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Delta 13C and delta 18O time record and palaeoclimatic implications of the holocene calcareous tufa from south-eastern Poland and eastern India (Orissa)

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Warianty tytułu
Języki publikacji
EN
Abstrakty
EN
Measurements of delta 18 O and delta 13 C in tufa samples dated by 14 C method have been used to reconstruct climatic changes in Southern and Eastern Poland and in Eastern India (Orissa) for the last ca 13,500 years. Stable isotope time record delta 18 O in calcareous tufa profiles can be interpreted as palaeoclimatic record if dependence between oxygen isotope composition and temperature for the specific climatic region is known. Estimated sedimentation temperatures of calcareous tufas from Polish sites indicate the mean year of air temperatures during the last 12,000 years and mean winter and summer temperature for Orissa state, using stable isotope analysis for calcareous tufa from Indian sites. The estimated temperatures have real values, comparable with contemporaneous sedimentation temperature. The characteristic trend of the temperature changes increasing for Poland and decreasing for Orissa, since the beginning of the Holocene till today, can be observed with climatic optimum ca 5000-6000 BP synchronous in both countries.
Słowa kluczowe
Wydawca
Czasopismo
Rocznik
Tom
Strony
97--108
Opis fizyczny
Bibliogr. 37 poz., rys.
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
  • 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
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 palaeoclimatic change in a British Holocene tufa. The Holocene 4: 349-355.
  • 2. Andrews J.E., Riding R. and Dennis P.F., 1993: Stable isotopic compositions of Recent freshwater cyanobacterial carbonates from British Isles: local and regional environmental controls. Sedimentology 40: 303-314.
  • 3. Augustithis S.S., 1982: Atlas of sphaeroidal textures and structures and their genetic significance. Theophrastus Publ., S.A., Athens: 329.
  • 4. Baker A., Smart P.L. and Ford D.C., 1993: Northwest European palaeoclimate as indicated by growth frequency variations of secondary calcite deposits. Palaeogeography, Palaeoclimatology, Palaeoecology 100: 291-301.
  • 5. Casanova J. and Hillaire-Marcel C., 1993: Carbon and Oxygen isotopes in African stromatolites: palaeo-hydrological interpretation. American Geophysical Union, Geophysical Monograph 78: 123-133.
  • 6. Chafetz H.S. and Lawrence J.R., 1994: Stable isotopic variability within modern travertine. Geographie Physique et Quaternaire 48(3): 257-273.
  • 7. Chafetz H.S., Rush P.F. and Utech, N.M., 1991: Microenvironmental controls on mineralogy and habit of CaCO3 precipitates: an example from an active travertine system. Sedimentology 38: 107-126.
  • 8. Dandurand J.L., Guirt R., Hoefs J., Menschell G., Schott J. and Usdowski E., 1982: Kinetically controlled variations of major components and carbon isotopes in calcite precipitating spring. Chemical Geology 36: 299-315.
  • 9. Das S. and Mohanti M., 1997: Holocene Microbial tufas: Orissa State, India. Carbonates and Evaporites 12(2): 204-219.
  • 10. Das S. and Mohanti M., 2001: The geochemistry of a tufa – depositing stream of Mayurbanj (Orissa), India: possible controls on calcite and dolomite precipitation. In preparation to print.
  • 11. Dobrowolski R., Durakiewicz T., Pazdur A. and Pazdur M.F., 1996: Chronostratygrafia i fazy rozwoju źródliskowego torfowiska kopułowego Krzywice kolo Chełma (Wyżyna Lubelska) (Chronostratigraphy and development stages of the spring peat – knoll at Krzywice near Chełm, Lublin Upland, South-eastern Poland). Zeszyty Naukowe Politechniki Śląskiej, Seria Matematyka- Fizyka, Zeszyt 80, Geochronometria Nr 17: 19-30.
  • 12. Dobrowolski R., Alexandrowicz S.W., Bałaga K., Durakiewicz T. and Pazdur A., 1999: Badania martwic wapiennych w obrębie źródliskowych torfowisk kopułowych 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 czwartorzędu Polski w świetle datowania radiowęglowego i luminescencyjnego (Geochronology of the Upper Quaternary in Poland in the light of radiocarbon and luminescence dating). WIND-J. Wojewoda, Wrocław: 179-197.
  • 13. Dobrowolski R., Durakiewicz T. and Pazdur A., 2002: Calcareous tufas in the soligenous mires of Eastern Poland as an indicator of the Holocene climatic changes. Acta Geologica Polonica, in print.
  • 14. Goslar T., Hercman H. and Pazdur A., 2000: Comparison of USeries and radiocarbon dates of speleothems. Radiocarbon 42: 403-414.
  • 15. Guiot J., Pons A., Bealieu J.L. and Reille M., 1989: A 140,000 year continental climate reconstruction from two European pollen records. Nature 338: 309-313.
  • 16. Guo L., Andrews J., Riding R., Dennis P. and Dresser Q., 1996: Possible microbial effects on stable carbon isotopes in hotspring travertines. Journal of Sedimentary Research 66(3): 468-473.
  • 17. Hercman H., 2000: Reconstruction of palaeoclimatic changes in Central Europe between 10 and 200 thousand years B, based on analysis of growth frequency of speleothems. Studia Quaternaria 17: 35-70.
  • 18. Kalsotra M.R. and Prasad S., 1979: Calc-tufa deposit of the Vindhyan scarp and its utilization. Geological Survey of India, Indian Minerals 33: 16-21.
  • 19. Merz M.U.E., 1992: The biology of carbonate precipitation by cyanobacteria. Facies 26: 81-102.
  • 20. Pawar N.J., Kale V.S., Atkinson T.C. and Rowe P.J., 1988: Early Holocene waterfall tufa from semi-arid Maharastra Plateau, India. Journal of Geological Society of India 32: 513-515.
  • 21. Pazdur A., 1988: The relations between carbon isotope composition and apparent age of freshwater tufaceous sediments. Radiocarbon 30(1): 7-18.
  • 22. Pazdur A., 2000. Radiocarbon in freshwater carbonates as tool of Late Quaternary studies. Geologos 5: 136-154.
  • 23. 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., Miller B. F. and Scott E. M., eds, Proceedings of the 15th International 14C Conference. Radiocarbon 37: 111-117.
  • 24. Pazdur A., Fontugne M. R., Goslar T. and Pazdur M. F., 1995b: Late Glacial and Holocene water-level changes of the Gosciąż Lake, Central Poland, derived from carbon isotope studies of laminated sediments. Quaternary Science Reviews 14: 125-135.
  • 25. Pazdur A., Pazdur M. F., Goslar T., Wicik B. and Arnold M., 1994: Radiocarbon chronology of Late Glacial and Holocene sedimentation and water-level changes in the area of the Gościąż Lake Basin. Radiocarbon 36: 187-202.
  • 26. Pazdur A., Pazdur M. F., Pawlyta J., Górny A. and Olszewski M, 1995: Palaeoclimatic implications of radiocarbon dating of speleothems from Cracow-Wieluń Upland, southern Poland. In: Cook G. T., Harkness D. D., Miller B. F. and Scott E. M., eds, Proceedings of the 15th International 14C Conference. Radiocarbon 37: 103-110.
  • 27. Pazdur A., Pazdur M.F. and Szulc J., 1988a: Radiocarbon dating of Holocene calcareous tufa from south Poland. Radiocarbon 30(2): 133-146.
  • 28. 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.
  • 29. Pentecost A. and Spiro B., 1990: Stable carbon and oxygen isotope composition of calcites associated with modern freshwater cyanobacteria and algae. Geomicrobiology Journal 8: 17-26.
  • 30. Różański K., 1985: Deuterium and oxygen-18 in European groundwaters links to atmospheric circulation in the past. Chemical Geology 52: 349-363.
  • 31. Schackleton N.J., 1967: Oxygen isotope analyses and Pleistocene temperatures re-assessed. Nature 215: 15-17.
  • 32. Smart P.L. and Richards D, 1992: Age estimates for the Late Quaternary sea-stands. Quaternary Science Review 11: 687-696.
  • 33. 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., Proceedings of 11th International 14C Conference: Radiocarbon 25(2): 421-427.
  • 34. 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., Proceedings of 10th International 14C Conference. Radiocarbon 22(3): 897-908.
  • 35. Turi, B., 1986: Stable isotope geochemistry in travertines. In: Fritz P. and Frontes J. C., eds., Handbook of Environmental Isotope Geochemistry 2. Elsevier, Amsterdam: 207-235. 107 A.
  • 36. Pazdur et al. 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.
  • 37. Van der Straaten C. M. and Mook W. G., 1983: Stable isotope composition of precipitation and climatic variability. In: Palaeoclimates and Palaeowaters: A collection of environmental isotope studies. IAEA, Vienna: 53-64.
Typ dokumentu
Bibliografia
Identyfikator YADDA
bwmeta1.element.baztech-article-BAT3-0007-0021
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