Climate of the Past Discussions www.clim-past-discuss.net 1814-9340 1814-9359 5 1 2009 10.5194/cpd-5-341-2009 http://www.clim-past-discuss.net/5/341/2009/ http://www.clim-past-discuss.net/5/341/2009/cpd-5-341-2009.html http://www.clim-past-discuss.net/5/341/2009/cpd-5-341-2009.pdf 341 367 2009-02-09 Western equatorial African forest-savanna mosaics: a legacy of late Holocene climatic change? A. Ngomanda ngomanda@yahoo.fr A. Chepstow-Lusty M. Makaya C. Favier P. Schevin J. Maley M. Fontugne R. Oslisly D. Jolly Institut de Recherche en Ecologie Tropicale, IRET/CENAREST, BP. 13354, Libreville, Gabon Institut des Sciences de l'Evolution de Montpellier, UMR 5554, Université de Montpellier II, Place Eugène Bataillon, cc 61, 34095 Montpellier Cedex 5, France Université des Sciences et Techniques de Masuku, Departement de Geologie, BP. 901, Franceville, Gabon Laboratoire des Sciences du Climat et de l'Environnement, UMR CEA/CNRS 1572, Domaine du CNRS, 91198 Gif sur Yvette cedex, France IRD – Cameroun, BP. 1857, Yaoundé, Cameroun Past vegetation and climate changes reconstructed using two pollen records from Lakes Maridor and Nguène, Gabon, provide new insights into the environmental history of western equatorial African rainforests during the last 4500 cal yr BP. The Lake Maridor pollen record indicates that the coastal savannas of western equatorial Africa did not exist during the mid-Holocene and instead the region was covered by evergreen rainforests. In the Lake Nguène pollen record, a rapid decline of hygrophilous evergreen rainforest occurred around 4000 cal yr BP, synchronously with grassland expansion around Lake Maridor. The establishment of coastal savannas in Gabon suggests decreasing humidity at the onset of the late Holocene. The marked reduction in evergreen rainforest and subsequent savanna expansion was associated with the colonization of secondary forests dominated by the palm, <i>Elaeis guineensis</i>, in the coastal region and the shrub, <i>Alchornea cordifolia</i>, further inland. A return to wetter climatic conditions from about 1400 cal yr BP led to the renewed spread of evergreen rainforest inland, whereas a forest-savanna mosaic still persists in the coastal region. There is no evidence to suggest that the major environmental changes observed are driven by human impact. 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