VEGETATION RESPONSE TO WILDFIRE AND CLIMATE FORCING IN A ROCKY MOUNTAIN LODGEPOLE PINE FOREST OVER THE PAST 2500 YEARS
This research uses paleoecological proxies to reconstruct the impacts of wildfire on a lodgepole forest over the past 2500 years, a period including significant changes in regional climate. Chickaree Lake, Colorado, U.S.A., in Rocky Mountain National Park was chosen for the study site because of its small catchment size and existing paleoecological datasets. Pollen samples (n=51) were analyzed over multiple high-severity fire events previously reconstructed through charcoal analysis. A change in overall pollen composition was identified around 1,100 years ago when climate shifted towards modern conditions and Artemisia and Rosaceae pollen increased. Pinus was the dominant species throughout the record, however, there were visible decreases in Pinus pollen after fire events and small (<4%) but potentially ecologically significant quantities of Alnus and Sarcobatus pollen, which could replenish nitrogen stocks in post-fire successional sequences. These results help uncover the mechanisms that confer resilience within lodgepole forests to fire activity and reveal that variability in post-fire vegetation recovery can be important in understanding the long-term ecosystem dynamics of Rocky Mountain lodgepole pine forests.