多摩丘陵に分布する下部更新統上総層群における化石珪藻<i>Lancineis rectilatus</i>の産出層準とその地質学的・古生物学的意義

DOI
  • 納谷 友規
    産業技術総合研究所地質調査総合センター地質情報研究部門
  • 鈴木 毅彦
    東京都立大学都市環境学部地理環境学科

書誌事項

タイトル別名
  • Stratigraphic distribution of the fossil diatom <i>Lancineis rectilatus</i> in the Lower Pleistocene Kazusa Group in the Tama Hills, central Japan, and its geological and palaeontological significance

抄録

Lancineis rectilatus is a fossil diatom that appeared in the middle Early Pleistocene and disappeared in the early Middle Pleistocene in the shallow marine sediments of the central Kanto Plain, central Japan. In this study, diatom assemblages of the Oyamada to Iimuro Formations of the Lower Pleistocene Kazusa Group exposed along the Tama River and in Honmoku, Yokohama City, are investigated to clarify the stratigraphic relationship between the tephra beds and the occurrence of L. rectilatus in the Tama Hills. The Oyamada to Inagi Formation section is dominated by coastal shallow-marine diatoms. The Ozenji to Iimuro Formation of the Yokohama-Honmoku section is dominated by pelagic diatoms. L. rectilatus is identified from above the NK tephra layer of the Iimuro Formation. The NK tephra in the Tama Hills and the Kd12 Type tephra in the central Kanto Plain are possibly correlative.

収録刊行物

  • 化石

    化石 114 (0), 23-35, 2023-09-30

    日本古生物学会

詳細情報 詳細情報について

  • CRID
    1390016262469590144
  • DOI
    10.14825/kaseki.114.0_23
  • ISSN
    24242632
    00229202
  • 本文言語コード
    ja
  • データソース種別
    • JaLC
  • 抄録ライセンスフラグ
    使用不可

問題の指摘

ページトップへ