Summary
Among the large number of limestone-eroding organisms, sponges, mainly of the family Clinonidae are of special interest because of their efficient means of substratum penetration by cellular etching and because they release characteristically shaped calcium carbonate chips which can be detected in the mud-size fraction of many sediments. Identifiable trace fossils and sediments are of great ecological and paleoecological significance.
As new data on the excavating mechanism have become available, the questions of burrowing rates and sediment production have gained importance. Extrapolation from shortterm experiments (under 6 months) on substrate invasion are inconclusive because of high initial penetration rates resulting from mechanical stimulation and lack of competition. New experiments show that the rate curve flattens after 6 months and that optimum longterm erosion of CaCO3 does not exceed 700 mg m-2 year-1 (Cliona lampa and C. aprica). Substrate limitations and competition will further reduce this rate.
By monitoring the production of CaCO3 chips by Cliona lampa, it was possible to link activity patterns to certain environmental factors. Mechanical stimuli, high light intensity, strong currents and, possibly, low temperature seem to accelerate the burrowing process. Sponge-generated chips can make up over 40% of coral mud when deposited in the current shadow of the reef framework.
Using transect counts and sponge area-biomass conversion factors, the mean abundance of burrowing sponges on the Bermuda platform could be calculated. On suitable hard bottom substrates it averages 16 g dry weight per m2. From this value the burrowing potential of sponges can be estimated as 256 g CaCO3 per m2 substrate per year. Since 97–98% of the eroded limestone remains in particulate form, the contribution of fine sediments can amount to 250 g m-2 year-1.
Attention is called to the fact that erosion rates by burrowers can not directly be compared with those of borers or scrapers. The former are intermittent and their activities are affected by environmental and biological interactions, while activities of the latter are rather constant and guided by the need for food.
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This work was supported by the Smithsonian Research Foundation, by the Smithsonian Environmental Sciences Program and by a Sydney L. Wright Fellowship, at the Bermuda Biological Station. Contribution No. 619, Bermuda Biological Station. Contribution No. 10, Investigations of Marine Shallow Water Ecosystems Project, Smithsonian Institution.
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Rützler, K. The role of burrowing sponges in bioerosion. Oecologia 19, 203–216 (1975). https://doi.org/10.1007/BF00345306
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DOI: https://doi.org/10.1007/BF00345306