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《Geochimica》 2006-05
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Geochemistry of REE in a Porites coral from Sai Kung,Hong Kong and its relationship with sea level rise

LIU Yi1,PENG Zi-cheng1 ,WEI Gang-jian2,CHEN Te-gu3,P.O.Ang4,HE Jian-feng1 and LIU Gui-jian11.School of Earth and Space Sciences,University of Science and Technology of China,Hefei 230026,China;2.Guangzhou Institute of Geochemistry,Chinese Academy of Sciences,Guangzhou 510640,China;3.South China Sea Institute of Oceanology,Chinese Academy of Sciences,Guangzhou 510301,China;4.Department of Biology,the Chinese University of Hong Kong,Hong Kong,China  
Inductively coupled plasma mass spectrometry has been used to produce a high resolution Porites coral record of rare earth elements(REE),from Sai Kung,Hong Kong,the west coast of Pearl River Estuary,which spans from 1991 to 2002.The distribution pattern of REE in the coral is similar to seawater,whose characteristics are Ce negative anomaly and heavy REE enrichment on the basis of standard of shale in Post-Archaean average Australian sedimentary rock(PAAS).The REE contents in Hong Kong coral are much higher than reported results from other areas,except corals from Misima Island,Papua New Guinea,which are affected by an open-cut gold mining.The high REE contents in Hong Kong coral are a direct response to high REE contents in the Pearl River and nearby surface sedimentary deposit,indicating a severe terrestrial influence and a closed marginal sea effect.Moreover,the decreasing trend of annual REE contents in the coral from Sai Kung,Hong Kong is very apparent,with severer Ce negative anomaly and heavy REE enrichment,from 1991 to 2002.REE composition in the coral is significantly negatively correlated with sea level,and heavy REE linear correlation coefficients are better than light REE.These results are associated with sea level rising caused by globe warming and polar ice melting.
【Fund】: 国家自然科学基金(40176031);; 中国科学院知识创新工程重要方向项目(KZCX2-SW-118 KZCX3-SW-120);; 中国科学院同位素年代学和地球化学重点实验室项目(GIGIso-05-07)
【CateGory Index】: P595
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