Hostname: page-component-8448b6f56d-qsmjn Total loading time: 0 Render date: 2024-04-18T23:26:59.376Z Has data issue: false hasContentIssue false
  • English
  • Français

Rudjer Bošković Institute Radiocarbon Measurements XII

Published online by Cambridge University Press:  18 July 2016

Dušan Srdoč ,
Nada Horvantinčić ,
Ines Krajcar Bronić ,
Bogomil Obelić  and
Adela Sliepčević
Dušan Srdoč
Affiliation:
Rudjer Bošković Institute, P. O. Box 1016, 41001 Zagreb, Croatia
Nada Horvantinčić
Affiliation:
Rudjer Bošković Institute, P. O. Box 1016, 41001 Zagreb, Croatia
Ines Krajcar Bronić
Affiliation:
Rudjer Bošković Institute, P. O. Box 1016, 41001 Zagreb, Croatia
Bogomil Obelić
Affiliation:
Rudjer Bošković Institute, P. O. Box 1016, 41001 Zagreb, Croatia
Adela Sliepčević
Affiliation:
University of Zagreb
Rights & Permissions [Opens in a new window]

Extract

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 present here radiocarbon analyses made since our previous list (Srdoč et al. 1989). Sample pretreatment, combustion and counting techniques are essentially the same as described previously (Srdoč, Breyer & Sliepčević 1971), supplemented by new techniques for groundwater processing (Srdoč et al. 1979). The calculation of ages follows conventional protocol (Stuiver & Polach 1977). These ages can be converted from the 5570-year half-life to the chronometrically more correct half-life of 5730 years by multiplying by the factor, 1.029. Ages and standard deviations of all samples are adjusted for stable isotope fractionation according to the recommendations in Stuiver and Polach (1977), except for groundwater, calcareous deposits and aquatic plants. The δ13C values of the latter reflect the environmental conditions during their formation or growth rather than fractionation (Mook 1976; Krajcar Bronić et al. 1986; Marčenko et al. 1989). Thus, any percent modern (pMC) correction based on δ13C values is meaningless or even misleading. Sample descriptions are prepared in collaboration with collectors and submitters. Calibrated ages were calculated using the program of Stuiver and Reimer (1987).

Type
Date Lists
Information
Radiocarbon , Volume 34 , Issue 1 , 1992 , pp. 155 - 175
Copyright
Copyright © The American Journal of Science 

References

Benkö, L., Horvath, F., Horvatinčić, N. and Obelić, B. 1989 Radiocarbon and thermoluminescence dating of prehistoric sites in Hungary and Yugoslavia. In Long, A., Kra, R.S. and Srdoč, D., eds., Proceedings of the 13th International 14C Conference. Radiocarbon 31(3): 992–1002.Google Scholar
Degmedžić, J. 1977 The Frankopans and the Sv. Lovro church. In Strbašić, M., ed., Požega, 1227–1977. Zagreb, Grafički zavod Hrvatske: 158–160 (in Croatian).Google Scholar
Durman, A. and Obelić, B. 1989 Radiocarbon dating of the Vučedol culture complex. In Long, A., Kra, R. S. and Srdoč, D., eds., Proceedings of the 13th International 14C Conference. Radiocarbon 31(3): 1003–1009.Google Scholar
Đurdjević, M. 1987 Barice/Laminci. Ljubljana, Arheološki pregled 1986: 50–51 (in Slovenian).Google Scholar
Horvat, Z. and Mirnik, I. 1977 The Middle Age architecture of the Požega Valley. In Strbašić, M., ed., Požega, 1227–1977. Zagreb, Grafički zavod Hrvatske: 121–157. (in Croatian) Google Scholar
Horvath, F. 1982 The Late Neolithic stratum of the Gorsza tell. Archaeologiai Ertesitö 109: 201–222.Google Scholar
Horvath, F. 1986 Aspects of Late Neolithic changes in the Tisza region. Beri Balogh Adám Múzeum Evkönyve 13: 89–102.Google Scholar
Horvath, F. 1987 Hádmezövásárhely-Gorsza. A settlement of the Tisza culture. In Tálas, L., Raczky, P., Bökönyi, S., Kalicz, N., Selmeczy, L., Trogmayer, O. and Kelemen, E., eds., The Late Neolithic of the Tisza Region. Budapest-Szolnok: 31–46.Google Scholar
Krajcar Bronić, I., Horvatinčtć, N., Srdoč, D. and Obelić, B. 1986 On the initial 14C activity in karst aquifers with short mean residence time. In Stuiver, M. and Kra, R. S., eds., Proceedings of the 12th International 14C Conference. Radiocarbon 28(2A): 436–440.Google Scholar
Krajcar Bronić, I., Horvatinčtć, N., Srdoč, D. and Obelić, B. 1992 Experimental determination of the l4C initial activity of calcareous deposits. In Long, A. and Kra, R. S., eds., Proceedings of the 14th International 14C Conference. Radiocarbon, in press.Google Scholar
Langhamer, J. 1966 The chronology of Sv. Lovro church. Požieški zbornik II, Ogranak Matice hrvatske, Slavonska Požega: 149–171 (in Croatian).Google Scholar
Marčenko, E., Srdoč, D., Golubić, S., Pezdič, J. and Head, M.J. 1989 Carbon uptake in aquatic plants deduced from their natural 13C and 14C content. In Long, A., Kra, R. S. and Srdoč, D., eds., Proceedings of the 13th International 14C Conference. Radiocarbon 31(3): 785–794.Google Scholar
Milovanović, B., Stanković, S., Komatina, M., Hadžišehović, M., Župančić, M., Miljević, N., Stepić, R. and Obelić, B. 1989 Isotopic investigation of the Surdulica geothermal system. In Long, A., Kra, R. S. and Srdoč, D., eds., Proceedings of the 13th International 14C Conference. Radiocarbon 31(3): 893–901.Google Scholar
Mook, W. G. 1976 The dissolution-exchange model for dating groundwater with 14C. Interpretation of environmental isotope and hydrochemical data. Groundwater Hydrology. Vienna, IAEA: 213–225.Google Scholar
Petrović, D. 1984 Sesalačka pećina cave. Beograd, Zbornik radova Instituta za geografiju 31: 9–18 (in Serbian).Google Scholar
Srdoč, D., Breyer, B. and Sliepčević, A. 1971 Rudjer Bošković Institute radiocarbon measurements I. Radiocarbon 13(1): 135–140.Google Scholar
Srdoč, D., Krajcar Bronić, I., Horvatinčić, N. and Obelić, B. 1986a Increase of 14C activity of dissolved inorganic carbon along a river course. In Stuiver, M. and Kra, R. S., eds, Proceedings of the 12th International 14C Conference. Radiocarbon 28(2A): 515–521.Google Scholar
Srdoč, D., Obelić, B., Horvatinčić, N., Krajcar Bronić, I., Marčenko, E., Merkt, J., Wong, H. K. and Sliepčević, A. 1986b Radiocarbon dating of lake sediment from two karst lakes in Yugoslavia. In Stuiver, M. and Kra, R. S., eds, Proceedings of the 12th International 14C Conference. Radiocarbon 28(2A): 495–502.Google Scholar
Srdoč, D., Obelić, B., Horvatinčić, N., Krajcar Bronić, I. and Sliepčević, A. 1984 Rudjer Bošković Institute radiocarbon measurements VIII. Radiocarbon 26(3): 449–460.Google Scholar
Srdoč, D., Obelić, B., Horvatinčić, N., Krajcar Bronić, I. and Sliepčević, A. 1989 Rudjer Bošković Institute radiocarbon measurements XI. Radiocarbon 31(1): 85–98.Google Scholar
Srdoč, D., Obelić, B., Sliepčević, A., Krajcar Bronić, I. and Horvatinčić, N. 1987 Rudjer Bošković Institute radiocarbon measurements X. Radiocarbon 29(1): 135–147.Google Scholar
Srdoč, D., Sliepčević, A. Obelić, B. and Horvatinčić, N. 1979 Rudjer Bošković Institute radiocarbon measurements V. Radiocarbon 21(1): 131–137.Google Scholar
Stuiver, M. and Polach, H. A. 1977 Discussion: Reporting of 14C data. Radiocarbon 19(3): 355–363.Google Scholar
Stuiver, M. and Reimer, P. J. 1987 User's guide to the programs CALIB and DISPLAY Rev 2.1: Quaternary Isotope Laboratory, University of Washington.Google Scholar