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Cyronak, Tyler; Santos, Isaac R; Eyre, Bradley D (2013): Permeable coral reef sediment dissolution driven by elevated pCO2 and pore water advection [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.833970, Supplement to: Cyronak, T et al. (2013): Permeable coral reef sediment dissolution driven by elevated pCO2 and pore water advection. Geophysical Research Letters, 40(18), 4876–4881, https://doi.org/10.1002/grl.50948

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Abstract:
Ocean acidification (OA) is expected to drive the transition of coral reef ecosystems from net calcium carbonate (CaCO3) precipitating to net dissolving within the next century. Although permeable sediments represent the largest reservoir of CaCO3 in coral reefs, the dissolution of shallow CaCO3 sands under future pCO2 levels has not been measured under natural conditions. In situ, advective chamber incubations under elevated pCO2 (~800 µatm) shifted the sediments from net precipitating to net dissolving. Pore water advection more than doubled dissolution rates (1.10 g CaCO3/m**2/day) when compared to diffusive conditions (0.42 g CaCO3/m**2 /day). Sediment dissolution could reduce net ecosystem calcification rates of the Heron Island lagoon by 8% within the next century, which is equivalent to a 25% reduction in the global average calcification rate of coral lagoons. The dissolution of CaCO3 sediments needs to be taken into account in order to address how OA will impact the net accretion of coral reefs under future predicted increases in CO2.
Keyword(s):
Benthos; Bottles or small containers/Aquaria (<20 L); Calcification/Dissolution; Coast and continental shelf; Entire community; Field experiment; Rocky-shore community; South Pacific; Tropical
Further details:
Lavigne, Héloïse; Epitalon, Jean-Marie; Gattuso, Jean-Pierre (2014): seacarb: seawater carbonate chemistry with R. R package version 3.0. https://cran.r-project.org/package=seacarb
Comment:
In order to allow full comparability with other ocean acidification data sets, the R package seacarb (Lavigne et al, 2014) 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). The date of carbonate chemistry calculation is 2014-07-11.
Parameter(s):
#NameShort NameUnitPrincipal InvestigatorMethod/DeviceComment
1IdentificationIDCyronak, Tyler
2TreatmentTreatCyronak, Tyler
3Oxygen, fluxO2 fluxmmol/m2/hCyronak, Tylernight
4Alkalinity, total, fluxAT fluxmmol(eq)/m2/hCyronak, Tylernight
5Oxygen, fluxO2 fluxmmol/m2/hCyronak, Tylerday
6Alkalinity, total, fluxAT fluxmmol(eq)/m2/hCyronak, Tylerday
7Oxygen, fluxO2 fluxmmol/m2/dayCyronak, Tylernet
8Alkalinity, total, fluxAT fluxmmol(eq)/m2/dayCyronak, Tylernet
9pHpHCyronak, TylerPotentiometricNBS scale
10Partial pressure of carbon dioxide (water) at sea surface temperature (wet air)pCO2water_SST_wetµatmCyronak, TylerCalculated using CO2SYS
11Aragonite saturation stateOmega ArgCyronak, TylerCalculated using CO2SYS
12SalinitySalCyronak, Tyler
13Temperature, waterTemp°CCyronak, Tyler
14Alkalinity, totalATµmol/kgCyronak, TylerPotentiometric titration
15Carbonate system computation flagCSC flagYang, YanCalculated using seacarb after Nisumaa et al. (2010)
16pHpHYang, YanCalculated using seacarb after Nisumaa et al. (2010)total scale
17Carbon dioxideCO2µmol/kgYang, YanCalculated using seacarb after Nisumaa et al. (2010)
18Partial pressure of carbon dioxide (water) at sea surface temperature (wet air)pCO2water_SST_wetµatmYang, YanCalculated using seacarb after Nisumaa et al. (2010)
19Fugacity of carbon dioxide (water) at sea surface temperature (wet air)fCO2water_SST_wetµatmYang, YanCalculated using seacarb after Nisumaa et al. (2010)
20Bicarbonate ion[HCO3]-µmol/kgYang, YanCalculated using seacarb after Nisumaa et al. (2010)
21Carbonate ion[CO3]2-µmol/kgYang, YanCalculated using seacarb after Nisumaa et al. (2010)
22Carbon, inorganic, dissolvedDICµmol/kgYang, YanCalculated using seacarb after Nisumaa et al. (2010)
23Aragonite saturation stateOmega ArgYang, YanCalculated using seacarb after Nisumaa et al. (2010)
24Calcite saturation stateOmega CalYang, YanCalculated using seacarb after Nisumaa et al. (2010)
Status:
Curation Level: Enhanced curation (CurationLevelC)
Size:
552 data points

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