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Status of Coral Reefs of the World 2000

Status of Coral Reefs of the World 2000.pdf

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<strong>Status</strong> <strong>of</strong> <strong>Coral</strong> <strong>Reefs</strong> <strong>of</strong> <strong>the</strong> <strong>World</strong>: <strong>2000</strong><br />

THE FRENCH CARIBBEAN<br />

Guadeloupe<br />

The Caribbean coast <strong>of</strong> Guadeloupe has a narrow island shelf and high levels <strong>of</strong> volcanic<br />

sedimentation, <strong>the</strong>refore <strong>the</strong>re are no true coral reefs. However, <strong>the</strong>re are most diverse coral<br />

communities on <strong>the</strong> rocky bottoms, particularly around <strong>the</strong> Pigeon Islets. The Grand Cul-de-<br />

Sac Marin in <strong>the</strong> north is enclosed by a barrier reef, 20km long, which encloses a 10km wide<br />

lagoon covering 15,000 ha. This barrier protects extensive seagrass beds in <strong>the</strong> lagoon and<br />

mangroves on <strong>the</strong> coast from oceanic swells. On <strong>the</strong> Atlantic coast <strong>of</strong> <strong>the</strong> island <strong>the</strong>re are<br />

fringing reefs, which are more developed on <strong>the</strong> eastern part <strong>of</strong> <strong>the</strong> Basse-Terre (Petit Culde-Sac<br />

Marin). The surrounding islands are ei<strong>the</strong>r devoid <strong>of</strong> coral reefs (Les Saintes) or<br />

possess narrow fringing reefs (Marie-Galante, La Désirade). A shallow, 3 0m deep island<br />

shelf (100 x 70km), has <strong>the</strong> islands <strong>of</strong> Saint-Barthélémy, Saint-Martin and Anguilla and several<br />

small islets with <strong>the</strong> bottom covered by sediments, which are periodically resuspended by<br />

hurricanes. This resuspension has probably limited <strong>the</strong> development <strong>of</strong> coral reefs around<br />

Saint-Barthélémy and Saint-Martin, which have only narrow fringing reefs.<br />

Martinique<br />

<strong>Reefs</strong> are absent on <strong>the</strong> leeward side <strong>of</strong> Martinique from <strong>the</strong> northwest and west coasts<br />

because <strong>of</strong> <strong>the</strong> narrow shelf and high levels <strong>of</strong> volcanic sediments washing <strong>of</strong>f Montagne<br />

Pelée. Never<strong>the</strong>less, <strong>the</strong> rocky bottoms have flourishing coral communities. Fringing reefs<br />

are <strong>the</strong> only types on <strong>the</strong> west and south coasts near Sainte-Luce. The nor<strong>the</strong>rn part <strong>of</strong> <strong>the</strong><br />

Atlantic coast has no coral reefs from <strong>the</strong> north to <strong>the</strong> Presqu’île de la Caravelle, due to <strong>the</strong><br />

steep slope and volcanic sediments. Around <strong>the</strong> Presqu’île de la Caravelle, <strong>the</strong>re are some<br />

fringing reefs, and fur<strong>the</strong>r south, a barrier reef system extends for about 25km. The barrier is<br />

separated from <strong>the</strong> shore by a lagoon 3 to 8km wide, with variable depth from a few<br />

metres to 30m with extensive seagrass beds. Fringing reefs have developed along <strong>the</strong> rocky<br />

shores behind this barrier.<br />

THE NETHERLANDS ANTILLES<br />

Bonaire and Curaçao<br />

These are small oceanic islands approximately 70km north <strong>of</strong> Venezuela. They lie on a<br />

northwest – sou<strong>the</strong>ast axis with <strong>the</strong> east coasts exposed to persistent trade winds. The shelf<br />

around each island is narrow extending up to 300m seawards, <strong>the</strong>n <strong>the</strong> bottom shelves <strong>of</strong>f<br />

steeply onto a sandy terrace at 50–60m, and <strong>the</strong>n drops <strong>of</strong>f again. The islands are<br />

surrounded by continuous fringing reefs which are much better developed on <strong>the</strong> leeward<br />

than on <strong>the</strong> windward shore, particularly in shallow water.<br />

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