[Coral-List] making little one out of big ones (John Ware) Issue 29
Gene Shinn
eshinn at marine.usf.edu
Sat Oct 21 15:56:13 EDT 2006
Thanks John for providing an opportunity to join in on this boring topic.
...Back in the stone age (1958) when I began helping Bob Ginsburg run
his Florida Keys field trips it was common practice to break open a
piece of dead coral at each dive stop and demonstrate to students the
various boring organisms that make little ones out of big ones. Bob
had published on the various boring organisms in the 1950s. More than
20 years later, following Hine and Risk (1974), Hudson (1977),
determined the long-term bioerosion rate of the combined activities
of 6 -species of boring sponges. He did this by taking overlapping
cores (in 1976) along the side of previously sampled core holes
(1974) that had been drilled in dead heads at Hens and Chickens reef
in the Florida Keys. This large inshore patch reef had been killed
during the cold-water outbreak of 1969-1970 (widely, and mistakenly,
reported in popular media at that time as death by pollution). Hudson
had originally cored both the living and the dead corals at Hens and
Chickens in 1974 as a way of determining the exact time of death.
Several obvious internal stress bands, visible in x-radiographs of
the cores from all the heads, allowed direct measurement of skeleton
removal from the dead heads since the time they died. He found that
between 1970 and 1974, 0.54 cm had been removed by borers and between
1974 and 1976 bioerosion rate increased to an average annual rate of
0.64 cm. The latter rate is essentially the annual growth rate of
live Montastrea sp. A roughly 50/50 ratio of growth versus removal by
bioerosion. By extrapolation Hudson concluded that bioersoion can
reduce a dead 1-m-high coral head to 0- m in 150 years (Hudson
1977) and that does not include simultaneous chewing and boring
around the base of the heads. How much might have also been removed
by dissolution, indolithic algae, and parrot fish, was not known but
it should be noted that sediment cover (produced by boring and biting
organisms along with Halimeda ) smothers and prevents further
bioerosion. If this did not happen we would not see coral skeletons
preserved in the fossil record. A fossil coral reef is generally
about 50/50 reef builders and reef-derived sand. Surprisingly, the
present-day Florida reef tract is composed mostly of lime sediment
and most of that is derived from calcifying algae, not coral. Even
the sediment pockets within individual coral reefs is principally
composed of algal grains, namely Halimeda. This was also true during
the Pleistocene when coral reefs and algae were forming what is now
the Florida Keys and sea level was about 7 m higher than today.
In the Hudson (1977) study, bioerosion increased in the time
interval between the first and second coring episode so one might
wonder if the increase had anything to do with increased nutrients?
Alternatively, was it due to a lag effect? Does the surface need to
be prepared by bacteria before the boring critters can get up to
speed? We may never know.
Another factor to throw into the discussion is sponge health.
Repeated blights of unknown origin decimated the commercial sponge
industry throughout the Caribbean and Gulf of Mexico in the 1930s and
1940s. Algal blooms and red tides also killed sponges in Florida Bay
in the late 1980s and early 1990s. The latter may be anthropogenic
but the Caribbean-wide blights of the 1930s and 40s most likely were
natural. Being of the same Phylum, one might wonder if the boring
sponges are subject to the same kinds of blights that have occurred
simultaneously throughout the Caribbean? Could sponge blights,
instead of nutrients, explain the waxing and waning of boring
activity or is it just us people who worry about these things that
are so boring? Gene
Hein, F. J. and Risk, M. J., 1975 Bioerosion of coral heads: inner
patch reefs, Florida reef tract: Bull of Mar. Sci. 25 (1) p. 133-138.
Hudson, J. H., 1977, Long-term bioerosion rates on a Florida reef: A
new method, Proceeding, 3rd International Coral Reef Symposium. p.
491-497
--
No Rocks, No Water, No Ecosystem (EAS)
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E. A. Shinn, Courtesy Professor
University of South Florida
Marine Science Center (room 204)
140 Seventh Avenue South
St. Petersburg, FL 33701
<eshinn at marine.usf.edu>
Tel 727 553-1158----------------------------------
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