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KUCHLER TYPE

KUCHLER TYPE: Southern mixed forest
KUCHLER-TYPE-NUMBER : K112 PHYSIOGNOMY : Tall forest of broadleaf deciduous and evergreen trees. OCCURRENCE : Southeastern United States, encompassing eight states: Florida, Georgia, the Carolinas, Virginia, Alabama, Louisiana, and Mississippi. In accordance with Ware and others [19], this report includes a slightly larger area than that recognized by Kuchler [10]. COMPILED BY AND DATE : S. A. Snyder, January 1994 LAST REVISED BY AND DATE : NO-ENTRY AUTHORSHIP AND CITATION : Snyder, S. A. 1994. Southern mixed forest. In: Remainder of Citation
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KUCHLER TYPE DESCRIPTION


PHYSIOGRAPHY : The Coastal Plain portion of this type is characterized by marine terraces, on the seaward side of which are often found fossilized sand dunes. Stream channels run throughout the southern mixed forest, and in places subsidence has resulted in "drowned" river mouths. This type is also characterized by bays, sounds, barrier islands, and wide estuaries. Along the coasts in Florida and the Carolinas, the terraces are poorly drained and may be saturated for part of the year. Inland terraces are narrower and more dissected than coastal terraces. Relief may be greater: 105 feet (35 m) compared to 45 feet (15 m) along the coast. Differences in relief of only a few meters can affect vegetation in these predominantly sandy soils [19]. CLIMATE : The southeastern Coastal Plain receives more than 48 inches (1,220 mm) per year of precipitation. This area has the highest frequency of heavy downpours combined with the most rain-free days per year. It also has the highest evaporation rates in the East [19]. For the whole area average annual precipitation is between 40 and 60 inches (1,000-1,520 mm) and average annual evaporation is 42 to 48 inches (1,060-1,220 mm). In the eastern part of this region precipitation is lowest in the fall and highest in midsummer. In the west it is lowest in winter and spring [7]. The southern mixed forest is subjected to annual hurricanes, especially along peninsular Florida and the Gulf Coast. The southern mixed forest experiences mild winters. Average monthly temperatures from December through February are above 40 degrees Fahrenheit (4 deg C), with inland areas slightly cooler than coastal areas. Frost-free days occur from April first to November first, and the growing season usually exceeds 210 days. Florida is the warmest area in the southern mixed forest with milder winters, longer growing seasons, and more frost-free days than elsewhere in the region [19]. SOILS : Most of the soils in the Coastal Plains area are sandy [19], but range from sandy or gravelly to moderately fine textured [7]. Soils in the longleaf-slash pine type are typically acidic, low in organic matter, and deficient in many essential plant nutrients [7]. In some places older calcareous soils have been exposed by erosion. Phosphate-rich calcareous soils are common in peninsular Florida and scattered throughout the region [19]. VEGETATION : The southern mixed forest region has been referred to as the oak-hickory association or the beech-magnolia association based on potential natural vegetation in the absence of fire [19]. Dominant overstory vegetation is listed as American beech (Fagus grandifolia [not in central Florida]), sweetgum (Liquidambar styraciflua), southern magnolia (Magnolia grandiflora), slash pine (Pinus elliottii), loblolly pine (P. taeda), white oak (Quercus alba), and laurel oak (Q. laurifolia) [10]. Loblolly pine now outnumbers the once abundant longleaf pine (Pinus palustris) and slash pine. Maps of the presettlement range of fire-maintained longleaf pine savannas have been reconstructed [19]. Presettlement forests of the Southeast, which were savanna woodland fire types, survive only as scattered relicts. Now the vegetation is largely postlogging, successional mixed pinehardwood forests [19]. Important nondominant species include pignut hickory (Carya glabra), mockernut hickory (C. tomentosa), redbay (Persea borbonia), and shortleaf pine (Pinus echinata) in the northern range of this type; southern sugar maple (Acer barbatum), American hornbeam (Carpinus caroliniana), flowering dogwood (Cornus florida), inkberry (Ilex glabra), American holly (I. opaca), yellow-poplar (Liriodendron tulipifera), wax myrtle (Myrica cerifera), and eastern hophornbeam (Ostrya virginiana) in all but central Florida; south Florida slash pine (Pinus elliottii var. densa); cabbage palmetto (Sabal palmetto) in the eastern part of the type; and southern red oak (Quercus falcata), bluejack oak (Q. incana), turkey oak (Q. laevis), blackjack oak (Q. marilandica), post oak (Q. stellata var. margaretta), live oak (Q. virginiana) and saw-palmetto (Serenoa repens) in Florida and coastal areas [10]. Understory species include wiregrass (Aristida stricta). Also found here are tickclover (Desmodium spp.), lespedeza (Lespedeza spp.), butterfly pea (Clitoria mariana), senna (Cassia spp.), tephrosia (Tephrosia virginiana), galactia (Galactia spp.), wild indigo (Baptisia spp.), and Heterothea graminifolia [19]. A publication listing vegetation types of the southern mixed forest follows. Vegetation of the Archbold Biological Station, Florida: an example of the southern Lake Wales Ridge [1] WILDLIFE : The southern mixed forest is home to an array of animals that includes opossum, raccoon, white-tailed deer, feral pigs, squirrels, warblers, woodpeckers, the cardinal, flycatchers, quail, snakes, frogs, and turtles [19]. For a list of endangered species see WILDLIFE VALUES. ECOLOGICAL RELATIONSHIPS : Before European settlement within the range of longleaf pine, mixed forests dominated by American beech, southern magnolia, other hardwoods, and semievergreen oaks may have been limited to small areas. Relict old-growth stands are still found on slopes, swamp islands, and upland flats on peninsulas. Due to a variety of moisture regimes and the historic prevalence of periodic fires, the potential climax vegetation following longleaf pine forests in the southern mixed forest is difficult to predict. Various authors have tried to extrapolate this information from trees present in second growth-forests [19]. See FIRE EFFECTS ON VEGETATION. Longleaf pine usually occurs in pure stands on dry sites and is considered fire subclimax [6,20,21]. It is a pioneer on areas cleared by stand-replacing fire and is maintained by fire on dry sites [12,20,21]. Slash pine has shallow spreading roots and is found on more wet sites that may seasonally flood. The two species may occur together where fire has been absent for 5 to 10 years [21]. Loblolly pine occurs on both well-drained and poorly drained sites and can establish following fire [21]. Fire exclusion favors slash pine over longleaf pine in Florida and favors loblolly pine over longleaf pine in the northern Coastal Plain. On mesic sites where soils are rich in phosphate and calcium, American beech and southern magnolia eventually replace pines in fire's absence [8]. Sandy or nutrient-deficient soils usually do not support hardwoods [3]. For more detailed information on community dynamics refer to Christensen [5], Ware and others [19], and Eyre [21]. For more detailed information on community dynamics related to fire in the southern mixed forest refer to Ware and others [19].

KUCHLER TYPE VALUE AND USE

KUCHLER TYPE: Southern mixed forest
FORESTRY VALUES : Intense logging from the late nineteenth century until the 1930's virtually eliminated all virgin stands of the southern mixed forest. There are about 15,315,000 acres (6,202,000 ha) of loblolly and slash pine plantations in the southern mixed forest, all of which are grown for pulpwood and sawtimber [19]. RANGE VALUES : Clearing of the southern mixed forest for grazing and agriculture began more than 400 years ago [19]. Agriculture is now a dominant use in the region. WILDLIFE VALUES : The southern mixed forest provides habitat for many threatened and endangered species including the red-cockaded woodpecker, Bachman's wood sparrow, the gopher tortoise, the Florida gopher frog, the indigo snake, the pine snake, the pine barrens tree frog, the Florida mouse, and the southeastern fox squirrel [19]. OTHER VALUES : From Colonial times through the early twentieth century longleaf pine was used extensively for tar, pitch, rosin, and turpentine. This decimated longleaf pine stands throughout the region by the 1920's [19]. MANAGEMENT CONCERNS : Ninety-seven percent of the uplands in the southern mixed forest consist of converted lands and vegetation that is present due to disturbance. Now less than 3 percent of the original landscape is natural vegetation. Feral pigs can consume up to 400 longleaf pine seedlings apiece per day [19].

KUCHLER TYPE FIRE ECOLOGY AND MANAGEMENT

KUCHLER TYPE: Southern mixed forest
FUELS, FLAMMABILITY, AND FIRE OCCURRENCE : The southeastern United States has one of the highest-known incidences of thunderstorms in North America, and lightning-caused fires are very common [8]. Some traits of southern pines related to fuel loading and fire resistance have been listed [11]. Along the coast from Virgina to Texas, there are thousands of square miles of land without a natural firebreak. Firebreaks occur more inland, where historic fire frequencies were probably lower than in coastal regions. During early European settlement, accounts describe Native Americans using fire during fall and winter to drive game animals. This could be done once a year in most areas because enough fuels accumulated in one year to carry fire. Along the Coastal Plains, fuels did not accumulate due to annual summer lightning fires, and effects of burning by early Native Americans were probably negligible [19]. Studies in longleaf pine savannas show that fires are usually low intensity surface fires and rarely reach the crown. Longleaf pine needles are highly flammable, and areas with more and larger trees usually burn hot if litter has accumulated [15]. More than 100 years ago, the fire maintained longleaf pine savannas had an average fire frequency of 1 to 3 years. In areas of slightly lower fire frequency (5-10 years) mixed pine savannas and woodlands dominated [19]. FIRE EFFECTS ON SITE : Burned soils in longleaf pine forests show higher average temperatures than soils in unburned areas. Soil moisture is as much as 50 percent lower on burned sites; with repeated burning, water-absorbing ability of longleaf soils decreases from 50 to 80 percent. Some studies report that organic matter and nitrogen may also be lost with frequent fire on abandoned old fields. Other reports show that organic matter and nitrogen may increase after fire in virgin forests. This could be due to an increase in leguminous species and charcoal deposition following fire. These differences may be accounted for by comparing differences in species composition and biomass between oldfield and virgin forest communities [6]. Detailed effects of fires on soil nutrients in Coastal Plain forests and their subsequent effects on vegetation have been listed for Coastal Plain forests [4]. FIRE EFFECTS ON VEGETATION : Fire played a major role in determining presettlement vegetation. Its effects on vegetation depend on soil moisture and topography. Longleaf pine is the only tree in this region whose seedlings are adapted to survive fire [19]. Most longleaf pine growth during the first 5 years is concentrated in the roots, which enables it to survive even when the leaves are consumed by fire [20]. Even then few seedlings may escape fire [22], but in virgin old-growth stands, one surviving seedling every 5 to 10 years could be enough to maintain a fully stocked stand [19]. Hot fires due to heavy needle litter accumulation can kill longleaf seedlings [21]. Longleaf pine perpetuates in pure stands when burned during winter every 3 to 4 years. Associated pines (loblolly, shortleaf, and slash) are more adapted to fire cycles of 10 to 15 years [6]. Slash pine is highly susceptible to fire during its first 2 years and vulnerable throughout the seedling stage [12,20,21]. After 10 to 12 years it can survive winter fires that do not crown. If less than 40 percent of its crown is scorched, slash pine growth may be enhanced by fire. The south Florida variety is more resistant than the typical variety [20]. Loblolly pine is not fire tolerant during its first 10 years, but mature trees are relatively resistant [2,20]. Mature trees with thick bark can survive low- to medium-severity fires [18]. After loblolly pines have reached 2 to 4 inches (5-10 cm) in diameter, they can be burned in winter every 5 to 10 years, which tends to suppress hardwoods [20]. Fire has the following effects on additional canopy dominant species (as listed by Kuchler): American beech is fire-intolerant. It can sprout following fire, but is susceptible to decay [3,16]. Sweetgum too is damaged by fire, opening it up to decay. It is more susceptible to summer fires than winter fires, but it does sprout following fire [9]. Southern magnolia is usually top-killed by fire, but can sprout [14]. Because of its thin bark, laurel oak is usually top-killed by light ground fires, but can sprout [13]. White oak needs periodic fire to perpetuate because it is shade intolerant. It is moderately resistant to fire and can sprout [17]. Important understory species in longleaf pine and slash pine stands, saw-palmetto and inkberry, are highly flammable. If not burned during winter every 3 years, fuel loading of these species can lead to fires severe enough to kill both the understory and overstory [12]. For more detailed information on fire's effects, refer to species write-ups in the FEIS database. Some vegetational patterns related to fire frequency in presettlement southern mixed forests were as follows: On dry, upland sites frequent fires maintained longleaf pine savannas. Turkey oak was also present in these stands. Fire may have been less frequent on dry sandhill sites because of dissected topography and sparse fuels. As moisture increased, longleaf pine occurred with slash pine, bluejack oak, blackjack oak, and post oak. Shortleaf and loblolly pines may have also been present. Pond pine occurred on moist sites where oaks were absent. Where fires were less frequent, longleaf pine and red oak dominated on dry sites. On moist sites longleaf pine was less prevalent; slash, loblolly, and shorleaf pines were more likely to occur with oaks. Beech-dominated stands probably occurred where areas were isolated from fire [19]. FIRE EFFECTS ON RESOURCE MANAGEMENT : The mesic, species-rich longleaf pine types, which need fire every 1 to 3 years, are in danger of extirpation [19]. With the exclusion of fire in recent decades, longleaf pine stands have been replaced with slash and loblolly pines. If not for intensive timber production and prescribed burning in the Southeast, all pine species would be a small part of the climax forest. Prescribed burns are an effective way of maintaining pine forests and of reducing severe wildfire hazards in this region [20]. Fire promotes palatable grasses and forbs under longleaf pine forests for livestock grazing and wildlife [12]. FIRE USE CONSIDERATIONS : Fire can be used to control brown spot disease, to which longleaf pine is very susceptible [20]. FIRE MANAGEMENT CONSIDERATIONS : On outer terraces of Coastal Plains, slopes greater than 15 degrees serve as effective fire breaks in longleaf pine savannas. Fires in these areas usually originate on the upland flats and not in the bottomlands [19]. REHABILITATION OF SITES FOLLOWING WILDFIRE : NO-ENTRY

REFERENCES

KUCHLER TYPE: Southern mixed forest
REFERENCES : 1. Hernandez, Helios. 1973. Natural plant recolonization of surficial disturbances, Tuktoyaktuk Peninsula region, Northwest Territories. Canadian Journal of Botany. 51: 2177-2196. [20372] 2. Brown, Arthur A.; Davis, Kenneth P. 1973. Forest fire control and use. 2nd ed. New York: McGraw-Hill. 686 p. [15993] 3. Christensen, Norman L. 1981. Fire regimes in southeastern ecosystems. In: Mooney, H. A.; Bonnicksen, T. M.; Christensen, N. L.; [and others], technical coordinators. Fire regimes and ecosystem properties: Proceedings of the conference; 1978 December 11-15; Honolulu, HI. Gen. Tech. Rep. WO-26. Washington, DC: U.S. Department of Agriculture, Forest Service: 112-136. [4391] 4. Christensen, Norman L. 1987. The biogeochemical consequences of fire and their effects on the vegetation of the Coastal Plain of the southeastern United States. In: Trabaud, L., ed. The role of fire in ecological systems. Hague, The Netherlands: SPB Academic Publishing: 1-21. [17285] 5. Christensen, Norman L. 1988. Vegetation of the southeastern Coastal Plain. In: Barbour, Michael G.; Billings, William Dwight, eds. North American terrestrial vegetation. Cambridge: Cambridge University Press: 317-363. [17414] 6. Garren, Kenneth H. 1943. Effects of fire on vegetation of the southeastern United States. Botanical Review. 9: 617-654. [9517] 7. Garrison, George A.; Bjugstad, Ardell J.; Duncan, Don A.; [and others]. 1977. Vegetation and environmental features of forest and range ecosystems. Agric. Handb. 475. Washington, DC: U.S. Department of Agriculture, Forest Service. 68 p. [998] 8. Komarek, E. V., Sr. 1968. Lightning and lightning fires as ecological forces. In: Proceedings, annual Tall Timbers fire ecology conference; 1968 March 14-15; Tallahassee, FL. No. 8. Tallahassee, FL: Tall Timbers Research Station: 169-197. [18928] 9. Kormanik, Paul P. 1990. Liquidambar styraciflua L. sweetgum. In: Burns, Russell M.; Honkala, Barbara H., technical coordinators. Silvics of North America. Vol. 2. Hardwoods. Agric. Handb. 654. Washington, DC: U.S. Department of Agriculture, Forest Service: 400-405. [17401] 10. Kuchler, A. W. 1964. Manual to accompany the map of potential vegetation of the conterminous United States. Special Publication No. 36. New York: American Geographical Society. 77 p. [1384] 11. 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. Tallahassee, FL: Tall Timbers Research Station: 61-95. [17601] 12. Lotan, James E.; Alexander, Martin E.; Arno, Stephen F.; [and others]. 1981. Effects of fire on flora: A state-of-knowledge review. National fire effects workshop; 1978 April 10-14; Denver, CO. Gen. Tech. Rep. WO-16. Washington, DC: U.S. Department of Agriculture, Forest Service. 71 p. [1475] 13. Curtis, James D. 1946. Preliminary observations on northern white cedar in Maine. Ecology. 27: 23-36. [19804] 14. Green, Jeffery, S.; Flinders, Jerran T. 1980. Habitat and dietary relationships of the pygmy rabbit. Journal of Range Management. 33(2): 136-142. [6257] 15. Platt, William J.; Glitzenstein, Jeff S.; Streng, Donna R. 1991. Evaluating pyrogenicity and its effects on vegetation in longleaf pine savannas. In: Proceedings, 17th Tall Timbers fire ecology conference; 1989 May 18-21; Tallahassee, FL. Tallahassee, FL: Tall Timbers Research Station: 143-161. [17606] 16. Swan, Frederick R., Jr. 1970. Post-fire response of four plant communities in south-central New York state. Ecology. 51(6): 1074-1082. [3446] 17. Van Lear, David H.; Waldrop, Thomas A. 1989. History, uses, and effects of fire in the Appalachians. Gen. Tech. Rep. SE-54. Asheville, NC: U.S. Department of Agriculture, Forest Service, Southeastern Forest Experiment Station. 20 p. [10126] 18. Wahlenberg, W. G. 1960. Loblolly pine, its use, ecology, regeneration, protection, growth and management. Durham, NC: Duke University, School of Forestry. 603 p. [17848] 19. Ware, Stewart; Frost, Cecil; Doerr, Phillip D. 1993. Southern mixed hardwood forest: the former longleaf pine forest. In: Martin, William H.; Boyce, Stephen G.; Echternacht, Arthur C., eds. Biodiversity of the southeastern United States: Lowland terrestrial communities. New York: John Wiley & Sons, Inc: 447-493. [22016] 20. Wright, Henry A.; Bailey, Arthur W. 1982. Fire ecology: United States and southern Canada. New York: John Wiley & Sons. 501 p. [2620] 21. Eyre, F. H., ed. 1980. Forest cover types of the United States and Canada. Washington, DC: Society of American Foresters. 148 p. [905] 22. Boyer, W. D. 1990. Pinus palustris Mill. longleaf 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: 405-412. [13398]

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