Seawater carbonate chemistry and growth and physiology of the marine diatom Thalassiosira pseudonana (Coscinodiscophyceae)
The marine diatom Thalassiosira pseudonana was grown in continuous culture systems to study the interactive effects of temperature, irradiance, nutrient limitation, and the partial pressure of CO2 (pCO2) on its growth and physiological characteristics. The cells were able to grow at all combinations...
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Language: | English |
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PANGAEA
2020
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Online Access: | https://doi.pangaea.de/10.1594/PANGAEA.929551 https://doi.org/10.1594/PANGAEA.929551 |
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ftpangaea:oai:pangaea.de:doi:10.1594/PANGAEA.929551 |
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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 Aragonite saturation state Bicarbonate ion Biomass/Abundance/Elemental composition Bottles or small containers/Aquaria (<20 L) Calcite saturation state Calculated using seacarb after Nisumaa et al. (2010) Carbon inorganic dissolved Carbon/Chlorophyll a ratio Carbon/Nitrogen ratio Carbonate ion Carbonate system computation flag Carbon dioxide Chromista DATE/TIME Fugacity of carbon dioxide (water) at sea surface temperature (wet air) Growth/Morphology Growth rate standard deviation Initial slope of the photosynthesis-irradiance curve standard error Irradiance Laboratory experiment Laboratory strains Light Macro-nutrients Maximum photosynthetic rate (carbon/chlorophyll a) Maximum quantum yield of photosystem II Nitrogen/chlorophyll a ratio Not applicable OA-ICC Ocean Acidification International Coordination Centre Ochrophyta Partial pressure of carbon dioxide (water) at sea surface temperature (wet air) Pelagos pH Phytoplankton Primary production/Photosynthesis Productivity index (carbon/chlorophyll a) Ratio Registration number of species Respiration Salinity |
spellingShingle |
Alkalinity total Aragonite saturation state Bicarbonate ion Biomass/Abundance/Elemental composition Bottles or small containers/Aquaria (<20 L) Calcite saturation state Calculated using seacarb after Nisumaa et al. (2010) Carbon inorganic dissolved Carbon/Chlorophyll a ratio Carbon/Nitrogen ratio Carbonate ion Carbonate system computation flag Carbon dioxide Chromista DATE/TIME Fugacity of carbon dioxide (water) at sea surface temperature (wet air) Growth/Morphology Growth rate standard deviation Initial slope of the photosynthesis-irradiance curve standard error Irradiance Laboratory experiment Laboratory strains Light Macro-nutrients Maximum photosynthetic rate (carbon/chlorophyll a) Maximum quantum yield of photosystem II Nitrogen/chlorophyll a ratio Not applicable OA-ICC Ocean Acidification International Coordination Centre Ochrophyta Partial pressure of carbon dioxide (water) at sea surface temperature (wet air) Pelagos pH Phytoplankton Primary production/Photosynthesis Productivity index (carbon/chlorophyll a) Ratio Registration number of species Respiration Salinity Laws, Edward A McClellan, S Alex Seawater carbonate chemistry and growth and physiology of the marine diatom Thalassiosira pseudonana (Coscinodiscophyceae) |
topic_facet |
Alkalinity total Aragonite saturation state Bicarbonate ion Biomass/Abundance/Elemental composition Bottles or small containers/Aquaria (<20 L) Calcite saturation state Calculated using seacarb after Nisumaa et al. (2010) Carbon inorganic dissolved Carbon/Chlorophyll a ratio Carbon/Nitrogen ratio Carbonate ion Carbonate system computation flag Carbon dioxide Chromista DATE/TIME Fugacity of carbon dioxide (water) at sea surface temperature (wet air) Growth/Morphology Growth rate standard deviation Initial slope of the photosynthesis-irradiance curve standard error Irradiance Laboratory experiment Laboratory strains Light Macro-nutrients Maximum photosynthetic rate (carbon/chlorophyll a) Maximum quantum yield of photosystem II Nitrogen/chlorophyll a ratio Not applicable OA-ICC Ocean Acidification International Coordination Centre Ochrophyta Partial pressure of carbon dioxide (water) at sea surface temperature (wet air) Pelagos pH Phytoplankton Primary production/Photosynthesis Productivity index (carbon/chlorophyll a) Ratio Registration number of species Respiration Salinity |
description |
The marine diatom Thalassiosira pseudonana was grown in continuous culture systems to study the interactive effects of temperature, irradiance, nutrient limitation, and the partial pressure of CO2 (pCO2) on its growth and physiological characteristics. The cells were able to grow at all combinations of low and high irradiance (50 and 300 μmol photons/m**2/ s, respectively, of visible light), low and high pCO2 (400 and 1,000 μatm, respectively), nutrient limitation (nitrate‐limited and nutrient‐replete conditions), and temperatures of 10–32°C. Under nutrient‐replete conditions, there was no adverse effect of high pCO2 on growth rates at temperatures of 10–25°C. The response of the cells to high pCO2 was similar at low and high irradiance. At supraoptimal temperatures of 30°C or higher, high pCO2 depressed growth rates at both low and high irradiance. Under nitrate‐limited conditions, cells were grown at 38 ± 2.4% of their nutrient‐saturated rates at the same temperature, irradiance, and pCO2. Dark respiration rates consistently removed a higher percentage of production under nitrate‐limited versus nutrient‐replete conditions. The percentages of production lost to dark respiration were positively correlated with temperature under nitrate‐limited conditions, but there was no analogous correlation under nutrient‐replete conditions. The results suggest that warmer temperatures and associated more intense thermal stratification of ocean surface waters could lower net photosynthetic rates if the stratification leads to a reduction in the relative growth rates of marine phytoplankton, and at truly supraoptimal temperatures there would likely be a synergistic interaction between the stresses from temperature and high pCO2 (lower pH). |
format |
Dataset |
author |
Laws, Edward A McClellan, S Alex |
author_facet |
Laws, Edward A McClellan, S Alex |
author_sort |
Laws, Edward A |
title |
Seawater carbonate chemistry and growth and physiology of the marine diatom Thalassiosira pseudonana (Coscinodiscophyceae) |
title_short |
Seawater carbonate chemistry and growth and physiology of the marine diatom Thalassiosira pseudonana (Coscinodiscophyceae) |
title_full |
Seawater carbonate chemistry and growth and physiology of the marine diatom Thalassiosira pseudonana (Coscinodiscophyceae) |
title_fullStr |
Seawater carbonate chemistry and growth and physiology of the marine diatom Thalassiosira pseudonana (Coscinodiscophyceae) |
title_full_unstemmed |
Seawater carbonate chemistry and growth and physiology of the marine diatom Thalassiosira pseudonana (Coscinodiscophyceae) |
title_sort |
seawater carbonate chemistry and growth and physiology of the marine diatom thalassiosira pseudonana (coscinodiscophyceae) |
publisher |
PANGAEA |
publishDate |
2020 |
url |
https://doi.pangaea.de/10.1594/PANGAEA.929551 https://doi.org/10.1594/PANGAEA.929551 |
op_coverage |
DATE/TIME START: 2012-01-24T00:00:00 * DATE/TIME END: 2014-11-19T00:00:00 |
genre |
Ocean acidification |
genre_facet |
Ocean acidification |
op_relation |
Laws, Edward A; McClellan, S Alex (2020): Interactive effects of CO2, temperature, irradiance, and nutrient limitation on the growth and physiology of the marine diatom Thalassiosira pseudonana (Coscinodiscophyceae). Journal of Phycology, 56(6), 1614-1624, https://doi.org/10.1111/jpy.13048 Laws, Edward A (2020): Thalassiosira pseudonana CCMP1335 in nitrate-limited and nutrient-replete cultures [dataset]. Biological & Chemical Oceanography Data Management Office, https://www.bco-dmo.org/dataset/779368 Gattuso, Jean-Pierre; Epitalon, Jean-Marie; Lavigne, Héloïse; Orr, James (2021): seacarb: seawater carbonate chemistry with R. R package version 3.2.16. https://cran.r-project.org/web/packages/seacarb/index.html https://doi.pangaea.de/10.1594/PANGAEA.929551 https://doi.org/10.1594/PANGAEA.929551 |
op_rights |
CC-BY-4.0: Creative Commons Attribution 4.0 International Access constraints: unrestricted info:eu-repo/semantics/openAccess |
op_doi |
https://doi.org/10.1594/PANGAEA.92955110.1111/jpy.13048 |
_version_ |
1810469850163707904 |
spelling |
ftpangaea:oai:pangaea.de:doi:10.1594/PANGAEA.929551 2024-09-15T18:28:29+00:00 Seawater carbonate chemistry and growth and physiology of the marine diatom Thalassiosira pseudonana (Coscinodiscophyceae) Laws, Edward A McClellan, S Alex DATE/TIME START: 2012-01-24T00:00:00 * DATE/TIME END: 2014-11-19T00:00:00 2020 text/tab-separated-values, 1763 data points https://doi.pangaea.de/10.1594/PANGAEA.929551 https://doi.org/10.1594/PANGAEA.929551 en eng PANGAEA Laws, Edward A; McClellan, S Alex (2020): Interactive effects of CO2, temperature, irradiance, and nutrient limitation on the growth and physiology of the marine diatom Thalassiosira pseudonana (Coscinodiscophyceae). Journal of Phycology, 56(6), 1614-1624, https://doi.org/10.1111/jpy.13048 Laws, Edward A (2020): Thalassiosira pseudonana CCMP1335 in nitrate-limited and nutrient-replete cultures [dataset]. Biological & Chemical Oceanography Data Management Office, https://www.bco-dmo.org/dataset/779368 Gattuso, Jean-Pierre; Epitalon, Jean-Marie; Lavigne, Héloïse; Orr, James (2021): seacarb: seawater carbonate chemistry with R. R package version 3.2.16. https://cran.r-project.org/web/packages/seacarb/index.html https://doi.pangaea.de/10.1594/PANGAEA.929551 https://doi.org/10.1594/PANGAEA.929551 CC-BY-4.0: Creative Commons Attribution 4.0 International Access constraints: unrestricted info:eu-repo/semantics/openAccess Alkalinity total Aragonite saturation state Bicarbonate ion Biomass/Abundance/Elemental composition Bottles or small containers/Aquaria (<20 L) Calcite saturation state Calculated using seacarb after Nisumaa et al. (2010) Carbon inorganic dissolved Carbon/Chlorophyll a ratio Carbon/Nitrogen ratio Carbonate ion Carbonate system computation flag Carbon dioxide Chromista DATE/TIME Fugacity of carbon dioxide (water) at sea surface temperature (wet air) Growth/Morphology Growth rate standard deviation Initial slope of the photosynthesis-irradiance curve standard error Irradiance Laboratory experiment Laboratory strains Light Macro-nutrients Maximum photosynthetic rate (carbon/chlorophyll a) Maximum quantum yield of photosystem II Nitrogen/chlorophyll a ratio Not applicable OA-ICC Ocean Acidification International Coordination Centre Ochrophyta Partial pressure of carbon dioxide (water) at sea surface temperature (wet air) Pelagos pH Phytoplankton Primary production/Photosynthesis Productivity index (carbon/chlorophyll a) Ratio Registration number of species Respiration Salinity dataset 2020 ftpangaea https://doi.org/10.1594/PANGAEA.92955110.1111/jpy.13048 2024-07-24T02:31:34Z The marine diatom Thalassiosira pseudonana was grown in continuous culture systems to study the interactive effects of temperature, irradiance, nutrient limitation, and the partial pressure of CO2 (pCO2) on its growth and physiological characteristics. The cells were able to grow at all combinations of low and high irradiance (50 and 300 μmol photons/m**2/ s, respectively, of visible light), low and high pCO2 (400 and 1,000 μatm, respectively), nutrient limitation (nitrate‐limited and nutrient‐replete conditions), and temperatures of 10–32°C. Under nutrient‐replete conditions, there was no adverse effect of high pCO2 on growth rates at temperatures of 10–25°C. The response of the cells to high pCO2 was similar at low and high irradiance. At supraoptimal temperatures of 30°C or higher, high pCO2 depressed growth rates at both low and high irradiance. Under nitrate‐limited conditions, cells were grown at 38 ± 2.4% of their nutrient‐saturated rates at the same temperature, irradiance, and pCO2. Dark respiration rates consistently removed a higher percentage of production under nitrate‐limited versus nutrient‐replete conditions. The percentages of production lost to dark respiration were positively correlated with temperature under nitrate‐limited conditions, but there was no analogous correlation under nutrient‐replete conditions. The results suggest that warmer temperatures and associated more intense thermal stratification of ocean surface waters could lower net photosynthetic rates if the stratification leads to a reduction in the relative growth rates of marine phytoplankton, and at truly supraoptimal temperatures there would likely be a synergistic interaction between the stresses from temperature and high pCO2 (lower pH). Dataset Ocean acidification PANGAEA - Data Publisher for Earth & Environmental Science |