Reduced calcification and lack of acclimatization by coral colonies growing in areas of persistent natural acidification, supplement to: Crook, Elizabeth Derse; Cohen, Anne L; Rebolledo-Vieyra, Mario; Hernandez, Laura; Paytan, Adina (2013): Reduced calcification and lack of acclimatization by coral colonies growing in areas of persistent natural acidification. Proceedings of the National Academy of Sciences, 110(27), 11044-11049
As the surface ocean equilibrates with rising atmospheric CO2, the pH of surface seawater is decreasing with potentially negative impacts on coral calcification. A critical question is whether corals will be able to adapt or acclimate to these changes in seawater chemistry. We use high precision CT...
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ftdatacite:10.1594/pangaea.831619 2023-05-15T17:37:10+02:00 Reduced calcification and lack of acclimatization by coral colonies growing in areas of persistent natural acidification, supplement to: Crook, Elizabeth Derse; Cohen, Anne L; Rebolledo-Vieyra, Mario; Hernandez, Laura; Paytan, Adina (2013): Reduced calcification and lack of acclimatization by coral colonies growing in areas of persistent natural acidification. Proceedings of the National Academy of Sciences, 110(27), 11044-11049 Crook, Elizabeth Derse Cohen, Anne L Rebolledo-Vieyra, Mario Hernandez, Laura Paytan, Adina 2013 text/tab-separated-values https://dx.doi.org/10.1594/pangaea.831619 https://doi.pangaea.de/10.1594/PANGAEA.831619 en eng PANGAEA - Data Publisher for Earth & Environmental Science https://cran.r-project.org/package=seacarb https://dx.doi.org/10.1073/pnas.1301589110 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 Benthic animals Benthos Calcification/Dissolution Cnidaria Field observation Growth/Morphology North Atlantic Porites astreoides Single species Tropical Figure Species Treatment Linear extension Linear extension, standard deviation Linear extension, standard error Density Density, standard deviation Density, standard error Calcification rate Calcification rate, standard deviation Calcification rate, standard error Thickness Thickness, standard deviation Thickness, standard error Volume ratio Salinity Temperature, water Carbon, inorganic, dissolved Carbon, inorganic, dissolved, standard deviation Alkalinity, total Alkalinity, total, standard deviation pH Aragonite saturation state Aragonite saturation state, standard deviation Calcification rate, ratio Carbonate system computation flag Carbon dioxide Partial pressure of carbon dioxide water at sea surface temperature wet air Fugacity of carbon dioxide water at sea surface temperature wet air Bicarbonate ion Carbonate ion Calcite saturation state Calculated using CO2SYS Calculated using seacarb after Nisumaa et al. 2010 Ocean Acidification International Coordination Centre OA-ICC Supplementary Dataset dataset Dataset 2013 ftdatacite https://doi.org/10.1594/pangaea.831619 https://doi.org/10.1073/pnas.1301589110 2021-11-05T12:55:41Z As the surface ocean equilibrates with rising atmospheric CO2, the pH of surface seawater is decreasing with potentially negative impacts on coral calcification. A critical question is whether corals will be able to adapt or acclimate to these changes in seawater chemistry. We use high precision CT scanning of skeletal cores of Porites astreoides, an important Caribbean reef-building coral, to show that calcification rates decrease significantly along a natural gradient in pH and aragonite saturation (Omega arag). This decrease is accompanied by an increase in skeletal erosion and predation by boring organisms. The degree of sensitivity to reduced Oarag measured on our field corals is consistent with that exhibited by the same species in laboratory CO2 manipulation experiments. We conclude that the Porites corals at our field site were not able to acclimatize enough to prevent the impacts of local ocean acidification on their skeletal growth and development, despite spending their entire lifespan in low pH, low Omega arag seawater. : In order to allow full comparability with other ocean acidification data sets, the R package seacarb (Lavigne and Gattuso, 2011) 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 by seacarb is 2014-04-09. Dataset North Atlantic Ocean acidification DataCite Metadata Store (German National Library of Science and Technology) Hernandez ENVELOPE(-62.167,-62.167,-74.500,-74.500) |
institution |
Open Polar |
collection |
DataCite Metadata Store (German National Library of Science and Technology) |
op_collection_id |
ftdatacite |
language |
English |
topic |
Animalia Benthic animals Benthos Calcification/Dissolution Cnidaria Field observation Growth/Morphology North Atlantic Porites astreoides Single species Tropical Figure Species Treatment Linear extension Linear extension, standard deviation Linear extension, standard error Density Density, standard deviation Density, standard error Calcification rate Calcification rate, standard deviation Calcification rate, standard error Thickness Thickness, standard deviation Thickness, standard error Volume ratio Salinity Temperature, water Carbon, inorganic, dissolved Carbon, inorganic, dissolved, standard deviation Alkalinity, total Alkalinity, total, standard deviation pH Aragonite saturation state Aragonite saturation state, standard deviation Calcification rate, ratio Carbonate system computation flag Carbon dioxide Partial pressure of carbon dioxide water at sea surface temperature wet air Fugacity of carbon dioxide water at sea surface temperature wet air Bicarbonate ion Carbonate ion Calcite saturation state Calculated using CO2SYS Calculated using seacarb after Nisumaa et al. 2010 Ocean Acidification International Coordination Centre OA-ICC |
spellingShingle |
Animalia Benthic animals Benthos Calcification/Dissolution Cnidaria Field observation Growth/Morphology North Atlantic Porites astreoides Single species Tropical Figure Species Treatment Linear extension Linear extension, standard deviation Linear extension, standard error Density Density, standard deviation Density, standard error Calcification rate Calcification rate, standard deviation Calcification rate, standard error Thickness Thickness, standard deviation Thickness, standard error Volume ratio Salinity Temperature, water Carbon, inorganic, dissolved Carbon, inorganic, dissolved, standard deviation Alkalinity, total Alkalinity, total, standard deviation pH Aragonite saturation state Aragonite saturation state, standard deviation Calcification rate, ratio Carbonate system computation flag Carbon dioxide Partial pressure of carbon dioxide water at sea surface temperature wet air Fugacity of carbon dioxide water at sea surface temperature wet air Bicarbonate ion Carbonate ion Calcite saturation state Calculated using CO2SYS Calculated using seacarb after Nisumaa et al. 2010 Ocean Acidification International Coordination Centre OA-ICC Crook, Elizabeth Derse Cohen, Anne L Rebolledo-Vieyra, Mario Hernandez, Laura Paytan, Adina Reduced calcification and lack of acclimatization by coral colonies growing in areas of persistent natural acidification, supplement to: Crook, Elizabeth Derse; Cohen, Anne L; Rebolledo-Vieyra, Mario; Hernandez, Laura; Paytan, Adina (2013): Reduced calcification and lack of acclimatization by coral colonies growing in areas of persistent natural acidification. Proceedings of the National Academy of Sciences, 110(27), 11044-11049 |
topic_facet |
Animalia Benthic animals Benthos Calcification/Dissolution Cnidaria Field observation Growth/Morphology North Atlantic Porites astreoides Single species Tropical Figure Species Treatment Linear extension Linear extension, standard deviation Linear extension, standard error Density Density, standard deviation Density, standard error Calcification rate Calcification rate, standard deviation Calcification rate, standard error Thickness Thickness, standard deviation Thickness, standard error Volume ratio Salinity Temperature, water Carbon, inorganic, dissolved Carbon, inorganic, dissolved, standard deviation Alkalinity, total Alkalinity, total, standard deviation pH Aragonite saturation state Aragonite saturation state, standard deviation Calcification rate, ratio Carbonate system computation flag Carbon dioxide Partial pressure of carbon dioxide water at sea surface temperature wet air Fugacity of carbon dioxide water at sea surface temperature wet air Bicarbonate ion Carbonate ion Calcite saturation state Calculated using CO2SYS Calculated using seacarb after Nisumaa et al. 2010 Ocean Acidification International Coordination Centre OA-ICC |
description |
As the surface ocean equilibrates with rising atmospheric CO2, the pH of surface seawater is decreasing with potentially negative impacts on coral calcification. A critical question is whether corals will be able to adapt or acclimate to these changes in seawater chemistry. We use high precision CT scanning of skeletal cores of Porites astreoides, an important Caribbean reef-building coral, to show that calcification rates decrease significantly along a natural gradient in pH and aragonite saturation (Omega arag). This decrease is accompanied by an increase in skeletal erosion and predation by boring organisms. The degree of sensitivity to reduced Oarag measured on our field corals is consistent with that exhibited by the same species in laboratory CO2 manipulation experiments. We conclude that the Porites corals at our field site were not able to acclimatize enough to prevent the impacts of local ocean acidification on their skeletal growth and development, despite spending their entire lifespan in low pH, low Omega arag seawater. : In order to allow full comparability with other ocean acidification data sets, the R package seacarb (Lavigne and Gattuso, 2011) 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 by seacarb is 2014-04-09. |
format |
Dataset |
author |
Crook, Elizabeth Derse Cohen, Anne L Rebolledo-Vieyra, Mario Hernandez, Laura Paytan, Adina |
author_facet |
Crook, Elizabeth Derse Cohen, Anne L Rebolledo-Vieyra, Mario Hernandez, Laura Paytan, Adina |
author_sort |
Crook, Elizabeth Derse |
title |
Reduced calcification and lack of acclimatization by coral colonies growing in areas of persistent natural acidification, supplement to: Crook, Elizabeth Derse; Cohen, Anne L; Rebolledo-Vieyra, Mario; Hernandez, Laura; Paytan, Adina (2013): Reduced calcification and lack of acclimatization by coral colonies growing in areas of persistent natural acidification. Proceedings of the National Academy of Sciences, 110(27), 11044-11049 |
title_short |
Reduced calcification and lack of acclimatization by coral colonies growing in areas of persistent natural acidification, supplement to: Crook, Elizabeth Derse; Cohen, Anne L; Rebolledo-Vieyra, Mario; Hernandez, Laura; Paytan, Adina (2013): Reduced calcification and lack of acclimatization by coral colonies growing in areas of persistent natural acidification. Proceedings of the National Academy of Sciences, 110(27), 11044-11049 |
title_full |
Reduced calcification and lack of acclimatization by coral colonies growing in areas of persistent natural acidification, supplement to: Crook, Elizabeth Derse; Cohen, Anne L; Rebolledo-Vieyra, Mario; Hernandez, Laura; Paytan, Adina (2013): Reduced calcification and lack of acclimatization by coral colonies growing in areas of persistent natural acidification. Proceedings of the National Academy of Sciences, 110(27), 11044-11049 |
title_fullStr |
Reduced calcification and lack of acclimatization by coral colonies growing in areas of persistent natural acidification, supplement to: Crook, Elizabeth Derse; Cohen, Anne L; Rebolledo-Vieyra, Mario; Hernandez, Laura; Paytan, Adina (2013): Reduced calcification and lack of acclimatization by coral colonies growing in areas of persistent natural acidification. Proceedings of the National Academy of Sciences, 110(27), 11044-11049 |
title_full_unstemmed |
Reduced calcification and lack of acclimatization by coral colonies growing in areas of persistent natural acidification, supplement to: Crook, Elizabeth Derse; Cohen, Anne L; Rebolledo-Vieyra, Mario; Hernandez, Laura; Paytan, Adina (2013): Reduced calcification and lack of acclimatization by coral colonies growing in areas of persistent natural acidification. Proceedings of the National Academy of Sciences, 110(27), 11044-11049 |
title_sort |
reduced calcification and lack of acclimatization by coral colonies growing in areas of persistent natural acidification, supplement to: crook, elizabeth derse; cohen, anne l; rebolledo-vieyra, mario; hernandez, laura; paytan, adina (2013): reduced calcification and lack of acclimatization by coral colonies growing in areas of persistent natural acidification. proceedings of the national academy of sciences, 110(27), 11044-11049 |
publisher |
PANGAEA - Data Publisher for Earth & Environmental Science |
publishDate |
2013 |
url |
https://dx.doi.org/10.1594/pangaea.831619 https://doi.pangaea.de/10.1594/PANGAEA.831619 |
long_lat |
ENVELOPE(-62.167,-62.167,-74.500,-74.500) |
geographic |
Hernandez |
geographic_facet |
Hernandez |
genre |
North Atlantic Ocean acidification |
genre_facet |
North Atlantic Ocean acidification |
op_relation |
https://cran.r-project.org/package=seacarb https://dx.doi.org/10.1073/pnas.1301589110 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.831619 https://doi.org/10.1073/pnas.1301589110 |
_version_ |
1766136942516240384 |