Sje. Wand et al., A preliminary study of the responsiveness to seasonal atmospheric and rainfall patterns of wash woodland species in the arid Richtersveld, PLANT ECOL, 142(1-2), 1999, pp. 149-160
Seasonal carbon and water relations were compared among seven tree or shrub
wash woodland species in the winter rainfall desert of the Richtersveld Na
tional Park, South Africa. Plants were generally aseasonal with respect to
gas exchange, but responsive to rainfall events with respect to water relat
ions and phenology. Relatively narrow annual ranges in potential evapotrans
piration due to the maritime influence could explain why these plants respo
nd more to fluctuations in water acquisition potential than to evaporative
demand. Two species were summer-deciduous, but one of them (Ozoroa concolor
) responded to aseasonal summer rainfall by leafing out and flowering. Thes
e two species had high shoot xylem water potentials when in leaf. All other
species were sclerophyllous evergreens with low water potentials, particul
arly the shallow-rooted shrub Zygophyllum prismatocarpum, and Boscia albitr
unca which may have a different rooting pattern to the other phreatophytes.
The latter species was also unique due to its high leaf nitrogen contents,
photosynthetic rates and stomatal conductances, despite very low leaf wate
r potentials. Leaf stable carbon isotope composition ((13)delta C) varied b
etween species (-22 to -27 parts per thousand), but was lower than the mean
for arid regions worldwide. The values indicated moderately high levels of
water use efficiency, but a less conservative strategy in two species, inc
luding Boscia albitrunca. The affinities of these species to summer rainfal
l biomes, their apparent decline in the western arid regions in recent geol
ogical history following aridification, and their absence southwards in the
winter rainfall regions, suggest that these wash species rely on sporadic
summer rainfall events to some extent. They may be at risk if predicted inc
reases in temperature and changes in rainfall patterns alter their effectiv
e moisture availability.