Here, I demonstrate that pycnodonts were polyphyodont animals, through radiographic highlights of dental gems in various states of maturation that are present in both the prearticular and the vomer of
The previous assignation of the material from La Venta are specified (Walton, 1990, 1997). * indicates the specimens selected by Walton (1990) as holotypes, *** indicates the specimens selected in thi
Neogene and Pleistocene African suids displayed convergent evolutionary trends in the third molar (M3) morphology, with increasingly elongated and higher crowns through time. While these features can
The associated preservation between dentitions and dentigerous elements is crucial for understanding diverse biological features. Notwithstanding, their fossil record in Sauropoda is relatively seldom
