Atlantic Southwest Europe (49,293 – 28,578 BCE):…
49293 BCE to 28578 BCE
Atlantic Southwest Europe (49,293 – 28,578 BCE): Coastal Plains, River Terraces, and Mountain Backdrops
Geographic and Environmental Context
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This subregion includes the Cantabrian coast, Galician littoral, the Minho–Douro–Tagus basins, and inland valleys up to the foothills of the Cantabrian Mountains and northern Portuguese ranges.
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Sea levels ~60–90 m lower exposed broad Atlantic shelves, extending estuaries and deltas far seaward.
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Landscapes blended coastal plains, deeply incised river valleys, and upland foothills that offered shelter and vantage.
Climate and Environmental Shifts
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Marked by Dansgaard–Oeschger warm phases and Heinrich cold/dry pulses.
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Interstadials: milder, with deciduous woodland (oak, hazel) expanding in sheltered valleys; rivers ran higher; wetlands and riparian zones flourished.
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Stadials: cooler, drier; steppe–tundra and open grassland spread; loess accumulated in leeward valleys; storm intensity along the Atlantic margin increased.
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Overall cooling trend reduced growing seasons and shifted plant/animal ranges downslope.
Subsistence and Settlement
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Coastal and estuarine foraging: shellfish, estuarine fish, and migratory birds; occasional exploitation of beached marine mammals.
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Open-country hunting: red deer, horse, bison, and ibex; reindeer more common in colder stadials.
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Rivers and terraces provided salmon, eel, and riparian plant foods in season.
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Seasonal mobility linked upland hunting grounds in summer with coastal and lowland foraging areas in winter.
Technology and Material Culture
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Upper Paleolithic blade industries, with endscrapers, burins, backed points; later in the interval, microblades for composite hunting weapons appear.
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Flint sources in Cantabria, Galicia, and northern Portugal distributed through exchange; quartzite and other local stones also widely used.
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Bone and antler tools included barbed points, needles, and ornaments.
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Ochre use and shell beads signal symbolic continuity.
Movement and Interaction Corridors
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Atlantic coastal corridor connected Cantabria, Galicia, and Portugal, enabling long-range exchange and movement without crossing high mountain barriers.
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River valleys (Douro, Minho, Tagus) acted as natural east–west travel routes into the Iberian interior.
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Cultural and lithic parallels suggest contact with Mediterranean Southwest Europe and Atlantic West Europe.
Cultural and Symbolic Expressions
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Coastal caves and rock shelters show repeated occupation and symbolic activity—engraving, pigment use, ornament production.
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Portable art and decorated bone tools indicate shared symbolic traditions with other parts of Upper Paleolithic Iberia.
Environmental Adaptation and Resilience
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Ecotone exploitation—coastal, riverine, and upland habitats—ensured a steady flow of resources across seasons.
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Risk reduction through dietary breadth and stored high-fat foods (marrow, dried meat) during cold phases.
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Mobility patterns allowed quick shifts between zones in response to climatic fluctuations.
Toward the Last Glacial Maximum
By 28,578 BCE, Atlantic Southwest European foragers maintained a flexible network of coastal refugia, river corridors, and upland hunting zones, enabling them to endure increasingly harsh winters and shortened growing seasons as the LGM approached.