West Micronesia (49,293 – 28,578 BCE): Upper …

Years: 49293BCE - 28578BCE

West Micronesia (49,293 – 28,578 BCE): Upper Pleistocene — Lowstand Reef Terraces, Seabird Kingdoms (No Human Presence)

Geographic & Environmental Context

West Micronesia includes the Mariana Islands (Guam, Saipan, Tinian, Rota, and the northern chain), Palau (Babeldaob, Koror, Rock Islands), and Yap (Yap proper and its outer atolls).

  • Anchors: Guam–Saipan–Tinian–Rota (limestone platforms with fringing reefs), Babeldaob–Koror (Palau’s volcanic/limestone high islands and the Rock Islands lagoon), Yap proper (raised reef islands) and the outer Yap atolls (Ulithi–Woleai arc).

  • Sea level lay ~100 m below modern, exposing wide limestone benches and reef flats around Marianas, Palau, and Yap; lagoons were shallower, passes narrower.

  • Palau combined volcanic uplands with emergent limestone rims; Marianas and Yap presented high-standing reef platforms.

Climate & Environmental Shifts

  • Last Glacial Maximum: cooler SSTs, stronger trades; reef accretion slowed, but intertidal foraging niches (future) expanded geomorphically.

Baseline Ecology

  • Seabird supercolonies nested on outer cays; turtles used broad beaches; giant clams and reef fish populated nearshore flats.

  • On Palau, montane forests fed clear streams into mangrove-lined embayments.

Long-Term Significance

Glacial lowstand set the reef foundations and coastal benches later engineered by settlers into canoe landings, fish weirs, and garden soils.

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