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Secondary calcification and dissolution respond differently to future ocean conditions

Fuente: PANGAEA

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Bibliographic Details
Main Authors:	Silbiger, N J, Donahue, M J
Format:	Dataset Open Access
Language:	en
Published:	PANGAEA 2015
Subjects:	Alkalinity, total; Alkalinity, total, standard error; Ammonium; Ammonium, standard error; Aragonite saturation state; Aragonite saturation state, standard error; Benthos; Bicarbonate ion; Bicarbonate ion, standard error; Calcification/Dissolution; Calcification rate of calcium carbonate; 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 ion, standard error; Carbonate system computation flag; Carbon dioxide; Coast and continental shelf; Coconut_Island; Containers and aquaria (20-1000 L or < 1 m**2); Entire community; EXP; Experiment; Fugacity of carbon dioxide (water) at sea surface temperature (wet air); Laboratory experiment; Net calcification rate of calcium carbonate; Net community production of carbon; Nitrate; Nitrate, standard error; Nitrite; Nitrite, standard error; North Pacific; OA-ICC; Ocean acidification; Ocean Acidification International Coordination Centre; 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, standard error; pH, total scale; Phosphate; Phosphate, standard error; Potentiometric titration; Primary production/Photosynthesis; Rocky-shore community; Salinity; Salinity, standard error; Silicate; Silicate, standard error; Spectrophotometric; Standardized climate change; Temperature; Temperature, water; Temperature, water, standard error; Treatment; Tropical
Online Access:	Acceder al recurso
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Internet

https://doi.org/10.1594/PANGAEA.846682