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Chronostratigraphy of Late Glacial aeolian activity in SW Poland – A case study from the Niemodlin Plateau Cover

Chronostratigraphy of Late Glacial aeolian activity in SW Poland – A case study from the Niemodlin Plateau

Open Access
|Dec 2020

Figures & Tables

Fig 1

Microregions of the Niemodlin Plain and location of investigated sites, Siedliska and Przechód, with digital elevation model (DEM).

Fig 2

Sedimentary succession, radiocarbon and OSL ages of deposits at Siedliska (A) and Przechód (B) sites.

Table 1

Basic information about investigated samples. Dose rate values obtained with different system detectors and final Bayesian estimation. Final obtained age using CAM model.

Sampling depthDose rate (Gy/ka)
Lab.codeSample ID(cm)Water content (%)Gamma spectrometryμDose systemBayesian averagingOSL age (ka)
GdTL-2638Przechód_121207±31.06±0.080.88±0.070.98±0.0511.85±0.91
GdTL-2639Przechód_363607±30.90±0.070.89±0.070.89±0.0412.68±1.00
GdTL-2640Przechód_454507±30.81±0.060.58±0.060.74±0.0414.88±1.11
GdTL-2641Przechód_606007±30.74±0.050.62±0.060.70±0.0418.96±1.46
GdTL-2642Siedliska_1501507±30.94±0.070.85±0.070.92±0.0512.39±0.98
GdTL-2643Siedliska_3203207±30.90±0.070.91±0.070.90±0.0512.47±1.04
GdTL-2644Siedliska_3653657±31.33±0.101.34±0.081.35±0.0613.21±1.04
GdTL-2645Siedliska_4254257±31.11±0.091.08±0.071.10±0.0614.26±1.27
GdTL-2646Siedliska_4504507±31.37±0.111.33±0.081.37±0.0714.50±1.21
Table 2

Calibrated 14C ages of charcoals. The age was calibrated using OxCal program v4.2, (Bronk Ramsey, 2009 and Southon et al., 2013) with calibration curve IntCal13 (Reimer et al., 2013).

No.Sample nameAge 14C (BP)Range of calendar (calibrated) age 68% confidence levelRange of calendar (calibrated) age 95% confidence level
1Przechód _top11270 ± 17013320BP - 12960BP13450BP - 12780BP
2Przechód_bottom10780 ± 8012750BP - 12640BP12810BP - 12560BP
3Siedliska10915 ± 4512800BP - 12730BP12880BP - 12700BP
Fig 3

Depositional succession at Siedliska (A-D) and Przechód (E-H) sites: A – general view at the Siedliska site; B – S-2 unit with large-scale involutions and ice-wedge cast (arrow); C – fluvio-aeolian deposits (S-3 unit) with the fossil soil (arrow) in top of unit; D – aeolian deposits within coversand (S-4 unit) and stoss slope of dune (S-5 unit); E – top of P-1 unit, and aeolian deposits within coversand and bottom part of moving dune lee slope; F – soil within the lee slope of dune (top of P-3 unit); G – aeolian deposits within arm of dune (P-4 unit); H – climbing ripple lithofacies (arrow), deposited up the lee slope.

Fig 4

Relative probability density functions (Berger 2010) for all samples are presented on the scale of age.

Fig 5

Model of environmental changes at the turn of Weichselian Pleniglacial and Late Glacial; 18O/16O ratio after Rasmussen et al. (2014), chronostratigraphy after Vandenberghe et al. (2013).

DOI: https://doi.org/10.2478/geochr-2020-0015 | Journal eISSN: 1897-1695 | Journal ISSN: 1733-8387
Language: English
Page range: 124 - 137
Submitted on: Nov 29, 2019
Accepted on: May 29, 2020
Published on: Dec 31, 2020
Published by: Sciendo
In partnership with: Paradigm Publishing Services

© 2020 Piotr Moska, Zdzisław Jary, Robert Jan Sokołowski, Grzegorz Poręba, Jerzy Raczyk, Marcin Krawczyk, Jacek Skurzyński, Paweł Zieliński, Adam Michczyński, Konrad Tudyka, Grzegorz Adamiec, Natalia Piotrowska, Fatima Pawełczyk, Michał Łopuch, Agnieszka Szymak, Kamila Ryzner, published by Sciendo
This work is licensed under the Creative Commons Attribution-NonCommercial-NoDerivatives 3.0 License.