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.
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Anchors: Ob–Irtysh steppe valleys, Altai foothills, Yenisei terraces, Ural forelands.
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Sea levels lower, steppe–tundra extended widely across western Siberia; glaciers capped the Altai ranges.
Climate & Environmental Shifts
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Last Glacial Maximum: cold, arid; permafrost deep; loess plains extended; river channels braided, unstable.
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Steppe–tundra mosaics supported megafauna.
Subsistence & Settlement
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Foragers hunted mammoth, woolly rhinoceros, bison, horse, and reindeer; riverside camps exploited fish and waterfowl.
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Rock shelters in Altai and Minusinsk served as recurrent winter bases.
Technology & Material Culture
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Blade–microblade industries, burins, scrapers; bone/antler points; eyed needles for tailored clothing.
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Portable ornaments: drilled teeth, ivory beads, ochre.
Movement & Interaction Corridors
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Ob–Irtysh–Yenisei rivers structured mobility; Altai passes linked to Mongolia; Ural forelands tied to Eastern Europe.
Cultural & Symbolic Expressions
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Cave art in the Altai (e.g., figurative engravings); ochred burials with personal ornaments; animal figurines.
Environmental Adaptation & Resilience
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High mobility between steppe–river–shelter zones buffered harsh winters; tailored hide clothing ensured survival.
