Publication | Closed Access

A 25,000-year record of climate-induced changes in lowland vegetation of eastern equatorial Africa revealed by the stable carbon-isotopic composition of fossil plant leaf waxes

Paleoenvironmental ReconstructionEngineeringEastern Equatorial AfricaPaleoenvironmental ChangeTerrestrial EcosystemAfrican DrylandsCarbon CyclePaleoecology25,000-Year RecordClimate-induced ChangesEarth ScienceSocial Sciences