A · BT · CT · DE · E · E1 · E1b1 · E1b1a · E1b1a1 · E1b1a1a · E1b1a1a1 · E-U175 · E-Z1725 · E-M191 · E-P115 · E-U290

Haplogroup E-U290

E1b1a1a1g (approximate ISOGG-like position)

Macro-haplogroup
E
Parent clade
E-P115
Formed (estimate)
around 4,500–6,000 years ago
TMRCA (estimate)
around 2,000 years ago (population-level variation applies)

Overview

E-U290 is one of the major downstream branches of E-P115 and represents a key paternal lineage that expanded widely across West Central and Central Africa. Its formation period corresponds with transitional phases between the late Holocene cultural horizons of the region and the earliest archaeological signatures associated with the Bantu expansions. E-U290 is notable for its strong representation among populations inhabiting the Congo rainforests, the northern Angolan plateau, and riverine corridors stretching from the Atlantic coast deep into Central Africa. Its phylogenetic diversity suggests a sequence of stepwise population increases rather than a single expansion wave, with regional differentiation tracking ecological and cultural boundaries.

Geographic distribution

Modern E-U290 lineages peak in Cameroon, Gabon, Equatorial Guinea and the western Congo Basin. Numerous branches continue into the Democratic Republic of the Congo, the Republic of the Congo, northern Angola and the Central African Republic. In eastern Africa, lower but consistent frequencies appear in Uganda, Rwanda, Burundi and western Tanzania, usually associated with west-to-east migrations during the Iron Age. Lineages identified in African diaspora communities across the Americas reflect embarkation patterns from West Central Africa, where E-U290 has long been a major paternal component.

Ancient DNA

  • Ancient DNA directly assigned to E-U290 remains limited, but archaeological and linguistic timelines allow its spread to be contextualised within early phases of the Bantu migration.
  • E-U290's inferred expansion matches the period when agricultural groups moved along forest–savanna ecotones and established early ironworking sites between Cameroon, Gabon and the Congo Basin.
  • Later dispersals into the Great Lakes region align with Iron Age settlement clusters and ceramic complexes that appear after 2,000 years ago.

Phylogeny & subclades

E-U290 contains several well-resolved internal branches that display strong regional signatures. West Central African clades cluster largely in Cameroon and Gabon, while central Basin branches are found predominantly in the DR Congo and Congo river region. Eastward segments of the tree form distinct clusters in the Great Lakes area. The distribution of downstream lineages suggests multiple expansions shaped by environmental corridors, especially major river systems and savanna–forest transition zones. E-U290 is phylogenetically parallel to E-Z1893 and E-Z1902, each representing a significant demographic engine within E-P115.

  • E-U290* basal lineages
  • Cameroon–Gabon Atlantic fringe branches
  • Central Congo Basin radiations
  • East-shifting branches toward Uganda / Rwanda / Burundi
  • Southern dispersal streams into Angola

Notes & context

E-U290 is a cornerstone lineage for understanding demographic transformations in Central Africa. Its expansion overlaps cultural transitions involving agriculture, metallurgy and large-scale population mobility. Despite being overshadowed by more frequently discussed branches like E-M2 or E-M191, E-U290 contains deep internal structure and region-specific clades that remain understudied due to sparse sampling in rainforest regions. Increasing whole-Y sequencing from Central African populations is expected to significantly refine the subtree.