| Summary: | <p>Effect of temperature and polymorph mineral solubility (high-Mg calcite > aragonite > low-Mg calcite) on average modelled dissolution rate over Ω<sub>A</sub> = 0.2 - 5.0 (using Ω<sub>A</sub> increments of 0.2) at 10.1 °C (± 0.02) and 25.0 °C (± 0.02). Results ranked by magnitude of temperature effect on average dissolution rate. Ω<sub>A</sub> = saturation state of seawater with respect to aragonite.</p> <p>See also related datasets for seawater chemistry, calcification rates, and dissolution rates. <br /> <a href=\"https://bco-dmo.org/dataset/723864\">Seawater chemistry</a> <br /> <a href=\"https://bco-dmo.org/dataset/723866\">Calcification rates</a><br /> <a href=\"https://bco-dmo.org/dataset/723867\">Dissolution rates</a></p> <p>These data are published in:</p> <p>Ries, J.B., Ghazaleh, M.N., Connolly, B., Westfield, I., Castillo, K.D., 2016, Impacts of ocean acidification and warming on the dissolution kinetics of whole-shell biogenic carbonates. Geochimica et Cosmochimica Acta 192: 318–337. doi: <a href=\"https://www.doi.org/10.1016/j.gca.2016.07.001\">10.1016/j.gca.2016.07.001</a></p> <p>Please see manuscript for complete methodology. </p> <p> </p>
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