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

doi:10.1016/j.sedgeo.2012.08.007

IEECAS OpenIR > 黄土与第四纪地质国家重点实验室（2010~）

	A reconstruction of late Pleistocene relative sea level in the south Bohai Sea, China, based on sediment grain-size analysis
	Yi,L(Yi,Liang)[1,2,3]; Yu,HJ(Yu,Hongjun)[1]; Ortiz,JD(Ortiz,Joseph D.)[3]; Xu,XY(Xu,Xingyong)[1]; Qiang,XK(Qiang,Xiaoke)[4]; Huang,HJ(Huang,Haijun)[5]; Shi,XF(Shi,Xuefa)[1]; Deng,CL(Deng,Chenglong)[6]
	2012-12-15
发表期刊	Sedimentary Geology
卷号	281 页码:88-100
文章类型	期刊论文
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.
关键词	Sea-level Reconstruction Sediment Grain Size Mathematical Partitioning Late Pleistocene Bohai Sea (China)
DOI	10.1016/j.sedgeo.2012.08.007
收录类别	SCI ; EI
语种	英语
引用统计	被引频次：49[WOS] [WOS记录] [WOS相关记录]
文献类型	期刊论文
条目标识符	http://ir.ieecas.cn/handle/361006/10206
专题	黄土与第四纪地质国家重点实验室（2010~）
通讯作者	Yi,L(Yi,Liang)[1,2,3]
作者单位	1.Key Laboratory of Marine Sedimentology and Environmental Geology, First Institute of Oceanography, State Oceanic Administration, Qingdao 266061, China; 2.State Key Laboratory of Estuarine and Coastal Research, East China Normal University, Shanghai 200062, China; 3.Department of Geology, Kent State University, Kent, OH 44242, USA; 4.State Key Laboratory of Loess and Quaternary Geology, Institute of Earth Environment, Chinese Academy of Sciences, Xi'an 710075, China; 5.Key Laboratory of Marine Geology and Environment, Institute of Oceanology, Chinese Academy of Sciences, Qingdao 266071, China; 6.State Key Laboratory of Lithospheric Evolution, Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing 100029, China
推荐引用方式 GB/T 7714	Yi,L,Yu,HJ,Ortiz,JD,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,L.,Yu,HJ.,Ortiz,JD.,Xu,XY.,Qiang,XK.,...&Deng,CL.(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,L,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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