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A survey of the vascular plants of The Francis Beidler Forest, A National Audubon Sanctuary in Four Holes Swamp in the Coastal Plain of South Carolina, is presented. Included are a description of major plant communities including an original growth bald cypress-tupelo gum swamp forest community, an annotated checklist of the vascular plants that includes ecological notes on rare and endangered species, and an historical account of Four Holes Swamp and Beidler Forest. Three hundred twelve species from 218 genera and 99 families are reported.
The Francis Beidler Forest is a National Audubon Sanctuary in Four Holes Swamp, located in the Coastal Plain of South Carolina in Berkeley and Dorchester counties. Within the Sanctuary is the largest stand of original growth bald cypress (Taxodium distichum) and tupelo gum (Nyssa aquatica) in the United States (Brunswig and Winton, 1978). Four Holes Swamp is a low gradient, brown water, swamp-river floodplain system that runs for approximately sixty miles through the Coastal Plain of South Carolina. It averages approximately one to one and one-half miles in width along most of its length. From its origin near Cameron in Calhoun County, Four Holes Swamp runs in a southeast direction through Calhoun, Orangeburg, Dorchester, and Berkeley counties to a point along the Berkeley-Dorchester county line. Here the swamp makes a right turn and runs southwest for nine miles until it empties into the Edisto River near Ghivans in Dorchester County. Through the Edisto River the waters of Four Holes Swamp flow into the Atlantic Ocean. A curious feature of the swamp is the sudden right turn it makes. Instead of continuing its course southeasterly to the sea, it turns southwestward and runs parallel to the coast until it joins the Edisto River. One geological explanation (Carr, 1971) is that at a time when the seas were higher and the lower part of Four Holes was an estuarine arm of the pre-Pleistocene Atlantic, the right turn was probably formed by currents that built an off-shore bar. This bar then deflected the lower reach of the then Four Holes River into its present southwesterly course.
Lumbering since the turn of the century has removed the original growth timber along the entire run of Four Holes Swamp except for an 1800-acre section immediately above where the swamp makes its right turn. This section of untimbered original growth forest was owned by Francis Beidler I, a lumberman from Chicago, who died in 1924. With the prospect of the sale of the Beidler property due to liquidation of the estate, local conservationists' action to preserve the swamp led to action by the Nature Conservancy and National Audubon Society. In 1970 these two organizations arranged for the purchase of the 1800-acre section of original growth timber plus 1700 additional acres of adjacent timbered swamp to act as a buffer zone. Title to the properties was originally vested in the Nature Conservancy; however, under an agreement between the two organizations, a 60% interest was deeded to the National Audubon Society. Under the same agreement the Audubon Society became administrator of the properties, and maintains a Visitor's Center and a 6,500-foot boardwalk to allow public access to the major communities of the swamp. The public is not allowed access to the Sanctuary except via the boardwalk and managed canoe trips, in order to insure preservation of the swamp ecosystem. Field trips for educational purposes are allowed by appointment and scientific studies are permitted under the auspicies of the Sanctuary Manager. The 3500-acre tract has been named The Francis Beidler Forest in honor of Francis Beidler I.
The origin of the name "Four Holes Swamp'' is uncertain. It appears on pre-revolutionary maps where the only road through the swamp is near Highway 78. Local history has it that the name comes from four "holes" through the swamp forming seasonally dry passageways used by early pioneers. But the exact origin of the name remains a mystery and will remain so unless new documents are uncovered.
This survey of the vascular plants of Beidler Forest, supported by a grant from the National Audubon Society, is confined to the 1800-acre original growth tract, a cutover upland area where the Visitor's Center is located, portions of the bluff slope that border the eastern side of the swamp, and the bluff slope along the western side of the swamp above Mallard's Lake. Although the bluff slope is not part of the Four Holes Swamp floodplain, its ecological relationship with the swamp system and high aesthetic appeal warrants its inclusion in this study. Actually only a short distance of the bluff slope on the eastern side of the swamp is part of Beidler Forest. Future acquisitions to Beidler Forest, however, include the possibility of acquiring as much of the bluff slope as possible, both to act as a buffer zone to the fragile swamp floodplain and because of the rich and diverse mixed mesophytic hardwood forest on the bluff slope. For these reasons I included in the study the portions of the bluff slope that appear to be likely candidates for future acquisition.
This survey of Beidler Forest is primarily intended to be a base-line study on which future studies of swamp ecology can be conducted. Two factors of Beidler Forest make for an unique opportunity to the scientific community to study swamp ecology, especially studies of plant succession: (1) the presence of a large stand of original growth forest, which has been virtually untouched by man's activities, and (2) areas of cutover forest within the boundaries of the Forest which can be managed (managed in this concept being more to insure that man's activities in the cutover area are excluded or controlled) to let natural succession occur. In addition to the cutover areas within Beidler Forest there are numerous adjacent tracts of swamp forest, under various owners (Figure 2), that have been selectively timbered since the early 1930's. Records as to the dates and type of timber harvest are available for these adjacent tracts, thus considerable data already exists for studies on plant succession following disturbances. These tracts are possible future acquisitions to Beidler Forest, and if acquired, would expedite future studies. The untimbered section of Beidler Forest has been referred to in this study as "original growth" forest rather than a "virgin" forest. This latter designation is often interpreted as meaning that no vegetation, especially trees, has been removed by man's activities. Such is not the case in Beidler Forest. Certainly in colonial times and later, an occasional large cypress was removed to make shingles for roofs, or an occasional hardwood tree was removed for firewood or to make furniture. A few trees were probably felled to make trails or primitive roads into the swamp, and certainly an occasional still, deep in the swamp, necessitated the clearing of small trees. But these activities did not significantly alter the swamp ecosystem. Today the original growth section of Beidler Forest represents a mature stand of timber, virtually the same as it was when the first settlers moved inland from the coastal settlements and began the transformation of our native woodlands and swamps to fields and secondary growth forests.
In recognition of the national significance of the original growth forest described in this study, and the efforts that have been made to preserve it, The Francis Beidler Forest was designated a Registered National Natural Landmark in May of 1979 by the Department of Interior.
The primary influence on the distribution and composition of communities in the Four Holes Swamp floodplain is the hydroperiod. Four Holes Swamp is a low gradient, creek or river swamp. From its headwaters near Cameron in Orangeburg County to a point below S. C. Highway 78, there is no discernible major channel. Instead the brown water flows slowly, slowly, through a series of small runs and streams that crisscross the floodplain and join and separate in a pattern that seems to have no purpose or identity. This pattern changes during heavy rains, however, as runoff from the adjacent uplands enters the floodplain, flooding it from upland to upland. Then the water moves swiftly in its relentless path to the sea. Only during severe droughts does the flow of water cease in Four Holes Swamp. During the summer of 1977 one could traverse the flood-plain without having to wade through any flowing water (although the lakes in the swamp retained water). Only where the swamp enters the Edisto River does a major channel develop.
Throughout the Four Holes Swamp floodplain the smaller runs and streams become deeper and wider where two or three merge forming numerous lakes of various sizes. It is along these runs, streams, and lakes that many of the cypress trees reach their largest size, and knees and buttresses obtain maximum development. Four such lakes occur in the original growth section of Beidler Forest: Goodson, Canoe, Singletary, and Mocossin. The largest of the lakes in Beidler Forest, Mallard's, occurs in the timbered section; however, a buffer zone of original growth was left along its northwest side. Another large lake, Mims Lake, occurs along the extreme southeast section of the cutover portion of Beidler Forest. Considerable marl outcrops occur along the edge of the bluff where it borders the lake on its southeast side.
Between the runs, streams, and lakes, eons of alluvial deposition on the floodplain and stream dissection have resulted in a gradual elevation of the soil resulting in three major hydroperiods: (1) flooded to extremely wet most of the year, (2) flooded for a few months from late winter to early spring, and (3) free from standing water most of the year, but flooded during heavy rains, and then draining very quickly. Under these conditions three climax bottomland forests, as described by Braun (1950), have developed in Four Holes Swamp: swamp forest, hardwood bottom, and ridge bottom. In light of recent studies by Dr. A. E. Radford, and his staff at UNC on natural diversity in our environment, the recognition of only three community types appears overly simplified. Even Braun (1950) recognized the simplification of the description of plant communities that prevailed during her time as she stated: "Most data on the composition of bottomland forests do not separate the communities of the several bottomland habitats. All hardwoods are considered together, thus developmental sequences and correlations with site factors are obscured." Dr. Radford and his students have stated the problem most eloquently (Radford et al., 1978): "We can no longer speak in terms of simply an American beech (Fagus grandifolia) forest, but must observe carefully, see relationships, and provide lists such as the following which truly demonstrate natural diversity: Fagus grandifolia/Kalmia latifolia, Fagus grandifolia /Aster Divaricatus, Fagus grandifolia / Mixed herbs, etc." It is obvious when reference is made to studies on swamp ecology that very little critical observation has been made of the distinctive communities that occur as the result of very slightly varying conditions such as elevation. Gaddy et al. (1976) did recognize eleven communities in their study on Congaree Swamp in South Carolina; however, they did not correlate the communities and the environmental parameters determining their distribution. This study of Beidler Forest followed a classical approach in describing the plant communities because time and financial considerations did not permit quantitative sampling. But as stated previously this study is intended as a base-line study on which to base future studies on swamp ecology in Beidler Forest. Plans are being formulated for a study of the original growth section of Beidler Forest in which correlations between plant communities and environmental parameters such as hydroperiod, soil, elevation, geology, etc., will be analyzed.
This approach should expand the list of distinct plant communities in Beidler Forest and determine the environmental parameters that determine their composition and distribution. Since this study will be made on an original growth bottomland forest system, an opportunity not available elsewhere, a significant contribution to the understanding of swamp ecology should result.
The following description of plant communities includes the three bottomland forest communities that occur on the flood-plain, a mixed mesophytic hardwood forest community on the bluff slope, and the seepage bogs at the base of the bluff slopes. As with the case with the hardwood bottom communities, the recognization of only one community on the bluff slope is simplified in light of the forementioned recent studies on natural diversity. This community will also be included in a future study of Beidler Forest.
1. Mixed Mesophytic Hardwood Forest. This community occurs on the bluff slope that flanks the eastern side of Four Holes Swamp and for a short distance along the southwest side above the northern end of Mallard's Lake. This community corresponds to Braun's (1950) mesophytic mixed hardwood community and Hunt's (1947) moist rich woods.
Along the eastern side of Four Holes Swamp, the bluff slope separates the floodplain from the adjacent uplands. In general the aspect of the slope is southwest; however, considerable local variation in aspect occurs along the entire slope due to numerous ravines dissecting the slope and acting as pathways for streams and branches that feed water into the swamp from the adjacent uplands. The bluff is approximately 25-30 feet above the flood-plain with a slope of 25-30 degrees along most of its length. A much steeper slope occurs along Mims Lake. The only comparable bluff slope on the southwest of the swamp is an area above the northern end of Mallard Lake's. Elsewhere along the southwest side of the swamp the uplands gently slope to the floodplain and no distinct mixed mesophytic hardwood forest occurs.
Only a small section of the bluff slope along the eastern side of the swamp is within the present boundary of Beidler Forest. Additional areas of the bluff slope were sampled, however, since future plans of the Audubon Society include acquisition of as much of this bluff slope as possible. During sampling of the bluff slope, it was noted that the majority of species found on the bluff slope outside of the Beidler Forest boundary were also found on the bluff slope within Beidler Forest.
It is at once evident that this mixed mesophytic hardwood community is more mesic than the oak-hickory, pine, or pine mixed-hardwood of the adjacent uplands, yet distinct from that of the alluvial bottomland of the floodplain. Canopy species include large specimens of Fagus grandifolia, Quercus michauxii, Q. falcata, &. alba, Q. nigra, &. schmardii, Liquidambar styraciflua, Liriodendron tulipifera, Juglans nigra, Acer rubrum, Nyssa syluatica, Ulmus americana Carya tomentosa, and C. glabra. An occasional loblolly pine (Pinus taeda) and spruce pine (P. glabra) are present. On the less mesic sites, oaks and hickories are more dominant, while on the more mesic sites Fagus grandifolia becomes more abundant. The bluff slope along Mims Lake actually fits the description of Braun's (1950) ravine slope forest because beech (Fagus grandifolia) comprises more than one-third of the canopy (based on field observation).
A distinct subcanopy is present, consisting of canopy species transgressives and the following common mesophytic subcanopy species: Cercis canadensis, Cornus florida, Carpinus caroliniana, Ilex opaca, and Asimina triloba.
The herbaceous species vary from the more shade tolerant species to the grasses, sedges, and legumes that became more abundant where the canopy becomes thinner. The herbaceous species growing under the dense canopy are particularly noteworthy since they include numerous of the more attractive wildflowers such as: Trillium cuneatum, Sanguinaria canadensis, Erythrina herbacea, Spigelia marilandica, Podophyllum peltatum, and six species of orchids, Malaxis spicata, M. uniflora, Tipularia discolor, Corallorhiza wisteriana, Hexalectris spicata, and Ponthieva racemosa.
The large size and old age of the canopy trees and the presence of canopy species transgressives indicate that the community is a mature, climax community, and will maintain itself barring any major disturbance. The absence of such introduced species as Lonicera japonica indicates that the community has been little disturbed in past times. The random mixture and composition of tree species throughout the community is probably due in part to the following factors: (1) its close proximity to a large wetland area and upland area whose hydrophytic (Ex.: Quercus nigra) and xerophytic (Ex.: Carya tomentosa) species respectively are present as waifs or carry-overs in a habitat much drier or wetter than typical for the species; (2) the localized variation in aspect and slope of the bluff, and (3) selective removal of species in past times. How much of the community represents original growth forest is not known, but judging from the size of many of the largest trees, it is likely that some of the trees are original growth. Many of the largest trees certainly date from colonial times. This community appears typical of the mixed mesophytic hardwood forest that occupies the slopes cut into the Pleistocene terraces of the Coastal Plain of S.C. (personal observation).
2. Seepage Bog. The upland area adjacent to Four Holes Swamp consists of sandy soil overlying a marl formation. Where the bluff slope intersects the level floodplain of the swamp, the marl is exposed as an outcrop. Groundwater from the upland sandy soil, unable to penetrate the substrata, spreads laterally and emerges as seepage where the substrata intersect the slope. This creates a bog-like condition which even in dry periods contains moisture since the flow of water is continuous. Even during the summer of 1977 when water ceased to flow in the swamp, the seepage bogs did not dry up. The water from the seepage undoubtedly tends to contribute to the water supply; however, this supply is minimal compared to the main water source of the swamp.
Three species of emergent herbs appear to be confined to the seepage bogs and have not been found elsewhere: Gratiola virginiana (hedge hyssop), Micranthemum unbrosum, and Cardamine pennsylvanica. These species tend to occur at the headwaters of the seepage where the water tends to puddle. Additional emergent herbs occurring in the bog include Saururus cernuus, Hydrocotyle verticillata, Boehmeria cylindrica, Pilea fontana, Impatiens capensis, Bacopa monnieri, and Senecio glabellus. These latter species are not confined to the seepage bog, but occur in the swamp forest wherever moisture conditions are sufficient. They do tend to be more concentrated in the bog, however, because of the permanent water supply.
In late summer and in the fall, many of the seepage bogs tend to be overgrown by Pilea fontana and Impatiens capensis. Numerous species of the adjacent swamp forest and mixed mesophytic hardwood forest tend to be localized around these seepage bogs.
Although I have not made a quantitative determination, I would estimate that there is in excess of a hundred seepage bogs scattered along the base of the bluff slope on the eastern side of Four Holes Swamp between the extremes of the Beidler Forest boundary (approximately six miles). The occurrence of seepage bogs along the remaining run of Four Holes Swamp has not been documented, but undoubtedly they are not confined to the bluff slope adjacent to Beidler Forest.
The literature on seepage bogs in the Coastal Plain is sparse. Hunt (1947) described seepage slopes in his description of the plant habitats in the Charleston area. Hunt's seepage slopes correspond to the seepage bogs described in this study. Hunt listed only the woody flora around the seepage slopes and stated that Alnus serrulata and Rhus vernix characterized the seepage slopes. In this study only A. serrulata was found, and that around only one seepage bog. A significant contribution could be made to the botany of the coastal region of S.C. by documentating the occurrence of seepage bogs and describing their vegetation.
3. Swamp Forest. The swamp forest community occupies the constantly flooded (except in extreme dry periods) alluvial soil on the lowest level of the Four Holes Swamp floodplain. In the Beidler Forest portion of Four Holes Swamp, the swamp forest community is original growth timber since no commercial lumbering has occurred in Beidler Forest. This community corresponds to Wells' (1942) "swamp forest," Hunt's (1947) "cypress swamps," Penfound's (1952) "deep freshwater southern cypress-tupelo gum swamp," and Braun's (1950) "bald cypress-tupelo gum swamp forest."
The dominant trees of the swamp forest are Taxodium distichum (bald cypress) and Nyssa aquatica (tupelo gum). Bald cypress forms the canopy, with the tallest trees around 120 feet, while tupelo gum comprises a sub-canopy approximately 80 feet tall. The largest cypress trees are around five to six feet in diameter and have been estimated to be 700 to 800 years old (Dennis, 1970). In the deeper water at the lowest elevation bald cypress and tupelo gum occur together in almost pure strands. Elsewhere in the swamp at slightly higher elevations, a variety of tree species forms a conspicuous growth. Most common is Fraxinus caroliniana, a small tree that in some areas forms a subcanopy below the Nyssa aquatica, but in most areas is not dense enough to be considered a separate subcanopy. F. caroliniana occurs in slightly raised sites and generally grows from the bases of cypress and gum trees. Nyssa sylvatica var. biflora occurs scattered throughout, occasionally reaching canopy size. Two additional hydric species, Gleditsia aquatica and Planera aquatica, occur as small trees scattered throughout the swamp, either growing from the bases of the cypress or tupelo gum or rooted in the soil. Four species characteristic of the hardwood bottom occur throughout the community rooted on fallen logs, large cypress knees, and buttresses: Quercus laurifolia, Acer rubrum, Liquidambar styraciflua,and Ulmus americana. These four species occur as small trees since they are unable to obtain large size due to the uncertain foundation on which they grow. Bald cypress exhibits typical cone buttresses and knees, and tupelo gum exhibits typical buttress formation.
A well-developed shrub layer occurs on the higher sites with species rooted in the soil or growing on buttresses, knees, fallen logs, or stumps. Species include Itea virginica, Styrax americana Leucothoe racemosa, Lyonia lucida, Cornus stricta, Cephalanthus occidentalis, Viburnum dentatum var. dentatum, and Ilex decidua. These shrubs, along with lianas and transgressives of canopy and subcanopy species, form a dense growth in most areas of this habitat. In the lower sites of the swamp forest where standing water occurs most of the year, a sparse shrub layer occurs consisting of I. virginica, S. americana, C. occidentalis, L. racemosa, and L. lucida growing from the buttresses of Taxodium and Nyssa.
The herbaceous flora of the swamp forest is exceptionally rich and varied and is worth noting. In the deeper areas of the swamp, particularly along the edges of the lakes and runs, the herbaceous flora is confined to floating logs, stumps, knees, and buttresses. This habitat is given community status by some authors (Dennis and Batson, 1974); however, I prefer to consider it a microhabitat, or dry phase, of the swamp forest. Three species appear to characterize this habitat as they do not occur elsewhere in the swamp (or in the hardwood bottom and ridge bottom); Scutellaria lateriflora, Lycopus rubellus, and Hypericum virginicum. Additional species that occur in this microhabitat, as well as in the higher areas of the swamp forest and adjacent communities, include Woodwardia aerolata, Boehmeria cylindrica, Senecio glabellus, Onoclea sensibilis, Lobelia cardinalis, Diodia virginiana, and Hypericum densiflorum. Two weedy species of the upland area, Phytolacca americana and Eupatorium compositifolium, occur as rare components of this microhabitat, an adaptation that allows these primarily terrestrial upland species to grow in an aquatic habitat by being situated above the high water level.
In the higher sites in the swamp forest where the surface water is shallow or the soil extremely wet, or where isolated, low raised areas occur, the following herbs are found: Dracocephalum purpureum, Sanolus parviflorus, Asclepias perennis, Orontium aquaticun, Peltandra virginica, Scirpus divaricatus, S. fontinalis, Proserpinaca palustris, and Lobelia cardinalis. Also found in this habitat are the species of the fallen log, stump, knee, and buttress microhabitat discussed above (with the exception of S. lateriflora, L. rubellus, and H. virginicum).
An interesting feature of the swamp forest is the presence of an occasional sapling of Pinus glabra, spruce pine, growing on the buttresses and knees of Taxodium. No large specimens were observed as they are undoubtedly unable to reach large size because of the uncertain foundation. Spruce pine is characteristic of the nearby ridge bottom community which probably acts as the seed source. Although spruce pine is frequent in the coastal counties of South Carolina north to Georgetown County (Radford et al., 1968), I know of no reference documenting its occurrence in swamp forest as described above. It is interesting to note that the more common loblolly pine, P. taeda, was not observed under similar circumstances.
That this is a mature, climax community, maintaining itself, is apparent by the following observations: (1) a considerable size variation in the dominant trees, bald cypress and tupelo gum, ranging from seedlings to large trees, and (2) the presence of numerous fire-scarred trunks of living trees and charred remains of stumps, indicating periods when the swamp was dry.
4. Hardwood Bottom. As the elevation of the floodplain increases, the swamp forest grades into a hardwood bottom community. This community corresponds to Braun's (1950) glade or hardwood bottom which she states is most common along the floodplains of the larger rivers of the southeast such as the Congaree, Wateree, Santee, Savannah, etc.
The hardwood bottoms generally occur as islands scattered throughout the swamp floodplain wherever the elevation is raised above the level of the swamp forest. The hardwood bottom is only occasionally flooded, generally for a few months during the late winter and early spring when the runoff into the swamp is too great to be carried away by the swamp drainage. However, the bottom can be flooded any time of the year when rains are unusually heavy. The soil is alluvial and the water table is probably never more than six inches below the surface. The surface is relatively flat except where earthen mounds have been produced by the root systems of large trees that have been blown over.
The canopy consists of a mixture of deciduous hardwoods with oaks predominating and an occasional cypress carry-over from the adjacent swamp forest. Knee development of cypress is either lacking or very reduced, and both the cypress and tupelo gums lack the cone buttresses characteristic of the swamp forest. Canopy tree species include: Carya aquatica, Quercus lyrata, Q. nigra, Q. phellos, Q. laurifolia, Acer rubrum, Liquidambar styraciflua, Ulmus americana, Nyssa aquatica, Nyssa sylvatica var. biflora, Fraxinus tomentosa, and Celtis laevigata. Transgressives of the canopy species are present indicating the community is maintaining itself. The stands of hardwood bottom in Beidler Forest, like the swamp forest, represent original growth timber, although undoubtedly in past times a few trees were probably removed for fuel, furniture, etc.
A poorly developed subcanopy consists of Carpinus caroliniana, Persea borbonia, Ilex opaca, and Crataegus marshallii. A shrub layer is poorly developed except for dense stands of Sabal minor at higher elevations. Herbaceous plants and lianas are sparse.
5. Ridge Bottom. At a slightly higher elevation, the hardwood bottom grades into a third bottomland forest, the ridge bottom. The ridge bottoms are free of standing water most of the year, being flooded only during the heaviest rains, and then drain very quickly when the water subsides in the floodplain. This community corresponds to Braun's (1950) ridge bottom. The distribution and abundance of this community in the South Carolina Coastal Plain is not documented in the literature, as little work on swamp ecology has been done in this area. Hunt (1947) does not mention ridge bottoms in his descriptions of plant communities in the Charleston area. Based on available literature and the author's observations of the river systems of the Coastal Plain, ridge bottoms as described by Braun (1950) and as occur in the Beidler Forest section of Four Holes Swamp, may be very limited.
Throughout the swamp floodplain, the ridge bottoms occur as islands surrounded by hardwood bottom and swamp forest. Occasionally where the gradient is somewhat steeper, a zone of hardwood bottom is absent, and the ridge bottoms border the swamp forest. Six tree species delimit the ridge from the adjacent hardwood bottom: Quercus michauxii, Q. alba, Pinus glabra, P. taeda, Carya glabra, Cornus florida, and occasionally Fagus grancliflora on the higher ridge bottoms. Most of the species from the wetter hardwood bottom complete the canopy of very large trees: Liquidambar styraciflua, Acer rubrum, Quercus laurifolia, Q. nigra and Ulmus americana. Pinus taeda, loblolly pine, occurs scattered throughout the ridge bottom, becoming locally abundant in the ridge bottom adjacent to the boardwalk. It undoubtedly became established within the hardwood forest when the canopy was opened due to the death and falling of a large canopy tree. Many of the loblollys are extremely large. The dominant trees of the swamp forest, bald cypress and tupelo gum, are absent from the ridge bottom.
The subcanopy consists of Ilex opaca, Cornus florida, Carpinus caroliniana, Diospyros virginiana, Crataegus marshallii, Morus rubra, and canopy transgressives. Unlike the adjacent hardwood bottom, the shrub layer is highly developed and represented by the following species: Ilex decidua, Aesculus pavia, Vaccinium elliottii, Sabal minor, Myrica cerifera, Rhododendron canescens, and Hamamelis virginiana. A well-developed herbaceous layer consists of a variety of carices, panic grasses, and beak rushes plus the ephemeral wildflowers Podophyllum peltatum, Zephyranthes atamasco, Trillium cuneatum, Arisaema triphyllum, Listera australis, Sanguinaria canadensis, Clematis crispa, and Trillium pusillum var. pusillum. This latter species is botanically significant since it is listed as a candidate for endangered status by the Department of Interior (1975). One population was found in the ridge bottom that lies adjacent to the boardwalk and consisted of approximately a hundred stems in a half-acre area. The rarity of this species in the Coastal Plain is reported by Radford et al. (1968) and by Percher (1979). No other populations were found in Beidler Forest although the brief flowering period makes it likely that it could easily have been overlooked.
Three hundred and twelve species of vascular plants, representing two hundred and eighteen genera and ninety-nine families, were collected in Beidler Forest and environs during this study. A summary of the flora is given at the end of this checklist. This checklist includes species found in the disturbed woods around the Visitor's Center. Plant collections were made primarily from March of 1976 through August of 1978, with a few made during the summer of 1979. One set of voucher specimens has been deposited in The Citadel Herbarium, Charleston, S.C. A second set is being maintained at The Citadel Herbarium, but will be ultimately maintained at the Visitor's Information Center at Beidler Forest when facilities are available. Nomenclature and sequence of families follows that of Radford et al. (1968). The habitat and frequency were determined by subjective field observations. Frequency of species is indicated by the relative terms: rare, occasional, locally abundant, and common. Frequency determinations are omitted from some species, such as Carer alata and Panicum dichotomiflorum, because of the difficulty in recognizing the species in the field.
For brevity the following numbers are used to represent the five communities: 1=mixed mesophytic hardwood forest, 2=seepage bog, 3=swamp forest, 4=hardwood bottom, and 5=ridge bottom.
| Summary of the Vascular Flora of Beidler Forest and Environs | |||||
|---|---|---|---|---|---|
| Ferns | Gymnosperms | Monocotyledons | Angiosperms Dicotyledons | Total | |
| Families | 8 | 3 | 15 | 73 | 99 |
| Genera | 12 | 3 | 48 | 155 | 218 |
| Species | 16 | 4 | 77 | 215 | 312 |
| Subspecies | 1 | 1 | |||
| Varieties | 1 | 7 | 15 | 23 | |
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