The Marnes d’Auzas Formation (Auzas Marls Formation) is a geological Formation in southwestern France (departments of Ariège and Haute-Garonne) whose strata date back to the Late Maastrichtian.[1] It is about 100 metres thick and consists primarily of marls with some interbeds of sandstones.[1] It corresponds to sediments whose depositional environment evolved from the paralic domain (coastal lagoons, tidal marsh, tidal muddy channel) at the base of the formation, towards a more continental domain (alluvial plain, fluvialchannels) in its upper part.[1] The Marnes d’Auzas Formation was deposited in the west coast of the former Ibero-Armorican Island, which included much of France and Spain.[2]
Vertebrate paleofauna
Theropods:
Theropoda indet. (a medium-sized form only known by a tooth)[1]
^ abcdefghijklmnopqrstuvwxyzaaabLaurent, Y. (2003). "Les faunes de vertébrés continentaux du Maastrichtien supérieur d'Europe : systématique et biodiversité". Strata (41): 1–81.
^Garcia, G.; Amicot, S.; Fournier, F.; Thouand, E.; Valentin, X. (2010). "A new Titanosaur genus (Dinosauria, Sauropoda) from the Late Cretaceous of southern France and its paleobiogeographic implications". Bulletin de la Société Géologique de France. 181 (3): 269–277. doi:10.2113/gssgfbull.181.3.269.
^Pérez-García, A.; Ortega, F.; Murelaga, X. (2012). "A new genus of Bothremydidae (Chelonii, Pleurodira) in the Cretaceous of southwestern Europe". Geobios. 45 (2): 219–229. doi:10.1016/j.geobios.2011.03.001.
^Laurent, Y.; Buffetaut, E.; Le Loeuff, J. (2000). "Un crâne de Thoracosaurine (Crocodylia, Crocodylidae) dans le Maastrichtien supérieur du sud de la France". Oryctos (3): 19–27.