Sulfate isotope composition of Messinian evaporites in the Piedmont basin (Italy)

Authors

  • Javier García-Veigas CCiTUB, Scientific and Technological Centers, Universitat de Barcelona, Spain
  • Luis Gibert Departament de Mineralogia, Petrologia i Geologia Aplicada, Universitat de Barcelona, Spain
  • Dioni I. Cendón ANSTO, Australian Nuclear Science and Technology Organisation, Kirrawee DC, Australia
  • Francesco Dela Pierre Dipartimento di Scienze della Terra, Università di Torino, Italy
  • Marcello Natalicchio Dipartimento di Scienze della Terra, Università di Torino, Italy
  • David Artiaga CCiTUB, Scientific and Technological Centers, Universitat de Barcelona, Spain

DOI:

https://doi.org/10.55407/geogaceta102282

Keywords:

Messinian, gypsum, evaporites, sulphate isotopy

Abstract

The Piedmont basin (NW Italy) records a Messinian Salinity Crisis (MSC) succession including a selenite gypsum deposit assigned to the Primary Lower Gypsum (PLG, MSC stage 1). Strontium isotope ratios are in the range of the PLG deposits of the Mediterranean area. Sulfate isotope compositions of vertically oriented selenite gypsum beds, in the lower part of the succession, are similar to those reported in other PLG deposits. However, flattened branching selenite cones in the upper part show higher isotope compositions, mainly in δ34S values, suggesting intense BSR conditions, stronger than reported in other PLG deposits. We interpret this chemical shift during deposition of the upper part of the PLG as the result of increased marine restriction assisted by the marginal position of this basin in the Adriatic Gulf during the Apennine and Alpine uplifts.

References

Carnevale, G., Gennari, R., Lozar, F., Natalicchio, M., Pellegrino, L., and Dela Pierre (2019). Bolletino della Società Paleontologica Italiana 58, 109-140.

CIESM (2008). CIESM Workshop Monographs 33, 168p.

Dela Pierre, F., Bernardi, E., Cavagna, S., Clari, P., Gennari, R., Irace, A., Lozar, F., Lugli, S., Manzi, V., Natalicchio, M., Roveri, M., and Violanti, D. (2011). Palaeogeography, Paleoclimatology, Palaeoecology 310, 238-255. https://doi.org/10.1016/j.palaeo.2011.07.017

Dela Pierre, F., Clari, P., Natalicchio, M., Ferrando, S., Giustetto, R., Lozar, F., Lugli, S., Manzi, V., Roveri, M., and Violanti, D. (2014) Marine Geology 355, 71-87. https://doi.org/10.1016/j.margeo.2014.05.010

García-Veigas, J., Cendón, D.I., Gibert, L., Lowenstein, T.K., and Artiaga, D. (2018). Marine Geology 403, 197-214. https://doi.org/10.1016/j.margeo.2018.06.005

Hsü, K.J., Ryan, W.B.F., and Cita, M.B. (1973). Nature 242, 240-244. https://doi.org/10.1038/242240a0

Sturani, C. (1976). Memorie della Società Geologica Italiana 16, 11-25.

Lugli, S., Manzi, V., Roveri, M., and Schreiber B.Ch. (2010). Palaeogeography, Paleoclimatology, Palaeoecology 297, 83-99.

Ryan, 1973. In: Drooger, C.W. (Ed.) Messinian events in the Mediterranean, 26-38.

Natalicchio, M., Dela Pierre, F., Clari, P., Birgel, D., Cavagna, S., Martire, L., and Peckman, J. (2013). Palaeogeography, Paleoclimatology, Palaeoecology 390, 68-80. https://doi.org/10.1016/j.palaeo.2012.11.015

Laguna evaporítica de Pastos Grandes (Bolivia)

Downloads

Published

2021-12-13 — Updated on 2023-10-31

Versions

How to Cite

García-Veigas, J., Gibert, L., Cendón, D. I. ., Dela Pierre, F., Natalicchio, M., & Artiaga, D. (2023). Sulfate isotope composition of Messinian evaporites in the Piedmont basin (Italy). GEOGACETA, 70, 19–22. https://doi.org/10.55407/geogaceta102282 (Original work published December 13, 2021)

Issue

Vol. 70 (2021): Julio-Diciembre

Section

Artículos

License

Creative Commons License

This work is licensed under a Creative Commons Attribution-NonCommercial-ShareAlike 4.0 International License.

Until the year 2023 the author assigned the copyright to the Sociedad Geológica de España, but from 2024 the author retains the copyright and grants the Sociedad Geológica de España the right of first publication and non-exclusive distribution of each article in all current or future media, while transferring, also non-exclusively, the commercial rights for the distribution of the printed version of Geogaceta. On the other hand, the articles, from the year 2023, are available simultaneously with their publication, under the Creative Commons CC BY-NC-SA 4.0 license, which allows copying, transforming the work, but if any transformation is distributed, the new work must be distributed under the same license, and never for commercial purposes, while acknowledging the authorship and original publication in GEOGACETA, so that the only role of copyright is to give authors control over the integrity of their works and the right to be properly acknowledged and cited.