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Peculiarities of sedimentation conditions in the oxbow lakes of Dubysa River (Lithuania)

Identyfikatory
Warianty tytułu
Języki publikacji
EN
Abstrakty
EN
Abundant wood remains and buried trees have been found in the western part of Lithuania near Zakeliškiai and Lyduv?nai on Dubysa River (a tributary of Nemunas River) where deposits are rich in organic remnants and buried soils. In Zakeliškiai and Skiručiai sections of Dubysa River ox-bow sediments were investigated by various methods (dendrochronological, carbonate, granulometric, pollen and mollusc fauna analysis). In addition, these sections were dated using the radiocarbon method. Samples were collected from deposits of Dubysa River outcrops. The studied oxbow lakes have existed for more than 5 thousand years (from ca. 4300 BC to 1000 AD). During this period or-ganic rich deposits with trees and branches were formed in the oxbow lake. This indicates that at the end of Atlantic, during Subboreal and in the early Subatlantic periods there was a forest growing that contained mainly oaks which were falling down into an oxbow lake and later were covered by sandy and silty deposits. The granulometry of alluvial deposits, as well as the mixture of medium-grained sand and silt show different stages of Dubysa River palaeochannel formation: riverbed and oxbow lakes. Three climate warming cycles were revealed according to carbonate analysis data in all investi-gated sections. The rheophile thermophilous Holocene age molluscs species Bithynia tentaculata L., Unio cf. crassus Philipsson, Pisidium amnicum (Müller), Theodoxus fluviatilis (Linnaeus) have been found. The pollen composition and sequences have been divided into five local pollen assemblage zones (LPAZ) and described according to pollen spectra in each zone. In this way it is possible restore palaeoclimatic coherent evolution, trends and cyclical change.
Wydawca
Czasopismo
Rocznik
Strony
22--32
Opis fizyczny
Bibliogr. 16 poz., rys., tab., wykr.
Twórcy
autor
autor
autor
autor
autor
  • Department of Geology and Mineralogy, Vilnius University, Ciurlonio 22/27, 2009 Vilnius, Lithuania, jacek.pawlyta@polsl.pl
Bibliografia
  • Bronk Ramsey C, 2001. Development of the radiocarbon calibration program OxCal. Radiocarbon 43(2A): 355-363.
  • Damušyte A, 2005. Fossil molluscs of the Lithuanian Baltic coast. Quaternary Geology and Landforming Processes. In: Proceedings of the International Field Symposium, Kola Peninsula, NW Russia, September 4-9, 2005. Apatity, 2005: 15-16.
  • Gaigalas A and Dvareckas V, 2002. The evolution of river valleys in Lithuania from deglaciation to recent changes and data from the sediment infill of oxbow lakes. Netherlands Journal of Geoscienc-es (Geologie en Minjnbouw) 81(3-4): 407-416.
  • Gaigalas A, Sanko A, Pazdur A, Pawlyta J, Michczyński A and Budenaite S, 2007. Buried oaks and malacofauna of Holocene ox-bow lake sediments in the Valakupiai section, Lithuania. Geologi-ja 58: 35-48.
  • Grichiuk VP, 1940. Processing of deposits poor in organic material for the pollen analysis. In: Grichiuk VP, Problems of the physical ge-ography, Nauka, Moskva: 40-68 (In Russian).
  • Gudelis WK, 1973. Holocene sediments of Baltic zone. In: Reliefs and Quaternary sediments of Baltic zone: 195-209 (In Russian).
  • Erdtman G, 1936. New methods in pollen analysis. Svensk Botanisk Tidsskrift 30: 154-164.
  • Kabailiene M, 2006. Development of natural environment in Lithuania during 14 000 years. Vilnius University, Vilnius: 471 (In Lithua-nian).
  • Pawlyta J, Gaigalas A, Michczynski A, Pazdur A and Sanko A, 2007. Time scale for climatic events of Subboreal/Subatlantic transition Valakupiai site, Lithuania. Radiocarbon 49(2): 889-897.
  • Pazdur A, Fogtman M, Michczyński A and Pawlyta J, 2003. Precision of 14C dating in Gliwice Radiocarbon Laboratory. FIRI Pro-gramme. Geochronometria 22: 27-40.
  • Pazdur A, Pawlyta J and Spahiu P, 2000. Comparison of the radiocar-bon dating methods used in the Gliwice Radiocarbon Laboratory. Geochronometria 18: 9-13.
  • Reimer PJ, Baillie MGL, Bard E, Bayliss A, Beck JW, Blackwell PG, Bronk Ramsey C, Buck CE, Burr GS, Edwards RL, Friedrich M, Grootes PM, Guilderson TP, Hajdas I, Heaton TJ, Hogg AG, Hughen KA, Kaiser KF, Kromer B, McCormac FG, Manning SW, Reimer RW, Richards DA, Southon JR, Talamo S, Turney CSM, van der Plicht J and Weyhenmeyer CE, 2009. IntCal09 and Ma-rine09 radiocarbon age calibration curves, 0-50,000 years cal BP. Radiocarbon 51(4):1111-1150.
  • Rudnickaite EL, 1980. The technique of the determination of carbonates in various age Pleistocene tills. In: Raukas A. (Ed.), Methods of the field and laboratory investigations of glacial deposits. Abstracts of the symposium, Tallinn: 121 (In Russian).
  • Rudnickaite EL, 2007. Reconstruction of palaeogeography of Pleisto-cene interglacials according carbonates content. XVII INQUA Congress The Tropics: Heat Engine of the Quaternary, July 27 – August 03, 2007, Cairns, Australia. Abstracts. Quaternary Inter-national 167-168, Supplement: 356, DOI 0.1016/j.quaint.2007.04.001.
  • Shczierbina V N, 1958. About the method of mass measurement of carbonates in sedimentary rocks. In: Trudy Instituta Geolog-icheskih Nauk AN BSSR 1, Minsk: 131–144 (In Russian).
  • Sanko A F, 1999. Malacofauna of Pleistocene and Holocene in Belarus. Minsk: 103 (In Russian).
Typ dokumentu
Bibliografia
Identyfikator YADDA
bwmeta1.element.baztech-article-BWMA-0021-0002
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