Temperate Southern Africa (49,293 – 28,578 …
Years: 49293BCE - 28578BCE
Temperate Southern Africa (49,293 – 28,578 BCE) Upper Pleistocene I — Strandlopers, Rock-Shelter Foragers, and Grassland Hunts
Geographic and Environmental Context
Temperate Southern Africa includes:-
South Africa (Cape littoral, Highveld, Drakensberg, Karoo, Namaqualand).
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Lesotho and Eswatini.
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Most of Namibia and Botswana, except the far northern sectors (Caprivi, Etosha, Okavango, Skeleton Coast — those are in Tropical Southern Africa).
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Southern Zimbabwe and southwestern Mozambique (Maputo–Limpopo region).
Anchors: Cape littoral & fynbos, Drakensberg–Lesotho massif, Highveld grasslands (Witwatersrand, Free State), Namaqualand semi-desert, Kalahari southern margins, Great Karoo, Maputo–Limpopo basins, southern Zimbabwe plateau (Great Zimbabwe heartland).
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At the Last Glacial Maximum (LGM), sea level ~100 m lower, exposing wide Cape coastal plains.
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Highveld grasslands spread in cooler, drier climate; Karoo semi-arid.
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Drakensberg slopes glaciated in places.
Climate & Environmental Shifts
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Colder, drier; reduced rainfall inland, though fynbos adapted to aridity persisted along the Cape.
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Larger ungulates roamed exposed coastal plains and grasslands.
Subsistence & Settlement
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Foragers exploited shellfish, seals, penguins, seabirds along coast.
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Grassland hunters targeted zebra, wildebeest, and springbok; ostrich eggs for protein and water storage.
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Rock shelters in Cederberg and Drakensberg served as refugia.
Technology & Material Culture
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Stone flake and blade industries (Late Middle Stone Age traditions).
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Bone points, hide scrapers; ochre used decoratively.
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Ostrich eggshell beads widely produced.
Movement & Interaction Corridors
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Cape–Karoo–Namaqualand coast as continuous forager highway.
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Drakensberg passes provided seasonal access to highland hunting grounds.
Cultural & Symbolic Expressions
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Early rock art motifs may have begun in Cederberg shelters.
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Ochre symbolic use in burials and body paint.
Environmental Adaptation & Resilience
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Coast–inland seasonal mobility buffered climatic extremes.
Transition
By 28,578 BCE, foragers of temperate southern Africa had forged coastal–grassland dual lifeways with symbolic depth
