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Ohde, Shigeru; Hossain, Mirza M Mozaffar (2004): Seawater carbonate chemistry and calcification during an experiment with a coral Porites lutea, 2004 [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.721879, Supplement to: Ohde, S; Hossain, MMM (2004): Effect of CaCO3 (aragonite) saturation state of seawater on calcification of Porites coral. Geochemical Journal, 38(6), 613-621, https://doi.org/10.2343/geochemj.38.613

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Abstract:
Using living corals collected from Okinawan coral reefs, laboratory experiments were performed to investigate the relationship between coral calcification and aragonite saturation state (W) of seawater at 25 infinity C. Calcification rate of a massive coral Porites lutea cultured in a beaker showed a linear increase with increasing Waragonite values (1.08-7.77) of seawater. The increasing trend of calcification rate (c) for W is expressed as an equation, c = aW + b (a, b: constants). When W was larger than ~4, the coral samples calcified during nighttime, indicating an evidence of dark calcification. This study strongly suggests that calcification of Porites lutea depends on W of ambient seawater. A decrease in saturation state of seawater due to increased pCO2 may decrease reef-building capacity of corals through reducing calcification rate of corals.
Keyword(s):
Animalia; Benthic animals; Benthos; Bottles or small containers/Aquaria (<20 L); Calcification/Dissolution; Cnidaria; Coast and continental shelf; Laboratory experiment; North Pacific; Porites lutea; Single species; Temperate
Funding:
Seventh Framework Programme (FP7), grant/award no. 211384: European Project on Ocean Acidification
Sixth Framework Programme (FP6), grant/award no. 511106: European network of excellence for Ocean Ecosystems Analysis
Event(s):
OH_04 * Method/Device: Experiment (EXP)
Comment:
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).
Parameter(s):
#NameShort NameUnitPrincipal InvestigatorMethod/DeviceComment
1SiteSiteOhde, Shigeru
2Sample IDSample IDOhde, Shigeru
3Date/time startDate/time startOhde, Shigeru
4Date/time endDate/time endOhde, Shigeru
5Temperature, waterTemp°COhde, ShigeruMeasured
6SalinitySalOhde, ShigeruSalinometer (601 MK III, YEO-KAL, Australia)
7Radiation, photosynthetically activePARµmol/m2/sOhde, ShigeruPAR-sensor LI-250, LI-COR Inc.
8Carbonate system computation flagCSC flagNisumaa, Anne-MarinCalculated using seacarb after Nisumaa et al. (2010)
9pHpHOhde, ShigerupH meter (HM-60S, TOA Electronic, Japan)NBS scale
10pHpHNisumaa, Anne-MarinCalculated using seacarb after Nisumaa et al. (2010)Total scale
11Alkalinity, totalATµmol/kgOhde, ShigeruTitration potentiometric
12Carbon, inorganic, dissolvedDICµmol/kgOhde, ShigeruCalculated using CO2SYS
13Carbon dioxideCO2µmol/kgNisumaa, Anne-MarinCalculated using seacarb after Nisumaa et al. (2010)
14Carbonate ion[CO3]2-µmol/kgNisumaa, Anne-MarinCalculated using seacarb after Nisumaa et al. (2010)
15Bicarbonate ion[HCO3]-µmol/kgNisumaa, Anne-MarinCalculated using seacarb after Nisumaa et al. (2010)
16Partial pressure of carbon dioxide (water) at sea surface temperature (wet air)pCO2water_SST_wetµatmNisumaa, Anne-MarinCalculated using seacarb after Nisumaa et al. (2010)
17Fugacity of carbon dioxide (water) at sea surface temperature (wet air)fCO2water_SST_wetµatmNisumaa, Anne-MarinCalculated using seacarb after Nisumaa et al. (2010)
18Aragonite saturation stateOmega ArgNisumaa, Anne-MarinCalculated using seacarb after Nisumaa et al. (2010)
19Calcite saturation stateOmega CalNisumaa, Anne-MarinCalculated using seacarb after Nisumaa et al. (2010)
20Calcification rate of calcium carbonateCalc rate CaCO3µmol/cm2/hOhde, ShigeruAlkalinity anomaly technique (Smith and Key, 1975)
Status:
Curation Level: Enhanced curation (CurationLevelC)
Size:
920 data points

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