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Subsistence farmers in Africa depend largely on the soil organic matter to sustain crop productivity. Long‐term changes in soil organic carbon and nitrogen were measured after woodland clearance for smallholder subsistence farming or for commercial farming. The contents of organic carbon and nitrogen in soil under reference woodlands were largest (53.3 t C ha⁻¹, 4.88 t N ha⁻¹) in a red clay soil (∼ 50% clay + silt), followed by a granitic sand (∼ 12% clay + silt; 22.8 t C ha⁻¹, 1.47 t N ha⁻¹) and least (19.5 t C ha⁻¹, 0.88 t N ha⁻¹) in a Kalahari sand (∼ 5% clay + silt). Organic carbon declined rapidly under cultivation to attain new equilibria within 10 years on all smallholdings. Greatest losses occurred in soils that initially contained most carbon and nitrogen in the order: red clay (22.4 t C ha⁻¹ and 1.0 t N ha⁻¹) > granitic sand (13.2 t C ha⁻¹ and 0.8 t N ha⁻¹) > Kalahari sand (10.6 t C ha⁻¹ and 0 …