Phenotypic plasticity of coralline algae in a High CO2 world
It is important to understand how marine calcifying organisms may acclimatize to ocean acidification to assess their survival over the coming century. We cultured the cold water coralline algae, Lithothamnion glaciale, under elevated pCO2 (408, 566, 770, and 1024 µatm) for 10 months. The results sho...
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ftpangaea:oai:pangaea.de:doi:10.1594/PANGAEA.831831 2024-09-30T14:39:43+00:00 Phenotypic plasticity of coralline algae in a High CO2 world Ragazzola, Federica 2013 text/tab-separated-values, 21046 data points https://doi.pangaea.de/10.1594/PANGAEA.831831 https://doi.org/10.1594/PANGAEA.831831 en eng PANGAEA Lavigne, Héloïse; Gattuso, Jean-Pierre (2011): seacarb: seawater carbonate chemistry with R. R package version 2.4 [webpage]. https://cran.r-project.org/package=seacarb https://doi.pangaea.de/10.1594/PANGAEA.831831 https://doi.org/10.1594/PANGAEA.831831 CC-BY-3.0: Creative Commons Attribution 3.0 Unported Access constraints: unrestricted info:eu-repo/semantics/openAccess Supplement to: Ragazzola, Federica; Foster, Laura C; Form, Armin; Büscher, Janina; Hansteen, Thor H; Fietzke, Jan (2013): Phenotypic plasticity of coralline algae in a High CO2 world. Ecology and Evolution, 3, 3436-3446, https://doi.org/10.1002/ece3.723 Alkalinity total standard deviation Aragonite saturation state Benthos Bicarbonate ion BIOACID Biological Impacts of Ocean Acidification 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 Cell biovolume Coast and continental shelf Fugacity of carbon dioxide (water) at sea surface temperature (wet air) Growth/Morphology Growth rate Laboratory experiment Lithothamnion glaciale Macroalgae Magnesium carbonate magnesite North Atlantic OA-ICC Ocean Acidification International Coordination Centre Partial pressure of carbon dioxide Partial pressure of carbon dioxide (water) at sea surface temperature (wet air) pH dataset 2013 ftpangaea https://doi.org/10.1594/PANGAEA.83183110.1002/ece3.723 2024-09-18T00:10:44Z It is important to understand how marine calcifying organisms may acclimatize to ocean acidification to assess their survival over the coming century. We cultured the cold water coralline algae, Lithothamnion glaciale, under elevated pCO2 (408, 566, 770, and 1024 µatm) for 10 months. The results show that the cell (inter and intra) wall thickness is maintained, but there is a reduction in growth rate (linear extension) at all elevated pCO2. Furthermore a decrease in Mg content at the two highest CO2 treatments was observed. Comparison between our data and that at 3 months from the same long-term experiment shows that the acclimation differs over time since at 3 months, the samples cultured under high pCO2 showed a reduction in the cell (inter and intra) wall thickness but a maintained growth rate. This suggests a reallocation of the energy budget between 3 and 10 months and highlights the high degree plasticity that is present. This might provide a selective advantage in future high CO2 world. Dataset North Atlantic 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 Benthos Bicarbonate ion BIOACID Biological Impacts of Ocean Acidification 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 Cell biovolume Coast and continental shelf Fugacity of carbon dioxide (water) at sea surface temperature (wet air) Growth/Morphology Growth rate Laboratory experiment Lithothamnion glaciale Macroalgae Magnesium carbonate magnesite North Atlantic OA-ICC Ocean Acidification International Coordination Centre Partial pressure of carbon dioxide Partial pressure of carbon dioxide (water) at sea surface temperature (wet air) pH |
spellingShingle |
Alkalinity total standard deviation Aragonite saturation state Benthos Bicarbonate ion BIOACID Biological Impacts of Ocean Acidification 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 Cell biovolume Coast and continental shelf Fugacity of carbon dioxide (water) at sea surface temperature (wet air) Growth/Morphology Growth rate Laboratory experiment Lithothamnion glaciale Macroalgae Magnesium carbonate magnesite North Atlantic OA-ICC Ocean Acidification International Coordination Centre Partial pressure of carbon dioxide Partial pressure of carbon dioxide (water) at sea surface temperature (wet air) pH Ragazzola, Federica Phenotypic plasticity of coralline algae in a High CO2 world |
topic_facet |
Alkalinity total standard deviation Aragonite saturation state Benthos Bicarbonate ion BIOACID Biological Impacts of Ocean Acidification 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 Cell biovolume Coast and continental shelf Fugacity of carbon dioxide (water) at sea surface temperature (wet air) Growth/Morphology Growth rate Laboratory experiment Lithothamnion glaciale Macroalgae Magnesium carbonate magnesite North Atlantic OA-ICC Ocean Acidification International Coordination Centre Partial pressure of carbon dioxide Partial pressure of carbon dioxide (water) at sea surface temperature (wet air) pH |
description |
It is important to understand how marine calcifying organisms may acclimatize to ocean acidification to assess their survival over the coming century. We cultured the cold water coralline algae, Lithothamnion glaciale, under elevated pCO2 (408, 566, 770, and 1024 µatm) for 10 months. The results show that the cell (inter and intra) wall thickness is maintained, but there is a reduction in growth rate (linear extension) at all elevated pCO2. Furthermore a decrease in Mg content at the two highest CO2 treatments was observed. Comparison between our data and that at 3 months from the same long-term experiment shows that the acclimation differs over time since at 3 months, the samples cultured under high pCO2 showed a reduction in the cell (inter and intra) wall thickness but a maintained growth rate. This suggests a reallocation of the energy budget between 3 and 10 months and highlights the high degree plasticity that is present. This might provide a selective advantage in future high CO2 world. |
format |
Dataset |
author |
Ragazzola, Federica |
author_facet |
Ragazzola, Federica |
author_sort |
Ragazzola, Federica |
title |
Phenotypic plasticity of coralline algae in a High CO2 world |
title_short |
Phenotypic plasticity of coralline algae in a High CO2 world |
title_full |
Phenotypic plasticity of coralline algae in a High CO2 world |
title_fullStr |
Phenotypic plasticity of coralline algae in a High CO2 world |
title_full_unstemmed |
Phenotypic plasticity of coralline algae in a High CO2 world |
title_sort |
phenotypic plasticity of coralline algae in a high co2 world |
publisher |
PANGAEA |
publishDate |
2013 |
url |
https://doi.pangaea.de/10.1594/PANGAEA.831831 https://doi.org/10.1594/PANGAEA.831831 |
genre |
North Atlantic Ocean acidification |
genre_facet |
North Atlantic Ocean acidification |
op_source |
Supplement to: Ragazzola, Federica; Foster, Laura C; Form, Armin; Büscher, Janina; Hansteen, Thor H; Fietzke, Jan (2013): Phenotypic plasticity of coralline algae in a High CO2 world. Ecology and Evolution, 3, 3436-3446, https://doi.org/10.1002/ece3.723 |
op_relation |
Lavigne, Héloïse; Gattuso, Jean-Pierre (2011): seacarb: seawater carbonate chemistry with R. R package version 2.4 [webpage]. https://cran.r-project.org/package=seacarb https://doi.pangaea.de/10.1594/PANGAEA.831831 https://doi.org/10.1594/PANGAEA.831831 |
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.83183110.1002/ece3.723 |
_version_ |
1811642328326078464 |