Seawater carbonate chemistry and calcification during experiments with coral communities, 2000, supplement to: Leclercq, Nicolas; Gattuso, Jean-Pierre; Jaubert, Jean (2000): CO2 partial pressure controls the calcification rate of a coral community. Global Change Biology, 6(3), 329-334

• Main Authors: Leclercq, Nicolas, Gattuso, Jean-Pierre, Jaubert, Jean
• Format: Dataset
• Language: English
• Published: PANGAEA - Data Publisher for Earth & Environmental Science 2000
• Subjects: Benthos; Calcification/Dissolution; Containers and aquaria 20-1000 L or < 1 m**2; Entire community; Laboratory experiment; Not applicable; Rocky-shore community; Experimental treatment; Salinity; Temperature, water; Partial pressure of carbon dioxide water at sea surface temperature wet air; Aragonite saturation state; Calcification rate of calcium carbonate; Carbonate ion; Carbonate system computation flag; pH; Carbon dioxide; Fugacity of carbon dioxide water at sea surface temperature wet air; Bicarbonate ion; Carbon, inorganic, dissolved; Alkalinity, total; Calcite saturation state; extracted from figure using GraphClick; Calculated using seacarb after Nisumaa et al. 2010; European network of excellence for Ocean Ecosystems Analysis EUR-OCEANS; European Project on Ocean Acidification EPOCA; Ocean Acidification International Coordination Centre OA-ICC; Ocean acidification
• Online Access: https://dx.doi.org/10.1594/pangaea.756651; https://doi.pangaea.de/10.1594/PANGAEA.756651

Previous studies have demonstrated that coral and algal calcification is tightly regulated by the calcium carbonate saturation state of seawater. This parameter is likely to decrease in response to the increase of dissolved CO2 resulting from the global increase of the partial pressure of atmospheric CO2. We have investigated the response of a coral reef community dominated by scleractinian corals, but also including other calcifying organisms such as calcareous algae, crustaceans, gastropods and echinoderms, and kept in an open-top mesocosm. Seawater pCO2 was modified by manipulating the pCO2 of air used to bubble the mesocosm. The aragonite saturation state (omega arag) of the seawater in the mesocosm varied between 1.3 and 5.4. Community calcification decreased as a function of increasing pCO2 and decreasing omega arag. This result is in agreement with previous data collected on scleractinian corals, coralline algae and in a reef mesocosm, even though some of these studies did not manipulate CO2 directly. Our data suggest that the rate of calcification during the last glacial maximum might have been 114% of the preindustrial rate. Moreover, using the average emission scenario (IS92a) of the Intergovernmental Panel on Climate Change, we predict that the calcification rate of scleractinian-dominated communities may decrease by 21% between the pre-industrial period (year 1880) and the time at which pCO2 will double (year 2065). : Caution! Values are not truly measured! In order to allow full comparability with other ocean acidification data sets, the R package seacarb (Lavigne and Gattuso, 2011) was used to compute a complete and consistent set of carbonate system variables, as described by Nisumaa et al. (2010). In this dataset the original values were archived in addition with the recalculated parameters (see related PI).Note that CO3 data was calculated from omega aragonite, solubility product of aragonite (Karag) and Ca concentration following: CO3=omega*Karag/Ca. Where the Karag=7.16*10**-7.Omega aragonite and calcification rate were digitized from scanned figure 1 using software GraphClick (http://www.arizona-software.ch).