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The Tundra of North America is a Level I ecoregion of North America designated by the Commission for Environmental Cooperation (CEC) in its North American Environmental Atlas.
One of the planet's most recent biomes, a result of the last ice age only 10,000 years ago, the tundra contains unique flora and fauna formed during the last glaciation in areas unrestricted by permanent ice. The tundra region is found in high latitudes, primarily in Alaska, Canada, Russia, Greenland, Iceland, and Scandinavia, as well as the Antarctic Islands. Consisting of the arctic, alpine, and Antarctic regions, and stemming from the Samer language, tundra literally means a "high and dry place".
The arctic tundra has an exceptionally short growing period, minimal sunlight, and limited resources, creating a brutal environment for plants and animals. By adapting to these harsh conditions, animals and plants represent iconic characteristics of the tundra. Plants grow in aggregated formations which provide shelter from wind, and ice and also improve seed success.[1] Animals have adapted with specialized organs, such as a rete mirabile, an organ that efficiently transfers heat. Frogs and amphibians use "anti-freeze" to prevent organ damage while hibernating. Polar bears, foxes, and owls use insulated fur and feathers to protect from the cold conditions.[2] These complex interactions between plants, animals and abiotic factors in the tundra are held together by the permafrost layer, located 450 metres (1,480 ft) under the soil.[3] However climate change is causing this crucial layer of frozen soil to melt. As a result, tundra communities are becoming unstable and basic processes are breaking down. Other factors such as oil development and drilling in tundra ecosystems have completely disheveled the wildlife and vegetation populations. Tundra exploration vehicles used for oil development and polar bear tours ("an eco-friendly" industry) leave traces of tire marks for 20-plus years after a disturbance occurs. Other factors such as high CO2 emissions from tourism and from warming tundra soil, create a positive feedback loop, accelerating changes to the tundra.[4]
^Fletcher, B; Gornal; Poyatos; Press; Stoy; Huntley; Baxter; Pheonis (2012). "Photosynthesis and productivity in heterogeneous arctic tundra: consequences for ecosystems function of mixing vegetation types at stand edges" (PDF). Journal of Ecology. 100 (2): 441–451. doi:10.1111/j.1365-2745.2011.01913.x.
^"Tundra Animals". Archived from the original on 10 December 2013. Retrieved 28 April 2013.
^"Dry, Cold and Windy". 12 February 2019. Archived from the original on 12 January 2010.
^"Potential impacts of proposed oil and gas development on the Arctic Refuge's coastal plain: Historical overview and issues of concern". Archived from the original on 29 May 2004.
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