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Ecological site R109XY031MO

Wet Floodplain Prairie

Last updated: 7/02/2024
Accessed: 07/17/2024

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General information

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

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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): 109X–Iowa and Missouri Heavy Till Plain

The Iowa and Missouri Heavy Till Plain is an area of rolling hills interspersed with interfluve divides and alluvial valleys. Elevation ranges from about 660 feet along the lower reaches of rivers, to about 980 feet on stable interfluve summits in southern Iowa. Relief is about 80 to 160 feet between major streams and adjacent interfluve summits. Most of the till plain drains south to the Missouri River via the Grand and Chariton River systems, but the northeastern portion drains southeast to the Mississippi River. Loess caps the pre-Illinoisan aged till on interfluves, whereas the till is exposed on side slopes. Mississippian aged limestone and Pennsylvanian aged sandstone and shale crop out on lower slopes in some areas.

Classification relationships

Terrestrial Natural Community Type in Missouri (Nelson, 2010):
The reference state for this ecological site is most similar to a Wet Bottomland Prairie.

National Vegetation Classification System Vegetation Association (NatureServe, 2010):
The reference state for this ecological site is most similar to Spartina pectinata - Carex spp. - Calamagrostis canadensis - Lythrum alatum - (Oxypolis rigidior) Herbaceous Vegetation (CEGL002224).

Geographic relationship to the Missouri Ecological Classification System (Nigh & Schroeder, 2002):
This ecological site occurs throughout the Central Dissected Till Plains Section.

Ecological site concept

NOTE: This is a “provisional” Ecological Site Description (ESD) that is under development. It contains basic ecological information that can be used for conservation planning, application and land management. As additional information is collected, analyzed and reviewed, this ESD will be refined and published as “Approved”.

Wet Floodplain Prairies are widespread in floodplains throughout the MLRA and adjacent areas. Typically, this ecological site occupies most of the floodplain between Terrace sites and the ribbon of Floodplain Forest sites along the stream channel. On larger floodplains, it occupies low areas in the floodplain associated with former meander scars, tributary stream channels and backwater lowlands between natural levees of these once dynamic rivers. Here they are often associated with Ponded Floodplain Prairies on lower areas, and Wet Floodplain Woodland sites on higher areas. Soils are very deep, seasonally wet, and subject to flooding. The reference plant community is prairie dominated by a dense cover of wetland species, including prairie cordgrass, sedges, and wetness-tolerant forbs.

Associated sites

F109XY030MO	Loamy Floodplain Forest Loamy Floodplain Forest sites are often in adjacent, natural levee positions between this site and the active stream channel.
F109XY037MO	Wet Floodplain Woodland Wet Floodplain Woodlands are often in adjacent, slightly higher positions closer to the active stream channel.
R109XY002MO	Loess Upland Prairie Loess Upland Prairies, and other upland prairie and savanna ecological sites, are upslope, on summits and shoulders.
R109XY032MO	Ponded Floodplain Prairie Ponded Floodplain Prairies are often in adjacent, depressional positions farther from the channel.

Similar sites

R109XY032MO	Ponded Floodplain Prairie Ponded Floodplain Prairies have many of the same prairie species and along with similar flooding frequencies but are in slightly lower positions and subject to ponding. The lowest and wettest areas may have marshes and marsh species.

R109XY032MO

Ponded Floodplain Prairie

Ponded Floodplain Prairies have many of the same prairie species and along with similar flooding frequencies but are in slightly lower positions and subject to ponding. The lowest and wettest areas may have marshes and marsh species.

Table 1. Dominant plant species

Tree	Not specified
Shrub	(1) Cephalanthus occidentalis (2) Amorpha fruticosa
Herbaceous	(1) Carex (2) Spartina pectinata

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Physiographic features

This site is on floodplains, with slopes of less than 5 percent. Typically these sites are in backswamp positions, not adjacent to the stream channel. Sites not protected by levees are subject to flooding.

The following figure (adapted from Abney, 1997) shows the typical landscape position of this ecological site, and landscape relationships among the major ecological sites of the floodplains and adjacent uplands. This site is within the area labeled as “2” on the figure, and is typically adjacent to the Loamy Floodplain Forest site that contains the active stream channel. In many places a band of Wet Floodplain Woodland occurs between this site and Loamy Floodplain Forest sites. Several sites occur in adjacent upland positions, such as the Loess Upland Prairie shown in the figure.

Figure 2. Landscape relationships for this ecological site

Table 2. Representative physiographic features

Landforms	(1) Flood plain
Flooding duration	Brief (2 to 7 days) to long (7 to 30 days)
Flooding frequency	Rare to occasional
Ponding duration	Very brief (4 to 48 hours)
Ponding frequency	None to rare
Slope	0 – 5%
Water table depth	0 – 61 cm
Aspect	Aspect is not a significant factor

Climatic features

The Iowa and Missouri Heavy Till Plain MLRA has a continental type of climate marked by strong seasonality. In winter, dry-cold air masses, unchallenged by any topographic barriers, periodically swing south from the northern plains and Canada. If they invade reasonably humid air, snowfall and rainfall result. In summer, moist, warm air masses, equally unchallenged by topographic barriers, swing north from the Gulf of Mexico and can produce abundant amounts of rain, either by fronts or by convectional processes. In some summers, high pressure stagnates over the region, creating extended droughty periods. Spring and fall are transitional seasons when abrupt changes in temperature and precipitation may occur due to successive, fast-moving fronts separating contrasting air masses.

This MLRA experiences small regional differences in climates that grade inconspicuously into each other. The basic gradient for most climatic characteristics is along a line from north to south. Both mean annual temperature and precipitation exhibit fairly minor gradients along this line. Mean January minimum temperature follows the north-to-south gradient. However, mean July maximum temperature shows hardly any geographic variation in the region. Mean July maximum temperatures have a range of only two to three degrees across the region.

Mean annual precipitation varies along the same gradient as temperature – lower annual precipitation in the north, higher in the south. Seasonality in precipitation is very pronounced due to strong continental influences. June precipitation, for example, averages four to five times greater than January precipitation. During years when precipitation comes in a fairly normal manner, moisture is stored in the top layers of the soil during the winter and early spring, when evaporation and transpiration are low. During the summer months the loss of water by evaporation and transpiration is high, and if rainfall fails to occur at frequent intervals, drought will result. Drought directly influences ecological communities by limiting water supplies, especially at times of high temperatures and high evaporation rates. Drought indirectly affects ecological communities by increasing plant and animal susceptibility to the probability and severity of fire. Frequent fires encourage the development of grass/forb dominated communities and understories.

Superimposed upon the basic MLRA climatic patterns are local topographic influences that create topoclimatic, or microclimatic variations. For example, air drainage at nighttime may produce temperatures several degrees lower in valley bottoms than on side slopes. At critical times during the year, this phenomenon may produce later spring or earlier fall freezes in valley bottoms. Slope orientation is an important topographic influence on climate. Summits and south-and-west-facing slopes are regularly warmer and drier, supporting more grass dominated communities than adjacent north- and-east-facing slopes that are cooler and moister that support more woody dominated communities. Finally, the cooler microclimate within a canopied forest is measurably different from the climate of a more open and warmer grassland or savanna area.

Source: University of Missouri Climate Center - http://climate.missouri.edu/climate.php; Land Resource Regions and Major Land Resource Areas of the United States, the Caribbean, and the Pacific Basin, United States Department of Agriculture Handbook 296 - http://soils.usda.gov/survey/geography/mlra/

Table 3. Representative climatic features

Frost-free period (characteristic range)	147-156 days
Freeze-free period (characteristic range)	168-186 days
Precipitation total (characteristic range)	965-1,041 mm
Frost-free period (actual range)	131-169 days
Freeze-free period (actual range)	155-196 days
Precipitation total (actual range)	940-1,067 mm
Frost-free period (average)	150 days
Freeze-free period (average)	176 days
Precipitation total (average)	1,016 mm

Characteristic range

Actual range

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Figure 3. Monthly precipitation range

Characteristic range

Actual range

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Figure 4. Monthly minimum temperature range

Characteristic range

Actual range

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Figure 5. Monthly maximum temperature range

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Figure 6. Monthly average minimum and maximum temperature

Figure 7. Annual precipitation pattern

Figure 8. Annual average temperature pattern

Climate stations used

(1) CONCEPTION [USC00231822], Conception, MO
(2) SALISBURY [USC00237514], Salisbury, MO
(3) CHARITON 1 E [USC00131394], Chariton, IA
(4) KEARNEY 3E [USC00234382], Kearney, MO
(5) TRENTON [USC00238444], Trenton, MO
(6) KEOKUK LOCK DAM 19 [USC00134381], Keokuk, IA

Influencing water features

This ecological site is in floodplains of perennial streams, primarily in backswamp positions, and are not typically adjacent to the current stream channel. They are influenced by a seasonal high water table, due to high groundwater levels in these topographically low positions. Most soils also have slow hydraulic conductivity, which impedes throughflow from precipitation and flood events. The water table is typically near the surface in late fall through spring, receding in the summer.

Stream levels typically respond quickly to storm events, especially in watersheds where surface runoff is dominant. Medium- to long-duration flooding is common in many areas, particularly during spring and early summer storm events. Constructed levees, often accompanied by stream channelization, have altered the hydrology and flooding dynamics in many places.

This site is in the RIVERINE wetlands class of the Hydrogeomorphic (HGM) classification system (Brinson, 1993), and are Emergent Palustrine wetlands (Cowardin et al., 1979).

Soil features

These soils were formed under prairie vegetation, and have dark, organic-rich surface horizons. Parent material is alluvium. They have silt loam or silty clay loam surface horizons, and loamy or clayey substrata lacking argillic horizons. These soils are affected by a seasonal water table in the spring months. Soil series associated with this site include Ackmore, Amana, Carlow, Chequest, Colo, Excello, Otter, Vesser, Wabash, and Zook.

Table 4. Representative soil features

Parent material	(1) Alluvium
Surface texture	(1) Silt loam (2) Silty clay loam
Family particle size	(1) Clayey
Drainage class	Very poorly drained to somewhat poorly drained
Permeability class	Very slow to moderately slow
Surface fragment cover <=3"	0%
Surface fragment cover >3"	0%
Available water capacity (0-101.6cm)	12.7 – 20.32 cm
Calcium carbonate equivalent (0-101.6cm)	0%
Electrical conductivity (0-101.6cm)	0 – 2 mmhos/cm
Sodium adsorption ratio (0-101.6cm)	0
Soil reaction (1:1 water) (0-101.6cm)	5.2 – 7.8
Subsurface fragment volume <=3" (Depth not specified)	0%
Subsurface fragment volume >3" (Depth not specified)	0%

Ecological dynamics

Information contained in this section was developed using historical data, professional experience, field reviews, and scientific studies. The information presented is representative of very complex vegetation communities. Key indicator plants, animals and ecological processes are described to help inform land management decisions. Plant communities will differ across the MLRA because of the naturally occurring variability in weather, soils, and aspect. The Reference Plant Community is not necessarily the management goal. The species lists are representative and are not botanical descriptions of all species occurring, or potentially occurring, on this site. They are not intended to cover every situation or the full range of conditions, species, and responses for the site.

Wet Floodplain Prairie ecological sites exist because of their association with low, persistent wet areas with very poorly drained, heavy, frequently flooded soils. These conditions along with periodic fire have a strong influence on excluding trees and shrubs. Wet Floodplain Prairies are dominated by a dense cover of wetland species, including prairie cordgrass, sedges and wet tolerant forbs.

Prior to levee development and channeling, these areas were regularly flooded by typically slow-moving backwater floods. Unaltered sites usually were flooded at least three months of the year. Seasonal high water table created further inundation and ponding.

Fire during dry periods removed the dense mat of leaf litter creating opportunities for plants less aggressive than the grasses and sedges. Peak water levels were usually high and persistent enough to preclude tree establishment under normal hydrologic regimes. In the long term, siltation slowly filled these depressions, altering flood duration and causing a shift toward floodplain woodland communities.

Today most of these ecological sites have been drained and farmed. Only a very few quality remnants exist. While their flood regime usually has been altered, because of their site conditions, during wet years, they still act as ephemeral farmed wetlands in the agricultural landscape. Their position and soil properties also still make them good candidates for wet prairie development management. Left unfarmed, these sites can quickly develop into naturally wet communities.

A State and Transition Diagram follows. Detailed descriptions of each state, transition, plant community, and pathway follow the model. This model is based on available experimental research, field observations, professional consensus, and interpretations.

State and transition model

Custom diagram

Standard diagram

Figure 9. State and transition diagram for this ecological s

More interactive model formats are also available. View Interactive Models

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

State 1
Reference

This state is typical of wet prairies or sedge meadows that are not connected to groundwater (not seepage communities or fens) and that experience full horizon saturation (endosaturation), at least briefly throughout the growing season. Long duration flooding regimes are common during some years. Two phases can occur that will transition back and forth depending on fire and flooding frequencies. Longer fire and flooding free intervals will allow woody species to increase such prairie willow, dogwoods and false indigo. When fire and flooding intervals shorten these woody species will decrease or be eliminated. This state is very rare. Nearly all sites have been converted to intensive agriculture cropland along with some cool season grassland or have reverted to wet savannas/woodlands.

Dominant plant species

buttonbush (Cephalanthus), shrub
false indigo (Amorpha), shrub
willow (Salix), shrub
sedge (Abildgaardia), other herbaceous
prairie cordgrass (Spartina pectinata), other herbaceous

Community 1.1
Buttonbush – False Indigo/Sedge – Prairie Cord Grass

This phase is dominated by sedges, prairie cord grass and a wide variety of prairie wildflowers. These areas long duration flooding. In addition to the flooding, fire played a key role, likely occurring at least once every 5 to 7 years.

Forest understory. The Forest Understory list is based on commonly occurring species listed in Nelson (2010).

Dominant plant species

buttonbush (Cephalanthus), shrub
false indigo (Amorpha), shrub
sedge (Abildgaardia), other herbaceous
prairie cordgrass (Spartina pectinata), other herbaceous

Community 1.2
Buttonbush – False Indigo – Willow/Sedge – Prairie Cord Grass

This phase is characterized by long fire free intervals and drier periods. Woody species would have increased in abundance and spread out onto the prairie. Slightly higher areas within or at the edge of the floodplain supported widely scattered bur oak, pin oak, elm, shellbark hickory and willow.

Dominant plant species

buttonbush (Cephalanthus), shrub
false indigo (Amorpha), shrub
willow (Salix), shrub
sedge (Abildgaardia), other herbaceous
prairie cordgrass (Spartina pectinata), other herbaceous

Pathway 1.1A
Community 1.1 to 1.2

Fire-free interval 10+ years; reduced flooding

Pathway 1.2A
Community 1.2 to 1.1

Flooding; prescribed fire

State 2
Woody Invaded Prairie

Degraded reference states that have experienced fire suppression and flooding reduction for 20 or more years will transition to this state. With fire suppression and reduced flooding, woody species such as silver maple, American elm and eastern cottonwood will begin to increase transitioning this state from a prairie to a Woody Invaded Prairie. Native ground cover will also decrease. Transition from this state to cool season grasslands (State 3) or intensive cropland (State 4) was very common.

Dominant plant species

silver maple (Acer saccharinum), tree
American elm (Ulmus americana), tree
dogwood (Cornus), shrub
sawtooth sunflower (Helianthus grosseserratus), other herbaceous
sedge (Abildgaardia), other herbaceous

Community 2.1
Silver Maple - American Elm/ Dogwood / Sawtootlh Sunflower/Sedge

Dominant plant species

silver maple (Acer saccharinum), tree
American elm (Ulmus americana), tree
dogwood (Cornus), shrub
sawtooth sunflower (Helianthus grosseserratus), other herbaceous
sedge (Abildgaardia), other herbaceous

State 3
Cool Season Grassland

Conversion of other states to non-native cool season species such as tall fescue, white clover, and red top has been common in this area. Occasionally, these pastures will have scattered bur oaks or pecan. Transitioning to a Cropland State to help eliminate non-native grassland species and then restoring to a reference state is usually the easiest and most useful method of restoration from this state.

Dominant plant species

tall fescue (Schedonorus arundinaceus), other herbaceous
redtop (Agrostis gigantea), other herbaceous
reed canarygrass (Phalaris arundinacea), other herbaceous
white clover (Trifolium repens), other herbaceous

Community 3.1
Cool Season Grassland

Dominant plant species

tall fescue (Schedonorus arundinaceus), other herbaceous
redtop (Agrostis gigantea), other herbaceous
reed canarygrass (Phalaris arundinacea), other herbaceous
white clover (Trifolium repens), other herbaceous

State 4
Cropland

This is the dominant state that exists currently with intensive cropping of corn, soybeans, and wheat occurring. A return to the reference state may be difficult and costly, requiring a very long term series of management options.

Dominant plant species

corn (Zea), other herbaceous
soybean (Glycine), other herbaceous
wheat (Triticum), other herbaceous

Community 4.1
Cropland

Transition T1A
State 1 to 2

Fire suppression >20 years; woody invasion; reduced flooding

Transition T1B
State 1 to 3

Tillage; vegetative seeding; grassland management; drainage water management

Transition T1C
State 1 to 4

Tillage; conservation cropping system; drainage water management

Restoration pathway R2A
State 2 to 1

Woody removal; prescribed fire

Transition T2A
State 2 to 3

Woody removal; tillage; vegetative seeding; grassland management

Transition T2B
State 2 to 4

Woody removal; tillage; vegetative seeding; grassland management

Transition T3A
State 3 to 4

Tillage; conservation cropping system

Restoration pathway R4A
State 4 to 1

Vegetative seeding; prescribed fire; restore natural hydrology

Restoration pathway T4A
State 4 to 3

Vegetative seeding; grassland management

Additional community tables

Table 5. Community 1.1 forest understory composition

Common name	Symbol	Scientific name	Nativity	Height (m)	Canopy cover (%)
Grass/grass-like (Graminoids)
prairie cordgrass	SPPE	Spartina pectinata	Native	–	20–40
shoreline sedge	CAHY3	Carex hyalinolepis	Native	–	10–20
hop sedge	CALU4	Carex lupulina	Native	–	10–20
fox sedge	CAVU2	Carex vulpinoidea	Native	–	10–20
fescue sedge	CAFE3	Carex festucacea	Native	–	10–20
Canada wildrye	ELCA4	Elymus canadensis	Native	–	10–20
rice cutgrass	LEOR	Leersia oryzoides	Native	–	10–20
fowl mannagrass	GLST	Glyceria striata	Native	–	5–10
Torrey's rush	JUTO	Juncus torreyi	Native	–	5–10
Forb/Herb
water knotweed	POAM8	Polygonum amphibium	Native	–	5–20
swamp milkweed	ASIN	Asclepias incarnata	Native	–	5–20
winged lythrum	LYAL4	Lythrum alatum	Native	–	5–20
white doll's daisy	BOAS	Boltonia asteroides	Native	–	5–20
bearded beggarticks	BIAR	Bidens aristosa	Native	–	5–20
prairie ironweed	VEFA2	Vernonia fasciculata	Native	–	5–20
sawtooth sunflower	HEGR4	Helianthus grosseserratus	Native	–	5–20
smooth white oldfield aster	SYRA5	Symphyotrichum racemosum	Native	–	5–20
Virginia iris	IRVI	Iris virginica	Native	–	5–20
American water horehound	LYAM	Lycopus americanus	Native	–	5–20
swamp smartweed	POHY2	Polygonum hydropiperoides	Native	–	5–20
harvestlice	AGPA6	Agrimonia parviflora	Native	–	5–20
Shrub/Subshrub
common buttonbush	CEOC2	Cephalanthus occidentalis	Native	–	5–20
false indigo bush	AMFR	Amorpha fruticosa	Native	–	5–20

Interpretations

Animal community

Wildlife
Game species that utilize this ecological site include:
White-tailed Deer will utilize this ecological site for browse (plant leaves in the growing season, seeds and soft mast in the fall/winter). This site type also can provide escape cover.

Migratory Waterbirds: Sora, Common Snipe and Virginia Rail
Furbearers: Muskrat, Beaver, and Mink.

Bird species associated with this ecological site’s reference state condition:
Breeding birds: Sedge Wren, Red-Winged Blackbird, American Bittern, Marsh Wren, and Common Yellowthroat.

Migratory birds: Sora, Virginia Rail, Sedge Wren, American Bittern, Yellow Rail and Common Snipe.

Amphibian and reptile species associated with this ecological site’s reference state condition: Western Chorus Frog (Pseudacris triseriata triseriata), Plains Leopard Frog (Rana blairi), Graham’s Crayfish Snake (Regina grahamii), Midland Brown Snake (Storeria dekayi wrightourm), prairies with crawfish burrows may have Northern Crawfish Frog (Rana areolata circulosa); Western Fox Snake (Elaphe vulpina vulpina), and Western Massasauga rattlesnake (Sistrurus catenatus tergeminus).

Small mammals associated with this ecological site’s reference state condition: Muskrat (Ondatra zibethicus), Southern Bog Lemming (Synaptomys cooperi), and Mink (Mustela vison).

Many native insect species are likely associated with this ecological site, especially native bees, ants, beetles, butterflies and moths, and crickets, grasshoppers and katydids. However information on these groups is often lacking enough resolution to assign them to individual ecological sites.

Insect species known to be associated with this ecological site’s reference state condition: Swamp Milkweed Leaf Beetle (Labidomera clivicollis), Cordgrass Planthopper (Prokelisia crocea), Dion Skipper butterfly (Euphyes dion), Duke’s Skipper butterfly (Euphyes dukesi), native bees (Lasioglossum hartii, Hesperapis carinata, Svastra atripes and Cemolobus ipomoeae), Bullate Meadow katydid (Orchelimum bullatum) and Sedge Grasshopper (Stethophyma celatum).

Other invertebrates: Grassland Crayfish (Procambarus gracilis)

(This section prepared by Mike Leahy, Natural Areas Coordinator, Missouri Department of Conservation, 2013. References for this section: Fitzgerald and Pashley 2000b; Heitzman and Heitzman 1996; Jacobs 2001; Johnson 2000; Pitts and McGuire 2000; Schwartz and others 2001)

Other information

Forestry
Management: This ecological site is not recommended for traditional timber management activity. Historically this site was dominated by a ground cover of native prairie grasses and forbs. Some scattered open grown trees may have also been present. Altered states may be suitable for non-traditional forestry uses such as windbreaks, environmental plantings, alley cropping (a method of planting, in which rows of trees or shrubs are interspersed with rows of crops) or woody bio-fuels.

Supporting information

Inventory data references

Potential Reference Sites: Wet Floodplain Prairie

Plot PERSSP_KS02 – Wabash soil
Located in Pershing State Park, Linn County, MO
Latitude: 39.773165
Longitude: - 93.218119

Plot PERSP_KS12 – Carlow soil
Located in Pershing State Park, Linn County, MO
Latitude: 39.738824
Longitude: -93.228899

Plot YECRCA_KS01 – Chequest soil
Located in Yellow Creek CA, Chariton County, MO
Latitude: 39.582209
Longitude: - 93.227056

Other references

Abney, Mark A. 1997. Soil Survey of Chariton County, Missouri. U.S. Dept. of Agric. Natural Resources Conservation Service.

Anderson, R.C. 1990. The historic role of fire in North American grasslands. Pp. 8-18 in S.L. Collins and L.L. Wallace (eds.). Fire in North American tallgrass prairies. University of Oklahoma Press, Norman.

Brinson, M.M. 1993. A hydrogeomorphic classification for wetlands. Technical Report WRP-DE-4, U.S. Army Corps of Engineers, Engineer Waterways Experiment Station, Vicksburg, MS.

Cowardin, L.M., V. Carter, F.C. Golet, & E.T. LaRoe. 1979. Classification of wetlands and deepwater habitats of the United States. U.S. Dept. of Interior, Fish & Wildlife Service, Office of Biological Services, Washington DC.

Fitzgerald, J.A. and D.N. Pashley. 2000b. Partners in Flight bird conservation plan for the Dissected Till Plains. American Bird Conservancy.

Frost, C., 1996. Pre-settlement Fire Frequency Regimes of the United States: A First Approximation. Pages 70-81, Proceedings of the 20nd Tall Timbers Fire Ecology Conference: Fire in Ecosystem Management: Shifting the Paradigm from Suppression to Prescription. Tall Timbers Research Station, Tallahassee, FL.

Heitzman, J.R. and J.E. Heitzman. 1996. Butterflies and moths of Missouri. 2nd ed. Missouri Department of Conservation, Jefferson City.

Jacobs, B. 2001. Birds in Missouri. Missouri Department of Conservation, Jefferson City.

Johnson, T.R. 2000. The amphibians and reptiles of Missouri. 2nd ed. Missouri Department of Conservation, Jefferson City.

Natural Resources Conservation Service. 2002. Woodland Suitability Groups. Missouri FOTG, Section II, Soil Interpretations and Reports. 30 pgs.
Natural Resources Conservation Service. Site Index Reports. Accessed May 2014. https://esi.sc.egov.usda.gov/ESI_Forestland/pgFSWelcome.aspx

NatureServe. 2010. Vegetation Associations of Missouri (revised). NatureServe, St. Paul, Minnesota.

Nelson, Paul W. 2010. The Terrestrial Natural Communities of Missouri. Missouri Department of Conservation, Jefferson City, Missouri.

Nigh, Timothy A. and Walter A. Schroeder. 2002. Atlas of Missouri Ecoregions. Missouri Department of Conservation, Jefferson City, Missouri.

Pitts, D.E. and W.D. McGuire. 2000. Wildlife management for Missouri landowners. 3rd ed. Missouri Department of Conservation, Jefferson City.
Schwartz, C.W., E.R. Schwartz and J.J. Conley. 2001. The wild mammals of Missouri. University of Missouri Press, Columbia and Missouri Department of Conservation, Jefferson City.

United States Department of Agriculture – Natural Resource Conservation Service (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. 682 pgs.

Contributors

Doug Wallace
Fred Young

Approval

Suzanne Mayne-Kinney, 7/02/2024

Acknowledgments

This site was originally approved on 07/28/2015 for publication.

Rangeland health reference sheet

Interpreting Indicators of Rangeland Health is a qualitative assessment protocol used to determine ecosystem condition based on benchmark characteristics described in the Reference Sheet. A suite of 17 (or more) indicators are typically considered in an assessment. The ecological site(s) representative of an assessment location must be known prior to applying the protocol and must be verified based on soils and climate. Current plant community cannot be used to identify the ecological site.

Author(s)/participant(s)
Contact for lead author
Date	07/17/2024
Approved by	Suzanne Mayne-Kinney
Approval date
Composition (Indicators 10 and 12) based on	Annual Production

Indicators

Number and extent of rills:
Presence of water flow patterns:
Number and height of erosional pedestals or terracettes:
Bare ground from Ecological Site Description or other studies (rock, litter, lichen, moss, plant canopy are not bare ground):
Number of gullies and erosion associated with gullies:
Extent of wind scoured, blowouts and/or depositional areas:
Amount of litter movement (describe size and distance expected to travel):
Soil surface (top few mm) resistance to erosion (stability values are averages - most sites will show a range of values):
Soil surface structure and SOM content (include type of structure and A-horizon color and thickness):
Effect of community phase composition (relative proportion of different functional groups) and spatial distribution on infiltration and runoff:
Presence and thickness of compaction layer (usually none; describe soil profile features which may be mistaken for compaction on this site):
Functional/Structural Groups (list in order of descending dominance by above-ground annual-production or live foliar cover using symbols: >>, >, = to indicate much greater than, greater than, and equal to):

Dominant:

Sub-dominant:

Other:

Additional:
Amount of plant mortality and decadence (include which functional groups are expected to show mortality or decadence):
Average percent litter cover (%) and depth ( in):
Expected annual annual-production (this is TOTAL above-ground annual-production, not just forage annual-production):
Potential invasive (including noxious) species (native and non-native). List species which BOTH characterize degraded states and have the potential to become a dominant or co-dominant species on the ecological site if their future establishment and growth is not actively controlled by management interventions. Species that become dominant for only one to several years (e.g., short-term response to drought or wildfire) are not invasive plants. Note that unlike other indicators, we are describing what is NOT expected in the reference state for the ecological site:
Perennial plant reproductive capability:

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Natural ResourcesConservation Service

Ecological site R109XY031MO

Wet Floodplain Prairie

Last updated: 7/02/2024 Accessed: 07/17/2024

General information

Figure 1. Mapped extent

MLRA notes

Classification relationships

Ecological site concept

Associated sites

Similar sites

Table 1. Dominant plant species

Ecosystem states

State 1 submodel, plant communities

State 2 submodel, plant communities

State 3 submodel, plant communities

State 4 submodel, plant communities

Natural Resources
Conservation Service

Last updated: 7/02/2024
Accessed: 07/17/2024