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Sea urchin response to rising pCO2 shows ocean acidification may fundamentally alter the chemistry of marine skeletons

Fuente: PANGAEA

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Bibliographic Details
Main Authors:	Bray, Laura, Pancucci-Papadopulou, M A, Hall-Spencer, Jason M
Format:	Dataset Open Access
Language:	en
Published:	PANGAEA 2014
Subjects:	Alkalinity, total; Alkalinity, total, standard error; Animalia; Aragonite saturation state; Arbacia lixula; Arsenic; Benthic animals; Benthos; Bicarbonate ion; Biomass/Abundance/Elemental composition; Bromine; Calcite saturation state; Calcium oxide; Calculated using CO2SYS; Calculated using seacarb after Nisumaa et al. (2010); Carbon, inorganic, dissolved; Carbonate ion; Carbonate system computation flag; Carbon dioxide; Cerium; Chromium; CO2 vent; Copper; Date; Echinodermata; Field observation; Fugacity of carbon dioxide (water) at sea surface temperature (wet air); Hafnium; Hellenic_Volcanic_Arc; Individuals; Iron oxide; Iron oxide, Fe2O3; LATITUDE; LONGITUDE; Manganese; Mediterranean Sea; Mediterranean Sea Acidification in a Changing Climate; MedSeA; Molybdenum; Nickel; OA-ICC; Ocean acidification; Ocean Acidification International Coordination Centre; Paracentrotus lividus; Partial pressure of carbon dioxide (water) at sea surface temperature (wet air); Partial pressure of carbon dioxide (water) at sea surface temperature (wet air), standard error; pH, NBS scale; pH, standard error; pH, total scale; Potentiometric; Potentiometric titration; Rubidium; Salinity; Salinity, standard error; Single species; Site; Species; Strontium; Tellurium; Temperate; Temperature, water; Temperature, water, standard error; Thorium; Tin; Yttrium; Zinc
Online Access:	Acceder al recurso
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Internet

https://doi.org/10.1594/PANGAEA.834210