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Mpumalanga Biodiversity Conservation Plan Handbook - bgis-sanbi

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MPUMALANGA BIODIVERSITY CONSERVATION PLAN HANDBOOK<br />

20<br />

Malachite Kingfisher<br />

Alcedo cristata<br />

Because of the<br />

ecological, social and<br />

economic importance of<br />

wetlands and their<br />

threatened status in South<br />

Africa, an extensive<br />

inventory of wetlands,<br />

their status and the<br />

threats they face is<br />

underway. The inventory<br />

is spearheaded by the<br />

Department of<br />

Agriculture and Land<br />

Administration but<br />

includes a wide range of<br />

stakeholders including<br />

government departments,<br />

NGOs, conservation<br />

bodies and research<br />

institutes.<br />

cover slows runoff, filters and purifies water and reduces the impacts of droughts and floods<br />

by regulating stream flow. They provide special habitats for many species of plants and<br />

animals. Besides these benefits, wetland vegetation also provides economic resources such<br />

as grazing, food, medicinal plants and natural fibre for thatch and craft making.<br />

Wetlands are controlled by the same basic ‘drivers’ as rivers. These features define their<br />

health and sustainability. A key property of wetlands is that they present a convergence of<br />

aquatic and terrestrial biodiversity at important positions in the landscape. It is here, as well<br />

as in rivers, where the health of key components of natural ecosystems can best be observed<br />

and measured. Our wetlands are typically variable, with over 90 different wetland biodiversity<br />

features recognised in the MBCP. These are based on a functional and Ecoregion<br />

level 2 classification as a surrogate for wetland biodiversity types. All wetlands may be<br />

allocated into four functional categories.<br />

CATEGORIES OF WETLANDS<br />

SEEPAGE WETLANDS – are generally seasonal, small and widely scattered. Often referred<br />

to as seeps or sponges, they mostly occur on obvious slopes and in upland areas. They are<br />

sometimes linear, across the slope and may be associated with bands of impermeable rock<br />

which provide an unexpected ‘perched water-table’. These are the least obvious wetlands<br />

as they are the most temporary and not located in obviously wet valley-bottom landscapes.<br />

VALLEY-BOTTOM WETLANDS – occur in bottom-lands and are generally wetter, and wet<br />

for longer periods, than seeps. In headwater areas they typically occur as seasonally waterlogged,<br />

shallow grassy valleys (vleis). In the mid and lower reaches of rivers they are also<br />

associated with streams and river banks, especially within the floodline. Valley-bottom<br />

wetlands include floodplains of the lower reaches of larger rivers, subjected to high-volume<br />

flood events.<br />

PANS – are shallow, usually seasonal bodies of open water; often circular and not directly<br />

connected to river systems by surface flow. Essentially they are internally draining systems<br />

that may contain either fresh or saline water, depending on local soil conditions. They may<br />

be temporary or perennial. Pans on different soils and at varying altitudes have substantially<br />

different ecological characteristics.<br />

LAKES AND DAMS – there are no true lakes in <strong>Mpumalanga</strong>. Strictly speaking, lakes are<br />

natural impoundments within the continuous river line. Dams are artificial impoundments<br />

that are not considered as wetlands as we have no natural fauna and flora that are adapted<br />

specifically to lake-type environments. The small ‘lakes’ in the Chrissiesmeer area are in<br />

fact pans, occasionally interconnected by wet-season overflows.<br />

M P U M A L A N G A<br />

<strong>Biodiversity</strong><br />

CONSERVATION PLAN HANDBOOK

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