A geochemical and palynological study of lake sediments at Mboandong, Cameroon: Chemical weathering and vegetation linked to Holocene palaeoclimate

Abstract

Geochemical and palynological analyses of core samples from Mboandong, a crater lake in western Cameroon, provide a record of response to climate and vegetation change in West Africa over the last 7000 years. Three palaeoclimatic phases were identified: a humid phase (6800-5700 cal. BP), characterized by a humid and warm palaeoclimate; a drying phase (5700-2000 cal. BP) with a less humid palaeoclimate; finally, a seasonal phase (2000 cal. BP to present), characterized by a seasonally varied, mainly humid and warm palaeoclimate. Pollen components show swamp and humid rainforest taxa being gradually replaced by semi-deciduous, regrowth and non-tree taxa such as grasses (Poaceae). There is a suggestion of increasing aridity over the last 200 years. The sediments are primarily weathered deposits mixed with volcanic eruptive material, rather than detritus derived from the UCC (upper continental crust). Chemical Index of Alteration (CIA) values are mostly high (mean 90.65%) and indicate a variable but mostly humid palaeoclimate. CIA values are most likely influenced by climate, as well as by runoff and physical erosion. Bands of volcanic ash are associated with frequent freshwater sponge spicules and diatoms, probably due to increased availability of silica. Ca and Na depletion is probably linked with soil leaching, while K depletion and Mg enrichment were probably caused by chemical alteration. Humid intervals may have higher organic carbon content, whereas increased amounts of iron occur in potentially drier intervals. A greatly increased presence of oil palm pollen (Elaeis guineensis) is interpreted as evidence of cultivation after 1700 cal. BP.