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Late Miocene Microstonyx remains (Suidae, Mammalia) from Northern China
Liu, LP; Kostopoulos, DS; Fortelius, M; Liu, LP (reprint author), Inst Vertebrate Paleontol & Paleoanthropol, POB 643, Beijing 100044, Peoples R China.
2004
发表期刊GEOBIOS
ISSN0016-6995
卷号37期号:1页码:49-64
文章类型Article
摘要Several large suid cranial remains attributed to Microstonyx major are part of a new Hipparion Fauna collection from the Hezheng area, Northern China. The new material confirms the presence of Microstonyx in the late Miocene of the area. The Chinese form belongs to a small-sized eastern population with reduced premolar row and clear sexual bimodality. Statistical comparison shows that Microstonyx major was a polymorphic species and reinforces recognition of Hippopotamodon as a separate genus, defined by relatively stout premolars resulting from a different underlying pattern of allometric growth. The presence of Microstonyx in North China and the distinct suid assemblage that lived there suggest biogeographic connections between Northern China and Western Eurasia in contrast to isolation from Southern China and the Indian subcontinent. The suid fauna of the late Miocene of Northern China seems to have been restricted to the later, more humid phase represented by the Red Clay faunas. (C) 2003 Published by Elsevier SAS.; Several large suid cranial remains attributed to Microstonyx major are part of a new Hipparion Fauna collection from the Hezheng area, Northern China. The new material confirms the presence of Microstonyx in the late Miocene of the area. The Chinese form belongs to a small-sized eastern population with reduced premolar row and clear sexual bimodality. Statistical comparison shows that Microstonyx major was a polymorphic species and reinforces recognition of Hippopotamodon as a separate genus, defined by relatively stout premolars resulting from a different underlying pattern of allometric growth. The presence of Microstonyx in North China and the distinct suid assemblage that lived there suggest biogeographic connections between Northern China and Western Eurasia in contrast to isolation from Southern China and the Indian subcontinent. The suid fauna of the late Miocene of Northern China seems to have been restricted to the later, more humid phase represented by the Red Clay faunas. (C) 2003 Published by Elsevier SAS.
关键词Microstonyx Suidae China Miocene Systematic Palaeoecology
WOS标题词Science & Technology ; Life Sciences & Biomedicine
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收录类别SCI
语种英语
WOS研究方向Paleontology
WOS类目Paleontology
WOS记录号WOS:000189262500005
引用统计
文献类型期刊论文
条目标识符http://119.78.100.205/handle/311034/3685
专题中科院古脊椎所(2000年以后)
通讯作者Liu, LP (reprint author), Inst Vertebrate Paleontol & Paleoanthropol, POB 643, Beijing 100044, Peoples R China.
作者单位1.Inst Vertebrate Paleontol & Paleoanthropol, Beijing 100044, Peoples R China
2.Univ Thessaloniki, Lab Paleontol, Dept Geol, Thessaloniki 54124, Greece
3.Univ Helsinki, Dept Geol, FIN-00014 Helsinki, Finland
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GB/T 7714
Liu, LP,Kostopoulos, DS,Fortelius, M,et al. Late Miocene Microstonyx remains (Suidae, Mammalia) from Northern China[J]. GEOBIOS,2004,37(1):49-64.
APA Liu, LP,Kostopoulos, DS,Fortelius, M,&Liu, LP .(2004).Late Miocene Microstonyx remains (Suidae, Mammalia) from Northern China.GEOBIOS,37(1),49-64.
MLA Liu, LP,et al."Late Miocene Microstonyx remains (Suidae, Mammalia) from Northern China".GEOBIOS 37.1(2004):49-64.
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