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Influence of Climate Change and Settlement on Lithology of Peat Deposits in the Zielonka Forest (Central-Western Poland) Cover

Influence of Climate Change and Settlement on Lithology of Peat Deposits in the Zielonka Forest (Central-Western Poland)

Open Access
|Sep 2026

Figures & Tables

Fig. 1.

Maps of the studied area: A – the upper Trojanka valley, B – close-up view of Głęboczek sites, C – the conical hillfort and locations of the studied profiles. 1 – flat morainic plateau; 2 – undulating morainic plateau; 3 – terminal moraine (mostly depositional); 4 – terminal moraine (mostly pushed); 5 – edges of subglacial valley; 6 – outwash plain; 7 – kames; 8 – depression formed by the exarative activity of the ice sheet; 9 – valleys floor; 10 – peat plain; 11 – cross-section; EM – Early Middle Ages; LM – Late Middle Ages; MP – Modern Period.

Table 1.

AMS radiocarbon dating of the GL I profile.

Sample nameDepthAge 14CCalibrationMaterial dated
[cm][14C BP][cal. AD]
Poz-17129451–52285 ± 30
  • 1500–1600 (60.0%)

  • 1615–1664 (34.0%)

  • 1786–1794 (1.4%)

Alnus sp.: fruit, three seeds
Poz-17129562–63345 ± 301470–1637 (95.4%)Alnus glutinosa: small twigs, seed
Poz-17133094–95−347 ± 24
  • 1956.5–1957.5 (27.6%)

  • 2007.96–2008.6 (25.9%)

  • 2008.88–2009.68 (41.9%)

Bud scale, seed
Poz-174243125–126330 ± 301480–1640 (95.4%)Plant remains
Poz-174556134–135710 ± 30
  • 1262–1310 (80.1%)

  • 1362–1387 (15.3%)

Plant remains
Poz-170386146–147355 ± 30
  • 1458–1529 (42.7%)

  • 1540–1635 (52.8%)

Alnus sp.: leaves, bark; coal
Poz-170388148–149350 ± 30
  • 1461–1530 (39.7%)

  • 1539–1636 (55.7%)

Plant remains
Poz-170389150–151850 ± 30
  • 1054–1060 (0.9%)

  • 1157–1267 (94.6%)

Alnus sp.: bark, twig
Poz-170390166–167340 ± 301474–1638 (95.4%)Alnus sp.: bud scale, leaf, bark, fruit
Fig. 2.

Lithological diagrams of studied profiles including: grain-size parameters of Folk and Ward (1957), LOI results, particle classes (Udden 1914, Wentworth 1922) and calibrated age. The course of the cross-section is marked on Figure 1C.

Table 2.

Characteristics of GL I litofacies.

FaciesDepthAgeSediment accumulation ratioOrganic matter content LOI550CaCO3 content LOI950GravelSandSiltFsClayFc
[cm][cal. AD][cm ∙ yr−1][%]
I165–1701020–10700.3016.06–46.300.48–6.470.0013.21–45.4154.59–86.790.03–0.74
II154–1651070–11800.1532.13–47.821.86–9.390.0017.55–36.1263.88–82.45<0.60
III118–1541180–15020.1054.69–88.060.47–10.810.0023.20–46.0054.00–76.80<0.45
IV96–1181502–15330.840.69–7.290.18–4.58<2.8324.42–85.9514.05–75.58<0.06
V91–961533–15410.6320.06–43.400.48–5.520.0055.25–69.0530.95–44.75<0.22
VI65–911541–16100.326.88–74.870.26–0.88<0.1714.73–93.256.75–85.27<0.01
VII32–651610–18000.1958.32–82.160.73–2.040.002.78–27.2572.75–97.22<0.01
VIII15–321800–19180.0971.75–85.020.71–1.330.003.35–32.4667.54–96.65<0.16
IX0–151918 to present0.0566.47–74.421.10–2.01<2.5930.81–84.4915.51–69.19<0.01
Fig. 3.

Age-depth model of the GL I profile with lithofacies (I–IX) and periodisation (Starkel et al. 2013, Przybylak 2011). SA2, SA3 – Subatlantic and its sub-zones; MWP – Medieval Warm Period; TP – Transitional Period; LIA – Little Ice Age; CWP – contemporary warming period; EM – Early Middle Ages; LM – Late Middle Ages; MP – Modern Period; green area – time conical hillfort was in active use (Jasnosz 1980); blue area – time-chartered town was in active use (Chmielewski et al. 1986).

Fig. 4.

Cumulative curve of mean grain-size distribution of the GL I lithofacies at the arithmetic scale.

Fig. 5.

Cumulative curve of mean grain-size distribution of the GL 1 to 3 profiles at the arithmetic scale.

Table 3.

Characteristics of the GL 1, GL 2 and GL 3 profiles.

CoreDepthOrganic matter content LOI550CaCO3 content LOI950GravelSandSilt FsClay Fc
[cm][%]
GL 10–1201.07–36.690.28–1.01<14.8873.11–93.654.19–26.89<0.01
GL 20–1050.67–9.9200.20–1.620.0089.70–94.385.62–10.30<0.01
GL 30–900.67–36.690.60–5.21<24.0768.32–93.256.75–29.03<0.01
Fig. 6.

Grain-size parameter relationship plots for the GL I lithofacies (I–IX) and the GL 1 to 3 profiles. (Upper row) Coordinate systems (Mycielska-Dowgiałło Ludwikowska-Kędzia 2011), (lower row Lithodynamics interpretation (Sly et al. 1983). Graphical indicators at the phi scale: MZ – mean grain-size; σI – sorting; SkI – skewness; moments indicators at the phi scale: MM1 – mean grain-size; MM2 – sorting; MM3 – skewness; 1 – channel deposits (1st syst.); 2a – overbank deposits (2nd syst.); 2b – overbank-pool deposits (1st syst.); A – accumulation conditions; B, C – transport conditions; D – erosion conditions; H – high energy regime; L – low energy regime; a – skewness divide; b – max kurtosis; gray – distribution of samples researched by Mycielskiej-Dowgiałło (2007).

Fig. 7.

Comparison of lithological diagrams of the GL I core (symbols explanation at Fig. 2) with: Esper et al. (2025) mean temperature (red line) and Luterbacher et al. (2010) temperature reconstruction (magenta line); dry (orange boxes) and wet (blue boxes) climate phases (Starkel et al. 2013); periods of increased fluvial activity (Starkel 2011). Periodisation and blue/green areas explained at Figure 2. SA2, SA3 – Subatlantic and its sub-zones; MWP – Medieval Warm Period; TP – Transitional Period; LIA – Little Ice Age; CWP – contemporary warming period; EM – Early Middle Ages; LM – Late Middle Ages; MP – Modern Period.

DOI: https://doi.org/10.14746/quageo-2026-0036 | Journal eISSN: 2081-6383 | Journal ISSN: 2082-2103 (formerly 0137-477X)
Language: English
Submitted on: Jan 29, 2026
Published on: Sep 23, 2026
Published by: Adam Mickiewicz University
In partnership with: Paradigm Publishing Services
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© 2026 Mateusz Robaczewski, published by Adam Mickiewicz University
This work is licensed under the Creative Commons Attribution 4.0 License.