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Ecological site F090AY014WI

Loamy Bedrock Upland

Last updated: 10/02/2023
Accessed: 11/21/2024

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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): 090A–Wisconsin and Minnesota Thin Loess and Till

MLRA 90A is part of the recently glaciated till and outwash plains of central Minnesota and northern Wisconsin. The area was covered with loamy alluvium or loess after glaciation. It is in Wisconsin (56 percent), Minnesota (40 percent), and Michigan (4 percent). It makes up about 21,967 square miles (56,901 square kilometers).

This MLRA has distinct boundaries to the north where it borders tills of a dissimilar origin on the less morainic landscapes of MLRAs 88, 92, and 93A. The boundary to the west is where the MLRA transitions to the calcareous tills of the Des Moines Lobe, in MLRA 57. To the south, MLRA 90A borders MLRA 90B, which has older soils and better-defined drainage patterns, and MLRA 91, which has the distinct lower landscape relief of an outwash channel.

The part of this area in Minnesota is mostly in the Western Lake section of the Central Lowland province of the Interior Plains. Nearly all the parts in Wisconsin and Michigan are in the Superior Upland province of the Laurentian Upland. Four distinct lobes of the Laurentide Ice Sheet (Rainy, Superior, Chippewa, and Green Bay) played major roles in shaping the landscape in this area. The landscape is characterized by gently undulating to rolling, loess-mantled till plains, drumlin fields, and end moraines mixed with outwash plains associated with major glacial drainageways, swamps, bogs, and fens. In some areas lake plains and ice-walled lakes are significant. Steeper areas occur mostly as valley side slopes along flood plains and as escarpments along the margins of lakes.

Lakes, ponds, and marshes are common throughout the area, and streams generally have a dendritic pattern. The major rivers in this area are the Chippewa, St. Croix, Mississippi, and Wisconsin Rivers. Elevation ranges from 1,100 to 1,950 feet (335 to 595 meters). Local relief is mainly less than 10 feet to 20 feet (3 to 6 meters), but some major valleys and hills are 200 feet (60 meters) above the adjacent lowland.

Precambrian-age bedrock underlies most of the glacial deposits in this MLRA. The bedrock is a complex of folded and faulted igneous and metamorphic rocks. The bedrock terrain has been modified by glaciation and is covered in most areas by Pleistocene deposits and windblown silts. The glacial deposits form an almost continuous cover in most areas. The drift is several hundred feet thick in many areas. Loess covered the area shortly after the glacial ice melted.

Ground water is abundant in deep glacial deposits in most of this area. It also occurs in sedimentary and volcanic rock in the western part of the area. It is scarce where the layer of drift is thin. The water meets the domestic, agricultural, municipal, industrial, rural, and irrigation needs of the area. The content of dissolved solids in the ground water from all the various aquifers in this area is low, and the water generally is moderately hard or hard. The level of total dissolved solids in some of the water can be much higher because of a high content of limestone in some of the glacial deposits. Most of this area obtains ground water from unconsolidated glacial sand and gravel deposits on or very near the surface. Some wells tap the Cambrian sandstone in the southwestern part of the area, in Wisconsin.

In northwest Wisconsin (Ashland and Bayfield Counties) where there are no glacial deposits and in much of the part of this area in Minnesota, ground water from sedimentary and volcanic rock aquifers is used. This water is of very good quality; however, many soils have very porous layers that are poor filters of domestic waste and agricultural chemicals, so there is a risk of contamination from development and agriculture. Minor water concerns are hardness and, in some areas, high concentrations of iron. Yields of water from the glacial deposits vary.

The dominant soil orders are Alfisols, Entisols, Histosols, and Spodosols. The soils in the area have a frigid temperature regime, a udic or aquic moisture regime, and mixed mineralogy.

This area has a significant acreage of public and private forestland used to support the paper and lumber industry Sap collection from sugar maple and syrup production are important forestry enterprises. Agricultural enterprises include row crops, dairy farms, and beef operations. Crops include corn, soybeans, oats, wheat, and alfalfa. Tourism, recreation, and wildlife management are important. Hunting, fishing, snowmobiling, hiking, and skiing are popular activities because of the area’s abundance of water, the many acres of national and county forests, and public hunting grounds. (United States Department of Agriculture, Natural Resources Conservation Service, 2022)

Classification relationships

Major Land Resource Area (MLRA 90A): Wisconsin and Minnesota Thin Loess and Till

USFS Subregions: Rib Mountain Rolling Ridges (212Qd), Lincoln Formation Till Plain - Hemlock Hardwoods (212Qc), Lincoln Formation Till Plain - Mixed Hardwoods (212Qb), Brule and Paint Rivers Drumlinized Ground Moraine (212Xc), Rosemont Baldwin Plains and Moraines (222Md)

Small sections occur in Crystal Falls Till and Outwash (212Xq), Perkinstown End Moraine (212Xe), Hayward Stagnation Moraines (212Xf), Mille Lacs Uplands (212Kb)

Wisconsin DNR Ecological Landscapes: Forest Transition, Western Prairie, North Central Forest, Northwest Lowlands

Ecological site concept

The Loamy Bedrock Upland ecological site is common to the southern portion of MLRA 90A, located on till plains. These sites are characterized by moderately deep to very deep, moderately well to well drained soils that formed primarily in loamy till deposits over bedrock, but also include loess, alluvium, outwash, and pedisediment. Bedrock types include granite, quartzite, gneiss, basalt, sandstone, interbedded sandstone and shale, limestone, and igneous and metamorphic rock. Precipitation and runoff from adjacent uplands are the primary sources of water. Soils range from very strongly acid to slightly alkaline.

Loamy Bedrock Upland is distinguished from other sites based on drainage and moderately deep profile. The underlying bedrock can perch water and cause limitations to growth, acting as a root restricting layer. These sites may be more vulnerable to tree tips. The loamy materials differentiate this site from other moderately well and well drained sites that have sandy or clayey deposits. Loamy materials often have higher pH and available water capacity than sand, but less than clay.

Associated sites

F090AY007WI	Wet Clayey Lowlands Wet Clayey Lowlands form in deep, loamy to clayey deposits derived from a mixture of alluvium, residuum, till, or lacustrine sources. These sites have a seasonally high water table at the surface, and some are subject to occasional ponding. Sustained saturation is enough for hydric conditions to occur. They are wetter and occur lower on the drainage sequence than Loamy Bedrock Upland.
F090AY008WI	Moist Sandy Bedrock Upland Moist Sandy Bedrock Upland sites consist of sandy to clayey alluvium, till, or eolian deposits over residuum weathered from bedrock. Bedrock contact occurs within two meters of the surface. Sites have seasonally high water table within a meter of the surface. Perching of the water table may occur as a result of bedrock contact. They are wetter and occur lower on the drainage sequence than Loamy Bedrock Upland.
F090AY021WI	Dry Loamy Upland Dry Loamy Upland consist of deep sandy to loamy outwash, alluvium, or till. The water table is deeper than two meters year-round. They are drier and occur higher on the drainage sequence than Loamy Bedrock Upland.

F090AY007WI

Wet Clayey Lowlands

Wet Clayey Lowlands form in deep, loamy to clayey deposits derived from a mixture of alluvium, residuum, till, or lacustrine sources. These sites have a seasonally high water table at the surface, and some are subject to occasional ponding. Sustained saturation is enough for hydric conditions to occur. They are wetter and occur lower on the drainage sequence than Loamy Bedrock Upland.

F090AY008WI

Moist Sandy Bedrock Upland

Moist Sandy Bedrock Upland sites consist of sandy to clayey alluvium, till, or eolian deposits over residuum weathered from bedrock. Bedrock contact occurs within two meters of the surface. Sites have seasonally high water table within a meter of the surface. Perching of the water table may occur as a result of bedrock contact. They are wetter and occur lower on the drainage sequence than Loamy Bedrock Upland.

F090AY021WI

Dry Loamy Upland

Dry Loamy Upland consist of deep sandy to loamy outwash, alluvium, or till. The water table is deeper than two meters year-round. They are drier and occur higher on the drainage sequence than Loamy Bedrock Upland.

Similar sites

F090AY017WI	Clayey Upland Clayey Upland consist of loamy to clayey residuum or lacustrine deposits overlain by loess or sandy outwash. Bedrock contact may occur within two meters of the surface. These sites have a seasonally high water table within one meter of the surface, though they are not saturated for sustained periods. They occupy the same landscape positions and have the same drainage class as Loamy Bedrock Upland but have finer textures.
F090AY016WI	Loamy Upland Loamy Upland consist of deep loamy till, alluvium, residuum, lacustrine, or eolian deposits. Sandy deposits of these parent materials, plus outwash, may also be present. The depth to the seasonally high water table ranges from as high as the surface to as low as almost two meters below the surface. A few sites are on floodplains and upland drainageways, where very brief flooding is rare but possible. They occupy the same landscape positions and have the same drainage class an particle size as Loamy Bedrock Upland, but they lack bedrock contact within two meters.
F090AY015WI	Loamy Upland with Carbonates Loamy Upland with Carbonates consist of deep loamy till, colluvium, alluvium, residuum, or eolian deposits. Some sites may also have sandy outwash or eolian deposits. Carbonates are present in these soils. They have a seasonally high water table within one meter of the surface, though they don't remain saturated for extended periods of time. They occupy the same landscape positions and have the same drainage class an particle size as Loamy Bedrock Upland, but they lack bedrock contact within two meters.

F090AY017WI

Clayey Upland

Clayey Upland consist of loamy to clayey residuum or lacustrine deposits overlain by loess or sandy outwash. Bedrock contact may occur within two meters of the surface. These sites have a seasonally high water table within one meter of the surface, though they are not saturated for sustained periods. They occupy the same landscape positions and have the same drainage class as Loamy Bedrock Upland but have finer textures.

F090AY016WI

Loamy Upland

Loamy Upland consist of deep loamy till, alluvium, residuum, lacustrine, or eolian deposits. Sandy deposits of these parent materials, plus outwash, may also be present. The depth to the seasonally high water table ranges from as high as the surface to as low as almost two meters below the surface. A few sites are on floodplains and upland drainageways, where very brief flooding is rare but possible. They occupy the same landscape positions and have the same drainage class an particle size as Loamy Bedrock Upland, but they lack bedrock contact within two meters.

F090AY015WI

Loamy Upland with Carbonates

Loamy Upland with Carbonates consist of deep loamy till, colluvium, alluvium, residuum, or eolian deposits. Some sites may also have sandy outwash or eolian deposits. Carbonates are present in these soils. They have a seasonally high water table within one meter of the surface, though they don't remain saturated for extended periods of time. They occupy the same landscape positions and have the same drainage class an particle size as Loamy Bedrock Upland, but they lack bedrock contact within two meters.

Table 1. Dominant plant species

Tree	(1) Acer saccharum (2) Fraxinus americana
Shrub	(1) Ostrya virginiana
Herbaceous	(1) Amphicarpaea (2) Actaea rubra

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Physiographic features

These sites formed on till plains. Slope is 0 to 60 percent.

These sites are not subject to ponding or flooding. Sites have a seasonally high water table at a depth of 24 to 80 inches. The water table may drop below 90 inches during dry conditions on these sites. Surface runoff is low 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) Till plain
Runoff class	Low to very high
Flooding frequency	None
Ponding frequency	None
Elevation	180 – 305 m
Slope	0 – 60%
Water table depth	61 – 201 cm
Aspect	Aspect is not a significant factor

Climatic features

The climate of the expansive Wisconsin and Minnesota Thin Loess and Till Plain is highly variable. The eco-climatic zone (the “Tension Zone”) that runs southeast-northwest across the state splits the MLRA. In general, the MLRA has cold winters and warm summers with an adequate amount of precipitation. Near Lake Superior, precipitation and temperature tend to increase. The far western section of the MLRA, known as the western prairie ecological landscape by the Wisconsin DNR, has warmer temperatures compared to the rest of the MLRA because it falls below the eco-climatic zone. The soil moisture regime of MLRA is udic (humid climate). The soil temperature regime is frigid and cryic.

The average annual precipitation for this ecological site is 31 inches. The average annual snowfall is 49 inches. The annual average maximum and minimum temperatures are 53°F and 33°F, respectively.

Table 3. Representative climatic features

Frost-free period (characteristic range)	91-113 days
Freeze-free period (characteristic range)	118-138 days
Precipitation total (characteristic range)	737-838 mm
Frost-free period (actual range)	46-116 days
Freeze-free period (actual range)	90-146 days
Precipitation total (actual range)	711-889 mm
Frost-free period (average)	93 days
Freeze-free period (average)	125 days
Precipitation total (average)	787 mm

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) HOLCOMBE [USC00473698], Holcombe, WI
(2) ROSHOLT 9 NNE [USC00477349], Wittenberg, WI
(3) STAMBAUGH 2SSE [USC00207812], Iron River, MI
(4) BIG FALLS HYDRO [USC00470773], Glen Flora, WI
(5) COUDERAY 7 W [USC00471847], Stone Lake, WI
(6) ISLE 12N [USC00214103], Isle, MN
(7) MOOSE LAKE 1 SSE [USC00215598], Moose Lake, MN
(8) MILACA [USC00215392], Milaca, MN
(9) WINTER [USC00479304], Ojibwa, WI
(10) LAKEWOOD 3 NE [USC00474523], Lakewood, WI
(11) MINONG 5 WSW [USC00475525], Minong, WI
(12) AMERY [USC00470175], Amery, WI
(13) BRUNO 7ENE [USC00211074], Bruno, MN

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 leaves the site primarily through runoff, evapotranspiration, and groundwater recharge. Subsurface flow may occur where water perches on bedrock.

Wetland description

Permeability of these sites is impermeable to moderately slow.
Hydrologic Group: A, B, C, D
Hydrogeomorphic Wetland Classification: None
Cowardin Wetland Classification: None

Soil features

These sites are represented by the Arland, Dakota, Eaupleine, Eaupleine Variant, Elevasil, Fenwood, Hiles, Hixton, Humbird, Marathon, Mequithy, Metonga, Milaca, Mosinee, Norgo, Norgo Variant, Ribhill, Ritchey, Rockton, and Whalan soil series. Arland, Eaupleine, Eaupleine Variant, Fenwood, Marathon, and Ribhill are classified as Haplic Glossudalfs; Mequithy is an Alfic Haplorthod; Metonga and Rosholt Variant are Entic Haplorthods; Lundeen is a Humic Dystrudept; Norgo and Ritchey are Lithic Hapludalfs; Hiles and Milaca are Oxyaquic Glossudalfs; Humbird is an Oxyaquic Ultic Haplorthod; Dakota and Rockton are Typic Argiudolls; Mosinee is a Typic Dystrudept; Norgo Variant, Rosholt Variant, Hixton, and Whalan are Typic Hapludalfs; Elevasil is an Ultic Hapludalf.

These sites formed in various parent materials including loess; loamy or silty alluvium; loamy till; loamy, sandy, or silty residuum; sandy and gravelly outwash; clayey pedisediment; and silty or loamy drift. Soil depth to bedrock ranges from 17 to 72 inches. Soils are moderately well and well drained and do not meet hydric soil requirements.

The surfaces textures of these sites are sandy loam, silt loam, or loam. Some horizons have fine or very fine sand, and cobbly modifiers. Subsurface horizons consist of sandy loam, silt loam, clay loam, loam, and clay, loamy sand, and sand textures. Some horizons have fine or very fine sand, and gravelly or cobbly modifiers. Soil pH ranges from very strongly acid to slightly alkaline with values from 4.5 to 7.5. Carbonates may be present up to 10 percent beginning at 10 inches.

Figure 7. Fenwood soil series photograph courtesy of UWSP taken on 7/19/2019 in Marathon County, WI.

Table 4. Representative soil features

Parent material	(1) Alluvium (2) Outwash (3) Till (4) Sandstone and shale (5) Residuum (6) Eolian deposits (7) Limestone, sandstone, and shale (8) Igneous and metamorphic rock
Surface texture	(1) Silt loam (2) Sandy loam (3) Loam
Drainage class	Moderately well drained to well drained
Permeability class	Very slow to moderately slow
Soil depth	43 – 183 cm
Surface fragment cover <=3"	0 – 6%
Surface fragment cover >3"	0 – 5%
Available water capacity (0-154.9cm)	3.33 – 10.46 cm
Calcium carbonate equivalent (0-100.1cm)	0 – 10%
Soil reaction (1:1 water) (0-100.1cm)	4.5 – 7.5
Subsurface fragment volume <=3" (Depth not specified)	2 – 22%
Subsurface fragment volume >3" (Depth not specified)	0 – 22%

Ecological dynamics

Historically, this site was dominated by mesic hardwoods in a landscape adapted to fire disturbance that allowed for a strong presence of oaks. In pre-European settlement time wildfire was the main controlling factor of forest community dynamics. 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 sugar maple, red maple, and other mesic hardwoods. Some sites have a strong presence of red oak, and white pine is successfully reinvading the landscape in some areas. 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 and white pine. 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. Early to Mid-Successional State

3. Agricultural State

T1A	-	Clear cutting or stand-replacing fire.
T1B	-	Removal of forest vegetation and tilling.
R2A	-	Disturbance-free period 70+ years.
T2A	-	Removal of forest cover and tilling for agricultural crop production.
T3A	-	Stopping of agricultural practices and allowing to natural revegetation, or site is replanted.

State 1 submodel, plant communities

1.1. Advanced Succession Phase

1.2. Rejuvenated Phase

1.1A	-	Light to moderate intensity fires, blow-downs, snow-ice breakage.
1.2A	-	Disturbance-free period for 30+ years.

State 2 submodel, plant communities

2.1. Aspen-Birch Phase

2.2. Red Oak- Red Maple Phase

2.3. Red oak – Red maple/Sugar maple – Hazelnuts/Hog peanut – Baneberry Phase

2.1A	-	Immigration and establishment of red oak and red maple.
2.2A	-	Immigration and establishment of red oak and red maple.
2.3A	-	Clear cutting or stand-replacing fire.

State 3 submodel, plant communities

3.1. Agricultural Phase

State 1
Reference State

Reference state is a forest community dominated by sugar maple (Acer saccharum) and white ash. Depending on history of disturbance, two community phases can be distinguished largely by differences in dominance of tree species and community age structure.

Community 1.1
Advanced Succession Phase

Figure 8. Photo courtesy of UWSP taken on 7/26/2019 in Pierce County, WI.

In the absence of any major disturbance, specifically fire, this community is dominated by sugar maple. Common associates include moderately shade tolerant white ash, basswood, and red oak. Some sites may be dominated by red oak but is unlikely without any disturbance. The shrub layer is often dominated by ironwood, witch hazel, and hazelnuts. The ground layer is dominated by hog peanut and baneberry, with goldenrod, Enchanter’s nightshade, and wood ferns also common.

Dominant plant species

sugar maple (Acer saccharum), tree
white ash (Fraxinus americana), tree
American hornbeam (Carpinus caroliniana), shrub
hogpeanut (Amphicarpaea), other herbaceous
baneberry (Actaea), other herbaceous

Community 1.2
Rejuvenated Phase

Figure 9. Photo courtesy of UWSP taken on 7/26/2019 in St. Croix County, WI.

This community is dominated by a mixture of hardwoods including sugar maple, red oak and white ash. Associates may include basswood and black cherry. The shrub and ground layers are similar to the advanced succession phase, but may include the establishment of new seedlings.

Dominant plant species

sugar maple (Acer saccharum), tree
northern red oak (Quercus rubra), tree
white ash (Fraxinus americana), tree
witchhazel (Hamamelis), shrub
hazelnut (Corylus), shrub
hogpeanut (Amphicarpaea), other herbaceous
baneberry (Actaea), other herbaceous

Pathway 1.1A
Community 1.1 to 1.2

Advanced Succession Phase

Rejuvenated Phase

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. These species may join the canopy composition.

Pathway 1.2A
Community 1.2 to 1.1

Rejuvenated Phase

Advanced Succession Phase

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 2
Early to Mid-Successional State

Following disturbances described in Transition T1A a wide range of forest community phases may come into temporary existence, the three most common ones are described here.

Community 2.1
Aspen-Birch Phase

Time and the immigration, establishment, and growth of red oak and red maple seedlings. These moderately shade tolerant species seed in beneath the aspen and birch and eventually outcompete these intolerant species

Dominant plant species

quaking aspen (Populus tremuloides), tree
paper birch (Betula papyrifera), tree

Community 2.2
Red Oak- Red Maple Phase

Figure 10. Photo courtesy of UWSP taken on 7/11/2019 in Trempealeau County, WI.

This community phase occurs by invading and succeeding a pioneer aspen-birch community.

Dominant plant species

northern red oak (Quercus rubra), tree
red maple (Acer rubrum), tree

Community 2.3
Red oak – Red maple/Sugar maple – Hazelnuts/Hog peanut – Baneberry Phase

Figure 11. Photo courtesy of UWSP taken on 7/25/2019 in Trempealeau County, WI.

Stand structure consists of dominant red oak and red maple in combination with a modest, or strong presence of mature, or decaying, aspen and/or paper birch. The shrub layer typically reaches its best development in this community phase. Depending on seed source, sugar maple has become established and a young cohort exists in the subcanopy.

Dominant plant species

northern red oak (Quercus rubra), tree
red maple (Acer rubrum), tree
sugar maple (Acer saccharum), tree
hazelnut (Corylus), shrub
hogpeanut (Amphicarpaea), other herbaceous
baneberry (Actaea), other herbaceous

Pathway 2.1A
Community 2.1 to 2.2

Pathway 2.2A
Community 2.2 to 2.3

Red Oak- Red Maple Phase

Red oak – Red maple/Sugar maple – Hazelnuts/Hog peanut – Baneberry Phase

Time and natural succession. Red oak and red maple have succeeded the aspen-birch community. Depending on seed source, sugar maple begins growth and establishment in the understory.

Pathway 2.3A
Community 2.3 to 2.1

Clear cutting or major fire disturbance allows for the reinvasion of the shade intolerant aspen-birch community.

State 3
Agricultural State

Indefinite period of applying agricultural practices.

Community 3.1
Agricultural Phase

The agricultural phase constitutes tillage and the planting of row crops or hay or pasture.

Transition T1A
State 1 to 2

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.

Transition T1B
State 1 to 3

Removal of forest cover, tilling and application of other agricultural techniques to grow agricultural crops.

Restoration pathway R2A
State 2 to 1

A period of some 70-100 years without major stand disturbance, especially fire, leads to decreased presence, through natural mortality, of early successional species and the dominance of shade tolerant sugar maple with less tolerant associates of red oak and white ash, returning the community to Reference State.

Transition T2A
State 2 to 3

Removal of forest cover, tilling and application of other agricultural techniques to grow agricultural crops.

Transition T3A
State 3 to 2

Abandonment of agricultural practices and allowing natural vegetation to colonize the site or apply artificial afforestation.

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 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.

Habitat Types of N. & S. Wisconsin (Kotar, 2002 & 1996): The sites of this ES keyed out to nine habitat types: Acer saccharum/Hydrophyllum (AH); Acer saccharum-Tsuga/Maianthemum (ATM); Acer saccharum/Hydrophyllum-Viburnum (AHVb); Acer saccharum/Vaccinium-Desmodium (AVDe); Acer saccharum/Athyrium (AAt); Acer rubrum/Circaea (ArCi); Pinus-Acer rubrum/Vaccinium-Hamamelis (PArVHa); Pinus/Vaccinium-Hamamelis (PVHa); Pinus/Vaccinium-Cornus (PVCr)

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

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., J. A. Kovach, and T. L. Burger. 2002. A Guide to Forest Communities and Habitat Types of Northern Wisconsin. Second edition. 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.

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Contributors

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

Approval

Suzanne Mayne-Kinney, 10/02/2023

Acknowledgments

NRCS contracted UWSP to write ecological sites in MLRA 90A, 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	11/21/2024
Approved by	Suzanne Mayne-Kinney
Approval date
Composition (Indicators 10 and 12) based on	Annual Production