2000
DOI: 10.1016/s0031-0182(99)00095-4
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Vegetation change in equatorial West Africa: time-slices for the last 150 ka

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Cited by 239 publications
(219 citation statements)
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“…2 and 5). This pattern agrees with reconstructions by Ray and Adams (2001) and Dupont et al (2000), who found a reduction in tropical forest in western and central Africa during the LGM period. Our model also agrees with pollen data from BIOME 6000 which show tropical forest on the west coast of Africa and grasslands in southern and northern Africa.…”
Section: Last Glacial Maximum Simulation (Lgm)supporting
confidence: 92%
“…2 and 5). This pattern agrees with reconstructions by Ray and Adams (2001) and Dupont et al (2000), who found a reduction in tropical forest in western and central Africa during the LGM period. Our model also agrees with pollen data from BIOME 6000 which show tropical forest on the west coast of Africa and grasslands in southern and northern Africa.…”
Section: Last Glacial Maximum Simulation (Lgm)supporting
confidence: 92%
“…Literature on the economic importance of West African wetlands, and how the benefits and costs resulting from their use are distributed is however weak. Results from this study of the Niger Delta wetlands, Africa's largest river delta and mangrove ecosystem (Dupont et al 2000) emphasise the economic importance and livelihood contribution of the wetlands as well as the potential disparity in the distribution of environmental costs and benefits among stakeholders.…”
Section: Discussionmentioning
confidence: 98%
“…According to Short and Staeuble (1967) beyond into the Gulf of Guinea, resulted in the formation of this complex and fragile delta with a rich biodiversity (Abam 2001). The Niger Delta is regarded as the third largest wetland in the world (Uluocha and Okeke 2004;Umoh 2008), and the largest river delta and mangrove ecosystem with the greatest extension of freshwater swamps in Africa (Ajonina et al 2008;Dupont et al 2000;Ogon 2006). …”
Section: Geography and Peoplementioning
confidence: 99%
“…During the Late Pleistocene, dry phases repeatedly reduced considerably the size of the tropical forest around the globe, around 60 kya, 40 kya, 25-11 kya (Dupont et al 2000, Maley 2004, Sémah & RenaultMiskovsky 2004, Sultan et al 2001, Van der Hammen & Hooghiemstra 2000. During the Last Glacial Maximum in Central Africa, for example, the rainforest at ~20 kya had almost disappeared except for a few crucial refugia that are still biodiversity hotspots, from where rainforest species expanded once climatic conditions improved and stabilized during the Holocene.…”
Section: Rainforests Biodiversity Long-time Depths and The Impact Omentioning
confidence: 99%