Articles | Volume 28, issue 23
https://doi.org/10.5194/hess-28-5311-2024
© Author(s) 2024. 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-28-5311-2024
© Author(s) 2024. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
The role of neotectonics and climate variability in the Pleistocene-to-Holocene hydrological evolution of the Fuente de Piedra playa lake (southern Iberian Peninsula)
Alejandro Jiménez-Bonilla
CORRESPONDING AUTHOR
Department of Physics, Chemistry and Natural Systems, Pablo de Olavide University, 41013 Seville, Spain
Lucía Martegani
Department of Biology and Geology, Water Resources and Environmental Geology Research Group, University of Almería, 04120 Almería, Spain
Andalusian Centre for Global Change – Hermelindo Castro. ENGLOBA, University of Almería, 04120 Almería, Spain
Miguel Rodríguez-Rodríguez
Department of Physics, Chemistry and Natural Systems, Pablo de Olavide University, 41013 Seville, Spain
Fernando Gázquez
Department of Biology and Geology, Water Resources and Environmental Geology Research Group, University of Almería, 04120 Almería, Spain
Andalusian Centre for Global Change – Hermelindo Castro. ENGLOBA, University of Almería, 04120 Almería, Spain
Manuel Díaz-Azpíroz
Department of Physics, Chemistry and Natural Systems, Pablo de Olavide University, 41013 Seville, Spain
Sergio Martos
Geological Survey of Spain (IGME), 28003 Madrid, Spain
Klaus Reicherter
Institute of Neotectonics and Natural Hazards, RWTH Aachen University, 52062 Aachen, Germany
Inmaculada Expósito
Department of Physics, Chemistry and Natural Systems, Pablo de Olavide University, 41013 Seville, Spain
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Cited articles
Allen, D. E., Singh, B. P., and Dalal, R. C.: Soil health indicators under climate change: a review of current knowledge, Soil Health Clim. Change, 29, 25–45, 2011.
Alonso-Zarza, A. M. and Wright, V. P.: Calcretes, Dev. Sedimentol., 61, 225–267, 2010.
Atalai, I.: Paleoenvironmental conditions of the Late Pleistocene and early Holocene in Anatolia, Turkey, in: Quaternary deserts and climate change, CRC Press, 227–237, eBook ISBN 9781003077862, 2020.
Balanya, J. C., Crespo-Blanc, A., Díaz-Azpiroz, M., Expósito, I., Torcal, F., Pérez-Peña, V., and Booth-Rea, G.: Arc-parallel vs back-arc extension in the Western Gibraltar arc: Is the Gibraltar forearc still active?, Geolog. Acta, 10, 249–263, 2012.
Barcos, L., Balanyá, J. C., Díaz-Azpiroz, M., Expósito, I., and Jiménez-Bonilla, A.: Kinematics of the Torcal Shear Zone: Transpressional tectonics in a salient-recess transition at the northern Gibraltar Arc, Tectonophysics, 663, 62–77, 2015.
Benavente, J., Carrasco, F., Almécija, C., Rodríguez-Jiménez, P., and Cruz Sanjulián, J.: La zona de transición agua dulce-salmuera bajo el borde norte de la laguna salada de Fuente de Piedra (Málaga), Geogaceta, 14, 6–8, 1993.
Berry, M., Van Wijk, J., Cadol, D., Emry, E., and Garcia-Castellanos, D.: Endorheic-exorheic transitions of the Rio Grande and East African rifts, Geochem. Geophy. Geosy., 20, 3705–3729, 2019.
Blaauw, M. and Christen, J. A.: Flexible paleoclimate age-depth models using an autoregressive gamma process, Bayesian Anal., 6, 457–474, https://doi.org/10.1214/11-BA618, 2011.
Camuera, J., Ramos-Román, M. J., Jiménez-Moreno, G., García-Alix, A., Ilvonen, L., Ruha, L., and Seppä, H.: Past 200 kyr hydroclimate variability in the western Mediterranean and its connection to the African Humid Periods, Sci. Rep., 12, 9050, https://doi.org/10.1038/s41598-022-12047-1, 2022.
Català, A., Cacho, I., Frigola, J., Pena, L. D., and Lirer, F.: Holocene hydrography evolution in the Alboran Sea: a multi-record and multi-proxy comparison, Clim. Past, 15, 927–942, https://doi.org/10.5194/cp-15-927-2019, 2019.
Cody, R. D. and Cody, A. M.: Gypsum nucleation and crystal morphology in analog saline terrestrial environments, J. Sediment. Res., 58, 247–255, 1988.
Cohen, T. J., Arnold, L. J., Gázquez, F., May, J. H., Marx, S. K., Jankowski, N. R., and Gadd, P.: Late quaternary climate change in Australia's arid interior: Evidence from Kati Thanda–Lake Eyre, Quaternary Sci. Rev., 292, 107635, https://doi.org/10.1016/j.quascirev.2022.107635, 2022.
Cruz-Sanjulián, J.: Mapa Geológico de Teba, 1:50.000, hoja no. 1.037, Instituto Tecnológico Geominero de España, Madrid, https://hdl.handle.net/20.500.14352/62998 (last access: 10 December 2024), 1991.
Díaz-Azpiroz, M., Barcos, L., Balanyá, J. C., Fernández, C., Expósito, I., and Czeck, D. M.: Applying a general triclinic transpression model to highly partitioned brittle-ductile shear zones: A case study from the Torcal de Antequera massif, external Betics, southern Spain, J. Struct. Geol., 68, 316–336, 2014.
Díaz Azpiroz, M., Asencio Almansa, R., Senín Andrades, J. R., and Jiménez Bonilla, A.: Shape preferred orientation of dolostone bodies of a Triassic broken formation at the western External Betics, Geogaceta, 67, 11–14, 2020.
Elez, J., Silva, P. G., Huerta, P., and Martínez-Graña, A.: Isostatic compensation in the Western-Central Betic Cordillera (South Spain) caused by erosional unloading from the Messinian to the present: the emergence of an orogen, Geogaceta, 64, 103–106, 2018.
Elez, J., Silva, P. G., and Martínez-Graña, A. M.: Quantification of Erosion and Uplift in a Rising Orogen – A Large-Scale Perspective (Late Tortonian to Present): The Case of the Gibraltar Arc, Betic Cordillera, Southern Spain, Remote Sens., 12, 3492, https://doi.org/10.3390/rs12213492, 2020.
Flinch, J. F. and Soto, J. I.: Allochthonous Triassic and salt tectonic processes in the Betic-Rif orogenic arc, in: Permo-Triassic salt provinces of Europe, North Africa and the Atlantic margins, Elsevier, 417–446, https://doi.org/10.1016/B978-0-12-809417-4.00020-3, 2017.
Flinch, J. F. and Soto, J. I.: Structure and Alpine tectonic evolution of a salt canopy in the western Betic Cordillera (Spain), Mar. Petrol. Geol., 143, 105782, https://doi.org/10.1016/j.marpetgeo.2022.105782, 2022.
García-Alix, A., Jiménez-Moreno, G., Gázquez, F., Monedero-Contreras, R., López-Avilés, A., Jiménez-Espejo, F. J., and Anderson, R. S.: Climatic control on the Holocene hydrology of a playa-lake system in the western Mediterranean, Catena, 214, 106292, https://doi.org/10.1016/j.catena.2022.106292, 2022.
Höbig, N., Mediavilla, R., Gibert, L., Santisteban, J. I., Cendón, D. I., Ibáñez, J., and Reicherter, K.: Palaeohydrological evolution and implications for palaeoclimate since the Late Glacial at Laguna de Fuente de Piedra, southern Spain, Quatern. Int., 407, 29–46, 2016.
Hughes, C. E. and Crawford, J.: Spatial and temporal variation in precipitation isotopes in the Sydney Basin, Australia, J. Hydrol., 489, 42–55, 2013.
Jiménez-Bonilla, A., Expósito, I., Balanyá, J. C., Díaz-Azpiroz, M., and Barcos, L.: The role of strain partitioning on intermontane basin inception and isolation, External Western Gibraltar Arc, J. Geodynam., 92, 1–17, 2015.
Jimenez-Bonilla, A., Torvela, T., Balanyá, J. C., Expósito, I., and Díaz-Azpiroz, M.: Changes in dip and frictional properties of the basal detachment controlling orogenic wedge propagation and frontal collapse: The external central Betics case, Tectonics, 35, 3028–3049, 2016.
Jiménez-Bonilla, A., Díaz-Azpiroz, M., and Rodríguez, M. R.: Tectonics may affect closed watersheds used to monitor climate change and human activity effects, Terra Nova, 35, 58–65, 2023a.
Jiménez-Bonilla, A., Rodríguez-Rodríguez, M., Yanes, J. L., and Gázquez, F.: Hydrological modelling and evolution of lakes and playa-lakes in southern Spain constrained by geology, human management and climate change, Sci. Total Environ., 905, 167183, https://doi.org/10.1016/j.scitotenv.2023.167183, 2023b.
Jiménez-Bonilla, A., Díaz-Azpiroz, M., Rodríguez-Rodríguez, M., Balanyá, J. C., and Expósito, I.: Tectonic Controls on Drainage Network, Topographic Barriers Building and the Development of Endorheic Areas in the Western Betics (S Spain), Implications on the Evolution of the Atlantic-Mediterranean Water Divide, in preparation, 2024.
Kohfahl, C., Sprenger, C., Herrera, J. B., Meyer, H., Chacón, F. F., and Pekdeger, A.: Recharge sources and hydrogeochemical evolution of groundwater in semiarid and karstic environments: A field study in the Granada Basin (Southern Spain), Appl. Geochem., 23, 846–862, 2008.
Linares, L.: Hydrogeology of Fuente de Piedra lake (Málaga), PhD Thesis Dissertation, University of Granada, 343 pp., 1990.
Macumber, P. G.: Hydrological processes in the Tyrrell Basin, southeastern Australia, Chem. Geol., 96, 1–18, 1992.
Mann, M., Amman, C., Bradley, R., Briffa, K., Jones, P., Osborn, T., and Wigley, T.: On past temperatures and anomalous late-20th-century warmth, Eos Trans. Am. Geophys. Union, 84, 256–256, 2003.
Martos-Rosillo, S., González-Ramón, A., Jiménez-Gavilán, P., Andreo, B., Durán, J. J., and Mancera, E.: Review on groundwater recharge in carbonate aquifers from SW Mediterranean (Betic Cordillera, S Spain), Environ. Earth Sci., 74, 7571–7581, 2015.
Matthews, J., Anderson, S., Geoghegan, T., Ayers, J., Warner, K., Fieldman, G., and Falloon, P.: Evapotranspiration in a warming climate: Model uncertainty and role for climate adaptation, IOP Conf. Ser.: Earth Environ. Sci., 6, 052014, https://doi.org/10.1088/1755-1307/6/5/052014, 2008.
Moral, F., Rodriguez-Rodriguez, M., Beltrán, M., Benavente, J., and Cifuentes, V. J.: Water regime of Playa Lakes from southern Spain: conditioning factors and hydrological modeling, Water Environ. Res., 85, 632–642, 2013.
Moral Martos, F.: Caracterización y origen de las lunetas asociadas a las lagunas de La Lantejuela (Sevilla, España), Geogaceta, 59, 3–6, 2016.
Morcillo-Montalbá, L., Rodrigo-Gámiz, M., Martínez-Ruiz, F., Ortega-Huertas, M., Schouten, S., and Sinninghe Damsté, J. S.: Rapid Climate Changes in the Westernmost Mediterranean (Alboran Sea) Over the Last 35 kyr: New Insights From Four Lipid Paleothermometers (UK'37, TEXH86, RI-OH', and LDI), Paleoceanogr. Paleoclimatol., 36, e2020PA004171, https://doi.org/10.1029/2020PA004171, 2021.
Obert, J. C., Muenker, C. Staubwasser, M., Herwartz, D., Reicherter, K., and Chong, G.: 230Th dating of gypsum from lacustrine, brackish-marine and terrestrial environments, Chemical Geol., 607, 121019, https://doi.org/10.1016/j.chemgeo.2022.121019, 2022.
Reimer, P. J., Austin, W. E. N., Bard, E., Bayliss, A., Blackwell, P. G., Bronk Ramsey, C., Butzin, M., Cheng, H., Edwards, R. L., Friedrich, M., Grootes, P. M., Guilderson, T. P., Hajdas, I., Heaton, T. J., Hogg, A. G., Hughen, K. A., Kromer, B., Manning, S. W., Muscheler, R., Palmer, J. G., Pearson, C., van der Plicht, J., Reimer, R. W., Richards, D. A., Scott, E. M., Southon, J. R., Turney, C. S. M., Wacker, L., Adolphi, F., Büntgen, U., Capano, M., Fahrni, S. M., Fogtmann-Schulz, A., Friedrich, R., Köhler, P., Kudsk, S., Miyake, F., Olsen, J., Reinig, F., Sakamoto, M., Sookdeo, A. and Talamo, S.: The IntCal20 Northern Hemisphere Radiocarbon Age Calibration Curve (0–55 cal kBP), Radiocarbon, 62, 725–757, 2020.
Roberts, N., Reed, J. M., Leng, M. J., Kuzucuoğlu, C., Fontugne, M., Bertaux, J., and Karabiyikoğlu, M.: The tempo of Holocene climatic change in the eastern Mediterranean region: new high-resolution crater-lake sediment data from central Turkey, Holocene, 11, 721–736, 2001.
Rodríguez-Hernández, L., Hernández-Bravo, J. C., and Fernández-Mejuto, M.: Processing and management of hidrologic time series: user manual: application, TRASERO, Diputación de Alicante, Ciclo Hídrico, https://ciclohidrico.com/download/tratamiento-y-gestion-de-series-temporales-hidrologicas/trasero/ (last access: 10 December 2024), 2007.
Rodríguez-Rodríguez, M., Moral, F., Benavente, J., and Beltrán, M.: Developing hydrological indices in semi-arid playa-lakes by analyzing their main morphometric, climatic and hydrochemical characteristics, J. Arid Environ., 74, 1478–1486, 2010.
Rodríguez-Rodríguez, M., Green, A. J., López, R., and Martos-Rosillo, S.: Changes in water level, land use, and hydrological budget in a semi-permanent playa lake, Southwest Spain, Environ. Monit. Assess., 184, 797–810, 2012.
Rodríguez-Rodríguez, M., Martos-Rosillo, S., Pedrera, A., and Benavente-Herrera, J.: Ratosa playa lake in southern Spain. Karst pan or compound sink?, Environ. Monit. Assess., 187, 1–15, 2015.
Rodríguez-Rodríguez, M., Martos-Rosillo, S., and Pedrera, A.: Hydrogeological behaviour of the Fuente-de-Piedra playa lake and tectonic origin of its basin (Malaga, southern Spain), J. Hydrol., 543, 462–476, 2016.
Sánchez-Moral, S., Ordóñez, S., Benavente, D., and del Cura, M. G.: The water balance equations in saline playa lakes: comparison between experimental and recent data from Quero Playa Lake (central Spain), Sediment. Geol., 148, 221–234, 2002.
Sandler, A., Meunier, A., and Velde, B.: Mineralogical and chemical variability of mountain red/brown Mediterranean soils, Geoderma, 239, 156–167, 2015.
Schröder, T., van't Hoff, J., López-Sáez, J. A., Viehberg, F., Melles, M., and Reicherter, K.: Holocene climatic and environmental evolution on the southwestern Iberian Peninsula: a high-resolution multi-proxy study from Lake Medina (Cádiz, SW Spain), Quaternary Sci. Rev., 198, 208–225, 2018.
Schröder, T., López-Sáez, J. A., van't Hoff, J., and Reicherter, K.: Unravelling the Holocene environmental history of south-western Iberia through a palynological study of Lake Medina sediments, Holocene, 30, 13–22, 2020.
Vera, J. A. (Ed.): Geología de españa, IGME – Instituto Geológico y Minero de España, ISBN 84-7840-546-1, 2004.
Short summary
We conducted an interdisciplinary study of the Fuente de Piedra playa lake's evolution in southern Spain. We made water balances for the Fuente de Piedra playa lake's lifespan. Our results indicate that the Fuente de Piedra playa lake's level moved and tilted south-west, which was caused by active faults.
We conducted an interdisciplinary study of the Fuente de Piedra playa lake's evolution in...