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Saurischian track assemblages from the Lower Cretaceous Shenhuangshan Formation in the Yuanma Basin,Southern China
Affiliation:1. Dinosaur Trackers Research Group, University of Colorado Denver, Denver, CO 80217, USA;2. Qingdao Institute of Marine Geology, China Geological Survey, Qingdao 266071, China;3. Department of Environmental Sciences, Tokyo Gakugei University, Koganei, Tokyo 184-8501, Japan;4. School of the Earth Sciences and Resources, China University of Geosciences, Beijing 100083, China;5. Beijing Museum of Natural History, Beijing, China;6. Shandong Provincial No.4 Institute of Geological and Mineral Resources, Weifang 261021, China;7. Institute of Vertebrate Paleontology and Paleoanthropology, Beijing, China
Abstract:Cretaceous dinosaur tracks from Hunan Province are historically significant as the basis for three ichnotaxa: Xiangxipus chenxiensis, Xiangxipus youngi, and Hunanpus jiuquwanensis all representing theropodan tracks, described from a single site in 1982. Although the type locality has since been destroyed, the type specimen and replicas remained available for restudy in 2006, when paratype Hunanpus tracks and sauropod footprints were described from a second, nearby locality. Material from both localities is here re-described in detail. It is proposed that while Xiangxipus chenxiensis can be regarded as a distinct ichnospecies, probably representing an ornithomimid trackmaker, Xiangxipus youngi cannot be accommodated in the same ichnogenus. We consider it similar to the ichnogenus Wupus from the Lower Cretaceous of Sichuan Province, and therefore of possible avian affinity. We also find no justification for regarding Hunanpus jiuquwanensis as generically distinct from the widespread ichnogenus Grallator, and therefore rename it Grallator jiuquwanensis comb. nov. The Hunan track record is generally consistent with the sparse record of theropod skeletal remains in the province, but adds evidence of sauropods that was previously lacking.
Keywords:Sauropod  Theropod  Footprints  Shenhuangshan Formation  Lower Cretaceous
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