Abstract

The postcranial morphology of the extremely long-necked Tanystropheus hydroides is well-known, but observations of skull morphology were previously limited due to compression of the known specimens. Here we provide a detailed description of the skull of PIMUZ T 2790, including a partial endocast and endosseous labyrinth, based on synchrotron microtomographic data, and compare its morphology to that of other early Archosauromorpha. In many features, such as the wide and flattened snout and the configuration of the temporal and palatal regions, Tanystropheus hydroides differs strongly from other early archosauromorphs. The braincase possesses a combination of derived archosaur traits, such as the presence of a laterosphenoid and the ossification of the lateral wall of the braincase, but also differs from archosauriforms in the morphology of the ventral ramus of the opisthotic, the horizontal orientation of the parabasisphenoid, and the absence of a clearly defined crista prootica. Tanystropheus hydroides was a ram-feeder that likely caught its prey through a laterally directed snapping bite. Although the cranial morphology of other archosauromorph lineages is relatively well-represented, the skulls of most tanystropheid taxa remain poorly understood due to compressed and often fragmentary specimens. The recent descriptions of the skulls of Macrocnemus bassanii and now Tanystropheus hydroides reveal a large cranial disparity in the clade, reflecting wide ecological diversity, and highlighting the importance of non-archosauriform Archosauromorpha to both terrestrial and aquatic ecosystems during the Triassic.

Highlights

  • Archosauromorpha, the lineage that includes modern crocodylians and birds, first appeared in the Permian and subsequently radiated during the Triassic into one of the dominant vertebrate groups of the terrestrial realm (Ezcurra, Scheyer & Butler, 2014; Foth et al, 2016)

  • (Specimens from the Besano Formation referred to Tanystropheus hydroides based on relative body size but lacking diagnostic cranial material are indicated by an asterisk)

  • Tanystropheus hydroides can be distinguished from other Tanystropheus species based on the following combination of characters: premaxilla lacking a postnarial process; single cusped marginal dentition; dentary tooth piercing through a foramen in the maxillaÃ; depression on the dorsal surface of the nasals; straight suture between frontals; fused parietals; conspicuously hooked dorsal quadrate head; wide and anteriorly rounded vomers with a single row of large recurved teeth along its outer marginÃ; edentulous palatine and pterygoid; dentary bearing a distinct ventral keel at its anterior endÃ; a maximum total length of over 5 m

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Summary

Introduction

Archosauromorpha, the lineage that includes modern crocodylians and birds, first appeared in the Permian and subsequently radiated during the Triassic into one of the dominant vertebrate groups of the terrestrial realm (Ezcurra, Scheyer & Butler, 2014; Foth et al, 2016). Tanystropheidae represents a ecomorphologically diverse group that includes terrestrial (e.g. Macrocnemus bassanii and Langobardisaurus pandolfii), largely aquatic (Tanytrachelos ahynis and Tanystropheus hydroides), and possibly even fully marine (Dinocephalosaurus orientalis) taxa (Liu et al, 2017; Miedema et al, 2020; Olsen, 1979; Renesto & Dalla Vecchia, 2000; Rieppel, Li & Fraser, 2008; Spiekman et al, 2020). The clade had a likely worldwide distribution and occurred between the Early and Late Triassic (De Oliveira et al, 2018, 2020; Formoso et al, 2019; Pritchard et al, 2015; Sennikov, 2011; Spiekman & Scheyer, 2019) Due to their unique morphology, diversity, distribution, and phylogenetic position, Tanystropheidae are important both in reconstructing early archosauromorph evolution and in understanding the complexity and composition of Triassic faunas. The dental morphology of Langobardisaurus pandolfii in particular is peculiar, as the premaxilla was likely edentulous and the posteriormost teeth of both the upper and lower jaw were modified into large and flat tooth plates used for crushing, representing a unique dental system among tetrapods (Renesto & Dalla Vecchia, 2000; Saller, Renesto & Dalla Vecchia, 2013)

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