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Lithostratigraphy and Chronology of Vistulian Periglacial Deposits in Józefów (Central Poland) Based on Luminescence Dating

Jacek Forysiak
Jacek Forysiak
, 
Aleksandra Majecka
Aleksandra Majecka
, 
Piotr Moska
Piotr Moska
 und 
Leszek Marks
Leszek Marks
   | 14. März 2024
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Online veröffentlicht: 14. März 2024
Seitenbereich: 182 - 194
Eingereicht: 18. Juli 2023
Akzeptiert: 10. Jan. 2024
DOI: https://doi.org/10.2478/geochr-2023-0015
Schlüsselwörter
© 2023 Jacek Forysiak et al., published by Sciendo
This work is licensed under the Creative Commons Attribution-NonCommercial-NoDerivatives 3.0 License.

Fig 1.

(A) Location of the study site in relation to extents of ice sheets, (B) Location on the geological background (according to SMGP 1:50,000). Holocene: 1 – fluvial sand and mud; Vistulian: 2 – mineral-organic mud, 3 – deluvial sand and mud, 4 – fluvial sands; Warta Stadial: 5 – glaciofluvial sand, 6 – glaciofluvial sand and gravel, 7 – glacial sand with gravel, 8 – sand, gravel and boulder (morainic), 9 – glacial till; 10 – study site.
(A) Location of the study site in relation to extents of ice sheets, (B) Location on the geological background (according to SMGP 1:50,000). Holocene: 1 – fluvial sand and mud; Vistulian: 2 – mineral-organic mud, 3 – deluvial sand and mud, 4 – fluvial sands; Warta Stadial: 5 – glaciofluvial sand, 6 – glaciofluvial sand and gravel, 7 – glacial sand with gravel, 8 – sand, gravel and boulder (morainic), 9 – glacial till; 10 – study site.

Fig 2.

Orthophotomap view of the Vistulian deposits sequence in sections I-V (their location is marked on topographic sketch below) with distinguished lithofacies (Table 2) and sampling sites for luminescence dating (Table 3).
Orthophotomap view of the Vistulian deposits sequence in sections I-V (their location is marked on topographic sketch below) with distinguished lithofacies (Table 2) and sampling sites for luminescence dating (Table 3).

Fig 3.

Lithostratigraphical scheme of the Vistulian deposits at the Józefów site with OSL age results in relationship to the Vistulian climatostratigraphy. OSL, optically stimulated luminescence.
Lithostratigraphical scheme of the Vistulian deposits at the Józefów site with OSL age results in relationship to the Vistulian climatostratigraphy. OSL, optically stimulated luminescence.

Lithofacies code used in this study.

Code Texture
G Gravel
S Sand
F Silt
C Organic matter
Code Structure
d Deformed
m Massive
h Horizontal

Results of lithological analysis for most samples of deposits used for luminescence dating.

Sample Ratios (phi) Morphoscopy of quartz grains (%)
ID Mz σI SkI RM EL M C NU
J_1 2.2 1.5 −0.5 34 10 31 19 6
J_8 2.2 09. 0.0 39 9 38 11 3
J_9 2.1 1.2 −0.3 35 9 36 16 4
J_10 2.2 1.4 −0.3 39 11 35 13 2
J_11 3.0 1.7 0.0 37 11 30 17 5
J_12 38 6 46 8 2
J_13 1.6 2.0 −0.1 50 4 38 6 2
J_14 50 5 33 10 2
J_15 4.9 3.4 0.7
J_16 4.4 1.8 0.5 28 18 36 15 3
J_17 2.1 1.05 −0.1 52 8 32 7 1
J_18 2.3 1.5 0.1 49 3 37 9 2
J_19 3.7 3.3 0.5 44 6 33 13 4
J_20 2.1 2.1 0.1 45 9 33 12 1
J_21 1.7 1.3 −0.1 41 10 39 9 1
J_22 1.7 1.1 −0.1 45 9 35 9 2
J_23 1.9 1.0 0.0 36 11 34 16 3
J_24 1.6 0.9 0.0 38 8 38 14 2
J_25 8.4 3.4 0.5 35 9 31 19 6

All important data for investigated luminescence samples: sample names, depth, radionuclide concentration, overdispersion, dose rate, equivalent dose (CAM model) and final age.

Lab. code Sample ID Sample depth (cm) Th (Bq/kg) U (Bq/kg) K (Bq/kg) Dose rate (Gy/ka) Overdispersion (%) Equivalent dose (Gy) OSL age (ka)
GdTL-3144 J_1 100 5.9±0.2 4.7±0.2 195±6 0.91±0.04 10 18.2±0.6 19.9±1.0
GdTL-3145 J_2 205 7.8±0.2 5.7±0.2 198±6 0.93±0.04 10 15.0±0.5 16.1±0.8
GdTL-3146 J_3 175 9.8±0.2 7.9±0.2 249±7 1.14±0.04 14 17.8±0.7 15.6±0.9
GdTL-3147 J_4 105 14.1±0.3 12.2±0.2 351±10 1.59±0.06 5 20.9±0.5 13.1±0.5
GdTL-3148 J_5 230 6.6±0.2 6.2±0.2 185±5 0.88±0.05 5 19.5±0.5 22.1±1.0
GdTL-3149 J_6 215 6.4±0.2 6.4±0.2 196±6 0.91±0.04 18 19.1±1.0 20.9±1.4
GdTL-3150 J_7 200 10.0±0.2 8.1±0.2 224±6 1.07±0.06 7 17.0±0.5 15.8±0.7
GdTL-3151 J_8 203 8.3±0.2 7.4±0.2 210±6 1.00±0.04 9 19.3±0.6 19.2±0.9
GdTL-3152 J_9 160 6.9±0.2 5.8±0.2 205±6 0.94±0.04 5 16.9±0.5 17.9±0.8
GdTL-3153 J_10 140 6.0±0.2 5.1±0.2 189±5 0.88±0.04 8 17.0±0.5 19.3±0.9
GdTL-3154 J_11 210 10.9±0.3 9.3±0.2 337±9 1.42±0.06 10 108.2±3.6 76.1±3.8
GdTL-3155 J_12 165 7.9±0.2 7.0±0.2 216±6 1.01±0.04 13 16.7±0.7 16.4±0.9
GdTL-3156 J_13 130 7.5±0.2 7.6±0.2 200±6 0.98±0.04 12 17.8±0.8 18.1±1.0
GdTL-3157 J_14 90 11.5±0.3 10.1±0.2 285±8 1.34±0.05 13 19.9±0.8 14.8±0.8
GdTL-3357 J_15 190 15.6±0.3 12.8±0.3 380±10 1.67±0.06 12 110.5±3.8 66.1±3.3
GdTL-3358 J_16 210 21.1±0.4 18.5±0.3 437±11 2.00±0.07 13 100.2±4.2 50.0±2.6
GdTL-3359 J_17 187 5.5±0.2 5.0±0.2 177±5 0.83±0.04 8 13.1±0.4 15.8±0.7
GdTL-3360 J_18 140 10.6±0.3 9.8±0.2 229±7 1.16±0.04 20 25.7±1.3 22.0±1.4
GdTL-3361 J_19 135 10.8±0.3 8.8±0.2 284±8 1.28±0.05 18 14.3±0.8 11.0±1.0
GdTL-3362 J_20 145 13.2±0.3 12.0±0.3 271±8 1.33±0.05 16 22.8±1.0 17.2±0.9
GdTL-3363 J_21 125 12.0±0.3 10.2±0.2 272±7 1.29±0.05 16 14.6±0.7 11.2±0.6
GdTL-3364 J_22 170 6.1±0.2 5.3±0.2 187±6 0.87±0.04 22 6.7±0.4 7.6±0.5
GdTL-3365 J_23 100 6.4±0.2 6.2±0.2 190±6 0.93±0.04 8 10.4±0.3 11.5±0.5
GdTL-3366 J_24 90 6.3±0.2 5.42±0.2 181±5 0.89±0.04 20 11.3±0.6 12.6±0.8
GdTL-3367 J_25 80 21.3±0.5 19.2±0.3 409±11 1.98±0.07 10 28.1±0.9 14.1±0.6
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