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Shaw, Emily; Carpenter, Robert C; Lantz, Coulson A; Edmunds, Peter J (2016): Seawater carbonate chemistry and calcification of scleractinian coral Acropora pulchra [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.956287

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Abstract:
Studies of coral colonies show that ocean acidification and temperature can affect calcification; however, less is known about the consequences for their populations. Understanding intraspecific variation in the response of corals to these conditions will be important for evaluating population-level consequences of environmental change. We examined intraspecific variability in the effects of elevated temperature and carbon dioxide levels on net calcification (Gn) in the coral Acropora pulchra in Moorea, French Polynesia. A common garden experiment showed that Gn in four colonies was affected negatively by high partial pressure of CO2 (pCO2) (1000 μatm cf. 400 μatm ambient conditions), whereas elevated temperature (30 °C cf. 27 °C) had a negative effect on one colony. Together, these results reveal intraspecific variation in the response of Gn to temperature but not to pCO2. The fastest growing colonies under ambient temperature and ambient pCO2 showed the greatest decline in Gn at high temperature and elevated pCO2. For reef corals, effects of temperature and pCO2 on calcification that depend on the intrinsic growth rate have potentially important consequences, because they imply that coral colonies contributing the most to population-level calcification will be disproportionately affected by changing environmental conditions.
Keyword(s):
Acropora pulchra; Animalia; Benthic animals; Benthos; Calcification/Dissolution; Cnidaria; Coast and continental shelf; Containers and aquaria (20-1000 L or < 1 m**2); Laboratory experiment; Single species; South Pacific; Temperature; Tropical
Supplement to:
Shaw, Emily; Carpenter, Robert C; Lantz, Coulson A; Edmunds, Peter J (2016): Intraspecific variability in the response to ocean warming and acidification in the scleractinian coral Acropora pulchra. Marine Biology, 163(10), 210, https://doi.org/10.1007/s00227-016-2986-8
Original version:
Edmunds, Peter J; Carpenter, Robert C (2023): Calcification rates of Acropora pulchra in ambient and elevated temperature and pCO2 conditions sampled during experiments at Richard B Gump Research Station, Moorea, French Polynesia from Oct to Nov of 2015. (Version 1) Version Date 2017-03-20. [access date: 2023-03-10]. Biological and Chemical Oceanography Data Management Office (BCO-DMO), https://doi.org/10.26008/1912/bco-dmo.684594.1
Edmunds, Peter J; Carpenter, Robert C (2023): Calcification rates of Acropora pulchra under two pCO2 levels and two temperatures sampled during experiments at Richard B Gump Research Station, Moorea, French Polynesia in July of 2015. (Version 1) Version Date 2017-03-20. [access date: 2023-03-10]. Biological and Chemical Oceanography Data Management Office (BCO-DMO), https://doi.org/10.26008/1912/bco-dmo.684581.1
Edmunds, Peter J; Carpenter, Robert C (2023): Carbonate chemistry sampled during Acropora pulchra calcification experiments that took place in Moorea, French Polynesia from Jul to Nov of 2015. (Version 1) Version Date 2017-03-20. [access date: 2023-03-10]. Biological and Chemical Oceanography Data Management Office (BCO-DMO), https://doi.org/10.26008/1912/bco-dmo.684605.1
Documentation:
Gattuso, Jean-Pierre; Epitalon, Jean-Marie; Lavigne, Héloïse; Orr, James (2021): seacarb: seawater carbonate chemistry with R. R package version 3.2.16. https://cran.r-project.org/web/packages/seacarb/index.html
Coverage:
Latitude: -17.490700 * Longitude: -149.826000
Event(s):
Moorea_coral * Latitude: -17.490700 * Longitude: -149.826000 * Method/Device: Experiment (EXP)
Comment:
In order to allow full comparability with other ocean acidification data sets, the R package seacarb (Gattuso et al, 2021) 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 by seacarb is 2023-03-08.
Parameter(s):
#NameShort NameUnitPrincipal InvestigatorMethod/DeviceComment
1TypeTypeEdmunds, Peter JStudy
2Species, unique identificationSpecies UIDEdmunds, Peter J
3Species, unique identification (URI)Species UID (URI)Edmunds, Peter J
4Species, unique identification (Semantic URI)Species UID (Semantic URI)Edmunds, Peter J
5ExperimentExpEdmunds, Peter J
6SiteSiteEdmunds, Peter J
7LATITUDELatitudeEdmunds, Peter JGeocode
8LONGITUDELongitudeEdmunds, Peter JGeocode
9GenotypeGenotypeEdmunds, Peter J
10IdentificationIDEdmunds, Peter Jtank
11TreatmentTreatEdmunds, Peter J
12Treatment: temperatureT:temp°CEdmunds, Peter J
13Calcification rate of calcium carbonateCalc rate CaCO3mg/cm2/dayEdmunds, Peter J
14Sample IDSample IDEdmunds, Peter J
15SalinitySalEdmunds, Peter J
16Temperature, waterTemp°CEdmunds, Peter J
17pHpHEdmunds, Peter Jtotal scale
18Alkalinity, totalATµmol/kgEdmunds, Peter J
19Carbonate system computation flagCSC flagYang, YanCalculated using seacarb after Nisumaa et al. (2010)
20Carbon dioxideCO2µmol/kgYang, YanCalculated using seacarb after Nisumaa et al. (2010)
21Partial pressure of carbon dioxide (water) at sea surface temperature (wet air)pCO2water_SST_wetµatmYang, YanCalculated using seacarb after Nisumaa et al. (2010)
22Fugacity of carbon dioxide (water) at sea surface temperature (wet air)fCO2water_SST_wetµatmYang, YanCalculated using seacarb after Nisumaa et al. (2010)
23Bicarbonate ion[HCO3]-µmol/kgYang, YanCalculated using seacarb after Nisumaa et al. (2010)
24Carbonate ion[CO3]2-µmol/kgYang, YanCalculated using seacarb after Nisumaa et al. (2010)
25Carbon, inorganic, dissolvedDICµmol/kgYang, YanCalculated using seacarb after Nisumaa et al. (2010)
26Aragonite saturation stateOmega ArgYang, YanCalculated using seacarb after Nisumaa et al. (2010)
27Calcite saturation stateOmega CalYang, YanCalculated using seacarb after Nisumaa et al. (2010)
Status:
Curation Level: Enhanced curation (CurationLevelC)
Size:
4948 data points

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