Andamanasia (49,293 – 28,578 BCE) Upper …
Years: 49293BCE - 28578BCE
Andamanasia (49,293 – 28,578 BCE) Upper Pleistocene I — Ice-Age Shelves, Reef Flats, and Island Forest Refugia
Geographic and Environmental Context
Andamanasia encompasses:
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Andaman Islands (North, Middle, South Andaman) and Nicobar Islands.
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Aceh in northern Sumatra, with nearby islands (Simeulue, Nias, Batu, Mentawai).
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The Cocos (Keeling) Islands.
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The Preparis, Coco, and Little Coco Islands (off Myanmar).
Anchors: North–South Andaman coasts and reefs, Nicobar Great Channel, Aceh’s Weh Island and Lhokseumawe–Banda Aceh corridor, Simeulue–Nias–Mentawai arc, Preparis/Coco islets, Cocos (Keeling) lagoon.
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Sea level ↓ ~100 m: Sunda Shelf largely exposed, connecting Sumatra to mainland SE Asia; Andamans/Nicobars remained island chains but closer to coastlines.
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Islands: forested Andamans; Nicobars with mangrove–reef systems; offshore islands (Cocos, Preparis) exposed limestone flats.
Climate & Environmental Shifts
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Glacial maximum: cooler SSTs, stronger winter monsoon winds; rainfall suppressed, but coastal mangroves and refugia persisted.
Subsistence & Settlement
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Likely unpeopled yet, though possible transient visits from early coastal voyagers hugging Sunda margins.
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Rich seabird/turtle rookeries, mangrove crabs, and reef fish provided high productivity if reached.
Technology & Material Culture
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Not directly evidenced, but contemporaneous SE Asian foragers used flake/microblade toolkits; dugouts or bamboo rafts possible for coastal movement.
Movement & Interaction Corridors
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Sunda coastal highway skirted Nicobar–Andaman arc; exposed shelf meant short crossings from Sumatra → Nicobars → Andamans.
Cultural & Symbolic Expressions
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None directly known; symbolic life inferred from mainland contexts (ochre, ornaments).
Environmental Adaptation & Resilience
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These islands acted as ecological storehouses awaiting human settlement.
Transition
By 28,578 BCE, Andamanasia’s forest–reef mosaics had matured as refugia; human settlement awaited deglaciation.
