Reef corals and the communities they form evidently possess effective mecha
nisms of adaptation and acclimation that have ensured their survival and re
currence over geologic time, Current reef degradation suggests that these m
echanisms are being taxed beyond their limits; understanding of the problem
is hampered by serious inadequacies in our understanding of physiological
stress responses, the range and implications of reproductive strategies, an
d the mechanisms of calcification and algal symbiosis, Reef community and p
opulation responses to environmental change appear substantially different
on different time scales, and a combination of short-term perspectives and
definitional confusion complicates interpretation and prediction of reef re
sponses. Calcium carbonate saturation state is now recognized as a potentia
lly important control of reef calcification, which means that rising atmosp
heric CO2 represents a direct threat to reef ecosystems on a global scale.