Late-Holocene equatorial environments inferred from deposition processes, carbon isotopes of organic matter, and pollen in three shallow lakes of Gabon, west-central Africa

• Published in: Journal of paleolimnology Vol. 41; no. 2; pp. 369 - 392
• Main Authors: Giresse, Pierre, Makaya Mvoubou, Maley, Jean, Ngomanda, Alfred
• Format: Journal Article
• Language: English
• Published: Dordrecht Springer Netherlands 01.02.2009; Springer Nature B.V
• Subjects: Carbon isotopes; Clay minerals; Climate Change; Earth and Environmental Science; Earth Sciences; Environmental changes; Freshwater & Marine Ecology; Geology; Holocene; Hydrology; Lakes; Organic matter; Original Paper; Outlets; Paleoclimate science; Paleolimnology; Paleontology; Physical Geography; Pollen; Radiocarbon dating; Rainforests; Savannahs; Seasonal variations; Sedimentology; Sediments; Slope stability; Gabon; C; δ; Pollen; Climatic trend; Lacustrine sediment; Holocene
• ISSN: 0921-2728; 1573-0417
• DOI: 10.1007/s10933-008-9231-5

Seven vibro-cores were collected from three shallow lakes of the Gabon (Kamalété, Nguène, Maridor) along a 300-km west–east transect close to the Equator. These lakes are located in very distinct landscapes: coastal forest-savanna mosaic, rain forest and savanna with colonising forest, respectively. Core chronologies were established by radiocarbon dating. Study of these lacustrine archives (textural variables, clay minerals, organic matter components, δ 13 C, pollen) allowed comparison of late Holocene environmental changes recorded at each site and with results from other studies. Lake Kamalété indicates minor climatic deterioration (increased drying and greater seasonality) between 1,410 and 500 cal. years BP, which is also recognised in southern Cameroon and east-central Africa. Lake Nguène was surrounded by dense moist forest throughout the last 4,110 years, but shows significant deterioration from ~2,800 cal. years BP, a phenomenon seen at nearby sites. Lake Maridor shows a decline of forest initiated a little after 3,800 cal. years BP, which indicates timing that is distinct from the two other sites. This was probably a response to local conditions (i.e. outlet damming). Although the three lakes display generally parallel climatic trends perhaps linked to SST oscillations, there is not perfect coherence between these three sites. Differences among the three basins may be attributable to local factors like groundwater hydrology and slope instabilities of such shallow lake systems in this equatorial region.