“…As characterised through the forest-savanna species dichotomy, a strong influence of soil physical and chemical properties on tropical vegetation structure as detected here are also indicative of a significant edaphic influence on woody plant community composition consistent with nu-merous regional studies where landscape-scale variations in vegetation structure/floristics have been related to effects of landscape position, underlying geology and/or soil texture, as for example, in Brigalow woodland in Central Queensland (Australia; Dowling et al, 1986), Mopane Woodland in Botswana (Mlambo, 2007), for Nylsvley Nature Reserve (Coetzee et al, 1976), Kruger National Park (Fraser et al, 1987;Ben-Shahar, 1991;Baldeck et al, 2014;Scholtz et al, 2014), northern Transvaal (O'Connor, 1992 and Klaserie Nature Reserve (Witkowski and O'Connor, 1996) in South Africa, for the southern Kalahari Desert (Botswana, Namibia and South Africa; Werger, 1978), in Etosha National Park in Namibia (Le Roux et al, 1988), for the Turkana District in Kenya (Coughenour and Ellis, 1993), across northern Yucatan Peninsula in Mexico (White and Hood, 2004), at Assis Ecological Station in southeast Brazil (de Assis et al, 2011), in W Regional Park in southwest Niger (Diouf et al, 2012), in the Zambesi Valley (Guy, 1977), at Malilangwe Wildlife Reserve (Clegg and O'Connor, 2012) and Gonarezhou National Park (Gandiwa et al, 2014) in Zimbabwe, and for Emas National Park in central Brazil (Dantas et al, 2015). At larger scales, soil-specific texture and depth effects on vegetation structure have also been noted for Zimbabwe (Dye and Walker, 1980) and, in conjunction with rainfall variations for Australia (Williams et al, 1996), Botswana (Skarpe, 1986;Ringrose et al, 2003) and Sudan (Smith, 1951).…”