| Summary: | <p>Estimated gross dissolution rates (this study), previously derived net calcification rates (Ries et al., 2009 – all species except <em>S. siderea</em>; Castillo et al., 2014 – <em>S. siderea</em>), and estimated gross calcification rates (net calcification minus gross dissolution) for eight species of marine calcifiers at 25.0 °C (± 0.02) at Ω<sub>A</sub> employed by Ries et al. (2009) and Castillo et al. (2014).</p> <p>References:<br /> Castillo K.D., Ries J.B., Bruno J.F., Westfield I.T., 2014, The reef-building coral <em>Siderastrea siderea </em>exhibits parabolic responses to ocean acidification and warming, Proceedings of the Royal Society of London B 281: 20141856. doi: <a href=\"http://rspb.royalsocietypublishing.org/content/281/1797/20141856\" target=\"_blank\">10.1098/rspb.2014.1856</a></p> <p>Ries, J.B., Cohen, A.L., McCorkle, D.C., 2010, A nonlinear calcification response to CO<sub>2</sub>-induced ocean acidification by the coral <em>Oculina arbuscula</em>, Coral Reefs 29: 661-674.</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>
|
|---|