Holocene relative sea-level change in Hiroshima Bay, Japan: a semi-quantitative reconstruction based on ostracodes

• YASUHARA Moriaki

  Division of Biology and Geosciences, Graduate School of Science, Osaka City University U.S. Geological Survey National Center, Reston

• SETO Koji

  Research Center for Coastal Lagoon Environments, Shimane University, Matsue

抄録

Holocene relative sea-level changes in Hiroshima Bay were reconstructed from fossil ostracodes from a core, using a semi-quantitative method. In Hiroshima Bay, relative sea level rose rapidly (about 25 m) between ca. 9000 cal yr BP and ca. 5800 cal yr BP, after which it gradually fell (about 5 m) to its present level. The peak in relative sea level occurred at ca. 5800 cal yr BP. The sea-level curve for Hiroshima Bay is similar to curves for tectonically stable areas of Japan (e.g., Osaka Bay).

収録刊行物

• Ｐａｌｅｏｎｔｏｌｏｇｉｃａｌ　Ｒｅｓｅａｒｃｈ

  Ｐａｌｅｏｎｔｏｌｏｇｉｃａｌ　Ｒｅｓｅａｒｃｈ 10 (2), 99-116, 2006

  日本古生物学会

キーワード

• Holocene
• Japan
• Ostracoda
• relative sea-level change
• semi-quantitative reconstruction
• Seto Inland Sea

詳細情報

• CRID: 1390001204087455360
• NII論文ID: 130004456670
• NII論文ID: 110004781722
• NII論文ID: 210000132248
• NII書誌ID: AA11137385
• DOI: 10.2517/prpsj.10.99
• ISSN: 18800068
• ISSN: 13428144
• NDL書誌ID: 8006492
• Web Site: https://ndlsearch.ndl.go.jp/books/R000000004-I8006492
• 本文言語コード: en
• データソース種別:
  • JaLC
  • NDL
  • Crossref
  • CiNii Articles
• 抄録ライセンスフラグ: 使用不可