Euechinoidea and Cidaroidea respond differently to ocean acidification, supplement to: Collard, Marie; Dery, Aurélie; Dehairs, Frank; Dubois, Philippe (2014): Euechinoidea and Cidaroidea respond differently to ocean acidification. Comparative Biochemistry and Physiology Part A: Molecular & Integrative Physiology, 174, 45-55

• Main Authors: Collard, Marie, Dery, Aurélie, Dehairs, Frank, Dubois, Philippe
• Format: Dataset
• Language: English
• Published: PANGAEA - Data Publisher for Earth & Environmental Science 2014
• Subjects: 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; Species; pH; Aquarium number; Time point, descriptive; Identification; Coelomic fluid, pH; Difference; Coelomic fluid, alkalinity; Alkalinity, total; Comment; Coelomic fluid, carbon, inorganic, dissolved; Carbon, inorganic, dissolved; δ13C, Coelomic fluid; δ13C; Feeding rate per individual; Temperature, water; Salinity; Partial pressure of carbon dioxide water at sea surface temperature wet air; Carbon dioxide; Bicarbonate ion; Carbonate ion; Calcite saturation state; Aragonite saturation state; Carbonate system computation flag; Fugacity of carbon dioxide water at sea surface temperature wet air; Potentiometric; Calculated; Potentiometric titration; Isotope ratio mass spectrometry; Calculated using CO2SYS; Calculated using seacarb after Nisumaa et al. 2010; Ocean Acidification International Coordination Centre OA-ICC; Collard; DuBois; Ocean acidification
• Online Access: https://dx.doi.org/10.1594/pangaea.835967; https://doi.pangaea.de/10.1594/PANGAEA.835967

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. : 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.