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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
ISSN1000-9515
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
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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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