Seawater carbonate chemistry and structural integrity of the coralline algae Lithothamnion glaciale in a laboratory experiment
The uptake of anthropogenic emission of carbon dioxide is resulting in a lowering of the carbonate saturation state and a drop in ocean pH. Understanding how marine calcifying organisms such as coralline algae may acclimatize to ocean acidification is important to understand their survival over the...
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ftpangaea:oai:pangaea.de:doi:10.1594/PANGAEA.823460 2023-05-15T17:50:57+02:00 Seawater carbonate chemistry and structural integrity of the coralline algae Lithothamnion glaciale in a laboratory experiment Ragazzola, Federica Foster, Laura C Form, Armin Anderson, Phillip S L Hansteen, Thor H Fietzke, Jan LATITUDE: 57.010160 * LONGITUDE: 11.583160 * DATE/TIME START: 2010-06-01T00:00:00 * DATE/TIME END: 2010-06-30T00:00:00 * MINIMUM ELEVATION: -20.0 m * MAXIMUM ELEVATION: -20.0 m 2012-12-02 text/tab-separated-values, 152 data points https://doi.pangaea.de/10.1594/PANGAEA.823460 https://doi.org/10.1594/PANGAEA.823460 en eng PANGAEA Lavigne, Héloïse; Gattuso, Jean-Pierre (2011): seacarb: seawater carbonate chemistry with R. R package version 2.4. https://cran.r-project.org/package=seacarb https://doi.pangaea.de/10.1594/PANGAEA.823460 https://doi.org/10.1594/PANGAEA.823460 CC-BY-3.0: Creative Commons Attribution 3.0 Unported Access constraints: unrestricted info:eu-repo/semantics/openAccess CC-BY Supplement to: Ragazzola, Federica; Foster, Laura C; Form, Armin; Anderson, Phillip S L; Hansteen, Thor H; Fietzke, Jan (2012): Ocean acidification weakens the structural integrity of coralline algae. Global Change Biology, 18(9), 2804-2812, https://doi.org/10.1111/j.1365-2486.2012.02756.x Alkalinity total standard deviation Aragonite saturation state Benthos Bicarbonate ion BIOACID Biological Impacts of Ocean Acidification Biomass/Abundance/Elemental composition Bottles or small containers/Aquaria (<20 L) Calcite saturation state Calculated using CO2SYS Calculated using seacarb after Nisumaa et al. (2010) Carbon inorganic dissolved Carbonate ion Carbonate system computation flag Carbon dioxide Cell density Coast and continental shelf Coralline algae wall thickness inter filament intra filament EXP Experiment Fugacity of carbon dioxide (water) at sea surface temperature (wet air) Growth/Morphology Dataset 2012 ftpangaea https://doi.org/10.1594/PANGAEA.823460 https://doi.org/10.1111/j.1365-2486.2012.02756.x 2023-01-20T09:01:55Z The uptake of anthropogenic emission of carbon dioxide is resulting in a lowering of the carbonate saturation state and a drop in ocean pH. Understanding how marine calcifying organisms such as coralline algae may acclimatize to ocean acidification is important to understand their survival over the coming century. We present the first long-term perturbation experiment on the cold-water coralline algae, which are important marine calcifiers in the benthic ecosystems particularly at the higher latitudes. Lithothamnion glaciale, after three months incubation, continued to calcify even in undersaturated conditions with a significant trend towards lower growth rates with increasing pCO2. However, the major changes in the ultra-structure occur by 589 µatm (i.e. in saturated waters). Finite element models of the algae grown at these heightened levels show an increase in the total strain energy of nearly an order of magnitude and an uneven distribution of the stress inside the skeleton when subjected to similar loads as algae grown at ambient levels. This weakening of the structure is likely to reduce the ability of the alga to resist boring by predators and wave energy with severe consequences to the benthic community structure in the immediate future (50 years). Dataset Ocean acidification PANGAEA - Data Publisher for Earth & Environmental Science ENVELOPE(11.583160,11.583160,57.010160,57.010160) |
institution |
Open Polar |
collection |
PANGAEA - Data Publisher for Earth & Environmental Science |
op_collection_id |
ftpangaea |
language |
English |
topic |
Alkalinity total standard deviation Aragonite saturation state Benthos Bicarbonate ion BIOACID Biological Impacts of Ocean Acidification Biomass/Abundance/Elemental composition Bottles or small containers/Aquaria (<20 L) Calcite saturation state Calculated using CO2SYS Calculated using seacarb after Nisumaa et al. (2010) Carbon inorganic dissolved Carbonate ion Carbonate system computation flag Carbon dioxide Cell density Coast and continental shelf Coralline algae wall thickness inter filament intra filament EXP Experiment Fugacity of carbon dioxide (water) at sea surface temperature (wet air) Growth/Morphology |
spellingShingle |
Alkalinity total standard deviation Aragonite saturation state Benthos Bicarbonate ion BIOACID Biological Impacts of Ocean Acidification Biomass/Abundance/Elemental composition Bottles or small containers/Aquaria (<20 L) Calcite saturation state Calculated using CO2SYS Calculated using seacarb after Nisumaa et al. (2010) Carbon inorganic dissolved Carbonate ion Carbonate system computation flag Carbon dioxide Cell density Coast and continental shelf Coralline algae wall thickness inter filament intra filament EXP Experiment Fugacity of carbon dioxide (water) at sea surface temperature (wet air) Growth/Morphology Ragazzola, Federica Foster, Laura C Form, Armin Anderson, Phillip S L Hansteen, Thor H Fietzke, Jan Seawater carbonate chemistry and structural integrity of the coralline algae Lithothamnion glaciale in a laboratory experiment |
topic_facet |
Alkalinity total standard deviation Aragonite saturation state Benthos Bicarbonate ion BIOACID Biological Impacts of Ocean Acidification Biomass/Abundance/Elemental composition Bottles or small containers/Aquaria (<20 L) Calcite saturation state Calculated using CO2SYS Calculated using seacarb after Nisumaa et al. (2010) Carbon inorganic dissolved Carbonate ion Carbonate system computation flag Carbon dioxide Cell density Coast and continental shelf Coralline algae wall thickness inter filament intra filament EXP Experiment Fugacity of carbon dioxide (water) at sea surface temperature (wet air) Growth/Morphology |
description |
The uptake of anthropogenic emission of carbon dioxide is resulting in a lowering of the carbonate saturation state and a drop in ocean pH. Understanding how marine calcifying organisms such as coralline algae may acclimatize to ocean acidification is important to understand their survival over the coming century. We present the first long-term perturbation experiment on the cold-water coralline algae, which are important marine calcifiers in the benthic ecosystems particularly at the higher latitudes. Lithothamnion glaciale, after three months incubation, continued to calcify even in undersaturated conditions with a significant trend towards lower growth rates with increasing pCO2. However, the major changes in the ultra-structure occur by 589 µatm (i.e. in saturated waters). Finite element models of the algae grown at these heightened levels show an increase in the total strain energy of nearly an order of magnitude and an uneven distribution of the stress inside the skeleton when subjected to similar loads as algae grown at ambient levels. This weakening of the structure is likely to reduce the ability of the alga to resist boring by predators and wave energy with severe consequences to the benthic community structure in the immediate future (50 years). |
format |
Dataset |
author |
Ragazzola, Federica Foster, Laura C Form, Armin Anderson, Phillip S L Hansteen, Thor H Fietzke, Jan |
author_facet |
Ragazzola, Federica Foster, Laura C Form, Armin Anderson, Phillip S L Hansteen, Thor H Fietzke, Jan |
author_sort |
Ragazzola, Federica |
title |
Seawater carbonate chemistry and structural integrity of the coralline algae Lithothamnion glaciale in a laboratory experiment |
title_short |
Seawater carbonate chemistry and structural integrity of the coralline algae Lithothamnion glaciale in a laboratory experiment |
title_full |
Seawater carbonate chemistry and structural integrity of the coralline algae Lithothamnion glaciale in a laboratory experiment |
title_fullStr |
Seawater carbonate chemistry and structural integrity of the coralline algae Lithothamnion glaciale in a laboratory experiment |
title_full_unstemmed |
Seawater carbonate chemistry and structural integrity of the coralline algae Lithothamnion glaciale in a laboratory experiment |
title_sort |
seawater carbonate chemistry and structural integrity of the coralline algae lithothamnion glaciale in a laboratory experiment |
publisher |
PANGAEA |
publishDate |
2012 |
url |
https://doi.pangaea.de/10.1594/PANGAEA.823460 https://doi.org/10.1594/PANGAEA.823460 |
op_coverage |
LATITUDE: 57.010160 * LONGITUDE: 11.583160 * DATE/TIME START: 2010-06-01T00:00:00 * DATE/TIME END: 2010-06-30T00:00:00 * MINIMUM ELEVATION: -20.0 m * MAXIMUM ELEVATION: -20.0 m |
long_lat |
ENVELOPE(11.583160,11.583160,57.010160,57.010160) |
genre |
Ocean acidification |
genre_facet |
Ocean acidification |
op_source |
Supplement to: Ragazzola, Federica; Foster, Laura C; Form, Armin; Anderson, Phillip S L; Hansteen, Thor H; Fietzke, Jan (2012): Ocean acidification weakens the structural integrity of coralline algae. Global Change Biology, 18(9), 2804-2812, https://doi.org/10.1111/j.1365-2486.2012.02756.x |
op_relation |
Lavigne, Héloïse; Gattuso, Jean-Pierre (2011): seacarb: seawater carbonate chemistry with R. R package version 2.4. https://cran.r-project.org/package=seacarb https://doi.pangaea.de/10.1594/PANGAEA.823460 https://doi.org/10.1594/PANGAEA.823460 |
op_rights |
CC-BY-3.0: Creative Commons Attribution 3.0 Unported Access constraints: unrestricted info:eu-repo/semantics/openAccess |
op_rightsnorm |
CC-BY |
op_doi |
https://doi.org/10.1594/PANGAEA.823460 https://doi.org/10.1111/j.1365-2486.2012.02756.x |
_version_ |
1766157907928285184 |