Abstract

Mesosaurs are basal amniotes that lived at the beginning of the Permian or close to the Permo–Carboniferous boundary. Despite the several hundred specimens that have been found, including complete skeletons of adult and juvenile individuals, mesosaur taxonomy has been subjected to a high controversy over time. Currently, three monotypic genera, Mesosaurus tenuidens Gervais, Stereosternum tumidum Cope, and Brazilosaurus sanpauloensis Shikama & Ozaki are recognized, but identification of new specimens using the available diagnostic characters are arbitrary and influenced by high subjectivity. We performed anatomical and morphometric analyses to look for statistical support to these previously suggested basic diagnostic characters through an exhaustive anatomical revision of these characters and also of some new attributes discovered during the course of our study. We found a notable influence of taphonomic features in most of the diagnostic characters used to differentiate the three monotypic genera, including strong bias derived from the preservation of individuals in different ontogenetic stages, whose size and degree of ossification could have been controlled by particular environmental conditions that resulted in subtle polymorphisms of these and other few characters. Other features may even represent sexual dimorphism. After the detailed revision of the type specimens of the three currently accepted mesosaur taxa, for which we include here good-quality photographs, and considering the lack of statistical support for the most applied putative diagnostic features such as the different ratio found when comparing skull and cervical region lengths and the low or higher intensity of pachyosteosclerosis observed in dorsal ribs, which can be controlled by taphonomic and ecological conditions, we recognize Mesosaurus as the only mesosaurid taxon in the Paraná and Karoo basins, probably including dwarf individuals. Therefore, S.tumidum and B. sanpauloensis are suggested here as nomina dubia taking into account that the autapomorphies that supported these taxa cannot be confirmed to be absent in Mesosaurus. Keywords: Mesosaurus, morphometrics, taxonomy, ?Early Permian, Gondwana.

Highlights

  • Mesosaurs are basal amniotes believed to be the first group that returned to the aquatic environment (Carroll, 1988), recent studies suggest that they could have been semiaquatic and capable of being active on land (Núñez Demarco et al, 2018)

  • Mesosaurs are represented by thousands of specimens including almost complete skeletons, their taxonomic composition of three monotypic taxa, Mesosaurus tenuidens Gervais, 1865, Stereosternum tumidum Cope, 1885a and Brazilosaurus sanpauloensis Shikama & Ozaki, 1966 was subjected to debate (e.g. Piñeiro, 2002, 2004, 2006; Piñeiro et al, 2012b)

  • The aim of this paper is to present an overview of the main diagnostic characters previously used to identify mesosaur species, specially focusing on finding a stronger characterization for Brazilosaurus sanpauloensis through a detailed anatomical, taphonomic and comparative morphometric study of more than three hundred of mesosaur specimens belonging to collections of Uruguay, Brazil, Germany, Japan, USA, Switzerland, South Africa, Namibia, United Kingdom and France

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Summary

Introduction

Mesosaurs are basal amniotes believed to be the first group that returned to the aquatic environment (Carroll, 1988), recent studies suggest that they could have been semiaquatic and capable of being active on land (Núñez Demarco et al, 2018). Because of their short time range and restricted geographic distribution, mesosaurs were considered good stratigraphic fossils for the Early Permian of Gondwana Their basal position in recent phylogenetic studies (Laurin & Piñeiro, 2017, 2018; MacDougall et al, 2018) and the fact that they are part of a community in which pygocephalomorph crustaceans, insects and plants suggest a Late Carboniferous or a transitional Permo-Carboniferous age for the strata (see Huene, 1940; Calisto & Piñeiro, 2019), mesosaurs could have a ghost lineage that lead their origin to at least Late Carboniferous (Piñeiro et al, 2012a). The major concerns are the poor definition and difficult identification of the diagnostic characters for each genus, even in the almost complete individuals This issue complicates the taxonomic assignment of the numerous articulated but fragmentary specimens available, which represent valuable evidence for reconstructing biological trends in mesosaurs and the influence of depositional environments

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