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Chronology of the Roman Imperial Period in the Prut-Dniester Barbaricum: Insights from typology and radiocarbon dating

Published online by Cambridge University Press:  29 December 2025

Nicolai Batog*
Affiliation:
Adam Mickiewicz University – Faculty of Archaeology, Uniwersytetu Poznańskiego 7, 61-614 Poznań, Poland
*
Corresponding author: Nicolai Batog; Email: batognicolai@gmail.com
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Abstract

Archaeological investigations in the Prut-Dniester region during the Roman Imperial Period have yielded numerous Sarmatian culture necropolises and isolated graves. Establishing a precise chronology for these remains has long been a challenge due to the limitations of typological dating alone. This study integrates radiocarbon (14C) analysis of 11 human bone samples from selected funerary contexts with traditional typological methods, refining the chronological framework of the Sarmatian culture in this region. The radiocarbon analyses were subjected to Bayesian modeling, which allowed for the delineation of these samples into distinct phases, thereby adjusting and improving the periodization established through traditional methods. The results not only confirm but also refine previously established chronologies, offering deeper insights into the cultural, social, and economic dynamics of Sarmatian communities in the Prut-Dniester Barbaricum. These findings represent a significant contribution to the broader understanding of the Roman Imperial Period beyond the Eastern Limes.

Information

Type
Research Article
Copyright
© The Author(s), 2025. Published by Cambridge University Press on behalf of University of Arizona
Figure 0

Figure 1. Figure 1 long description.(a) Map of Sarmatian culture barrow graves (after Topal and Bubulici 2024) and (b) map of provenance of 14C samples from the Prut-Dniester region.

Figure 1

Figure 2. Figure 2 long description.14C data calibration graph: laboratory calibration (after AMS 14C Laboratory, Poznań).

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Table 1. The dataset presented above reflects the atomic nitrogen-to-carbon (N:C) ratios in human bone collagen from a selection of archaeological contexts in Republic of Moldova. These values are pivotal in assessing collagen preservation and, by extension, the reliability of isotopic data for paleodietary and chronological analysis. A commonly accepted threshold for well-preserved collagen is an N:C atomic ratio between 0.29 and 0.44 (DeNiro 1985). All the samples analyzed—except for Copceac T3G1, which falls below the minimum at 0.250—meet this criterion, indicating overall good collagen preservation. This reinforces the interpretive value of isotopic results from these samples. Of note is Șalvii Noi/Palanca T1G8, with N:C ratios exceeding 0.400, suggesting especially well-preserved sample, potentially reflecting good burial conditions or prompt post-mortem treatment. In contrast, Cazaclia T1G3 and Chirileni T3G11, while still within acceptable limits, hover near the lower bound and may merit cautious interpretation.Table 1 long description.

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Figure 3. Figure 3 long description.Chronological periodization of Sarmatian culture and Roman time, by different authors and their correlations (after Topal and Batog).

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Figure 4. Figure 4 long description.Plan of the barrows and graves: 1. Cazaclia T1G3 (after Agul’nikov, Kurchatov 2013); 2. Chirileni T3G11 (after Abyzova, Klochko 2005); 3. Cimișlia T8G7 (after Popovici and Ciobanu 2021); 4. Copceac T3G1 (after Bejlekchi 1990); 5. Cazaclia T20G1 (after Sava et al. 2019); 6. Hancăuți T2G3 (after Dergachev 1982); 7. Ocnița T6G12 and Ocnița T6G15 (after Manzura and Klochko 1989); 8. Taraclia Gaidabul G1 (after Sava et al. 2020); 9. Șalvirii Noi/Palanca T1G8 and G3 (after Kurchatov 1991).

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Figure 5. Figure 5 long description.Grave goods: A. Cazaclia T1G3 (after Agul’nikov and Kurchatov 2013); B. Cazaclia T20G1 (after Sava et al. Sava et al. 2019); C. Chirileni T3G11 (after Abyzova and Klochko 2005); D. Cimișlia T8G7 (after Popovici and Ciobanu 2021); E. Copceac T3G1 (after Bejlekchi 1990); F. Hancăuți T2G3 (after Dergachev 1982); G. Ocnița T6G12 (after Manzura and Klochko 1989); H. Ocnița T6G15 (after Manzura and Klochko 1989); J. Taraclia Gaidabul G1 (after Sava et al. 2020); K. Șalvirii Noi/Palanca T1G8 (after Kurchatov 1991); L. Șalvirii Noi/Palanca G3 (after Kurchatov 1991).

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Figure 6. Figure 6 long description.Summation (SUM) of radiocarbon date probabilities.

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Figure 7. Figure 7 long description.Bayesian model for delimiting the evolutionary phases of the Sarmatian culture.

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Figure 8. Figure 8 long description.Individual calibrated radiocarbon dates plotted against the IntCal20 calibration curve.

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Figure 9. Figure 9 long description.Bayesian modeling of grouped radiocarbon dates into chronological phases.

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Table 2. By applying Bayesian modeling, these intervals are refined, providing a more precise chronological framework. The modeled results place the 68.3% probability range between 73 and 119 AD, narrowing the span to 46 years, and the 95.4% probability range between 47 and 201 AD, reducing the span to 154 years. This refinement significantly enhances the accuracy of the dating, demonstrating the advantages of Bayesian statistical approaches in archaeological chronology (Table 2)Table 2 long description.

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