The Densuș-Ciula Formation is a geological formation in Romania whose strata date back to the

Late Cretaceous The Late Cretaceous (100.5–66 Ma) is the more recent of two epochs into which the Cretaceous Period is divided in the geologic time scale. Rock strata from this epoch form the Upper Cretaceous Series. The Cretaceous is named after ''cre ...

. It forms part of the

Hațeg Island Hațeg Island was a large offshore Former island, island in the Tethys Sea which existed during the Late Cretaceous period, probably from the Cenomanian to the Maastrichtian ages. It was situated in an area corresponding to the region around moder ...

assemblage. Dinosaur remains are among the fossils that have been recovered from the formation.Weishampel, 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. . It is divided up into three members, the lower member is noted for high content of volcanogenic material and is poorly fossiliferous. While the Middle member consists of silty mudstones, sandstones and conglomerates containing volcanogenic clasts and is richly fossiliferous, while the upper member consists of matrix supported red conglomerates and is poorly fossiliferous.

Fossil content

Indeterminate dromaeosaurid and possible indeterminate troodontid remains present in Județul Hunedoara, Romania. An unnamed theropod is also present.

Amphibians

Squamates

Turtles

Crocodyliformes

Dinosaurs

Pterosaurs

Mammals

References

Geologic formations of Romania Upper Cretaceous Series of Europe Maastrichtian Stage Mudstone formations Sandstone formations Conglomerate formations {{paleo-site-stub