Age and sedimentological features of fluvial series in the Toruń Basin and the Drwęca Valley (Poland)

[1] Bøtter-Jensen L and Duller GAT, 1992. A new system for measuring optically stimulated luminescence from quartz samples. Nuclear Tracks and Radiation Measurements 20(4): 549–553, DOI 10.1016/1359-0189(92)90003-E. http://dx.doi.org/10.1016/1359-0189(92)90003-E10.1016/1359-0189(92)90003-ESearch in Google Scholar

[2] Boulton GS, Dongelmans P, Punkari M and Broadgate M, 2001. Palaeoglaciology of an ice sheet through a glacial cycle: the European ice sheet through the Weichselian. Quaternary Science Reviews 20(4): 591–625, DOI 10.1016/S0277-3791(00)00160-8. http://dx.doi.org/10.1016/S0277-3791(00)00160-810.1016/S0277-3791(00)00160-8Search in Google Scholar

[3] Cailleux A, 1942. Les actiones éoliennes périglaciaires en Europe. Mémoire de la société Géologique de France 41: 176pp (in French). Search in Google Scholar

[4] Cant DJ and Walker RG, 1976. Development of a braided-fluvial facies model for the Devonian Battery Point Sandstone, Quebec. Canadian Journal of Earth Sciences 13: 102–119, DOI 10.1139/e76-010 http://dx.doi.org/10.1139/e76-01010.1139/e76-010Search in Google Scholar

[5] Cant DJ and Walker RG, 1978. Fluvial processes and facies sequences in the sandy braided South Saskatchewan River, Canada. Sedimentology 25(5): 625–648, DOI 10.1111/j.1365-3091.1978.tb00323.x. http://dx.doi.org/10.1111/j.1365-3091.1978.tb00323.x10.1111/j.1365-3091.1978.tb00323.xSearch in Google Scholar

[6] Collinson J, Mountney N and Thompson D, 2006. Sedimentary structures, 3. Terra Publishing Harpenden, England: 304pp. Search in Google Scholar

[7] Duller GAT, 2007. Assessing the error on equivalent dose estimates derived from single aliquot regenerative dose measurements. Ancient TL 25: 15–24. Search in Google Scholar

[8] Folk RL and Ward WC, 1957. Brazos River bar: a study in the significance of grain size parameters. Journal of Sedimentary Petrology 27(1): 3–26. 10.1306/74D70646-2B21-11D7-8648000102C1865DSearch in Google Scholar

[9] Goździk J, 1980. Zastosowanie morfometrii i graniformametrii do badań osadów w kopalni węgla brunatnego Bełchatów. Studia Regionalne IV(IX). PWN Warszawa-Łódź: 101–114 (in Polish). Search in Google Scholar

[10] Houmark-Nielsen M, 2007. Extent and age of Middle and Late Pleistocene glaciations and periglacial episodes in southern Jylland, Denmark. Bulletin of the Geological Society of Denmark 55: 9–35. 10.37570/bgsd-2007-55-02Search in Google Scholar

[11] Houmark-Nielsen M, 2010. Extent, age and dynamics of Marine Isotope Stage 3 glaciations in the southwestern Baltic Basin. Boreas 39(2): 343–359, DOI 10.1111/j.1502-3885.2009.00136.x. http://dx.doi.org/10.1111/j.1502-3885.2009.00136.x10.1111/j.1502-3885.2009.00136.xSearch in Google Scholar

[12] Houmark-Nielsen M and Kjær KH, 2003. Southwest Scandinavia 40-15 ka BP: Plaleogeography and environmental change. Journal of Quaternary Science 18(8): 769–786, DOI 10.1002/jqs.802. http://dx.doi.org/10.1002/jqs.80210.1002/jqs.802Search in Google Scholar

[13] Krinsley DH and Doornkamp JC, 1973. Atlas of quartz sand surface textures. Cambrige Univ. Press. Search in Google Scholar

[14] Krinsley DH and Takahashi T, 1962. The surface textures of sand grains: an application of electron microscopy: glaciation. Science 138(3546): 1262–1264, DOI 10.1126/science.138.3546.1262. http://dx.doi.org/10.1126/science.138.3546.126210.1126/science.138.3546.1262Search in Google Scholar

[15] Krinsley DH, Takahashi T, Silberman ML and Newman WS, 1964. Transportation of sand grains along the Atlantic shore Long Island, New York: An application of electron microscopy. Marine Geology 2: 100–120, DOI 10.1016/0025-3227(64)90029-5. http://dx.doi.org/10.1016/0025-3227(64)90029-510.1016/0025-3227(64)90029-5Search in Google Scholar

[16] Krumbein WC, 1941. Measurement and geological significance of shape and roundness of sedimentary particles. Journal of Sedimentary Petrology 11: 64–72, DOI 10.1306/D42690F3-2B26-11D7-8648000102C1865D. 10.1306/D42690F3-2B26-11D7-8648000102C1865DSearch in Google Scholar

[17] Latałowa M, 2003. Późny Vistulian (Late Vistulian). In: Dybowa-Jachowicz S and Sadowska A, eds, Palinologia. Wyd. PAN Instytut Botaniki, Kraków: 266–273 (in Polish). Search in Google Scholar

[18] Makowska A, 1979. Interglacjał eemski w Dolinie Dolnej Wisły (Eemian interglacial In the Valley of Lower Vistula River). Studia Geologica Polonica 63: 90pp (in Polish). Search in Google Scholar

[19] Manickam S and Barbaroux L, 1987. Variations in the surface texture of suspended quartz grains in the Loire river: An SEM study. Sedimentology 34(3): 495–510, DOI 10.1111/j.1365-3091.1987.tb00581.x. http://dx.doi.org/10.1111/j.1365-3091.1987.tb00581.x10.1111/j.1365-3091.1987.tb00581.xSearch in Google Scholar

[20] Margolis S and Kennett JP, 1971. Cenozoic, paleoglacial history of Antarctica, recrded in subarctic deep-sea cores. American Journal of Science 271: 1–36, DOI 10.2475/ajs.271.1.1. http://dx.doi.org/10.2475/ajs.271.1.110.2475/ajs.271.1.1Search in Google Scholar

[21] Marks L, 2010. Timing of the Late Vistulian (Weichselian) glacial phases in Poland. Quaternary Science Reviews (in press), DOI 10.1016/j.quascirev.2010.08.008. Search in Google Scholar

[22] Marren PM, 2005. Magnitude and frequency in proglacial rivers: a geomorphological and sedimentological perspective. Earth-Science Reviews 70(3–4): 203–251, DOI 10.1016/j.earscirev.2004.12.002 http://dx.doi.org/10.1016/j.earscirev.2004.12.00210.1016/j.earscirev.2004.12.002Search in Google Scholar

[23] Miall AD, 1978. Lithofacies types and vertical profile models in braided rivers: A summary. In: Miall AD, ed., Fluvial Sedimentology. Canadian Society of Petroleum Geologists, Memoir 5: 597–604. Search in Google Scholar

[24] Miall AD, 1985. Architectural-element analysis: a new metod of facies analysis applied to fluvial deposits. Earth-Science Reviews 22(4): 261–308, DOI 10.1016/0012-8252(85)90001-7. http://dx.doi.org/10.1016/0012-8252(85)90001-710.1016/0012-8252(85)90001-7Search in Google Scholar

[25] Molewski P, 2007. Neotektoniczne i glacidynamiczne uwarunkowania wykształcenia plejstocenu Wysoczyzny Kujawskiej (Neotectonic and glaciodynamic conditions for the formation of the Pleistocene of the Kujawy Moraine Plateau). Wydawnictwo Naukowe Uniwersytetu Mikołaja Kopernika, Toruń: 140pp (in Polish). Search in Google Scholar

[26] Morawska M and Morawski M, 2009. Formy po strumieniach lodowych w Polsce Zachodniej i Północno-Zachodniej — identyfikacja w rzeźbie. In: Kostrzewski A, ed., Geneza, litologia, stratygrafia utworów czwartorzędowych (Genesis, lithology and stratigraphy of Quaternary deposits). SGP, UAM Poznań, t. V (in Polish). Search in Google Scholar

[27] Murray AS and Wintle AG, 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. http://dx.doi.org/10.1016/S1350-4487(99)00253-X10.1016/S1350-4487(99)00253-XSearch in Google Scholar

[28] Mycielska-Dowgiałło E, 2007. Metody badań cech teksturalnych osadów klastycznych i wartość interpretacyjna wyników (Methods of researches of the textural features of clastic deposits and their interpretation value). In: Mycielska-Dowgiałło E and Rutkowski J, eds., Badania cech teksturalnych osadów czwartorzędowych i wybrane metody oznaczania ich wieku. WSWPR, Warszawa: 95–180 (in Polish). Search in Google Scholar

[29] Mycielska-Dowgiałło E and Woronko B, 1998. Analiza obtoczenia i zmatowienia powierzchni ziarn kwarcowych frakcji piaszczystej i jej wartość interpretacyjna (Rounding and frosting analysis of quarto grains of Sand fraction, and its interpretative value). Przegląd Geologiczny 46: 1275–1281 (in Polish). Search in Google Scholar

[30] Nanson GC and Knighton AD, 1996. Anabranching rivers: their cause, character and classification. Earth Surface Processes and Landforms 21(3): 217–239, DOI 10.1002/(SICI)1096-9837(199603)21:3<217::AID-ESP611>3.0.CO;2-U. http://dx.doi.org/10.1002/(SICI)1096-9837(199603)21:3<217::AID-ESP611>3.0.CO;2-U10.1002/(SICI)1096-9837(199603)21:3<217::AID-ESP611>3.0.CO;2-USearch in Google Scholar

[31] Oczkowski HL and Przegiętka K, 1998. Partial Matrix Doses for Thermoluminescence Dating. Physica Scripta 58(5): 534–537, DOI 10.1088/0031-8949/58/5/019. http://dx.doi.org/10.1088/0031-8949/58/5/01910.1088/0031-8949/58/5/019Search in Google Scholar

[32] Oczkowski HL, Przegiętka K, Lankauf KR and Szmańda JB, 2000. Gamma Spectrometry in Thermoluminescence Dating. Geochronometria 18: 63–68. Search in Google Scholar

[33] Olsen H, 1988. The architecture of a sandy braided-meandering river system: an example from the Lower Triassic Solling Formation (M. Buntsandstein) in W-Germany. Geologische Rundschau 77(3): 797–814, DOI 10.1007/BF01830186. http://dx.doi.org/10.1007/BF0183018610.1007/BF01830186Search in Google Scholar

[34] Ostrowska M, 2008. Wpływ środowiska fluwialnego na charakter powierzchni ziaren kwarcowych na przykładzie aluwiów rzeki Nurzec. Master’s thesis. WGSR UW. Warszawa (in Polish). Search in Google Scholar

[35] Punkari M, 1993. Modelling of the dynamics of the Scandinavian ice sheet using remote sensing and GIS methods. In: Aber JS, ed., Glaciotectonics and mapping glacial deposits. Canadian Plains Research Center. University of Regina: 232–250. Search in Google Scholar

[36] Salamon T and Zieliński T, 2010. Unusual development of sandur sedimentary succession, an example from the Pleistocene of S Poland. Geologos 16(2): 83–99, DOI 10.2478/v10118-009-0007-9. http://dx.doi.org/10.2478/v10118-009-0007-910.2478/v10118-009-0007-9Search in Google Scholar

[37] Smith ND, 1970. The braided stream depositional environment: comparison of the Platte River with some Silurian clastic rocks, North-Central Appalachians. Geological Society of America Bulletin 81(10): 2993–3014, DOI 10.1130/0016-7606(1970)81[2993:TBSDEC]2.0.CO;2. http://dx.doi.org/10.1130/0016-7606(1970)81[2993:TBSDEC]2.0.CO;2Search in Google Scholar

[38] Schwartz DE, 1978. Hydrology and current orientation analysis of braided-to-meandering transition: the Red River in Oklahoma and Texas, U.S.A. In: Miall AD, ed., Fluvial sedimentology. Canadian Society of Petroleum Geologists: 231–255. Search in Google Scholar

[39] Tunbridge IP, 1981. Sandy high-energy flood sedimentation some criteria for recognition, with an example from the Devonian of SW England. Sedimentary Geology 28(2): 79–95, DOI 10.1016/0037-0738(81)90058-0. http://dx.doi.org/10.1016/0037-0738(81)90058-010.1016/0037-0738(81)90058-0Search in Google Scholar

[40] Tunbridge IP, 1984. Facies model for a sandy ephemeral stream and clay playa complex: the Middle Devonian Trentishoe Formation of North Devon, UK. Sedimentology 31(5): 697–715, DOI 10.1111/j.1365-3091.1984.tb01231.x. http://dx.doi.org/10.1111/j.1365-3091.1984.tb01231.x10.1111/j.1365-3091.1984.tb01231.xSearch in Google Scholar

[41] Weckwerth P, 2004. Morfogeneza wybranych obszarów Kotliny Toruńskiej a problem jej roli w układzie hydrograficznym podczas górnego plenivistulianu (Morphogenesis selected areas of the Toruń Basin and their part in hydrographic network during upper plenivistulian). PhD thesis, UMK Toruń (in Polish). Search in Google Scholar

[42] Weckwerth P, 2007. Późnovistuliański rozwój sieci rzecznej w rejonie Kotliny Toruńskiej na tle struktur starszego podłoża (The river network development in the Toruń Basin in the Late Weichselian on the basis of older geological structures). In: Florek W, ed., Słupskie Prace Geograficzne 4: 143–156 (in Polish). Search in Google Scholar

[43] Weckwerth P, 2009a. Środowisko depozycji fluwialnej w stadiale głównym zlodowacenia Wisły — stanowisko Nowe Dąbie, południowo-zachodnia część Kotliny Toruńskiej (Fluvial depositional envinronment in the Main Stadial of Weichselian Glaciation. In: Pisarska-Jamroży M and Babiński Z, eds., Plejstoceńskie środowiska sedymentacyjne Pojezierza Pomorskiego, Wydawnictwo UKW, Bydgoszcz: 90–99 (in Polish). Search in Google Scholar

[44] Weckwerth P, 2009b. Warunki depozycji osadów plenivistuliańskiej rzeki roztokowej w Kotlinie Toruńskiej (Depositional conditions of Plenivistulian breided river in the Toruń Basin). In: Żarski M and Lisicki S, eds., XVI Konferencja Stratygrafia Plejstocenu Polski, Strefa marginalna lądolodu zlodowacenia warty i pojezierza plejstoceńskie na południowym Podlasiu: 135–138 (in Polish). Search in Google Scholar

[45] Weckwerth P, 2010. Evolution of the Toruń Basin in the Late Weichselian. Landform Analysis 14: 57–84. Search in Google Scholar

[46] Weckwerth P, Przegiętka KR and Chruścińska A, 2011. The OSL Age inversion of sand-bed braided river deposits in the Toruń Basin (Poland), submitted to Quaternary Geochronology. Search in Google Scholar

[47] Wintle AG and Murray AS, 2006. A review of quartz optically stimulated luminescence characteristics and their relevance in single-aliquot regeneration dating protocols. Radiation Measurements 41(4): 369–391, DOI 10.1016/j.radmeas.2005.11.001. http://dx.doi.org/10.1016/j.radmeas.2005.11.00110.1016/j.radmeas.2005.11.001Search in Google Scholar

[48] Włodek M, 1980. Młodszy plejstocen w rejonie Nakła nad Notecią(Younger Pleistocene in the area of Nakło on the Noteć). Przegląd Geologiczny 8: 453–456 (in Polish). Search in Google Scholar

[49] Woronko B, 2001. Znaczenie analizy obtoczenia i zmatowienia powierzchni ziarn kwarcowych frakcji piaszczystej w interpretacji genetycznej osadów czwartorzędowych. In: Mycielska-Dowgiałło E, ed., Eolizacja osadów jako wskażnik stratygraficzny Czwartorzędu. Pracownia Sedymentologiczna, WGiSR: 33–38 (in Polish). Search in Google Scholar

[50] Woronko B and Ostrowska M, 2009. Wpływ środowiska fluwialnego na charakter powierzchni ziarn kwarcowych — dyskusja. In: Kostrzewski A and Paluszkiewicz R, eds, Geneza, litologia i stratygrafia utworów czwartorzędowych (Genesis, lithology and stratigraphy of Quaternary deposits) V: 605–622 (in Polish). Search in Google Scholar

[51] Wysota W, 2002. Stratygrafia i środowiska sedymentacji zlodowacenia wisły w południowej części dolnego Powiśla (Stratigraphy and sedimentary environments of the Vistulian (Weichselian) glaciation in the southern part of the Lower Vistula region, middle-north Poland). Wydawnictwo UMK: 144pp (in Polish). Search in Google Scholar

[52] Wysota W, Lankauf KR, Molewski P and Szmańda J, 1996. Sedymen-tologia interstadialnej serii rzecznej (Rzęczkowo) zlodowacenia Wisły (Vistulian) odsłoniętej w SW krawędzi Wysoczyzny Chełmińskiej (Sedimentology of the interstadial fluvial series (Rzęczkowo) of the Vistulian glaciation expose in the SW margin of the Chełmno Moraine Plateau). Acta Universitatis Nicolai Copernic, Geografia 28: 39–63 Search in Google Scholar

[53] Wysota W, Molewski P and Sokołowski RJ, 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. http://dx.doi.org/10.1016/j.quaint.2008.12.01510.1016/j.quaint.2008.12.015Search in Google Scholar

[54] Zieliński T, 1992. Proglacial valley facies of the Silesian Upland — genetic factors and their sedimentological effects. Geologica Sudetica 26(1–2): 83–118. Search in Google Scholar

[55] Zieliński T, 1993. Sandry Polski północno-wschodniej — osady i warunki sedymentacji (Outwash plains of NE Poland — sediments and deposits processes). Prace Naukowe Uniwersytetu Śląskiego 1398: 97pp (in Polish). Search in Google Scholar

[56] Zieliński T, 1998. Litofacjalna identyfikacja osadów rzecznych (Lithofacial identification of alluvial sediments). In. Mycielska-Dowgiałło E, ed., Struktury sedymentacyjne i postsedymentacyjne w osadach czwartorzędowych i ich wartość interpretacyjna (Sedimentological and postsedimentological structures in Quaternary sediments and their value for interpretation) Wydział Geografii I Studiów Regionalnych Uniwersytetu Warszawskiego, Warszawa: 195–257. Search in Google Scholar