Permeable coral reef sediment dissolution driven by elevated pCO2 and pore water advection, supplement to: Cyronak, Tyler; Santos, Isaac R; Eyre, Bradley D (2013): Permeable coral reef sediment dissolution driven by elevated pCO2 and pore water advection. Geophysical Research Letters, 40(18), 4876–4881

• Main Authors: Cyronak, Tyler, Santos, Isaac R, Eyre, Bradley D
• Format: Dataset
• Language: English
• Published: PANGAEA - Data Publisher for Earth & Environmental Science 2013
• Subjects: Benthos; Bottles or small containers/Aquaria <20 L; Calcification/Dissolution; Coast and continental shelf; Entire community; Field experiment; Rocky-shore community; South Pacific; Tropical; Identification; Treatment; Oxygen, flux; Alkalinity, total, flux; pH; Partial pressure of carbon dioxide water at sea surface temperature wet air; Aragonite saturation state; Salinity; Temperature, water; Alkalinity, total; Carbonate system computation flag; Carbon dioxide; Fugacity of carbon dioxide water at sea surface temperature wet air; Bicarbonate ion; Carbonate ion; Carbon, inorganic, dissolved; Calcite saturation state; Potentiometric; Calculated using CO2SYS; Potentiometric titration; Calculated using seacarb after Nisumaa et al. 2010; Ocean Acidification International Coordination Centre OA-ICC; Heron Island; Pacific; Ocean acidification
• Online Access: https://dx.doi.org/10.1594/pangaea.833970; https://doi.pangaea.de/10.1594/PANGAEA.833970

Ocean acidification (OA) is expected to drive the transition of coral reef ecosystems from net calcium carbonate (CaCO3) precipitating to net dissolving within the next century. Although permeable sediments represent the largest reservoir of CaCO3 in coral reefs, the dissolution of shallow CaCO3 san...