Chalk of the Pays de Caux | |
---|---|
Stratigraphic range: Late Cretaceous, lower | |
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 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]
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 |
Seine-Maritime is a department of France in the Normandy region of northern France. It is situated on the northern coast of France, at the mouth of the Seine, and includes the cities of Rouen and Le Havre. Until 1955 it was named Seine-Inférieure. It had a population of 1,255,633 in 2019.
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