Tectonic plate movement (continental drift) reshapes rainforest canopies over millions of years, impacting species through:
As continents shift, climatic zones move. Canopy habitats shift latitude/altitude. Species unable to disperse fast enough face extinction. Fragmentation isolates populations.
Continent position changes ocean currents, wind patterns, rainfall. A rainforest may become drier (savannization) or cooler—mismatching species' niches.
Land bridges (e.g., Panama Isthmus 3 Ma) connect isolated faunas. Northern predators invade south; southern species move north. Canopy specialists face new competitors/predators.
Populations split by rising seas, mountains, or rifts diverge genetically → new species (allopatric speciation). Canopy species with poor dispersal (e.g., flightless insects, certain birds) are prone.
Specialized pollination/seed dispersal mutualisms (figs/fig wasps, specific birds/flowers) break if partners separate.
Collision zones (Andes, Himalayas) create new montane habitats—cloud forests with unique canopies—driving adaptive radiation.
Current rapid anthropogenic climate change mimics these slow geological forces at catastrophic speed, giving species little time to adapt or move.