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Early Earth History Sci 4.2. Question 1 Precambrian time 1 st 4 bil. years Few rocks older than 3.5...

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Early Earth History Sci 4.2
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Page 1: Early Earth History Sci 4.2. Question 1 Precambrian time 1 st 4 bil. years Few rocks older than 3.5 bil. due to erosion and remelting.

Early Earth History

Sci 4.2

Page 2: Early Earth History Sci 4.2. Question 1 Precambrian time 1 st 4 bil. years Few rocks older than 3.5 bil. due to erosion and remelting.

Question 1

Page 3: Early Earth History Sci 4.2. Question 1 Precambrian time 1 st 4 bil. years Few rocks older than 3.5 bil. due to erosion and remelting.

Precambrian time• 1st 4 bil. years

• Few rocks older than 3.5 bil.

due to erosion and remelting

Page 4: Early Earth History Sci 4.2. Question 1 Precambrian time 1 st 4 bil. years Few rocks older than 3.5 bil. due to erosion and remelting.

Question 2

Page 5: Early Earth History Sci 4.2. Question 1 Precambrian time 1 st 4 bil. years Few rocks older than 3.5 bil. due to erosion and remelting.

1st organisms were single celled• cyanobacteria: (blue-green algae) did photosynthesis• Produced stromatolite fossils

Page 6: Early Earth History Sci 4.2. Question 1 Precambrian time 1 st 4 bil. years Few rocks older than 3.5 bil. due to erosion and remelting.

Question 3

Page 7: Early Earth History Sci 4.2. Question 1 Precambrian time 1 st 4 bil. years Few rocks older than 3.5 bil. due to erosion and remelting.

photosynthesis• In chlorophyll, CO2 is taken apart

A fewtypes ofCyano-bacteria

• CO2 light C + O2

• In stratosphere O2 UV light O3 (ozone layer)

Page 8: Early Earth History Sci 4.2. Question 1 Precambrian time 1 st 4 bil. years Few rocks older than 3.5 bil. due to erosion and remelting.

Question 4

Page 9: Early Earth History Sci 4.2. Question 1 Precambrian time 1 st 4 bil. years Few rocks older than 3.5 bil. due to erosion and remelting.

Invertebrates:• Animals without backbones• Appeared late Precambrian• Ediacaran fauna

Page 10: Early Earth History Sci 4.2. Question 1 Precambrian time 1 st 4 bil. years Few rocks older than 3.5 bil. due to erosion and remelting.

Question 5

Page 11: Early Earth History Sci 4.2. Question 1 Precambrian time 1 st 4 bil. years Few rocks older than 3.5 bil. due to erosion and remelting.

Paleozoic era• 1st animals with hard parts• 1st insects• 1st Vertebrates • Shallow seas

Page 12: Early Earth History Sci 4.2. Question 1 Precambrian time 1 st 4 bil. years Few rocks older than 3.5 bil. due to erosion and remelting.

Dunkleosteus a.k.a. Bonefish

Page 13: Early Earth History Sci 4.2. Question 1 Precambrian time 1 st 4 bil. years Few rocks older than 3.5 bil. due to erosion and remelting.

Question 6

Page 14: Early Earth History Sci 4.2. Question 1 Precambrian time 1 st 4 bil. years Few rocks older than 3.5 bil. due to erosion and remelting.

Amphibians:• Lungs, must lay eggs in moist places

• May have evolved from fish like

Had both lungs and gills

Page 15: Early Earth History Sci 4.2. Question 1 Precambrian time 1 st 4 bil. years Few rocks older than 3.5 bil. due to erosion and remelting.
Page 16: Early Earth History Sci 4.2. Question 1 Precambrian time 1 st 4 bil. years Few rocks older than 3.5 bil. due to erosion and remelting.
Page 17: Early Earth History Sci 4.2. Question 1 Precambrian time 1 st 4 bil. years Few rocks older than 3.5 bil. due to erosion and remelting.

Question 7

Page 18: Early Earth History Sci 4.2. Question 1 Precambrian time 1 st 4 bil. years Few rocks older than 3.5 bil. due to erosion and remelting.

1st Insects• Appeared about same time as

amphibians

Page 19: Early Earth History Sci 4.2. Question 1 Precambrian time 1 st 4 bil. years Few rocks older than 3.5 bil. due to erosion and remelting.
Page 20: Early Earth History Sci 4.2. Question 1 Precambrian time 1 st 4 bil. years Few rocks older than 3.5 bil. due to erosion and remelting.

Reptiles:• Evolved from amphibians• Have scales to retain water• Eggs have protective membrane

Page 21: Early Earth History Sci 4.2. Question 1 Precambrian time 1 st 4 bil. years Few rocks older than 3.5 bil. due to erosion and remelting.

Question 8

Page 22: Early Earth History Sci 4.2. Question 1 Precambrian time 1 st 4 bil. years Few rocks older than 3.5 bil. due to erosion and remelting.

Appalachian/Atlas mtn.s

Pangea formsin late Paleozoic

Breaks apart inearly Mesozoic

Page 23: Early Earth History Sci 4.2. Question 1 Precambrian time 1 st 4 bil. years Few rocks older than 3.5 bil. due to erosion and remelting.

Question 9

Page 24: Early Earth History Sci 4.2. Question 1 Precambrian time 1 st 4 bil. years Few rocks older than 3.5 bil. due to erosion and remelting.

End of Paleozoic• 90% marine species became extinct

• 70% land “ “ “

• Pangea and glaciers formed

Page 25: Early Earth History Sci 4.2. Question 1 Precambrian time 1 st 4 bil. years Few rocks older than 3.5 bil. due to erosion and remelting.

Question 10

Page 26: Early Earth History Sci 4.2. Question 1 Precambrian time 1 st 4 bil. years Few rocks older than 3.5 bil. due to erosion and remelting.

Organize in order of appearance on earth

• Invertebrates

• Vertebrates (fish)

• Amphibians

(and insects)

• Reptiles

• Amphibians

(and insects)

• Vertebrates (fish)

• Reptiles

• Invertebrates

Page 27: Early Earth History Sci 4.2. Question 1 Precambrian time 1 st 4 bil. years Few rocks older than 3.5 bil. due to erosion and remelting.

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