The O2, pH and Ca2+ Microenvironment of Benthic Foraminifera in a High CO2 World
Ocean acidification (OA) can have adverse effects on marine calcifiers. Yet, phototrophic marine calcifiers elevate their external oxygen and pH microenvironment in daylight, through the uptake of dissolved inorganic carbon (DIC) by photosynthesis. We studied to which extent pH elevation within thei...
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ftpangaea:oai:pangaea.de:doi:10.1594/PANGAEA.833612 2024-09-09T20:01:24+00:00 The O2, pH and Ca2+ Microenvironment of Benthic Foraminifera in a High CO2 World Glas, Martin S Fabricius, Katharina Elisabeth de Beer, Dirk Uthicke, Sven Gilbert, Jack Anthony 2012 text/tab-separated-values, 22899 data points https://doi.pangaea.de/10.1594/PANGAEA.833612 https://doi.org/10.1594/PANGAEA.833612 en eng PANGAEA Lavigne, Héloïse; Epitalon, Jean-Marie; Gattuso, Jean-Pierre (2014): seacarb: seawater carbonate chemistry with R. R package version 3.0 [webpage]. https://cran.r-project.org/package=seacarb https://doi.pangaea.de/10.1594/PANGAEA.833612 https://doi.org/10.1594/PANGAEA.833612 CC-BY-3.0: Creative Commons Attribution 3.0 Unported Access constraints: unrestricted info:eu-repo/semantics/openAccess Supplement to: Glas, Martin S; Fabricius, Katharina Elisabeth; de Beer, Dirk; Uthicke, Sven; Gilbert, Jack Anthony (2012): The O2, pH and Ca2+ Microenvironment of Benthic Foraminifera in a High CO2 World. PLoS ONE, 7(11), e50010, https://doi.org/10.1371/journal.pone.0050010 Alkalinity total standard deviation Amphistegina radiata Aragonite saturation state Benthos Bicarbonate ion BIOACID Biological Impacts of Ocean Acidification Bottles or small containers/Aquaria (<20 L) Calcite saturation state Calcium ion Calculated using CO2SYS Calculated using seacarb after Nisumaa et al. (2010) Carbon inorganic dissolved Carbonate ion Carbonate system computation flag Carbon dioxide Chromista Coast and continental shelf Coulometric titration Date Figure Foraminifera Fugacity of carbon dioxide (water) at sea surface temperature (wet air) Group Heterostegina depressa Heterotrophic prokaryotes Hydrogen ion concentration Identification Individual code Irradiance dataset 2012 ftpangaea https://doi.org/10.1594/PANGAEA.83361210.1371/journal.pone.0050010 2024-07-24T02:31:32Z Ocean acidification (OA) can have adverse effects on marine calcifiers. Yet, phototrophic marine calcifiers elevate their external oxygen and pH microenvironment in daylight, through the uptake of dissolved inorganic carbon (DIC) by photosynthesis. We studied to which extent pH elevation within their microenvironments in daylight can counteract ambient seawater pH reductions, i.e. OA conditions. We measured the O2 and pH microenvironment of four photosymbiotic and two symbiont-free benthic tropical foraminiferal species at three different OA treatments (~432, 1141 and 2151 µatm pCO2). The O2 concentration difference between the seawater and the test surface (delta O2) was taken as a measure for the photosynthetic rate. Our results showed that O2 and pH levels were significantly higher on photosymbiotic foraminiferal surfaces in light than in dark conditions, and than on surfaces of symbiont-free foraminifera. Rates of photosynthesis at saturated light conditions did not change significantly between OA treatments (except in individuals that exhibited symbiont loss, i.e. bleaching, at elevated pCO2). The pH at the cell surface decreased during incubations at elevated pCO2, also during light incubations. Photosynthesis increased the surface pH but this increase was insufficient to compensate for ambient seawater pH decreases. We thus conclude that photosynthesis does only partly protect symbiont bearing foraminifera against OA. Dataset Ocean acidification PANGAEA - Data Publisher for Earth & Environmental Science |
institution |
Open Polar |
collection |
PANGAEA - Data Publisher for Earth & Environmental Science |
op_collection_id |
ftpangaea |
language |
English |
topic |
Alkalinity total standard deviation Amphistegina radiata Aragonite saturation state Benthos Bicarbonate ion BIOACID Biological Impacts of Ocean Acidification Bottles or small containers/Aquaria (<20 L) Calcite saturation state Calcium ion Calculated using CO2SYS Calculated using seacarb after Nisumaa et al. (2010) Carbon inorganic dissolved Carbonate ion Carbonate system computation flag Carbon dioxide Chromista Coast and continental shelf Coulometric titration Date Figure Foraminifera Fugacity of carbon dioxide (water) at sea surface temperature (wet air) Group Heterostegina depressa Heterotrophic prokaryotes Hydrogen ion concentration Identification Individual code Irradiance |
spellingShingle |
Alkalinity total standard deviation Amphistegina radiata Aragonite saturation state Benthos Bicarbonate ion BIOACID Biological Impacts of Ocean Acidification Bottles or small containers/Aquaria (<20 L) Calcite saturation state Calcium ion Calculated using CO2SYS Calculated using seacarb after Nisumaa et al. (2010) Carbon inorganic dissolved Carbonate ion Carbonate system computation flag Carbon dioxide Chromista Coast and continental shelf Coulometric titration Date Figure Foraminifera Fugacity of carbon dioxide (water) at sea surface temperature (wet air) Group Heterostegina depressa Heterotrophic prokaryotes Hydrogen ion concentration Identification Individual code Irradiance Glas, Martin S Fabricius, Katharina Elisabeth de Beer, Dirk Uthicke, Sven Gilbert, Jack Anthony The O2, pH and Ca2+ Microenvironment of Benthic Foraminifera in a High CO2 World |
topic_facet |
Alkalinity total standard deviation Amphistegina radiata Aragonite saturation state Benthos Bicarbonate ion BIOACID Biological Impacts of Ocean Acidification Bottles or small containers/Aquaria (<20 L) Calcite saturation state Calcium ion Calculated using CO2SYS Calculated using seacarb after Nisumaa et al. (2010) Carbon inorganic dissolved Carbonate ion Carbonate system computation flag Carbon dioxide Chromista Coast and continental shelf Coulometric titration Date Figure Foraminifera Fugacity of carbon dioxide (water) at sea surface temperature (wet air) Group Heterostegina depressa Heterotrophic prokaryotes Hydrogen ion concentration Identification Individual code Irradiance |
description |
Ocean acidification (OA) can have adverse effects on marine calcifiers. Yet, phototrophic marine calcifiers elevate their external oxygen and pH microenvironment in daylight, through the uptake of dissolved inorganic carbon (DIC) by photosynthesis. We studied to which extent pH elevation within their microenvironments in daylight can counteract ambient seawater pH reductions, i.e. OA conditions. We measured the O2 and pH microenvironment of four photosymbiotic and two symbiont-free benthic tropical foraminiferal species at three different OA treatments (~432, 1141 and 2151 µatm pCO2). The O2 concentration difference between the seawater and the test surface (delta O2) was taken as a measure for the photosynthetic rate. Our results showed that O2 and pH levels were significantly higher on photosymbiotic foraminiferal surfaces in light than in dark conditions, and than on surfaces of symbiont-free foraminifera. Rates of photosynthesis at saturated light conditions did not change significantly between OA treatments (except in individuals that exhibited symbiont loss, i.e. bleaching, at elevated pCO2). The pH at the cell surface decreased during incubations at elevated pCO2, also during light incubations. Photosynthesis increased the surface pH but this increase was insufficient to compensate for ambient seawater pH decreases. We thus conclude that photosynthesis does only partly protect symbiont bearing foraminifera against OA. |
format |
Dataset |
author |
Glas, Martin S Fabricius, Katharina Elisabeth de Beer, Dirk Uthicke, Sven Gilbert, Jack Anthony |
author_facet |
Glas, Martin S Fabricius, Katharina Elisabeth de Beer, Dirk Uthicke, Sven Gilbert, Jack Anthony |
author_sort |
Glas, Martin S |
title |
The O2, pH and Ca2+ Microenvironment of Benthic Foraminifera in a High CO2 World |
title_short |
The O2, pH and Ca2+ Microenvironment of Benthic Foraminifera in a High CO2 World |
title_full |
The O2, pH and Ca2+ Microenvironment of Benthic Foraminifera in a High CO2 World |
title_fullStr |
The O2, pH and Ca2+ Microenvironment of Benthic Foraminifera in a High CO2 World |
title_full_unstemmed |
The O2, pH and Ca2+ Microenvironment of Benthic Foraminifera in a High CO2 World |
title_sort |
o2, ph and ca2+ microenvironment of benthic foraminifera in a high co2 world |
publisher |
PANGAEA |
publishDate |
2012 |
url |
https://doi.pangaea.de/10.1594/PANGAEA.833612 https://doi.org/10.1594/PANGAEA.833612 |
genre |
Ocean acidification |
genre_facet |
Ocean acidification |
op_source |
Supplement to: Glas, Martin S; Fabricius, Katharina Elisabeth; de Beer, Dirk; Uthicke, Sven; Gilbert, Jack Anthony (2012): The O2, pH and Ca2+ Microenvironment of Benthic Foraminifera in a High CO2 World. PLoS ONE, 7(11), e50010, https://doi.org/10.1371/journal.pone.0050010 |
op_relation |
Lavigne, Héloïse; Epitalon, Jean-Marie; Gattuso, Jean-Pierre (2014): seacarb: seawater carbonate chemistry with R. R package version 3.0 [webpage]. https://cran.r-project.org/package=seacarb https://doi.pangaea.de/10.1594/PANGAEA.833612 https://doi.org/10.1594/PANGAEA.833612 |
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.83361210.1371/journal.pone.0050010 |
_version_ |
1809933213164896256 |