Setting out to isolate uncultivated deep marine sediment microorganisms, we engineered and operated a methane-fed continuous-flow bioreactor system for more than 2,000 days to enrich such organisms from anaerobic marine methane-seep sediments 15 (Supplementary Note 1). We successfully enriched many phylogenetically diverse yetto-be cultured microorganisms, including Asgard archaea members (Loki-, Heimdall-and Odinarchaeota) 15. For further enrichment and isolation, samples of the bioreactor community were inoculated in glass tubes with simple substrates and basal medium. After approximately one year, we found faint cell turbidity in a culture containing casamino acids supplemented with four bacteria-suppressing antibiotics (Supplementary Note 2) that was incubated at 20 °C. Clone librarybased small subunit (SSU) rRNA gene analysis revealed a simple community that contained Halodesulfovibrio and a small population of Lokiarchaeota (Extended Data Table 1). In pursuit of this archaeon, which we designated strain MK-D1, we repeated subcultures when MK-D1 reached maximum cell densities as measured by quantitative PCR (qPCR). This approach gradually enriched the archaeon, which has an extremely slow growth rate and low cell yield (Fig. 1a). The culture consistently had a 30-60-day lag phase and required more

Although dense animal communities at hydrothermal vents and cold seeps rely on symbioses with chemoautotrophic bacteria [1, 2], knowledge of the mechanisms underlying these chemosynthetic symbioses is still fragmentary because of the difficulty in culturing the symbionts and the hosts in the laboratory. Deep-sea Calyptogena clams harbor thioautotrophic bacterial symbionts in their gill epithelial cells [1, 2]. They have vestigial digestive tracts and nutritionally depend on their symbionts [3], which are vertically transmitted via eggs [4]. To clarify the symbionts' metabolic roles in the symbiosis and adaptations to intracellular conditions, we present the complete genome sequence of the symbiont of Calyptogena okutanii. The genome is a circular chromosome of 1,022,154 bp with 31.6% guanine + cytosine (G + C) content, and is the smallest reported genome in autotrophic bacteria. It encodes 939 protein-coding genes, including those for thioautotrophy and for the syntheses of almost all amino acids and various cofactors. However, transporters for these substances to the host cell are apparently absent. Genes that are unnecessary for an intracellular lifestyle, as well as some essential genes (e.g., ftsZ for cytokinesis), appear to have been lost from the symbiont genome. Reductive evolution of the genome might be ongoing in the vertically transmitted Calyptogena symbionts.

SummaryThe stator-force generator that drives Na + -dependent motility in alkaliphilic Bacillus pseudofirmus OF4 is identified here as MotPS, MotAB-like proteins with genes that are downstream of the ccpA gene, which encodes a major regulator of carbon metabolism. B. pseudofirmus OF4 was only motile at pH values above 8. Disruption of motPS resulted in a non-motile phenotype, and motility was restored by transformation with a multicopy plasmid containing the motPS genes. Purified and reconstituted MotPS from B. pseudofirmus OF4 catalysed amiloride analogue-sensitive Na + translocation. In contrast to B. pseudofirmus , Bacillus subtilis contains both MotAB and MotPS systems. The role of the motPS genes from B. subtilis in several motility-based behaviours was tested in isogenic strains with intact motAB and motPS loci, only one of the two mot systems or neither mot system. B. subtilis MotPS (BsMotPS) supported Na + -stimulated motility, chemotaxis on soft agar surfaces and biofilm formation, especially after selection of an up-motile variant. BsMotPS also supported motility in agar soft plugs immersed in liquid; motility was completely inhibited by an amiloride analogue. BsMotPS did not support surfactin-dependent swarming on higher concentration agar surfaces.These results indicate that BsMotPS contributes to biofilm formation and motility on soft agar, but not to swarming, in laboratory strains of B. subtilis in which MotAB is the dominant stator-force generator. BsMotPS could potentially be dominant for motility in B. subtilis variants that arise in particular niches.

34The origin of eukaryotes remains enigmatic. Current data suggests that eukaryotes may 35 have risen from an archaeal lineage known as "Asgard archaea". Despite the eukaryote-36 like genomic features found in these archaea, the evolutionary transition from archaea to 37 eukaryotes remains unclear due to the lack of cultured representatives and corresponding 38 physiological insight. Here we report the decade-long isolation of a Lokiarchaeota-related 39Asgard archaeon from deep marine sediment. The archaeon, "Candidatus 40Prometheoarchaeum syntrophicum strain MK-D1", is an anaerobic, extremely slow-41 growing, small cocci (~550 nm), that degrades amino acids through syntrophy. Although 42 eukaryote-like intracellular complexities have been proposed for Asgard archaea, the 43 isolate has no visible organella-like structure. Ca. P. syntrophicum instead displays 44 morphological complexity -unique long, and often, branching protrusions. Based on 45 cultivation and genomics, we propose an "Entangle-Engulf-Enslave (E 3 ) model" for 46 eukaryogenesis through archaea-alphaproteobacteria symbiosis mediated by the physical 47 complexities and metabolic dependency of the hosting archaeon. 48 49 How did the first eukaryotic cell emerge? So far, among various competing evolutionary 50 models, the most widely accepted are the symbiogenetic models in which an archaeal 51 host cell and an alphaproteobacterial endosymbiont merged to become the first eukaryotic 52 cell 1-4 . Recent metagenomic discovery of Lokiarchaeota (and the Asgard archaea 53 superphylum) led to the theory that eukaryotes originated from an archaeon closely 54 related to Asgard archaea 5,6 . The Asgard archaea genomes encode a repertory of proteins 55 hitherto only found in Eukarya (eukaryotic signature proteins -ESPs), including those 56 involved in membrane trafficking, vesicle formation/transportation, ubiquitin and 57 cytoskeleton formation 6 . Subsequent metagenomic studies have suggested that Asgard 58 archaea have a wide variety of physiological properties, including hydrogen-dependent 59 anaerobic autotrophy 7 , peptide or short-chain hydrocarbon-dependent organotrophy 8-11 60 and rhodopsin-based phototrophy 12,13 . A recent study suggests that an ancient Asgard 61 archaea degraded organic substances and syntrophically handed off reducing equivalents 62 (e.g., hydrogen and electrons) to a bacterial partner, and further proposes a symbiogenetic 63 model for the origin of eukaryotes based on this interaction 14 . However, at present, no 64 single representative of the Asgard archaea has been cultivated and, thus, the physiology 65 and cell biology of this clade remains unclear. In an effort to close this knowledge gap, 66 3 we successfully isolated the first Asgard archaeon and here report the physiological 67 characteristics, potentially key insights into the evolution of eukaryotes. 68 69 Isolation of an Asgard archaeon 70Setting out to isolate uncultivated deep marine sediment microorganisms, we engineered 71 and operated a methane-fed continuous-fl...

The bacterial endosymbionts of 3 hydrothermal vent mussels from Japanese waters were characterized by transmission electron microscopic (TEM) observation and phylogenetic analyses of 16S ribosomal RNA gene sequences. Endosymbionts of Bathymodiolus septemdierum were related to sulfur-oxidizing bacteria (thioautotrophs), while endosymbionts of B. platifrons and B. japonicus were related to methane-oxidizing bacteria (methanotrophs). This is the first report of deep-sea mussels containing only methanotrophs (lacking thioautotrophs) from hydrothermal vents. Comparison of methane and hydrogen sulfide concentrations in end-member fluids from deep-sea hydrothermal vents indicated that methane concentrations were much higher in habitats containing Bathymodiolus spp. which harbored only methanotrophs than in other habitats of hydrothermal vent mussels. The known distribution of other mussels containing only methanotrophs has thus far been limited to cold-seep environments with high methane concentrations from the interstitial water. These results suggest that the distribution of methanotrophic symbioses between deep-sea mussels and methanotrophs is strongly influenced by the methane or hydrocarbon concentrations provided from hydrothermal vent and cold-seep activities (or that methane concentration is a possible limiting factor that restricts the distribution of methanotrophy-dependent symbioses in the deep sea).