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Haplogroup R-L389

Macro-haplogroup
R
Parent clade
R-L754
Formed (estimate)
c. 16,000 - 20,000 years before present (estimate)
TMRCA (estimate)
c. 13,000 - 17,000 years ago (estimate)

Overview

Haplogroup R-L389 is a crucial early branch of R1b and represents the stage at which the R1b lineage began to diversify into the major forms known today. L389 is often referred to as one of the key transitional markers that connects the oldest R1b lineages, such as R-L278 and R-PH155, to the younger and more widespread branches including R-P297 and the later expansions of R-M269. As such, R-L389 is a pivotal node that anchors the deep evolutionary structure of R1b. During the period when R-L389 was diversifying, Upper Paleolithic and early Holocene populations across western Asia, the Caucasus and eastern Europe were undergoing demographic and ecological shifts driven by climate change. Groups carrying L389 likely belonged to mobile hunter gatherer communities that moved seasonally across steppe and forest steppe environments. These populations later gave rise to distinct branches associated with different regions of Eurasia. The later descendants of L389 include the major radiations of R1b that spread across Europe during the Neolithic and Bronze Age, as well as the smaller early Asian branches such as M73 and M478. The presence of L389 in early steppe populations is supported by its close relationship to lineages appearing in ancient genomes from the Pontic Caspian zone.

Geographic distribution

Today, L389 is rarely seen as a basal lineage. Most L389 derived individuals fall into downstream branches such as R-P297 and R-M269. Modern traces of basal L389 occur at very low frequency in the Caucasus, eastern Anatolia and parts of the Near East.

Ancient DNA

  • Many Mesolithic and early Neolithic individuals in eastern Europe that carry early R1b lineages ultimately descend from L389.
  • Ancient DNA from the Caucasus and the steppe shows early R1b presence consistent with L389 intermediate stages.
  • The widespread European R-M269 lineage traces back through L389, making this node essential for modeling Bronze Age expansions.

Phylogeny & subclades

R-L389 divides into two major branches: R-P297, the ancestor of the large western and central Eurasian expansions, and rare basal R-L389* lineages. It forms the structural transition between the deep Paleolithic R1b lineages and the later widespread expansions.

  • R-P297
  • R-L389* (very rare retained upstream variants)

Notes & context

L389 is the backbone node linking ancient R1b diversity with later widespread branches. Its placement is critical for a complete representation of early R1b structure.