Seawater carbonate chemistry and the photophysiology of Thalassiosira pseudonana (Bacillariophyceae) and Emiliania huxleyi (Haptophyta) in a laboratory experiment
Increasing anthropogenic carbon dioxide is causing changes to ocean chemistry, which will continue in a predictable manner. Dissolution of additional atmospheric carbon dioxide leads to increased concentrations of dissolved carbon dioxide and bicarbonate and decreased pH in ocean water. The concomit...
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Language: | English |
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PANGAEA
2012
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Online Access: | https://doi.pangaea.de/10.1594/PANGAEA.824665 https://doi.org/10.1594/PANGAEA.824665 |
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ftpangaea:oai:pangaea.de:doi:10.1594/PANGAEA.824665 |
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record_format |
openpolar |
institution |
Open Polar |
collection |
PANGAEA - Data Publisher for Earth & Environmental Science |
op_collection_id |
ftpangaea |
language |
English |
topic |
Alkalinity total Aragonite saturation state Bicarbonate ion 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 Carbon/Nitrogen ratio Carbonate ion Carbonate system computation flag Carbon dioxide Cell biovolume Cell density CF1 subunit of ATP synthase protein Chlorophyll a Chlorophyll c1/chlorophyll a ratio Chlorophyll c2/chlorophyll a ratio Chlorophyll c3/chlorophyll a ratio Chromista Cytochrome c1 Diadinoxanthin/chlorophyll a ratio Diatoxanthin/chlorophyll a ratio Effective absorbance cross-section of photosystem II Emiliania huxleyi Fucoxanthin/chlorophyll a ratio Fugacity of carbon dioxide (water) at sea surface temperature (wet air) Growth/Morphology Growth rate Haptophyta Identification Irradiance Laboratory experiment Laboratory strains Non photochemical quenching North Atlantic OA-ICC Ocean Acidification International Coordination Centre Ochrophyta Partial pressure of carbon dioxide (water) at sea surface temperature (wet air) Pelagos pH Phosphate |
spellingShingle |
Alkalinity total Aragonite saturation state Bicarbonate ion 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 Carbon/Nitrogen ratio Carbonate ion Carbonate system computation flag Carbon dioxide Cell biovolume Cell density CF1 subunit of ATP synthase protein Chlorophyll a Chlorophyll c1/chlorophyll a ratio Chlorophyll c2/chlorophyll a ratio Chlorophyll c3/chlorophyll a ratio Chromista Cytochrome c1 Diadinoxanthin/chlorophyll a ratio Diatoxanthin/chlorophyll a ratio Effective absorbance cross-section of photosystem II Emiliania huxleyi Fucoxanthin/chlorophyll a ratio Fugacity of carbon dioxide (water) at sea surface temperature (wet air) Growth/Morphology Growth rate Haptophyta Identification Irradiance Laboratory experiment Laboratory strains Non photochemical quenching North Atlantic OA-ICC Ocean Acidification International Coordination Centre Ochrophyta Partial pressure of carbon dioxide (water) at sea surface temperature (wet air) Pelagos pH Phosphate McCarthy, Avery Rogers, Susan P Duffy, Stephen J Campbell, Douglas A Seawater carbonate chemistry and the photophysiology of Thalassiosira pseudonana (Bacillariophyceae) and Emiliania huxleyi (Haptophyta) in a laboratory experiment |
topic_facet |
Alkalinity total Aragonite saturation state Bicarbonate ion 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 Carbon/Nitrogen ratio Carbonate ion Carbonate system computation flag Carbon dioxide Cell biovolume Cell density CF1 subunit of ATP synthase protein Chlorophyll a Chlorophyll c1/chlorophyll a ratio Chlorophyll c2/chlorophyll a ratio Chlorophyll c3/chlorophyll a ratio Chromista Cytochrome c1 Diadinoxanthin/chlorophyll a ratio Diatoxanthin/chlorophyll a ratio Effective absorbance cross-section of photosystem II Emiliania huxleyi Fucoxanthin/chlorophyll a ratio Fugacity of carbon dioxide (water) at sea surface temperature (wet air) Growth/Morphology Growth rate Haptophyta Identification Irradiance Laboratory experiment Laboratory strains Non photochemical quenching North Atlantic OA-ICC Ocean Acidification International Coordination Centre Ochrophyta Partial pressure of carbon dioxide (water) at sea surface temperature (wet air) Pelagos pH Phosphate |
description |
Increasing anthropogenic carbon dioxide is causing changes to ocean chemistry, which will continue in a predictable manner. Dissolution of additional atmospheric carbon dioxide leads to increased concentrations of dissolved carbon dioxide and bicarbonate and decreased pH in ocean water. The concomitant effects on phytoplankton ecophysiology, leading potentially to changes in community structure, are now a focus of concern. Therefore, we grew the coccolithophore Emiliania huxleyi (Lohmann) W. W. Hay et H. Mohler and the diatom strains Thalassiosira pseudonana (Hust.) Hasle et Heimdal CCMP 1014 and T. pseudonana CCMP 1335 under low light in turbidostat photobioreactors bubbled with air containing 390 ppmv or 750 ppmv CO2. Increased pCO2 led to increased growth rates in all three strains. In addition, protein levels of RUBISCO increased in the coastal strains of both species, showing a larger capacity for CO2 assimilation at 750 ppmv CO2. With increased pCO2, both T. pseudonana strains displayed an increased susceptibility to PSII photoinactivation and, to compensate, an augmented capacity for PSII repair. Consequently, the cost of maintaining PSII function for the diatoms increased at increased pCO2. In E. huxleyi, PSII photoinactivation and the counter-acting repair, while both intrinsically larger than in T. pseudonana, did not change between the current and high-pCO2 treatments. The content of the photosynthetic electron transport intermediary cytochrome b6/f complex increased significantly in the diatoms under elevated pCO2, suggesting changes in electron transport function. |
format |
Dataset |
author |
McCarthy, Avery Rogers, Susan P Duffy, Stephen J Campbell, Douglas A |
author_facet |
McCarthy, Avery Rogers, Susan P Duffy, Stephen J Campbell, Douglas A |
author_sort |
McCarthy, Avery |
title |
Seawater carbonate chemistry and the photophysiology of Thalassiosira pseudonana (Bacillariophyceae) and Emiliania huxleyi (Haptophyta) in a laboratory experiment |
title_short |
Seawater carbonate chemistry and the photophysiology of Thalassiosira pseudonana (Bacillariophyceae) and Emiliania huxleyi (Haptophyta) in a laboratory experiment |
title_full |
Seawater carbonate chemistry and the photophysiology of Thalassiosira pseudonana (Bacillariophyceae) and Emiliania huxleyi (Haptophyta) in a laboratory experiment |
title_fullStr |
Seawater carbonate chemistry and the photophysiology of Thalassiosira pseudonana (Bacillariophyceae) and Emiliania huxleyi (Haptophyta) in a laboratory experiment |
title_full_unstemmed |
Seawater carbonate chemistry and the photophysiology of Thalassiosira pseudonana (Bacillariophyceae) and Emiliania huxleyi (Haptophyta) in a laboratory experiment |
title_sort |
seawater carbonate chemistry and the photophysiology of thalassiosira pseudonana (bacillariophyceae) and emiliania huxleyi (haptophyta) in a laboratory experiment |
publisher |
PANGAEA |
publishDate |
2012 |
url |
https://doi.pangaea.de/10.1594/PANGAEA.824665 https://doi.org/10.1594/PANGAEA.824665 |
genre |
North Atlantic Ocean acidification |
genre_facet |
North Atlantic Ocean acidification |
op_source |
Supplement to: McCarthy, Avery; Rogers, Susan P; Duffy, Stephen J; Campbell, Douglas A (2012): Elevated carbon dioxide differentially alters the photophysiology of Thalassiosira pseudonana (Bacillariophyceae) and Emiliania huxleyi (Haptophyta). Journal of Phycology, 48(3), 635-646, https://doi.org/10.1111/j.1529-8817.2012.01171.x |
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.824665 https://doi.org/10.1594/PANGAEA.824665 |
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.82466510.1111/j.1529-8817.2012.01171.x |
_version_ |
1810464812089475072 |
spelling |
ftpangaea:oai:pangaea.de:doi:10.1594/PANGAEA.824665 2024-09-15T18:24:27+00:00 Seawater carbonate chemistry and the photophysiology of Thalassiosira pseudonana (Bacillariophyceae) and Emiliania huxleyi (Haptophyta) in a laboratory experiment McCarthy, Avery Rogers, Susan P Duffy, Stephen J Campbell, Douglas A 2012 text/tab-separated-values, 1086 data points https://doi.pangaea.de/10.1594/PANGAEA.824665 https://doi.org/10.1594/PANGAEA.824665 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.824665 https://doi.org/10.1594/PANGAEA.824665 CC-BY-3.0: Creative Commons Attribution 3.0 Unported Access constraints: unrestricted info:eu-repo/semantics/openAccess Supplement to: McCarthy, Avery; Rogers, Susan P; Duffy, Stephen J; Campbell, Douglas A (2012): Elevated carbon dioxide differentially alters the photophysiology of Thalassiosira pseudonana (Bacillariophyceae) and Emiliania huxleyi (Haptophyta). Journal of Phycology, 48(3), 635-646, https://doi.org/10.1111/j.1529-8817.2012.01171.x Alkalinity total Aragonite saturation state Bicarbonate ion 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 Carbon/Nitrogen ratio Carbonate ion Carbonate system computation flag Carbon dioxide Cell biovolume Cell density CF1 subunit of ATP synthase protein Chlorophyll a Chlorophyll c1/chlorophyll a ratio Chlorophyll c2/chlorophyll a ratio Chlorophyll c3/chlorophyll a ratio Chromista Cytochrome c1 Diadinoxanthin/chlorophyll a ratio Diatoxanthin/chlorophyll a ratio Effective absorbance cross-section of photosystem II Emiliania huxleyi Fucoxanthin/chlorophyll a ratio Fugacity of carbon dioxide (water) at sea surface temperature (wet air) Growth/Morphology Growth rate Haptophyta Identification Irradiance Laboratory experiment Laboratory strains Non photochemical quenching North Atlantic OA-ICC Ocean Acidification International Coordination Centre Ochrophyta Partial pressure of carbon dioxide (water) at sea surface temperature (wet air) Pelagos pH Phosphate dataset 2012 ftpangaea https://doi.org/10.1594/PANGAEA.82466510.1111/j.1529-8817.2012.01171.x 2024-07-24T02:31:32Z Increasing anthropogenic carbon dioxide is causing changes to ocean chemistry, which will continue in a predictable manner. Dissolution of additional atmospheric carbon dioxide leads to increased concentrations of dissolved carbon dioxide and bicarbonate and decreased pH in ocean water. The concomitant effects on phytoplankton ecophysiology, leading potentially to changes in community structure, are now a focus of concern. Therefore, we grew the coccolithophore Emiliania huxleyi (Lohmann) W. W. Hay et H. Mohler and the diatom strains Thalassiosira pseudonana (Hust.) Hasle et Heimdal CCMP 1014 and T. pseudonana CCMP 1335 under low light in turbidostat photobioreactors bubbled with air containing 390 ppmv or 750 ppmv CO2. Increased pCO2 led to increased growth rates in all three strains. In addition, protein levels of RUBISCO increased in the coastal strains of both species, showing a larger capacity for CO2 assimilation at 750 ppmv CO2. With increased pCO2, both T. pseudonana strains displayed an increased susceptibility to PSII photoinactivation and, to compensate, an augmented capacity for PSII repair. Consequently, the cost of maintaining PSII function for the diatoms increased at increased pCO2. In E. huxleyi, PSII photoinactivation and the counter-acting repair, while both intrinsically larger than in T. pseudonana, did not change between the current and high-pCO2 treatments. The content of the photosynthetic electron transport intermediary cytochrome b6/f complex increased significantly in the diatoms under elevated pCO2, suggesting changes in electron transport function. Dataset North Atlantic Ocean acidification PANGAEA - Data Publisher for Earth & Environmental Science |