The floodplain ecosystem of the Nyl River is located in a semi-arid re
gion of South Africa where water limits both human development and eco
system functioning. Proposed upstream impoundments threaten the ecosys
tem's functioning and hence its conservation value and eco-tourist pot
ential. Articulation of these threats to the floodplain ecosystem requ
ires a predictive understanding of the relationships between the biota
and hydro-geomorphic processes. This study provides the basis for the
establishment of these relationships by presenting a description of t
he plant assemblages of the Nyl River floodplain, identifying environm
ental correlates of this vegetation pattern, and by distinguishing fun
ctional plant groups. A correspondence analysis identified three major
vegetation associations on the floodplain ecosystem: near-channel sit
es, hydromorphic sites and sodic sites, Geomorphic landform type, soil
moisture and soil texture were the best correlates of the vegetation
pattern. Elevation above the channel and distance from the channel wer
e poor correlates of vegetation pattern. The distribution of functiona
l groups, which were defined by plant life forms, showed that the near
-channel sites were dominated by prostrate and decumbent grasses, hydr
omorphic sites by erect grasses, and sodic sites by a variety of succu
lent life forms. The plant-environment relationships recognized sugges
t that future distributions of functional plant groups may provide a s
ensitive index of the impacts of anticipated reductions in run-off.