The effect of carbonate chemistry on calcification and photosynthesis in the hermatypic coral Acropora eurystoma

The rise in atmospheric CO2 has caused significant decrease in sea surface pH and carbonate ion (CO32-) concentration. This decrease has a negative effect on calcification in hermatypic corals and other calcifying organisms. We report the results of three laboratory experiments designed specifically to separate the effects of the different carbonate chemistry parameters (pH, CO32-, CO2 [aq], total alkalinity [A(T)], and total inorganic carbon [C-T]) on the calcification, photosynthesis, and respiration of the hermatypic coral Acropora eurystoma. The carbonate system was varied to change pH (7.9-8.5), without changing C-T; C-T was changed keeping the pH constant, and C-T was changed keeping the PCO2 constant. In all of these experiments, calcification (both light and dark) was positively correlated with CO32- concentration, suggesting that the corals are not sensitive to pH or C-T but to the CO32- concentration. A decrease of similar to 30% in the CO32- concentration (which is equivalent to a decrease of about 0.2 pH units in seawater) caused a calcification decrease of about 50%. These results suggest that calcification in today's ocean (pCO(2) = 370 ppm) is lower by similar to 20% compared with preindustrial time (pCO(2) = 280 ppm). An additional decrease of similar to 35% is expected if atmospheric CO2 concentration doubles (pCO(2) = 560 ppm). In all of these experiments, photosynthesis and respiration did not show any significant response to changes in the carbonate chemistry of seawater. Based on this observation, we propose a mechanism by which the photosynthesis of symbionts is enhanced by coral calcification at high pH when CO,(aq) is low. Overall it seems that photosynthesis and calcification support each other mainly through internal pH regulation, which provides CO32- ions for calcification and CO2(aq) for photosynthesis.