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).
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Southern Oman (Dhofar Highlands with the khareef monsoon, al-Wusta gravel plains, Sharqiyah Desert fringes).
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The Empty Quarter (Rubʿ al-Khālī) margins in adjoining Saudi territory.
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The offshore island of Socotra in the Arabian Sea.
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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.
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Coastal plains alternated with limestone scarps and gravel plains; the Dhofar escarpments trapped Indian Ocean moisture, creating fog-fed uplands.
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Socotra lay isolated offshore, its endemic flora (dragon’s-blood trees, frankincense relatives) forming a unique biotic world, probably still uninhabited.
Climate & Environmental Shifts
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Dansgaard–Oeschger warm interstadials: monsoon strengthened, rains reached inland wadis; ephemeral streams and pasture belts expanded.
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Heinrich dry stadials: aridity dominated; dunes advanced; only perennial springs in highlands persisted; coastal productivity declined as upwelling weakened.
Subsistence & Settlement
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Highlands & wadis: Foragers hunted gazelle, ibex, and small game; gathered roots, fruits, and nuts in seasonal flushes.
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Coastal zones: Shellfish, turtle eggs, mullet, and crabs provided fallback protein in dry seasons.
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Dry-phase strategy: Mobility focused on spring-fed uplands and the richest coastal embayments.
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Socotra: no firm evidence for human presence, though transient visits in wet pulses cannot be excluded.
Technology & Material Culture
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Late Middle Paleolithic flake industries dominated, with emerging microlithic elements in wetter episodes.
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Chert/quartzite used for points and scrapers; expedient coral limestone tools along the coast.
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Organic tools (digging sticks, nets, fish traps) likely, but preservation poor.
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Use of ochre and shell beads attested regionally (Levant, Red Sea), suggesting shared symbolism.
Movement & Interaction Corridors
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Coastal corridor tied southeastern Arabia to central/eastern Arabia, passable in wetter pulses.
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Wadis linked coasts to uplands; critical routes to highland pastures.
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Maritime: Dhofar–Mahra strip may have linked by canoe to the southern Red Sea in interstadials.
Cultural & Symbolic Expressions
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Symbolism inferred from ochre and ornaments in adjacent regions.
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Seasonal aggregation likely at highland springs and productive coves.
Environmental Adaptation & Resilience
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Dual mobility (upland springs + coast) buffered variability.
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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.
