M
Masanori Kaneko
Researcher at National Institute of Advanced Industrial Science and Technology
Publications - 32
Citations - 943
Masanori Kaneko is an academic researcher from National Institute of Advanced Industrial Science and Technology. The author has contributed to research in topics: Methanogenesis & Archaea. The author has an hindex of 14, co-authored 29 publications receiving 755 citations. Previous affiliations of Masanori Kaneko include Kobe University & Japan Agency for Marine-Earth Science and Technology.
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Journal ArticleDOI
Exploring deep microbial life in coal-bearing sediment down to ~2.5 km below the ocean floor
Fumio Inagaki,Kai-Uwe Hinrichs,Yusuke Kubo,Marshall W. Bowles,Verena B Heuer,Wei-Li Hong,Tatsuhiko Hoshino,Akira Ijiri,Hiroyuki Imachi,Motoo Ito,Masanori Kaneko,Mark A. Lever,Yu-Shih Lin,Barbara A. Methé,Sumito Morita,Yuki Morono,Wataru Tanikawa,Monika Bihan,Stephen A. Bowden,Marcus Elvert,Clemens Glombitza,D Gross,Guy J. Harrington,Tomoyuki Hori,Kelvin Li,D Limmer,Chang-Hong Liu,Masafumi Murayama,Naohiko Ohkouchi,Shuhei Ono,Y. S. Park,Stephen C. Phillips,Xavier Prieto-Mollar,M Purkey,Natascha Riedinger,Yoshinori Sanada,Justine Sauvage,Glen Snyder,Rita Susilawati,Yoshinori Takano,Eiji Tasumi,Takeshi Terada,Hitoshi Tomaru,Elizabeth Trembath-Reichert,David T. Wang,Yasuhiro Yamada,Yasuhiro Yamada +46 more
TL;DR: Evidence is provided for the existence of microbial communities in ~40° to 60°C sediment associated with lignite coal beds at ~1.5 to 2.5 km below the seafloor in the Pacific Ocean off Japan, which suggests that terrigenous sediments retain indigenous community members tens of millions of years after burial in the seabed.
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Methane sources and production in the northern Cascadia margin gas hydrate system
TL;DR: In this article, a transect was used to identify the relevant methane evolution pathways in the northern Cascadia accretionary margin, a four-site traning was drilled during Integrated Ocean Drilling Program Expedition 311, and the δ13C values of methane range from a minimum value of −82.2 to −39.5
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Magnetostratigraphy of Plio-Pleistocene sediments in a 1700-m core from Osaka Bay, southwestern Japan and short geomagnetic events in the middle Matuyama and early Brunhes chrons
D.K Biswas,Masayuki Hyodo,Y Taniguchi,Masanori Kaneko,Shigehiro Katoh,Hiroshi Sato,Y Kinugasa,K Mizuno +7 more
TL;DR: A magnetic polarity stratigraphy spanning more than the past 3.2 Myr was determined for a long 1545 m continuous sedimentary sequence of marine, fluvial, and lacustrine deposits from the Osaka Basin, southwestern Japan as discussed by the authors.
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Temperature limits to deep subseafloor life in the Nankai Trough subduction zone
Verena B Heuer,Fumio Inagaki,Yuki Morono,Yusuke Kubo,Arthur J. Spivack,Bernhard Viehweger,Tina Treude,Felix Beulig,Florence Schubotz,Satoshi Tonai,Stephen A. Bowden,M Cramm,Susann Henkel,Takehiro Hirose,K. Homola,Tatsuhiko Hoshino,Akira Ijiri,Hiroyuki Imachi,Nana Kamiya,Masanori Kaneko,Lorenzo Lagostina,Hayley Manners,H L O McClelland,K. Metcalfe,Natsumi Okutsu,Donald Pan,M J Raudsepp,Justine Sauvage,Man-Yin Tsang,David T. Wang,E Whitaker,Yuzuru Yamamoto,Kiho Yang,Lena Maeda,Rishi Ram Adhikari,Clemens Glombitza,Yohei Hamada,Jens Kallmeyer,Jenny Wendt,Lars Wörmer,Yasuhiro Yamada,Masataka Kinoshita,Kai-Uwe Hinrichs +42 more
TL;DR: Investigating microbial life in up to 1.2-kilometer-deep and up to 120°C hot sediments in the Nankai Trough subduction zone found that microbial life decreases as depth and temperature increases down to ∼600 meters below the seafloor, corresponding to temperatures of ∼70°C.
Journal ArticleDOI
Quantitative analysis of coenzyme F430 in environmental samples: a new diagnostic tool for methanogenesis and anaerobic methane oxidation.
Masanori Kaneko,Yoshinori Takano,Yoshito Chikaraishi,Nanako O. Ogawa,Susumu Asakawa,Takeshi Watanabe,Seigo Shima,Martin Krüger,Makoto Matsushita,Hiroyuki Kimura,Naohiko Ohkouchi +10 more
TL;DR: The development of a technique for high-sensitivity analysis of F430 in environmental samples, including paddy soils, marine sediments, microbial mats, and an anaerobic groundwater is reported.