Thermal Ionization Mass Spectrometry (TIMS)-U-Series Ages of Corals from the South China Sea and Holocene High Sea Level  

作　　者：彭子成 何学贤 罗晓忠 贺剑峰 刘桂建 聂宝符 

机构地区：[1]Department of Earth and Space Sciences, University of Science and Technology of China [2]Department of Geological Sciences, Michigan University [3]South China Sea Institute of Oceanology, Chinese Academy of Sciences

出　　处：《Chinese Journal Of Geochemistry》2003年第2期133-139,共7页中国地球化学学报

基　　金：FinanciallysupportedjointlybyNKBRSFProjectFunds (G19990 43 40 0 1) ,theInnovation engineeringProjectFundsoftheChineseAcademyofSciences(KZCX2 SW 118) ,theNationalNaturalScienceFoundationofChina (GrantNo .40 1760 3 1)andChineseUniversityofScienceandTechno

摘　　要：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+{234}U(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.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+{234}U(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.

关 键 词：南海 珊瑚虫 全新世 热致电离质谱测定法 雷州半岛 海南岛 地质年代学 古气候 古环境 

分 类 号：P597[天文地球—地球化学]