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^14C ages of speleothems are usually younger than the Uranium-Series ages. The difference is often explained by changes of atmospheric radiocarbon concentration in the past, and in fact, speleothems have been as a material for radiocarbon time scale calibration. However in other works large spread of data points has been obtained. Comparison with the ^14C calibration data suggests that many ^14C of speleothems ages are too young or the Uranium-Series ages too old. ^14C dates of speleothems are commonly treated with caution, because of the reservoir effect, producing an apparent age, which is usually not accurately known. However, the reservoir effect may be of minor importance when compared to contamination with younger carbon.
Słowa kluczowe
Czasopismo
Rocznik
Tom
Strony
35--41
Opis fizyczny
Bibliogr. 25 poz.,
Twórcy
autor
- Institute of Geological Sciences, Polish Academy of Sciences, ul. Twarda 51/55, PL-00-818 Warsaw, Poland
autor
- Radiocarbon Laboratory, Institute of Physics, Silesian University of Technology, ul. Krzywoustego 2, PL-44-100 Gliwice, Poland
Bibliografia
- 1. BARD E., HAMELIN, B., FAIRBANKS R.G., ZINDLER, A. 1990. Calibration of the 14C timescale over the past 30,000 years using mass spectrometric U-Th ages from Barbados corals. Nature, 345, 405-410.
- 2. BARD, E., ARNOLD, M., FAIRBANKS, R., HAMELIN, B. 1993. 230Th-234U and 14C ages obtained by mass spectrometry on corals. Radiocarbon, 35, 191-199.
- 3. BARD , E., A RNOLD , M., H AMELIN , B., T ISNERAT -L ABORDE , N., C ABIOCH , G. 1998. Radiocarbon calibration by means of mass spectrometric 230 Th/ 234 U and 14 C ages of corals: an updated database including samples from Barbados, Mururoa and Tahiti. Radiocarbon, 40 (3), 1085-1092.
- 4. BASTIN, B. & GEWELT, M. 1986. Analyse pollinique et datation 14C de concretions stalagmitiques holocenes: apports complementaires des deux methodes. Geomorphie Physique Quaternaire, 40, 185-196.
- 5. GENTY, D. & MASSAULT, M. 1997. Bomb 14C recorded in laminated speleothems: calculation of dead carbon proportion. Radiocarbon, 39, 33-48.
- 6. GEWELT, M. 1985. Cinetique du concretionnement dans quelques grottes belges: Apport des datations 14C et 230Th/234U. Annales de la Societe Geologique de Belgique, 108, 267-273.
- 7. GEWELT, M. 1986. Datation 14C des concretions de grottes belges: Vitesses de croissance durant l’Holocene et implications paleoclimatiques. In: PETERSON, K., SWEETING, M.M. (Eds), New Directions in Karst; Proceedings of the Anglo-French Karst Symposium, September 1983. 293-322. Geo Books; Norwich.
- 8. GEYH, M.A. & HENNING, G.J. 1986. Multiple dating of a long flowstone profile. Radiocarbon, 28, 503-509.
- 9. GEYH, M.A. & SCHLÜCHTER, C. 1998. Calibration of the 14C time scale beyond 22,000 BP. Radiocarbon, 40 (1), 475-482.
- 10. GOSLAR, T., HERCMAN, H. & PAZDUR, A. 2000. Comparison of U-Series and radiocarbon dates of speleothems. Radiocarbon, 42, 403-413.
- 11. HERCMAN, H. 1991. Reconstruction of geological environment of the Western Tatra Mts. based on isotopic dating of speleothems. Geochronometria 8, 1-139. [In Polish with English summary].
- 12. 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. Studia Quaternaria, 17, 35-70.
- 13. HOLMGREN , K., L AURITZEN , S.-E. & P OSSNERT , G. 1994. 230Th/234U dating of a Late Pleistocene stalagmite in Lobatse II Cave, Botswana. Quaternary Science Reviews, 13, 111-119.
- 14. IVANOVICH , M. & H ARMON , R.S. 1982. Uranium Series Disequilibrium. Applications to environmental problems. Clarendon; Oxford.
- 15. KITAGAWA, H. & VAN DER PLICHT, J. 1998. Atmospheric radiocarbon calibration to 45,000 yr B.P.: late glacial fluctuations and cosmogenic isotope production. Science, 279, 1187-1190.
- 16. OSMOND, J.K., MAY, J.P. & TANNER, W.F. 1970. Age of the Cape Kennedy barrier-and-lagoon-complex. Journal of Geophysical Research, 75, 469-479.
- 17. PRZYBYŁWICZ, W., SCHWARCZ, H.P. & LATHAM, A.G. 1991. Dirty calcites; 2, Uranium-series dating of artificial calcitedetritus mixtures. Chemical Geology, 86, 161-178.
- 18. SCHWARCZ, H.P. 1980. Absolute age determinations of archaeological sites by uranium dating of travertines. Archaeometry, 22, 3-24.
- 19. SCHWARCZ, H.P. &LATHAM, A.G. 1989. Dirty calcites I: Uranium series dating of contaminated calcite using leachates alone. Isotope Geoscience, 80, 35-43.
- 20. STUIVER, M. (Ed.) 1993. Calibration 1993. Radiocarbon, 35 (1), 1-244.
- 21. STUIVER, M. & VAN DER PLICHT, J. (Eds) 1998. INTCAL 98: Calibration Issue. Radiocarbon, 40, 1041-1164.
- 22. TALMA A.S. & VOGEL J.C. 1992. Late Quaternary paleotemperatures derived from a speleothem from Cango Caves, Cape Province, South Africa. Quaternary Research, 37, 203-213.
- 23. VOGEL, J. 1983 14C variations during the Upper Pleistocene. Radiocarbon, 25 (2), 213-218.
- 24. VOGEL, J.C. & KRONFELD, J. 1997. Calibration of radiocarbon dates for the Late Pleistocene using U-Th dates on stalagmites. Radiocarbon, 39, 27-32.
- 25. W HITEHEAD , N.E., D ITCHBURN , R.G., W ILLIAMS , P.W. & MCCABE, W.J. 1999. 231 Pa and 230 Th contamination at zero age: a possible limitation on U/Th series dating of speleothem material. Chemical Geology, 156, 359-366.
Typ dokumentu
Bibliografia
Identyfikator YADDA
bwmeta1.element.baztech-article-BGPK-0379-2704