A new late-diverging non-hadrosaurid hadrosauroid (Dinosauria: Ornithopoda) from southwest China: Support for interchange of dinosaur faunas across East Asia during the Late Cretaceous

被引:0
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作者
Dai, Hui [1 ,2 ]
Ma, Qingyu [1 ,2 ]
Xiong, Can [1 ,2 ]
Lin, Yu [1 ,2 ]
Zeng, Hui [3 ]
Tan, Chao [1 ,2 ]
Wang, Jun [4 ]
Zhang, Yuguang [5 ]
Xing, Hai [5 ,6 ,7 ,8 ]
机构
[1] Chongqing Bur Geol & Mineral Resource Explorat & D, Hydrogeol & Engn Geol Team 208, Chongqing 400700, Peoples R China
[2] Chongqing Key Lab Paleontol & Paleoenvironm Coevol, Chongqing 400700, Peoples R China
[3] Bur Planning & Nat Resources Qianjiang Dist, Chongqing 409000, Peoples R China
[4] Yunnan Univ, Sch Earth Sci, Kunming 650500, Yunnan, Peoples R China
[5] Natl Nat Hist Museum China, Beijing 100050, Peoples R China
[6] Canadian Museum Nat, Beaty Ctr Species Discovery, Ottawa, ON K1P 6P4, Canada
[7] Canadian Museum Nat, Palaeobiol Sect, Ottawa, ON K1P 6P4, Canada
[8] Chinese Acad Sci, Nanjing Inst Geol & Palaeontol, Key Lab Palaeobiol & Petr Stratig, Nanjing 210008, Jiangsu, Peoples R China
基金
中国国家自然科学基金; 芬兰科学院;
关键词
Non-hadrosaurid hadrosauroid; Zhengyang Formation; Late Cretaceous; Qianjiang district; Southwest China; ORNITHISCHIA; THEROPODA; DEPOSITS; HISTORY; AGE;
D O I
10.1016/j.cretres.2024.105995
中图分类号
P5 [地质学];
学科分类号
0709 ; 081803 ;
摘要
A non-hadrosaurid hadrosauroid, Qianjiangsaurus changshengi gen. et sp. nov., is named and described here based on an incomplete, partially articulated skeleton from the top of the Upper Cretaceous Zhengyang Formation in Qianjiang District, Chongqing Municipality, southwest China. The skeleton displays a transitional morphology between non-hadrosaurid hadrosauroids and hadrosaurids. The diagnosis of the taxon is therefore defined as a unique combination of characters, including a series of plesiomorphic features typical of non-hadrosaurid hadrosauroids, some apomorphic features common among hadrosaurids but rarely reported in non-hadrosaurid hadrosauroids, and a probable autopomorphy, namely the fan-shaped prepubic process of the pubis strongly anteroposteriorly constricted and dorsoventrally expanded, with the length/height ratio of similar to 0.79. Phylogenetic analysis recovers a sister-taxon relationship between Qianjiangsaurus and Plesiohadros outside of Hadrosauridae, and the clade consisting of the two taxa is positioned higher on the tree than Gobihadros and Gilmoreosaurus, but below the clade of Telmatosaurus + Tethyshadros, Eotrachodon and Zhanghenglong. Combining the morphological data with the phylogenetic topology identifies Q. changshengi as a late-branching non-hadrosaurid hadrosauroid. Given that the age assemblage of the eight hadrosauroids closely related to Qianjiangsaurus in phylogeny spans the Santonianeearly Maastrichtian time interval, the top of the Zhengyang Formation, from which Qianjiangsaurus is recovered, is possibly restricted to the late Late Cretaceous in age. Hierarchical clustering of twelve hadrosauroid-bearing dinosaur assemblages from the Late Cretaceous deposits of Asia shows a strong correlation between the Zhengyang Formation and the Djadokhta and Baruungoyot formations in Mongolia that supports coeval interchange of dinosaur faunas across East Asia. (c) 2024 Elsevier Ltd. All rights are reserved, including those for text and data mining, AI training, and similar technologies.
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页数:18
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