Abstract
Appendicular remains of squamate reptiles are barely described in the fossil record due to their low preservational potential and generally poor diagnostic information. Not many squamate fossil individuals preserve appendicular bony elements, these being mainly restricted to the rare articulated specimens found in a limited number of localities with specific conditions that favor exceptional preservation. Detailed descriptions of these bones, especially tarsals and metatarsals, are thus scarce in the literature due to the lesser relevance given to these elements in most anatomical descriptions. In this study we analyze an unpublished fossil specimen from the Maastrichtian of Basturs-1 (Lleida, Catalonia, Spain) corresponding to several articulated appendicular pes bones of a possible member of Varaniformes. We also provide detailed insights on the anatomy of the tarsalia and metatarsalia, particularly in anguimorphs. The fossil specimen here described, with an estimated snout-vent length (SVL) of ∼581 mm, reveals the putative varaniform from Basturs-1 as one of the largest Mesozoic terrestrial lizards, and possibly the largest from the European fossil record. Previous observations of an association between large lizards and dinosaur nesting sites are further supported by the find of this giant form in a locality known for the presence of numerous dinosaur eggs.
| Original language | English |
|---|---|
| Article number | 105094 |
| Journal | Cretaceous Research |
| Volume | 131 |
| Early online date | 17 Nov 2021 |
| DOIs | |
| Publication status | Published - Mar 2022 |
Bibliographical note
Funding Information:This research has been funded by the Ministerio de Ciencia e Innovación of the Spanish Government ( PID2019-111488RB-I00 ). A.B. work is supported by a Juan de la Cierva Incorporación Fellowship (IJC2018-037685-I, funded by Ministerio de Ciencia e Innovación of the Spanish Government). A.T. is supported by La Rioja Government by “Convenio para la financiación de actividades de la Cátedra Extraordinaria de Patrimonio Paleontológico” in the Universidad de La Rioja . Support from the CERCA programme (ICP) from the Generalitat de Catalunya is acknowledged. Authors thank M. Padilla (MACV), M. Calvo (MNCN), M. A. Brown, K. Bader (University of Texas at Austin) and S. Bailón (MNHN) for providing access to material and measures. M. Martín-Jiménez and A. Serrano (UNED) for their collaboration to obtain the 3D model; and, especially, to the late Nieves López Martínez (UCM), who encouraged us to carry out the study of the Basturs-1 specimen. The authors also thank the editor E. Koutsoukos and two anonymous reviewers for their useful and constructive comments.
Funding Information:
This research has been funded by the Ministerio de Ciencia e Innovación of the Spanish Government (PID2019-111488RB-I00). A.B. work is supported by a Juan de la Cierva Incorporación Fellowship (IJC2018-037685-I, funded by Ministerio de Ciencia e Innovación of the Spanish Government). A.T. is supported by La Rioja Government by “Convenio para la financiación de actividades de la Cátedra Extraordinaria de Patrimonio Paleontológico” in the Universidad de La Rioja. Support from the CERCA programme (ICP) from the Generalitat de Catalunya is acknowledged. Authors thank M. Padilla (MACV), M. Calvo (MNCN), M. A. Brown, K. Bader (University of Texas at Austin) and S. Bailón (MNHN) for providing access to material and measures. M. Martín-Jiménez and A. Serrano (UNED) for their collaboration to obtain the 3D model; and, especially, to the late Nieves López Martínez (UCM), who encouraged us to carry out the study of the Basturs-1 specimen. The authors also thank the editor E. Koutsoukos and two anonymous reviewers for their useful and constructive comments.
Publisher Copyright:
© 2021 Elsevier Ltd