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Resúmenes XII Reunión Nacional de Cuaternario

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[Abad, Manuel|PublicAdministrativeSpace:Abad, Manuel] [Bernal, D.|PublicAdministrativeSpace:Bernal, D.] [Chamorro, S.|PublicAdministrativeSpace:Chamorro, S.] [Cáceres, L. M.|PublicAdministrativeSpace:Cáceres, L. M.] [López-González, N.|PublicAdministrativeSpace:López-González, N.] [Ramos, J.|PublicAdministrativeSpace:Ramos, J.] [Rodríguez-Vidal, Joaquin|PublicAdministrativeSpace:Rodríguez-Vidal, Joaquin] [Ruiz, F.|PublicAdministrativeSpace:Ruiz, F.]

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2007

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The micro-morphologic and bioerosive features, analyzed in the Benzú shelter (Ceuta), allow us to deduce an erosion marine surface elaborated onto dolomite triassic substrate. The Entobia-Gastrochaenolites Ichnoassociation and Entobia ichnofacies denote high energy coastal or shallow marine environment with low sedimentation rates. Two phases are differentiate in the evolution of these bioerosive structures: the first one defined by great borings of Gastrochaenolites, and the second recorded by bioerosive activity of Entobia and truncation of both, the previous borings and the cliff surface.

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