Abstract

The endemic dormouse Leithia melitensis from the Pleistocene of Sicily is considered an insular giant, whose body size is exceptionally large in comparison to that of any extant dormouse species. However, knowledge of the skull morphology of this giant glirid species is limited as cranial material is rare and mostly fragmentary. A fossil conglomerate representing a cave floor segment from Poggio Schinaldo, Sicily, presented an exceptional opportunity to reconstruct the cranium of Leithia melitensis. Following microCT scanning, five partial crania were digitally extracted from the conglomerate. A composite skull of the partial crania was then reconstructed with the use of merging and warping techniques, resulting in the best approximation to the complete skull morphology of this species thus far. All major structures except for the nasal bone are present in the composite model, indicating very robust morphology, especially in the zygomatic area and the pterygoid flange. This model could potentially be very important for our understanding of the morphology and ecology of this gigantic dormouse, as well as for providing valuable data for understanding the phenomenon of insular gigantism more generally.

Highlights

  • The Late to Middle Pleistocene faunas on Sicily are characterised by the presence of endemic animals such as the dwarf elephants Palaeoloxodon falconeri and P. (E.) mnaidriensis, resulting in eponymous Faunal Complexes (Accordi & Colacicchi, 1962; Accordi, 1963; Bonfiglio, Marra & Masini, 2000; Bonfiglio et al, 2002; Burgio et al, 2002)

  • The aim of this study was to evaluate the cranial morphology of Leithia melitensis by creating a composite digital model from a number of partial crania present within the conglomerate

  • Comparative dental characteristics of Leithia melitensis Dental characteristics for the crania within the slab are best preserved in the right molar row of Skull 5

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Summary

Introduction

The Late to Middle Pleistocene faunas on Sicily are characterised by the presence of endemic animals such as the dwarf elephants Palaeoloxodon (alternatively: Elephas) falconeri and P. (E.) mnaidriensis, resulting in eponymous Faunal Complexes (Accordi & Colacicchi, 1962; Accordi, 1963; Bonfiglio, Marra & Masini, 2000; Bonfiglio et al, 2002; Burgio et al, 2002). (E.) mnaidriensis, resulting in eponymous Faunal Complexes (Accordi & Colacicchi, 1962; Accordi, 1963; Bonfiglio, Marra & Masini, 2000; Bonfiglio et al, 2002; Burgio et al, 2002) During this time, the dwarf elephants were accompanied by the presence of the endemic dormouse genera Maltamys and Leithia (Adams, 1863). Geological Setting Poggio Schinaldo is a small, low-ceilinged cave approximately 15 m in diameter, located south of the town of Terrasini in northwest Sicily (Esu, Kotsakis & Burgio, 1986) (Figure 1A) It was discovered during the construction of the Palermo-Mazara del Vallo motorway in 1976, and a rescue excavation was carried out before the entrance was resealed. Excavated segments of the cave floor are currently on display at Museo Geologico Gemmellaro, Palermo

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