Abstract
Coral samples collected from the waters off the Leizhou Peninsula, the Hainan Island and the Yongxing Island of the Xisha Islands were analyzed by thermal ionization mass spectrometry (TIMS) and multi-collector inductively coupled plasma mass spectrometry (MC-ICP-MS) for their U-Th systematics. Their uranium contents are mostly lower than 3μg/g, and the δ234U (T) values are within the range of 150 ±5. X-ray diffraction analysis showed that the corals are all composed of aragonite. This demonstrates that the corals determined have maintained a close system for 7000 years and their skeletons bear much information about the primitive tropical marine environment. The highly precise age sequence of the corals determined has revealed that there occurred three phases of high sea level in the South China Sea waters, which are dated at 6799-6307 a B. P., 4472-4285 a B. P. and 1279-1012 a B. P., respectively. The three phases lasted 492 a, 187 a and 267 a, respectively. These three phases of high sea level are corresponding to the warm environments that had appeared in China during the Megathermal Period and the Medieval Warm Period in the past ten thousand years.
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Financially supported jointly by NKBRSF Project Funds (G19990434001 ), the Innovation-engineering Project Funds of the Chinese Academy of Sciences (KZCX2-SW-118 ), the National Natural Science Foundation of China (Grant No. 40176031) and Chinese University of Science and Technology Resource and Environment Research Base Projects.
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Zicheng, P., Xuexian, H., Xiaozhong, L. et al. Thermal ionization mass spectrometry (TIMS)-U-Series ages of corals from the South China Sea and holocene high sea level. Chin. J. Geochem. 22, 133–139 (2003). https://doi.org/10.1007/BF02831522
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DOI: https://doi.org/10.1007/BF02831522