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Articles

The vertebrate fauna of the Upper Permian of Niger—X. The mandible of the captorhinid reptile Moradisaurus grandis

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Article: e1531877 | Received 11 Sep 2017, Accepted 25 Jul 2018, Published online: 07 Feb 2019
 

ABSTRACT

Recent field work in the upper Permian Moradi Formation of Niger has yielded new material of the late-occurring and largest moradisaurine captorhinid, Moradisaurus grandis. The material includes two right hemimandibles, which represent individuals that are slightly smaller than the holotype. The smaller size of these mandibles, together with evidence in the form of tooth replacement, strongly suggest that the new material is ontogenetically younger than the holotype. The available evidence implies that tooth rows were added during growth in M. grandis. The mandible of M. grandis is distinguished from other moradisaurines in the extreme lingual extension of the tooth plate, which forms a dental shelf or plateau that supports the three lingual-most rows of teeth. In addition, a mentomeckelian bone is preserved, the first to be reported in a Paleozoic reptile. In contrast to the conspicuous wear documented on the teeth of certain other moradisaurines, wear facets are not observed on the teeth of the M. grandis specimens described here. The absence of tooth wear is surprising because the articular morphology of M. grandis is virtually identical to, albeit slightly larger than, that of Labidosaurikos meachami, for which propalinal jaw movement was first inferred in a moradisaurine. A phylogenetic analysis incorporating the new anatomical information confirms the hypothesis that M. grandis forms a clade with Rothianiscus multidontus and Gansurhinus qingtoushanensis within Moradisaurinae, and positions Captorhinikos chozaensis as the basal-most member of the subfamily.

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ACKNOWLEDGMENTS

We thank R. O’Keefe, S. Steyer, R. Smith, B. Gado, A. Maga, A. Dindine, and D. Sindy for their assistance in the field; R. Masek and B. Crowley for preparation of MNN MOR78 and MOR42, respectively; and J. Swales for the fine illustrations. D. Berman, J. Bolt, R. Cifelli, M. Carrano, A. Henrici, C. Mehling, and M. Norell graciously provided comparative material and/or casts from their respective institutions. S.P.M. thanks R. Reisz for photographs of MNHN MRD1 and FMNH UR 713. We are indebted to the United States Embassy and Cultural Center (Niamey) for diplomatic assistance and hospitality, and H. M. Salissou for permission to conduct research in Niger. Field work in 2003 was supported by a grant from the National Geographic Society (CRE 7258-02 to C.A.S.) with continuing research on the Permian of Niger by National Science Foundation (NSF) grant EAR-0617718 (to C.A.S.).

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