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Monthly sea surface temperature records reconstructed by δ~(18)O of reef-building coral in the east of Hainan Island, South China Sea
引用本文:何学贤,刘敦一,彭子成,刘卫国.Monthly sea surface temperature records reconstructed by δ~(18)O of reef-building coral in the east of Hainan Island, South China Sea[J].中国科学B辑(英文版),2002,45(Z1).
作者姓名:何学贤  刘敦一  彭子成  刘卫国
作者单位:Institute of Geology Chinese Academy of Geological Sciences Beijing 100037 China,Institute of Geology Chinese Academy of Geological Sciences Beijing 100037 China,Department of Earth and Space Sciences. University of Science and Technology of China Hefei 230026 China,Key Laboratory of Loess and Quaternary Geology Chinese Academy of Sciences Xi'an 710054 China
摘    要:Stable oxygen isotopic compositions of a coral colony of Porites lutea obtained on acore allowed the reconstruction of a 56-a (1943-1998) proxy record of the sea surface tempera-tures. This coral δ~(18)O data are from the east of Hainan Island water (22°20'N, 110°39'E), SouthChina Sea. The relationship between δ~(18)O in the skeletal aragonite carbonate and the sea surfacetemperature (SST) is SST=-5.36 δ~(18)O_(PDB)-3.51 (r=0.73, n=470), dδ~(18)O/d(SST)=-0.187‰/℃; and the thermometer was set at monthly resolution. The 56-a (1943-1998) proxy record of thesea surface temperatures reflected the same change trend in the northern part of South China Seaas the air temperature change trend in China.


Monthly sea surface temperature records reconstructed by δ18O of reef-building coral in the east of Hainan Island,South China Sea
HE Xuexian,LIU Dunyi,PENG Zicheng LIU Weiguo.Monthly sea surface temperature records reconstructed by δ18O of reef-building coral in the east of Hainan Island,South China Sea[J].Science in China(Chemistry),2002,45(Z1).
Authors:HE Xuexian  LIU Dunyi  PENG Zicheng LIU Weiguo
Institution:1. Institute of Geology, Chinese Academy of Geological Sciences, Beijing 100037, China
2. Department of Earth and Space Sciences, University of Science and Technology of China, Hefei 230026, China
3. Key Laboratory of Loess and Quaternary Geology, Chinese Academy of Sciences, Xi'an 710054, China
Abstract:Stable oxygen isotopic compositions of a coral colony of Porites lutea obtained on a core allowed the reconstruction of a 56-a (1943-1998) proxy record of the sea surface temperatures. This coral δ18O data are from the east of Hainan Island water (22°20′N, 110°39′E), South China Sea. The relationship between δ18O in the skeletal aragonite carbonate and the sea surface temperature (SST) is SST = -5.36 δ18OPDB-3.51 (r = 0.73, n = 470), dδ18O/d(SST) = -0.187‰/ ℃; and the thermometer was set at monthly resolution. The 56-a (1943-1998) proxy record of the sea surface temperatures reflected the same change trend in the northern part of South China Sea as the air temperature change trend in China.
Keywords:reef-building coral  oxygen isotope  thermometer  mass spectrometry
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