Dentaries of a caenagnathid (Dinosauria: Theropoda) from the Nemegt Formation of the Gobi Desert in Mongolia

被引:10
|
作者
Tsuihiji, Takanobu [1 ]
Watabe, Mahito [2 ]
Tsogtbaatar, Khishigjav [3 ]
Barsbold, Rinchen [3 ]
机构
[1] Univ Tokyo, Dept Earth & Planetary Sci, Bunkyo Ku, 7-3-1 Hongo, Tokyo 1130033, Japan
[2] Osaka City Univ, Dept Geosci, Sumiyoshi Ku, 3-3-138 Sugimoto, Osaka 5588585, Japan
[3] Mongolian Acad Sci, Inst Paleontol & Geol, Enkh Taivan St 63, Ulaanbaatar 210351, Mongolia
关键词
Dinosauria; Theropoda; Caenagnathidae; Oviraptorosauria; Upper Cretaceous; OVIRAPTOROSAURIA; CHIROSTENOTES; STRATIGRAPHY; SPECIMENS; INSIGHTS;
D O I
10.1016/j.cretres.2016.03.007
中图分类号
P5 [地质学];
学科分类号
0709 ; 081803 ;
摘要
A symphyseal region of the fused dentaries of a caenagnathid theropod is described from the Upper Cretaceous Nemegt Formation at the Bugin Tsav locality in the Mongolian Gobi Desert. In contrast to the high diversity of Caenagnathidae in the upper Campanian to Maastrichtian in North America, only specimens of a single caenagnathid, Elmisaurus raurus, have been reported in the coeval strata in Asia. Although dentaries are commonly-found bones in the fossil record of Caenagnathidae, the present specimen is the first discovery of caenagnathid dentaries from the upper Campanian to Maastrichtian in Asia. The Nemegt Formation is unique for its diverse oviraptorosaurian fauna that includes both Caenagnathidae and Oviraptoridae as well as the non-caenagnathoid Avimimus portentosus. Hypothesized coexistence of eolian and fluvial environments in the Gobi Basin during the deposition of the Nemegt Formation might explain such co-occurrence of Caenagnathidae and Oviraptoridae. (C) 2016 Elsevier Ltd. All rights reserved.
引用
收藏
页码:148 / 153
页数:6
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