@conference{10272/7485,
year = {2007},
url = {http://hdl.handle.net/10272/7485},
abstract = {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
differentiated 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.},
publisher = {Asociación Española para el Estudio del Cuaternario},
title = {Rasgos morfológicos y bioerosivos en un alto nivel marino del pleistoceno medio : el abrigo arqueológico de la Cabililla de Benzú (Ceuta)},
title = {Morphologic and bioerosive features from an old marine highstand: the Cabililla archaeological shelter, Benzú, Ceuta},
author = {Abad de los Santos, Manuel and Cáceres Puro, Luis Miguel and Rodríguez Vidal, Joaquín and Ruiz Muñoz, Francisco and López González, Nieves and Chamorro, S. and Bernal, D. and Ramos, J.},
}