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Ocean Research Institute, University of Tokyo, Minami-dai, Nakano, Tokyo 164 Japan
Division of Earth and Planetary Sciences, Graduate School of Science, Hokkaido University, N10 W8, Sapporo 060-0810, Japan; Ocean Research Institute, The University of Tokyo, Nakano, Tokyo 164-8639, Japan.
DSM-CEA, Gif sur Yvette, France
Ocean Research Institute, University of Tokyo, Minamidai, Nakano-ku, Tokyo 164, Japan
Ocean Research Institute, University of Tokyo, Tokyo, Japan
Ocean Research Institute, University of Tokyo, Nakano-ku, Tokyo, Japan
Ocean Research Institute, University of Tokyo, Japan
Ocean Research Institute, The University of Tokyo, 1-15-1 Minamidai Nakano, Tokyo, Japan
Division of Earth and Planetary Sciences, Graduate School of Science, Hokkaido University, N10 W8, Kita-ku, Sapporo 060-0810, Japan; Marine Inorganic Chemistry Group, Department of Chemical Oceanography, Ocean Research Institute, The University of Tokyo, 1-15-1, Minamidai, Nakano-ku, Tokyo 164-8639, Japan
Ocean Research Institute, University of Tokyo, Minamidai, Tokyo, Japan
Ocean Research Institute, University of Tokyo, Minamidai 1-15-1, Tokyo 164, Japan
Ocean Research Institute, University of Tokyo, Minamidai 1-15-1, Nakano-ku, Tokyo 164, Japan
Ocean Research Institute, University of Tokyo, 1-15-1 Minamidai, Nakano-ku, Tokyo 164, Japan
Tokyo Univ., Tokyo, Japan
"Microbial plumes" as inferred from the increase of stable carbon isotope composition of methane originated from submarine hydrothermal activity
10% decrease of dissolved oxygen in the Japan Sea (East Sea) bottom water for the last 30 years
An evaluation for mixing and biological processes based on oxygen isotopic ratios of dissolved oxygen
Boron and halide systematics in submarine hydrothermal systems: Effects of phase separation and sedimentary contributions
Carbon and helium isotope systematics of North Fiji Basin basalt glasses: carbon geochemical cycle in the subduction zone
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