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A study of the bioerosion structures and the skeletobionts associated with the most common bivalves (infauna and epifauna) from the classic Upper Tortonian site of Cacela, Algarve region, SE Portugal, revealed 24 different ichnotaxa and five systematic groups of encrusters (Foraminifera, Annelida, Bryozoa, Balanomorpha and Bivalvia).

Despite a relatively high ichnodiversity, the percentage of bioerosion in the specimens analysed is quite low (10–12%). This is explained by rapid sedimentation with only short periods of exposure on the sea-floor.

The dominant bioerosion structures were linked to the boring activity of nonpredatory organisms. Algal microborings are the most common, followed by annelid borings (Caulostrepsis-Maeandropolydora), sponge borings (Entobia) and ctenostome bryozoans (Pinaceocladichnus).

Spatial distribution of bioerosion structures and encrusters allow the reconstruction of three …