“…The decrease in ∆ 13 C in the red spruce tree rings from 1940 to 1989, corresponding to reductions in A and g c , has been shown in many studies examining the effects of acidic sulfur pollution on the C isotope signatures of trees (Boettger, Haupt, Friedrich, & Waterhouse, ; Kwak et al., ; Rinne, Loader, Switsur, Treydte, & Waterhouse, ; Santruckova, Santrucek, Setlik, Svoboda, & Kopacek, ; Savard, Bégin, Parent, Smirnoff, & Marion, ), including species from the eastern United States (Li et al., ; Thomas et al., ). The increase in ∆ 13 C, corresponding to increases in A and g c , that we observed after 1989 as SO 2 emissions declined, has also been found in studies as a function of decreasing pollution (Boettger et al., ; Li et al., ; Thomas et al., ), and is opposite from observations of reduced tree ring ∆ 13 C with increased tree height or as trees get older (Brienen et al., ; McDowell, Bond, Dickman, & Ryan, ). Thus, our data are consistent with the hypothesis that reductions in acidic air pollution and deposition from the historically high totals in the 1970s reached a critical level around 1989 that red spruce trees were better able to tolerate, thereby beginning the recovery of tree growth and photosynthetic physiology of red spruce trees in the Central Appalachian Mountains that has persisted for 25 years as pollution levels continued to decline.…”