A Developing Computer Model of the Auob River Ecosystem, Kalahari Gemsbok National Park
The Auob River is one of two major rivers traversing the Kalahari Gemsbok National Park (Figure 1). The river is a relict of wetter epochs and flows approximately once every ten years. The Auob is in a region of low rainfall (200 mm) which is variable in amount and spatial distribution. The rain which does fall consequently has a dominating influence on the flora and fauna of the ecosystem.
KeywordsBiomass Clay Migration Clarification
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- Bothma J du P and M G L Mills 1977. Patterns of ungulate abundance in the Nossob River valley in the south-western Kalahari Desert. Proceedings of the Thirteenth International Congress of Game Biologists Atlanta, March 1977.Google Scholar
- Leistner O A 1959. Notes on the vegetation of the Kalahari Gemsbok National Park with special reference to its influence on the distribution of antelopes. Koedoe 2, 128–151.Google Scholar
- Leistner O A 1967. The plant ecology of the Southern Kalahari. Memoirs of the Botanical Survey of South Africa 38, 1–172.Google Scholar
- Leistner O A and M J A Werger 1973. Southern Kalahari phytosociology. Vegetation 28, 353–399.Google Scholar
- Retief P F and P T van der Walt 1978. Kalahari Gemsbok National Park. Auob River ecosystem project. Notes on computer model. Unpublished manuscript.Google Scholar
- Stanley-Price M R 1976. Feeding studies of oryx on the Galana Ranch. African Wildlife Leadership Foundation News 11 (3), 7–11.Google Scholar