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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 />

transect. Turf algae (2.8%) were <strong>the</strong> only living material. This shallow zone (1m low tide)<br />

was severely impacted during <strong>the</strong> 1998 El Niño with around 95% coral mortality. In <strong>2000</strong>,<br />

some living corals appeared (0.9%), along with zoanthids (Palythoa - 10%) and algae<br />

(12.3% - calcareous and macroalgae -Turbinaria). There were no new Acropora recruits,<br />

but <strong>the</strong> calcareous algae will constitute a good substrate for new coral settlement. On <strong>the</strong><br />

outer slope, <strong>the</strong>re was a low cover <strong>of</strong> living corals (2.1%), mostly massive forms and some<br />

s<strong>of</strong>t corals. All <strong>the</strong> branching Acropora disappeared during <strong>the</strong> 1998 bleaching event.<br />

Some coral recovery was observed in <strong>2000</strong> with 0.5% branching Acropora, and a definite<br />

increase, although not quantified, <strong>of</strong> non-Acropora forms, mostly massive and s<strong>of</strong>t corals.<br />

Algae were just 6.2% <strong>of</strong> cover, mostly calcareous algae (2.3%) and a few Turbinaria sp.<br />

The Silhouette site was added in <strong>2000</strong>. The reef flat is heavily impacted by <strong>the</strong> south-east<br />

monsoons and has always had low coral cover. The site at 2m depth has no Acropora, a 9%<br />

cover <strong>of</strong> non-Acropora (encrusting and massive corals), and some s<strong>of</strong>t zoanthids (Palythoa).<br />

Most <strong>of</strong> <strong>the</strong> cover (over 50%) was dead coral rubble and sand. The outer slope (5-6m<br />

depth) had alive and dead massive corals (>15%) scattered over a sandy zone, with<br />

submassive corals (>15%), some encrusting corals, and 0.7% branching, very young<br />

Acropora which showed signs <strong>of</strong> fish grazing. This site appeared to escape most <strong>of</strong> <strong>the</strong> 1998<br />

El Niño bleaching, possibly due to better water exchange with <strong>the</strong> cooler deeper waters.<br />

COMPARISON OF 1997 – <strong>2000</strong> DATA<br />

<strong>Coral</strong> cover on <strong>the</strong> Ternay Bay outer slope dropped from 54.6% in November 1997 to 3.5%<br />

in June 1998, 2.1% in January 1999 and 5.1% in March <strong>2000</strong>. Acropora was more affected<br />

(29.1% in 1997, 0% in 1998 and 1999, and 0.5% in <strong>2000</strong>) than non-Acropora massive<br />

corals (25.5% in 1997, 3.5% in 1998, 2.1% in 1999 and 4.6% in <strong>2000</strong>). S<strong>of</strong>t corals appear to<br />

be fast growing, opportunistic species. As a reflection <strong>of</strong> <strong>the</strong>se changes, abiotic forms<br />

went from 37% in 1997 to 92.3% in 1998, 92.8% in 1998 and 86.8% in <strong>2000</strong>. These losses<br />

can be attributed to <strong>the</strong> 1998 bleaching phenomenon, as human activities are limited, and<br />

recovery is predicted for good coral cover, provided bleaching does not happen again<br />

within <strong>the</strong> next few years. A similar pattern was evident on <strong>the</strong> reef flat with a total loss <strong>of</strong><br />

coral after <strong>the</strong> 1998 bleaching event; here recovery is predicted to be very slow.<br />

MAIN PROBLEMS AFFECTING THE COASTAL ENVIRONMENT<br />

Comoros<br />

These islands experience both natural and anthropogenic disturbances, with <strong>the</strong> major<br />

impact being <strong>the</strong> global warming in 1997-98 which caused extensive coral bleaching and<br />

mortality in large areas, particularly to species <strong>of</strong> Acropora. The majority <strong>of</strong> reefs e.g. <strong>the</strong><br />

small islands <strong>of</strong> Nioumachouioi, are subjected to strong swells from Monsoons and<br />

particularly from cyclones which destruct <strong>the</strong> more fragile corals, especially acroporids.<br />

However, this damage was always within natural recovery capacity and is now insignificant<br />

compared with anthropogenic degradations.<br />

Blast or dynamite fishing is one <strong>of</strong> <strong>the</strong> major damaging factors, and is currently practised in<br />

Moheli, where <strong>the</strong> entire reef flat bordering <strong>the</strong>se small islands is covered with newly-broken<br />

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