Abstract

Saturnalia tupiniquim is a sauropodomorph dinosaur from the Late Triassic (Carnian–c. 233 Ma) Santa Maria Formation of Brazil. Due to its phylogenetic position and age, it is important for studies focusing on the early evolution of both dinosaurs and sauropodomorphs. The osteology of Saturnalia has been described in a series of papers, but its cranial anatomy remains mostly unknown. Here, we describe the skull bones of one of its paratypes (only in the type-series to possess such remains) based on CT Scan data. The newly described elements allowed estimating the cranial length of Saturnalia and provide additional support for the presence of a reduced skull (i.e. two thirds of the femoral length) in this taxon, as typical of later sauropodomorphs. Skull reduction in Saturnalia could be related to an increased efficiency for predatory feeding behaviour, allowing fast movements of the head in order to secure small and elusive prey, a hypothesis also supported by data from its tooth and brain morphology. A principal co-ordinates analysis of the sauropodomorph jaw feeding apparatus shows marked shifts in morphospace occupation in different stages of the first 30 million years of their evolutionary history. One of these shifts is observed between non-plateosaurian and plateosaurian sauropodomorphs, suggesting that, despite also having an omnivorous diet, the feeding behaviour of some early Carnian sauropodomorphs, such as Saturnalia, was markedly different from that of later Triassic taxa. A second shift, between Late Triassic and Early Jurassic taxa, is congruent with a floral turnover hypothesis across the Triassic-Jurassic boundary.

Highlights

  • The first steps of sauropodomorph evolution are mainly known based on the fossil record of two South American Carnian deposits, the Santa Maria (c. 233 Ma) and the Ischigualasto (c. 231 Ma) formations of Brazil and Argentina, respectively [1,2]

  • A large foramen (‘nvf’ in Fig 1) pierces the lateral surface of the bone, but its size (= 3.6 mm long anteroposteriorly) might have been exaggerated due to poor preservation. We identify this foramen as the posterior most neurovascular foramen of the lateral surface of the maxilla, which in sauropodomorphs is typically larger than more anterior maxillary foramina [4,25,26]

  • An elliptical groove is associated with this foramen, resembling the condition seen in other sauropodomorphs

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Summary

Introduction

The first steps of sauropodomorph evolution are mainly known based on the fossil record of two South American Carnian deposits, the Santa Maria (c. 233 Ma) and the Ischigualasto (c. 231 Ma) formations of Brazil and Argentina, respectively [1,2]. The first steps of sauropodomorph evolution are mainly known based on the fossil record of two South American Carnian deposits, the Santa Maria 231 Ma) formations of Brazil and Argentina, respectively [1,2]. Council for Scientific and Technological Development (CNPq) – Science without Borders grant 246610/2012-3 to MB; Pos-Doutorado Junior grant 170867/2017-0 to MB. - São Paulo Research Foundation (FAPESP) - grant 14/03825-3 to MCL. The funders had no role in study design, data collection and analysis, decision to publish, or preparation of the manuscript

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