Results/Conclusions
The fire scar data indicates a peak of burn frequency every 6-7 years from ca. 1880-1930 that is followed by a period virtually void of fire across the landscape. This changing fire regime was simultaneous with myriad other changes. For instance, our reconstructions indicate that there have been seven significant multi-year droughts in the last 500 years, yet none has occurred in the last 100 years. The most extreme droughts were centered on the years 1565 and 1630. PRISM data over the last century supported this finding, indicating a 100-year trend of cooler (-4-5° C) and wetter (3-15%) growing season conditions. Land-use has also been highly dynamic in the recent past. Forest cover in eastern North America was approximately 50-75% in 1850, but after a period of intense land-utilization (ending ca. 1930) that value had dropped to <5% across large portions of the region. This broad land-use dynamic surely influenced forest dynamics. Many other factors, including the loss of American chestnut and dramatic changes in wildlife population numbers, must also be drivers of ongoing forest dynamics. We propose a “multiple interacting disturbances hypothesis” for forests in the EDF which explicitly recognizes these complex and interacting forces.