S. Jose et Ar. Gillespie, COMPENSATORY MECHANISMS OF CENTRAL US HARDWOOD FOREST COMMUNITIES IN A CHANGING ENVIRONMENT, Plant ecology, 135(2), 1998, pp. 125-134
Although it is known that forest productivity is highly correlated wit
h canopy leaf area, the influence of environmental gradients within a
forest on leaf area-productivity relationships has not been well-docum
ented, particularly for mixed-species forests. The present study was c
onducted to define the mechanisms by which Central Hardwood forest com
munities respond to changes in environment. Ecological Land Type Phase
s (ELTPs) of the Central Hardwood region, delineated by soils, topogra
phy, and indicator vegetation, provided a framework to examine the imp
acts of environmental gradients on leaf area-productivity relationship
s at a landscape level. Three ELTPs(1) Quercus prinus / Carex picta-Va
ccinium, Dry slope, (2) Quercus alba-Acer saccharum / Parthenocissus,
Dry-Mesic Slope, and (3) Fagus-Acer saccharum / Arisaema, Mesic Slope-
were selected and stratified into three slope positions viz. the uppe
r edge of the community, the middle or center of the community on the
slope, and the lower edge of the community. Circular plots of 0.02 ha
in size were established for sampling. Standing stock (basal area, vol
ume, and biomass), annual production, leaf area index, and growth effi
ciency were determined for each slope position and examined to determi
ne the mechanisms and trends for community change across slope positio
ns. Among the three communities studied, dry slopes compensated for dr
ier conditions through both a shift in species composition and reduced
annual production. Dry-mesic slopes exhibited adaptation only through
changing species composition whereas mesic slopes compensated for dri
er conditions primarily through reduction in annual production. These
results indicate that mixed-species forest communities adjust to envir
onmental gradients through several mechanisms and that the relative im
portance of these mechanisms changes with community type.