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Articles

Hybodontiform shark remains (Chondrichthyes, Elasmobranchii) from the Lower Triassic of Yunnan Province, China, with comments on hybodontiform diversity across the PTB

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Article: e2108712 | Received 20 Dec 2021, Accepted 09 Jul 2022, Published online: 06 Sep 2022
 

ABSTRACT

Hybodontiform shark teeth, cephalic and fin spines as well as placoid scales are reported here for the first time from the continental, Lower Triassic Dongchuan Formation near the village of Zhaojia (Huize County, Yunnan Province) in south-west China. The isolated teeth are assigned to three unidentified hybodontiforms but also to a new species of Parvodus, P. huizodus sp. nov., the oldest record of this small-toothed lonchidiid shark genus, extending its range well down into the Lower Triassic. This new species, together with additional hybodontiform remains, provides new evidence of shark occurrences in the aftermath of the end-Permian mass extinction event, when freshwater environments might have acted as centers of origin rather than refugia for sharks. A review of the species assigned to Parvodus and similar small hybodontiform sharks reveals two distinct ecomorphological groups. Group 1, which is characterized by clutching-type dentitions, includes eight species (three of which remain unnamed) ranging from the Middle Triassic to Lower Cretaceous, while group 2, characterized by cutting-crushing type dentitions, comprises 11 species (six of which remain unnamed) including the type-species, P. rugianus ranging from the Lower Triassic to the Lower Cretaceous. The new fossils documented here reveal that hybodontiforms were already adapted to freshwater environments in the Lower Triassic rather than in the Jurassic in China.

ACKNOWLEDGMENTS

We thank G. M. Ren, X. Z. Cui, Z. B. Gou for the Zircon U-Pb analysis, G. Wang for help with using the SEM, S. L. Lin and Y. D. Qin for measuring the section. We thank C. Underwood and A. López-Arbarello for editorial assistance, and J. Fischer and an anonymous reviewer for constructive suggestions. This work is supported by National Natural Science Foundation of China (No. 42102019, 41772022, and 41661134047), projects from China Geological Survey (DD20190054, DD20160020, DD20221635) and Observation and Research Station, Ministry of Natural Resources of the People’s Republic of China.

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