An Impact of Short-Term Climate Oscillations in the Late Pleniglacial and Lateglacial Interstadial on Sedimentary Processes and the Pedogenic Record in Central Poland

References

• Aitken, M. J. 1985. Thermoluminescence dating. London: Academic Press.
   Google Scholar
• Ammann, B., J. Schwander, U. Eicher, U. J. van Raden, D. Colombaroli, J. F. N. van Leeuwen, H. Lischke, S. J. Brooks, K. Novakova, M. R. van Hardenbroek, et al. 2013. Biotic responses to rapid warming at Termination 1a at Gerzensee (Central Europe)—Synthesis and hypotheses on primary succession, nutrients, albedo and ecological interactions. Palaeogeography Palaeoclimatology Palaeoecology 391:111–31. doi: 10.1016/j.quaint.2012.07.071.
   Web of Science ®Google Scholar
• Berger, G. W. 2010. An alternate form of probability-distribution plot for De values. Ancient TL 28:11–22.
   Google Scholar
• Bockheim, J. G. 2010. Evolution of desert pavements and the vesicular layer in soils of the Transantarctic Mountains. Geomorphology 118 (3–4):433–43. doi: 10.1016/j.geomorph.2010.02.012.
   Web of Science ®Google Scholar
• Bos, J. A. A., P. De Smedt, H. Demiddele, W. Z. Hoek, R. Langohr, V. Marcelino, N. Van Asch, D. Van Damme, T. Van der Meeren, J. Verniers, et al. 2017. Multiple oscillations during the Lateglacial as recorded in a multi-proxy, high-resolution record of the Moervaart palaeolake (NW Belgium). Quaternary Science Reviews 162:26–41. doi: 10.1016/j.quascirev.2017.02.005.
   Web of Science ®Google Scholar
• Bos, J. A. A., P. De Smedt, H. Demiddele, W. Hoek, R. Langohr, V. Marcelino, N. Van Asch, D. Van Damme, T. Van Der Meeren, J. Verniers, et al. 2018. Weichselian Lateglacial environmental and vegetation development in the Moervaart palaeolake area (NW Belgium): Implications for former human occupation patterns. Review of Palaeobotany and Palynology 248:1–14. doi: 10.1016/j.revpalbo.2017.09.006.
   Web of Science ®Google Scholar
• Bos, J. A. A., F. Verbruggen, S. Engels, and P. Crombé. 2013. The influence of environmental changes on local and regional vegetation patterns at Rieme, (NW Belgium): Implications for Final Palaeolithic habitation. Vegetation History and Archaeobotany 22 (1):17–38. doi: 10.1007/s00334-012-0356-0.
   Web of Science ®Google Scholar
• Bronk Ramsey, C. 2009. Bayesian analysis of radiocarbon dates. Radiocarbon 51 (1):337–60. doi: 10.1017/S0033822200033865.
   Web of Science ®Google Scholar
• Christiansen, H. H., and H. Svensson. 1998. Windpolished boulders as indicators of a Late Weichselian wind regime in Denmark in relation to neighbouring areas. Permafrost and Periglacial Processes 9 (1):1–21. doi: 10.1002/(SICI)1099-1530(199801/03)9:1<1::AID-PPP271>3.0.CO;2-X.
   Web of Science ®Google Scholar
• Crombé, P., J. A. Bos, F. Cruz, and J. Verhegge. 2020. Repeated aeolian deflation during the Allerød/GI-1a-c in the coversand lowland of NW Belgium. Catena 188:104453. doi: 10.1016/j.catena.2020.104453.
   Web of Science ®Google Scholar
• Derese, C., D. A. G. Vandenberghe, M. Van Gils, F. Mees, E. Paulissen, and P. Van Den Haute. 2012. Final Palaeolithic settlements of the Campine region (NE Belgium) in their environmental context: Optical age constraints. Quaternary International 251:7–21. doi: 10.1016/j.quaint.2011.03.023.
   Web of Science ®Google Scholar
• Galbraith, R. F., R. G. Roberts, G. M. Laslett, H. Yoshida, and J. M. Olley. 1999. Optical dating of single and multiple grains of quartz from Jinminum Rock Shelter, Northern 12 Australia. Part I, experimental design and statistical models. Archaeometry 41 (2):339–1857. doi: 10.1111/j.1475-4754.1999.tb00987.x.
   Web of Science ®Google Scholar
• Good, T. R., and I. D. Bryant. 1985. Fluvio-aeolian sedimentation—An example from Banks Island, N.W.T., Canada. Geografiska Annaler 67 (1–2):33–46. doi: 10.1080/04353676.1985.11880128.
   Google Scholar
• Goździk, J. 2000. Aeolian cover sands in the south-eastern part of the Łódź region. In2000 Aeolian processes in different landscape zones: Dissertations of Faculty of Earth Sciences vol. 5, ed. R. J. Dulias and J. Pełka-Gościniak, 80–8. Sosnowiec, Poland: University of Silesia.
   Google Scholar
• Gozdzik, J. S., and H. M. French. 2004. Apparent upfreezing of stones in late‐Pleistocene coversand, Bełchatów vicinity. Permafrost and Periglacial Processes 15 (4):359–66. doi: 10.1002/ppp.491.
   Web of Science ®Google Scholar
• Guerin, G., N. Mercier, and G. Adamiec. 2011. Dose-rate conversion factors: Update. Ancient TL 29:5–8.
   Google Scholar
• Holloway, J. E., and A. G. Lewkowicz. 2020. Half a century of discontinuous permafrost persistence and degradation in western Canada. Permafrost and Periglacial Processes 31 (1):85–96. doi: 10.1002/ppp.2017.
   Web of Science ®Google Scholar
• Hunter, R. E. 1977. Basic types of stratification in small eolian dunes. Sedimentology 24 (3):361–87. doi: 10.1111/j.1365-3091.1977.tb00128.x.
   Web of Science ®Google Scholar
• Hunter, R. E., and D. M. Rubin. 1983. Interpreting cyclic crossbedding, with an example from the Navajo Sandstone. In Eolian sediments and processes, development in sedimentology, vol. 38, ed. M. E. Brookfield and T. S. Ahlbrandt, 407–27. Amsterdam: Elsevier.
   Google Scholar
• Jahn, R., H. P. Blume, V. B. Asio, O. Spaargaren, and P. Schad. 2006. Guidelines for soil description. Rome: FAO.
   Google Scholar
• James, M., A. G. Lewkowicz, S. L. Smith, and C. M. Miceli. 2013. Multi-decadal degradation and persistence of permafrost in the Alaska Highway corridor, northwest Canada. Environmental Research Letters 8 (4):045013. doi: 10.1088/1748-9326/8/4/045013.
   Web of Science ®Google Scholar
• Jankowski, M. 2012. Lateglacial soil paleocatena in inland-dune area of the Toruń Basin, Northern Poland. Quaternary International 265:116–25. doi: 10.1016/j.quaint.2012.02.006.
   Web of Science ®Google Scholar
• Kaiser, K., A. Hilgers, N. Schlaak, M. Jankowski, P. Kühn, S. Bussemer, and K. Przegiętka. 2009. Palaeopedological marker horizons in northern central Europe: Characteristics of Lateglacial Usselo and Finow soils. Boreas 38 (3):591–609. doi: 10.1111/j.1502-3885.2008.00076.x.
   Web of Science ®Google Scholar
• Kaiser, K., T. Schneider, M. Küster, E. Dietze, A. Fülling, S. Heinrich, C. Kappler, O. Nelle, M. Schult, M. Theuerkauf, et al. 2020. Palaeosols and their cover sediments of a glacial landscape in northern central Europe: Spatial distribution, pedostratigraphy and evidence on landscape evolution. Catena 193:104647. doi: 10.1016/j.catena.2020.104647.
   Web of Science ®Google Scholar
• Kasse, C. 2002. Sandy aeolian deposits and environments and their relation to climate during the Last Glacial Maximum and Lateglacial in northwest and Central Europe. Progress in Physical Geography 26:507–32. doi: 10.1191/0309133302pp350ra.
   Web of Science ®Google Scholar
• Kasse, C., and G. Aalbersberg. 2019. A complete Late Weichselian and Holocene record of aeolian coversands, drift sands and soils forced by climate change and human impact, Ossendrecht, the Netherlands. Netherlands Journal of Geosciences 98:1–22. doi: 10.1017/njg.2019.3.
   Google Scholar
• Kasse, C., S. J. P. Bohncke, J. Vandenberghe, and G. Gabris. 2010. Fluvial style changes during the last glacial–interglacial transition in the middle Tisza valley (Hungary). Proceedings of the Geologists' Association 121 (2):180–94. doi: 10.1016/j.pgeola.2010.02.005.
   Web of Science ®Google Scholar
• Kasse, C., R. T. Van Balen, S. J. P. Bohncke, J. Wallinga, and M. Vreugdenhil. 2017. Climate and base-level controlled fluvial system change and incision during the last glacial–interglacial transition, Roer river, the Netherlands–western Germany. Netherlands Journal of Geosciences 96 (2):71–92. doi: 10.1017/njg.2016.50.
   Web of Science ®Google Scholar
• Kasse, C., D. Vandenberghe, F. De Corte, and P. Van Den Haute. 2007. Late Weichselian fluvio-aeolian sands and coversands of the type locality Grubbenvorst (southern Netherlands): Sedimentary environments, climate record and age. Journal of Quaternary Science 22 (7):695–708. doi: 10.1002/jqs.1087.
   Web of Science ®Google Scholar
• Kasse, C., H. A. G. Woolderink, M. E. Kloos, and W. Z. Hoek. 2020. Source-bordering aeolian dune formation along the Scheldt River (southern Netherlands–northern Belgium) was caused by Younger Dryas cooling, high river gradient and southwesterly summer winds. Netherlands Journal of Geosciences 99:13–15. doi: 10.1017/njg.2020.15.
   Web of Science ®Google Scholar
• Klatkowa, H., J. Czyż, and J. Forysiak. 1999. Szczegółowa mapa geologiczna Polski w skali 1:50 000, arkusz Szadek wraz z objaśnieniami [Detailed geological map of Poland in scale 1:50 000, sheet Szadek with explanations]. Warsaw, Poland: PIG.
   Google Scholar
• Kocurek, G. 1988. First-order and super bounding surfaces in eolian sequences—Bounding surfaces revisited. In Late Paleozoic and Mesozoic eolian deposits of the Western interior of the United States: Sedimentary geology, vol. 56, ed. G. Kocurek, 193–206. Amsterdam: Elsevier.
   Google Scholar
• Kolstrup, E., A. Murray, and G. Possnert. 2007. Luminescence and radiocarbon ages from laminated Lateglacial aeolian sediments in western Jutland, Denmark. Boreas 36 (3):314–25. doi: 10.1080/03009480601024606.
   Web of Science ®Google Scholar
• Koster, A. E. 1988. Ancient and modern cold-climate aeolian sand deposition: A review. Journal of Quaternary Science 3 (1):69–83. doi: 10.1002/jqs.3390030109.
   Google Scholar
• Kozarski, S., and B. Nowaczyk. 1991. Lithofacies variation and chronostratigraphy of Late Vistulian and Holocene aeolian phenomena in northwestern Poland. Zeitschrift für Geomorphologie N.F., Supplementband 90:107–22.
   Google Scholar
• Kreutzer, S., C. Burow, M. Dietze, M. Fuchs, C. Schmidt, M. Fischer, J. Friedrich, S. Riedesel, M. Autzen, and D. Mittelstrass. 2020. Luminescence: Comprehensive luminescence dating data analysis. R package version 0.9.10. Accessed July 28, 2021. https://CRAN.R-project.org/package=Luminescence.
   Google Scholar
• Kreutzer, S., C. Schmidt, M. C. Fuchs, M. Dietze, M. Fischer, and M. Fuchs. 2012. Introducing an R package for luminescence dating analysis. Ancient TL 30:1–8.
   Google Scholar
• Kruczkowska, B., M. Błaszkiewicz, J. Jonczak, Ł. Uzarowicz, P. Moska, A. Brauer, A. Bonk, and M. Słowiński. 2020. The Late Glacial pedogenesis interrupted by aeolian activity in central Poland—Records from the Lake Gościąż catchment. Catena 185:104286. doi: 10.1016/j.catena.2019.104286.
   Web of Science ®Google Scholar
• Krüger, S., and M. Damrath. 2020. In search of the Bølling-Oscillation: A new high resolution pollen record from the locus classicus Lake Bølling, Denmark. Vegetation History and Archaeobotany 29 (2):189–211. doi: 10.1007/s00334-019-00736-3.
   Web of Science ®Google Scholar
• Kurkowski, S., and W. Popielski. 1991. Szczegółowa mapa geologiczna Polski w skali 1:50 000, arkusz Gorzkowice wraz z objaśnieniami [Detailed geological map of Poland in scale 1:50 000, sheet Gorzkowice with explanations]. Warsaw, Poland: PIG.
   Google Scholar
• Lea, P. D. 1990. Pleistocene periglacial aeolian deposits in southwestern Alaska: Sedimentary facies and depositional processes. Journal of Sedimentary Petrology 60:582–91. doi: 10.1306/212F91F1-2B24-11D7-8648000102C1865D.
   Google Scholar
• Manikowska, B. 1991. Vistulian and Holocene aeolian activity, pedostratigraphy and relief evolution in central Poland. Zeitschrift für Geomorphologie N.F., Supplmentband 90:131–41.
   Google Scholar
• Manikowska, B. 1995. Aeolian activity differentation in the area of Poland during the period 20-8 ka BP. Biuletyn Peryglacjalny 34:125–66.
   Google Scholar
• Manikowska, B. 2002. Fossil paleosols and pedogenetic periods in the evolution of central Poland environment after the Wartian Glaciation. In Paleopedology problems in Poland, ed. B. Manikowska, K. Konecka-Betley, and R. Bednarek, 165–212. Łódź, Poland: Łódzkie Towarzystwo Naukowe.
   Google Scholar
• Marks, L., J. Dzierżek, R. Janiszewski, J. Kaczorowski, L. Lindner, A. Majecka, M. Makos, M. Szymanek, A. Tołoczko-Pasek, and B. Woronko. 2016. Quaternary stratigraphy and palaeogeography of Poland. Acta Geologica Polonica 66 (3):410–34. doi: 10.1016/j.quaint.2015.07.047.
   Web of Science ®Google Scholar
• Miall, A. D. 2006. The geology of fluvial deposits: Sedimentary facies, basin analysis and petroleum geology, 4th ed. Berlin: Springer.
   Google Scholar
• Mirosław-Grabowska, J., M. Obremska, E. Zawisza, J. Stańczak, M. Słowiński, and A. Mulczyk. 2020. Biological and geochemical indicators of climatic oscillations during the Last Glacial Termination, the Kaniewo palaeolake (central Poland). Ecological Indicators 114:106301. doi: 10.1016/j.ecolind.2020.106301.
   Web of Science ®Google Scholar
• Mol, J. 1997. Fluvial response to Weichselian climate changes in the Niederlausitz (Germany). Journal of Quaternary Science 12 (1):43–60. doi: 10.1002/(SICI)1099-1417(199701/02)12:1<43::AID-JQS291>3.0.CO;2-0.
   Web of Science ®Google Scholar
• Moska, P. 2019. Luminescence dating of Quaternary sediments—Some practical aspects. Studia Quaternaria 36:161–69. doi: 10.24425/sq.2019.126387.
   Web of Science ®Google Scholar
• Moska, P., A. Bluszcz, G. Poręba, K. Tudyka, G. Adamiec, A. Szymak, and A. Przybyła. 2021. Luminescence dating procedures at Gliwice luminescence dating laboratory. Geochronometria 48 (1):1–15. doi: 10.2478/geochr-2021-0001.
   Web of Science ®Google Scholar
• Moska, P., Z. Jary, R. J. Sokołowski, G. Poręba, J. Raczyk, M. Krawczyk, J. Skurzyński, P. Zieliński, A. Michczyński, K. Tudyka, et al. 2020. Chronostratigraphy of Late Glacial aeolian activity in SW Poland—A case study from the Niemodlin Plateau. Geochronometria 47 (1):124–37. doi: 10.2478/geochr-2020-0015.
   Web of Science ®Google Scholar
• Moska, P., R. J. Sokołowski, Z. Jary, P. Zieliński, J. Raczyk, A. Szymak, M. Krawczyk, J. Skurzyński, G. Poręba, M. Łopuch, et al. 2021. Stratigraphy of the Late Glacial and Holocene aeolian series in different sedimentary zones related to the Last Glacial maximum in Poland. Quaternary International 630:65–83. doi: 10.1016/j.quaint.2021.04.004.
   Web of Science ®Google Scholar
• Murray, A. S., and A. G. Wintle. 2000. Luminescence dating of quartz using an improved single-aliquot regenerative-dose protocol. Radiation Measurements 32 (1):57–73. doi: 10.1016/S1350-4487(99)00253-X.
   Web of Science ®Google Scholar
• Nowaczyk, B. 1986. Wiek wydm, ich cechy granulometryczne i strukturalne a schemat cyrkulacji atmosferycznej w Polsce w późnym vistulianie i holocenie [The age of dunes, their textural and structural properties against atmospheric circulation pattern of Poland during the Late Vistulian and Holocene]. In Seria Geografia, vol. 28, ed. A. Jędrzejczak, 1–245. Poznań, Poland: Wyd. Naukowe UAM.
   Google Scholar
• Nowaczyk, B. 2000. Development of dunes and eolian cover sands in Poland in the Late Vistulian and Holocene. In Polish geography: Problems, researches, applications, ed. Z. Chojnicki and J. J. Parysek, 133–51. Poznań, Poland: Bogucki Wyd. Naukowe S.C.
   Google Scholar
• Petera-Zganiacz, J., and D. Dzieduszyńska. 2017. Palaeoenvironmental proxies for permafrost presence during the Younger Dryas, central Poland. Permafrost and Periglacial Processes 28 (4):726–40. doi: 10.1002/ppp.1956.
   Web of Science ®Google Scholar
• Poręba, G., K. Tudyka, A. Walencik-Łata, and A. Kolarczyk. 2020. Bias in 238U decay chain members measured by γ-ray spectrometry due to 222Rn leakage. Applied Radiation and Isotopes: Including Data, Instrumentation and Methods for Use in Agriculture, Industry and Medicine 156:108945. doi: 10.1016/j.apradiso.2019.108945.
   Web of Science ®Google Scholar
• Prescott, J. R., and L. G. Stephan. 1982. The contribution of cosmic radiation to the environmental dose for thermoluminescence dating. In Latitude, altitude and depth dependencies TLS II-1, PACT 6, 17–25 16–25. Council of Europe.
   Google Scholar
• Rasmussen, S. O., M. Bigler, S. P. Blockley, T. Blunier, S. L. Buchardt, H. Clausen, I. Cvijanovic, D. Dahl-Jensen, S. J. Johnsen, H. Fischer, et al. 2014. A stratigraphic framework for abrupt climatic changes during the Last Glacial period based on three synchronized Greenland ice-core records: Refining and extending the INTIMATE event stratigraphy. Quaternary Science Reviews 106:14–28. doi: 10.1016/j.quascirev.2014.09.007.
   Web of Science ®Google Scholar
• Rdzany, Z. 2009. Rekonstrukcja przebiegu zlodowacenia warty w regionie łódzkim [Reconstruction of the course of theWarta Glaciation in the Łódź region]. Łódź, Poland: Wydawnictwo Uniwersytetu Łódzkiego.
   Google Scholar
• Reimer, P. J., W. E. N. Austin, E. Bard, A. Bayliss, J. Blackwell, C. Bronk Ramsey, P. M. Grootes, M. Butzin, H. Cheng, R. L. Edwards, et al. 2020. The IntCal20 Northern hemisphere radiocarbon age calibration curve (0-55 cal kBP). Radiocarbon 62 (4):725–57. doi: 10.1017/RDC.2020.41.
   Web of Science ®Google Scholar
• Retallack, G. J. 2001. Soils of the past: An introduction to paleopedology, 2nd ed. New York: Blackwell Science.
   Google Scholar
• Roman, M., D. Dzieduszyńska, and J. Petera-Zganiacz. 2014. Łódź region and its northern vicinity under Vistulian Glaciation conditions. Quaestiones Geographicae 33 (3):155–63. doi: 10.2478/quageo-2014-0038.
   Google Scholar
• Rotnicki, K., J. Rotnicka, and Z. Młynarczyk. 2005. Szczegółowa mapa geologiczna Polski w skali 1:50 000, arkusz Trąbczyn wraz z objaśnieniami [Detailed geological map of Poland in scale 1:50 000, sheet Trąbczyn with explanations]. Warsaw, Poland: PIG.
   Google Scholar
• Schirmer, W. 1999. Dune phases and fossil soils in the European sand belt. In Dunes and fossil soils: GeoArchaeo-Rhein, vol. 3, ed. W. Schirmer, 11–42. Münster, LIT Verlag.
   Google Scholar
• Schwan, J. 1986. The origin of horizontal alternating bedding in Weichselian aeolian sands in northwestern Europe. Sedimentary Geology 49 (1–2):73–108. doi: 10.1016/0037-0738(86)90016-3.
   Web of Science ®Google Scholar
• Sewerniak, P., M. Jankowski, and M. Dąbrowski. 2017. Effect of topography and deforestation on regular variation of soils on inland dunes in the Toruń Basin (N Poland). Catena 149:318–30. doi: 10.1016/j.actao.2017.06.003.
   Web of Science ®Google Scholar
• Sharp, R. P. 1963. Wind ripples. The Journal of Geology 71 (5):617–36. doi: 10.1086/626936.
   Web of Science ®Google Scholar
• Sitzia, L., P. Bertran, J.-J. Bahain, M. D. Bateman, M. Hernandez, H. Garon, G. de Lafontaine, N. Mercier, C. Leroyer, A. Queffelec, et al. 2015. The Quaternary coversands of southwest France. Quaternary Science Reviews 124:84–105. doi: 10.1016/j.quascirev.2015.06.019.
   Web of Science ®Google Scholar
• Tolksdorf, J. F., and K. Kaiser. 2012. Holocene aeolian dynamics in the European sand‐belt as indicated by geochronological data. Boreas 41 (3):408–21. doi: 10.1111/j.1502-3885.2012.00247.x.
   Web of Science ®Google Scholar
• Vandenberghe, D. A. G., C. Derese, C. Kasse, and P. Van Den Haute. 2013. Late Weichselian (fluvio-) aeolian sediments and Holocene drift-sands of the classic type locality in Twente (E Netherlands): A high-resolution dating study using optically stimulated luminescence. Quaternary Science Reviews 68:96–113. doi: 10.1016/j.quascirev.2013.02.009.
   Web of Science ®Google Scholar
• Vandenberghe, J., C. Kasse, S. J. P. Bohncke, and S. Kozarski. 1994. Climate-related river activity at the Weichselian–Holocene transition: A comparative study of the Warta and Maas rivers. Terra Nova 6 (5):476–85. doi: 10.1111/j.1365-3121.1994.tb00891.x.
   Web of Science ®Google Scholar
• Van der Hammen, T., and T. A. Wijmstra. 1971. The Upper Quaternary of the Dinkel Valley (Twente, Eastern Overijssel, The Netherlands). Mededelingen Rijks Geologische Dienst 22:55–212.
   Google Scholar
• Van Huissteden, J., J. Vandenberghe, T. Van Der Hammen, and W. Laan. 2000. Fluvial and aeolian interaction under permafrost condition: Weichselian Late Pleniglacial, Twente, Eastern Netherlands. Catena 40 (3):307–21. doi: 10.1016/S0341-8162(00)00085-0.
   Web of Science ®Google Scholar
• Wachecka-Kotkowska, L. 2015. Rozwój rzeźby obszaru między Piotrkowem Trybunalskim, Radomskiem a Przedborzem w czwartorzędzie [Development of land relief between Piotrków Trybunalski, Radomsko and Przedbórz in the Quaternary]. Łodź, Poland: Wydawnictwo Uniwersytetu Łódzkiego.
   Google Scholar
• Wachecka-Kotkowska, L., and M. Ludwikowska-Kędzia. 2007. Plenivistuliański poziom wysoki w dolinach rzek Luciąży (Równina Piotrkowska/Wzgórza Radomszczańskie) i Belnianki (Góry Świętokrzyskie). Porównanie cech strukturalnych i teksturalnych osadów [Plenivistulian high level in the valleys of the Luciaza rivers (Piotrkowska Plain/Radomszczańskie Hills) and Belnianki (Świętokrzyskie Mountains): Comparison of the structural and textural features of sediments]. Acta Geographica Lodziensia 93:107–32.
   Google Scholar
• Walker, M. J. C., M. Berkelhammer, S. Bjorck, L. C. Cwynar, D. A. Fisher, A. J. Long, J. J. Lowe, R. N. Newnham, S. O. Rasmussen, and H. Weiss. 2012. Formal subdivision of the Holocene series/epoch: A discussion paper by a working group of INTIMATE (integration of ice-core, marine and terrestrial records) and the subcommission on quaternary stratigraphy (International Commission on Stratigraphy). Journal of Quaternary Science 27 (7):649–59. doi: 10.1002/jqs.2565.
   Web of Science ®Google Scholar
• Wysota, W., P. Molewski, and R. J. Sokołowski. 2009. Record of the Vistula ice lobe advances in the Late Weichselian glacial sequence in north-central Poland. Quaternary International 207 (1–2):26–41. doi: 10.1016/j.quaint.2008.12.015.
   Google Scholar
• Zeeberg, J. J. 1998. The European sand belt in eastern Europe—And comparison of Late Glacial dune orientation with GCM simulation results. Boreas 27 (2):127–39. doi: 10.1111/j.1502-3885.1998.tb00873.x.
   Web of Science ®Google Scholar
• Zieliński, P. 2016. Regionalne i lokalne uwarunkowania późnovistuliańskiej depozycji eolicznej w środkowej części europejskiego pasa piaszczystego [Regional and local conditions of the Late Vistulian aeolian deposition in the central part of the European Sand Belt]. Lublin, Poland: Wydawnictwo UMCS.
   Google Scholar
• Zieliński, P., and K. Issmer. 2008. Propozycja kodu genetycznego osadów środowiska eolicznego. [The proposal of genetic code of aeolian deposits]. Przegląd Geologiczny 56:67–72.
   Google Scholar
• Zieliński, P., R. J. Sokołowski, S. Fedorowicz, B. Woronko, B. Hołub, M. Jankowski, M. Kuc, and M. Tracz. 2016. Depositional conditions on an alluvial fan at the turn of Weichselian and Holocene—Case study of Żmigród Basin (SW Poland). Geologos 22 (2):105–20. doi: 10.1515/logos-2016-0012.
   Google Scholar
• Zieliński, P., R. J. Sokołowski, S. Fedorowicz, and I. Zaleski. 2014. Periglacial structures within fluvio-aeolian successions of the end of the Last Glaciation—Examples from SE Poland and NW Ukraine. Boreas 43 (3):712–21. doi: 10.1111/bor.12052.
   Web of Science ®Google Scholar
• Zieliński, P., R. J. Sokołowski, M. Jankowski, K. Standzikowski, and S. Fedorowicz. 2019. The climatic control of sedimentary environment changes during the Weichselian—An example from the Middle Vistula Region (eastern Poland). Quaternary International 501:120–34. doi: 10.1016/j.quaint.2018.04.036.
   Web of Science ®Google Scholar
• Zieliński, P., R. J. Sokołowski, B. Woronko, M. Jankowski, S. Fedorowicz, I. Zaleski, A. Molodkov, and P. Weckwerth. 2015. The depositional conditions of the fluvio-aeolian succession during the last climate minimum based on the examples from Poland and NW Ukraine. Quaternary International 386:30–41. doi: 10.1016/j.quaint.2014.08.013.
   Web of Science ®Google Scholar
• Ziomek, J. 1989. Szczegółowa mapa geologiczna Polski w skali 1:50 000, arkusz Bełchatów wraz z objaśnieniami [Detailed geological map of Poland in scale 1:50 000, sheet Bełchatów with explanations]. Warsaw, Poland: PIG.
   Google Scholar
• Zolitschka, B., P. Francus, A. E. Ojala, and A. Schimmelmann. 2015. Varves in lake sediments—A review. Quaternary Science Reviews 117:1–41. doi: 10.1016/j.quascirev.2015.03.019.
   Web of Science ®Google Scholar