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Dataset: Dissolution kinetics of 10 marine calcifiers: Temperature and polymorph mineralogy

Project: 
Principal Investigator: 
Justin B. Ries (Northeastern University)
BCO-DMO Data Manager: 
Megan Switzer (Woods Hole Oceanographic Institution, WHOI BCO-DMO)
Version: 
1
Version Date: 
2018-01-17
Restricted: 
No
Validated: 
No
Current State: 
Preliminary and in progress

Effect of temperature and polymorph mineral solubility on average modeled dissolution rates.

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Description

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. 

 

Data Files
File
723865.csv
(Comma Separated Values (.csv), 676 bytes)
MD5:ba89878e26fbcc0cc85e37c1b9228c1f
Primary data file for dataset ID 723865
More Information about this dataset