Terrestrial Mio-Pliocene Boundary in the Linxia Basin, Gansu, China
文献类型：期刊论文
| 作者 | Deng Tao1 ; Hou Sukuan1,2; Shi Qinqin1,2; Chen Shaokun1,2; He Wen3; Chen Shanqin3; dengtao@ivpp.ac.cn
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| 刊名 | ACTA GEOLOGICA SINICA-ENGLISH EDITION
 |
| 出版日期 | 2011-04-01 |
| 卷号 | 85期号:2页码:452-464 |
| 关键词 | Miocene Pliocene Boundary Stratotype Mammalian Fauna Hipparion Red Clay Linxia Basin |
| ISSN号 | 1000-9515 |
| 文献子类 | Article |
| 英文摘要 | The Lower Pliocene of the Linxia Basin in Gansu Province is one of only a few representative sections for the Early Pliocene sedimentary records in northern China, and even in East Asia. Recently, abundant mammalian fossils were found from the base of red clays of the Lower Pliocene Hewangjia Formation at Duikang in Guanghe County within this basin. Previously, the Pliocene mammals were sparsely found in China, and most were collected from fluvial and lacustrine deposits in the eastern Loess Plateau. Mammals from the widely distributed Pliocene Hipparion Red Clay are less in number. The known fossils from Duikang include 20 species and belong to the Shilidun Fauna. Their faunal components are similar to the Early Pliocene Gaozhuang Fauna from Yushe, Shanxi. On the other hand, some taxa from Duikang have not been found in the Gaozhuang Fauna, are slightly more primitive in evolutionary level, and appeared mainly in the Late Miocene. As a result, the age of the Dui g fossils may be slightly earlier than that of the Gaozhuang Fauna and closer to the lower boundary of the Pliocene. The Duikang fossiliferous bed is 0.8 m above the top of the Late Miocene Liushu Formation, and the first occurrence of the three-toed horse Hipparion pater can be regarded as a biostratigraphical marker of the Miocene/Pliocene boundary. In conclusion, Dui g is an ideal candidate locality to establish as the stratotype of the lower boundary of the Chinese terrestrial Pliocene. |
| WOS关键词 | ENVIRONMENTAL-CHANGE ; NORTHERN CHINA ; MIOCENE ; RECORD ; PALEOSOLS ; PALEODIET ; PAKISTAN ; PLATEAU ; NEOGENE ; ORIGIN |
| WOS研究方向 | Geology |
| 语种 | 英语 |
| WOS记录号 | WOS:000289845800018 |
| 公开日期 | 2013-11-27 |
| 源URL | [http://119.78.100.205/handle/311034/4430]  |
| 专题 | 古脊椎动物与古人类研究所_图书馆1 古脊椎动物与古人类研究所_古哺乳动物研究室 |
| 通讯作者 | dengtao@ivpp.ac.cn |
| 作者单位 | 1.Chinese Acad Sci, Key Lab Evolutionary Systemat Vertebrates, Inst Vertebrate Paleontol & Paleoanthropol, Beijing 100044, Peoples R China 2.Chinese Acad Sci, Grad Sch, Beijing 100039, Peoples R China 3.Hezheng Paleozool Museum, Hezheng 731200, Gansu, Peoples R China |
| 推荐引用方式 GB/T 7714 | Deng Tao,Hou Sukuan,Shi Qinqin,et al. Terrestrial Mio-Pliocene Boundary in the Linxia Basin, Gansu, China[J]. ACTA GEOLOGICA SINICA-ENGLISH EDITION,2011,85(2):452-464. |
| APA | Deng Tao.,Hou Sukuan.,Shi Qinqin.,Chen Shaokun.,He Wen.,...&dengtao@ivpp.ac.cn.(2011).Terrestrial Mio-Pliocene Boundary in the Linxia Basin, Gansu, China.ACTA GEOLOGICA SINICA-ENGLISH EDITION,85(2),452-464. |
| MLA | Deng Tao,et al."Terrestrial Mio-Pliocene Boundary in the Linxia Basin, Gansu, China".ACTA GEOLOGICA SINICA-ENGLISH EDITION 85.2(2011):452-464. |
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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