Chapter 47 . Ecosystems. Bye-Bye Blue Bayou. READ PGs 842-843. Energy and raw materials in a physical environment organize the interactions among species in a community. Ecosystem: the organisms with their environment that interact by a flow of energy and resource cycle.
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Ecosystem: the organisms with their environment that interact by a flow of energy and resource cycle.The Nature of ecosystems
Hydrogen, oxygen, carbon, phosphorous and nitrogen are all required for biosynthesis.
Decomposition of wastes and remains releases these nutrients back into the environment.
Sometimes the nutrients are lost to the ecosystem when they flow out in water.Nutrient Cycles
Works as a nerve cell poison that takes 2-15 years to break down.
DDT accumulates in tissues of animals that come into contact with it.
The higher an animal’s trophic level is, the more DDT ends up in its tissues.
Read more about DDT on page 849.DDT- A case of Biological Magnification
Net Ecosystem Production- Primary production minus energy used by producers and decomposers.
The harsher conditions are, the lower primary productivity.Energy Flow Through Ecosystems
Oxygen, hydrogen, carbon, nitrogen, phosphorous.
Water provides hydrogen and oxygen and other elements that dissolve in it.Biogeochemical Cycles
Atmospheric- a gaseous form of a nutrient moves through an ecosystem (carbon and nitrogen)
Sedimentary- elements with no gaseous form (solids) move through an ecosystem (phosphorous). Earth’s crust is reservoir for these nutrients.Types of biogeochemical cycles
Groundwater is easily contaminated by chemicals from landfills, hazardous waste dumps, gasoline, oil, sewage, toxins from power plants.
Water is also contaminated with pesticides, phosphates and other chemicals.
Desalinization uses huge amounts of fossil fuels.
We use more groundwater than the environment is replacing.A global water crisis
Carbon required for life’s quantity. All organic molecules are made of carbon.
Sometimes referred to as the carbon-oxygen cycle since CO2 is the main source of carbon for autotrophs.
Humans put 6 gigatons more carbon into the atmosphere than can be cycled back to the earth.
This carbon may be contributing to global warming.Carbon cycle
Greenhouse gases (carbon dioxide, water, nitrous oxide, methane, chlorofluorocarbons) allow visible light from the sun to pass through them on the way to earth.
The earth’s crust absorbs the light and emits longer wavelengths in the form of heat.
The gaseous molecules do NOT allow the heat to pass through them, but absorbe the longer wavelengths and radiate them back to earth.
Nitrogen travels as N2 (two nitrogen atoms bonded with a triple covalent bond).
Most of our atmosphere is nitrogen!
Although volcanoes and lightening can split some nitrogen, most enters the food web through nitrogen fixation.
Bacteria are nitrogen fixers, converting N2 to ammonia (and later ammonium and nitrate), which plants easily take up.Nitrogen cycle