Articles | Volume 23, issue 21
https://doi.org/10.5194/bg-23-7911-2026
https://doi.org/10.5194/bg-23-7911-2026
Research article
 | 
06 Nov 2026
Research article |  | 06 Nov 2026

Tracking sulfate, magnesium and amorphous phases in cultured benthic foraminifera

Guillaume Paris, Caroline Thaler, Marc Dellinger, Jérôme Aléon, Smail Mostefaoui, Alice Aléon-Toppani, Claire Rollion-Bard, David Troadec, Guillaume Yangshu Wang, and Annachiara Bartolini

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Impact of seawater sulfate concentration on sulfur concentration and isotopic composition in calcite of two cultured benthic foraminifera
Caroline Thaler, Guillaume Paris, Marc Dellinger, Delphine Dissard, Sophie Berland, Arul Marie, Amandine Labat, and Annachiara Bartolini
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Cited articles

Addadi, L., Raz, S., and Weiner, S.: Taking Advantage of Disorder: Amorphous Calcium Carbonate and Its Roles in Biomineralization, Adv. Mater., 15, 959–970, https://doi.org/10.1002/adma.200300381, 2003. 
Aléon-Toppani, A., Brunetto, R., Aléon, J., Dionnet, Z., Rubino, S., Levy, D., Troadec, D., Brisset, F., Borondics, F., and King, A.: A preparation sequence for multi-analysis of µm-sized extraterrestrial and geological samples, Meteorit. Planet. Sci., 56, 1151–1172, https://doi.org/10.1111/maps.13696, 2021. 
Alkhatib, M., Qutob, M., Alkhatib, S., and Eisenhauer, A.: Influence of precipitation rate and temperature on the partitioning of magnesium and strontium in calcite overgrowths, Chem. Geol., 599, 120841, https://doi.org/10.1016/j.chemgeo.2022.120841, 2022. 
Angell, R. W.: The Test Structure and Composition of the Foraminifer Rosalina floridana, J. Protozool., 14, 299–307, https://doi.org/10.1111/j.1550-7408.1967.tb02001.x, 1967. 
Arns, A. I., Evans, D., Schiebel, R., Fink, L., Mezger, M., Alig, E., Linckens, J., Jochum, K. P., Schmidt, M. U., Jantschke, A., and Haug, G. H.: Mesocrystalline Architecture in Hyaline Foraminifer Shells Indicates a Non-Classical Crystallisation Pathway, Geochem. Geophy. Geosy., 23, e2022GC010445, https://doi.org/10.1029/2022GC010445, 2022. 
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To understand sulfate incorporation in the calcitic tests of foraminifera, we grew specimens with labeled sulfur. We documented sulfur, magnesium and calcium distribution across the cell, together with the ultrastructure of the test. S and Mg often co-occur and are particularly concentrated in amorphous blocks within organic linings . Strong biological control of those three elements likely plays a role in amorphous calcium carbonate formation and its evolution to calcite.
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