中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
Provenance and climate changes inferred from magnetic properties of the sediments from the lower Yangtze River (China) during the last 130 years

文献类型:期刊论文

作者Zheng, Yan1,2; Yang, Shouye3; Deng, Chenglong4
刊名JOURNAL OF ASIAN EARTH SCIENCES
出版日期2019-05-15
卷号175页码:128-137
ISSN号1367-9120
关键词Provenance Climate change Yangtze River Flood/drought events
DOI10.1016/j.jseaes.2019.01.036
通讯作者Zheng, Yan(zhengyan@ivpp.ac.cn)
英文摘要It is essential to have a clear scientific view on paleoclimate change and its potential environmental and socioeconomic impacts for the prediction of future climate change. Fluvial sediment is one of the best archives for the investigations of high-resolution environmental variability and anthropogenic impacts on catchment over the last hundreds or even thousands years (Anthropocene). In this study, we examine magnetic properties of a 130-year fluvial sediment profile from an island in the main channel of the lower Yangtze mainstream, which aims to determine the connections between modern observational data and paleoclimate signals from sediments. Sediments from the upper Yangtze River is characterized by high concentration of magnetite, which is different from the middle reach. The difference of magnetic properties allows us to trace particles in the lower reach back to upstream of the Yangtze River. Climate change that reconstructed from physical properties of sediment (susceptibility and mean grain size) is comparable to those records in historical documents, which provides a possible way to obtain precise ages. The calibrated sedimentation rate reflects long-term variation of flood/drought events over the catchment, which is dominantly controlled by the climate circulation of Pacific. The enhanced human impacts since 1950s especially in the mid-lower reaches are observed. Therefore, riverine sediment not only contains paleoclimate information, but also reflects human activities.
WOS关键词HEAVY-METAL POLLUTION ; DIAGENETIC ALTERATION ; LOWER REACHES ; MAJOR RIVERS ; INNER SHELF ; CHANGJIANG ; EAST ; IMPACTS ; SOIL ; SEA
资助项目National Natural Science Foundation of China (NSFC)[41472146] ; National Natural Science Foundation of China (NSFC)[41730531] ; National Natural Science Foundation of China (NSFC)[41574061] ; National Natural Science Foundation of China (NSFC)[41104043] ; 973 project from Ministry of Science and Technology in China[2015CB953800]
WOS研究方向Geology
语种英语
出版者PERGAMON-ELSEVIER SCIENCE LTD
WOS记录号WOS:000464298500012
资助机构National Natural Science Foundation of China (NSFC) ; 973 project from Ministry of Science and Technology in China
源URL[http://119.78.100.205/handle/311034/9584]  
专题古脊椎动物与古人类研究所_图书馆1
通讯作者Zheng, Yan
作者单位1.Chinese Acad Sci, Inst Vertebrate Paleontol & Paleoanthropol, Key Lab Vertebrate Evolut & Human Origins, Beijing 100044, Peoples R China
2.CAS Ctr Excellence Life & Paleoenvironm, Beijing 100044, Peoples R China
3.Tongji Univ, State Key Lab Marine Geol, Shanghai 200092, Peoples R China
4.Chinese Acad Sci, Inst Geol & Geophys, State Key Lab Lithospher Evolut, Beijing 100029, Peoples R China
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Zheng, Yan,Yang, Shouye,Deng, Chenglong. Provenance and climate changes inferred from magnetic properties of the sediments from the lower Yangtze River (China) during the last 130 years[J]. JOURNAL OF ASIAN EARTH SCIENCES,2019,175:128-137.
APA Zheng, Yan,Yang, Shouye,&Deng, Chenglong.(2019).Provenance and climate changes inferred from magnetic properties of the sediments from the lower Yangtze River (China) during the last 130 years.JOURNAL OF ASIAN EARTH SCIENCES,175,128-137.
MLA Zheng, Yan,et al."Provenance and climate changes inferred from magnetic properties of the sediments from the lower Yangtze River (China) during the last 130 years".JOURNAL OF ASIAN EARTH SCIENCES 175(2019):128-137.

入库方式: OAI收割

来源:古脊椎动物与古人类研究所

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