Other Charente fossil sites

Charente and its neighbours: comparing fossil sites

Nearby sites, different records

The region’s fossil sites record different times and environments. Champblanc, at Cherves-Richemont in Charente, and Chassiron, on the Île d’Oléron in Charente-Maritime, provide essential comparisons for understanding Angeac.

These regional fossil sites preserve faunas of different ages.

Regional setting: Allain et al., 2022 ↗, introduction and figure 1.

Geological map of Chassiron, Cherves and Angeac
Locations of the three fossil sites. Figure 1, p. 686. © Publications scientifiques du MNHN, Paris. Allain et al., 2022 ↗

Champblanc: a history of lagoons and lakes

Gypsum deposits in the Champblanc quarry at Cherves
The Champblanc gypsum quarry. © Jean-François Tournepiche.

A few kilometres north of Cognac, the Champblanc quarry preserves a succession of Late Jurassic and Early Cretaceous deposits. Gypsum, clays, marls and limestones record changes between a coastal lagoon and lake conditions.

Small vertebrate remains are particularly important here. They complement larger fish, turtle and crocodyliform fossils. Their study forms a distinct research history for this site.

Discover Champblanc and its collections →

Chassiron: a Late Jurassic coastline

At the northern tip of the Île d’Oléron, Chassiron records the Tithonian, before Angeac’s Berriasian deposits. Its assemblages combine terrestrial, freshwater and marine organisms, documenting a coastal environment.

This Charente-Maritime site complements regional research with a fauna and coastal environment older than those of Angeac.

What is compared

Fossil siteAgeRecorded environment
Chassiron · Charente-MaritimeTithonian, Late JurassicCoastal; terrestrial, freshwater and marine influences
Champblanc / Cherves · CharenteTithonian–Berriasian successionCoastal lagoon and lake; alternating deposits
Angeac-Charente · CharenteBerriasian, Early CretaceousFreshwater wetland plain near a river

The age and environment of the deposits, together with fossil preservation, explain some differences between these assemblages. Comparing them sheds light on changes in faunas and landscapes across the Jurassic–Cretaceous transition.

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