Vertebrate paleobiodiversity of the Early Cretaceous (Berriasian) Angeac-Charente Lagerstätte (southwestern France): implications for continental faunal turnover at the J/K boundary
DOKPE
Allain, RonanMuséum national d'Histoire naturelle, Centre de Recherche en Paléontologie – Paris (CR2P), CNRS/MNHN/Sorbonne Université, CP 38, 57 rue Cuvier, F-75231 Paris cedex 05 (France)
Vullo, RomainUniv Rennes, Géosciences, CNRS UMR 6118, Campus de Beaulieu, bât. 15, 263 avenue du Général Leclerc, F-35042 Rennes cedex (France)
Rozada, LeeMuséum national d'Histoire naturelle, Centre de Recherche en Paléontologie – Paris (CR2P), CNRS/MNHN/Sorbonne Université, CP 38, 57 rue Cuvier, F-75231 Paris cedex 05 (France)
Anquetin, JérémyJurassica Museum, Route de Fontenais 21, 2900 Porrentruy, Switzerland Département des Géosciences, Université de Fribourg, Chemin du Musée 6, 1700 Fribourg (Switzerland)
Bourgeais, RenaudRésidence du Clos des Ormes, F-91820 Vayres-sur-Essonne (France)
Goedert, JeanUniversité de Bordeaux, De la préhistoire à l'actuel: culture, environnement et anthropologie, UMR 5199, Bâtiment B8, Allée Geoffroy Saint Hilaire, CS 50023 F-33615 Pessac cedex (France)
Lasseron, MaximeMuséum national d'Histoire naturelle, Centre de Recherche en Paléontologie – Paris (CR2P), CNRS/MNHN/Sorbonne Université, CP 38, 57 rue Cuvier, F-75231 Paris cedex 05 (France)
Pérez-García, AdánGrupo de Biología Evolutiva, Facultad de Ciencias, UNED, Paseo Senda del Rey 9, 28040 Madrid (Spain)
De Fabrègues, Claire PeyreCentre for Vertebrate Evolutionary Biology, Institute of Palaeontology, Yunnan University, Kunming, 650091 (China)
Royo-Torres, RafaelFundación Conjunto Paleontológico de Teruel-Dinópolis, 44002 Teruel (Spain)
Augier, DominiqueMusée d'Angoulême, 1 rue Friedland, F-16000 Angoulême (France)
Bailly, GillesMusée d'Angoulême, 1 rue Friedland, F-16000 Angoulême (France)
Cazes, LilianMuséum national d'Histoire naturelle, Centre de Recherche en Paléontologie – Paris (CR2P), CNRS/MNHN/Sorbonne Université, CP 38, 57 rue Cuvier, F-75231 Paris cedex 05 (France)
Despres, YohanMuséum national d'Histoire naturelle, Centre de Recherche en Paléontologie – Paris (CR2P), CNRS/MNHN/Sorbonne Université, CP 38, 57 rue Cuvier, F-75231 Paris cedex 05 (France)
Gailliègue, AurélianeInstitut des Sciences du Calcul et des Données (ISCD/MNHN/LJLL) 4, place Jussieu – F-75005 Paris (France)
Gomez, BernardCNRS-UMR 5276 Terre, Planètes, Environnement, Université Lyon 1, 2, rue Raphaël Dubois, F-69622 Villeurbanne, France
Goussard, FlorentMuséum national d'Histoire naturelle, Centre de Recherche en Paléontologie – Paris (CR2P), CNRS/MNHN/Sorbonne Université, CP 38, 57 rue Cuvier, F-75231 Paris cedex 05 (France)
Lenglet, Thierry76 rue de la République, F-17150 Mirambeau (France)
Vacant, RenaudMuséum national d'Histoire naturelle, Centre de Recherche en Paléontologie – Paris (CR2P), CNRS/MNHN/Sorbonne Université, CP 38, 57 rue Cuvier, F-75231 Paris cedex 05 (France)
Mazan, .Rue du Bourg, F-16290 Champmillon (France)
English
This contribution describes the continental micro- and macrovertebrate fauna of Angeac-Charente (Berriasian, Early Cretaceous). The rich and diversified fauna includes at least 38 different vertebrate taxa from all major clades, and is represented by more than 50 000 specimens. The Angeac-Charente locality includes the most diverse earliest Cretaceous mixed continental bonebed and the only Lagerstätte known to date in the World, and it provides a good picture of a Purbeckian paleocommunity. It includes remarkable taxa such as a new ornithomimosaur, a large turiasaur, an helochelydrid turtle and numerous mammals. The vertebrate fauna of Angeac-Charente has beyond all a Purberckian character. Many exclusively European genera and species belong to families with an essentially Laurasian paleogeographic distribution. Some taxa nevertheless suggest dispersal events between Africa and Europe at the Jurassic/Cretaceous transition. The successive Charentese faunas of Chassiron (Tithonian), Cherves-de-Cognac (Berriasian) and Angeac-Charente improve our poor knowledge of the evolution of continental vertebrate faunas at the Jurassic/Cretaceous transition. Rather than reflecting an important faunal turnover between the Tithonian and the Berriasian, they record environmental changes related to the sea–level regression that characterizes the end of the Jurassic.