Seawater carbonate chemistry and particulate organic and inorganic carbon, growth of Emiliania huxleyi ...

Coccolithophore responses to changes in carbonate chemistry speciation such as CO2 and H+ are highly modulated by light intensity and temperature. Here, we fit an analytical equation, accounting for simultaneous changes in carbonate chemistry speciation, light and temperature, to published and origi...

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Bibliographic Details
Main Authors: Gafar, Natasha A, Schulz, Kai Georg
Format: Dataset
Language:English
Published: PANGAEA 2018
Subjects:
pH
Online Access:https://dx.doi.org/10.1594/pangaea.924611
https://doi.pangaea.de/10.1594/PANGAEA.924611
id ftdatacite:10.1594/pangaea.924611
record_format openpolar
spelling ftdatacite:10.1594/pangaea.924611 2024-09-09T19:58:06+00:00 Seawater carbonate chemistry and particulate organic and inorganic carbon, growth of Emiliania huxleyi ... Gafar, Natasha A Schulz, Kai Georg 2018 text/tab-separated-values https://dx.doi.org/10.1594/pangaea.924611 https://doi.pangaea.de/10.1594/PANGAEA.924611 en eng PANGAEA https://CRAN.R-project.org/package=seacarb https://dx.doi.org/10.5194/bg-15-3541-2018 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 Bottles or small containers/Aquaria <20 L Calcification/Dissolution Chromista Coast and continental shelf Emiliania huxleyi Growth/Morphology Haptophyta Laboratory experiment Light North Atlantic Pelagos Phytoplankton Primary production/Photosynthesis Single species Temperate Type Species Registration number of species Uniform resource locator/link to reference Growth rate Carbon, organic, particulate, production per cell Carbon, inorganic, particulate, production per cell Carbon, organic, particulate, per cell Carbon, inorganic, particulate, per cell 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 Temperature, water Salinity Carbonate system computation flag Partial pressure of carbon dioxide water at sea surface temperature wet air 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 2018 ftdatacite https://doi.org/10.1594/pangaea.92461110.5194/bg-15-3541-2018 2024-06-17T10:47:13Z Coccolithophore responses to changes in carbonate chemistry speciation such as CO2 and H+ are highly modulated by light intensity and temperature. Here, we fit an analytical equation, accounting for simultaneous changes in carbonate chemistry speciation, light and temperature, to published and original data for Emiliania huxleyi, and compare the projections with those for Gephyrocapsa oceanica. Based on our analysis, the two most common bloom-forming species in present-day coccolithophore communities appear to be adapted for a similar fundamental light niche but slightly different ones for temperature and CO2, with E. huxleyi having a tolerance to lower temperatures and higher CO2 levels than G. oceanica. Based on growth rates, a dominance of E. huxleyi over G. oceanica is projected below temperatures of 22 °C at current atmospheric CO2 levels. This is similar to a global surface sediment compilation of E. huxleyi and G. oceanica coccolith abundances suggesting temperature-dependent dominance shifts. For a ... : In order to allow full comparability with other ocean acidification data sets, the R package seacarb (Gattuso et al, 2020) 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 2020-10-30. ... Dataset North Atlantic Ocean acidification DataCite
institution Open Polar
collection DataCite
op_collection_id ftdatacite
language English
topic Bottles or small containers/Aquaria <20 L
Calcification/Dissolution
Chromista
Coast and continental shelf
Emiliania huxleyi
Growth/Morphology
Haptophyta
Laboratory experiment
Light
North Atlantic
Pelagos
Phytoplankton
Primary production/Photosynthesis
Single species
Temperate
Type
Species
Registration number of species
Uniform resource locator/link to reference
Growth rate
Carbon, organic, particulate, production per cell
Carbon, inorganic, particulate, production per cell
Carbon, organic, particulate, per cell
Carbon, inorganic, particulate, per cell
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
Temperature, water
Salinity
Carbonate system computation flag
Partial pressure of carbon dioxide water at sea surface temperature wet air
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
Coast and continental shelf
Emiliania huxleyi
Growth/Morphology
Haptophyta
Laboratory experiment
Light
North Atlantic
Pelagos
Phytoplankton
Primary production/Photosynthesis
Single species
Temperate
Type
Species
Registration number of species
Uniform resource locator/link to reference
Growth rate
Carbon, organic, particulate, production per cell
Carbon, inorganic, particulate, production per cell
Carbon, organic, particulate, per cell
Carbon, inorganic, particulate, per cell
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
Temperature, water
Salinity
Carbonate system computation flag
Partial pressure of carbon dioxide water at sea surface temperature wet air
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
Schulz, Kai Georg
Seawater carbonate chemistry and particulate organic and inorganic carbon, growth of Emiliania huxleyi ...
topic_facet Bottles or small containers/Aquaria <20 L
Calcification/Dissolution
Chromista
Coast and continental shelf
Emiliania huxleyi
Growth/Morphology
Haptophyta
Laboratory experiment
Light
North Atlantic
Pelagos
Phytoplankton
Primary production/Photosynthesis
Single species
Temperate
Type
Species
Registration number of species
Uniform resource locator/link to reference
Growth rate
Carbon, organic, particulate, production per cell
Carbon, inorganic, particulate, production per cell
Carbon, organic, particulate, per cell
Carbon, inorganic, particulate, per cell
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
Temperature, water
Salinity
Carbonate system computation flag
Partial pressure of carbon dioxide water at sea surface temperature wet air
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 Coccolithophore responses to changes in carbonate chemistry speciation such as CO2 and H+ are highly modulated by light intensity and temperature. Here, we fit an analytical equation, accounting for simultaneous changes in carbonate chemistry speciation, light and temperature, to published and original data for Emiliania huxleyi, and compare the projections with those for Gephyrocapsa oceanica. Based on our analysis, the two most common bloom-forming species in present-day coccolithophore communities appear to be adapted for a similar fundamental light niche but slightly different ones for temperature and CO2, with E. huxleyi having a tolerance to lower temperatures and higher CO2 levels than G. oceanica. Based on growth rates, a dominance of E. huxleyi over G. oceanica is projected below temperatures of 22 °C at current atmospheric CO2 levels. This is similar to a global surface sediment compilation of E. huxleyi and G. oceanica coccolith abundances suggesting temperature-dependent dominance shifts. For a ... : In order to allow full comparability with other ocean acidification data sets, the R package seacarb (Gattuso et al, 2020) 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 2020-10-30. ...
format Dataset
author Gafar, Natasha A
Schulz, Kai Georg
author_facet Gafar, Natasha A
Schulz, Kai Georg
author_sort Gafar, Natasha A
title Seawater carbonate chemistry and particulate organic and inorganic carbon, growth of Emiliania huxleyi ...
title_short Seawater carbonate chemistry and particulate organic and inorganic carbon, growth of Emiliania huxleyi ...
title_full Seawater carbonate chemistry and particulate organic and inorganic carbon, growth of Emiliania huxleyi ...
title_fullStr Seawater carbonate chemistry and particulate organic and inorganic carbon, growth of Emiliania huxleyi ...
title_full_unstemmed Seawater carbonate chemistry and particulate organic and inorganic carbon, growth of Emiliania huxleyi ...
title_sort seawater carbonate chemistry and particulate organic and inorganic carbon, growth of emiliania huxleyi ...
publisher PANGAEA
publishDate 2018
url https://dx.doi.org/10.1594/pangaea.924611
https://doi.pangaea.de/10.1594/PANGAEA.924611
genre North Atlantic
Ocean acidification
genre_facet North Atlantic
Ocean acidification
op_relation https://CRAN.R-project.org/package=seacarb
https://dx.doi.org/10.5194/bg-15-3541-2018
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_doi https://doi.org/10.1594/pangaea.92461110.5194/bg-15-3541-2018
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