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Bioerosion




Bioerosion of coral reefs generates the fine and white Coral Sand characteristic of tropical islands. The coral is converted to sand by internal bioeroders such as Algae , Fungi , Bacteria (microborers) and Sponge s ( Clionidae ), Bivalve s ( Lithophaga ), Sipunculan s ( Aspidosiphon ), polychaetes ( Eunicidae ), generating extremely fine sediment of 10 to 100 micrometres. External bioeroders include Urchin s ( Diadema ) and Chiton s ( Acanthopleura ). These forces in concern result in a great deal of erosion. Sea Urchin erosion of CaCO3 has been reported in some reefs at annual rates exceeding 20 kg/m².

Fish also erode coral while eating Algae . Parrotfish cause a great deal of bioerosion, due to their well developed jaw muscle and tooth armature, and a Pharyngeal Mill , which grinds up ingested material into sand-sized particles. Bioerosion of reef Calcium Carbonate by parrotfish can range from 1017.7±186.3 kg yr-¹ (0.41±0.07 m³ yr-¹) for Chlorurus Gibbus and 23.6±3.4 kg yr-¹ (9.7 10-³±1.3 10-³ m²yr-¹) for Chlorurus Sordidus (Bellwood, 1995).


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REFERENCES


Belwood, D. R. (1995). Direct estimate of bioerosion by two parrotfish species, ''Chlorurus gibbus'' and ''C. sordidus'', on the Great Barrier Reef, Australia. ''Marine Biology'', 121(3), 419-429. {Link without Title}