The responses of eight coral reef calcifiers to increasing partial pressure of CO2 do not exhibit a tipping point

• Main Authors: Comeau, Steeve, Edmunds, Peter J, Spindel, N B, Carpenter, Robert C
• Format: Dataset
• Language: English
• Published: PANGAEA 2013
• Subjects: Acropora pulchra; Alkalinity; total; Animalia; Aragonite saturation state; Benthic animals; Benthos; Bicarbonate ion; Buoyant weighing technique (Davies; 1989); Calcification/Dissolution; Calcification rate of calcium carbonate; Calcite saturation state; Calculated using seacarb after Nisumaa et al. (2010); Carbon; inorganic; dissolved; Carbonate ion; Carbonate system computation flag; Carbon dioxide; Chlorophyta; Cnidaria; Coast and continental shelf; Containers and aquaria (20-1000 L or < 1 m**2); Date/time end; Date/time start; Fugacity of carbon dioxide (water) at sea surface temperature (wet air); Halimeda macroloba; Halimeda minima; Hydrolithon reinboldii; Laboratory experiment; Lithophyllum flavescens; Macroalgae; OA-ICC; Ocean Acidification International Coordination Centre; Partial pressure of carbon dioxide (water) at sea surface temperature (wet air); Pavona cactus; pH; Plantae; Pocillopora damicornis; Porites rus; Potentiometric; Potentiometric titration; Rhodophyta; Salinity; Single species; South Pacific; Species; Temperature; water; Pacific; Rus’; Ocean acidification
• Online Access: https://doi.pangaea.de/10.1594/PANGAEA.833687; https://doi.org/10.1594/PANGAEA.833687

The objective of this study was to investigate whether a tipping point exists in the calcification responses of coral reef calcifiers to CO2. We compared the effects of six partial pressures of CO2 (PCO2) from 28 Pa to 210 Pa on the net calcification of four corals (Acropora pulchra, Porites rus, Pocillopora damicornis, and Pavona cactus), and four calcified algae (Hydrolithon onkodes, Lithophyllum flavescens, Halimeda macroloba, and Halimeda minima). After 2 weeks of acclimation in a common environment, organisms were incubated in 12 aquaria for 2 weeks at the targeted PCO2 levels and net calcification was quantified. All eight species calcified at the highest PCO2 in which the calcium carbonate aragonite saturation state was ~1. Calcification decreased linearly as a function of increasing partial PCO2 in three corals and three algae. Overall, the decrease in net calcification as a function of decreasing pH was ~10% when ambient PCO2 (39 Pa) was doubled. The calcification responses of P. damicornis and H. macroloba were unaffected by increasing PCO2. These results are inconsistent with the notion that coral reefs will be affected by rising PCO2 in a response characterized by a tipping point. Instead, our findings combined among taxa suggest a gradual decline in calcification will occur, but this general response includes specific cases of complete resistance to rising PCO2. Together our results suggest that the overall response of coral reef communities to ocean acidification will be monotonic and inversely proportional to PCO2, with reef-wide responses dependent on the species composition of calcifying taxa.