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Miombo Ecoregion Vision Report - Biodiversity Foundation for Africa

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<strong>Miombo</strong> <strong>Ecoregion</strong> <strong>Report</strong>, page 20<br />

Edaphic grasslands, floodplains, dambos and wetlands are, however, included within the revised<br />

ecoregion. They are considered to be an integral part of the woodland landscape and ecological<br />

processes, and functionally are not separable.<br />

Table 1. Revised <strong>Miombo</strong> <strong>Ecoregion</strong> vegetation units. 2<br />

Vegetation unit WWF (1999) unit area (km 2 )<br />

Itigi thicket 48 15,405<br />

Cryptosepalum dry <strong>for</strong>est 32 37,908<br />

Wet miombo woodland 49 (most), 50 1,358,175<br />

Dry miombo woodland 52, 53 1,214,533<br />

Burkea–Terminalia woodland 57 (part) 96,162<br />

Mopane woodland 54 (part), 55 (part) 384,037<br />

Baikiaea woodland 51, 58 (part) 260,171<br />

Acacia–Combretum woodland 54 (part) 103,887<br />

Wetland grasslands 56 (part), 63 179,290<br />

Other areas (not part of ecoregion), e.g. water<br />

bodies, mountains<br />

167,636<br />

TOTAL 3,817,204<br />

3.2 Vegetation Types<br />

The two characteristic features of the Southern Caesalpinoid Woodland <strong>Ecoregion</strong> are the<br />

presence of woodland dominated by trees from the legume subfamily Caesalpinioideae, such as<br />

Brachystegia, Julbernardia, Isoberlinia, Baikiaea, Cryptosepalum, Colophospermum and<br />

Burkea, and the presence of a well-developed grass layer composed of C4 grasses. Caesalpinoid<br />

woodlands are composed of pinnate broad-leaved tree species, most being deciduous <strong>for</strong> at least<br />

a short period each year, the seasonality being related to a period of water stress and/or low<br />

temperatures. The woodland canopy is from 6 to 20 m in height, and ranges from 20% cover to<br />

almost closed-canopy <strong>for</strong>est.<br />

Caesalpinoid woodlands are mostly found on nutrient-poor soils (except Colophospermum and<br />

Acacia–Combretum woodland). Vegetation composition and structure are determined by climate<br />

(rainfall amount, length of dry season, mean temperature, frost), position in the landscape and<br />

soil type. Most changes in vegetation type within the ecoregion are gradual. Fire is an important<br />

feature.<br />

Another characteristic feature is the presence of large termite mounds, especially where sub-soil<br />

drainage is impeded. These are composed of cation-rich (particularly calcium) soils owing to<br />

their high clay contents, and generally have lower soil moisture levels. Termitaria support very<br />

different species from the surrounding woodlands. Their presence, as nutrient-enriched 'islands',<br />

is of major significance <strong>for</strong> both species diversity and woodland ecology.<br />

2 Areas taken from version of original hand-drawn map of Timberlake, digitized by WWF SARPO GIS Unit in 2001.

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