Slow shell building, a possible trait for resistance to the effects of acute ocean acidification, supplement to: Waldbusser, George G; Gray, Matthew W; Hales, Burke; Langdon, Chris; Haley, Brian A; Gimenez, Iria; Smith, Stephanie R; Brunner, Elizabeth L; Hutchinson, Greg (2016): Slow shell building, a possible trait for resistance to the effects of acute ocean acidification. Limnology and Oceanography, 61(6), 1969-1983
Increasing anthropogenic carbon dioxide is altering marine carbonate chemistry through a process called ocean acidification. Many calcium carbonate forming organisms are sensitive to changes in marine carbonate chemistry, especially mollusk bivalve larvae at the initial shell building stage. Rapid c...
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Language: | English |
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PANGAEA - Data Publisher for Earth & Environmental Science
2016
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Online Access: | https://dx.doi.org/10.1594/pangaea.868738 https://doi.pangaea.de/10.1594/PANGAEA.868738 |
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ftdatacite:10.1594/pangaea.868738 |
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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 |
Animalia Bottles or small containers/Aquaria <20 L Coast and continental shelf Growth/Morphology Laboratory experiment Mollusca North Pacific Ostrea lurida Pelagos Single species Temperate Zooplankton Type Species Registration number of species Uniform resource locator/link to reference Experiment Treatment Replicate Partial pressure of carbon dioxide water at sea surface temperature wet air Aragonite saturation state Temperature, water Salinity Alkalinity, total Carbon, inorganic, dissolved Bicarbonate ion Carbonate ion pH Proportion Shell length Shell length, standard deviation Carbonate system computation flag Carbon dioxide Fugacity of carbon dioxide water at sea surface temperature wet air Calcite saturation state Calculated using seacarb after Nisumaa et al. 2010 Ocean Acidification International Coordination Centre OA-ICC |
spellingShingle |
Animalia Bottles or small containers/Aquaria <20 L Coast and continental shelf Growth/Morphology Laboratory experiment Mollusca North Pacific Ostrea lurida Pelagos Single species Temperate Zooplankton Type Species Registration number of species Uniform resource locator/link to reference Experiment Treatment Replicate Partial pressure of carbon dioxide water at sea surface temperature wet air Aragonite saturation state Temperature, water Salinity Alkalinity, total Carbon, inorganic, dissolved Bicarbonate ion Carbonate ion pH Proportion Shell length Shell length, standard deviation Carbonate system computation flag Carbon dioxide Fugacity of carbon dioxide water at sea surface temperature wet air Calcite saturation state Calculated using seacarb after Nisumaa et al. 2010 Ocean Acidification International Coordination Centre OA-ICC Waldbusser, George G Gray, Matthew W Hales, Burke Langdon, Chris Haley, Brian A Gimenez, Iria Smith, Stephanie R Brunner, Elizabeth L Hutchinson, Greg Slow shell building, a possible trait for resistance to the effects of acute ocean acidification, supplement to: Waldbusser, George G; Gray, Matthew W; Hales, Burke; Langdon, Chris; Haley, Brian A; Gimenez, Iria; Smith, Stephanie R; Brunner, Elizabeth L; Hutchinson, Greg (2016): Slow shell building, a possible trait for resistance to the effects of acute ocean acidification. Limnology and Oceanography, 61(6), 1969-1983 |
topic_facet |
Animalia Bottles or small containers/Aquaria <20 L Coast and continental shelf Growth/Morphology Laboratory experiment Mollusca North Pacific Ostrea lurida Pelagos Single species Temperate Zooplankton Type Species Registration number of species Uniform resource locator/link to reference Experiment Treatment Replicate Partial pressure of carbon dioxide water at sea surface temperature wet air Aragonite saturation state Temperature, water Salinity Alkalinity, total Carbon, inorganic, dissolved Bicarbonate ion Carbonate ion pH Proportion Shell length Shell length, standard deviation Carbonate system computation flag Carbon dioxide Fugacity of carbon dioxide water at sea surface temperature wet air Calcite saturation state Calculated using seacarb after Nisumaa et al. 2010 Ocean Acidification International Coordination Centre OA-ICC |
description |
Increasing anthropogenic carbon dioxide is altering marine carbonate chemistry through a process called ocean acidification. Many calcium carbonate forming organisms are sensitive to changes in marine carbonate chemistry, especially mollusk bivalve larvae at the initial shell building stage. Rapid calcification, limited energy reserves, and more exposed calcification surfaces, are traits at this stage that increase vulnerability to ocean acidification through our previously argued kinetic-energetic hypothesis. These developmental traits are common to broadcast spawning bivalve species that are the focus of most ocean acidification studies to date. Some oyster species brood their young, which results in slower development of the embryos through the initial shell formation stage. We examined the responses of the brooding Olympia oyster, Ostrea lurida, during their initial shell building stage. We extracted fertilized eggs from, O. lurida, prior to shell development, then exposed developing embryos to a wide range of marine carbonate chemistry conditions. Surprisingly, O. lurida showed no acute negative response to any ocean acidification treatments. Compared to the broadcast spawning Pacific oyster, Crassostrea gigas, calcification rate and standardized endogenous energy lipid consumption rate were nearly 10 and 50 times slower, respectively. Our results suggest that slow shell building may lessen the energetic burden of acidification at this stage and provides additional support for our kinetic-energetic hypothesis. Furthermore, these results may represent an example of exaptation; fitness conveyed by a coopted trait that evolved for another purpose, a concept largely lacking in the current perspective of adaptation and global climate change. : In order to allow full comparability with other ocean acidification data sets, the R package seacarb (Gattuso et al, 2016) 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 2016-11-23. |
format |
Dataset |
author |
Waldbusser, George G Gray, Matthew W Hales, Burke Langdon, Chris Haley, Brian A Gimenez, Iria Smith, Stephanie R Brunner, Elizabeth L Hutchinson, Greg |
author_facet |
Waldbusser, George G Gray, Matthew W Hales, Burke Langdon, Chris Haley, Brian A Gimenez, Iria Smith, Stephanie R Brunner, Elizabeth L Hutchinson, Greg |
author_sort |
Waldbusser, George G |
title |
Slow shell building, a possible trait for resistance to the effects of acute ocean acidification, supplement to: Waldbusser, George G; Gray, Matthew W; Hales, Burke; Langdon, Chris; Haley, Brian A; Gimenez, Iria; Smith, Stephanie R; Brunner, Elizabeth L; Hutchinson, Greg (2016): Slow shell building, a possible trait for resistance to the effects of acute ocean acidification. Limnology and Oceanography, 61(6), 1969-1983 |
title_short |
Slow shell building, a possible trait for resistance to the effects of acute ocean acidification, supplement to: Waldbusser, George G; Gray, Matthew W; Hales, Burke; Langdon, Chris; Haley, Brian A; Gimenez, Iria; Smith, Stephanie R; Brunner, Elizabeth L; Hutchinson, Greg (2016): Slow shell building, a possible trait for resistance to the effects of acute ocean acidification. Limnology and Oceanography, 61(6), 1969-1983 |
title_full |
Slow shell building, a possible trait for resistance to the effects of acute ocean acidification, supplement to: Waldbusser, George G; Gray, Matthew W; Hales, Burke; Langdon, Chris; Haley, Brian A; Gimenez, Iria; Smith, Stephanie R; Brunner, Elizabeth L; Hutchinson, Greg (2016): Slow shell building, a possible trait for resistance to the effects of acute ocean acidification. Limnology and Oceanography, 61(6), 1969-1983 |
title_fullStr |
Slow shell building, a possible trait for resistance to the effects of acute ocean acidification, supplement to: Waldbusser, George G; Gray, Matthew W; Hales, Burke; Langdon, Chris; Haley, Brian A; Gimenez, Iria; Smith, Stephanie R; Brunner, Elizabeth L; Hutchinson, Greg (2016): Slow shell building, a possible trait for resistance to the effects of acute ocean acidification. Limnology and Oceanography, 61(6), 1969-1983 |
title_full_unstemmed |
Slow shell building, a possible trait for resistance to the effects of acute ocean acidification, supplement to: Waldbusser, George G; Gray, Matthew W; Hales, Burke; Langdon, Chris; Haley, Brian A; Gimenez, Iria; Smith, Stephanie R; Brunner, Elizabeth L; Hutchinson, Greg (2016): Slow shell building, a possible trait for resistance to the effects of acute ocean acidification. Limnology and Oceanography, 61(6), 1969-1983 |
title_sort |
slow shell building, a possible trait for resistance to the effects of acute ocean acidification, supplement to: waldbusser, george g; gray, matthew w; hales, burke; langdon, chris; haley, brian a; gimenez, iria; smith, stephanie r; brunner, elizabeth l; hutchinson, greg (2016): slow shell building, a possible trait for resistance to the effects of acute ocean acidification. limnology and oceanography, 61(6), 1969-1983 |
publisher |
PANGAEA - Data Publisher for Earth & Environmental Science |
publishDate |
2016 |
url |
https://dx.doi.org/10.1594/pangaea.868738 https://doi.pangaea.de/10.1594/PANGAEA.868738 |
geographic |
Pacific |
geographic_facet |
Pacific |
genre |
Crassostrea gigas Ocean acidification Pacific oyster |
genre_facet |
Crassostrea gigas Ocean acidification Pacific oyster |
op_relation |
https://cran.r-project.org/package=seacarb https://dx.doi.org/10.1002/lno.10348 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.868738 https://doi.org/10.1002/lno.10348 |
_version_ |
1766394993653579776 |
spelling |
ftdatacite:10.1594/pangaea.868738 2023-05-15T15:59:12+02:00 Slow shell building, a possible trait for resistance to the effects of acute ocean acidification, supplement to: Waldbusser, George G; Gray, Matthew W; Hales, Burke; Langdon, Chris; Haley, Brian A; Gimenez, Iria; Smith, Stephanie R; Brunner, Elizabeth L; Hutchinson, Greg (2016): Slow shell building, a possible trait for resistance to the effects of acute ocean acidification. Limnology and Oceanography, 61(6), 1969-1983 Waldbusser, George G Gray, Matthew W Hales, Burke Langdon, Chris Haley, Brian A Gimenez, Iria Smith, Stephanie R Brunner, Elizabeth L Hutchinson, Greg 2016 text/tab-separated-values https://dx.doi.org/10.1594/pangaea.868738 https://doi.pangaea.de/10.1594/PANGAEA.868738 en eng PANGAEA - Data Publisher for Earth & Environmental Science https://cran.r-project.org/package=seacarb https://dx.doi.org/10.1002/lno.10348 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 Animalia Bottles or small containers/Aquaria <20 L Coast and continental shelf Growth/Morphology Laboratory experiment Mollusca North Pacific Ostrea lurida Pelagos Single species Temperate Zooplankton Type Species Registration number of species Uniform resource locator/link to reference Experiment Treatment Replicate Partial pressure of carbon dioxide water at sea surface temperature wet air Aragonite saturation state Temperature, water Salinity Alkalinity, total Carbon, inorganic, dissolved Bicarbonate ion Carbonate ion pH Proportion Shell length Shell length, standard deviation Carbonate system computation flag Carbon dioxide Fugacity of carbon dioxide water at sea surface temperature wet air Calcite saturation state Calculated using seacarb after Nisumaa et al. 2010 Ocean Acidification International Coordination Centre OA-ICC Supplementary Dataset dataset Dataset 2016 ftdatacite https://doi.org/10.1594/pangaea.868738 https://doi.org/10.1002/lno.10348 2021-11-05T12:55:41Z Increasing anthropogenic carbon dioxide is altering marine carbonate chemistry through a process called ocean acidification. Many calcium carbonate forming organisms are sensitive to changes in marine carbonate chemistry, especially mollusk bivalve larvae at the initial shell building stage. Rapid calcification, limited energy reserves, and more exposed calcification surfaces, are traits at this stage that increase vulnerability to ocean acidification through our previously argued kinetic-energetic hypothesis. These developmental traits are common to broadcast spawning bivalve species that are the focus of most ocean acidification studies to date. Some oyster species brood their young, which results in slower development of the embryos through the initial shell formation stage. We examined the responses of the brooding Olympia oyster, Ostrea lurida, during their initial shell building stage. We extracted fertilized eggs from, O. lurida, prior to shell development, then exposed developing embryos to a wide range of marine carbonate chemistry conditions. Surprisingly, O. lurida showed no acute negative response to any ocean acidification treatments. Compared to the broadcast spawning Pacific oyster, Crassostrea gigas, calcification rate and standardized endogenous energy lipid consumption rate were nearly 10 and 50 times slower, respectively. Our results suggest that slow shell building may lessen the energetic burden of acidification at this stage and provides additional support for our kinetic-energetic hypothesis. Furthermore, these results may represent an example of exaptation; fitness conveyed by a coopted trait that evolved for another purpose, a concept largely lacking in the current perspective of adaptation and global climate change. : In order to allow full comparability with other ocean acidification data sets, the R package seacarb (Gattuso et al, 2016) 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 2016-11-23. Dataset Crassostrea gigas Ocean acidification Pacific oyster DataCite Metadata Store (German National Library of Science and Technology) Pacific |