- Article
A New Ammonite Biostratigraphic Framework for Distal Urgonian Successions of North Provence and a Correlation with Southern Vercors
- Camille Frau,
- Anthony J.-B. Tendil and
- Cyprien Lanteaume
New ammonite discoveries from the south-facing flank of Mont Ventoux (southern France) provide robust and refined age constraints on the maximum northward progradation of Urgonian depositional environments in northern Provence during the late Barremian to early Aptian. The succession records distal Urgonian depositional environments during the late Barremian, spanning from the Toxancyloceras vandenheckii to the upper Gerhardtia sartousiana Zone, followed by strongly progradational distal Urgonian deposits with an age interval from the terminal Barremian into the early Aptian. These new data permit an updated and simplified regional correlation of Urgonian successions across the Barremian–Aptian boundary in northern Provence and along the northern margin of the Vocontian Basin. Our correlations reveal clear, coeval sedimentary signals across both regions, emphasizing the regional synchronicity of Urgonian platform development at the basin scale.
7 March 2026


![(A) Barremian–Aptian palaeogeography of the western Tethys. The red square indicates the location of panels (B,C). (B) Late Barremian palaeogeographic reconstruction of southeastern France showing the coalescent Urgonian platforms surrounding the Vocontian Basin. The red square marks the location of the study area (Mont Ventoux). (C) Latest Barremian to early Aptian palaeogeographic reconstruction of southeastern France illustrating the initiation of the intra-shelf South Provence Basin and the differentiation of the North Provence Urgonian platform. The red square marks the location of the study area (Mont Ventoux). All figures are modified after [3].](https://mdpi-res.com/cdn-cgi/image/w=470,h=317/https://mdpi-res.com/diversity/diversity-18-00162/article_deploy/html/images/diversity-18-00162-g001-550.jpg)




