History of Life
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1. HC can be used to date fossils about 30,000 years old or younger (half-life is ca 5700 years).
2. 40K has been used to date many older events in Earth history (half-life is ca. 1.3 billion years; decays to 40Ar).
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1. age of divisions vs. their duration
D. Earliest bacteria that evolved the ability to use H20 as a source of H for their metabolism liberated O2
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1. As O2 levels increased, organisms evolved the ability to use O2, metabolically.
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1. only tiny cells would be able to survive in the low oxygen environment of early Earth (surface area/volume ratio)
2. greater amounts of O2 allowed evolution of larger cells
3. eventually enough O2 was available to support multicellular life
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1. continental drift
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a. sea floor spreading - new crust is added from the mantle at rifts in the sea floor
b. this causes continents to move
c. when plates meet, they slide past each other or one goes under the other (can result in formation of mountains)
d. affects climate, sea level, ocean currents, distribution of organisms, volcanic activity
e. Pangaea - all continents together, harsh climates in interior (properties of water)
f. Laurasia - North America, Europe, Asia
g. Gondwanaland - South America, Africa, Madagascar, India, Australia, Antarctica
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a. Earth's orbit sometimes changed slightly
b. change in ocean currents
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a. major volcanic episodes can affect Earth's climate
b. ash in the atmosphere reduces penetration of sunlight, reducing temperatures
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a. small meteorites regularly hit Earth
b. large meteor collisions are rare but do occur (Kansas, 1948, 5 ton meteor)
c. mass extinction at end of Cretaceaous (about 65 mya) have been caused by a meteor collision
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- estimated size - 10 km diameter
- a large crater (180 km diameter) was found of coast of Yucatan
- thin layer of iridium
- this hypothesis is still debated but has fairly strong support
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1. Earth forms - 4.6 bya
2. origin of life - 3.8 bya (prokaryotes)
3. oldest known fossils - 3.5 bya (stromatolites - left by bacteria)
4. O2 begins accumulating - 2.5 bya
5. oldest eukaryote fossils - 1.5 bya
6. first animals - 700 mya
7. origin of most invertebrate phyla; diverse algae - Cambrian (544-500 mya)
8. first vertebrates (jawless fishes); abundant marine algae - Ordovician - probably due to extensive glaciation
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1. Cambrian explosion (ca. 500 mya)
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a. gave rise to most animal phyla
b. Burgess Shale in British Columbia
c. Wonderful Life by S.J. Gould
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a. first animals colonize land
b. many new families, genera, etc. but no new phyla (i.e., no significantly different body plans)
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a. notable exception - insects
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a. arms race
b. shells and shell breakers
c. toxins and tolerance
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1. Smithsonian - Washington D.C.
2. American Museum of Natural History - New York
3. Carnegie Museum of Natural History - Pittsburgh
4. California Academy of Natural History - San Fransisco
5. Field Museum of Natural History - Chicago
6. Dallas Museum of Natural History (not as big but closer)
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1. Humans alter environments
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a. pollution
b. habitat destruction
c. oil spills
d. pesticides/herbicides
e. fertilizer
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a. zebra mussel
b. lamprey
c. rats, cats, etc.
d. brown tree snake
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a. directly by over harvesting
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- great auk
- passenger pigeon
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- ivory-billed woodpecker

