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Class 4: Stratigraphy & Age Dating Geologic History and Extinctions Today’s topics: Characterizing geologic time Relative ages (stratigraphy) Absolute ages (radioactive decay) Today’s topics: Earth History Mass Extinctions Geologic Time Scale
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Class 4: Stratigraphy & Age Dating Geologic History and Extinctions Class updates: Reading: Section 4.0-4.6 Homework 1 due today Homework 2 online, due next Mon. Midterm practice online (website) Midterm review online (website) Midterm 1 on Feb. 28 th (next Mon.)
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How old is that rock?
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Determining Relative Geologic Time 1.Principle of Original Horizontality 2.Principle of Superposition 3.Principle of Cross-Cutting Relationship 4.Principle of Faunal Succession
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Principle of Original Horizontality
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San Juan River, Utah Canadian Rockies, Alberta
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Principle of Superposition
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Principle of Cross-Cutting Relationships Faulted rock Igneous intrusion
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Principle of Cross-Cutting Relationships
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Grand Canyon
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Order of Events? 1 2 3 4
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Grand Canyon Example Order of Events? 1 2 3 4
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Principle of Faunal (fossil) Succession
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Index Fossils Def.: accurately indicate the ages of sedimentary rocks 1) Abundantly preserved in rocks 2) Geographically widespread 3) Fast evolving - existed for a relatively short time 4) Easily identified
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Relative Dating: Unconformities comformity unconformity
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The Great Unconformity
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Types of Unconformity
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Relative Dating: Correlation
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How old is that rock? Relative age: order of events Absolute age: age in years Relative dating tells us what order things happened, but not how many years ago they happened.
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Absolute Dating: Radioactive Decay
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Radioactive Half-Life
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Half-life Example You start with $1000 in your bank account Every week your spouse or boyfriend/girlfriend removes half of the money The half-life of your account = 1 week 1 week
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Your Bank Account Start: $1000 Week 1: $500 Week 2: $250 Week 3: $125 Week 4: $62.50 Week 5: $31.25 Week 6: $15.63 Week 7: $7.81 Week 8: $3.90 Week 9: $1.95 Week 10: $0.98 Week 11: $0.49 Week 12: $0.24 Week 13: $0.12 Week 14: $0.06 Week 15: $0.03 Week: 16: $0.015 left in your bank account (1 half-life)
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Isotopes & Half Lives Young things Old things
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Radiometric Dating
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Radioactive Decay Curve
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Calculating Absolute Age Potassium-40 included in mineral (start clock) Begins decaying to Argon-40 Brilliant scientists have told us the half-life of K-Ar is 1.3 billion yrs (Gyr) We count # parents & daughters in sample We find that our sample contains 50% K & 50% Ar So 1/2 of our initial sample (K) has decayed How old is it? We find another sample that is 25% K & 75% Ar How old is it?
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Mass Extinctions
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A Bad Day…. 65 Million Years Ago
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Mass Extinctions: Extraterrestrial Impacts
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Fig. 4-2, p.75 Mass Extinctions: Volcanic Eruptions
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Fig. 4-2, p.75 Example Eruptions:
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Mass Extinctions: Atmosphere-Ocean-Continent Interactions
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Evolution of Earth Atmosphere Nitrogen Oxygen All Others
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Fig. 4-2, p.75 Mass Extinctions: Atmosphere-Ocean Interaction (1)
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Mass Extinctions: Atmosphere-Ocean Interaction (2)
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Mass Extinctions: Atmosphere-Ocean-Continent Interactions
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Mass Extinctions: Ocean-Continent Interaction
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Geologic Time & Biology Geologic time (millions of years)
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Fig. 4-1b, p.74 Geologic Time & Biology Geologic time (millions of years)
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Geologic Time & Biology Geologic time (millions of years)
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Geologic Time Major divisions Cenozoic: 66 - 2.5 m.y.a Mesozoic: 245 - 66 m.y.a. Paleozoic: 544 - 245 m.y.a. Precambrian: pre-544 m.y.a. (proterozoic)
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Geologic Time
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Precambrian (4.6 Ga – 570 Ma)
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Paleozoic Era (570 Ma - 245 Ma)
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Mesozoic Era (245 Ma – 66 Ma)
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Cenozoic Era (66 Ma - present)
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Satellites1 (Moon) Size (radius)6378 km Bulk density5.5 g/cm 3 (4.1 g/cm 3 uncompressed) Surface gravity 9.8 m/s 2 Tectonism, volcanismyes (today) Rotation 1 day Orbit365.25 days Atmosphere 78% N 2, 21% O 2 Surface pressure1 atm Surface temperature 20°C (diurnal, seasonal changes) Plate tectonicsyes Wateryes Earth
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