Southeast Arabia (49,293 – 28,578 BCE) …

Years: 49293BCE - 28578BCE

Southeast Arabia (49,293 – 28,578 BCE) Upper Pleistocene I — Monsoon Margins, Highland Refugia, and Desert Shelves

Geographic and Environmental Context

Southeast Arabia covers the southern and eastern margins of the Arabian Peninsula:
  • Eastern Yemen (Hadhramaut, eastern Aden interior, al-Mahra).

  • Southern Oman (Dhofar Highlands with the khareef monsoon, al-Wusta gravel plains, Sharqiyah Desert fringes).

  • The Empty Quarter (Rubʿ al-Khālī) margins in adjoining Saudi territory.

  • The offshore island of Socotra in the Arabian Sea.

  • Anchors: Wādī Ḥaḍramawt–Shibam–Tarim, Dhofar escarpments (Ẓafār/Al-Balīd, Mirbat), al-Mahra dunes, al-Wusta plains, Sharqiyah sands, Socotra’s Hagghier Mountains and dragon’s-blood groves.

  • Coastal plains alternated with limestone scarps and gravel plains; the Dhofar escarpments trapped Indian Ocean moisture, creating fog-fed uplands.

  • Socotra lay isolated offshore, its endemic flora (dragon’s-blood trees, frankincense relatives) forming a unique biotic world, probably still uninhabited.

Climate & Environmental Shifts

  • Dansgaard–Oeschger warm interstadials: monsoon strengthened, rains reached inland wadis; ephemeral streams and pasture belts expanded.

  • Heinrich dry stadials: aridity dominated; dunes advanced; only perennial springs in highlands persisted; coastal productivity declined as upwelling weakened.

Subsistence & Settlement

  • Highlands & wadis: Foragers hunted gazelle, ibex, and small game; gathered roots, fruits, and nuts in seasonal flushes.

  • Coastal zones: Shellfish, turtle eggs, mullet, and crabs provided fallback protein in dry seasons.

  • Dry-phase strategy: Mobility focused on spring-fed uplands and the richest coastal embayments.

  • Socotra: no firm evidence for human presence, though transient visits in wet pulses cannot be excluded.

Technology & Material Culture

  • Late Middle Paleolithic flake industries dominated, with emerging microlithic elements in wetter episodes.

  • Chert/quartzite used for points and scrapers; expedient coral limestone tools along the coast.

  • Organic tools (digging sticks, nets, fish traps) likely, but preservation poor.

  • Use of ochre and shell beads attested regionally (Levant, Red Sea), suggesting shared symbolism.

Movement & Interaction Corridors

  • Coastal corridor tied southeastern Arabia to central/eastern Arabia, passable in wetter pulses.

  • Wadis linked coasts to uplands; critical routes to highland pastures.

  • Maritime: Dhofar–Mahra strip may have linked by canoe to the southern Red Sea in interstadials.

Cultural & Symbolic Expressions

  • Symbolism inferred from ochre and ornaments in adjacent regions.

  • Seasonal aggregation likely at highland springs and productive coves.

Environmental Adaptation & Resilience

  • Dual mobility (upland springs + coast) buffered variability.

  • Broad-spectrum diets combining marine and terrestrial foods ensured survival.

Transition

By 28,578 BCE, Southeast Arabian groups had stabilized a coastal–highland adaptive cycle, enabling persistence in one of the world’s driest inhabited frontiers.

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