Stable isotopes of gypsum hydration water in recent playa-lake sediments: implications for paleoclimate reconstructions

Authors

  • Jorge Cañada-Pasadas Department of Biology and Geology, University of Almería
  • Fernando Gázquez Department of Biology and Geology, University of Almería - Andalusian Centre for Global Change - Hermelindo Castro (ENGLOBA), University of Almería
  • Lucía Martegani Department of Biology and Geology, University of Almería - Andalusian Centre for Global Change - Hermelindo Castro (ENGLOBA), University of Almería
  • Claudia Voigt Department of Biology and Geology, University of Almería
  • Antonio García-Alix Department of Stratigraphy and Paleontology, Campus de Fuentenueva, University of Granada
  • Gonzalo Jiménez-Moreno Department of Stratigraphy and Paleontology, Campus de Fuentenueva, University of Granada
  • Miguel Rodríguez-Rodríguez Department of Physical, Chemical and Natural Systems, Pablo de Olavide University, Seville

DOI:

https://doi.org/10.55407/geogaceta104479

Keywords:

gypsum, stable isotopes, playa-lake, gypsum hydration water, modern lake sediments

Abstract

We investigate the oxygen and hydrogen stable isotopes of hydration water in gypsum (CaSO4·2H2O) from surface sediment of Laguna de la Ratosa playa-lake (northern Málaga Province, Spain). We aim to enhance the understanding of how lacustrine gypsum from playa-lakes can be used for paleoclimate reconstruction. Gypsum samples were collected at 30-meter intervals along a transect from the shore to the depocenter of the lake. Comparison of δ18O and δ2H values of gypsum hydration water with the modern seasonal isotope variability of lake water point to gypsum formation in spring and early summer, before complete desiccation of the lake. An increasing trend in the δ18O and δ2H values of gypsum hydration water, by ~1,5 and ~15‰, respectively, is observed from the shore to the depocenter. This indicates that coeval gypsum formed in different parts of the lakebed record slightly different isotopic values of the lake water during precipitation. This spatial variability should be considered when interpreting stable isotope series of gypsum hydration water from ephemeral lake sediments.

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Published

2024-12-02

How to Cite

Cañada-Pasadas, J., Gázquez, F., Martegani, L., Voigt, C., García-Alix, A., Jiménez-Moreno, G., & Rodríguez-Rodríguez, M. (2024). Stable isotopes of gypsum hydration water in recent playa-lake sediments: implications for paleoclimate reconstructions. GEOGACETA, 76, 71–74. https://doi.org/10.55407/geogaceta104479

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