Sea surface temperature evolution in the western South China Sea since MIS 12 as evidenced by planktonic foraminiferal assemblages and Globigerinoides ruber Mg/Ca ratio
文献类型:期刊论文
作者 | Li BaoHua (李保华)![]() ![]() |
刊名 | SCIENCE CHINA-EARTH SCIENCES
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出版日期 | 2012 |
卷号 | 55期号:11页码:1827-1836 |
ISSN号 | 1674-7313 |
公开日期 | 2013-03-26 |
源URL | [http://ir.nigpas.ac.cn/handle/332004/4528] ![]() |
专题 | 中国科学院南京地质古生物研究所 南京地质古生物研究所_其他 |
推荐引用方式 GB/T 7714 | Li BaoHua ,Wang XiaoYan . Sea surface temperature evolution in the western South China Sea since MIS 12 as evidenced by planktonic foraminiferal assemblages and Globigerinoides ruber Mg/Ca ratio[J]. SCIENCE CHINA-EARTH SCIENCES,2012,55(11):1827-1836. |
APA | Li BaoHua ,&Wang XiaoYan .(2012).Sea surface temperature evolution in the western South China Sea since MIS 12 as evidenced by planktonic foraminiferal assemblages and Globigerinoides ruber Mg/Ca ratio.SCIENCE CHINA-EARTH SCIENCES,55(11),1827-1836. |
MLA | Li BaoHua ,et al."Sea surface temperature evolution in the western South China Sea since MIS 12 as evidenced by planktonic foraminiferal assemblages and Globigerinoides ruber Mg/Ca ratio".SCIENCE CHINA-EARTH SCIENCES 55.11(2012):1827-1836. |
入库方式: OAI收割
来源:南京地质古生物研究所
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