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Research Article

A new elasmothere genus and species from the middle Miocene of Tongxin, Ningxia, China, and its phylogenetic relationship

ORCID Icon, , &
Article: 2236619 | Received 04 Sep 2022, Accepted 12 Jun 2023, Published online: 18 Aug 2023
 

Abstract

The elasmotheres were well diversified and widespread throughout the Neogene in Eurasia and East Africa. Here we report a new elasmothere genus and species, Tongxinotherium latirhinum gen. et sp. nov., from the Zhang’enbao Formation (middle Miocene) of Tongxin, Ningxia, China. The new genus is characterized by a broad and thick nasal bone, the ‘U’-shaped nasal notch located at the level of P3, the anterior margin of the orbit situated at the level of M2, subhypsodont teeth covered and filled by plentiful cement, slightly developed enamel foldings, expanded protocone with anterior and posterior constrictions, the middle valley and posterior valley closed on the premolars, protoloph separated from the ectoloph on P2, and buccal and lingual cingula present on premolars, but absent on molars. A phylogenetic analysis reveals that Tongxinotherium latirhinum gen. et sp. nov. is more derived than the early elasmotheres, and more primitive than Iranotherium and Ningxiatherium, bridging a morphological and stratigraphical gap between them. The discovery of new material improves the morphological characteristics of the early elasmotheres’ horns and increases the diversity of the middle Miocene elasmotheres.

http://zoobank.org/urn:lsid:zoobank.org:pub:7DF2F57F-38DD-4FBF-B3DF-57AADD510131

Disclosure statement

No potential conflict of interest was reported by the author(s).

Acknowledgements

We thank Prof. Zhanxiang Qiu for his constructive suggestions and comments. We thank Yu Chen and Xiaocong Guo for their illustrations; Wei Gao for his photographs; Dan Su for her assistance in the repair of the fossil. We are grateful to the editors Zerina Johanson, Sue Greene, Jérémy Tissier, an anonymous reviewer, and especially Pierre-Olivier Antoine for their constructive comments and criticisms. We thank the Second Comprehensive Scientific Expedition on the Tibetan Plateau (2019QZKK0705). This research was supported by the Chinese Academy of Sciences (XDB26000000, XDA20070203, QYZDY-SSW-DQC022) and the National Natural Science Foundation of China (42172001).

Supplemental material

Supplemental material for this article can be accessed here: http://dx.doi.org/10.1080/14772019.2023.2236619.

Associate Editor: Jérémy Tissier

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