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  • 1
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    Unknown
    PANGAEA
    In:  Supplement to: Fietzke, Jan; Ragazzola, Federica; Halfar, Jochen; Dietze, Heiner; Foster, Laura C; Hansteen, Thor H; Eisenhauer, Anton; Steneck, Robert S (2015): Century-scale trends and seasonality in pH and temperature for shallow zones of the Bering Sea. Proceedings of the National Academy of Sciences, 201419216, https://doi.org/10.1073/pnas.1419216112
    Publication Date: 2023-02-24
    Description: Increasing atmospheric CO2 concentrations are potentially affecting marine ecosystems twofold, by warming and acidification. The rising amount of CO2 taken up by the ocean lowers the saturation state of calcium carbonate, complicating the formation of this key biomineral used by many marine organisms to build hard parts like skeletons or shells. Reliable time-series data of seawater pH are needed to evaluate the ongoing change and compare long-term trends and natural variability. For the high-latitude ocean, the region facing the strongest CO2 uptake, such time-series data are so far entirely lacking. Our study provides, to our knowledge, the first reconstruction of seasonal cycle and long-term trend in pH for a high-latitude ocean obtained from 2D images of stable boron isotopes from a coralline alga.
    Keywords: Aleutian Islands Alaska; Attu_Island; BIOACID; Biological Impacts of Ocean Acidification; DIVER; Sampling by diver
    Type: Dataset
    Format: application/zip, 4 datasets
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  • 2
    Publication Date: 2024-01-09
    Keywords: 208-1263; Age, relative; Calcite, volume normalized; COMPCORE; Composite Core; Depth, composite revised; DEPTH, sediment/rock; DSDP/ODP/IODP sample designation; Joides Resolution; Leg208; Nuttallides truempyi, calcite volume; Nuttallides truempyi, chamber number; Nuttallides truempyi, maximum test width; Nuttallides truempyi, penultimate chamber width; Nuttallides truempyi, penultimate chamber width/maximum test width ratio; Nuttallides truempyi, pore volume; Nuttallides truempyi, pore volume/test volume ratio; Nuttallides truempyi, size of proloculus; Nuttallides truempyi, test volume; Ocean Drilling Program; ODP; Sample code/label; Walvis Ridge, Southeast Atlantic Ocean
    Type: Dataset
    Format: text/tab-separated-values, 141 data points
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  • 3
    Publication Date: 2024-01-09
    Keywords: 208-1263C; Age, relative; Depth, composite revised; DEPTH, sediment/rock; DRILL; Drilling/drill rig; DSDP/ODP/IODP sample designation; Joides Resolution; Leg208; Number of species; Ocean Drilling Program; ODP; rarefied; Sample code/label; Walvis Ridge, Southeast Atlantic Ocean
    Type: Dataset
    Format: text/tab-separated-values, 193 data points
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  • 4
    Publication Date: 2024-01-09
    Keywords: 208-1263; Age, relative; COMPCORE; Composite Core; Depth, composite revised; DEPTH, sediment/rock; DSDP/ODP/IODP sample designation; Joides Resolution; Leg208; Number of species; Ocean Drilling Program; ODP; rarefied; Sample code/label; Walvis Ridge, Southeast Atlantic Ocean
    Type: Dataset
    Format: text/tab-separated-values, 204 data points
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  • 5
    Publication Date: 2024-01-09
    Keywords: 208-1262; Age, relative; Calcite, volume normalized; Comment; COMPCORE; Composite Core; Depth, composite revised; DEPTH, sediment/rock; DSDP/ODP/IODP sample designation; Joides Resolution; Leg208; Ocean Drilling Program; ODP; Oridorsalis umbonatus, calcite volume; Oridorsalis umbonatus, chamber number; Oridorsalis umbonatus, maximum test width; Oridorsalis umbonatus, penultimate chamber width; Oridorsalis umbonatus, penultimate chamber width/maximum test width ratio; Oridorsalis umbonatus, size of proloculus; Oridorsalis umbonatus, test volume; Sample code/label; Walvis Ridge, Southeast Atlantic Ocean
    Type: Dataset
    Format: text/tab-separated-values, 128 data points
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  • 6
    Publication Date: 2024-01-09
    Keywords: 208-1263A; 208-1263C; 208-1263D; Age, relative; Calcite, volume normalized; Comment; Depth, composite revised; DEPTH, sediment/rock; DRILL; Drilling/drill rig; DSDP/ODP/IODP sample designation; Event label; Joides Resolution; Leg208; Ocean Drilling Program; ODP; Oridorsalis umbonatus, calcite volume; Oridorsalis umbonatus, chamber number; Oridorsalis umbonatus, maximum test width; Oridorsalis umbonatus, penultimate chamber width; Oridorsalis umbonatus, penultimate chamber width/maximum test width ratio; Oridorsalis umbonatus, size of proloculus; Oridorsalis umbonatus, test volume; Sample code/label; Walvis Ridge, Southeast Atlantic Ocean
    Type: Dataset
    Format: text/tab-separated-values, 264 data points
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  • 7
    Publication Date: 2024-01-09
    Keywords: 208-1262A; 208-1263C; Age, relative; Calcite, volume normalized; Depth, composite revised; DEPTH, sediment/rock; DRILL; Drilling/drill rig; DSDP/ODP/IODP sample designation; Event label; Joides Resolution; Leg208; Ocean Drilling Program; ODP; Oridorsalis umbonatus, calcite volume; Oridorsalis umbonatus, chamber number; Oridorsalis umbonatus, maximum test width; Oridorsalis umbonatus, penultimate chamber width; Oridorsalis umbonatus, penultimate chamber width/maximum test width ratio; Oridorsalis umbonatus, size of proloculus; Oridorsalis umbonatus, test volume; Sample code/label; Walvis Ridge, Southeast Atlantic Ocean
    Type: Dataset
    Format: text/tab-separated-values, 186 data points
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  • 8
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    PANGAEA
    In:  Supplement to: Foster, Laura C; Schmidt, Daniela N; Thomas, Ellen; Arndt, Sandra; Ridgwell, Andy (2013): Surviving rapid climate change in the deep sea during the Paleogene hyperthermals. Proceedings of the National Academy of Sciences of the United States of America, 110(23), 9273-9276, https://doi.org/10.1073/pnas.1300579110
    Publication Date: 2024-01-09
    Description: Predicting the impact of ongoing anthropogenic CO2 emissions on calcifying marine organisms is complex, owing to the synergy between direct changes (acidification) and indirect changes through climate change (e.g., warming, changes in ocean circulation, and deoxygenation). Laboratory experiments, particularly on longer-lived organisms, tend to be too short to reveal the potential of organisms to acclimatize, adapt, or evolve and usually do not incorporate multiple stressors. We studied two examples of rapid carbon release in the geological record, Eocene Thermal Maximum 2 (~53.2 Ma) and the Paleocene Eocene Thermal Maximum (PETM, ~55.5 Ma), the best analogs over the last 65 Ma for future ocean acidification related to high atmospheric CO2 levels. We use benthic foraminifers, which suffered severe extinction during the PETM, as a model group. Using synchrotron radiation X-ray tomographic microscopy, we reconstruct the calcification response of survivor species and find, contrary to expectations, that calcification significantly increased during the PETM. In contrast, there was no significant response to the smaller Eocene Thermal Maximum 2, which was associated with a minor change in diversity only. These observations suggest that there is a response threshold for extinction and calcification response, while highlighting the utility of the geological record in helping constrain the sensitivity of biotic response to environmental change.
    Keywords: Ocean Drilling Program; ODP
    Type: Dataset
    Format: application/zip, 6 datasets
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  • 9
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    PANGAEA
    In:  Supplement to: Ragazzola, Federica; Foster, Laura C; Jones, C J; Scott, T B; Fietzke, Jan; Kilburn, M R; Schmidt, Daniela N (2016): Impact of high CO2 on the geochemistry of the coralline algae Lithothamnion glaciale. Scientific Reports, 6, 20572, https://doi.org/10.1038/srep20572
    Publication Date: 2024-03-15
    Description: Coralline algae are a significant component of the benthic ecosystem. Their ability to withstand physical stresses in high energy environments relies on their skeletal structure which is composed of high Mg-calcite. High Mg-calcite is, however, the most soluble form of calcium carbonate and therefore potentially vulnerable to the change in carbonate chemistry resulting from the absorption of anthropogenic CO2 by the ocean. We examine the geochemistry of the cold water coralline alga Lithothamnion glaciale grown under predicted future (year 2050) high pCO2 (589 matm) using Electron microprobe and NanoSIMS analysis. In the natural and control material, higher Mg calcite forms clear concentric bands around the algal cells. As expected, summer growth has a higher Mg content compared to the winter growth. In contrast, under elevated CO2 no banding of Mg is recognisable and overall Mg concentrations are lower. This reduction in Mg in the carbonate undermines the accuracy of the Mg/Ca ratio as proxy for past temperatures in time intervals with significantly different carbonate chemistry. Fundamentally, the loss of Mg in the calcite may reduce elasticity thereby changing the structural properties, which may affect the ability of L. glaciale to efficiently function as a habitat former in the future ocean.
    Keywords: Alkalinity, total; 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 seacarb after Nisumaa et al. (2010); Carbon, inorganic, dissolved; Carbonate ion; Carbonate system computation flag; Carbon dioxide; Coast and continental shelf; EXP; Experiment; Fugacity of carbon dioxide (water) at sea surface temperature (wet air); Kattegat_OA; Laboratory experiment; Lithothamnion glaciale; Location; Macroalgae; Magnesium/Calcium ratio; Magnesium/Calcium ratio, standard error; North Atlantic; OA-ICC; Ocean Acidification International Coordination Centre; Partial pressure of carbon dioxide (water) at sea surface temperature (wet air); pH; pH, standard deviation; Plantae; Potentiometric titration; Registration number of species; Rhodophyta; Salinity; Salinity, standard deviation; Sample ID; Single species; Species; Strontium/Calcium ratio; Strontium/Calcium ratio, standard error; Temperate; Temperature, water; Temperature, water, standard deviation; Type; Uniform resource locator/link to reference
    Type: Dataset
    Format: text/tab-separated-values, 600 data points
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  • 10
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    PANGAEA
    In:  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
    Publication Date: 2024-03-15
    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).
    Keywords: Alkalinity, total; Alkalinity, total, standard deviation; Aragonite saturation state; Aragonite saturation state, standard deviation; Benthos; Bicarbonate ion; Bicarbonate ion, standard deviation; BIOACID; Biological Impacts of Ocean Acidification; Biomass/Abundance/Elemental composition; Bottles or small containers/Aquaria (〈20 L); Calcite saturation state; Calcite saturation state, standard deviation; Calculated using CO2SYS; Calculated using seacarb after Nisumaa et al. (2010); Carbon, inorganic, dissolved; Carbon, inorganic, dissolved, standard deviation; Carbonate ion; Carbonate system computation flag; Carbon dioxide; Cell density; Cell density, standard deviation; Coast and continental shelf; Coralline algae, wall thickness, inter filament, standard deviation; Coralline algae, wall thickness, intra filament; Coralline algae, wall thickness, intra filament, standard deviation; EXP; Experiment; Fugacity of carbon dioxide (water) at sea surface temperature (wet air); Growth/Morphology; Growth rate; Growth rate, standard deviation; Kattegat_OA; Laboratory experiment; Lithothamnion glaciale; Macroalgae; North Atlantic; OA-ICC; Ocean Acidification International Coordination Centre; Partial pressure of carbon dioxide, standard deviation; Partial pressure of carbon dioxide (water) at sea surface temperature (wet air); pH; pH, standard deviation; Plantae; Potentiometric; Potentiometric titration; Rhodophyta; Salinity; Salinity, standard deviation; Single species; Species; Temperate; Temperature, standard deviation; Temperature, water; Treatment
    Type: Dataset
    Format: text/tab-separated-values, 152 data points
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