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#Status of Coral Reefs 2002 - International Coral Reef Action Network

#Status of Coral Reefs 2002 - International Coral Reef Action Network

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Status <strong>of</strong> <strong>Coral</strong> <strong><strong>Reef</strong>s</strong> <strong>of</strong> the World: <strong>2002</strong><br />

<strong><strong>Reef</strong>s</strong> <strong>of</strong> the Capricorn Bunker group had high coral cover until 1988 when it is probable that a<br />

storm removed most <strong>of</strong> the coral cover. After a lag <strong>of</strong> several years, the coral cover has increased<br />

steadily from virtually zero to over 60% cover, which is mostly rapid growing table Acropora<br />

species. This illustrates the value <strong>of</strong> long term observations.<br />

Elizabeth and Middleton <strong><strong>Reef</strong>s</strong>: These large atolls are particularly remote and there have<br />

been no surveys since the 2000 report. They are remote from human impacts but exposed<br />

to strong waves and storms.<br />

Lord Howe Island: This is one <strong>of</strong> the most southern coral fringing reefs in the world<br />

(31°40’S) and also a World Heritage Site. The reefs have low species diversity with mostly<br />

tropical species mixed with more temperate species. Surveys between 1978 and 1993<br />

showed significant differences in coral species, suggesting that the rare species may<br />

become locally extinct after impacts <strong>of</strong> COTS, coral bleaching and storms. Replacement by<br />

larvae from reefs to the north may be a very irregular event. A habitat mapping program is<br />

in progress, but there is no regular monitoring.<br />

Other Areas: There is coral growth on rocky reefs south <strong>of</strong> the GBR in southern<br />

Queensland: the Gneering Shoals (26°S), Flinders <strong><strong>Reef</strong>s</strong> (27°S) and northern New South<br />

Wales (28°S 30’S) with populations up to 50% coral cover.<br />

Western Australia<br />

Ashmore and Cartier <strong><strong>Reef</strong>s</strong>, Scott and Seringapatam <strong><strong>Reef</strong>s</strong> and Rowley Shoals: These<br />

remote oceanic and shelf-edge reefs receive no mainland influence, being at least 300km<br />

<strong>of</strong> the Western Australian coast. Ashmore <strong>Reef</strong> is now a Marine Reserve and currently<br />

closed to all exploitation except subsistence fishing by Indonesian fishermen. Scott and<br />

Seringapatam <strong><strong>Reef</strong>s</strong> (14°S) are fished by Indonesians for sea cucumbers, trochus and<br />

sharkfin and is a prospective site for extraction <strong>of</strong> liquid natural gas. In 1998, elevated seasurface<br />

temperatures caused massive coral mortality down to a depth <strong>of</strong> 30 metres. Since<br />

1998, the corals on these reefs have recovered only slightly (see Chapter 1). Further south,<br />

the three reefs <strong>of</strong> the Rowley Shoals (17°S) are protected as State and Commonwealth<br />

marine parks. Anthropogenic impacts on the Rowley Shoals are minimal, with fishing for<br />

most species banned. <strong>Coral</strong> communities at all reefs were in good condition through most<br />

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