1 In an investigation of the impact of the extreme drought of 1995, me
asurements of the relative water content (RWC) of leaves were conducte
d on a wide range of herbaceous species, distributed over a vegetation
mosaic coinciding with local gradients in soil depth in a limestone d
ale at Burton in northern England. Variation in leaf RWC was analysed
in relation to soil depth, soil water potential and species compositio
n of the vegetation at the sampled sites. 2 Despite the unusual severi
ty of the drought, low RWC was confined to the vegetation of shallow d
aleside soils and rock outcrops where turgor remained conspicuously hi
gher in tap-rooted forbs such as Sanguisorba minor and Pimpinella saxi
fraga. Over the sampled area as a whole, it was apparent that desiccat
ion-avoidance through continued access to subsoil moisture was more im
portant as a controller of leaf RWC than restriction of transpiration.
3 Under the extreme conditions of 1995 differences in water relations
became apparent between several pairs of congeners and morphologicall
y similar species co-existing in the same communities. 4 In species wi
th distributions concentrated on the deeper soils of the plateau and v
alley bottom, a consistent correlation was established between declini
ng frequency of occurrence and falling values in RWC. This relationshi
p was due to the failure of outlying populations on shallow soil to ma
intain turgor and suggested that extreme moisture stress was acting as
a resetting mechanism restricting the excursion of drought-sensitive
species on to the areas of shallow soil. 5 With the exception of a sma
ll number of tap-rooted plants, species associated with the shallow so
ils and rock outcrops showed a negative relationship between abundance
in communities and leaf RWC; this supports the hypothesis that areas
of shallow soil are suboptimal for such species and merely provide a r
efuge from the competitive effects of the more robust species occupyin
g the deeper soils.