1,206 results on '"Takai, Ken"'
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52. Geochemical Constraints on Potential Biomass Sustained by Subseafloor Water–Rock Interactions
53. Introduction of TAIGA Concept
54. Cultivable microbial community in 2-km-deep, 20-million-year-old subseafloor coalbeds through ~1000 days anaerobic bioreactor cultivation
55. In Situ Measurement of Liquid and Gas CO2 with High Purity at Deep-Sea Hydrothermal Vents in the Mariana Arc Using Raman Spectroscopy.
56. Supplementary Figure Legend from HTLV-1 bZIP Factor Suppresses Apoptosis by Attenuating the Function of FoxO3a and Altering Its Localization
57. Data from HTLV-1 bZIP Factor Suppresses Apoptosis by Attenuating the Function of FoxO3a and Altering Its Localization
58. Supplementary Figures 1 - 7 from HTLV-1 bZIP Factor Suppresses Apoptosis by Attenuating the Function of FoxO3a and Altering Its Localization
59. Identification and genomic analysis of temperate Pseudomonas bacteriophage PstS-1 from the Japan trench at a depth of 7000 m
60. Mariprofundus micogutta sp. nov., a novel iron-oxidizing zetaproteobacterium isolated from a deep-sea hydrothermal field at the Bayonnaise knoll of the Izu-Ogasawara arc, and a description of Mariprofundales ord. nov. and Zetaproteobacteria classis nov.
61. The Family Nautiliaceae: The Genera Caminibacter, Lebetimonas, and Nautilia
62. The Family Hydrogenothermaceae
63. Hadal biosphere : Insight into the microbial ecosystem in the deepest ocean on Earth
64. R/V Kaimei, KM-ROV, and BMS Cruise Report KM23-05
65. Genetics, Genomics, Evolution
66. Biochemistry
67. Physiology
68. Quantification of polysulfide species in aqueous sulfur thermocell
69. A Simple and Effective Method for Solid Medium Cultivation of Strictly Hydrogen- and Sulfur-oxidizing Chemolithoautotrophs Predominant in Deep-sea Hydrothermal Fields
70. Domain-level Identification of Single Prokaryotic Cells by Optical Photothermal Infrared Spectroscopy
71. Isotopic evidence for water-column denitrification and sulfate reduction at the end-Guadalupian (Middle Permian)
72. Nitrosophilus kaiyonis sp. nov., a hydrogen-, sulfur- and thiosulfate-oxidizing chemolithoautotroph within “Campylobacteria” isolated from a deep-sea hydrothermal vent in the Mid-Okinawa Trough
73. Physiological and comparative proteomic characterization of Desulfolithobacter dissulfuricans gen. nov., sp. nov., a novel mesophilic, sulfur-disproportionating chemolithoautotroph from a deep-sea hydrothermal vent
74. Nitrogen isotope chemostratigraphy across the Permian–Triassic boundary at Chaotian, Sichuan, South China
75. Hydrogen isotope systematics among H2–H2O–CH4 during the growth of the hydrogenotrophic methanogen Methanothermobacter thermautotrophicus strain ΔH
76. Compositional, Physiological and Metabolic Variability in Microbial Communities Associated with Geochemically Diverse, Deep-Sea Hydrothermal Vent Fluids
77. Electrochemical CO2 Reduction by Ni-containing Iron Sulfides: How Is CO2 Electrochemically Reduced at Bisulfide-Bearing Deep-sea Hydrothermal Precipitates?
78. Physiological and isotopic characteristics of nitrogen fixation by hyperthermophilic methanogens: Key insights into nitrogen anabolism of the microbial communities in Archean hydrothermal systems
79. Nitrogen isotope chemostratigraphy of the Ediacaran and Early Cambrian platform sequence at Three Gorges, South China
80. FTIR microspectroscopy of Ediacaran phosphatized microfossils from the Doushantuo Formation, Weng'an, South China
81. Planetary protection on international waters: An onboard protocol for capsule retrieval and biosafety control in sample return mission
82. Unexpected discovery of a serpentinite‐hosted chemosynthetic ecosystem on Asùt Tesoru Seamount, Mariana Forearc.
83. FTIR microspectroscopy of carbonaceous matter in ~ 3.5 Ga seafloor hydrothermal deposits in the North Pole area, Western Australia
84. Cool, alkaline serpentinite formation fluid regime with scarce microbial habitability and possible abiotic synthesis beneath the South Chamorro Seamount
85. Hydrogen and carbon isotope systematics in hydrogenotrophic methanogenesis under H2-limited and H2-enriched conditions: implications for the origin of methane and its isotopic diagnosis
86. Reactions between komatiite and CO2-rich seawater at 250 and 350 °C, 500 bars: implications for hydrogen generation in the Hadean seafloor hydrothermal system
87. In situ electrosynthetic bacterial growth using electricity generated by a deep-sea hydrothermal vent
88. Unusual bromine enrichment in the gastric mill and setae of the hadal amphipod Hirondellea gigas
89. Reactions between basalt and CO2-rich seawater at 250 and 350 °C, 500 bars: Implications for the CO2 sequestration into the modern oceanic crust and the composition of hydrothermal vent fluid in the CO2-rich early ocean
90. Decrease of seawater CO2 concentration in the Late Archean: An implication from 2.6 Ga seafloor hydrothermal alteration
91. Nitrification-driven forms of nitrogen metabolism in microbial mat communities thriving along an ammonium-enriched subsurface geothermal stream
92. Geochemical origin of hydrothermal fluid methane in sediment-associated fields and its relevance to the geographical distribution of whole hydrothermal circulation
93. Hydrogen-rich hydrothermal environments in the Hadean ocean inferred from serpentinization of komatiites at 300 °C and 500 bar
94. Seasonal change in microbial sulfur cycling in monomictic Lake Fukami-ike, Japan
95. Uniaxial orientation of β-chitin nanofibres used as an organic framework in the scales of a hot vent snail
96. SPOTLIGHT 9 | South Chamorro Seamount : 13°7.00'N, 146°00.00'E
97. Abiogenic formation of H2, light hydrocarbons and other short-chain organic compounds within the serpentinite mud volcanoes of the Marianna Trench
98. Cell Proliferation at 122°C and Isotopically Heavy CH₄ Production by a Hyperthermophilic Methanogen under High-Pressure Cultivation
99. A Potential Link between Alternative Splicing of the NBS1 Gene and DNA Damage/Environmental Stress
100. Archaeal diversity and community development in deep-sea hydrothermal vents
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