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Status of the Worlds Coral Reefs
Executive Summary
THE CORAL
BLEACHING EVENT OF 19971998
There has been
unprecedented bleaching of hard and soft corals
throughout the coral reefs of the world from
mid-1997 to late-1998. Information is coming in
daily via the internet and from GCRMN and Reef
Check teams. Much of the bleaching coincided with
a large El Niño event, followed by a strong La
Niña, but bleaching in other areas appears
uncorrelated. Four overlapping levels of
bleaching are apparent:
- catastrophic,
with massive mortality (often near 95% of
shallow corals) in Bahrain, the Maldives,
Sri Lanka, Singapore, and in large areas
of Tanzania;
- severe
bleaching with around 5070% mortality, and also
coral recovery, in Kenya, Seychelles,
Japan, Thailand, Vietnam, and Belize;
- moderate
and patchy bleaching on some reefs
in large areas, with a mix of coral
recovery and around 2050% mortality, but no
effects in other parts, such as in Oman,
Madagascar, the inner Great Barrier Reef,
parts of Indonesia and the Philippines,
Taiwan, Palau, French Polynesia, the
Galapagos, the Bahamas, Florida, the
Cayman Islands, Bermuda, and Brazil;
- insignificant
or no bleaching in large areas of the
worlds reefs such as the Red Sea,
the southern Indian Ocean, the Andaman
Sea, most of Indonesia, large parts of
the Great Barrier Reef, most of the
central Pacific, and parts of the
southern and eastern Caribbean.
Bleaching and
mortality were most pronounced in shallow water
(less than 15 m) and particularly affected
staghorn and plate Acropora and other fast
growing corals. Many of the massive, slow-growing
species bleached, but many recovered within 1 or
2 months. The consensus is that this is the most
severe bleaching event ever observed, although in
this case there were also more people looking
specifically for bleaching following internet
advice of the location of above average
sea-surface temperatures. More observations and
monitoring are required to determine whether
bleached corals will recover (or die), and
whether damaged reefs have the potential to
bounce back. More importantly, there
is a need for continued observations to determine
whether this is a rare, severe event, or part of
a pattern of increasing disturbance associated
with global climate change.
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