Conservation Value of the Egoli Granite Grassland, an Endemic Grass- Land in Gauteng, South Africa
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Conservation value of the Egoli Granite Grassland, an endemic grass- land in Gauteng, South Africa G.J. BREDENKAMP, L.R. BROWN and M.F. PFAB Bredenkamp, G.J., L.R. Brown and M.F. Pfab. 2006. Conservation value of the Egoli Granite Grassland, an endemic grassland in Gauteng, South Africa. Koedoe 49(2): 59–66. Pretoria. ISSN 0075-6458. Gauteng is the most densely populated province in South Africa. Its remaining natural areas are constantly under threat from urban development and the associated impacts. Presently, the natural areas of Gauteng support a large diversity of ecosystems. One such ecosystem is the Egoli Granite Grassland, endemic to the province, poorly conserved and therefore highly threatened. This paper describes the original Egoli Granite Grassland and the anthropogenic Hyparrhenia hirta dominated grassland that has replaced it in many of the remnant areas. Human impacts on this sensitive ecosystem have resulted in an altered species composition, loss of many species, and a change from a species-rich grassland with high conservation value to a species-poor grassland with low conser- vation value. The conservation of the last remaining relicts of original Egoli Granite Grassland is essential. Keywords: Egoli Granite Grassland; conservation value; Hyparrhenia hirta, Gauteng. G.J. Bredenkamp, African Vegetation and Plant Diversity Research Centre, University of Pretoria; L.R. Brown, Applied Behavioural Ecology and Ecosystem Research Unit, University of South Africa; M.F. Pfab, Bioregional Planning, Gauteng Department of Agriculture, Conservation and Environment, Johannesburg, 2001 South Africa. Introduction in the transition zone between the Grassland and Savanna biomes. The Egoli Granite Grassland is a type of grassland and a mapping unit (Gm10) clas- From a conservation planning or urban devel- sified under the Mesic Highveld Grassland opment viewpoint, the range of structural Bioregion according to the new Vegetation and floristic variation is considered too large Map of South Africa, Lesotho and Swazi- to define Bankenveld as a single unit, even land (Mucina et al. 2005). This grassland on the reconnaissance level of vegetation was mapped as Bankenveld (veld type 61) investigation. Bredenkamp & Brown (2003) by Acocks (1988), and Rocky Highveld recognised 16 major vegetation types within Grassland (Vegetation Type 34) by Breden- Bankenveld. The Egoli Granite Grassland kamp & Van Rooyen (1996). Acocks (1988) is considered as mainly belonging to the describes the Bankenveld as a False Grass- Hyparrhenia hirta Anthropogenic Grassland veld Type. The climax vegetation of this (Bredenkamp & Brown 2003). veld type should be, according to Acocks, an Egoli Granite Grassland is restricted to the open savanna, that is a bushveld vegetation, Gauteng Province of South Africa and is but it has been changed to, and maintained located north of the Roodepoort / Krugers- as grassveld by regular veld fires. How- dorp ridge complex and stretches over a ever, Bredenkamp & Brown (2003) consider distance of approximately 35 km to Centu- Bankenveld vegetation as a mosaic of grass- rion in the north. This grassland stretches land and woodland communities controlled over a distance of approximately 50 km in a by (micro-)climatic conditions that exist in westerly direction from the R21 highway in the topographically heterogeneous landscape the east. The 28º longitude and 26º latitudi- ISSN 0075-6458 59 Koedoe 49/2 (2006) bredenkamp.indd 59 2006/10/15 10:51:01 PM PTA JHB N 10 0 10 20 Kilometers 60 0 60 120 Km Fig. 2. Dark gray represents remnant areas of poten- Fig. 1. Locality map of the Egoli Granite Grassland. tially original Egoli Granite Grassland; perennial Grey areas indicate urbanisation rivers shown. nal lines cross in the centre of this grassland ing 3 ha in Glen Austin Bird Sanctuary, 3 ha (Fig. 1). in Melville Koppies Nature Reserve, 9 ha in Ruimsig Nature Reserve, and 11 ha in the Due to high demand for developable land in Walter Sisulu Botanical Gardens (Fig. 2). Gauteng, and especially the Johannesburg / The current protection status of Egoli Granite Pretoria corridor, the Egoli Granite Grassland Grassland is therefore completely inadequate, is under extreme pressure. Large areas are with only 0.1 % of the national target actually already developed for residential, industrial achieved. In order to meet South Africa’s and commercial purposes. This has led to the international obligations, it is imperative that destruction of vast tracts of this grassland. the Gauteng provincial government put in At least 61 % of Egoli Granite Grassland has place measures to improve the conservation been permanently transformed: 27 % by urban status of Egoli Granite Grassland. development (Fig. 2); 17 % by smallholdings; 12 % by agriculture (cultivated lands); and Any viable remnant patch of original Egoli 5 % by other impacts such as exotic plan- Granite Grassland must therefore be pro- tations, mining and planted pastures. An tected from transforming land uses. In order estimated additional 17 % of Egoli Granite to assess whether a valuable remnant patch Grassland is degraded due to overgrazing and will be affected by a proposed develop- the influence of edge effects associated with ment, environmental consultants involved in a highly fragmented landscape (Fahrig 2003). vegetation impact assessments are required Other effects, such as trampling, increased by the Gauteng Department of Agriculture, pollutants and the infestation of weeds and Conservation and Environment (GDACE) to alien species also contribute to degradation assess the presence and condition of Egoli of this grassland. It is therefore highly likely Granite Grassland on any site proposed for that the national target for conservation of development. this grassland type, i.e., 25 % of the total As this grassland was only recently defined extent, will never be realised. with the development of the new Vegetation Egoli Granite Grassland is extremely poorly Map of South Africa, Lesotho and Swaziland conserved, with only 0.02 % (26 ha) of the (Mucina et al. 2005), very little information vegetation type currently protected, includ- on its floristic composition, condition, the Koedoe 49/2 (2006) 60 ISSN 0075-6458 bredenkamp.indd 60 2006/10/15 10:51:02 PM extent of the grassland, and the manage- Vegetation ment thereof exists, causing some confusion among nature conservationists, environmen- Current vegetation tal consultants and local authorities. The aim of this paper is therefore to provide an eco- This tall grassland occurs over vast areas, logical overview of this grassland. usually on shallow, leached soils on the Johannesburg Granite Dome. Disturbed grassland or other disturbed areas such as Physical Environment road reserves or old fields, not cultivated for some years, are also usually Hyparrhenia This area is generally characterised by rocky species-dominated and low in species rich- undulating plains representing crests, slopes ness. Although some of these tall grasslands and valley bottoms with shallow, nutrient- appear to be quite natural, they are mostly poor soils. Shallow drainage lines and vlei- associated with an anthropogenic influence like wetland areas occur in the valley bot- from recent or even iron-age times. toms. Rockiness of the soil surface is a fur- These grasslands are characterised by the ther common characteristic shared by most tall-growing dominant grass Hyparrhenia Bankenveld areas. hirta and the invader dwarf shrub Seriphium Mean monthly temperature in the study area plumosum (=Stoebe vulgaris), indicating its low successional status or degraded condi- is 16.8 ºC with a mean maximum of 22.6 ºC tion. and a mean minimum of 10.8 ºC. The mean winter temperature is 13.8 ºC and mean sum- Dense Hyparrhenia species-dominated grass- mer temperature, 25.6 ºC (Weather Bureau land mostly has low species richness, with 2000; Grobler et al. 2002). Mean annual rain- only a few other species able to establish or fall in Gauteng is 670 mm (Gauteng 1997). survive in the shade of the dense sward of tall grass. Most of these species are relict Old granitic and gneissic rocks at least 2 400 pioneers or early seral species. The most million years old (Kerfoot 1987) are exposed prominent species include the grasses Cyno- in the Egoli Granite Grassland area. The Half- don dactylon, Eragrostis chloromelas, E. way House Granites (Fig. 3) of the Johannes- racemosa, E. curvula and Aristida congesta. burg Dome are intensively weathered with Forbs are rarely encountered, though a few deep drainage lines resulting in a gently individuals of species such as Anthospermum rolling topography, with shallow, coarse, hispidulum, Pseudognaphalium luteo-album, nutrient-poor, well-drained soils. The granite Conyza albida, C. podocephala, Crabbea areas are mostly covered by grassland vege- angustifolia, Helichrysum nudifolium and tation though patches of woodland vegetation H. rugulosum are often present. The woody are found at sheltered sites on hillslopes and layer, which has a very low cover, consists of rocky outcrops within this veld type (Grobler small clumps of indigenous trees and shrubs widely scattered within this grassland. The 2000; Grobler et al. 2002, 2006). scanty woody species include the trees Rhus The Bb land type predominates over the pyroides and Ziziphus mucronata, together entire region (Land Type Survey Staff 1984, with the scandent shrub Ziziphus zeyheri- 1985, 1987) (Fig. 3). The residual granitic ana. Declared alien invasive species such as soils are very shallow