Monday, July 21, 2008

Human Populations Demographics Online Lab


World Vs. High Fertility Rate Country (Ethiopia)

World Vs. Low Fertility Rate Country (Barbados)

Answer the following questions:

1. What was your high fertility rate country and what was its fertility rate? My high fertility rate country was Ethiopia. Its fertility rate was 6.90 children.

2. What was your low fertility rate country and what was its fertility rate? My low fertility rate country was Barbados. Its fertility rate was 1.80 children.

3. The initial demographic "shape" of your high fertility rate country should have been a pyramid, with high population in young age groups. Explain why high fertility rate results in a high percentage of young people in the population. How does this affect future population growth? If a country has a high fertility rate, it means that women in their reproductive years (approximately 20-40) are producing a large number of offspring. The more women reproducing, the more young people there would be in the population. As the young population grows with more births, it is understandable that the population of young people could surpass the population of old. Future population growth would be affected because the more young people you have in a population, the more potential for growth. There would be more children who will reach reproductive years and reproduce, so the population will continue to increase.

4. Your low fertility rate country might have had a more oval-shaped curve with high population in middle age groups. This is especially exaggerated if the fertility rate is below 2.00. Explain why low fertility rate leads to lots of middle-aged people. Low fertility rate means that there are less people of reproductive age who are producing. In other words, if you have a group of 50 women who are of reproductive age, but only 10 of them reproduce, you would obviously have more middle-aged people than young, because not many are reproducing. The older generation will die of natural causes / old age, so the "largest" population would be the middle-aged people.

5. Write ten adjectives or descriptive phrases for what you might expect life, people's attitudes, conditions on the streets, etc. will be like in each of those situations. Imagine a situation with lots of middle-aged and older people in the population and write ten quick "brain-storm" descriptors for you think it would be like (Prescott, Arizona?). Then do the same for a situation with lots of children in the population.
Middle Ages / Older Population:
1. Wise / Educated
2. Responsible
3. Quiet
4. Organized
5. Comfortable
6. Clean
7. Sad (Children bring joy!)
8. Efficient
9. Conservative
10. Lacking in energy
Children / Young Population:
1. Energetic
2. Boisterous
3. Happy- Family Units
4. Carefree
5. Joyous
6. Disorganized
7. Loud
8. Supportive
9. More diverse
10. More culturally accepting

Compendium Review Chapter 24- Pictures


Species Extinction by State

Biodiversity Loss

Wind Farm

Global Warming

Desertification Risk

(World Map- Population Density)

Compendium Review Chapter 24

I. Human Population Growth
II. Human Use of Resources and Pollution
III. Biodiversity
IV. Working Toward a Sustainable Society

I. Human Population Growth
A. Current world population: Approx. 7 billion people.
- Exponential Growth: Increase of growth by a great deal.
- Growth Rate: Determined by considering the difference between the number of persons born per year and the number who die per year. Rates are recorded per 1000 people.
- Biotic Potential: Maximum growth rate under ideal conditions.
- Growth declines due to factors such as food and space.
- Carrying Capacity: Maximum population that the environment can support for an indefinite period.
B. MDCs Versus the LDCs
1b. MDCs: More Developed Countries: (countries like N American and Europe.) MDCs are those in which populatin growth is modest and the people enjoy a good standard of living.
- 1850-1950: Big population increases due to development of modern medicine and improvements in public health and socioeconomic conditions. Since then, the decline in death rate was folllowed by a decline in birthrate, so there has only been modest growth since 1950.
- Population by 2050 is expected to be about 1.2 billion.
2b. LDCs: Less-developed countries: (Africa, Asia)
- Death rate declined steeply w/ modern medicine, but birthrate remained high.
- Women in sub-Saharan Africa average 5 children each.
- Population by 2050 is expected to be about 8 billion.
- Asia is the "worst", in that they are expected to experience acute water scarcity, loss of biodiversity, and more urban pollution. 12 of 15 most polluted cities are located in Asia.
(Insert World Map / Population Density picture / mapsofworld.com / http://mapsofworld.com/world-population-density.htm)
C. Comparing Age Structure: Populations have 3 age groups: pre-reproductve, reproductive, and postreproductive.
- Replacement Reproduction: The idea of couples limiting themselves to 2 children equalling zero population grwoth.
- Untrue, beccause since more young women are entering the reproductive years than older women leaving them, the population continues to increase. (Mader 512-513)
II. Human Use of Resources and Pollution
A. Resources used the most by humans: land, water, food, energy, and minerals.
1a. Nonrenewable Resources: Limited in supply. Land, fossil fuels, and minerals is finite and can be exhausted.
- Renewable Resources: Capable of being naturally replenished. Water, certain forms of energy, plants, animals, etc. can be replenished.
B. Pollution: Side effect of resource consumption. Any alteration of the environment in an undesirable way.
- Often caused by human activity. Effect is proportional to the size of the population.
1b. Land: Worldwide, there are approx. 83 persons per square mile of all available land.
- Land is alse required for agriculature, power plants, highways, other buildings (hospitals), etc., in addition to homes.
2b. Beaches and Human Habitation: Approx 40% of world population lives within 60 miles of a coastline, and is expected to increase.
- Causes beach erosion, loss of habitat for marine organisms, and loss of buffer zone for storms.
- Particularly susceptible to pollution.
3b. Semiarid Lands and Human Habitation: 40% of Earth's lands are deserts.
- Desertification: The conversion of semiarid land to desertlike conditions.
- Begins w/ overgrazing of land. Soil can't hold rainwater, so it runs off instead of nourishing life. Any vegetation is removed by humans, and results in a lifeless desert.
(Insert Desertification Risk picture / www.sou.edu http://www.sou.edu/Geography/JONES/GEOG111.112/atlas/atlas.htm)
4b. Tropical Rain Forest and Human Habitation:
- Deforestation: Removal of trees.
- People are settling tropical rain forests, like the Amazon. This land then becomes subject to desertification.
- Land quickly loses its fertility because most of the nutrients are in trees or other vegetation.
- Loss of biodiversity.
C. Water: Worldwide, 70% of all freshwater is used to irrigate crops.
- In MDCs, more water is usde for bathing, flushing toilets, and watering lawns than for drinking and cooking.
- humans increase the supply of freshwater by damming rivers and withdrawing water from aquifers.
1c. Dams: Worlwide, 45,000 dams catch 14% of all precipitation runoff, provide water for up to 40% of irrigated land, and provide approx. 65 countries w/ more than 1/2 of their electricity.
- Lots of water loss due to evaporatin and seepage into underlying rock beds.
- Salt left behind by evap. and runoff increases alinity and can make a river's water unusable.
- Hold back less h2n w/ sediment buildup.
2c. Aquifers: Reservoirs found just below or as much as 1km below surface.
- Causes ground-water depletion.
- Consequences: Causing land subsidence, a settling of soil as it dries out. Causes surface of ground to drop. Subsidence causes damage to canals, buildings, and underground pipes.
- Can cause sinkholes: Underground collapsing of cavern when water no longer holds up roof.
- Saltwater Intrusion: As water is withdrawn, water table can lower to the point that seawater backs up into streams and aquifers, which reduces supply of freshwater.
3c. Conservation of Water:
- By 2025, approx. 2/3 of world's population may be living in countries facing seriuos water shortages.
- Possible solutions: Planting drought and salt-tolerant crops, using drip irrigation, re-use of water, and adopting conservation measures. (Mader 514-515)
D. Food: Comes from growing crops, raising animals, and fishing the seas.
1d. Harmful practices of farming methods:
- Monoculture: planting of only a few genetic varieties means a single type of parasite can cause total devestation.
- Heavy use of ferilizers, pesticides, and herbicides. (Causing water pollution, decreased soil fertility, development of cancer.)
- Agricultural runoff: Causes chemicals to enter our water supply.
- Generous irrigation: Too much water is extracted from aquifers.
- Excessive fuel consumption.
2d. Soil Loss and Degredation: Land that is good for farming and grazing animals is being degraded worlwide.
- Soil erosion causes loss of topsoil, causing desertification. Farmland is unproductive.
- U.S. and Canada have the highest rates of soil erosion in the world.
- Salinization: Accumulation of mineral salts due to evaporation of excess irrigation water. Makes land unsuitable for growing crops.
3d. Green Revolutions: Dramatic increase in yield of crops in LDSs due to introduction of new varieites of crops. Still require high levels of fertilizer, water, and pesticides, so they cause the same problem as modern farming methods.
4d. Genetic Engineering: Can produce transgenic plants resistant to insects and herbicides. Soil erosion is minimized.
5d. Domestic Livestock: 2/3 of cropland is devoted to producing livestock feed. Therefore, raising livestock accouts for much of the pollution associated with farming.
- Problems: waste, water use for washing livestock, etc. (Mader 516-519)
E. Energy:
1e. Nonrenewable Sources: Nuclear power (approx. 6% of world's energy supply) and fossil fuels (approx. 75%).
- Nuclear power: Not used very much because of nuclear power dangers and radioactive wastes.
- Fossil Fuels: Oil, natural gas, and coal. Derived from compressed remains of ploants and animal that died many thousands of years ago. U.S. is only 5% of world's population, yet it uses more than half of the fossil fuel energy supply! Pollutants are released into the air as it burns.
2e. Fossil Fuels and Global Climate Change:
- Burning of fossil fuels and burning of forests has caused increase in carbon dioxide in the atmosphere.
- Human activities cause emission of other gases, too, such as methane. These are greenhouse gases, because they allow solar radiation to pass through but hinder the escape of infrared heat back into space.
- Global Warming: Earth may warm to temps never before experienced by living things. If this happens, glaciers will melt, sea levels will rise, and coastal cities could be threatened. Would endanger coral reefs, present assmeblage of species in ecosystems will be disrupted as species migrate north for cooler weather. Loss of species unable to migrate.
(Insert Global Warming picture / global.mitsubishielectric.com / http://global.mitsubishielectric.com/bu/solar/environment/main.html)
3e. Renewable Energy Sources: Hydropower, geothermal, wind, and solar.
- Hydropower: Converts energy of falling water into electricity. Approx. 10% of electric power generated in US, and almost 98% of total renewable energy used.
- Geothermal Energy: Uranium, thorium, radium, and plutonium undergo radioactive decay below Earth's surface and heat the surrounding rocks. When they are in contact w/ water, it heats water. Can be piped up to surface for use.
- Wind Power: Space needed for wind farms that produce electricity is comparable to amount of land required by a coal-fired power plant or solar energy system. Expected to increase use in future.
(Insert Wind Farm picture / www.ronsaari.com / http://www.ronsaari.com/stockImages/windmills/WindFarmPalmSpringsCA.php)
- Energy and the Solar-Hydrogen Revolution: Solar energy must be collected, converted, and stored. Can be used for passive-solar heating of houses, and heat can be sotred in water tanks, rocks, bricks, etc.
- Photovoltaic (solar) cell: A wafer of electron-emitting metal is in contact with another metal that collects the eletrons and passes them along into wires in a steady stream. These cells can be placed on roofs to generate electricity. Can be used to create hydrogen fuel, to be used in future cars. (Mader 520-522)
F. Minerals: Nonrenewable raw materials in Earth's crust that can be extracted. Includes fossil fuels, nonmetallic raw materials, such as sand, gravel, and phophate; and metals, such as aluminum copper, iron, lead, and gold.
- Heavy metals are dangerous to humans: lead, mercury, arsenic, cadmium, tin, chromium, zinc, and copper. Used in electronics, medicines, paints, etc. Inhibit vital enzymes in body.
- Strip / surface mining: One of greatest threats to maintenance of ecosystem and biodiversity. Rain washes toxic waste deposits into streams and rivers.
1f. Hazardous Wastes: Nine most common: heavy metals, synthetic organic compounds, benzene, polychlorinated biphenyls, and chloroform.
- Chlorofluorocarbons: Type of halogenated hydrocarbon in which both chlorine and flourine atoms replace some of the hydrogen atoms. Thin ozone shield, which is essentail for protection of utraviolet radiation.
- Biological Magnification: Wastes that enter and accumulate in the fat or organisms, ans since they are not excreted, they become more and more concentrated as they pass along a food chain. (Mader 522-523)
III. Biodiversity
A. Biodiversity is the variety of life on Earth, described in terms of the number of different species.
- We are in biodiversity crisis: Number of extinctions expected to occur in the near future is unparallel in the history of the Earth.
B. Loss of Biodiversity is due to all of the following:
- Habitat Loss: Human occupation and expansion.
- Alien Species (Exotics): Nonnative members of an ecosystem. Humans introduce them to ecosystems due to colonization, horticulture, and agriculture, and accidental transport. Some are invasive, and crowd out native species.
- Pollution: Acid deposition (weakens trees), global warming (loss of habitat, etc.), ozone depletion (CFCs), and synthetic organic chemicals.
- Overexploitation: Too many individuals are taken from a wild population so it is reduced in number. ie. exotic pets. (Poaching, overfishing, etc.)
- Disease: Exposure to domestic animals and their pathogens occur when humans encroach on wildlife habitats.
(Insert Biodiversity Loss picture / www.greenfacts.org http://www.greenfacts.org/en/desertification/l-3/7-climate-change-biodiversity-loss.htm)
C. Direct Value of Biodiversity: Direct value of wildlife is related to their medicianl value, agricultural value,and consumptive use value.
1c. Medicinal Value: Potent medicines are dervied from plants, fungus, some animals (ie horseshoe crab) and certain types of bacteria.
2c. Agricultural Value: Crops are dervied from wild plants that have been modified to be high producers. Biological pest control, bees pollinating plants, etc/
3c. Consumptive Use Value: Catching of fishes, crustatceans, and mammals. Products sold in marketplaces. Trees for wood, etc.
D. Indirect Value of Biodiversity: Services that are pervasive and not easily discernable.
- Waste Disposal: Decomposers break down dead organic matter and other types of wastes to inorganic nutrients that are used by the producers within ecosystems. If not for this service, Earth would be covered in waste. Some biological communities can break down and immobilize pollutants.
- Provision of freshwater: Water cycle supplies freshwater to terrestrial ecosystems. Provide us w/ fish and other food. "Sponge Effect": Forests soak up water and release it at a regular rate.
- Prevention of Soil Erosion: Intact ecosystems naturally retain soil and prevent soil erosion.
- Biogeochemical Cycles: Biodiversity within ecosystems contributes to the workings of the water, phophorus, nitrogen, carbon, and other biogeochemical cycles, which we depend on for freshwater.
- Regulation of Climate: Trees provide shade and reduce the need for fans and air conditioners. Forests ameliorate the climate because they take up carbon dioxide. Carbon dioxide has a significant impact on global warming, which is increased with deforestation.
- Ecotourism: Relaxing in the wild! :) (Mader 524-530)
IV. Working Toward a Sustainable Society
A. Sustainable Society: One that could always provide the same amount of goods and services for future generations as it does at present. Biodiversity would also be preserved.
1a. Today's Unsustainable Society: Population growth and excessive resource consumption stresses the environment, including worldwide pollution and the extnction of wildlife.
(Insert Species Extinction by State picture / www.unl.edu / http://www.unl.edu/nac/conservation/atlas/Map_Html/Biodiversity/National/Species_Extinctions/Species_extinctions.htm)
2a. Characteristics of a Sustainable Society:
- Makes use of only renewable solar energy.
- Materials cycle through the various populations back to the producer.
- Protection of natural ecosystmes.
- Efficiency (cars, etc.)
3a. Rural Sustainability:
- Emphasis on preservation: ecosystems, agricultural land, groves of fruit trees, etc. Possible steps: plant cover crops, multiuse farming, replenish soil nutrients, low flow or trickle irrigation, increase planting of cultivars, use precision farming, use integrated pest management, etc.
4a. Urban Sustainability:
- Sharing of resources. Possible steps: Energy-efficient transportation system, solar or geothermal energy, utilize green roofs, improve storm-water management, plant native species grasses, create greenbelts, etc.
B. Assessing Economic Well-Being and Quality of Life:
- Gross National Product: Measurement of the flow of money from consumers to businesses, in the form of goods and services purchased. (Total costs of manufacturing, production and srvices in the form of salaries, wages, mortgage and rent, interets and loans, taxes, and profit. Use value, option value, existence value, aesthetic value, cultural value, and scientific and educational value are all factors. (Mader 530-533)

Ok... So I'm not going to lie... I had a REALLY hard time fitting the last part of your powerpoint into chapter 24. I felt like I was reading the wrong chapter, or something. So, I'm including it here in the end:

In a community, relationships among species can be beneficial, damaging or neutral:
Symbiotic: mutually beneficial, both species benefit
Parasitic: one species benefits (“parasite”) and the other is harmed (“host”)
Commensal: One species benefits, the other is unharmed
Mutualism: both species benefit, like symbiosis, but it may appear one species has the advantage, but evolutionarily, over the long-term, both benefit
Predation: Usually considered parasitic, where the predator is the parasite, but can also be seen as mutualistic.
(Frolich PowerPoint Slide 26)

A. Relationships Among Species
- We do still have ecological relationships with “wild” species. Examples:
- Hunt mushrooms
- Create game reserves
- Create national parks
- Household and urban/rural “pests” (e.g. molds, sewer rats)
- Symbiotic micro-organisms (skin and mouth bacteria)
- Disease-causing micro-organisms
(Frolich PowerPoint Slide 26)

B. Our Relationships w/ Domesticated Species
- But mostly we have tight relationships with domesticated species. Basis for ecological relationship:
- Food and agriculture (by far most common—food crops and animals)
- Transportation (“beasts of burden”)
- Care and protection (pets)
- Laboratory study and production
(Frolich PowerPoint Slide 29)

Friday, July 18, 2008

Compendium Review Chapter 23- Pictures


Phosphorous Cycle

Nitrogen Cycle

Greenhouse Effect

The Water Cycle

Grazing and Detrital Food Webs

Terrestrial Biomes

Compendium Review Chapter 23

I. The Nature of Ecosystems
II. Energy Flow
III. Global Biogeochemcial Cycles

I. The Nature of Ecosystems
A. Biosphere: Where organisms are found on planet Earth, from the atmosphere above to the depths of the oceans below, and everything in between.
B. Entire Biosphere is one giant Ecosystem: A place where organisms interact among themselves and with the physical and chemical environment.
- These interactions help maintain both the ecosystem and the biosphere.
- Human interactions can alter interactions between organisms and their environments in ways that reduce the abundance and diversity of life within the ecosystem.
C. Ecosystems: Many different types of terrestial ecosystems, also called biomes.
- Biomes: Temperature and rainfall define the biomes, whose organisms are adapted to the regional climate.
- Examples: Tropical rain forest, savanna, temperate grasslands, temperate forests, deserts, taiga, and tundra.
(Insert Terrestrial Biomes picture / ecology.botany.ufl.edu / http://ecology.botany.ufl.edu/ecologyf02/biodiv.html )
- Aquatic ecosystems: Divided by whether they are freshwater or salt water.
D. Biotic Components of an Ecosystem:
1d. Abiotic components: nonliving.
2d. Biotic components: living things categorized according to the food source.
- Autotrophs: Require only inorganic nutrients and an outside energy source to produce organic nutrients for their own use and for the other members of a community. They are called producers. (ie algae, photosynthetic organisms.)
- Heterotrophs: Need a source of organic nutrients. They are consumers.
* Herbivores: Animals that eat plants or algae. (ie insects, protists.)
* Carnivores: Feed on other animals. (ie birds that feed on insects, hawks feed on birds, etc.)
* Omnivores: Feed on both. (ie humans.)
* Detritus Feeders: Organisms that feed on detritus, which is decomposing particles of organic matter. (ie Earthworms, beetles, etc.)
E. Niche: Role of an organism in an ecosystem: how it eats its food and what eats it, and how it interacts with other populations in the same community.
F. Chemical Flow and Chemical Cycling
1f. Every ecosystem is characterized by two phenomena: energy flow and chemical cycling.
- Energy flow: Begins when producers absorb solar energy.
- Chemical Cycling: Begins when producers take in inorganic nutrients from the physical environment.
- Next, through photosynthesis, producers make organic nutrients directly for themselves and indirectly for the other populations of the ecosystem.
* Energy Flow: As nutrients pass from one population to another, all energy content is converted to heat, which dissipates in the environment.
- Most ecosystems require a constant supply of solar energy.
* Chemicals cycle when inorganic nutrients are returned to the producers from the atmosphere or soil. (Mader 493-495)
II. Energy Flow
A. Various interconnecting paths of energy flow are represented by a food web, which is a diagram that describes trophic (feeding) relationships.
- Two examples: Grazing Web- Begins with an oak tree and grass. Detrital Web- Begins with detritus and the decomposers found within detritus.
(Insert Grazing and Detritus Food Webs picture / project.bio.iastate.edu / http://project.bio.iastate.edu/Courses/biol123/lectures/Lecture06-Ecosystems/slide10.htm)
B. Trophic Levels:
1b. Food Chains: Diagrams that show a single path of energy flow. Ex. In grazing food chain, you would have leaves, followed by caterpillars, followed by birds, followed by hawks. In detrital food chain, you would have detritus, followed by earthworms, followed by shrews.
2b. Trophic level: Composed of all the organisms that feed at a particular link in a food chain. Example: In grazing food web, trees are producers (first trophic level), first series of animals are primary consumers (second trophic level), and the next group of animals are secondary consumers (third trophic level).
C. Ecological Pyramids: The flow of energy with large losses between successive trophic levels.
- Only about 10% of the energy of one trophic level is available to the next tropic level.
1c. Biomass: The number of organisms multiplied by the weight of organic matter within one organism. (Mader 497-498)
III. Global Biogeochemical Cycles
A. All organisms require a variety of organic and / or inorganic nutrients.
1a. Biogeochemical Cycles: Pathways by which chemicals circulate through ecosystems involve both living (biotic) and nonliving (geological) components.
- Gaseous: Element returns to and is withdrawn from the atmosphere as a gas. (ie carbon and nitrogen cycles.)
- Sedimentary: The chemical is absorbed from the soil by plant roots, passed to heterotrophs, and returned to soil by decomposers. (ie phosphorus cycle.)
2a. Chemical Cycling involves a reservoir, an exchange pool, and a biotic community.
- Human activities remove chemicals from reservoirs and exchange pools, and make them available to the biotic community. Can result in pollution, because it upsets the normal balance of nutrients for producers in the environment.
B. The Water Cycle:
1b. Evaporation, precipitation, runoff, etc. See picture. All water is eventually returned to the sea. Aquifer: Rock layers that contain water and release it.
(Insert Water Cycle picture / Frolich PowerPoint Slide 18)
2b. Human Activities:
-Humans interfere w/ water cycle in three ways: First, they take water from aquifers. Second, They clear vegetation from land and build roads and buildings that prevent percolation and increase runoff. Third, they interfere with the natural processes that purify water and instead add pollutants like sewage and chemicals to water.
C. The Carbon Cycle:
1c. Carbon dioxide in atmosphere is the exchange pool for the carbon cycle.
- In this cycle, organisms in both terrestrial and aquatic ecosystems exchange carbon dioxide with the atmosphere. ie. Plants take co2 from air, and through photosynthesis, incorporate carbon into nutrients that are used by autotrophs and heterotrophs. When organisms respire, carbon is returned to the atmosphere as co2. In aquatic, it is indirect: co2 from air combines with h2o to produce bicarbonate ion, a source of carbon for algae that makes food for themselves and for heterotrophs. When aquatic organisms respire, the co2 they give off becomes bicarbonate ion.
2c. Living and dead organisms contain organic carbon and serve as one of the reservoirs for the carbon cycle. Decomposition returns co2 to the atmosphere.
3c. Fossil Fuels: When plant and animal remains are transformed into coal, oil, and natural gas.
4c. Human Activities:
- More co2 is being deposited in the atmosphere than is being removed. Largely due to burning of fossil fuels and destruction of forest. When a forest is destroyed, we reduce a reservoir and the very organisms that take up excess co2.
5c. Global Warming: Human activities emit co2 and other gases, like nitrous oxide into the atmosphere. These gases are known as greenhouse gases, because they allow solar radiation to pass through but hinder the escape of infrared rays back into space.
- Contribute to rise in Earth's ambient temperature, = global warming.
- Higher temperature = greater evaporation of h2o, forming more clouds, and setting up a positive feedback effect that will increase global warming even more.
- Other effects: Temps in polar regions rise, glaciers will melt, sea levels will rise, h2o evap. will increase, = increased rainfall along coasts and dryer conditions inland. Droughts reduce agricultural yields, trees will die, etc. Coastal cities could sink! (Mader 498-499)
(Insert Greenhouse Effect picture / Frolich PowerPoint Slide 21)
D. The Nitrogen Cycle: Nitrogen gas accounts for approx. 78% of the atmosphere.
1d. Ammonium Formation and Use:
- Nitrogen fixation occurs when nitrogen gas is converted to ammonium, a form plants can use.
2d. Nitrate Formation and Use:
- Plants can use nitrates as a source of nitrogen.
- Nitrification: Production of nitrates during the nitrogen cycle. Can occur when cosmic radiation, meteor trails, and lightning provide high energy needed for nitrogen to react with oxygen. Or, when ammonium in the soil is converted to nitrate by soil bacteria, or when nitrate-producing bacteria converts nitrite to nitrate.
- Assimilation: Plants take up ammonia and nitrate from the sol and use these ions to produce proteins and nucleic acids.
(Insert Nitrogen Cycle picture / www.stormfront.org / http://www.stormfront.org/forum/showthread.php?t=325972)
3d. Formation of Nitrogen Gas from Nitrate:
- Denitrification: The conversion of nitrate back to nitrogen gas, which enters the atmosphere. Counterbalances nitrogen fixatin except for human activities.
4d. Human Activities: Significantly alter the transfer rates in the nitrogen cycle by producing fertilizers from nitrogen- nearly doubles the fixation rate. Runs off into water, creates overgrowth of algae, causes over-enrichment, and when algae die off, increased decomposer populations use up all oxygen in water, and results in massive fish kill.
1e. Acid Deposition: Nitrogen oxides and sulfur dioxide enter atmosphere from burning of fossil fuels. These gases combine with water vapor to form acids that return to the earth, and their deposit affects forest and lakes.
- Creation of smog, and trapped pollutants.
E. The Phosphorus Cycle: Phosphorous trapped in oceanic sediments moves onto land after a geological upheaval. Weathering of rocks places phosphate ions into soil. Some of this phosphate is used by plants in a variety of molecules, and the nucleotides that become a part of DNA and RNA. Animals eat producers and incorporate some of the phosphate into teeth, bones, and shells, which take many years to decompose.
(Insert Phosphorous Cycle picture / www.biologycorner.com / http://www.biologycorner.com/bio4/notes/chap45.html )
1e. Phosphorus and Water Pollution:
- Cultural Eutrophication: Overenrichment of waterways due to humans use of phosphate for fertilizer, animal wastes from livestock feedlots, and discharge from sewage treatment plants.
- Biological Magnification: Occurs as materials pass along a food chain and become more and more concentrated because they remain in body and are not excreted.
- Pollutants: Waste dumping, offshore mining and shipping, oil spills, etc.
- Many species are at the brink of extinction. (Mader 500-505)

Compendium Review Chapter 22- Pictures


Cro-Magnon Skull

Neanderthal and Modern Human Skull Comparison

Homo erectus

Homo habilis

Evolution of Primates

Human / Chimpanzee Skeletons 2

Human / Chimpanzee Skeletons 1

Evidence for Historical Fact of Evolution

Ambulocetus: Believes to have given rise to whales.

Charles Darwin

Early Earth

Stanley Miller Experiment

Stanley Miller

History of Life on Earth Chart

Compendium Review Chapter 22

I. Origin of Life
II. Biological Evolution
III. Classification of Humans
IV. Evolution of Hominids
V. Evolution of Humans

I. Origin of Life
A. Fundamental Principle of Biology: All living things are made of cells and every cell comes from a preexisting cell.
1a. Chemical Evolution: A slow increase in the complexity of chemicals. (Mader 468)
B. To understand evolution, we must appreciate deep time- time stretching beyond what is easy to intuitively grasp.
1b. Toilet paper analogy—if a roll of toilet paper is Earth history, humans reside in the shreds at the end of the very last sheet. (Frolich PowerPoint Slide 4)
(Insert Key Events of History of Life picture / Frolich PowerPoint Slide 5)
C. The Primitive Earth:
1c. Sun and Planets: Probably formed from aggregates of dust particles and debris,taking approx. 10-billion years.
- 4.6 billion years ago: solar system in place.
2c. First atmosphere was probably formed by gases escaping from volcanoes. Therefore, the primitive atmosphere would have been made up of mostly water vapor, nitrogen, and carbon dioxide, along with small amounts of hydrogen and carbon monoxide. (Free oxygen was scarce, if any.)
- Earth was extremely hot, and as it cooled, it formed dense clouds.
- Water vapor condensed to liquid water, and rain began to fall. = Oceans. (Mader 468)
- How do we know? Existing ancient rocks. (Frolich PowerPoint Slide 6)
D. Small Organic Molecules:
1d. Rain washed gases into oceans.
- The great deal of energy present (ie volcanoes, lightning, ultraviolet radiation, etc.) made the primitive gases react with one another and produce small organic compounds, such as nucleotides and amino acids.
- Experiment conducted by Stanley Miller confirms this theory. (Mader 468-469)
(Insert Stanley Miller picture / fig.cox.miami.edu / http://fig.cox.miami.edu/~cmallery/150/life)
(Insert Stanly Miller Experiment picture / Frolich PowerPoint Slide 7)
E. Macromolecules: Newly formed small organic molecules probably joined to produce organic macromolecules.
1e. RNA- first hypothesis: The only macromolecule needed to progress toward formation of the first cell was RNA (ribonucleic acid). It is possible that, then, RNA could have carried out the processes of life commonly associated today with DNA.
2e. Protein-first hypothesis: Amino acids join together when exposed to dry heat. This theory suggests that amino acids collected in shallow puddles, and the heat of the sun caused to to form proteinoids (small polypeptides) that have some catalytic properties. When returned to water, they form microspheres, sturctues that are made of only protein but have mnay of the properties of a cell.
F. The Protocell: Can carry on metablism but not reproduce.
- Could have come about by a lipd that was made available to microspheres, the two tend to associate, and produce a pipid-protein membrane.
- Protocell could have used the abundant small organic molecules in the ocean as food.
- Protocell was most likely a heterotroph: organism that takes in preformed food.
- Also would have been a fementer, since there was no free oxygen. (Mader 469)
(Insert Early Earth picture / Frolich PowerPoint Slide 6)
G. The True Cell: How did the first cell acquire both DNA and enzymatic proteins?
1g. RNA-first Hypothesis: First cell had RNA genes that, similar to mRNA, could have specified protein synthesis. Some of these proteins would have been enzymes. One of these enzymes may have used RNA as a template to form DNA, and replication would have then proceeded normally.
2g. Protein-first Hypothesis: Some of the proteins in the protocell would have evolved the enzymatic ability to synthesize DNA from nucleotides in the ocean. DNA would have then gone on to specify protein synthesis, and the cell could have acquired all its enzymes, inlcuding those that replicate DNA. (Mader 468-469)
II. Biological Evolution
A. Since the first true cells were the simplest of life cells, they must have been prokaryotic cells, lacking a nucleus.
- Eukaryotic cells, which have nuclei, evolved from these first cells.
- Multi-cellular organisms and other kingdoms evolved, like fungi and plants.
B. Biological Evolution: The process by which a species changes throughout time. Two important aspects:
- Descent from a common ancestor, which explains what all living things have a commno chemistry and cellular structure.
- Adaptation to the environment, which enables an organism to survive and reproduce in its environment. (Explains diversity of life.)
C. Common Descent: Life forms change over time and from place to place.
1c. Charles Darwin: English naturlaist who first formulated the teory of evolution based on his travels at the age of 22.
- Gathered evidence to support the idea of common descent, based in fossil, anatomical, and biogeographical data. (Mader 470)
(Insert Charles Darwin picture /www.paracompusa.com / http://www.paracompusa.com/SmartScience/Popa/Vol4-2.html)
D. Evidence for Historical Fact of Evolution
1d. Fossil record
–Most rocks contain fossils (in sedimentary rock). (Frolich PowerPoint Slide 8) Best evidence because they are the actual remains of species that lived on Earth at least 10000 years ago and up to billions of years ago. Includes trails, footprints, burrows, casts, preserved droppings, bone, impressions, and insects trapped in tree resin.
- Paleontologists: Find and remove fossils from strata.
- Fossil Record: History of life recorded by fossils.
(Mader 470)
–Long-term change in biological communities. (Frolich PowerPoint Slide 8)
- In general, life progressed from the simple to the complex: Unicellular prokaryotes, unicellular eukaryotes, multicellular eukaryotes, fishes, terrestial plants, animals. On land, nonflowering plants, flowering plants, amphibians, reptiles (including dinosaurs), birds, etc. (Mader 471)
(Insert picture of Ambulocetus / http://www.flickr.com/ / http://www.flickr.com/photos/68509222@N00/384835318/)
2d. Transitional Fossils: Those that have characteristics of two different groups: origin of mammals, origin of birds.
- Anatomical similarities.
- Shared embryological features.
- Shared biochemical and genetic features.
(Insert Evidence for Historical Fact of Evolution picture / Frolich PowerPoint Slide 8)
(Frolich PowerPoint Slide 8)
E. Different Types of Evidence Support the Hypothesis that Organisms are Related Through Common Descent.
1e. Biogeographical Evidence: Biogeography: The study of the distribution of plants and animals in different places throughout the world.
- Life forms evolved in a particular locale and then spread out, which provides for a variety of plants and animals where geography separates continents, islands, or seas.
- Ex. Rabbits were not found in S. America, though the geography was suited for them, because they evolved somewhere else and could not reach S. America.
2e. Anatomical Evidence: Common Descent allows for the explanation for anatomical similarities among organisms.
- Ex. Forelimbs are used by birds, whales, horses, lizards, and monkeys, for different purposes.
- These are Homologous Structures: similar in structure anatomically because they are inherited from a common ancestor.
- Analogous Structures: Serve the same function, but are not constructed similarly, nor do they share a common ancestry.
- Ex. Wings of birds and insects, the jointed appendages of a lobster, and humans are analogous structures.
- Vestigal Structures: Anatomical features that are fully developed in one group of organisms, but are reduced and may have no function in similar groups.
- Ex. Ancestors of whales walked on land. "Modern" whales have a vestigial pelvic girdle and legs, but are completely aquatic. These are also explained by Common Descent. Traces of evolutionary history.
3e. Biochemical Evidence: Almost all living organisms use the same basic biochemical molecules, including DNA, ATP, etc.
- Therefore, humans share a large number of genes with much simpler organisms. Life's vast diversity has come about by only a slight difference in the regulation of genes.
F. Intelligent Design:
- Evolutionary theory has been supported by repeated scientific experiments and observations.
- Intelligent Design argues that the diversity of life could never have arisen without the involvement of an "intelligent agent". Faith-based, not science-based.
G. Natural Selection: Mechanism for adaptation.
- Adaptation: A species becomes suited to its environment.
- Critical Elements of Natural Selection are as follows:
* Variation: Individual members of a species vary in physical characteristics. Physical variations can be passed from generation to generation.
* Competition for Limited Resources: The number in each generation usually stays about the same: resources are limited and competition for resources reults in unequal reporduction among members of a population.
* Adaptation: Members of a population with advantageous traits capture more resources and are more likely to reproduce and pass on those traits. Over time, the environment "selects" for the better-adapted traits. Therefore, each subsequent generation includes more individuals that are adapted in the same way to the environment.
- Accounts for great diversity of life. (Mader 474)
III. Classification of Humans
A. Biologists classify organisms according to their evolutionary relatedness.
1a. Binomial Name: Each organism has a name that gives its genus and species.
- Organisms in the same domain have general characteristics in common.
- Those in the same genus have very specific characteristics in common.
B. DNA Data and Human Evolution: DNA data is being relied on more heavily today to trace the history of life.
1b. 1970s: Carl Woese reports that on the basis of rRNA data, there are three domains of life and the archaea are more closely related to eukaryotes than to bacteria. Animals are more closely related to fungi than plants. (Mader 475)
(Insert Three Domain System of Classification picture / kilby.sac.on.ca / http://kilby.sac.on.ca/faculty/dgalajda/oacbiology/domains__cladistics.htm)
C. Humans Are Primates
- Our closest living relatives are monkeys and apes (anthropoids).
- We share a common ancestor, most recently with apes, farther into deep time with monkeys and even farther in with lemurs and tarsurs (prosimians).
- The living species are not our actual ancestors—we need the fossil record to see them.
(Frolich PowerPoint Slide 9)
- Primates have mobile limbs (w/ five digits each, opposable thumb); grasping hands; a flattened face; binocular vision (including cones); a large, complex brain; and a reduced reproductive rate.
- All traits shared with humans.
D. Comparing Human Skeleton to the Chimpanzee Skeleton
1d. The genomes of humans and chimpanzees are 99% identical.
- 1% difference: Humans, not chimps, are adapted for an upright stance. (Mader 476-477)
(Insert Human / Chimpanzee Skeletons pictures / http://www.flickr.com/ / http://www.flickr.com/photos/mindfuldocumentation/71000531/)
(Insert Evolution of Primates picture / Frolich PowerPoint Slide 9)
IV. Evolution of Hominids
A. Evolutionary Tree: A working hypothesis of the past history of a group of organisms. (See Evolution of Primates picture.)
B. The First Hominids: Hominid refers to our branch of the evolutionary tree.
- Lineage: Any two lines of descent.
- Each lineage throughout time accumulates genetic changes, which lead to RNA and protein changes.
- Molecular data suggest that hominids split from the ape line of descent about 7 mya.
C. Hominid Features: Anatomical features are used to determine if a fossil is a hominid.
- Bipedal posture: Walking on two feet.
- Shape of the face: Flatter, more pronounced chin.
- Teeth are generally smaller and less specialized.
- Brain size.
D. Earliest Fossil Hominids
- Odest fossil: Sahelanthropus tchadensis, dated 7 mya, found in Chad, central Africa. Only found a skull.
- Orrorin tugenensis: dated 6 mya, found in eastern Africa. Limb anatomy suggests bipedal posture.
- Ardipithecus kadabba: dated between 5.8-5.2 mya.
E. Evolution of Australopithecines: Beginning of hominid line of descent.
- Group of species that evolved and diversified in Africa.
- Some were slender, some were powerful.
- Fed on soft fruits and leaves, some of the more "robust" fed on a more fibrous diet.
- First was unearthed in Southern Africa. (Australopithecus africanus)
- Walked upright. Proportions of limbs were apelike.
- Relatively large brain.
- A. afarensis: Lucy. Dated at 3.18 mya, she stood upright and walked bipedally.
Ape-like above waist (small brain) and humanlike below the waist (walked erect). Proves human characteristics did not evolve all at one time. = Mosaic evolution.
V. Evolution of Humans
A.Fossils are assigned to the genus Homo if the following criteria are met:
- Brain size is 600 cm3 or greater.
- The jaw and teeth resemble those of humans.
- Tool use is evident.
B. Early Homo: Homo habilis "handy man": Dated between 2.0 and 1.9 mya.
- May be ancestral to early humans due to larger brain size, smaller cheek teeth, possibility of speech, and indication of tool use. May have been the beginnings of society and culture, if they hunted and ate together.
(Insert Homo Habilis picture / primatas.no.sapo.pt / http://primatas.no.sapo.pt/homem.htm)
C. Homo Erectus: Fossils found in Africa, Asia, and Europe. Dated between 1.9 and 0.3 mya.
- First H. erectus to be unearthed was in 1891, by Eugene Dubois.
- Several different species are included in this group, although all are similar in appearance.
- Compared with H. habilis, H. erectus had a larger brain and a flatter face. Nose projected, much taller. Were erect, with striding gait. Skeleton still showed some australopithecine features. Believed to have migrated from Africa into Asia and Europe.
- First hominid to use fire, and fashioned more advanced tools than early Homos.
- Believed to have used "home bases".
- Language and culture.
(Insert Homo Erectus picture / www.forcesitaly.org / http://www.forcesitaly.org/italy/immagini?M=D)
D. Evolution of Modern Humans
1d. Most accept the idea that Homo sapiens (modern humans) evolved from H. erectus. (Mader 482-484)
- Ability to interbreed.
- Little anatomical difference among populations.
- Little biochemical difference among populations.
- DNA and protein analysis show recent single common ancestor within 1 million years, perhaps only 200,000 years ago. (Frolich PowerPoint Slide 11)
2d. Multiregional Continuity Hypothesis: Belief that Homo sapiens evolved in several different locations. (ie. Asia, Africa, and Europe.)
3d. Others argue that it is unlikely that evolution would have produced essentially the same result in these different places. They suggest the following theory:
4d. Out-of-Africa Hypothesis: Proposes that H. sapiens evolved from H. erectus only in Africa, and thereafter migrated to Europe and Asia about 100000 years BP. This hypothesis suggests that we are more genetically similar than the other hypothesis, and this is the more accepted hyposthesis of the two.
E. Neandertals:
- First Neandertal discovered in Neander Valley, Germany, approx. 200000 years BP.
- Massive brow ridges, and their nose, jaws and teeth protruded far forward. Low forehead, lower jaw lacked a chin. Brain was slightly larger than modern humans. Heavily muscled. Lived in Europe and Asia during the lst ice age.
- Culturally advanced. May have built houses when not living in caves. Manufactured a variety of stone tools, including spear points. Hunted bears, woolly mammoths, rhinos, etc. Used and controlled fire. Buried their dead w/ flowers. may have even had a religion. Capable of thinking symbolically. (Mader 485)
(Insert Neanderthal and Modern Human Skulls Comparison picture / Frolich PowerPoint Slide 13)
F. Cro-Magnons: Oldest fossils to be designated Homo sapiens.
- Named after fossil location in France.
- Believed to be the modern humans who entered Asia and Europe from Africa 100000 years BP.
- Thoroughly modern appearance.
- Did not interbreed with Neanderthals, but seemed to coexist.
- Made advanced stone tools, including compound tools.
- May have been first to throw spears, and were accomplished hunters.
- Culture included art.
(Insert Cro-Magnon Skull picture / www.skadi.net / http://www.skadi.net/forum/showthread.php?t=11043)
G. Human Variation
1g. Widely distributed about the globe. Different ethnicities.
- Could be due to environmental adaptations. (ie dark and light skin)
- Bergmann's rule: animals in colder regions have a bulkier body build.
- Allen's rule: Animals in colder regions have shorter limbs, digits, and ears, to help regulate body temperature.