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6. Example: - K40-Ar40 suppose 1/2 of total is Ar40 = 1.3by (Now, you may be thinking, "be real"! How can we measure something that is this slow?) - by the way - what type of decay?

6. Example: - K40-Ar40 suppose 1/2 of total is Ar40 = 1.3by (Now, you may be thinking, "be real"! How can we measure something that is this slow?) - by

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6. Example: - K40-Ar40 suppose 1/2 of total is Ar40 = 1.3by (Now, you may be thinking, "be real"! How can we measure something that is this slow?) - Well, 40 grams of Potassium (K) contains: 6.0 x atoms (Avogadro's number, remember that little chemistry tid-bit?). So, For 1/2 of them to change, that would be: 3.0 x atoms in 1.3 billion years (1.3 x 10 9 )

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Page 1: 6. Example: - K40-Ar40 suppose 1/2 of total is Ar40 = 1.3by (Now, you may be thinking, "be real"! How can we measure something that is this slow?) - by

6. Example:                   - K40-Ar40  suppose 1/2 of total is Ar40 = 1.3by

                (Now, you may be thinking, "be real"! How can we measure something that is this slow?)                  - by the way - what type of decay?

Page 2: 6. Example: - K40-Ar40 suppose 1/2 of total is Ar40 = 1.3by (Now, you may be thinking, "be real"! How can we measure something that is this slow?) - by

6. Example:                   - K40-Ar40  suppose 1/2 of total is Ar40 = 1.3by

                (Now, you may be thinking, "be real"! How can we measure something that is this slow?)                 

- Well, 40 grams of Potassium (K) contains:                                  6.0 x 1023 atoms (Avogadro's number, remember that little chemistry tid-bit?).                         

Page 3: 6. Example: - K40-Ar40 suppose 1/2 of total is Ar40 = 1.3by (Now, you may be thinking, "be real"! How can we measure something that is this slow?) - by

6. Example:                   - K40-Ar40  suppose 1/2 of total is Ar40 = 1.3by

                (Now, you may be thinking, "be real"! How can we measure something that is this slow?)                 

- Well, 40 grams of Potassium (K) contains:                                  6.0 x 1023 atoms (Avogadro's number, remember that little chemistry tid-bit?).                   So, For 1/2 of them to change, that would be:                   3.0 x 1023 atoms in 1.3 billion years (1.3 x 109)

Page 4: 6. Example: - K40-Ar40 suppose 1/2 of total is Ar40 = 1.3by (Now, you may be thinking, "be real"! How can we measure something that is this slow?) - by

6. Example:                   - K40-Ar40  suppose 1/2 of total is Ar40 = 1.3by

                (Now, you may be thinking, "be real"! How can we measure something that is this slow?)                 

- Well, 40 grams of Potassium (K) contains:                                  6.0 x 1023 atoms (Avogadro's number, remember that little chemistry tid-bit?).                   So, For 1/2 of them to change, that would be:                   3.0 x 1023 atoms in 1.3 billion years (1.3 x 109)                   So, divide 3.0 x 1023  by 1.3 x 109 = 2.3 X 1014 atoms/year.                  

Page 5: 6. Example: - K40-Ar40 suppose 1/2 of total is Ar40 = 1.3by (Now, you may be thinking, "be real"! How can we measure something that is this slow?) - by

6. Example:                   - K40-Ar40  suppose 1/2 of total is Ar40 = 1.3by

                (Now, you may be thinking, "be real"! How can we measure something that is this slow?)                 

- Well, 40 grams of Potassium (K) contains:                                  6.0 x 1023 atoms (Avogadro's number, remember that little chemistry tid-bit?).                   So, For 1/2 of them to change, that would be:                   3.0 x 1023 atoms in 1.3 billion years (1.3 x 109)                   So, divide 3.0 x 1023  by 1.3 x 109 = 2.3 X 1014 atoms/year.                   Then, divide 2.3 x 1014 by 365 (3.65 x 102) days per year

= 0.62 x 1012 per day ( shift decimal = 6.2 x 1011)                 

Page 6: 6. Example: - K40-Ar40 suppose 1/2 of total is Ar40 = 1.3by (Now, you may be thinking, "be real"! How can we measure something that is this slow?) - by

6. Example:                   - K40-Ar40  suppose 1/2 of total is Ar40 = 1.3by

                (Now, you may be thinking, "be real"! How can we measure something that is this slow?)                 

- Well, 40 grams of Potassium (K) contains:                                  6.0 x 1023 atoms (Avogadro's number, remember that little chemistry tid-bit?).                   So, For 1/2 of them to change, that would be:                   3.0 x 1023 atoms in 1.3 billion years (1.3 x 109)                   So, divide 3.0 x 1023  by 1.3 x 109 = 2.3 X 1014 atoms/year.                   Then, divide 2.3 x 1014 by 365 (3.65 x 102) days per year

= 0.62 x 1012 per day ( shift decimal = 6.2 x 1011)                   Then, divide 6.2 x 1011 by 24*60*60 = 86,400 seconds/day:

(= 8.64 x 104) = 0.7 x 107 atoms/second                   

Page 7: 6. Example: - K40-Ar40 suppose 1/2 of total is Ar40 = 1.3by (Now, you may be thinking, "be real"! How can we measure something that is this slow?) - by

6. Example:                   - K40-Ar40  suppose 1/2 of total is Ar40 = 1.3by

                (Now, you may be thinking, "be real"! How can we measure something that is this slow?)                 

- Well, 40 grams of Potassium (K) contains:                                  6.0 x 1023 atoms (Avogadro's number, remember that little chemistry tid-bit?).                   So, For 1/2 of them to change, that would be:                   3.0 x 1023 atoms in 1.3 billion years (1.3 x 109)                   So, divide 3.0 x 1023  by 1.3 x 109 = 2.3 X 1014 atoms/year.                   Then, divide 2.3 x 1014 by 365 (3.65 x 102) days per year

= 0.62 x 1012 per day ( shift decimal = 6.2 x 1011)                   Then, divide 6.2 x 1011 by 24*60*60 = 86,400 seconds/day:

(= 8.64 x 104) = 0.7 x 107 atoms/second                    0.7 x 107 = 7 x 106 = 7 million atoms changing from Potassium to Argon every second!!!      (and the energy given off is measurable...)    

Page 8: 6. Example: - K40-Ar40 suppose 1/2 of total is Ar40 = 1.3by (Now, you may be thinking, "be real"! How can we measure something that is this slow?) - by

Post Darwinian Developments

II. Geology

A. The Age of the Earth

B. The Dynamic Earth

Page 9: 6. Example: - K40-Ar40 suppose 1/2 of total is Ar40 = 1.3by (Now, you may be thinking, "be real"! How can we measure something that is this slow?) - by

Post Darwinian Developments

II. Geology

A. The Age of the Earth

B. The Dynamic Earth

- why do coastlines fit?

Page 10: 6. Example: - K40-Ar40 suppose 1/2 of total is Ar40 = 1.3by (Now, you may be thinking, "be real"! How can we measure something that is this slow?) - by

Post Darwinian Developments

II. Geology

A. The Age of the Earth

B. The Dynamic Earth

1. why do coastlines fit?

- 1801 - Von Humboldt - intervening land sank (Atlantis?) or flood excavated it.

- 1858 - Pellegrini-Snider - outpouring of material at time of flood caused rifting and pushed continents apart to form the Atlantic.

Page 11: 6. Example: - K40-Ar40 suppose 1/2 of total is Ar40 = 1.3by (Now, you may be thinking, "be real"! How can we measure something that is this slow?) - by

Post Darwinian Developments

II. Geology

A. The Age of the Earth

B. The Dynamic Earth

2. Disjunct Distributions?

- southern beech

- marsupial fauna

Page 12: 6. Example: - K40-Ar40 suppose 1/2 of total is Ar40 = 1.3by (Now, you may be thinking, "be real"! How can we measure something that is this slow?) - by

Post Darwinian Developments

II. Geology

A. The Age of the Earth

B. The Dynamic Earth

3. How do mountains form?

- 1890's - Suess - "Contraction Hypothesis"- Interior of Kelvin's earth cools - condenses- contraction caused certain areas to collapse and subside to

form oceans. Left continents (mountains) standing high - earth wrinkles like a prune

Page 13: 6. Example: - K40-Ar40 suppose 1/2 of total is Ar40 = 1.3by (Now, you may be thinking, "be real"! How can we measure something that is this slow?) - by

Post Darwinian Developments

II. Geology

A. The Age of the Earth

B. The Dynamic Earth

3. How do mountains form?

- 1890's - Suess - "Contraction Hypothesis"- Interior of Kelvin's earth cools - condenses- contraction caused certain areas to collapse and subside to

form oceans. Left continents (mountains) standing high - earth wrinkles like a prune

- 1900's - Hall - "Geosyncline Hypothesis" - Lateral pressure from oceanic crusts pushes mountains up... - but what causes the "push"?

Page 14: 6. Example: - K40-Ar40 suppose 1/2 of total is Ar40 = 1.3by (Now, you may be thinking, "be real"! How can we measure something that is this slow?) - by

Post Darwinian Developments

II. Geology

A. The Age of the Earth

B. The Dynamic Earth

4. Continental Drift

- 1915 - Alfred Wegener

Page 15: 6. Example: - K40-Ar40 suppose 1/2 of total is Ar40 = 1.3by (Now, you may be thinking, "be real"! How can we measure something that is this slow?) - by

- Not accepted until the 1960’s and 1970’s, when sea floor spreading was observed, sonar was used to map the ocean, and paleomagnetism demonstrated where continents had been in the past relative to magnetic north.

Page 16: 6. Example: - K40-Ar40 suppose 1/2 of total is Ar40 = 1.3by (Now, you may be thinking, "be real"! How can we measure something that is this slow?) - by

- North and South Atlantic and Indian Ocean Basins.

Page 17: 6. Example: - K40-Ar40 suppose 1/2 of total is Ar40 = 1.3by (Now, you may be thinking, "be real"! How can we measure something that is this slow?) - by

Post Darwinian Developments

III. Paleontology

A. Intermediate Fossils

Page 18: 6. Example: - K40-Ar40 suppose 1/2 of total is Ar40 = 1.3by (Now, you may be thinking, "be real"! How can we measure something that is this slow?) - by

IchthyostegaFISH AMPHIBIANS

XXX

- Fins and gill covers (FISH)

- Feet (AMPHIBIANS)

- After fish, before amphibians (just where evolution predicts it should be)

Page 19: 6. Example: - K40-Ar40 suppose 1/2 of total is Ar40 = 1.3by (Now, you may be thinking, "be real"! How can we measure something that is this slow?) - by

Archeopteryx

REPTILES BIRDS

XXX

- Fingers, teeth, tail (Reptiles)-Feathers (birds)

- After reptiles, before birds (just where evolution predicts it should be)

Page 20: 6. Example: - K40-Ar40 suppose 1/2 of total is Ar40 = 1.3by (Now, you may be thinking, "be real"! How can we measure something that is this slow?) - by

Therapsids

REPTILES MAMMALS

XXX

- Mammalian skeleton- Intermediate ear- scales

- After reptiles, before mammals (just where evolution predicts it should be)

Page 21: 6. Example: - K40-Ar40 suppose 1/2 of total is Ar40 = 1.3by (Now, you may be thinking, "be real"! How can we measure something that is this slow?) - by

Mammals from the Jurassic (185 mya)

Pelycosaur Reptiles of the Carboniferous (300 mya)

Therapsids from the Permian (280 mya) to the Triassic (200mya)

Page 22: 6. Example: - K40-Ar40 suppose 1/2 of total is Ar40 = 1.3by (Now, you may be thinking, "be real"! How can we measure something that is this slow?) - by

Australopithecines

Australopithecus afarensis

Page 23: 6. Example: - K40-Ar40 suppose 1/2 of total is Ar40 = 1.3by (Now, you may be thinking, "be real"! How can we measure something that is this slow?) - by

Teeth

Page 24: 6. Example: - K40-Ar40 suppose 1/2 of total is Ar40 = 1.3by (Now, you may be thinking, "be real"! How can we measure something that is this slow?) - by

Legs

Page 25: 6. Example: - K40-Ar40 suppose 1/2 of total is Ar40 = 1.3by (Now, you may be thinking, "be real"! How can we measure something that is this slow?) - by

Skulls

Page 26: 6. Example: - K40-Ar40 suppose 1/2 of total is Ar40 = 1.3by (Now, you may be thinking, "be real"! How can we measure something that is this slow?) - by

Australopithecines

APES HUMANS

XXX

- After apes, before humans (just where evolution predicts it should be)

- bipedal (human trait)

- chimp-sized cranial volume

Page 27: 6. Example: - K40-Ar40 suppose 1/2 of total is Ar40 = 1.3by (Now, you may be thinking, "be real"! How can we measure something that is this slow?) - by

Post Darwinian Developments

III. Paleontology

A. Intermediate Fossils

- A test of Four Hypotheses using Fossils

Page 28: 6. Example: - K40-Ar40 suppose 1/2 of total is Ar40 = 1.3by (Now, you may be thinking, "be real"! How can we measure something that is this slow?) - by

Question 1: There are many kinds of life forms (species) on Earth. Where do species come from?

1. Four Alternate Hypotheses A. B. C. D.

A B C D A B C D A B C D A B C D

E

A B C D

E F F

A B C D E F E F G H G

Page 29: 6. Example: - K40-Ar40 suppose 1/2 of total is Ar40 = 1.3by (Now, you may be thinking, "be real"! How can we measure something that is this slow?) - by

Question 1: There are many kinds of life forms (species) on Earth. Where do species come from?

A.

2. Testing Hypotheses in an experiment:

- if ‘A’ is true, then we should see the same species in all layers of the fossil record.

A B C D

A B C D

Page 30: 6. Example: - K40-Ar40 suppose 1/2 of total is Ar40 = 1.3by (Now, you may be thinking, "be real"! How can we measure something that is this slow?) - by

Question 1: There are many kinds of life forms (species) on Earth. Where do species come from?

B.

2. Testing Hypotheses in an experiment:

- if ‘B’ is true, then we should see different species in the layers of the fossil record, but no intermediates.

A B C D

A B C D E F

E F

Page 31: 6. Example: - K40-Ar40 suppose 1/2 of total is Ar40 = 1.3by (Now, you may be thinking, "be real"! How can we measure something that is this slow?) - by

Question 1: There are many kinds of life forms (species) on Earth. Where do species come from?

C.

2. Testing Hypotheses in an experiment:

- if ‘C’ is true, then we should see different species in the layers of the fossil record, intermediates (E A) but no shared intermediates (linking A and B).

A B C D

E F G H

Page 32: 6. Example: - K40-Ar40 suppose 1/2 of total is Ar40 = 1.3by (Now, you may be thinking, "be real"! How can we measure something that is this slow?) - by

Question 1: There are many kinds of life forms (species) on Earth. Where do species come from?

D.

2. Testing Hypotheses in an experiment:

- if ‘D’ is true, then we should see different species in the layers of the fossil record, and shared intermediates (linking A and B).

A B C D

E

F

G

Page 33: 6. Example: - K40-Ar40 suppose 1/2 of total is Ar40 = 1.3by (Now, you may be thinking, "be real"! How can we measure something that is this slow?) - by

- RESULTS: Data from the physical world:

* Fossils differ from species alive today (refutes ‘A’)

Page 34: 6. Example: - K40-Ar40 suppose 1/2 of total is Ar40 = 1.3by (Now, you may be thinking, "be real"! How can we measure something that is this slow?) - by

- RESULTS: Data from the physical world:

* There are sequences of intermediate fossils (refutes ‘B’)

Page 35: 6. Example: - K40-Ar40 suppose 1/2 of total is Ar40 = 1.3by (Now, you may be thinking, "be real"! How can we measure something that is this slow?) - by

IchthyostegaFISH AMPHIBIANS

XXX

- Fins and gill covers (FISH)

- Feet (AMPHIBIANS)

- After fish, before amphibians (just where evolution predicts it should be)

- RESULTS: Data from the physical world:

* There are “linking species” – (refutes ‘C’)

Page 36: 6. Example: - K40-Ar40 suppose 1/2 of total is Ar40 = 1.3by (Now, you may be thinking, "be real"! How can we measure something that is this slow?) - by

Conclusion: Hypotheses A, B, and C are refuted by physical evidence, and hypothesis D is supported.

This is the Theory of Evolution by Common Ancestry

A. B. C. D.

A B C D A B C D A B C D A B C D

E

A B C D

E F F

A B C D E F E F G H G