Biology subjects

Takai, K.

Publications and source records attributed to Takai, K..

10 recordsLinked to original sources

bioRxiv2026

Microorganisms consume trace gases present throughout the Mariana Trench water column

Dark waters harbour two-thirds of the ocean's bacterial and archaeal cells, yet the energy sources sustaining microbial life at these depths remain poorly understood. Here we integrate hydrographic profiles with metagenomic analyses and ex situ activity measurements to investigate whether carbon monoxide (CO) and molecular hydrogen (H2) are viable energy sources for epipelagic and mesopelagic microbial populations in the Mariana Trench region. Both gases were detected from 5 to 9,371 m, with concentrations generally higher in the photic zone but anomalously high in several deeper waters. Metagenomic analyses indicate a shift from phototrophic towards lithotrophic energy acquisition with depth. Microbial populations encoding CO dehydrogenases increased from 6.1% at 5 m to 45% at 1,000 m, while those encoding uptake hydrogenases were much less abundant, but increased from 0.34% to 0.63%. Ex situ incubations revealed that in situ cell-specific CO oxidation rates declined with depth, whereas corresponding H2 oxidation rates were significantly higher at 1,000 m than at the surface. At 1,000 m, cell-specific H2 oxidation rates were approximately 4,500-fold higher than those of CO. These contrasting trends suggest that CO oxidation is a widespread auxiliary energy-acquisition strategy, whereas H2 oxidation may sustain hydrogenotrophic growth in dark waters. Together, our results suggest H2 and CO are readily available to pelagic microbial populations and are biologically oxidised in the dark zone, supporting microbial energy acquisition and oceanic biogeochemical cycling.

microbiology↗

bioRxiv2026

A Tripartite Co-culture System Reveals Defensive Mutualism Between a Nanobdellati Symbiont and Its Host

Archaeal symbioses remain among the least understood cellular interactions. Ultra-small Nanobdellati (initially called DPANN) archaea rely on larger hosts for survival, yet their effects on host eco-physiology and their interactions with infecting viruses have not yet been examined experimentally. Here, we established the first stable tripartite co-culture comprising a Nanobdellales symbiont (YN4), its archaeal host (YN4HA), and a virus (MTIV4). We analyzed this system using physiological, genomic, transcriptomic, glycoproteomic, and cryo-electron tomography (cryoET) approaches. CryoET analysis revealed that the Nanobdellales archaeon formed cone-like structures to contact the host, as has been observed in other Nanobdellati-host systems. In this system, the host is infected by the virus. The Nanobdellales archaeon mitigated virus-induced growth inhibition of the host without any detectable fitness cost, indicating a defensive mutualism rather than a strictly parasitic relationship. This protective effect may involve Nanobdellati-driven remodeling of host cell surface glycans, suggesting a previously unrecognized glycan-mediated defense strategy. Overall, our tripartite system provides new insight into complex archaeal interactions in extreme environments that cannot be captured through conventional binary co-culture systems.

microbiology↗

bioRxiv2025

Discovery of a chemosynthetic community at the serpentinite-hosted seep on the Quaker Seamount, Mariana Forearc

Deep-sea chemosynthesis-based ecosystems in the Mariana Region include hydrothermal vents on the Mariana Arc and in the Mariana Back-Arc, and serpentinite-hosted seeps on the Mariana Forearc - with the latter being by far the least studied. Here, we surveyed the biodiversity of the serpentine seep on the Quaker Seamount. At first glance, the area appears to be devoid of megafauna, but examination of the carbonates revealed dense aggregations of animals dominated by the limpets Bathyacmaea and Pyropelta on brucite-carbonate chimney structures exhibiting visible fluid venting. Sorting of recovered material yielded a total of 14 species and together with an observation of a Munidopsis squat lobster we report a total of 15 species; six of these are considered endemics of chemosynthetic ecosystems. The occurrence of taxa such as the snail Lurifax cf. japonicus and the limpet Pyropelta ryukyuensis, otherwise only known from distant vents in the Izu-Ogasawara Arc and Okinawa Trough off Japan, strengthens the hypothesis that serpentine seeps may function as dispersal stepping-stones across arc and back-arc systems.

ecology↗

bioRxiv2025

Direct carbon monoxide fixation via the bacterial and archaeal Wood-Ljungdahl pathways

The Wood-Ljungdahl (WL) pathway, which is widely distributed in both archaea and bacteria, is an ancient carbon fixation pathway from CO2. CO2 fixation proceeds via two branches of pathway: progressive reduction to the methyl group in the methyl branch and one-step reduction to CO in the carbonyl branch. In the final step of the pathway, the methyl group, CO, and CoA are combined into a carbon monoxide dehydrogenase (CODH)/acetyl-CoA synthase (ACS) complex to form acetyl-CoA. Here, we show direct CO fixation to the carbonyl group of acetyl-CoA in both archaeal and bacterial WL pathways under hydrogenogenic growth conditions using 13C tracer-based metabolomics. A combination of metabolomics and proteomics suggested that the hydrogenotrophically grown Thermodesulfatator indicus and Archaeoglobus sp. strain MCR cells, directly fixed CO using free-form ACS in the carbonyl branch with relatively low CO availability. In contrast, carboxydotrophically grown Archaeoglobus cells utilize the CODH/ACS complex for CO2 fixation rather than CO fixation. Direct CO fixation by free-form ACS is more advantageous for conserving reduced ferredoxin compared with the thermodynamically challenged CO2 reduction by CODH. These findings provide further insight into the origin and evolution of the most ancient inorganic carbon fixation pathway and geochemical cycles on early Earth.

microbiology↗

bioRxiv2025

Population genomics of the endangered scaly-foot snail defines conservation units amid deep-sea mining threats in Indian Ocean vents

Hydrothermal vents in the Indian Ocean face imminent deep-sea mining, yet lack baseline high-resolution connectivity data for their endemic fauna. We present the first population genomic study of the endangered scaly-foot snail (Chrysomallon squamiferum), an iconic species distributed across three vent biogeographic provinces. Analysing 125 individuals from eight vent fields using 14 million single-nucleotide polymorphisms, we identify five genetic groups that warrant recognition as evolutionarily significant units. Demographic modelling reveals critical contributions from extinct or unsampled phantom populations to the contemporary genetic structure. Together with physical ocean modelling, we show that the deep currents drive asymmetric south-to-north gene flows, while transform faults act as dispersal barriers. We propose Longqi-Duanqiao fields on the Southwest Indian Ridge and Wocan field on the Carlsberg Ridge as two isolated populations prioritised for protection. Given its exceptional adaptations, wide distribution, and public recognition, the scaly-foot snail is well-positioned to serve as both a flagship and umbrella species to ensure the survival of a broader suite of vent biodiversity. As the International Seabed Authority finalises its Mining Code in 2025, our findings provide essential genomic evidence to mitigate the impacts of mining on genetic diversity and inform transboundary conservation strategies for this vulnerable ecosystem.

ecology↗

bioRxiv2025

Eukaryotes' closest relatives are internally simple syntrophic archaea

Eukaryotes are theorized to have originated from an archaeal phylum Promethearchaeota (formerly Asgard archaea)1,2. The first cultured representatives revealed valuable insight3,4 but are distantly related to the first eukaryotic common ancestor (FECA), leaving many unknowns regarding this archaeons biology. Here, we report isolation of two strains belonging to the order proposed as FECAs closest relative, Hodarchaeales,5 as members of a pure co- and tri-culture with methanogenic partners. Both are obligately anaerobic, syntrophic, peptide-degrading, and mesophilic archaea that have simple internal cell structure and produce protrusions and vesicles, like Promethearchaeales3,4. All strains demonstrate behavior focused on cell construction rather than division, unlike typical prokaryotes6. Strain HC1 possesses genes associated with aerobic lifestyles but lacks complete pathways for aerobic respiration and co-cultures cannot grow under (micro)aerobic conditions, suggesting the genes support oxygen detoxification rather than respiration. Reflecting this, HC1 can survive and grow under microaerobic conditions only when aerobic organisms are present. Phylogenetic analyses indicate FECA may have possessed these genes and thus some aerotolerance. Physiological, genomic, and phylogenetic observations indicate FECA was a simple-celled anaerobic syntrophic peptide-degrading archaeon with a non-growth-centric lifestyle and potential adaptations towards an oxygenated planet--the archaea-eukaryote transition was steep in both cell structure and aerobiosis.

microbiology↗

bioRxiv2023

DNA-PK and the TRF2 iDDR inhibit MRN-initiated resection at leading-end telomeres

Telomeres replicated by leading-strand synthesis lack the 3 overhang required for telomere protection. Surprisingly, resection of these blunt telomere is initiated by the telomere-specific 5 exonuclease Apollo rather than the Mre11-Rad50-Nbs1 (MRN) complex, the nuclease that acts at DNA breaks. Without Apollo, leading-end telomeres undergo fusion, which, as demonstrated here, are mediated by alternative End Joining. Here, we show that DNA-PK and TRF2 coordinate the repression of MRN at blunt telomeres. DNA-PK represses an MRN-dependent long range resection at blunt telomeres, while the endonuclease activity of MRN/CtIP, which could cleave DNA-PK off of blunt telomere ends, is inhibited in vitro and in vivo by the iDDR of TRF2. AlphaFold-Multimer predicts a conserved association of the iDDR with Rad50 potentially interfering with CtIP binding and MRN endonuclease activation. We propose that repression of MRN-mediated resection is a conserved aspect of telomere maintenance and represents an ancient feature of DNA-PK and the iDDR.

molecular biology↗

bioRxiv2020

Structural variant evolution after telomere crisis

Telomere crisis contributes to cancer genome evolution, yet only a subset of cancers display breakage-fusion-bridge (BFB) cycles and chromothripsis, hallmarks of previous experimental telomere crisis studies. We examine the spectrum of SVs instigated by natural telomere crisis. Spontaneous post-crisis clones from prior studies had both complex and simple SVs without BFB cycles or chromothripsis. In contrast, BFB cycles and chromothripsis occurred in clones that escaped from telomere crisis after CRISPR-controlled telomerase activation in MRC5 fibroblasts. This system revealed convergent evolutionary lineages altering one allele of 12p, where a short telomere likely predisposed to fusion. Remarkably, the 12p chromothripsis and BFB events were stabilized by independent fusions to 21. Telomere crisis can therefore generate a wide spectrum of SVs, and lack of BFB patterns and chromothripsis does not indicate absence of past crisis.

genomics↗

bioRxiv2019

Microbial community and geochemical analyses of trans-trench sediments for understanding the roles of hadal environments

Hadal trench bottom (>6,000 m below sea level) sediments harbor higher microbial cell abundance compared to adjacent abyssal plain sediments. This is supported by the accumulation of sedimentary organic matter (OM), facilitated by trench topography. However, the distribution of benthic microbes in different trench systems has not been explored yet. Here, we carried out small subunit ribosomal RNA gene tag sequencing for 92 sediment subsamples of seven abyssal and seven hadal sediment cores collected from three trench regions in the northwest Pacific Ocean: the Japan, Izu-Ogasawara, and Mariana Trenches. Tag-sequencing analyses showed specific distribution patterns of several phyla associated with oxygen and nitrate. The community structure was distinct between abyssal and hadal sediments, following geographic locations and factors represented by sediment depth. Co-occurrence network revealed six potential prokaryotic consortiums that covaried across regions. Our results further support that the endogenous OM cycle is driven by hadal currents and/or rapid burial shapes microbial community structures at trench bottom sites, in addition to vertical deposition from the surface ocean. Our trans-trench analysis highlights intra- and inter-trench distributions of microbial assemblages and geochemistry in surface seafloor sediments, providing novel insights into ultra-deep-sea microbial ecology, one of the last frontiers on our planet.

microbiology↗

bioRxiv2019

Isolation of an archaeon at the prokaryote-eukaryote interface

The origin of eukaryotes remains enigmatic. Current data suggests that eukaryotes may have risen from an archaeal lineage known as \"Asgard archaea\". Despite the eukaryote-like genomic features found in these archaea, the evolutionary transition from archaea to eukaryotes remains unclear due to the lack of cultured representatives and corresponding physiological insight. Here we report the decade-long isolation of a Lokiarchaeota-related Asgard archaeon from deep marine sediment. The archaeon, \"Candidatus Prometheoarchaeum syntrophicum strain MK-D1\", is an anaerobic, extremely slow-growing, small cocci ([~]550 nm), that degrades amino acids through syntrophy. Although eukaryote-like intracellular complexities have been proposed for Asgard archaea, the isolate has no visible organella-like structure. Ca. P. syntrophicum instead displays morphological complexity - unique long, and often, branching protrusions. Based on cultivation and genomics, we propose an \"Entangle-Engulf-Enslave (E3) model\" for eukaryogenesis through archaea-alphaproteobacteria symbiosis mediated by the physical complexities and metabolic dependency of the hosting archaeon.

microbiology↗