Late Quaternary linkage of sedimentary records to three astronomical rhythms and the Asian monsoon, inferred from a coastal borehole in the south Bohai Sea, China
文献类型:期刊论文
作者 | Yi, Liang1,2,3; Yu, Hong-Jun1; Ortiz, Joseph D.3; Xu, Xing-Yong1; Chen, Shen-Liang4; Ge, Jun-Yi5; Hao, Qing-Zhen5; Yao, Jing1; Shi, Xue-Fa1; Peng, Shu-Zhen6 |
刊名 | PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY
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出版日期 | 2012-04-15 |
卷号 | 329页码:101-117 |
关键词 | Late Quaternary Marine records Orbital forcing Asian monsoon Bohai Sea Nonlinear climatic response |
ISSN号 | 0031-0182 |
DOI | 10.1016/j.palaeo.2012.02.020 |
文献子类 | Article |
英文摘要 | The Bohai Sea was formed by subsidence during the Cenozoic. Some 2000-3000 m of fluvial, lacustrine and marine sediments has been deposited in this basin. Previous studies focused mainly on the transgression history, with little examination of orbital variation in relation to other areas within the Asian monsoon domain. Here, we present the late Quaternary results of a new borehole in the south Bohai Sea. Optically stimulated luminescence and radiocarbon dating, which provide concordant age estimates, were employed to generate an initial chronology for the borehole. After refining the chronology through astronomical tuning, the results showed that: (1) the grain size variation represents Asian monsoon intensity which was dominated by both solar insolation (major) and global ice volume (minor) forcing; (2) the magnetic susceptibility indicates river incision processes which were sensitive to orbital tilt with influence from solar insolation; (3) the vegetation coverage responded to global ice volume coupled obliquity changes; and that (4) neither external nor internal factors could dominate the paleoenvironmental evolution on orbital timescales in an independent way, and they are both integrated in a complex pattern. We conclude that three different astronomical rhythms have affected coastal evolution, and that the sedimentary records in the south Bohai Sea, China, result from the nonlinear interaction and the complex response to driving processes. (C) 2012 Elsevier B.V. All rights reserved. |
WOS关键词 | HOLOCENE LAKE SEDIMENTOLOGY ; LU FAULT ZONE ; LATE PLEISTOCENE ; LOESS PLATEAU ; NORTH-ATLANTIC ; TIBETAN PLATEAU ; CLIMATE-CHANGE ; EASTERN CHINA ; TREE-RING ; FORCING MECHANISMS |
WOS研究方向 | Physical Geography ; Geology ; Paleontology |
语种 | 英语 |
WOS记录号 | WOS:000303221500008 |
出版者 | ELSEVIER SCIENCE BV |
资助机构 | National Basic Research Project of China(2010CB951200) ; National Basic Research Project of China(2010CB951200) ; State Oceanic Research Project for Public Benefit(201105020 ; State Oceanic Research Project for Public Benefit(201105020 ; Chinese Offshore Investigation and Assessment(908-01-ZH2) ; Chinese Offshore Investigation and Assessment(908-01-ZH2) ; State Key Laboratory of Loess and Quaternary Geology of China(SKLLQG1018) ; State Key Laboratory of Loess and Quaternary Geology of China(SKLLQG1018) ; 200805063) ; 200805063) ; National Basic Research Project of China(2010CB951200) ; National Basic Research Project of China(2010CB951200) ; State Oceanic Research Project for Public Benefit(201105020 ; State Oceanic Research Project for Public Benefit(201105020 ; Chinese Offshore Investigation and Assessment(908-01-ZH2) ; Chinese Offshore Investigation and Assessment(908-01-ZH2) ; State Key Laboratory of Loess and Quaternary Geology of China(SKLLQG1018) ; State Key Laboratory of Loess and Quaternary Geology of China(SKLLQG1018) ; 200805063) ; 200805063) ; National Basic Research Project of China(2010CB951200) ; National Basic Research Project of China(2010CB951200) ; State Oceanic Research Project for Public Benefit(201105020 ; State Oceanic Research Project for Public Benefit(201105020 ; Chinese Offshore Investigation and Assessment(908-01-ZH2) ; Chinese Offshore Investigation and Assessment(908-01-ZH2) ; State Key Laboratory of Loess and Quaternary Geology of China(SKLLQG1018) ; State Key Laboratory of Loess and Quaternary Geology of China(SKLLQG1018) ; 200805063) ; 200805063) ; National Basic Research Project of China(2010CB951200) ; National Basic Research Project of China(2010CB951200) ; State Oceanic Research Project for Public Benefit(201105020 ; State Oceanic Research Project for Public Benefit(201105020 ; Chinese Offshore Investigation and Assessment(908-01-ZH2) ; Chinese Offshore Investigation and Assessment(908-01-ZH2) ; State Key Laboratory of Loess and Quaternary Geology of China(SKLLQG1018) ; State Key Laboratory of Loess and Quaternary Geology of China(SKLLQG1018) ; 200805063) ; 200805063) |
源URL | [http://ir.iggcas.ac.cn/handle/132A11/84496] ![]() |
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.Chinese Acad Sci, Inst Earth Environm, State Key Lab Loess & Quaternary Geol, Xian 710075, Peoples R China 3.Kent State Univ, Dept Geol, Kent, OH 44242 USA 4.E China Normal Univ, State Key Lab Estuarine & Coastal Res, Shanghai 200062, Peoples R China 5.Chinese Acad Sci, Inst Geol & Geophys, Key Lab Cenozo Geol & Environm, Beijing 100029, Peoples R China 6.Taishan Univ, Key Lab Tourism & Resources Environm Univ Shandon, Tai An 271021, Shandong, Peoples R China |
推荐引用方式 GB/T 7714 | Yi, Liang,Yu, Hong-Jun,Ortiz, Joseph D.,et al. Late Quaternary linkage of sedimentary records to three astronomical rhythms and the Asian monsoon, inferred from a coastal borehole in the south Bohai Sea, China[J]. PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY,2012,329:101-117. |
APA | Yi, Liang.,Yu, Hong-Jun.,Ortiz, Joseph D..,Xu, Xing-Yong.,Chen, Shen-Liang.,...&Peng, Shu-Zhen.(2012).Late Quaternary linkage of sedimentary records to three astronomical rhythms and the Asian monsoon, inferred from a coastal borehole in the south Bohai Sea, China.PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY,329,101-117. |
MLA | Yi, Liang,et al."Late Quaternary linkage of sedimentary records to three astronomical rhythms and the Asian monsoon, inferred from a coastal borehole in the south Bohai Sea, China".PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY 329(2012):101-117. |
入库方式: OAI收割
来源:地质与地球物理研究所
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