# Regional variability in the Acheulian to Middle Stone Age transition in southern Africa

**Authors:** A. F. Blackwood, J. Wilkins, L. J. Arnold, M. Demuro, G. Boschian, M. V. Caruana, E. F. Lalunio, M. Spate, A. Hatton, R. A. Muir, C. G. Wilson, L. J. Quick, M. Meredith-Williams, A. I. R. Herries

PMC · DOI: 10.1038/s41598-026-40075-8 · Scientific Reports · 2026-03-19

## TL;DR

This paper examines the transition from Acheulian to Middle Stone Age technologies in southern Africa, showing regional differences in timing and patterns.

## Contribution

The study provides a new stratified sequence of lithic assemblages from Amanzi Springs, revealing an earlier emergence of the Middle Stone Age in southern Africa than previously known.

## Key findings

- The Middle Stone Age emerged around 230 ± 18 ka at Amanzi Springs, earlier than previously documented along the southern coast.
- The transition from Acheulian to MSA in the southern coastal plain shows a gradual shift without clear diagnostic MSA elements in the late Acheulian.
- The study highlights regionally distinct technological trajectories in southern Africa during the Middle Pleistocene.

## Abstract

Homo sapiens emerged in Africa around 300 − 200 thousand years ago (ka). Although the earliest H. sapiens fossils are associated with the Middle Stone Age (MSA), lithic technologies considered diagnostic of the MSA have been found alongside Acheulian technology in eastern Africa and the interior of southern Africa by ~ 500 − 400 ka, suggesting a deep evolutionary history of our species in these regions. The southern coastal plain of South Africa, geographically separated from the interior by the Cape Fold Belt and Great Escarpment, has one of the best documented records of the MSA in Africa; however, only a single site is older than 125 ka and little is known about the origins of the MSA in this region. Here, we report a stratified sequence of Acheulian to MSA lithic assemblages from the open-air site of Amanzi Springs covering the period between ~ 379 to 95 ka. We show that the MSA emerged around 230 ± 18 ka, significantly earlier than previously documented along the southern coast. The pattern of technological change also differs to the interior, with no diagnostic MSA elements found in the late Acheulian, although persistent methods of flake production indicate a gradual transition and continuity into the MSA. The relatively late emergence of the MSA along the southern coast highlights the variable and complex nature of demographic and behavioural change during this period, with regionally distinct technological trajectories extending into the Middle Pleistocene in southern Africa.

The online version contains supplementary material available at 10.1038/s41598-026-40075-8.

## Linked entities

- **Species:** Homo sapiens (taxon 9606)

## Full-text entities

- **Genes:** GH1 (growth hormone 1) [NCBI Gene 2688] {aka GH, GH-N, GHB5, GHN, IGHD1A, IGHD1B}, GH2 (growth hormone 2) [NCBI Gene 2689] {aka GH-V, GHB2, GHL, GHV, hGH-V}
- **Chemicals:** MG (MESH:D008274), 87Rb (MESH:C000615483), sodium hexametaphosphate (MESH:C009285), ASP18-2 (-), HF (MESH:D006195), PVC (MESH:D011143), H2O2 (MESH:D006861), carbonates (MESH:D002254), Th (MESH:D013910), feldspar (MESH:C016447), acetone (MESH:D000096), quartz (MESH:D011791), 232Th (MESH:C000615164), humic acids (MESH:D006812), HCl (MESH:D006851), SG (MESH:C000603632), (CH3CO)2O (MESH:C031800), NaI: Tl (MESH:C477364), metal (MESH:D008670), K (MESH:D011188), sodium pyrophosphate (MESH:C003319), water (MESH:D014867), aluminium oxide (MESH:D000537), NaOH (MESH:D012972), H2SO4 (MESH:C033158)
- **Species:** Podocarpus (genus) [taxon 3363], Lycopodium (genus) [taxon 3251], Homo sapiens (human, species) [taxon 9606], Bryophyta (mosses, clade) [taxon 3208]

## Full text

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## Figures

5 figures with captions in the complete paper: https://tomesphere.com/paper/PMC13004965/full.md

## References

23 references — full list in the complete paper: https://tomesphere.com/paper/PMC13004965/full.md

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Source: https://tomesphere.com/paper/PMC13004965