Hostname: page-component-78c5997874-j824f Total loading time: 0 Render date: 2024-11-03T01:29:50.775Z Has data issue: false hasContentIssue false

Dating of Total Soil Organic Matter Used in Kurgan Studies

Published online by Cambridge University Press:  18 July 2016

M Molnár*
Affiliation:
Institute of Nuclear Research of the Hungarian Academy of Sciences (INR/HAS), Laboratory of Environmental Studies, H-4026 Debrecen, Bem tér 18/c, Hungary.
K Joó
Affiliation:
Szent István University, Department of Landscape Ecology H-2103 Gödöllo Páter Károly u l., Hungary.
A Barczi
Affiliation:
Szent István University, Department of Landscape Ecology H-2103 Gödöllo Páter Károly u l., Hungary.
Zs Szántó
Affiliation:
Institute of Nuclear Research of the Hungarian Academy of Sciences (INR/HAS), Laboratory of Environmental Studies, H-4026 Debrecen, Bem tér 18/c, Hungary.
I Futó
Affiliation:
Institute of Nuclear Research of the Hungarian Academy of Sciences (INR/HAS), Laboratory of Environmental Studies, H-4026 Debrecen, Bem tér 18/c, Hungary.
L Palcsu
Affiliation:
Institute of Nuclear Research of the Hungarian Academy of Sciences (INR/HAS), Laboratory of Environmental Studies, H-4026 Debrecen, Bem tér 18/c, Hungary.
L Rinyu
Affiliation:
Institute of Nuclear Research of the Hungarian Academy of Sciences (INR/HAS), Laboratory of Environmental Studies, H-4026 Debrecen, Bem tér 18/c, Hungary.
*
Corresponding author. Email: [email protected].
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 investigated Csípo-halom, one of the kurgans that served as a burial place in the Hortobágy area of the Hungarian Great Plain. For pedological description and other studies of the protected mound and its surroundings, only a few monitoring drillings were permitted to get soil samples. On the basis of morphological and visual studies, the structure and layers of the mound were reconstructed. The Laboratory of Environmental Studies of the Institute of Nuclear Research at the Hungarian Academy of Sciences (INR/HAS) performed radiocarbon measurements of soil samples, applying a bulk combustion pretreatment method. The measured 14C ages of soil samples from reference points, such as the top layer of the mound, the center of mound body, the base layer of the mound, the near surroundings, and the distant surroundings, are in good agreement with the preliminary archaeological concept for this field and give substantial information about the rate of soil generation processes in this area.

Type
Articles
Copyright
Copyright © 2004 by the Arizona Board of Regents on behalf of the University of Arizona 

References

Alexandrovskiy, AL. 1996. Natural environment as seen in soil. Eurasian Soil Science 29(3):277–87.Google Scholar
Alexandrovskiy, AL, van der Plicht, J, Belinskiy, AB, Khokhlova, OS. 2001. Chronology of soil evolution and climatic changes in the dry steppe zone of the Northern Caucasus, Russia, during the 3rd millennium BC. Radiocarbon 38(2):629–35.Google Scholar
Birks, HJ, Birks, HH. 1980. Quaternary Palaeoecology. London: E. Arnold Press. 297 p.Google Scholar
Csongor, É, Szabó, I, Hertelendi, E. 1982. Preparation of counting gas of proportional counters for radiocarbon dating. Radiochemical and Radioanalytical Letters 55:303.Google Scholar
Gennadiev, AN, Ivanov, IV. 1989. Generation of soil and palaeopedology: problems, conceptions, and methodology. Pocsvovedenije 10(1):3443. In Russian.Google Scholar
Hertelendi, E, Csongor, É, Záborszky, L, Molnár, J, Dajkó, G, Györffi, M, Nagy, S. 1989. A counter system for high-precision 14C dating. Radiocarbon 31(1):399406.Google Scholar
Kalicz, N. 1970. Claygods. The Memories of Age of Neolithic and Brass in Hungary. Budapest: Corvina Kiaddó. 4858. In Hungarian.Google Scholar
Kovács, T. 1977. Bronze Age in Hungary. Budapest: Corvina Kiadó. p 51–6. In Hungarian.Google Scholar
Magyari, E, Sümegi, P, Braun, M, Jakab, G, Molnár, M. 2001. Retarded wetland succession: anthropogenic and climatic signals in a Holocene peat bog profile from northeast Hungary. Journal of Ecology 89:1019–32.Google Scholar
Pessenda, LC, Gouveia, SE, Aravena, R. 2001. Radiocarbon dating of total soil organic matter and humin fraction and its comparison with 14C ages of fossil charcoal. Radiocarbon 38(2):595601.Google Scholar
Stuiver, M, Reimer, PJ, Bard, E, Beck, JW, Burr, GS, Hughen, KA, Kromer, B, McCormac, G, van der Plicht, J, Spurk, M. 1998. INTCAL98 radiocarbon age calibration, 24,000-0 cal BP Radiocarbon 40(3):1041–83.Google Scholar
Tóth, A. 1999. Cumanian Mounds. Kisújszállás: Alföldkutatásért Alapítvány Kiadványa. 77 p. In Hungarian.Google Scholar