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  • 1
    Publication Date: 2023-01-30
    Description: This dataset comprises magnetic parameters of seven sediment cores from the South China Sea. The parameters are given versus age (in kyr): S-ratio = -IRM@-0.3T/IRM@1T (IRM is for Isothermal Remanent Magnetization), k (10^-6SI): low field magnetic susceptibility, ARM (10^-2 A/m): Anhysteretice remanent magnetization acquired with 100 mT alternating field and 50µT BC field IRM@1T (A/m): isothermal remanent magnetization acquired at 1T.
    Keywords: last climatic cycle; magnetic grain size; magnetic mineralogy; South China Sea
    Type: Dataset
    Format: application/zip, 7 datasets
    Location Call Number Limitation Availability
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  • 2
    Publication Date: 2023-06-27
    Keywords: 184-1145; AGE; Anhysteretic Remanent Magnetization; ARM, 100 mT AF, 0.05 mT DF; COMPCORE; Composite Core; Isothermal remanent magnetization; Joides Resolution; last climatic cycle; Leg184; magnetic grain size; magnetic mineralogy; Magnetic susceptibility, low-field; Sample code/label; South China Sea; S-ratio (hematite/magnetite)
    Type: Dataset
    Format: text/tab-separated-values, 6410 data points
    Location Call Number Limitation Availability
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  • 3
    Publication Date: 2023-06-27
    Keywords: 184-1143; AGE; Anhysteretic Remanent Magnetization; ARM, 100 mT AF, 0.05 mT DF; COMPCORE; Composite Core; Isothermal remanent magnetization; Joides Resolution; last climatic cycle; Leg184; magnetic grain size; magnetic mineralogy; Magnetic susceptibility, low-field; Sample code/label; South China Sea; S-ratio (hematite/magnetite)
    Type: Dataset
    Format: text/tab-separated-values, 2600 data points
    Location Call Number Limitation Availability
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  • 4
    Publication Date: 2023-06-27
    Keywords: 184-1147; AGE; Anhysteretic Remanent Magnetization; ARM, 100 mT AF, 0.05 mT DF; COMPCORE; Composite Core; Isothermal remanent magnetization; Joides Resolution; last climatic cycle; Leg184; magnetic grain size; magnetic mineralogy; Magnetic susceptibility, low-field; Sample code/label; South China Sea; S-ratio (hematite/magnetite)
    Type: Dataset
    Format: text/tab-separated-values, 4780 data points
    Location Call Number Limitation Availability
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  • 5
    Publication Date: 2023-06-27
    Keywords: AGE; Anhysteretic Remanent Magnetization; ARM, 100 mT AF, 0.05 mT DF; Giant piston corer; GPC; IMAGES VII - WEPAMA; Isothermal remanent magnetization; last climatic cycle; magnetic grain size; magnetic mineralogy; Magnetic susceptibility, low-field; Marion Dufresne (1995); MD012393; MD01-2393; MD122; Sample code/label; South China Sea; S-ratio (hematite/magnetite)
    Type: Dataset
    Format: text/tab-separated-values, 7510 data points
    Location Call Number Limitation Availability
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  • 6
    Publication Date: 2023-06-27
    Keywords: AGE; Anhysteretic Remanent Magnetization; ARM, 100 mT AF, 0.05 mT DF; Calypso Square Core System; CASQS; IMAGES XII - MARCO POLO; Isothermal remanent magnetization; last climatic cycle; magnetic grain size; magnetic mineralogy; Magnetic susceptibility, low-field; Marion Dufresne (1995); MD052896; MD05-2896; MD147; Sample code/label; South China Sea; S-ratio (hematite/magnetite)
    Type: Dataset
    Format: text/tab-separated-values, 3265 data points
    Location Call Number Limitation Availability
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  • 7
    Publication Date: 2023-06-27
    Keywords: AGE; Anhysteretic Remanent Magnetization; ARM, 100 mT AF, 0.05 mT DF; Calypso Square Core System; CASQS; IMAGES XII - MARCO POLO; Isothermal remanent magnetization; last climatic cycle; magnetic grain size; magnetic mineralogy; Magnetic susceptibility, low-field; Marion Dufresne (1995); MD052900; MD05-2900; MD147; Sample code/label; South China Sea; S-ratio (hematite/magnetite)
    Type: Dataset
    Format: text/tab-separated-values, 2685 data points
    Location Call Number Limitation Availability
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  • 8
    Publication Date: 2023-06-27
    Keywords: AGE; Anhysteretic Remanent Magnetization; ARM, 100 mT AF, 0.05 mT DF; Calypso Square Core System; CASQS; IMAGES XII - MARCO POLO; Isothermal remanent magnetization; last climatic cycle; magnetic grain size; magnetic mineralogy; Magnetic susceptibility, low-field; Marion Dufresne (1995); MD052898; MD05-2898; MD147; Sample code/label; South China Sea; S-ratio (hematite/magnetite)
    Type: Dataset
    Format: text/tab-separated-values, 1995 data points
    Location Call Number Limitation Availability
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  • 9
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    PANGAEA
    In:  Supplement to: Crook, Elizabeth Derse; Cohen, Anne L; Rebolledo-Vieyra, Mario; Hernandez, Laura; Paytan, Adina (2013): Reduced calcification and lack of acclimatization by coral colonies growing in areas of persistent natural acidification. Proceedings of the National Academy of Sciences, 110(27), 11044-11049, https://doi.org/10.1073/pnas.1301589110
    Publication Date: 2024-03-15
    Description: As the surface ocean equilibrates with rising atmospheric CO2, the pH of surface seawater is decreasing with potentially negative impacts on coral calcification. A critical question is whether corals will be able to adapt or acclimate to these changes in seawater chemistry. We use high precision CT scanning of skeletal cores of Porites astreoides, an important Caribbean reef-building coral, to show that calcification rates decrease significantly along a natural gradient in pH and aragonite saturation (Omega arag). This decrease is accompanied by an increase in skeletal erosion and predation by boring organisms. The degree of sensitivity to reduced Oarag measured on our field corals is consistent with that exhibited by the same species in laboratory CO2 manipulation experiments. We conclude that the Porites corals at our field site were not able to acclimatize enough to prevent the impacts of local ocean acidification on their skeletal growth and development, despite spending their entire lifespan in low pH, low Omega arag seawater.
    Keywords: Alkalinity, total; Alkalinity, total, standard deviation; Animalia; Aragonite saturation state; Aragonite saturation state, standard deviation; Benthic animals; Benthos; Bicarbonate ion; Calcification/Dissolution; Calcification rate; Calcification rate, ratio; Calcification rate, standard deviation; Calcification rate, standard error; Calcite saturation state; 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; Cnidaria; Density; Density, standard deviation; Density, standard error; Field observation; Figure; Fugacity of carbon dioxide (water) at sea surface temperature (wet air); Growth/Morphology; Linear extension; Linear extension, standard deviation; Linear extension, standard error; North Atlantic; OA-ICC; Ocean Acidification International Coordination Centre; Partial pressure of carbon dioxide (water) at sea surface temperature (wet air); pH; Porites astreoides; Salinity; Single species; Species; Temperature, water; Thickness; Thickness, standard deviation; Thickness, standard error; Treatment; Tropical; Volume ratio
    Type: Dataset
    Format: text/tab-separated-values, 479 data points
    Location Call Number Limitation Availability
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  • 10
    Publication Date: 2024-03-15
    Description: Ocean acidification is a pervasive threat to coral reef ecosystems, and our understanding of the ecological processes driving patterns in tropical benthic community development in conditions of acidification is limited. We deployed limestone recruitment tiles in low aragonite saturation (Omega arag) waters during an in-situ field experiment at Puerto Morelos, Mexico, and compared them to tiles placed in control zones over a 14-month investigation. The early stages of succession showed relatively little difference in coverage of calcifying organisms between the low Omega arag and control zones. However, after 14 months of development, tiles from the low Omega arag zones had up to 70% less cover of calcifying organisms coincident with 42% more fleshy algae than the controls. The percent cover of biofilm and turf algae was also significantly greater in the low Omega arag zones, while the number of key grazing taxa remained constant. We hypothesize that fleshy algae have a competitive edge over the primary calcified space holders, coralline algae, and that acidification leads to altered competitive dynamics between various taxa. We suggest that as acidification impacts reefs in the future, there will be a shift in community assemblages away from upright and crustose coralline algae toward more fleshy algae and turf, established in the early stages of succession.
    Keywords: Alkalinity, total; Alkalinity, total, standard error; Aragonite saturation state; Aragonite saturation state, standard error; Benthos; Bicarbonate ion; Biomass/Abundance/Elemental composition; Calcite saturation state; Calculated using CO2SYS; Calculated using seacarb after Nisumaa et al. (2010); Carbon, inorganic, dissolved; Carbon, inorganic, dissolved, standard error; Carbonate ion; Carbonate system computation flag; Carbon dioxide; Coast and continental shelf; Community composition and diversity; Coulometric titration; Coverage; Diameter; Duration; Entire community; Event label; EXP; Experiment; Field observation; Fugacity of carbon dioxide (water) at sea surface temperature (wet air); Group; Growth/Morphology; LATITUDE; LONGITUDE; Nitrate; Nitrate, standard error; North Atlantic; Number; OA-ICC; Ocean Acidification International Coordination Centre; Ojo_Gorgos; Ojo_Laja; Partial pressure of carbon dioxide (water) at sea surface temperature (wet air); pH; pH, standard error; Phosphate; Phosphate, standard error; Potentiometric titration; Replicate; Salinity; Salinity, standard error; Silicate; Silicate, standard error; Site; Temperature, water; Temperature, water, standard error; Tropical; Type; Zone
    Type: Dataset
    Format: text/tab-separated-values, 16432 data points
    Location Call Number Limitation Availability
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