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Timescale for Climatic Events of Subboreal/Subatlantic Transition Recorded at the Valakupiai Site, Lithuania

Published online by Cambridge University Press:  18 July 2016

Jacek Pawlyta ,
Algirdas Gaigalas ,
Adam Michczyński ,
Anna Pazdur  and
Aleksander Sanko
Jacek Pawlyta*
Affiliation:
Department of Radioisotopes, GADAM Centre of Excellence, Institute of Physics, Silesian University of Technology, Krzywoustego 2, 44–100 Gliwice, Poland
Algirdas Gaigalas
Affiliation:
Department of Geology and Mineralogy, Vilnius University, Čiurlionio 22/27, 2009 Vilnius, Lithuania
Adam Michczyński
Affiliation:
Department of Radioisotopes, GADAM Centre of Excellence, Institute of Physics, Silesian University of Technology, Krzywoustego 2, 44–100 Gliwice, Poland
Anna Pazdur
Affiliation:
Department of Radioisotopes, GADAM Centre of Excellence, Institute of Physics, Silesian University of Technology, Krzywoustego 2, 44–100 Gliwice, Poland
Aleksander Sanko
Affiliation:
Laboratory of Quaternary Geology, Institute of Geochemistry and Geophysics, National Academy of Sciences of Belarus, Kuprevich 7, 220141 Minsk, Republic of Belarus
*
Corresponding author. Email: jacek.pawlyta@polsl.pl
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Abstract

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Oxbow lake deposits of the Neris River at the Valakupiai site in Vilnius (Lithuania) have been studied by different methods including radiocarbon dating. A timescale was attained for the development of the oxbow lake and climatic events recorded in the sediments. 14C dates obtained for 24 samples cover the range 990–6500 BP (AD 580 to 5600 BC). Medieval human activity was found in the upper part of the sediments. Mollusk fauna found in the basal part of the terrace indicate contact between people living in the Baltic and the Black Sea basins. Mean rates were calculated for erosion of the river and for accumulation during the formation of the first terrace.

Type
Articles
Information
Radiocarbon , Volume 49 , Issue 2 , 2007 , pp. 889 - 897
Copyright
Copyright © 2007 by the Arizona Board of Regents on behalf of the University of Arizona 

References

Bronk Ramsey, C. 1995. Radiocarbon calibration and analysis of stratigraphy: the OxCal program. Radiocarbon 37(2):425–30.CrossRefGoogle Scholar
Bronk Ramsey, C. 2001. Development of the radiocarbon program. Radiocarbon 43(2A):355–63.CrossRefGoogle Scholar
Gaigalas, A. 1998. The evolution of the geological environment of the castles of Vilnius. PACT 54:111–30.Google Scholar
Gaigalas, A. 2004. Environmental study of the Bronze–Iron Age transition period of eastern Europe. In: Scott, EM, Alekseev, AY, Zaitseva, G, editors. Impact of the Environment on Human Migration in Eurasia. Dordrecht: Kluwer Academic. p 243–54.Google Scholar
Gaigalas, A, 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 Geosciences 81(3–4):407–16.CrossRefGoogle Scholar
Gaigalas, A, Galčeienė, J, Banys, J, Breivė, A. 1976. Radiocarbon dating of Late Glacial deposits and underground waters. In: Gaigalas, A, editor. The Buried Palaeoincisions of Sub-Quaternary Rock Surfaces of the Southeast Baltic Region. Vilnius: Mokslas. p 102–14. In Russian.Google Scholar
Gaigalas, A, Dvareckas, V, Banys, J. 1987. Reconstructions of sedimentation conditions in the oxbow lakes of the Lithuanian river valleys. In: Kabailienė, M, editor. Methods for the Investigation of Lake Deposits: Palaeoecological and Palaeoclimatic Aspects. Vilnius: Vilnius University. p 228–34.Google Scholar
Nowaczyk, B, Pazdur, MF. 1990. Problems concerning the 14C dating of fossil dune soil. Quaestions Geographicae 11–12:135–51.Google Scholar
Pazdur, A, Michczyński, A, Pawlyta, J, Spahiu, P. 2000. Comparison of the radiocarbon dating methods used in the Gliwice Radiocarbon Laboratory. Geochronometria 18:9–14.Google Scholar
Pazdur, A, Fogtman, M, Michczyński, A, Pawlyta, J. 2003. Precision of 14C dating in Gliwice Radiocarbon Laboratory. FIRI programme. Geochronometria 22:27–40.Google Scholar
Pessenda, LCR, Gouveia, SEM, Aravena, R. 2001. Radiocarbon dating of total soil organic matter and humin fraction and its comparison with 14C ages of fossil charcoal. Radiocarbon 43(2B):595–601.CrossRefGoogle Scholar
Reimer, PJ, Baillie, MGL, Bard, E, Bayliss, A, Beck, JW, Bertrand, CJH, Blackwell, PG, Buck, CE, Burr, GS, Cutler, KB, Damon, PE, Edwards, RL, Fairbanks, RG, Friedrich, M, Guilderson, TP, Hogg, AG, Hughen, KA, Kromer, B, McCormac, G, Manning, S, Bronk Ramsey, C, Reimer, RW, Remmele, S, Southon, JR, Stuiver, M, Talamo, S, Taylor, FW, van der Plicht, J, Weyhenmeyer, CE. 2004. IntCal04 terrestrial radiocarbon age calibration, 0–26 cal kyr BP. Radiocarbon 46(3):1029–58.Google Scholar
Sanko, AF. 1999. Mollusk Fauna in the Glacio-Pleistocene and Holocene of Belarus. Minsk: Institute of Geological Sciences of the National Academy of Sciences. 103 p. In Russian.Google Scholar
Šulija, K, Lujanas, V, Kibilda, Z, Banys, J, Genutienė, I. 1967. Stratigraphy and chronology of the deposits in hollow of Lake Bebrukas. In: Kabailienė, M, editor. On Some Problems of Geology and Palaeogeography of the Quaternary Period in Lithuania (Transactions , Volume 5). Vilnius: Mintis. p 231–9. In Russian.Google Scholar