Bauxite of Cornet

Bauxite of Cornet Stratigraphic range: Early Cretaceous
Type	Geological formation
Location
Country	Romania

The Bauxite of Cornet is a geological formation in Romania whose strata date back to the Early Cretaceous. Dinosaur remains are among the fossils that have been recovered from the formation.^[1]

Vertebrate paleofauna

Dinosaurs

Color key Taxon Reclassified taxon Taxon falsely reported as present Dubious taxon or junior synonym Ichnotaxon Ootaxon Morphotaxon		Notes Uncertain or tentative taxa are in small text; crossed out taxa are discredited.

Dinosaurs of the Bauxite of Cornet
Genus	Species	Location	Member	Abundance	Notes	Images
Archaeopteryx[2]	Indeterminate[2]	Judetul Bihor[2]			Possible indeterminate avialan remains.[2]	Hypsilophodon. Valdosaurus femur.
Aristosuchus[2]	Indeterminate[2]	Judetul Bihor[2]			Indeterminate theropod remains.[2]
Dryosaurus[2]	Indeterminate[2]	Judetul Bihor[2]
Eurolimnornis[2]	E. corneti[2]	Judetul Bihor[2]
Hypsilophodon[2]	Indeterminate[2]	Judetul Bihor[2]
Iguanodon[2]	I. mantelli[2]	Judetul Bihor[2]			The "I. mantelli" remains are referable to Iguanodon, but not diagnostic to the species level.[2]
Palaeocursornis[2]	P. corneti[2]	Judetul Bihor[2]
Thescelosaurus[3]	Indeterminate[3]	Judetul Bihor[2]
Valdosaurus[2]	V. canaliculatus[2]	Judetul Bihor[2]

See also

• List of dinosaur-bearing rock formations

Footnotes

1. Weishampel, 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. ISBN 0-520-24209-2.
2. "29.1 Judetul Bihor, Romania; 1. Bauxite of Cornet," in Weishampel, et al. (2004). Page 562.
3. Listed as "cf. Thescelosaurus sp." in "29.1 Judetul Bihor, Romania; 1. Bauxite of Cornet," in Weishampel, et al. (2004). Page 562.

References

• Weishampel, David B.; Dodson, Peter; and Osmólska, Halszka (eds.): The Dinosauria, 2nd, Berkeley: University of California Press. 861 pp. ISBN 0-520-24209-2.