Rangeland and wildlife resources
Rangelands are expansive natural areas primarily characterized by native vegetation like grasses, shrubs, and forbs. Covering about 50% of the Earth's land surface, they play a vital role in supporting livestock, wildlife, and diverse ecosystems. These lands are not typically suitable for intensive agriculture due to limitations such as low precipitation and poor soil quality. Rangelands provide essential resources, including recreational opportunities and habitats for various animal species, while also serving as watersheds and mining locations.
The dynamic nature of rangelands is influenced by numerous factors, including climate changes, grazing practices, and human encroachment. Modern environmental concerns focus on the degradation of these ecosystems, particularly due to livestock grazing and its impact on riparian zones. Additionally, rangelands face pressures from increased agricultural development and the challenges faced by nomadic herders in adapting to changing conditions. Despite these challenges, rangelands have demonstrated resilience, historically supporting both wildlife and human communities for centuries and holding the potential for sustainable use in the future.
Rangeland and wildlife resources
Rangeland encompasses a wide variety of land types, including grasslands, shrublands, marshes, and meadows as well as much desert and alpine land. Rangeland is a valuable and resilient ecosystem resource that supports considerable plant and animal life.
Background
Rangeland generally refers to a kind of land rather than a use of that land. The Society for Range Management defines rangelands as “land on which the native vegetation (climax or natural potential) is predominantly grasses, grasslike plants, forbs, or shrubs.” Rangeland, states the society, “includes lands revegetated naturally or artificially when routine management of that vegetation is accomplished mainly through manipulation of grazing” as well as “natural grasslands, savannas, shrublands, most deserts, tundra, alpine communities, coastal marshes and wet meadows.”

Rangelands usually have some limitation on intensive agriculture, such as low and erratic precipitation, lack of soil fertility, shallow or rocky soil, or steep slopes. In addition to habitat for livestock and wildlife grazing, rangelands serve other multiple-use functions, such as providing recreational opportunities, watersheds, mining locations, and habitat for many animal species. Renewable natural resources associated with rangelands are plants and animals (and, in some senses, water). Nonrenewable resources include minerals and other extractable materials.
Variety of Rangelands
Rangelands are extensive and extremely variable. As defined by the Society for Range Management, they occupy approximately 50 percent of the world’s total land surface and about 500 million hectares in the United States alone. Rangelands are home to countless nomadic herders on nearly every continent. They vary from high-elevation alpine tundra and high-latitude Arctic tundra to tropical grasslands. The tall grass prairies in the United States (now mostly plowed for intensive agriculture) and the rich grasslands of eastern Africa are among the most productive. Rangelands grade into woodlands and forest as woody species and trees become more abundant. Some forests are grazed by wild and domestic animals, and the distinction between rangeland and forest is often not clear. The other difficult distinction is between rangeland and pastureland. Pastureland is generally improved by seeding, fertilization, or irrigation, whereas rangelands support native plants and have little intensive improvement.
In the United States, rangeland improvements during the twenty years after World War II often included brush control, grazing management, seeding, and other practices, but rangelands were not irrigated. After the 1970s, when fuel costs increased and environmental concerns over use increased, brush control practices were reduced considerably. Modern environmental concerns include rangeland degradation from livestock grazing, especially on riparian vegetation along streams, endangered animal and plant species. These issues have become controversial in the United States.
Rangelands as Ecosystems
Rangelands constitute natural ecosystems with nonliving environmental factors such as soil and climatic factors, primary producers (grasses, forbs, and shrubs), herbivores (livestock; big game animals such as deer, bison, pronghorn antelope; and many rodents and insects), carnivores and omnivores (coyotes, bears, weasels, eagles, spiders, and cougars), and decomposers that break down organic matter into elements that can be utilized by plants. Plants convert carbon dioxide and water into complex carbohydrates, fats, and proteins that can be utilized by animals feeding on the plants. Individual chemical elements are circulated throughout the various components. Many of these elements are present in the parent material of the soil (for example, phosphorus, magnesium, potassium, and sulfur). Nitrogen, on the other hand, is present in large amounts in the but must be converted (fixed) into forms that can be utilized by plants before it can be cycled.
When chemicals are taken up by plant roots from the soil solution, they are available to a wide group of herbivores from small microbes to large ungulates. Eventually, nutrients are passed on to higher trophic groups (omnivores and carnivores). Both plant and animal litter is eventually broken down by decomposers—bacteria, fungi, and other small soil organisms—and returned to the soil or, in the case of nitrogen, given off to the atmosphere.
Energy is fixed through the process of photosynthesis and transformed to forms useful for the plants themselves and animals that feed on the plants. However, energy is degraded at each step along the way and cannot be used again. Energy is transferred but not cycled. Grazing animals on rangelands influence plants by removing living tissue, by trampling, and by altering competitive relations with other plants. Large grazing animals tend to compact the soil and reduce infiltration and increase surface runoff. Plants furnish all the nutrients obtained by herbivores and eventually by carnivores and omnivores as well.
Rangeland Dynamics
Rangelands vary considerably with time; they are not static. Scientists are gaining a better understanding of some factors related to rangeland change over time. Pollen records and, in the southwestern United States, packrat middens have been used to reconstruct past and vegetational changes. Some areas have become drier and others more mesic. Formation and retreat of glaciers have influenced rangelands, climatic patterns, and soil development. A recent general trend in many rangelands of the world is an increase in woody plants at the expense of grasses. Many factors are probably responsible for these shifts, but fire control, excessive livestock grazing, climatic shifts, introduction of exotic species, and the influence of native animals are likely causal agents.
Rangelands are threatened by encroachment from crop agriculture as human populations increase. Nomadic herders traditionally dealt with periodic drought conditions by moving to areas not impacted by drought. In modern society, with reductions of area available for livestock grazing and restrictions for political reasons, herders are often forced to maintain higher livestock numbers to support their growing families and others directly dependent on livestock. Despite various kinds of disturbances and stresses on rangelands, these areas have supported many large grazing animals and people for centuries. They are resilient and will likely be sustained for many more centuries to come.
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