Holocene sea-level change in the goto islands, japan

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概要

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• In order to examine the cause of underwater Jomon sites observed in the Goto Islands, sea-level change during the past 8,000 yr BP at Fukue Island has been evaluated based on diatom assemblage and pyrite-sulfer analyses for boring cores and ^＜14＞C dating for mollusks. The data indicate that the mean sea-level at about 5,000 yr BP was -1.9m and gradually rose to the present level. Thus the sea-level obtained in this study and underwater sites are indicative of crustal subsidence caused by sea-water loading by Holocene transgression.

• 東京都立大学の論文

著者

• Yokoyama Yusuke

  Research School Of Earth Sciences Australian National University

• Nagaoka Shinji

  Department Of Geography Faculty Of Education Nagasaki University

• Nakada Masao

  Department of Earth and Planetary Sciences, Faculty of Science, Kyushu University

• Maeda Yasuo

  Institute for Science of Mathematics,Education Development, Universty of the Philippines

• Nagaoka Shinji/yokoyama

  Department Of Geography Faculty Of Education Nagasaki University/research School Of Earth Sciences A

関連論文

• Holocene sea-level change in the goto islands, japan
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