Shift from coral to macroalgae dominance on a volcanically acidified reef

• Main Authors: Enochs, I C, Manzello, Derek P, Donham, E M, Kolodziej, Graham, Okano, R, Johnston, Lyza, Young, Craig S, 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 2015
• Subjects: Alkalinity; total; Aragonite saturation state; Benthos; Bicarbonate ion; Calcite saturation state; Calculated using seacarb after Nisumaa et al. (2010); Carbon; inorganic; dissolved; Carbonate ion; Carbonate system computation flag; Carbon dioxide; CO2 vent; Coast and continental shelf; Community composition and diversity; Entire community; EXP; Experiment; Field observation; Fugacity of carbon dioxide (water) at sea surface temperature (wet air); Identification; Individuals; Maug_Island; Name; North Pacific; OA-ICC; Ocean Acidification International Coordination Centre; Partial pressure of carbon dioxide (water) at sea surface temperature (wet air); pH; Rocky-shore community; Salinity; Site; Temperature; water; Tropical; Type; Ocean acidification
• Online Access: https://doi.pangaea.de/10.1594/PANGAEA.867324; https://doi.org/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...