Paleogene integrative stratigraphy and timescale of China
文献类型：期刊论文
| 作者 | Wang, Yuanqing1,2,3 ; Li, Qian1,2; Bai, Bin1,2; Jin, Xun1,2; Mao, Fangyuan1,2; Meng, Jin4
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| 刊名 | SCIENCE CHINA-EARTH SCIENCES
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| 出版日期 | 2019 |
| 卷号 | 62期号:1页码:287-309 |
| 关键词 | Paleogene Correlation Biostratigraphy Magnetostratigraphy Chronostratigraphy |
| ISSN号 | 1674-7313 |
| DOI | 10.1007/s11430-018-9305-y |
| 通讯作者 | Wang, Yuanqing(wangyuanqing@ivpp.ac.cn) |
| 英文摘要 | The Paleogene is the first period after the Mesozoic Mass Extinction. Mammals become the dominant group in the terrestrial ecosystem with a rapid radiation, and Asia has been considered to be the origin place of several mammalian groups. The Paleogene System consists mostly of terrestrial deposits in Asia, especially in East Asia. A well-established regional chronostratigraphic framework is the foundation for understanding both the Paleogene geologic history and evolutionary history of Asia and their relationships. The Paleogene is subdivided into the Paleocene, Eocene and Oligocene in the International Chronostratigraphic Chart. Based on the land mammal ages, the Chinese terrestrial Paleogene can be subdivided into 11 stages: the Shanghuan, Nongshanian and Bayanulanian stages of the Paleocene, the Lingchan, Arshantan, Irdinmanhan, Sharamurunian, Ulangochuian and Baiyinian stages of the Eocene, and the Ulantatalian and Tabenbulukian stages of the Oligocene. These stages have distinctive paleontological characters, with special significance of fossil mammals, which provide a reliable practical basis. The bases of the Shanghuan, Lingchan, and Ulantatalian stages are coincident respectively with those of the Paleocene, Eocene and Oligocene. The ages for their bases are determined as 66.0, 56.0 and 33.9 Ma, respectively, following that for the corresponding series in the International Chronostratigraphic Chart. For other stages, estimated ages are provided based on available paleomagnetic results. |
| WOS关键词 | GLOBAL STRATOTYPE SECTION ; EOCENE THERMAL MAXIMUM ; POINT GSSP ; MIDDLE PALEOCENE ; NANXIONG BASIN ; OLIGOCENE ; RECORD ; BOUNDARY ; TERTIARY ; MAMMALS |
| 资助项目 | National Natural Science Foundation of China[41572021] ; National Commission on Stratigraphy of China |
| WOS研究方向 | Geology |
| 语种 | 英语 |
| WOS记录号 | WOS:000455070400012 |
| 出版者 | SCIENCE PRESS |
| 资助机构 | National Natural Science Foundation of China ; National Commission on Stratigraphy of China |
| 源URL | [http://119.78.100.205/handle/311034/9299]  |
| 专题 | 中国科学院古脊椎动物与古人类研究所 |
| 通讯作者 | Wang, Yuanqing |
| 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.Univ Chinese Acad Sci, Coll Earth Sci, Beijing 100049, Peoples R China 4.Amer Museum Nat Hist, New York, NY 10024 USA |
| 推荐引用方式 GB/T 7714 | Wang, Yuanqing,Li, Qian,Bai, Bin,et al. Paleogene integrative stratigraphy and timescale of China[J]. SCIENCE CHINA-EARTH SCIENCES,2019,62(1):287-309. |
| APA | Wang, Yuanqing,Li, Qian,Bai, Bin,Jin, Xun,Mao, Fangyuan,&Meng, Jin.(2019).Paleogene integrative stratigraphy and timescale of China.SCIENCE CHINA-EARTH SCIENCES,62(1),287-309. |
| MLA | Wang, Yuanqing,et al."Paleogene integrative stratigraphy and timescale of China".SCIENCE CHINA-EARTH SCIENCES 62.1(2019):287-309. |
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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