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This dissertation summarizes the stratigraphic description of three Pleistocene archaeological sites in the middle Ter river valley. A long history of archaeological research in this region suggests the possibility of developing contextual studies. This work is basically an investigation of two soil formation processes from the deep soil horizons of the Mediterranean region: clay illuviation and carbonatation. This approach has been developed by soil micromorphology, a technique well suited fordoi:10.15160/1824-2707/406 fatcat:hhe2wg7znjbujm3pnnshan26zq