COS 15-6
Using tree rings of red spruce in the Central Appalachian Mountains to explore growth trends before and after the Clean Air Act

Monday, August 10, 2015: 3:20 PM
338, Baltimore Convention Center
Justin M. Mathias, Department of Biology, West Virginia University, Morgantown, WV
Leigh A. Scholtz, Biology, West Virginia University
Benjamin Russell, Biology, West Virginia University
Richard B. Thomas, Department of Biology, West Virginia University, Morgantown, WV

Acid deposition caused by pollutant emissions (NOx and SO2) has detrimental effects on ecosystem structure and function. Acid deposition causes cation leaching from leaves and soils, reduced soil pH, and reductions in frost hardiness in some tree species. Red spruce (Picea rubens Sarg.) trees are considered to be an iconic indicator species for the effects of acid deposition. Since the Clean Air Act (1970), pollutant emissions have declined nationally by ~58% from the highest recorded emissions in 1973. We analyzed annual growth rings of red spruce trees growing in the central Appalachian Mountains to examine the growth response to historical changes in pollution. Twenty red spruce trees were cored at each of three forested sites along an 800 km latitudinal transect in eastern West Virginia from which basal area increment (BAI) was calculated. On a subset of five trees δ13C was measured on bulk wood on an annual time scale and converted to D13C to account for changes in atmospheric δ13C. To determine environmental drivers of BAI and D13C from 1940-2013, we used a multivariate analysis with local climatic variables (e.g. mean annual precipitation and temperature), U.S. SO2 and NOx emissions, and atmospheric CO2 concentrations.


We observed that red spruce tree BAI increased from ~1900 to 1940, after which there were large declines in growth. However, at all three red spruce stands, BAI increased after the Clean Air Act. We used a third order polynomial function to estimate the year when the trend changed from a decline to an increase in BAI. For two red spruce sites this change occurred ~1986 and in the third site ~1992. The rates of decline between 1940 and the mid-1980s were not different between sites; nor was the rate of recovery after the mid-1980s. Preliminary isotopic data from one of the sites indicates a sharp transition in D13C, where there is a strong enrichment in the heavier isotope prior to 1989, after which there is a reversal in D13C, indicating a strong depletion in the heavier isotope. These isotopic results are consistent with those found for red cedar trees in a close-by site, which suggests that recovery from acidic deposition involved increased stomatal conductance and photosynthesis. Our data suggest a similar response by red spruce trees and a potentially more widespread response to reduced acid deposition since the Clean Air Act.