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Tynan, Sarah; Opdyke, Bradley N (2011): Seawater carbonate chemistry and community calcification near Lizar Island, 2011 [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.763348, Supplement to: Tynan, S; Opdyke, BN (2011): Effects of lower surface ocean pH upon the stability of shallow water carbonate sediments. Science of the Total Environment, 409(6), 1082-1086, https://doi.org/10.1016/j.scitotenv.2010.12.007

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Abstract:
It is predicted that surface ocean pH will reach 7.9, possibly 7.8 by the end of this century due to increased carbon dioxide (CO2) in the atmosphere and in the surface ocean. While aragonite-rich sediments don't begin to dissolve until a threshold pH of ~ 7.8 is reached, dissolution from high-Mg calcites is evident with any drop in pH. Indeed, it is high-Mg calcite that dominates the reaction of carbonate sediments with increased CO2, which undergoes a rapid neomorphism process to a more stable, low-Mg calcite. This has major implications for the future of the high-Mg calcite producing organisms within coral reef ecosystems. In order to understand any potential buffering system offered by the dissolution of carbonate sediments under a lower oceanic pH, this process of high-Mg calcite dissolution in the reef environment must be further elucidated.
Keyword(s):
Benthos; Bottles or small containers/Aquaria (<20 L); Calcification/Dissolution; Coast and continental shelf; Entire community; Laboratory experiment; Rocky-shore community; South Pacific; Tropical
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
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
1IdentificationIDTynan, Sarah
2SiteSiteTynan, Sarah
3Sample IDSample IDTynan, Sarah
4Time of dayTime of dayTynan, Sarah
5Incubation durationInc durhTynan, Sarah
6SalinitySalTynan, Sarah
7Temperature, waterTemp°CTynan, Sarah
8pHpHTynan, SarahMeasuredNBS/NIST scale
9CalciumCa2+mg/kgTynan, SarahVarian Vista Pro Inductively Coupled Plasma Atomic Emission Spectrometer
10MagnesiumMg2+mg/kgTynan, SarahVarian Vista Pro Inductively Coupled Plasma Atomic Emission Spectrometer
11Alkalinity, totalATµmol/kgTynan, SarahMetrohm Titrando titrator
12Δ alkalinity, totalΔ ATTynan, Sarah
13Calcification rate of calcium carbonateCalc rate CaCO3µmol/cm2/hTynan, SarahAlkalinity anomaly technique (Smith and Key, 1975)
14Carbon, inorganic, dissolvedDICµmol/kgTynan, SarahCalculated using CO2SYS
15Carbonate system computation flagCSC flagNisumaa, Anne-MarinCalculated using seacarb after Nisumaa et al. (2010)
16pHpHNisumaa, Anne-MarinCalculated using seacarb after Nisumaa et al. (2010)Total scale
17Carbon dioxideCO2µmol/kgNisumaa, Anne-MarinCalculated using seacarb after Nisumaa et al. (2010)
18Partial pressure of carbon dioxide (water) at sea surface temperature (wet air)pCO2water_SST_wetµatmNisumaa, Anne-MarinCalculated using seacarb after Nisumaa et al. (2010)
19Fugacity of carbon dioxide (water) at sea surface temperature (wet air)fCO2water_SST_wetµatmNisumaa, Anne-MarinCalculated using seacarb after Nisumaa et al. (2010)
20Bicarbonate ion[HCO3]-µmol/kgNisumaa, Anne-MarinCalculated using seacarb after Nisumaa et al. (2010)
21Carbonate ion[CO3]2-µmol/kgNisumaa, Anne-MarinCalculated using seacarb after Nisumaa et al. (2010)
22Aragonite saturation stateOmega ArgNisumaa, Anne-MarinCalculated using seacarb after Nisumaa et al. (2010)
23Calcite saturation stateOmega CalNisumaa, Anne-MarinCalculated using seacarb after Nisumaa et al. (2010)
Status:
Curation Level: Enhanced curation (CurationLevelC)
Size:
2353 data points

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