Natural Resources
Conservation Service
Ecological site F116CY003MO
Dry Igneous Upland Woodland
Accessed: 04/23/2024
General information
Approved. An approved ecological site description has undergone quality control and quality assurance review. It contains a working state and transition model, enough information to identify the ecological site, and full documentation for all ecosystem states contained in the state and transition model.
Figure 1. Mapped extent
Areas shown in blue indicate the maximum mapped extent of this ecological site. Other ecological sites likely occur within the highlighted areas. It is also possible for this ecological site to occur outside of highlighted areas if detailed soil survey has not been completed or recently updated.
MLRA notes
Major Land Resource Area (MLRA): 116C–St. Francois Knobs and Basins
The St Francois Knobs and Basins is the structural center of the Ozark Dome. Elevation ranges from about 450 feet along the rivers in the southern part of the area, to 1,772 feet on the summit of Taum Sauk Mountain, the highest point in Missouri. Prominent features of this major land resource area (MLRA) are the Precambrian igneous knobs and hills that rise conspicuously to various elevations, interspersed with smooth-floored basins and valleys overlying dolomite and sandstone. Ecological sites defined for this MLRA are associated with the igneous parent materials, either in knob or basin positions. Areas influenced primarily by dolomite and/or sandstone are included in ecological sites within MLRA 116A (Ozark Highlands).
Classification relationships
Atlas of Missouri Ecoregions (Nigh and Schroeder 2002):
This ecological site occurs primarily within the following Land Type Association:
OZ10a St. Francois Igneous Glade/Oak Forest Knobs
Terrestrial Natural Community Type (Nelson, 2010):
The reference state for this ecological site is most similar to: Dry Igneous Woodlands
National Vegetation Classification System Vegetation Association (NatureServe, 2010):
The reference state for this ecological site is most similar to: (CEGL005029) Quercus velutina - (Quercus ellipsoidalis) - Quercus alba / Deschampsia flexuosa Woodland
Ecological site concept
Dry Igneous Upland Woodlands occur throughout the MLRA and on outlying igneous knobs in adjacent counties. Soils are moderately deep, often with abundant volcanic rock fragments, and are low in bases. These sites are often adjacent to both Igneous Upland Woodland and Shallow Igneous Knob Glade ecological sites, and in places, are mapped in complex with them. Igneous Upland Woodland sites do not have root-restricting bedrock in the upper part of the soil profile, whereas Shallow Igneous Knob Glade sites are shallow to bedrock and are interspersed with rock outcrop. Vegetation of the reference state is woodland dominated by short, open-grown post oak mixed with scattered northern red, blackjack and black oaks.
Associated sites
| F116CY002MO |
Igneous Upland Woodland Igneous Upland Woodlands are often upslope from Dry Igneous Upland Woodlands, but are intermingled in other areas and mapped as a complex. |
|---|---|
| F116CY005MO |
Dry Igneous Protected Backslope Woodland Igneous Protected Backslope Woodlands are typically downslope from Dry Igneous Upland Woodlands, and are steeper. |
| F116CY011MO |
Dry Igneous Exposed Backslope Woodland Dry Igneous Exposed Backslope Woodlands are typically downslope from Dry Igneous Upland Woodlands, and are steeper. |
| R116CY006MO |
Shallow Igneous Knob Glade Shallow Igneous Knob Glades have shallow soils with significant amounts of bedrock outcrop. These two ecological sites are typically intermingled, and mapped as a complex. |
Similar sites
| F116CY011MO |
Dry Igneous Exposed Backslope Woodland Dry Igneous Exposed Backslope Woodlands are typically downslope from Dry Igneous Upland Woodlands, and are steeper but similar in species composition. |
|---|
Table 1. Dominant plant species
| Tree |
(1) Quercus stellata |
|---|---|
| Shrub |
(1) Rhus aromatica |
| Herbaceous |
(1) Danthonia spicata |
Physiographic features
This site is on upland summit crests, shoulders and backslopes with slopes of 3 to 15 percent. The site generates runoff to adjacent, downslope ecological sites. This site does not flood.
The following figure (adapted from Simmons et al., 2006) shows the typical landscape position of this ecological site, and landscape relationships among the major ecological sites in the igneous uplands. The site is within the area labeled “3”, generally upslope from steeper, backslope ecological sites.
Figure 2. Major ecological sites of the igneous uplands.
Table 2. Representative physiographic features
| Landforms |
(1)
Ridge
(2) Interfluve (3) Hill (4) Knob |
|---|---|
| Flooding frequency | None |
| Ponding frequency | None |
| Elevation | 600 – 1,700 ft |
| Slope | 3 – 15% |
| Water table depth | 24 – 60 in |
| Aspect | Aspect is not a significant factor |
Climatic features
The St. Francois Knobs and Basins have a continental type of climate marked by strong seasonality. In winter, dry-cold air masses, unchallenged by any topographic barriers, periodically swing south from the northern plains and Canada. If they invade reasonably humid air, snowfall and rainfall result. In summer, moist, warm air masses, equally unchallenged by topographic barriers, swing north from the Gulf of Mexico and can produce abundant amounts of rain, either by fronts or by convectional processes. In some summers, high pressure stagnates over the region, creating extended droughty periods. Spring and fall are transitional seasons when abrupt changes in temperature and precipitation may occur due to successive, fast-moving fronts separating contrasting air masses.
The St. Francois Knobs and Basins experience few regional differences in climates. The average annual precipitation in this area is 42 to 46 inches. The average annual temperature is about 54 to 56 degrees F. The lower temperatures occur at the higher elevations. Mean July maximum temperatures have a range of only one or two degrees across the area.
Mean annual precipitation varies somewhat along a west to east gradient. The rainfall is fairly evenly distributed throughout the year. Snow falls nearly every winter, but the snow cover lasts for only a few days.
During years when precipitation is normal, moisture is stored in the soil profile during the winter and early spring, when evaporation and transpiration are low. During the summer months, the loss of water by evaporation and transpiration is high, and if rainfall fails to occur at frequent intervals, drought will result. Drought directly affects plant and animal life by limiting water supplies, especially at times of high temperatures and high evaporation rates.
Superimposed upon the basic MLRA climatic patterns are local topographic influences that create topoclimatic, or microclimatic variations. For example, air drainage at night may produce temperatures several degrees lower in the basin and floodplain ecological sites downslope from this ecological site. At critical times during the year, this phenomenon may produce later spring or earlier fall freezes in basins and valleys. Nearby glade ecological sites may have higher daytime temperatures due to bare rock and higher reflectivity of these un-vegetated surfaces. Slope orientation is an important topographic influence on climate. Summits and south-and-west-facing slopes are regularly warmer and drier than adjacent north- and-east-facing slopes. Finally, the micro-climate within closed-canopy woodland communities is measurably different from the micro-climate of open-canopy woodlands within this ecological site.
References:
University of Missouri Climate Center. Accessed May 2012. http://climate.missouri.edu/climate.php.
United States Department of Agriculture, Natural Resources Conservation Service. 2006. Land Resource Regions and Major Land Resource Areas of the United States, the Caribbean, and the Pacific Basin. U.S. Department of Agriculture Handbook 296.
Table 3. Representative climatic features
| Frost-free period (characteristic range) | 137-145 days |
|---|---|
| Freeze-free period (characteristic range) | 164-169 days |
| Precipitation total (characteristic range) | 45-47 in |
| Frost-free period (actual range) | 136-148 days |
| Freeze-free period (actual range) | 163-170 days |
| Precipitation total (actual range) | 45-47 in |
| Frost-free period (average) | 141 days |
| Freeze-free period (average) | 166 days |
| Precipitation total (average) | 46 in |
Figure 3. Monthly precipitation range
Figure 4. Monthly minimum temperature range
Figure 5. Monthly maximum temperature range
Figure 6. Monthly average minimum and maximum temperature
Figure 7. Annual precipitation pattern
Figure 8. Annual average temperature pattern
Climate stations used
-
(1) FARMINGTON [USC00232809], Farmington, MO
-
(2) FREDERICKTOWN [USC00233038], Fredericktown, MO
-
(3) ARCADIA [USC00230224], Arcadia, MO
Influencing water features
This ecological site is not influenced by wetland or riparian water features. This site generates runoff to adjacent, downslope ecological sites. The water features of this upland ecological site include evapotranspiration, surface runoff, and drainage. Each water balance component fluctuates to varying extents from year-to-year. Evapotranspiration remains the most constant. Precipitation and drainage are highly variable between years. Seasonal variability differs for each water component. Precipitation generally occurs as single day events. Evapotranspiration is lowest in the winter and peaks in the summer. Water stored as ice and snow decreases drainage and surface runoff rates throughout the winter and increases these fluxes in the spring. The surface runoff pulse is greatly influenced by extreme events. Conversion to cropland or other high intensities land uses tends to increase runoff, but also decreases evapotranspiration. Depending on the situation, this might increase groundwater discharge, and decrease baseflow in receiving streams.
Soil features
These soils have rhyolitic volcanic bedrock at 20 to 40 inches, and acidic subsoils that are low in bases. The soils were formed under woodland vegetation, and have thin, light-colored surface horizons. Parent material is slope alluvium and residuum weathered from acid igneous rock such as rhyolite. Some areas on summit crests have loess in the upper part. They have loam surface horizons that range to very gravelly and cobbly, and typically have skeletal subsoils with high amounts of volcanic gravel and cobbles. These soils are not affected by seasonal wetness. Soil series associated with this site include Irondale and Knobtop.
The accompanying picture of the Knobtop series shows a thin, light-colored silt loam surface horizon over a brown silty clay loam subsoil. Igneous rock fragments are shown in this profile below about 2 feet. Hard igneous bedrock is at the bottom of the picture, just above 3 feet. Scale is in feet.
Figure 9. Knobtop series
Table 4. Representative soil features
| Parent material |
(1)
Slope alluvium
–
rhyolite
(2) Residuum – rhyolite |
|---|---|
| Surface texture |
(1) Gravelly silt loam |
| Family particle size |
(1) Loamy |
| Drainage class | Moderately well drained to well drained |
| Permeability class | Moderate |
| Soil depth | 20 – 40 in |
| Surface fragment cover <=3" | 5 – 40% |
| Surface fragment cover >3" | 5 – 40% |
| Available water capacity (0-40in) |
2 – 4 in |
| Calcium carbonate equivalent (0-40in) |
Not specified |
| Electrical conductivity (0-40in) |
2 mmhos/cm |
| Sodium adsorption ratio (0-40in) |
Not specified |
| Soil reaction (1:1 water) (0-40in) |
3.5 – 6 |
| Subsurface fragment volume <=3" (Depth not specified) |
10 – 45% |
| Subsurface fragment volume >3" (Depth not specified) |
5 – 55% |
Ecological dynamics
Information contained in this section was developed using historical data, professional experience, field reviews, and scientific studies. The information presented is representative of very complex vegetation communities. Key indicator plants, animals and ecological processes are described to help inform land management decisions. Plant communities will differ across the MLRA because of the naturally occurring variability in weather, soils, and aspect. The Reference Plant Community is not necessarily the management goal. The species lists are representative and are not botanical descriptions of all species occurring, or potentially occurring, on this site. They are not intended to cover every situation or the full range of conditions, species, and responses for the site.
Dry Igneous Upland Woodlands are dominated by short (30 to 50 feet) open grown post oak (Quercus stellata), with scattered northern red oak (Quercus rubra), blackjack oak (Quercus marilandica) and black oak (Quercus velutina) and an occasional shortleaf pine (Pinus echinata). Canopy closure varies with aspect and the soil depth range within the soil component. This created conditions from open 30 to 50 percent canopy on the most exposed positions and shallower soil ranges, to a more closed 50 to 80 percent canopy on protected positions and the deeper soil depth ranges for this soil component. The understory is open with a dense ground flora of native grasses and forbs (Nelson, 2010).
The somewhat shallow soils and upland landscape position of Dry Igneous Upland Woodlands limits the growth of trees and supports an abundance of native grasses and forbs in the understory. Fire played an important role in the maintenance of these systems as well. It is likely that these ecological sites, along with adjacent knobs burned at least once every 5 years. These periodic fires would have kept woodlands open, removed the litter, and stimulated the growth and flowering of the grasses and forbs (Ladd, 1991; Frost, 1996).
These sites were also subjected to occasional disturbances from wind and ice, as well as grazing by native large herbivores, such as bison (Bison bison), elk (Cervus Canadensis), and white-tailed deer (Odocoileus virginianus). Wind and ice would have periodically opened the canopy up by knocking over trees or breaking substantial branches off canopy trees. Grazing by native herbivores would have effectively kept understory conditions more open, creating conditions more favorable to oak reproduction and sun-loving ground flora species.
In the long term absence of fire, woody species have encroached into these woodlands. Once established, these species can quickly increase in density. Most occurrences today are dense and shady with a greatly diminished ground flora. Removal of the younger understory and the application of prescribed fire have proven to be effective management tools.
Currently, domestic grazing is absent or very limited on these sites due to lack of water, access issues, and high amounts of acorns on the ground in the fall that are detrimental to cattle. Timber harvesting also occurs but is restricted on these sites because of the lower site productivity. Where deeper soil depths range for this soil component, occasional oaks are harvested. They are excellent wildlife sites. (Missouri Department of Conservation, 2006)
A state and transition model for the Dry Igneous Upland Woodland Ecological Site (F116CY003MO) follows this narrative. Descriptions of each state, transition, plant community, and pathway follow the model. Experts base this model on available experimental research, field observations, professional consensus, and interpretations. It is likely to change as knowledge increases. The following diagram suggests some pathways that the vegetation on this site might take. There may be other states not shown on the diagram. This information is intended to show what might happen in a given set of circumstances. It does not mean that this would happen the same way in every instance. Local professional guidance should always be sought before pursuing a treatment scenario.
The following diagram suggests some pathways that the vegetation on this site might take. There may be other states not shown on the diagram. This information is intended to show what might happen in a given set of circumstances. It does not mean that this would happen the same way in every instance. Local professional guidance should always be sought before pursuing a treatment scenario.
State and transition model
Figure 10. State and Transition Diagram
More interactive model formats are also available.
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More interactive model formats are also available.
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Click on state and transition labels to scroll to the respective text
Ecosystem states
State 1 submodel, plant communities
State 2 submodel, plant communities
State 3 submodel, plant communities
State 1
Reference State
The reference state was old growth woodland dominated by short (30 to 50 feet) open grown post oak, with scattered blackjack oak, northern red oak, and black oak and an occasional shortleaf pine. Canopy closure varies with aspect and soil depth from open 30 to 50 percent canopy, on most exposed positions, on shallower soils, to more closed, 50 to 80 percent canopy on more protected positions with deeper soil profiles. The understory is open with a dense ground flora of native grasses and forbs. Fire played an important role in the maintenance of this state as well. It is likely that these ecological sites, along with adjacent knobs burned at least once every 5 years. These periodic fires would have kept woodlands open, removed the litter, and stimulated the growth and flowering of the grasses and forbs. Soil fertility and site productivity are low. Two community phases are recognized in the reference state, with shifts between phases based on disturbance frequency. Old growth woodlands are very rare today.
Dominant plant species
-
post oak (Quercus stellata), tree
-
northern red oak (Quercus rubra), tree
-
black oak (Quercus velutina), tree
-
black hickory (Carya texana), tree
-
shagbark hickory (Carya ovata), tree
-
mockernut hickory (Carya tomentosa), tree
-
scarlet oak (Quercus coccinea), tree
-
blackjack oak (Quercus marilandica), tree
-
shortleaf pine (Pinus echinata), tree
-
farkleberry (Vaccinium arboreum), tree
-
fragrant sumac (Rhus aromatica), shrub
-
winged elm (Ulmus alata), shrub
-
Carolina rose (Rosa carolina), shrub
-
Blue Ridge blueberry (Vaccinium pallidum), shrub
-
St. Andrew's cross (Hypericum hypericoides), shrub
-
common serviceberry (Amelanchier arborea), shrub
-
flowering dogwood (Cornus florida), shrub
-
little bluestem (Schizachyrium scoparium), grass
-
poverty oatgrass (Danthonia spicata), grass
-
rock muhly (Muhlenbergia sobolifera), grass
-
whitetinge sedge (Carex albicans), grass
-
Indiangrass (Sorghastrum nutans), grass
-
big bluestem (Andropogon gerardii), grass
-
slimleaf panicgrass (Dichanthelium linearifolium), grass
-
cypress panicgrass (Dichanthelium dichotomum), grass
-
ribbed sedge (Carex virescens), grass
-
fuzzy wuzzy sedge (Carex hirsutella), grass
-
blue sedge (Carex glaucodea), grass
-
nakedflower ticktrefoil (Desmodium nudiflorum), other herbaceous
-
shrubby lespedeza (Lespedeza frutescens), other herbaceous
-
birdfoot violet (Viola pedata), other herbaceous
-
elmleaf goldenrod (Solidago ulmifolia), other herbaceous
-
downy ragged goldenrod (Solidago petiolaris), other herbaceous
-
perplexed ticktrefoil (Desmodium perplexum), other herbaceous
-
hairy sunflower (Helianthus hirsutus), other herbaceous
-
smooth violet prairie aster (Symphyotrichum turbinellum), other herbaceous
-
wild quinine (Parthenium integrifolium), other herbaceous
-
stiff tickseed (Coreopsis palmata), other herbaceous
Community 1.1
Post Oak-Northern Red Oak/Aromatic Sumac/Poverty Oat Grass-Little Bluestem
This phase has scattered post oak and northern red oak with little bluestem and poverty oat grass dominating the dense ground layer. Numerous forbs are also present and locally abundant.
Forest overstory. Post oak and northern red oak are typical overstory species. Other oak species and hickories are also usually present. Canopy cover can range from 30 percent to nearly 70 percent.
Forest understory. Little bluestem and poverty oat grass dominate the dense ground layer. Numerous forbs are also present and locally abundant.
Table 5. Soil surface cover
| Tree basal cover | 1-2% |
|---|---|
| Shrub/vine/liana basal cover | 0-1% |
| Grass/grasslike basal cover | 0.1-1.0% |
| Forb basal cover | 0.1-1.0% |
| Non-vascular plants | 0-1% |
| Biological crusts | 0% |
| Litter | 60-80% |
| Surface fragments >0.25" and <=3" | 0-2% |
| Surface fragments >3" | 0-2% |
| Bedrock | 0-5% |
| Water | 0% |
| Bare ground | 0-5% |
Table 6. Woody ground cover
| Downed wood, fine-small (<0.40" diameter; 1-hour fuels) | 0-1% |
|---|---|
| Downed wood, fine-medium (0.40-0.99" diameter; 10-hour fuels) | 0-1% |
| Downed wood, fine-large (1.00-2.99" diameter; 100-hour fuels) | 0-1% |
| Downed wood, coarse-small (3.00-8.99" diameter; 1,000-hour fuels) | 0-2% |
| Downed wood, coarse-large (>9.00" diameter; 10,000-hour fuels) | 0-1% |
| Tree snags** (hard***) | – |
| Tree snags** (soft***) | – |
| Tree snag count** (hard***) | 0-2 per acre |
| Tree snag count** (hard***) | 0-2 per acre |
* Decomposition Classes: N - no or little integration with the soil surface; I - partial to nearly full integration with the soil surface.
** >10.16cm diameter at 1.3716m above ground and >1.8288m height--if less diameter OR height use applicable down wood type; for pinyon and juniper, use 0.3048m above ground.
*** Hard - tree is dead with most or all of bark intact; Soft - most of bark has sloughed off.
Table 7. Canopy structure (% cover)
| Height Above Ground (ft) | Tree | Shrub/Vine | Grass/ Grasslike |
Forb |
|---|---|---|---|---|
| <0.5 | – | – | – | – |
| >0.5 <= 1 | – | – | – | 0-5% |
| >1 <= 2 | – | 5-10% | 5-10% | 5-20% |
| >2 <= 4.5 | 0-5% | 10-30% | 20-60% | 10-40% |
| >4.5 <= 13 | 0-5% | – | – | – |
| >13 <= 40 | 20-60% | – | – | – |
| >40 <= 80 | – | – | – | – |
| >80 <= 120 | – | – | – | – |
| >120 | – | – | – | – |
Community 1.2
Post Oak-Northern Red Oak/Eastern Redcedar-Oak and Hickory Saplings/Poverty Oat Grass
This phase is similar to community phase 1.1, but oak and hickory species are increasing due to longer periods of fire suppression. Some displacement of some grasses and forbs may be occurring due to shading and competition from the increased densities of oaks and hickories.
Forest overstory. Post oak and northern red oak are typical overstory species. Other oak species and hickories are also usually present. Canopy cover can range from 50% to nearly 80%.
Forest understory. Poverty oat grass is the dominate grass. Numerous forbs and other grasses are also present and locally abundant. Shrubs and oak and hickory saplings are increasing.
Table 8. Soil surface cover
| Tree basal cover | 1-2% |
|---|---|
| Shrub/vine/liana basal cover | 0-1% |
| Grass/grasslike basal cover | 0.1-1.0% |
| Forb basal cover | 0.1-1.0% |
| Non-vascular plants | 0-1% |
| Biological crusts | 0% |
| Litter | 60-80% |
| Surface fragments >0.25" and <=3" | 0-1% |
| Surface fragments >3" | 0-1% |
| Bedrock | 0-5% |
| Water | 0% |
| Bare ground | 0-5% |
Table 9. Woody ground cover
| Downed wood, fine-small (<0.40" diameter; 1-hour fuels) | 0-1% |
|---|---|
| Downed wood, fine-medium (0.40-0.99" diameter; 10-hour fuels) | 0-1% |
| Downed wood, fine-large (1.00-2.99" diameter; 100-hour fuels) | 0-1% |
| Downed wood, coarse-small (3.00-8.99" diameter; 1,000-hour fuels) | 0-2% |
| Downed wood, coarse-large (>9.00" diameter; 10,000-hour fuels) | 0-1% |
| Tree snags** (hard***) | – |
| Tree snags** (soft***) | – |
| Tree snag count** (hard***) | 0-2 per acre |
| Tree snag count** (hard***) | 0-2 per acre |
* Decomposition Classes: N - no or little integration with the soil surface; I - partial to nearly full integration with the soil surface.
** >10.16cm diameter at 1.3716m above ground and >1.8288m height--if less diameter OR height use applicable down wood type; for pinyon and juniper, use 0.3048m above ground.
*** Hard - tree is dead with most or all of bark intact; Soft - most of bark has sloughed off.
Table 10. Canopy structure (% cover)
| Height Above Ground (ft) | Tree | Shrub/Vine | Grass/ Grasslike |
Forb |
|---|---|---|---|---|
| <0.5 | – | – | – | – |
| >0.5 <= 1 | – | – | 0-5% | 5-10% |
| >1 <= 2 | – | 5-10% | 5-20% | 5-10% |
| >2 <= 4.5 | 5-10% | 10-30% | 20-40% | 20-40% |
| >4.5 <= 13 | 5-10% | – | – | – |
| >13 <= 40 | 30-70% | – | – | – |
| >40 <= 80 | – | – | – | – |
| >80 <= 120 | – | – | – | – |
| >120 | – | – | – | – |
Pathway 1.1A
Community 1.1 to 1.2
This pathway results from fire suppression of 10 to 15 years in length. Fire suppression is causing oak and hickory species to increase. Displacement of some grasses and forbs may be occurring due to shading and competition from the increased densities of oaks and hickories.
Pathway 1.2A
Community 1.2 to 1.1
This pathway has increased fire frequencies that is keeping woodlands open, removing the litter, and stimulating the growth and flowering of the grasses and forbs.
Conservation practices
| Prescribed Burning | |
|---|---|
| Upland Wildlife Habitat Management |
State 2
Fire Excluded Mixed-Oak Woodland
This state is dominated by post oak and northern red oak. They can form relatively even-aged stands, dating to when fire suppression became the dominant management characteristic on the site. This stage can occur relatively quickly (10 to 20 years). Canopy closures can approach 80 percent with little or no ground flora. Without active management or long term presence of fire, woody species will encroach into these woodlands. Once established, these woody species can quickly fill the woodland system. Most occurrences of this state today are dense, and shady with a greatly diminished ground flora. Removal of the younger understory, opening the upper canopy, and the application of prescribed fire has proven to be effective management tools. Timber harvesting is very limited on these sites because of the poor quality and tree size. This state is an excellent wildlife site.
Dominant resource concerns
-
Plant productivity and health
-
Plant structure and composition
-
Plant pest pressure
-
Wildfire hazard from biomass accumulation
Community 2.1
Post Oak-Northern Red Oak/Eastern Redcedar-Oak and Hickory Saplings/ Huckleberry
Due to fire exclusion, this phase has higher densities of eastern redcedar, oak and hickory saplings. Grass and forb diversity and ground cover is decreasing. A restoration pathway consists of the removal of eastern redcedar and oak and hickory saplings. Prescribed fire should be reestablished on a periodic basis of every 5 years.
Forest overstory. Post oak and northern red oak are common overstory species. Canopy cover can range from 50 percent to nearly 80 percent.
Forest understory. Eastern redcedar and oak and hickory saplings are increasing in densities. Grass and forb diversity and ground cover is decreasing with increasing canopy cover.
State 3
Fire Excluded-Logged Mixed-Oak Woodland
In the long term absence of fire, woody species have encroached into this woodland state. Once established, these woody species will quickly fill the woodland system. Removal of the younger understory and the application of prescribed fire have proven to be effective management tools. Timber harvesting is very limited on these sites because of the poor quality and tree size. This state, while of limited timber value, has experienced occasional uncontrolled harvesting (high grading) of northern red oak and white oak that has reduced the densities of these species causing an increase in black oak and blackjack oak.
Dominant resource concerns
-
Sheet and rill erosion
-
Plant productivity and health
-
Plant structure and composition
-
Plant pest pressure
-
Wildfire hazard from biomass accumulation
-
Terrestrial habitat for wildlife and invertebrates
Community 3.1
Black Oak-Post Oak/Hickory/Buckbrush
This long-term fire exclusion phase has experienced occasional harvesting (high grading) of northern red oak and post oak that has reduced the densities of these species, causing an increase in black oak, hickories, and blackjack oak. The remaining red oaks and post oaks are generally of lower quality. A restoration pathway results in the removal of eastern redcedar, black oak and buckbrush. Post oak and northern red oak species are favored to be retained. Prescribed fire is reestablished on a periodic basis of every 5 years. This restoration time may take 20 to 30 years before a reference community is reestablished.
Forest overstory. Northern red oak and post oak have reduced densities, with an increase in black oak, hickories, and blackjack oak.
Forest understory. Repeated unmanaged harvesting allows an increase in buckbrush and a decrease in forbs and grasses.
Transition 1A
State 1 to 2
This transition is the result of fire suppression that exceeds 20 years.
Transition 1B
State 1 to 3
This transition is the result of fire suppression that exceeds 20 years and periodic indiscriminant logging of the higher quality oaks.
Restoration pathway 2A
State 2 to 1
This restoration pathway results in the removal of eastern redcedar and oak and hickory saplings. Prescribed fire is reestablished on a periodic basis of every 5 years.
Conservation practices
| Prescribed Burning | |
|---|---|
| Restoration and Management of Rare and Declining Habitats | |
| Forest Stand Improvement |
Restoration pathway 3A
State 3 to 1
This restoration pathway results in the removal of eastern redcedar, black oak, and buckbrush. Post oak and northern red oak species are favored to be retained. Prescribed fire is reestablished on a periodic basis of every 5 years. This restoration time may take 20 to 30 years before a reference community is reestablished.
Conservation practices
| Brush Management | |
|---|---|
| Prescribed Burning | |
| Restoration and Management of Rare and Declining Habitats | |
| Forest Stand Improvement |
Transition 3A
State 3 to 2
This transition is the result of cessation of periodic indiscriminate logging operations.
Additional community tables
Table 11. Community 1.1 forest overstory composition
| Common name | Symbol | Scientific name | Nativity | Height (ft) | Canopy cover (%) | Diameter (in) | Basal area (square ft/acre) |
|---|---|---|---|---|---|---|---|
|
Tree
|
|||||||
| post oak | QUST | Quercus stellata | Native | 24–40 | 20–40 | 5–15 | – |
| northern red oak | QURU | Quercus rubra | Native | 30–50 | 10–30 | 5–25 | – |
| black hickory | CATE9 | Carya texana | Native | 24–40 | 10–20 | 11–13 | – |
| shortleaf pine | PIEC2 | Pinus echinata | Native | 30–50 | 5–20 | – | – |
| shagbark hickory | CAOV2 | Carya ovata | Native | 24–40 | 5–20 | 5–9 | – |
| blackjack oak | QUMA3 | Quercus marilandica | Native | 15–30 | 5–20 | – | – |
| black oak | QUVE | Quercus velutina | Native | 30–50 | 5–20 | – | – |
| white oak | QUAL | Quercus alba | – | 20–40 | 1–10 | 11–15 | – |
| eastern redcedar | JUVI | Juniperus virginiana | Native | 2–30 | 0–5 | – | – |
Table 12. Community 1.1 forest understory composition
| Common name | Symbol | Scientific name | Nativity | Height (ft) | Canopy cover (%) | |
|---|---|---|---|---|---|---|
|
Grass/grass-like (Graminoids)
|
||||||
| little bluestem | SCSC | Schizachyrium scoparium | Native | 0.1–3 | 10–20 | |
| fuzzy wuzzy sedge | CAHI6 | Carex hirsutella | Native | 0.1–2 | 5–10 | |
| poverty oatgrass | DASP2 | Danthonia spicata | Native | 0.1–2 | 5–10 | |
| rock muhly | MUSO | Muhlenbergia sobolifera | Native | 0.1–2 | 5–10 | |
| whitetinge sedge | CAAL25 | Carex albicans | Native | 0.1–2 | 5–10 | |
| ribbed sedge | CAVI4 | Carex virescens | Native | 0.1–2 | 5–10 | |
|
Forb/Herb
|
||||||
| downy ragged goldenrod | SOPE | Solidago petiolaris | Native | 0.1–3 | 5–10 | |
| perplexed ticktrefoil | DEPE80 | Desmodium perplexum | Native | 0.1–2 | 5–10 | |
| manyray aster | SYAN2 | Symphyotrichum anomalum | Native | 0.3–3 | 5–10 | |
| trailing lespedeza | LEPR | Lespedeza procumbens | Native | 0.1–0.3 | 5–10 | |
| St. Andrew's cross | HYHY | Hypericum hypericoides | Native | 0.5–3 | 5–10 | |
| skyblue aster | SYOO | Symphyotrichum oolentangiense | Native | 0.5–2 | 5–10 | |
| hairy sunflower | HEHI2 | Helianthus hirsutus | Native | 0.1–2 | 5–10 | |
| shrubby lespedeza | LEFR5 | Lespedeza frutescens | Native | 0.1–1 | 5–10 | |
| birdfoot violet | VIPE | Viola pedata | Native | 0.1–0.3 | 5–10 | |
| elmleaf goldenrod | SOUL2 | Solidago ulmifolia | Native | 0.1–2 | 5–10 | |
| licorice bedstraw | GACI2 | Galium circaezans | Native | 0.1–0.2 | 5–10 | |
| stiff tickseed | COPA10 | Coreopsis palmata | Native | 0.1–0.5 | 5–10 | |
| wild quinine | PAIN3 | Parthenium integrifolium | Native | 0.1–3 | 5–10 | |
|
Shrub/Subshrub
|
||||||
| fragrant sumac | RHAR4 | Rhus aromatica | Native | 0.5–5 | 10–30 | |
| winged elm | ULAL | Ulmus alata | Native | 2–6 | 5–20 | |
| lowbush blueberry | VAAN | Vaccinium angustifolium | Native | 0.3–3 | 5–20 | |
| nakedflower ticktrefoil | DENU4 | Desmodium nudiflorum | Native | 0.5–1 | 5–10 | |
|
Tree
|
||||||
| common serviceberry | AMAR3 | Amelanchier arborea | Native | 5–10 | 0–5 | |
| sassafras | SAAL5 | Sassafras albidum | Native | 5–10 | 0–5 | |
Table 13. Community 1.2 forest overstory composition
| Common name | Symbol | Scientific name | Nativity | Height (ft) | Canopy cover (%) | Diameter (in) | Basal area (square ft/acre) |
|---|---|---|---|---|---|---|---|
|
Tree
|
|||||||
| post oak | QUST | Quercus stellata | Native | 24–40 | 30–40 | 5–15 | – |
| northern red oak | QURU | Quercus rubra | Native | 30–50 | 20–30 | 5–25 | – |
| shortleaf pine | PIEC2 | Pinus echinata | Native | 30–50 | 5–20 | – | – |
| blackjack oak | QUMA3 | Quercus marilandica | Native | 15–30 | 10–20 | – | – |
| black oak | QUVE | Quercus velutina | Native | 30–50 | 10–20 | – | – |
| shagbark hickory | CAOV2 | Carya ovata | Native | 24–40 | 10–20 | 5–9 | – |
| black hickory | CATE9 | Carya texana | Native | 24–40 | 10–20 | 11–13 | – |
| eastern redcedar | JUVI | Juniperus virginiana | Native | 2–30 | 5–10 | – | – |
| white oak | QUAL | Quercus alba | Native | 20–40 | 1–10 | 11–15 | – |
Table 14. Community 1.2 forest understory composition
| Common name | Symbol | Scientific name | Nativity | Height (ft) | Canopy cover (%) | |
|---|---|---|---|---|---|---|
|
Grass/grass-like (Graminoids)
|
||||||
| poverty oatgrass | DASP2 | Danthonia spicata | Native | 0.1–2 | 10–20 | |
| whitetinge sedge | CAAL25 | Carex albicans | Native | 0.1–2 | 5–10 | |
| fuzzy wuzzy sedge | CAHI6 | Carex hirsutella | Native | 0.1–2 | 5–10 | |
| ribbed sedge | CAVI4 | Carex virescens | Native | 0.1–2 | 5–10 | |
| rock muhly | MUSO | Muhlenbergia sobolifera | Native | 0.1–2 | 5–10 | |
| little bluestem | SCSC | Schizachyrium scoparium | Native | 0.1–3 | 5–10 | |
|
Forb/Herb
|
||||||
| trailing lespedeza | LEPR | Lespedeza procumbens | Native | 0.1–0.3 | 5–10 | |
| wild quinine | PAIN3 | Parthenium integrifolium | Native | 0.1–3 | 5–10 | |
| downy ragged goldenrod | SOPE | Solidago petiolaris | Native | 0.1–3 | 5–10 | |
| elmleaf goldenrod | SOUL2 | Solidago ulmifolia | Native | 0.1–2 | 5–10 | |
| manyray aster | SYAN2 | Symphyotrichum anomalum | Native | 0.1–3 | 5–10 | |
| skyblue aster | SYOO | Symphyotrichum oolentangiense | Native | 0.1–2 | 5–10 | |
| stiff tickseed | COPA10 | Coreopsis palmata | Native | 0.1–0.5 | 5–10 | |
| perplexed ticktrefoil | DEPE80 | Desmodium perplexum | Native | 0.1–2 | 5–10 | |
| licorice bedstraw | GACI2 | Galium circaezans | Native | 0.1–0.2 | 5–10 | |
| hairy sunflower | HEHI2 | Helianthus hirsutus | Native | 0.1–2 | 5–10 | |
| St. Andrew's cross | HYHY | Hypericum hypericoides | Native | 0.5–3 | 5–10 | |
| shrubby lespedeza | LEFR5 | Lespedeza frutescens | Native | 0.1–1 | 5–10 | |
| birdfoot violet | VIPE | Viola pedata | Native | 0.1–0.3 | 5–10 | |
| nakedflower ticktrefoil | DENU4 | Desmodium nudiflorum | Native | 0.5–1 | 5–10 | |
|
Shrub/Subshrub
|
||||||
| fragrant sumac | RHAR4 | Rhus aromatica | Native | 1–5 | 15–30 | |
| winged elm | ULAL | Ulmus alata | Native | 2–6 | 10–20 | |
| lowbush blueberry | VAAN | Vaccinium angustifolium | Native | 0.5–3 | 10–20 | |
|
Tree
|
||||||
| black hickory | CATE9 | Carya texana | Native | 5–10 | 5–10 | |
| eastern redcedar | JUVI | Juniperus virginiana | Native | 0.2–10 | 5–10 | |
| blackjack oak | QUMA3 | Quercus marilandica | Native | 5–10 | 5–10 | |
| black oak | QUVE | Quercus velutina | Native | 5–10 | 5–10 | |
| sassafras | SAAL5 | Sassafras albidum | Native | 5–10 | 5–10 | |
| common serviceberry | AMAR3 | Amelanchier arborea | Native | 5–10 | 5–10 | |
Interpretations
Animal community
Wildlife (MDC, 2006):
Wildlife habitat: Oaks on this site provide abundant hard mast; scattered shrubs provide soft mast; native legumes provide high-quality wildlife food.
Sedges and native cool-season grasses provide green browse; native warm-season grasses provide cover and nesting habitat; and a diversity of forbs provides a diversity and abundance of insects.
Post-burn areas can provide temporary bare-ground and herbaceous cover habitat is important for turkey poults and quail chicks.
Birds species associated with this site are Indigo Bunting, Red-headed Woodpecker, Eastern Bluebird, Northern Bobwhite, Summer Tanager, Eastern Wood-Pewee, Whip-poor-will, Chuck-will’s widow, and Red-eyed Vireo.
Reptiles and amphibians associated with this ecological site include ornate box turtle, northern fence lizard, five-lined skink, coal skink, broad-headed skink, six-lined racerunner, western slender glass lizard, prairie ring-necked snake, flat-headed snake, rough earth snake, red milk snake, western pygmy rattlesnake, and timber rattlesnake.
Domestic livestock:
Currently, domestic cattle grazing is absent or very limited on these sites due to lack of water, access issues, and high amounts of acorns on the ground in the fall that are detrimental to cattle.
Hydrological functions
The water features of this upland ecological site include evapotranspiration, surface runoff, and drainage. Each water balance component fluctuates to varying extents from year-to-year. Evapotranspiration remains the most constant. Precipitation and drainage are highly variable between years. Seasonal variability differs for each water component. Precipitation generally occurs as single day events. Evapotranspiration is lowest in the winter and peaks in the summer. Water stored as ice and snow decreases drainage and surface runoff rates throughout the winter and increases these fluxes in the spring. The surface runoff pulse is greatly influenced by extreme events. Conversion to cropland or other high intensities land uses tends to increase runoff, but also decreases evapotranspiration. Depending on the situation, this might increase groundwater discharge, and decrease baseflow in receiving streams.
Recreational uses
Hunting, bird watching, horseback riding, camping, and hiking are recreational uses of this ecological site. Reference and well managed sites provide good hunting for turkey, white-tailed deer, and squirrel. Recreational uses are reduced in the highgraded state.
Wood products
This ecological site is not productive but some managed, limited harvesting can occur. Care must be taken to maintain the integrity and character of the site.
Potential wood products include lower grade lumber and pallet materials.
Management: Field measured site index values averaged 47 for black oak and 52 for shortleaf pine (NRCS, 2014). Timber management opportunities are fair. Create group openings of at least 2 acres. Large clearcuts should be minimized if possible to reduce impacts on wildlife and aesthetics. This site responds well to fire. Using prescribed fire can be an effective management tool.
Limitations: Large amounts of coarse fragments throughout profile; bedrock may be within 60 inches. Surface stones and rocks are problems for efficient and safe equipment operation and will make equipment use somewhat difficult. Disturbing the surface excessively in harvesting operations and building roads increases soil losses, which leaves a greater amount of coarse fragments on the surface. Hand planting or direct seeding may be necessary. Seedling mortality due to low available water capacity may be high. Mechanical tree planting will be limited. Erosion is a hazard when slopes exceed 15 percent. On steep slopes greater than 35 percent, traction problems increase and equipment use is not recommended (NRCS, 2002).
Other products
Additional opportunities exist in the reference and well managed woodland states for possible agroforestry wild crafting activities, such as harvesting spring and summer florals and native blueberries.
Other information
Historically, black bears were common across the area. Their reduced numbers were directly correlated with the westward expansion of the European settlers and uncontrolled hunting. Like other mobile animals in the area, bears would have used multiple ecological sites. Other predators like the mountain lion and wolf have also disappeared from these sites in a similar manner. Today sightings of black bears and mountain lions are increasing due a natural migration of these species from other states and regions.
Table 15. Representative site productivity
Supporting information
Inventory data references
The data contained in this document is derived from analysis of inventories, ecological interpretation from field evaluations, and various reference papers and books.
Nelson, Paul W. 2010. The Terrestrial Natural Communities of Missouri. Missouri Department of Conservation, Jefferson City, Missouri.
Yatskievych, George A. 1999/2006/2013. Flora of Missouri. Missouri Department of Conservation in cooperation with Missouri Botanical Garden Press, Volumes 1-3.
Sampling methods (nested plots/transects/relevee)
Reference Inventory Plots:
BUMOCA03 Buford Mountain CA; Irondale
PERACA05 Peck Ranch CA; Knobtop
RUMOCA01 Russell Mountain CA; Irondale
Level 2 and reconnaissance inventory:
2003: Nigh/Meinert-Initial reconnaissance/Mapping. Three weeks of recon on numerous 116C mountains.
2007: Reconnaissance plots on Stegall Mountain and Taum Sauk.
2012: Field stops on igneous sites during the Central States Forest Soils Workshop.
2013: Reconnaissance on numerous mountains working on reference plots. Taum Sauk, Hughes, Peck Ranch, Russel Mountain, Johnson Shut-Ins, Mill Mountain NA, Buford
Type locality
| Location 1: Iron County, MO | |
|---|---|
| Township/Range/Section | T35N R3E S34 |
| UTM zone | N |
| UTM northing | 4174905 |
| UTM easting | 703390 |
| Latitude | 37° 41′ 55″ |
| Longitude | -90° 41′ 34″ |
| General legal description | Dry Igneous Upland Woodland at Buford Mountain Conservation Area. |
| Location 2: Carter County, MO | |
| Township/Range/Section | T28N R2W S19 |
| UTM zone | N |
| UTM northing | 4104426 |
| UTM easting | 659528 |
| Latitude | 37° 4′ 21″ |
| Longitude | -91° 12′ 19″ |
| General legal description | Dry Igneous Upland Woodland on Stegall Mountain at Peck Ranch Conservation Area. |
| Location 3: Iron County, MO | |
| Township/Range/Section | T33N R3E S3 |
| UTM zone | N |
| UTM northing | 4160455 |
| UTM easting | 703204 |
| Latitude | 37° 34′ 7″ |
| Longitude | -90° 41′ 56″ |
| General legal description | Dry Igneous Upland Woodland at Russell Mountain Conservation Area. |
Other references
Batek, M.J., A.J. Rebertus, W.A. Schroeder, T.L. Haithcoat, E. Compas, and R.P. Guyette. 1999. Reconstruction of early nineteenth-century vegetation and fire regimes in the Missouri Ozarks. Journal of Biogeography 26:397-412.
Conant, R. T., K. Paustian, and E. T. Elliott. 2001. Grassland management and conversion
into grassland: effects on soil carbon. Ecological Applications, 11(2). pp. 343–355
Frost, C., Pre-settlement Fire Frequency Regimes of the United States: A First Approximation. Pages 70-81, May 1996., Proceedings of the 20nd Tall Timbers Fire Ecology Conference: Fire in Ecosystem Management: Shifting the Paradigm from Suppression to Prescription. Tall Timbers Research Station, Tallahassee, FL.
Guyette, R.P. and B.E. Cutter. 1991. Tree-ring analysis of fire history of a post oak savanna in the Missouri Ozarks. Natural Areas Journal 11: 93-99.
Ladd, D. 1991. Reexamination of the role of fire in Missouri oak woodlands. Pp. 67-80 in G.V. Brown, James K.; Smith, Jane Kapler, eds. 2000. 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. 257 p.
Missouri Natural Heritage Inventory Database. 2013. Woodland element occurrence records. Missouri Department of Conservation. Jefferson City, Missouri.
Missouri Department of Conservation, 2006. Missouri Forest and Woodland Community Profiles. Jefferson City, Missouri.
National Vegetation Classification System Vegetation Association. 2010. http://www.natureserve.org/prodServices/ecomapping.jsp
Natural Resources Conservation Service. 2002. Woodland Suitability Groups. Missouri FOTG, Section II, Soil Interpretations and Reports. 30 pgs.
Natural Resources Conservation Service. Site Index Reports. Accessed May 2014. https://esi.sc.egov.usda.gov/ESI_Forestland/pgFSWelcome.aspx
Nelson, P. W. 2010. The Terrestrial Natural Communities of Missouri. Missouri Department of Conservation, Jefferson City, Missouri. 550p.
Nigh, T. A., and W. A. Schroeder. 2002. Atlas of Missouri Ecoregions. Missouri Department of Conservation, Jefferson City, Missouri. 212p.
Simmons, M., J. D. Childress, K. Godsey, & R. Taylor. 2006. Soil Survey of Reynolds County, Missouri. U.S. Dept. of Agric. Natural Resources Conservation Service.
United States Department of Agriculture, Natural Resources Conservation Service. 2006. Land Resource Regions and Major Land Resource Areas of the United States, the Caribbean, and the Pacific Basin. U.S. Department of Agriculture Handbook 296.
University of Missouri Climate Center - http://climate.missouri.edu/climate.php
Contributors
Doug Wallace
Fred Young
Acknowledgments
Missouri Department of Conservation and Missouri Department of Natural Resources personnel provided significant and helpful field and technical support in the development of this ecological site.
Rangeland health reference sheet
Interpreting Indicators of Rangeland Health is a qualitative assessment protocol used to determine ecosystem condition based on benchmark characteristics described in the Reference Sheet. A suite of 17 (or more) indicators are typically considered in an assessment. The ecological site(s) representative of an assessment location must be known prior to applying the protocol and must be verified based on soils and climate. Current plant community cannot be used to identify the ecological site.
| Author(s)/participant(s) | |
|---|---|
| Contact for lead author | |
| Date | 09/08/2022 |
| Approved by | Nels Barrett |
| Approval date | |
| Composition (Indicators 10 and 12) based on | Annual Production |
Indicators
-
Number and extent of rills:
-
Presence of water flow patterns:
-
Number and height of erosional pedestals or terracettes:
-
Bare ground from Ecological Site Description or other studies (rock, litter, lichen, moss, plant canopy are not bare ground):
-
Number of gullies and erosion associated with gullies:
-
Extent of wind scoured, blowouts and/or depositional areas:
-
Amount of litter movement (describe size and distance expected to travel):
-
Soil surface (top few mm) resistance to erosion (stability values are averages - most sites will show a range of values):
-
Soil surface structure and SOM content (include type of structure and A-horizon color and thickness):
-
Effect of community phase composition (relative proportion of different functional groups) and spatial distribution on infiltration and runoff:
-
Presence and thickness of compaction layer (usually none; describe soil profile features which may be mistaken for compaction on this site):
-
Functional/Structural Groups (list in order of descending dominance by above-ground annual-production or live foliar cover using symbols: >>, >, = to indicate much greater than, greater than, and equal to):
Dominant:
Sub-dominant:
Other:
Additional:
-
Amount of plant mortality and decadence (include which functional groups are expected to show mortality or decadence):
-
Average percent litter cover (%) and depth ( in):
-
Expected annual annual-production (this is TOTAL above-ground annual-production, not just forage annual-production):
-
Potential invasive (including noxious) species (native and non-native). List species which BOTH characterize degraded states and have the potential to become a dominant or co-dominant species on the ecological site if their future establishment and growth is not actively controlled by management interventions. Species that become dominant for only one to several years (e.g., short-term response to drought or wildfire) are not invasive plants. Note that unlike other indicators, we are describing what is NOT expected in the reference state for the ecological site:
-
Perennial plant reproductive capability:
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