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Ecology
Ecology is the scientific study of interactions which determine the distribution and abundance of organisms. Ecology is part of a broader realm of science (physical and biological), having vital roots in plant geography and natural history and makes predictions on how various things effect us. Basic questions addressed
by ecologists:
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Watch Promo Clip of "Planet Earth"
Image from Purves et al., Life: The Science of Biology, 4th Edition, by Sinauer Associates (www.sinauer.com) and WH Freeman (www.whfreeman.com), used with permission.
Classification,
or
taxonomy,
is a system of categorizing living things. There are seven divisions in the
system:
Kingdom is the broadest division. There is no agreement about the number of kingdoms, but most scientists support a four-kingdom (Animalia, Plantae, Protista, and Monera) or five-kingdom (Animalia, Plantae, Protista, Monera, and Fungi) system. For our purposes, we will use the five-kingdom system. See Biology page for more Taxonomy Information. Practice with genus and species... Cassowary Casuarius casuarius Photos by Mrs. King at the Brevard ZOO ~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~~
Energy Flow Through The Ecosystem Sunshine
State Standards SC.G.1.4 SC.G.2.4
Ecosystems are comprised of a combination of biotic (living) and abiotic (non-living) components where energy flows in the form of carbon-carbon bonds and materials are recycled. Energy, however, does not recycle. When respiration occurs, the c-c bonds are broken and the carbon is combined with oxygen to form CO2 . This process releases the energy which is either used by the organism ( to move muscles, digest food, excrete wastes, think, etc.) or the energy may be lost as heat.
Ecosystems include both living and nonliving components. These living, or biotic, components include habitats and niches occupied by organisms. Nonliving, or abiotic, components include soil, water, light, inorganic nutrients, and weather. An organism's place of residence, where it can be found, is its habitat. A niche is is often viewed as the role of that organism in the community, factors limiting its life, and how it acquires food. Producers, a major niche in all ecosystems, are autotrophic, usually photosynthetic, organisms. In terrestrial ecosystems, producers are usually green plants. Freshwater and marine ecosystems frequently have algae as the dominant producers. Consumers are heterotrophic organisms that eat food produced by another organism. Herbivores are a type of consumer that feeds directly on green plants (or another type of autotroph). Since herbivores take their food directly from the producer level, we refer to them as primary consumers. Carnivores feed on other animals (or another type of consumer) and are secondary or tertiary consumers. Omnivores, the feeding method used by humans, feed on both plants and animals. Decomposers are organisms, mostly bacteria and fungi that recycle nutrients from decaying organic material. Decomposers break down detritus, nonliving organic matter, into inorganic matter. Small soil organisms are critical in helping bacteria and fungi shred leaf litter and form rich soil. Even if communities do differ in structure, they have some common uniting processes such as energy flow and matter cycling. Energy flows move through feeding relationships. The term ecological niche refers to how an organism functions in an ecosystem. Food webs, food chains, and food pyramids are three ways of representing energy flow. Producers absorb solar energy and convert it to
chemical bonds from inorganic nutrients taken from environment. Energy content
of organic food passes up food chain; eventually all energy is lost as heat,
therefore requiring continu Energy flow in ecosystems, as with all other energy, must follow the two laws of thermodynamics. The first law states that energy is neither created nor destroyed, but instead changes from one form to another (potential to kinetic). The second law states that when energy is transformed from one form to another, some energy is lost as heat. This means in any given food chain some energy must be lost as we move up the food chain.
The main source of energy for almost all forms of life is the Sun. Scientists discovered an exception, communities of organisms around ocean vents where food chains begin with chemosynthetic bacteria. These organisms oxidize hydrogen sulfide generated by inorganic chemical reactions inside the Earth's crust. Their source of energy is the internal heat of the Earth instead of the heat of the Sun. Food chains indicate who eats whom in an ecosystem. Natural ecosystems have numerous interconnected food chains, much like a complex web. Each level of producer and consumers is a trophic level. Some primary consumers feed on plants and make grazing food chains; other consumers like mushrooms feed on detritus. The population size in an undisturbed ecosystem is
limited by the food supply, competition, predation, and parasitism.
A food chain is a series of organisms each feeding on the one preceding it. There are two types of food chains:
primary producer
Energy flow and the relative porportions of various levels in the food chain. Images from Purves et al., Life: The Science of Biology, 4th Edition, by Sinauer Associates (www.sinauer.com) and WH Freeman (www.whfreeman.com), used with permission. Food chains are simplifications of complex relationships. A food web is a more realistic and accurate representation of energy flow. Food webs are networks of feeding interactions within any given species. The food pyramid provides a detailed view
of energy flow in an ecosystem. The first level consists of the producers
(usually plants). All higher levels are consumers. The shorter the food
chain the more energy is available to organisms.
Most humans occupy a top carnivore role,
about 2% of all calories available from producers ever reach the tissues
of top carnivores. Leakage of energy occurs between each feeding level.
Most natural ecosystems therefore do not have more than five levels to
their food pyramids. Large carnivores are rare because there is so little
energy available to them at the top of the pyramid.
Food generation by producers varies significantly between ecosystems. Net primary productivity (NPP) is the rate at which producer biomass is formed. Tropical forests and swamps are the most productive terrestrial ecosystems. Reefs and estuaries are the most productive aquatic ecosystems. All of these productive areas are in danger from human activity. Humans redirect nearly 40% of the net primary productivity and directly or indirectly use nearly 40% of all the land food pyramid.
Photosynthesis and Respiration
Biogeochemical
Cycles
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The phosphorus cycle is different from the water, carbon, and nitrogen cycles because phosphorus is found in sedimentary rock, not the atmosphere. Phosphorus is a necessary element in DNA, in many molecules found in living cells, and in the bones of vertebrate animals. A smaller, less important source of phosphorus is the droppings (guano) of fish-eating sea birds. Erosion caused by rainfall and the runoff of streams removes phosphorus from phosphate rock. This results in a phosphorus supply in the soil which is available to plants. The phosphorus is absorbed by the plants' roots and used to make organic compounds. As animals eat the plants, the phosphorus is passed along to them. Decomposing plant or animal tissue and animal droppings return organic forms of phosphorus to the water and soil. The ecosystem phase of the phosphorus cycle moves quicker. All organisms require phosphorus for synthesizing phospholopids, NADPH, ATP, nucleic acids, and other compounds. Plants absorb phosphorus very quickly. Herbivores obtain phosphorus by eating plants, carnivores obtain phosphorus by eating herbivores. Eventually, these organisms will excrete phosphorus as waste and this decomposition will release phosphorus into the soil. Plants absorb the phosphorus from the soil and they recycle it within the ecosystem. Much of the phosphorus
is eventually lost in the oceans. The phosphorus in the soil is dissolved
in water, which in turn flows into bodies of water. Some of this phosphorus
is used by plankton, which in turn is eaten by fish. These fish are then
consumed by sea birds. But the majority of phosphorus washed into the sea
sinks to the ocean floor and is not recycled.
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The Carbon Cycle is a complex series of processes through which all of the carbon atoms in existence rotate. The same carbon atoms in your body today have been used in countless other molecules since time began. The wood burned just a few decades ago could have produced carbon dioxide, which through photosynthesis became part of a plant. When you eat that plant, the same carbon from the wood which was burnt can become part of you. The carbon cycle is the great natural recycler of carbon atoms. Unfortunately, the extent of its importance is rarely stressed enough. Without the proper functioning of the carbon cycle, every aspect of life could be changed dramatically. We believe that it's vital to understand how the carbon cycle works in order to see the danger of it not working. Therefore, let's look at a sample carbon cycle and explore how carbon atoms move through our natural world. Plants, animals, and soil interact to make up the basic cycles of nature. In the carbon cycle, plants absorb carbon dioxide from the atmosphere and use it, combined with water they get from the soil, to make the substances they need for growth. The process of photosynthesis incorporates the carbon atoms from carbon dioxide into sugars. Animals, such as the rabbit, eat the plants and use the carbon to build their own tissues. Other animals, such as the fox, eat the rabbit and then use the carbon for their own needs. These animals return carbon dioxide into the air when they breathe, and when they die, since the carbon is returned to the soil during decomposition. The carbon atoms in soil may then be used in a new plant or small microorganisms. Ultimately, the same carbon atom can move through many organisms and even end in the same place where it began. Herein lies the fascination of the carbon cycle; the same atoms can be recycled for millennia! |
There's a whole lot of water on Earth! Something like 326,000,000,000,000,000,000 gallons (326 million trillion gallons) of the stuff (roughly 1,260,000,000,000,000,000,000 liters) can be found on our planet. This water is in a constant cycle where it evaporates from the ocean, travels through the air, rains down on the land and then flows back to the ocean.
The reason there is so much water is because the oceans are huge. About 70% of the planet is covered in ocean, and the average depth of the ocean is several thousand feet (about 1,000 meters). 98% of the water on the planet is in the oceans of the world, and therefore is unusable for drinking because of the salt. About 2% of the planet's water is fresh, but 1.6% of the planet's water is locked up in the polar ice caps and glaciers. Another 0.36% is found underground in aquifers and wells. Only about 0.036% of the planet's total water supply is found in lakes and rivers! That's still thousands of trillions of gallons, but it's a very small amount compared to all the water available. The rest of the water on the planet is either
floating in the air as clouds and water vapor, or is locked up in plants
and animals (your body is 65% water, so if you weigh 100 pounds, 65 pounds
of you is water!).
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| Geologic Time | Rock Cycle (Beyond Books) |
| Rock Cycle |




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