Northern Prairie Wildlife Research Center
Understanding two characteristics of the region, spatial heterogeneity and
temporal instability, is essential to sound habitat management. Actions that
do not address the questions of where and when, as well as what and why, may
yield disappointing results. Glaciation resulted in a collage of landscape
features. At a distance, the most obvious features are glacial lake beds,
till plains, and moraines (Stewart, 1975; Kantrud et al., 1989). Viewed from
close up, even these features are highly heterogeneous. For example, the Missouri
Coteau, a large morainal belt, contains various types of moraines, glacial
outwash plains, and small lake beds, each possessing different topography,
soil types, and vegetation. Temporally, the climate of the Prairie Pothole
Region is characterized by instability and extremes. Droughts recur frequently
and cause cyclic changes in the flora and fauna of the region. Also, there
is a gradient in annual precipitation from wet in the east to dry in the west
(Winter, 1989, pp. 24-28). Associated with this variation is a gradient in
plant communities from bluestem prairie in the east, through the mixed prairie
of wheatgrass, bluestem, and needlegrass, to wheatgrass and needlegrass in
the west (Küchler, 1964).
Plant communities of the region, especially those in wetlands, have always
been unstable. Cyclic weather patterns, grazing by huge herds of bison and
other ungulates, and fires were integral to the landscape. Settlement of the
region by Europeans resulted in massive changes to the prairie landscape.
Tillage of natural grasslands not only caused the loss of much of the original
prairie but fragmented the remaining grassland into small blocks surrounded
by cropland. Free-ranging bison were nearly extirpated from the region and
replaced by cattle. Eurasian plant species were introduced on purpose or by
accident, and subsequently invaded the native grassland communities. Wildfires,
essential to maintaining native plant communities, were suppressed, which
allowed invasion of the region by woody species. Droughts in the 1930s brought
extreme soil erosion to the denuded lands. In response to the erosion problem,
windbreaks were planted. Woody species introduced in these windbreaks, as
well as around farmsteads, small towns, and cities, further changed and fragmented
the landscape of the region.
Wetland ecosystems also were substantially altered. Many of the potholes
were drained to create new lands for agriculture and to increase the efficiency
of tillage operations. In Iowa and southern Minnesota, nearly all of the original
wetlands were eliminated (Mann, 1974). From the 1780s to the 1980s, about
42%, 50%, 35%, and 26% of wetlands were lost in the states of Minnesota, North
Dakota, South Dakota, and Montana, respectively (Dahl, 1992). Further, dams
were constructed on most of the major river systems, inundating the natural
riverine and riparian habitats.
Along with these habitat alterations came profound changes in the community
of predators; this story has been nicely summarized by Sargeant et al. (1993).
Before settlement, the top predators throughout most of the region were gray
wolves (Canis lupus) and occasional grizzly bears (Ursus arctos).
Populations of coyotes (Canis latrans) and red foxes (Vulpes vulpes)
were low, while those of swift foxes (Vulpes velox) were high. The
primary prey for wolves and bears were bison and other large ungulates.
Early settlers were intolerant of wolves and, by the early 1900s, virtually
eliminated them from much of the region. In the absence of wolves, coyotes
greatly increased in number. The favored natural prey of coyotes includes
deer and smaller mammals. Coyotes also became targets of human dislike and
were aggressively persecuted by hunting, trapping, and poisoning. When they
were reduced, especially in the eastern part of the area, the numbers of red
foxes began to explode. Among the preferred prey of foxes are ducks, especially
nesting females, and their eggs. Predation by red foxes on ducks and other
large ground-nesting birds is often severe; Sargeant and Raveling (1992) estimated
that foxes take about 800,000 adult ducks in the Prairie Pothole Region during
a typical breeding season.
Currently, restrictions on the use of poisons and aerial huntingalong
with low fur prices, which reduces trapping pressureare causing the
numbers of coyotes to increase again, especially in the US portion of the
region. This change is depressing densities of red foxes (A.B. Sargeant, US
Fish and Wildlife Service, personal communication, 1992). Like so many other
features of the prairie landscape, predator communities are dynamic and change
in response to natural and, especially, human actions.
Because the Prairie Pothole Region can produce as much as 50% of the continental
waterfowl population ( Smith et al., 1964; Crissey, 1969) and host even more
during migration, programs were designed to protect these birds and their
habitats. Accordingly, wildlife refuges were established throughout the Region.
Habitats protected by these refuges, however, are not typical of those in
the Prairie Pothole Region. Rather, they usually contain one or more large
lakes (often created by river impoundments), surrounded by various amounts
of upland habitat.
Precipitous declines in waterfowl populations and continued loss of wetland
habitat prompted the US Fish and Wildlife Service to initiate its Small Wetlands
Acquisition Program in 1962 (Sidle, 1983). Under that program, the Service
purchased wetlands and, more extensively, acquired easements that prevented
landowners from draining, filling, or burning wetlands within easement tracts.
Most tracts owned in fee title are small, often appearing as islands of grassland
and wetland in a sea of tilled land. Although these programs have been effective
in preserving some of the wetland base, rarely have they maintained the integrity
of the original prairie ecosystem.
Declining commodity prices owing to overproduction and an alarming loss
of soil prompted the initiation of a number of programs designed to convert
cropland to grass and legume cover over the past four decades. The Soil Bank
Program, initiated in the 1950s, converted vast areas from cropland to grassland,
but by the late 1960s these lands were returned to cultivation. The Water
Bank Program of the 1970s restored grassland to some cropped areas. More recently,
the Conservation Reserve Program has been successful in converting cropland
to grassland on highly erodible soils.
In summary, natural variability and changing priorities for land management
have created a mosaic of habitat types, each of which is in constant flux.
It is impossible to return to the landscape that was present in pre-settlement
times. Some species have been extirpated, certain habitats eliminated, and
wetland hydrology irreversibly altered. The Prairie Pothole Region, although
sparsely populated, is one of the most intensively managed landscapes in North
America. It will remain so despite talk of the Buffalo Commons. The challenge
for wildlife agencies is to manage those parts of the system they control
and to influence management on those parts outside their jurisdiction. A landscape
perspective facilitates this approach.
Fig. 1. The Prairie Pothole Region of
North America (after Mann, 1974).
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