Founded in 1966, the internationally recognized and acclaimed
Series Palaeoecology of Africa publishes interdisciplinary
scientific papers on landscape evolution and on former environments
of the African continent. Beginning with topics such as changes in
climate and vegetation cover, the papers expand horizons and
interconnections to various types of environmental dynamics from
the Cainozoic up to the present; moreover, the aspect of human
influence since the Late Quaternary is related to many of the areas
studied.
Volume 31 presents four comprehensive papers on long- and
short-term processes of landscape evolution (geological history,
neotectonics and proxy Quaternary alluvia), as well as a recent
regional perspective on environmental problems in Southern
Cameroon. The book acts as a showcase for successful North-South
cooperation and capacity building for empowering African
Universities. It is problem oriented and applied, and illustrates
how scientific and interdisciplinary cooperation can work. In the
framework of the German Research Foundation s (DFG, Deutsche
Forschungsgemeinschaft) funded "Rain Forest Savanna Contact"
project (2003-2009) two abbreviated English versions of PhD theses
are here published, one by J. Eisenberg on neotectonics and the
other by M. Sangen on river sediments in rain forest-savanna
transitional zones. Complementary articles are an introduction on
geological history, by B. Kankeu et al. and a paper on
environmental risks by M. Tchindjang et al., together these
complete the results of this joint German-Cameroonian research
project.
This book will be of interest to all concerned with ecosystems
dynamics, tropical forests, savannas and related development
problems of Third World countries, especially regional planners,
ecologists, botanists, earth scientists and students of the
Quaternary (e.g. LGM and Holocene ecosystem dynamics, Global
Change). It will be valuable for advanced undergraduates and
postgraduates as a reference for new research articles on the topic
of long term geologic tectonic and Quaternary landscape evolution
in an up to now not well explored marginal area of the Western
Congo basin.
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