At least 45 of the approximately 600 species of molluscs documented from the Bowden shell bed exhibit evidence of bioerosion in the form of completely or incompletely penetrative (failed) small round holes. Assessment of previously illustrated material, together with new collections made by us, shows that these borings are assignable to the ichnotaxon Oichnus Bromley, 1981, in particular O. paraboloides Bromley, 1981 and O. simplex Bromley, 1981. Observations suggest that the borings were not a result of parasitism nor simple random excavations by bioeroding organisms. Rather, they are interpreted as a result of opportunistic predatory activities of cannibalistic gastropods, O. paraboloides probably having been produced by naticids and O. simplex by muricids.

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Mededelingen van de Werkgroep voor Tertiaire en Kwartaire Geologie

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Werkgroep voor Tertiaire en Kwartaire Geologie

Ron K. Pickerill, & Stephen K. Donovan. (1998). Ichnology of the Pliocene Bowden shell bed, southeast Jamaica. Mededelingen van de Werkgroep voor Tertiaire en Kwartaire Geologie, 35(1/4), 161–175.