Coral reef bleaching, the whitening of diverse invertebrate taxa, resu
lts from the loss of symbiotic zooxanthellae and/or a reduction in pho
tosynthetic pigment concentrations in zooxanthellae residing within th
e gastrodermal tissues of host animals. Of particular concern are the
consequences of bleaching of large numbers of reef-building scleractin
ian corals and hydrocorals. Published records of coral reef bleaching
events from 1870 to the present suggest that the frequency (60 major e
vents from 1979 to 1990), scale (co-occurrence in many coral reef regi
ons and often over the bathymetric depth range of corals) and severity
(> 95% mortality in some areas) of recent bleaching disturbances are
unprecedented in the scientific literature. The causes of small scale,
isolated bleaching events can often be explained by particular stress
ors (e.g., temperature, salinity, light, sedimentation, aerial exposur
e and pollutants), but attempts to explain large scale bleaching event
s in terms of possible global change (e.g., greenhouse warming, increa
sed UV radiation flux, deteriorating ecosystem health, or some combina
tion of the above) have not been convincing. Attempts to relate the se
verity and extent of large scale coral reef bleaching events to partic
ular causes have been hampered by a lack of (a) standardized methods t
o assess bleaching and (b) continuous, long-term data bases of environ
mental conditions over the periods of interest. An effort must be made
to understand the impact of bleaching on the remainder of the reef co
mmunity and the long-term effects on competition, predation, symbioses
, bioerosion and substrate condition, all factors that can influence c
oral recruitment and reef recovery. If projected rates of sea warming
are realized by mid to late AD 2000, i.e. a 2-degrees-C increase in hi
gh latitude coral seas, the upper thermal tolerance limits of many ree
f-building corals could be exceeded. Present evidence suggests that ma
ny corals would be unable to adapt physiologically or genetically to s
uch marked and rapid temperature in creases.