Microatoll record for large century-scale sea-level fluctuations in the mid-Holocene

被引:52
作者
Yu, Ke-Fu [1 ,2 ]
Zhao, Jian-Xin [2 ]
Done, Terry [3 ]
Chen, Te-Gu [1 ]
机构
[1] Chinese Acad Sci, S China Sea Inst Oceanol, Guangzhou 510301, Guangdong, Peoples R China
[2] Univ Queensland, Ctr Microscopy & Microanal, Radiogenic Isotope Lab, Brisbane, Qld 4072, Australia
[3] Australian Inst Marine Sci, Townsville, Qld 4810, Australia
基金
澳大利亚研究理事会; 中国国家自然科学基金;
关键词
Microatoll; Sea level; Mid-Holocene; South China Sea; U-series; Coral reef; SOUTH CHINA SEA; CORAL MICROATOLLS; LEIZHOU PENINSULA; HOLOCENE; REEF; PACIFIC; INDICATORS; ISLANDS; QUEENSLAND; AUSTRALIA;
D O I
10.1016/j.yqres.2009.02.003
中图分类号
P9 [自然地理学];
学科分类号
0705 ; 070501 ;
摘要
Coral microatolls have been long used as precise indicators of past sea level. but their use for precise definition of detailed sea-level fluctuations is still rare. Here we report twelve high-precision thermal ionization mass spectrometric Th-230 ages for twelve rims of five mid-Holocene microatolls from all emerged reef terrace at Leizhou Peninsula, northern South China Sea. This is a tectonically stable area, enabling Lis to reconstruct both the timing and trajectory of local sea-level fluctuations accurately. The elevations of these microatoll rims and cores were accurately determined relative to the surface of modern livin., microatolls at the same site. The results indicate that the sea level during, the period of 7050-6600 yr bp (years before AD 1950) Was about 171 to 219 cm above the present, With at least four Cycles of fluctuations. Over this 450 yr interval, sea level fluctuated by 20-40 cm on century scales. Crown Copyright (c) 2009 Published by University of Washington. All rights reserved.
引用
收藏
页码:354 / 360
页数:7
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