KMS Institute of Vertebrate Paleontology and Paleoanthropology
Sequence of the Cenozoic mammalian faunas of the Linxia Basin in Gansu, China | |
Deng, T; Wang, XM; Ni, XJ; Liu, LP; Deng, T (reprint author), Chinese Acad Sci, Inst Vertebrate Paleontol & Paleoanthropol, Beijing 100044, Peoples R China. | |
2004 | |
发表期刊 | ACTA GEOLOGICA SINICA-ENGLISH EDITION |
ISSN | 1000-9515 |
卷号 | 78期号:1页码:8-14 |
文章类型 | Article |
摘要 | In the Linxia Basin on the northeast margin of the Tibetan Plateau, the Cenozoic strata are very thick and well exposed. Abundant mammalian fossils are discovered in the deposits from the Late Oligocene to the Early Pleistocene. The Dzungariotherium fauna comes from the sandstones of the Jiaozigou Formation, including many representative Late Oligocene taxa. The Platybelodon fauna comes from the sandstones of the Dongxiang Formation and the conglomerates of the Laogou Formation, and its fossils are typical Middle Miocene forms, such as Hemicyon, Amphicyon, Platybelodon, Choerolophodon, Anchitherium, and Hispanotherium. ne Hipparion fauna comes from the red clay of the Liushu and Hewangiia Formations, and its fossils can be distinctly divided into four levels, including three Late Miocene levels and one Early Pliocene level. In the Linxia Basin, the Hipparion fauna has the richest mammalian fossils. The Equus fauna comes from the Wucheng Loess, and it is slightly older than that of the classical Early Pleistocene Nihewan Fauna. The mammalian faunas from the Linxia Basin provide the reliable evidence to divide the Cenozoic strata of this basin and correlate them with European mammalian sequence.; In the Linxia Basin on the northeast margin of the Tibetan Plateau, the Cenozoic strata are very thick and well exposed. Abundant mammalian fossils are discovered in the deposits from the Late Oligocene to the Early Pleistocene. The Dzungariotherium fauna comes from the sandstones of the Jiaozigou Formation, including many representative Late Oligocene taxa. The Platybelodon fauna comes from the sandstones of the Dongxiang Formation and the conglomerates of the Laogou Formation, and its fossils are typical Middle Miocene forms, such as Hemicyon, Amphicyon, Platybelodon, Choerolophodon, Anchitherium, and Hispanotherium. ne Hipparion fauna comes from the red clay of the Liushu and Hewangiia Formations, and its fossils can be distinctly divided into four levels, including three Late Miocene levels and one Early Pliocene level. In the Linxia Basin, the Hipparion fauna has the richest mammalian fossils. The Equus fauna comes from the Wucheng Loess, and it is slightly older than that of the classical Early Pleistocene Nihewan Fauna. The mammalian faunas from the Linxia Basin provide the reliable evidence to divide the Cenozoic strata of this basin and correlate them with European mammalian sequence. |
关键词 | Linxia Basin Cenozoic Stratigraphy Mammalian Fossil Gansu China |
WOS标题词 | Science & Technology ; Physical Sciences |
关键词[WOS] | SUBDIVISION ; NEOGENE ; FOSSILS |
收录类别 | SCI ; ISTP |
语种 | 英语 |
WOS研究方向 | Geology |
WOS类目 | Geosciences, Multidisciplinary |
WOS记录号 | WOS:000221717300003 |
引用统计 | |
文献类型 | 期刊论文 |
条目标识符 | http://119.78.100.205/handle/311034/3675 |
专题 | 中科院古脊椎所(2000年以后) 古哺乳动物研究室 |
通讯作者 | Deng, T (reprint author), Chinese Acad Sci, Inst Vertebrate Paleontol & Paleoanthropol, Beijing 100044, Peoples R China. |
作者单位 | 1.Chinese Acad Sci, Inst Vertebrate Paleontol & Paleoanthropol, Beijing 100044, Peoples R China 2.Museum Nat Hist Los Angeles Cty, Los Angeles, CA 90007 USA |
推荐引用方式 GB/T 7714 | Deng, T,Wang, XM,Ni, XJ,et al. Sequence of the Cenozoic mammalian faunas of the Linxia Basin in Gansu, China[J]. ACTA GEOLOGICA SINICA-ENGLISH EDITION,2004,78(1):8-14. |
APA | Deng, T,Wang, XM,Ni, XJ,Liu, LP,&Deng, T .(2004).Sequence of the Cenozoic mammalian faunas of the Linxia Basin in Gansu, China.ACTA GEOLOGICA SINICA-ENGLISH EDITION,78(1),8-14. |
MLA | Deng, T,et al."Sequence of the Cenozoic mammalian faunas of the Linxia Basin in Gansu, China".ACTA GEOLOGICA SINICA-ENGLISH EDITION 78.1(2004):8-14. |
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