Southern Australasia (49,293–28,578 BCE) Southern Australasia …
Years: 49292BCE - 28578BCE
Southern Australasia (49,293–28,578 BCE)
Southern Australasia includes central and southern Australia (southern WA and NT margins; central/southern Queensland; NSW, Victoria, South Australia, Tasmania) + New Zealand’s South Island and SW North Island coast.
Anchors: Willandra Lakes–Mungo, Murray–Darling basin, Bassian Plain (Australia–Tasmania land bridge), Nullarbor–Eyre, Flinders Ranges, Gippsland coasts, NZ South Island Alps & Canterbury/Otago plains.
Geographic & Environmental Context
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LGM sea-level fall exposed the Bassian Plain, joining Tasmania to mainland Australia; vast coastal shelves expanded.
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Interior: dune fields and salt lakes proliferated; Willandra lake system alternated levels.
Climate & Environmental Shifts
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Cooler/drier; westerlies displaced; interior aridity intensified; alpine glaciation in NZ South Island; snowlines lower in mainland ranges.
Subsistence & Settlement
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Australia: Humans present long before 49 ka; by this epoch, Pleistocene foragers occupied deserts, riverine corridors, coasts, and lakeshores.
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Willandra Lakes: fishing, waterfowl, marsupials; cremation/burial traditions (Mungo).
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Coasts & shelves: shellfish, fish, pinnipeds, beached whales; plant geophytes.
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New Zealand South Island: unpeopled (Aotearoa settled much later, late 1st–early 2nd millennium CE).
Technology & Material Culture
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Flake/blade cores, backed artifacts emerging; grindstones in some regions; ochre widely used.
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Wooden spear throwers, clubs; fiber nets; hearth/earth ovens.
Movement & Interaction Corridors
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Murray–Darling and Lake Eyre/Willandra waterways; coastal highways along expanded shelves; Bassian crossings between mainland–Tasmania.
Cultural & Symbolic Expressions
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Early engraving/painting traditions; ochre burials; structured hearths and shell middens.
Environmental Adaptation & Resilience
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Highly mobile estate systems coordinated use of water points, lakes, and coasts; fire management promoted mosaic productivity.
Transition
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Post-LGM sea rise will drown the Bassian Plain, isolating Tasmania; Holocene humid pulses will expand estuaries and shellfish grounds.
