Holocene relative sea-level change in Hiroshima Bay, Japan : a semi-quantitative reconstruction based on ostracodes
スポンサーリンク
概要
- 論文の詳細を見る
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 25m) between ca. 9000 cal yr BP and ca. 5800 cal yr BP, after which it gradually fell (about 5m) 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).
- 日本古生物学会の論文
- 2006-06-30
著者
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Seto Koji
Research Center For Coastal Lagoon Environments Shimane University
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Yasuhara Moriaki
Division Of Biology And Geosciences Graduate School Of Science Osaka City University:(present Addres
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Seto Koji
Shimane Univ. Matsue Jpn
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