Dataset: Estimated gross dissolution rates, previously derived net calcification rates, and estimated gross calcification rates for eight species of marine calcifiers at 25.0 °C.

This dataset has not been validatedPreliminary and in progressVersion 1 (2018-01-17)Dataset Type:experimental

Principal Investigator: Justin B. Ries (Northeastern University)

BCO-DMO Data Manager: Megan Switzer (Woods Hole Oceanographic Institution)


Project: A combined boron isotope, pH microelectrode and pH-sensitive dye approach to constraining acid/base chemistry in the calcifying fluids of corals (CoralCalcifyFluid_pH)

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Estimated gross dissolution rates (this study), previously derived net calcification rates (Ries et al., 2009 – all species except S. siderea; Castillo et al., 2014 – S. siderea), and estimated gross calcification rates (net calcification minus gross dissolution) for eight species of marine calcifiers at 25.0 °C (± 0.02) at ΩA employed by Ries et al. (2009) and Castillo et al. (2014).

References:
Castillo K.D., Ries J.B., Bruno J.F., Westfield I.T., 2014, The reef-building coral Siderastrea siderea exhibits parabolic responses to ocean acidification and warming, Proceedings of the Royal Society of London B 281: 20141856. doi: 10.1098/rspb.2014.1856

Ries, J.B., Cohen, A.L., McCorkle, D.C., 2010, A nonlinear calcification response to CO2-induced ocean acidification by the coral Oculina arbuscula, Coral Reefs 29: 661-674.

These data are published in:

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: 10.1016/j.gca.2016.07.001

Please see manuscript for complete methodology. 


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