中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
Late Miocene Microstonyx remains (Suidae, Mammalia) from Northern China

文献类型:期刊论文

作者Liu, LP; Kostopoulos, DS; Fortelius, M; Liu, LP (reprint author), Inst Vertebrate Paleontol & Paleoanthropol, POB 643, Beijing 100044, Peoples R China.
刊名GEOBIOS
出版日期2004
卷号37期号:1页码:49-64
关键词Microstonyx Suidae China Miocene Systematic Palaeoecology
ISSN号0016-6995
文献子类Article
英文摘要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.
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WOS研究方向Paleontology
语种英语
WOS记录号WOS:000189262500005
公开日期2013-11-27
源URL[http://119.78.100.205/handle/311034/3686]  
专题古脊椎动物与古人类研究所_图书馆1
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
推荐引用方式
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.

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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