Methanogenesis is an ancient metabolism of key ecological relevance, with direct impact on the evolution of Earth’s climate. Recent results suggest that the diversity of methane metabolisms and their derivations have probably been vastly underestimated. Here, by probing thousands of publicly available metagenomes for homologues of methyl-coenzyme M reductase complex (MCR), we have obtained ten metagenome-assembled genomes (MAGs) belonging to potential methanogenic, anaerobic methanotrophic and short-chain alkane oxidizing archaea. Five of these MAGs represent under-sampled (e.g., Verstraetearchaeota, Methanonatronarchaeia, ANME-1) or previously genomically undescribed (ANME-2c) archaeal lineages. The remaining five MAGs correspond to lineages that are only distantly related to previously known methanogens and span the entire archaeal phylogeny. Comprehensive comparative annotation significantly expands the metabolic diversity and energy conservation systems of MCR-bearing archaea. It also suggests the potential existence of a yet uncharacterized type of methanogenesis linked to short-chain alkane/fatty acid oxidation in a previously undescribed class of archaea (‘ Ca . Methanoliparia’). We redefine a common core of marker genes specific to methanogenic, anaerobic methanotrophic and short-chain alkane-oxidizing archaea, and propose a possible scenario for the evolutionary and functional transitions that led to the emergence of such metabolic diversity.

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The identification of a region of sequence variability among individual isolates of Bacillus anthracis as well as the two closely related species, Bacillus cereus and Bacillus mycoides, has made a sequence-based approach for the rapid differentiation among members of this group possible. We have identified this region of sequence divergence by comparison of arbitrarily primed (AP)-PCR ''fingerprints'' generated by an M13 bacteriophagederived primer and sequencing the respective forms of the only polymorphic fragment observed. The 1,480-bp fragment derived from genomic DNA of the Sterne strain of B. anthracis contained four consecutive repeats of CAATATCAACAA. The same fragment from the Vollum strain was identical except that two of these repeats were deleted. The Ames strain of B. anthracis differed from the Sterne strain by a single-nucleotide deletion. More than 150 nucleotide differences separated B. cereus and B. mycoides from B. anthracis in pairwise comparisons. The nucleotide sequence of the variable fragment from each species contained one complete open reading frame (ORF) (designated vrrA, for variable region with repetitive sequence), encoding a potential 30-kDa protein located between the carboxy terminus of an upstream ORF (designated orf1) and the amino terminus of a downstream ORF (designated lytB). The sequence variation was primarily in vrrA, which was glutamine-and proline-rich (30% of total) and contained repetitive regions. A large proportion of the nucleotide substitutions between species were synonymous. vrrA has 35% identity with the microfilarial sheath protein shp2 of the parasitic worm Litomosoides carinii.

Although once thought to be devoid of biology, recent studies have identified salt deposits as oases for life in the hyperarid Atacama Desert. To examine spatial patterns of microbial species and key nutrient sources, we genomically characterized 26 salt crusts from three sites along a fog gradient. The communities are dominated by a large variety of Halobacteriales and Bacteroidetes, plus a few algal and Cyanobacterial species. CRISPR locus analysis suggests the distribution of a single Cyanobacterial population among all sites. This is in stark contrast to the extremely high sample specificity of most other community members. Only present at the highest moisture site is a genomically characterized Thermoplasmatales archaeon (Marine Group II) and six Nanohaloarchaea, one of which is represented by a complete genome. Parcubacteria (OD1) and Saccharibacteria (TM7), not previously reported from hypersaline environments, were found at low abundances. We found no indication of a N2 fixation pathway in the communities, suggesting acquisition of bioavailable nitrogen from atmospherically derived nitrate. Samples cluster by site based on bacterial and archaeal abundance patterns and photosynthetic capacity decreases with increasing distance from the ocean. We conclude that moisture level, controlled by coastal fog intensity, is the strongest driver of community membership.