EGU24-4748, updated on 08 Mar 2024
https://doi.org/10.5194/egusphere-egu24-4748
EGU General Assembly 2024
© Author(s) 2024. This work is distributed under
the Creative Commons Attribution 4.0 License.

Physical and chemical controls on ikaite (calcium carbonate hexahydrate) precipitation in seawater

Madeleine Vickers1 and David Evans2
Madeleine Vickers and David Evans
  • 1University of Oslo, Department of Geosciences, Oslo, Norway (m.l.vickers@geo.uio.no)
  • 2School of Ocean and Earth Science, University of Southampton, Southampton, SO14 3ZH, UK (d.evans@soton.ac.uk)

Ikaite, CaCO3•6H2O, is a metastable polymorph of calcium carbonate which is the parent mineral to glendonites (stellate calcite pseudomorphs found throughout the geological record). In the modern ocean, ikaite may be found below the sediment-water interface, or in tufa columns, at temperatures of<7 °C (Buchardt et al., 2001; Zhou et al., 2015; Vickers et al., 2022), yet the presence of glendonites in marine sediments believed to have been deposited under much warmer conditions (i.e. > 10 °C) suggests that this ikaite could have formed under warmer conditions than it does today, or that short-duration cooling interrupted hyperthermal episodes of the early Cenozoic (Vickers et al., 2024). As much uncertainty surrounds the timing, and physical and chemical conditions of the formation, and transformation, of the precursor ikaite, the usefulness of glendonite for (semi-)quantitatively reconstructing temperature and environmental conditions is uncertain, and the explanation for the early Cenozoic glendonites remains obscure. This study examines the physical and chemical controls on ikaite nucleation, growth and transformation in seawater, with a view to understanding trace element and isotope partitioning into ikaite and ikaite transformation products, and if and how certain elemental and isotopic environmental proxies may be applied to glendonite calcite phases.

References

Buchardt, B., Israelson, C., Seaman, P. and Stockmann, G., 2001. Ikaite tufa towers in Ikka Fjord, southwest Greenland: their formation by mixing of seawater and alkaline spring water. Journal of Sedimentary Research, 71(1), 176-189.

Zhou, X., Lu, Z., Rickaby, R.E., Domack, E.W., Wellner, J.S. and Kennedy, H.A., 2015. Ikaite abundance controlled by porewater phosphorus level: Potential links to dust and productivity. The Journal of Geology, 123(3), 269-281.

Vickers, M.L., Vickers, M., Rickaby, R.E., Wu, H., Bernasconi, S.M., Ullmann, C.V., Bohrmann, G., Spielhagen, R.F., Kassens, H., Schultz, B.P. and Alwmark, C., 2022. The ikaite to calcite transformation: Implications for palaeoclimate studies. Geochimica et Cosmochimica Acta, 334, 201-216.

Vickers, M.L., Jones, M.T., Longman, J., Evans, D., Ullmann, C.V., Wulfsberg Stokke, E., Vickers, M., Frieling, J., Harper, D.T., Clementi, V.J. and Expedition, I.O.D.P., 2024. Paleocene–Eocene age glendonites from the Mid-Norwegian Margin–indicators of cold snaps in the hothouse?. Climate of the Past, 20(1), 1-23.

How to cite: Vickers, M. and Evans, D.: Physical and chemical controls on ikaite (calcium carbonate hexahydrate) precipitation in seawater, EGU General Assembly 2024, Vienna, Austria, 14–19 Apr 2024, EGU24-4748, https://doi.org/10.5194/egusphere-egu24-4748, 2024.