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Erauso, G.

Publications and source records attributed to Erauso, G..

2 recordsLinked to original sources

Thermococcales pangenome uncovers new genera and modular evolution.

The order Thermococcales is unusual among Archaea in being known primarily from hundreds of lab-cultured isolates rather than metagenome-assembled genomes. Such cultivation is powerful for comparative genomics, allowing access to complete closed genomes rather than fragmented assemblies. We analysed 122 complete genomes, comprising all publicly available type species plus 67 new isolates, as a single pangenome. A combination of genome-scale metrics resolved 70 species across five genus-level clades, two proposed here as the new genera Oleococcus and Piezococcus, in addition to the canonical Pyrococcus, Palaeococcus, and Thermococcus. Only 6.1% of the 21,490 gene families are persistent, yet these contribute over half the genes in any genome. We observe that accessory functions, such as amino-acid biosynthesis, often behave modularly, being gained and lost as intact cassettes from genus-specific chromosomal loci. Combined with 114 mobile genetic elements, 72 of which are integrated in the chromosome at conserved tRNA genes, we find that Thermococcales genomes accommodate rapid horizontal turnover through a constrained chromosomal architecture.

genomics↗

Cultivating microbial communities from the serpentinite-hosted Prony Bay Hydrothermal Field on different carbon sources in hydrogen-fed bioreactors

The primary source of carbon is one of the most fundamental questions regarding the development of microbial communities in serpentinite-hosted systems. The hydration of ultramafic rock to serpentinites generates hydrogen and creates hyper-alkaline conditions that deplete the environment of dissolved inorganic carbon. Metagenomic studies suggest that serpentinite-hosted microbial communities depend on the local redissolution of bicarbonate as well as on small organic molecules produced by abiotic reactions associated with serpentinization. To test these hypotheses, microbial consortia collected from the Prony Bay hydrothermal field were grown under anoxic conditions in hydrogen-fed bioreactors using bicarbonate, formate, acetate, or glycine as the sole carbon source. In contrast to glycine, the other three carbon substrates allowed the growth of microbial consortia characterized by significant enrichment of individual taxa. Surprisingly, these taxa were dominated by microbial genera characterized as aerobic rather than anaerobic as expected. We propose that an intricate feedback loop between autotrophic and heterotrophic foundation species facilitates the establishment of serpentinite-hosted shallow subsurface ecosystems. Bicarbonate-fixing Meiothermus and Hydrogenophaga, as well as formate-fixing Meiothermus, Thioalkalimicrobium, and possibly a novel genotype of Roseibaca might produce organic compounds for heterotrophs at the first trophic level. In addition, the base of the trophic network may include heterotrophic Roseibaca, Acetoanaerobium, and Meiothermus species producing CO2 from acetate for a more diverse community of autotrophs. The cultivated archaeal community is expected to recycle CH4 and CO2 between Methanomicrobiales and Methanosarcinales with putative Woesearchaeales symbionts.

microbiology↗