Maritime East Africa (49,293–28,578 BCE) Upper Pleistocene …
Years: 49293BCE - 28578BCE
Maritime East Africa (49,293–28,578 BCE) Upper Pleistocene I — Lowstand Shores, Forager Refugia, and Reef Flats
Geographic and Environmental Context
Maritime East Africa includes littoral and nearshore islands from Somalia through Kenya and Tanzania to northern/central Mozambique and southern Malawi, plus Lamu–Pate–Mombasa, Zanzibar–Pemba–Mafia, Kilwa Kisiwani–Songo Mnara, the Comoros, Madagascar, Seychelles, and the Mascarene Islands.
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Anchors: Lamu archipelago, Mombasa–Kilifi, Zanzibar–Pemba–Mafia, Kilwa Kisiwani–Songo Mnara, Comoros (Ngazidja, Nzwani, Mwali), Madagascar highlands/coasts, Seychelles/Mascarene atolls.Sea level ~100 m lower, exposing broad Somali–Kenyan–Tanzanian shelves
- Sea level ~100 m lower, exposing broad Somali–Kenyan–Tanzanian shelves.
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Lagoons diminished; tidal flats and coral benches stretched far offshore.
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Madagascar isolated but unpeopled; Seychelles/Mascarene uninhabited volcanic/atoll systems.
Climate & Environmental Shifts
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LGM: cooler, drier, but upwelling supported marine productivity.
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Inland savannas contracted; mangroves shrank.
Subsistence & Settlement
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Littoral foragers in Somalia/Kenya harvested shellfish, crabs, turtles.
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Fish taken in estuaries; dugouts possible in rivers.
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No Madagascar/Seychelles/Mascarene settlement.
Technology & Material Culture
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Flake–core stone tools; shell scrapers; bone points.
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Beads from shell/ostracods.
Movement & Interaction Corridors
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Seasonal shuttles between estuaries and reefs; Red Sea/Horn linked culturally.
Cultural & Symbolic Expressions
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Early shell beads/ochre body paint indicate symbolic networks.
Environmental Adaptation & Resilience
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Mobility along coast buffered aridity; fallback on reefs.
Transition
By 28,578 BCE, a durable littoral foraging adaptation persisted along the coast, absent offshore settlement.
