Calcification rates in stony corals are expected to decline significantly in the near future due to ocean acidification. In this study we provide a global estimate of the decline in calcification of coral reefs as a result of increase in sea surface temperature and partial pressure of CO 2 . This estimate, unlike previously reported estimates, is based on an empirical rate law developed from field observations for gross community calcification as a function of aragonite degree of saturation (Ω arag ), sea surface temperature and live coral cover. Calcification rates were calculated for more than 9,000 reef locations using model values of Ω arag and sea surface temperature at different levels of atmospheric CO 2 . The maps we produced show that by the time atmospheric partial pressure of CO 2 will reach 560 ppm all coral reefs will cease to grow and start to dissolve.
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Silverman et al. (2009) studied this question.
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