Hostname: page-component-586b7cd67f-rdxmf Total loading time: 0 Render date: 2024-11-27T13:59:15.255Z Has data issue: false hasContentIssue false
  • English
  • Français

Radiocarbon Chronology of Late Glacial and Holocene Sedimentation and Water-Level Changes in the Area of the Gościąż Lake Basin

Published online by Cambridge University Press:  18 July 2016

Anna Pazdur ,
M. F. Pazdur ,
Tomasz Goslar ,
Bogumił Wicik  and
Maurice Arnold
Anna Pazdur
Affiliation:
Radiocarbon Laboratory, Silesian Technical University, Krzywoustego 2, PL-44-100 Gliwice, Poland
M. F. Pazdur
Affiliation:
Radiocarbon Laboratory, Silesian Technical University, Krzywoustego 2, PL-44-100 Gliwice, Poland
Tomasz Goslar
Affiliation:
Radiocarbon Laboratory, Silesian Technical University, Krzywoustego 2, PL-44-100 Gliwice, Poland
Bogumił Wicik
Affiliation:
Faculty of Geography, Warsaw University, Krakowskie Przedmieście 30, PL-00-927 Warsaw, Poland
Maurice Arnold
Affiliation:
Centre des Faibles Radioactivités, Laboratoire mixte CNRS-CEA, Domaine du CNRS, Avenue de la Terrasse, F-91198 Gif sur Yvette Cedex, France
Rights & Permissions [Opens in a new window]

Abstract

Core share and HTML view are not available for this content. However, as you have access to this content, a full PDF is available via the ‘Save PDF’ action button.

We obtained 14C ages on samples of lake marl and other sediments from cores taken in Gościąż Lake and its environs. Comparison of 14C dates of bulk samples of laminated sediment with varve chronology and available AMS dates of terrestrial macrofossils indicates a reservoir correction of 2000 ± 120 yr for the basal series of lake sediments. 14C dates obtained on peat layers underlying the oldest lacustrine sediments in Gościąż and other lakes consistently locate the beginning of organogenic sedimentation in this area at ca. 13 ka bp. We distinguished three periods of lacustrine gyttja sedimentation in cores taken in Gościąż and adjacent lakes: 11.8–10.2 ka, 8–7 ka and 2.7–2.1 ka bp. From the 14C dates of lithological boundaries in these cores, we reconstruct a pattern of lake-level changes during the last 12 ka, remarkably similar to Swedish lakes and generally agreeing with available records from European and American lakes. The behavior of Gościąż Lake during the last 12 ka fairly well reflects global climate changes in the temperate zone during the Late Glacial and Holocene periods.

Type
Articles
Information
Radiocarbon , Volume 36 , Issue 2 , 1994 , pp. 187 - 202
Copyright
Copyright © The American Journal of Science 

References

Arnold, M., Bard, E., Maurice, P. and Duplessy, J.-C. 1987 C-14 dating with Gif-sur-Yvette tandetron accelerator: Status report. In Gove, H. E., Litherland, A. E. and Elmore, D., eds., Proceedings of the 4th International Conference on Accelerator Mass Spectrometry. Nuclear Instruments and Methods in Physics Research B29: 120–123.CrossRefGoogle Scholar
Digerfeldt, G. 1988 Reconstruction and regional correlation of Holocene lake-level fluctuations in Lake Bysjön, South Sweden. Boreas 17:165–172.CrossRefGoogle Scholar
Goslar, T. 1993 Varve chronology of laminated sediments of Lake Gościąż. Polish Botanical Studies, Guidebook Series 8: 105–119 (in Polish).Google Scholar
Goslar, T., Kuc, T., Pazdur, M. F., Ralska-Jasiewiczowa, M., Różański, K., Szeroczyńska, K., Walanus, A., Wicik, B., Więckowski, K., Arnold, M. and Bard, E. 1992 Possibilities for reconstructing radiocarbon level changes during the late glacial by using a laminated sequence of Gościąż Lake. In Long, A. and Kra, R. S., eds., Proceedings of the 14th International 14C Conference. Radiocarbon 34(3): 826–832.CrossRefGoogle Scholar
Goslar, T., Kuc, T., Ralska-Jasiewiczowa, M., Różański, K., Arnold, M., Bard, E., van Gel, B., Pazdur, M. F., Szeroczyńska, K., Wicik, B., Więckowski, K. and Walanus, A. 1993 High-resolution lacustrine record of the Late Glacial/Holocene transition in Central Europe. Quaternary Science Reviews 12: 287–294.CrossRefGoogle Scholar
Goslar, T., Pazdur, A., Pazdur, M. F. and Walanus, A. 1989 Radiocarbon and varve chronologies of annually laminated lake sediments of Gościąż Lake, Central Poland. In Srdoč, D., Long, A. and Kra, R. S., eds., Proceedings of the 13th International 14C Conference. Radiocarbon 31(3): 940–947.CrossRefGoogle Scholar
Harrison, S. P. 1989 Lake levels and climatic changes in eastern North America. Climate Dynamics 3: 157–167.CrossRefGoogle Scholar
Harrison, S. P., Prentice, C. and Guiot, J. 1993 Climatic controls on Holocene lake-level changes in Europe. Climate Dynamics 8: 189–200.CrossRefGoogle Scholar
Madeyska, T. 1993 Geomorphological map of the Płock Basin. Polish Botanical Studies, Guidebook Series 8: 9–13 (in Polish).Google Scholar
Magny, M. 1992 Holocene lake-level fluctuations in the Jura and the northern subalpine ranges, France: Regional patterns and climatic implications. Boreas 21: 319–334.CrossRefGoogle Scholar
Magny, M. 1993 Solar influences on Holocene climatic changes illustrated by correlations between past lake-level fluctuations and atmospheric 14C record. Quaternary Research 40: 1–9.CrossRefGoogle Scholar
Pazdur, A., Fontugne, M. R., Goslar, T. and Pazdur, M. F. (ms.) Late Glacial and Holocene water-level changes of Gościściąż Lake, Central Poland, derived from carbon isotope studies of laminated sediment. Submitted to Quaternary Science Reviews. Google Scholar
Pazdur, A., Pazdur, M. F., Wicik, B. and Więckowski, K. 1987a Radiocarbon chronology of annually laminated sediments from the Gościąż Lake. Bulletin of the Polish Academy of Sciences, Earth Sciences 35: 139–145.Google Scholar
Pazdur, A. and Starkel, L. 1989 New approach to explanation of changes in the volume and water level of the Gościąż Lake. Zeszyty Naukowe Politechniki Slaskiej, Seria Matematyka-Fizyka 57. Geochronometria 5: 29–44.Google Scholar
Pazdur, M. F., Awsiuk, R., Goslar, T., Pazdur, A., Walanus, A., Wicik, B. and Więckowski, K. 1987b. Calibrated radiocarbon chronology of annually laminated sediments from the Gościąż Lake. Zeszyty Naukowe Politechniki Slaskiej, Seria Matematyka-Fizyka 56. Geochronometria 4: 69–83.Google Scholar
Ralska-Jasiewiczowa, M., Wicik, B. and Więckowski, K. 1987 Lake Gościąż—a site of annually laminated sediments covering 12,000 years. Bulletin of the Polish Academy of Sciences, Earth Sciences 35: 139–145.Google Scholar
Różański, K., Goslar, T., Dulinski, M., Kuc, T., Pazdur, M. F. and Walanus, A. 1992 The Late Glacial-Holocene transition in laminated sediments of the Lake Gościąż (Central Poland). In Bard, E. and Broecker, W. S., eds., The Last Deglaciation: Absolute and Radiocarbon Chronologies. NATO ASI Series I, Global Environmental Change, Vol. 2. Berlin/Heidelberg, Springer-Verlag: 69–80.CrossRefGoogle Scholar
Sierzega, P. and Narwojsz, A. (ms.) 1988 The grip of groundwater from Quaternary sediment in the Jozefowek region near Wlocawek. Archive of Geological Enterprise, Gdansk Division, Gdansk (in Polish).Google Scholar
Skompski, S. 1971 Comments on the Detailed Geological Map of Poland, Scale 1:50000, Dobrzyn Chart. Wydawnictwa Geologiczne, Warsaw (in Polish).Google Scholar
Stuiver, M. and Polach, H. A. 1977 Discussion: Reporting of 14C data. Radiocarbon 19(3): 355–363.CrossRefGoogle Scholar
Wicik, B. and Więckowski, K. 1991 The sediments of the “Na Jazach” lakes in the Płock Basin—conditions of their sedimentation and role in reconstruction and prognosis of the natural environment. Przeglad Geograficzny 63: 57–76 (in Polish).Google Scholar
Więckowski, K. 1993 The current state of recognition of bottom sediments in the “Na Jazach” lakes according to their macroscopic features. Polish Botanical Studies, Guidebook Series 8: 77–92 (in Polish).Google Scholar