We investigated stable carbon isotope ratios of soil organic matter in the
forests of the Hluhluwe-Umfolozi Game Reserve, KwaZulu-Natal. Analysis of s
oil profiles in the forest indicated a shift from C-3 to C-4 vegetation wit
h depth. These results suggest that the area now covered by mature, tall fo
rest in the region was once grassland. These findings support the hypothesi
s that the grasslands of KwaZulu-Natal are older than previously thought.