Geochemistry of REY-rich mud in the Japanese Exclusive Economic Zone around Minamitorishima Island

  • Fujinaga Koichiro
    Ocean Resources Research Center for Next Generation, Chiba Institute of Technology Frontier Research Center for Energy and Resources, School of Engineering, The University of Tokyo
  • Yasukawa Kazutaka
    Ocean Resources Research Center for Next Generation, Chiba Institute of Technology Department of Systems Innovation, School of Engineering, The University of Tokyo
  • Nakamura Kentaro
    Department of Systems Innovation, School of Engineering, The University of Tokyo
  • Machida Shiki
    Research and Development Center for Submarine Resources, Japan Agency for Marine-Earth Science and Technology (JAMSTEC)
  • Takaya Yutaro
    Frontier Research Center for Energy and Resources, School of Engineering, The University of Tokyo Research and Development Center for Submarine Resources, Japan Agency for Marine-Earth Science and Technology (JAMSTEC) Department of Resources and Environmental Engineering, School of Creative Science and Engineering, Waseda University
  • Ohta Junichiro
    Department of Solid Earth Geochemistry, Japan Agency for Marine-Earth Science and Technology (JAMSTEC)
  • Araki Shuhei
    Department of Systems Innovation, School of Engineering, The University of Tokyo
  • Liu Hanjie
    Department of Systems Innovation, School of Engineering, The University of Tokyo
  • Usami Ryo
    Department of Systems Innovation, School of Engineering, The University of Tokyo
  • Maki Ryota
    Department of Systems Innovation, School of Engineering, The University of Tokyo
  • Haraguchi Satoru
    Department of Solid Earth Geochemistry, Japan Agency for Marine-Earth Science and Technology (JAMSTEC)
  • Nishio Yoshiro
    Department of Marine Resource Sciences, Faculty of Agriculture and Marine Science, Kochi University
  • Usui Yoichi
    Research and Development Center for Submarine Resources, Japan Agency for Marine-Earth Science and Technology (JAMSTEC)
  • Nozaki Tatsuo
    Frontier Research Center for Energy and Resources, School of Engineering, The University of Tokyo Research and Development Center for Submarine Resources, Japan Agency for Marine-Earth Science and Technology (JAMSTEC) Department of Planetology, Graduate School of Science, Kobe University
  • Yamazaki Toshitsugu
    Department of Ocean Floor Geoscience, Atmosphere and Ocean Research Institute, The University of Tokyo Geological Survey of Japan, National Institute of Advanced Industrial Science and Technology
  • Ichiyama Yuji
    Department of Earth Sciences, Faculty of Science, Chiba University
  • Ijiri Akira
    Research and Development Center for Submarine Resources, Japan Agency for Marine-Earth Science and Technology (JAMSTEC) Kochi Institute for Core Sample Research, Japan Agency for Marine-Earth Science and Technology (JAMSTEC)
  • Inagaki Fumio
    Research and Development Center for Submarine Resources, Japan Agency for Marine-Earth Science and Technology (JAMSTEC) Kochi Institute for Core Sample Research, Japan Agency for Marine-Earth Science and Technology (JAMSTEC)
  • Machiyama Hideaki
    Research and Development Center for Submarine Resources, Japan Agency for Marine-Earth Science and Technology (JAMSTEC)
  • Iijima Koichi
    Research and Development Center for Submarine Resources, Japan Agency for Marine-Earth Science and Technology (JAMSTEC)
  • Suzuki Katsuhiko
    Research and Development Center for Submarine Resources, Japan Agency for Marine-Earth Science and Technology (JAMSTEC)
  • Kato Yasuhiro
    Ocean Resources Research Center for Next Generation, Chiba Institute of Technology Frontier Research Center for Energy and Resources, School of Engineering, The University of Tokyo Department of Systems Innovation, School of Engineering, The University of Tokyo Research and Development Center for Submarine Resources, Japan Agency for Marine-Earth Science and Technology (JAMSTEC)

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Abstract

<p>We report detailed lithological and chemical characteristics of deep-sea sediments, including rare-earth elements and yttrium-rich mud (REY-rich mud), in the Japanese Exclusive Economic Zone (EEZ) around Minamitorishima Island. Three research cruises obtained fourteen sediment cores collected by piston coring. Based on the visual descriptions and geochemical analysis of the sediment cores, we confirm the presence of REY-rich mud containing more than 400 ppm total REY (∑REY) in the southern and northwestern areas of the Minamitorishima EEZ. The REY-rich mud layers are characterized by abundant grains of phillipsite, biogenic calcium phosphate, and manganese oxides, and are widely distributed in relatively shallow depths beneath the seafloor. In contrast, relatively thick, non-REY-rich mud lies near the seafloor in the northern areas of the EEZ. In the three cores from the southern part of the EEZ, we also confirm the presence of highly/extremely REY-rich mud layers. Further accumulation of geochemical data from the sediments will be required to constrain the extent of the highly/extremely REY-rich mud layers.</p>

Journal

  • GEOCHEMICAL JOURNAL

    GEOCHEMICAL JOURNAL 50 (6), 575-590, 2016-11-30

    GEOCHEMICAL SOCIETY OF JAPAN

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