Planktonic foraminifera and sea surface temperature (SST) of the Xisha Trough, South China Sea since Last Glaciation
文献类型：期刊论文
| 作者 | Jiang, MS; Li, XJ |
| 刊名 | SCIENCE IN CHINA SERIES D-EARTH SCIENCES
 |
| 出版日期 | 2003 |
| 卷号 | 46期号:1页码:1-9 |
| 关键词 | South China Sea Oxygen Isotope Planktonic Foraminifera Sea Surface Temperature "younger Dryas Event" |
| ISSN号 | 1006-9313 |
| 文献子类 | Article |
| 英文摘要 | The high-resolution analysis on the carbon and oxygen isotopes and planktonic foraminifera of core SA12-19 dated with C-14 approach in the Xisha Trough of South China Sea indicates that sediments are attributed to oxygen isotope stages 1-3 (stage 3 is not included completely), during the late-glacial to post-glacial periods. The sea surface temperature (SST) of each sample is calculated based on palaeoecological transfer functions (FP-12E). The results reveal a gradual thermocline increase in this area during oxygen isotope stages 1-3 e.g. a temporal thermocline deepening in the middle Holocene. During the Holocene, the SST was 23.3-27.2degreesC in winter, 28.8-29.8degreesC in summer. During oxygen isotope stage 2, the SST was 21.4-24.4degreesC in winter, 28.1-29.0degreesC in summer; and 21.9-25.2degreesC in winter, 28.5-29.3degreesC in summer during oxygen isotope stage 3. The SST in winter during oxygen isotope stage 2 was 2-6degreesC lower than that of stage 3. During the transitional period, a "Younger Dryas Event", standing for a rapid climate return, occurred obviously. |
| WOS关键词 | OXYGEN-ISOTOPE ; RECORDS ; CORE |
| WOS研究方向 | Geology |
| 语种 | 英语 |
| WOS记录号 | WOS:000181415400001 |
| 出版者 | SCIENCE CHINA PRESS |
| 源URL | [http://ir.iggcas.ac.cn/handle/132A11/78567]  |
| 专题 | 中国科学院地质与地球物理研究所 |
| 通讯作者 | Jiang, MS |
| 作者单位 | 1.Chinese Acad Sci, Inst Geol & Geophys, Beijing 100029, Peoples R China 2.Tongji Univ, Lab Marine Geol, Shanghai 200092, Peoples R China 3.Guangzhou Marine Geol Survey, Inst Marine Environm & Engn Geol, Guangzhou 510760, Peoples R China |
| 推荐引用方式 GB/T 7714 | Jiang, MS,Li, XJ. Planktonic foraminifera and sea surface temperature (SST) of the Xisha Trough, South China Sea since Last Glaciation[J]. SCIENCE IN CHINA SERIES D-EARTH SCIENCES,2003,46(1):1-9. |
| APA | Jiang, MS,&Li, XJ.(2003).Planktonic foraminifera and sea surface temperature (SST) of the Xisha Trough, South China Sea since Last Glaciation.SCIENCE IN CHINA SERIES D-EARTH SCIENCES,46(1),1-9. |
| MLA | Jiang, MS,et al."Planktonic foraminifera and sea surface temperature (SST) of the Xisha Trough, South China Sea since Last Glaciation".SCIENCE IN CHINA SERIES D-EARTH SCIENCES 46.1(2003):1-9. |
入库方式： OAI收割
来源：地质与地球物理研究所
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