A PLEISTOCENE PERSPECTIVE ON THE EFFECTIVENESS OF THE HOL CHAN MARINE

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Paper No. 5-0
A PLEISTOCENE PERSPECTIVE ON THE
EFFECTIVENESS OF THE HOL CHAN MARINE
PRESERVE, BELIZE C.A
BISHOP, Dana Christine and GREENSTEIN, Benjamin, Geology, Cornell College, 810
Commons Circle, Mt. Vernon, IA 52314, d-bishop@cornellcollege.edu
Globally, coral reefs appear to be suffering from a combination of anthropogenic and natural
disturbances. While ecologists have noted the waning health of coral reefs, the lack of initial (or
“baseline”) data to center our concept of a “pristine” reef has confounded attempts to establish
marine protected areas (MPAs) to conserve coral reefs. The Pleistocene fossil reef record has been
demonstrated to preserve reef coral communities that were thriving long before humans could
potentially degrade them. Utilizing paleoecological studies of Pleistocene fossil coral reefs to
provide baseline ecological data should allow us to begin to conceptualize the enormity of present
day coral reef degradation. The purpose of this study is to determine how the composition of coral
reefs inside the Hol Chan marine preserve, established in 1987 in Belize C.A., compares to the reefs
outside of the preserve and to a nearby Pleistocene fossil reef (Rocky Point). The Hol Chan marine
preserve has involved the help of many organizations on many different levels. However, it is
possible that the most essential source of relief to the coral reefs of Belize is rooted in the newfound appreciation, respect, and pride of the local Belizeans. We compared the taxonomic
composition and relative abundances of corals composing modern reefs within and outside the
preserve to those obtained from the fossil reef. Results suggest that the reefs in the preserve are
very comparable to Pleistocene reefs exposed at Rocky Point and therefore the marine preserve
appears to conserve a reef system similar to those which existed before human disturbance.
Worldwide, the development of a land ethic is a vital step in the salvation of the coral reef
ecosystems.
North-Central Section (36th) and Southeastern Section (51st), GSA Joint Annual Meeting (April
3–5, 2002)
Session No. 5--Booth# 17
Paleoclimatology and Paleoceanography (Posters)
Heritage Hall: East
1:00 PM-5:00 PM, Wednesday, April 3, 2002
© Copyright 2002 The Geological Society of America (GSA), all rights reserved. Permission is hereby granted to the
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