Print Report

G175 Schizachyrium scoparium - Panicum virgatum - Andropogon glomeratus Patch Prairie Group

Type Concept Sentence: This vegetation group encompasses the medium-scale grassland, "barrens" and prairie-like perennial grass-dominated vegetation of the inner coastal plains of the southeastern United States, including the Atlantic and Gulf coastal plains and a portion of the Mississippi River Alluvial Plain of Arkansas. Examples which have not experienced recent disturbance may contain scattered trees and shrubs.


Common (Translated Scientific) Name: Little Bluestem - Switchgrass - Bushy Bluestem Patch Prairie Group

Colloquial Name: Southeastern Coastal Plain Patch Prairie

Hierarchy Level:  Group

Type Concept: This vegetation group encompasses the medium-scale grassland, "barrens" and prairie-like vegetation of the inner coastal plains of the southeastern United States, including the Atlantic and Gulf coastal plains from Georgia to Texas, and a specific portion of the Mississippi River Alluvial Plain of Arkansas. These communities are dominated by perennial grasses, with some scattered trees and shrubs, particularly in examples which have not experienced recent disturbance. The most extensive and noteworthy examples are known from specific areas where particular substrates or edaphic conditions favor the development and maintenance of this grassland vegetation. This includes the chalky Cretaceous "Black Belt" of Alabama and Mississippi (and related areas in Georgia), calcareous or saline clay-influenced areas of the Gulf coastal plains of Louisiana and Texas, and silty or loess-influenced plains of western Tennessee, Arkansas, Oklahoma, and Mississippi. These are all Cretaceous and younger substrates, in contrast to prairie-like vegetation on soils developed from older (e.g., Mississippian) limestones in the Interior Low Plateau. In the presettlement landscape and throughout the nineteenth century, the combination of grazing (first by native ungulates and then by free-ranging cattle into the mid-twentieth century) and fire (from lightning and/or Native Americans), combined with the unusual edaphic conditions, kept these areas relatively free of woody vegetation. High-quality examples would support a dense herbaceous layer dominated by tall grasses such as Schizachyrium scoparium and Sorghastrum nutans, but many stands currently suffer from a lack of disturbance which inhibits woody plant succession. With range enclosure and an increasing lack of fire during the twentieth century, the dynamics of the landscape have changed, and the coverage of fire-intolerant woody species has increased. The grassland vegetation is now reduced to patches, or its flora persists in pastures which are under more continuous grazing pressure than would have occurred under the former processes and disturbance regime. Other frequent graminoid taxa include Andropogon glomeratus, Andropogon virginicus, Bouteloua curtipendula, Carex cherokeensis, and Paspalum floridanum. In depressions and drainages, Andropogon gerardii and/or Panicum virgatum will have greater importance and Tripsacum dactyloides may be present. At this more mesic end of the continuum, invasion by woody plants is an even more serious threat.

Diagnostic Characteristics: These are perennial grasslands of the coastal plains, found on a variety of soil types, many of which have unusual edaphic features (droughtiness, impeded drainage, salinity). The primary dominant grasses include Schizachyrium scoparium and Sorghastrum nutans, as well as Andropogon spp., Panicum spp., and Sporobolus spp. Other more mesic grasses (Andropogon gerardii, Panicum virgatum, Tripsacum dactyloides) are found in mesic and wet phases. Some proposed factors which have functioned to maintain the openness of these vegetation types include the distinctive soils and resulting stresses to vegetation, as well as the effects of fire and grazing.

Rationale for Nominal Species or Physiognomic Features: No Data Available

Classification Comments: This vegetation group includes a variety of grassland associations ranging from relatively dry to wet-mesic, occurring in a variety of areas across the inner coastal plains physiographic province.

Similar NVC Types: No Data Available
note: No Data Available

Physiognomy and Structure: This vegetation is primarily dominated by perennial grasses, but examples may have scattered to patchy trees and shrubs. Most examples occur on circumneutral soils, or other unusual substrates (clay, gravels, saline soils, etc.).

Floristics: The typical perennial grasses that dominate examples of this vegetation include Andropogon gerardii, Schizachyrium scoparium, and Sorghastrum nutans. Moist to wetter swales or zones may be embedded within and among the typical stands; in these areas, Andropogon gerardii and/or Panicum virgatum will have greater importance (DeSelm and Murdock 1993), and Tripsacum dactyloides may be present. Among the most frequent trees in the Jackson Purchase barrens include Quercus marilandica, Quercus stellata, and Quercus velutina (Bryant and Martin 1988). Dominant plants in stands of this group vary across this broad region. There are several subregional types and variability among these which is expressed in the associations. Typical trees (whose cover may be sparse) include Carya illinoinensis, Carya myristiciformis, Juniperus virginiana var. virginiana, Maclura pomifera (within its native range), Quercus muehlenbergii, Quercus pagoda, Quercus shumardii, Quercus sinuata, and Quercus stellata. Some typical shrubs and small trees include Cercis canadensis var. canadensis, Crataegus spp., Diospyros virginiana, Forestiera ligustrina, Frangula caroliniana, Ilex decidua, Prunus angustifolia, Rhus copallinum, Rhus aromatica, Rosa setigera, Sideroxylon lycioides, Symphoricarpos orbiculatus, and Ulmus alata. Other grasses and graminoids may include Bouteloua curtipendula, Carex cherokeensis, Carex microdonta, Fimbristylis puberula var. puberula, Leersia virginica, Muhlenbergia capillaris, Panicum anceps, Panicum flexile, and Sporobolus compositus. Forbs (which vary across the broad geographic range) may include Allium canadense var. mobilense, Dalea candida, Dalea purpurea, Desmanthus illinoensis, Desmodium ciliare, Echinacea pallida, Echinacea purpurea, Liatris aspera, Liatris squarrosa, Liatris squarrulosa, Lythrum alatum, Manfreda virginica, Marshallia caespitosa, Nemastylis geminiflora, Packera tampicana, Ratibida pinnata, Silphium integrifolium, Silphium laciniatum, Silphium terebinthinaceum, Silphium trifoliatum var. latifolium, Solidago auriculata, Symphyotrichum dumosum (= Aster dumosus), Symphyotrichum patens (= Aster patens), Symphyotrichum lanceolatum var. lanceolatum (= Aster lanceolatus), Thelesperma filifolium, and Zigadenus nuttallii. Some more western taxa that are present in West Gulf Coastal Plain examples are Acacia angustissima, Dalea compacta var. compacta, Dracopis amplexicaulis, Euphorbia bicolor, Eustoma exaltatum ssp. russellianum (= Eustoma russellianum), Grindelia lanceolata, Indigofera miniata (= Indigofera miniata var. leptosepala), Neptunia lutea, Onosmodium bejariense var. occidentale (= Onosmodium occidentale), Palafoxia reverchonii, Rudbeckia missouriensis, and Stenosiphon linifolius.

Dynamics:  Much of the natural vegetation of the Black Belt region (and the rest of the inner coastal plain as well) has been converted to pasture and agricultural uses, with concomitant destruction of most prairie remnants (DeSelm and Murdock 1993). Of the approximately 100,000 acres of Blackland Prairies mapped during the general land surveys of the early and mid 1800s in Mississippi, probably less than 500 acres of Jackson Prairie vegetation exists today, even if one considers grazed areas and vacant agricultural lands with a semblance of prairie species (R. Wieland pers. comm.). Almost all of the lands were converted to agriculture. Some of the lands are now reverting back to prairie after being abandoned. More recently, lands are being converted to fescue pasture; other abandoned lands have become stands of eastern red-cedar. The number of acres in good condition is probably less than 100.

In western Tennessee and Kentucky (the "Jackson Purchase" or "Jackson Plain" barrens), a number of early reports mentioned extensive prairies and emphasized the importance of annual fires in maintaining these grasslands (Bryant and Martin 1988). Scattered groves of fire-tolerant oaks were likely interspersed among these grasslands (M. Evans pers. comm.). With fire suppression, groves of trees rapidly expanded and largely replaced the prairies. In the Black Belt (and in other areas as well), the presence of Juniperus virginiana-dominated zones may represent invasion by this species in the absence of sufficiently frequent or intense fire (DeSelm and Murdock 1993). Fire return time is variable (and speculative in some cases), but fires were probably frequent (potentially on a two- to five-year return interval), originating from lightning or human ignition origin, and are thought to have occurred in late summer to early autumn prior to European settlement. Under current conditions, individual prairie openings or barrens are small and isolated from one another but were formerly more extensive prior to European settlement, forming a more extensive mosaic of grassland and woodlands under frequent fire regimes. Some proposed factors which have functioned to maintain the openness of this vegetation following the reduction of fire frequency include the droughty soils (with clay, chalk, gravel) and resulting stresses to vegetation, as well as some occasional fire. Fralish et al. (1999) noted that both post oak and chestnut oak woodlands are essentially the result of fire suppression in the barrens and historic savannas. In some areas, where the soils are particularly harsh (droughty, nutrient-poor, and/or rocky), stands may retain an open aspect in the absence of fire. Some of the extant examples are largely dependent on contemporary management regimes.

Environmental Description:  The most extensive and noteworthy examples are known from specific areas where particular substrates or edaphic conditions favor the development and maintenance of this grassland vegetation. This includes the chalky Cretaceous "Black Belt" of Alabama and Mississippi (and related areas in Georgia), calcareous or saline clay-influenced areas of the Gulf coastal plains of Louisiana and Texas, and well-drained, gravelly, thin-soil plains of western Tennessee and Kentucky, as well as related areas in Texas, Arkansas, Oklahoma, and Mississippi. Climate: Climate varies somewhat across the coastal plains, but the Black Belt area has an average annual precipitation of 130-140 cm and a frost-free period of 200-250 days.

Soil/substrate/hydrology: Examples are found on edaphically distinctive substrates, including the chalky Cretaceous "Black Belt" soils of Alabama and Mississippi (and related areas in Georgia), calcareous or saline clay-influenced areas of the Gulf coastal plains of Louisiana and Texas, and the thin-soil, well-drained, and gravelly plains of western Tennessee, Arkansas, Oklahoma, and Mississippi. The Black Belt region derives its name from the nearly black, rich topsoil that developed over Selma chalk, and has long been noted as a distinct topographic region in the state of Mississippi (Lowe 1921). The Black Belt associations generally occur on Cretaceous-age chalk, marl and calcareous clay. This includes calcareous soils of the Sumter, Binnsville, and Demopolis series, described as beds of marly clay over Selma chalk (including the Demopolis and Mooreville formations). The soils of the Jackson Prairie openings are presently mapped as the Maytag Series, a fine montmorillonitic, thermic Entic Chromudert. This deep, slowly permeable soil has formed in residuum weathered from marl of chalk of the Blackland Prairies (Wieland 1995). The soils of some examples in the Upper West Gulf Coastal Plain of Arkansas and Oklahoma include relatively deep soils with circumneutral surface pH, as well as on chalk deposits, and thin soils over limestone outcrops with rock fragments. In Louisiana, examples are documented from the Fleming geologic formation, but are also known from the Cook Mountain Formation, the Jackson Group, as well as the Morse Clay Calcareous Prairie of the northwestern part of the state. The examples in the Jackson Purchase region of Kentucky and adjacent Tennessee are found on soils that are predominantly thin, well-drained, and gravelly. This group likely did not develop on the deeper loess soils of the region. The former barrens were on flat to gently rolling lands just to the dry side of the moisture gradient (Bryant and Held 2001).

Geographic Range: Examples are known from several distinct areas in the coastal plains of the southeastern United States. In particular, these include (but are not limited to) the Jackson Purchase area of western Kentucky (primarily Graves County and parts of Calloway County), extending into limited areas of adjacent Tennessee; a relatively small natural region of the Upper West Gulf Coastal Plain of Arkansas and adjacent Oklahoma; and another relatively small natural region of Louisiana and Texas. The Black Belt Prairie component is primarily restricted to the Black Belt (Subsection 231Ba) (Keys et al. 1995) or Blackland Prairie area (Ecoregion 65a) and Flatwoods/Blackland Prairie Margins area (Ecoregion 65b) of Griffith et al. (2001). This region is primarily in Alabama and Mississippi, ranging north in a depauperate form to southern Tennessee (McNairy County) (DeSelm 1989b). The Jackson Prairie component of this group is found in a relatively small natural region of Mississippi, known as the Jackson Hills Subsection 231Bj of Keys et al. (1995) and Cleland et al. (2007) and the Jackson Prairie Ecoregion 65r of EPA (2004). There is also a recently recognized component found in limited parts of Georgia (e.g., on both sides of the Ocmulgee River on the Fort Valley Plateau of Bleckley, Houston, Peach, and Twiggs counties). There are also outlying occurrences southward in the Chunnenuggee Hills and Red Hills (both of these parts of the Southern Hilly Coastal Plain (Ecoregion 65d)), and Buhrstone/Lime Hills (Ecoregion 65q) of southern Alabama (in Washington, Wilcox, Monroe, and Clark counties). There are some limited examples in Ecoregion 65i (Fall Line Hills; e.g., Jones Bluff in Alabama). Examples of the Grand Prairie vegetation occur on the oldest land surfaces in the Mississippi River Alluvial Valley and the highest land surface in the river-deposited portions of the ecoregion (234 of Keys et al. 1995 and Cleland et al. 2007) (T. Foti pers. comm.).

Nations: US

States/Provinces:  AL, AR, GA, KY, LA, MS, OK, TN, TX




Confidence Level: Moderate

Confidence Level Comments: No Data Available

Grank: GNR

Greasons: No Data Available


Concept Lineage: No Data Available

Predecessors: No Data Available

Obsolete Names: No Data Available

Obsolete Parents: No Data Available

Synonomy: No Data Available

Concept Author(s): H.R. DeSelm and N. Murdock (1993)

Author of Description: M. Pyne

Acknowledgements: No Data Available

Version Date: 05-12-15

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