![]() Romme WH, Kaufmann M, Veblen TT, Regan C (2003) Interim Hayman Fire case study analysis: ecological effects. ![]() Romme W, Turner M (2004) Ten years after the 1988 Yellowstone fires: is restoration needed? In ‘After the Fires: the Ecology of Change in Yellowstone National Park’. Frontiers in Ecology and the Environment 4, 481–487. (2006 ) Managing fire-prone forests in the western United States. ![]() Noss RF, Franklin JF, Baker WL, Schoennagel T , Moyle PB NIFC (2007) National Interagency Fire Center. (2006 ) Wildfire effects on microbial biomass and diversity in pine forests at three topographic positions. (Washington State University, Cooperative Extension Service, College of Agriculture: Pullman, WA) In ‘Management of Lodgepole Pine Ecosystems: Symposium Proceedings’. Lotan JE (1975) The role of cone serotiny in lodgepole pine forests. (2004 ) Salvage harvesting policies after natural disturbance. Lindenmayer DB, Foster DR, Franklin JF, Hunter ML, Noss RF, Schmiegelow FA , Perry D MS thesis, University of Wisconsin, Madison. Levitt EA (2006) Sources of variation in soil nitrogen availability among post-fire lodgepole pine stands in Yellowstone National Park. ![]() (1999 ) A 70-year retrospective analysis of carbon fluxes in the Canadian Forest Sector. Koch P (1996) ‘Lodgepole Pine in North America.’ (Forest Product Society: Madison, WI) (2005 ) Effects of prior land use on spatial heterogeneity of soil nutrients in southern Appalachian forests. (Springer: New York)įraterrigo JM, Turner MG, Pearson SM , Dixon P (Eds GM Lovett, CG Jones, MG Turner, KC Weathers) pp. In ‘Ecosystem Function in Heterogeneous Landscapes’. Forest Ecology and Management 136, 85–95.įranklin JF (2005) Spatial pattern and ecosystem function: reflections on current knowledge and future directions. (2000 ) Suitability and use of the 15N-isotope dilution method to estimate nitrogen fixation by actinorhizal shrubs. Journal of Geophysical Research 108, WFX 1-1 to 1-10. | Crossref | GoogleScholarGoogle Scholar |īond-Lamberty B, Wang C, Gower ST (2003) Annual carbon flux from woody debris for a boreal black spruce fire chronosequence. Frontiers in Ecology and the Environment 5, 145–152. (2007 ) Filling key gaps in population and community ecology. In summary, the YNP landscape is recovering rapidly from the 1988 fires through natural mechanisms, owing to the abundance and spatial heterogeneity of post-fire residuals, but other systems with fewer biotic legacies may be less resilient to such large, severe fires.Īgrawal AA, Ackerly DD, Adler F, Arnold AE, Cáceres C, Doak DF, Post E, Hudson PJ, Maron J, Mooney KA, Power M, Schemske D, Stachowicz J, Strauss S, Turner MG , Werner E For example, at broad scales, C storage in YNP appears resistant to changes in age-class structure associated with large stand-replacing fires. In response to these post-fire patterns, heterogeneity in carbon (C) and nitrogen (N) storage, N mineralisation, decomposition, and productivity was also evident at multiple scales and may confer resiliency to large fires. Post-fire heterogeneity in stand age, coarse wood abundance, microbial and understorey communities reflected interactions between existing pre-fire patterns and fire severity at different scales, suggesting that environmental context plays an important role in successional responses to large fires. Ecological heterogeneity at multiple scales may enhance resilience to large, severe disturbances by providing structural, biological and functional redundancy. We characterised the remarkable heterogeneity following the large, severe fires of 1988 in Yellowstone National Park (YNP), in the northern Rocky Mountains, Wyoming, USA, by focussing on spatial variation in post-fire structure, composition and ecosystem function at broad, meso, and fine scales.
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