Major cellular and physiological impacts of ocean acidification on a reef building coral, supplement to: Kaniewska, Paulina; Campbell, Paul R; Kline, David I; Rodriguez-Lanetty, Mauricio; Miller, David J; Dove, Sophie; Hoegh-Guldberg, Ove (2012): Major Cellular and Physiological Impacts of Ocean Acidification on a Reef Building Coral. PLoS ONE, 7(4), e34659

• Main Authors: Kaniewska, Paulina, Campbell, Paul R, Kline, David I, Rodriguez-Lanetty, Mauricio, Miller, David J, Dove, Sophie, Hoegh-Guldberg, Ove
• Format: Dataset
• Language: English
• Published: PANGAEA - Data Publisher for Earth & Environmental Science 2012
• Subjects: Acropora millepora; Animalia; Benthic animals; Benthos; Calcification/Dissolution; Cnidaria; Coast and continental shelf; Containers and aquaria 20-1000 L or < 1 m**2; Gene expression incl. proteomics; Laboratory experiment; Primary production/Photosynthesis; Respiration; Single species; South Pacific; Temperate; Species; Identification; Treatment; Incubation duration; Category; Gene expression, fold change, relative; Gene name; Gene expression; Symbiodinium cell concentration; Photosynthetic capacity, oxygen production per cell; Respiration rate, oxygen, dark per cell; Calcification rate; Temperature, water; Salinity; Alkalinity, total; Alkalinity, total, standard deviation; Carbon, inorganic, dissolved; Carbon, inorganic, dissolved, standard deviation; Carbonate system computation flag; pH; Carbon dioxide; Partial pressure of carbon dioxide water at sea surface temperature wet air; Fugacity of carbon dioxide water at sea surface temperature wet air; Bicarbonate ion; Carbonate ion; Aragonite saturation state; Calcite saturation state; Calculated using seacarb after Nisumaa et al. 2010; Ocean Acidification International Coordination Centre OA-ICC; Hoegh; Pacific; Paulina; Rodriguez; Ocean acidification
• Online Access: https://dx.doi.org/10.1594/pangaea.831180; https://doi.pangaea.de/10.1594/PANGAEA.831180

As atmospheric levels of CO2 increase, reef-building corals are under greater stress from both increased sea surface temperatures and declining sea water pH. To date, most studies have focused on either coral bleaching due to warming oceans or declining calcification due to decreasing oceanic carbon...