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Evolution- Change in life forms over time
Why do things change? How do they change?
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Estimated age of earth-4.6 Billion years
4 geologic eras Precambrian Paleozoic Mesozoic Cenozoic episodes of mass extinction separates eras
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At the beginning Hot, lots of volcanic activity, no free oxygen, but lots of water vapor. 3.9 Billion years ago, oceans formed 3.5 BYA first fossil evidence of life- photosynthetic bacteria
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The history of earth is written in the rocks.
Fossil: evidence of existence preserved in rock Structure indicates function 2 questions – how are fossils formed and how to we determine their age Oldest fossils found are 3.5 billion years old and are microscopic photosynthetic bacteria
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Analyzing the fossil record
Life was incredible diverse Size, structure, function Episodes of mass extinction Episodes of evolutionary explosions
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Covered with mud, sand- no decay
Fossil Formation Organism dies Covered with mud, sand- no decay Compression over time = sedimentary rock and fossil Where might fossils be forming today?
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Formation of fossils Casts- minerals fill in Mold- leaves an empty space Amber-preserved or frozen Trace or carbon imprint
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Determining the age of a fossil: 2 ways
Relative dating Absolute dating
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Relative dating Fossils in deepest layer are oldest
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2. Absolute dating More accurate than relative dating Uses radioactive decay of isotopes Isotopes are radioactive natural variations of elements
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Examples of Isotopes T1/2 in years
C-14 decays to N years Uranium 235 to Lead million Potassium 40 to Argon billion Half life is the time it takes for half (50%) of the isotope to change into new form.
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“Parent” compound is C14 “Daughter “ compound is N14 T1/2 is 5730 years Start with 12.5g of C14 and g of N14. How old is your fossil?
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Carbon 14 is used for fossils < 50,000 years old
Potassium-40 for older specimens
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