Reconstruction of sediment provenance and transport processes from the surface textures of quartz grains from Late Pleistocene sandurs and an ice-marginal valley in NW Poland

Barbara Woronko 1 , Małgorzata Pisarska-Jamroży 2 , and A.J. (Tom) van Loon 3 , 4
  • 1 Faculty of Geology, University of Warsaw, Żwirki i Wigury 93, 02-089 Warsaw, Poland;
  • 2 Institute of Geology, Adam Mickiewicz University, Maków Polnych 16, 61-606 Poznań, Poland;
  • 3 Institute of Geology, Adam Mickiewicz University, Maków Polnych 16, 61-606 Poznań, Poland
  • 4 Emeritus

Abstract

During the Pomeranian phase of the Weichselian glaciation (~17-16 ka), the Toruń-Eberswalde ice-marginal valley (NW Poland and easternmost Germany) drained water from the Pomeranian ice sheet, while intensive aeolian processes took place across Europe in the foreland of the Scandinavian ice sheet (‘European Sand Belt’). The micromorphology of the quartz grains in the Toruń-Eberswalde ice-marginal valley shows no traces of these aeolian processes, or only vague signs of aeolian abrasion. This is unique among the aeolian sediments in other Pleistocene ice-marginal valleys in this part of Europe. The study of the surfaces of the quartz grains shows that the supply of grains by streams from the south was minimal, which must be ascribed to the climate deterioration during the Last Glacial Maximum, which resulted in a decrease of the discharge of these extraglacial rivers to the ice-marginal valley.

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  • Antczak-Górka, B., 2005. Głazy rzeźbione przez wiatr jako wskaźniki różnowiekowych stref peryglacjalnych ostatniego zlodowacenia w Polsce Zachodniej [Wind-polished stones as indicators of last-glaciation periglacial zones of various ages in western Poland]. UAM Press (Poznań), 209 pp.

  • Böse, M. & Górska, M., 1995. Lithostratigraphical studies in the outcrop at Ujscie, Toruń-Eberswalde Pradolina, western Poland. Eiszeitalter und Gegenwart 45, 1-14.

  • Cailleux, A., 1942. Les actionnes éoliennes périglaciaires en Europe. Mémoires de la Société Géologique de France 41, 176 pp.

  • Dietzel, M., 2005. Impact of cyclic freezing on precipitation of silica in Me-SiO2-H2O systems and geochemical implications for cryosoils and sediments. Chemical Geology 216, 79-88.

  • Galon, R., 1961. Morphology of the Noteć-Warta (or Toruń- Eberswalde) ice marginal streamway. Prace Geograficzne 29, 7-115.

  • Galon, R., 1968. New facts and problems pertaining to the origin of the Notec-Warta Pradolina and the valleys linked with it. Przegląd Geograficzny 40, 307-315.

  • Goździk, J., 2007. The Vistulian aeolian succession in central Poland. Sedimentary Geology 193, 211-220.

  • Hart, J.K., 2006. An investigation of subglacial processes at the microscale from Briksdalsbreen, Norway. Sedimentology 53, 125-146.

  • Iverson, N.R., Hooyer, T.S. & Hooke, R.L., 1996. A laboratory study of sediment deformation: stress heterogeneity and grain-size evolution. Annals of Glaciology 22, 167-175.

  • Kamińska, R., Konecka-Betley, K. & Mycielska-Dowgiałło, E., 1986. The Liszyno dune in the Vistula Valley (east of Płock). Biuletyn Peryglacjalny 31, 141-162.

  • Kasse, C., 1997. Cold-climate aeolian sand-sheet formation in North-Western Europe (c. 14-12.4 ka); a response to permafrost degradation and increased aridity. Permafrost and Periglacial Processes 8, 295-311.

  • Kasse, C., Vandenberghe, J., van Huissteden, J., Bohncke, S.J.P. & Bos, J.A.A., 2003. Sensitivity of Weichselian fluvial systems to climate change (Nochten mine, eastern Germany). Quaternary Science Reviews 22, 2141-2156.

  • Kaulbarsz, D., Jurys, L., Kramarska, R. & Słodkowska, B., 2008. Orłowo cliff - geology, glaciotectonics and palynological study of Neogene deposits. [In:] S. Lisicki (Ed.): Quaternary of the Gulf of Gdańsk and Lower Vistula regions in Northern Poland: sedimentary environments, stratigraphy and palaeogeography. PIG Press, Warsaw, 91-92.

  • Koster, E.A., 1988. Ancient and modern cold-climate aeolian sand deposition: a review. Journal of Quaternary Science 3, 69-83.

  • Kozarski, S., 1965. Zagadnienie drogi odpływu wód pradolinnych z zachodniej części Pradoliny Noteci-Warty [The problem of the outflow from the western part of Noteć-Warta ice-marginal valley]. Prace Komisji Geograficzno-Geologicznej 5, 87 pp.

  • Kozarski, S., 1986. Skale czasu a rytm zdarzeń zdarzeń geomorfologicznych vistulianu na Niżu Polskim [Time scales and rhythm of geomorphological events during the Vistulian in the Polish Lowlands]. Czasopismo Geograficzne 57, 247-270.

  • Kozarski, S., 1991. Litostratygrafia górnego plenivistulianu Niziny Wielkopolskiej w granicach ostatniego zlodowacenia: nowe dane i interpretacje [Lithostratigraphy of the upper Plenivistulian in the Wielkopolska Lowland during the last glaciation: new data and interpretations]. [In:] A. Kostrzewski (Ed.): Geneza, litologia i stratygrafia utworów czwartorzędowych [Genesis, lithology and stratigraphy of Quaternary sediments]. Geografia 50, 471-496.

  • Kozarski, S. & Nowaczyk, B., 1985. Stratygrafia osadów plejstoceńskich w profilu Ujście nad Notecią [Stratigraphy of the Pleistocene sediments at Ujście]. Sprawozdanie Poznańskiego Towarzystwa Przyjaciół Nauk 101, 49-51.

  • Lindé, K., 1984. Scanning electron microscope studies of different sands and silts. Acta Universitatis Upsaliensis 748, 1-10.

  • Lindé, K. & Mycielska-Dowgiałło, E., 1980. Some experimentally produced microtextures on grain surfaces of quartz sand. Geografiska Annaler 62A, 171-184.

  • Mahaney, W.C., 1995. Pleistocene and Holocene glacier thicknesses and/or transport histories inferred from microtextures and quartz particles. Boreas 24, 293-304.

  • Mahaney, W.C., 2002. Atlas of sand grain surface textures and applications. Oxford University Press, Oxford, 237 pp.

  • Manikowska, B., 1991. Vistulian and Holocene aeolian activity, pedostratigraphy and relief evolution in central Poland. Zeitschrift für Geomorphologie 90, 131-141.

  • Marks, L., 2012. Timing of the Late Vistulian (Weichselian) glacial phases in Poland. Quaternary Science Reviews 44, 81-88.

  • Miall, A.D., 1978. Lithofacies types and vertical profile models in braided river deposits: a summary. [In:] A.D. Miall (Ed.): Fluvial sedimentology. Canadian Society of Petroleum Geologists 5, 597-604.

  • Mojski, J.E., 2005. Ziemie polskie w czwartorzędzie. Zarys morfogenezy [Poland in the Quaternary. Morphogenesis]. PIG Press, Warsaw, 404 pp.

  • Mol, J., Vandenberghe, J. & Kasse, C., 2000. River response to variations of periglacial climate in mid-latitude Europe. Geomorphology 33, 131-148.

  • Mycielska-Dowgiałło, E., 1993. Estimates of Late Glacial and Holocene aeolian activity in Belgium, Poland and Sweden. Boreas 22, 165-170.

  • Mycielska-Dowgiałło, E., 2001. Wpływ warunków klimatycznych na cechy strukturalne i tekstualne osadów mineralnych [The influence of climatic conditions on structural and textual features of mineral deposits]. [In:] A. Karczewski & Z. Zwoliński (Eds): Funkcjonowanie geosystemów w zróżnicowanych warunk ach morfoklimatycznych - monitoring, ochrona, edukacja [The functioning of geosystems under different morphoclimatic conditions - monitoring, protection, education]. Wydawnictwo Naukowe UAM, Poznań, 377-394.

  • Mycielska-Dowgiałło, E. & Woronko, B., 1998. Analiza obtoczenia i zmatowienia powierzchni ziarn kwarcowych frakcji piaszczystej i jej wartość interpretacyjna [Rounding and frosting analysis of quartz sand-grain surfaces and their significance for interpretations]. Przegląd Geologiczny 46, 1275-1281.

  • Mycielska-Dowgiałło, E. & Woronko, B., 2004. The degree of aeolization of Quaternary deposits in Poland as a tool for stratigraphic interpretation. Sedimentary Geology 168, 149-163.

  • Pisarska-Jamroży, M., 2015. Factors controlling sedimentation in the Toruń-Eberswalde ice-marginal valley during the Pomeranian phase of the Weichselian glaciation: an overview. Geologos 21, 1-29.

  • Pisarska-Jamroży, M. & Zieliński, T., 2011. Genesis of a till/sand breccia (Pleistocene, Noteć Valley near Atanazyn, central Poland). Sedimentary Geology 236, 109-116.

  • Pisarska-Jamroży, M. & Zieliński, T., 2014. Pleistocene sandur rhythms, cycles and megacycles: Interpretation of depositional scenarios and palaeoenvironmental conditions. Boreas 43, 330-348.

  • Pisarska-Jamroży, M., van Loon, A.J., Woronko, B. & Sternal, B., 2015a. Heavy-mineral analysis as a tool to trace the source areas of sediments in an ice-marginal valley, with an example from the Pleistocene in NW Poland. Netherlands Journal of Geosciences 94, 185-200.

  • Pisarska-Jamroży, M., van Loon, A.J. & Woronko, B., 2015b. Sorting of heavy minerals in sediments deposited at a high accumulation rate, with examples from sandurs and an ice-marginal valley in NW Poland. GFF, 137, 126-140

  • Rose, K.C. & Hart, J.K., 2008. Subglacial comminution in the deforming bed: inferences from SEM analysis. Sedimentary Geology 203, 87-97.

  • Traczyk, A. & Woronko, B., 2010. Historia zlodowacenia doliny Łomnicy w Karkonoszach w zapisie mikromorfologii powierzchni ziarn kwarcowych [The history of glaciation of the Łomnica Valley at Karkonosze as shown by the records of the quartz-grain surface micromorphology]. Przegląd Geologiczny 58, 1182-1191.

  • Tricart, J., 1965. Principes et méthodes de géomorphologie. Masson, Paris, 496 pp.

  • Tylman, K., Wysota, W., Adamiec, G., Molewski, P. & Chabowski, M., 2013. Relict sand wedges in glacial till sequences: indicators of late Pleistocene periglacial environment in north-central Poland. [In:] Palaeolandscapes from Saalian to Weichselian. South Eastern Lithuania. Abstracts of International Field Symposium, 2013, Vilnius-Trakai-Lithuania, 95.

  • van Huissteden, J., Schwan, J.C.G. & Bateman, M.D., 2001. Environmental conditions and paleowind directions at the end of the Weichselian Late Pleniglacial recorded in aeolian sediments and geomorphology (Twente, Eastern Netherlands). Netherlands Journal of Geosciences 80, 1-18.

  • van Vliet-Lanoë, B., 2010. Frost action. [In:] G. Stoops, V. Marcellino & F. Mees (Eds): Interpretation of micromorphological features of soils and regoliths. Elsevier, London, 81-108.

  • Ward, J.H., 1963. Hierarchical grouping to optimize an objective function. Journal of the American Statistical Association 58, 236-244.

  • Weckwerth, P., 2013. Procesy fluwialne toruńskiego basenu sedymentacyjnego podczas zlodowacenia wisły [Fluvial processes of the Toruń Basin during the Weichselian glaciation]. Nicolaus Copernicus University Press, Toruń, 205 pp.

  • Weckwerth, P. & Chabowski, M., 2013. Heavy minerals as a tool to reconstruct river activity during the Weichselian glaciation (Toruń Basin, Poland). Geologos 19, 25-46.

  • Weckwerth, P. & Pisarska-Jamroży, M., 2015. Periglacial and fluvial factors controlling the sedimentation of Pleistocene breccia, NW Poland. Geografiska Annaler, 97A, 415-430.

  • Woronko, B., 2007. Typy mikromorfologii powierzchni ziarn kwarcowych frakcji pylastej i ich wartość interpretacyjna [Micromorphology types of quartz grains surface of silt fraction of their interpretative meaning]. [In:] E. Mycielska-Dowgiałło & J. Rutkowski (Eds): Badania cech teksturalnych osadów czwartorzędowych i wybrane metody oznaczania ich wieku [Textural features of Quaternary sediments and some methods to determine their age]. SWPR Press, Warsaw, 181-204.

  • Woronko, B., 2012. Micromorphology of quartz grains as a tool in the reconstruction of periglacial environment. [In:]: P. Churski (Ed): Contemporary issues in Polish geography, Wydawnictwo Naukowe UAM, Poznań, 111-131.

  • Woronko, B. & Hoch, M. 2011. The development of frost-weathering microstructures on sand-sized quartz grains: Examples from Poland and Mongolia. Permafrost and Periglacial Processes 22, 214-227.

  • Woronko, B., Szwarczewski, P. & Bujak, P., 2011. Zapis zmian środowiska przyrodniczego w dolinie rzeki Mlecznej w rejonie wczesnośredniowiecznego grodziska Piotrówka w Radomiu na podstawie charakteru powierzchni ziarn kwarcowych frakcji piaszczystej [The record of environmental changes in the Mleczna river valley in the region of the early medieval Piotrówka settlement at Radom, based on the nature of the surface of sand-sized quartz grains]. [In:] A. Buko, D. Główka & M. Trzeciecki (Eds): Radom: korzenie miasta i regionu. Radomski zespół osadniczy w dolinie rzeki Mlecznej. Wyniki badań interdyscyplinarnych [Radom: the roots of the city and the region. The Radom settlement in the valley of the Mleczna river. Results of interdisciplinary investigations]. Instytut Archeologii i Etnologii PAN 2, Warsaw, 149-167.

  • Woronko, B., Rychel, J., Karasiewicz, M.K., Ber, A., Krzywicki, T., Marks, L. & Pochocka-Szwarc, K., 2013. Heavy and light minerals as a tool for reconstructing depositional environments: an example from the Jałówka site (northern Podlasie region, NE Poland). Geologos 19, 47-66.

  • Woronko, B. & Pisarska-Jamroży, M. in press. Micro-scale frost weathering of sand-sized quartz grains. Permafrost and Periglacial Processes. DOI: 10.1002/ppp.1855.

  • Zeeberg, J.J., 1998. The European sand belt in eastern Europe - and comparison of Late Glacial dune orientation with GCM simulation results. Boreas 27, 127-139.

  • Zieliński, P., Sokołowski, R.J., Woronko, B., Jankowski, M., Fedorowicz, S., Zaleski, I., Molodkov, A. & Weckwerth, P., in press. The depositional conditions of the fluvio-aeolian succession during the last climate minimum based on the examples from Poland and NW Ukraine. Quaternary International, doi. org/10.1016/j.quaint.2014.08.013.

  • Zieliński, T. & Pisarska-Jamroży, M., 2012. Jakie cechy litologiczne warto kodować, a jakie nie? [Which features of deposits should be included in a code and which not?]. Przegląd Geologiczny 60, 387-397.

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