Dinosaur tracks from the Lower Cretaceous Xiguayuan Formation in the Luanping Basin, Hebei Province, China

被引：3
|
作者：
Xing, Lida [1 ,2 ,3 ]
Lockley, Martin G. [4 ]
Qin, Zuohuan [2 ]
Klein, Hendrik [5 ]
Romilio, Anthony [6 ]
Persons, W. Scott [7 ]
Nie, Xin [8 ]
Wan, Xiaoqiao [1 ,2 ]
机构：
[1] China Univ Geosci, State Key Lab Biogeol & Environm Geol, Beijing 100083, Peoples R China
[2] China Univ Geosci, Sch Earth Sci & Resources, Beijing 100083, Peoples R China
[3] Chinese Acad Sci, Nanjing Inst Geol & Palaeontol, State Key Lab Palaeobiol & Stratig, Nanjing 210008, Jiangsu, Peoples R China
[4] Univ Colorado, Dinosaur Tracks Museum, POB 173364, Denver, CO 80217 USA
[5] Saurierwelt Palaontol Museum, Alte Richt 7, D-92318 Neumarkt, Germany
[6] Univ Queensland, Sch Biol Sci, Brisbane, Qld 4072, Australia
[7] Univ Alberta, Dept Biol Sci, 11455 Saskatchewan Dr, Edmonton, AB T6G 2E9, Canada
[8] Fourth Exploit Factor Fluabei Oilfield Co, Langfang 065000, Peoples R China
来源：
CRETACEOUS RESEARCH | 2019年 / 103卷
基金：
中国国家自然科学基金;
关键词：
Xiguayuan Formation; Caririchnium; Jialingpus; Eubrontes; Jehol Biota; JIAGUAN FORMATION; JINZHOUSAURUS-YANGI; DIVERSE SAUROPOD; YIXIAN FORMATION; SICHUAN BASIN; EAST-ASIA; THEROPOD; FOOTPRINTS; BIRD; PRESERVATION;
D O I：
10.1016/j.cretres.2019.06.009
中图分类号：
P5 [地质学];
学科分类号：
0709 ; 081803 ;
摘要：
The Qiaomaigoumen dinosaur tracksite was previously described briefly in 1995 and 2006 based on examination of a single surface (similar to 200 m(2)) with five trackways representing two quadrupedal ornithopods (Caririchnium isp.) and three bipedal theropods. While confirming this general description, this study also revealed that two additional sites (Sangyuan I and II) had been found, and that tracks from all three sites had been collected for local institutions. This created the opportunity to describe the ichnofauna more completely, including a variety of theropod morphotypes (cf. Jialingpus isp. and cf. Eubrontes isp.) not previously identified in this area. It is also inferred that the tracksites occur in the Xiguayuan Formation, not in the Jiufotang Formation as previously suggested. This indicates an equivalency with the Jehol Biota and some track elements corresponding generally to Jehol body fossils. (C) 2019 Elsevier Ltd. All rights reserved.
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页数：13
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