Articles | Volume 71, issue 1
E&G Quaternary Sci. J., 71, 59–81, 2022
https://doi.org/10.5194/egqsj-71-59-2022
E&G Quaternary Sci. J., 71, 59–81, 2022
https://doi.org/10.5194/egqsj-71-59-2022
Research article
01 Apr 2022
Research article | 01 Apr 2022

Chronostratigraphic and geomorphologic challenges of last glacial loess in Poland in the light of new luminescence ages

Ludwig Zöller et al.

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Cited articles

Aitken, M. J.: An introduction to optical dating, 267 pp., University Press, Oxford, ISBN 0198540922 (Hbk), 1998. 
Antoine, P.: Thermokarst processes and features from west-European loess series: new evidences for rapid climatic warming events during the Last Glacial, Quatern. Int., 21, 279–280, https://doi.org/10.1016/j.quaint.2012.07.088, 2013. 
Antoine, P., Goval, E., Jamet, G., Coutard, S., Moine, O., Herisson, D., Auguste, P., Guerin, G., Lagroix, F., Schmidt, E., Robert, V., Debenham, N., Meszner, S., and Bahain, J.-J.: Les séquences loessiques pléistocène supérieur d'Havrincourt (Pas-de-Calais, France): stratigraphie, paléoenvironnement, géochronologie et occupations paléolithiques, Quaternaire, 25, 321–368, https://doi.org/10.4000/quaternaire.7278, 2014. 
Antoine, P., Coutard, S., Guerin, G., Deschodt, L., Goval, E., and Locht, J.-L.: Upper Pleistocene loess-palaeosol records from northern France in the European context: environmental background and dating of the Middle Palaeolithic, Quatern. Int., 411, 4–24, https://doi.org/10.1016/j.quaint.2015.11.036, 2015. 
Avram, A., Constantin, D., Veres, D., Kelemen, S., Obreht, I., Hambach, U., Markovic, S. B., and Timar-Gabor, A.: Testing polymineral post-IR IRSL and quartz SAR-OSL protocols on Middle to Late Pleistocene loess at Batajnica, Serbia, Boreas, 49, 615–633, https://doi.org/10.1111/bor.12442, 2020. 
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Short summary
Comparing quartz optically stimulated luminescence (OSL) and fine-grain post-infrared infrared stimulated luminescence (pIRIR) ages, agreement was largely found, e.g. the bracketing of the L1SS1 pedocomplex to ca. 30–40 ka. Nevertheless some age differences between the Bayreuth (OSL) and the Gliwice (pIRIR) data invite further discussion. Exact dating using various protocols and grain sizes remains challenging, in particular for a periglacial environment with strong heterogeneity of material.