
Figure 1
Location of sites mentioned in the text. 1: Balcarova skála, 2: Brno Štýřice III (formerly known as Brno, Videňska st. 3), 3: Brzoskwinia, 4: Deszczowa Cave, 5: Dzierżysław 35, 6: Hłomcza, 7: Keblice, 8: Klementowice-Kolonia 20, 9: Komarowa Cave, 10: Koněpruská Cave, 11: Kraków, Spadzista St. C2, 12: Krucza Skała Cave, 13: Mamutowa Cave, 14: Maszycka Cave, 15: Mosty 13, 16: Nová Drátenicka, 17: Pekárna Cave, 18: Putim, 19: Sowin 7, 20: Stránská skála IV, 21: Svobodné Dvory, 22: Targowisko 10, 23: Wierzawice 31, 24: Wilczyce 10, 25: Wołowice, 26: Zalas Cave, 27: Zawalona Cave, 28: Žitného Cave. Legend items: a: Magdalenian sites, b: Epigravettian sites, c: LGM range, d: Pommeranian phase range.
Table 1
List of analysed Epigravettian, middle and late Magdalenian dates from the territory of Poland. The last column indicates if the date was considered as outlier and rejected from the further analysis.
| Site | Method | Lab code | Measured age (BP) | Is outlier? |
|---|---|---|---|---|
| Epigravettian | ||||
| Deszczowa Cave | 14C | Gd-10212 | 17480 ± 310 | no |
| Deszczowa Cave | 14C | GdA-964 | 16150 ± 280 | no |
| Kraków - Spadzista C2 | 14C | Ly-2541 | 17400 ± 310 | no |
| Targowisko | 14C | Poz-14691 | 14820 ± 70 | no |
| Targowisko | 14C | Poz-14692 | 14790 ± 80 | no |
| Targowisko | 14C | Poz-14695 | 14720 ± 70 | no |
| Targowisko | 14C | Poz-14694 | 14520 ± 70 | no |
| Targowisko | 14C | Poz-14693 | 13720 ± 70 | yes |
| Zawalona Cave | 14C | n.a. | 15380 ± 340 | no |
| Zawalona Cave | 14C | n.a. | 14060 ± 340 | no |
| Sowin 7 | OSL | GdTL-2497 | 16204 ± 916 | no |
| Sowin 7 | OSL | GdTL-2496 | 15474 ± 857 | no |
| Maszycka Cave (Middle Magdalenian) | ||||
| Maszycka Cave | 14C | Ly-2454 | 15490 ± 319 | no |
| Maszycka Cave | 14C | KIA-39228 | 15115 ± 60 | no |
| Maszycka Cave | 14C | KIA-39226 | 15025 ± 50 | no |
| Maszycka Cave | 14C | KIA-39227 | 15015 ± 50 | no |
| Maszycka Cave | 14C | KIA-39225 | 14855 ± 60 | no |
| Maszycka Cave | 14C | Ly-2453 | 14520 ± 240 | no |
| Late Magdalenian | ||||
| Krucza Skała Cave | 14C | Poz-27245 | 12970 ± 60 | no |
| Krucza Skała Cave | 14C | Poz-1138 | 12520 ± 70 | no |
| Krucza Skała Cave | 14C | Poz-27261 | 12480 ± 60 | no |
| Krucza Skała Cave | 14C | Poz-1139 | 11980 ± 70 | no |
| Krucza Skała Cave | 14C | Lod-407 | 11450 ± 200 | no |
| Krucza Skała Cave | 14C | Poz-1141 | 11210 ± 80 | no |
| W Zalasie Cave | 14C | OxA-6625 | 12820 ± 80 | no |
| W Zalasie Cave | 14C | OxA-6591 | 12530 ± 110 | no |
| Klementowice 20 | 14C | Poz-54822 | 12730 ± 90 | no |
| Wilczyce 10 | 14C | OxA-16728 | 13180 ± 60 | no |
| Wilczyce 10 | 14C | OxA-26545 | 13155 ± 65 | no |
| Wilczyce 10 | 14C | OxA-26546 | 13125 ± 65 | no |
| Wilczyce 10 | 14C | Poz-14891 | 13020 ± 60 | no |
| Wilczyce 10 | 14C | Poz-19048 | 13000 ± 110 | no |
| Wilczyce 10 | 14C | Poz-3914 | 12960 ± 60 | no |
| Wilczyce 10 | 14C | OxA-16729 | 12870 ± 60 | no |
| Wilczyce 10 | 14C | Poz-3927 | 12840 ± 70 | no |
| Wilczyce 10 | 14C | Poz-14892 | 12770 ± 120 | no |
| Wilczyce 10 | 14C | Poz-3926 | 12620 ± 60 | no |
| Wilczyce 10 | 14C | Poz-14463 | 12550 ± 80 | no |
| Wilczyce 10 | 14C | Poz-14384 | 12480 ± 70 | no |
| Wilczyce 10 | 14C | Poz-14385 | 12390 ± 100 | no |
| Wilczyce 10 | 14C | Ua-20413 | 12315 ± 90 | no |
| Wilczyce 10 | 14C | Ua-20412 | 12110 ± 90 | no |
| Wilczyce 10 | 14C | Poz-19046 | 11960 ± 140 | no |
| Wilczyce 10 | 14C | Ua-15723 | 11890 ± 105 | no |
| Wilczyce 10 | 14C | Poz-19049 | 11870 ± 120 | no |
| Wilczyce 10 | 14C | Ua-15722 | 11665 ± 135 | no |
| Wilczyce 10 | 14C | Ua-15720 | 11400 ± 135 | no |
| Wilczyce 10 | 14C | Poz-19047 | 11340 ± 60 | no |
| Dzierżysław 35 | 14C | Poz-10136 | 14150 ± 70 | yes |
| Dzierżysław 35 | 14C | GdA-69 | 13500 ± 80 | no |
| Dzierżysław 35 | 14C | GdA-193 | 13370 ± 80 | no |
| Dzierżysław 35 | 14C | GdA-70 | 13220 ± 70 | no |
| Dzierżysław 35 | 14C | Poz-10135 | 13180 ± 60 | no |
| Dzierżysław 35 | 14C | Poz-7318 | 12150 ± 70 | yes |
| Sowin 7 | OSL | GdTL-2494 | 14711 ± 856 | no |
| Sowin 7 | OSL | GdTL-2495 | 13830 ± 895 | no |
| Komarowa Cave | 14C | Poz-6621 | 12260 ± 60 | no |
| Mosty | 14C | Lod-107 | 11290 ± 280 | no |
| Wierzawice | 14C | Poz-36901 | 11560 ± 40 | no |
| Wierzawice | 14C | Poz-41200 | 11080 ± 130 | no |

Figure 2
Bayesian models of the chronology of Epigravettian and Magdalenian on the background of palaeoclimatic event record of NGRIP oxygen isotope curve (GICC05modelext timescale, by Rasmussen et al., 2014). Probability distributions for dates and modelled events shown with 95,4% confidence level.
Table 2
Results of Bayesian age modelling of two discussed models of Epigravettian and Magdalenian settlement chronology. Amodel: model agreement index, Aoverall: overall agreement index, %: probability distribution range, C: convergence integral.
| Model | Name | Modelled (BP) | ||||||
|---|---|---|---|---|---|---|---|---|
| from | to | % | from | to | % | C | ||
| Model 1 (Amodel=80.0, Aoverall=75.7) | Phase | |||||||
| Sequence | ||||||||
| Boundary Start Epiqravettian | 21940 | 20820 | 68.2 | 22950 | 20460 | 95.4 | 95.6 | |
| Phase Epigravettian | ||||||||
| Boundary End Epigravettian | 16810 | 15130 | 68.2 | 17370 | 13890 | 95.4 | 96.8 | |
| Span Epigravettian | 4400 | 6660 | 68.2 | 3670 | 8260 | 95.4 | 97.0 | |
| Sequence | ||||||||
| Boundary Start Maszycka | 18500 | 18220 | 68.2 | 18850 | 18130 | 95.4 | 98.2 | |
| Phase Maszycka | ||||||||
| Boundary End Maszycka | 18260 | 17950 | 68.2 | 18320 | 17560 | 95.4 | 97.9 | |
| Span Maszycka | 0 | 480 | 68.2 | 0 | 1180 | 95.4 | 97.5 | |
| Sequence | ||||||||
| Boundary Start Magdalenian | 16300 | 16060 | 68.2 | 16470 | 15960 | 95.4 | 99.7 | |
| Phase Magdalenian | ||||||||
| Boundary End Magdalenian | 13080 | 12860 | 68.2 | 13150 | 12680 | 95.4 | 99.6 | |
| Span Magdalenian | 3050 | 3410 | 68.2 | 2920 | 3640 | 95.4 | 99.7 | |
| Order | ||||||||
| =End Magdalenian | 13080 | 12860 | 68.2 | 13150 | 12680 | 95.4 | 99.6 | |
| =Start Magdalenian | 16300 | 16060 | 68.2 | 16470 | 15960 | 95.4 | 99.7 | |
| =End Maszycka | 18260 | 17950 | 68.2 | 18320 | 17560 | 95.4 | 97.9 | |
| =Start Maszycka | 18500 | 18220 | 68.2 | 18850 | 18130 | 95.4 | 98.2 | |
| =End Epigravettian | 16810 | 15130 | 68.2 | 17370 | 13890 | 95.4 | 96.8 | |
| =Start Epigravettian | 21940 | 20820 | 68.2 | 22950 | 20460 | 95.4 | 95.6 | |
| Difference End Epigravettian – Start Magdalenian | −620 | 1060 | 68.2 | −1200 | 2320 | 95.4 | 97.5 | |
| Model 2 (Amodel=82.4, Aoverall=78.9) | Phase | |||||||
| Sequence | ||||||||
| Boundary Start Epigravettian | 22020 | 20840 | 68.1 | 23410 | 20480 | 95.4 | 96.4 | |
| Phase Epigravettian | ||||||||
| Boundary End Epigravettian | 17800 | 17030 | 68.2 | 17910 | 15680 | 95.4 | 99.1 | |
| Span Epigravettian | 3310 | 4990 | 68.2 | 2840 | 7060 | 95.4 | 98.6 | |
| Sequence | ||||||||
| Boundary Start Maszycka | 18500 | 18220 | 68.2 | 18850 | 18130 | 95.4 | 96.0 | |
| Phase Maszycka | ||||||||
| Boundary End Maszycka | 18270 | 17950 | 68.2 | 18320 | 17550 | 95.4 | 96.4 | |
| Span Maszycka | 0 | 470 | 68.2 | 0 | 1170 | 95.4 | 96.6 | |
| Sequence | ||||||||
| Boundary Start Magdalenian | 16300 | 16060 | 68.2 | 16470 | 15960 | 95.4 | 99.8 | |
| Phase Magdalenian | ||||||||
| Boundary End Magdalenian | 13080 | 12860 | 68.2 | 13150 | 12690 | 95.4 | 98.7 | |
| Span Magdalenian | 3050 | 3410 | 68.2 | 2920 | 3640 | 95.4 | 99.7 | |
| Order | ||||||||
| =End Magdalenian | 13080 | 12860 | 68.2 | 13150 | 12690 | 95.4 | 98.7 | |
| =Start Magdalenian | 16300 | 16060 | 68.2 | 16470 | 15960 | 95.4 | 99.8 | |
| =End Maszycka | 18270 | 17950 | 68.2 | 18320 | 17550 | 95.4 | 96.4 | |
| =Start Maszycka | 18500 | 18220 | 68.2 | 18850 | 18130 | 95.4 | 96.0 | |
| =End Epigravettian | 17800 | 17030 | 68.2 | 17910 | 15680 | 95.4 | 99.1 | |
| =Start Epigravettian | 22020 | 20840 | 68.1 | 23410 | 20480 | 95.4 | 96.4 | |
| Difference End Epigravettian – Start Magdalenian | −1670 | −780 | 68.2 | −1810 | 580 | 95.4 | 98.9 | |

Figure 3
Two models of probabilities of possible chronological relationships between Epigravettian and late Magdalenian, based on the results of the OxCal Order query (Bronk Ramsey, 2009a), generated by prob.phases.relatr script (Alberti, 2016). E – Epigravettian, M – late Magdalenian, startE – start of Epigravettian, startM – start of late Magdalenian, endE, – end of Epigravettian, endM – end of late Magdalenian.