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Free Online Course on World Geography, Weather, Climate & Regions

Lesson 7: The Earth's Bounty

DISCUSS THE VALUE OF RAINFORESTS.

Biosphere

As you learned in lesson 3, the biosphere includes all life forms on the earth. Everything that we eat comes from the biosphere. The cotton our jeans are made of is part of the biosphere. The lumber used to frame our homes is part of the biosphere. In this segment of the lesson, you will learn about one part of the biosphere that is in danger—the rainforests. Many life forms are part of the rainforests. This means that if the rainforests disappear, it will not just change the lay of the land; it means that thousands of animal and plant species could disappear forever.

Rainforests

Hoh Valley Rainforest, part of the Olympic National Park. (Olympic National Park, Copyright 2008 Jupiterimages Corporation)

There are two types of rainforests: tropical and temperate. The two types share certain characteristics. For example, their vegetation is dense, tall, and very green, and they are rich with plant and animal species.

Tropical rainforests are located near the equator. More than half of all tropical rainforests are found in South America. One-third of the tropical rainforests are located in Brazil. Significant portions of tropical rainforests are also located in Southeast Asia, the Pacific Islands, and West Africa. Tropical rainforests only cover about 7 percent of the earth's surface, but nearly half of the world's species of plants and animals live in them.

The temperate rainforests are located in coastal regions. The largest temperate rainforests are located in North America along the north Pacific coast starting in Oregon and running over 1,200 miles all the way to Alaska. Although this strip of forest may seem vast, it is really only about 3 percent of North America's original temperate rainforest. Some smaller temperate rainforests are located along the southeast coast of Chile in South America, and small coastal regions in the United Kingdom, Norway, Japan, New Zealand, and southern Australia.

Rainforests are quickly disappearing. Some scientists estimate that we are losing an area of rainforest the size of Pennsylvania every single year. If this rate of deforestation continues, we may lose all the rainforests within the next one hundred years.

Deforestation occurs for many reasons. In the United States, widespread deforestation occurred along the Pacific coast more than a century ago when people created settlements and cleared land for farming. Currently, in many tropical regions, people are moving away from overcrowded cities into forest areas. Once there, they clear forest land to use as small farms. Commercial agricultural projects also clear large plots of rainforest land. Logging and using rainforest as pastureland also contributes to the shrinking of the rainforest. Mining operations have led to massive erosion, which has also wiped out large areas of rainforest.

In the United States, the National Park Service monitors and cares for the rainforests. The following information was created by the park services to help us better understand this important resource.

"The temperate rainforests in the valleys of the [Pacific Northwest] contain some of the most spectacular examples of undisturbed Sitka spruce/western hemlock forests in the lower forty-eight states. This ecosystem stretches along the Pacific coast from Oregon to Alaska. Other temperate rainforests are found in several isolated areas throughout the world. What defines a rainforest quite simply is rain, and lots of it. Precipitation in the rainforest along the Pacific coast ranges from 140 to 167 inches—12 to 14 feet—every year. The mountains to the east also protect the coastal areas from severe weather extremes. Seldom does the temperature drop below freezing in the rainforest, and summertime highs rarely exceed 80°F."1

"All life, including you, is dependent on other life. In the Olympic National Park's rainforests, interdependency is essential for life to continue. When wind blows giant Sitka spruce trees over and they fall to the forest floor, they become spongy nurse logs. Seedlings find root in these dead trees and feed on the stored water and nutrients found within them. As a seedling matures, it establishes crucial connections with fungi beneath the forest floor. Of course, fungi have needs too. In addition to all the sugars they extract from the roots of their tree partners, they need fundamental chemical building blocks, which they receive from microorganisms and bacteria living in the forest floor. Lastly, and possibly most importantly, are the dependencies of the "little ones." Bacteria and blue-green algae seek the chemistry of clean wind, water, and soil for the oxygen, nitrogen, carbon dioxide, and primary chemistry they use to feed the forest. And the feedback loops go on and on and on..."2



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