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Collard, Marie; Dery, Aurélie; Dehairs, Frank; Dubois, Philippe (2014): Euechinoidea and Cidaroidea respond differently to ocean acidification [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.835967, Supplement to: Collard, M et al. (2014): Euechinoidea and Cidaroidea respond differently to ocean acidification. Comparative Biochemistry and Physiology Part A: Molecular & Integrative Physiology, 174, 45-55, https://doi.org/10.1016/j.cbpa.2014.04.011

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Abstract:
The impact of the chemical changes in the ocean waters due to the increasing atmospheric CO2 depends on the ability of an organism to control extracellular pH. Among sea urchins, this seems specific to the Euechinoidea, sea urchins except Cidaroidea. However, Cidaroidea survived two ocean acidification periods: the Permian-Trias and the Cretaceous-Tertiary crises. We investigated the response of these two sea urchin groups to reduced seawater pH with the tropical cidaroid Eucidaris tribuloides, the sympatric euechinoid Tripneustes ventricosus and the temperate euechinoid Paracentrotus lividus. Both euechinoid showed a compensation of the coelomic fluid pH due to increased buffer capacity. This was linked to an increased concentration of DIC in the coelomic fluid and thus of bicarbonate ions (most probably originating from the surrounding seawater as isotopic signature of the carbon -delta 13C- was similar). On the other hand, the cidaroid showed no changes within the coelomic fluid. Moreover, the delta 13C of the coelomic fluid did not match that of the seawater and was not significantly different between the urchins from the different treatments. Feeding rate was not affected in any species. While euechinoids are able to regulate their extracellular acid-base balance, many questions are still unanswered on the costs of this capacity. On the contrary, cidaroids do not seem affected by a reduced seawater pH. Further investigations need to be undertaken to cover more species and physiological and metabolic parameters in order to determine if energy trade-offs occur and how this mechanism of compensation is distributed among sea urchins.
Keyword(s):
Acid-base regulation; Animalia; Behaviour; Benthic animals; Benthos; Coast and continental shelf; Containers and aquaria (20-1000 L or < 1 m**2); Echinodermata; Eucidaris tribuloides; Laboratory experiment; North Atlantic; Paracentrotus lividus; Single species; Tripneustes ventricosus; 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 2014-09-13.
Parameter(s):
#NameShort NameUnitPrincipal InvestigatorMethod/DeviceComment
1SpeciesSpeciesCollard, Marie
2pHpHCollard, Marienominal, total scale
3Aquarium numberAquariumCollard, Marie
4Time point, descriptiveTime pointCollard, Marieexposure day
5IdentificationIDCollard, Marieurchin
6Coelomic fluid, pHpH (cf)Collard, MariePotentiometrictotal scale
7pHpHCollard, MariePotentiometrictotal scale, mean seawater
8DifferenceDiffCollard, MarieCalculatedpH, total scale
9Coelomic fluid, alkalinityAT (cf)µmol/kgCollard, MariePotentiometric titration
10Alkalinity, totalATµmol/kgCollard, MariePotentiometric titrationseawater
11DifferenceDiffCollard, MarieCalculatedalkalinity, total
12CommentCommentCollard, Marieurchin combination
13Coelomic fluid, carbon, inorganic, dissolvedDIC (cf)mmol/lCollard, MarieIsotope ratio mass spectrometry
14Carbon, inorganic, dissolvedDICmmol/lCollard, MarieIsotope ratio mass spectrometryseawater
15DifferenceDiffCollard, MarieCalculatedcarbon, inorganic, dissolved
16δ13C, Coelomic fluidδ13C (cf)‰ PDBCollard, MarieIsotope ratio mass spectrometry
17δ13Cδ13C‰ PDBCollard, MarieIsotope ratio mass spectrometryseawater
18Feeding rate per individualFeed rate/ind#/#/dayCollard, Mariepellets per individual per day
19Temperature, waterTemp°CCollard, Marie
20SalinitySalCollard, Marie
21pHpHCollard, MariePotentiometrictotal scale
22Alkalinity, totalATµmol/kgCollard, MariePotentiometric titration
23Carbon, inorganic, dissolvedDICµmol/kgCollard, MarieIsotope ratio mass spectrometry
24Partial pressure of carbon dioxide (water) at sea surface temperature (wet air)pCO2water_SST_wetµatmCollard, MarieCalculated using CO2SYS
25Carbon dioxideCO2µmol/kgCollard, MarieCalculated using CO2SYS
26Bicarbonate ion[HCO3]-µmol/kgCollard, MarieCalculated using CO2SYS
27Carbonate ion[CO3]2-µmol/kgCollard, MarieCalculated using CO2SYS
28Calcite saturation stateOmega CalCollard, MarieCalculated using CO2SYS
29Aragonite saturation stateOmega ArgCollard, MarieCalculated using CO2SYS
30Carbonate system computation flagCSC flagYang, YanCalculated using seacarb after Nisumaa et al. (2010)
31Carbon dioxideCO2µmol/kgYang, YanCalculated using seacarb after Nisumaa et al. (2010)
32Partial pressure of carbon dioxide (water) at sea surface temperature (wet air)pCO2water_SST_wetµatmYang, YanCalculated using seacarb after Nisumaa et al. (2010)
33Fugacity of carbon dioxide (water) at sea surface temperature (wet air)fCO2water_SST_wetµatmYang, YanCalculated using seacarb after Nisumaa et al. (2010)
34Bicarbonate ion[HCO3]-µmol/kgYang, YanCalculated using seacarb after Nisumaa et al. (2010)
35Carbonate ion[CO3]2-µmol/kgYang, YanCalculated using seacarb after Nisumaa et al. (2010)
36Carbon, inorganic, dissolvedDICµmol/kgYang, YanCalculated using seacarb after Nisumaa et al. (2010)
37Aragonite saturation stateOmega ArgYang, YanCalculated using seacarb after Nisumaa et al. (2010)
38Calcite saturation stateOmega CalYang, YanCalculated using seacarb after Nisumaa et al. (2010)
Status:
Curation Level: Enhanced curation (CurationLevelC)
Size:
13257 data points

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