These small slits, each about two millimeters long, were excavated by acrothoracican barnacles in an oyster shell (Cenomanian, Upper Cretaceous, southern Israel). These particular traces are somewhat aligned with the long axis of the oyster (probably because of a current), but most aggregations of barnacle borings are not. This trace fossil is known as Rogerella.

 

 Main Bioerosion Page

 Bioeroding Organisms

 Common Macroborings

 Marine Hard Substrates

 Geology Department

 Website design by Mark A. Wilson & Amy E. Wilson