Record of Depositional and Palaeoenvironmental Conditions of the Vrakúň Palaeomeander (SW Slovakia, Danube Plain)
Abstract
Former river channels serve as vital geoarchives for reconstructing palaeoenvironmental shifts. This study investigates the Vrakúň palaeomeander, a cut-off bend of the Barč branch (Danube Plain, Žitný ostrov, Slovakia). Based on a sediment core, we conducted grain-size, lithodynamic, and paleobotanical analyses. Textural indices (Visher curves, Passega diagrams, Folk-Ward parameters) differentiated channel and overbank facies. Basal high-energy deposits transition upward into fine-grained overbank layers and organic peat. Mineral interbeddings in gyttja sediments indicate four flood events. Radiocarbon (AMS) dating traces the evolution of the meander from its neck cutoff in the Iron Age (609–448 cal BC) to progressive infilling and a shift from lacustrine to paludic environment. Drainage systems accelerated groundwater decline, inducing peat earthification and soil salinization. These findings provide baseline palaeohydrological data and highlight the meander’s value as an ecological refuge.
© 2026 Peter Pišút, Ewa Smolska, Piotr Szwarczewski, Juraj Procházka, Šárka Mindová, published by University of Warsaw
This work is licensed under the Creative Commons Attribution-NonCommercial-NoDerivatives 4.0 License.