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L'analyse biostratigraphique et sédimentaire d'une série réduite du J. Serj (Tunisie), rapportée au Campanien–Maastrichtien, nous a permis de caractériser, pour la première fois, par la composition de la biophase, deux épisodes de remaniements sous-marins en milieu distal, qui sont successivement d'âge anté-Maastrichtien supérieur (zone à Rosita contusa) et anté-Paléocène supérieur (zone à Morozovella...
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