Toki Tomohiro

写真a

Title

Associate Professor

Researcher Number(JSPS Kakenhi)

50396925

Homepage URL

http://www.cc.u-ryukyu.ac.jp/~toki/index.html

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Current Affiliation Organization 【 display / non-display

  • Duty   University of the Ryukyus   Faculty of Science   Chemistry, Biology and Marine Science   Associate Professor  

University 【 display / non-display

  •  
    -
    1999.03

    The University of Tokyo   Faculty of Science   Department of Chemistry   Graduated

Graduate School 【 display / non-display

  •  
    -
    2001.03

    The University of Tokyo  Graduate School, Division of Natural Science  Master's Course  Completed

  •  
    -
    2004.03

    Hokkaido University  Graduate School, Division of Natural Science  Division of Earth and Planetary Sciences  Doctor's Course (second term)  Completed

Academic degree 【 display / non-display

  • Hokkaido University -  Doctor of Science

External Career 【 display / non-display

  • 2007.04
    -
    2015.04

    University of the Ryukyus, Faculty of Science, Department of Chemistry, Biology, and Marine Science, Chemistry Program, Research Associate  

  • 2015.05
     
     

    University of the Ryukyus, Faculty of Science, Department of Chemistry, Biology, and Marine Science, Chemistry Program, Associate Professor  

Affiliated academic organizations 【 display / non-display

  • 2000.04
    -
    Now
     

    The Geochemical Society of Japan 

  • 2001.04
    -
    Now
     

    The Geological Society of Japan 

  • 2002.04
    -
    Now
     

    American Geophysical Union 

  • 2015.06
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    Now
     

    The Soceity of Sea Water Science, Japan 

Research Interests 【 display / non-display

  • Geochemistry

  • Geochemistry

Research Areas 【 display / non-display

  • Earth Astrochemistry

Published Papers 【 display / non-display

  • Sr isotopic ratios of hydrothermal fluids from the Okinawa Trough and the implications of variation in fluid–sediment interactions

    Tomohiro Toki, Tasuku Nohara, Yoshiaki Urata, Ryuichi Shinjo, Shuko Hokakubo-Watanabe, Jun-ichiro Ishibashi, and Shinsuke Kawagucci

    Progress in Earth and Planetary Science ( Springer Nature )  9 ( 1 ) 59   2022.11 [ Peer Review Accepted ]

    Type of publication: Research paper (scientific journal)

     View Summary

    沖縄トラフにおける海底熱水中のSr同位体比を比較すると,海水の混入を補正しても,海水よりもはるかに高い同位体比を示すことがわかった。このことから,海水よりもはるかに高い固体と反応していることが示唆され,沖縄トラフに供給されている大陸地殻を起源とする粘土鉱物と反応していることが示唆された。こういった高いSr同位体比は,堆積物が被覆している海底熱水系で見られる共通の特徴であると言える。

  • Origin of helium in basement rocks and carbonate veins in Yonaguni Island

    Toki, T; Yasumura, K; Takahata, N; Miyajima, Y; Miyaki, H; Oohashi, K; Otsubo, M

    GEOCHEMICAL JOURNAL ( 一般社団法人日本地球化学会 )  58 ( 6 ) 293 - 303   2024 [ Peer Review Accepted ]

    Type of publication: Research paper (scientific journal)

     View Summary

    <p>Minerals formed in high-temperature environments are distributed along faults on Yonaguni Island. Volcanic activity is thought to be a possible heat source. In this study, samples from the carbonate veins distributed around the basement rocks and faults of Yonaguni Island were melted in vacuum, and the concentrations and isotope ratios of the noble gases in the furnace were investigated. The observed isotope ratios suggest that the noble gases were dominated by crustal helium, with little influence from mantle helium. These results suggest that there was some kind of non-volcanic heat supply at Yonaguni Island (e.g., eruption of non-volcanic hot springs).</p>

  • Identification of a large mud volcano field in the Hyuga-nada, northern end of the Ryukyu trench, offshore Japan

    Asada, M; Yamashita, M; Fukuchi, R; Yokota, T; Toki, T; Ijiri, A; Kawamura, K

    FRONTIERS IN EARTH SCIENCE ( Frontiers in Earth Science )  11   2023.11 [ Peer Review Accepted ]

    Type of publication: Research paper (scientific journal)

     View Summary

    We identified 27 new mud volcanoes, including potential ones, in a part of the Hyuga-nada area, southwest offshore Japan, at the northern end of the Ryukyu Trench, based on subseafloor geological structures using geophysical investigations. These mud volcanoes exhibited high density and breadth and were likely connected to other mud volcano fields in the south. Acoustic investigations indicated subseafloor structures. Multiple acoustically transparent bodies were interpreted as a region containing gas. They were likely to appear along faults and below the bottom of valleys and sometimes reached the seafloor, expressing mud volcanoes onto the seafloor. They also indicated the wide distribution of subseafloor free-gas throughout the area. These acoustic investigations suggested that a swarm of mud volcanoes exists over the Hyuga-nada area, heterogeneously distributed along a series of plate convergent margins, the Nankai Trough, and the northern part of the Ryukyu Trench.

  • Distribution of dissolved methane in seawater from the East China Sea to the Ryukyu forearc

    Toki, T; Chibana, H; Shimabukuro, T; Yamakawa, Y

    FRONTIERS IN EARTH SCIENCE ( Frontiers in Earth Science )  11   2023.11 [ Peer Review Accepted ]

    Type of publication: Research paper (scientific journal)

  • Assessing the activity of mud volcanism using boron isotope ratios in pore water from surface sediments of mud volcanoes off Tanegashima (SW Japan)

    Mitsutome, Y; Agena, K; Toki, T; Song, KH; Shinjo, R; Ijiri, A

    FRONTIERS IN MARINE SCIENCE ( Frontiers in Marine Science )  10   2023.09 [ Peer Review Accepted ]

    Type of publication: Research paper (scientific journal)

     View Summary

    Mud volcanoes can cause various geohazards, so it is very important to know their activity level and their distribution. Surface sediments were collected from four submarine mud volcanoes (MVs) off Tanegashima (SW Japan), namely, MV1, MV2, MV3, and MV14. We extracted pore water from the surface sediments and investigated its chemical and isotopic compositions. The sodium (Na) and chloride (Cl<sup>-</sup>) concentrations decreased and the boron (B) and lithium (Li) concentrations increased with increasing depth, suggesting that some fluids with lower Na and Cl<sup>-</sup> concentrations and higher B and Li concentrations than seawater were supplied upward from the deep sub-seafloor. The fluid advection velocities estimated from the pore-water profiles differed for each MV, and those of MV3 were the fastest (14 cm/yr) in this study. The estimated equilibrium temperature with clay minerals using Na and Li concentrations were 93-134°C, corresponding to the temperature of environments around 3.7 to 5.3 km below the seafloor. This indicates that these components originated from these depths and that the origin depth did not reach the plate boundary in this area. The B isotope ratio in the pore water was extremely high up to +57 ‰, suggesting that it was strongly affected by adsorption onto the surface of the sediments. A higher B isotope ratio (+57 ‰) was detected in MV3, which was considered to be more active, indicating that more B was adsorbed onto clay minerals supplied from deeper depths.

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Books 【 display / non-display

  • Nature in the Ryukyu Archipelago

    Tomohiro Toki ( Part: Single Author ,  When do you research hydrothermal systems? Now! )

    Change and Coral Reef/Island Dynamics Faculty of Science, University of the Ryukyus  2015

     View Summary

    沖縄トラフの海底熱水研究の最新トピックをわかりやすく英語で紹介。

  • Deep-sea Life - Biological observations using research submersibles

    Jun-ichiro Ishibashi, Tomhiro Toki ( Part: Multiple Authorship )

    Tokai University Press  2008.02

Other Papers 【 display / non-display

  • Contribution and mission of geochemistry to mud volcano study

    Tomohiro Toki

    Bulletin of the Faculty of Science, University of the Ryukyus ( Faculty of Science, University of the Ryukyus )  ( 108 ) 1 - 26   2020.03

     

  • Simple method of collecting pyrolysis gas from bagasse

    Ryo Itou, Keiko Nakasone, Tomohiro Toki

    Bulletin of the Faculty of Science, University of the Ryukyus ( Faculty of Science, University of the Ryukyus )  ( 102 ) 1 - 11   2016.09

     

  • Community structure of a microbial mat from the methane seep off Yagaji Island

    Tomohiro Toki, Hisako Hirayama, Syogo Oshima

    Bulletin of the Faculty of Science, University of the Ryukyus ( Faculty of Science, University of the Ryukyus )  ( 100 ) 5 - 12   2015.09

     

  • Geochemical and geological investigations in the area around the southern Ryukyu islands - Report on RN10 cruise by T/S Nagasaki-maru -

    Tomohiro Toki, Masahide Furukawa, Hiroshi Yoshimura, Youji Kanda, Dae-Yul Baek, Kazuhiko Fujita, and Hiroyuki Fujimura

    Bulletin of the Faculty of Science, University of the Ryukyus ( Faculty of Science, University of the Ryukyus )  ( 91 ) 9 - 19   2011.03

     

  • Geochemical exploration in the Nankai Trough using a time Sseries water sampler

    Tomohiro Toki, Urumu Tsunogai, Toshitaka Gamo

    Chikyu monthly   51   204 - 212   2005.07

     

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Presentations 【 display / non-display

  • Indigenous traditions and water governance: The case of the Erfeng irrigation canal

    Miyuki Shimabukuro, Tomohiro Toki, Yoshiaki Kubo, Hitoshi Shimabukuro

    The 2nd International Sociohydrology Conference  (東京大学・本郷キャンパス)  2025.07  -  2025.07 

  • Origin of lithium in pore fluids near offshore fault zone, northern Noto Peninsula, two months after the 2024 Noto Peninsula earthquake (M7.6) during the R/V Hakuho-maru cruise

    Zahra Zandvakili, Yoshiro Nishio, Tomohiro Toki, Takanori Kagoshima, Jin-Oh Park

    日本地球惑星科学連合2025年大会  (幕張メッセ)  2025.05  -  2025.05 

  • Distribution of dissolved methane in seawater from the East China Sea to the Ryukyu forearc

    TOKI, Tomohiro

    Annual Meeting of the Geological Society of Japan  2024.09  -  2024.09 

  • Origin of fluids in surface sediments of submarine mud volcanoes off Hyuga-nada, Tanegashima Island, and Kikaijima Island

    Kantaro Yamada, Tomohiro Toki, Hironori Otsuka, Takuya Itaki, Masafumi Murayama, Akira Ijiri

    Abstracts of Annual Meeting of the Geochemical Society of Japan  2024  -  2024 

    CiNii Research

  • Toward detection of slow slips in Hyuga-Nada: Challenge with seafloor optical-fiber strainmeter

    KINOSHITA Masa, ARAKI Eiichiro, NAKATA Rie, TOKI Tomohiro, YOKOTA Yusuke, YAMASHITA Yusuke, HASHIMOTO Yoshitaka, HAMADA Yohei, SAWAI Michiyo

    Annual Meeting of the Geological Society of Japan  2024  -  2024 

    CiNii Research

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Grant-in-Aid for Scientific Research 【 display / non-display

  • Can seamount subduction weaken locking of megathrust earthquake? Test at 2 seamounts in Nankai Trough

    Grant-in-Aid for Scientific Research(S)

    Project Year: 2024.04  -  2029.03 

    Direct: 152,900,000 (YEN)  Overheads: 198,770,000 (YEN)  Total: 45,870,000 (YEN)

  • Geosphere-hydrosphere-biosphere connected by submarine mud volcanism: Diffusion processes of deep life and carbon, and their effects on the ocean

    Grant-in-Aid for Scientific Research(A)

    Project Year: 2024.04  -  2029.03 

    Direct: 36,800,000 (YEN)  Overheads: 47,840,000 (YEN)  Total: 11,040,000 (YEN)

  • Grant-in-Aid for Scientific Research(C)

    Project Year: 2023.04  -  2027.03 

    Direct: 3,600,000 (YEN)  Overheads: 4,680,000 (YEN)  Total: 1,080,000 (YEN)

  • Fluid flow in the uppermost part of the incoming plate seaward of the trench: Regional variations and influence on processes around the plate interface

    Grant-in-Aid for Scientific Research(B)

    Project Year: 2023.04  -  2026.03 

    Direct: 14,400,000 (YEN)  Overheads: 18,720,000 (YEN)  Total: 4,320,000 (YEN)

  • Construction of a model for the diffusion and circulation of deep subsurface life and carbon to the ocean via submarine mud volcanism

    Grant-in-Aid for Scientific Research(B)

    Project Year: 2020.04  -  2023.03 

    Direct: 13,500,000 (YEN)  Overheads: 17,550,000 (YEN)  Total: 4,050,000 (YEN)

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Other External funds 【 display / non-display

  • Project Name: Research Project

    Project Year: 2019.04  -  2027.03 

    Offer Organization: Research Institute for Humanity and Nature

SDGs 【 display / non-display

  • 与那国島の湧水への海水侵入の進行について

  • 南の島における水資源の有効活用に関する教材

Amount of external funds acquired by year 【 display / non-display

  • 2022year   基盤A,東京地学協会,FOST   3500000yen

  • 2012year   新学術領域   3000000yen

  • 2015year   萌芽   1900000yen

  • 2016year   地域志向推進経費,萌芽   2046755yen

  • 2017year   萌芽   525879yen

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Social Activity 【 display / non-display

  • 2025.03
     
     

  • 2024.12
     
     

  • 2024.12
     
     

  • 2024.08
     
     

  • 2024.07
     
     

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Media Coverage 【 display / non-display

  • 「流体」の謎…海底の泥を分析  TV or radio program

    ㈱テレビ朝日  サンデーステーション  2024.3

    Author: Other 

     View Summary

    能登半島地震では,地球深部から供給されている”流体”が地震を引き起こしていることが指摘されてきているものの,その正体はよくわかっていない。当研究室では,能登半島地震の震源域近くの海底堆積物中から間隙水を抽出して持ち帰り,陸上において化学分析を行うことで,流体の化学組成を明らかにすることを目指している。

  • 種子島沖海底泥火山における表層堆積物中の希ガスを用いた流体の起源深度の推定  Internet

    Chem-Station  Chem-Station  2023.5

    Author: Other 

     View Summary

    種子島沖海底泥火山の表層堆積物中から抽出したガス中の希ガス濃度から,溶解平衡温度を見積もり,その深度を推定したところ,海底下数kmであることが明らかとなった。このことから,本泥火山の表層堆積物中の希ガスが,採取される直前まで海底下数kmにあったことが示唆され,泥火山の噴出現象によって海底直下まで移動させられたことが示唆された。

  • 水が枯渇したら全員の負け 研究者が考案した「南の島」のボードゲーム  Newspaper, magazine

    沖縄タイムス  沖縄タイムス  2023.2

    Author: Other 

     View Summary

    南の島特有の地域課題である水資源問題を,老若男女楽しく学ぶことができる環境教材ツール”すいまーる”を監修したことについて,関連論文が受理された。

  • 巨大岩から水が出ていた  TV or radio program

    ㈱テレビ朝日  ナニコレ珍百景  2022.8

    Author: Myself 

     View Summary

    投稿者の家の裏山の巨大な岩から水が滴っていたことを,通常の湧水にすぎない,と解説した。オンラインでインタビューを録画してVTRは作製したが,放映はされなかった。

  • JAMSTEC調査研究船「新青丸」の調査航海、種子島沖海底泥火山でメタンハイドレートを発見  Internet

    FUNECO船舶ニュース  FUNECO船舶ニュース  2022.1

    Author: Other 

     View Summary

    種子島沖海底泥火山の表層堆積物中から,メタンハイドレートの採取に成功した。本海域では,初めての成果となり,今後周辺海底に大量のメタンハイドレートの分布が期待される。

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