Sediment provenance discrimination in northern Okinawa Trough during the last 24 ka and paleoenvironmental implication: rare earth elements evidence
文献类型：期刊论文
| 作者 | Xu Zhaokai1; Li Tiegang1 ; Chang Fengming1; Choi Jinyong2; Dhongil, Lim3; Xu Fangjian4
|
| 刊名 | JOURNAL OF RARE EARTHS
 |
| 出版日期 | 2012-11-01 |
| 卷号 | 30期号:11页码:1184-1190 |
| 关键词 | sediment provenance discriminant function rare earth elements Tsushima Warm Current northern Okinawa Trough |
| ISSN号 | 1002-0721 |
| 通讯作者 | Li, TG (reprint author), Chinese Acad Sci, Inst Oceanol, Key Lab Marine Geol & Environm, Qingdao 266071, Peoples R China. |
| 英文摘要 | Rare earth elements (REE) compositions and discriminant function were successfully used to examine high resolution sediment source changes in the northern Okinawa Trough over, the last 24.1 ka, especially for the influence from the Yellow River and the Tsushima Warm Current (TWC) that has not been well solved. Variations of these parameters were clearly divided into three distinct depositional units. During Interval 1 (24.1-16.0 ka BP), the paleo-Yellow River and the paleo-Yangtze River mouths were situated near the studied area and could have played major roles in the sedimentation therein. In Interval 2 (16.0-7.3 ka BP), these river mouths gradually retreated with global sea-level rise, leading to less fluvial inputs from them to the northern Okinawa Trough. Meanwhile, formation of the TWC could carry some sediment loads of Taiwan to the studied core, especially during its late phase (8.0-7.3 ka BP). Modern oceanographic conditions, with a predominance of the TWC, were finally established since the beginning of Interval 3, causing more terrigenous contribution from Taiwan to the studied area. Sub-sequently, modern depositional environments mainly influenced by the Yellow River, the Yangtze River, and the TWC were finally formed. |
| 学科主题 | Chemistry, Applied |
| 收录类别 | SCI |
| 原文出处 | 10.1016/S1002-0721(12)60202-6 |
| 语种 | 英语 |
| WOS记录号 | WOS:000312915800021 |
| 公开日期 | 2013-09-24 |
| 源URL | [http://ir.qdio.ac.cn/handle/337002/12515]  |
| 专题 | 海洋研究所_海洋地质与环境重点实验室 |
| 作者单位 | 1.Chinese Acad Sci, Inst Oceanol, Key Lab Marine Geol & Environm, Qingdao 266071, Peoples R China 2.Kunsan Natl Univ, Dept Oceanog, Kunsan 573701, South Korea 3.Korea Ocean Res & Dev Inst, S Sea Inst, Geoje 656830, South Korea 4.China Univ Petr, Sch Geosci, Qingdao 266555, Peoples R China |
| 推荐引用方式 GB/T 7714 | Xu Zhaokai,Li Tiegang,Chang Fengming,et al. Sediment provenance discrimination in northern Okinawa Trough during the last 24 ka and paleoenvironmental implication: rare earth elements evidence[J]. JOURNAL OF RARE EARTHS,2012,30(11):1184-1190. |
| APA | Xu Zhaokai,Li Tiegang,Chang Fengming,Choi Jinyong,Dhongil, Lim,&Xu Fangjian.(2012).Sediment provenance discrimination in northern Okinawa Trough during the last 24 ka and paleoenvironmental implication: rare earth elements evidence.JOURNAL OF RARE EARTHS,30(11),1184-1190. |
| MLA | Xu Zhaokai,et al."Sediment provenance discrimination in northern Okinawa Trough during the last 24 ka and paleoenvironmental implication: rare earth elements evidence".JOURNAL OF RARE EARTHS 30.11(2012):1184-1190. |
入库方式： OAI收割
来源：海洋研究所
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