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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 />

GEOGRAPHY, ENVIRONMENT AND POLLUTION<br />

Because <strong>of</strong> <strong>the</strong> north-south orientation <strong>of</strong> East<br />

Africa, <strong>the</strong>re is a strong temperature gradient in<br />

<strong>the</strong> coastal waters <strong>of</strong> this region with a peak in<br />

<strong>the</strong> mid-latitudes <strong>of</strong> approximately 4-15 o S<br />

(sou<strong>the</strong>rn Kenya to nor<strong>the</strong>rn Mozambique), and<br />

lower temperatures to <strong>the</strong> south and north. This<br />

geographic variation had a particularly strong<br />

influence on <strong>the</strong> health and status <strong>of</strong> reefs<br />

during 1998 when <strong>the</strong> region experienced <strong>the</strong><br />

major El Niño climate event.<br />

The East African coast is strongly influenced by<br />

river discharges and high nutrient levels, which<br />

affects coral reef distribution at both regional<br />

and local scales. Large expanses <strong>of</strong> <strong>the</strong> central<br />

Mozambique coast (800km) are devoid <strong>of</strong> reefs<br />

due to discharges from <strong>the</strong> large Limpopo and<br />

Zambezi rivers. Many fringing reefs have breaks<br />

opposite short coastal rivers that empty through<br />

deep mangrove creeks. The few measures <strong>of</strong><br />

nutrient concentrations show high levels<br />

compared to o<strong>the</strong>r reefs systems, which are<br />

consistent with low levels <strong>of</strong> water clarity due<br />

to increased plankton and sediment loads.<br />

Information on coral reef status along <strong>the</strong> Indian<br />

Ocean coast <strong>of</strong> Somalia is poor, though patch<br />

reefs are known to extend to Mogadishu. It is<br />

likely that reefs do extend as far as <strong>the</strong> Horn <strong>of</strong><br />

Africa, with expansion <strong>of</strong> many reef organisms<br />

onto <strong>the</strong> Socotra Archipelago (see Chapter 3).<br />

South Africa<br />

The coral reefs and coral communities <strong>of</strong> South<br />

Africa lie between 26-27 o S. These are <strong>the</strong> most<br />

sou<strong>the</strong>rly reefs in <strong>the</strong> western Indian Ocean.<br />

They are generally deep (below 8m), <strong>of</strong>fshore,<br />

have high energy banks, and normal<br />

temperatures ranging from 22-26 o C to 29.5 o C. The reefs grow on a narrow continental shelf<br />

only 2-7km wide, which is remote from major human populations. The principal use <strong>of</strong> <strong>the</strong><br />

reefs has been for game fishing and diving.<br />

Mozambique<br />

The 2,700km coastline extends from 26 o S to 12 o S, encompassing a full spectrum <strong>of</strong> reef<br />

types from <strong>the</strong> high latitude reefs <strong>of</strong> South Africa to <strong>the</strong> fringing and island reef complexes<br />

along <strong>the</strong> Mozambique-Tanzanian border where <strong>the</strong> South Equatorial Current meets <strong>the</strong><br />

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