Seawater carbonate chemistry and intertidal benthic foraminiferal growth and calcification, supplement to: Guaman-Guevara, Fabricio; Austin, Heather; Hicks, Natalie; Streeter, Richard; Austin, William EN (2019): Impacts of ocean acidification on intertidal benthic foraminiferal growth and calcification. PLoS ONE, 14(8), e0220046

• Main Authors: Guaman-Guevara, Fabricio, Austin, Heather, Hicks, Natalie, Streeter, Richard, Austin, William EN
• Format: Dataset
• Language: English
• Published: PANGAEA - Data Publisher for Earth & Environmental Science 2019
• Subjects: Benthos; Bottles or small containers/Aquaria <20 L; Brackish waters; Calcification/Dissolution; Chromista; Elphidium williamsoni; Foraminifera; Growth/Morphology; Heterotrophic prokaryotes; Laboratory experiment; Mortality/Survival; North Atlantic; Single species; Temperate; Type; Species; Registration number of species; Uniform resource locator/link to reference; Treatment; Number; Category; Diameter; Mass; pH; pH, standard deviation; Temperature, water; Temperature, water, standard deviation; Salinity; Salinity, standard deviation; Alkalinity, total; Alkalinity, total, standard deviation; Carbon, inorganic, dissolved; Carbon, inorganic, dissolved, standard deviation; Partial pressure of carbon dioxide water at sea surface temperature wet air; Partial pressure of carbon dioxide, standard deviation; Bicarbonate ion; Bicarbonate ion, standard deviation; Carbonate ion; Carbonate ion, standard deviation; Calcite saturation state; Calcite saturation state, standard deviation; Aragonite saturation state; Aragonite saturation state, standard deviation; Carbonate system computation flag; Carbon dioxide; Fugacity of carbon dioxide water at sea surface temperature wet air; Experiment; Potentiometric; Potentiometric titration; Calculated using CO2SYS; Calculated using seacarb after Nisumaa et al. 2010; Ocean Acidification International Coordination Centre OA-ICC; Austin; Hicks; Ocean acidification
• Online Access: https://dx.doi.org/10.1594/pangaea.911695; https://doi.pangaea.de/10.1594/PANGAEA.911695

Foraminifera are expected to be particularly susceptible to future changes in ocean carbonate chemistry as a function of increased atmospheric CO2. Studies in an experimental recirculating seawater system were performed with a dominant benthic foraminiferal species collected from intertidal mudflats...