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    Volume 47 Issue 11
    Nov.  2022
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    Article Contents
    Li Yangui, Yao Huazhou, Foster William J., Xing Lida, Wang Chuanshang, Tahir Asma, Khan Junaid, An Zhihui, Zhao He, Wang Jianxiong, 2022. First Discovery of Middle Jurassic Theropod Trackways in Changdu Region, Eastern Tibet of China. Earth Science, 47(11): 4222-4244. doi: 10.3799/dqkx.2022.395
    Citation: Li Yangui, Yao Huazhou, Foster William J., Xing Lida, Wang Chuanshang, Tahir Asma, Khan Junaid, An Zhihui, Zhao He, Wang Jianxiong, 2022. First Discovery of Middle Jurassic Theropod Trackways in Changdu Region, Eastern Tibet of China. Earth Science, 47(11): 4222-4244. doi: 10.3799/dqkx.2022.395

    First Discovery of Middle Jurassic Theropod Trackways in Changdu Region, Eastern Tibet of China

    doi: 10.3799/dqkx.2022.395
    • Received Date: 2022-06-27
      Available Online: 2022-12-07
    • Publish Date: 2022-11-25
    • A new dinosaur track site, Anietang site, was discovered in Changdu region of eastern Tibet. The lithostratigraphy of this track site is mainly lakeside purplish red medium-fine sandstone of the Middle Jurassic Dabuka Formation. Four exquisitely convex track layers (footprint types including Grallator, large theropods, small theropods and small sauropods) and two perfect track-ways were found. Four sequential Grallator footprints that make up the T1 trackway are named Grallator anietangensis isp nov., and a detailed morphological analysis was performed on it. It is doubtless that the Grallator was found in Tibet for the first time, and the size and gait of track-maker are discussed. Nine large theropod footprints that make up T2 trackway are classified as Theropoda igen et isp. indet.. The current study has described the morphology of Theropoda igen et isp. indet., and it is determined that this kind of footprint is found for the first time in China. The consecutive and clear trail tracks of T2 indicate that the trackmaker was not in a normal gait, but a special behavior to deal with a particular situation. It is speculated that the trackmaker was detecting situation with its raised body while walking at a very low speed. The forequarters were raised, resulted in the tail to sag correspondingly, and left trail tracks. Both trackways show that the trackmakers were walking along the bank of ancient Changdu Lake. At present, the dinosaur skeletons and the Grallator footprints found in China all show a migration pattern with the Southwest China as the center and then spreading around. But the speed of dinosaur migration reflected by the Grallator footprints is faster than that of skeletons.

       

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