Ra. Reed et al., SCALE DEPENDENCE OF VEGETATION-ENVIRONMENT CORRELATIONS - A CASE-STUDY OF A NORTH-CAROLINA PIEDMONT WOODLAND, Journal of vegetation science, 4(3), 1993, pp. 329-340
Vegetation and its correlation with environment has been traditionally
studied at a single scale of observation. If different ecological pro
cesses are dominant at different spatial and temporal scales, the resu
lts obtained from such observations will be specific to the single sca
le of observation employed and will lack generality. Consequently, it
is important to assess whether the processes that determine community
structure and function are similar at different scales, or whether, ho
w rapidly, and under what circumstances the dominant processes change
with scale of observation. Indeed, early work by Greig-Smith and assoc
iates (Greig-Smith 1952; Austin & Greig-Smith 1968; see Greig-Smith 19
79; Kershaw & Looney 1985; Austin & Nicholls 1988) suggested that plan
t-plant interactions are typically important at small scales, but that
the physical environment dominates at large scales. Using a gridded a
nd mapped 6.6 ha portion of the Duke Forest on the North Carolina pied
mont for a case study, we examined the importance of scale in vegetati
on studies by testing four hypotheses. First, we hypothesized that the
correlation between vegetation composition and environment should inc
rease with increasing grain (quadrat) size. Our results support this h
ypothesis. Second, we hypothesized that the environmental factors most
highly correlated with species composition should be similar at all g
rain sizes within the 6.6-ha study area, and should be among the envir
onmental factors strongly correlated with species composition over the
much larger extent of the ca. 3500 ha Duke Forest. Our data are not c
onsistent with either portion of this hypothesis. Third, we hypothesiz
ed that at the smaller grain sizes employed in this study (less-than-o
r-equal-to 256 m2), the composition of the tree canopy should contribu
te significantly to the vegetation pattern in the understory. Our resu
lts do not support this hypothesis. Finally, we predicted that with in
creased extent of sampling, the correlation between environment and ve
getation should increase. Our data suggest the opposite may be true. T
his study confirms that results of vegetation analyses can depend grea
tly on the grain and extent of the samples employed. Whenever possible
, sampling should include a variety of grain sizes and a carefully sel
ected sample extent so as to ensure that the results obtained are robu
st. Application of the methods used here to a variety of vegetation ty
pes could lead to a better understanding of whether different ecologic
al processes typically dominate at different spatial scales.