Paleoenvironmental changes in the Hiwegi Formation (lower Miocene) of Rusinga Island, Lake Victoria, Kenya

The Early Miocene of Rusinga Island (Lake Victoria, Kenya) is best known for its vertebrate fossil assemblage—particularly of early hominoids and catarrhines—but the multiple stratigraphic intervals with well-preserved fossil leaves have received much less attention. The Hiwegi Formation has three fossil leaf-rich intervals: Kiahera Hill, R5, and R3. Here, we made new fossil collections from Kiahera Hill and R3 and compared these floras to previous work from R5 as well as modern African floras. The Kiahera Hill flora was most similar to a modern tropical rainforest or tropical seasonal forest and was a warm and wet, closed forest. This was followed by a relatively dry and open environment at R5, and R3, which was most similar to a modern tropical seasonal forest, was a warm and wet spatially heterogenous forest. Floral composition of these floras differed dramatically but Kiahera Hill and R3 were more similar to each other than either flora was to R5. The Kiahera Hill flora had few monocots or herbaceous taxa and was dominated by large leaves and had a higher species richness and greater evenness than the R3 flora. Our work, coupled with previous studies, suggests that R3 had a landscape of both closed forest and more open areas with seasonal ponding. The absence of morphotypes from the R5 flora that were present in the Kiahera Hill and R3 floras provides evidence for local expatriation during the R5 time interval. These results demonstrate that there was a considerable change in both climate and vegetation over an ~500 kyr interval of the Kiahera Hill, R5, and R3 floras. Thus, this work suggests that the Hiwegi Formation on Rusinga Island samples multiple environments in the Early Miocene and provides important context for the evolution and habitat preference of early apes.