Northern West Indies (49,293–28,578 BCE) Upper …

Years: 49293BCE - 28578BCE

Northern West Indies (49,293–28,578 BCE) Upper Pleistocene I — Reef Benches, Limestone Lenses, and Seabird Realms (No People)

Geographic and Environmental Context

Northern West Indies includes the Outer Bahamas (Lucayan archipelago), the Turks & Caicos Islands, and northern Hispaniola — northern Haiti (Cap-Haïtien, Massif du Nord) and the Cibao/north coast of the Dominican Republic (Santiago de los Caballeros, Puerto Plata).

Anchors: Andros–Abaco–Eleuthera–San Salvador–Exuma banks, Turks & Caicos banks and passes, Cap-Haïtien–Massif du Nord, Cibao–Puerto Plata–Santiago river valleys and coastal shelves.

  • Sea level ~100 m lower exposed broad carbonate benches and dune fields on Bahama and Caicos banks; northern Hispaniola held narrow shelf and uplifted limestone foothills.

Climate & Environmental Shifts

  • LGM cooling strengthened winter trades and lowered SSTs; upwelling pulses still supported reef productivity.

Subsistence & Settlement

  • No human occupation; seabird/turtle rookeries and shallow lagoons formed dense trophic webs.

Technology & Material Culture — N/A.

Movement & Interaction Corridors

  • Ocean currents (Florida Current/North Equatorial) set cross-bank drift patterns; purely ecological connectivity.

Cultural & Symbolic Expressions — N/A.

Environmental Adaptation & Resilience

  • Pristine island biotas matured on freshwater lenses beneath the larger cays.

Transition
By 28,578 BCE, the banks and north Hispaniola coast were high-productivity carbonate landscapes awaiting people.

Related Events

Filter results