Reduced resilience of a globally distributed coccolithophore to ocean acidification: Confirmed up to 2000 generations
Ocean acidification (OA), induced by rapid anthropogenic CO2 rise and its dissolution in seawater, is known to have consequences for marine organisms. However, knowledge on the evolutionary responses of phytoplankton to OA has been poorly studied. Here we examined the coccolithophore Gephyrocapsa oc...
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ftpangaea:oai:pangaea.de:doi:10.1594/PANGAEA.860281 2024-09-15T18:27:55+00:00 Reduced resilience of a globally distributed coccolithophore to ocean acidification: Confirmed up to 2000 generations Jin, Peng Gao, Kunshan 2016 text/tab-separated-values, 25329 data points https://doi.pangaea.de/10.1594/PANGAEA.860281 https://doi.org/10.1594/PANGAEA.860281 en eng PANGAEA Gattuso, Jean-Pierre; Epitalon, Jean-Marie; Lavigne, Héloïse (2015): seacarb: seawater carbonate chemistry with R. R package version 3.0.8. https://cran.r-project.org/package=seacarb https://doi.pangaea.de/10.1594/PANGAEA.860281 https://doi.org/10.1594/PANGAEA.860281 CC-BY-3.0: Creative Commons Attribution 3.0 Unported Access constraints: unrestricted info:eu-repo/semantics/openAccess Supplement to: Jin, Peng; Gao, Kunshan (2016): Reduced resilience of a globally distributed coccolithophore to ocean acidification: Confirmed up to 2000 generations. Marine Pollution Bulletin, 103(1-2), 101-108, https://doi.org/10.1016/j.marpolbul.2015.12.039 Alkalinity total standard deviation Aragonite saturation state Bicarbonate Bicarbonate ion Biomass/Abundance/Elemental composition Bottles or small containers/Aquaria (<20 L) Calcite saturation state Calculated using CO2SYS Calculated using seacarb after Nisumaa et al. (2010) Carbon inorganic dissolved organic particulate per cell production per cell Carbon/Nitrogen ratio Carbonate ion Carbonate system computation flag Carbon dioxide Chromista Fugacity of carbon dioxide (water) at sea surface temperature (wet air) Generation Gephyrocapsa oceanica Growth/Morphology Growth rate Haptophyta Incubation duration Laboratory experiment Laboratory strains Nitrogen North Pacific dataset 2016 ftpangaea https://doi.org/10.1594/PANGAEA.86028110.1016/j.marpolbul.2015.12.039 2024-07-24T02:31:33Z Ocean acidification (OA), induced by rapid anthropogenic CO2 rise and its dissolution in seawater, is known to have consequences for marine organisms. However, knowledge on the evolutionary responses of phytoplankton to OA has been poorly studied. Here we examined the coccolithophore Gephyrocapsa oceanica, while growing it for 2000 generations under ambient and elevated CO2 levels. While OA stimulated growth in the earlier selection period (from generations 700 to 1550), it reduced it in the later selection period up to 2000 generations. Similarly, stimulated production of particulate organic carbon and nitrogen reduced with increasing selection period and decreased under OA up to 2000 generations. The specific adaptation of growth to OA disappeared in generations 1700 to 2000 when compared with that at 1000 generations. Both phenotypic plasticity and fitness decreased within selection time, suggesting that the species' resilience to OA decreased after 2000 generations under high CO2 selection. Dataset Ocean acidification PANGAEA - Data Publisher for Earth & Environmental Science |
institution |
Open Polar |
collection |
PANGAEA - Data Publisher for Earth & Environmental Science |
op_collection_id |
ftpangaea |
language |
English |
topic |
Alkalinity total standard deviation Aragonite saturation state Bicarbonate Bicarbonate ion Biomass/Abundance/Elemental composition Bottles or small containers/Aquaria (<20 L) Calcite saturation state Calculated using CO2SYS Calculated using seacarb after Nisumaa et al. (2010) Carbon inorganic dissolved organic particulate per cell production per cell Carbon/Nitrogen ratio Carbonate ion Carbonate system computation flag Carbon dioxide Chromista Fugacity of carbon dioxide (water) at sea surface temperature (wet air) Generation Gephyrocapsa oceanica Growth/Morphology Growth rate Haptophyta Incubation duration Laboratory experiment Laboratory strains Nitrogen North Pacific |
spellingShingle |
Alkalinity total standard deviation Aragonite saturation state Bicarbonate Bicarbonate ion Biomass/Abundance/Elemental composition Bottles or small containers/Aquaria (<20 L) Calcite saturation state Calculated using CO2SYS Calculated using seacarb after Nisumaa et al. (2010) Carbon inorganic dissolved organic particulate per cell production per cell Carbon/Nitrogen ratio Carbonate ion Carbonate system computation flag Carbon dioxide Chromista Fugacity of carbon dioxide (water) at sea surface temperature (wet air) Generation Gephyrocapsa oceanica Growth/Morphology Growth rate Haptophyta Incubation duration Laboratory experiment Laboratory strains Nitrogen North Pacific Jin, Peng Gao, Kunshan Reduced resilience of a globally distributed coccolithophore to ocean acidification: Confirmed up to 2000 generations |
topic_facet |
Alkalinity total standard deviation Aragonite saturation state Bicarbonate Bicarbonate ion Biomass/Abundance/Elemental composition Bottles or small containers/Aquaria (<20 L) Calcite saturation state Calculated using CO2SYS Calculated using seacarb after Nisumaa et al. (2010) Carbon inorganic dissolved organic particulate per cell production per cell Carbon/Nitrogen ratio Carbonate ion Carbonate system computation flag Carbon dioxide Chromista Fugacity of carbon dioxide (water) at sea surface temperature (wet air) Generation Gephyrocapsa oceanica Growth/Morphology Growth rate Haptophyta Incubation duration Laboratory experiment Laboratory strains Nitrogen North Pacific |
description |
Ocean acidification (OA), induced by rapid anthropogenic CO2 rise and its dissolution in seawater, is known to have consequences for marine organisms. However, knowledge on the evolutionary responses of phytoplankton to OA has been poorly studied. Here we examined the coccolithophore Gephyrocapsa oceanica, while growing it for 2000 generations under ambient and elevated CO2 levels. While OA stimulated growth in the earlier selection period (from generations 700 to 1550), it reduced it in the later selection period up to 2000 generations. Similarly, stimulated production of particulate organic carbon and nitrogen reduced with increasing selection period and decreased under OA up to 2000 generations. The specific adaptation of growth to OA disappeared in generations 1700 to 2000 when compared with that at 1000 generations. Both phenotypic plasticity and fitness decreased within selection time, suggesting that the species' resilience to OA decreased after 2000 generations under high CO2 selection. |
format |
Dataset |
author |
Jin, Peng Gao, Kunshan |
author_facet |
Jin, Peng Gao, Kunshan |
author_sort |
Jin, Peng |
title |
Reduced resilience of a globally distributed coccolithophore to ocean acidification: Confirmed up to 2000 generations |
title_short |
Reduced resilience of a globally distributed coccolithophore to ocean acidification: Confirmed up to 2000 generations |
title_full |
Reduced resilience of a globally distributed coccolithophore to ocean acidification: Confirmed up to 2000 generations |
title_fullStr |
Reduced resilience of a globally distributed coccolithophore to ocean acidification: Confirmed up to 2000 generations |
title_full_unstemmed |
Reduced resilience of a globally distributed coccolithophore to ocean acidification: Confirmed up to 2000 generations |
title_sort |
reduced resilience of a globally distributed coccolithophore to ocean acidification: confirmed up to 2000 generations |
publisher |
PANGAEA |
publishDate |
2016 |
url |
https://doi.pangaea.de/10.1594/PANGAEA.860281 https://doi.org/10.1594/PANGAEA.860281 |
genre |
Ocean acidification |
genre_facet |
Ocean acidification |
op_source |
Supplement to: Jin, Peng; Gao, Kunshan (2016): Reduced resilience of a globally distributed coccolithophore to ocean acidification: Confirmed up to 2000 generations. Marine Pollution Bulletin, 103(1-2), 101-108, https://doi.org/10.1016/j.marpolbul.2015.12.039 |
op_relation |
Gattuso, Jean-Pierre; Epitalon, Jean-Marie; Lavigne, Héloïse (2015): seacarb: seawater carbonate chemistry with R. R package version 3.0.8. https://cran.r-project.org/package=seacarb https://doi.pangaea.de/10.1594/PANGAEA.860281 https://doi.org/10.1594/PANGAEA.860281 |
op_rights |
CC-BY-3.0: Creative Commons Attribution 3.0 Unported Access constraints: unrestricted info:eu-repo/semantics/openAccess |
op_doi |
https://doi.org/10.1594/PANGAEA.86028110.1016/j.marpolbul.2015.12.039 |
_version_ |
1810469210542833664 |