Could the acid-base status of Antarctic sea urchins indicate a better-than-expected resilience to near-future ocean acidification?

Increasing atmospheric carbon dioxide concentration alters the chemistry of the oceans towards more acidic conditions. Polar oceans are particularly affected due to their low temperature, low carbonate content and mixing patterns, for instance upwellings. Calcifying organisms are expected to be high...

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Main Authors: Collard, Marie, De Ridder, Chantal, David, Bruno, Dehairs, Frank, Dubois, Philippe
Format: Dataset
Language:English
Published: PANGAEA 2015
Subjects:
pH
Online Access:https://doi.pangaea.de/10.1594/PANGAEA.839887
https://doi.org/10.1594/PANGAEA.839887
id ftpangaea:oai:pangaea.de:doi:10.1594/PANGAEA.839887
record_format openpolar
institution Open Polar
collection PANGAEA - Data Publisher for Earth & Environmental Science
op_collection_id ftpangaea
language English
topic Abatus cavernosus
Acid-base regulation
Alkalinity
total
standard deviation
Amphipneustes lorioli
Amphipneustes rostratus
Amphipneustes similis
Animalia
Antarctic
Aporocidaris eltaniana
Aragonite saturation state
Benthic animals
Benthos
Bicarbonate ion
Bransfield_Strait
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
Coulometric titration
Ctenocidaris gigantea
DATE/TIME
spellingShingle Abatus cavernosus
Acid-base regulation
Alkalinity
total
standard deviation
Amphipneustes lorioli
Amphipneustes rostratus
Amphipneustes similis
Animalia
Antarctic
Aporocidaris eltaniana
Aragonite saturation state
Benthic animals
Benthos
Bicarbonate ion
Bransfield_Strait
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
Coulometric titration
Ctenocidaris gigantea
DATE/TIME
Collard, Marie
De Ridder, Chantal
David, Bruno
Dehairs, Frank
Dubois, Philippe
Could the acid-base status of Antarctic sea urchins indicate a better-than-expected resilience to near-future ocean acidification?
topic_facet Abatus cavernosus
Acid-base regulation
Alkalinity
total
standard deviation
Amphipneustes lorioli
Amphipneustes rostratus
Amphipneustes similis
Animalia
Antarctic
Aporocidaris eltaniana
Aragonite saturation state
Benthic animals
Benthos
Bicarbonate ion
Bransfield_Strait
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
Coulometric titration
Ctenocidaris gigantea
DATE/TIME
description Increasing atmospheric carbon dioxide concentration alters the chemistry of the oceans towards more acidic conditions. Polar oceans are particularly affected due to their low temperature, low carbonate content and mixing patterns, for instance upwellings. Calcifying organisms are expected to be highly impacted by the decrease in the oceans' pH and carbonate ions concentration. In particular, sea urchins, members of the phylum Echinodermata, are hypothesized to be at risk due to their high-magnesium calcite skeleton. However, tolerance to ocean acidification in metazoans is first linked to acid-base regulation capacities of the extracellular fluids. No information on this is available to date for Antarctic echinoderms and inference from temperate and tropical studies needs support. In this study, we investigated the acid-base status of 9 species of sea urchins (3 cidaroids, 2 regular euechinoids and 4 irregular echinoids). It appears that Antarctic regular euechinoids seem equipped with similar acid-base regulation systems as tropical and temperate regular euechinoids but could rely on more passive ion transfer systems, minimizing energy requirements. Cidaroids have an acid-base status similar to that of tropical cidaroids. Therefore Antarctic cidaroids will most probably not be affected by decreasing seawater pH, the pH drop linked to ocean acidification being negligible in comparison of the naturally low pH of the coelomic fluid. Irregular echinoids might not suffer from reduced seawater pH if acidosis of the coelomic fluid pH does not occur but more data on their acid-base regulation are needed. Combining these results with the resilience of Antarctic sea urchin larvae strongly suggests that these organisms might not be the expected victims of ocean acidification. However, data on the impact of other global stressors such as temperature and of the combination of the different stressors needs to be acquired to assess the sensitivity of these organisms to global change.
format Dataset
author Collard, Marie
De Ridder, Chantal
David, Bruno
Dehairs, Frank
Dubois, Philippe
author_facet Collard, Marie
De Ridder, Chantal
David, Bruno
Dehairs, Frank
Dubois, Philippe
author_sort Collard, Marie
title Could the acid-base status of Antarctic sea urchins indicate a better-than-expected resilience to near-future ocean acidification?
title_short Could the acid-base status of Antarctic sea urchins indicate a better-than-expected resilience to near-future ocean acidification?
title_full Could the acid-base status of Antarctic sea urchins indicate a better-than-expected resilience to near-future ocean acidification?
title_fullStr Could the acid-base status of Antarctic sea urchins indicate a better-than-expected resilience to near-future ocean acidification?
title_full_unstemmed Could the acid-base status of Antarctic sea urchins indicate a better-than-expected resilience to near-future ocean acidification?
title_sort could the acid-base status of antarctic sea urchins indicate a better-than-expected resilience to near-future ocean acidification?
publisher PANGAEA
publishDate 2015
url https://doi.pangaea.de/10.1594/PANGAEA.839887
https://doi.org/10.1594/PANGAEA.839887
op_coverage MEDIAN LATITUDE: -63.162757 * MEDIAN LONGITUDE: -57.123713 * SOUTH-BOUND LATITUDE: -64.004500 * WEST-BOUND LONGITUDE: -61.162667 * NORTH-BOUND LATITUDE: -61.948333 * EAST-BOUND LONGITUDE: -54.107000 * DATE/TIME START: 2013-01-26T00:00:00 * DATE/TIME END: 2013-03-12T00:00:00
long_lat ENVELOPE(-61.162667,-54.107000,-61.948333,-64.004500)
geographic Antarctic
geographic_facet Antarctic
genre Antarc*
Antarctic
Ocean acidification
genre_facet Antarc*
Antarctic
Ocean acidification
op_source Supplement to: Collard, Marie; De Ridder, Chantal; David, Bruno; Dehairs, Frank; Dubois, Philippe (2014): Could the acid-base status of Antarctic sea urchins indicate a better-than-expected resilience to near-future ocean acidification? Global Change Biology, https://doi.org/10.1111/gcb.12735
op_relation 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
https://doi.pangaea.de/10.1594/PANGAEA.839887
https://doi.org/10.1594/PANGAEA.839887
op_rights CC-BY-3.0: Creative Commons Attribution 3.0 Unported
Access constraints: unrestricted
info:eu-repo/semantics/openAccess
op_rightsnorm CC-BY
op_doi https://doi.org/10.1594/PANGAEA.839887
https://doi.org/10.1111/gcb.12735
_version_ 1766273562958626816
spelling ftpangaea:oai:pangaea.de:doi:10.1594/PANGAEA.839887 2023-05-15T14:03:04+02:00 Could the acid-base status of Antarctic sea urchins indicate a better-than-expected resilience to near-future ocean acidification? Collard, Marie De Ridder, Chantal David, Bruno Dehairs, Frank Dubois, Philippe MEDIAN LATITUDE: -63.162757 * MEDIAN LONGITUDE: -57.123713 * SOUTH-BOUND LATITUDE: -64.004500 * WEST-BOUND LONGITUDE: -61.162667 * NORTH-BOUND LATITUDE: -61.948333 * EAST-BOUND LONGITUDE: -54.107000 * DATE/TIME START: 2013-01-26T00:00:00 * DATE/TIME END: 2013-03-12T00:00:00 2015-12-02 text/tab-separated-values, 2540 data points https://doi.pangaea.de/10.1594/PANGAEA.839887 https://doi.org/10.1594/PANGAEA.839887 en eng PANGAEA 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 https://doi.pangaea.de/10.1594/PANGAEA.839887 https://doi.org/10.1594/PANGAEA.839887 CC-BY-3.0: Creative Commons Attribution 3.0 Unported Access constraints: unrestricted info:eu-repo/semantics/openAccess CC-BY Supplement to: Collard, Marie; De Ridder, Chantal; David, Bruno; Dehairs, Frank; Dubois, Philippe (2014): Could the acid-base status of Antarctic sea urchins indicate a better-than-expected resilience to near-future ocean acidification? Global Change Biology, https://doi.org/10.1111/gcb.12735 Abatus cavernosus Acid-base regulation Alkalinity total standard deviation Amphipneustes lorioli Amphipneustes rostratus Amphipneustes similis Animalia Antarctic Aporocidaris eltaniana Aragonite saturation state Benthic animals Benthos Bicarbonate ion Bransfield_Strait 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 Coulometric titration Ctenocidaris gigantea DATE/TIME Dataset 2015 ftpangaea https://doi.org/10.1594/PANGAEA.839887 https://doi.org/10.1111/gcb.12735 2023-01-20T09:04:48Z Increasing atmospheric carbon dioxide concentration alters the chemistry of the oceans towards more acidic conditions. Polar oceans are particularly affected due to their low temperature, low carbonate content and mixing patterns, for instance upwellings. Calcifying organisms are expected to be highly impacted by the decrease in the oceans' pH and carbonate ions concentration. In particular, sea urchins, members of the phylum Echinodermata, are hypothesized to be at risk due to their high-magnesium calcite skeleton. However, tolerance to ocean acidification in metazoans is first linked to acid-base regulation capacities of the extracellular fluids. No information on this is available to date for Antarctic echinoderms and inference from temperate and tropical studies needs support. In this study, we investigated the acid-base status of 9 species of sea urchins (3 cidaroids, 2 regular euechinoids and 4 irregular echinoids). It appears that Antarctic regular euechinoids seem equipped with similar acid-base regulation systems as tropical and temperate regular euechinoids but could rely on more passive ion transfer systems, minimizing energy requirements. Cidaroids have an acid-base status similar to that of tropical cidaroids. Therefore Antarctic cidaroids will most probably not be affected by decreasing seawater pH, the pH drop linked to ocean acidification being negligible in comparison of the naturally low pH of the coelomic fluid. Irregular echinoids might not suffer from reduced seawater pH if acidosis of the coelomic fluid pH does not occur but more data on their acid-base regulation are needed. Combining these results with the resilience of Antarctic sea urchin larvae strongly suggests that these organisms might not be the expected victims of ocean acidification. However, data on the impact of other global stressors such as temperature and of the combination of the different stressors needs to be acquired to assess the sensitivity of these organisms to global change. Dataset Antarc* Antarctic Ocean acidification PANGAEA - Data Publisher for Earth & Environmental Science Antarctic ENVELOPE(-61.162667,-54.107000,-61.948333,-64.004500)