Abstract
Understanding plant physiological response to a rising atmospheric CO(2) concentration (c(a)) is key in predicting Earth system plant-climate feedbacks; however, the effects of long-term rising c(a) on plant gas-exchange characteristics in the tropics are largely unknown. Studying this long-term trend using herbarium records is challenging due to specimen trait variation. We assessed the impact of a c(a) rise of ~95 ppm (1927-2015) on the intrinsic water-use efficiency (iWUE) and maximum stomatal conductance (g(smax)) of five tropical tree species in Fiji using the isotopic composition and stomatal traits of herbarium leaves. Empirical results were compared with simulated values using models that uniquely incorporated the variation in the empirical g(smax) responses and species-specific parameterisation. The magnitude of the empirical iWUE and g(smax) response was species-specific, ranging from strong to negligible. Stomatal density was more influential than the pore size in determining the g(smax) response to c(a). While our simulation results indicated that photosynthesis is the main factor contributing to the iWUE gain, stomata were driving the iWUE trend across the tree species. Generally, a stronger increase in the iWUE was accompanied by a stronger decline in stomatal response. This study demonstrates that the incorporation of variation in the g(smax) in simulations is necessary for assessing an individual species' iWUE response to changing c(a).