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Record of Depositional and Palaeoenvironmental Conditions of the Vrakúň Palaeomeander (SW Slovakia, Danube Plain) Cover

Record of Depositional and Palaeoenvironmental Conditions of the Vrakúň Palaeomeander (SW Slovakia, Danube Plain)

Open Access
|Sep 2026

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.

DOI: https://doi.org/10.48128/pisg-2026-71.3-07 | Journal eISSN: 2543-7313 | Journal ISSN: 0208-4589
Language: Polish, English
Page range: 105 - 122
Submitted on: Aug 10, 2026
Accepted on: Sep 3, 2026
Published on: Sep 21, 2026
Published by: University of Warsaw
In partnership with: Paradigm Publishing Services
Publication frequency: 4 issues per year

© 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.