The Arcillas de Morella Formation is a geological formation in Spain whose strata date back to the Barremian stage of the Early Cretaceous.[1] Dinosaur remains are among the fossils that have been recovered from the formation.[2]
Geology
The formation was formally named and defined by Canérot and colleagues in 1982.[3] The formation predominantly consists of red clays and continental sandstones, with some marine intercalations.[4]
^ abcdWeishampel, David B; et al. (2004). "Dinosaur distribution (Early Cretaceous, Europe)." In: Weishampel, David B.; Dodson, Peter; and Osmólska, Halszka (eds.): The Dinosauria, 2nd, Berkeley: University of California Press. Pp. 562. ISBN0-520-24209-2.
^ abElisabete Malafaia; José Miguel Gasulla; Fernando Escaso; Iván Narváez; José Luis Sanz; Francisco Ortega (2019). "A new spinosaurid theropod (Dinosauria: Megalosauroidea) from the late Barremian of Vallibona, Spain: Implications for spinosaurid diversity in the Early Cretaceous of the Iberian Peninsula". Cretaceous Research. in press: 104221. doi:10.1016/j.cretres.2019.104221.
^Mocho, Pedro; Escaso, Fernando; Gasulla, José M; Galobart, Àngel; Poza, Begoña; Santos-Cubedo, Andrés; Sanz, José L; Ortega, Francisco (2023-09-28). "New sauropod dinosaur from the Lower Cretaceous of Morella (Spain) provides new insights on the evolutionary history of Iberian somphospondylan titanosauriforms". Zoological Journal of the Linnean Society. 201: 214–268. doi:10.1093/zoolinnean/zlad124. ISSN0024-4082.
^Mocho, P.; Pérez-García, A.; Gasulla, J. M.; Ortega, F. (2017-06-01). "High sauropod diversity in the upper Barremian Arcillas de Morella Formation (Maestrat Basin, Spain) revealed by a systematic review of historical material". Journal of Iberian Geology. 43 (2): 111–128. Bibcode:2017JIbG...43..111M. doi:10.1007/s41513-017-0012-8. ISSN1886-7995. S2CID134844724.