Abstract
The Gran Banco de Buena Esperanza (GBBE) coral reef system in Golfo de Guacanayabo in southeastern Cuba consists of a reticular structure comprising a maze of steep to vertical ridges with planar tops rising 20–25 m from the bay floor. The planar tops of the ridges are densely populated by small colonies of sediment-resistant Scleractinia with fragile, branching colony growth forms. The initiation of a reticulate reef system in the absence of karst or other antecedent hard substrates is unprecedented. In this note, we describe the unique geological setting, geomorphology and scleractinian diversity of the GBBE and present an explanation for its development. We suggest that convection-driven self-organization of coral skeletal fragments may be responsible for the reticulate pattern observed as 75 m of reef limestone accreted during Holocene time. Finally, we briefly discuss the evolutionary benefits of coral hybridization and the potential for rapid coral reef growth in turbid, muddy environments.
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Acknowledgements
Ms. J. Granatino of the Barrington Public Library in Rhode Island provided assistance in obtaining access to many publications. We benefited from discussion of the geological setting of the bay with Dr. M. Cabrera Castellanos and consultation with Dr. N. Fogarty concerning A. prolifera. The manuscript benefited a great deal from the suggestions of the Editor in Chief and the Topic Editor of Coral Reefs and the reviews of Dr. S. J. Purkis and Dr. D. Blakeway, to whom we also are grateful for drafting Fig. 2. Kevin O’Rourke (Center for Scholarship, Teaching and Technology, Roger Williams University) provided technical assistance with Fig. 3.
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Zlatarski, V.N., Greenstein, B.J. The reticulate coral reef system in Golfo de Guacanayabo, SE Cuba. Coral Reefs 39, 509–513 (2020). https://doi.org/10.1007/s00338-020-01933-7
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DOI: https://doi.org/10.1007/s00338-020-01933-7