The longest theropod trackway from East Asia, and a diverse sauropod-, theropod-, and ornithopod-track assemblage from the Lower Cretaceous Jiaguan Formation, southwest China

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• 作者：Lida Xing^a ; ^{xinglida@gmail.com" class="auth_mail" title="E-mail the corresponding author} ; Martin G. Lockley^b ; Jianping Zhang^a ; Hendrik Klein^c ; Daniel Marty^d ; Guangzhao Peng^e ; Yong Ye^e ; Richard T. McCrea^f ; W.Scott Persons IV^g ; Ting Xu^h
• 关键词：Grallator ; Eubrontes ; Ornithopodichnus ; Lower Cretaceous ; Jiaguan Formation ; China
• 刊名：Cretaceous Research
• 出版年：2015
• 出版时间：September-December 2015
• 年：2015
• 卷：56
• 期：Complete
• 页码：345-362
• 全文大小：7827 K

文摘

Here we report a large dinosaur tracksite from an extensive fluvial sandstone surface in the Lower Cretaceous Jiaguan Formation of Sichuan Province, China. The site contains over 250 individual tracks comprising at least 18 recognizable trackways, including the longest theropod trackway (cf. Eubrontes) known from China. This exceptional theropod trackway consists of 81 successive footprints covering a distance of 69 m. The tracks are well-preserved and are expressed both as true tracks on the main “upper” surface and as transmitted undertracks on a locally exposed “lower” bed. Also recorded are six other theropod trackways, including small Grallator-like ichnites, eight sauropod trackways (cf. Brontopodus), and three small ornithopod (cf. Ornithopodichnus) trackways with a parallel orientation, which may indicate gregarious behavior. Several trackways of a larger theropod trackmaker show pes imprints with elongated traces of the metatarsals, suggesting extramorphological (substrate-controlled) variation and/or plantigrade posture, which is here interpreted as indicating a change in gait assumed in response to deep and soft sediment. The assemblage indicates a diverse dinosaur fauna in the Lower Cretaceous Sichuan Basin with variously sized theropods, sauropods, and ornithopods. The late occurrence of footprints of the Grallator-Eubrontes plexus in Lower Cretaceous strata is further evidence of the extended stratigraphic range of this morphotype and the distinct palaeobiogeographic distribution of these trackmakers in East Asia.