Seawater carbonate chemistry and shell dissolution in dead gastropod larvae and adult Limacina helicina pteropods

• Main Authors: Bausch, Alexandra Renee, Gallego, M Angeles, Harianto, Januar, Thibodeau, Patricia, Bednaršek, Nina, Havenhand, Jonathan N, Klinger, Terrie
• Format: Dataset
• Language: English
• Published: PANGAEA 2018
• Subjects: Alkalinity; total; standard deviation; Animalia; Aragonite saturation state; Bicarbonate ion; Bottles or small containers/Aquaria (<20 L); Calcification/Dissolution; 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; Event label; EXP; Experiment; Experiment duration; Fugacity of carbon dioxide (water) at sea surface temperature (wet air); Laboratory experiment; Limacina helicina; Mollusca; North Pacific; OA-ICC; Ocean Acidification International Coordination Centre; Other; Partial pressure of carbon dioxide (water) at sea surface temperature (wet air); Pelagos; Percentage; pH; Puget_Sound_OA; Registration number of species; Replicates; Salinity; San_Juan_Channel; Single species; Species; Temperate; Temperature; Ocean acidification
• Online Access: https://doi.pangaea.de/10.1594/PANGAEA.899574; https://doi.org/10.1594/PANGAEA.899574

Ocean acidification (OA) increases aragonite shell dissolution in calcifying marine organisms. It has been proposed that bacteria associated with molluscan shell surfaces in situ could damage the periostracum and reduce its protective function against shell dissolution. However, the influence of bac...