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8-2 NOTES: HISTORY OF LIFE CHAPTER 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?

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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!