中国地球化学学报(英文版)
中國地毬化學學報(英文版)
중국지구화학학보(영문판)
CHINESE JOURNAL OF GEOCHEMISTRY
2003年
2期
133-139
,共7页
彭子成%何学贤%罗晓忠%贺剑峰%刘桂建%聂宝符
彭子成%何學賢%囉曉忠%賀劍峰%劉桂建%聶寶符
팽자성%하학현%라효충%하검봉%류계건%섭보부
South China Sea coral%mass spectrometry U-series age%Holocene%high sea level
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 δ 234U (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.