Greater Yellowstone Ecosystem
The Greater Yellowstone Ecosystem (GYE) is one of the last remaining large, nearly intact ecosystems in the northern temperate zone of the Earth. It is located within the northern Rocky Mountains, in areas of northwestern Wyoming, southwestern Montana, and eastern Idaho. Yellowstone National Park and the Yellowstone Caldera 'hotspot' are within it. 
Conflict over ecological and resource management has been controversial, and the area is a flagship site among conservation groups that promote ecosystem management. The Greater Yellowstone Ecosystem (GYE) is one of the world's foremost natural laboratories in landscape ecology and Holocene geology, and is a world-renowned recreational destination. It is also home to the diverse native plants and animals of Yellowstone.
Yellowstone National Park boundaries were drawn in 1872 to include all the known geothermal basins in the region. No other landscape ecology considerations were incorporated into boundary decisions. By the 1970s, however, the grizzly bear's (Ursus arctos) range in and near the park became the first informal minimum boundary of a theoretical "Greater Yellowstone Ecosystem" that included at least 16,000 square kilometres (4,000,000 acres). Since then, definitions of the greater ecosystem's size have steadily grown larger. A 1994 study listed the size as 76,890 square kilometres (19,000,000 acres), while a 1994 speech by a Greater Yellowstone Coalition leader enlarged that to 80,000 square kilometres (20,000,000 acres).
In 1985 the United States House of Representatives Subcommittees on Public Lands and National Parks and Recreation held a joint subcommittee hearing on Greater Yellowstone, resulting in a 1986 report by the Congressional Research Service outlining shortcomings in interagency coordination and concluding that the area's essential values were at risk.
Federally managed areas within the GYE include:
- United States National Park Service (NPS) — Yellowstone National Park, Grand Teton National Park, and John D. Rockefeller, Jr. Memorial Parkway.
- United States National Forest Service (USFS): Gallatin, Custer, Caribou-Targhee, Bridger-Teton and Shoshone National Forests
- United States Fish and Wildlife Service (USFWS) — National Elk Refuge
The GYE also encompasses some privately held lands surrounding those managed by the U.S. Government.
Ecosystem management by species
The great ecosystem concept has been most often advanced through concerns over individual species rather than over broader ecological principles. Though 20 or 30 or even 50 years of information on a population may be considered long-term by some, one of the important lessons of Greater Yellowstone management is that even half a century is not long enough to give a full idea of how a species may vary in its occupation of a wild ecosystem.
The Yellowstone hot springs are important for their diversity of thermophilic bacteria. These bacteria have been useful in studies of the evolution of photosynthesis and as sources of thermostable enzymes for molecular biology. Although the smell of sulfur is common and there are some sulfur fixing cyanobacteria, it has been found that hydrogen is being used as an energy source by extremophile microbes.
Among native plants of the GYE, whitebark pine (Pinus albicaulis) is a species of special interest, in large part because of its seasonal importance to grizzly bears, but also because its distribution could be dramatically reduced by relatively minor global warming. In this case, researchers do not have a good long-term data set on the species, but they understand its ecology well enough to project declining future conservation status. A more immediate and serious threat to whitebark pines is an introduced fungal rust disease, White Pine Blister Rust (Cronartium ribicola), which is causing heavy mortality in the species. Occasional resistant individuals occur, but in the short to medium term, a severe population decline is expected.
Estimates of the decline of quaking aspen (Populus tremuloides) on the park's northern range since 1872 range from 50% to 95%. Perhaps no conservation controversy underway in Greater Yellowstone more clearly reveals the need for comprehensive interdisciplinary research.
Several factors are suspected in the quaking aspen's changing status, including:
- Native American influences on numerous mammal species and on fire ecology-return intervals before the creation of the park in 1872.
- European influences on wildfire frequency since 1886; regional climate warming.
- Human harvests of beaver and ungulates in the first 15 years of the park's history, and of wolves and other predators before 1930.
- Human settlement on traditional ungulate migration routes north of the park since 1872; ungulate (especially elk) effects on all other parts of the ecosystem since 1900; and human influences on elk distribution in the park.
Anecdotal information on grizzly bear abundance dates to the mid-19th century, and administrators have made informal population estimates for more than 70 years. From these sources, ecologists know the species was common in Greater Yellowstone when Europeans arrived and that the population was not isolated before the 1930s, but is now. Researchers do not know if bears were more or less common than now.
A 1959-1970 bear study suggested a grizzly bear population size of about 176, later revised to about 229. Later estimates have ranged as low as 136 and as high as 540; the most recent is a minimum estimate of 236. Although the Greater Yellowstone population is relatively close to recovery goals, the plan's definition of recovery is controversial. Thus, even though the population may be stable or possibly increasing in the short term, in the longer term, continued habitat loss and increasing human activities may well reverse the trend.
Yellowstone cutthroat trout (Oncorhynchus clarki bouvieri) have suffered considerable declines since European settlement, but recently began flourishing in some areas. Especially in Yellowstone Lake itself, long-term records indicate an almost remarkable restoration of robust populations from only three decades ago when the numbers of this fish were depleted because of excessive harvest. Its current recovery, though a significant management achievement, does not begin to restore the species' historical abundance.
Early accounts of pronghorn (Antilocapra americana) in Greater Yellowstone described herds of hundreds seen ranging through most major river valleys. These populations were decimated by 1900, and declines continued among remaining herds. On the park's northern range, pronghorn declined from 500-700 in the 1930s to about 122 in 1968. By 1992 the herd had increased to 536.
Gray Wolf reintroduction
The park is a commonly cited example of apex predators affecting an ecosystem through a trophic cascade. After the reintroduction of the gray wolf in 1995, researchers noticed drastic changes occurring. Elk, the primary prey of the gray wolf, became less abundant and changed their behavior, freeing riparian zones from constant grazing. The respite allowed willows and aspens to grow, creating habitat for beaver, moose, and scores of other species. In addition to the effects on prey species, the gray wolf's presence also affected the park's grizzly bear population. The bears, emerging from hibernation, chose to scavenge off wolf kills to gain needed energy and fatten up after fasting for months. Dozens of other species have been documented scavenging from wolf kills.
- Schullery, Paul. "The Greater Yellowstone Ecosystem". Our Living Resources. U.S. Geological Survey. Archived from the original on 2006-09-27. Retrieved 2007-03-13.
- Initial wikipedia article was based on public domain Biology.usgs.gov content written by Paul Schullery, from the U.S. National Park Service.
- "Beyond the Headlines". Living on Earth. March 20, 2015. Retrieved March 22, 2015.
- Gray Wolves as Climate Change Buffers in Yellowstone
- Turner, Jack (2008). Travels in Greater Yellowstone. New York: St. Martin's Press. ISBN 978-0-312-26672-1.