The Densuș-Ciula Formation is a geological formation in Romania, with strata dating to the Late Cretaceous. It forms part of the Hațeg Island assemblage, with dinosaur remains among the fossils recovered from the formation.[1]
The formation is divided into three members. The lower member contains a high proportion of volcanogenic material and is poorly fossiliferous. The middle member consists of silty mudstones, sandstones, and conglomerates containing volcanogenic clasts, and is richly fossiliferous. The upper member is composed of matrix-supported red conglomerates and contains few fossils.[2]
Fossil content
Indeterminate dromaeosaurid and possible indeterminate troodontid remains present in Județul Hunedoara, Romania.[1] An unnamed theropod is also present.[1]
A partial skeleton of a juvenile individual and a left dentary
Originally “Zalmoxes” shqiperorum but subsequently recognized as a distinct ceratopsian taxon closely related to Ajkaceratops. Only the pelvic material has been referred to Ferenceratops as of the taxon’s description in 2026.
^ abcdWeishampel, David B; et al. (2004). “Dinosaur distribution (Late Cretaceous, Europe).” In: Weishampel, David B.; Dodson, Peter; and Osmólska, Halszka (eds.): The Dinosauria, 2nd, Berkeley: University of California Press. Pp. 588-593. ISBN 0-520-24209-2.
^VASILE, ŞTEFAN; CSIKI, ZOLTÁN; GRIGORESCU, DAN (2011). “Reassessment of the Spatial Extent of the Middle Member, Densuş-Ciula Formation (Maastrichtian), Haţeg Basin, Romania”. Acta Palaeontologica Romaniae: 335–342.
^Magyar, J.; Ősi, A.; Csiki-Sava, Z.; Budai, S.; Botfalvai, G. (2026). “New early Maastrichtian ‘duck-billed’ dinosaur from Hațeg Basin (Densuș-Ciula Formation, Romania) documents an endemic clade of non-hadrosaurid hadrosauroids in the south-eastern Late Cretaceous European Archipelago”. Journal of Systematic Palaeontology. 24 2607800. doi:10.1080/14772019.2025.2607800.
^ abBuffetaut, E., Grigorescu, D., and Csiki, Z. (2002). “A new giant pterosaur with a robust skull from the latest Cretaceous of Romania.” Naturwissenschaften, 89(4): 180-184. Abstract