The climate experienced by early hominins (2 million–100,000 years ago) was anything but stable. It oscillated violently between glacial and interglacial cycles, forcing adaptation, migration, and innovation.
Driven by Milankovitch cycles (orbital eccentricity, axial tilt, precession), Earth cycled every 41,000 years (early Pleistocene) then ~100,000 years (late Pleistocene) between:
Not uniformly wet/dry. Orbital precession drove 20,000-year "Green Sahara" cycles: lush savannas with lakes ↔ hyper-arid desert. East African Rift valleys buffered extremes, offering mosaic habitats (gallery forests, grasslands, wetlands) where hominins thrived.
Glacials pushed populations south into refugia (Iberia, Balkans, Caucasus, Southeast Asia). Interglacials allowed northward expansions. Neanderthals adapted to cold; H. sapiens used cultural buffering (clothing, shelter, fire).
These pressures selected for: behavioral flexibility, complex toolkits, long-distance trade/exchange, symbolic culture, and ultimately, the cognitive capacity to modify environments rather than just adapt to them.