Post‐fire succession and 20th century reduction in fire frequency on xeric southern Appalachian sites

. We document post-fire succession on xeric sites in the southern Appalachian Mountains, USA and assess effects of 20th century reduction in fire frequency on vegetation structure and composition. Successional studies over 18 yr on permanent plots that had burned in 1976–1977 indicate that tree mortality and vegetation response varied with fuel load and fire season. In the first three years after fire, hardwood sprouts dominated tree regeneration. On sites where summer and autumn fires reduced litter depth to less than 1 cm, densities of shade-intolerant Pinus seedlings increased steadily over this period. 4 to 8 yr after fire, large numbers of newly established seedlings and sprouts had grown to 1 – 10 cm DBH. By year 18 growth of these saplings led to canopy closure on most sites. Herbaceous cover and richness peaked in the first decade after fire, then declined. On similar sites that had not burned in more than 50 yr, regeneration of shade-intolerant Pinus spp. and mean cover and richness of herbs were considerably lower than those observed on recently burned plots. Reconstructions of landscape conditions based on observed post-fire succession and 20th century changes in fire regime suggest that reductions in fire frequency circa 1940 led to substantial changes in forest structure and decreases in cover and richness of herbaceous species.

[1]  C. Pyle The Type and Extent of Anthropogenic Vegetation Disturbance in the Great Smoky Mountains Before National Park Service Acquisition , 1988 .

[2]  W. B. Critchfield,et al.  Subdivisions of the genus Pinus (Pines). , 1969 .

[3]  Robert H. Whittaker,et al.  Vegetation of the Great Smoky Mountains , 1956 .

[4]  James M. Vose,et al.  Vegetation dynamics after a prescribed fire in the southern Appalachians , 1999 .

[5]  D. Engle,et al.  Effects of late growing‐season and late dormant‐season prescribed fire on herbaceous vegetation in restored pine‐grassland communities , 1998 .

[6]  B. H. Honkala,et al.  Silvics of North America , 1990 .

[7]  T. Waldrop,et al.  A comparison of fire intensity levels for stand replacement of table mountain pine (Pinus pungens Lamb.) , 1999 .

[8]  L. S. Barden,et al.  Effects of Fire on Pine and Pine-Hardwood Forests in the Southern Appalachians , 1976 .

[9]  J. Vose,et al.  Using fire to restore pine/hardwood ecosystems in the Southern Appalachians of North Carolina , 1997 .

[10]  Margaret M. Moore,et al.  Southwestern Ponderosa Forest Structure: Changes Since Euro-American Settlement , 1994, Journal of Forestry.

[11]  P. White,et al.  Changes in Xeric Forests in Western Great Smoky Mountains National Park, 1936-1995 , 1998 .

[12]  Catherine Keever,et al.  Causes of Succession on Old Fields of the Piedmont, North Carolina , 1950 .

[13]  C. E. Van Wagner,et al.  The theory and use of two fire history models , 1985 .

[14]  L. S. Barden Lightning Fires in Southern Appalachian Forests , 1974 .

[15]  M. Harmon Survival of trees after low-intensity surface fires in Great Smoky Mountains National Park , 1984 .

[16]  R. Peet,et al.  Prediction of man’s impact on plant species diversity , 1983 .

[17]  M. Harmon Fire History of the Westernmost Portion of Great Smoky Mountains National Park , 1982 .

[18]  C. Woodhouse,et al.  Two centuries of fire in a southwestern Virginia Pinus pungens community , 1995 .

[19]  John Kartesz,et al.  A Synonymized Checklist of the Vascular Flora of the United States, Canada and Greenland , 1980 .