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Ecological site PX138X00Y020

Sandy Over Loamy Flood Plain Marshes and Swamps

Last updated: 6/09/2025
Accessed: 12/05/2025

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General information

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

MLRA notes

Major Land Resource Area (MLRA): 138X–North-Central Florida Ridge

The MLRA notes section provides a brief description of the entire MLRA. This description is intended to provide some context about the MLRA within which this ecological site is associated. A more complete description of the MLRA can be found in Ag Handbook 296 (USDA-NRCS, 2022).

This MLRA is on a limestone upland that is mantled with sandy marine deposits and has an irregular, gently rolling topography. Because of the underlying karst topography, there are a moderate number of limestone sinkholes, some filled with water. Production of cash crops, hay, and pasture is the primary land use. This area comprises about 2,196 square miles (5,688 square kilometers) and is entirely within Florida.

This area is underlain by sediments of the Quaternary Period (present to 2.58 million years ago) that overlie the Neogene (2.53 to 23.03 million years ago) and Paleogene (23.03 to 66 million years ago) formations of the Hawthorn Group (Green et al., 2006). The rocks are progressively older to the south. The Quaternary sediments are largely undifferentiated marine deposits consisting of fine to coarse sands that are poorly to moderately sorted with variable mixtures of clay and organic material. The formations of the Hawthorn Group are, from youngest to oldest, the Statesville Formation, Coosawhatchie Formation, Suwannee Limestone, and Ocala Limestone. The Statesville Formation consists of thinly interbedded, and commonly cross-bedded, dolostone and clay alternating with beds of sand. Phosphate grains are common to abundant. The Coosawhatchie Formation is made up of poorly to moderately sorted sandy clay or clayey sand with phosphate grains, limestone, and dolostone. The Suwannee Limestone is a cream colored to tan, crystalline, vuggy and muddy, fossiliferous, variably dolomitic carbonate. It has chert nodules in some areas. The Ocala Limestone was deposited in the Eocene (33.9 to 56 million years ago) and is the oldest rock formation exposed in Florida. It is a white to cream-colored, fossiliferous limestone and has chert nodules in some areas.

This area borders MLRA 133A to the north, which has only slight differences in use and management due to the underlying karst topography. Its boundaries with MLRA 152A to the west and MLRA 153A to the east are distinguishable by an abrupt scarp on a lower, younger marine terrace. Its boundary with MLRA 154 is a gradual transition to slightly younger marine sediments to the south.

Elevation of the MLRA ranges from 26 to 197 feet (8 to 60 meters). Local relief is generally 10 to 20 feet (3 to 6 meters) but can be as much as 35 feet (10 meters).

The dominant soil orders are Ultisols, Entisols, and Alfisols. The soils in the area dominantly have a thermic temperature regime, a udic moisture regime, and siliceous mineralogy.

This area supports open pine and oak vegetation. Major wildlife species include white-tailed deer, raccoon, skunk, opossum, rabbit, gray squirrel, fox squirrel, turkey, bobwhite quail, and mourning dove.

The abundant rainfall and the Floridan aquifer are the principal sources of water in the area. The many lakes and ponds are used for recreation. Most of the river water is suitable for almost all uses. Shallow and deep wells in the Floridan aquifer provide water for public supply, domestic use, industry, mining, livestock, and irrigation. This aquifer is one of the most productive sources of ground water in the United States. Its water is hard but of good quality. Wells yield large quantities of the calciumbicarbonate type of water. The Floridan aquifer is a thick sequence of Tertiary limestone and dolomite. The Eocene Avon Park Formation and Ocala Limestone are the thickest and most productive units in the aquifer system.

A significant portion of this MLRA along riparian areas remains wooded with some larger holdings used exclusively for forestry. Pulpwood and lumber are the principal forest products. Hay and pasture are of great extent throughout this MLRA. The cropland in the area is used mainly for corn, peanuts, tobacco, soybeans, vegetables, and melons.

The major resource concerns are maintenance of organic matter and productivity of the soils, management of soil moisture, and management of animal waste. Conservation practices on cropland generally include crop rotations, cover crops, nutrient management, pest management, and irrigation water management.

(USDA, NRCS, 2022)

Classification relationships

Most of this area is in the East Gulf Coastal Plain section of the Coastal Plain province of the Atlantic Plain. The southern one-quarter is in the Floridian section of the same province and division. (McNab et al., 2007; USDA, NRCS, 2022)

MLRA 138 is relatively small and comprises the eastern half of EPA level IV ecoregion 65o, Tallahassee Hills and Valdosta Limesink, which is part of level III ecoregion 65, Southeastern Plains. (U.S. EPA, 2013)

The reference community of this site corresponds approximately with the Floodplain Swamp community (FNAI, 2010).

The improved pasture community of the managed grassland state corresponds well with Forage Suitability Group G138XA245FL. The improved drained pasture community corresponds well with Forage Suitability Group G138XA241FL. (USDA, NRCS, 2013)

Ecological site concept

This site occurs on flood plains along major rivers and streams, and it experiences occasional to frequent flooding, or would in the absence of water control structures. Soils are poorly to very poorly drained. The land is flat with slopes mostly from 0 to 2 percent.

Soils are mostly sandy over loamy, and have an argillic horizon between 20 and 40 inches. Some soils may have a mollic or umbric horizon.

This site often supports Flood Plain Swamp, Mixed Scrub-Shrub Wetland, Coniferous Plantation, and Improved Pasture communities.

Associated sites

PX138X00Y050	Sandy or Sandy Over Loamy Upland Pine on Stream Terraces A diverse array of flood plain and stream terrace soils and sites are associated together adjacent to a riverine system. These soils are in a different landscape position but have similar physical properties, such as texture, and different levels of productivity.
PX138X00Y010	Sandy Flood Plain Marshes and Swamps A diverse array of flood plain and stream terrace soils and sites are associated together adjacent to a riverine system. These soils are in a similar landscape position but have different physical properties and productivity.
PX138X00Y030	Loamy and Clayey Flood Plain Marshes and Swamps A diverse array of flood plain and stream terrace soils and sites are associated together adjacent to a riverine system. These soils are in a similar landscape position but have different physical properties and productivity.
PX138X00Y040	Sandhill or Scrub on Stream Terraces A diverse array of flood plain and stream terrace soils and sites are associated together adjacent to a riverine system.
PX138X00Y060	Loamy and Clayey Bottomland Forests on Stream Terraces A diverse array of flood plain and stream terrace soils and sites are associated together adjacent to a riverine system.

Similar sites

PX138X00Y010	Sandy Flood Plain Marshes and Swamps These sites support similar native vegetation communities, but production is somewhat different, especially regarding grazing forage production.
PX138X00Y030	Loamy and Clayey Flood Plain Marshes and Swamps These sites support similar native vegetation communities, but production is somewhat different, especially regarding grazing forage production.
PX138X00Y080	Sandy Over Loamy Depression Basin and Dome Swamps PX138X00Y080 will typically display different native vegetation than PX138X00Y020, but grazing forage production will be very similar.

PX138X00Y010

Sandy Flood Plain Marshes and Swamps

These sites support similar native vegetation communities, but production is somewhat different, especially regarding grazing forage production.

PX138X00Y030

Loamy and Clayey Flood Plain Marshes and Swamps

These sites support similar native vegetation communities, but production is somewhat different, especially regarding grazing forage production.

PX138X00Y080

Sandy Over Loamy Depression Basin and Dome Swamps

PX138X00Y080 will typically display different native vegetation than PX138X00Y020, but grazing forage production will be very similar.

Table 1. Dominant plant species

Tree	(1) Taxodium distichum (2) Nyssa aquatica
Shrub	Not specified
Herbaceous	Not specified

Legacy ID

F138XY020AL

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Physiographic features

This site occurs on flood plains along major rivers and streams and experiences regular flooding, or would in the absence of water control structures. Dominant hydrology on this site is typically flooding. Slope is typically 0 to 2 percent.

Table 2. Representative physiographic features

Landforms	(1) Marine terrace > Flood plain (2) Marine terrace > Stream terrace
Runoff class	Very low
Flooding duration	Brief (2 to 7 days) to very long (more than 30 days)
Flooding frequency	Occasional
Ponding duration	Very long (more than 30 days)
Ponding frequency	None to frequent
Elevation	110 – 200 ft
Slope	2%
Ponding depth	Not specified
Water table depth	18 in
Aspect	Aspect is not a significant factor

Table 3. Representative physiographic features (actual ranges)

Runoff class	Very low
Flooding duration	Brief (2 to 7 days) to very long (more than 30 days)
Flooding frequency	Occasional
Ponding duration	Very long (more than 30 days)
Ponding frequency	None to frequent
Elevation	25 – 200 ft
Slope	2%
Ponding depth	12 in
Water table depth	18 in

Climatic features

The maximum precipitation occurs in summer, and the minimum occurs in winter and late autumn. Rainfall occurs during high-intensity, convective thunderstorms in summer. The average annual temperature is 68 to 69 degrees F (20 to 21 degrees C).

An additional hazard of concern during late summer through early fall are tropical cyclones. While most impacts from hurricanes and tropical storms are confined along the coastal zone, heavy rainfall, severe flooding, and high winds can occur well into Florida when such systems pass through the area. To the extreme, the region is susceptible to the effects of a strong Bermuda High during the summer, which can cause devastating drought conditions for weeks and even months in some years.

(USDA, NRCS, 2022)

Table 4. Representative climatic features

Frost-free period (characteristic range)	217-225 days
Freeze-free period (characteristic range)	253-263 days
Precipitation total (characteristic range)	52-54 in
Frost-free period (actual range)	213-231 days
Freeze-free period (actual range)	241-274 days
Precipitation total (actual range)	52-54 in
Frost-free period (average)	221 days
Freeze-free period (average)	258 days
Precipitation total (average)	53 in

Characteristic range

Actual range

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Figure 1. Monthly precipitation range

Characteristic range

Actual range

Bar

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Figure 2. Monthly minimum temperature range

Characteristic range

Actual range

Bar

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Figure 3. Monthly maximum temperature range

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Figure 4. Monthly average minimum and maximum temperature

Figure 5. Annual precipitation pattern

Figure 6. Annual average temperature pattern

Climate stations used

(1) JASPER [USC00084394], Jasper, FL
(2) LIVE OAK [USC00085099], Live Oak, FL
(3) MAYO [USC00085539], Live Oak, FL
(4) LAKE CITY 2 E [USC00084731], Lake City, FL
(5) HIGH SPRINGS [USC00083956], High Springs, FL
(6) BELL 4NW [USC00080598], Old Town, FL

Influencing water features

The Suwannee River, which originates in the Okefenokee Swamp to the northeast and is spring-fed, flows through this MLRA. The Alapaha and Withlacoochee Rivers join the Suwannee River in the area. Another Suwannee River tributary, the Santa Fe River, crosses the southern part of the area. (USDA, NRCS, 2022)

Wetland description

Dominant hydrology on this site is flooding. This site is very poorly to poorly drained. It represents locations where the soils may or may not meet hydric field criteria, and the variation between the two may be exceptionally subtle. In situations where the soil is hydric, this site represents locations that are periodically flooded, but are not exposed to tidal influences. Any wetlands that occur within a channel are riverine in nature. All others on this site are palustrine in nature.

Soil features

Please note that the soils listed in this section of the description may not be all inclusive. There may be additional soils that fit the site’s concepts. Additionally, the soils that provisionally form the concepts of this site may occur elsewhere, either within or outside of the MLRA and may or may not have the same geomorphic characteristics or support similar vegetation. Some soil map units and soil series included in this “provisional” ecological site were used as a “best fit” for a particular soil – landform catena during a specific era of soil mapping, regardless of the origin of parent material or the location of MLRA boundaries. Therefore, the listed soils may not be typical for MLRA 138 or a specific location, and the associated soil map units may warrant further investigation in a joint ecological site inventory – soil survey project. When utilizing this provisional description, the user is encouraged to verify that the area of interest meets the appropriate ecological site concepts by reviewing the soils, landform, vegetation, and physical location. If the site concepts do not match the attributes of the area of interest, please review the Similar or Associated Sites listed in the General Information section of this description to determine if another site may be a better fit for your area of interest.

This site is comprised of soils in the Mascotte, Surrency, and Pelham series. These soils are very poorly to poorly drained, sandy over loamy, and they have an Argillic horizon between 20 and 40 inches. Some soils may have a mollic or umbric horizon.
.

Table 5. Representative soil features

Parent material	(1) Marine deposits
Surface texture	(1) Fine sand (2) Sand
Drainage class	Very poorly drained to poorly drained
Permeability class	Moderately rapid
Soil depth	80 in
Surface fragment cover <=3"	Not specified
Surface fragment cover >3"	Not specified
Available water capacity (0-40in)	2.3 – 4 in
Soil reaction (1:1 water) (0-10in)	3.5 – 5.5
Subsurface fragment volume <=3" (Depth not specified)	3%
Subsurface fragment volume >3" (Depth not specified)	Not specified

Table 6. Representative soil features (actual values)

Drainage class	Very poorly drained to poorly drained
Permeability class	Moderately rapid
Soil depth	80 in
Surface fragment cover <=3"	Not specified
Surface fragment cover >3"	Not specified
Available water capacity (0-40in)	2 – 4.3 in
Soil reaction (1:1 water) (0-10in)	3.5 – 5.5
Subsurface fragment volume <=3" (Depth not specified)	3%
Subsurface fragment volume >3" (Depth not specified)	Not specified

Ecological dynamics

The information presented in this ecological site description (ESD) and state-and-transition model (STM) were developed using archaeological and historical information, published and unpublished scientific reports, professional experience, consultation with technical experts, and NRCS inventories and studies. The information presented represents a complex set of plant community dynamics and environmental variables. Not all scenarios or plants are represented and included. Key indicator plants, animals, and ecological processes are described to help guide land management decisions and actions.

Historically, these sites have been drained frequently to support a variety of land uses including pasture. This drained state is included in this STM because this state exists widely today across the landscape. This site may or may not represent a wetland but drainage of wetlands today is significantly regulated. NRCS is required to consider impacts to wetlands according to Federal laws including, but not limited to, the Clean Water Act, the Wetland Conservation provisions of the Food Security Act of 1985, and State, Tribal, and local laws. It is the policy of NRCS to protect and promote wetland functions and values in all NRCS assistance (National Environmental Compliance Handbook (NECH) 610.36).

Flood plain swamp along channels may be regularly inundated by flowing aerobic water. However, backswamps are flooded with stagnant water for extensive periods of time, resulting in highly anaerobic conditions. The lack of available oxygen inhibits breakdown of leaf litter and leads to considerable peat accumulation. Anaerobic conditions may contribute to increased nutrient release from sediments through bacterial processes. During dry summer months when evapotranspiration rates increase, surface water may be entirely lacking. Floods redistribute detrital accumulations to other portions of the flood plain or into the main river channel. This rich organic debris is essential to the functional integrity of downriver ecosystems such as estuaries, providing a vital source of nutrients. Flood plain swamp may also act as a nutrient sink or transformer depending on local conditions, making these wetlands particularly valuable in disposal of partially treated wastewater. The topography of alluvial forest and flood plain swamp, particularly in larger alluvial river systems, is a result of a seasonal flooding pattern which builds levees and point bars, creates scour channels and depressions, and introduces flowing water into backswamps. Old channels and levees left behind by the changing meander of the river itself become part of the complex mosaic. The oxbows and backswamps created by meander processes are important breeding grounds for fish when high water connects them to the river. Flood plain swamp is usually too wet to support fire; however, large cypress trees are somewhat fire-resistant, and thus infrequent fires during very dry conditions may contribute to cypress dominance. Fires may greatly damage the understory. (FNAI, 2010)

Following this narrative, a “provisional” state and transition model is provided that includes the “perceived” reference state and several alternative (or altered) vegetation states that have been observed and/or projected for this ecological site. This model is based on limited inventories, literature, expert knowledge, and interpretations. Plant communities may differ from one location to the next depending on the severity of local land use activities and rates of deposition. Depending on objectives, the reference plant community may not necessarily be the management goal.

The environmental and biological characteristics of this site are complex and dynamic. As such, the following diagram suggests pathways that the vegetation on this site might take, given that the modal concepts of climate and soils are met within an area of interest. Specific locations with unique soils and disturbance histories may have alternate pathways that are not represented in the model. This information is intended to show the possibilities within a given set of circumstances and represents the initial steps toward developing a defensible description and model. The model and associated information are subject to change as knowledge increases and new information is garnered. This is an iterative process. Most importantly, local and/or state professional guidance should always be sought before pursuing a treatment scenario.

State and transition model

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

Ecosystem states

1. Naturalized Vegetation: Flood Plain Swamp

2. Managed Grassland

3. Pine Plantation

4. Degraded

T1.2	-	Land clearing, introduction of grasses, and applied grassland management
T1.3	-	Land clearing, site preparation, and tree planting
T1.4	-	Introduction of non-native species
T2.4	-	Introduction of non-native species
T3.4	-	Introduction of non-native species
T4.1	-	Mechanical, chemical or biological control
T4.2	-	Mechanical, chemical or biological control
T4.3	-	Mechanical, chemical or biological control

State 1 submodel, plant communities

1.1. Reference Community: Even-aged, Closed-canopy, Flood Plain Swamp

1.2. Flood Plain Marsh

1.3. Uneven-age Open to Closed Canopy Alluvial Forest

1.4. Uneven-age Closed Canopy Flood Plain Swamp

P1.1.2	-	Clearcut, widescale blowdown, insect, or disease infestation
P1.1.3	-	Selective logging of cypress
P1.1.4	-	Undisturbed succession, time, and natural die off
P1.2.1	-	Reforestation/Regeneration
P1.2.3	-	Tupelo dominance post disturbance
P1.3.2	-	Clearcut, widescale blowdown, insect, or disease infestation
P1.3.4	-	Hardwood reduction, cypress regrowth, and canopy closure
P1.4.2	-	Clearcut, widescale blowdown, insect, or disease infestation
P1.4.3	-	Selective logging of cypress

State 2 submodel, plant communities

2.1. Improved Undrained Pasture (FSG_G138XA245FL)

2.2. Improved Drained Pasture (FSG_G138XA241FL )

2.3. Unimproved Pasture with Woody Encroachment

P2.1.2	-	Drained
P2.1.3	-	Pasture abandonment
P2.2.1	-	Hydrologic restoration
P2.2.3	-	Pasture abandonment and/or mismanagement
P2.3.1	-	Pasture restoration and applied grazing
P2.3.2	-	Pasture restoration and applied grazing

State 1
Naturalized Vegetation: Flood Plain Swamp

A flood plain swamp occurs along or near rivers and streams with organic/alluvial substrate; usually inundated; Panhandle to central peninsula; rare or no fire; closed canopy dominated by cypress, tupelo, and/or black gum. (FNAI, 2010) According to FNAI (2010) flood plain swamp is a closed-canopy forest of hydrophytic trees occurring on frequently or permanently flooded hydric soils adjacent to stream and river channels and in depressions and oxbows within flood plains. Trees are often buttressed, and the understory and groundcover are sparse. The canopy is sometimes a pure stand of bald cypress (Taxodium distichum), but more commonly bald cypress shares dominance with one or more of the following tupelo species: water tupelo (Nyssa aquatica), swamp tupelo (N. sylvatica var. biflora), or ogeechee tupelo (N. ogeche). The “knees” arising from the root systems of both cypress and tupelo are common features in floodplain swamp. Other canopy trees capable of withstanding frequent inundation may be present but rarely dominant, including water hickory (Carya aquatica), overcup oak (Quercus lyrata), red maple (Acer rubrum), green ash (Fraxinus pennsylvanica), American elm (Ulmus americana), and swamp laurel oak (Q. laurifolia). Pond cypress (T. ascendens) is sometimes present in backswamps and depressions of the more hydrologically isolated areas of the flood plain.

Dominant plant species

bald cypress (Taxodium distichum), tree
pond cypress (Taxodium ascendens), tree
water tupelo (Nyssa aquatica), tree
swamp tupelo (Nyssa biflora), tree
Ogeechee tupelo (Nyssa ogeche), tree

Community 1.1
Reference Community: Even-aged, Closed-canopy, Flood Plain Swamp

Community 1.2
Flood Plain Marsh

Community 1.3
Uneven-age Open to Closed Canopy Alluvial Forest

Community 1.4
Uneven-age Closed Canopy Flood Plain Swamp

Pathway P1.1.2
Community 1.1 to 1.2

Clearcut, widescale blowdown, insect, or disease infestation

Pathway P1.1.3
Community 1.1 to 1.3

Selective logging of cypress

Pathway P1.1.4
Community 1.1 to 1.4

Undisturbed succession, time, and natural die off

Pathway P1.2.1
Community 1.2 to 1.1

Reforestation/Regeneration

Pathway P1.2.3
Community 1.2 to 1.3

Tupelo dominance post disturbance

Pathway P1.3.2
Community 1.3 to 1.2

Clearcut, widescale blowdown, insect, or disease infestation

Pathway P1.3.4
Community 1.3 to 1.4

Hardwood reduction, cypress regrowth, and canopy closure

Pathway P1.4.2
Community 1.4 to 1.2

Clearcut, widescale blowdown, insect, or disease infestation

Pathway P1.4.3
Community 1.4 to 1.3

Selective logging of cypress

State 2
Managed Grassland

Managed grassland represents both improved and unimproved pasture including wooded pasture.

Community 2.1
Improved Undrained Pasture (FSG_G138XA245FL)

Figure 7. Annual production by plant type (representative values) or group (midpoint values)

Figure 8. Plant community growth curve (percent production by month). FL0014, Limpograss. Growth Curves and Dry Matter Distribution for Introduced Warm Season Perennial Grass: Limpograss (Hemarthria altissima).

Jan	Feb	Mar	Apr	May	Jun	Jul	Aug	Sep	Oct	Nov	Dec
J	F	M	A	M	J	J	A	S	O	N	D
1	1	2	13	14	13	21	22	9	2	1	1

Figure 9. Plant community growth curve (percent production by month). FL0019, Maidencane. Growth Curves and Dry Matter Distribution for Native Warm Season Perennial Grass: Maidencane (Panicum hemitomon).

Jan	Feb	Mar	Apr	May	Jun	Jul	Aug	Sep	Oct	Nov	Dec
J	F	M	A	M	J	J	A	S	O	N	D
5	20	22	22	33	10	1	1	10	10	0	0

Figure 10. Plant community growth curve (percent production by month). FL0020, Japanese Millet. Growth Curves and Dry Matter Distribution for Warm Season Annual Grass: Japanese Millet (Echinochloa esculenta).

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	7	15	26	39	7	4	2	0	0	0

Community 2.2
Improved Drained Pasture (FSG_G138XA241FL )

Dominated by planted non-native or domesticated native forage species and evidence of current or recent pasture activity and/or cultural treatments (mowing, grazing, burning, fertilizing; Agro-Ecology Grazing Issues Working Group 2009). Improved pastures have been cleared of their native vegetation. Weedy native species are often common in improved pastures in Florida and include dogfennel (Eupatorium capillifolium), many species of flatsedge (Cyperus spp.), carpetgrasses (Axonopus spp.), crabgrasses (Digitaria spp.), and rustweed (Polypremum procumbens) among many others. (FNAI, 2010) Historically, these sites have been drained frequently to support a variety of land uses including pasture. This drained state is included in this STM because this state exists widely today across the landscape. This site may or may not represent a wetland but drainage of wetlands today is significantly regulated. NRCS is required to consider impacts to wetlands according to Federal laws including, but not limited to, the Clean Water Act, the Wetland Conservation provisions of the Food Security Act of 1985, and State, Tribal, and local laws. It is the policy of NRCS to protect and promote wetland functions and values in all NRCS assistance (National Environmental Compliance Handbook (NECH) 610.36). The native forage species listed are considered adapted to grow on the soils in this group at their natural pH levels. All introduced grass and legume species will need native pH raised to minimum 5.5 (unless noted) for best production. All forages listed are adapted to dryland conditions. Perennial Species: Grasses Warm season (Introduced) • Bahiagrass (Paspalum notatum, pH 5.0 – 6.5) • Bermudagrass (Cynodon dactylon) • Limpograss (Hemarthria altissima) Warm season (Native) • Big Bluestem (Andropogon gerardii) • Purple Bluestem (Andropogon glomeratus var. glaucopsis) • Yellow Indiangrass (Sorghastrum nutans) • Lopsided Indiangrass (Sorghastrum secundum) • Switchgrass (Panicum virgatum) • Eastern Gamagrass (Tripsacum dactyloides) Legumes Warm season • Rhizoma Perennial Peanut (Arachis glabrata, pH 5.8-7.0; additional management required for high water table) Annual Species: Grasses Warm season • Browntop Millet (Urochloa ramosa; =Panicum ramosum) • Pearl Millet (Pennisetum glaucum) • Sorghum (Sorghum bicolor; includes forage sorghums, sudangrass, and their hybrids) Cool season • Ryegrass, annual (Lolium perenne ssp. multi-florum; =L. multiflorum) • Oat (Avena sativa) • Rye (Secale cereale) • Wheat (Triticum aestivum) • Triticale (x Triticosecale) Legumes Warm season • Aeschynomene (Aeschynomene americana) • Hairy Indigo (Indigofera hirsuta) Cool season • White Clover (Trifolium repens, pH 6.0-7.5) • Berseem Clover (Trifolium alexandrinum, pH 6.5-8.0) • Ball Clover (Trifolium nigrescens, pH >6.5) (USDA, NRCS, 2013m)

Figure 11. Annual production by plant type (representative values) or group (midpoint values)

Figure 12. Plant community growth curve (percent production by month). FL0007, Introduced Warm Season Annual Grasses. Growth Curves and Dry Matter Distribution for Introduced Warm Season Annual Grasses.

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	0	4	11	23	35	16	10	3	0	0

Figure 13. Plant community growth curve (percent production by month). FL0005, Native Warm Season Perennial Grasses. Growth Curves and Dry Matter Distribution for Native Warm Season Perennial Grasses.

Jan	Feb	Mar	Apr	May	Jun	Jul	Aug	Sep	Oct	Nov	Dec
J	F	M	A	M	J	J	A	S	O	N	D
1	2	3	5	10	20	27	19	7	3	2	1

Community 2.3
Unimproved Pasture with Woody Encroachment

This community is characterized by a mixture of native and naturalized non-native species. Forage is usually grazed and/or harvested as stored forage, hay or haylage. Stands are generally productive, and forage and grazing management can maintain the community. Woody species grow quickly on this site and can be difficult and expensive to control. Maintenance of grass stands requires implementing pest management practices to control unwanted weedy and woody species.

Pathway P2.1.2
Community 2.1 to 2.2

If previously drained

Pathway P2.1.3
Community 2.1 to 2.3

Pasture abandonment

Pathway P2.2.1
Community 2.2 to 2.1

Hydrologic restoration

Pathway P2.2.3
Community 2.2 to 2.3

Pasture abandonment and/or mismanagement

Pathway P2.3.1
Community 2.3 to 2.1

Pasture restoration and applied grazing

Pathway P2.3.2
Community 2.3 to 2.2

Pasture restoration and applied grazing

State 3
Pine Plantation

Pine plantations in Florida are often dominated by evenaged loblolly, sand, or slash pine (Pinus taeda, P. clausa, or P. elliottii, respectively). Dense pine plantations typically have sparse to absent herbaceous vegetation as a result of shading or a cover of deep pine needle duff. These plantations may be very shrubby or vine-dominated or open at ground level. The groundcover in most cases has been severely impacted by mechanical site preparation, such as roller chopping and bedding. However, while perennial grasses such as wiregrass (Aristida stricta var. beyrichiana) may be greatly reduced, many components of the native groundcover persist even though the relative abundance is altered. Groundcover can be partially restored by thinning and/or frequent burning, although some planting of perennial grasses such as wiregrass may be required. (FNAI, 2010)

Dominant plant species

loblolly pine (Pinus taeda), tree
slash pine (Pinus elliottii), tree
sand pine (Pinus clausa), tree

State 4
Degraded

The degraded State represents vegetation conditions that have been degraded by the introduction and spread of non-native species.

Transition T1.2
State 1 to 2

Land clearing, introduction of grasses, and applied grassland management

Transition T1.3
State 1 to 3

Land clearing, site preparation, and tree planting

Transition T1.4
State 1 to 4

Introduction of non-native species

Transition T2.4
State 2 to 4

Introduction of non-native species

Transition T3.4
State 3 to 4

Introduction of non-native species

Transition T4.1
State 4 to 1

Mechanical, chemical or biological control

Transition T4.2
State 4 to 2

Mechanical, chemical or biological control

Transition T4.3
State 4 to 3

Mechanical, chemical or biological control

Additional community tables

Table 7. Community 2.1 plant community composition

Group	Common name	Symbol	Scientific name	Annual production (lb/acre)	Foliar cover (%)
Grass/Grasslike
1	Graminoids			2100–13000
	limpograss	HEAL5	Hemarthria altissima	8000–13000	–
	maidencane	PAHE2	Panicum hemitomon	5000–6700	–
	Japanese millet	ECES	Echinochloa esculenta	4000–6000	–
	blue maidencane	AMPU6	Amphicarpum purshii	2100–2500	–
Forb
2	Legumes			2000–3000
	shyleaf	AEAM	Aeschynomene americana	2000–3000	–

Table 8. Community 2.2 plant community composition

Group	Common name	Symbol	Scientific name	Annual production (lb/acre)	Foliar cover (%)
Grass/Grasslike
1	Graminoids			900–14000
	Bermudagrass	CYDA	Cynodon dactylon	11000–14000	–
	limpograss	HEAL5	Hemarthria altissima	8800–13000	–
	pearl millet	PEGL2	Pennisetum glaucum	6600–12000	–
	eastern gamagrass	TRDA3	Tripsacum dactyloides	4000–6750	–
	bahiagrass	PANO2	Paspalum notatum	3300–6000	–
	big bluestem	ANGE	Andropogon gerardii	900–1800	–
Forb
2	Legumes			2200–3000
	shyleaf	AEAM	Aeschynomene americana	2200–3000	–
	hairy indigo	INHI	Indigofera hirsuta	2200–3000	–

Supporting information

Inventory data references

Data collection and analysis of field data will be performed during the Verification Stage of ESD development.

Production data for pasture communities taken from the USDA, NRCS Florida Field Office Technical Guide, forage suitability groups (USDA, NRCS, 2013).

Other references

Carr, S. C., Robertson, K. M., & Peet, R. K. 2010. A vegetation classification of fire-dependent pinelands of Florida. Castanea, 75(2), 153-189.

Casey, W. P., & Ewel, K. C. 2006. Patterns of succession in forested depressional wetlands in north Florida, USA. Wetlands, 26(1), 147-160.

Dey, D. C., Brissette, J. C., Schweitzer, C. J., & Guldin, J. M. 2012. Silviculture of forests in the Eastern United States. Cumulative watershed effects of fuel management in the Eastern United States Gen Tech Rep SRS-161. Asheville, NC: US Department of Agriculture Forest Service, Southern Research Station, 7-40.

Florida Chapter Soil and Water Conservation Society. 1989. 26 Ecological Communities of Florida

Greenberg, C. H., & Simons, R. W. 1999. Age, composition, and stand structure of old-growth oak sites in the Florida high pine landscape: implications for ecosystem management and restoration. Natural Areas Journal. 19 (1): 30-40.

Grelen, H. E. 1962. Plant succession on cleared sandhills in northwest Florida. American Midland Naturalist, 36-44.

Haag, K. H., Lee, T. M., & Water, T. B. 2010. Hydrology and ecology of freshwater wetlands in central Florida: a primer. Reston, VA, USA: US Geological Survey.

Inventory, F. N. A. 2010. Guide to the natural communities of Florida: 2010 edition. Florida Natural Areas Inventory, Tallahassee, FL.

Kellison, R. C., & Young, M. J. 1997. The bottomland hardwood forest of the southern United States. Forest Ecology and Management, 90(2-3), 101-115.

Landers, J. L., & Boyer, W. D. 1999. An old-growth definition for upland longleaf and south Florida slash pine forests, woodlands, and savannas (Vol. 29). US Department of Agriculture, Forest Service, Southern Research Station.

LaPierre, G. D. J., Irizarry, N. M., & Andreu, M. G. 2022. Florida Soil Series and Natural Community Associations: FOR384/FR455, 5/2022. EDIS, 2022(3).

Light, H. M. 1993. Hydrology, vegetation, and soils of four North Florida river flood plains with an evaluation of state and federal wetland determinations (Vol. 93, No. 4033). US Department of the Interior, US Geological Survey.

Martin, T. A., & Jokela, E. J. 2004. Stand development and production dynamics of loblolly pine under a range of cultural treatments in north-central Florida USA. Forest Ecology and Management, 192(1), 39-58.

Martin, T. A., Adams, D. C., Cohen, M. J., Crandall, R. M., Gonzalez-Benecke, C. A., Smith, J. A., & Vogel, J. G. 2017. Managing Florida's plantation forests in a changing climate. Florida's Climate: Changes, Variations, & Impacts.

McNab, W.H.; Cleland, D.T.; Freeouf, J.A.; Keys, Jr., J.E.; Nowacki, G.J.; Carpenter, C.A., comps. 2007. Description of ecological subregions: sections of the conterminous United States [CD-ROM]. Gen. Tech. Report WO-76B. Washington, DC: U.S. Department of Agriculture, Forest Service. 80 p

Monk, C. D. 1968. Successional and environmental relationships of the forest vegetation of north central Florida. American Midland Naturalist, 441-457.

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

Schoeneberger, P.J., and Wysocki, D.A. 2017. Geomorphic Description System, Version 5.0. Natural Resources Conservation Service, National Soil Survey Center, Lincoln, NE.

Scott, T. M. 2001. Text to accompany the geologic map of Florida. Florida Geologic Survey, Tallahassee, Florida.

Tamang, B., Hedman, C., Haines, F., Stone, D., & Andreu, M. 2023. Upland forest community composition and structure by ecoregion in 73 Florida state parks–Insights for ongoing management. Forest Ecology and Management, 545, 121237.

U.S. Department of Agriculture, Natural Resources Conservation Service. 2013. Forage Suitability Groups, MLRA 138XA. Retrieved from https://efotg.sc.egov.usda.gov/#/state/FL/documents/section=2&folder=52895.

U.S. Department of Agriculture, Natural Resources Conservation Service. 2013a. Forage Suitability Group G138XA111, Sandy Soils on Ridges and Dunes of Xeric Uplands. Retrieved from https://efotg.sc.egov.usda.gov/references/public/FL/FSG_MLRA_138XA111FL.pdf

U.S. Department of Agriculture, Natural Resources Conservation Service. 2013b. Forage Suitability Group G138XA113, Sandy Soils on Strongly Sloping to Steep Side Slopes of Xeric Uplands. Retrieved from https://efotg.sc.egov.usda.gov/references/public/FL/FSG_MLRA_138XA113FL.pdf

U.S. Department of Agriculture, Natural Resources Conservation Service. 2013c. Forage Suitability Group G138XA114, Sandy Xeric Soils on Stream Terraces or Flood Plains. Retrieved from https://efotg.sc.egov.usda.gov/references/public/FL/FSG_MLRA_138XA114FL.pdf

U.S. Department of Agriculture, Natural Resources Conservation Service. 2013d. Forage Suitability Group G138XA121, Sandy Soils on Rises, Knolls, and Ridges of Mesic Uplands. Retrieved from https://efotg.sc.egov.usda.gov/references/public/FL/FSG_MLRA_138XA121FL.pdf

U.S. Department of Agriculture, Natural Resources Conservation Service. 2013e. Forage Suitability Group G138XA123, Sandy Soils on Strongly Sloping to Steep Side Slopes of Mesic Uplands. Retrieved from https://efotg.sc.egov.usda.gov/references/public/FL/FSG_MLRA_138XA123FL.pdf

U.S. Department of Agriculture, Natural Resources Conservation Service. 2013f. Forage Suitability Group G138XA124, Very Deep, Sandy Soils on Terraces and Floodplains. Retrieved from https://efotg.sc.egov.usda.gov/references/public/FL/FSG_MLRA_138XA124FL.pdf

U.S. Department of Agriculture, Natural Resources Conservation Service. 2013g. Forage Suitability Group G138XA131, Sandy Soils on Rises and Knolls of Mesic Uplands. Retrieved from https://efotg.sc.egov.usda.gov/references/public/FL/FSG_MLRA_138XA131FL.pdf

U.S. Department of Agriculture, Natural Resources Conservation Service. 2013h. Forage Suitability Group G138XA134, Sandy or Sandy Over Loamy Soils on Stream Terraces or Flood Plains. Retrieved from https://efotg.sc.egov.usda.gov/references/public/FL/FSG_MLRA_138XA134FL.pdf

U.S. Department of Agriculture, Natural Resources Conservation Service. 2013i. Forage Suitability Group G138XA141, Sandy Soils, on Flats on Mesic and Hydric Lowlands. Retrieved from https://efotg.sc.egov.usda.gov/references/public/FL/FSG_MLRA_138XA141FL.pdf

U.S. Department of Agriculture, Natural Resources Conservation Service. 2013j. Forage Suitability Group G138XA145, Sandy Soils on Stream Terraces, Flood Plains, or in Depressions. Retrieved from https://efotg.sc.egov.usda.gov/references/public/FL/FSG_MLRA_138XA145FL.pdf

U.S. Department of Agriculture, Natural Resources Conservation Service. 2013j’. Forage Suitability Group G138XA211, Sandy Over Loamy Soils on Knolls and Ridges of Mesic Uplands. Retrieved from https://efotg.sc.egov.usda.gov/references/public/FL/FSG_MLRA_138XA211FL.pdf

U.S. Department of Agriculture, Natural Resources Conservation Service. 2013k. Forage Suitability Group G138XA221, Sandy Over Loamy Soils on Rises, Knolls, and Ridges of Mesic Uplands. Retrieved from https://efotg.sc.egov.usda.gov/references/public/FL/FSG_MLRA_138XA221FL.pdf

U.S. Department of Agriculture, Natural Resources Conservation Service. 2013l. Forage Suitability Group G138XA231, Sandy Over Loamy Soils on Flats and Rises of Mesic Uplands. Retrieved from https://efotg.sc.egov.usda.gov/references/public/FL/FSG_MLRA_138XA231FL.pdf

U.S. Department of Agriculture, Natural Resources Conservation Service. 2013m. Forage Suitability Group G138XA241, Sandy Over Loamy Soils on Flats of Hydric or Mesic Lowlands. Retrieved from https://efotg.sc.egov.usda.gov/references/public/FL/FSG_MLRA_138XA241FL.pdf

U.S. Department of Agriculture, Natural Resources Conservation Service. 2013n. Forage Suitability Group G138XA245, Sandy Over Loamy Soils on Stream Terraces, Flood Plains or in Depressions. Retrieved from https://efotg.sc.egov.usda.gov/references/public/FL/FSG_MLRA_138XA245FL.pdf

U.S. Department of Agriculture, Natural Resources Conservation Service. 2013o. Forage Suitability Group G138XA311, Loamy and Clayey Soils on Knolls and Ridges of Mesic Uplands. Retrieved from https://efotg.sc.egov.usda.gov/references/public/FL/FSG_MLRA_138XA311FL.pdf

U.S. Department of Agriculture, Natural Resources Conservation Service. 2013p. Forage Suitability Group G138XA312, Loamy and Clayey Soils on Ridges and Side Slopes of Mesic Uplands. Retrieved from https://efotg.sc.egov.usda.gov/references/public/FL/FSG_MLRA_138XA312FL.pdf

U.S. Department of Agriculture, Natural Resources Conservation Service. 2013p’. Forage Suitability Group G138XA321, Loamy and Clayey Soils on Rises and Knolls of Mesic Uplands. Retrieved from https://efotg.sc.egov.usda.gov/references/public/FL/FSG_MLRA_138XA321FL.pdf

U.S. Department of Agriculture, Natural Resources Conservation Service. 2013p’’. Forage Suitability Group G138XA322, Loamy and Clayey Sols on Rises, Knolls, and Ridges of Mesic Uplands. Retrieved from https://efotg.sc.egov.usda.gov/references/public/FL/FSG_MLRA_138XA322FL.pdf

U.S. Department of Agriculture, Natural Resources Conservation Service. 2013q. Forage Suitability Group G138XA331, Loamy and Clayey Soils on Flats and Rises of Mesic Uplands. Retrieved from https://efotg.sc.egov.usda.gov/references/public/FL/FSG_MLRA_138XA331FL.pdf

U.S. Department of Agriculture, Natural Resources Conservation Service. 2013r. Forage Suitability Group G138XA334, Loamy and Clayey Soils on Stream Terraces and Flood Plains. Retrieved from https://efotg.sc.egov.usda.gov/references/public/FL/FSG_MLRA_138XA334FL.pdf

U.S. Department of Agriculture, Natural Resources Conservation Service. 2013s. Forage Suitability Group G138XA341, Loamy and Clayey Soils on Flats of Hydric or Mesic Lowlands. Retrieved from https://efotg.sc.egov.usda.gov/references/public/FL/FSG_MLRA_138XA341FL.pdf

U.S. Department of Agriculture, Natural Resources Conservation Service. 2013t. Forage Suitability Group G138XA345, Loamy and Clayey Soils on Stream Terraces, Flood Plains or in Depressions. Retrieved from https://efotg.sc.egov.usda.gov/references/public/FL/FSG_MLRA_138XA345FL.pdf

U.S. Department of Agriculture, Natural Resources Conservation Service. 2013u. Forage Suitability Group G138XA521, Shallow or Moderately Deep, Sandy or Loamy Soils on Rises and Ridges of Mesic Uplands. Retrieved from https://efotg.sc.egov.usda.gov/references/public/FL/FSG_MLRA_138XA521FL.pdf

U.S. Department of Agriculture, Natural Resources Conservation Service. 2017. Geomorphic Description System, Version 5.0. Schoeneberger, P.J., and D.A. Wysocki (eds). USDA-NRCS, National Soil Survey Center, Lincoln, NE.

U.S. Department of Agriculture, Natural Resources Conservation Service. 2022. Land resource regions and major land resource areas of the United States, the Caribbean, and the Pacific Basin. Agriculture Handbook 296.

U.S. Environmental Protection Agency. 2013. Level III and IV ecoregions of the continental United States: Corvallis, Oregon, U.S. EPA, National Health and Environmental Effects Research Laboratory, map scale 1:3,000,000, https://www.epa.gov/eco-research/level-iii-and-iv-ecoregions-continental-united-states.

Contributors

Ferrara, Jack
Figueroa, Martin
Duvall, Matthew

Approval

Charles Stemmans, 6/09/2025

Acknowledgments

Sincere appreciation goes to the MLRA 138X ecological sites technical team, especially NRCS Florida State Soil Scientist, Isabelle Giuliani, and NRCS Florida State Forester, Conrad Wysocki, for their persistent collaboration in the development of these Provisional ESDs.

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	06/09/2025
Approved by	Charles Stemmans
Approval date
Composition (Indicators 10 and 12) based on	Annual Production