中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
Paleomagnetic and astronomical dating of sediment core BH08 from the Bohai Sea, China: Implications for glacial-interglacial sedimentation

文献类型:期刊论文

作者Yao, Zhengquan1; Shi, Xuefa1; Liu, Qingsong2; Liu, Yanguang1; Cruz Larrasoana, Juan3,4; Liu, Jianxing1,2,5; Ge, Shulan1; Wang, Kunshan1; Qiao, Shuqing1; Li, Xiaoyan1
刊名PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY
出版日期2014
卷号393页码:90-101
ISSN号0031-0182
关键词Bohai Sea Magnetostratigraphy Astronomical tuning Sea level Glacial interglacial
DOI10.1016/j.palaeo.2013.11.012
文献子类Article
英文摘要Sediments from the continental shelf/coastal region bear significant signals of sea-level, climate change as well as local tectonic information. This study presents a high-resolution magnetostratigraphic and rock magnetic study of a 212.4 m core (BH08, with a basal age of 1.06 Ma) recovered from the shallow (<30 m below sea level) Bohai Sea, China. Astronomical tuning based on the sediment redness (a*) of core BH08 allows the construction of a high-resolution chronology that is assisted by magnetostratigraphic data. Sedimentology and associated proxies (grain size and redness) indicate that the cyclic alternation of neritic/littoral sandy deposits and terrestrial silts/ clayey silts was mainly controlled by changes in sea-level and associated base-level at glacial-interglacial timescales. The a* record of the core can be correlated with marine 6180 records at 40- and 100-kyr cycles, indicating that the sediments in the study area are continuous at least at orbital timescales regardless of significant baselevel variations. This is likely due to continued subsidence in the basin and creation of accommodation space. The significant lower sedimentary accumulation rates since 750 ka might be due to the deviation of the depositional locus from core site because of extreme low sea-level stands during the glacials since the Mid-Pleistocene transition (MPT). Especially the glacial sea-level lowstands might have resulted in bypassing or erosion of sediments on the BH08 core site during peak glacials (MIS 6, MIS 10 and MIS 16), limiting the sediment preservation potential. This study documents the longest Quaternary sedimentary succession in the Bohai Sea and provides, for the first time, a clear link between sedimentation in the area and glacial-interglacial climate-driven sea-level changes. This study also highlights the feasibility of astronomical tuning to obtain high-resolution chronology for shallow shelf deposits, which is otherwise very difficult to be achieved on the basis of magnetostratigraphic data alone. Crown Copyright (C) 2013 Published by Elsevier B.V. All rights reserved.
WOS关键词VISCOUS MAGNETIZATION ; ICE-SHEET ; MULTIDOMAIN MAGNETITE ; FLUVIAL ARCHITECTURE ; NORTHERN CHINA ; LEVEL CHANGE ; GRAIN-SIZE ; QUATERNARY ; CLIMATE ; LOESS
WOS研究方向Physical Geography ; Geology ; Paleontology
语种英语
出版者ELSEVIER SCIENCE BV
WOS记录号WOS:000331024900007
资助机构National Natural Science Foundation of China(41006039 ; National Natural Science Foundation of China(41006039 ; Basic Scientific Fund for National Public Research Institutes of China(2011G21) ; Basic Scientific Fund for National Public Research Institutes of China(2011G21) ; State Oceanic Administration of China(908-01-BC15 ; State Oceanic Administration of China(908-01-BC15 ; 41025013) ; 41025013) ; 2012317 ; 2012317 ; 2012325 ; 2012325 ; 2012G35) ; 2012G35) ; National Natural Science Foundation of China(41006039 ; National Natural Science Foundation of China(41006039 ; Basic Scientific Fund for National Public Research Institutes of China(2011G21) ; Basic Scientific Fund for National Public Research Institutes of China(2011G21) ; State Oceanic Administration of China(908-01-BC15 ; State Oceanic Administration of China(908-01-BC15 ; 41025013) ; 41025013) ; 2012317 ; 2012317 ; 2012325 ; 2012325 ; 2012G35) ; 2012G35) ; National Natural Science Foundation of China(41006039 ; National Natural Science Foundation of China(41006039 ; Basic Scientific Fund for National Public Research Institutes of China(2011G21) ; Basic Scientific Fund for National Public Research Institutes of China(2011G21) ; State Oceanic Administration of China(908-01-BC15 ; State Oceanic Administration of China(908-01-BC15 ; 41025013) ; 41025013) ; 2012317 ; 2012317 ; 2012325 ; 2012325 ; 2012G35) ; 2012G35) ; National Natural Science Foundation of China(41006039 ; National Natural Science Foundation of China(41006039 ; Basic Scientific Fund for National Public Research Institutes of China(2011G21) ; Basic Scientific Fund for National Public Research Institutes of China(2011G21) ; State Oceanic Administration of China(908-01-BC15 ; State Oceanic Administration of China(908-01-BC15 ; 41025013) ; 41025013) ; 2012317 ; 2012317 ; 2012325 ; 2012325 ; 2012G35) ; 2012G35)
源URL[http://ir.iggcas.ac.cn/handle/132A11/84836]  
专题中国科学院地质与地球物理研究所
通讯作者Shi, Xuefa
作者单位1.State Ocean Adm, Inst Oceanog 1, Key Lab Marine Sedimentol & Environm Geol, Qingdao 266061, Peoples R China
2.Chinese Acad Sci, Inst Geol & Geophys, Paleomagnetism & Geochronol Lab SKL LE, Beijing 100029, Peoples R China
3.Inst Geol & Minero Espana, Unidad Zaragoza, Zaragoza 50006, Spain
4.ICTJA CSIC, Inst Earth Sci Jaume Almera, Barcelona 08028, Spain
5.Univ Chinese Acad Sci, Beijing 100049, Peoples R China
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Yao, Zhengquan,Shi, Xuefa,Liu, Qingsong,et al. Paleomagnetic and astronomical dating of sediment core BH08 from the Bohai Sea, China: Implications for glacial-interglacial sedimentation[J]. PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY,2014,393:90-101.
APA Yao, Zhengquan.,Shi, Xuefa.,Liu, Qingsong.,Liu, Yanguang.,Cruz Larrasoana, Juan.,...&Duan, Zongqi.(2014).Paleomagnetic and astronomical dating of sediment core BH08 from the Bohai Sea, China: Implications for glacial-interglacial sedimentation.PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY,393,90-101.
MLA Yao, Zhengquan,et al."Paleomagnetic and astronomical dating of sediment core BH08 from the Bohai Sea, China: Implications for glacial-interglacial sedimentation".PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY 393(2014):90-101.

入库方式: OAI收割

来源:地质与地球物理研究所

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