A · BT · CT · DE · E · E1 · E1b · E1b1 · E1b1a · E1b1a1 · E1b1a1a · E1b1a1a1 · E-U175 · E-Z1725 · E-Z1722

Haplogroup E-Z1722

E1b1a1a1c1a (older ISOGG classification)

Macro-haplogroup
E
Parent clade
E-Z1725
Formed (estimate)
approximately 5,000–6,500 years ago
TMRCA (estimate)
around 2,200–2,800 years ago

Overview

E-Z1722 is a noteworthy downstream branch of E-Z1725 that occupies a strategic position within the male lineages of the West African forest–savanna transition belt. Emerging near the midpoint of the Holocene, E-Z1722 developed during a phase of increasing demographic complexity characterized by the growth of food-producing communities, intensifying interaction networks and the formation of proto-regional cultural clusters. Compared to the massive E-Z1724 branch, E-Z1722 shows a more structured, medium-sized phylogeny, demonstrating both regional stability and episodic expansions. Its genetic footprint highlights the interconnected histories of Nigeria, Cameroon and portions of the Lower Guinea region.

Geographic distribution

E-Z1722 is concentrated primarily in Nigeria and western Cameroon, where it appears among several Niger–Congo-speaking populations including Igbo, Yoruba, Bantoid groups and various tribes across the Cross River and Benue plateau areas. Its presence also extends, at lower but significant levels, into Equatorial Guinea, Gabon and the western edges of the Congo Basin. Some downstream clades have been detected in Central African populations, plausibly due to pre-Bantu and early Bantu-era dispersal patterns. In African diaspora datasets, E-Z1722 appears at moderate frequencies relative to E-Z1724 and E-Z2336, reflecting its mid-range regional distribution in the historic slave-trading zones.

Ancient DNA

  • Chronological analyses place the early diversification of E-Z1722 in a period marked by significant cultural transitions within West Africa, including early ironworking and expanding agricultural regimes.
  • Ancient DNA from West Africa remains limited, but archaeological and linguistic correlates suggest that groups carrying E-Z1722 were part of networks shaping early sedentary life in forest–savanna ecotones.
  • The timing of its coalescence indicates a pre-Bantu origin, with lineage structures predating the major expansions that later reshaped much of sub-Saharan paternal diversity.

Phylogeny & subclades

Within E-Z1725, E-Z1722 represents a cluster of medium complexity defined by several cleanly separated downstream branches. These subclades exhibit micro-geographical partitioning between Nigeria, Cameroon and lower Guinea, suggesting longstanding community continuity rather than rapid large-scale movement. The phylogeny combines older basal lineages with more recent expansions around the late Iron Age, coinciding with pronounced demographic growth in the wider region. While not the largest E-U175 sub-branch, E-Z1722’s internal structure makes it highly informative for fine-grained historical reconstruction.

  • E-Z1722* (basal forms, uncommon)
  • Nigerian-centered downstream clades
  • Cameroon highland and Bantoid-associated branches
  • Lower Guinea microclades reaching Gabon and Equatorial Guinea

Notes & context

E-Z1722 contributes significantly to the understanding of early population structures in West Africa before the demographic reshaping caused by Bantu expansions. Its geographic footprint mirrors linguistic and archaeological patterns of middle Holocene communities that played foundational roles in forming modern Niger–Congo cultural spheres. Although the lineage is not as widespread as some of its sister clades, its focused regional signature makes it especially useful for reconstructing internal West African demographic history.