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The tropical–subtropical western Atlantic realm harbours abundant fringing reefs, two major barrier reefs (Belize, Florida), several atolls and large reef‐fringed carbonate platforms (Bahamas). Data from Belize and south Florida indicate that major barrier reefs were established during the high sea‐levels of the long and warm marine isotope stage 11. Reefs formed during Pleistocene sea‐level highstands,...
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