Robert W. Christopherson Charlie Thomsen Chapter 11 The Dynamic Planet.
Chapter 20 Terrestrial Biomes Geosystems 6e An Introduction to Physical Geography Robert W....
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Transcript of Chapter 20 Terrestrial Biomes Geosystems 6e An Introduction to Physical Geography Robert W....
![Page 1: Chapter 20 Terrestrial Biomes Geosystems 6e An Introduction to Physical Geography Robert W. Christopherson Charles E. Thomsen.](https://reader035.fdocuments.in/reader035/viewer/2022062216/56649e105503460f94afc05d/html5/thumbnails/1.jpg)
Chapter 20Terrestrial Biomes
Geosystems 6eAn Introduction to Physical Geography
Robert W. ChristophersonCharles E. Thomsen
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Terrestrial Biomes Biogeographic Realms: geographic region where a group of plant and animal species have evolved; generally correspond to continents There are no rigidly defined boundaries between realms; transition zonesEcotone: boundary transition zone between adjoining ecosystem regions
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Biogeographic Realms
Terrestrial Ecosystems: self-sustaining association of land-based plants and animals and their abiotic environment; characterized by specific plant formation classesBiome: large, stable terrestrial ecosystem characterized by specific plant and animal communities
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BiomesUsually named for dominant vegetation
6 broad biomes: forest, savanna, grassland, shrubland, desert, and tundra
These divided into more specific vegetation units
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Earth’s Major Terrestrial BiomesEquatorial and Tropical Rain Forest Tropical Seasonal Forest and Scrub Tropical Savanna Midlatitude Broadleaf and Mixed Forest Needleleaf Forest and Montane Forest Temperate Rain Forest Mediterranean Shrubland Midlatitude Grasslands Deserts Arctic and Alpine Tundra
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Figure 20.3
Tropical Savanna
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Tropical Savanna ClimatesSouth FloridaInfluenced by ITCZTwo temperature maximumGrasslands with scattered, drought-resistant treesTransitional biome between tropical forests and semiarid regionsSavanna originally covered 40% of land
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Tropical Savanna BiomeBetter agricultural soils
Sorghum, wheat, peanuts
Xerophytic plantsSmall, thick leaves; rough bark; waxy or hairy leaf surfaces
Under the influence of the ITCZ for 6 months
Convectional thunderstorms
Semi-permanent high pressure
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Serengeti Plains
Sahel Region
Home to large land mammals
Zebras, giraffe, buffalo, elephant, lions, cheetahs, ostrich, crocodile
Figure 20.8
Tropical Savanna Biome
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Midlatitude Broadleaf and Mixed ForestSoutheastern US, Atlantic coastal plain, New England, and Great Lakes region
Pines historically dominated the coastal plain
A more even mix of hardwoods and pines occurs farther north and inland
Red fox, white-tailed deer, flying squirrel, possum, bear, cardinal
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Broadleaf Mixed Forest
Figure 20.9
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Midlatitude Broadleaf and Mixed Forest
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Midlatitude Broadleaf and Mixed ForestDeciduous broadleaf trees are common, such as:
Many, many oak species
All hickories
Maples (red and sugar)
Elms
Pines and other conifers are also important.
Poor agricultural soils
Pine plantations
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Needleleaf Forest and Montane Forest
In northern North America and northern Eurasia, the closed-canopy version of this forest is called boreal forest.
In the transitional forests in the higher latitudes, the more open version of this forest is called taiga.
This biome is also found in higher elevations and is called montane forest.
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Needleleaf Forest and Montane
Forest
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Needleleaf Forest and Montane Forest
Consist almost exclusively of needleleaf trees
Pines
Spruces
Firs
Larches
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Temperate Rain Forest
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Temperate Rain Forest
Dense forests of firs, cedars, hemlocks, and spruces dominate
Persistent moisture, humidity in understory (lots of moss)
In Pacific Northwest, called the coastal evergreen forest
Some of the largest trees in the world exist here
Lower biodiversity than tropical rain forest
Thick undergrowth - ferns
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Mediterranean Shrubland
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Mediterranean Shrublandaka temperate shrubland, chaparral
Woody shrubs and grassy woodlands
Important for agriculture
Fire adapted speciesDeep rooted with sprouting capabilities
schlerophyllous
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Midlatitude Grasslands
Figure 20.15 Figure 20.16
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Midlatitude Grasslands
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Precipitation great enough to support grasses and some trees, but not forests.
Drought and fire prevent large forests from growing.
Fires are very common in the grassland biome.
Soils found in grasslands are some of the most fertile in the world, though.
Tallgrass and shortgrass prairie in U.S.
The Grassland Biome
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DesertsCamel, bighorn sheep, kangaroo rat, scorpion, snakes, and roadrunners
Most animals are nocturnal to avoid high temperatures; cold-blooded animals
Low organic content of the soil; high salt content
Xerophytes
Warm deserts = tropics, subtropics
Cold deserts = midlatitudes
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The Desert Biome
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DesertificationDesertification: expansion of the desert
Occurs along the margins of semiarid and arid lands
Caused by poor agricultural practices, such as: overgrazing, soil overuse/abuse, improper management of soil moisture, erosion, salinization, deforestation, and climate change.
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Arctic and Alpine Tundra
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Arctic TundraAssociated with high latitudes
60-80 day growing seasons
No trees, dwarf plants, soggy ground
Low temperatures, precipitation, and evaporation
Poorly developed soils underlain by permafrost
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Tundra vegetation: mosses, sedges, snow lichen, arctic meadow grass
Musk ox, caribou, reindeer, weasels, rabbits, polar bears, and mosquitoes
Important breeding ground for migratory birds: geese, swans, waterfowl
Arctic Tundra
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Alpine TundraAssociated with high elevations; above timberlineSimilar composition to Arctic TundraNo permafrost, better drainageAndes, White Mts of California, Alps, HimalayasVegetation: grasses, herbs, stunted shrubsMountain goats, bighorn sheep, elk, voles
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End of Chapter 20
Geosystems 6eAn Introduction to Physical Geography
Robert W. ChristophersonCharles E. Thomsen