Articles | Volume 29, issue 6
https://doi.org/10.5194/hess-29-1783-2025
© Author(s) 2025. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/hess-29-1783-2025
© Author(s) 2025. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
How seasonal hydroclimate variability drives the triple oxygen and hydrogen isotope composition of small lake systems in semiarid environments
Department of Biology and Geology, University of Almería, Almería, 04120, Spain
Analusian Center for Global Change – Hermelindo Castro (ENGLOBA), University of Almería, Almería, 04120, Spain
Fernando Gázquez
Department of Biology and Geology, University of Almería, Almería, 04120, Spain
Analusian Center for Global Change – Hermelindo Castro (ENGLOBA), University of Almería, Almería, 04120, Spain
Lucía Martegani
Department of Biology and Geology, University of Almería, Almería, 04120, Spain
Analusian Center for Global Change – Hermelindo Castro (ENGLOBA), University of Almería, Almería, 04120, Spain
Ana Isabel Sánchez Villanueva
Department of Biology and Geology, University of Almería, Almería, 04120, Spain
Analusian Center for Global Change – Hermelindo Castro (ENGLOBA), University of Almería, Almería, 04120, Spain
Antonio Medina
Department of Geology and Center for Advanced Studies in Earth Sciences, Energy and Environment (CEACTEMA), University of Jaén, Jaén, 23071, Spain
Rosario Jiménez-Espinosa
Department of Geology and Center for Advanced Studies in Earth Sciences, Energy and Environment (CEACTEMA), University of Jaén, Jaén, 23071, Spain
Juan Jiménez-Millán
Department of Geology and Center for Advanced Studies in Earth Sciences, Energy and Environment (CEACTEMA), University of Jaén, Jaén, 23071, Spain
Miguel Rodríguez-Rodríguez
Department of Physical, Chemical and Natural Systems, University Pablo de Olavide, Seville, 41013, Spain
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Short summary
This research explores the use of a new isotope tracer, 17O excess, to better understand how hydrological processes drive large seasonal water level changes in small lakes in semiarid regions. The study shows that triple oxygen isotopes offer a more detailed understanding of these changes compared to traditional methods. These findings are valuable for reconstructing past climates and predicting how climate change, influenced by human activity, will affect small lakes in these dry areas.
This research explores the use of a new isotope tracer, 17O excess, to better understand how...