Leclercq, Nicolas; Gattuso, Jean-Pierre; Jaubert, Jean (2000): Seawater carbonate chemistry and calcification during experiments with coral communities, 2000 [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.756651, Supplement to: Leclercq, N et al. (2000): CO2 partial pressure controls the calcification rate of a coral community. Global Change Biology, 6(3), 329-334, https://doi.org/10.1046/j.1365-2486.2000.00315.x
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Abstract:
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).
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Funding:
Sixth Framework Programme (FP6), grant/award no. 511106: European network of excellence for Ocean Ecosystems Analysis
Comment:
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).
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License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Status:
Curation Level: Enhanced curation (CurationLevelC)
Size:
1360 data points