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8-2 NOTES: HISTORY OF LIFE CHAPTER 14
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8-2 NOTES: HISTORY OF LIFE CHAPTER 14. AGE OF EARTH The earth is about 4.5 billion years old How did we measure that? .

Jan 12, 2016

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Page 1: 8-2 NOTES: HISTORY OF LIFE CHAPTER 14. AGE OF EARTH The earth is about 4.5 billion years old How did we measure that? .

8-2 NOTES: HISTORY OF LIFECHAPTER 14

Page 2: 8-2 NOTES: HISTORY OF LIFE CHAPTER 14. AGE OF EARTH The earth is about 4.5 billion years old How did we measure that? .

AGE OF EARTHThe earth is about 4.5 billion years old

How did we measure that?

https://www.youtube.com/watch?v=H2_6cqa2cP4

Page 3: 8-2 NOTES: HISTORY OF LIFE CHAPTER 14. AGE OF EARTH The earth is about 4.5 billion years old How did we measure that? .

AGE OF EARTHThe earth is about 4.5 billion years old

How did we measure that?

• Radiometric Dating = calculating the age of an object by measuring proportions of radioactive isotopes

Page 4: 8-2 NOTES: HISTORY OF LIFE CHAPTER 14. AGE OF EARTH The earth is about 4.5 billion years old How did we measure that? .

RADIOMETRIC DATINGRadioactive Isotope = an unstable form of an element, decays into stable element, gives off energy (radiation)

• Ex. Carbon-14 decays into Nitrogen • Ex. Potassium-40 decays into Argon-40

Page 5: 8-2 NOTES: HISTORY OF LIFE CHAPTER 14. AGE OF EARTH The earth is about 4.5 billion years old How did we measure that? .

RADIOMETRIC DATINGHalf-life = the time it takes for half of a radioactive isotope to decay

• Ex. K-40 half life is 1.3 billion years

Page 6: 8-2 NOTES: HISTORY OF LIFE CHAPTER 14. AGE OF EARTH The earth is about 4.5 billion years old How did we measure that? .

PRACTICE

The half life of carbon-14 is 5,730 years. If only 25% of the original amount of carbon-14 is left in an object, how hold it the object?

Page 7: 8-2 NOTES: HISTORY OF LIFE CHAPTER 14. AGE OF EARTH The earth is about 4.5 billion years old How did we measure that? .

PRACTICE

The half life of carbon-14 is 5,730 years. If only 25% of the original amount of carbon-14 is left in an object, how hold it the object?

1.Determine how many half lives have elapsed.

• 25% or ¼ = 2 half lives

Page 8: 8-2 NOTES: HISTORY OF LIFE CHAPTER 14. AGE OF EARTH The earth is about 4.5 billion years old How did we measure that? .

PRACTICE

The half life of carbon-14 is 5,730 years. If only 25% of the original amount of carbon-14 is left in an object, how hold it the object?

1.Determine how many half lives have elapsed.

• 25% or ¼ = 2 half lives

2.Multiply this by the known half life.

• Carbon half life = 5,730 years• 2(5,730 yrs) = 11,460 years

Page 9: 8-2 NOTES: HISTORY OF LIFE CHAPTER 14. AGE OF EARTH The earth is about 4.5 billion years old How did we measure that? .

FIRST ORGANIC COMPOUNDS

Spontaneous Origin: organic compounds developing from non-living chemical reactions

Page 10: 8-2 NOTES: HISTORY OF LIFE CHAPTER 14. AGE OF EARTH The earth is about 4.5 billion years old How did we measure that? .

SPONTANEOUS ORIGINOparin: (1920) Hypothesized that primitive Earth’s atmosphere was:

• NH3 (ammonia)

• H2

• H2O• CH4 (methane)

No Oxygen!

Page 11: 8-2 NOTES: HISTORY OF LIFE CHAPTER 14. AGE OF EARTH The earth is about 4.5 billion years old How did we measure that? .

SPONTANEOUS ORIGIN

Miller-Urey: (1953) Produced organic compounds (amino acids) based on the hypothesized composition of early earth’s atmosphere

Page 12: 8-2 NOTES: HISTORY OF LIFE CHAPTER 14. AGE OF EARTH The earth is about 4.5 billion years old How did we measure that? .

FIRST LIFE FORMS - THE FIRST CELLS

Prokaryotes before eukaryotes

Page 13: 8-2 NOTES: HISTORY OF LIFE CHAPTER 14. AGE OF EARTH The earth is about 4.5 billion years old How did we measure that? .

FIRST LIFE FORMS - THE FIRST CELLS

Prokaryotes before eukaryotes

3 major trends all interrelated:

•Anaerobic Aerobic

Inferences based on early earth environment having:1. No Oxygen Gas

(anaerobic)

Page 14: 8-2 NOTES: HISTORY OF LIFE CHAPTER 14. AGE OF EARTH The earth is about 4.5 billion years old How did we measure that? .

FIRST LIFE FORMS - THE FIRST CELLS

Prokaryotes before eukaryotes

3 major trends all interrelated:

•Anaerobic Aerobic

•Heterotrophic Autotrophic•Chemosynthetic Photosynthetic

Inferences based on early earth environment having:1. No Oxygen Gas

(anaerobic)2. Many organic

molecules for food (hetero)

3. Extreme harsh conditions (chemosynthetic)

Page 15: 8-2 NOTES: HISTORY OF LIFE CHAPTER 14. AGE OF EARTH The earth is about 4.5 billion years old How did we measure that? .

THE FIRST EUKARYOTES

ENDOSYMBIOSIS THEORY

• Mitochondria (aerobic prok) and chloroplasts (chemosynthetic prok) are thought to be prokaryotic cells that were engulfed by a bigger prokaryote.

• Created mutual beneficial relationship• Bigger prokaryote provided a beneficial environment• Smaller prokaryote provided a source of energy

Page 16: 8-2 NOTES: HISTORY OF LIFE CHAPTER 14. AGE OF EARTH The earth is about 4.5 billion years old How did we measure that? .

THE FIRST EUKARYOTES

ENDOSYMBIOSIS THEORY

• Mitochondria (aerobic prok) and chloroplasts (chemosynthetic prok) are thought to be prokaryotic cells that were engulfed by a bigger prokaryote.

Supporting Evidence:

• Both organelles contain their own DNA• DNA is circular (like other prokaryotes)• Can replicate on their own.

Page 17: 8-2 NOTES: HISTORY OF LIFE CHAPTER 14. AGE OF EARTH The earth is about 4.5 billion years old How did we measure that? .

PUT THESE IN THE ORDER IN WHICH THEY ARE THOUGHT TO HAVE ORIGINATED ON EARTH

1. Anaerobic heterotrophic prokaryotes

2. Aerobic eukaryotes

3. Chemosynthetic prokaryotes

4. Photosynthetic prokaryotes

Answer: 1, 3, 4, 2

Page 18: 8-2 NOTES: HISTORY OF LIFE CHAPTER 14. AGE OF EARTH The earth is about 4.5 billion years old How did we measure that? .

SEQUENCE OF FIRST CELLSAnaerobicHeterotrophicProkaryotes

ChemosyntheticProkaryotes

PhotosyntheticProkaryotes

PhotosyntheticEukaryotes

AerobicEukaryotes

Endosymbiosis Occurs Here!