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Desert and Tundra Biomes
Chapter 3
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7.1 Deserts Objectives Describe the characteristics of a desert Explain how desert organisms adapt to live in their environment Deserts are different, but they all receive very little rain.
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Deserts continued Desert soil
Rich in minerals Poor in organic materials Very little leaching Leaching a process where rainwater moving through soil carries minerals deeper into the soil Little rain -> little leaching -> upper desert soil rich in minerals
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Deserts continued Lack of rainfall makes deserts dry
Prevents many plants from living there Slows decay of organic material Not much topsoil Soil easily blown away Exposing the Pavement
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Pavement The lower layer of the desert soil It is the desert floor
Made mostly of Hard-baked sand Bare rock particles Or both
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Types of Deserts in the US
Cool Deserts - Sagebrush On eastern side of the mountains in western US Hot Deserts - Cactus In the southwest: Arizona, New Mexico and western Texas
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Desert Climate Lack of precipitation is the limiting factor
Less than 25 cm per year, most less than 10 cm Determines the types of plants Determines the types of animals Most rain during a few short storms Most water runs off due to compacted pavement
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Desert Temperature Varies Greatly
Moisture helps to stabilize temperature Acts like a blanket Absorbs heat in day Holds in warmth at night Without this moisture, desert temperature rise and fall dramatically within 24 hour periods
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Desert Biome Video
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Desert Organisms Must be adapted to survive with
Lack of water Extreme temperatures Despite these challenges, deserts are actually species-rich complex ecosystems
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Desert Plants They Must
Be able to absorb scarce water from ground Prevent water loss form tissues Cactus spines (leaves) reduce water loss by reducing surface area Succulents – have thick water filled tissue (cacti, aloe vera) An attractive source of food and water for desert animals Spines also help protect from being eaten by animals
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Desert Plants continued
Another adaptation is the roots Some shallow but covering a wide area Others grow very deep Both help to maximize the amount of water they can get
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Desert Animals Many types Most get water from their food
Most have adaptations to help reduce water loss Also adaptations to survive the heat Many are nocturnal – active at night, sleeping during the heat of the day
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7.2 Formation of Deserts Objective
Illustrate the processes that cause deserts to form.
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Natural Desert Formation
Two broad belts of deserts Northern one near Tropic of Cancer Southern near Tropic of Capricorn Around the equator (tropics) very moist air After moisture has fallen as rain air becomes dry Then flows towards poles becoming cooler and heavier Sinks back to earth as dry winds forming deserts
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Rainshadow Effect Exact locations are determined by local geographic features such as mountains In U.S. Winds move from west to east Forces warm moist air over mountains Drops moisture on mountains Cool dry air reaches eastern side Picks up moisture from soil Soil becomes very dry forming desert
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Life in the Desert Video
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Desertification Deserts often bordered by semiarid regions with grasses and shrubs Human activity (raising livestock) has caused these semiarid regions to become deserts The process of changing semiarid land into desert as a result of human activity is called desertification
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Human Impact on the Desert
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7.3 Tundra Objectives Describe why the characteristics of the tundra make it a fragile ecosystem Compare the characteristics of tundra organisms with those of their relatives in warmer climates The tundra is a cold , windy, dry region.
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Tundra Facts In northern hemisphere just south of polar ice caps in Alaska, Canada, Greenland, Iceland, Norway and Asia A large biome –10% of Earth’s surface Fewer types of organisms than any other biome Lack of diversity makes them fragile and unstable
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Tundra Video
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Tundra Climate Like a desert little precipitation A cold climate
Less than 25cm per year A cold climate Usually below 10 degrees Celsius Most precipitation falls as ice or snow Temperature is the limiting factor
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Permafrost Only the top layer, or active zone, of soil thaws in summer
The active zone may be as thin as 8 cm The frozen soil beneath the active zone is called permafrost A dense mat of mosses, grasses, and other plant life keeps the ground insulated and prevents the permafrost from melting Any disruption of this mat affects the permafrost
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Tundra Climate continued
Tundra vegetation does not recover from disruption as quickly as in other biomes Rain in summer cannot penetrate the permafrost Water collects forming bogs,, marshes, ponds, and streams Creates a great breeding ground for mosquitoes and black flies (an important link in the food web) Permafrost is therefore important to the stability of a tundra ecosystem
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Tundra Organisms Plants Short growing season Small and close to ground
Ground warmed by radiant energy Roots close to surface Small trees (less than 1 meter) Lichens are very important producers
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Tundra Animals Seasonal visitors (migrate south for winter)
Safe place for breeding due to less predators Birds feed on mosquitoes and flies Predators feed on birds Caribou- large migratory mammal Thick coat big hooves Feed on lichen Fox, Bears, Wolverines don’t migrate
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The End
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