Metagenome of a versatile chemolithoautotroph from expanding oceanic dead zones Summary: Time-resolved metagenomic approaches are used to describe carbon and energy metabolism of an ecologically relevant microbe from expanding oceanic dead zones mediating carbon sequestration, sulfur-detoxification and biological nitrogen loss.

Our current knowledge about nucleocytoplasmic large DNA viruses (NCLDVs) is largely derived from viral isolates that are co-cultivated with protists and algae. Here we reconstructed 2,074 NCLDV genomes from sampling sites across the globe by building on the rapidly increasing amount of publicly available metagenome data. This led to an 11-fold increase in phylogenetic diversity and a parallel 10-fold expansion in functional diversity. Analysis of 58,023 major capsid proteins from large and giant viruses using metagenomic data revealed the global distribution patterns and cosmopolitan nature of these viruses. The discovered viral genomes encoded a wide range of proteins with putative roles in photosynthesis and diverse substrate transport processes, indicating that host reprogramming is probably a common strategy in the NCLDVs. Furthermore, inferences of horizontal gene transfer connected viral lineages to diverse eukaryotic hosts. We anticipate that the global diversity of NCLDVs that we describe here will establish giant viruses—which are associated with most major eukaryotic lineages—as important players in ecosystems across Earth’s biomes.

Saturated thalassic brines are among the most physically demanding habitats on Earth: few microbes survive in them. Salinibacter ruber is among these organisms and has been found repeatedly in significant numbers in climax saltern crystallizer communities. The phenotype of this bacterium is remarkably similar to that of the hyperhalophilic Archaea (Haloarchaea). The genome sequence suggests that this resemblance has arisen through convergence at the physiological level (different genes producing similar overall phenotype) and the molecular level (independent mutations yielding similar sequences or structures). Several genes and gene clusters also derive by lateral transfer from (or may have been laterally transferred to) haloarchaea. S. ruber encodes four rhodopsins. One resembles bacterial proteorhodopsins and three are of the haloarchaeal type, previously uncharacterized in a bacterial genome. The impact of these modular adaptive elements on the cell biology and ecology of S. ruber is substantial, affecting salt adaptation, bioenergetics, and photobiology.halophile ͉ lateral gene transfer ͉ convergence ͉ prokaryotic evolution ͉ rhodopsins U ntil recently, halophilic archaea (haloarchaea) were thought to be the only cells capable of thriving in saltern crystallizers. These impoundments contain Ϸ37% NaCl, at the limits of tolerance for this environmental factor. Further concentration of thalassic (seawater-derived) hypersaline water leads to precipitation of magnesium salts and sterility. Fluorescent in situ hybridization indicates that one crystallizer morphotype, well defined large rods, corresponds to a bacterium of the Cytophaga cluster (1), within the Bacteroides͞Chlorobi group. This organism represents 10-20% of the cells in climax crystallizer communities (spring and summer in temperate latitudes). Representative strains (as defined by 16S rRNA sequences) have been isolated from the same environment and described as the previously uncharacterized genus and species Salinibacter ruber (2).The closest cultivated relative of S. ruber (henceforth Salinibacter) is Rhodothermus marinus (89% 16S rRNA sequence similarity), a slightly halophilic thermophile isolated from marine hot springs (2). Salinibacter displays many remarkable similarities to haloarchaea, one being a very high concentration of potassium in the cytoplasm (3). This property is associated, as in haloarchaea, with a high content of acidic amino acids and a low content of hydrophobic residues in bulk protein, necessary for protein solubility at such high ionic strength (4). Cell integrity requires high salt concentrations in both cases, and growth only occurs at Ͼ2 M NaCl. Both Salinibacter and the haloarchaea are aerobic heterotrophs that exploit the large stock of organic nutrients produced in previous stages of seawater concentration, mostly by the green alga Dunaliella, and they use a similar range of organic compounds as carbon and energy sources (5). Like haloarchaea, Salinibacter contains a high proportion of carotenoids in its membrane, pro...

Lateral gene transfer (LGT) is now known to be a major force in the evolution of prokaryotic genomes. To date, most analyses have focused on either (a) verifying phylogenies of individual genes thought to have been transferred, or (b) estimating the fraction of individual genomes likely to have been introduced by transfer. Neither approach does justice to the ability of LGT to effect massive and complex transformations in basic biology. In some cases, such transformation will be manifested as the patchy distribution of a seemingly fundamental property (such as aerobiosis or nitrogen fixation) among the members of a group classically defined by the sharing of other properties (metabolic, morphological, or molecular, such as small subunit ribosomal RNA sequence). In other cases, the lineage of recipients so transformed may be seen to comprise a new group of high taxonomic rank ("class" or even "phylum"). Here we review evidence for an important role of LGT in the evolution of photosynthesis, aerobic respiration, nitrogen fixation, sulfate reduction, methylotrophy, isoprenoid biosynthesis, quorum sensing, flotation (gas vesicles), thermophily, and halophily. Sometimes transfer of complex gene clusters may have been involved, whereas other times separate exchanges of many genes must be invoked.