Changes due to fire suppression in a Quercus velutina Lam. (black oak) savanna at Sand Ridge State Forest, Mason County, Illinois.
In the prairie-forest interface of the prairie peninsula of Illinois the presence of prairie, savanna, woodland, and forest was determined largely by environmental factors, including extent and intensity of fire, climate, water bodies, and topography (Transeau 1935, Anderson 1991, Ebinger and McClain 1991, Abrams 1992). Other contributing factors important on a local level included soil texture, drought frequency, and browsing by large herbivores (Nuzzo 1986).
Savanna communities were extremely common in the landscape of Illinois in the 1800s, and are generally defined as having overstories of scattered, open-grown trees and a grass-dominated ground layer (Curtis 1959, Bray 1960, Nuzzo 1986, White and Madany 1978). Journals of many early travelers and settlers recount the open park-like landscape in much of the state (Bourne 1820, Engelmann 1863, Vestal 1936). Government Land Office (GLO) survey records also indicate that many "forests" were actually savanna and woodland communities based on distance of witness trees to corner posts (Cottam and Curtis 1949, Clements 1958, Hutchison 1988). Furthermore, many present day old-growth forests retain a few open-grown "wolf trees" with low branches and branch-scars, and fire scares, indicating they were formerly part of an open landscape (Curtis 1959, Ebinger and McClain 1991).
European man cleared most "black soil" savannas in Illinois soon after settlement. These savannas, with few trees, thinner sod, and often drier soil, were easier to cultivate with wooden plows of the settlers than the dense, thick prairie sod. The few remaining "black soil" savanna communities are extensively degraded due to a massive influx of exotic species and canopy closure due to fire suppression and subsequent woody invasion of native species. In contrast, sand savanna communities are still relatively common in the northern half of Illinois on major sand deposits. These deposits are mostly on outwash plains that resulted from erosional events associated with Wisconsin glaciation (Willman and Frye 1970, King 1981). Gleason (1910), and more recently Jenkins et al. (1991), Coates et al. (1992), McClain et al. (2002), and Phillippe et al. (2009) studied the structure and composition of the Illinois River sand deposit woodlands, while Rodgers and Anderson (1979) studied the presettlement vegetation of Mason County. Mostly modified by human activity, a few nature preserves and other good quality natural areas remain on these extensive sand deposits. The present study was undertaken to determine the woody overstory and understory species composition and structure of a degraded sand savanna at Sand Ridge State.
DESCRIPTION OF THE STUDY SITE
Sand Ridge State Forest is located in north-western Mason County about 21 km northwest of Havana and just west of Forest City, Illinois (parts of townships T22N R7W and T23N R7W). This 3,035 ha (11.7 sq. miles) state forest, with initial land purchases starting in 1939, lies within the Illinois River Section of the Mississippi River and Illinois River Sand Area Natural Division in Mason and Cass counties (Schwegman 1973, Willman 1973). These deposits were formed about 14,500 years ago when glacial moraines and ice dams were breached. The resulting Kankakee Torrent carried extensive deposits of sand and gravel from glacial lakes in northeastern Illinois and adjacent Indiana. Most of this sand and gravel was deposited when the waters of the Kankakee Torrent slowed upon entering the broad lowlands of the Illinois River. Winds reworked these deposits, creating the present dune and swale topography (Willman 1973).
The original reason for purchasing the land for what is now the Sand Ridge State Forest was to stabilize soil on abandoned farmland, develop a wood product industry, and set land aside for recreation (Andrews 2004). During the early years, and into the 1950's, pine plantations were established, mostly on old pastureland and abandoned cultivated fields, but also in dry sand prairies and sand savannas. Presently, 1,012 ha of pine plantations exist with most of the remainder in oak-hickory dry sand forest and savanna (Andrews 2004).
Sand Ridge State Forest has a continental climate with warm summers and cold winters. Based on weather data from Havana, mean annual precipitation is 96.0 cm, with May having the highest rainfall (11.3 cm). Mean annual temperature is 10.8[degrees]C with the hottest month being July (average of 24.6[degrees]C), and the coldest January (average of -5.0[degrees]C). Frost-free days range from 140 to 206, averaging 173 days (Midwestern Regional Climate Center 2004). Soils are primarily excessively drained Plainfield and Bloomfield sands (Calsyn 1995) that form the dune and swale topography known as the Parkland Formation (Willman and Frye 1970).
During late summer of 2004 a 100 m by 300 m section of the state forest was surveyed by dividing the area into 48 contiguous quadrats 25 m on a side. This 3 ha area was located on a large stabilized dune having an east/west orientation, the centerline of the transect running along the ridge of the dune (N1/2 NW1/4 NE1/4 S4 T22N R7W). The GPS readings for the line transect at 0 m (40.39064[degrees]N/-089.89060[degrees]W), and at 300 m (40.39064[degrees]N/-089.89420[degrees]W) were recorded and marked with permanent metal stakes. All living and dead-standing woody individuals [greater than or equal to]10.0 cm dbh were identified and their diameters recorded. From this data, living-stem density (stems/ha), basal area ([m.sup.2]/ha), relative density, relative dominance, importance value (IV), and average diameter (cm) were calculated for each species. Determination of the IV follows the procedure used by McIntosh (1957), and is the sum of the relative density and relative dominance (basal area). Dead-standing density (stems/ha) and basal area ([m.sup.2]/ha) was also determined. Multiple stemmed trees (coppice) were recorded as separate individuals. Nomenclature follows Mohlenbrock (2002).
Woody understory composition and density (stems/ha) were determined using nested circular plots 0.0001, 0.001, and 0.01 ha in size located at 15 meter intervals along randomly located east-west line transects within the study area (48 plots). Four additional 0.0001 ha circular plots were located 7 m from the center points of each of the 48 plot centers along cardinal compass directions (240 plots). In the 0.0001 ha plots, woody tree seedlings ([greater than or equal to]50 cm tall) and shrubs and vines were counted; in the 0.001 ha circular plots small saplings (>50 cm tall and <2.5 cm dbh) were recorded; and in the 0.01 ha circular plots large saplings (2.5-9.9 cm dbh) were tallied.
Changes in overstory cover within the state forest was measured using aerial photographs from 1939, 1957, 1969, 1988, and 1998 that were digitized to determine the extent of woody encroachment (trees and large shrubs). These photographs were borrowed from the University of Illinois Map Library and scanned with a Microtek ScanMaker. A total of 20 stratified randomly located 5 ha circular plots (100 ha total area), representing approximately 20% of the study sites, were interpreted and then digitized using ARC/INFO.
Eleven tree species were encountered in the overstory (Table 1). Quercus velutina Lam. (black oak) dominated all diameter classes with the 10-29 cm diameter classes accounting for more than 50% of all tallied individuals, with only three stems/ha greater than 60 cm dbh. This species had an IV of 143.5, averaged 321.1 stems/ha, averaged 23.6 cm dbh, and accounted for 78.1% of the total basal area. Quercus marilandica Muench. (blackjack oak), second in IV (34.7), was mostly restricted to smaller diameter classes, averaged 111.6 stems/ha, and averaged 16.5 cm dbh. The remaining species were mostly in the 10-39 cm diameter classes, Carya texana Buckl. (black hickory) averaged 26.3 stems/ha, while Pinus strobus L. (white pine) averaged 26.1 stems/ ha. Coppice stems accounted for about 16% of the stems encountered. Quercus velutina accounted for the majority, averaging 27 coppice trees/ha with 57.7 stems/ha, and accounted for about 10% of the total basal area on the site (Table 2).
Dead-standing individuals averaged 24.6 stems/ha with a basal area of 1.01 m2/ha, nearly all being oaks. Quercus velutina averaged 15.6 dead-standing stems/ha while Q. marilandica accounted for nearly all of the remainder. Most of the dead-standing individuals were in the lower diameter classes. A few dead-standing Q. velutina exceeded 40 cm dbh.
The woody understory averaged 15,200 seedlings/ha, 1,775 small saplings/ha, and 295 large saplings/ha (Table 3). Seedling density was relatively high, but the majority was shrubby species. Quercus velutina and Carya texana accounted for nearly all tree seedlings. Because of the relatively few saplings, the woody understory was open. Again, Q. velutina and C. texana accounted for the majority of individuals (Table 3). Woody shrubs that were important in the understory included, Rubus allegheniensis Porter (common blackberry), Rhus aromatica Ait. (fragrant sumac), Toxicodendron radicans (L.) Kuntze (poison ivy), and Cornus drummondii C. A. Mey. (rough-leaved dogwood) (Table 3). Woody exotic shrubs were uncommon with Lonicera maackii (Rupr.) Maxim. (Amur honeysuckle) occurred in a few plots.
In approximately 60 years the sand savanna at Sand Ridge State Forest became a closed forest. Based on an analysis of 1939 aerial photographs approximately 50.18% of the study area was covered by trees and large shrubs. Canopy cover increased dramatically by 1957 to 68.96%, followed by an increase of 78.66% by 1969, 88.08% by 1988, and 89.50% by 1998. Woody encroachment is most obvious where pine plantations were introduced in the 1940s and 1950s. The cover in 1939 lacked introduced conifers, and only the native Juniperus virginiana (red cedar) was present. Conifers were not observed in the 50 sites digitized from the 1939 aerial photographs, but they were found in 35 of the 50 digitized sites in the 1998 photographs.
The woody plant communities at Sand Ridge State Forest are very different today compared to the early 1800s, mostly due to the planting of pines and reduced fire frequencies followed by the total absence of fire in recent decades (Taft 1997). In presettlement times repeated fires were probably responsible for maintaining an open savanna with a sparse woody understory (Ebinger and McClain 1991, McClain and Elzinga 1994). The larger trees maintained an open-grown appearance with low branches and branch-scars. A few large, open-grown trees were still present in the study plots. Because of fire and droughty conditions, most of this present day forest was originally savanna communities with numerous prairie openings.
Presently, occasional fires and droughty conditions have allowed the perpetuation of oak species. Quercus velutina is reproducing with numerous seedlings and saplings in the understory (Table 3). Quercus marilandica, in contrast, has a very low rate of reproduction. The large number of seedlings, saplings, and small diameter trees of Carya texana suggests this species will increase in importance (Table 3). As canopy closure continues, shade-intolerant oaks may not effectively reproduce. Carya texana, a fire-sensitive but relatively shade-tolerant species, could become the dominant understory species and became more common in the lower diameter classes, particularly if management fires are not introduced on a regular basis.
Woody exotic species are common in Sand Ridge State Forest. At least 10 species of pine were planted in the 1940s and early 1950s, and many pine plantations are present (Maier 1976, Andrews 2004). The most commonly planted species was Pinus strobus. A few rows of this introduced exotic species were present in our study plots, indicating this species was also planted in native hardwood forests and savannas. Smaller individuals, plus occasional seedlings indicate that this species is reproducing.
Using GLO survey records, Rodgers and Anderson (1979) described the presettlement vegetation of Mason County. They found that tree density averaged 7.44 trees/ ha with an average basal area of 1.19 [m.sup.2]/ha in savanna communities. Quercus velutina was, by far, the dominant woody species, accounting for more than half of the IV. Quercus marilandica was second in IV followed by various Carya (hickory) species. The many small diameter witness trees reported in the GLO survey indicate that the relatively shade-intolerant oaks and hickories were reproducing, and were replacing themselves in savanna, woodland, and closed forest communities (Rodgers and Anderson 1979).
Most forests studied within the Illinois River sand deposits were closed canopy dry sand forests located on dune deposits where Quercus velutina and Q. marilandica were usually the leading dominants along with a few hickory species. Carya texana occasionally replaced Q. marilandica as second in IV in those forests (Jenkins et al. 1991, Coates et al. 1992, McClain et al. 2002). These forests probably represented sand savannas that have become closed forests due to fire suppression and woody species invasion (Considine et al. 2013). This study at Sand Ridge State Forests suggests that a combination of increased fire frequency, selective timber harvest, and possibly grazing will be necessary to restore and maintain the savanna communities that were once characteristic of this site.the 1998 photographs.
The authors thank John Wilker, Natural Areas Program Manager, Illinois Department of Natural Resources, for his help and advice. The Illinois Department of Natural Resources, Wildlife Preservation Fund and the Illinois Department of Transportation supported this project.
Abrams, M.D. 1992. Fire and the development of oak forests. BioScience 42:346-353.
Anderson R.C. 1991. Presettlement forest of Illinois. pages 9-19. in G.V. Burger, J.E. Ebinger, and G.S. Wilhelm (editors). Proceedings of the Oak Woods Management Workshop. Eastern Illinois University, Charleston, Illinois.
Andrews, K. 2004. Forest Treasures. Outdoor Illinois. December 2004:2-5.
Bourne, A. 1820. On the prairies and barrens of the west. American Journal of Science and Arts 2:30-34.
Bray, J.R. 1960. The composition of savanna vegetation in Wisconsin. Ecology 41:721-732.
Calsyn, D.E. 1995. Soil survey of Mason County, Illinois. Soil Report 146, University of Illinois Agricultural Experiment Station, Urbana. ix+211 pp.
Clements, D.B. 1958. Public land surveys-history and accomplishments. Survey and Mapping 18:213-219.
Coates, D.T., S.E. Jenkins, J.E. Ebinger, and W.E. McClain. 1992. Woody vegetation survey of Barkhausen Woods, a closed canopy sand forest in Mason County, Illinois. Erigenia 12:1-6.
Considine, C.D., J.W. Groninger, C.M. Ruffner, M.D. Therrell, and S.G. Baer. 2013. Fire history and stand structure of a high quality black oak (Quercus velutina) sand savanna. Natural Areas Journal 30:10-20.
Cottam, G. and J.T. Curtis. 1949. A method for making rapid surveys of woodlands by means of pairs of randomly selected trees. Ecology 30:101-104.
Curtis, J.T. 1959. The vegetation of Wisconsin. The University of Wisconsin Press. Madison. 657 pp.
Ebinger, J.E. and W.E. McClain. 1991. Forest succession in the prairie peninsula of Illinois. Illinois Natural History Survey Bulletin 34:375-381.
Engelmann, H. 1863. Remarks upon the causes producing the different characters of vegetation known as prairie, flats, and barrens in southern Illinois, with special reference to observations made in Perry and Jackson counties. American Journal of Science 86:384-396.
Gleason, H.A. 1910. The vegetation of the inland sand deposits of Illinois. Bulletin of the Illinois State Laboratory of Natural History 9:21-174.
Hutchison, M. 1988. A guide to understanding, interpreting, and using the Public Land Survey field notes in Illinois. Natural Areas Journal 8:245-255.
Jenkins, S.E., J.E. Ebinger, and W.E. McClain. 1991. Woody vegetation survey of Bishop's Woods, a sand forest in Mason County, Illinois. Transactions of the Illinois State Academy of Science 84:20-27.
King, J.E. 1981. Late Quaternary vegetational history of Illinois. Ecological Monographs 51:43-62.
Maier, C.T. 1976. An annotated list of the vascular plants of Sand Ridge State Forest, Mason County, Illinois. Transactions of the Illinois State Academy of Science 69:153-175.
McClain, W.E. and S.L. Elzinga. 1994. The occurrence of prairie and forest fires in Illinois and other Midwestern states, 1679 to 1854. Erigenia 13:79-90.
McClain, W.E., S.D. Turner, and J.E. Ebinger. 2002. Vegetation of forest communities at the Sand Prairie-Scrub Oak Nature Preserve, Mason County, Illinois. Transactions of the Illinois State Academy of Science 95:37-46.
McIntosh, R.P. 1957. The York Woods. A case history of forest succession in southern Wisconsin. Ecology 38:29-37.
Midwestern Regional Climate Center. 2004. http://mcc.sws.uiuc.edu
Mohlenbrock, R.H. 2002. Vascular Flora of Illinois. Southern Illinois University Press, Carbondale, Illinois. xi+490 pp.
Nuzzo, V.A. 1986. Extent and status of mid-west oak savanna: presettlement and 1985. Natural Areas Journal 6:6-36.
Phillippe, L.R., J.L.Ellis, D.T Busemeyer, W.E. McClain and J.E. Ebinger. 2009. Vegetation survey of Tomlin Timber Nature Preserve, Mason County, Illinois. Erigenia 22:36-44.
Rodgers, C.S. and R.C. Anderson. 1979. Presettlement vegetation of two prairie peninsula counties. Botanical Gazette 232-240.
Schwegman, J.E. 1973. Comprehensive plan for the Illinois nature preserves system. Part 2. The natural divisions of Illinois. Illinois Nature Preserves Commission, Rockford, Illinois. map+32 pp.
Taft, J.B. 1997. Savanna and open woodland communities. Pages 24-54. in M.W. Schwartz (editor). Conservation in highly fragmented landscapes. Chapman and Hall, New York.
Transeau, E.N. 1935. The prairie peninsula. Ecology 16:423-437.
Vestal, A.G. 1936. Barrens vegetation in Illinois. Transactions of the Illinois State Academy of Science 29:29-30.
Willman, H.B. 1973. Geology along the Illinois waterway--a basis for environmental planning. Illinois State Geological Survey Circular 478. Urbana. 48 pp.
Willman, H.B. and J.C. Frye. 1970. Pleistocene stratigraphy of Illinois. Illinois State Geological Survey Bulletin 94:1-204.
White, J. and M.H. Madany. 1978. Classification of natural communities in Illinois. Pp. 310-405 in Illinois natural areas inventory. Technical report. (J. White, Editor). Illinois Natural Areas Inventory, Urbana, Illinois.
Loy R. Phillippe, Paul B. Marcum, Daniel T. Busemeyer, William E. McClain, Mary Ann Feist, and John E. Ebinger
Illinois Natural History Survey, Champaign, Illinois 61820
Table 1. Densities (stems/ha), diameter classes, basal areas ([m.sup.2]/ha), relative values, importance values and average diameters of the woody species at Sand Ridge State Forest, Mason County, Illinois. Other species include: Carya tomentosa (Poir.) Nutt., Diospyros virginiana L., Juniperus virginiana L., Pinus banksiana Lamb., Pinus sylvestris L., Prunus serotina Ehrh., Ulmus americana L. Diameter Classes (cm) Species 10-19 20-29 30-39 40-49 50-59 60+ Quercus velutina 145.3 107.7 37.7 20.7 6.7 3.0 Quercus 92.0 17.0 2.3 0.3 -- -marilandica Pinus strobus 12.7 8.7 2.7 2.0 -- - Carya texana 20.0 3.3 1.7 1.0 0.3 - Others (7 spp.) 5.7 -- -- -- -- - Totals 275.7 136.7 44.4 24.0 7.0 3.0 Total Basal Rel. Rel. Av. Species Stems/ Area Den. Dom. I.V. Diam. ha [m.sup.2] (cm) /ha Quercus velutina 321.1 16.995 65.4 78.1 143.5 23.6 Quercus 111.6 2.601 22.8 11.9 34.7 16.5 marilandica Pinus strobus 26.1 1.243 5.3 5.7 11.0 23.0 Carya texana 26.3 0.849 5.4 3.9 9.3 17.9 Others (7 spp.) 5.7 0.080 1.1 0.4 1.5 - Totals 490.8 21.768 100.0 100.0 200.0 Table 2. Density (#/ha) of coppice trees and stems, coppice stems per tree, average basal area ([m.sup.2]/ha) of coppice stems, and the average diameter (cm) of coppice stems at Sand Ridge State Forest, Mason County, Illinois. Species Trees Stems Stems/ Basas Are Avg. (#/ha) (#/ha) tree ([m.sup.2] Diameter /ha) (cm) Quercus velutina 27.0 57.7 2.1 2.721 23.4 Quercus marilandica 9.0 19.3 2.2 0.540 17.9 Carya texana 1.7 3.3 2.0 0.099 17.1 Totals 37.7 80.3 3.360 Table 3. Density (individuals/ha) of woody understory species in a woodland community at Sand Ridge State Forest, Mason County, Illinois. ( * exotic species) Species Seedlings Small Saplings Large Saplings Quercus velutina 3750 575 100.0 Carya texana 2850 600 85.0 Prunus serotina 250 250 20.0 Quercus marilandica 250 25 30.0 Carya tomentosa 150 125 17.5 * Pinus strobus 150 25 17.5 Juniperus virginia -- 100 15.0 * Pinus sylvestris -- -- 5.0 Ulmus americana -- -- 2.5 Celtis occidentalis -- -- 2.5 Rubus allegheniens 2250 -- - Rhus aromatica 1850 -- - Toxicodendron radicans 1650 -- - Cornus drummondii 1600 50 - Rubus occidentalis300 -- -- - Ribes missouriense100 -- -- - Viburnum prunifolium50 -- -- - * Lonicera maackii -- 25 -- - Totals 15200 1775 295.0
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|Author:||Phillippe, Loy R.; Marcum, Paul B.; Busemeyer, Daniel T.; McClain, William E.; Feist, Mary Ann; Ebin|
|Publication:||Transactions of the Illinois State Academy of Science|
|Date:||Jan 1, 2013|
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