| ITCZ and ENSO pacing on East Asian winter monsoon variation during the Holocene: Sedimentological evidence from the Okinawa Trough | |
| Zheng, Xufeng1,2; Li, Anchun1; Wan, Shiming1; Jiang, Fuqing1; Kao, Shuh Ji3; Johnson, Cody4; Li, AC (reprint author), Chinese Acad Sci, Inst Oceanol, Key Lab Marine Geol & Environm, Qingdao, Peoples R China. | |
| 2014-07-01 | |
| 发表期刊 | JOURNAL OF GEOPHYSICAL RESEARCH-OCEANS
 |
| 卷号 | 119期号:7页码:4410-4429 |
| 文章类型 | Article |
| 摘要 | Deep-sea fan sediments provide an excellent geological archive for paleoenvironment reconstruction. Grain size, clay mineral and elemental (Ti, Fe, Ca) compositions were measured for a core retrieved from a submarine fan in the Okinawa Trough. Varimax-rotated Principal Component Analysis (V-PCA) on time-evolution of grain size spectrum reveals that, since the Holocene, sediment was transported mainly by the benthic nepheloid layer (33%) and upper layers (33%) which is driven by the East Asian winter monsoon (EAWM). The intensification of the Kuroshio Current during the Holocene, masks the fluvial signal of the summer monsoon and obstructs clay minerals derived from the Yellow River, a major contributor prior to 12 ka BP. A new grain size index (GSI), which represents the EAWM well, exhibits a negative correlation with the delta O-18 record in Dongge Cave, China during the Holocene when sea level was relatively steady. This anti-correlation suggests the southward migration of the Intertropical Convergence Zone (ITCZ). The consistency among our records and rainfall records in Peru, Ti counts in the Cariaco Basin, monsoon records in Oman and the averaged summer insolation pattern at 30 degrees N further support the ITCZ's impact on monsoon systems globally. Cross-Correlation Analyses for GSI and log(Ti/Ca) against delta O-18 record in Dongge Cave reveal a decoupling between the East Asian winter and summer monsoon during 5500-2500 cal yr BP, with greater complexity in the last 2500 years. This can be attributed to exacerbated ENSO mode fluctuations and possibly anthropogenic interference superimposed on insolation and ITCZ forcing. |
| 学科领域 | Oceanography |
| DOI | 10.1002/2013JC009603 |
| 收录类别 | SCI |
| 语种 | 英语 |
| WOS记录号 | WOS:000340415500024 |
| 引用统计 | |
| 文献类型 | 期刊论文 |
| 条目标识符 | http://ir.qdio.ac.cn/handle/337002/23821 |
| 专题 | 海洋地质与环境重点实验室 |
| 通讯作者 | Li, AC (reprint author), Chinese Acad Sci, Inst Oceanol, Key Lab Marine Geol & Environm, Qingdao, Peoples R China. |
| 作者单位 | 1.Chinese Acad Sci, Inst Oceanol, Key Lab Marine Geol & Environm, Qingdao, Peoples R China 2.Chinese Acad Sci, South China Sea Inst Oceanol, Key Lab Marginal Sea Geol, Guangzhou, Guangdong, Peoples R China 3.Xiamen Univ, State Key Lab Marine Environm Sci, Xiamen, Peoples R China 4.Louisiana State Univ, Dept Civil & Environm Engn, Baton Rouge, LA 70803 USA |
| 第一作者单位 | 中国科学院海洋研究所 |
| 推荐引用方式 GB/T 7714 | Zheng, Xufeng,Li, Anchun,Wan, Shiming,et al. ITCZ and ENSO pacing on East Asian winter monsoon variation during the Holocene: Sedimentological evidence from the Okinawa Trough[J]. JOURNAL OF GEOPHYSICAL RESEARCH-OCEANS,2014,119(7):4410-4429. |
| APA | Zheng, Xufeng.,Li, Anchun.,Wan, Shiming.,Jiang, Fuqing.,Kao, Shuh Ji.,...&Li, AC .(2014).ITCZ and ENSO pacing on East Asian winter monsoon variation during the Holocene: Sedimentological evidence from the Okinawa Trough.JOURNAL OF GEOPHYSICAL RESEARCH-OCEANS,119(7),4410-4429. |
| MLA | Zheng, Xufeng,et al."ITCZ and ENSO pacing on East Asian winter monsoon variation during the Holocene: Sedimentological evidence from the Okinawa Trough".JOURNAL OF GEOPHYSICAL RESEARCH-OCEANS 119.7(2014):4410-4429. |
| 条目包含的文件 | ||||||
| 文件名称/大小 | 文献类型 | 版本类型 | 开放类型 | 使用许可 | ||
| ITCZ and ENSO pacing（1844KB） | 限制开放 | ODC PDDL | 浏览 | |||
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