Abstract
The Lower Jurassic characterisation and particularly the Pliensbachian–Toarcian limit is of a paramount importance in the geological history of the Atlantic and the circum-Mediterranean field. In the Moroccan central High Atlas and in the Todrha-Dades region particularly, this passage is similar to a hinge area marked with tectono-eustatic and bio-sedimentary events. La caractérisation de la limite Pliensbachien–Toarcien revêt une grande importance dans l’histoire géologique du domaine atlasique et du domaine circum-méditerranéen. Dans le Haut Atlas central marocain, en particulier dans la région de Todrha-Dadès, ce passage correspond à une époque charnière, marquée par des événements bio-sédimentaires et tectono-eustatiques.
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