Climate of the Past Discussions www.clim-past-discuss.net 1814-9340 1814-9359 4 1 2008 10.5194/cpd-4-111-2008 http://www.clim-past-discuss.net/4/111/2008/ http://www.clim-past-discuss.net/4/111/2008/cpd-4-111-2008.html http://www.clim-past-discuss.net/4/111/2008/cpd-4-111-2008.pdf 111 147 2008-01-31 Thirty thousand years of vegetation development and climate change in Angola (Ocean Drilling Program Site 1078) L. M. Dupont dupont@uni-bremen.de H. Behling J.-H. Kim Marum, University of Bremen, Bremen, Germany Palynology and Climate Dynamics, Albrecht-von-Haller-Institute for Plant Sciences, University of Göttingen, Göttingen, Germany NIOZ, Texel, The Netherlands ODP Site 1078 situated under the coast of Angola provides the first record of the vegetation history for Angola. The upper 11 m of the core covers the past 30 thousand years, which has been analysed palynologically in decadal to centennial resolution. Alkenone sea surface temperature estimates were analysed in centennial resolution. We studied sea surface temperatures and vegetation development during full glacial, deglacial, and interglacial conditions. During the glacial the vegetation in Angola was very open consisting of grass and heath lands, deserts and semi-deserts, which suggests a cool and dry climate. A change to warmer and more humid conditions is indicated by forest expansion starting in step with the earliest temperature rise in Antarctica, 22 thousand years ago. We infer that around the period of Heinrich Event 1 a northward excursion of the Angola Benguela Front and the Congolian Air Boundary resulted in cool sea surface temperatures and a northward extension of desert vegetation along the coast. Rain forest and dry forest returned 15 thousand years ago. During the Holocene, dry forests and Miombo woodlands expanded. 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