Villalba de la Sierra Formation
The Villalba de la Sierra Formation is a Campanian to Maastrichtian geologic formation in Spain . Fossil dinosaur eggs have been reported from the formation, that comprises gypsiferous , grey, argillaceous mudstones and sandstones , deposited in a floodplain environment [ 1] [ 2] characterised by high seasonality and variability in water availability.[ 3]
Fossil content
Color key
Notes Uncertain or tentative taxa are in small text ; crossed out taxa are discredited.
Dinosaur
Sauropods
Theropods
Reptiles
Crocodiles
Turtles
See also
References
^ Lo Hueco, Fuentes (G1) at Fossilworks .org
^ Weishampel et al., 2004, pp.517-607
^ Peyrot, Daniel; Barroso-Barcenilla, Fernando; Cambra-Moo, Oscar (1 October 2013). "Paleoecology of the late Campanian/early Maastrichtian Fossil-Lagerstätte of "Lo Hueco" (Cuenca, Spain): Palynological insights" . Palaeogeography, Palaeoclimatology, Palaeoecology . 387 : 27– 39. Bibcode :2013PPP...387...27P . doi :10.1016/j.palaeo.2013.07.005 . Retrieved 22 November 2022 .
^ V. Díez Díaz; P. Mocho; A. Páramo; F. Escaso; F. Marcos-Fernández; J.L. Sanz; F. Ortega (2016). "A new titanosaur (Dinosauria, Sauropoda) from the Upper Cretaceous of Lo Hueco (Cuenca, Spain)". Cretaceous Research . 68 : 49– 60. Bibcode :2016CrRes..68...49D . doi :10.1016/j.cretres.2016.08.001 .
^ Mocho, P.; Escaso, F.; Marcos-Fernández, F.; Páramo, A.; Sanz, J. L.; Vidal, D.; Ortega, F. (2024). "A Spanish saltasauroid titanosaur reveals Europe as a melting pot of endemic and immigrant sauropods in the Late Cretaceous". Communications Biology. 7. 1016. doi:10.1038/s42003-024-06653-0. PMC 11375222. PMID 39232208.
^ Malafaia, E.; Escaso, F.; Coria, R. A.; Pérez-García, A.; Ortega, F. (2024). "Theropod teeth from the Upper Cretaceous of central Spain: assessing the paleobiogeographic history of European abelisaurids" . Cretaceous Research . 106072. doi :10.1016/j.cretres.2024.106072 .
^ I. Narváez; C.A. Brochu; F. Escaso; A. Pérez-García; F. Ortega (2016). "New Spanish Late Cretaceous eusuchian reveals the synchronic and sympatric presence of two allodaposuchids" . Cretaceous Research . 65 : 112– 125. Bibcode :2016CrRes..65..112N . doi :10.1016/j.cretres.2016.04.018 .
^ Iván Narváez; Christopher A. Brochu; Fernando Escaso; Adán Pérez-García; Francisco Ortega (2015). "New Crocodyliforms from Southwestern Europe and Definition of a Diverse Clade of European Late Cretaceous Basal Eusuchians" . PLOS ONE . 10 (11): e0140679. Bibcode :2015PLoSO..1040679N . doi :10.1371/journal.pone.0140679 . PMC 4633049 . PMID 26535893 .
^ Tong, Haiyan; Eugene S Gaffney; Eric Buffetaut (1998). "Foxemys , a new side-necked turtle (Bothremydidae, Pelomedusoides) from the late Cretaceous of France" . American Museum Novitates (3251): 1– 19. hdl :2246/3157 . Retrieved 19 January 2012 .
^ Adán Pérez-García; Francisco Ortega; Xabier Murelaga (2012). "A new genus of Bothremydidae (Chelonii, Pleurodira) in the Cretaceous of Southwestern Europe". Geobios . 45 (2): 219– 229. Bibcode :2012Geobi..45..219P . doi :10.1016/j.geobios.2011.03.001 .
Bibliography
Díez Díaz, V.; Mocho, P.; Páramo, A.; Escaso, F.; Marcos-Fernández, F.; Sanz, J.L.; Ortega, F. (2016). "A new titanosaur (Dinosauria, Sauropoda) from the Upper Cretaceous of Lo Hueco (Cuenca, Spain)". Cretaceous Research . 68 : 49– 60. Bibcode :2016CrRes..68...49D . doi :10.1016/j.cretres.2016.08.001 .
Ortega, F.; Bardet, N.; Barroso-Barcenilla, F.; Callapez, P.M.; Cambra-Moo, O.; Daviero- Gómez, V.; Díez Díaz, V.; Domingo, L.; Elvira, A.; Escaso, F.; García-Oliva, M.; Gómez, B.; Houssaye, A.; Knoll, F.; Marcos-Fernández, F.; Martín, M.; Mocho, P.; Narváez, I.; Pérez- García, A.; Peyrot, D.; Segura, M.; Serrano, H.; Torices, A.; Vidal, D.; Sanz, J.L. (2015). "The biota of the Upper Cretaceous site of "Lo Hueco" (Cuenca, Spain)" . Journal of Iberian Geology . 41 (1). doi :10.5209/rev_JIGE.2015.v41.n1.48657 . hdl :10486/675918 .
Weishampel , David B.; Dodson , Peter; Osmólska , Halszka, eds. (2004). The Dinosauria (2nd ed.). Berkeley: University of California Press. pp. 1– 880. ISBN 0-520-24209-2 . Retrieved 2019-02-21 .