Nighttime dissolution in a temperate coastal ocean ecosystem increases under acidification, supplement to: Kwiatkowski, Lester; Gaylord, B; Hill, Tessa M; Hosfelt, J D; Kroeker, Kristy J; Nebuchina, Yana; Ninokawa, Aaron; Russell, Ann D; Rivest, Emily B; Sesboüé, Marine; Caldeira, Ken (2016): Nighttime dissolution in a temperate coastal ocean ecosystem increases under acidification. Scientific Reports, 6, 22984

• Main Authors: Kwiatkowski, Lester, Gaylord, B, Hill, Tessa M, Hosfelt, J D, Kroeker, Kristy J, Nebuchina, Yana, Ninokawa, Aaron, Russell, Ann D, Rivest, Emily B, Sesboüé, Marine, Caldeira, Ken
• Format: Dataset
• Language: English
• Published: PANGAEA - Data Publisher for Earth & Environmental Science 2016
• Subjects: Benthos; Calcification/Dissolution; Coast and continental shelf; Entire community; Field observation; North Pacific; Primary production/Photosynthesis; Rocky-shore community; Temperate; Type; Identification; Time of day; Calcification rate of calcium carbonate; Net photosynthesis rate; Alkalinity, total; Carbon, inorganic, dissolved; pH; Partial pressure of carbon dioxide water at sea surface temperature wet air; Carbonate ion; Aragonite saturation state; Calcite saturation state; Temperature, water; Salinity; Carbonate system computation flag; Carbon dioxide; Fugacity of carbon dioxide water at sea surface temperature wet air; Bicarbonate ion; Experiment; Potentiometric titration; Calculated using CO2SYS; Calculated using seacarb after Nisumaa et al. 2010; Ocean Acidification International Coordination Centre OA-ICC; Lester; Pacific; Ocean acidification
• Online Access: https://dx.doi.org/10.1594/pangaea.864039; https://doi.pangaea.de/10.1594/PANGAEA.864039

Anthropogenic emissions of carbon dioxide (CO2) are causing ocean acidification, lowering seawater aragonite (CaCO3) saturation state (Omega arag), with potentially substantial impacts on marine ecosystems over the 21st Century. Calcifying organisms have exhibited reduced calcification under lower s...