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Correlation between δ^(18)O, Sr/Ca and Mg/Ca of coral Acropora and seawater temperature from coral culture experiments

Correlation between δ^(18)O, Sr/Ca and Mg/Ca of coral Acropora and seawater temperature from coral culture experiments

作     者:XIAO YingKai LIU WeiGuo MA YunQi ZHANG YanLing HE MaoYong LUO ChongGuang LIAO QingQiang 

作者机构:Qinghai Institute of Salt LakesChinese Academy of Sciences State Key Laboratory of Loess and Quaternary GeologyInstitute of Earth Environment Chinese Academy of Sciences Beihai Aquarium 

出 版 物:《Science China Earth Sciences》 (中国科学(地球科学英文版))

年 卷 期:2014年第57卷第5期

页      面:1048-1060页

核心收录:

学科分类:07[理学] 0708[理学-地球物理学] 0704[理学-天文学] 0713[理学-生态学] 

基  金:supported by National Natural Science Foundation of China (Grant Nos. 40976074 and 41173019) State Key Laboratory of Loess and Quaternary Geology, Institute of Earth Environment, CAS (Grant. No SKLLQG1126) 

主  题:coral culture seawater temperature oxygen isotope microelement ratio 

摘      要:To be used as proxies of seawater surface temperature (SST), the 61Soc values and Sr/Ca and Mg/Ca ratios of scleractinian coral skeletons must be verified by coral culture experiments in the laboratory. This paper describes a coral culture experiment that was conducted at several seawater temperatures T (21-28℃) using a tandem aquarium system and the new method for depositing coral skeletons grown under controlled conditions. The δ180c values and the St/Ca and Mg/Ca ratios of the cultured coral were measured. We concluded that the δ18Oc values and Sr/Ca and Mg/Ca ratios of the cultured coral are clearly corre- lated with T. The linear regression curve is δ18Oc(‰)=-0.1427×T(℃)-0.1495 (n=18, r=0.955, p〈0.0001), and the slope of -0.1427‰/°d℃ is at the low end of the range of published values (-0.13-0.29‰/°d℃). The Sr/Ca ratio decreases with increas- ing T, whereas the Mg/Ca ratio increases with increasing T, indicating a negative correlation between Sr/Ca and Mg/Ca. Their linear regression curves are Sr/Ca(mmol/mol)=-O.O4156×T+lO.59 (n=15, r=-0.789, p〈0.005) and Mg/Ca (mmol/mol)= 0.04974×T+2.339 (n=17, r=-0.457, p〈0.05), respectively, which demonstrate that when Mg/Ca and Sr/Ca are increased by one unit, T increases by 5.19℃and decreases by 15.62℃, respectively. These variations are significantly lower than published values.

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