Sullivan, R.M. and Lucas, S.G., eds., 2016, Fossil Record 5. New Mexico Museum of Natural History and Science Bulletin 74. 339 A POSSIBLE ANKYLOSAURIAN (THYREOPHORA) TRACKWAY FROM THE LOWER CRETACEOUS JIAGUAN FORMATION OF EMEI, SOUTHWEST CHINA: PALEOECOLOGICAL IMPLICATIONS LIDA XING1, RICHARD T. MCCREA2, MARTIN G. LOCKLEY3, TINGQING LU4, MICHAEL E. BURNS5, GUANGZHAO PENG6 and JIANPING ZHANG1 1School of the Earth Sciences and Resources, China University of Geosciences Beijing 100083, China; -email:
[email protected]; 2Peace Region Palaeontology Research Centre, Tumbler Ridge, British Columbia, Canada; 3Dinosaur Tracks Museum, University of Colorado Denver, P.O. Box 173364, CO, 80217, Denver; 4School of Resources and Environmental Engineering, Southwest Petroleum University, Chengdu, Sichuan, China; 5Department of Biology, Jacksonville State University, 700 Pelham Rd, Jacksonville, AL 36265; 6Zigong Dinosaur Museum, Zigong, Sichuan, China Abstract—Ankylosaurian trackways are rare in the Cretaceous red beds of China, and in Asia, in general. Here we report on a possible thyreophoran (ankylosaurian) trackway from the Jiaguan Formation of Sichuan Province, China inferred from an important historical (1970s) report, the first dealing with tracks from this formation. The Jiaguan Formation has recently become well known for an abundance of saurischian-dominated tracksites, indicating that the 1970s report is anomalous. Nevertheless, the record describes a trackway, which represents a large animal with a wide pes up to ~41 cm and a transverse morphology (length/width ~0.8). The trackway is unusual because of the lack of visible manus tracks, perhaps due to preservational factors. The rarity of such trackway morphotypes in China is attributed to the facies preference of Cretaceous ankylosaurians for organic-rich coastal plain substrates, which abound in North America where ankylosaur dominated ichnofacies have been defined.