Timing of the last-interglacial high sea level on the Seychelles Islands, Indian ocean

被引:50
作者
Israelson, C
Wohlfarth, B
机构
[1] Univ Copenhagen, Inst Geol, DK-1350 Copenhagen K, Denmark
[2] Univ Lund, Dept Quaternary Geol, S-22363 Lund, Sweden
关键词
last interglaciation; sea level; U-Th dating; corals; Seychelles; Indian Ocean;
D O I
10.1006/qres.1998.2030
中图分类号
P9 [自然地理学];
学科分类号
0705 ; 070501 ;
摘要
Corals from the Seychelles Islands, Indian Ocean, occur mainly as small coralline algae-vermetid remnants found in cavities adhering to the rock surface, and they rarely attain more than 2 m(2) in area. Samples of Goniastrea and Porites from elevations between 1.7 and 6 m above present mean sea level were dated by TIMS U-238-U-234-Th-230 techniques. The ages from well-preserved corals lie between 131,000 and 122,000 yr B.P., in agreement with most other observations of the last-interglacial sea level. Field evidence and dating from high marine limestones from two sections at La Digue Island indicate a period of coral buildup until 131,000 yr B.P., followed by a drop in sea level between 131,000 and 122,000 yr B.P. (C) 1999 University of Washington.
引用
收藏
页码:306 / 316
页数:11
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