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The 1988 fires in Yellowstone National Park (YNP), Wyoming, affected > 250,000 ha, creating a striking mosaic of burn severities across the landscape which is likely to influence ecological processes for decades to come (Christensen et al. 1989, Knight and Wallace 1989, Turner et al. 1994). Substantial spatial heterogeneity in early post-frre succession has been observed in the decade since the frres, resulting largely from spatial variation in frre severity and in the availability of lodgepole pine (Pinus contorta var. latifolia) seeds in or near the burned area (Anderson and Romme 1991, Tinker et al. 1994, Turner et al. 1997). Postfire vegetation now includes pine stands ranging from relatively low to extremely high pine sapling density (ca 10,000 to nearly 100,000 stems ha-) as well as non-forest or marginally forested communities ( < 1000 saplings ha-) in some areas previously characterized by coniferous forest.

Above-Ground Net Primary Production, Leaf Area Index, and Nitrogen Dynamics in Early Post-Fire Vegetation, Yellowstone National Park