Takaki, Yoshihiro

Marine sediments are vast, underexplored habitats and represent one of the largest carbon deposits on our planet. Microbial communities drive nutrient cycling in these sediments, but the full extent of their taxonomic and metabolic diversity remains to be explored. Here, we analysed shallow coastal and deep subseafloor sediment cores from 0.01 to nearly 600 metres below the seafloor, in the Western Pacific Region. Applying metagenomics, we identified several taxonomic clusters across all samples, which mainly aligned with depth and sediment type. Inferring functional patterns provided insights into possible ecological roles of the main microbial taxa. These included Chloroflexota, the most abundant phylum across all samples, whereby the classes Dehalococcoida and Anaerolineae dominated deep-subsurface and most shallow coastal sediments, respectively. Thermoproteota and Asgardarchaeota were the most abundant phyla among Archaea, contributing to high relative abundances of Archaea reaching over 50% in some samples. We recovered high-quality metagenome-assembled genomes for all main prokaryotic lineages and proposed names for three phyla, i.e. Tangaroaeota phyl. nov. (former RBG-13-66-14), Ryujiniota phyl. nov. (former UBA6262) and Spongiamicota phyl. nov. (former UBA8248). Metabolic capabilities across all samples ranged from aerobic respiration and photosynthesis in the shallowest sediment layers to heterotrophic carbon utilization, sulphate reduction and methanogenesis in deeper anoxic sediments. We also identified taxa with the potential to be involved in nitrogen and sulphur cycling and heterotrophic carbon utilization. In summary, this study contributes to our understanding of the taxonomic and functional diversity in benthic prokaryotic communities across marine sediments in the Western Pacific Region.

An anaerobic, mesophilic, syntrophic, archaeon strain MK-D1T, was isolated as a pure co-culture with Methanogenium sp. strain MK-MG from deep-sea methane seep sediment. This organism is, to our knowledge, the first cultured representative of ‘Asgard’ archaea, an archaeal group closely related to eukaryotes. Here, we describe the detailed physiology and phylogeny of MK-D1T and propose Promethearchaeum syntrophicum gen. nov., sp. nov. to accommodate this strain. Cells were non-motile, small cocci, approximately 300–750 nm in diameter and produced membrane vesicles, chains of blebs and membrane-based protrusions. MK-D1T grew at 4–30 °C with optimum growth at 20 °C. The strain grew chemoorganotrophically with amino acids, peptides and yeast extract with obligate dependence on syntrophy with H2-/formate-utilizing organisms. MK-D1T showed the fastest growth and highest maximum cell yield when grown with yeast extract as the substrate: approximately 3 months to full growth, reaching up to 6.7×106 16S rRNA gene copies ml−1. MK-D1T had a circular 4.32 Mb chromosome with a DNA G+C content of 31.1 mol%. The results of phylogenetic analyses of the 16S rRNA gene and conserved marker proteins indicated that the strain is affiliated with ‘Asgard’ archaea and more specifically DHVC1/DSAG/MBG-B and ‘Lokiarchaeota’/‘Lokiarchaeia’. On the basis of the results of 16S rRNA gene sequence analysis, the most closely related isolated relatives were Infirmifilum lucidum 3507LTT (76.09 %) and Methanothermobacter tenebrarum RMAST (77.45 %) and the closest relative in enrichment culture was Candidatus ‘Lokiarchaeum ossiferum’ (95.39 %). The type strain of the type species is MK-D1T (JCM 39240T and JAMSTEC no. 115508). We propose the associated family, order, class, phylum, and kingdom as Promethearchaeaceae fam. nov., Promethearchaeales ord. nov., Promethearchaeia class. nov., Promethearchaeota phyl. nov., and Promethearchaeati regn. nov., respectively. These are in accordance with ICNP Rules 8 and 22 for nomenclature, Rule 30(3)(b) for validation and maintenance of the type strain, and Rule 31a for description as a member of an unambiguous syntrophic association.