This paper deals with shell bioerosion in a population of Terebratula scillae Seguenza from the Lower Pleistocene in Lecce area, Southern Italy. The most important traces belong to shell breakage attributed to predatory activity; borings (Entobia isp., Maeandropolydora isp.); drill holes (Oichnus simplex Bromley; Oichnus isp.); and etching scars (Centrichnus eccentricus Bromley and Martinell; Podichnus centrifugalis Bbromlry and Surlyk). The distribution analysis of the traces of epibiosis on the shells of T. scillae induces us to think that we are dealing with a pedicleanchored form, living with completely raised valves. Besides, both percentage and nature of predation marks (probably due to gastropods or decapod crustaceans) do not depose for a very intense predation pressur.