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Location: Luoyang (Loyang) Henan (Honan) China

Northern Macaronesia (28,577 – 7,822 BCE) Upper …

Years: 28577BCE - 7822BCE

Northern Macaronesia (28,577 – 7,822 BCE) Upper Pleistocene II — Deglaciation and Expanding Forests

Geographic and Environmental Context

Northern Macaronesia includes the Azores, Madeira, Porto Santo, and the Selvagens Islands.

  • The Azores: nine volcanic islands in the mid-North Atlantic (São Miguel, Terceira, Pico, Faial, São Jorge, Graciosa, Flores, Corvo, Santa Maria).

  • Madeira Archipelago: Madeira, Porto Santo, and the uninhabited Desertas.

  • Selvagens: small rocky outcrops south of Madeira.

Anchors: Azores volcanic cones and crater lakes (Furnas, Sete Cidades), Madeira’s laurisilva-clad mountains, Porto Santo’s dunes, and Selvagens’ seabird colonies.

  • Glacial retreat and sea-level rise reshaped island coasts.

  • Laurisilva forests in Madeira and early Azores expanded as rainfall increased.

Climate & Environmental Shifts

  • Bølling–Allerød: warmer/wetter, forests flourished.

  • Younger Dryas: brief cooling, minor contraction of forests.

  • Early Holocene: warming stabilized, producing lush evergreen canopies.

Subsistence & Settlement

  • No human settlement yet. Ecosystems dominated by birds and reptiles.

Technology & Material Culture

  • N/A.

Movement & Interaction Corridors

  • Islands served as mid-Atlantic waypoints for migratory birds, but not for humans.

Cultural & Symbolic Expressions

  • None.

Environmental Adaptation & Resilience

  • Island flora/fauna adapted to changing climate, with laurisilva stabilizing erosion and fog-fed hydrology.

Transition
By 7,822 BCE, Northern Macaronesia hosted dense forests and seabird refugia, but remained unpeopled.

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