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Gobiolagus (Lagomorpha, Mammalia) from Eocene Ula Usu, Inner Mongolia, and comments on Eocene Lagomorphs of Asia
Meng, J; Hu, YM; Li, CK; Meng, J (reprint author), Amer Museum Nat Hist, Div Paleontol, Cent Pk W 79th St, New York, NY 10024 USA.
2005
发表期刊PALAEONTOLOGIA ELECTRONICA
ISSN1094-8074
卷号8期号:1页码:
文章类型Article
摘要Lagomorph specimens collected in 1925 by the Central Asiatic Expedition from the late middle Eocene Shara Murun Formation at Ula Usu, Shara Murun Region of Inner Mongolia, are described. These specimens belong to Gobiolagus tolmachovi and a new species, G. burkei. Gobiolagus burkei sp. nov. is similar to other species of the genus in having the pear-shaped p4 trigonid, short talonid on p4 and m1, talonid transverse and shorter than trigonid except for m2, enamel ridge connecting the trigonid and talonid at the lingual side, p4 significantly smaller than m1, and m2 the largest cheek teeth. It differs from other species in being smaller and having lower crowned cheek teeth, incisor ventral to cheek teeth so that a lingual protuberance is absent, and incisor extending posteriorly below the talonid of m2. It further differs from G. tolmachovi and G. andrewsi in having a less reduced p4 talonid. Eocene lagomorph genera and species are briefly reviewed. Diagnoses are emended or provided for G. tolmachovi, G. andrewsi, G. lii, Lushilagus, Shamolagus, Hypsimylus, Strenulagus, and Dituberolagus. Two Eocene species of Desmatolagus, D. vetustus and D. ardynense, are also discussed. Photographs of holotype specimens housed in the American Museum of Natural History are presented.; Lagomorph specimens collected in 1925 by the Central Asiatic Expedition from the late middle Eocene Shara Murun Formation at Ula Usu, Shara Murun Region of Inner Mongolia, are described. These specimens belong to Gobiolagus tolmachovi and a new species, G. burkei. Gobiolagus burkei sp. nov. is similar to other species of the genus in having the pear-shaped p4 trigonid, short talonid on p4 and m1, talonid transverse and shorter than trigonid except for m2, enamel ridge connecting the trigonid and talonid at the lingual side, p4 significantly smaller than m1, and m2 the largest cheek teeth. It differs from other species in being smaller and having lower crowned cheek teeth, incisor ventral to cheek teeth so that a lingual protuberance is absent, and incisor extending posteriorly below the talonid of m2. It further differs from G. tolmachovi and G. andrewsi in having a less reduced p4 talonid. Eocene lagomorph genera and species are briefly reviewed. Diagnoses are emended or provided for G. tolmachovi, G. andrewsi, G. lii, Lushilagus, Shamolagus, Hypsimylus, Strenulagus, and Dituberolagus. Two Eocene species of Desmatolagus, D. vetustus and D. ardynense, are also discussed. Photographs of holotype specimens housed in the American Museum of Natural History are presented.
关键词Lagomorphs Eocene Taxonomy Holotype Asia
WOS标题词Science & Technology ; Life Sciences & Biomedicine
关键词[WOS]MIDDLE OLIGOCENE ; NEI MONGOL ; CHINA
收录类别SCI
语种英语
WOS研究方向Paleontology
WOS类目Paleontology
WOS记录号WOS:000235796500009
引用统计
文献类型期刊论文
条目标识符http://119.78.100.205/handle/311034/3587
专题中科院古脊椎所(2000年以后)
古低等脊椎动物研究室
古哺乳动物研究室
通讯作者Meng, J (reprint author), Amer Museum Nat Hist, Div Paleontol, Cent Pk W 79th St, New York, NY 10024 USA.
作者单位1.Amer Museum Nat Hist, Div Paleontol, New York, NY 10024 USA
2.Chinese Acad Sci, Inst Vertebrate Paleontol & Paleoanthropol, Beijing 100044, Peoples R China
3.NYU, Grad Sch, Biol Program, New York, NY 10016 USA
4.CUNY City Coll, New York, NY 10016 USA
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Meng, J,Hu, YM,Li, CK,et al. Gobiolagus (Lagomorpha, Mammalia) from Eocene Ula Usu, Inner Mongolia, and comments on Eocene Lagomorphs of Asia[J]. PALAEONTOLOGIA ELECTRONICA,2005,8(1):—.
APA Meng, J,Hu, YM,Li, CK,&Meng, J .(2005).Gobiolagus (Lagomorpha, Mammalia) from Eocene Ula Usu, Inner Mongolia, and comments on Eocene Lagomorphs of Asia.PALAEONTOLOGIA ELECTRONICA,8(1),—.
MLA Meng, J,et al."Gobiolagus (Lagomorpha, Mammalia) from Eocene Ula Usu, Inner Mongolia, and comments on Eocene Lagomorphs of Asia".PALAEONTOLOGIA ELECTRONICA 8.1(2005):—.
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