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Kintampo Complex

Early West African complex

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  • 4 chapters

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Through Pastoralism, Ghana and Building

Origin

Watson (2005) states:

Based on excavation and archaeological data from the Sahara, Sahel, and southern West Africa, this article proposes a migration model as explanation for the distinctive discontinuity signalled by the appearance of the Kintampo Tradition between 3,600 bp-3,200 bp and the origin of food production in the forest/forested zone, similar to the event envisaged by DAVIES (1966, 1980). Distinctions between the pottery of the Kintampo and indigenous Punpun foragers are a critical element of this argument, as fundamental stylistic and, especially, technological differences observed correspond to social and/or ethnic boundaries documented in ethnoarchaeological studies. Combined with evident similarities in Kintampo material culture and economy with contemporaneous groups in the Sahel, and the lack of any convincing evidence for an indigenous syncretic development within the savanna-forest/forest zone, this strongly suggests that the Kintampo was an intrusive population. The Punpun and Kintampo Traditions were two distinct socio-economic groups whose co-occupation of central Ghana signals the meeting of two different' worlds', represented by the 'Saharan derived' agro-pastoralists from the Sahel, who brought with them the values/technologies associated with food production (e.g. social differentiation), which eventually dominated a landscape that had been previously occupied solely by 'southern' hunter-gatherers.

Champion et al. (2022) state:

The cultivation of pearl millet diffused from the desiccating West and Central Sahara into the West African savanna zone after 2500 cal bc, in the context of southwards population movements (Ozainne et al. 2014; Neumann 2018; Fuller et al. 2021). Previously published evidence proposed three main branches of pearl millet diffusion, based on archaeobotanical data (Neumann 2018; Champion 2020; Fuller et al. 2021), but also on recent genetic studies (Oumar et al. 2008; Burgarella et al. 2018) and archaeological data (Ozainne et al. 2009, 2014). The two best documented are a western branch from Tichitt/Mauritania, after 2000 cal bc (Fuller et al. 2007; MacDonald et al. 2009), and a central branch from Tilemsi/Mali, after 2500 cal bc (Manning et al. 2011). Pearl millet cultivation spread quickly throughout the Niger River Basin, from the Tilemsi Valley in Mali to northern Burkina Faso (Tin-Akof, Oursi West) and to the rainforest of Ghana [4. Kintampo B-Sites and 14. Bosumpra Cave] between 2500 and 1000 cal bc (Fig. 8).

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