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Patterns of lodgepole pine regeneration following the 1988 Yellowstone fires
Affiliation:1. U.S. Geological Survey, MS 963 Denver Federal Center, Denver, CO 80225, USA;2. U.S. Geological Survey, School of Oceanography, University of Washington, Seattle, WA 98195, USA;3. Department of Biology, University of South Dakota, Vermillion, SD 57069, USA;4. U.S. Geological Survey, Fort Collins Science Center, 2150 Centre Ave, Fort Collins, CO 80526, USA;5. U.S. Geological Survey, Colorado Water Science Center, Denver Federal Center, Denver, CO 80225, USA;1. Institute of Geography, Friedrich-Alexander-University Erlangen-Nürnberg, Erlangen, Germany;2. Department of Wood and Paper Science & Technology, University of Tehran, Karaj, Iran;1. Department of Mathematics, North Carolina State University, Raleigh, NC 27695, United States;2. Department of Mathematics, Kennesaw State University, Marietta, GA 30060, United States
Abstract:In 1988, fires killed extensive lodgepole pine (Pinus contorta Dougl. ex. Loud) in Yellowstone National Park. This species bears both serotinous and non-serotinous cones, with the former most common in fire-origin stands of an even-aged character. Reconnaissance of burned stands indicated that former even-aged communities regenerated effectively. Others did not. The larger and more uniformly-sized seedling under formerly even-aged communities suggests primarily a single wave of regeneration there. Seedlings appeared to initiate to some degree over multiple years under other stands, but not sufficiently to make them well stocked. Four different regeneration pathways seem to characterize the natural reforestation of lodgepole pine following the 1988 fires. These include: (1) a dense, uniformly distributed cohort that will develop as a single-storied stand; (2) lodgepole pine islands that form over long periods around isolated seedlings; (3) a moderate to low density cohort that will gradually fill with multiple age classes over a protracted period; and (4) a cohort of only widely scattered single seedlings that initially form as small nearby tree islands, and may eventually converge into a more continuous stand with multiple age classes.
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