Accueil | Réalisations | Usage | Expliquer et Transmettre | Des moulages de fossiles d‘ammonites pour le site géologique du Serre de l’Âne
A la fin du Jurassique, l’océan recouvre une partie du globe ; Au fil du temps, des sédiments marins s’accumulent. Le site du Serre de l’Âne, appartenant au bassin vocontien, est marqué par une sédimentation marine profonde. On y retrouve aujourd’hui de nombreux fossiles parmi lesquels des ammonites représentatives du Hauterivien.
Les moulages de tables de fossiles que Ducaroy Grange a réalisés ont été reproduits à partir des fossiles originaux empruntés au laboratoire géologique de Lyon. Des mesures de précaution ont été prises pour que ces pièces de collection soient parfaitement préservées.
Ducaroy Grange a exécuté les réalisations avec son propre personnel, selon les règles de l’art et mené régulièrement à bonne fin la prestation.
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