©2020 Biological and Chemical Oceanography Data Management Office.Funded by the U.S. National Science Foundation
Effect of temperature and polymorph mineral solubility (high-Mg calcite > aragonite > low-Mg calcite) on average modelled dissolution rate over ΩA = 0.2 - 5.0 (using ΩA 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. ΩA = saturation state of seawater with respect to aragonite.
See also related datasets for seawater chemistry, calcification rates, and dissolution rates.
Seawater chemistry
Calcification rates
Dissolution rates
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.
Ries, J. B. (2018) Effect of temperature and polymorph mineral solubility on average modeled dissolution rates.. Biological and Chemical Oceanography Data Management Office (BCO-DMO). (Version 1) Version Date 2018-01-17 [if applicable, indicate subset used]. http://lod.bco-dmo.org/id/dataset/723865 [access date]
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©2020 Biological and Chemical Oceanography Data Management Office.