Seawater carbonate chemistry and body size of the keystone sea urchin Strongylocentrotus purpuratus
A rapidly growing body of literature documents the potential negative effects of CO2-driven ocean acidification (OA) on marine organisms. However, nearly all of this work has focused on the effects of future conditions on modern populations, neglecting the role of adaptation. Rapid evolution can alt...
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2013
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Online Access: | https://doi.pangaea.de/10.1594/PANGAEA.950284 https://doi.org/10.1594/PANGAEA.950284 |
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ftpangaea:oai:pangaea.de:doi:10.1594/PANGAEA.950284 |
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openpolar |
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Open Polar |
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PANGAEA - Data Publisher for Earth & Environmental Science |
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ftpangaea |
language |
English |
topic |
Alkalinity total standard deviation Animalia Aragonite saturation state Bicarbonate ion Bottles or small containers/Aquaria (<20 L) Calcite saturation state Calculated using CO2SYS Calculated using seacarb after Nisumaa et al. (2010) Calculated using seacarb after Orr et al. (2018) Carbon inorganic dissolved Carbonate ion Carbonate system computation flag Carbon dioxide Coast and continental shelf Echinodermata Fugacity of carbon dioxide (water) at sea surface temperature (wet air) Fugacity of carbon dioxide in seawater Growth/Morphology Identification Laboratory experiment Length North Pacific OA-ICC Ocean Acidification International Coordination Centre Origin Partial pressure of carbon dioxide Partial pressure of carbon dioxide (water) at sea surface temperature (wet air) Pelagos |
spellingShingle |
Alkalinity total standard deviation Animalia Aragonite saturation state Bicarbonate ion Bottles or small containers/Aquaria (<20 L) Calcite saturation state Calculated using CO2SYS Calculated using seacarb after Nisumaa et al. (2010) Calculated using seacarb after Orr et al. (2018) Carbon inorganic dissolved Carbonate ion Carbonate system computation flag Carbon dioxide Coast and continental shelf Echinodermata Fugacity of carbon dioxide (water) at sea surface temperature (wet air) Fugacity of carbon dioxide in seawater Growth/Morphology Identification Laboratory experiment Length North Pacific OA-ICC Ocean Acidification International Coordination Centre Origin Partial pressure of carbon dioxide Partial pressure of carbon dioxide (water) at sea surface temperature (wet air) Pelagos Kelly, Morgan W Padilla-Gamiño, Jacqueline L Hofmann, Gretchen E Seawater carbonate chemistry and body size of the keystone sea urchin Strongylocentrotus purpuratus |
topic_facet |
Alkalinity total standard deviation Animalia Aragonite saturation state Bicarbonate ion Bottles or small containers/Aquaria (<20 L) Calcite saturation state Calculated using CO2SYS Calculated using seacarb after Nisumaa et al. (2010) Calculated using seacarb after Orr et al. (2018) Carbon inorganic dissolved Carbonate ion Carbonate system computation flag Carbon dioxide Coast and continental shelf Echinodermata Fugacity of carbon dioxide (water) at sea surface temperature (wet air) Fugacity of carbon dioxide in seawater Growth/Morphology Identification Laboratory experiment Length North Pacific OA-ICC Ocean Acidification International Coordination Centre Origin Partial pressure of carbon dioxide Partial pressure of carbon dioxide (water) at sea surface temperature (wet air) Pelagos |
description |
A rapidly growing body of literature documents the potential negative effects of CO2-driven ocean acidification (OA) on marine organisms. However, nearly all of this work has focused on the effects of future conditions on modern populations, neglecting the role of adaptation. Rapid evolution can alter demographic responses to environmental change, ultimately affecting the likelihood of population persistence, but the capacity for adaptation will differ among populations and species. Here, we measure the capacity of the ecologically important purple sea urchin Strongylocentrotus purpuratus to adapt to OA, using a breeding experiment to estimate additive genetic variance for larval size (an important component of fitness) under future high pCO2/low pH conditions. Although larvae reared under future conditions were smaller than those reared under present-day conditions, we show that there is also abundant genetic variation for body size under elevated pCO2, indicating that this trait can evolve. The observed heritability of size was 0.40±0.32 (95% CI) under low pCO2, and 0.50±0.30 under high pCO2 conditions. Accounting for the observed genetic variation in models of future larval size and demographic rates substantially alters projections of performance for this species in the future ocean. Importantly, our model shows that after incorporating the effects of adaptation, the OA-driven decrease in population growth rate is up to 50% smaller, than that predicted by the “no-adaptation” scenario. Adults used in the experiment were collected from two sites on the coast of the Northeast Pacific that are characterized by different pH regimes, as measured by autonomous sensors. Comparing results between sites, we also found subtle differences in larval size under high pCO2 rearing conditions, consistent with local adaptation to carbonate chemistry in the field. These results suggest that spatially varying selection may help to maintain genetic variation necessary for adaptation to future ocean acidification. |
format |
Dataset |
author |
Kelly, Morgan W Padilla-Gamiño, Jacqueline L Hofmann, Gretchen E |
author_facet |
Kelly, Morgan W Padilla-Gamiño, Jacqueline L Hofmann, Gretchen E |
author_sort |
Kelly, Morgan W |
title |
Seawater carbonate chemistry and body size of the keystone sea urchin Strongylocentrotus purpuratus |
title_short |
Seawater carbonate chemistry and body size of the keystone sea urchin Strongylocentrotus purpuratus |
title_full |
Seawater carbonate chemistry and body size of the keystone sea urchin Strongylocentrotus purpuratus |
title_fullStr |
Seawater carbonate chemistry and body size of the keystone sea urchin Strongylocentrotus purpuratus |
title_full_unstemmed |
Seawater carbonate chemistry and body size of the keystone sea urchin Strongylocentrotus purpuratus |
title_sort |
seawater carbonate chemistry and body size of the keystone sea urchin strongylocentrotus purpuratus |
publisher |
PANGAEA |
publishDate |
2013 |
url |
https://doi.pangaea.de/10.1594/PANGAEA.950284 https://doi.org/10.1594/PANGAEA.950284 |
genre |
Ocean acidification |
genre_facet |
Ocean acidification |
op_relation |
Kelly, Morgan W; Padilla-Gamiño, Jacqueline L; Hofmann, Gretchen E (2013): Natural variation and the capacity to adapt to ocean acidification in the keystone sea urchin Strongylocentrotus purpuratus. Global Change Biology, 19(8), 2536-2546, https://doi.org/10.1111/gcb.12251 Gattuso, Jean-Pierre; Epitalon, Jean-Marie; Lavigne, Héloïse; Orr, James (2021): seacarb: seawater carbonate chemistry with R. R package version 3.2.16. https://cran.r-project.org/web/packages/seacarb/index.html https://doi.pangaea.de/10.1594/PANGAEA.950284 https://doi.org/10.1594/PANGAEA.950284 |
op_rights |
CC-BY-4.0: Creative Commons Attribution 4.0 International Access constraints: unrestricted info:eu-repo/semantics/openAccess |
op_doi |
https://doi.org/10.1594/PANGAEA.95028410.1111/gcb.12251 |
_version_ |
1810469267504627712 |
spelling |
ftpangaea:oai:pangaea.de:doi:10.1594/PANGAEA.950284 2024-09-15T18:27:58+00:00 Seawater carbonate chemistry and body size of the keystone sea urchin Strongylocentrotus purpuratus Kelly, Morgan W Padilla-Gamiño, Jacqueline L Hofmann, Gretchen E 2013 text/tab-separated-values, 155571 data points https://doi.pangaea.de/10.1594/PANGAEA.950284 https://doi.org/10.1594/PANGAEA.950284 en eng PANGAEA Kelly, Morgan W; Padilla-Gamiño, Jacqueline L; Hofmann, Gretchen E (2013): Natural variation and the capacity to adapt to ocean acidification in the keystone sea urchin Strongylocentrotus purpuratus. Global Change Biology, 19(8), 2536-2546, https://doi.org/10.1111/gcb.12251 Gattuso, Jean-Pierre; Epitalon, Jean-Marie; Lavigne, Héloïse; Orr, James (2021): seacarb: seawater carbonate chemistry with R. R package version 3.2.16. https://cran.r-project.org/web/packages/seacarb/index.html https://doi.pangaea.de/10.1594/PANGAEA.950284 https://doi.org/10.1594/PANGAEA.950284 CC-BY-4.0: Creative Commons Attribution 4.0 International Access constraints: unrestricted info:eu-repo/semantics/openAccess Alkalinity total standard deviation Animalia Aragonite saturation state Bicarbonate ion Bottles or small containers/Aquaria (<20 L) Calcite saturation state Calculated using CO2SYS Calculated using seacarb after Nisumaa et al. (2010) Calculated using seacarb after Orr et al. (2018) Carbon inorganic dissolved Carbonate ion Carbonate system computation flag Carbon dioxide Coast and continental shelf Echinodermata Fugacity of carbon dioxide (water) at sea surface temperature (wet air) Fugacity of carbon dioxide in seawater Growth/Morphology Identification Laboratory experiment Length North Pacific OA-ICC Ocean Acidification International Coordination Centre Origin Partial pressure of carbon dioxide Partial pressure of carbon dioxide (water) at sea surface temperature (wet air) Pelagos dataset 2013 ftpangaea https://doi.org/10.1594/PANGAEA.95028410.1111/gcb.12251 2024-07-24T02:31:34Z A rapidly growing body of literature documents the potential negative effects of CO2-driven ocean acidification (OA) on marine organisms. However, nearly all of this work has focused on the effects of future conditions on modern populations, neglecting the role of adaptation. Rapid evolution can alter demographic responses to environmental change, ultimately affecting the likelihood of population persistence, but the capacity for adaptation will differ among populations and species. Here, we measure the capacity of the ecologically important purple sea urchin Strongylocentrotus purpuratus to adapt to OA, using a breeding experiment to estimate additive genetic variance for larval size (an important component of fitness) under future high pCO2/low pH conditions. Although larvae reared under future conditions were smaller than those reared under present-day conditions, we show that there is also abundant genetic variation for body size under elevated pCO2, indicating that this trait can evolve. The observed heritability of size was 0.40±0.32 (95% CI) under low pCO2, and 0.50±0.30 under high pCO2 conditions. Accounting for the observed genetic variation in models of future larval size and demographic rates substantially alters projections of performance for this species in the future ocean. Importantly, our model shows that after incorporating the effects of adaptation, the OA-driven decrease in population growth rate is up to 50% smaller, than that predicted by the “no-adaptation” scenario. Adults used in the experiment were collected from two sites on the coast of the Northeast Pacific that are characterized by different pH regimes, as measured by autonomous sensors. Comparing results between sites, we also found subtle differences in larval size under high pCO2 rearing conditions, consistent with local adaptation to carbonate chemistry in the field. These results suggest that spatially varying selection may help to maintain genetic variation necessary for adaptation to future ocean acidification. Dataset Ocean acidification PANGAEA - Data Publisher for Earth & Environmental Science |