Abstract The Peñón the Bernal section in the Sierra de Gádor comprises a succession of limestones, marly limestones and marls in the upper part of the Gádor unit, which belongs to the Alpujárride Complex in the Internal Zones of the Betic Cordillera. Several shell beds in this section and the locality of La Zarba in the same unit include relatively well-preserved macroinvertebrate assemblages. These beds reflect shell concentrations caused by storms and later colonised by epifaunal communities of cemented, epibyssate and endobyssate bivalves. Sedimentary features, fossil traces, and composition of bivalve assemblages indicate that the succession accumulated in a peritidal environment in a restricted carbonate platform with cyclic changes in water depth. The identified bivalve and ammonoid taxa suggest a Ladinian (Middle Triassic) age for the limestones, marly limestones and marls culminating the Gádor unit, so far considered as Upper Triassic in age. Like in other domains in the Betic Cordillera, the macroinvertebrate fauna has strong affinities with the Sephardic bioprovince.
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