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
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 acidificat...
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Format: | Dataset |
Language: | English |
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PANGAEA - Data Publisher for Earth & Environmental Science
2014
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Online Access: | https://dx.doi.org/10.1594/pangaea.835967 https://doi.pangaea.de/10.1594/PANGAEA.835967 |
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ftdatacite:10.1594/pangaea.835967 |
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record_format |
openpolar |
institution |
Open Polar |
collection |
DataCite Metadata Store (German National Library of Science and Technology) |
op_collection_id |
ftdatacite |
language |
English |
topic |
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 |
spellingShingle |
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, Marie Dery, Aurélie Dehairs, Frank Dubois, Philippe 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 |
topic_facet |
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 |
description |
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. |
format |
Dataset |
author |
Collard, Marie Dery, Aurélie Dehairs, Frank Dubois, Philippe |
author_facet |
Collard, Marie Dery, Aurélie Dehairs, Frank Dubois, Philippe |
author_sort |
Collard, Marie |
title |
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 |
title_short |
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 |
title_full |
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 |
title_fullStr |
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 |
title_full_unstemmed |
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 |
title_sort |
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 |
publisher |
PANGAEA - Data Publisher for Earth & Environmental Science |
publishDate |
2014 |
url |
https://dx.doi.org/10.1594/pangaea.835967 https://doi.pangaea.de/10.1594/PANGAEA.835967 |
long_lat |
ENVELOPE(31.117,31.117,-72.633,-72.633) ENVELOPE(-67.166,-67.166,-66.266,-66.266) |
geographic |
Collard DuBois |
geographic_facet |
Collard DuBois |
genre |
North Atlantic Ocean acidification |
genre_facet |
North Atlantic Ocean acidification |
op_relation |
https://cran.r-project.org/package=seacarb https://dx.doi.org/10.1016/j.cbpa.2014.04.011 https://cran.r-project.org/package=seacarb |
op_rights |
Creative Commons Attribution 3.0 Unported https://creativecommons.org/licenses/by/3.0/legalcode cc-by-3.0 |
op_rightsnorm |
CC-BY |
op_doi |
https://doi.org/10.1594/pangaea.835967 https://doi.org/10.1016/j.cbpa.2014.04.011 |
_version_ |
1766137169354686464 |
spelling |
ftdatacite:10.1594/pangaea.835967 2023-05-15T17:37:19+02:00 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 Collard, Marie Dery, Aurélie Dehairs, Frank Dubois, Philippe 2014 text/tab-separated-values https://dx.doi.org/10.1594/pangaea.835967 https://doi.pangaea.de/10.1594/PANGAEA.835967 en eng PANGAEA - Data Publisher for Earth & Environmental Science https://cran.r-project.org/package=seacarb https://dx.doi.org/10.1016/j.cbpa.2014.04.011 https://cran.r-project.org/package=seacarb Creative Commons Attribution 3.0 Unported https://creativecommons.org/licenses/by/3.0/legalcode cc-by-3.0 CC-BY 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 Supplementary Dataset dataset Dataset 2014 ftdatacite https://doi.org/10.1594/pangaea.835967 https://doi.org/10.1016/j.cbpa.2014.04.011 2021-11-05T12:55:41Z 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. Dataset North Atlantic Ocean acidification DataCite Metadata Store (German National Library of Science and Technology) Collard ENVELOPE(31.117,31.117,-72.633,-72.633) DuBois ENVELOPE(-67.166,-67.166,-66.266,-66.266) |