East Asia (49,293 – 28,578 BCE): Upper …
Years: 49293BCE - 28578BCE
East Asia (49,293 – 28,578 BCE): Upper Pleistocene I — River Plains, Exposed Shelves, and Steppe–Taiga Frontiers
Geographic & Environmental Context
At glacial lowstand (~60–90 m below present), East Asia spanned two interlocking realms that shared people, tools, and seasonal movements:
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Maritime East Asia: broad exposed shelves along the Yellow Sea, East China Sea, and Taiwan Strait; extended lower courses of the Yangtze, Yellow (Huang He), and Liao formed vast estuarine wetlands far seaward of today’s coasts. Honshu–Shikoku–Kyushu were joined into a single main Japanese island with enlarged lowlands; Taiwan was intermittently land-bridged or separated by narrow straits.
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Upper East Asia: steppe–taiga mosaics from Mongolia and the Amur–Sungari–Liao basins to Primorye and the Sea of Japan/East Sea rim. Wider coastal plains in Primorye and narrowed straits between Sakhalin–Hokkaidō–the mainland reshaped corridors for game and people.
Together, these lands offered a full spectrum of habitats—river valleys, shelf coasts, temperate forests, taiga, and open steppe—stitched by monsoon rhythms and cold-season winds.
Climate & Environmental Shifts
Glacial climate imposed strong seasonality and pulsed between cooler/drier stadials and warmer/wetter interstadials:
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Dansgaard–Oeschger warm phases: stronger summer monsoon, broadleaf forest expansion, higher river productivity, and stable estuaries.
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Heinrich/cold stadials & approach to the LGM: weakened monsoon, steppe and open woodland spread over lowlands; heavier dust flux from inland deserts; longer, colder winters in northern China and Korea.
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Regional contrast: the Amur basin remained a relatively milder corridor than the Mongolian plateaus; shelf coasts stayed productive even in cool phases.
Subsistence & Settlement
Foragers mastered dual terrestrial–aquatic economies, moving seasonally across coast–river–upland belts:
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Lowlands & coasts: hunted red deer, sika deer, boar, wild cattle; fished estuaries, tidal flats, and shelf-edge bays; collected shellfish and seaweeds in sheltered embayments.
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Uplands & interior valleys: pursued sika/red deer, elk/moose, gazelle or wild horse on steppe margins; gathered nuts, fruits, tubers during interstadials.
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Northern rivers & coasts: targeted anadromous fish (salmon runs) and marine mammals in ice-free seasons.
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Mobility: regular river-valley⇄upland⇄coastal rounds; winter aggregation near protected river benches or rock shelters; warm-season dispersal to hunt, fish, and collect plant foods.
Technology & Material Culture
Toolkits reflected both cold adaptation and aquatic specialization:
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Lithics: flake and blade industries across the south; widespread microblade complexes in the north and east for composite weapons suited to mobile hunting. Raw materials ranged from fine chert and quartzite to obsidian in the Russian Far East.
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Organic tools: bone points, gorges, barbed tips for fish and marine mammals; hide/fiber nets, traps, and probable weirs along major waterways.
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Processing & craft: grindstones for nuts/seeds, bark- and hide-working; ochre as pigment and adhesive additive; shell and tooth ornaments signaling identity and alliances.
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Clothing & shelter: tailored furs and layered garments; insulated dwellings and hearths for severe winters.
Movement & Interaction Corridors
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Shelf-coast routes linked populations along the exposed Yellow/East China Sea margins, easing movement between mainland China, Taiwan, and southern Japan.
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River corridors—especially the Yangtze and Yellow, and in the north the Amur–Liao—connected interior foragers with estuary fishers and shellfishers, enabling seasonal aggregation and exchange.
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Strait crossings narrowed between Korea and the Japanese archipelago and between Sakhalin–Hokkaidō–the mainland, allowing occasional maritime passages in favorable windows.
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Khingan passes and Primorye coast provided east–west and north–south conduits during mild summers.
Cultural & Symbolic Expressions
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Ornaments: perforated shells and animal teeth, beads, and pendants mark social ties and group identity.
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Pigment: ochre for body decoration, hide treatment, and ritual.
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Mark-making: probable early engravings/paint in caves and shelters; structured hearths and curated spaces suggest seasonal aggregation rites tied to monsoon peaks, fish runs, and game migrations.
Environmental Adaptation & Resilience
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Risk buffering: dual reliance on terrestrial hunting and aquatic foraging mitigated monsoon variability and winter scarcity.
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Seasonal scheduling: coast/river/upland alternation matched spawning runs, mast pulses, and herd movements.
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Preservation: drying/smoking of fish and meat, storage of nuts and tubers, and hide processing bridged cold seasons.
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Habitat flexibility: readiness to pivot between forest refugia, steppe edges, and estuarine flats as climates oscillated.
Toward the Last Glacial Maximum
By 28,578 BCE, East Asian foragers were fully at home in a cold, highly seasonal world—ranging across exposed shelves, great river plains, and steppe–taiga frontiers with microblade weaponry, watercraft-assisted mobility, and wide social networks.
These lifeways—broad-spectrum diets, corridor travel, cold-weather craft, and shared symbolism—formed the durable base from which Early Holocene communities would later develop low-level plant tending (proto-rice in the lower Yangtze, millet in the north) and more permanent coastal settlement as seas rose and forests recovered.
