By J. Runge
This booklet contains clinical papers as a result of a global workshop:?Environmental and Cultural swap in West- and significant Africa? geared up via the German study beginning (DFG) in Yaoundé, Cameroon, March 2006. difficulties of Holocene and past due Pleistocene differences of the rain woodland savanna fringe and their attainable impression on cultural thoughts are discussed.
summary: This booklet includes clinical papers caused by a global workshop:?Environmental and Cultural swap in West- and valuable Africa? geared up through the German examine origin (DFG) in Yaoundé, Cameroon, March 2006. difficulties of Holocene and past due Pleistocene adjustments of the rain wooded area savanna fringe and their attainable impact on cultural techniques are mentioned
Read or Download Dynamics of Forest Ecosystems in Central Africa during the Holocene, Past? Present? Future : Palaeoecology of Africa, An International Yearbook of Landscape Evolution and Palaeoenvironments PDF
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Extra info for Dynamics of Forest Ecosystems in Central Africa during the Holocene, Past? Present? Future : Palaeoecology of Africa, An International Yearbook of Landscape Evolution and Palaeoenvironments
Faure gives an overview of some of the most important geo- and bio-scientific conclusions about the development of climate and vegetation of Central Africa (and other regions) for the Quaternary. For the Central African area the following scenario resulted on the basis of the preceded proxy-data discussion: The majority of the newer geomorphologic, zoological and palaeobotanical indications underline the fact that today’s Central African rain forest spread in the Congo Basin was clearly reduced in extension during the LGM due to profound reductions in temperature and precipitation (Runge, 1992, 2001; Thomas, 1994; Kadomura, 1995, 1998).
In addition even younger, apparently Holocene glacier fluctuations dated from 4,4 to 6,7 ka document at least sporadic younger glacial dynamics for the Liki III advance (Johansson and Holmgren, 1985). 100 m asl. 000 m asl and determines by 14C-dating of the organic lake sediments an age of 14,7 ka, which he sets for the end of the LGM in the high levels of the western Rift Valley. Other morainic tracts like the ones from Orumubaho are yet not dated. Alexandre et al. (1994) presume due to the significant geomorphological similarity with the Liki III moraines at Mount Kenya that these glacial forms also give evidence for a minimum age of 10 ka.
Bulletin de la Société Belge de Géologie, 3, pp. 199–207. , 1964a, Cartographie geomorphologique et morphogenese aux environs du Stanley-Pool (Congo). Acta Geographica Lovaniensia, 3, pp. 431–441. , 1964b, Nappes de gravats et couvertures argilo-sableuses au Bas-Congo: leur genèse et l’action des termites. In Etudes sur les termites Africains, edited by Bouillon, A. –16. Mai 1964), pp. 399–414. , 1965, Position géomorphologique, génèse et chronologie de certains dépôtssuperficiels au Congo occidental.