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Optical dating and sedimentary record from the terrace depositional profile of the Warta River (Central Poland)

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Języki publikacji
EN
Abstrakty
EN
Results of OSL dating and sedimentary studies from the profile of the low alluvial terrace of the middle Warta River are presented. The samples were dated using the single-aliquot regenera-tive method. Dating was used to establish a timing of the Weichselian Late Glacial events in the river valley environment. Stable conditions on the floodplain are expressed by the deposition of organic-rich series radiocarbon dated at 12 900-12 600 cal BP and 11 600-10 770 cal BP. Samples for OSL dating were collected from the mineral material deposited during the intensification of flood events during the Weichselian decline. The results obtained for the alluvia range from 12.78 ± 0.62 ka b2k to 14.33 ± 0.74 ka b2k. Sedimentological criteria allowed to distinguish between particular flood events. Overestimation of OSL ages is probably a result of rapidity of environmental changes in that time.
Słowa kluczowe
Czasopismo
Rocznik
Strony
361--368
Opis fizyczny
Bibliogr. 33 poz., rys., tab.
Twórcy
  • Department of Geomorphology and Palaeogeography, Faculty of Geographical Sciences, University of Lodz, ul. Narutowicza 88, 90-139 Lodz, Poland
  • Department of Geomorphology and Palaeogeography, Faculty of Geographical Sciences, University of Lodz, ul. Narutowicza 88, 90-139 Lodz, Poland
autor
  • Department of Geomorphology and Palaeogeography, Faculty of Geographical Sciences, University of Lodz, ul. Narutowicza 88, 90-139 Lodz, Poland
autor
  • Department of Geomorphology and Palaeogeography, Faculty of Geographical Sciences, University of Lodz, ul. Narutowicza 88, 90-139 Lodz, Poland
autor
  • Department of Radioisotopes, Institute of Physics–Centre for Science and Education, Silesian University of Technology, ul. Krzywoustego 2, 44-100 Gliwice, Poland
autor
  • Department of Radioisotopes, Institute of Physics–Centre for Science and Education, Silesian University of Technology, ul. Krzywoustego 2, 44-100 Gliwice, Poland
Bibliografia
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  • 2.Anketell JM, Cegła J and Dżułyński S, 1970. On the deformational structures in systems with reversed density gradients. Rocznik Polskiego Towarzystwa Geologicznego 40(1): 3–29.
  • 3.Björck S, Walker M, Cwynar L, Johnsen S, Knudsen K.-L, Lowe J, Wohlfarth B and INTIMATE Members, 1998. An event stratigraphy for the last Termination in the North Atlantic region based on the Greenland ice-core record: a proposal by the INTIMATE group. Journal of Quaternary Science 13(4): 283–292, DOI 10.1002/(SICI)1099-1417(199807/08)13:4<283::AID-JQS386>3.0.CO;2-A.
  • 4.Bortolot VJ, 2000. A new modular high capacity OSL reader system. Radiation Measurements 32(5–6): 751–757, DOI 10.1016/S1350-4487(00)00038-X.
  • 5.Broecker WS, 2006. Abrupt climate changes revisited. Global and Planetary Change 54(3–4): 211–215, DOI 10.1016/j.gloplacha.2006.06.019.
  • 6.Bronk Ramsey C, 2001. Development of the radiocarbon calibration program. Radiocarbon 43(2A): 355–363.
  • 7.Bronk Ramsey C, 2009. Bayesian analysis of radiocarbon dates. Radiocarbon 51: 337–360.
  • 8.Czubla P, Forysiak J, Petera-Zganiacz J, Grajoszek M and Wiśniewska M, 2013. Charakterystyka litologiczno-pertograficzna osadów czwartorzędowych w dolinie Warty (stanowisko Koźmin-Północ) (The lithological and petrographic features of the Quaternary deposits in the Warta River valley (Koźmin-North site). Przegląd Geologiczny 61(2): 120–126 (in Polish with English summary).
  • 9.Dzieduszyńska D and Petera-Zganiacz J, 2012. Geologic position of the Younger Dryas subfossil forest in the Warta River Valley, central Poland. Bulletin of the Geological Society of Finland 84: 69–79.
  • 10.Dzieduszyńska D, Kittel P, Petera-Zganiacz J, and Twardy J, 2012. Paleogeograficzne elementy rozwoju doliny Warty w Kotlinie Kolskiej w świetle badań w stanowisku „Koźmin Las” (Palaeoge-ographical elements of the Warta River evolution within the Koło Basin in the light of investigations at the site “Koźmin Las”). Acta Geographica Lodziensia 100: 35–50 (in Polish with English summary).
  • 11.Dzieduszyńska D, Kittel P, Petera-Zganiacz J, Brooks SJ, Korzeń K, Krąpiec M, Pawłowski D, Płaza DK, Płóciennik M, Stachowicz-Rybka R and Twardy J, 2014. Environmental influence on forest development and decline in the Warta River Valley (Central Poland) during the Late Weichselian. Quaternary International 324: 99–114, DOI 10.1016/j.quaint.2013.07.017.
  • 12.Forysiak J, 2005. Rozwój doliny Warty między Burzeninem a Dobrowem po zlodowaceniu warty (The development of the Warta River Valley between Burzenin and Dobrów in the late Quaternary period). Acta Geographica Lodziensia 90: 116 pp (in Polish with English summary).
  • 13.Galbraith RF, Roberts RG, Laslett GM, Yoshida H and Olley JM, 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): 339–364, DOI 10.1111/j.1475-4754.1999.tb00987.x.
  • 14.Gradziński R, Kostecka A, Radomski A and Unrug R, 1986. Zarys sedymentologii (Sedimentology). Wyd. Geolog., Warszawa: 628 pp (in Polish).
  • 15.Kittel P, Petera-Zganiacz J, Dzieduszyńska D, Twardy J, Krąpiec M, Bijak Sz, Bronisz K, Zasada M and Płaza D, 2012. Badania „kopalnego lasu” ze schyłku vistulianu w dolinie Warty, Kotlina Kolska, środkowa Polska (Research of subfossil forest from the Weichselian decline in the Warta River Valley, Koło Basin, central Poland). Studia i Materiały Centrum Edukacji Przyrodniczo-Leśnej 1(30): 238–245 (in Polish with English summary).
  • 16.Litt T, Brauer A, Goslar T, Merkt J, Bałaga K, Müller H, Ralska-Jasiewiczowa M, Stebich M and Negendank JFM, 2001. Correlation and synchronisation of Lateglacial continental sequences in northern central Europe based on annually laminated lacustrine sediments. Quaternary Science Reviews 20(11): 1233–1249, DOI 10.1016/S0277-3791(00)00149-9.
  • 17.Lowe JJ, Hoek WZ and INTIMATE group, 2001. Interregional correlation of palaeoclimatic records for the Last Glacial-Interglacial Transition: a protocol for improved precision recommended by the INTIMATE project group. Quaternary Science Reviews 20(11): 1175–1187, DOI 10.1016/S0277-3791(00)00183-9.
  • 18.Lowe JJ, Rasmussen SO, Björck S, Hoek WZ Steffensen JP, Walker MJC, Yu ZC and the INTIMATE group, 2008. Synchronization of paleaoenvironmental events in the North Atlantic region during the Last Termination: a revised protocol recommended by the INTI-MATE group. Quaternary Science Reviews 27(1–2): 6–17, DOI 10.1016/j.quascirev.2007.09.016.
  • 19.Mangerud J, Anderson ST, Berglund BE and Danner JJ, 1974. Quaternary stratigraphy of Norden, a proposal for terminology and classification. Boreas 3(3): 109–126, DOI 10.1111/j.1502-3885.1974.tb00669.x.
  • 20.Marks L, 2005. Pleistocene glacial limits in the territory of Poland. Przegląd Geologiczny 53: 988–993.
  • 21.Miall AD (ed.), 1978. Fluvial Sedimentology. Canadian Society of Petrolium Geologists Memoir 5: 859 pp.
  • 22.Murray AS and Wintle AG, 2000. Luminescence dating of quartz using an improved singlealiquot regenerative-dose protocol. Radiation Measurements 32(1): 57–73, DOI 10.1016/S1350-4487(99)00253-X.
  • 23.Petera J, 2002. Vistuliańskie osady dolinne w basenie uniejowskim i ich wymowa paleogeograficzna (Vistulian valley deposits in the Uniejów Basin and their palaeogeographical significance). Acta Geographica Lodziensia 83: 174 pp (in Polish with English summary).
  • 24.Prescott JR and Hutton JT, 1994. Cosmic ray contributions to dose rates for luminescence and ESR dating: large depths and long-term time variations. Radiation Measurements 23(2–3): 497–500, DOI 10.1016/1350-4487(94)90086-8.
  • 25.Reimer PJ, Baillie MGL, Bard E, Bayliss A, Blackwell PG, Bronk Ramsey C, Buck CE, Burr GS, Edwards RL, Freidrich M, Grootes PM, Guilderson TP, Hajdas I, Heaton TJ, Hogg AG, Hughen KA, Kaiser KF, Kromer B, McCormac G, Manning S, Reimer RW, Richards DA, Southon JR, Talamo S, Turney CMS, van der Plicht J and Weyhenmeyer CE, 2009. Intcal09 and Marine09 radiocarbon age calibration curves, 0–50 000 years cal BP. Radiocarbon 51: 1111–1150.
  • 26.Starkel L, Michczyńska DJ, Krąpiec M, Margielewski W, Nalepka D and Pazdur A, 2013. Progress in the Holocene chrono-climatostratigraphy of Polish territory. Geochronometria 40(1): 1–21, DOI 10.2478/s13386-012-0024-2.
  • 27.Sundborg A, 1956. The River Klarälven: a study of fluvial processes. Geografiska Annaler 38: 125–237, DOI 10.2307/520140.
  • 28.Turkowska K, Forysiak J, Petera J and Miotk-Szpiganowicz G, 2004. A Warta River system during the Younger Dryas in the Koło Basin (Middle Poland). Quaestiones Geographicae 23: 83–107.
  • 29.Walanus A and Goslar T, 2009. Datowanie radiowęglowe (Radiocarbon dating). Wyd. AGH, Kraków: 147 pp (in Polish).
  • 30.Widera M, 2007. Litostratygrafia i paleotektonika kenozoiku podplej-stoceńskiego Wielkopolski (Lithostratigraphy and palaeotectonics of the sub-Pleistocene Cenozoic of Wielkopolska). Wyd. Naukowe UAM, Seria Geologia 18: 223 pp (in Polish with English sum-mary).
  • 31.Zieliński T, 1995. Kod litofacjalny i litogenetyczny – konstrukcja i zastosowanie (Lithofacies and genetic codes: construction and application). In: Mycielska-Dowgiałło E and Rutkowski J, Eds., Badania osadów czwartorzędowych. Wybrane metody i interpretacja wyników. WGiSR UW, Warszawa: 220–235 (in Polish with English summary).
  • 32.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. WGiSR UW, Warszawa: 193–257 (in Polish with English summary).
  • 33.Zieliński T and Pisarska-Jamroży M, 2012. Jakie cechy litologiczne osadów warto kodować, a jakie nie? (Which features of deposits should be included in a code and which not?). Przegląd Geologiczny 60(7): 387–397 (in Polish with English summary).
Typ dokumentu
Bibliografia
Identyfikator YADDA
bwmeta1.element.baztech-22779482-860c-48dc-a558-e4fb7d2ae0ad
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