Benavente Herrera, JoséAlmécija Ruiz, CarmenCarrasco Cantos, FranciscoRodríguez Jiménez, P.Cruz Sanjulián, J. J.2019-06-122019-06-121992http://hdl.handle.net/10272/16400Some small temporary and permanent lakes near Antequera (Malaga) have been monitored in order to identify their main hydrochemical features. They display a wide variety both in chemical facies and salinity. The origin of these wetlands is related to triassic evaporite karst: closed depressions induced by dissolution and collapse. The results show in general a close similarity between these waters and those of the most significative springs that drain this karst, with a overimposed effect of saline concentration due to evaporationspaAtribución-NoComercial-SinDerivadas 3.0 Españahttp://creativecommons.org/licenses/by-nc-nd/3.0/es/HydrochemistryWetlandsEvaporite Karstjournal articleopen access