Filters:
Location: Luoyang (Loyang) Henan (Honan) China

Maritime East Africa (28,577–7,822 BCE) Upper …

Years: 28577BCE - 7822BCE

Maritime East Africa (28,577–7,822 BCE) Upper Pleistocene II — Deglaciation, Rising Seas, and Lagoon Productivity

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–MafiaKilwa Kisiwani–Songo Mnara, the Comoros, Madagascar, Seychelles, and the Mascarene Islands.

  • 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

  • Rapid sea rise drowned terraces, creating estuaries and mangroves.

  • Offshore islands remained unpeopled.

Climate & Environmental Shifts

  • Bølling–Allerød: wetter, mangroves expanded.

  • Younger Dryas: aridity; reefs exposed.

  • Early Holocene: warm/moist stability.

Subsistence & Settlement

  • Broad diets: shellfish, fish, dugong, estuarine mollusks, turtle.

  • Coastal settlements became more fixed around lagoons.

Technology & Material Culture

  • Microlithic industries; fish gorges, harpoons.

  • Net weights suggest weirs.

Movement & Interaction Corridors

  • Coastal canoe traffic stitched lagoons; seasonal movement along Horn → Kenya.

Cultural & Symbolic Expressions

  • Shell middens served as ancestral markers.

  • Ritual feasts around fish runs.

Adaptation & Resilience

  • Dual estuary–reef strategy maintained resilience.

Transition
By 7,822 BCE, estuarine foragers built semi-sedentary shell-midden villages.

Related Events

Filter results