An approach is detailed for calculating historical rates of CO2 uptake
and water loss of leaves from measurements of leaf delta(13)C composi
tion and climatic information. This approach was applied to investigat
e leaf gas exchange metabolism of woody taxa during the past 200 years
of atmospheric CO2 increase and in response to the longer-term atmosp
heric CO2 increases plants experienced over the Pleistocene. Reconstru
cted net assimilation rates and water use efficiencies increased in re
sponse to increasing atmospheric CO2 concentrations in both sets of ma
terial, whereas stomatal conductance, showing the combined responses o
f changes in stomatal density and leaf assimilation rates, was general
ly less responsive. Woody temperate taxa maintained a nearly constant
c(i)/c(a), ratio in response to the increase in atmospheric CO2 concen
trations over both timescales, in part, as a result of changes in stom
atal density. The reconstructed leaf-scale physiological responses to
past global climatic and atmospheric change corroborated those anticip
ated from experimental work indicating the adequate capacity of experi
ments, at least at the scale of individual leaves, to predict plant re
sponses to future environmental change.