Northwest Asia (49,293 – 28,578 BCE): Upper …

Years: 49293BCE - 28578BCE

Northwest Asia (49,293 – 28,578 BCE): Upper Pleistocene I — Mammoth-Steppe Foragers and Ural–Altai Corridors

Geographic and Environmental Context

Northwest Asia includes the lands from the Ural Mountains east to ~130°E, encompassing Western and Central Siberia.

  • Anchors: Ob–Irtysh steppe valleys, Altai foothills, Yenisei terraces, Ural forelands.

  • Sea levels lower, steppe–tundra extended widely across western Siberia; glaciers capped the Altai ranges.

Climate & Environmental Shifts

  • Last Glacial Maximum: cold, arid; permafrost deep; loess plains extended; river channels braided, unstable.

  • Steppe–tundra mosaics supported megafauna.

Subsistence & Settlement

  • Foragers hunted mammoth, woolly rhinoceros, bison, horse, and reindeer; riverside camps exploited fish and waterfowl.

  • Rock shelters in Altai and Minusinsk served as recurrent winter bases.

Technology & Material Culture

  • Blade–microblade industries, burins, scrapers; bone/antler points; eyed needles for tailored clothing.

  • Portable ornaments: drilled teeth, ivory beads, ochre.

Movement & Interaction Corridors

  • Ob–Irtysh–Yenisei rivers structured mobility; Altai passes linked to Mongolia; Ural forelands tied to Eastern Europe.

Cultural & Symbolic Expressions

  • Cave art in the Altai (e.g., figurative engravings); ochred burials with personal ornaments; animal figurines.

Environmental Adaptation & Resilience

  • High mobility between steppe–river–shelter zones buffered harsh winters; tailored hide clothing ensured survival.

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