Provenance and climate change inferred from Sr-Nd-Pb isotopes of late Quaternary sediments in the Huanghe (Yellow River) Delta, China | |
Hu, Bangqi1,2; Li, Guogang3,4; Li, Jun1; Bi, Jianqiang3,4; Zhao, Jingtao1; Bu, Ruyuan3,4 | |
刊名 | QUATERNARY RESEARCH |
2012-11 | |
卷号 | 78期号:3页码:561-571 |
关键词 | Sr Nd and Pb isotopes Late Quaternary Huanghe Provenance Climate changes |
ISSN号 | 0033-5894 |
DOI | 10.1016/j.yqres.2012.07.005 |
英文摘要 | We present a provenance study of core ZK2 from the Huanghe (Yellow River) Delta in order to assess the impacts of climate change on the sediment supplies during the last glacial-interglacial cycle. Facies analysis and sequence stratigraphy methods are used to construct the age model. Sr isotopic compositions of ZK2 range from 0.716389 to 0.723884, with Sr-87/Sr-86 increased with decreasing grain size. Nd and Pb isotopic compositions display two large major excursions during Marine Oxygen Isotope stages (MIS) 2 and 4, with less radiogenic epsilon Nd and lower Pb-208/Pb-204, Pb-207/Pb-204, and Pb-206/Pb-204 values during these periods. These excursions have been explained in terms of changes in the mixing proportion of sediments from the Loess Plateau and Ordos Plateau, resulting from East Asian monsoon intensity variations. The weak summer monsoon precipitation resulted in decreased erosion of Loess Plateau during MIS 2, 4 and the middle of MIS 3. Meanwhile, both the intensified East Asian winter monsoon and the southward expansions of Mu Us desert significantly enhanced the eolian sand entering the Huanghe. Therefore, our results highlight the impact of monsoon variability on erosion patterns in the Huanghe basin. (c) 2012 University of Washington. Published by Elsevier Inc. All rights reserved. |
资助项目 | Open Foundation of the State Key Laboratory of Loess and Quaternary Geology[SKLLQG1107] |
WOS研究方向 | Physical Geography ; Geology |
语种 | 英语 |
出版者 | ACADEMIC PRESS INC ELSEVIER SCIENCE |
WOS记录号 | WOS:000310822100015 |
内容类型 | 期刊论文 |
源URL | [http://ir.fio.com.cn/handle/2SI8HI0U/4057] |
专题 | 自然资源部第一海洋研究所 |
作者单位 | 1.Minist Land & Resources, Qingdao Inst Marine Geol, Key Lab Marine Hydrocarbon Resources & Environm G, Qingdao 266071, Peoples R China; 2.Chinese Acad Sci, State Key Lab Loess & Quaternary Geol, Inst Earth Environm, Xian 710075, Peoples R China; 3.Shandong Prov Key Lab Marine Ecol & Environm & Di, Qingdao 266033, Peoples R China; 4.State Ocean Adm, N China Sea Branch, Marine Engn & Prospecting Inst N China Sea, Qingdao 266033, Peoples R China |
推荐引用方式 GB/T 7714 | Hu, Bangqi,Li, Guogang,Li, Jun,et al. Provenance and climate change inferred from Sr-Nd-Pb isotopes of late Quaternary sediments in the Huanghe (Yellow River) Delta, China[J]. QUATERNARY RESEARCH,2012,78(3):561-571. |
APA | Hu, Bangqi,Li, Guogang,Li, Jun,Bi, Jianqiang,Zhao, Jingtao,&Bu, Ruyuan.(2012).Provenance and climate change inferred from Sr-Nd-Pb isotopes of late Quaternary sediments in the Huanghe (Yellow River) Delta, China.QUATERNARY RESEARCH,78(3),561-571. |
MLA | Hu, Bangqi,et al."Provenance and climate change inferred from Sr-Nd-Pb isotopes of late Quaternary sediments in the Huanghe (Yellow River) Delta, China".QUATERNARY RESEARCH 78.3(2012):561-571. |
个性服务 |
查看访问统计 |
相关权益政策 |
暂无数据 |
收藏/分享 |
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。
修改评论