South Central Europe (4,365 – 2,638 BCE)…
4365 BCE to 2638 BCE
South Central Europe
(4,365 – 2,638 BCE) Late Neolithic/Chalcolithic — Pile-Dwelling Fluorescence, Copper Trails, and Alpine Clearances
Geographic and Environmental Context
Western Southeast Europe includes southern and western Austria (including Carinthia; excluding Salzburg), Liechtenstein, Switzerland (excluding Basel and the eastern Jura), southeastern Swabia (southeastern Baden-Württemberg), and southwestern Bavaria.-
Anchors: Cortaillod–Pfyn–Horgen lake villages; Valais copper nodes; Inn–Tyrol upland clearances; Carinthia alpine forelands.
Climate & Environmental Shifts
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Stable with cool pulses; wetlands expanded/contracted with lake-level swings.
Subsistence & Settlement
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Pile-dwellings proliferated with orchards/gardens; dairying intensified; upland summer pastures (transhumance).
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Copper exploited in Valais–Grisons–Tyrol; exchange reached the plateau.
Technology & Material Culture
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Corded wares and Bell Beaker influences late; copper pins, daggers; flint mining/trade; fiber/textile advances.
Movement & Interaction Corridors
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Pass traffic in copper and prestige goods (amber, axes) increased; Rheintal–Gotthard–Brenner triad integrated north–south.
Cultural & Symbolic Expressions
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Wetland votives (antler, ceramics); burial differentiation suggests rank.
Groups
Topics
Neolithic Europe
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Neolithic Subpluvial, or Holocene climatic optimum, or Holocene Wet Phase
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Older Peron Transgression during the Neolithic Subpluvial
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5.9 kiloyear event during the Neolithic Subpluvial
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Subboreal Period during the Neolithic Subpluvial
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Piora Oscillation ending the Neolithic Subpluvial
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Subboreal Period
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