Euechinoidea and Cidaroidea respond differently to ocean acidification
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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ftpangaea:oai:pangaea.de:doi:10.1594/PANGAEA.835967 2024-09-15T18:24:28+00:00 Euechinoidea and Cidaroidea respond differently to ocean acidification Collard, Marie Dery, Aurélie Dehairs, Frank Dubois, Philippe 2014 text/tab-separated-values, 13257 data points https://doi.pangaea.de/10.1594/PANGAEA.835967 https://doi.org/10.1594/PANGAEA.835967 en eng PANGAEA Lavigne, Héloïse; Epitalon, Jean-Marie; Gattuso, Jean-Pierre (2014): seacarb: seawater carbonate chemistry with R. R package version 3.0 [webpage]. https://cran.r-project.org/package=seacarb https://doi.pangaea.de/10.1594/PANGAEA.835967 https://doi.org/10.1594/PANGAEA.835967 CC-BY-3.0: Creative Commons Attribution 3.0 Unported Access constraints: unrestricted info:eu-repo/semantics/openAccess 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, https://doi.org/10.1016/j.cbpa.2014.04.011 Acid-base regulation Alkalinity total Animalia Aquarium number Aragonite saturation state Behaviour Benthic animals Benthos Bicarbonate ion Calcite saturation state Calculated Calculated using CO2SYS Calculated using seacarb after Nisumaa et al. (2010) Carbon inorganic dissolved Carbonate ion Carbonate system computation flag Carbon dioxide Coast and continental shelf Coelomic fluid pH Comment Containers and aquaria (20-1000 L or < 1 m**2) Difference Echinodermata Eucidaris tribuloides Feeding rate per individual Fugacity of carbon dioxide (water) at sea surface temperature (wet air) Identification Isotope ratio mass spectrometry Laboratory experiment North Atlantic OA-ICC Ocean Acidification International Coordination Centre Paracentrotus lividus Partial pressure of carbon dioxide (water) at sea surface temperature (wet air) Potentiometric Potentiometric titration Salinity Single species Species dataset 2014 ftpangaea https://doi.org/10.1594/PANGAEA.83596710.1016/j.cbpa.2014.04.011 2024-07-24T02:31:32Z 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. Dataset North Atlantic Ocean acidification PANGAEA - Data Publisher for Earth & Environmental Science |
institution |
Open Polar |
collection |
PANGAEA - Data Publisher for Earth & Environmental Science |
op_collection_id |
ftpangaea |
language |
English |
topic |
Acid-base regulation Alkalinity total Animalia Aquarium number Aragonite saturation state Behaviour Benthic animals Benthos Bicarbonate ion Calcite saturation state Calculated Calculated using CO2SYS Calculated using seacarb after Nisumaa et al. (2010) Carbon inorganic dissolved Carbonate ion Carbonate system computation flag Carbon dioxide Coast and continental shelf Coelomic fluid pH Comment Containers and aquaria (20-1000 L or < 1 m**2) Difference Echinodermata Eucidaris tribuloides Feeding rate per individual Fugacity of carbon dioxide (water) at sea surface temperature (wet air) Identification Isotope ratio mass spectrometry Laboratory experiment North Atlantic OA-ICC Ocean Acidification International Coordination Centre Paracentrotus lividus Partial pressure of carbon dioxide (water) at sea surface temperature (wet air) Potentiometric Potentiometric titration Salinity Single species Species |
spellingShingle |
Acid-base regulation Alkalinity total Animalia Aquarium number Aragonite saturation state Behaviour Benthic animals Benthos Bicarbonate ion Calcite saturation state Calculated Calculated using CO2SYS Calculated using seacarb after Nisumaa et al. (2010) Carbon inorganic dissolved Carbonate ion Carbonate system computation flag Carbon dioxide Coast and continental shelf Coelomic fluid pH Comment Containers and aquaria (20-1000 L or < 1 m**2) Difference Echinodermata Eucidaris tribuloides Feeding rate per individual Fugacity of carbon dioxide (water) at sea surface temperature (wet air) Identification Isotope ratio mass spectrometry Laboratory experiment North Atlantic OA-ICC Ocean Acidification International Coordination Centre Paracentrotus lividus Partial pressure of carbon dioxide (water) at sea surface temperature (wet air) Potentiometric Potentiometric titration Salinity Single species Species Collard, Marie Dery, Aurélie Dehairs, Frank Dubois, Philippe Euechinoidea and Cidaroidea respond differently to ocean acidification |
topic_facet |
Acid-base regulation Alkalinity total Animalia Aquarium number Aragonite saturation state Behaviour Benthic animals Benthos Bicarbonate ion Calcite saturation state Calculated Calculated using CO2SYS Calculated using seacarb after Nisumaa et al. (2010) Carbon inorganic dissolved Carbonate ion Carbonate system computation flag Carbon dioxide Coast and continental shelf Coelomic fluid pH Comment Containers and aquaria (20-1000 L or < 1 m**2) Difference Echinodermata Eucidaris tribuloides Feeding rate per individual Fugacity of carbon dioxide (water) at sea surface temperature (wet air) Identification Isotope ratio mass spectrometry Laboratory experiment North Atlantic OA-ICC Ocean Acidification International Coordination Centre Paracentrotus lividus Partial pressure of carbon dioxide (water) at sea surface temperature (wet air) Potentiometric Potentiometric titration Salinity Single species Species |
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. |
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 |
title_short |
Euechinoidea and Cidaroidea respond differently to ocean acidification |
title_full |
Euechinoidea and Cidaroidea respond differently to ocean acidification |
title_fullStr |
Euechinoidea and Cidaroidea respond differently to ocean acidification |
title_full_unstemmed |
Euechinoidea and Cidaroidea respond differently to ocean acidification |
title_sort |
euechinoidea and cidaroidea respond differently to ocean acidification |
publisher |
PANGAEA |
publishDate |
2014 |
url |
https://doi.pangaea.de/10.1594/PANGAEA.835967 https://doi.org/10.1594/PANGAEA.835967 |
genre |
North Atlantic Ocean acidification |
genre_facet |
North Atlantic Ocean acidification |
op_source |
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, https://doi.org/10.1016/j.cbpa.2014.04.011 |
op_relation |
Lavigne, Héloïse; Epitalon, Jean-Marie; Gattuso, Jean-Pierre (2014): seacarb: seawater carbonate chemistry with R. R package version 3.0 [webpage]. https://cran.r-project.org/package=seacarb https://doi.pangaea.de/10.1594/PANGAEA.835967 https://doi.org/10.1594/PANGAEA.835967 |
op_rights |
CC-BY-3.0: Creative Commons Attribution 3.0 Unported Access constraints: unrestricted info:eu-repo/semantics/openAccess |
op_doi |
https://doi.org/10.1594/PANGAEA.83596710.1016/j.cbpa.2014.04.011 |
_version_ |
1810464832169705472 |