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Radiocarbon time scale for deposition of holocene calcareous tufa from Poland and India (Orissa)

Identyfikatory
Warianty tytułu
Języki publikacji
EN
Abstrakty
EN
14 C concentration measurements together with carbon and oxygen stable isotope analysis in calcareous tufa give possibilities for reconstruction of time scale and palaeoclimatic conditions of sedimentary processes. Results of isotope examinations of 2 profiles with organic and tufa sediments from Eastern Poland and 8 calcareous tufa sites from Eastern India (Orissa) are given. A systematic error of 14 C conventional age of carbonate fraction of tufa samples as reservoir age (T R ) was estimated. The T R values of different type of tufa sediment are determined by stream water energy. On the basis of known experimental dependence between T R and delta 13 C for tufas deposited in high, average and low energy water, unknown values of T R and corrected 14 C ages (T CCA ) were calculated for samples from India tufa sites. Continuous deposition of organic and carbonate sediments in Polish profiles give the possibility to calculate the approximated T CCA ages on the basis of dependence between T CCA and a sample depth in a profile, and time scale reconstruction of delta 13 C and delta 18 O changes in carbonate fraction of tufa samples during the whole Holocene.
Słowa kluczowe
Wydawca
Czasopismo
Rocznik
Tom
Strony
85--96
Opis fizyczny
Bibliogr. 29 poz., rys. tab.
Twórcy
autor
  • Department of Radioisotopes, Institute of Physics, Silesian University of Technology, Krzywoustego 2, 44-100 Gliwice, Poland
  • Department of Physical Geography and Palaeogeography, Maria Curie-Skłodowska University, Akademicka 19, 20-033 Lublin, Poland
  • Mass Spectrometry Laboratory, Maria Curie-Skłodowska University, Plac Marii Curie-Skłodowskiej 1, 20-031 Lublin, Poland;
  • Los Alamos Laboratory, Condensed Matter and Thermal Physics Group, Los Alamos, Mailstop K764, NM 87545, USA
autor
  • Department of Geology, Utkal University Bhubaneswar - 751004 (Orissa) India
  • Department of Radioisotopes, Institute of Physics, Silesian University of Technology, Krzywoustego 2, 44-100 Gliwice, Poland
autor
  • Department of Geology, Utkal University Bhubaneswar - 751004 (Orissa) India
Bibliografia
  • 1. Andrews J.E., Pedley H.M. and Dennis P.F., 1994: Stable isotope record of paleoclimatic: palaeo-hydrological interpretation. Geophysical Monograph 78, American Geophysical Union: 123-133.
  • 2. Das S. and Mohanti M., 1997: Holocene Microbial tufas: Orissa State, India. Carbonates and Evaporites 12(2): 204-219.
  • 3. Dobrowolski R., Alexandrowicz S.W., Ba³aga K., Durakiewicz T. and Pazdur A., 1999: Badania martwic wapiennych w obrêbie Ÿródliskowych torfowisk kopu³owych we wschodniej Polsce (Studies of tufa within spring cupola peatbogs in Eastern Poland). In: Pazdur A., Bluszcz A., Stankowski W. and Starkel L., eds, Geochronologia górnego czwartorzêdu Polski w œwietle datowañ radiowêglowych i luminescencyjnych (Geochronology of Upper Quaternary of Poland in the light of radiocarbon and luminescence dating). WIND-Wojewoda, Wroc³aw: 179-198.
  • 4. Dobrowolski R., Durakiewicz T. and Pazdur A., 2001: Calcareous tufa in the soligenous mires of Eastern Poland as an indicator of the Holocene climatic changes. Acta Geologica Polonica, in print.
  • 5. Friedman I., 1970: Some investigations of the deposition of travertine from hot springs-I. The isotopic chemistry of a travertine depositing spring. Geochimica et Cosmochimica Acta 34: 1303- 1315.
  • 6. Geyh M. A. and Schleicher H., 1990: Absolute Age Determination. Physical and Chemical dating Methods and Their Applications. Berlin-Heidelberg, Springer-Verlag: 162-180.
  • 7. Hercman H., 2000: Reconstruction of Palaeoclimatic changes in Central Europe between 10 and 200 thousand years BP, based on analysis of growth frequency of speleothems. Folia Quaternaria 17: 35-70.
  • 8. Holmgren K., Lauritzen S. E. and Possnert G., 1994: 230Th/234U and 14C dating of a Late Pleistocene stalagmite in Lobaste II Cave, Botswana. Quaternary Science Reviews 13: 111-119.
  • 9. Mook W.G., 1976: The dissolution-exchange model for dating groundwater with 14C. In: Interpretation of environmental and isotope data in groundwater hydrology. IAEA, Vienna: 213-225.
  • 10. Pazdur A., 1988: The relations between carbon isotope composition and apparent age of freshwater tufaceous sediments. Radiocarbon 30(1): 7-18.
  • 11. Pazdur A., 2000: Radiocarbon in freshwater carbonates as tool of Late Quaternary studies. Geologos 5: 136-154.
  • 12. Pazdur M. F., Bluszcz A., Pazdur A. and Morawiecka I., 1995a: Radiocarbon and thermoluminescence studies of the karst pipe systems in Southwest England and South Wales. In: Cook G. T., Harkness D. D. and Miller B., eds, Proceedings of the 15th International 14C Conference. Radiocarbon 37(2 ): 111-117.
  • 13. Pazdur A., Dobrowolski R., Durakiewicz T., Piotrowska N., Mohanti M. and Das S., 2002: δ13C and δ18O time record and palaeoclimatic implications of the Holocene calcareous tufa from Poland and India (Orissa). Geochronometria, this issue.
  • 14. Pazdur A., Fontugne M. F., Goslar T. and M. F. Pazdur, 1995b: Lateglacial and Holocene water-level changes of the Goœci¹¿ Lake, Central Poland, derived from carbon isotope studies of laminated sediments. Quaternary Sciences Review 14: 125-135.
  • 15. Pazdur A., Goslar T., Pawlyta M., Hercman H. and Gradziñski M., 1999: Variation of isotopic composition of carbon in the karst environment from Southern Poland, present and past. Radiocarbon 41(1): 81-97.
  • 16. Pazdur A., Michczyñski A., Pawlyta J. and Spahiu P., 2000: Comparison of the radiocarbon dating methods used in the Gliwice Radiocarbon Laboratory. Geochronometria 18: 9-14.
  • 17. Pazdur A. and Pazdur M. F., 1990: Further investigations on 14C dating of calcareous tufa. Radiocarbon 32(1): 17-22.
  • 18. Pazdur A., Pazdur M.F., Starkel L. and Szulc J., 1988b: Stable isotopes of the Holocene calcareous tufa in Southern Poland as palaeoclimatic indicators. Quaternary Research 30: 177-189.
  • 19. Pazdur A., Pazdur M.F. and Szulc J., 1988a: Radiocarbon dating of Holocene calcareous tufa from Southern Poland. Radiocarbon 30(2): 133-146.
  • 20. Pearson F.J., Jr, 1992: Effects of Parameter Uncertainty in Modelling 14C. In: Taylor R.E., Long A. and Kra R.S., eds, Radiocarbon After four Decades. An Interdisciplinary Perspective. SpringerVerlag, New York: 262-275.
  • 21. Srdoc D., Horvatincic N., Obelic B. and Sliepcevic A., 1982: Rudjer Boskovic Institute radiocarbon measurements VII. Radiocarbon 24(3): 352-371.
  • 22. Srdoc D., Horvatincic N., Obelic B. and Sliepcevic A., 1983: Radiocarbon dating of tufa in palaeoclimatic studies. In: Stuiver M. and Kra R.S., eds., International 14C Conference 11th, Proceedings. Radiocarbon 25(2): 421-427.
  • 23.Srdoc D., Obelic B., Horvatincic N. and Sliepcevic A., 1980: Radiocarbon dating of calcareous tufa : How reliable results can we expect? In: Stuiver M. and Kra R. S, eds, International 14C Conference 10th, Proceedings. Radiocarbon 22(3): 858-862.
  • 24. Stuiver M. and Polach H., 1977: Discussion: Reporting of 14C data. Radiocarbon 19: 355-363.
  • 25. Szulc J., 1983: Genesis and classification of travertine deposits. Przegląd Geologiczny 31: 231-236.
  • 26. Thorpe P.M., Holydak D.T., Preece R. C. and Willing M.J., 1981: Validity of corrected 14C dates from calcareous tufa. In: Formations carbonates externes, tufas et travertines. Actes Colloques AGF. Paris:151-156.
  • 27. Thorpe P.M., Otlet R. L. and Sweeting M. M., 1980: Hydrological implications from 14C profiling of UK tufa. In: Stuiver M. and Kra R. S., eds, International 14C Conference, 10th, Proceedings. Radiocarbon 22(3):897-908.
  • 28. Turi B., 1986: Stable isotope geochemistry in travertines. In: Fritz P. and Frontes J. S., eds, Handbook of Environmental Isotope Geochemistry 2. Elsevier, Amsterdam: 207-235.
  • 29. Usdowski E., Hoefs J. and Menschel G., 1979: Relationship between 13C and 18O fractionation and changes in major elements composition in a recent calcite-depositing spring - a model of chemical variations with inorganic CaCO3 precipitation. Earth and Planetary Science Letters 42: 267-276.
Typ dokumentu
Bibliografia
Identyfikator YADDA
bwmeta1.element.baztech-article-BAT3-0007-0020
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