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...

Full description

Bibliographic Details
Main Authors: McCarthy, Avery, Rogers, Susan P, Duffy, Stephen J, Campbell, Douglas A
Format: Dataset
Language:English
Published: PANGAEA 2012
Subjects:
pH
Online Access:https://doi.pangaea.de/10.1594/PANGAEA.824665
https://doi.org/10.1594/PANGAEA.824665
id ftpangaea:oai:pangaea.de:doi:10.1594/PANGAEA.824665
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