Vertebrate paleobiodiversity of the Early Cretaceous (Berriasian) Angeac-Charente Lagerstätte (southwestern France): implications for continental faunal turnover at the J / K boundary Author Allain, Ronan Author Vullo, Romain Author Rozada, Lee Author Anquetin, Jérémy Author Bourgeais, Renaud Author Goedert, Jean Author Lasseron, Maxime Author Martin, Jeremy E. Author Pérez-García, Adán Author Fabrègues, Claire Peyre De Author Royo-Torres, Rafael Author Augier, Dominique Author Bailly, Gilles text Geodiversitas 2022 2022-07-21 44 25 683 752 journal article 107849 10.5252/geodiversitas2022v44a25 d0184974-bea3-4f97-a2f8-98887ec4f87e 1638-9395 6902033 urn:lsid:zoobank.org:pub:EA12DCB7-A5BE-4763-B805-25087EBD726D Bernissartiidae indet. ( Figs 17E ; 19 A-C) DESCRIPTION Several mesiodistally elongate, bulbous and low-crowned isolated teeth have been recovered at Angeac-Charente ( Figs 17E ; 19 A-C) and their morphology is reminiscent of the tribodont condition described for the small neosuchian Bernissartia ( Buffetaut & Ford 1979 ; Martin et al. 2020 ). An incomplete left jugal (ANG15R-1205) is inflated on its lateral surface and might also belong to a bernissartiid. A small osteoderm (ANG16- 4907) also resemble the dorsal row of osteoderms figured by Buffetaut (1975) in Bernissartia fagesii . Here, the specimen is slightly wider than long although it is not as rectangular as in Bernissartia fagesii . A double-keel runs on its dorsal surface and an anterolateral process is present. The recently described bernissartiid Koumpiodontosuchus aprosdokiti ( Sweetman et al. 2015 ) also shares tribodont teeth with Bernissartia fagesii and, for this reason, we cannot yet ascertain a generic or specific attribution for the Angeac-Charente material.