Filters:
Location: Luoyang (Loyang) Henan (Honan) China

Southern Macaronesia (28,577 – 7,822 BCE) …

Years: 28577BCE - 7822BCE

Southern Macaronesia (28,577 – 7,822 BCE) Upper Pleistocene II — Deglaciation, Rising Seas, and Forest Recovery (No Humans)

Geographic and Environmental Context

Southern Macaronesia includes:

  • The Canary Islands (Gran Canaria, Tenerife, Fuerteventura, Lanzarote, La Palma, La Gomera, El Hierro).

  • The Cape Verde archipelago (Sotavento and Barlavento groups).

Anchors: Tenerife (Teide massif), Gran Canaria (Caldera de Tejeda), La Palma (Caldera de Taburiente), La Gomera(garajonay–laurisilva), El Hierro (El Golfo fault scarp), Fuerteventura–Lanzarote (low, arid shield islands and malpaísfields), Cape Verde (Fogo stratovolcano, Santo Antão and Santiago highlands, Sal–Boa Vista arid flats).

 

  • Sea-level rise drowned benches, cut new calas and coves; landslides and occasional eruptions reworked coastal outlines (esp. in Canaries).

Climate & Environmental Shifts

  • Bølling–Allerød: warmer, wetter; laurisilva expanded;

  • Younger Dryas: brief cooling/drying contracted forests;

  • Early Holocene: stable warmth restored fog-fed cloud belts.

Subsistence & Settlement

  • None; ecosystems matured; soils thickened in older volcanic terrains (Gran Canaria, La Gomera), remained thinner on Fuerteventura–Lanzarote and Cape Verde windward flats.

Technology & Material Culture

  • N/A.

Movement & Interaction Corridors

  • Ocean/atmosphere only; increased rafting of pumice/wood after eruptions and storms.

Cultural & Symbolic Expressions

  • None.

Environmental Adaptation & Resilience

  • Fog-drip hydrology sustained evergreen forests; arid islands stabilized with drought-adapted scrub.

Transition

By 7,822 BCE, Southern Macaronesia’s Holocene balance was established without human disturbance.

Related Events

Filter results