and bacterial 16S rRNA phylotypes identified, 53% branched into the sponge-specific, monophyletic sequence clusters determined by previous studies (considering predominantly shallow-water sponge species), whereas 26% appeared to be P. cf. corticata specifically associated microorganisms (“specialists”); 21% of the phylotypes were confirmed to represent seawater- and sediment-derived proteobacterial species (“contaminants”) acquired by filtration processes from the host environment. Consistently, the aprA and amoA gene-based analyses indicated the presence of environmentally derived sulfur- and ammonia-oxidizers besides putative sponge-specific sulfur-oxidizing Gammaproteobacteria and Alphaproteobacteria and a sulfate-reducing archaeon. A sponge-specific, endosymbiotic sulfur cycle as described for marine oligochaetes is proposed to be also present in P. cf. corticata. Overall, the results of this work support the recent studies that demonstrated the sponge species specificity of the associated microbial community while the biogeography of the host collection site has only a minor influence on the composition. In P. cf. corticata, the specificity of the sponge–microbe associations is even extended to the spatial distribution of the microorganisms within the sponge body; distinct bacterial populations were associated with the different tissue sections, papillae, outer and inner cortex, and choanosome. The local distribution of a phylotype within P. cf. corticata correlated with its (1) phylogenetic affiliation, (2) classification as sponge-specific or nonspecifically associated microorganism, and (3) potential ecological role in the host sponge.