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Status of Caribbean coral reefs after bleaching and hurricanes in 2005

Status of Caribbean coral reefs after bleaching and hurricanes in 2005

Status of Caribbean coral reefs after bleaching and hurricanes in 2005

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The Effects <strong>of</strong> Coral Bleach<strong>in</strong>g <strong>in</strong> the Northern <strong>Caribbean</strong> <strong>and</strong> Western Atlanticon 12 September, 2004. Large masses <strong>of</strong> s<strong>and</strong> piled up on back-reef <strong>coral</strong>s <strong>and</strong> <strong>in</strong> lagoons onthe south side <strong>of</strong> Little Cayman. By November 2004, there was little obvious damage on thefore-reef slopes.CubaGeographic Distribution <strong>and</strong> Extent <strong>of</strong> Coral Reefs: The ma<strong>in</strong> isl<strong>and</strong> <strong>of</strong> Cuba, the Isle <strong>of</strong> Youth<strong>and</strong> 4195 cays <strong>and</strong> islets are distributed over 110,860 km 2 . The isl<strong>and</strong>s are at the entrance <strong>of</strong>the Gulf <strong>of</strong> Mexico, between the Atlantic Ocean <strong>and</strong> the <strong>Caribbean</strong> Sea. Numerous fr<strong>in</strong>g<strong>in</strong>g<strong>and</strong> bank-barrier <strong>reefs</strong> border more than 98% <strong>of</strong> Cuba’s 3200 km shelf marg<strong>in</strong>, although morethan 50% are separated from the ma<strong>in</strong>l<strong>and</strong> by cays or by broad, shallow lagoons with manypatch <strong>reefs</strong>. This separation has provided the outer <strong>reefs</strong> with protection from anthropogenic<strong>in</strong>fluences, except for fish<strong>in</strong>g <strong>and</strong>, <strong>in</strong> some places, tourist div<strong>in</strong>g. Reef crests <strong>in</strong> Cuba tendto be more abundant at the edge <strong>of</strong> the 4 broad sections <strong>of</strong> the Cuban shelf: the Golfo deGuanahacabibes (Northwest Cuba); Archipiélago Sabana-Camagüey (central north); Golfo deAna María-Guacanayabo (southeast); <strong>and</strong> Golfo de Batabanó (southwest). The narrow shelf<strong>of</strong> the Northeast also has well developed reef crests. Inshore patch <strong>reefs</strong> are dispersed on thenorthwest (Golfo <strong>of</strong> Guanahacabibes), southwest (Golfo de Batabanó) <strong>and</strong> southeast (Golfo deAna María-Guacanayabo) where there are unique <strong>reefs</strong> on muddy substrata. There are 2 barrier<strong>reefs</strong>: Archipiélago Los Colorados (NW Cuba); <strong>and</strong> Archipiélago Jard<strong>in</strong>es de la Re<strong>in</strong>a.<strong>Status</strong> <strong>of</strong> <strong>coral</strong> <strong>reefs</strong> prior to <strong>2005</strong>: Live <strong>coral</strong> cover averaged 21% on Cuban reef crests <strong>and</strong>shallow <strong>reefs</strong> <strong>and</strong> 18% on fore-<strong>reefs</strong>. The <strong>coral</strong>s have been stressed by organic <strong>and</strong> chemicalpollution around populated areas, diseases, the Diadema die-<strong>of</strong>f <strong>and</strong> resultant competitionwith algae, <strong>and</strong> some earlier <strong>bleach<strong>in</strong>g</strong>. The <strong>reefs</strong> were recover<strong>in</strong>g from these stresses until<strong>2005</strong>, when <strong>bleach<strong>in</strong>g</strong> <strong>and</strong> <strong>hurricanes</strong> resulted <strong>in</strong> <strong>coral</strong> mortality.Impacts <strong>of</strong> Coral Bleach<strong>in</strong>g <strong>in</strong> <strong>2005</strong>: In summer <strong>2005</strong>, <strong>coral</strong> <strong>bleach<strong>in</strong>g</strong> was widespread<strong>and</strong> <strong>in</strong>tense. Assessments conducted by the Early Warn<strong>in</strong>g Coral Reef Volunteer Monitor<strong>in</strong>gNetwork showed that <strong>coral</strong> <strong>bleach<strong>in</strong>g</strong> around Cuba varied from 1-10% to 75-100% <strong>of</strong> colonies,predom<strong>in</strong>antly between categories 50-75% <strong>and</strong> 75-100% (at 89% <strong>of</strong> reported sites). Only onesite, Punta Francés (SW <strong>of</strong> Isla de la Juventud), suffered lower <strong>in</strong>tensity <strong>bleach<strong>in</strong>g</strong> (1-30%).Most anecdotal reports refer to a high degree <strong>of</strong> recovery by May 2006.Impacts <strong>of</strong> Coral Bleach<strong>in</strong>g <strong>in</strong> 2006: Coral <strong>bleach<strong>in</strong>g</strong> <strong>in</strong> 2006 was widespread but with vary<strong>in</strong>g<strong>in</strong>tensities, <strong>in</strong>creas<strong>in</strong>g <strong>after</strong> mid-September. The volunteer monitor<strong>in</strong>g network reported that<strong>coral</strong> <strong>bleach<strong>in</strong>g</strong> did not exceed 10% <strong>and</strong> was generally not higher than 5%. María la Gorda wasan exception with 10-30% colonies bleached at 20-25 m depth, but much less <strong>in</strong> shallowerareas. Warm<strong>in</strong>g <strong>in</strong>creased <strong>in</strong> mid-September, <strong>and</strong> moderate <strong>bleach<strong>in</strong>g</strong> (10-30%) was recordedat Havana City <strong>and</strong> Jard<strong>in</strong>es de la Re<strong>in</strong>a Archipelago, <strong>and</strong> <strong>in</strong>tense <strong>bleach<strong>in</strong>g</strong> (75-100%) at PuntaFrancés (SW Isla de la Juventud). Bleach<strong>in</strong>g was low <strong>in</strong> the Sabana-Camagüey Archipelago <strong>and</strong>Bahía de Coch<strong>in</strong>os. No <strong>in</strong>formation is available from Santiago de Cuba <strong>and</strong> Granma prov<strong>in</strong>ces,to the east.Impacts <strong>of</strong> Hurricanes <strong>in</strong> <strong>2005</strong>: Hurricane Denis, which made l<strong>and</strong>fall <strong>in</strong> July, <strong>2005</strong>near Punta del Inglés, caused only m<strong>in</strong>or damage at Cabo Cruz <strong>and</strong> Pilón (Nacional ParkDesembarco del Granma, south-eastern Cuba), despite w<strong>in</strong>d velocities reach<strong>in</strong>g 310 km/h.77

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