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CULTURE, PERIOD OR STYLE? RECONSIDERATION OF EARLY AND MIDDLE COPPER AGE CHRONOLOGY OF THE GREAT HUNGARIAN PLAIN

Published online by Cambridge University Press:  21 January 2021

Zsuzsanna Siklósi*
Affiliation:
Institute of Archaeological Sciences, Eötvös Loránd University, H-1088 Budapest, Múzeum körút 4/B, Hungary
Márton Szilágyi
Affiliation:
Gemeinde Oberschneiding, Pfarrer-Handwercher-Platz 4, 94363 Oberschneiding, Lower Bavaria, Germany; and Institute of Archaeological Sciences, Eötvös Loránd University, H-1088 Budapest, Múzeum körút 4/B, Hungary
*
*Corresponding author. Email: siklosi.zsuzsanna@btk.elte.hu.
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Abstract

The main goal of our research project was to date the Early and Middle Copper Age (4500/4450–3800 cal BC) of the Great Hungarian Plain more precisely. In our project, we took samples for accelerator mass spectrometry (AMS) dating from both settlement features and burials, and the data were analyzed using Bayesian modeling. We examined the Early and Middle Copper Age finds of the Great Hungarian Plain on several levels (site, microregional, and regional levels) using a bottom-up approach. The AMS measurements were supplemented by statistics-based pottery analysis in order to make our understanding of the relationship between the Tiszapolgár and Bodrogkeresztúr cultures more detailed. As a result, we can see a significant, 130 (68.2%) 230 years overlap between the two types of find assemblages, which contradicts to the earlier accepted chronological sequences created by the traditional culture-historical approach. According to the stylistic analyzes, the two ceramic styles are not clearly distinguishable.

Information

Type
Research Article
Creative Commons
Creative Common License - CCCreative Common License - BYCreative Common License - NCCreative Common License - ND
This is an Open Access article, distributed under the terms of the Creative Commons Attribution-NonCommercial-NoDerivatives licence (http://creativecommons.org/licenses/by-nc-nd/4.0/), which permits non-commercial re-use, distribution, and reproduction in any medium, provided the original work is unaltered and is properly cited. The written permission of Cambridge University Press must be obtained for commercial re-use or in order to create a derivative work.
Copyright
© 2021 by the Arizona Board of Regents on behalf of the University of Arizona
Figure 0

Table 1 New AMS radiocarbon dates measured in this project from ECA and MCA sites and their archaeological context. δ13C values of the Poznan Radiocarbon Laboratory cannot be used for palaeoecological reconstructions because of the method of sample preparation.

Figure 1

Table 2 Posterior density estimates for the start and end of different sites, and the estimated span of activity on ECA and MCA sites. For local model see Appendix 1, for regional model see Appendix 2. All probability distribution is given in 68.2% probability.

Figure 2

Figure 1 Map of the sites discussed in the text. 1. Barca Baloty, 2. Berettyóújfalu-Berettyólapos-Sertéshízlalda, 3. Berettyóújfalu-Szilhalom, 4. Csongrád-Kettőshalom, 5. Hajdúböszörmény-Ficsori-tó, 6. Jászberény-Borsóhalom, 7. Körösladány-Bikeri, 8. Kunszentmárton-Pusztaistvánháza, 9. Malé Raškovce, 10. Polgár-Királyér-part site 1, 11. Polgár-Nagy-Kasziba, 12. Polgár-Bacsókert, 13. Pusztataskony-Ledence, 14. Rákóczifalva-Bagi föld site 8, 15. Rákóczifalva-Bivaly-tó site 1/a, 16. Rákóczifalva-Bivaly-tó site 1/c, 17. Tiszalúc-Sarkad, 18. Tiszapolgár-Basatanya, 19. Tiszavalk-Tetes, 20. Uivar, 21. Vésztő-Bikeri, 22. Vésztő-Mágor, 23. Vinča-Belo Brdo.

Figure 3

Figure 2 Map of the excavation in Polgár-Királyér-part highlighting the AMS-dated features.

Figure 4

Figure 3 Map of the excavation in Rákóczifalva-Bagi föld site 8 highlighting the AMS-dated features.

Figure 5

Figure 4 Map of the excavation in Rákóczifalva-Bivaly-tó site 1/a highlighting the AMS-dated features.

Figure 6

Figure 5 Map of the excavation in Rákóczifalva-Bivaly-tó site 1/c highlighting the AMS-dated features.

Figure 7

Table 3 Radiocarbon dates from ECA and MCA sites and their archaeological context discussed in the study. δ13C values of the Poznan Radiocarbon Laboratory cannot be used for palaeoecological reconstructions because of the method of sample preparation.

Figure 8

Figure 6 Probability distributions of radiocarbon dates from Hunyadihalom sites. The square brackets on the left side along with the OxCal keywords exactly define the model.

Figure 9

Figure 7 The difference obtained between the estimated start of the Bodrogkeresztúr style and the end of the Tiszapolgár style.