PROTECTING WISCONSIN'S BIODIVERSITY

 
 
   
 
Community Name Global Rank State Rank Community Group

Wet Prairie

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Photo by Andy Clark

 

Counties with Mapped NHI Occurrences

Wet prairies are tall grassland communities that tend to occur on ecotones between more upland wet-mesic prairies and wetter sedge meadows. Soils are mineral, usually clay, sandy clay, or sandy clay loam, sometimes with a layer of loam (rarely mucky mineral) above. They occur most often on glacial lakeplain landforms but can also be found in wetland pockets on till plains and other landforms. Wet prairies are almost always small in size, seldom reaching more than a few acres except in large, intact lakeplain prairies.

Wet prairies are dominated by graminoids such as Canada bluejoint grass (Calamagrostis canadensis) and prairie cordgrass (Spartina pectinata) along with tussock sedge (Carex stricta) and yellow-headed fox sedge (Carex annectens). Other sedges may also be present such as running marsh sedge (Carex sartwellii), Bebb's sedge (Carex bebbii), marsh straw sedge (Carex tenera), and woolly sedge (Carex pellita). Big bluestem (Andropogon gerardii) is also often present in low amounts but is never dominant. In contrast to wet-mesic prairies, prairie grasses typically found in drier habitats are usually absent from wet prairies, such as Indian grass (Sorghastrum nutans), little bluestem (Schizachyrium scoparium), and prairie dropseed (Sporobolus heterolepis).

Indicator forbs include winged loosestrife (Lythrum alatum) and cowbane (Oxypolis rigidior), though they are seldom abundant. Other more common forbs include species found in wet-mesic prairies such as swamp thistle (Cirsium muticum), mountain-mint (Pycnanthemum virginianum), yellow-headed coneflower (Ratibida pinnata), prairie dock (Silphium terebinthinaceum), Riddell’s goldenrod (Solidago riddellii), New England aster (Symphyotrichum novae-angliae), Culver’s root (Veronicastrum virginicum), and golden Alexander's (Zizia aurea) alongside forbs found in wetter habitats such as tall sunflower (Helianthus giganteus), giant goldenrod (Solidago gigantea), tall meadow-rue (Thalictrum dasycarpum), spotted Joe-pye-weed (Eutrochium maculatum), and grass-leaved goldenrod (Euthamia graminifolia). In general, the vegetation in wet prairies tends to be taller, and more rank and robust compared to either wet-mesic prairies or sedge meadows.

 
 
 

Wet prairies are characterized by their grass and sedge dominance on moist mineral soils. They often occur as a fringe along the upland edge of sedge meadows or emergent marshes or on the lower edge of wet-mesic prairies. They can be distinguished from wet-mesic prairies by their higher water table (usually within 12" of the surface during a normal year), taller (usually 3' or more), more rank vegetation, and higher prevalence of grasses and forbs associated with wetter habitats such as bluejoint grass, prairie cord grass, Joe-Pye-weed, boneset (Eupatorium perfoliatum), common water hemlock (Cicuta maculata), swamp milkweed (Asclepias incarnata), and water smartweed (Persicaria amphibia). In addition, wet prairies lack grasses found in drier habitats such as Indian grass, little bluestem, and prairie dropseed.

Wet prairies also share similarities with southern sedge meadows, though sedge meadows tend to occur on organic soils (rarely mineral soils) while wet prairies almost always occur on mineral soils. Wet prairies also have a higher prevalence of grasses such as prairie cordgrass, bluejoint grass, and occasionally big bluestem, while southern sedge meadows have a higher prevalence of sedges. Similarly, calcareous fens (sometimes called prairie fens due to their prairie flora) are also usually located on organic soils (peat and/or marl) rather than mineral soils. While fens impacted by past land use such as plowing or hydrologic alteration can have vegetation very similar to a wet prairie (including prairie cord grass and tall sunflower), examination of the soil with a soil probe (at least 36-40" deep) will almost always reveal peat (sometimes oxidizing to mucky mineral) and marl rather than a shallow clay layer that typifies wet prairies.

Wet prairies have some forbs in common with emergent marshes but lack the dominance of cattails and bulrushes that typify marshes, although aggressive non-native cattails (e.g.,Typha angustifolia, T. glauca) may invade and take over wet prairies, blurring this distinction.

Wet prairies also sometimes occur in wetland complexes with shrub-carr, and can become invaded by shrubs if the hydrology and fire regime is disrupted. The dividing line between shrub-carr and prairie is generally the degree of shrub cover, with shrub-carr having greater than 50% cover but the length of time shrubs have been dominant and the presence of prairie indicators can help distinguish a shrub-invaded but restorable wet prairie from a shrub-carr with a long presence on the landscape.

Species of Greatest Conservation Need (SGCN) are associated with habitats (or natural communities) and places on the landscape. Understanding relationships among SGCN, natural communities and ecological landscapes help us make decisions about issues affecting SGCN and their habitat and how to respond. Download the Wildlife Action Plan association score spreadsheet to explore rare species, natural communities and ecological landscape associations

Conservation actions respond to issues or threats, which adversely affect species of greatest conservation need (SGCN) or their habitats. Besides actions such as restoring wetlands or planting resilient tree species in northern communities, research, surveys and monitoring are also among conservation actions described in the Wisconsin Wildlife Action Plan because lack of information can threaten our ability to successfully preserve and care for natural resources.