| 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″N 1°59′26″E / 43.3681°N 1.9906°E |
| Region | Normandy |
| Country | France |
| Extent | Pays de Caux |
  Chalk of the Pays de Caux (France) | |
The Chalk of the Paus 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]
- ^ a b Hoyez, B.; Girard, J.; Cottard, N. Le (2020) Cénomanien du littoral normand entre la valleuse d’Antifer et le cap de la Hève; Carnets Géol.: Madrid, Spain; 225p, ISBN 13: 978-2-916733-19-7, Book 2020/01 (CG2020_B01).
- ^ Buffetaut, E.; Tong, H.; Girard, J.; Hoyez, B.; Párraga, J. (2024). "Caletodraco cottardi: A New Furileusaurian Abelisaurid (Dinosauria: Theropoda) from the Cenomanian Chalk of Normandy (North-Western France)". Fossil Studies. 2 (3): 177–195. doi:10.3390/fossils2030009.