Abstract - Large Mammalian Herbivores, Plant Interactions, and Ecosystem Processes in Five National Parks
Singer, Francis J. and Zeigenfuss, Linda. 1998. Large Mammalian Herbivores, Plant Interactions, and Ecosystem Processes in Five National Parks. 17 p.
Deciduous shrubs of wooded riparian areas may be declining in Wind Cave National Park, South Dakota. It is theorized that encroachment of Ponderosa pine (Pinus ponderosa) as the result of fire suppression and heavy utilization of shrubs by elk (Cervus elaphus) are contributing to this decline. Using large fenced exclosures and prescribed burning, we investigated the impacts of these factors on shrub production and regeneration. Four hypotheses were proposed: (1) Fire suppression has led to the decline of shrubs in Woody draw communities, and conversely reintroduction of burning will lead to an increase in shrub production and regeneration. (2) Excessive grazing has an effect on the production and regeneration of shrubs. (3) Hot fall burns (fall vs. spring) have a greater effect on the production and regeneration of shrubs. (4) Some combination of these two factors (grazing and fire suppression) is responsible for the decline in shrub production in woody draws. Burning reduced shrub canopy volume in areas open to browsing/grazing immediately following burning, but increased regeneration of elm (Ulmus americana) and box elder (Acer negundo). Herbivory on shrubs in burned plots increased in the summer and winter following burning, particularly on spring burns. Fall burning had a greater impact than spring burning, increasing canopy volume, area and production of Rosa spp. and Ribes aureum, but suppressed height and growth compared to spring burns. The combination of burning and grazing led to significant decreases in canopy cover, particularly on spring burns. Results suggest that fall prescribed burning could be used to increase regeneration in riparian areas of Wind Cave NP, but that provisions should be made to keep browsing intensities low immediately following burning.
Did You Know?
Winds caused by changes in barometric pressure are what give Wind Cave its name. These winds have been measured at the cave's walk-in entrance at over 70 mph. The winds at the natural entrance of the cave attracted the attention of Native Americans and early settlers.