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Euston-Brown, D., Rathogwa, N & Richardson ... - DWA Home Page

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To further complicate matters, Iron Age farmers have been having an impact on these savanna<br />

systems for about 2000 years (Goodall & Zacharias, 2002; Bond et al. 2003). The previous farmers<br />

of Kruger National Park burnt the veld on a regular basis for grazing cattle, and were successful in<br />

maintaining an open savanna system (e.g. Terminalia sericea thicket at Pretoriuskop today used to be<br />

an open savanna 100 years ago, historical pictures at reception in Pretoriuskop). However, there is<br />

overwhelming evidence showing that the open savanna system predated hominid use of fire, and that<br />

open grassy systems are an even more ancient phenomenon (Bond et al. 2003).<br />

Savanna systems are not stable. Fluctuations in species abundances are regarded as normal and are<br />

related to variability in rainfall (O’Conner, 1985). Soil moisture is regarded as most important for<br />

germination and establishment of most savanna plants. In general germination and growth occurs after<br />

spring and summer rainfall, but not that much after winter rainfall. It could also be generalised that the<br />

time that it takes a seedling to survive a fire is pivotal for determining the minimum fire-return interval<br />

that should not be exceeded if eradication of the plant is desired. Resprouting is a well-developed<br />

feature of most savanna plants allowing most species to persist through disturbances such as fire or<br />

alien plant control (Bond & Midgley, 2001).<br />

Botanically the ecosystems have an astonishing diversity of woody trees and shrubs (Scmidt et al.<br />

2002). In general, the bush encroachment phenomenon is one we need to consider carefully if<br />

wanting to deal effectively with the problem of Chromolaena, Lantana and many other weeds of this<br />

ecosystem. The invasion of these two plants has largely been facilitated by the bush encroachment<br />

problem because they would struggle to invade frequently burnt grasslands that were present before<br />

the thickening of some parts of these savanna systems (Goodall & Zacharias, 2002; Zachariades &<br />

Strathie, 2006).<br />

Chromolaena was probably introduced by accident as seed in packaging material off a ship from the<br />

Jamaican islands at Durban harbour in the late 1940’s. By 1980 it had spread south along the coast<br />

to Port St Johns and northwards through Swaziland and into Limpopo province. Today it is still<br />

spreading and thickening in the frost free areas of South Africa with rainfall above about 500 mm per<br />

annum (Zachariades and Goodall, 2002). The South African biotype is different from the biotype that<br />

is invading western/central Africa and Asia. Our biotype is more cold tolerant and it has high plasticity<br />

both in the habitats it invades and in growth form. It can form dense impenetrable thickets that replace<br />

indigenous vegetation and this impacts negatively on cattle ranching, game farms, forestry and eco-<br />

tourism.<br />

Lantana was introduced as an ornamental from Tropical America and is one of the world’s worst<br />

weeds. It was first recorded in the Western Cape in 1858, and rapidly spread eastwards and northwards<br />

into the Limpopo province. It has a much wider tolerance of climate than chromolaena, but is also<br />

restricted to frost-free areas. There are over 50 different variants within the species, with variation<br />

in susceptibility to herbicides and bio-control agents. The plant is toxic to cattle and it forms dense<br />

impenetrable thickets that replace indigenous vegetation. It impacts negatively on cattle ranching,<br />

game farms, forestry and eco-tourism.<br />

Development of a clearing protocol based on ecological criteria for Mesic Savannas and Sweet Grassveld for the Working for Water Programme<br />

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