Macedonia: Iron Age Echoes

The Macedonia_IA individuals—dated between 900 and 489 BCE—come from a cluster of inland and lakeshore sites in present‑day North Macedonia: Bucinci and Govrlevo near Skopje, Lisicin Dol (Marvinci, Valandovo), Plaosnik at Ohrid, and Vodovratski Pat / V. Vodovrati‑Gradsko. Archaeological data indicates these communities formed in the wake of Late Bronze Age transformations and the wider Iron Age cultural reorganization of the central Balkans.

Material traces from the region show a mixture of local continuity and external contacts: pottery styles, metalwork, and settlement morphology reflect influences from neighboring Thracian and Greek worlds along with persistent local traditions. Limited evidence suggests funerary practices vary by site, with primary inhumations and tomb architecture attesting to community differentiation. While the 14 sampled individuals offer a tangible window into emergence patterns, their geographic clustering and modest sample size mean interpretations about population origins should remain cautious. Genome‑scale data beyond mitochondrial haplotypes would better resolve the timing and source of any incoming ancestries versus long‑term local continuity.

Mitochondrial DNA from the Macedonia_IA assemblage shows a dominance of haplogroups commonly found across Europe since the Neolithic: H (3) and K (3), with additional lineages J (2), U (2), and T2b (1). These maternal markers align with a mixed ancestry profile seen elsewhere in the Balkans: strong continuity of Neolithic farmer–related lineages (H, K, J, T) together with remnants of older European hunter‑gatherer lineage U. Such a composition is consistent with archaeological expectations of long‑term local descent with periodic inputs from neighboring regions.

No consistent, high‑confidence Y‑chromosome pattern is reported across the 14 samples in the dataset, so paternal lineage dynamics remain unresolved here. Genome‑wide autosomal data would be required to quantify contributions from Steppe‑related, Anatolian farmer, and Mesolithic components for this population. Note that although 14 individuals provide meaningful signals, they are geographically clustered; therefore, genetic inferences are moderately informative but should be treated as provisional pending broader sampling. Future samples from more sites and explicit Y‑DNA reporting will clarify male‑line continuity, migration events, and affinities with contemporary and later populations in the Balkans.