Seawater carbonate chemistry and particulate inorganic carbon, particulate organic carbon production, and growth rates of Scyphosphaera apsteinii

Coccolithophores are unicellular marine phytoplankton and important contributors to global carbon cycling. Most work on coccolithophore sensitivity to climate change has been on the small, abundant bloom-forming species Emiliania huxleyi and Gephyrocapsa oceanica. However, large coccolithophore spec...

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Main Authors: Gafar, Natasha A, Eyre, Bradley D, Schulz, Kai Georg
Format: Dataset
Language:English
Published: PANGAEA - Data Publisher for Earth & Environmental Science 2019
Subjects:
pH
Online Access:https://dx.doi.org/10.1594/pangaea.919773
https://doi.pangaea.de/10.1594/PANGAEA.919773
id ftdatacite:10.1594/pangaea.919773
record_format openpolar
spelling ftdatacite:10.1594/pangaea.919773 2023-05-15T17:51:22+02:00 Seawater carbonate chemistry and particulate inorganic carbon, particulate organic carbon production, and growth rates of Scyphosphaera apsteinii Gafar, Natasha A Eyre, Bradley D Schulz, Kai Georg 2019 text/tab-separated-values https://dx.doi.org/10.1594/pangaea.919773 https://doi.pangaea.de/10.1594/PANGAEA.919773 en eng PANGAEA - Data Publisher for Earth & Environmental Science https://CRAN.R-project.org/package=seacarb https://dx.doi.org/10.1038/s41598-019-38661-0 https://CRAN.R-project.org/package=seacarb Creative Commons Attribution 4.0 International https://creativecommons.org/licenses/by/4.0/legalcode cc-by-4.0 CC-BY Bottles or small containers/Aquaria <20 L Calcification/Dissolution Chromista Growth/Morphology Haptophyta Laboratory experiment Laboratory strains Light Not applicable Phytoplankton Primary production/Photosynthesis Scyphosphaera apsteinii Single species Type Species Registration number of species Uniform resource locator/link to reference Salinity Temperature, water Growth rate Production of particulate organic carbon per cell Carbon, inorganic, particulate, per cell Carbon, organic, particulate, per cell Particulate inorganic carbon/particulate organic carbon ratio Fugacity of carbon dioxide water at sea surface temperature wet air Carbon dioxide Bicarbonate ion Carbonate ion pH Hydrogen ion concentration Alkalinity, total Carbon, inorganic, dissolved Irradiance Partial pressure of carbon dioxide water at sea surface temperature wet air Number Number, standard deviation Length Length, standard deviation Width Width, standard deviation Ratio Ratio, standard deviation Cell biovolume Cell biovolume, standard deviation Carbonate system computation flag Aragonite saturation state Calcite saturation state Calculated using CO2SYS Calculated using seacarb after Nisumaa et al. 2010 Ocean Acidification International Coordination Centre OA-ICC Dataset dataset 2019 ftdatacite https://doi.org/10.1594/pangaea.919773 https://doi.org/10.1038/s41598-019-38661-0 2022-02-09T12:04:35Z Coccolithophores are unicellular marine phytoplankton and important contributors to global carbon cycling. Most work on coccolithophore sensitivity to climate change has been on the small, abundant bloom-forming species Emiliania huxleyi and Gephyrocapsa oceanica. However, large coccolithophore species can be major contributors to coccolithophore community production even in low abundances. Here we fit an analytical equation, accounting for simultaneous changes in CO2 and light intensity, to rates of photosynthesis, calcification and growth in Scyphosphaera apsteinii. Comparison of responses to G. oceanica and E. huxleyi revealed S. apsteinii is a low-light adapted species and, in contrast, becomes more sensitive to changing environmental conditions when exposed to unfavourable CO2 or light. Additionally, all three species decreased their light requirement for optimal growth as CO2 levels increased. Our analysis suggests that this is driven by a drop in maximum rates and, in G. oceanica, increased substrate uptake efficiency. Increasing light intensity resulted in a higher proportion of muroliths (plate-shaped) to lopadoliths (vase shaped) and liths became richer in calcium carbonate as calcification rates increased. Light and CO2 driven changes in response sensitivity and maximum rates are likely to considerably alter coccolithophore community structure and productivity under future climate conditions. : In order to allow full comparability with other ocean acidification data sets, the R package seacarb (Gattuso et al, 2019) was used to compute a complete and consistent set of carbonate system variables, as described by Nisumaa et al. (2010). In this dataset the original values were archived in addition with the recalculated parameters (see related PI). The date of carbonate chemistry calculation by seacarb is 2020-06-12. Dataset Ocean acidification DataCite Metadata Store (German National Library of Science and Technology)
institution Open Polar
collection DataCite Metadata Store (German National Library of Science and Technology)
op_collection_id ftdatacite
language English
topic Bottles or small containers/Aquaria <20 L
Calcification/Dissolution
Chromista
Growth/Morphology
Haptophyta
Laboratory experiment
Laboratory strains
Light
Not applicable
Phytoplankton
Primary production/Photosynthesis
Scyphosphaera apsteinii
Single species
Type
Species
Registration number of species
Uniform resource locator/link to reference
Salinity
Temperature, water
Growth rate
Production of particulate organic carbon per cell
Carbon, inorganic, particulate, per cell
Carbon, organic, particulate, per cell
Particulate inorganic carbon/particulate organic carbon ratio
Fugacity of carbon dioxide water at sea surface temperature wet air
Carbon dioxide
Bicarbonate ion
Carbonate ion
pH
Hydrogen ion concentration
Alkalinity, total
Carbon, inorganic, dissolved
Irradiance
Partial pressure of carbon dioxide water at sea surface temperature wet air
Number
Number, standard deviation
Length
Length, standard deviation
Width
Width, standard deviation
Ratio
Ratio, standard deviation
Cell biovolume
Cell biovolume, standard deviation
Carbonate system computation flag
Aragonite saturation state
Calcite saturation state
Calculated using CO2SYS
Calculated using seacarb after Nisumaa et al. 2010
Ocean Acidification International Coordination Centre OA-ICC
spellingShingle Bottles or small containers/Aquaria <20 L
Calcification/Dissolution
Chromista
Growth/Morphology
Haptophyta
Laboratory experiment
Laboratory strains
Light
Not applicable
Phytoplankton
Primary production/Photosynthesis
Scyphosphaera apsteinii
Single species
Type
Species
Registration number of species
Uniform resource locator/link to reference
Salinity
Temperature, water
Growth rate
Production of particulate organic carbon per cell
Carbon, inorganic, particulate, per cell
Carbon, organic, particulate, per cell
Particulate inorganic carbon/particulate organic carbon ratio
Fugacity of carbon dioxide water at sea surface temperature wet air
Carbon dioxide
Bicarbonate ion
Carbonate ion
pH
Hydrogen ion concentration
Alkalinity, total
Carbon, inorganic, dissolved
Irradiance
Partial pressure of carbon dioxide water at sea surface temperature wet air
Number
Number, standard deviation
Length
Length, standard deviation
Width
Width, standard deviation
Ratio
Ratio, standard deviation
Cell biovolume
Cell biovolume, standard deviation
Carbonate system computation flag
Aragonite saturation state
Calcite saturation state
Calculated using CO2SYS
Calculated using seacarb after Nisumaa et al. 2010
Ocean Acidification International Coordination Centre OA-ICC
Gafar, Natasha A
Eyre, Bradley D
Schulz, Kai Georg
Seawater carbonate chemistry and particulate inorganic carbon, particulate organic carbon production, and growth rates of Scyphosphaera apsteinii
topic_facet Bottles or small containers/Aquaria <20 L
Calcification/Dissolution
Chromista
Growth/Morphology
Haptophyta
Laboratory experiment
Laboratory strains
Light
Not applicable
Phytoplankton
Primary production/Photosynthesis
Scyphosphaera apsteinii
Single species
Type
Species
Registration number of species
Uniform resource locator/link to reference
Salinity
Temperature, water
Growth rate
Production of particulate organic carbon per cell
Carbon, inorganic, particulate, per cell
Carbon, organic, particulate, per cell
Particulate inorganic carbon/particulate organic carbon ratio
Fugacity of carbon dioxide water at sea surface temperature wet air
Carbon dioxide
Bicarbonate ion
Carbonate ion
pH
Hydrogen ion concentration
Alkalinity, total
Carbon, inorganic, dissolved
Irradiance
Partial pressure of carbon dioxide water at sea surface temperature wet air
Number
Number, standard deviation
Length
Length, standard deviation
Width
Width, standard deviation
Ratio
Ratio, standard deviation
Cell biovolume
Cell biovolume, standard deviation
Carbonate system computation flag
Aragonite saturation state
Calcite saturation state
Calculated using CO2SYS
Calculated using seacarb after Nisumaa et al. 2010
Ocean Acidification International Coordination Centre OA-ICC
description Coccolithophores are unicellular marine phytoplankton and important contributors to global carbon cycling. Most work on coccolithophore sensitivity to climate change has been on the small, abundant bloom-forming species Emiliania huxleyi and Gephyrocapsa oceanica. However, large coccolithophore species can be major contributors to coccolithophore community production even in low abundances. Here we fit an analytical equation, accounting for simultaneous changes in CO2 and light intensity, to rates of photosynthesis, calcification and growth in Scyphosphaera apsteinii. Comparison of responses to G. oceanica and E. huxleyi revealed S. apsteinii is a low-light adapted species and, in contrast, becomes more sensitive to changing environmental conditions when exposed to unfavourable CO2 or light. Additionally, all three species decreased their light requirement for optimal growth as CO2 levels increased. Our analysis suggests that this is driven by a drop in maximum rates and, in G. oceanica, increased substrate uptake efficiency. Increasing light intensity resulted in a higher proportion of muroliths (plate-shaped) to lopadoliths (vase shaped) and liths became richer in calcium carbonate as calcification rates increased. Light and CO2 driven changes in response sensitivity and maximum rates are likely to considerably alter coccolithophore community structure and productivity under future climate conditions. : In order to allow full comparability with other ocean acidification data sets, the R package seacarb (Gattuso et al, 2019) was used to compute a complete and consistent set of carbonate system variables, as described by Nisumaa et al. (2010). In this dataset the original values were archived in addition with the recalculated parameters (see related PI). The date of carbonate chemistry calculation by seacarb is 2020-06-12.
format Dataset
author Gafar, Natasha A
Eyre, Bradley D
Schulz, Kai Georg
author_facet Gafar, Natasha A
Eyre, Bradley D
Schulz, Kai Georg
author_sort Gafar, Natasha A
title Seawater carbonate chemistry and particulate inorganic carbon, particulate organic carbon production, and growth rates of Scyphosphaera apsteinii
title_short Seawater carbonate chemistry and particulate inorganic carbon, particulate organic carbon production, and growth rates of Scyphosphaera apsteinii
title_full Seawater carbonate chemistry and particulate inorganic carbon, particulate organic carbon production, and growth rates of Scyphosphaera apsteinii
title_fullStr Seawater carbonate chemistry and particulate inorganic carbon, particulate organic carbon production, and growth rates of Scyphosphaera apsteinii
title_full_unstemmed Seawater carbonate chemistry and particulate inorganic carbon, particulate organic carbon production, and growth rates of Scyphosphaera apsteinii
title_sort seawater carbonate chemistry and particulate inorganic carbon, particulate organic carbon production, and growth rates of scyphosphaera apsteinii
publisher PANGAEA - Data Publisher for Earth & Environmental Science
publishDate 2019
url https://dx.doi.org/10.1594/pangaea.919773
https://doi.pangaea.de/10.1594/PANGAEA.919773
genre Ocean acidification
genre_facet Ocean acidification
op_relation https://CRAN.R-project.org/package=seacarb
https://dx.doi.org/10.1038/s41598-019-38661-0
https://CRAN.R-project.org/package=seacarb
op_rights Creative Commons Attribution 4.0 International
https://creativecommons.org/licenses/by/4.0/legalcode
cc-by-4.0
op_rightsnorm CC-BY
op_doi https://doi.org/10.1594/pangaea.919773
https://doi.org/10.1038/s41598-019-38661-0
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