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Haplogroup E-Z1725

E1b1a1a1c1 (in some schemes)

Macro-haplogroup
E
Parent clade
E-U175
Formed (estimate)
around 6,000 to 8,000 years before present
TMRCA (estimate)
approximately 3,000 to 4,000 years ago

Overview

E-Z1725 is a major downstream branch of E-U175 and represents one of the principal paternal backbones for a wide range of West and Central African populations. Its formation falls in the middle Holocene, at a time when ecological conditions in West Africa were favorable for population growth and when early food production and more permanent settlement patterns were becoming established. The coalescence time of E-Z1725 around three to four thousand years ago places its main demographic expansion in the same broad window as the early iron working traditions and the consolidation of many Niger Congo speaking communities. This makes E-Z1725 a central clade for understanding how pre Bantu West African populations structured themselves and how later migrations carried these lineages into Central Africa and beyond.

Geographic distribution

E-Z1725 is common in a wide belt stretching from coastal West Africa into the interior of Central Africa. High frequencies are seen in Nigeria, Cameroon, Benin, Togo, Ghana and surrounding regions. The lineage also appears in populations of Gabon, the Republic of Congo and parts of the Congo Basin, often alongside other E1b1a derived haplogroups. In many West African populations, E-Z1725 and its downstream clades form a dominant or near dominant paternal component. Outside Africa, E-Z1725 is present in the African diaspora, especially in the Americas and Caribbean, reflecting the export of West and Central African males during the trans Atlantic slave trade. Subclade distributions show clear regional clustering, with some branches heavily concentrated among particular ethnic or linguistic groups within Nigeria and Cameroon.

Ancient DNA

  • Direct assignment of ancient individuals to E-Z1725 is not yet common, but the lineage's time depth and geographic focus align well with Iron Age and Late Holocene archaeological cultures in Nigeria, Cameroon and adjacent regions.
  • Patterns of haplotype diversity and branch ages indicate that E-Z1725 was already differentiated within West Africa before the full scale Bantu expansion, which later carried some of its subclades into Central Africa and occasionally further south.
  • The demographic signatures obtained from coalescent analyses suggest a period of growth that matches the spread of iron metallurgy, regional trade networks and the emergence of more complex political structures in West and Central Africa.

Phylogeny & subclades

Within E-U175, E-Z1725 forms a large subtree composed of multiple nested clades. Several of these subclades correspond to strong regional and sometimes ethnolinguistic signals. The phylogeny displays a combination of deep internal splits and recent star shaped expansions. Some branches appear to be associated primarily with populations in the Nigeria Cameroon border region, while others have extended further into Central Africa. This structure is consistent with a scenario in which a set of related lineages diversified in a West African core area and then underwent secondary expansions during the last three millennia.

  • E-Z1725* (rare basal lineages confined to parts of West Africa)
  • Regionally focused subclades that peak in Nigeria and Cameroon
  • Sub branches that extend into Gabon and the western Congo Basin
  • Several micro lineages observed in diaspora populations in the Americas

Notes & context

E-Z1725 is an important reference point for fine scale reconstructions of West and Central African demography. Many Y DNA studies that attempt to link African American or Afro Caribbean paternal lineages back to specific regions in Africa find that a significant fraction fall within E-U175 and more specifically within E-Z1725 derived clusters. The clade illustrates how late Holocene sociocultural processes, including the spread of iron technology, regional trade and the rise of centralized polities, can leave strong signatures in the Y chromosome tree. At the same time, its deep internal diversification shows that the roots of these processes reach back into earlier Holocene phases of West African prehistory.