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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Bibliographic Details
Main Authors: Kelly, Morgan W, Padilla-Gamiño, Jacqueline L, Hofmann, Gretchen E
Format: Dataset
Language:English
Published: PANGAEA 2013
Subjects:
Online Access:https://doi.pangaea.de/10.1594/PANGAEA.950284
https://doi.org/10.1594/PANGAEA.950284
id ftpangaea:oai:pangaea.de:doi:10.1594/PANGAEA.950284
record_format openpolar
institution Open Polar
collection PANGAEA - Data Publisher for Earth & Environmental Science
op_collection_id 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