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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Bibliographic Details
Main Authors: Laws, Edward A, McClellan, S Alex
Format: Dataset
Language:English
Published: PANGAEA 2020
Subjects:
pH
Online Access:https://doi.pangaea.de/10.1594/PANGAEA.929551
https://doi.org/10.1594/PANGAEA.929551
id ftpangaea:oai:pangaea.de:doi:10.1594/PANGAEA.929551
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
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