Prairie Pothole Region

Last updated
Map of the Prairie Pothole Region of North America (U.S. Geological Survey, Northern Prairie Wildlife Research Center) PrairiePotholeRegionMap.gif
Map of the Prairie Pothole Region of North America (U.S. Geological Survey, Northern Prairie Wildlife Research Center)
Barringer Slough in Iowa, a remnant of the extensive prairie wetlands that once covered the region. Barringer-Arial.jpg
Barringer Slough in Iowa, a remnant of the extensive prairie wetlands that once covered the region.

The Prairie Pothole Region (PPR) is an expansive area of the northern Great Plains that contains thousands of shallow wetlands known as potholes. These potholes are the result of glacier activity in the Wisconsin glaciation, which ended about 10,000 years ago. The decaying ice sheet left behind depressions formed by the uneven deposition of till as buried ice blocks melted in ground moraines. [1] These depressions are called potholes, glacial potholes, kettles, or kettle lakes. They fill with water in the spring, creating wetlands, which range in duration from temporary to semi-permanent. [2] The region covers an area of about 800,000 sq. km and expands across three Canadian provinces (Saskatchewan, Manitoba, and Alberta) and five U.S. states (Minnesota, Iowa, North and South Dakota, and Montana). The hydrology of the wetlands is variable, which results in long term productivity and biodiversity. The PPR is a prime spot during breeding and nesting season for millions of migrating waterfowl. [3]

Contents

Hydrology

Few natural surface water drainage systems occur in the region as pothole wetlands are not connected by surface streams. They receive most of their water from spring snowmelt and precipitation. [4] Some pothole wetlands also receive groundwater inflow, so they typically last longer each year than those that only receive water from precipitation. Shorter-duration wetlands fed only by precipitation typically are sources of groundwater recharge. [5] The hydrology of the potholes is very variable, responding to changes in precipitation and groundwater, and results in regular wet-and-dry cycles. [6]

Vegetation

Prairie Pothole wetlands in South Dakota Prairie Pothole Landscape South Dakota - 53106527617.jpg
Prairie Pothole wetlands in South Dakota

The vegetation of the PPR consists of emergent plants and tall grasses, while the prairie surrounding the region has dense grassland vegetation. The composition of a local plant community is heavily affected by the amount of water available. In wetter wetlands that retain water through the summer, the common plant is hard-stem bulrush, along with soft-stem bulrush and common threesquare in slightly drier regions of the wetlands. The vegetation in permanently flooded wetlands is more aquatic; duckweeds, pondweeds, aquatic buttercups, and aquatic smartweeds are some of the most common. In drier wetlands of the PPR, the vegetation varies from spikerush, which is found in the wetter areas of the wetland, to foxtail barley and wheatgrass on the outer edges of the wetland. [7] The variable availability of water in the Prairie Pothole Region is buffered by an abundant seed bank under the soil, comprising species that thrive under different water regimes. During times of drought, shortgrass species increase and expand their range, while during wetter periods, tallgrass and mixed prairie communities become more common. [8]

Wildlife

The Prairie Pothole Region provides important habitats for migratory waterfowl and other wildlife, supporting more than 50% of North America's migratory waterfowl. [9] In particular, the region is one of North America's most important breeding areas for ducks. Although the region contains only about one-tenth of the continent's habitat area for breeding of waterfowl, roughly half the primary species of game ducks on the continent breed there. The region accounts for more than 60% of the breeding populations of mallard, gadwall, blue-winged teal, northern shoveler, northern pintail, redhead, and canvasback ducks. [10]

Threats

Conversion of land for agriculture is a significant factor in the loss of wetlands in the PPR. More than half of the wetlands have been drained for farming. [5] [9] In particular, 90% of the prairie wetlands of the Minnesota River basin have been lost as habitat. [11] The wetlands that do persist, surrounded as they are by agricultural lands, are also affected. Chemical runoff, sedimentation, and nutrient flow into the wetlands have adverse impacts. [12]

Climate change is an adverse factor in the long-term viability of PPR wetlands for breeding ducks and other birds. Without mitigation, severe droughts and rising temperatures will cause many pothole wetlands to dry up sooner in the spring. In turn, due to the timing of waterfowl migrations, these dried wetlands will not present suitable breeding habitat. Warming-related drought may affect as much as 90 percent of the PPR's remaining wetlands. [12] Simulations suggest that climate change will shift the most productive wetlands from the center of the region (southeastern Saskatchewan and the Dakotas) to edges of the PPR in the east and north. [2] However, research has suggested that the effect of global warming is overshadowed by that of intensified land use and drainage of wetlands. [13]

See also

Related Research Articles

<span class="mw-page-title-main">Marsh</span> Low-lying and seasonally waterlogged land

In ecology, a marsh is a wetland that is dominated by herbaceous plants rather than by woody plants. More in general, the word can be used for any low-lying and seasonally waterlogged terrain. In Europe and in agricultural literature low-lying meadows that require draining and embanked polderlands are also referred to as marshes or marshland.

<span class="mw-page-title-main">Redhead (bird)</span> Species of North American diving duck

The redhead is a medium-sized diving duck. The scientific name is derived from Greek aithuia, an unidentified seabird mentioned by authors including Hesychius and Aristotle, and Latin americana, of America. The redhead is 40–56 cm (16–22 in) long with an 74–84 cm (29–33 in) wingspan; the weight ranges from 1,030–1,080 g (36–38 oz), with males weighing an average of 1,080 g (38 oz) and females an average of 1,030 g (36 oz). It belongs to the genus Aythya, together with 11 other described species. The redhead and the common pochard form a sister group which together is sister to the canvasback. This waterfowl is easily distinguished from most other ducks by the male's copper colored head and pale blue bill during the breeding season; from its close relative canvasback it is distinguished by the more rounded head, shorter bill, and yellow, not red, eye. The Eurasian common pochard is even more similar, but very rarely overlaps in range; it also differs in having a red eye, and a more acute, less rounded head shape.

<span class="mw-page-title-main">Sora (bird)</span> Species of bird

The sora, sora rail or Carolina crake is a small waterbird of the rail family Rallidae, sometimes also referred to as the sora rail or sora crake, that occurs throughout much of North America. The genus name Porzana is derived from Venetian terms for small rails, and the specific carolina refers to the Carolina Colony. The common name "Sora" is probably taken from a Native American language.

<span class="mw-page-title-main">Aspen parkland</span> Temperate grasslands, savannas, and shrublands ecoregion of Canada and the United States

Aspen parkland refers to a very large area of transitional biome between prairie and boreal forest in two sections, namely the Peace River Country of northwestern Alberta crossing the border into British Columbia, and a much larger area stretching from central Alberta, all across central Saskatchewan to south central Manitoba and continuing into small parts of the US states of Minnesota and North Dakota. Aspen parkland consists of groves of aspen, poplar and spruce, interspersed with areas of prairie grasslands, also intersected by large stream and river valleys lined with aspen-spruce forests and dense shrubbery. This is the largest boreal-grassland transition zone in the world and is a zone of constant competition and tension as prairie and woodlands struggle to overtake each other within the parkland.

<span class="mw-page-title-main">Ducks Unlimited</span> American conservation organization

Ducks Unlimited (DU) is an American 501(c)(3) nonprofit organization dedicated to the conservation of wetlands and associated upland habitats for waterfowl, other wildlife, and people.

<span class="mw-page-title-main">Erie National Wildlife Refuge</span> Protected area in Pennsylvania, United States

The Erie National Wildlife Refuge is an 8,777-acre (3,552 ha) National Wildlife Refuge located in Crawford County, Pennsylvania. Named after the Erie tribe, it was established to provide waterfowl and other migratory birds with nesting, feeding, brooding, and resting habitat.

<span class="mw-page-title-main">Chase Lake Prairie Project</span> Effort to restore and protect waterfowl in North Dakota, United States

The Chase Lake Prairie Project is considered the "National Flagship Project" of the North American Waterfowl Management Plan (NAWMP). The goal is to rehabilitate 5,500,000 acres (2,200,000 ha) of wetland around Chase Lake on the Missouri Coteau. The project was dedicated in September 1989.

Grays Lake is a wetland in Idaho, United States. It lies in Bonneville County and Caribou County. Grays Lake National Wildlife Refuge was established in the area in 1965. Ranching is the predominant use of surrounding lands.

<span class="mw-page-title-main">Oak Hammock Marsh</span> Marsh in Manitoba, Canada

Oak Hammock Marsh is a marsh and a wildlife management area located 34 kilometres (21 mi) north of Winnipeg, Manitoba, Canada. The WMA is considered to be a Class IV protected area under the IUCN protected area management categories. The marsh is recognized as an Important Bird Area (IBA) for its globally significant numbers of waterfowl and shorebirds. It is a designated Ramsar site due to its international importance as a breeding and staging area for waterfowl and other migratory birds. It is 3,578.47 hectares in size.

The North American Waterfowl Management Plan (NAWMP) is an international plan to conserve waterfowl and migratory birds in North America. It was established in 1986 by Canada and the United States, and expanded to include Mexico in 1994.

<span class="mw-page-title-main">Lacassine National Wildlife Refuge</span> Wildlife refuge in Louisiana

Lacassine National Wildlife Refuge is located in Cameron and Evangeline Parishes in southwestern Louisiana, was established in 1937 by Executive Order No. 7780 as "a refuge and breeding ground for migratory birds and other wildlife." The refuge is nearly 35,000 acres (140 km2) in size, including 653 acres (2.64 km2) leased from the Cameron Parish School Board. The Evangeline Parish unit is called Duralde Prairie and is currently being developed. It is located south of the city of Eunice.

<span class="mw-page-title-main">Big Stone National Wildlife Refuge</span> National wildlife refuge in Minnesota, United States

Straddling the headwaters of the Minnesota River in west-central Minnesota, Big Stone National Wildlife Refuge is within the heart of the tallgrass prairie's historic range. Today, less than one-percent of tallgrass prairie remains.

Litchfield Wetland Management District is located on the eastern edge of the Prairie Pothole Region in central Minnesota. More than 33,000 acres (130 km2) of United States Fish and Wildlife Service-owned land and 8,000 acres (32 km2) of wetland easements provide marsh, prairie, transition, and woodland habitats. District lands are located on over 150 waterfowl production areas scattered throughout seven counties. These areas vary greatly in size and vegetation and provide habitat for numerous plant and animal species.

<span class="mw-page-title-main">Long Lake Wetland Management District</span>

Long Lake Wetland Management District encompasses three counties in south-central North Dakota, an area famed for its wealth of waterfowl-producing potholes and native prairie grasslands. Headquarters for the Wetland Management District is located in the Long Lake National Wildlife Refuge office near Moffit, North Dakota, which is about 35 miles southeast of Bismarck. Topographical landforms of the area include Missouri Coteau and Missouri River Slope. Precipitation averages just under 16 inches per year. Approximately 68 percent of the land in the three county area remains virgin sod - native mixed-grass prairie. The dominant land use is cattle grazing. The Coteau wetlands found in the northeastern portion of the Wetland Management District are classic prairie potholes of various sizes and types that are prime duck production habitat. These areas, when wet, are very productive. Soils in this area are generally deep and quite productive. Due to the rolling nature of the landscape on the Coteau, a lot of the land is also characterized as highly erodible. Conversely, many of the wetlands on Missouri River Slope portion of the Wetland Management District are large semi-permanent and permanent alkali wetlands. There are 21 wetland sites on the Missouri River Slope that have a history of periodic avian botulism outbreaks. These areas occasionally present localized problems for significant numbers of migratory birds. Soils on the Missouri River Slope are characteristically shallow with high proportions of sand and gravel. Much of the land is highly erodible. Since 1985, substantial land acreage in the three county area that was once farmed has been retired to Conservation Reserve Program grasslands. The program has assisted in restoring waterfowl populations for many species in the Wetland Management District which exceed the highest level ever recorded since surveys began.

The effects of climate change in the Canadian province of Saskatchewan are now being observed in parts of the province. There is evidence of reduction of biomass in Saskatchewan's boreal forests that is linked by researchers to drought-related water stress stemming from global warming, most likely caused by greenhouse gas emissions. While studies, as early as 1988 have shown that climate change will affect agriculture, whether the effects can be mitigated through adaptations of cultivars, or crops, is less clear. Resiliency of ecosystems may decline with large changes in temperature. The provincial government has responded to the threat of climate change by introducing a plan to reduce carbon emissions, "The Saskatchewan Energy and Climate Change Plan", in June 2007.

<span class="mw-page-title-main">Blanca Wetlands</span>

The Blanca Wetlands Area of Critical Environmental Concern, or Blanca Wildlife Habitat Area, is an area of the San Luis Valley in Colorado, United States, that serves as a refuge for birds, fish and other wildlife. It is about 11 miles (18 km) northeast of Alamosa on County Road 25. The wetlands had been completely destroyed by pumping and diversion of water for irrigation. Starting in 1965 the Bureau of Land Management began to restore them, and they have become an increasingly important ecological habitat for shorebirds, waterbirds and other wildlife and native plants.

The ecology of the Great Plains is diverse, largely owing to their great size. Differences in rainfall, elevation, and latitude create a variety of habitats including short grass, mixed grass, and tall-grass prairies, and riparian ecosystems.

Heron Lake is a lake in Jackson County, in the U.S. state of Minnesota.

Last Mountain Lake National Wildlife Area is a National Wildlife Area (NWA) in the Canadian province of Saskatchewan. The protected area is in the Prairie Pothole Region of North America, which extends throughout three Canadian provinces and five U.S. states. It is also within Palliser's Triangle and the Great Plains ecoregion. The site is an Important Bird Area (IBA) of Canada, designated as Last Mountain Lake NWA .

<span class="mw-page-title-main">Chase Lake</span> Lake in North Dakota

Chase Lake is a 2,053 acres (8.31 km2), shallow lake in Stutsman County, North Dakota. It is the focal point of several protected areas administered by the U.S. Fish and Wildlife Service and U.S. Geographical Survey. It is known as one of the largest nesting areas for the American white pelican.

References

  1. Johnson, Rex R.; Oslund, Fred T.; Hertel, Dan R. "The past, present, and future of prairie potholes in the United States". Researchgate. Journal of Soil and Water Conservation. Retrieved 8 December 2024.
  2. 1 2 Johnson, W. Carter; Millet, Bruce V.; Gilmanov, Tagir; Voldseth, Richard A.; Guntenspergen, Glenn R.; Naugle, David E. (2005). "Vulnerability of Northern Prairie Wetlands to Climate Change". BioScience. 55 (10): 863. doi: 10.1641/0006-3568(2005)055[0863:vonpwt]2.0.co;2 . ISSN   0006-3568.
  3. "Prairie Pothole Region". www.ducks.org. Retrieved 2019-11-13.
  4. "Comprehensive Report Ecological System - Great Plains Prairie Pothole". explorer.natureserve.org. Retrieved 2019-12-02.
  5. 1 2 Euliss, Ned H. Jr.; Wrubleski, Dale A.; Muchet, David M. (1999). "Wetlands of the Prairie Pothole Region: Invertebrate species composition, ecology, and management". In Batzer, Darold P.; Rader, Russell B.; Wissinger, Scott A. (eds.). Invertebrates in freshwater wetlands of North America: Ecology and management. John Wiley and Sons. pp. 471–514. ISBN   978-0-471-29258-6 . Retrieved 22 November 2019.
  6. Mitsch, William; Gosselink, James (2015). Wetlands (5th ed.). Hoboken, New Jersey: Wiley. pp. 61–62. ISBN   978-1-118-67682-0.
  7. Montana Natural Heritage Program. "Great Plains Prairie Pothole". Montana Field Guide. Retrieved 19 October 2020.
  8. Anderson, Jim; Samargo, Emily. "Wetland Types: Prairie Potholes". Wetlands Management. Archived from the original on 28 November 2012. Retrieved 19 October 2020.
  9. 1 2 "Regional Ecosystems: The Prairie Pothole Region". National Biological Information Infrastructure. Archived from the original on 25 October 2011. Retrieved 26 October 2020.
  10. Austin, Jane E. (3 August 2006). "Waterfowl in the Prairie Pothole Region". Northern Prairie Wildlife Research Center. United States Geological Survey. Archived from the original on 29 June 2011. Retrieved 26 October 2020.
  11. "Wetlands". Fact Sheets. Minnesota River Basin Data Center, Minnesota State University, Mankato. 15 April 2011. Retrieved 26 October 2020.
  12. 1 2 "Prairie Potholes". National Wildlife Federation. Retrieved 26 October 2020.
  13. Niemuth, Neal D.; Fleming, Kathleen K.; Reynolds, Ronald E. (2014-06-17). "Waterfowl Conservation in the US Prairie Pothole Region: Confronting the Complexities of Climate Change". PLOS ONE. 9 (6): e100034. Bibcode:2014PLoSO...9j0034N. doi: 10.1371/journal.pone.0100034 . ISSN   1932-6203. PMC   4061047 . PMID   24937641.