An account is given of a typical rainfed waterbody in the Al-Ammariyah Wadi
(Saudi Arabia), with special reference to charophyte vegetation, water che
mistry and topography of the area, which was studied from April 1996 to Jul
y 1997. Recurring patterns following rainfall and inundation of the waterbo
dy are described as a model of temporal succession of biotic communities. U
nispecific Chara braunii Gm. meadows were the first aquatic vegetation to e
merge and overwhelmingly dominated the freshwater lentic ecosystem. This wa
s followed by plankton and desert plants as the waterbody dried out. Chara
braunii is reported as a new record for the Saudi Arabian charoflora. The s
pecies is characterised as stenohaline and tends to grow in vivo and in vit
ro in the salinity range of 0.2-0.8 parts per thousand. A gradual increase
in elements and ions (Si 20-31 mg L-1 and pH 6.8-7.6) in the water was demo
nstrated as the waterbody desiccated. As a result of the increasing concent
ration of ions and pH, C. braunii developed heavy encrustation, and hastene
d fructification prior to desiccation of the waterbody between June and Jul
y 1997. Survival and emergence of C. braunii is positively correlated with
drought resistant-oospores, specificity to hyposalinity, water-level fluctu
ations, and absence of herbivores.