Slow shell building, a possible trait for resistance to the effects of acute ocean acidification
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
2016
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Online Access: | https://doi.pangaea.de/10.1594/PANGAEA.868738 https://doi.org/10.1594/PANGAEA.868738 |
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ftpangaea:oai:pangaea.de:doi:10.1594/PANGAEA.868738 |
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openpolar |
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Open Polar |
collection |
PANGAEA - Data Publisher for Earth & Environmental Science |
op_collection_id |
ftpangaea |
language |
English |
topic |
Alkalinity total Animalia Aragonite saturation state Bicarbonate ion Bottles or small containers/Aquaria (<20 L) Calcite saturation state Calculated using seacarb after Nisumaa et al. (2010) Carbon inorganic dissolved Carbonate ion Carbonate system computation flag Carbon dioxide Coast and continental shelf Experiment Fugacity of carbon dioxide (water) at sea surface temperature (wet air) Growth/Morphology Laboratory experiment Mollusca North Pacific OA-ICC Ocean Acidification International Coordination Centre Ostrea lurida Partial pressure of carbon dioxide (water) at sea surface temperature (wet air) Pelagos pH Proportion Registration number of species Replicate Salinity Shell length standard deviation Single species Species Temperate Temperature water Treatment Type Uniform resource locator/link to reference Zooplankton |
spellingShingle |
Alkalinity total Animalia Aragonite saturation state Bicarbonate ion Bottles or small containers/Aquaria (<20 L) Calcite saturation state Calculated using seacarb after Nisumaa et al. (2010) Carbon inorganic dissolved Carbonate ion Carbonate system computation flag Carbon dioxide Coast and continental shelf Experiment Fugacity of carbon dioxide (water) at sea surface temperature (wet air) Growth/Morphology Laboratory experiment Mollusca North Pacific OA-ICC Ocean Acidification International Coordination Centre Ostrea lurida Partial pressure of carbon dioxide (water) at sea surface temperature (wet air) Pelagos pH Proportion Registration number of species Replicate Salinity Shell length standard deviation Single species Species Temperate Temperature water Treatment Type Uniform resource locator/link to reference Zooplankton 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 |
topic_facet |
Alkalinity total Animalia Aragonite saturation state Bicarbonate ion Bottles or small containers/Aquaria (<20 L) Calcite saturation state Calculated using seacarb after Nisumaa et al. (2010) Carbon inorganic dissolved Carbonate ion Carbonate system computation flag Carbon dioxide Coast and continental shelf Experiment Fugacity of carbon dioxide (water) at sea surface temperature (wet air) Growth/Morphology Laboratory experiment Mollusca North Pacific OA-ICC Ocean Acidification International Coordination Centre Ostrea lurida Partial pressure of carbon dioxide (water) at sea surface temperature (wet air) Pelagos pH Proportion Registration number of species Replicate Salinity Shell length standard deviation Single species Species Temperate Temperature water Treatment Type Uniform resource locator/link to reference Zooplankton |
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. |
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 |
title_short |
Slow shell building, a possible trait for resistance to the effects of acute ocean acidification |
title_full |
Slow shell building, a possible trait for resistance to the effects of acute ocean acidification |
title_fullStr |
Slow shell building, a possible trait for resistance to the effects of acute ocean acidification |
title_full_unstemmed |
Slow shell building, a possible trait for resistance to the effects of acute ocean acidification |
title_sort |
slow shell building, a possible trait for resistance to the effects of acute ocean acidification |
publisher |
PANGAEA |
publishDate |
2016 |
url |
https://doi.pangaea.de/10.1594/PANGAEA.868738 https://doi.org/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_source |
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, https://doi.org/10.1002/lno.10348 |
op_relation |
Gattuso, Jean-Pierre; Epitalon, Jean-Marie; Lavigne, Héloïse; Orr, James C; Gentili, Bernard; Proye, Aurélien; Soetaert, Karline; Rae, James (2016): seacarb: seawater carbonate chemistry with R. R package version 3.1. https://cran.r-project.org/package=seacarb https://doi.pangaea.de/10.1594/PANGAEA.868738 https://doi.org/10.1594/PANGAEA.868738 |
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.868738 https://doi.org/10.1002/lno.10348 |
_version_ |
1766394933769404416 |
spelling |
ftpangaea:oai:pangaea.de:doi:10.1594/PANGAEA.868738 2023-05-15T15:59:09+02:00 Slow shell building, a possible trait for resistance to the effects of acute ocean acidification Waldbusser, George G Gray, Matthew W Hales, Burke Langdon, Chris Haley, Brian A Gimenez, Iria Smith, Stephanie R Brunner, Elizabeth L Hutchinson, Greg 2016-11-23 text/tab-separated-values, 3451 data points https://doi.pangaea.de/10.1594/PANGAEA.868738 https://doi.org/10.1594/PANGAEA.868738 en eng PANGAEA Gattuso, Jean-Pierre; Epitalon, Jean-Marie; Lavigne, Héloïse; Orr, James C; Gentili, Bernard; Proye, Aurélien; Soetaert, Karline; Rae, James (2016): seacarb: seawater carbonate chemistry with R. R package version 3.1. https://cran.r-project.org/package=seacarb https://doi.pangaea.de/10.1594/PANGAEA.868738 https://doi.org/10.1594/PANGAEA.868738 CC-BY-3.0: Creative Commons Attribution 3.0 Unported Access constraints: unrestricted info:eu-repo/semantics/openAccess CC-BY 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, https://doi.org/10.1002/lno.10348 Alkalinity total Animalia Aragonite saturation state Bicarbonate ion Bottles or small containers/Aquaria (<20 L) Calcite saturation state Calculated using seacarb after Nisumaa et al. (2010) Carbon inorganic dissolved Carbonate ion Carbonate system computation flag Carbon dioxide Coast and continental shelf Experiment Fugacity of carbon dioxide (water) at sea surface temperature (wet air) Growth/Morphology Laboratory experiment Mollusca North Pacific OA-ICC Ocean Acidification International Coordination Centre Ostrea lurida Partial pressure of carbon dioxide (water) at sea surface temperature (wet air) Pelagos pH Proportion Registration number of species Replicate Salinity Shell length standard deviation Single species Species Temperate Temperature water Treatment Type Uniform resource locator/link to reference Zooplankton Dataset 2016 ftpangaea https://doi.org/10.1594/PANGAEA.868738 https://doi.org/10.1002/lno.10348 2023-01-20T09:08:13Z 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. Dataset Crassostrea gigas Ocean acidification Pacific oyster PANGAEA - Data Publisher for Earth & Environmental Science Pacific |