

Natural Resources
Conservation Service
Ecological site R055BY060ND
Saline Lowland
Last updated: 4/25/2025
Accessed: 05/19/2025
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.

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): 055B–Central Black Glaciated Plains
The Central Black Glaciated Plains MLRA is an expansive and agriculturally important region consisting of more than 10,000,000 acres and including all or a portion of 27 counties in east-central and southeastern North Dakota and northeastern South Dakota.
Most of MLRA 55B is covered by till: material that was moved and redeposited by the glaciers. Pre-glaciated bedrock (shale) is exposed on the breaks to some of the valleys and incised drainageways; but what covers the bedrock is glacial sediment, known as drift. These areas have the Late Wisconsin age till plain integrated drainage system in contrast to the closed drainage of much of the till plain and moraines. Some soils, particularly along the Elm, James and Sheyenne rivers, have weathered shale beds in the substratum.
The Drift Prairie Region consists of nearly level to gently rolling glacial till plains dissected by glacial outwash channels. MLRA 55B is located within the boundaries of the Prairie Pothole Region with numerous wetlands in areas without integrated drainage systems. Seven rivers flow through parts of the MLRA. The James and Sheyenne Rivers both have their headwaters in the northern part of the MLRA. A relatively narrow, low range of hills separates these rivers creating a continental watershed divide. The James River flows generally southward through the MLRA and empties into the Missouri River beyond the MLRA border. The Sheyenne River flows to the south and to the east; it empties into the Red River of the North in MLRA 56A. Major tributaries to the James River are the Pipestem and Elm Rivers. The Sheyenne River receives additional water from Devils Lake (during periods of high lake levels) via two outlet pumping stations. Other important rivers in the MLRA are the Goose, Maple, and Wild Rice rivers which are also tributaries to the Red River of the North. The Wild Rice River begins in northeastern South Dakota and flows northward and eastward. In Sargent County, North Dakota, major ditch construction has served to straighten this river and more quickly drain water off adjacent farmland.
Surface and subsurface (tile) drainage systems have been constructed/installed in many areas to manage excess water and/or salinity on cropland. Soils that were poorly drained prior to wide-spread drainage may now function as somewhat poorly drained or moderately well drained soils. Restoration of hydrology to the natural conditions of the reference state may not be possible.
This region is utilized mostly by farms and ranches; about 75 percent is non-irrigated cropland. Cash-grain, bean and oil production crops are the principal enterprise on many farms, but other feed grains and hay are also grown. The vegetation on the steeper slopes, very stony areas, and thinner (or sandy) soils is still native rangeland. About 1 percent of this area is forested. Most forested areas occur along rivers, particularly the Sheyenne River Valley.
Classification relationships
Level IV Ecoregions of the Conterminous United States: 46c – Glacial Lake Basins; 46d – Glacial Lake Deltas; 46e – Tewaukon Dead Ice Moraine; 46f – End Moraine Complex; 46i – Drift Plains; 46j – Glacial Outwash; 46n – James River Lowland.
Stream Type: DA6 (Rosgen System) on riparian systems.
Wetland Description: System Subsystem Class Sub-class
Cowardin, et. al., 1979 Palustrine N/A Emergent Wetland Persistent
Ecological site concept
The Saline Lowland ecological site generally is located on flats and depressions on glaciated uplands, on flood plains, and in drainageways. It is also located on some lakeshores, particularly in the Devils Lake Basin. The soil parent material is very deep; however, some soils have a root-restrictive, dense, claypan subsoil. Salt accumulations are common throughout the rooting zone; soil salinity is moderate or higher (E.C. >8 dS/m) within a depth of 20 inches. Areas within this site can become nearly barren due to the accumulation of salts at the surface. The soils in this site are poorly drained with redoximorphic features within a depth of 18 inches. Soil salinity is the primary factor used in identifying this site. All textures are included in the site. Slopes range from 0 to 3 percent. On the landscape, this site is below the Loamy Overflow and Thin Claypan ecological sites and above the Shallow Marsh sites. The Sodic Subirrigated and Wet Meadow ecological sites occur on similar, poorly drained landscape positions as this site; they are non-saline to slightly saline to a depth greater than 20 inches. Limy Subirrigated ecological sites occur on somewhat poorly drained positions; typically, they are non-saline to slightly saline (E.C. <8 dS/m), but a Salinized State is recognized. On sandy lake plains, the Sandy Claypan site may also be associated; it is slightly above the Saline Lowland site. Note: Some frequently flooded soils may be included in this site. The Riparian Complex ecological site should be considered for such soils.
To see a full copy of the ecological site description with all tables and the full version 5 rangeland health worksheet, please use the following hyperlink: https://efotg.sc.egov.usda.gov/references/public/ND/55B_Saline_Lowland_Narrative_FINAL_Ref_FSG.pdf
Associated sites
R055BY058ND |
Limy Subirrigated This site occurs on somewhat poorly drained landscape positions. The soils are highly calcareous within a depth of 16 inches. Redoximorphic features occur at a depth between 18 and 30 inches. Salinity, typically, is none to slight (E.C. <8 dS/m); however, a Salinized State is recognized. All textures are included in this site. |
---|---|
R055BY059ND |
Loamy Overflow This site occurs on flood plains and upland swales. The surface and subsoil layers form a ribbon 1 to 2 inches long. It is non-saline and is >30 inches to redoximorphic features. |
R055BY066ND |
Thin Claypan This site typically occurs somewhat higher on the landscape. The depth to redoximorphic features is >18 inches. It has a dense, claypan layer within a depth of 6 inches and has salt accumulations within a depth of 16 inches. |
R055BY071ND |
Wet Meadow This site occurs on similar, poorly drained landscape positions. Redoximorphic features occur within a depth of 18 inches. Where salts occur, E.C. is <8 dS/m to a depth >20 inches. All textures are included in this site. |
R055BY072ND |
Sandy Claypan This site occurs on sandy lake plains and is slightly higher on the landscape than Saline Lowland. It is typically moderately well drained. It has a claypan layer starting at a depth between 6 and 20 inches; salt accumulations, where present, are deeper than 16 inches. |
R055BY070ND |
Shallow Marsh This site occurs in deep depressions which have frequent ponding through most of the growing season. It is very poorly drained. All textures are included in this site. Some soils with slight or moderate salt accumulations are included. |
Similar sites
R055BY058ND |
Limy Subirrigated This site occurs on somewhat poorly drained landscape positions. The soils are highly calcareous within a depth of 16 inches. Redoximorphic features occur at a depth between 18 and 30 inches. Salinity, typically, is none to slight (E.C. <8 dS/m); however, a Salinized State is recognized. All textures are included in this site. |
---|---|
R055BY066ND |
Thin Claypan This site typically occurs somewhat higher on the landscape. The depth to redoximorphic features is >18 inches. It has a dense, claypan layer within a depth of 6 inches and has salt accumulations within a depth of 16 inches. |
R055BY071ND |
Wet Meadow This site occurs on similar, poorly drained landscape positions. Redoximorphic features occur within a depth of 18 inches. Where salts occur, E.C. is <8 dS/m to a depth >20 inches. All textures are included in this site. |
Table 1. Dominant plant species
Tree |
Not specified |
---|---|
Shrub |
Not specified |
Herbaceous |
(1) Elymus trachycaulus |
Physiographic features
This site typically occurs on flats and shallow depressions on uplands, on flood plains, and in drainageways; it also occurs on some lake shore areas. As the landforms vary considerably, so do the parent materials. Slopes are typically less than 3 percent.
Table 2. Representative physiographic features
Landforms |
(1)
Flat
(2) Depression (3) Drainageway (4) Lakeshore (5) Flood plain |
---|---|
Runoff class | Negligible to medium |
Flooding duration | Long (7 to 30 days) |
Flooding frequency | None to frequent |
Ponding duration | Very long (more than 30 days) |
Ponding frequency | None to frequent |
Elevation | 950 – 2,525 ft |
Slope | 3% |
Ponding depth | 12 in |
Water table depth | 18 in |
Aspect | Aspect is not a significant factor |
Climatic features
MLRA 55B is considered to have a continental climate – cold winters and hot summers, low humidity, light rainfall, and much sunshine. Extremes in temperature are characteristic of the MLRA. The climate is the result of this MLRA’s location in the geographic center of North America. There are few natural barriers on the northern Great Plains. The air masses move unobstructed across the plains and account for rapid changes in temperature.
Annual precipitation ranges from 18 to 23 inches per year. The normal average annual temperature is about 41.5° F. January is the coldest month with average low temperature ranging from about -4.3° F (Petersburg, ND) to about 2.5° F (Mellette, SD). July is the warmest month with temperatures averaging from about 79° F (Petersburg, ND) to about 84° F (Mellette, SD). The range of normal average monthly temperatures between the coldest and warmest months is about 64° F. This large annual range attests to the continental nature of this MLRA's climate. Winds average about 11 miles per hour annually, ranging from about 13 miles per hour during the spring to about 10 miles per hour during the summer. Daytime winds are generally stronger than nighttime and strong storms may bring brief periods of high winds with gusts to more than 50 miles per hour.
Growth of native cool-season plants begins in late March and continues to early to mid-July. Native warm- season plants begin growth in mid-May and continue to the end of August. Greening up of cool-season plants can occur in September and October when adequate soil moisture is present.
Table 3. Representative climatic features
Frost-free period (characteristic range) | 111-117 days |
---|---|
Freeze-free period (characteristic range) | 128-134 days |
Precipitation total (characteristic range) | 19-22 in |
Frost-free period (actual range) | 105-119 days |
Freeze-free period (actual range) | 124-135 days |
Precipitation total (actual range) | 18-23 in |
Frost-free period (average) | 114 days |
Freeze-free period (average) | 131 days |
Precipitation total (average) | 21 in |
Figure 2. Monthly precipitation range
Figure 3. Monthly minimum temperature range
Figure 4. Monthly maximum temperature range
Figure 5. Monthly average minimum and maximum temperature
Figure 6. Annual precipitation pattern
Figure 7. Annual average temperature pattern
Climate stations used
-
(1) BUTTE 5SE [USC00321225], Butte, ND
-
(2) CARRINGTON [USC00321360], Carrington, ND
-
(3) FORMAN 5 SSE [USC00323117], Forman, ND
-
(4) HARVEY 4NE [USC00324013], Harvey, ND
-
(5) LA MOURE [USC00324937], Lamoure, ND
-
(6) MELLETTE 4 W [USC00395456], Northville, SD
-
(7) PETERSBURG 2 N [USC00327027], Petersburg, ND
-
(8) COLUMBIA 8 N [USC00391873], Columbia, SD
Influencing water features
This site most commonly occurs as a discharge site with evaporation during the growing season resulting in the accumulation of salts at or near the soil surface. During the growing season, the water table is typically within a depth of 18 inches in the spring months; it may lower to a depth >3 feet during mid-summer. Most areas of this site have endosaturation (the soil is saturated with water in all layers); however, areas of episaturation (perched water table above a subsoil layer with very slow or slow permeability) also occur. Surface infiltration rates range from very slow to moderately rapid; permeability, typically, is slow to moderately rapid. Water loss is through evapotranspiration and percolation below the root zone.
Note: Hydrology (e.g., depth/movement of water table) and water chemistry (e.g., salinity/sodicity) are the main drivers for this site. The interactions of these two drivers, coupled with management, can cause vegetation to change quickly or over long periods of time.
Some areas have wetland functions due to prolonged, near-surface saturation which supports salt-tolerant, hydrophytic vegetation. In other areas, under normal climatic conditions, soil saturation is not shallow enough to support hydrophytic vegetation.
Early in the growing season and after heavy rains, areas of this site on flats may pond as deep as 6 inches; this ponding is very brief or brief (<7 days). Areas in depressions may pond as deep as 12 inches for longer periods (>7 to >30 days). On flood plains, this site has rare to frequent flooding of brief to long duration. Areas on lake shores may be inundated periodically for extended periods.
Wetland description
Stream Type: DA6 (Rosgen System) on riparian systems.
Wetland Description: System Subsystem Class Sub-class Water Regime
Cowardin, et. al., 1979 Palustrine N/A Emergent Persistent Temporary/Saturated
Soil features
Soils associated with Saline Lowland ecological site are in the Mollisol, Vertisol, and Entisol orders. The Mollisols are further classified as Typic Calciaquolls, Cumulic Endoaquolls, and Typic Natraquolls. The Vertisols are further classified as Typic Calciaquerts, Typic Endoaquerts, and Typic Natraquerts. The Entisols are further classified as Vertic Fluvaquents and Typic Psammaquents. These soils were developed under prairie or wetland vegetation. They formed in glaciolacustrine sediments, till, or alluvium. The soils on this site are very deep. The common feature of these soils is the presence of soluble salts within the rooting zone. Soil salinity is moderate or higher (E.C. >8 dS/m).
The soils in this site are poorly drained with redoximorphic features within a depth of 18 inches. Since soil salinity is the primary factor used in identifying this site; all textures are included. Therefore, soil physical properties associated with texture vary widely. Some soils in this site also have a sodic claypan which restricts rooting depth.
Sodicity is low to high (SAR <3 to >13). Soil reaction is slightly acid strongly alkaline (pH 6.1 to 9.0). Calcium carbonate content ranges from none to high (<45%).
Areas within this site can become nearly barren due to the accumulation of salts at the surface. The soil surface is stable and intact. Sub-surface soil layers can be restrictive to water movement and root penetration. Salt accumulation strongly influences the soil/water/plant relationship.
Major soil series correlated to the Saline Lowland site are Arveson, Borup, Colvin, Easby, Harriet, Hegne, Lallie, Lamoure, Lowe, Ludden, Manfred, Marysland, Ojata, Ryan, and Vallers.
Access Web Soil Survey (https://websoilsurvey.sc.egov.usda.gov/App/WebSoilSurvey.aspx) for specific local soils information.
Table 4. Representative soil features
Parent material |
(1)
Till
(2) Glaciolacustrine deposits (3) Glaciofluvial deposits (4) Alluvium (5) Outwash |
---|---|
Surface texture |
(1) Loam (2) Clay loam (3) Silt loam (4) Silty clay loam (5) Silty clay (6) Fine sandy loam |
Family particle size |
(1) Loamy (2) Sandy (3) Clayey |
Drainage class | Poorly drained |
Permeability class | Slow to moderately rapid |
Depth to restrictive layer | 2 – 80 in |
Surface fragment cover <=3" | 3% |
Surface fragment cover >3" | 1% |
Available water capacity (0-40in) |
0.5 – 8 in |
Calcium carbonate equivalent (0-40in) |
45% |
Electrical conductivity (0-20in) |
8 – 16 mmhos/cm |
Sodium adsorption ratio (0-40in) |
1 – 25 |
Soil reaction (1:1 water) (0-40in) |
6.1 – 9 |
Subsurface fragment volume <=3" (Depth not specified) |
12% |
Subsurface fragment volume >3" (Depth not specified) |
2% |
Ecological dynamics
This ecological site description is based on nonequilibrium ecology and resilience theory and utilizes a State- and-Transition Model (STM) diagram to organize and communicate information about ecosystem change as a basis for management. The ecological dynamics characterized by the STM diagram reflect how changes in these ecological drivers, feedback mechanisms, and controlling variables can maintain or induce changes in plant community composition (phases and/or states). The application of various management actions, combined with weather variables, impact the ecological processes which influence the competitive interactions, thereby maintaining or altering plant community structure.
The main drivers for this site are hydrology (e.g., fluctuating depth of the water table) and water chemistry (e.g., salinity/sodicity). Depth to water table can be quite variable on this site due to inter-seasonal or intra- seasonal variations in precipitation and other factors. It is a major factor influencing vegetation on the site. When the water table is near the surface, capillary action tends to bring salts upward to the soil surface. The critical period is during the summer months when evaporation rates are high. Conversely, when the water table is deeper the salts tend to be driven downward in the soil through precipitation. As a result, the changes in salinity within the rooting zone can lead to marked changes in the botanical composition of the site.
Management of the site should focus on moving water downward in the soil. Managerial techniques to move water downward (eventually below the rooting zone) should focus on maintaining soil surface cover, plant vigor, and diversity. Conversely, techniques that facilitate the movement of salts upward to the soil surface can be expected to result in a decreased production with expanding areas of bare salt-encrusted soil. A critical time for management is when the soil is drying out after a period of saturation. Overgrazing during this time may increase surface evaporation and salt accumulation.
Prior to European influence, the historical disturbance regime for MLRA 55B included frequent fires, both anthropogenic and natural in origin. Most fires, however, were anthropogenic fires set by Native Americans. Native Americans set fires in all months except perhaps January. These fires occurred in two peak periods, one from March-May with the peak in April and another from July-November with the peak occurring in October. Most of these fires were scattered and of small extent and duration. The grazing history would have involved grazing and browsing by large herbivores (such as American bison, elk, and whitetail deer). Herbivory by small mammals, insects, nematodes, and other invertebrates are also important factors influencing the production and composition of the communities. Grazing and fire interaction, particularly when coupled with drought events, influenced the dynamics discussed and displayed in the following state and transition diagram and descriptions.
Following European influence, this ecological site generally has had a history of grazing by domestic livestock, particularly cattle, which along with other related activities (e.g., fencing, water development, fire suppression) has changed the disturbance regime of the site. Changes will occur in the plant communities due to these and other factors.
Weather fluctuations coupled with managerial factors may lead to changes in the plant communities and may, under adverse impacts, result in a slow decline in vegetative vigor and composition. However, under favorable conditions the botanical composition may resemble that prior to European influence.
Four vegetative states have been identified for the site (Reference, Native/Invaded, Invaded, and Go-Back). Within each state, one or more community phases have been identified. These community phases are named based on the more dominant and visually conspicuous species; they have been determined by study of historical documents, relict areas, scientific studies, and ecological aspects of plant species and plant communities. Transitional pathways and thresholds have been determined through similar methods.
State 1: Reference State represents the natural range of variability that dominated the dynamics of this ecological site prior to European influence. Dynamics of the state were largely determined by variations in climate and weather (e.g., drought), as well as that of fire (e.g., timing, frequency) and grazing by native herbivores (e.g., frequency, intensity, selectivity). Due to those variations, the Reference State is thought to have shifted temporally and spatially between three plant community phases.
Currently the primary disturbances include widespread introduction of exotic plants, concentrated livestock grazing, lack of fire, and perhaps long-term non-use or very light grazing, and no fire. Because of these changes, particularly the widespread occurrence of exotic species, as well as other environmental changes, the Reference State is considered to no longer exist. Thus, the presence of exotic plants on the site precludes it from being placed in the Reference State. It must then be placed in one of the other states, commonly State 2: Native/Invaded State (T1A).
State 2: Native/Invaded State. Colonization of the site by exotic plants results in a transition from State 1: Reference State to State 2: Native/Invaded State (T1A). This transition was inevitable; it often resulted from colonization by exotic cool-season grasses (e.g., Kentucky bluegrass, smooth brome, quackgrass) which have been particularly and consistently invasive under extended periods of non-use or very light grazing, and no fire. Other exotics plants (e.g., field sowthistle, Canada thistle, burning bush) are also known to invade the site.
Three community phases have been identified for this state; they are similar to the community phases in the Reference State but have now been invaded by exotic cool-season grasses. These exotic cool-season grasses can be expected to increase. As that increase occurs, plants more desirable to wildlife and livestock may decline. A decline in forb diversity can also be expected. Under non-use or minimal use management, mulch increases and may become a physical barrier to plant growth. This also changes the micro-climate near the soil surface and may alter infiltration, nutrient cycling, and biological activity near the soil surface. As a result, these factors coupled with shading cause desirable native plants to have increasing difficulty remaining viable and recruitment declines.
To slow or limit the invasion of these exotic grasses or other exotic plants, it is imperative that managerial techniques (e.g., prescribed grazing, prescribed burning) be carefully constructed, monitored, and evaluated with respect to that objective. If management does not include measures to control or reduce these exotic plants, the transition to State 3: Invaded State should be expected (T2A).
State 3: Invaded State. The threshold for this state is reached when the exotic cool-season grasses (e.g., Kentucky bluegrass, smooth brome, quackgrass) exceed 30% of the plant community and native grasses represent less than 40% of the community. One community phase has been identified for this state.
The exotic cool-season grasses can be quite invasive and often form monotypic stands. As they increase, both forage quantity and quality of the annual production becomes increasingly restricted to late spring and early summer, even though annual production may increase. Forb diversity often declines. Under non-use or minimal use management, mulch can increase and become a physical barrier to plant growth which alters nutrient cycling, infiltration, and soil biological activity. As such, desirable native plants become increasingly displaced.
Once the state is well established, prescribed burning and prescribed grazing techniques have been largely ineffective in suppressing or eliminating the exotic cool-season grasses, even though some short-term reductions may appear successful. However, assuming there is an adequate component of native grasses to respond to treatments, a restoration pathway to State 2: Native/Invaded State may be accomplished with the implementation of long-term prescribed grazing in conjunction with prescribed burning (R3A).
State 4: Go-Back State often results following cropland abandonment and consists of only one plant community phase. This weedy assemblage may include noxious weeds that need control. Over time, the exotic cool-season grasses (e.g., Kentucky bluegrass, smooth brome, quackgrass) will likely predominate.
Initially, due to extensive bare ground and a preponderance of shallow rooted annual plants, the potentials for soil erosion and increased salinization are high. Plant species richness may be high, but overall diversity (i.e., equitability) is typically low with the site dominated by a relatively small assemblage of species. Due to the lack of native perennials and other factors, restoring the site with the associated ecological processes is difficult. However, a successful range planting may result in something approaching State 2: Native/Invaded State (R4A). Following planting, prescribed grazing, prescribed burning, haying, and the use of herbicides will generally be necessary to achieve the desired result and control weeds, some of which may be noxious weeds. A failed range planting and/or secondary succession will lead to State 3: Invaded State (R4B).
Woody Invasion. Historically, individual (or small patches of) shrubs and/or trees were not present on this site. However, a marked increase in fire suppression, climate change, increase in non-use, and other factors enabled woody species to colonize and begin to or encroach on the site. These changes have enabled saline tolerant species, such as Russian olive, to expand and become more widespread and impinging on the ecological integrity of the grassland biome. Windbreaks and other tree plantings can contain problematic and invasive species which can contaminate surrounding grasslands. This results in increased long-term costs to maintain or restore this ecological site in native grasses and forbs.
The following state and transition model diagram illustrates the common states, community phases, community pathways, and transition and restoration pathways that can occur on the site. These are the most common plant community phases and states based on current knowledge and experience; changes may be made as more data are collected. Pathway narratives describing the site’s ecological dynamics reference various management practices (e.g., prescribed grazing, prescribed fire, brush management, herbaceous weed treatment) which, if properly designed and implemented, will positively influence plant community competitive interactions. The design of these management practices will be site specific and should be developed by knowledgeable individuals; based upon management goals and a resource inventory; and supported by an ongoing monitoring protocol.
When the management goal is to maintain an existing plant community phase or restore to another phase within the same state, modification of existing management to ensure native species have the competitive advantage may be required. To restore a previous state, the application of two or more management practices in an ongoing manner will be required. Whether using prescribed grazing, prescribed burning, or a combination of both with or without additional practices (e.g., brush management), the timing and method of application needs to favor the native species over the exotic species. Adjustments to account for variations in annual growing conditions and implementing an ongoing monitoring protocol to track changes and adjust management inputs to ensure desired outcome will be necessary.
The plant community phase composition table(s) has been developed from the best available knowledge including research, historical records, clipping studies, and inventory records. As more data are collected, plant community species composition and production information may be revised.
Drainage/Hydrological Manipulation: Hydrological manipulation (surface or tile drainage, pumping, surface water diversion, etc.) modifies this ecological site. For more detailed information on drainage/hydrological manipulation of the site, see the “Hydrology Functions” section of this document.
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
T1A | - | Introduction of exotic cool-season grasses |
---|---|---|
T2A | - | Long-term non-use or very light grazing, and no fire |
R3A | - | Long-term prescribed grazing and prescribed burning |
R4A | - | Successful range planting |
R4B | - | Failed range planting and/or secondary succession |
T5A | - | Cessation of annual cropping |
State 1 submodel, plant communities
1.1a | - | Multiyear drought with or without heavy long-term grazing |
---|---|---|
1.2a | - | Return to average precipitation, light to moderate grazing |
1.2b | - | Multiyear drought with or without heavy long-term grazing |
1.3a | - | Return to average precipitation, light to moderate grazing |
State 2 submodel, plant communities
2.1a | - | Multiyear drought with or without heavy long-term grazing |
---|---|---|
2.2a | - | Return to average precipitation, long-term prescribed grazing |
2.2b | - | Multiyear drought with heavy grazing |
2.3a | - | Return to average precipitation, long-term prescribed grazing |
State 3 submodel, plant communities
State 4 submodel, plant communities
State 1
Reference
This state represents the natural range of variability that dominated the dynamics of this ecological site prior to European influence. This state is composed of a co-dominant mixture of warm-season and cool-season grasses and other graminoids. The primary disturbance mechanisms for this site in the reference condition included occasional fire and grazing by large herding ungulates. Timing of fires and grazing, coupled with weather events, dictated the dynamics that occurred within the natural range of variability. Today the primary disturbance is from a lack of fire and concentrated livestock grazing. Grasses that are desirable for livestock and wildlife may decline and a corresponding increase in less desirable grasses will occur. These factors likely caused the community to shift both spatially and temporally between three community phases. Two of these phases were dominated by wheatgrasses with another containing conspicuous and, in some cases, extensive areas of bare ground and an abundance of forbs.
Characteristics and indicators. Because of changes in disturbances and other environmental factors (particularly the widespread occurrence of exotic species), the Reference State is considered to no longer exist.
Resilience management. If intact, the reference state should probably be managed with current disturbance regimes which has permitted the site to remain in reference condition, as well as maintaining the quality and integrity of associated ecological sites. Maintenance of the reference condition is contingent upon a monitoring protocol to guide management.
Community 1.1
Wheatgrasses-Cordgrasses-Nuttall's Alkaligrass (Pascopyrum smithii, Elymus trachycaulus-Spartina spp.-Puccinellia nuttallii)
This community phase was historically the most dominant both temporally and spatially. The major grasses include western wheatgrass, slender wheatgrass, prairie cordgrass, and alkali cordgrass. Other grasses included Nuttall’s alkaligrass, saltgrass, scratchgrass, and foxtail barley. Salt tolerant forbs (such as redwool plantain, western dock, seaside arrowgrass, and seepweed) may also be common associates. Annual production likely varied from about 2800-4800 pounds per acre with graminoids and forbs contributing about 95% and 5%, respectively. Both warm and cool-season grasses were well represented in the community. As a result, production would have been distributed throughout the growing season. This community represents the plant community phase upon which interpretations are primarily based and is described in the “Plant Community Composition and Group Annual Production” portion of this ecological site description.
Figure 8. Annual production by plant type (representative values) or group (midpoint values)
Table 5. Annual production by plant type
Plant type | Low (lb/acre) |
Representative value (lb/acre) |
High (lb/acre) |
---|---|---|---|
Grass/Grasslike | 2765 | 3686 | 4585 |
Forb | 35 | 114 | 215 |
Total | 2800 | 3800 | 4800 |
Figure 9. Plant community growth curve (percent production by month). ND5507, Central Black Glaciated Plains, cool-season dominant, warm-season sub-dominant.. Cool-season dominant, warm-season sub-dominant, lowland..
Jan | Feb | Mar | Apr | May | Jun | Jul | Aug | Sep | Oct | Nov | Dec |
---|---|---|---|---|---|---|---|---|---|---|---|
J | F | M | A | M | J | J | A | S | O | N | D |
0 | 0 | 2 | 7 | 36 | 35 | 10 | 3 | 6 | 1 | 0 | 0 |
Community 1.2
Wheatgrasses-Foxtail Barley-Saltgrass (Pascopyrum smithii, Elymus trachycaulus-Hordeum jubatum-Distichlis spicata)
This community developed with multiyear drought with or without heavy, long-term grazing. Western wheatgrass, slender wheatgrass, prairie cordgrass, alkali cordgrass, and Nuttall’s alkaligrass have decreased in comparison to Plant Community Phase 1.1 with corresponding increases in saltgrass and foxtail barley. Forbs (such as silverleaf cinquefoil, western dock, and redwool plantain) also increased.
Community 1.3
Bare Ground/Halophytes
This plant community occurred during multiyear drought with or without heavy long-term grazing. Increased salt accumulation on and near the soil surface resulted in increases in bare, salt encrusted areas which supported largely halophytic vegetation. Common plants included saltgrass, seaside arrowgrass, red swampfire, and Pursh seepweed.
Pathway 1.1a
Community 1.1 to 1.2
Community Phase Pathway 1.1 to 1.2 occurred with multiyear drought with or without heavy, long-term grazing leading to marked increases in foxtail barley and saltgrass with a corresponding decrease in cordgrasses.
Pathway 1.2a
Community 1.2 to 1.1
Community Phase Pathway 1.2 to 1.1 occurred with the return to average precipitation and light to moderate grazing. This resulted in notable decreases in foxtail barley and saltgrass with a corresponding increase in cordgrasses.
Pathway 1.2b
Community 1.2 to 1.3
Community Phase Pathway 1.2 to 1.3 occurred with multiyear drought with or without heavy long-term grazing. This resulted in the site becoming characterized by increased areas of bare ground and halophytic vegetation.
Pathway 1.3a
Community 1.3 to 1.1
Community Phase Pathway 1.3 to 1.2 occurred with the return to average precipitation with light to moderate grazing resulting in noticeable increases in wheatgrasses, foxtail barley, and saltgrass with corresponding decreases in bare ground and halophytic plants.
State 2
Native/Invaded
This state is similar to State 1: Reference State but has now been colonized by the exotic cool-season grasses (e.g., Kentucky bluegrass, smooth brome, quackgrass) which are now present in small amounts. Although the state is still dominated by native grasses, an increase in these exotic cool-season grasses can be expected. These exotic cool-season grasses can be quite invasive on the site and are particularly well adapted to heavy grazing. They also often form monotypic stands. As these exotic cool-season grasses increase, both forage quantity and quality become increasingly restricted to late spring and early summer due to the monotypic nature of the stand, even though annual production may increase. Native forbs generally decrease in production, abundance, diversity, and richness compared to that of State 1: Reference State. These exotic cool-season grasses have been particularly and consistently invasive under extended periods of non-use and no fire. To slow or limit the invasion of these exotic grasses, it is imperative that managerial techniques (e.g., prescribed grazing, prescribed burning) be carefully constructed, monitored, and evaluated with respect to that objective. If management does not include measures to control or reduce these exotic cool-season grasses, the transition to State 3: Invaded State should be expected. Annual production of this state can be quite variable, in large part due to the amount of exotic cool-season grasses. However, as the exotic cool-season grasses increase, peak production will shift to earlier in the growing season.
Characteristics and indicators. The presence of trace amounts of exotic cool-season grasses indicates a transition from State 1 to State 2. The presence of exotic biennial or perennial leguminous forbs (i.e., sweet clover, black medic) may not, on their own, indicate a transition from State 1 to State 2 but may facilitate that transition.
Resilience management. To slow or limit the invasion of these exotic grasses, it is imperative that managerial techniques (e.g., prescribed grazing, prescribed burning) be carefully constructed, monitored, and evaluated with respect to that objective. Grazing management should be applied that enhances the competitive advantage of native grass and forb species. This may include: (1) grazing when exotic cool-season grasses are actively growing and native cool- season grasses are dormant; (2) applying proper deferment periods allowing native grasses to recover and maintain or improve vigor; (3) adjusting overall grazing intensity to reduce excessive plant litter (above that needed for rangeland health indicator #14 – see Rangeland Health Reference Worksheet); (4) incorporating early heavy spring utilization which focuses grazing pressure on exotic cool-season grasses and reduces plant litter, provided that livestock are moved when grazing selection shifts from exotic cool-season grasses to native grasses. Prescribed burning should be applied in a manner that maintains or enhances the competitive advantage of native grass and forb species. Prescribed burns should be applied as needed to adequately reduce/remove excessive plant litter and maintain the competitive advantage for native species. Timing of prescribed burns (spring vs. summer vs. fall) should be adjusted to account for differences in annual growing conditions and applied during windows of opportunity to best shift the competitive advantage to the native species.
Community 2.1
Wheatgrasses-Cordgrasses-Nuttall's Alkaligrass (Pascopyrum smithii, Elymus trachycaulus-Spartina spp.-Puccinellia nuttallii)
This plant community is similar to Community Phase 1.1 but has now been colonized by exotic cool-season grasses (e.g., Kentucky bluegrass, quackgrass, smooth brome). Nuttall’s alkaligrass often becomes a conspicuous component of the community although western wheatgrass, slender wheatgrass, and cordgrasses may still be present but have declined in importance compared to the Reference State.
Community 2.2
Wheatgrasses-Foxtail Barley-Saltgrass (Pascopyrum smithii, Elymus trachycaulus-Hordeum jubatum-Distichlis spicata)

Figure 10. Community Phase 2.2: Wheatgrasses-Foxtail Barley-Saltgrass, dominated by foxtail barley.
This community phase is similar to Reference State Community Phase 1.2 but now supports minor amounts of exotic cool-season grasses (e.g., Kentucky bluegrass, quackgrass, smooth brome).
Community 2.3
Bare Ground/Halophytes
This community phase is similar to Community Phase 1.3 but now includes exotic cool-season grasses (e.g., Kentucky bluegrass, quackgrass, smooth brome). Common plants often include saltgrass, seaside arrowgrass, red swampfire, and Pursh seepweed. Burningbush (aka kochia) and field sowthistle may also be present. This community phase is often dispersed throughout a pasture in an overgrazed/undergrazed pattern, typically referred to as patch grazing. Some overgrazed areas will exhibit the impacts of heavy use, while the ungrazed areas will have a build-up of litter and increased plant decadence. This is a typical pattern found in properly stocked pastures grazed season long. As a result, Kentucky bluegrass tends to increase more in the undergrazed areas while the more grazing tolerant short statured species, such as blue grama and sedges, increase in the heavily grazed areas. If present, Kentucky bluegrass may increase under heavy grazing. Increasing amounts of exotic cool-season grasses will be dependent upon salinity levels. Higher salinity levels will limit increase in cool-season exotic grasses. Lower salinity levels will facilitate invasion by exotic cool- season grasses, particularly Kentucky bluegrass. If management does not include measures to control or reduce Kentucky bluegrass, the transition to State 3: Invaded State should be expected.
Pathway 2.1a
Community 2.1 to 2.2
Community Phase Pathway 2.1 to 2.2. occurs with multiyear drought with or without heavy, long-term grazing. This results in marked declines in cordgrasses and corresponding increases in foxtail barley and saltgrass.
Pathway 2.2a
Community 2.2 to 2.1
Community Phase Pathway 2.2 to 2.1 occurs with the return to average precipitation and implementation of long-term prescribed grazing. This results in notable decreases in foxtail barley and saltgrass with corresponding increases in cordgrasses.
Pathway 2.2b
Community 2.2 to 2.3
Community Phase Pathway 2.2 to 2.3 occurs with multiyear drought with or without heavy long-term grazing. This resulted in the site becoming characterized by increased areas of bare ground and halophytic vegetation.
Pathway 2.3a
Community 2.3 to 2.2
Community Phase Pathway 2.3 to 2.2 may occur with the return to average precipitation and implementation of long-term prescribed grazing. This results in noticeable decreases in bare ground and halophytes. The wheatgrasses, foxtail barley, saltgrass, and the exotic cool-season grasses are often among the more common plants.
State 3
Invaded
This state is the result of invasion and dominance by the exotic cool-season grasses (e.g., Kentucky bluegrass, smooth brome, quackgrass). Other exotic plants (e.g., field sowthistle, burningbush) may also invade the site. These exotic cool-season grasses can be quite invasive on the site and are particularly well adapted to heavy grazing. They also often form monotypic stands. As these exotic cool-season grasses increase, both forage quantity and quality become increasingly restricted to late spring and early summer due to the monotypic nature of the stand, even though annual production may increase. Native forbs generally decrease in production, abundance, diversity, and richness compared to that of State 1: Reference State. Once the state is well established, prescribed burning and grazing techniques have been largely ineffective in suppressing or eliminating these species, even though some short-term reductions may appear successful. Annual production of this state may vary widely, in part due to variations in the extent of invasion by exotic cool-season grasses. However, as the exotic cool-season grasses increase, peak production will shift to earlier in the growing season.
Characteristics and indicators. This site is characterized by exotic cool-season grasses constituting greater than 30 percent of the annual production and native grasses constituting less than 40 percent of the annual production.
Resilience management. Light or moderately stocked continuous, season-long grazing or a prescribed grazing system which incorporates adequate deferment periods between grazing events and proper stocking rate levels will maintain this State. Application of herbaceous weed treatment, occasional prescribed burning may be needed to manage noxious weeds.
Community 3.1
Exotic Cool Season Grasses/Exotic Forbs
This community phase is often dominated by quackgrass, Kentucky bluegrass, and/or smooth brome. Associated graminoids include foxtail barley, prairie cordgrass, and sedges. Field sowthistle is a common exotic forb. Native forbs may include Norwegian cinquefoil, white panicle aster, as well as the exotic common dandelion. Russian olive is also known to invade the site. The longer this community phase exists, the more resilient it becomes. Natural or management disturbances that reduce the cover of Kentucky bluegrass or smooth brome are typically short-lived.
State 4
Go-Back
This state typically results from the abandonment of cropland or hayland. The site often consists of areas of vegetation and areas of bare ground where salts have accumulated at the soil surface in concentrations that preclude vegetative growth. Vegetation is patchy and variable but often initially consists of a mixture of burningbush (aka kochia) and foxtail barley. Other plants which may be present include Kentucky bluegrass, quackgrass, smooth brome, field sowthistle, Canada thistle, and curlycup gumweed.
Characteristics and indicators. Tillage has destroyed the native plant community, altered soil structure and biology, reduced soil organic matter, and resulted in the formation of a tillage induced compacted layer which is restrictive to root growth. Removal of perennial grasses/forbs changes the predominant water movement from downward to upward. As salt-laden water moves upward, soil salinity increases. Successful restoration to Native/Invaded State 2.0 may be hindered by increased soil surface salinity. Noxious weeds, if present, will need to be managed.
Resilience management. Continued tillage will maintain the state. Control of noxious weeds will be required.
Community 4.1
Annual/Pioneer Perennial/Exotics
This community phase is highly variable depending on the level and duration of disturbance related to the T5A transitional pathway. In this MLRA, the most probable origin of this phase is secondary succession following cropland abandonment. It can also result from heavy season-long grazing. This plant community will initially include a variety of annual forbs (e.g., burningbush, red swampfire) and grasses (e.g., foxtail barley, quackgrass). Over time, a mixture of native and exotic cool-season perennial grasses may become dominant (often quackgrass and Kentucky bluegrass).
State 5
Any Plant Community
Transition T1A
State 1 to 2
This is the transition from the State 1: Reference State to the State 2: Native/Invaded State due to the introduction and establishment of exotic cool-season grasses (e.g., Kentucky bluegrass, smooth brome, quackgrass). The transition was inevitable and corresponded to a decline in native warm-season and cool- season grasses; it may have been exacerbated by chronic season-long or heavy late season grazing. Complete rest from grazing and suppression of fire could also have hastened the transition. The threshold between states was crossed when Kentucky bluegrass, smooth brome, quackgrass, or other exotic species became established on the site.
Constraints to recovery. Current knowledge and technology will not facilitate a successful restoration to Reference State.
Transition T2A
State 2 to 3
This transition from the State 2: Native/Invaded State to State 3: Invaded State generally occurs with long-term non-use or very light grazing, and no fire. Studies indicate that a threshold may exist in this transition when the exotic cool-season grasses exceed 30% of the plant community and native grasses represent less than 40% of the plant community composition. This transition may occur under other managerial conditions, for example heavy season-long grazing (primarily Kentucky bluegrass).
Constraints to recovery. Variations in growing conditions (e.g., cool, wet spring) will influence effects of various management activities on exotic cool-season grass populations.
Restoration pathway R3A
State 3 to 2
This restoration pathway from State 3: Invaded State to State 2: Native/Invaded State may be accomplished with the implementation of long-term prescribed grazing and prescribed burning, assuming there is an adequate component of native grasses to respond to the treatments. Both prescribed grazing and prescribed burning are likely necessary to successfully initiate this restoration pathway, the success of which depends upon the presence of a remnant population of native grasses in Community Phase 3.1. That remnant population, however, may not be readily apparent without close inspection. The application of several prescribed burns may be needed at relatively short intervals in the early phases of this restoration process. Early season prescribed burns have been successful; however, fall burning may also be an effective technique. The prescribed grazing should include adequate recovery periods following each grazing event and stocking levels which match the available resources. If properly implemented, this will shift the competitive advantage from the exotic cool-season grasses to the native cool-season grasses.
Context dependence. Grazing management should be applied in a manner that enhances/maximizes the competitive advantage of native grass and forb species over the exotic species. This may include the use of prescribed grazing to reduce excessive plant litter accumulations above that needed for rangeland health indicator #14 (see Rangeland Health Reference Worksheet). Increasing livestock densities may facilitate the reduction in plant litter provided length and timing of grazing periods are adjusted to favor native species. Grazing prescriptions designed to address exotic grass invasion and favor native species may involve earlier, short, intense grazing periods with proper deferment to improve native species health and vigor. Fall (e.g., September, October) prescribed burning followed by an intensive, early spring graze period with adequate deferment for native grass recovery may shift the competitive advantage to the native species, facilitating the restoration to State 2: Native/Invaded. Prescribed burning should be applied in a manner that enhances the competitive advantage of native grass and forb species over the exotic species. Prescribed burns should be applied at a frequency which mimics the natural disturbance regime, or more frequently as is ecologically (e.g., available fuel load) and economically feasible. Burn prescriptions may need adjustment to: (1) account for change in fine fuel orientation (e.g., “flopped” Kentucky bluegrass); (2) fire intensity and duration by adjusting ignition pattern (e.g., backing fires vs head fires); (3) account for plant phenological stages to maximize stress on exotic species while favoring native species (both cool- and warm-season grasses).
Restoration pathway R4A
State 4 to 2
This Restoration Pathway from State 4: Go-Back State to the State 2: Native/Invaded State can be accomplished with a successful range planting. Following planting, prescribed grazing, prescribed burning, haying, or use of herbicides will generally be necessary to achieve the desired result and control any noxious weeds. It may be possible using selected plant materials and agronomic practices to approach something very near the functioning of State 2: Native/Invaded State. Application of chemical herbicides and the use of mechanical planting methods using adapted varieties of the dominant native grasses are possible and can be successful. After establishment of the native plant species, prescribed grazing should include adequate recovery periods following each grazing event and stocking levels which match the available resources; management objectives must include the maintenance of those species, the associated reference state functions, and continued treatment of exotic grasses.
Context dependence. A successful range planting will include proper seedbed preparation, weed control (both prior to and after the planting), selection of adapted native species representing functional/structural groups inherent to the State 1, and proper planting technique. Management (e.g., prescribed grazing, prescribed burning) during and after establishment must be applied in a manner that maintains the competitive advantage for the seeded native species. Adding non-native species can impact the above and below ground biota. Elevated soil nitrogen levels have been shown to benefit smooth brome and Kentucky bluegrass more than some native grasses. As a result, fertilization, exotic legumes in the seeding mix, and other techniques that increase soil nitrogen may promote smooth brome and Kentucky bluegrass invasion. The method or methods of herbaceous weed treatment will be site specific to each situation; but generally, the goal would be to apply the pesticide, mechanical control, or biological control (either singularly or in combination) in a manner that shifts the competitive advantage from the targeted species to the native grasses and forbs. The control method(s) should be as specific to the targeted species as possible to minimize impacts to non-target species.
Restoration pathway R4B
State 4 to 3
A failed range planting and/or secondary succession will lead to State 3: Invaded State.
Context dependence. Failed range plantings can result from many causes (both singularly and in combination) including drought, poor seedbed preparation, improper planting methods, seeded species not adapted to the site, insufficient weed control, herbicide carryover, poor seed quality (purity & germination), and/or improper management.
Transition T5A
State 5 to 4
This transition from any plant community to State 4: Go-Back State. It is most commonly associated with the cessation of cropping without the benefit of range planting, resulting in a “go-back” situation. Soil conditions can be quite variable on the site, in part due to variations in the management/cropping history (e.g., development of a tillage induced compacted layer (plow pan), erosion, fertility, and/or herbicide/pesticide carryover). Thus, soil conditions should be assessed when considering restoration techniques.
Additional community tables
Table 6. Community 1.1 plant community composition
Group | Common name | Symbol | Scientific name | Annual production (lb/acre) | Foliar cover (%) | |
---|---|---|---|---|---|---|
Grass/Grasslike
|
||||||
1 | Wheatgrass | 570–1140 | ||||
slender wheatgrass | ELTR7 | Elymus trachycaulus | 190–1140 | – | ||
western wheatgrass | PASM | Pascopyrum smithii | 190–1140 | – | ||
2 | Cordgrass | 570–1140 | ||||
prairie cordgrass | SPPE | Spartina pectinata | 190–1140 | – | ||
alkali cordgrass | SPGR | Spartina gracilis | 190–1140 | – | ||
3 | Cool-season Grasses | 380–950 | ||||
Nuttall's alkaligrass | PUNU2 | Puccinellia nuttalliana | 380–760 | – | ||
plains bluegrass | POAR3 | Poa arida | 38–304 | – | ||
foxtail barley | HOJU | Hordeum jubatum | 38–190 | – | ||
Grass, perennial | 2GP | Grass, perennial | 0–190 | – | ||
4 | Warm-season Grasses | 38–380 | ||||
saltgrass | DISP | Distichlis spicata | 38–304 | – | ||
Grass, perennial | 2GP | Grass, perennial | 0–190 | – | ||
scratchgrass | MUAS | Muhlenbergia asperifolia | 38–114 | – | ||
mat muhly | MURI | Muhlenbergia richardsonis | 0–114 | – | ||
5 | Grass-likes | 38–190 | ||||
sedge | CAREX | Carex | 38–190 | – | ||
mountain rush | JUARL | Juncus arcticus ssp. littoralis | 0–114 | – | ||
Grass-like (not a true grass) | 2GL | Grass-like (not a true grass) | 0–114 | – | ||
Forb
|
||||||
6 | Forbs | 38–190 | ||||
silver cinquefoil | POAR8 | Potentilla argentea | 38–76 | – | ||
seepweed | SUAED | Suaeda | 38–76 | – | ||
redwool plantain | PLER | Plantago eriopoda | 0–76 | – | ||
western dock | RUAQ | Rumex aquaticus | 0–76 | – | ||
Pursh seepweed | SUCA2 | Suaeda calceoliformis | 0–76 | – | ||
Forb, native | 2FN | Forb, native | 0–76 | – | ||
Cuman ragweed | AMPS | Ambrosia psilostachya | 0–38 | – | ||
silverscale saltbush | ATAR2 | Atriplex argentea | 0–38 | – | ||
curlycup gumweed | GRSQ | Grindelia squarrosa | 0–38 | – | ||
white prairie aster | SYFA | Symphyotrichum falcatum | 0–38 | – | ||
marsh arrowgrass | TRPA28 | Triglochin palustris | 0–38 | – |
Interpretations
Animal community
Landscape:
The MLRA 55B landscape is characterized by mostly nearly level to gently rolling till plains with some steep slopes adjacent to streams and many poorly defined drainage channels. The continental drainage divide occurs in the east central part of the MLRA. The MLRA is located within the Prairie Pothole Region with temporary, seasonal, and semi-permanent wetlands throughout the MLRA. The MLRA includes areas of eskers, kames, and ground moraines. MLRA 55B is considered to have a continental climate with cold winters and hot summers, low humidity, light rainfall, and much sunshine. Extremes in temperature are common and characteristic of the MLRA. This area supports mid- to tall-grass prairie vegetation with American elm, bur oak, green ash, and willow species growing along the riparian zones of river systems found throughout the MLRA. Complex intermingled ecological sites create diverse grass/shrub land habitats interspersed with varying densities of linear, slope, depressional, and in-stream wetlands associated with headwater streams and tributaries of the James, Pipestem, Maple, Goose, Sheyenne, Wild Rice, and Elm Rivers. MLRA 55B is located within North and South Dakota and within the boundaries of the Prairie Pothole Region.
Three Hydrologic Unit Areas make up this MLRA. Approximately 6% drains into the Mouse River into MLRA 55A, with the balance split between the James and Sheyenne Rivers.
By the mid-19th century, over 76% of the MLRA had been converted from mid- to tall-grass prairie to annual crop production. To alleviate crop production loss from wetlands and overland flow, a system of shallow surface ditches, judicial ditches, and road ditches removes surface water in spring and during high rainfall events. Tile drainage systems have been or are being installed extensively throughout MLRA 55B for sub-surface field drainage to enhance annual crop production.
Historic Communities/Conditions within MLRA 55B:
The northern tall- and mixed-grass prairie were disturbance-driven ecosystems with fire, herbivory, and climate functions as the primary ecological drivers (either singly or often in combination). American bison roamed MLRA 55B, wintering along the Mouse River in MLRA 55A and migrating through MLRA 55B and into MLRA 56A. Many species of grassland birds, small mammals, insects, reptiles, amphibians, elk, moose, pronghorn, white-tailed deer, and large herds of American bison were historically among the inhabitants adapted to this region. Roaming herbivores, as well as several small mammals and insect species, were the primary consumers linking the grassland resources to large predators (such as the wolf, American black bear, grizzly bear) and smaller carnivores (such as the coyote, bobcat, red fox, and raptors). Extirpated species include free- ranging American bison and gray wolf (breeding). Extinct is the Rocky Mountain locust.
Present Communities/Conditions within MLRA 55B:
This area supports natural prairie vegetation characterized by western wheatgrass, green needlegrass, needle and thread, and blue grama. Little bluestem is an important species on the more sloping and shallower soils. Prairie cordgrass, northern reedgrass, big bluestem, and wheat sedge (aka slough sedge) are important species on wet soils. Western snowberry, leadplant, and prairie rose are commonly interspersed throughout the area.
Over 80% of MLRA 55B has been converted to annual crop production. These influences fragmented the landscape, reduced or eliminated ecological drivers (fire), and introduced exotic plant species including smooth brome, crested wheatgrass, Kentucky bluegrass, and leafy spurge; this further impacted plant and animal communities. The loss of the bison and fire as primary ecological drivers greatly influenced the character of the remaining native plant communities and the associated wildlife, moving towards a less diverse and more homogeneous landscape. Annual cropping is the main factor contributing to habitat fragmentation, reducing habitat quality for area- sensitive species.
Hydrological manipulation is extensive throughout the MLRA. Extensive wetland and subsurface tile drainage have taken place. Straightened segments of ephemeral and intermittent tributary streams of the James, Wild Rice, and Sheyenne River have reduced sinuosity, created oxbows, and enabled the conversion of riparian ecological sites to annual crop production. These anthropogenic impacts have reduced flood water detention and retention on the landscape. The results have been increasing storm water runoff sediment and nutrient loading to the James and Sheyenne Rivers and their tributaries (along with lakes and reservoirs within the MLRA). Large dams on the James, Pipestem and Sheyenne rivers, along with installation of instream structures have reduced aquatic species movement within the MLRA.
National wildlife refuges, waterfowl production areas, state wildlife management areas, and North and South Dakota Department of Trust Lands provide herbaceous and woody cover for wildlife. In addition, the United States Army Corps of Engineers and the United States Bureau of Reclamation manage three man-made reservoirs - Jamestown Reservoir, Pipestem Reservoir, and Lake Ashtabula for flood control, also providing fish habitat and adjacent uplands for wildlife cover.
Lonetree Wildlife Management Area (WMA) is the largest state managed wildlife area covering 32,800 acres. Arrowwood National Wildlife Refuge is the largest refuge consisting of 16,000 acres.
Characteristic wildlife species in this area are:
Birds: Common goldeye, bufflehead, broad-winged hawk, alder flycatcher, mourning warbler, mallard, blue-winged teal, red-tailed hawk, American kestrel, killdeer, eastern and western kingbird, western meadowlark, American crow, common yellowthroat, clay-colored sparrow, vesper sparrow, red-necked grebe, Savannah sparrow, downy and hairy woodpeckers, black-capped chickadee, white-breasted nuthatch, and brown-headed cowbird.
Mammals: Northern short-tailed shrew, white-tailed jackrabbit, Franklin’s ground squirrel, thirteen- lined ground squirrel, northern pocket gopher, plains pocket gopher, western harvest mouse, deer mouse, meadow vole, meadow jumping mouse, western jumping mouse, coyote, red fox, racoon, American badger, striped skunk, white-tailed deer, elk, moose, beaver, muskrat, mink, weasel, woodchuck, and red, eastern gray and fox squirrels.
Reptiles/Amphibians: American toad, Great Plains toad, northern leopard frog, chorus frog, tiger salamander, plains garter snake, smooth green snake, wood frog, and common garter snake.
Presence of wildlife species is often determined by ecological site characteristics including grass and forb species, tree and shrub species, hydrology, aspect, and other associated ecological sites. The home ranges of a majority of species are usually larger than one ecological site or are dependent upon more than one ecological site for annual life requisites. Ecological sites offer different habitat elements as the annual life requisites change. Habitat improvement and creation must be conducted within the mobility limits of a known population for the species.
Insects play an important role in providing ecological services for plant community development. Insects that are scavengers or aid in decomposition provide the food chain baseline sustaining the carnivorous insects feeding upon them. Many insects provide the ecological services necessary for pollination, keeping plant communities healthy and productive. Insects provide a protein food source for numerous species including grassland-nesting birds, woodpeckers, woodland edge and interior species, and their young. Extensive use of insecticides for specialty crops such as soybeans, corn, and other crops has greatly reduced insects within this MLRA.
Species of Concern within MLRA 55B:
The following is a list of species considered “species of conservation priority” in the North Dakota State Wildlife Action Plan (2015) and South Dakota State Wildlife Action Plan (2014); and species listed as “threatened, endangered, or petitioned” under the Endangered Species Act within MLRA 55B at the time this section was developed:
Invertebrates: Dakota skipper, Iowa skipper, monarch butterfly, northern sandy tiger beetle, Ottoe skipper, Poweshiek skipperling, regal fritillary, yellow-banded bumble bee, and western bumble bee.
Birds: America avocet, American bittern, American kestrel, American white pelican, Baird’s sparrow, bald eagle, black-billed cuckoo, black tern, bobolink, burrowing owl, canvasback, chestnut-collared longspur, Dickcissel, ferruginous hawk, Franklin’s gull, grasshopper sparrow, horned grebe, lark bunting, LeConte’s sparrow, lesser scaup, marbled godwit, Nelson’s sparrow, northern goshawk, northern harrier, northern pintail, osprey (migration), peregrine falcon (migration), piping plover (migration), red knot (migration), sharp-tailed grouse, short-eared owl, Swainson’s hawk, upland sandpiper, western meadowlark, willet, Wilson’s phalarope, whooping crane (migration), and yellow rail.
Mammals: Arctic shrew, big and little brown bats, Franklin’s ground squirrel, northern river otter, plains pocket mouse, pygmy shrew, Richardson’s ground squirrel, and silver-haired bat.
Amphibians and Reptiles: Canadian toad, plains hognose snake, smooth green snake, and snapping turtle.
Fish and Mussels: Black sandshell, blacknose shiner, Carmine shiner, creek heelsplitter, creeper, deertoe, fragile papershell, mapleleaf, northern pearl dace, northern redbelly dace, pink heelsplitter, threeridge, trout-perch, yellow sandshell, and Wabash pigtoe.
Grassland Management for Wildlife in MLRA 55B:
Management activities within the community phase pathways impact wildlife but are essential for maintenance of healthy grassland ecosystems. Community phase, transitional, and restoration pathways are keys to long-term management within each State and between States. Timing, intensity, and frequency of these inputs can have dramatic positive or negative effects on local wildlife species. Ranchers and other land managers must always consider the long-term beneficial management effects of grassland and woodland resources in comparison to typically short-term negative effects to the habitats of individual species.
Ecological sites occur as intermingled complexes on the landscape with gradual or sometimes abrupt transitions. Rarely do ecological sites exist in large enough acreage to manage independently.
Ecological sites supporting a dominance of herbaceous vegetation (Loamy/Sandy) can be located adjacent to ecological sites that support medium to tall shrubs (Loamy Overflow or Loamy-Wooded State). Conversely, ecological sites that are dominated by short- to mid-statured grasses (Claypan) can be adjacent to sites with bare soil only supporting a minor amount of short grasses and forbs (Thin Claypan).
Management of these complex ecological sites can provide a heterogeneous or a homogenous landscape. Grassland bird use reduces as the plant community transitions to a homogenous state. Managers must recognize ecological sites and the complexes in which they occur to properly manage the landscape. A management regime for one ecological site may negatively impact an adjacent site; for example, alteration of a grazing regime within the Invaded Wooded State in a Loamy ecological site to encourage understory growth may encourage exotic cool-season grasses to increase or dominate an adjacent ecological site.
Life requisites and habitat deficiencies are determined for targeted species. Deficiencies need to be addressed along community phase, transitional, and restoration pathways as presented in specific state-and-transition models. Ecological sites should be managed and restored within the site’s capabilities to provide sustainable habitat for targeted species or species guilds. Managers also need to consider vegetative associations provided by adjacent/intermingled ecological sites for species with home ranges or life requisites that may not be provided by one ecological site.
Grassland-nesting birds use various grass heights for breeding, nesting, foraging, or winter habitat. While most species use varying heights, many have a preferred vegetative stature height or sensitivity to woody vegetation. Understanding the sensitivity of grassland species to woody vegetation and preferred vegetative structure enables managers to determine which grassland-nesting bird species avoid grassland habitats adjacent to woody dominated plant community phases. The following chart provides sensitivity to woody vegetation and preferred vegetative stature heights.
To see the chart please follow the hyperlink: https://efotg.sc.egov.usda.gov/references/public/ND/55B_Saline_Lowland_Narrative_FINAL_Ref_FSG.pdf
Saline Lowland Wildlife Habitat Interpretation:
Saline Lowland ecological sites are poorly drained; soluble salts are present within the rooting zone (typically at the surface) and significantly impact the plant community. The surface can become nearly barren due to the presence of salts. In some soils, subsurface soil layers may be restrictive to water movement and root penetration. Associated ecological sites commonly include Limy Subirrigated, Sodic Subirrigated, Thin Claypan, Shallow Marsh, Wet Meadow, Loamy Overflow, and Sandy Claypan. This complex of ecological sites provides habitat for many edge-sensitive, grassland bird species preferring medium- to tall-statured vegetation.
Saline Lowland habitat features and components commonly support grassland-nesting birds that prefer short- to medium stature vegetation. Low diversity and density of forb species provide limited pollen and nectar resources for pollinating insects. In turn, invertebrate production is low, providing limited protein resources for grassland-nesting birds. Saline Lowland ecological sites provide forage for small and large herbivores.
Saline Lowland ecological sites may be found in four plant community states (1.0 Reference State, 2.0 Native/Invaded State, 3.0 Invaded State, and 4.0 Go-Back State) within a local landscape. Multiple plant community phases exist within States 1.0 and 2.0. Today, these states occur primarily in response to drought, fire, grazing, and non-use and other anthropogenic disturbances.
Because there is no known restoration pathway from State 2.0 to State 1.0, it is important to intensively manage using Community Phase Pathways in State 1.0 to prevent further plant community degradation along the T1A Transitional Pathway to State 2.0. Native wildlife generally benefits from the heterogeneous grasslands found in State 1.0 that include grass and forb species of varying stature and density. As plant communities degrade and transition to State 2.0, foxtail barley increases while native forbs are reduced.
Management along community phase, transition, or restoration pathways should focus upon attainable changes. Short- and long-term monetary costs must be evaluated against short- and long- term ecological services in creating and maintaining habitat of enough quality to support a sustainable population density.
1.0 Reference State
Community Phase 1.1 Wheatgrasses-Cordgrasses-Nuttall’s Alkaligrass: These plant communities offer quality vegetative cover for wildlife; if found, every effort should be made to maintain this ecological site within this community phase. This phase retains high functionality through continued maintenance including prescribed grazing with adequate recovery period as well as prescribed fire. Prescribed fire frequency maintains a grass-dominated plant community providing habitat for bird species that are sensitive to woody vegetation. Predominance of grass species in these communities favors grazers and mixed-feeders (animals selecting grasses as well as forbs and shrubs). The structural diversity provides habitat for a wide array of migratory and resident birds.
Invertebrates: Insects play a role in maintaining the forb community and provide a forage base for grassland birds, reptiles, and rodents. Ecological services, historically provided by bison, are simulated by domestic livestock. These services include putting plant material and dung in contact with mineral soil to be used by lower trophic level consumers (such as invertebrate decomposers, scavengers, shredders, predators, herbivores, dung beetles, and fungal feeders). As salinity levels increase, invertebrate activity may decrease.
Dakota skippers do not prefer this site due to salinity and wetness along with limited host plants, such as little bluestem and prairie dropseed. Regal fritillary habitat is limited due to salinity and wetness and the short stature of this plant community and uncommon Nuttall’s and prairie violets. Monarch butterflies may use limited flowering forbs on this site; however, no milkweed species are found on this site to support caterpillar food. Overall nectar and pollen availability are limited due to low forb diversity due the combination of salinity and wetness. Bumblebees and other native bees utilize limited forbs as a nectar source. Although bare ground is common, wetness and salinity will limit nesting.
Birds: This plant community provide limited nesting, foraging, and escape habitats favored by short- to mid-grass-nesting birds. In association with Wet Meadow, this site may provide foraging sites for shore birds. This site provides limited hunting opportunities for grassland raptors.
Mammals: Limited diversity of grasses and forbs provide reduced nutrition levels for small and large herbivores including voles, mice, jackrabbits, and white-tailed deer. This site has less diversity and shorter plant stature compared to associated sites (such as Wet Meadow, Shallow Marsh, Limy Subirrigated and Loamy Overflow). Short- to mid-statured vegetation, wetness, and salinity provide limited food and thermal, protective, and escape cover for small herbivores.
Amphibians and Reptiles: Due to potential high salinity levels and wetness, these ecological sites do not provide suitable habitat for many amphibians and reptiles except during periods of above normal precipitation reducing the effects of high salinity levels. Ponded water during above average precipitation events will provide foraging habitat for the northern leopard frog and Canadian toad, depending upon salinity levels. Ponded water will not be deep enough to provide breeding habitat.
Fish and Mussels: These ecological sites can be located adjacent to streams, rivers, or water bodies. These sites receive run-on hydrology from adjacent ecological sites and provide hydrology to Wet Meadow or Shallow Marsh ecological sites. Management on Saline Lowland sites, in conjunction with neighboring run-on sites, can have a direct effect on aquatic species in streams and/or tributaries receiving water from Saline Lowland and adjacent sites. Optimum hydrological function and nutrient cycling limit potential for sediment yield and nutrient loading to the adjacent aquatic ecosystems from Community Phase 1.1.
Community Phase 1.2 Wheatgrasses-Foxtail Barley-Saltgrass: Multiyear drought, with or without heavy grazing, with lack of recovery periods gives foxtail barley and other salt tolerant grasses a competitive edge. This plant community is adapted to increased salinity and is relatively stable. Every effort should be made to manage this plant community via Community Pathway 1.2A (prescribed grazing with adequate recovery periods) to move back to Plant Community Phase 1.1. Improper management such as heavy continuous season-long grazing will transition this plant community to State 2.0, increasing abundance of foxtail barley, inland saltgrass, and bare ground. Structural diversity and density reduce habitat for a wide array of migratory and resident birds.
Invertebrates: Provides similar life requisites as Community Phase 1.1. However, heavy continuous grazing with lack of recovery periods further reduces density and diversity of pollinating forb species.
Birds: Heavy continuous grazing with lack of recovery periods gives foxtail barley, inland saltgrass, and other salt tolerant grasses a competitive edge reducing density and stature of grasses.
Grassland nesting birds, favoring short statured structure, may use this plant community. Dependent upon water depth and duration, this plant community may be attractive to various shorebirds.
Mammals: This site is no longer favored by large herbivores and provides limited life requests for small herbivores.
Amphibians and Reptiles: Provides similar life requisites as Community Phase 1.1.
Fish and Mussels: Provides similar life requisites as Community Phase 1.1; however, increased bare ground will yield additional sediment to nearby water bodies.
Community Phase 1.3 Bare Ground/Halophytes: This plant community phase is characterized by bare ground and halophytes. Continued heavy grazing, repeated drought, or a combination of these disturbances will shift to increased bare ground and halophytes with a reduction in perennial grasses. Moderate perennial forb stature and abundance are being replaced by short-statured halophytes. Bare ground increases and litter amounts and infiltration rates decline while soil surface temperatures increase. Although, this plant community is resilient, retaining sufficient grazing sensitive native plant species to return to the 1.1 community phase (via Community Phase Pathway 1.3A) will take long term management.
Invertebrates: A switch to mainly halophytes will have a significant impact to invertebrates due to the reduction of season-long nectar and pollen. Season-long nectar sources may be found on adjacent plant communities or ecological sites for mobile species. Increased bare ground provides increased nesting sites for bumble bees and other ground-nesting insects but, due to wetness and salinity, will not provide quality nesting sites.
Birds: Bare ground coupled with salinity will not provide adequate habitat for grassland nesting birds. Dependent upon water depth and duration, this plant community may be attractive to various shorebirds.
Mammals: Bare ground and the loss of grasses provides limited food, thermal cover, and escape cover for most mammals.
Amphibians and Reptiles: Provides similar life requisites as Community Phase 1.1.
Fish and Mussels: Provides similar life requisite benefits as Community Phase 1.1.
2.0 Native/Invaded State
Community Phase 2.1 Wheatgrasses-Cordgrasses-Nuttall’s Alkaligrass: Introduction and establishment of exotic cool-season grasses, coupled with chronic season-long or heavy late season grazing without adequate recovery periods (along Transition Pathway T1), causes native forbs to decrease in production, abundance, diversity, and richness. Bare ground has increased due to the presence of alkaligrass.
Invertebrates: Provides similar life requisites as Community Phase 1.1. Birds: Provides similar life requisites as Community Phase 1.1.
Mammals: Provides similar life requisites as Community Phase 1.1.
Amphibians and Reptiles: Provides similar life requisites as Community Phase 1.1.
Fish and Mussels: Provides similar life requisites as Community Phase 1.1
Community Phase 2.2 Wheatgrasses-Foxtail Barley-Saltgrass: Multiyear drought (with or without heavy, long-term grazing) results in a marked decline in cordgrass and corresponding increases in foxtail barley and saltgrass.
Invertebrates: Provides similar life requisites as Community Phase 1.2. Birds: Provides similar life requisites as Community Phase 1.2.
Mammals: Provides similar life requisites as Community Phase 1.2.
Amphibians and Reptiles: Provides similar life requisites as Community Phase 1.1.
Fish and Mussels: Provides similar life requisites as Community Phase 1.2.
Community Phase 2.3 Bare Ground/Halophytes: This plant community phase is characterized by bare ground and grazing-tolerant exotic grasses and annual forbs. Continued heavy long-term grazing will shift this plant community to increased bare ground with exotic grasses (such as Kentucky bluegrass, quackgrass, and annual forbs). Native forbs may include silverleaf cinquefoil, western dock, redwool plantain, seaside arrowgrass, red swampfire, and Pursh seepweed. The forbs are mainly wind-pollinated. This plant community is resilient, retaining sufficient grazing sensitive native plant species to return to the 2.1 community phase (via Community Phase Pathway 2.3A).
Invertebrates: Provides similar life requisites as Community Phase 1.3.
Birds: Heavy, long-term grazing increase bare ground and coupled with salinity will not provide adequate habitat for grassland nesting birds.
Mammals: Heavy, long-term grazing increases bare ground; with the loss of grasses, this plant community provides limited food, thermal cover, and escape cover for most mammals.
Amphibians and Reptiles: Provides similar life requisites as Community Phase 1.1.
Fish and Mussels: Provides similar life requisite benefits as Community Phase 1.1.
3.0 Invaded State
Community Phase 3.1 Exotic Cool-Season Grasses/Forbs: Extended periods of non-use and no fire, or continuous season long grazing (via Transitional Pathway T2A) results in a plant community phase dominated by smooth brome and Kentucky bluegrass with other species difficult to find on the site.
Restoration Pathway R3A, through prescribed burning, chemical treatment mechanical replanting, and/or high levels of grazing management, requires remnant amounts of native warm- and cool- season and forbs to be successful. The remnant native community needs frequent prescribed burns and high levels of grazing management targeting the exotic cool-season grasses to improve competitiveness and increase vigor and density. Without intensive management, the remnant native plants will not increase adequately to transition back to State 2.0. Intensified management along the R3A Pathway will have significant short-term negative impacts on wildlife habitat; however, this is necessary to restore long-term native habitat functions.
Invertebrates: Exotic grasses limits use by beneficial insects provided in States 1.0 and 2.0. Increased litter and lack of grazing leads to limited contact between plant material and mineral soil resulting in a cooler micro-climate, which is unfavorable to most insects. Lack of nectar-producing plants and native forb and grass host plants eliminates life requisites for invertebrate species of concern in MLRA 55B. Heavy continuous season-long grazing reduces forb diversity and abundance, limiting nectar and pollen availability.
Birds: The homogeneous community phase, dominated by exotic plant species, provides limited habitat and life requisites for most obligate grassland-nesting birds. Lack of plant diversity and stature (along with increased litter and the tendency of Kentucky bluegrass and smooth brome to lay down) limits use by many grassland-nesting birds. Sharp-tailed grouse may use this plant community for lek sites and nesting cover; however, winter cover must be provided by adjacent ecological sites or plant communities. Heavy continuous season-long grazing reduces or eliminates nesting cover and insect populations for food sources.
Mammals: Litter accumulation and exotic grass cover favors thermal, protective, and escape cover for small rodents. Thermal, protective, or escape cover is limited for large mammals. Heavy continuous season-long grazing reduces or eliminates thermal cover for most mammals.
Amphibians and Reptiles: Provides similar life requisites as Community Phase 1.1.
Fish and Mussels: Provides similar life requisites as Community Phase 1.1
4.0 Go-Back State
Community Phase 4.1 Annual/Pioneer Perennial/Exotics: These plant communities are the result of severe soil disturbance (such as cropping, recreational activity, or concentrated livestock activity for a prolonged period). Following cessation of disturbances, the resulting plant community is dominated by early pioneer annual and perennial plant species. Plant species composition and production are highly variable. Weedy plants can provide pollinator habitat along with spring and summer cover for many mammals and birds, and their young. The response by wildlife species will be dependent upon plant community composition, vegetative stature, patch size, and management activities (such as prescribed grazing, burning, inter-seeding, haying, or noxious weed control).
Successful restoration of native species along Transitional Pathway R3A can result in a native grass and forb community in State 2.0. Over time, with no management, the exotic cool-season perennial grasses (Kentucky bluegrass, smooth brome, and/or quackgrass) generally become re-established and dominate the community. Successful range planting, via Transition Pathway R4A, can result in State 2.0. Prescribed grazing and/or fire will be needed to maintain this plant community within State 2.0. Failed native range planting, along Transitional Pathway R4B, will keep this plant community within Invaded State 3.0.
Animal Community – Grazing Interpretations
This site is well adapted to managed grazing by domestic livestock. The predominance of herbaceous plants across all plant community phases best lends these sites to grazing by cattle, but other domestic grazers with differing diet preferences may also be a consideration depending upon management objectives. Often, the current plant community does not match any particular plant community (as described in the ecological site description). Because of this, a resource inventory is necessary to document plant composition and production. Proper interpretation of this inventory data will permit the establishment of a safe, initial stocking rate for the type and class of animals and level of grazing management. More accurate stocking rate estimates should eventually be calculated using actual stocking rate information and monitoring data.
NRCS defines prescribed grazing as “managing the harvest of vegetation with grazing and/or browsing animals with the intent to achieve specific ecological, economic, and management objectives”. As used in this site description, the term ‘prescribed grazing’ is intended to include multiple grazing management systems (e.g., rotational grazing, twice-over grazing, conservation grazing, targeted grazing, etc.) provided that, whatever management system is implemented, it meets the intent of prescribed grazing definition.
The basic grazing prescription addresses balancing forage demand (quality and quantity) with available forage, varying grazing and deferment periods from year-to-year, matching recovery/deferment periods to growing conditions when pastures are grazed more than once in a growing season, implementation of a contingency (e.g., drought) plan, and a monitoring plan. When the management goal is to facilitate change from one plant community phase or state to another, then the prescription needs to be designed to shift the competitive advantage to favor the native grass and forb species.
Grazing levels are noted within the plant community narratives and pathways in reference to grazing/prescribed grazing management. “Degree of utilization” is defined as the proportion of the current years forage production that is consumed and/or destroyed by grazing animals (may refer to a single plant species or a portion or all the vegetation). “Grazing utilization” is classified as slight, moderate, full, close, and severe (see the following table for description of each grazing use category). The following utilization levels are also described in the Ranchers Guide to Grassland Management IV. Utilization levels are determined by using the landscape appearance method as outlined in the Interagency Technical Reference “Utilization Studies and Residual Measurements” 1734-3.
Utilization Level % Use Description
Slight (Light) 0-20 Appears practically undisturbed when viewed obliquely. Only choice areas and forage utilized.
Moderate 20-40 Almost all of accessible range shows grazing. Little or no use of poor forage. Little evidence of trailing to grazing.
Full 40-60 All fully accessible areas are grazed. The major sites have key forage species properly utilized (about half taken, half left). Points of concentration with overuse limited to 5 to 10 percent of accessible area.
Close (Heavy) 60-80 All accessible range plainly shows use and major sections closely cropped. Livestock forced to use less desirable forage, considering seasonal preference.
Severe > 80 Key forage species completely used. Low-value forages are dominant.
Hydrological functions
Available water is the principal factor limiting forage production on this site. Soil salinity significantly reduces the availability of water (hinders osmosis) to plants growing on the site. Under natural conditions, this site is dominated by soils in hydrologic groups B and C, but incudes some soils in group D. Where the natural hydrology has been altered, the soils are predominantly in hydrologic groups B/D and C/D with some soils in group A/D. Infiltration varies from slow to moderately rapid (depending upon surface soil texture and structure); runoff potential varies from negligible to low depending on soil hydrologic group, surface texture, slope and ground cover.
Hydrological manipulation (surface or tile drainage, pumping, surface water diversion, etc.) modifies this ecological site. Under natural conditions, this ecological site includes a wide range of soil textures; after hydrologic manipulation, soil texture often becomes a more significant factor in vegetative response if the degree salinity is also reduced. Where a vegetation change has occurred; a transition to a completely different ecological site may also have occurred. The transition to an altogether different ecological site will depend upon severity of altered hydrology, soil properties, and corresponding vegetation. Due to the many variables (e.g., hydrology, type and success of drainage, etc.), impacts to the ecological site will be site-specific. As a result, each situation will require field investigation to determine what, if any, change in ecological site designation is necessary and proceed accordingly.
Without restoring hydrologic function (which may include range planting), managers need to reference state and transition models within those sites. Hydrology will need to be fully restored in Wet Meadow and Shallow Marsh ecological sites for these sites to properly function. It is recommended that managers review the appropriate State and Transition Models prior to wetland restoration.
Recreational uses
Hunting and Bird Watching: National wildlife refuges, waterfowl production areas, state wildlife management areas (WMA), and North Dakota and South Dakota Department of Trust Lands provide herbaceous and woody cover for wildlife. National Wildlife Refuges and waterfowl production areas are owned and managed by the United States Fish and Wildlife Service and are available for public hunting, hiking, and bird watching. In addition, the United States Army Corps of Engineers and the United States Bureau of Reclamation manage three man-made reservoirs - Jamestown Reservoir (2,036 acres), Pipestem Reservoir (1,027 acres), and Lake Ashtabula (5,174 acres) for flood control, also providing fish habitat and adjacent uplands for wildlife cover.
Lonetree WMA is the largest state managed wildlife area covering 32,800 acres. Numerous WMAs in North Dakota and Game Production Areas in South Dakota are found within this MLRA. The largest refuges managed by the United States Fish and Wildlife service are Arrowwood National Wildlife Refuge (NWR) Complex consists of 75,000 acres and Tewaukon National NWR covers 8,363 acres.
Fishing: Approximately 100 lakes are managed for public fishing within MLRA 55B. Most of these lakes offer boat docks and ramps. These lakes contain various sport fish including walleye, northern pike, yellow perch, catfish, trout, crappie, and bluegill. Many of these lakes are known for excellent round-around walleye and yellow perch fishery.
Camping: Fort Ramson State Park, Pipestem Reservoir, Jamestown Reservoir, Spiritwood Lake, Clausen Springs, Little Yellowstone, Richmond Lake State Recreation Area, Mina Lake State Recreation Area, and other public and private campgrounds are found within the MLRA. Limited, primitive camping is available on wildlife management areas. Ft. Ransom State Park (North Dakota), located along the Sheyenne River has a designated horse park with 15 miles of trails.
Hiking/Biking/Horseback Riding: Horseback riders, hikers, and biker can enjoy over 15 miles of multi-use trails at Fort Ransom State Park. The Jamestown Reservoir (5 miles), Pipestem Reservoir (8 miles) and Arrowwood National Wildlife Refuge (9.4 miles) maintain hiking trails. The Lonetree Wildlife Management Area has a 32- mile segment of the North Country Trail. It is designed for hiking and non-motorized travel including mountain bikes or horseback riding.
Canoeing/Kayaking: The Sheyenne River offers 278 miles of canoeing/kayaking from May-July. A kayak kiosk is located at Valley City and canoe/kayak rentals are available at Fort Ransom State Park. The James River has a canoe trail starting in Grand Rapids and canoeing down to the James River Dam site in LaMoure; no rentals are available.
Auto Tour: A 63-mile scenic drive starts north of Valley City and heading south through Sheyenne River Valley. Audubon National Wildlife Refuge offers a 5.5-mile auto-tour route winding through both prairie grassland and wetland habitats of the lower portion of the James River Valley.
Wood products
There are no significant wood products found on this site.
Other products
Seed harvest of native plant species can provide additional income on this site.
Other information
Site Development and Testing Plan
• Further investigation is needed on the wide range of landforms and soil textures (and associated properties) and their relationship to hydrology/plant dynamics.
-Further investigation is needed on poorly drained claypan soils included in this site as compared to other soils in the site.
• Further investigation is needed on areas of this site associated with drainageways and flood plains. Harriet and Lowe occur in drainageways as do some Marysland soils. Lamoure, Ludden, and Ryan soils occur on flood plains of streams and rivers. The impact of occasional or frequent flooding on these areas needs evaluation.
• Further investigation of areas of this site on lake shores and in shallow lake basins is needed. These areas are periodically inundated for extended periods. When many of the soil surveys were completed, these soils were not inundated; currently many of these sites are inundated and have been for many consecutive years. Major components in this site affected by recent inundation are Lallie and Minnewaukan. Some delineations of these soils have been impacted by the construction of a dike along the shores of Devils Lake protecting some areas from flooding while maintaining inundation on other areas. Along with ecological site investigations, an SDJR project is needed for these with some soil spatial data review. Spatial data revisions may be needed. MLRA map units needing investigation are:
- Lallie, saline-Minnewaukan complex, 0 to 2 percent slopes (map unit 2q5n3)
- Mauvais-Minnewaukan, saline complex, 0 to 6 percent slopes (map unit 2q5mv)
• Further evaluation and refinement of the State-and-Transition model may be needed to identify disturbance driven dynamics. Additional states and/or phases may be required to address grazing response.
• Further documentation may be needed for plant communities in all states. Plant data has been collected in previous range-site investigations, including clipping data; however, this data needs review. If geo-referenced sites meeting Tier 3 standards for either vegetative or soil data are not available, representative sites will be selected for further investigation.
• Site concepts will be refined as the above noted investigations are completed.
• The long-term goal is to complete an approved, correlated Ecological Site Description as defined by the National Ecological Site Handbook.
-NASIS revisions needed:
During the recently completed Ecological Site Description update, saline phases of Aeric Calciaquolls were reassigned from Saline Lowland to the Salinized State of Limy Subirrigated. Numerous components of Bearden, Doran, Fram, Glyndon, Hamerly, and Wyndmere need to be relinked, as well as one component each of Antler and Moritz.
During the recently completed Ecological Site Description update, the Sodic Subirrigated ecological site was developed; all Stirum and Totten components need to be relinked from Saline Lowland to Sodic Subirrigated.
This ESD is the best available knowledge. The site concept and species composition table have been used in the field and tested for more than five years. It is expected that as additional information becomes available revisions may be required.
Supporting information
Inventory data references
Information presented here has been derived from NRCS and other federal/state agency clipping and inventory data. Also, field knowledge of range-trained personnel was used. All descriptions were peer reviewed and/or field-tested by various private, state and federal agency specialists.
Other references
Bakker, K.K. 2003. The effect of woody vegetation on grassland nesting birds: an annotated bibliography. The Proceedings of the South Dakota Academy of Science 82:119-141.
Barker, W.T. and W. C. Whitman. 1988. Vegetation of the Northern Great Plains. Rangelands 10(6): 266-272. Bluemle. J.P. 2016. North Dakota’s geologic legacy. North Dakota State University Press. 382 pages.
Briske, D.D. (editor). 2017. Rangeland systems – processes, management, and challenges. Springer Series on Environmental Management. 661 pages.
Burgess, R.L. 1965. A study of plant succession in the sandhills of southeastern North Dakota. Proceedings ND Academy of Science 19:62-80
DeKeyser, E.S., G. Clambey, K. Krabbenhoft, and J. Ostendorf. 2009. Are changes in species composition on central North Dakota rangelands due to non-use management? Rangelands 31:16-19
Dix, R.L. and F.E. Smeins. 1967. The prairie, meadow, and marsh vegetation of Nelson County, North Dakota. Canadian Journal of Botany 45:21-57.
Dornbusch, M.J., R.F. Limb, and C.K. Gasch. 2018. Facilitation of an exotic grass through nitrogen enrichment by an exotic legume. Rangeland Ecology & Management 71:691-694.
Dyke, S.R., S.K. Johnson, and P.T. Isakson. 2015. North Dakota state wildlife action plan. North Dakota Game and Fish Department, Bismarck, ND. 468 pages.
Ehrenfeld, Joan G. 2002. Effects of exotic plant invasions on soil nutrient cycling processes. Ecosystems 6:503-523.
Endangered and threatened wildlife and plants; designation of critical habitat for the Dakota skipper and Poweshiek skipperling; Vol. 79 No. Final Rule October 1, 2015, 50 CFR Part 17.
Ereth, C., J. Hendrickson, D. Kirby, E. DeKeyser, K. Sedevic, and M. West. Controlling Kentucky bluegrass with herbicide and burning is influenced by invasion level. Invasive Plant Science and Management 10: 80-89.
Ewing, J. 1924. Plant succession on the brush prairie in northwestern Minnesota. Journal of Ecology 12:228- 266.
Gilgert, W.; and S. Zack. 2010. Integrating multiple ecosystem services introduction ecological site descriptions. Rangelands: 32:49-54.
Grant, T.A. and R.K. Murphy. 2005. Changes on woodland cover on prairie refuges in North Dakota, USA. Natural Areas Journal 25:359-368.
Heitschmidt, R. K., K. D. Klement, and M. R. Haferkamp. 2005. Interactive effects of drought and grazing on Northern Great Plains rangelands. Rangeland Ecology and Management 58:11-19.
Hendrickson, J.R., P. S. Johnson, M. A. Liebig, K. K. Sedivec, and G. A. Halvorson. 2016. Use of ecological sites in managing wildlife and livestock: an example with prairie dogs. Rangelands
Hendrickson, J.R., S.L. Kronberg, and E.J. Scholljegerdes. 2020. Can targeted grazing reduce abundance of invasive perennial grass (Kentucky bluegrass) on native mixed-grass prairie? Rangeland Ecology and Management, 73:547-551.
Higgins, K.F. 1984. Lightning fires in grasslands in North Dakota and in pine-savanna lands in nearby South Dakota and Montana. J. Range Manage. 37:100-103.
Higgins, K.F. 1986. Interpretation and compendium of historical fire accounts in the Northern Great Plains. United States Department of Interior, Fish and Wildlife Service. Resource Publication 161. 39 pages.
Higgins, K.F., A.D. Kruse, and J.L. Piehl. 1989. Effects of fire in the Northern Great Plains. U.S. Fish and Wildlife Service and Cooperative Extension Service South, Dakota State University. Extension Circular 761. 48 pages.
High Plains Regional Climate Center, University of Nebraska, 830728 Chase Hall, Lincoln, NE 68583-0728. (http://hprcc.unl.edu)
Johnson, Sandra. 2015. Reptiles and amphibians of North Dakota. North Dakota Game and Fish Department. 64 pages.
Jordan, N. R., D.L. Larson, and S.C. Huerd. 2008. Soil modification by invasive plants: effects on native and invasive species of mixed-grass prairies. Biological Invasions 10:177-190
Mader, E., M. Shepherd, M. Vaughan, and S.H. Black. 2011. Attracting native pollinators: protecting North America's bees and butterflies. Accessed at https://xerces.org, May 1, 2017.
North Dakota Division of Tourism, Accessed on February 25, 2019. Available at https://www.ndtourism.com/sports-recreation
North Dakota Parks and Recreation Department, Accessed on February 25, 2019. Available at http://www.parkrec.nd.gov/recreationareas/recreationareas.html
Palit, R., G. and E.S. DeKeyser. 2022. Impacts and drivers of smooth brome (Bromus inermis Leyes.) invasion in native ecosystems. Plants: 10,3390. http://https://www.mdpi.com/2223-7747/11/10/1340
Palit, R., G. Gramig, and E.S. DeKeyser. 2021. Kentucky bluegrass invasion in the Northern Great Plains and prospective management approaches to mitigate its spread. Plants: 10,817. https://doi.org/10.3390/plants10040817
Printz, J.L. and J.R. Hendrickson. 2015. Impacts of Kentucky bluegrass Invasion (Poa pratensis) on ecological processes in the Northern Great Plains. Rangelands 37(6):226-232.
Redmann, Robert E. 1975. Production ecology of grassland plant communities in western North Dakota. Ecological Monographs 45:83-106.
Reeves, J.L., J.D. Derner, M.A. Sanderson, J.R. Hendrickson, S.L. Kronberg, M.K. Petersen, and L.T. Vermeire. 2014. Seasonal weather influences on yearling beef steer production in C3-dominated Northern Great Plains rangeland. Agriculture, Ecosystems and Environment 183:110-117.
Royer, R. A., 2003. Butterflies of North Dakota: an atlas and guide. Minot State University, Minot, ND.
Seabloom, R. 2020. Mammals of North Dakota. North Dakota Institute for Regional Studies, Fargo, ND. 470 pages.
Sedivec, K.D., J.L. Printz. 2014. Ranchers guide to grassland management IV. NDSU Extension Service publication R1707.
Severson, K. E. and C. Hull Sieg. 2006. The nature of eastern North Dakota: Pre-1880 Historical Ecology. North Dakota Institute for Regional Studies.
South Dakota Dept. of Game, Fish and Parks. 2014. South Dakota wildlife action plan. Wildlife Division Report 2014-03.
Spaeth, K.E., Hayek, M.A., Toledo, D., and Hendrickson, J. 2019. Cool season grass impacts on native mixedgrass prairie species in the Norther Great Plains. America’s Grassland Conference: Working Across Boundaries. The Fifth Biennial Conference on the Conservation of America’s Grasslands. Bismarck, ND. 20- 22 August.
Tidwell, D., D.T. Fogarty, and J.R. Weir. 2021. Woody encroachment in grasslands, a guide for understanding risk and vulnerability. Oklahoma State University, Oklahoma Cooperative Extension Service publication E- 1054. 32 pages.
Toledo, D., M. Sanderson, K. Spaeth, J. Hendrickson, and J. Printz. 2014. Extent of Kentucky bluegrass and its effect on native plant species diversity and ecosystem services in the Northern Great Plains of the United State. Invasive Plant Science and Management 7(4): 543-552.
USDA, NRCS. 2021. National Range and Pasture Handbook, (https://www.nrcs.usda.gov/wps/portal/nrcs/detailfull/national/landuse/rangepasture/?cid=stelprdb1043084)
USDA, NRCS. 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.
USDA, NRCS. National Soil Information System, 100 Centennial Mall North, Room 152, Lincoln, NE 68508- 3866. (https://www.nrcs.usda.gov/wps/portal/nrcs/detail/soils/survey/tools/?cid=nrcs142p2_053552)
USDA, NRCS. National Water & Climate Center, 1201 NE Lloyd Blvd, Suite 802, Portland, OR 97232-1274. (https://www.wcc.nrcs.usda.gov/)
USDA, NRCS. 2001. The PLANTS Database, Version 3.1 (http://plants.usda.gov). National Plant Data Center, Baton Rouge, LA 70874-4490 USA.
USDA, NRCS, Various Published Soil Surveys.
USDI BLM.1999. Utilization studies and residual measurements. Interagency Technical Reference 1734-3.
Vinton, M.A. and E.M. Goergen. 2006. Plant-soil feedbacks contribute to the persistence of Bromus inermis in tallgrass prairie. Ecosystems 9: 967-976.
Whitman, W.H., H. Hanson, and R. Peterson. 1943. Relation of drought and grazing to North Dakota range lands. North Dakota Agricultural Experimentation Bulletin 340.
Contributors
David Dewald
Jonathan Fettig
Alan Gulsvig
Mark Hayek
Chuck Lura
Jeff Printz
Steve Sieler
Hal Weiser
Approval
Suzanne Mayne-Kinney, 4/25/2025
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) | USDA-NRCS North Dakota |
---|---|
Contact for lead author | NRCS State Rangeland Management Specialist |
Date | 04/25/2025 |
Approved by | Suzanne Mayne-Kinney |
Approval date | |
Composition (Indicators 10 and 12) based on | Annual Production |
Indicators
-
Number and extent of rills:
Rills are not expected on this site. -
Presence of water flow patterns:
Water flow patterns are not visible. -
Number and height of erosional pedestals or terracettes:
Neither pedestals nor terracettes are expected. -
Bare ground from Ecological Site Description or other studies (rock, litter, lichen, moss, plant canopy are not bare ground):
Bare ground is less than 5% occurring as small (less than 2 inches in diameter), scattered, disconnected patches. Slickspots of varying size can occur in complex with this site and will be mostly bare ground with sparse, salt-tolerant vegetation. -
Number of gullies and erosion associated with gullies:
Active gullies are not expected on this site. -
Extent of wind scoured, blowouts and/or depositional areas:
No wind-scoured or depositional areas expected on this site. -
Amount of litter movement (describe size and distance expected to travel):
Plant litter movement not expected. -
Soil surface (top few mm) resistance to erosion (stability values are averages - most sites will show a range of values):
Stability class expected to average averages 5 or greater. -
Soil surface structure and SOM content (include type of structure and A-horizon color and thickness):
Use soil series description for depth, color, and structure of A-horizon. -
Effect of community phase composition (relative proportion of different functional groups) and spatial distribution on infiltration and runoff:
Tall-statured rhizomatous grasses and mid- and short-statured bunch grasses are dominant and well distributed across the site. Mid- and short rhizomatous grasses are subdominant. -
Presence and thickness of compaction layer (usually none; describe soil profile features which may be mistaken for compaction on this site):
No compaction layers occur naturally on this site. Naturally occurring platy soil surface structure may be observable. -
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:
Phase 1.1:
Tall C4 rhizomatous grasses (2); Mid & short C3 bunch grasses (3)Sub-dominant:
Phase 1.1:
Mid & short C3 rhizomatous grasses (2); Mid & short C4 rhizomatous grasses (2)Other:
Minor - Phase 1.1:
Forbs; ShrubsAdditional:
Due to differences in phenology, root morphology, soil biology relationships, and nutrient cycling Kentucky bluegrass, smooth brome, and crested wheatgrass are included in a new Functional/structural group, mid- and short-statured early cool-season grasses (MSeC3), not expected for this site.
To see a full version 5 rangeland health worksheet with functional/structural group tables, please use the following hyperlink:
https://efotg.sc.egov.usda.gov/references/public/ND/55B_Saline_Lowland_Narrative_FINAL_Ref_FSG.pdf -
Amount of plant mortality and decadence (include which functional groups are expected to show mortality or decadence):
Rare to not occurring on this site. -
Average percent litter cover (%) and depth ( in):
Plant litter cover is 45 to 65% with a depth of 0.25 to 0.5 inches. Litter is in contact with the soil surface. -
Expected annual annual-production (this is TOTAL above-ground annual-production, not just forage annual-production):
Annual air-dry production is 3800 lbs./ac (reference value) with normal precipitation and temperatures. Low and high production years should yield 2800 lbs./ac to 4800 lbs./ac, respectively. -
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:
State and local noxious species, Kentucky bluegrass, smooth bromegrass, crested wheatgrass, quackgrass, and Russian olive. -
Perennial plant reproductive capability:
Noninvasive species in all functional/structural groups are vigorous and capable of reproducing annually under normal weather conditions.
Print Options
Sections
Font
Other
The Ecosystem Dynamics Interpretive Tool is an information system framework developed by the USDA-ARS Jornada Experimental Range, USDA Natural Resources Conservation Service, and New Mexico State University.
Click on box and path labels to scroll to the respective text.
T1A | - | Introduction of exotic cool-season grasses |
---|---|---|
T2A | - | Long-term non-use or very light grazing, and no fire |
R3A | - | Long-term prescribed grazing and prescribed burning |
R4A | - | Successful range planting |
R4B | - | Failed range planting and/or secondary succession |
T5A | - | Cessation of annual cropping |
State 1 submodel, plant communities
1.1a | - | Multiyear drought with or without heavy long-term grazing |
---|---|---|
1.2a | - | Return to average precipitation, light to moderate grazing |
1.2b | - | Multiyear drought with or without heavy long-term grazing |
1.3a | - | Return to average precipitation, light to moderate grazing |
State 2 submodel, plant communities
2.1a | - | Multiyear drought with or without heavy long-term grazing |
---|---|---|
2.2a | - | Return to average precipitation, long-term prescribed grazing |
2.2b | - | Multiyear drought with heavy grazing |
2.3a | - | Return to average precipitation, long-term prescribed grazing |