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Ecological site R105XY010WI

Shallow Mollic Loamy-Silty Upland

Last updated: 2/23/2024
Accessed: 11/23/2024

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General information

Provisional. A provisional ecological site description has undergone quality control and quality assurance review. It contains a working state and transition model and enough information to identify the ecological site.

MLRA notes

Major Land Resource Area (MLRA): 105X–Upper Mississippi River Bedrock Controlled Uplands and Valleys

The Northern Mississippi Valley Loess Hills area corresponds closely to the Western Coulees and Ridges and Southwest Savanna Ecological Landscapes. Some of the following brief overview is borrowed from the Wisconsin Department of Natural Resources Ecological Landscape publication (2015).

Fifty-two percent of the Upper Mississippi River Bedrock Controlled Uplands and Valleys MLRA is in Wisconsin; Iowa, Minnesota, and Illinois contain the rest. This region is the only area in Wisconsin that has not been covered by glaciers within the past 2.4 million years. The Wisconsin portion of this MLRA is approximately 7.4 million acres (11,600 square miles). The landscape is characterized by dissected topography with deeply-incised, steep-walled valleys between bedrock controlled ridges.

Though it’s called the “Driftless Region”, some glacial drift is found in the major river valleys of this region in the form of outwash, deposited by proglacial streams of glacial meltwater. Wisconsin’s most recent glaciations also impacted the sediment of the area through the deposition of loess. After the glacier receded and before vegetation established, the bare surfaces of the glaciated areas were highly susceptible to wind erosion. As a result, a veneer of loess (wind-blown silt) was deposited over the entire region. The thickest deposits—nearly five meters—are on ridges near the Mississippi River and gradually thin moving eastward. The loess caps in Dane and Green counties are generally 0.5-1.5 meters deep. Much of the loess has eroded downslope and collected in floodplains.

Bedrock is shallow throughout this MLRA and is a major influence on topography and hydrology. Most of the MLRA has bedrock within two meters, except in the deep river valleys that are filled with outwash and alluvium materials. Sandstone is the dominant bedrock type in MLRA 105, but the southernmost portion is dominated by dolomite. Military Ridge is an escarpment that straddles the boundary between sandstone and dolomite bedrock. The sandstone north of the ridge is weaker than the erosion-resistant dolomite south of the ridge. The sandstone is deeply cut and dissected into steep slopes and valleys. The dolomite-controlled ridges tend to be less dissected and broader with more gentle, south sloping topography. Geomorphic and fluvial processes formed these landscapes by way of sheet wash, soil creep, and flowage. These processes eroded the hillslopes, cut into bedrock, and transported the debris to streams, forming floodplains and terraces.

Underfit streams are common in MLRA 105, especially in the southern portion. These streams currently occupy large river valleys—especially those of the Black, Chippewa, Mississippi, and Wisconsin Rivers—that were carved by proglacial meltwater streams carrying much larger quantities of water than what’s present today. As the climate dried, waterflow decreased and the valleys filled with alluvial sediment. Narrow meanders were formed by the shrinking streams and are often dissimilar to the meanders of the larger valleys they occupy. Fluvial landforms – including terraces, oxbow lakes, sandbars, eroding bluffs, and large floodplain complexes – are found within these large valleys and are subject to varying flooding frequencies, intensities, and durations.
Karst topography formed in this region from dissolution of carbonate bedrock by surface and groundwater. Dolomite and limestone are more easily affected by dissolution, but karst topography also formed in sandstone. Erosion by water (stream meanders, rain/runoff, and groundwater), wind, and frost weaken joints and bedding planes that can cause collapse. In addition, sandstone materials collapse into cavities in underlying dolomite or limestone.

Historically, MLRA 105 was dominated by oak forests and oak openings making up more than 50% of the area. Prairies were significant and covered 32% of the area south of Military Ridge. Maple-basswood forests covered 19% of the are north of Military Ridge. Dominant tree species were white oak (Quercus alba), bur oak (Quercus macrocarpa), black oak (Quercus velutina), and sugar maple (Acer saccharum).

Classification relationships

Relationship to Established Framework and Classification Systems:

Habitat Types of S. Wisconsin (Kotar, 1996): This ES most likely keys to habitat types of Acer saccharum-Tilia/Cornus racemose(Arismaea) [ATiCr(As)], Acer saccharum-Tilia/Desmodium [ATiDe], Acer saccharum-Tilia/Arismaea(Desmodium) [ATiAs(De)], Acer saccharum-Acer rubrum/Viburnum [AArVb], and Pinus strobus/Vaccinium-Hammamelis [PVHa] due to its similarity to Shallow Loamy-Silty Upland.

Biophysical Settings (Landfire, 2014): This ES is largely mapped as North-Central Interior Dry-Mesic Oak Forest and Woodland, North-Central Interior Maple-Basswood Forest, Eastern Cool Temperate Pasture and Hayland, Eastern Cool Temperate Close Grown Crop, Eastern Cool Temperate Wheat, and Eastern Cool Temperate Row Crop

WDNR Natural Communities (WDNR, 2015): This ES is most similar to Mesic Prairie as described by the Wisconsin DNR.

Hierarchical Framework Relationships:

Major Land Resource Area (MLRA): Upper Mississippi River Bedrock Controlled Uplands and Valleys (105)

USFS Subregions: Mississippi-Wisconsin River Ravines (222Lc), Kickapoo-Wisconsin River Ravines (222Ld), Mineral Point Prairie-Savannah (222Le)

Wisconsin DNR Ecological Landscapes: Western Coulee and Ridges, Southwest Savannah

Ecological site concept

The Shallow Mollic Loamy-Silty Upland site occupies approximately 70,000 acres in MLRA 105, or about 1% of the total land area. The site is found on loess hills and steep ridges in upland positions. It is found in the southern half of MLRA 105 where the depth to bedrock is shallow and the loess deposits are thick.

This site is characterized by well drained to somewhat excessively drained, loamy to clayey soils that have contact with dolomite, sandstone, or limestone bedrock within 1 meter of the soil surface. These sites have deep, dark surfaces (mollic epipedons) resulting from long-term additions of organic materials, especially from fine, fibrous roots of grassy vegetation.

Historically, these sites were prairies, though modern fire suppression has resulted in the encroachment by woody species. Today, many sites are forested. The bedrock acts as a root restricting layer and can limit root growth and perch water. These sites may be vulnerable to tree trips.

Associated sites

F105XY008WI	Moist Loamy-Clayey Lowland These sites form in loamy and clayey materials. They are somewhat poorly drained. They are found on similar landforms as Shallow Mollic Loamy-Silty Upland in lower positions on the landform.
R105XY011WI	Mollic Loamy-Silty Upland These sites form in loamy to silty materials, often silty loess and residuum. They have deep, dark surfaces. They are moderately well to somewhat excessively drained. They are often found adjacent to Shallow Mollic Loamy-Silty Upland where bedrock contact is deeper.
F105XY012WI	Shallow Loamy-Silty Upland These sites form in loamy to silty materials, often silty loess and residuum. They have bedrock contact within one meter of the soil surface. They are moderately well to well drained. They may be found adjacent to Shallow Mollic Loamy-Silty Upland.
F105XY013WI	Loamy-Silty Upland These sites form in loamy to silty materials, often silty loess and residuum. They are moderately well to well drained. They are often found adjacent to Shallow Mollic Loamy-Clayey Uplands. They may be found adjacent to Shallow Mollic Loamy-Silty Upland.

Similar sites

F105XY012WI	Shallow Loamy-Silty Upland These sites form in loamy to silty materials, often silty loess and residuum. They have bedrock contact within one meter of the soil surface. They are moderately well to well drained. Like Shallow Mollic Loamy-Silty Upland, they form in weathered bedrock materials, but they have shallower surface horizons of organic-enriched soil (ochric rather than mollic epipedons).
F105XY015WI	Shallow Clayey Upland These sites form in clayey materials, often clayey pedisediment and residuum. They have bedrock contact within one meter of the soil surface. They are moderately well to well drained. Like Shallow Mollic Loamy-Silty Upland, they form in weathered bedrock materials, but have finer textures and shallower surface horizons of organic-enriched soil (ochric rather than mollic epipedons).
R105XY014WI	Mollic Clayey Upland These sites form in clayey materials, often clayey pedisediment and residuum. They have deep, dark surfaces. They are well drained. Like Shallow Mollic Loamy-Silty Upland, they form in weathered bedrock materials and have deep surface horizons of organic-enriched soil (mollic epipedons) but they lack bedrock contact within 3 feet (one meter) of the soil surface.

F105XY012WI

Shallow Loamy-Silty Upland

These sites form in loamy to silty materials, often silty loess and residuum. They have bedrock contact within one meter of the soil surface. They are moderately well to well drained. Like Shallow Mollic Loamy-Silty Upland, they form in weathered bedrock materials, but they have shallower surface horizons of organic-enriched soil (ochric rather than mollic epipedons).

F105XY015WI

Shallow Clayey Upland

These sites form in clayey materials, often clayey pedisediment and residuum. They have bedrock contact within one meter of the soil surface. They are moderately well to well drained. Like Shallow Mollic Loamy-Silty Upland, they form in weathered bedrock materials, but have finer textures and shallower surface horizons of organic-enriched soil (ochric rather than mollic epipedons).

R105XY014WI

Mollic Clayey Upland

These sites form in clayey materials, often clayey pedisediment and residuum. They have deep, dark surfaces. They are well drained. Like Shallow Mollic Loamy-Silty Upland, they form in weathered bedrock materials and have deep surface horizons of organic-enriched soil (mollic epipedons) but they lack bedrock contact within 3 feet (one meter) of the soil surface.

Table 1. Dominant plant species

Tree	Not specified
Shrub	Not specified
Herbaceous	(1) Andropogon gerardii (2) Sorghastrum nutans

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Physiographic features

These sites are found on hills and ridges in the summit, shoulder, or backslope positions. Slope shape is convex or linear. Slopes range from 2 to 60 percent. Elevation of the landform ranges from 705 to 853 feet (215 to 260 meters) above sea level.

These sites are not subject to inundation by water. They generally lack evidence of a seasonally high water table within the soil profile. Runoff potential is medium to very high.

Table 2. Representative physiographic features

Hillslope profile	(1) Summit (2) Shoulder (3) Backslope
Slope shape across	(1) Convex
Slope shape up-down	(1) Linear
Landforms	(1) Hill (2) Ridge
Runoff class	Medium to very high
Flooding frequency	None
Ponding frequency	None
Elevation	705 – 853 ft
Slope	2 – 60%
Water table depth	79 in
Aspect	Aspect is not a significant factor

Climatic features

The climate of the Upper Mississippi River Bedrock Controlled Uplands and Valleys MLRA is typical of southern Wisconsin, with warmer winters, warmer summers, and higher precipitation rates than MLRA in northern Wisconsin. The MLRA stretches over about 2.9 degrees of latitude, or nearly 200 miles, from its northern tip in Barron county to its southern Wisconsin extent on the border of Illinois. This results in considerable variation in climate throughout the MLRA. The growing season ranges from 117 to 181 growing degree days, with longer growing seasons in the southern portion.

The average annual precipitation for this ecological site is 36 inches. The average annual snowfall is 39 inches. The annual average maximum and minimum temperatures are 56°F and 36°F, respectively.

Table 3. Representative climatic features

Frost-free period (characteristic range)	121-137 days
Freeze-free period (characteristic range)	149-164 days
Precipitation total (characteristic range)	35-37 in
Frost-free period (actual range)	118-138 days
Freeze-free period (actual range)	146-165 days
Precipitation total (actual range)	35-38 in
Frost-free period (average)	127 days
Freeze-free period (average)	157 days
Precipitation total (average)	36 in

Characteristic range

Actual range

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Figure 1. Monthly precipitation range

Characteristic range

Actual range

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Figure 2. Monthly minimum temperature range

Characteristic range

Actual range

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Figure 3. Monthly maximum temperature range

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Figure 4. Monthly average minimum and maximum temperature

Figure 5. Annual precipitation pattern

Figure 6. Annual average temperature pattern

Climate stations used

(1) GAYS MILLS [USC00473022], Gays Mills, WI
(2) PRAIRIE DU CHIEN [USC00476827], Prairie du Chien, WI
(3) MAZOMANIE [USC00475189], Mazomanie, WI
(4) LANCASTER 4 WSW [USC00474546], Bloomington, WI
(5) PLATTEVILLE [USC00476646], Platteville, WI
(6) DARLINGTON [USC00472001], Darlington, WI

Influencing water features

Water is received through precipitation, runoff from adjacent uplands, and groundwater discharge. Water levels are greatly influenced by precipitation rates and runoff from upland sites. Water is lost from the site primarily through runoff, evapotranspiration, and groundwater recharge.

Permeability of the soils is very slow to moderately slow. The hydrologic group for these sites is D.

Wetland description

Not Applicable.

Soil features

This site is represented by the Elizabeth and Sogn soil series. These soils are Lithic Hapludalfs.

These soils formed in loess and loamy residuum weathered from dolomite. They have contact with the underlying bedrock within 39 inches (100 cm) of the soil surface. Subsurface fragments smaller than 3 inches in diameter (gravel) may occupy up to 10 percent volume. Larger subsurface fragments may occupy up to 55 percent volume. These fragments are composed of dolomite weathered from the bedrock.

These soils have rick, dark surface horizons rich in base-forming cations (mollic epipedons). They are neutral to slightly alkaline and will generally have accumulations of secondary carbonates. They are well drained to somewhat excessively drained. They do not meet hydric soil requirements.

Figure 7. Sogn soil series sampled on 07/29/2020 in Iowa County, WI.

Table 4. Representative soil features

Parent material	(1) Loess (2) Residuum (3) Pedisediment
Surface texture	(1) Silt loam (2) Loam
Drainage class	Well drained to somewhat excessively drained
Permeability class	Very slow to moderately slow
Soil depth	7 – 39 in
Surface fragment cover <=3"	2%
Surface fragment cover >3"	1%
Available water capacity (0-59.1in)	0.5 – 1.12 in
Calcium carbonate equivalent (0-39.4in)	3 – 20%
Soil reaction (1:1 water) (0-39.4in)	7.3 – 7.8
Subsurface fragment volume <=3" (0-39.4in)	3 – 10%
Subsurface fragment volume >3" (0-39.4in)	3 – 55%

Ecological dynamics

In pre-European settlement time wildfire was the main controlling factor of range and forest community dynamics. Some areas had been persistent in grasslands, but had the capacity to support both grassland and forest depending on the frequency and intensity of fire and the presence of large grazers. Shorter fire return intervals led to grasslands, intermediate fire return intervals to scrub, and long fire return intervals to forest. Any scrub or forest community was dependent on the presence of adjacent seed source. Many of the previous grasslands have been converted to agriculture or have reverted to forest following fire suppression.

Forest communities can be described thusly, following a severe, stand-replacing fire, any of the species present on the landscape could become established, depending on seed source availability and specific conditions of post-fire seedbed. The newly established young stands of any species were easily eliminated by recurring fires, but differences in fire-resisting properties among the species began to play a role in any species’ survival success. Many pine and oak species were dominant in the region because of their fire-resistant properties and successful regeneration post-fire. With clear cutting and continued fire suppression, many of these species adapted to fire and intolerant of shade are replaced by other species. Species such as white pine and red oak are still common on the landscape based on their tolerance to some shade; these species to establish under a canopy, and in time, may become a component of the canopy. Mesic hardwoods are sensitive to fire, but in its absence, the have the ability to dominate sites based on their shade tolerance and prolific seed production.

Today, these forests most commonly include stands of red oak, white oak, and other mesic hardwoods may be present as well. Some sites have a the likely reference community of sugar maple and basswood with a mixture of ashes. These sites have the conditions to support shade tolerant mesic hardwoods, but historically had significant wind throw and fire disturbance that allowed for a strong presence of oak species. As long as fire is continually suppressed, maples and other mesic hardwoods will continue to dominate the canopy.

State and transition model

More interactive model formats are also available. View Interactive Models
Click on state and transition labels to scroll to the respective text

Ecosystem states

1. Reference State

2. Fire Suppressed Scrub State

3. Stable Forest State

4. Pioneer Forest State

5. Agricultural State

States 2 and 5 (additional transitions)

2. Fire Suppressed Scrub State

5. Agricultural State

T1A	-	Suppression of fire.
R2A	-	Return of fire and/or large grazers to the landscape
T2A	-	Continued fire suppression for over 20 years
T2B	-	Removal of forest/shrub cover and tilling for agricultural crop production.
T3A	-	Cutting, fire, or blowdown removing existing tree canopy
R4A	-	Low intensity moderate return interval fire removing fire intolerant species and regeneration
R4B	-	Deciduous forest community is slowly invaded by conifers.
T5A	-	Removal of forest/shrub cover and tilling for agricultural crop production.

3.1A	-	Light to moderate intensity fires, blow-downs, ice storms.
3.2A	-	Disturbance-free period for 30+ years.

State 4 submodel, plant communities

4.1. Pioneer Forest Community Phase

State 5 submodel, plant communities

5.1. Agricultural Community Phase

State 1
Reference State

The Reference State is a grassland state dominated by big bluestem, but also includes Indian grass, and little bluestem. Leadplant and sunflowers are common. The reference state for this ES is very rare today and was maintained by frequent fire removing the encroachment of tree and shrub species.

Community 1.1
Mesic Prairie Phase

The Wet-Mesic Prairie Phase is a grassland state dominated by tall grasses including big bluestem, Canada blue joint, Sedges and others with a mixture of forbs including goldenrods. This phase is very rare today.

Dominant plant species

big bluestem (Andropogon gerardii), grass
Indiangrass (Sorghastrum nutans), grass
little bluestem (Schizachyrium scoparium), grass
sunflower (Helianthus), other herbaceous
leadplant (Amorpha canescens), other herbaceous

State 2
Fire Suppressed Scrub State

A mostly open grassland with sporadic shrubs and trees. As soon as fire is suppressed tree and shrub species invade this ES and various tree and shrub species may take hold resulting in a grassland with sparse and sporadic tree and shrub cover.

Community 2.1
Fire Suppressed Scrub Phase

Fire Suppressed Scrub is a tree and shrub invaded grassland. The grassland species are similar to the reference state with the addition of various species of tree or shrub beginning to create a sparse canopy.

Dominant plant species

quaking aspen (Populus tremuloides), tree
oak (Quercus), tree
red maple (Acer rubrum), tree
pine (Pinus), tree
big bluestem (Andropogon gerardii), grass
Indiangrass (Sorghastrum nutans), grass
little bluestem (Schizachyrium scoparium), grass
sunflower (Helianthus), other herbaceous

State 3
Stable Forest State

Stable Forest state is a forest community dominated by sugar maple (Acer saccharum) with American basswood (Tilia americana), and a mixture of Ashes (Fraxinus spp.), and Oaks (Quercus spp.). Depending on history of disturbance, two community phases can be distinguished largely by differences in dominance of tree species and community age structure. In some places sugar maple seed source may be missing leading to other dominant canopy species.

Community 3.1
Advanced Succession Community Phase

In the absence of any major disturbance, specifically fire, this community is dominated by sugar maple. Common associates include American basswood, ashes, and oaks. Other species may be present in the canopy as well, including: black cherry, red maple, and shagbark hickory. The shrub layer is typically not well developed in this phase, but is likely to contain regenerating overstory species. The ground layer is often sparse but includes rich site species such as virginia creeper, enchanter’s nightshade, and pointedleaf ticktrefoil.

Dominant plant species

sugar maple (Acer saccharum), tree
American basswood (Tilia americana), tree
currant (Ribes), shrub
black cherry (Prunus serotina), shrub
pointedleaf ticktrefoil (Desmodium glutinosum), other herbaceous
Jack in the pulpit (Arisaema triphyllum), other herbaceous

Community 3.2
Rejuvenated Community Phase

This community is dominated by a mixture of hardwoods including sugar maple, basswood, red oak, white oak, and ashes. Associates may include shagbark hickory, and black cherry. The shrub (often more developed in this phase) and ground layers are similar to the advanced succession phase, but may include the establishment of new seedlings to include more shade intolerant species. This community phase will quickly return to the mature or advanced succession phase with limited disturbance.

Dominant plant species

sugar maple (Acer saccharum), tree
American basswood (Tilia americana), tree
northern red oak (Quercus rubra), tree
white oak (Quercus alba), tree
ash (Fraxinus), tree
currant (Ribes), shrub
black cherry (Prunus serotina), shrub
pointedleaf ticktrefoil (Desmodium glutinosum), other herbaceous
Jack in the pulpit (Arisaema triphyllum), other herbaceous

Pathway 3.1A
Community 3.1 to 3.2

Light intensity fires, crown breakage from ice and snow and small scale blow-downs create canopy openings, allowing gap regeneration of less shade tolerant species such as white ash red oak and others. These species may join the canopy composition.

Pathway 3.2A
Community 3.2 to 3.1

A long period without major canopy disturbance allows gradual replacement of oldest canopy trees by younger cohorts. Lacking a major disturbance, the canopy will likely be replaced primarily with sugar maple. Small scale disturbances may still occur periodically, but once second or third canopies are established there is minimal new regeneration taking place and the forest gradually returns to mature state.

State 4
Pioneer Forest State

Community 4.1
Pioneer Forest Community Phase

These species have a very narrow window of environmental and ecological conditions for successful establishment. Main requirements are exposed mineral soil and elimination, most effectively by fire, of on-site seed sources of potential competing vegetation. In addition, adequate soil moisture must be available for initial seedling development. Once seedlings are firmly established, height growth of both species is relatively rapid and able to outgrow most competitive species. Paper birch seedlings and saplings tolerate partial shade and often become members of mixed species communities. This is not true for aspen which requires continuous full-sun exposure for survival. Aspen stands are initially very dense due to sprouting from extensive lateral roots, but rapid natural thinning ensues as stems compete for available light.

Dominant plant species

quaking aspen (Populus tremuloides), tree
European white birch (Betula pendula), tree
red maple (Acer rubrum), tree
oak (Quercus), tree
black cherry (Prunus serotina), shrub
beaked hazelnut (Corylus cornuta), shrub
Canada mayflower (Maianthemum canadense), other herbaceous

State 5
Agricultural State

Indefinite period of applying agricultural practices.

Community 5.1
Agricultural Community Phase

Indefinite period of applying agricultural practices. Crops likely include alfalfa, corn, soybeans, and hay or pasture. It is possible that some areas have been abandoned, but persist in a domesticated grassland condition having been previously pasture or hay ground.

Transition T1A
State 1 to 2

Suppression of fire leading to the encroachment of wood species. Continued suppression for 10+ years required for the establishment of woody species.

Restoration pathway R2A
State 2 to 1

Reintroduction of fire causing the mortality of encroaching trees and shrubs. This fire must then return at relatively short intervals to continue to suppress the growth of woody vegetation.

Transition T2A
State 2 to 4

Continued fire suppression for several decades will lead to a dominant woody cover on the site.

Transition T2B
State 2 to 5

Removal of forest/shrub cover and tilling for agricultural crop production.

Transition T3A
State 3 to 4

Clear cutting with initial control of competing vegetation, or stand-replacing fire, prepare the site for occupancy by shade intolerant species. This may occur through natural regeneration or by planting.

Restoration pathway R4A
State 4 to 2

Low intensity moderate return interval fire removing fire intolerant species and regeneration

Restoration pathway R4B
State 4 to 3

Deciduous forest community is slowly invaded by conifers

Transition T5A
State 4 to 5

Removal of forest/shrub cover and tilling for agricultural crop production.

Additional community tables

Supporting information

Inventory data references

Plot and other supporting inventory data for site identification and community phases is located on a NRCS North Central Region shared and one drive folder. University of Wisconsin-Stevens Point described soils, took photographs, and inventoried vegetation data at community phases within the reference state. The data sources include WI ESD Plot Data Collection Form - Tier 2, Releve Method, NASIS pedon description, NRCS SOI 036, photographs, and Kotar Habitat Types.

Other references

Cleland, D.T.; Avers, P.E.; McNab, W.H.; Jensen, M.E.; Bailey, R.G., King, T.; Russell, W.E. 1997. National Hierarchical Framework of Ecological Units. Published in, Boyce, M. S.; Haney, A., ed. 1997. Ecosystem Management Applications for Sustainable Forest and Wildlife Resources. Yale University Press, New Haven, CT. pp. 181-200.

County Soil Surveys from St. Croix, Polk, Barron, Rusk, Chippewa, Clark, Marathon, Taylor, Price, Sawyer, Burnett, Washburn, Douglas, Bayfield, Ashland, Lincoln, Oneida, Langlade, Shawano, Menominee, Forest, Florence, Marinette, and Pierce Counties.

Curtis, J.T. 1959. Vegetation of Wisconsin: an ordination of plant communities. University of Wisconsin Press, Madison. 657 pp.
Davis, R.B. 2016. Bogs and Fens, A Guide to the Peatland Plants of Northeastern United States and Adjacent Canada. University Press of New England, Hanover and London. 296 pp.
Finley, R. 1976. Original vegetation of Wisconsin. Map compiled from U.S. General Land Office notes. U.S. Forest Service, North Central Forest Experiment Station, St. Paul, Minnesota.

Hvizdak, David. Personal knowledge and field experience.

Jahnke, J. and Gienccke, A. 2002. MLRA 92 Clay Till Field Investigations. Summary of field day investigations by Region 10 Soil Data Quality Specialists.
Kotar, J. 1986. Soil – Habitat Type relationships in Michigan and Wisconsin. J. For. and Water Cons. 41(5): 348-350.
Kotar, J., J.A. Kovach and G. Brand. 1999. Analysis of the 1996 Wisconsin Forest Statistics by Habitat Type. U.S.D.A. For. Serv. N.C. Res. Stn. Gen. Tech. Rept. NC-207.
Kotar, J. and T. L. Burger. 1996. A Guide to Forest Communities and Habitat Types of Central and Southern Wisconsin. University of Wisconsin-Madison, Department of Forest Ecology and Management, Madison.

Kotar, J., and T. L. Burger. 2017. Wetland Forest Habitat Type Classification System for Northern Wisconsin: A Guide for Land Managers and landowners. Wisconsin Department of Natural Resources, PUB-FR-627 2017, Madison.

Martin, L. 1965. The physical geography of Wisconsin. Third edition. The University of Wisconsin Press, Madison.

McNab, W.H. and P.W. Avers. 1994. Ecological Subregions of the United States: Section Descriptions. USDA For. Serv. Pun. WO-WSA-5, Washington, D.C.

NatureServe. 2018. International Ecological Classification Satandard: Terrestrial Ecological Classifications. NautreServe Centreal Databases. Arlington, VA. U.S.A. Data current as of 28 August 2018.

Radeloff, V.C., D.J. Mladenoff, H.S. He and M.S. Boyce. 1999. Forest landscape change in Northwestern Wisconsin Pine Barrens from pre-European settlement to the present. Can. J. For. Res. 29: 1649-1659.
Schulte, L.A., and D.J. Mladenoff. 2001. The original U.S. public land sur¬vey records: their use and limitations in reconstructing pre-European settlement vegetation. Journal of Forestry 99:5–10.

Schulte, L.A., and D.J. Mladenoff. 2005. Severe wind and fire regimes in northern forests: historical variability at the regional scale. Ecology 86(2):431–445.

Soil Survey Staff. Input based on personal experience. Tim Miland, Scott Eversoll, Ryan Bevernitz, and Jason Nemecek.
Stearns, F. W. 1949. Ninety years change in a northern hardwood forest in Wisconsin. Ecology, 30: 350-58.

United States Department of Agriculture, Forest Service. 1989. Proceedings – Land Classification Based on Vegetation: Applications for Management. Gen. Tech. Report INT-527.

United States Department of Agriculture, Forest Service. 1990. Silvics of North America, Vol. 1, Hardwoods. Agricultural Handbook 654, Washington, D.C.

United States Department of Agriculture, Forest Service. 1990. Silvics of North America, Vol. 2, Conifers. Agricultural Handbook 654, Washington, D.C.

United States Department of Agriculture, Natural Resources Conservation Service. 2006. Land Resource and Major Land Resource Areas of the United Sates, the Caribbean, and the Pacific Basin. U.S. Department of Agriculture Handbook 296.

United States Department of Agriculture, Natural Resources Conservation Service. 2008. Hydrogeomorphic Wetland Classification System: An Overview and Modification to Better Meet the Needs of the Natural Resources Conservation Service. Technical Note No. 190-8-76. Washington D.C.

Wilde, S.A. 1933. The relation of soil and forest vegetation of the Lake States Region. Ecology 14: 94-105.

Wilde, S.A. 1976. Woodlands of Wisconsin. University of Wisconsin Cooperative Extension, Pub. G2780, 150 pp.

Wisconsin Department of Natural Resources. 2015. The ecological landscapes of Wisconsin: An assessment of ecological resources and a guide to planning sustainable management. Wisconsin Department of Natural Resources, PUB-SS-1131 2015, Madison.

Contributors

Jacob Prater, Associate Professor at University of Wisconsin Stevens Point
Bryant Scharenbroch, Assistant Professor at University of Wisconsin Stevens Point
John Kotar, Ecological Specialist Independent Contractor

Approval

Suzanne Mayne-Kinney, 2/23/2024

Acknowledgments

NRCS contracted UWSP to write ecological sites in MLRA 105. Completed in 2021.

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	02/25/2024
Approved by	Suzanne Mayne-Kinney
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:

Download reference sheet

Click on box and path labels to scroll to the respective text.

Ecosystem states

1. Reference State

2. Fire Suppressed Scrub State

3. Stable Forest State

4. Pioneer Forest State

5. Agricultural State

States 2 and 5 (additional transitions)

2. Fire Suppressed Scrub State

5. Agricultural State

T1A	-	Suppression of fire.
R2A	-	Return of fire and/or large grazers to the landscape
T2A	-	Continued fire suppression for over 20 years
T2B	-	Removal of forest/shrub cover and tilling for agricultural crop production.
T3A	-	Cutting, fire, or blowdown removing existing tree canopy
R4A	-	Low intensity moderate return interval fire removing fire intolerant species and regeneration
R4B	-	Deciduous forest community is slowly invaded by conifers.
T5A	-	Removal of forest/shrub cover and tilling for agricultural crop production.