Bantavanou, Panagiota. "Cremation as a Multicultural Proxy: An Integrated Osteobiographical and Literary Analysis of Cremation Practices from the Hellenistic to the Roman Period in Thessaloniki." CHS Research Bulletin 14 (2026). https://nrs.harvard.edu/URN-3:HLNC.ESSAY:107279771.
Introduction
The Timeline of Cremation in Europe
The site: Thessaloniki

Methods
Ancient Greek and Latin Literature
Osteological Material and Anthropological Methods
Light Histology

Scanning Electron Microscopy – Energy Dispersive X-ray Spectrometry (SEM-EDS)
Fourier Transform Infrared Spectrometry – Attenuated Total Reflection (FTIR-ATR)
Results
Funerary rites in ancient literature




Histological analysis
Elemental analysis
- Ca/P: indicating the crystallization level of hydroxyapatite
- C/P: indicating the intensity of cremation
- C/O: indicating the carbon oxide levels revealing the oxidation of the pyre
- Ca/O: indicating the calcium oxide produced mainly in high temperature cremations
The Kendall correlation coefficient test resulted in weak correlation of the ratios with temperature and chronological period. This result is due to the impact of the small sample size. However, observable patterns were revealed through specific ratios. The Ca/P ratio derived from the outer and inner surface resulted no correlation with temperature, however, the ratio calculated from the measurements of the inner bone revealed a difference between chronological periods. The Ca/P ratios of the Hellenistic period reveal higher variation with values indicating a diversity in the crystallization pattern, whilst in the Roman period the Ca/P ratios are concentrated around the median value indicating a more standardized pattern of low crystallization with a few exceptions (Fig. 7). A similar pattern is also observable in the case of the C/O ratio of the outer surface. Although there was no correlation with temperature, a finer insight between chronological periods revealed a diversity of C/O values in the Hellenistic period, whilst a more distinct pattern with two clusters was observed in the Roman period (Fig. 8). The C/Ca ratios revealed opposite patterns with the values from the outer surface being more diverse in the Roman times than in the Hellenistic, while the values from the inner bone were equally diverse (Fig. 9).



