Marnes d'Auzas Formation

Marnes d’Auzas Formation
Stratigraphic range: Late Cretaceous (Late Maastrichtian)
~
TypeGeological formation
UnderliesAurignac Formation
OverliesJadet Calcarenites Formation
ThicknessAbout 100 m
Lithology
PrimaryMarls
OtherSandstones
Location
Coordinates43°25′N 1°30′E
RegionEurope
CountryFrance
Marnes d'Auzas Formation (France)

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, fluvial channels) 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

See also

References

  1. ^ a b c d e f g h i j k l m n o p q r s t u v w x y z aa ab Laurent, Y. (2003). "Les faunes de vertébrés continentaux du Maastrichtien supérieur d'Europe : systématique et biodiversité". Strata (41): 1–81.
  2. ^ Csiki-Sava, Z.; Buffetaut, E.; Ősi, A.; Pereda-Suberbiola, X.; Brusatte, S.L. (2015). "Island life in the Cretaceous-faunal composition, biostratigraphy, evolution, and extinction of land-living vertebrates on the Late Cretaceous European archipelago". ZooKeys (469): 1–161. doi:10.3897/zookeys.469.8439. PMC 4296572. PMID 25610343.
  3. ^ a b c d Prieto-Márquez, A.; Dalla Vecchia, F.M.; Gaete, R.; Galobart, À. (2013). "Diversity, Relationships, and Biogeography of the Lambeosaurine Dinosaurs from the European Archipelago, with Description of the New Aralosaurin Canardia garonnensis". PLOS ONE. 8 (7): e69835. Bibcode:2013PLoSO...869835P. doi:10.1371/journal.pone.0069835. PMC 3724916. PMID 23922815.
  4. ^ a b c d e f g h i j k l m Laurent, Y.; Bilotte, M.; Le Loeuff, J. (2002). "Late Maastrichtian continental vertebrates from southwestern France: correlation with marine fauna" (PDF). Palaeogeography, Palaeoclimatology, Palaeoecology. 187 (1–2): 121–135. Bibcode:2002PPP...187..121L. doi:10.1016/S0031-0182(02)00512-6.
  5. ^ 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.
  6. ^ Buffetaut, E.; Laurent, Y.; Le Loeuff, J.; Bilotte, M. (1997). "A terminal Cretaceous giant pterosaur from the French Pyrenees". Geological Magazine. 134 (4): 553–556. Bibcode:1997GeoM..134..553B. doi:10.1017/S0016756897007449. S2CID 140631899.
  7. ^ 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.
  8. ^ Garcia, G.; Bardet, N.; Houssaye, A.; Pereda-Suberbiola, X.; Valentin, X. (2015). "Mosasauroid (Squamata) discovery in the Late Cretaceous (Early Campanian) continental deposits of Villeveyrac-L'Olivet, Southern France – Découverte de Mosasauroidea (Squamata) dans le Crétacé supérieur (Campanien inférieur) continental de Villeveyrac – L'Olivet, sud de la France". Comptes Rendus Palevol. 14 (6–7): 495–505. doi:10.1016/j.crpv.2015.05.002.
  9. ^ 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.
  10. ^ Brochu, C.A. (2004). "A new Late Cretaceous gavialoid crocodylian from eastern North America and the phylogenetic relationships of Thoracosaurs" (PDF). Journal of Vertebrate Paleontology. 24 (3): 610–633. doi:10.1671/0272-4634(2004)024[0610:ANLCGC]2.0.CO;2. S2CID 131176447.