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Rust, U. 1989. Grundsätzliches über Flußterrassen als paläoklimatische Zeugen in der südwestafrikanischen Namibwüste. In: A. A. Balkema (Ed.). Palaeoecology of Africa and the surrounding islands, 20: 119-132


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Grundsätzliches über Flußterrassen als paläoklimatische Zeugen in der südwestafrikanischen Namibwüste.

Summary / Notes:

In der Namib existieren drei für die palaeoklimatische Inwertsetzung von FluBterrassen entscheidende Lagegegebenheiten: Leitergefüge, hypsome- trischer Gradient, hygrischer Gradient. In den Unterläufen der Riviere sind FluBterrassen nur eingeschränkt als Palaeoklimazeugen zu behandeln. In den Mittelläufen der Riviere sind sie exzellente Palaeoklimaindikatoren. Erosionsterrassen belegen feuchtere (als heute) Verhältnisse in der Namib. Akkumulationsterrassen belegen trockenere (als heute) Verhältnisse im Hinterland. Aus 14C-gestützten Analysen von FluBterrassen ergibt sich, daB die Namib regional differenzierte Klimaschwankungen im Jungquartär erfahren hat. Keywords: Namibia, Namib Desert, Kuiseb River, ephemeral rivers, palaeoenvironment, palaeoclimate, fluvial terraces, geomorphology, aeolian deposits, landform evolution, landform geology ACCESSION NUMBER: 560.909 HEI.

Year: 1989

Type: Book, Book Section, Booklet

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