Rogerella
Encyclopedia
Rogerella is a small pouch-shaped boring
(a type of trace fossil
) with a slit-like aperture currently produced by acrothoracican
barnacles. These crustaceans extrude their legs upwards through the opening for filter-feeding
(Seilacher, 1969; Lambers and Boekschoten, 1986). They are known in the fossil record as borings in carbonate substrates (shells and hardgrounds) from the Devonian
to the Recent (Taylor and Wilson, 2003).
Bioerosion
Bioerosion describes the erosion of hard ocean substrates – and less often terrestrial substrates – by living organisms. Marine bioerosion can be caused by mollusks, polychaete worms, phoronids, sponges, crustaceans, echinoids, and fish; it can occur on coastlines, on coral reefs, and...
(a type of trace fossil
Trace fossil
Trace fossils, also called ichnofossils , are geological records of biological activity. Trace fossils may be impressions made on the substrate by an organism: for example, burrows, borings , urolites , footprints and feeding marks, and root cavities...
) with a slit-like aperture currently produced by acrothoracican
Acrothoracica
The Acrothoracica are a superorder of barnacles.Acrothoracicans bore into calcareous material such as mollusc shells, coral, crinoids or hardgrounds, producing a slit-like hole in the surface known by the trace fossil name Rogerella. They are typically smaller than other types of barnacle, being...
barnacles. These crustaceans extrude their legs upwards through the opening for filter-feeding
Filter feeder
Filter feeders are animals that feed by straining suspended matter and food particles from water, typically by passing the water over a specialized filtering structure. Some animals that use this method of feeding are clams, krill, sponges, baleen whales, and many fish and some sharks. Some birds,...
(Seilacher, 1969; Lambers and Boekschoten, 1986). They are known in the fossil record as borings in carbonate substrates (shells and hardgrounds) from the Devonian
Devonian
The Devonian is a geologic period and system of the Paleozoic Era spanning from the end of the Silurian Period, about 416.0 ± 2.8 Mya , to the beginning of the Carboniferous Period, about 359.2 ± 2.5 Mya...
to the Recent (Taylor and Wilson, 2003).
External links
- Bioerosion Website at The College of WoosterThe College of WoosterThe College of Wooster is a private liberal arts college primarily known for its Independent study program. It has roughly 2,000 students and is located in Wooster, Wayne County, Ohio, United States . Founded in 1866 by the Presbyterian church as the University of Wooster, it was from its creation...
- Comprehensive bioerosion bibliography