Shift from coral to macroalgae dominance on a volcanically acidified reef, supplement to: Enochs, I C; Manzello, Derek P; Donham, E M; Kolodziej, Graham; Okano, R; Johnston, Lyza; Young, C; Iguel, John; Edwards, C B; Fox, M D; Valentino, L; Johnson, Steven; Benavente, D; Clark, S J; Carlton, R; Burton, T; Eynaud, Y; Price, Nichole N (2015): Shift from coral to macroalgae dominance on a volcanically acidified reef. Nature Climate Change, 5(12), 1083-1088

• Main Authors: Enochs, I C, Manzello, Derek P, Donham, E M, Kolodziej, Graham, Okano, R, Johnston, Lyza, Young, C, Iguel, John, Edwards, C B, Fox, M D, Valentino, L, Johnson, Steven, Benavente, D, Clark, S J, Carlton, R, Burton, T, Eynaud, Y, Price, Nichole N
• Format: Dataset
• Language: English
• Published: PANGAEA - Data Publisher for Earth & Environmental Science 2015
• Subjects: Benthos; CO2 vent; Coast and continental shelf; Community composition and diversity; Entire community; Field observation; North Pacific; Rocky-shore community; Tropical; Type; Identification; Name; Site; Individuals; Salinity; Temperature, water; Alkalinity, total; Carbon, inorganic, dissolved; Carbonate system computation flag; pH; Carbon dioxide; Fugacity of carbon dioxide water at sea surface temperature wet air; Partial pressure of carbon dioxide water at sea surface temperature wet air; Bicarbonate ion; Carbonate ion; Aragonite saturation state; Calcite saturation state; Experiment; Calculated using seacarb after Nisumaa et al. 2010; Ocean Acidification International Coordination Centre OA-ICC; Burton; Pacific; Ocean acidification
• Online Access: https://dx.doi.org/10.1594/pangaea.867324; https://doi.pangaea.de/10.1594/PANGAEA.867324

Rising anthropogenic CO2 in the atmosphere is accompanied by an increase in oceanic CO2 and a concomitant decline in seawater pH (ref. 1). This phenomenon, known as ocean acidification (OA), has been experimentally shown to impact the biology and ecology of numerous animals and plants2, most notably...