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A reconstruction of late Pleistocene relative sea level in the south Bohai Sea, China, based on sediment grain-size analysis

文献类型：期刊论文

作者Yi, Liang1,2,3; Yu, Hongjun1; Ortiz, Joseph D.3; Xu, Xingyong1; Qiang, Xiaoke4; Huang, Haijun5; Shi, Xuefa1; Deng, Chenglong6
刊名SEDIMENTARY GEOLOGY
出版日期2012-12-15
卷号281页码:88-100
关键词Sea-level reconstruction Sediment grain size Mathematical partitioning Late Pleistocene Bohai Sea (China)
ISSN号0037-0738
DOI10.1016/j.sedgeo.2012.08.007
文献子类Article
英文摘要Future anthropogenic sea-level rise and its impact on coastal regions is an important issue facing human civilizations. Due to the short nature of the instrumental record of sea-level change, development of proxies for sea-level change prior to the advent of instrumental records is essential to reconstruct long-term background sea-level changes on local, regional and global scales. Here, we employ numerical methods to partition sediment grain size using a combined database of marine surface and core samples, and to quantitatively reconstruct sea-level variation since the late Pleistocene in the south Bohai Sea, China. Our sea-level reconstruction indicates that relative sea-level changes in the southern Bohai Sea track global sea-level variation for the duration of the record. The results also indicate substantial regression from 70 to 30 cal kyr BP, and potentially subarial exposure from 38 to 20 cal kyr BP. Our results document the feasibility of reconstructing relative sea-level change by numerical partitioning of sediment grain size data, demonstrating the potential for future applications. (C) 2012 Elsevier B.V. All rights reserved.
WOS关键词LAST GLACIAL CYCLE ; YELLOW-RIVER DELTA ; LU FAULT ZONE ; SALT-MARSH ; UNFLOCCULATED SEDIMENTS ; ROUND DISTRIBUTIONS ; POLYMODAL SEDIMENTS ; THERMAL HISTORY ; HUON PENINSULA ; CORAL TERRACES
WOS研究方向Geology
语种英语
WOS记录号WOS:000312754900007
出版者ELSEVIER SCIENCE BV
资助机构State Oceanic Research Project for Public Benefit of China(201105020) ; State Oceanic Research Project for Public Benefit of China(201105020) ; Chinese Offshore Investigation and Assessment(908-01-ZH2) ; Chinese Offshore Investigation and Assessment(908-01-ZH2) ; Open Research Fund of State Key Laboratory of Estuarine and Coastal Research(SKLEC201208) ; Open Research Fund of State Key Laboratory of Estuarine and Coastal Research(SKLEC201208) ; National Basic Research Program of China(2012CB821900) ; National Basic Research Program of China(2012CB821900) ; National Natural Science Foundation of China(40925012) ; National Natural Science Foundation of China(40925012) ; State Oceanic Research Project for Public Benefit of China(201105020) ; State Oceanic Research Project for Public Benefit of China(201105020) ; Chinese Offshore Investigation and Assessment(908-01-ZH2) ; Chinese Offshore Investigation and Assessment(908-01-ZH2) ; Open Research Fund of State Key Laboratory of Estuarine and Coastal Research(SKLEC201208) ; Open Research Fund of State Key Laboratory of Estuarine and Coastal Research(SKLEC201208) ; National Basic Research Program of China(2012CB821900) ; National Basic Research Program of China(2012CB821900) ; National Natural Science Foundation of China(40925012) ; National Natural Science Foundation of China(40925012) ; State Oceanic Research Project for Public Benefit of China(201105020) ; State Oceanic Research Project for Public Benefit of China(201105020) ; Chinese Offshore Investigation and Assessment(908-01-ZH2) ; Chinese Offshore Investigation and Assessment(908-01-ZH2) ; Open Research Fund of State Key Laboratory of Estuarine and Coastal Research(SKLEC201208) ; Open Research Fund of State Key Laboratory of Estuarine and Coastal Research(SKLEC201208) ; National Basic Research Program of China(2012CB821900) ; National Basic Research Program of China(2012CB821900) ; National Natural Science Foundation of China(40925012) ; National Natural Science Foundation of China(40925012) ; State Oceanic Research Project for Public Benefit of China(201105020) ; State Oceanic Research Project for Public Benefit of China(201105020) ; Chinese Offshore Investigation and Assessment(908-01-ZH2) ; Chinese Offshore Investigation and Assessment(908-01-ZH2) ; Open Research Fund of State Key Laboratory of Estuarine and Coastal Research(SKLEC201208) ; Open Research Fund of State Key Laboratory of Estuarine and Coastal Research(SKLEC201208) ; National Basic Research Program of China(2012CB821900) ; National Basic Research Program of China(2012CB821900) ; National Natural Science Foundation of China(40925012) ; National Natural Science Foundation of China(40925012)
源URL[http://ir.iggcas.ac.cn/handle/132A11/84348]  
专题中国科学院地质与地球物理研究所
通讯作者Yi, Liang
作者单位1.State Ocean Adm, Inst Oceanog 1, Key Lab Marine Sedimentol & Environm Geol, Qingdao 266061, Peoples R China
2.E China Normal Univ, State Key Lab Estuarine & Coastal Res, Shanghai 200062, Peoples R China
3.Kent State Univ, Dept Geol, Kent, OH 44242 USA
4.Chinese Acad Sci, State Key Lab Loess & Quaternary Geol, Inst Earth Environm, Xian 710075, Peoples R China
5.Chinese Acad Sci, Inst Oceanol, Key Lab Marine Geol & Environm, Qingdao 266071, Peoples R China
6.Chinese Acad Sci, Inst Geol & Geophys, State Key Lab Lithospher Evolut, Beijing 100029, Peoples R China
推荐引用方式
GB/T 7714		 Yi, Liang,Yu, Hongjun,Ortiz, Joseph D.,et al. A reconstruction of late Pleistocene relative sea level in the south Bohai Sea, China, based on sediment grain-size analysis[J]. SEDIMENTARY GEOLOGY,2012,281:88-100.
APA Yi, Liang.,Yu, Hongjun.,Ortiz, Joseph D..,Xu, Xingyong.,Qiang, Xiaoke.,...&Deng, Chenglong.(2012).A reconstruction of late Pleistocene relative sea level in the south Bohai Sea, China, based on sediment grain-size analysis.SEDIMENTARY GEOLOGY,281,88-100.
MLA Yi, Liang,et al."A reconstruction of late Pleistocene relative sea level in the south Bohai Sea, China, based on sediment grain-size analysis".SEDIMENTARY GEOLOGY 281(2012):88-100.

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来源：地质与地球物理研究所

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