Hybrids: Dorman  suggests that natural hybridization occurs, to a small degree, between Table Mountain pine and shortleaf pine (Pinus echinata), and between Table Mountain pine and pitch pine (P. rigida). This conclusion is based on occurrence of trees with intermediate morphological characteristics.
FEDERAL LEGAL STATUS:
No special status
Information on state-level protected status of plants in the United States is available at Plants Database.
HABITAT TYPES AND PLANT COMMUNITIES:
Table Mountain pine is common in upland yellow pine communities that are dominated by Table Mountain pine, pitch pine, shortleaf pine, and Virginia pine (Pinus virginiana) with an understory of chestnut oak (Quercus prinus) [7,13]. It is also often found in pure stands or co-dominant with pitch pine . Other understory tree species that may be present in Table Mountain pine stands are red maple (Acer rubrum), black tupelo (Nyssa sylvatica), sourwood (Oxydendrum arboreum), scarlet oak (Quercus coccinea), bear oak (Q. ilicifolia), white oak (Q. alba), post oak (Q. stellata), southern red oak (Q. falcata), blackjack oak (Q. marilandica), black oak (Q. velutina), American chestnut (Castanea dentata), black locust (Robinia pseudoacacia), eastern hemlock (Tsuga canadensis), and sweet birch (Betula lenta) [4,7,12,19,69]. Table Mountain pine populations in northeastern Georgia are also associated with hickory (Carya spp.) and eastern white pine (Pinus strobus) . On Looking Glass Rock, western North Carolina, Table Mountain pine grows with eastern redcedar (Juniperus virginiana) . Mountain-laurel (Kalmia latifolia) is the most common shrub species associated with Table Mountain pine stands. Other ericaceous shrub species such as mountain fetterbush (Pieris floribunda), hillside blueberry (Vaccinium pallidum), black huckleberry (Gaylussacia baccata), bear huckleberry (G. ursina), and several species of rhododendron (Rhododendron spp.) are common associates [12,23,85].
Table Mountain pine is associated with the Virginia pine-oak , Virginia pine , pitch pine , shortleaf pine , and chestnut oak  cover types, as recognized by the Society of American Foresters.
Table Mountain pine is a dominant species in the following vegetation types and plant communities:North Carolina:
Morphology: Table Mountain pine is a native, slow-growing conifer. It is often small in stature and exceedingly limby . It rarely grows beyond 66 feet (20 m) tall [21,66,92], though the tallest individual recorded was 95 feet (29 m) . Table Mountain pine is typically around 16 inches (40 cm) DBH [21,66,92]. The maximum recorded DBH was 34 inches (94 cm) .
The trunks of Table Mountain pine are often crooked and have irregularly shaped cross-sections [23,91,92]. Older trees tend to be flat-topped, while young trees can vary in form from that of a large bush when open-grown, to slender with relatively small limbs when grown in a dense stand . Table Mountain pine typically has long, low-lying, thick limbs on much of the trunk [23,91,92]. The limbs remain alive on over half of the length of the bole. Even in closed stands, where branches are smaller and limited to the upper trunk, Table Mountain pine retains branch stubs for long periods of time [91,92]. The bark of Table Mountain pine is broken by fissures into irregular plates  and is nearly smooth to flaky . Zobel  states that bark thickness increases linearly with the increase in diameter.
Throughout its range, the needles of Table Mountain pine average 2.7 inches (6.8 cm) in length, ranging from 1.3 inches (3.3 cm) to 4.1 inches (10 cm). They are borne in a 2-needle fascicle. Three-needle fascicles may occur on the same tree but are rare [21,92]. Needles and fascicles are retained for 2 to 3 years [22,60].
Male cones are 0.6 inches (1.5 cm) long. Female cones are sessile, range from 1.7 to 4.1 inches (4.2-10 cm) long, and occur in whorls of 2 to 7. Cone scales are tough and armed with broad, stout, upwardly curving spines [21,23,55,66,92]. Female cones are typically serotinous, although serotiny varies among individuals  and populations [91,92]. See Seed dispersal for more information on the serotiny of this species. Seeds are triangular and approximately 0.25 inches (0.63 cm) long, with wings about 1 inch (2.5 cm) long . The size of cones and seeds decreases with increasing elevation .
Table Mountain pine seedlings generally anchor their taproot into a rock crevice. Secondary or lateral roots then spread through soil and litter, taking up both moisture and nutrients. Other sinker roots descend into additional crevices, utilizing accumulated soil and the thin skins of finely weathered, nutrient-rich, moist soil-like rock which coat the crevice surface .
Age class structure: The age class structure of many Table Mountain pine stands suggests that fire is an important influence on stand structure and regeneration . Many Table Mountain pine stands observed on the Chattahoochee National Forest, Georgia are represented by large DBH size classes, suggesting older age classes, and show no evidence of pine regeneration . Williams and Johnson  report that the age distribution of Table Mountain pine in pine-oak forests near Blacksburg, Virginia, was bimodal with peaks in the seedling (10 year old) and large tree (45 to 80 year old) age classes. Estimated stem ages for the study area ranged from 1 to 124 years. There were few individuals in the 20- to 35-year age classes. This gap in age distributions suggests that recruitment may be episodic  (e.g., following periodic fire) in these populations.
The presence of many size classes suggests that some Table Mountain pine stands can persist for long periods in the absence of fire. Table Mountain pine stands that appear to be "permanent" are generally associated with a sparse understory, shallower litter, more rock outcrop, and less basal area, than stands that are moving towards a late-seral, oak-dominated forest, with 1 size class of pines, no pine reproduction, and a dense understory of shrubs . Three Table Mountain pine stands located on a xeric, southwest shoulder of Looking Glass Rock, North Carolina, were reported to have continuous recruitment in the absence of fire for 87 years. The age structure of these stands suggests relatively continuous recruitment during each of 3, 20-year periods with a mortality rate of 50% per period, except for one period in which 2 severe droughts were thought to decrease recruitment and increase mortality of saplings and seedlings. Sites supporting continuous recruitment had shallow, rapidly draining soils and little or no mountain-laurel present .
A maximum age of 250 years is reported for Table Mountain pine. The oldest recorded individuals in the Appalachians were 227 and 205 years, and were found in the southwest corner of North Carolina .RAUNKIAER  LIFE FORM:
Fire aids the regeneration of Table Mountain pine in several ways. It opens the serotinous cones, consumes litter, exposes mineral soil, and eliminates competing vegetation, allowing more light and water for pine seedlings and minimizing allelopathic effects .
Pollination: Table Mountain pine is pollinated by wind .
Breeding system: Table Mountain pine is monoecious . Feret and others  found that Table Mountain pine stands in southwest Virginia have large genetic variability within a relatively small area.
Table Mountain pine is predominantly outcrossed .
For information on how fire relates to Table Mountain pine genetic diversity see Recurrent fire and maintenance of genetic diversity.
Seed production: Table Mountain pine begins cone and viable seed production when saplings are 5 to 7 years old [15,47,49,76]. Della-Bianca  states that, although Table Mountain pine cones shed their seeds irregularly, large numbers of seeds are disseminated annually. On Looking Glass Rock, North Carolina, Table Mountain pine produced one whorl of 2 to 5 cones each year on the new growth of branches. Cones remained closed for 2 to 5 years after maturity, and then about 40% of them opened without fire. Cones remained attached to the stem for a decade or longer, whether or not they opened .
Patterns of seed production in Table Mountain pine were studied by Gray and others  to determine if Table Mountain pine seed viability and availability varied with tree age, cone age, and season. Cones were collected from stands where Table Mountain pine was the main component and where a wide range of age classes was present. Seed viability was determined in a greenhouse where cones were dried in an oven for a minimum of 12 hours at 140 °F (60 °C) to allow them to open. Following drying, seeds were extracted, wings removed and germination tests conducted. The average number of seeds per cone tended to be higher in the younger age classes (5-25 years); however, viability was lowest in the 5- to 10-year-old age class .
|Average number of seeds/cone and percent viability of seeds for Table Mountain pine by tree age class |
|Tree age class (years)||Average number of seeds/cone*||Average percent viability of seed|
|5 to 10||46.0a, b||8.8b|
|11 to 25||51.9a||33.3a|
|26 to 50||43.5a, b||32.7a|
|51 to 75||41.5b||32.9a|
|*Averages followed by the same letter do not differ at alpha=0.05|
|Average number of seeds/cone and percent viability of seeds for Table Mountain pine by cone age |
|Cone age (years)||Average number of seeds/cone*||Average percent viability of seed|
|*Averages followed by the same letter do not differ at alpha=0.05|
|Average number of seeds/cone and percent viability of seeds for Table Mountain pine by season collected |
|Season collected||Average number of seeds/cone*||Average percent viability of seed|
|*Averages followed by the same letter do not differ at alpha=0.05|
Table Mountain pine cones open in response to heat. When cones were heated in an oven at 210 °F (100 °C), 9% opened within 2 minutes, 78% opened between 2 and 4 minutes, and 100% opened after 7.5 minutes . McIntyre  observed that Table Mountain pine cones placed by a furnace "opened readily" at approximately 95 °F (35 °C), and that the temperature at the end of a Table Mountain pine branch in full sunlight in the field averaged 95 °F (35 °C). This suggests that cones in the shade may not be exposed to temperatures sufficient to open cones, and may therefore remain closed for several years until exposed to adequate temperature regimes .
Table Mountain pine seeds are dispersed with the aid of large wings .
Seed banking: Table Mountain pine maintains an aerial seed bank of viable seeds in serotinous cones an average of 9 to 11 years [3,6,49] and up to 30 years . Table Mountain pine establishes from seed released from canopy seed banks after fire .
Germination: Germination of Table Mountain pine occurs after cones open and seeds are released, as long as there is a suitable seedbed . Groeschl and others  state that overstory canopy reduction, a decrease in forest floor litter, and the elimination of dense shrub layers are necessary to ensure adequate germination and establishment of Table Mountain pine. In the past, infrequent, high-severity crown fires provided these conditions [3,33,85,91]. However, a field and greenhouse study by Waldrop  reported that germination was higher under shade than in full sun, and was highest under 63% shade. Germination on 2 and 4 inches (5 and 10 cm) of duff was comparable to germination on no duff. Results suggest that lower severity fires can produce a suitable seedbed for germination of Table Mountain pine . Barden [2,3,6] describes stands of Table Mountain pine on an extremely xeric site in western North Carolina that exhibited continuous recruitment despite the absence of fire since 1889.
A greenhouse study by Mohr and others  compared germination rates of Table Mountain pine seeds on different duff depth and shade level combinations to determine the best microhabitat for germination and survival of Table Mountain pine seedlings. Seeds were placed on duff 0, 2, and 4 inches (0, 5, and 10 cm) deep, and shade levels were 0% (full sun), 38%, 52%, and 98%. Samples were watered twice a week during June, once a week in July, and every 10 days in August. Germination was not statistically different on different duff depths or under different shade levels (see table below). Seedling height varied little among duff depths, while shade had a significant effect on seedling height (see table below). Seedling survival was greatest with 2 or 4 inches (5 or 10 cm) of duff. Moderate shade (52%) with either 2 or 4 inches (5 or 10 cm) of duff was the best treatment combination in this study for Table Mountain pine seedling survival. These results suggest that germination and establishment of Table Mountain pine is possible after low-severity fire or possibly without fire.
|Mean percent germination and seedling height by duff depth and shade level |
|Treatment level||Mean percent germination||Seedling height* (inches)|
|Duff depth (inches)|
|Shade level (percent)|
|*Means followed by the same letter within a treatment group are not significantly different at the 0.05 level|
Seedling establishment/growth: The requirements for successful Table Mountain pine seedling establishment and growth are unclear, and may vary among sites and plant communities. Zobel  states that very few Table Mountain pine seedlings occur on sites without exposed mineral soil or on sites with a dense canopy or shrub layer. These microsite conditions often occur after fire . Whether or not high-severity, stand-replacing fires are needed to create these conditions is unclear. A greenhouse study  found that seedling establishment of Table Mountain pine was most successful on 2 or 4 inches (5 or 10 cm) of duff and under moderate shade (52%) (see table above). These results suggest that establishment of Table Mountain pine may be possible after low-severity fire or possibly without fire. For complete details on how seedling establishment and regeneration is effected by fire, see Discussion and Qualification of Plant Response.
In Virginia, the low availability of suitable seedling habitat strongly limits recruitment of Table Mountain pine in pine-oak forests. Williams  found that Table Mountain pine seedlings occurred almost exclusively in open microsites with shallow pine litter, which are relatively rare in mature pine-oak forest. Summer drought also contributed to low seedling survivorship, particularly in very young seedlings. He concludes that optimal regeneration and maintenance of Table Mountain pine are unlikely in the absence of fire when occurring in pine-oak forests suitable for growth of hardwoods, particularly oaks. Increased oak dominance leads to site modifications that are detrimental to Table Mountain pine recruitment such as litter accumulation and shading [84,86,87].
Oak litter accumulation and available soil moisture impact Table Mountain pine seedling establishment. A greenhouse study was conducted by Williams and others  to distinguish these effects. Soil and litter were taken from a pine-oak forest on Brush Mountain, Virginia. Oak litter was comprised of chestnut oak and scarlet oak. Pine litter was comprised of Table Mountain pine and pitch pine needles. Litter-free flats lost more water than flats with litter, and there was little difference in soil moisture between the pine and oak litter flats. Leaf litter, water regime, and the interaction of these factors had significant (P=0.0001) effects upon seedling mortality and survival. Mean seedling emergence and mortality for Table Mountain pine are provided in the table below .
|Mean seedling emergence and mortality (percent) for Table Mountain pine under different soil moisture regimes and leaf litter accumulations |
|Litter-free||Pine litter||Oak litter|
|Watering interval||Seedling emergence||Mortality||Seedling emergence||Mortality||Seedling emergence||Mortality|
Oak litter had a negative effect on Table Mountain pine seedlings when compared to that of pine litter and litter-free treatments, although it did not completely hinder recruitment. Several germinated but desiccated Table Mountain pine seeds were recovered from oak litter treatments during harvest of seedlings. Allelopathic effects are not believed to be the reason for lowered seedling emergence in oak litter, since the seedling mortality was similar between the oak and pine litter treatments. Further studies are needed to understand possible allelopathic effects of oak litter on establishment of Table Mountain pine .
Vegetative regeneration: Table Mountain pine can sprout from the base after the stem is injured [19,39,46,56,65,91]. It has one or more basal buds near the cotyledonary level with additional buds often appearing an inch or so above this point that elongate readily only after injury [19,65,91]. Seedlings of "natural origin" usually have a crook just above or just below ground level which may serve to protect basal buds against fire [19,91]. Some buds appear to be short-lived, but the sprouting of cut stumps of large Table Mountain pine trees suggest that some persist .
Table Mountain pine is endemic to the Appalachian Mountains and commonly dominates steep, rocky ridges and exposed escarpments too marginal for many tree species [23,28,41,91]. Throughout its range, Table Mountain pine is most commonly found on south- and west-facing slopes at elevations ranging from 1,000 to 4,000 feet (305-1,220 m) [7,12,91]. Elevation extremes are noted from about 150 feet (46 m) near Delaware to over 4,700 feet (1,430 m) in Tennessee. In the Great Smoky Mountains of Tennessee and North Carolina, it has been reported in elevations up to 5,800 feet (1,767 m). Outlying populations are associated with monadnocks (isolated mountain or rocky mass in an otherwise level area), and other eastern range extensions are along major rivers. Table Mountain pine has been reported around bogs on Mt. Pisgah, North Carolina, and at Big Meadows, Shenandoah National Park, Virginia .
Soils: Stands dominated by Table Mountain pine are usually associated with exposed rocky sites with shallow soil over bedrock or a very high rock content [23,42]. The soil series where Table Mountain pine dominates are generally stony; shallow, sometimes without profile development; strongly acidic (pH 4.5-5.5); infertile and of low productivity; and well to excessively drained [12,42,91].
On Looking Glass Rock, western North Carolina, stunted (<33 feet (<10 m) tall) Table Mountain pine survive where the soil depth in cracks and depressions in the granite is 4 to 16 inches (10-40 cm) .
Climate: The climate throughout Table Mountain pine's narrow range is warm, humid, and continental. Average monthly high temperatures range from 20 °F (-7 °C) in January to 85 °F (29 °C) in July. Mean annual precipitation ranges from 30 to more than 80 inches (760-2,030 mm) distributed evenly throughout the year [13,19]. The average number of frost-free days in Pennsylvania varies from 150 to 170, and from 170 to 180 in the mountains of Tennessee, North Carolina, and northern Georgia . Table Mountain pine most often occurs on the warmest and driest microsites within these areas .
Table Mountain pine is a shade-intolerant and drought tolerant pioneer species that typically establishes stands following disturbance, such as fire [12,15,25,40,41,70]. In later seral stages, on sites suitable for growth of hardwood species, it is replaced by more shade-tolerant hardwoods, specifically oaks, with mountain-laurel understories [12,15,56,68]. Stands with dense mountain-laurel understories and established oaks lack regeneration niches needed by Table Mountain pine . Outbreaks of southern pine bark beetle and ice storms hasten succession toward oak dominance because they both select against Table Mountain pine . Regeneration of Table Mountain pine on sites favorable for the growth of oaks and other hardwoods, like the pine-oak forests of Brush Mountain, Virginia, occurs only after fire. On sites favorable for the growth of oaks, incorporating fire at frequent intervals would facilitate the maintenance of Table Mountain pine .
Table Mountain pine may produce self-maintaining or nonsuccessional populations . Populations of Table Mountain pine occur and reproduce in the absence of fire on dry exposed ridges and bedrock outcrops .
In northwestern North Carolina, pollen release at 1,500 feet (457 m) elevation begins the last week of March and ends during the first week in April; at 2,500 feet (762 m), pollen release begins about the second week in April and ends near the end of the third week. Cones ripen in autumn of the second season. The opening of cones depends on the degree of serotiny . Seeds are shed from September to November , although on Brush Mountain, Virginia, seedfall of Table Mountain pine occurred throughout the year but was primarily concentrated in the spring and summer months .
Table Mountain pine's early spring development and reproductive activity (development of male and female strobili) could exclude it from extensively colonizing areas with later spring frosts. By "flowering" and initiating twig growth earlier, Table Mountain pine is more susceptible to frost damage than other pine species studied .
FIRE ECOLOGY OR ADAPTATIONS:
Fire adaptations: Table Mountain pine has adaptations to fire that are consistent with both long- and short-return-interval fire regimes. Medium-thick to thick bark, a deep rooting habit, self-pruning limbs, and pitch production to seal wounds are characteristics of Table Mountain pine that suggest it is adapted to survive frequent, low-severity fire [3,39,47,52,67,73,76,85]. Delayed seed release from serotinous cones and trees that produce viable seed at a young age also allow Table Mountain pine populations to persist after infrequent, high-severity fire [47,73].
Table Mountain pine can sprout following injury [39,46,56,65], such as that from fire or animal damage , but no data in the literature describe resprouting after fire in Table Mountain pine. Table Mountain pine seedlings of "natural origin" usually have a crook just above or just below ground level which may serve to protect basal buds against fire [19,91].
Fire regimes: Table Mountain pine was historically subject to a full range of fire types: frequent low-severity surface fires, mixed-severity fires, and stand-replacement fires [27,36,74]. Table Mountain pine is also adapted to a range of fire frequencies . Fire occurs infrequently on contemporary Appalachian landscapes  where Table Mountain pine is common.
Fire histories developed for 2 Table Mountain pine communities in southwestern Virginia revealed that between 1758 and 1944, fires burned approximately every 5 to 10 years during the dormant season. Recent regeneration failure of Table Mountain pine and increasing dominance of oak species appear to coincide with fire exclusion practices initiated after 1950 [67,68]. Based on USDA Forest Service records, Wade and others  state that between 1800 and 1944 the fire interval in sampled Table Mountain pine stands averaged 10 to 12 years, and that it is currently 7 to 70 years with an average of 40 years . The mean interval between fires, based on fire scars from pine forests in the Great Smoky Mountains National Park, for the period 1856 to 1940 was 12.7 years. Fires were more frequent, however, at lower elevations. Most of these fires were probably anthropogenic and may have been an important influence ever since Native Americans settled in the Little Tennessee River Valley .
Frost  uses the term polycyclic (communities with 2 or more kinds of fire cycles) to describe presettlement fire regimes in pitch pine-Table Mountain pine stands on dry, south-facing slopes. Past fire regimes in these communities consisted of a cycle of high-frequency, understory fires (about 5 to 7 years apart) interrupted periodically by a long fire-free interval (about 75 years) followed by stand-replacing fire. Frost categorizes Table Mountain pine as having a short fire-return interval (25 to 100 years). "Canopy thinning" occurs when fuel loading, fuel moisture, and wind create prolonged or severe fire behavior but fall short of initiating crown fire, and has been observed in pitch pine-Table Mountain pine stands in the southern Appalachians .
In the eastern United States, pitch and Virginia pine forests that Table Mountain pine is commonly associated with were subject to mixed fire regimes. Where burning by Native Americans was common, fire regimes in pitch pine communities were characterized by understory fires on a 2- to 10-year interval. Fire in Virginia pine was probably less frequent and resulted in higher tree mortality. These forest types are still characterized as mixed fire regime type because the fire return intervals are longer and the majority of wildfires occur during the growing season when damage is greater .
Based on species traits and presettlement site descriptions, Landers  suggests an "inferred fire regime" for Table Mountain pine stands in the southeastern United States, with "very intense fires" at a frequency of 2 per century . Where Table Mountain pine forms even-aged, pure stands, Wade and others  classify the fire regime as typically stand-replacement at intervals of <35 to 200 years.
|Fire regime information on vegetation communities in which Table Mountain pine may occur. For each community, fire regime characteristics are taken from the LANDFIRE Rapid Assessment Vegetation Models . These vegetation models were developed by local experts using available literature, local data, and/or expert opinion as documented in the PDF file linked from the name of each Potential Natural Vegetation Group listed below. Cells are blank where information is not available in the Rapid Assessment Vegetation Model.|
|Vegetation Community (Potential Natural Vegetation Group)||Fire severity*||Fire regime characteristics|
|Percent of fires||Mean interval
|Eastern woodland mosaic||Replacement||2%||200||100||300|
|Surface or low||89%||4||1||7|
|Rocky outcrop pine (Northeast)||Replacement||16%||128|
|Surface or low||52%||40|
|Surface or low||65%||12|
|Oak-pine (eastern dry-xeric)||Replacement||4%||185|
|Surface or low||90%||8|
|Appalachian oak forest (dry-mesic)||Replacement||2%||625||500||>1,000|
|Surface or low||92%||15||7||26|
|Vegetation Community (Potential Natural Vegetation Group)||Fire severity*||Fire regime characteristics|
|Percent of fires||Mean interval
|Southern Appalachians Woodland|
|Appalachian shortleaf pine||Replacement||4%||125|
|Surface or low||92%||6|
|Table Mountain-pitch pine||Replacement||5%||100|
|Surface or low||92%||5|
|Southern Appalachians Forested|
|Surface or low||89%||6||3||10|
|Oak (eastern dry-xeric)||Replacement||6%||128||50|
|Surface or low||78%||10||1||10|
|Appalachian Virginia pine||Replacement||20%||110||25||125|
|Surface or low||64%||35||10||40|
|Appalachian oak forest (dry-mesic)||Replacement||6%||220|
|Surface or low||79%||17|
Replacement=Any fire that causes greater than 75% top removal of a vegetation-fuel type, resulting in general replacement of existing vegetation; may or may not cause a lethal effect on the plants.
Mixed=Any fire burning more than 5% of an area that does not qualify as a replacement, surface, or low-severity fire; includes mosaic and other fires that are intermediate in effects.
Surface or low=Any fire that causes less than 25% upper layer replacement and/or removal in a vegetation-fuel class but burns 5% or more of the area [35,43].
IMMEDIATE FIRE EFFECT ON PLANT:
Table Mountain pine often survives fire, but trees can be top-killed or killed [71,75,77,79].
After passage of fire, the resin of the serotinous cones melts and the scales reflex for seed release and dispersal. Barden  reveals that 78% of cones opened after 2 minutes but before 4 minutes when heated in an oven at 210 °F (100 °C).
DISCUSSION AND QUALIFICATION OF FIRE EFFECT:
The effect of fire on Table Mountain pine is related to fire intensity and severity but cannot always be immediately determined. One year after prescribed fire in a mixed hardwood and pine (Table mountain pine and pitch pine) stand, tree mortality was significantly higher in areas of high and medium-high fire intensity, compared to areas with lower fire intensity. However, by the end of the 6th growing season after fire, almost all overstory pines and hardwoods were dead in all study plots burned at all intensities [75,77]. For a more complete summary of this study, see Early postfire response of Table Mountain pine stands burned under prescription at varying intensities.
PLANT RESPONSE TO FIRE:
Fire plays an important role in the maintenance of Table Mountain pine in most of the communities where it occurs . Fire opens serotinous cones, prepares a suitable seedbed for germination, and removes competition from the understory and overstory in the short-term .
DISCUSSION AND QUALIFICATION OF PLANT RESPONSE:
While it is commonly perceived that Table Mountain pine communities require high-severity crown fires for regeneration (e.g., [85,91]), additional evidence (e.g., [14,52,75,77]) suggests that Table Mountain pine communities can reproduce and persist under a regime of frequent, low-severity fire, and in some cases, in the absence of fire [3,6]. High-severity fires certainly result in reduced shading and competition, the opening of serotinous cones, and removal of forest floor, thus providing seed and a favorable seed bed for germination and establishment; and ample data provide evidence that Table Mountain pine reproduces and persists after high-severity fires [15,33,37,56,57,61,91]. Low-severity fires may not provide optimum conditions for Table Mountain pine regeneration . For example, about 3 months following a low-severity, spring prescribed burn on the Grandfather Ranger District, Pisgah National Forest, North Carolina, frequency and cover of Table Mountain pine seedlings increased; however, seedlings were not expected to survive due to shading and competition from overstory, midstory, and understory species [71,79]. For a complete summary of this study, see Early postfire response of southern Appalachian Table Mountain-pitch pine stands to prescribed fires.
Several studies have found greater regeneration of Table Mountain pine after high-severity fire than after low-severity fire. Zobel  sampled a recently burned Table Mountain pine stand in western North Carolina and noted that all Table Mountain pine cones were open, even though fire had been "light" in portions of the area. However, 2 years after fire, regeneration persisted only in areas where the overstory trees were killed, the undergrowth was almost completely killed, and erosion had exposed mineral soil . High-severity fire provided a favorable seedbed for germination of Table Mountain pine following a lightning-caused wildfire on Dovel Mountain, Shenandoah National Park, Virginia. The number of Table Mountain pine seedlings on burned areas the second year after fire was considerably higher than on unburned areas with high-severity, low-severity, and unburned patches averaging 6,997, 1,489, and 386 seedlings/ha, respectively . Regeneration of Table Mountain pine following an April 1986 fire on Bote Mountain, Great Smoky Mountains National Park, was most successful where fire severities were high. Study plots were located on areas that experienced low-severity (surface fire only), moderate-severity (surface fire with some scorching and torching of individual trees), and high-severity (crown fire) fires. Overall Table Mountain pine seedling densities were 1,250/ha, 15,312/ha, 18,304/ha in low-, moderate-, and high-severity plots, respectively. Of all seedlings counted 75.4% were found growing where the organic matter depth was less than 0.4 inches (1 cm) . Pine regeneration (Table Mountain pine and pitch pine combined) was greater after high-intensity fires (mean bark char height of 25 feet (7.6 m)) than repeated low-intensity fires, when dormant season prescribed burns were carried out in stands on xeric ridgetops in western North Carolina. Pine regeneration was 9,440 stems/ha on high-intensity burned plots, 34 stems/ha on low-intensity burned plots, and 7 stems/ha on control plots. Sparse regeneration on low-intensity plots could be due to the amount of duff left on these sites, the type of litter (hardwood litter detrimental to Table Mountain pine seedling survival), or the amount of shading from remaining overstory trees [56,57].
High-intensity, stand-replacement fires have been recommended to regenerate stands of Table Mountain pine; however, Mohr and others  (see Germination for details), Brose and Waldrop , and Waldrop and Brose [75,77] provide evidence that successful regeneration of Table Mountain pine can occur after low- and moderate-severity fires.
Brose and Waldrop  provide evidence from 9 uneven-aged Table Mountain pine-pitch pine stands across Georgia, Tennessee, and South Carolina, that suggests frequent periodic or continuous pine and hardwood recruitment under a regime of periodic surface fires during the past 100 to 150 years. These fires were likely low- to moderate-severity, given that cores and cross-sections were sampled from living chestnut oaks which would have been killed by a high-severity fire . The results of this study suggest that successful seedling establishment of Table Mountain pine can occur following low- and moderate-severity fire.
Waldrop and Brose [75,77] report effects of low, medium-low, medium-high, and high intensity fires on the establishment of Table Mountain pine seedlings after prescribed burning in the War Woman Wildlife Management Area of the Tallulah Ranger District in Georgia. Sixty sample plots were surveyed at the end of the 1st and 6th growing seasons after burning. In the 1st growing season, postburn pine density ranged from 1,396 seedlings/acre on the high intensity plots to more
Recurrent fire and maintenance of genetic diversity: Evaluation of the morphological features and life-history characteristics of Table Mountain pine provides strong evidence that the evolution of this species has been uniquely shaped by fire. Fire is instrumental in opening cones and creating suitable environmental and edaphic conditions for stand regeneration. Frequent fires are also important in perpetuating genetic diversity within stands. Routine burning of stands would allow for regular population turnover, in turn preventing loss of individual genotypes due to stand senescence and maintaining a majority of the intrapopulational genetic variation in living individuals .
Other information: This fire study provides information on postfire responses of plant species in communities that include Table Mountain pine:
Findings by Welch and others  on the first-year response of southern Appalachian Table Mountain pine and pitch pine stands to prescribed burning, suggest that prescribed fires in which objective is to restore these communities must open the canopy, reduce accumulated litter and duff layers, and expose regenerative buds of hardwoods to lethal temperatures in order to lessen postburn sprouting. Prescribed burns that do not accomplish these goals may further encourage succession towards hardwood-dominated stands . For complete details of this study, see Early postfire response of southern Appalachian Table Mountain-pitch pine stands to prescribed fires.
Declines in Table Mountain pine populations during the era of fire exclusion have greatly reduced the seed source for this species. Oaks have spread into these communities and, in many cases, dominate the canopy. In addition, there is tremendous litter build-up on these areas. A review by Buckner and Turrill  recommends intense, small scale prescribed burning to clear the forest floor down to mineral soil, eliminate hardwood competition, and allow Table Mountain pine regeneration. If the previous Table Mountain pine community was much depleted, this process might have to be repeated on a 5- to 7-year cycle, similar to the "pulsed" prescribed fire regime used to manage other yellow or hard pines of eastern North America . Such burning practices could restore Table Mountain pine populations on a local scale .
If management of declining populations of Table Mountain pine is to be effective, the
development of a prescribed burning plan should consider tree age and burn season to ensure
that an adequate and viable seed source is present. This conclusion was drawn from a study on
the patterns of seed production in Table Mountain pine, which revealed that the number of
seeds and viability of seeds was greatest in cones collected in the winter, even
though cones are mature in the fall of the second year .
Palatability/nutritional value: No information is available on this topic.
Cover value: No information is available on this topic.VALUE FOR REHABILITATION OF DISTURBED SITES:
Wood Products: Table Mountain pine is a softwood species  and has limited economic importance for timber products because of its small stature and often poor stem shape. Small amounts of Table Mountain pine are harvested, along with other pines, for fuel and commercially for pulp, paper production, and small roundwood [19,23,49]. Table Mountain pine has some potential for small saw timber when reintroduced in mixture with naturally occurring hardwoods .
Table Mountain pine is commonly found on steep slopes with limited access that are likely to be unsuitable for timber production .OTHER MANAGEMENT CONSIDERATIONS:
The needles of Table Mountain pine can be affected by hypoderma needle blight which causes mortality of infected needles . The European pine sawfly can defoliate trees of their previous year's needles but seldom kills the trees . The cones of Table Mountain pine are susceptible to Table Mountain pine coneworm (Diorytria yatesi) , and cone boring insects may have a significant effect on Table Mountain pine. The larva eats the part of the maturing cone between the central core and the outer layer of the cone, destroying the seeds. Damage varies from year to year, but in some years it appears to have destroyed the entire seed crop of an area. Heart rot is common in larger Table Mountain pine trees, usually over 100 years old. It appears to enter most often through fire scars and from long-persistent branch stubs characteristic of Table Mountain pine .
On Brush Mountain, Virginia, seed predators that attack cones of Table Mountain pine include red squirrels, larvae of the mountain pine coneworm, and the shield-backed pine seed bug .
Ice storms cause extensive damage to Table Mountain pine trees and can decrease basal area [41,81]. In a study by Whitney and Johnson , over 82% of Table Mountain pine were damaged by heavy glaze. Of these trees, 85% experienced 50% crown loss. Sampling was done two years after storm. Seedlings did increase after the storm due to the canopy gap created by fallen trees .
1. Anderson, R. F.; Doggett, C. A. 1993. Host preference of southern pine beetle in North Carolina. Forestry Note No. 66. Raleigh, NC: Division of Forest Resource, North Carolina Forest Service. 7 p. 
2. Barden, Lawrence S. 1977. Self-maintaining populations of Pinus pungens Lam. in the southern Appalachian Mountains. Castanea. 42(1): 316-323. 
3. Barden, Lawrence S. 1979. Serotiny and seed viability of Pinus pungens in the southern Appalachians. Castanea. 44(1): 44-47. 
4. Barden, Lawrence S. 1985. Bear oak (Quercus ilicifolia) in North Carolina. Castanea. 50(2): 121-123. 
5. Barden, Lawrence S. 1988. Drought and survival in a self-perpetuating Pinus pungens population: equilibrium or nonequilibrium? The American Midland Naturalist. 119(2): 253-257. 
6. Barden, Lawrence S. 2000. Population maintenance of Pinus pungens Lam. (Table Mountain pine) after a century without fire. Natural Areas Journal. 20(3): 227-233. 
7. Barden, Lawrence S.; Woods, Frank W. 1974. Characteristics of lightning fires in southern Appalachian forests. In: Proceedings, annual Tall Timbers fire ecology conference; 1973 March 22-23; Tallahassee, FL. No. 13. Tallahassee, FL: Tall Timbers Research Station: 345-361. 
8. Baskin, Carol C.; Baskin, Jerry M. 2001. Seeds: ecology, biogeography, and evolution of dormancy and germination. San Diego, CA: Academic Press. 666 p. 
9. Boyce, John S., Jr. 1954. Hypoderma needle blight of southern pines. Journal of Forestry. 52(7): 496-498. 
10. Bramlett, David L. 1980. Virginia pine-oak. In: Eyre, F. H., ed. Forest cover types of the United States and Canada. Washington, DC: Society of American Foresters: 60-61. 
11. Bramlett, David L. 1980. Virginia pine. In: Eyre, F. H., ed. Forest cover types of the United States and Canada. Washington, DC: Society of American Foresters: 54-55. 
12. Brose, Patrick H.; Waldrop, Thomas A. 2000. Using prescribed fire to regenerate Table Mountain pine in the southern Appalachian Mountains. In: Moser, W. Keith; Moser, Cynthia F., eds. Fire and forest ecology: innovative silviculture and vegetation management: Proceedings of the 21st Tall Timbers fire ecology conference: an international symposium; 1998 April 14-16; Tallahassee, FL. No. 21. Tallahassee, FL: Tall Timbers Research, Inc: 191-196. 
13. Brose, Patrick H.; Waldrop, Thomas A. 2006. Changes in the disturbance regime of upland yellow pine stands in the southern Appalachian Mountains during the 20th century. In: Conner, Kristina F., ed. Proceedings, 13th biennial southern silvicultural research conference; 2005 February 28 - March 4; Memphis, TN. Gen. Tech. Rep. SRS-92. Asheville, NC: U.S. Department of Agriculture, Forest Service, Southern Research Station: 467-470. 
14. Brose, Patrick H.; Waldrop, Thomas A. 2006. Fire and the origin of Table Mountain pine - pitch pine communities in the southern Appalachian Mountains, USA. Canadian Journal of Forest Research. 36: 710-718. 
15. Buckner, Edward R.; Turrill, Nicole L. 1999. Fire management. In: Peine, John D., ed. Ecosystem management for sustainability: Principles and practices illustrated by a regional biosphere reserve cooperative. Washington, DC: Lewis Publishers: 329-347. 
16. Critchfield, William B.; Little, Elbert L., Jr. 1966. Geographic distribution of the pines of the world. Misc. Publ. 991. Washington, DC: U.S. Department of Agriculture, Forest Service. 97 p. 
17. Delcourt, Hazel R.; Delcourt, Paul A. 1997. Pre-Columbian Native American use of fire on southern Appalachian landscapes. Conservation Biology. 11(4): 1010-1014. 
18. Della-Bianca, Lino. 1980. Chestnut oak. In: Eyre, F. H., ed. Forest cover types of the United States and Canada. Washington, DC: Society of American Foresters: 41. 
19. Della-Bianca, Lino. 1990. Pinus pungens Lamb. Table Mountain pine. In: Burns, Russell M.; Honkala, Barbara H., technical coordinators. Silvics of North America. Volume 1. Conifers. Agric. Handb. 654. Washington, DC: U.S. Department of Agriculture, Forest Service: 425-432. 
20. Dorman, Keith W. 1976. The genetics and breeding of southern pines. Agriculture Handbook 471. Washington, DC: U.S. Department of Agriculture, Forest Service. 407 p. 
21. Duncan, Wilbur H.; Duncan, Marion B. 1988. Trees of the southeastern United States. Athens, GA: The University of Georgia Press. 322 p. 
22. Ewers, Frank W.; Schmid, Rudolf. 1981. Longevity of needle fascicles of Pinus longaeva (bristlecone pine) and other North American pines. Oecologia. 5: 107-115. 
23. Farjon, Aljos; Frankis, Michael. 2002. Pinus pungens: Pinaceae. Curtis's Botanical Magazine. 19(2): 97-103. 
24. Feret, P. P.; Smith, D. Wm.; Rauscher, H. M. 1979. Dry matter accumulation in twenty wind-pollinated Pinus pungens families from southwest Virginia. Silvae Genetica. 28(5/6): 194-196. 
25. Feret, Peter P. 1974. Genetic differences among three small stands of Pinus pungens. Theoretical and Applied Genetics. 44(4): 173-177. 
26. Flora of North America Association. 2007. Flora of North America: The flora, [Online]. Flora of North America Association (Producer). Available: http://www.fna.org/FNA. 
27. Frost, Cecil C. 1998. Presettlement fire frequency regimes of the United States: a first approximation. In: Pruden, Teresa L.; Brennan, Leonard A., eds. Fire in ecosystem management: shifting the paradigm from suppression to prescription: Proceedings, Tall Timbers fire ecology conference; 1996 May 7-10; Boise, ID. No. 20. Tallahassee, FL: Tall Timbers Research Station: 70-81. 
28. Gibson, J. P., Hamrick, J. L. 1991. Genetic diversity and structure in Pinus pungens (Table Mountain pine) populations. Canadian Journal of Forest Research. 21: 635-642. 
29. Gibson, J. P.; Hamrick, J. L. 1991. Heterogeneity in pollen allele frequencies among cones, whorls, and trees of Table Mountain pine (Pinus pungens). American Journal of Botany. 78(9 ): 1244-1251. 
30. Golden, Michael S. 1981. An integrated multivariate analysis of forest communities of the central Great Smoky Mountains. The American Midland Naturalist. 106(1 ): 37-53. 
31. Gray, Ellen A.; Rennie, John C.; Waldrop, Thomas A.; Hanula, James L. 2002. Patterns of seed production in Table Mountain pine. In: Outcalt, Kenneth W., ed. Proceedings, 11th biennial southern silvicultural research conference; 2001 March 20-22; Knoxville, TN. Gen. Tech. Rep. SRS-48. Asheville, NC: U.S. Department of Agriculture, Forest Service, Southern Research Station: 302-305. 
32. Groeschl, David A.; Johnson, James E.; Smith, David Wm. 1991. Forest soil characteristics following wildfire in the Shenandoah National Park, Virginia. In: Nodvin, Stephen C.; Waldrop, Thomas A., eds. Fire and the environment: ecological and cultural perspectives: Proceedings of an international symposium; 1990 March 20-24; Knoxville, TN. Gen. Tech. Rep. SE-69. Asheville, NC: U.S. Department of Agriculture, Forest Service, Southeastern Forest Experiment Station: 129-137. 
33. Groeschl, David A.; Johnson, James E.; Smith, David Wm. 1992. Early vegetative response to wildfire in a Table Mountain pine - pitch pine forest. International Journal of Wildland Fire. 2(4): 177-184. 
34. Groeschl, David A.; Johnson, James E.; Smith, David Wm. 1993. Wildfire effects on forest floor and surface soil in a Table Mountain pine - pitch pine forest. International Journal of Wildland Fire. 3(3): 149-154. 
35. Hann, Wendel; Havlina, Doug; Shlisky, Ayn; [and others]. 2005. Interagency fire regime condition class guidebook. Version 1.2, [Online]. In: Interagency fire regime condition class website. U.S. Department of Agriculture, Forest Service; U.S. Department of the Interior; The Nature Conservancy; Systems for Environmental Management (Producer). Variously paginated [+ appendices]. Available: http://www.frcc.gov/docs/184.108.40.206/Complete_Guidebook_V1.2.pdf [2007, May 23]. 
36. Harmon, Mark. 1982. Fire history of the westernmost portion of Great Smoky Mountains National Park. Bulletin of the Torrey Botanical Club. 109(1): 74-79. 
37. Harrod, Jonathan; White, Peter S.; Harmon, Mark E. 1998. Changes in xeric forests in western Great Smoky Mountains National Park, 1936-1995. Castanea. 63(3): 346-360. 
38. Kartesz, John T. 1999. A synonymized checklist and atlas with biological attributes for the vascular flora of the United States, Canada, and Greenland. 1st ed. In: Kartesz, John T.; Meacham, Christopher A. Synthesis of the North American flora (Windows Version 1.0), [CD-ROM]. Chapel Hill, NC: North Carolina Botanical Garden (Producer). In cooperation with: The Nature Conservancy; U.S. Department of Agriculture, Natural Resources Conservation Service; U.S. Department of the Interior, Fish and Wildlife Service. 
39. Keeley, Jon E.; Zedler, Paul H. 1998. Evolution of life histories in Pinus. In: Richardson, David M., ed. Ecology and biogeography of Pinus. Cambridge, UK: The Press Syndicate of the University of Cambridge: 219-250. 
40. Komarek, E. V. 1974. Effects of fire on temperate forests and related ecosystems: southeastern United States. In: Kozlowski, T. T.; Ahlgren, C. E., eds. Fire and ecosystems. New York: Academic Press: 251-277. 
41. Lafon, Charles W.; Kutac, Martin J. 2003. Effects of ice storms, southern pine beetle infestation, and fire on Table Mountain pine forests of southwestern Virginia. Physical Geography. 24(6): 502-519. 
42. Landers, J. Larry. 1991. Disturbance influences on pine traits in the southeastern United States. In: Proceedings, 17th Tall Timbers fire ecology conference; 1989 May 18-21; Tallahassee, FL. No. 17. Tallahassee, FL: Tall Timbers Research Station: 61-95. 
43. LANDFIRE Rapid Assessment. 2005. Reference condition modeling manual (Version 2.1), [Online]. In: LANDFIRE. Cooperative Agreement 04-CA-11132543-189. Boulder, CO: The Nature Conservancy; U.S. Department of Agriculture, Forest Service; U.S. Department of the Interior (Producers). 72 p. Available: http://www.landfire.gov/downloadfile.php?file=RA_Modeling_Manual_v2_1.pdf [2007, May 24]. 
44. LANDFIRE Rapid Assessment. 2007. Rapid assessment reference condition models. In: LANDFIRE. U.S. Department of Agriculture, Forest Service, Rocky Mountain Research Station, Fire Sciences Lab; U.S. Geological Survey; The Nature Conservancy (Producers). Available: http://www.landfire.gov/models_EW.php 
45. Little, Silas. 1980. Pitch pine. In: Eyre, F. H., ed. Forest cover types of the United States and Canada. Washington, DC: Society of American Foresters: 49-50. 
46. McCarthy, E. F. 1922. Fire increases dry site type. USDA Forest Service Bulletin. 66(22): 4-5. 
47. McCune, Bruce. 1988. Ecological diversity in North American pines. American Journal of Botany. 75(3): 353-368. 
48. McDaniel, Virginia L.; Gatlinburg, T. N.; Benzing, N. L. 2004. The role of fire in tree mortality and regeneration in yellow pine (Pinus pungens, P. rigida, and P. virginiana) communities of Great Smoky Mountains National Park: preliminary results, [Online]. In: 2nd international wildland fire ecology and fire management congress: Proceedings; 2003 November 17; Orlando, FL. Poster Session 2 - Fire Effects. Washington, DC: American Meterological Society (Producer). Available: http://ams.confex.com/ams/FIRE2003/techprogram/paper_67066.htm [2006, October 12]. 
49. McIntyre, Arthur C. 1929. A cone and seed study of the mountain pine (Pinus pungens Lambert). American Journal of Botany. 16(6): 402-406. 
50. McLeod, Donald Evans. 1988. Vegetation patterns, floristics, and environmental relationships in the Black and Craggy Mountains of North Carolina. Chapel Hill, NC: University of North Carolina. 222 p. Dissertation. 
51. Mead, Margaret A.; Dolezal, W. E.; Tainter, F. H. 1978. Eighteen newly discovered pine hosts of comandra blister rust. Plant Disease Reporter. 62(10): 885-887. 
52. Moher, Helen H.; Waldrop, Thomas A.; Shelburne, Victor B. 2002. Optimal seedbed requirements for regenerating Table Mountain pine. In: Outcalt, Kenneth W., ed. Proceedings, 11th biennial southern silvicultural research conference; 2001 March 20-22; Knoxville, TN. Gen. Tech. Rep. SRS-48. Asheville, NC: U.S. Department of Agriculture, Forest Service, Southern Research Station: 306-309. 
53. Mohlenbrock, Robert H.; Ladd, Douglas M.. 1978. Distribution of Illinois vascular plants. Carbondale, IL: Southern Illinois University Press at Carbondale and Edwardsville. 282 p. 
54. Payne, Thomas L. 1983. Life history and traits. In: Thatcher, Robert C.; Searcy, Janet L.; Coster, Jack E.; Hertel, Gerard D., eds. The southern pine beetle. Technical Bulletin 1631. Washington, DC: U.S. Department of Agriculture, Forest Service, Expanded Southern Pine Beetle Research and Applications Program, Science and Education Program: 7-28. 
55. Radford, Albert E.; Ahles, Harry E.; Bell, C. Ritchie. 1968. Manual of the vascular flora of the Carolinas. Chapel Hill, NC: The University of North Carolina Press. 1183 p. 
56. Randles, Russell B. 2001. Effects of multiple, low-intensity fires on vegetation and wildlife habitat in Pinus pungens-Pinus rigida stands of the southern Appalachians. Clemson, SC: Clemson University. 48 p. Thesis. 
57. Randles, Russell B.; Van Lear, David H.; Waldrop, Thomas A. 2002. Periodic burning in Table Mountain-pitch pine stands. In: Outcalt, Kenneth W., ed. Proceedings, 11th biennial southern silvicultural research conference; 2001 March 20-22; Knoxville, TN. Gen. Tech. Rep. SRS-48. Asheville, NC: U.S. Department of Agriculture, Forest Service, Southern Research Station: 114-118. 
58. Raunkiaer, C. 1934. The life forms of plants and statistical plant geography. Oxford: Clarendon Press. 632 p. 
59. Reilly, Matthew J.; Wimberly, Michael C.; Newell, Claire L. 2006. Wildfire effects on plant species richness at multiple spatial scales in forest communities of the southern Appalachians. Journal of Ecology. 94(1): 118-130. 
60. Richardson, David M.; Rundel, Philip W. 1998. Ecology and biogeography of Pinus: an introduction. In: Richardson, David M., ed. Ecology and biogeography of Pinus. Cambridge, UK: The Press Syndicate of the University of Cambridge: 3-46. 
61. Sanders, Greg; Buckner, Edward. 1989. The effects of fire on Table Mountain pine communities. In: Waldrop, Thomas A., ed. Proceedings of pine-hardwood mixtures: a symposium on management and ecology of the type; 1989 April 18-19; Atlanta, GA. Gen. Tech. Rep. SE-58. Asheville, NC: U.S. Department of Agriculture, Forest Service, Southeastern Forest Experiment Station: 259. 
62. Schafale, Michael P.; Weakley, Alan S. 1990. Classification of the natural communities of North Carolina: 3rd approximation. Raleigh, NC: Department of Environment, Health, and Natural Resources, Division of Parks and Recreation, North Carolina Natural Heritage Program. 325 p. Available online: http://ils.unc.edu/parkproject/nhp/publications/class.pdf [2005, February 14]. 
63. Sheffield, Raymond M.; Birch, Thomas W.; Leatherberry, Earl C.; McWilliams, William H. 1989. The pine-hardwood resource in the eastern United States. In: Waldrop, Thomas A., ed. Proceedings of pine-hardwood mixtures: a symposium on management and ecology of the type; 1989 April 18-19; Atlanta, GA. Gen. Tech. Rep. SE-58. Asheville, SC: U.S. Department of Agriculture, Forest Service, Southeastern Forest Experiment Station: 9-19. 
64. Stickney, Peter F. 1989. Seral origin of species comprising secondary plant succession in Northern Rocky Mountain forests. FEIS workshop: Postfire regeneration. Unpublished draft on file at: U.S. Department of Agriculture, Forest Service, Intermountain Research Station, Fire Sciences Laboratory, Missoula, MT. 10 p. 
65. Stone, E. L., Jr.; Stone, M. H. 1954. Root collar sprouts in pine. Journal of Forestry. 52: 487-491. 
66. Strausbaugh, P. D.; Core, Earl L. 1977. Flora of West Virginia. 2nd ed. Morgantown, WV: Seneca Books, Inc. 1079 p. 
67. Sutherland, E. K., Grissino-Mayer, H.; Woodhouse, C. A.; Covington, W. W.; Horn, S.; Huckaby, L.; Keer, R.; Kuch, J.; Moore, M.; Plumb, T. 1995. Two centuries of fire in a southwestern Virginia Pinus pungens community. In: Inventory and management techniques in the context of catastrophic events: altered states of the forest: Proceedings; 1993 June 21-24; University Park, PA. University Park, PA: Penn State University, Office for Remote Sensing of Earth Resources. In: Environmental Information System, Center for Ecological Sciences (Producer). Available: http://ces.iisc.ernet.in/hpg/envis/proceed/sthrland.txt.html [2007, August 28]. 
68. Sutherland, Elaine Kennedy; Grissino-Mayer, Henri; Woodhouse, Connie. 1998. The history of fire in a southwestern Virginia Pinus pungens stand. In: Pruden, Teresa L.; Brennan, Leonard A., eds. Fire in ecosystem management: shifting the paradigm from suppression to prescription: Proceedings, Tall Timbers fire ecology conference; 1996 May 7-10; Boise, ID. No. 20. Tallahassee, FL: Tall Timbers Research Station: 115. 
69. Trumbo, H. A.; Chappell, W. E. 1959. Techniques involved in the use of chemicals for establishing wildlife clearings. Proceedings, Northeast Weed Control Conference. 13: 337-341. 
70. Turrill, Nicole L.; Buckner, Edward R.; Waldrop, Thomas A. 1997. Pinus pungens Lam. (Table Mountain pine): a threatened species without fire? In: Greenlee, Jason M., ed. Proceedings, 1st conference on fire effects on rare and endangered species and habitats; 1995 November 13-16; Coeur d'Alene, ID. Fairfield, WA: International Association of Wildland Fire: 301-306. 
71. Turrill, Nicole Leigh. 1998. Using prescribed fire to regenerate Pinus echinata, P. pungens, and P. rigida forests in the southern Appalachian Mountains. Knoxville, TN: University of Tennessee. 148 p. Dissertation. 
72. U.S. Department of Agriculture, Natural Resources Conservation Service. 2007. PLANTS Database, [Online]. Available: http://plants.usda.gov/. 
73. Van Lear, D. H.; Harlow, R. F. 2002. Fire in the eastern United States: influence on wildlife habitat. In: Ford, W. Mark; Russell, Kevin R.; Moorman, Christopher E., eds. The role of fire in nongame wildlife management and community restoration: traditional uses and new directions: Proceedings of a special workshop; 2000 December 15; Nashville, TN. Gen. Tech. Rep. NE-288. Newtown Square, PA: U.S. Department of Agriculture, Forest Service, Northeastern Research Station: 2-10. 
74. Wade, Dale D.; Brock, Brent L.; Brose, Patrick H.; Grace, James B.; Hoch, Greg A.; Patterson, William A., III. 2000. Fire in eastern ecosystems. In: Brown, James K.; Smith, Jane Kapler, eds. Wildland fire in ecosystems: Effects of fire on flora. Gen. Tech. Rep. RMRS-GTR-42-vol. 2. Ogden, UT: U.S. Department of Agriculture, Forest Service, Rocky Mountain Research Station: 53-96. 
75. Waldrop, Thomas A.; Brose, Patrick H. 1999. A comparison of fire intensity levels for stand replacement of Table Mountain pine (Pinus pungens Lamb.). Forest Ecology and Management. 113: 155-166. 
76. Waldrop, Thomas A.; Brose, Patrick H.; Welch, Nicole Turrill; Mohr, Helen H.; Gray, Ellen A.; Tainter, Frank H.; Ellis, Lisa E. 2003. Are crown fires necessary for Table Mountain pine? In: Galley, K. E. M.; Klinger, R. C.; Sugihara, N. G., eds. Fire conference 2000: the first national congress on fire ecology, prevention and management. Miscellaneous Publication No. 13. Tallahassee, FL: Tall Timbers Research Station: 157-163. 
77. Waldrop, Thomas A.; Mohr, Helen H.; Brose, Patrick H. 2006. Early dynamics of Table Mountain pine stands following stand-replacement prescribed fires of varying intensity. In: Conner, Kristina F., ed. Proceedings of the 13th biennial southern silvicultural research conference; 2005 February 28 - March 4; Memphis, TN. Gen. Tech. Rep. SRS-92. Asheville, NC: U.S. Department of Agriculture, Forest Service, Southern Research Station: 471-474. 
78. Waldrop, Thomas A.; Mohr, Helen H.; Brose, Patrick H.; Baker, Richard B. 1999. Seedbed requirements for regenerating Table Mountain pine with prescribed fire. In: Haywood, James D., ed. Proceedings, 10th biennial southern silvicultural research conference; 1999 February 16-18; Shreveport, LA. Gen. Tech. Rep. SRS-30. Asheville, NC: U.S. Department of Agriculture, Forest Service, Southern Research Station: 369-373. 
79. Welch, N. T.; Waldrop, T. A.; Buckner, E. R. 2000. Response of southern Appalachian Table Mountain pine (Pinus pungens) and pitch pine (Pinus rigida) stands to prescribed burning. Forest Ecology and Management. 136(1-3): 185-197. 
80. White, Fred M. 1980. Shortleaf pine. In: Eyre, F. H., ed. Forest cover types of the United States and Canada. Washington, DC: Society of American Foresters: 53-54. 
81. Whitney, Helen E.; Johnson, W. Carter. 1984. Ice storms and forest succession in southwestern Virginia. Bulletin of the Torrey Botanical Club. 111(4): 429-437. 
82. Whittaker, R. H. 1956. Vegetation of the Great Smoky Mountains. Ecological Monographs. 26(1): 1-79. 
83. Williams, Charles E. 1990. The pines of Virginia: identification, distribution and ecology. Virginia Journal of Science. 41(4B): 478-486. 
84. Williams, Charles E. 1991. Maintenance of the disturbance-dependent Appalachian endemic, Pinus pungens, under low-disturbance regimes. Natural Areas Journal. 11(3): 169-170. 
85. Williams, Charles E. 1998. History and status of Table Mountain pine - pitch pine forests of the southern Appalachian Mountains (USA). Natural Areas Journal. 18(1): 81-90. 
86. Williams, Charles E.; Johnson, W. Carter. 1990. Age structure and the maintenance of Pinus pungens in pine-oak forests of southwestern Virginia. The American Midland Naturalist. 124(1): 130-141. 
87. Williams, Charles E.; Johnson, W. Carter. 1992. Factors affecting recruitment of Pinus pungens in the southern Appalachian Mountains. Canadian Journal of Forest Research. 22: 878-887. 
88. Williams, Charles E.; Lipscomb, Mary V.; Johnson, W. Carter; Nilsen, Erik T. 1990. Influence of leaf litter and soil moisture regime on early establishment of Pinus pungens. The American Midland Naturalist. 124(1): 142-152. 
89. Wofford, B. Eugene. 1989. Guide to the vascular plants of the Blue Ridge. Athens, GA: The University of Georgia Press. 384 p. 
90. Zahner, Robert; Smalley, Glendon W. 1989. Site quality: the ecological basis for pine-hardwood management decisions. In: Waldrop, Thomas A., ed. Proceedings of pine-hardwood mixtures: a symposium on management and ecology of the type; 1989 April 18-19; Atlanta, GA. Gen. Tech. Rep. SE-58. Asheville, SC: U.S. Department of Agriculture, Forest Service, Southeastern Forest Experiment Station: 59-63. 
91. Zobel, Donald B. 1969. Factors affecting the distribution of Pinus pungens, an Appalachian endemic. Ecological Monographs. 39: 302-333. 
92. Zobel, Donald B. 1970. Morphological characterization of Pinus pungens. Journal of the Elisha Mitchell Scientific Society. 86(4): 214-221. 
FEIS Home Page