Sea surface temperature variations recorded on coralline Sr/Ca ratios during Mid-Late Holocene in Leizhou Peninsula  

作　　者：WEIGangjian YUKefu ZHAOJianxin 

机构地区：[1]GuangzhouInstituteofGeochemistry,ChineseAcademyofSciences,Guangzhou510640,China [2]SouthChinaSeaInstituteofOceanology,ChineseAcademyofSciences,Guangzhou510301,China [3]GuangzhouInstituteofGeochemistry,ChineseAcademyofSciences,Guangzhou510640,China//AdvancedCentreforQueenslandUniversityIsotopeResearchExcellence(ACQUIRE),TheUniversityofQueensland,Q1d4072,Australia

出　　处：《Chinese Science Bulletin》2004年第17期1876-1881,共6页

摘　　要：High-resolution Sr/Ca ratios of two Porites cor- als from Leizhou Peninsula were measured using inductively coupled plasma atomic spectrometry (ICP-AES). TIMS U-Th dating reveals that the life-spans of the two corals are 489—500 AD and 539—530 BC, respectively. Monthly sea surface temperatures (SSTs) during these two periods can be reconstructed from their skeletal Sr/Ca ratios. The results reveal that SSTs during 539—530 BC were roughly the same as those during 1990—2000 AD in this area, indicating a relative warm climate period. However, the period of 489— 500 AD was significantly cooler, with annual mean SST, the 10-a average of minimum monthly winter SSTs and the 10-a average of maximum monthly summer SSTs being about 2, 2.9 and 1℃ lower than that in the 1990s, respectively. Such climate patterns agree well with the phenological results re- corded in the historic documents in other areas of China.High-resolution Sr/Ca ratios of two Porites cor- als from Leizhou Peninsula were measured using inductively coupled plasma atomic spectrometry (ICP-AES). TIMS U-Th dating reveals that the life-spans of the two corals are 489—500 AD and 539—530 BC, respectively. Monthly sea surface temperatures (SSTs) during these two periods can be reconstructed from their skeletal Sr/Ca ratios. The results reveal that SSTs during 539—530 BC were roughly the same as those during 1990—2000 AD in this area, indicating a relative warm climate period. However, the period of 489— 500 AD was significantly cooler, with annual mean SST, the 10-a average of minimum monthly winter SSTs and the 10-a average of maximum monthly summer SSTs being about 2, 2.9 and 1℃ lower than that in the 1990s, respectively. Such climate patterns agree well with the phenological results re- corded in the historic documents in other areas of China.

关 键 词：Sr/Ca比率 全新世 雷州半岛 滨珊瑚属 珊瑚虫 海面温度 

分 类 号：Q959.133[生物学—动物学]