@inbook{10498/21399,
year = {2008},
url = {http://hdl.handle.net/10498/21399},
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.},
keywords = {Benzú},
keywords = {Ceuta},
keywords = {Geología},
keywords = {Cabililla},
keywords = {Arqueología},
keywords = {Bioerosión},
keywords = {Socave marino},
keywords = {Pleistoceno Medio},
title = {Rasgos morfológicos y bioerosivos en un alto nivel marino del Pleistoceno Medio: el abrigo arqueológico de la Cabililla de Benzú (Ceuta)},
author = {Abad, Manuel and Ramos Muñoz, José Francisco and Bernal Casasola, Darío and Rodríguez-Vidal, Joaquín and Ruiz, F and López-González, N and Chamorro-Moreno, Simón},
}