| Chalk of the Pays de Caux | |
|---|---|
| Stratigraphic range: Late Cretaceous, lower | |
| The Chalk of the Pays de Caux outcropping at Saint-Jouin-Bruneval | |
| Type | Geological formation |
| Sub-units | Several ammonite subunits, including: [1]
|
| Underlies | Watinoceras devonense zone |
| Overlies | Surface rav. Octeville |
| Lithology | |
| Primary | Glauconitic chalk |
| Location | |
| Coordinates | 43°22′05″N1°59′26″E / 43.3681°N 1.9906°E |
| Region | Normandy |
| Country | France |
| 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. [1]
Ammonite and fish fossils are known from this locality. [1] [2]
| Genus | Species | Location | Stratigraphic position | Material | Notes | Image |
|---|---|---|---|---|---|---|
| Abelisauridae [2] | Indeterminate | Saint-Jouin-Bruneval | C3 ( Mantelliceras dixoni zon) | An isolated tooth | May belong to Caletodraco , or a taxon that predated or scavenged it | |
| Caletodraco [2] | 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 [3] [4] | Indeterminate | Scant remains | ||||
| ?Lamniformes [2] | Indeterminate | Saint-Jouin-Bruneval | C3 (Mantelliceras dixoni zone) | A single tooth | Discovered alongside the holotype of Caletodraco | |