| Chalk of the Pays de Caux | |
| Caption: | The Chalk of the Pays de Caux outcropping at Saint-Jouin-Bruneval |
| Type: | Geological formation |
| Period: | Cenomanian |
| Age: | Late Cretaceous, lower |
| Prilithology: | Glauconitic chalk |
| Region: | Normandy |
| Country: | France |
| Coordinates: | 43.3681°N 1.9906°W |
| Subunits: | Several ammonite subunits, including:[1]
|
| Underlies: | Watinoceras devonense zone |
| Overlies: | Surface rav. Octeville |
| Extent: | Pays de Caux |
The Chalk of the Pays de Caux is a geologic locality dating to the Late Cretaceous (lower Cenomanian age), outcropping in the Pays de Caux region of France.[2] Dinosaur and reptile fossils are among the known remains found in the Chalk of the Pays de Caux.
Ammonite and fish fossils are known from this locality.
| Abelisauridae | Indeterminate | Saint-Jouin-Bruneval | C3 (Mantelliceras dixoni zon) | An isolated tooth | May belong to Caletodraco, or a taxon that predated or scavenged it | ||
| Caletodraco | C. cottardi | Saint-Jouin-Bruneval | C3 (Mantelliceras dixoni zone) | The sacrum, partial ilia, the first caudal vertebra, and various fragmentary bones, possibly ribs | |||
| Crocodilia[3] [4] | Indeterminate | Scant remains | |||||
| Ichthyosauria | Indeterminate | Scant remains | |||||
| ?Lamniformes | Indeterminate | Saint-Jouin-Bruneval | C3 (Mantelliceras dixoni zone) | A single tooth | Discovered alongside the holotype of Caletodraco |