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Haplogroup N2a2

N2a2-Y111068

Macro-haplogroup
K
Parent clade
N2a
Formed (estimate)
c. 8,000 - 11,000 years before present
TMRCA (estimate)
c. 2,500 - 4,500 years ago

Overview

N2a2 is a sister branch to N2a1 and represents the western and northwestern European extension of the rare N2a-P189.2 complex. While N2a1 is focused on the Balkans and Anatolia, N2a2 is characterized by lineages in Atlantic western Europe and adjacent parts of central Europe, indicating that a subset of the N2a paternal pool followed more westerly routes during the Bronze and Iron Ages. The clade likely formed among groups already carrying N2a in the north Eurasian or steppe sphere but became established in western Europe through small founder events, perhaps involving movements along the Danube, through the Carpathian basin and into central and Atlantic Europe. Its modest time depth and low overall frequency imply that N2a2 never underwent a large scale demographic expansion, instead persisting in small local lineages that survived various historical population turnovers.

Geographic distribution

Modern N2a2 lineages are best documented in western Europe, including individuals from France (for example in the Charente Maritime region) and the British Isles, as well as in Russia (Moscow region) and Turkey. This distribution suggests a chain of westward dispersals from the north Pontic or Balkan zones followed by localized founder effects in Atlantic communities. The presence of N2a2 in populations that otherwise carry typical western European Y lineages such as R1b-M269, I1 and I2a points to a minor, often cryptic component of paternal ancestry. In genealogical projects N2a2 generally appears as isolated family clusters rather than broad regional peaks, reinforcing the interpretation of a rare lineage that has been carried forward by a small number of paternal lines across time.

Ancient DNA

  • The overall N-P189.2 signal in ancient genomic datasets, including Botai and steppe related individuals, provides indirect support for an early presence of the wider N2a complex in north central Eurasia, from which N2a2 later diverged.
  • The western European occurrences of N2a2 are consistent with low level input from steppe or Balkan related groups into Atlantic Europe during the Bronze and Iron Ages, although no ancient individual has yet been directly assigned to N2a2-Y111068.
  • The combination of modern evidence and archaeological pathways suggests that N2a2 spread westward along existing cultural and trade networks rather than through a stand alone migration event.

Phylogeny & subclades

N2a2 is defined by Y111068 and further subdivides into younger branches including N2a2a (FT352925) and N2a2b (Y101945). Present day lineages under these nodes show very shallow coalescence times, typically within the last two to three millennia, consistent with small family based expansions. Within the N2 tree, N2a2 forms a mirror to N2a1: both branches derive from P189.2 but track different directions of dispersal. Whereas N2a1 is embedded in southeast European and Anatolian contexts, N2a2 highlights west European reception of rare N2a ancestry. This makes N2a2 particularly interesting for fine scale Y DNA projects in Atlantic Europe, where it can reveal subtle connections to steppe and Balkan genetic threads that are not obvious from autosomal data alone.

  • N2a2* (scattered basal lineages in western and central Europe)
  • N2a2a-FT352925 (documented in France and Turkey, reflecting a southern Atlantic Mediterranean corridor)
  • N2a2b-Y101945 (United Kingdom and Moscow region branch indicating central and north European dispersal)
  • Private terminal N2a2 lineages in individual families across western Europe

Notes & context

Because N2a2 is extremely rare in most surveyed populations, its reconstruction relies heavily on whole Y sequencing and detailed project level data. For personal ancestry, membership in N2a2 usually indicates a paternal line that has traversed multiple historical layers of European population history while preserving a deep connection to the north Eurasian P189.2 stem.