crowberry, (genus Empetrum), genus of three species of low evergreen shrubs of the heath family (Ericaceae). The plants thrive in subarctic, alpine, and boreal regions and produce juicy edible fruits that are somewhat acidic in taste. The fruits are an important food source for numerous species of songbirds and waterfowl as well as bears, voles, and other mammals. They have a long history of use by indigenous peoples as a food and medicine.

Physical description

Crowberries grow about 25 cm (10 inches) tall and are somewhat trailing in habit. The narrow simple leaves are about 1 cm (0.4 inch) long and somewhat succulent. The flowers are very small and purplish pink. The fruits are true berries, about 1 cm long, and range from reddish to purple to black, depending on the species.

Species

Crowberry, or black crowberry (Empetrum nigrum), is native to cool regions of North America, Asia, and Europe and is the most common species of the genus. Purple crowberry, or rockberry (E. eamesii), is found in the northeastern United States and eastern Canada, and red crowberry (E. rubrum) is native to Chile, Argentina, and the Falkland Islands.

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tundra, a major zone of treeless level or rolling ground found in cold regions, mostly north of the Arctic Circle (Arctic tundra) or above the timberline on high mountains (alpine tundra). Tundra is known for large stretches of bare ground and rock and for patchy mantles of low vegetation such as mosses, lichens, herbs, and small shrubs. This surface supports a meagre but unique variety of animals. The Finns called their treeless northern reaches the tunturi, but the concept of a vast frozen plain as a special ecological realm called tundra was developed by the Russians.

One constant factor shaping the tundra is alternate freezing and thawing of the ground. Along with the factors mentioned above, this freeze-thaw cycle sets the tundra apart from two ecosystems frequently found adjacent to it—the icy polar barrens on the one hand and the evergreen taiga on the other. Permafrost—perennially frozen ground—is a significant feature of the Arctic tundra; however, it does not typically occur in alpine regions.

Distribution

The global extent of the tundra biome is considerable, accounting for roughly 10 percent of Earth’s surface. The southern limit of Arctic tundra follows the northern edge of the coniferous forest belt. In North America this line lies above latitude 60° N, while in Eurasia most of it occurs north of 70° N—except in eastern Siberia, where it extends southward to 60° N in Kamchatka. The northward bulge of forest in Eurasia is a result of the warmer summers that occur over that large contiguous landmass.

Alpine tundra covers approximately 3 percent of Earth’s land surface, and it is mostly found in the Northern Hemisphere. This habitat can be found in mountainous areas worldwide, occurring at high elevations where temperatures are too low and winds are too strong for the growth of trees. The average elevation where alpine tundra occurs is generally higher near the Equator than at the poles.

Because nearly all of Antarctica is covered with ice, it lacks a well-developed tundra, though lichens, mosses, and at least three species of flowering plants occur in more favourable habitats there.

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