Sediment provenance and paleoenvironmental change in the middle Okinawa Trough during the last 18.5 ky: Clay mineral and geochemical evidence
文献类型：期刊论文
| 作者 | Xu, Zhaokai1,2; Li, Tiegang2,3 ; Clift, Peter D.4; Lim, Dhongil5; Nan, Qingyun1; Wan, Shiming1,2; Choi, Jinyong6; Cai, Mingjiang1,7; Chen, Hongjin1,7
|
| 刊名 | QUATERNARY INTERNATIONAL
 |
| 出版日期 | 2017-06-08 |
| 卷号 | 440页码:139-149 |
| 关键词 | Clay Minerals East Asian Monsoon Kuroshio Current Middle Okinawa Trough Sediment Provenance |
| DOI | 10.1016/j.quaint.2016.07.058 |
| 文献子类 | Article |
| 英文摘要 | We investigated grain size, clay mineralogy, elemental geochemistry, organic composition, and AMS C-14 dating ages in Core KX12-3 from the middle Okinawa Trough in order to better understand the sediment provenances and transport processes and also the forcing mechanisms behind their variations over the last 18.5 ky. The geochemical-mineralogical indices reveal three notable phases of change in the sediment provenance of the core, which are related to the development of the Kuroshio Current coupled with sea-level fluctuations, the position shift of the mouths of large rivers, the magnitude of tidal bottom stress, and the East Asian monsoon intensity. The sea-level lowstand deposits of Interval 1 (18.5-9.3 ka) formed from mixed sediments originating mostly from Chinese rivers (the paleo-Huanghe and the paleo-Changjiang) as well as from materials eroded from seafloor by the strong tidal stress. Thereafter during Interval 2 (9.3-8.7 ka), a significant sea-level rise, the moderate tidal bottom stress, and a gradual landward retreat of river mouths led to obviously decreased sediment supplies from both seafloor erosion and mainland China rivers (especially the paleo-Huanghe) into to the study area. After this transitional period, the dominant sediment provenance during the mid-to-late Holocene (Interval 3) changed to the Changjiang and seafloor erosion, resulting in lower detrital linear sedimentation rate and finer grain size. At the same time, some fine-grained materials from Taiwan may have been transported northward to the study area by the Kuroshio Current, as evidenced by higher values of chlorite/kaolinite ratio and chemical index of illite, and lower TOC/TN values. In addition, a prominent decline in chlorite/kaolinite values that occurred at 5.0-3.5 ka may have been linked to a suppression of the Kuroshio Current, probably related to the Pulleniatina minimum event and/or the late Holocene Neoglacial cold event commonly found in the northwestern Pacific. (C) 2016 Elsevier Ltd and INQUA. All rights reserved. |
| 语种 | 英语 |
| WOS记录号 | WOS:000404315300014 |
| 版本 | 出版稿 |
| 源URL | [http://ir.qdio.ac.cn/handle/337002/137135]  |
| 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.Qingdao Natl Lab Marine Sci & Technol, Lab Marine Geol, Qingdao 266061, Peoples R China 3.SOA, Inst Oceanog 1, Key Lab Marine Sedimentol & Environm Geol, Qingdao 266061, Peoples R China 4.Louisiana State Univ, Dept Geol & Geophys, Baton Rouge, LA 70803 USA 5.Korea Inst Ocean Sci & Technol, South Sea Res Inst, Geoje 656830, South Korea 6.Kunsan Natl Univ, Dept Oceanog, Kunsan 573701, South Korea 7.Univ Chinese Acad Sci, Beijing 100049, Peoples R China |
| 推荐引用方式 GB/T 7714 | Xu, Zhaokai,Li, Tiegang,Clift, Peter D.,et al. Sediment provenance and paleoenvironmental change in the middle Okinawa Trough during the last 18.5 ky: Clay mineral and geochemical evidence[J]. QUATERNARY INTERNATIONAL,2017,440:139-149. |
| APA | Xu, Zhaokai.,Li, Tiegang.,Clift, Peter D..,Lim, Dhongil.,Nan, Qingyun.,...&Chen, Hongjin.(2017).Sediment provenance and paleoenvironmental change in the middle Okinawa Trough during the last 18.5 ky: Clay mineral and geochemical evidence.QUATERNARY INTERNATIONAL,440,139-149. |
| MLA | Xu, Zhaokai,et al."Sediment provenance and paleoenvironmental change in the middle Okinawa Trough during the last 18.5 ky: Clay mineral and geochemical evidence".QUATERNARY INTERNATIONAL 440(2017):139-149. |
入库方式： OAI收割
来源：海洋研究所
浏览0
下载0
收藏0
其他版本
除非特别说明，本系统中所有内容都受版权保护，并保留所有权利。