1. Earth History

2. Eons – largest time division
Eons determined by major changes in the Earth
Most recent Eon started with the appearance of multicellular animals = Phanerozoic Eon
Three Eons make up what was previously know as the Precambrian Period
1) Proterozoic
2) Archean
3) Hadean

3. The Hadean Eon: 4.5 billion years ago
Earth & planets formed from dust and gasses surrounding the sun

4. Heavy elements in planets suggest dust/gas from supernova
We observe other solar systems forming
They form in diffuse nebulae like nebula M16.

5. Electrostatic forces gather dust into large lumps, called planetisimals
Collisions between lumps makes lots of heat
The Earth was molten during the Hadeon Eon.
Steam atmosphere formed as ice comets collided with Earth

6. After most planetisimals had become part of a planet, …
After most planetisimals had become part of a planet, …..fewer collisions
Earth’s temperature dropped below 1,000 ۫C
First rocks formed as crust cooled
The oldest Earth rocks currently known are 3.8 billion years old.
The oldest meteorites and lunar rocks are about 4.5 billion years old
Erosion and plate tectonics have probably destroyed all of the Earth rocks older than 3.8 billion years.

7. The Archaean Eon: 3.8 - 2.5 billion years ago
Began with the formation of solid rock
Volcanic activity added heavier gasses to atmosphere (CO2, N2)
Water condensed
Early oceans formed
First life appeared on Earth

8. Archean Atmosphere What’s missing? (CO2, H2O, N2, CO, H2S, HCl)
No free oxygen O2…..so no ozone either O3
Still present in
modern atmosphere
Rare in
What’s missing?

9. WHEN Did Life Evolve?
Life must have evolved before there was free oxygen in the atmosphere
O2 breaks down macromolecules
If macromolecules couldn’t form….
…....living cells could not form

10. Early Archean sediment dark-colored = unoxidized
Formed before (O2) in atmosphere
oxidized (rusted) sediment appears 2.2 billion years ago in Proterozoic Eon
The free oxygen produced by living cells doing .…
photosynthesis
Therefore, life must have evolved before 2.2 bya

11. BIFs (Banded Iron Formations)
Indirect (non-fossil) evidence for the presence of
cyanobacteria ~ 3.5 bya
oldest fossils of life-forms ~3.5 byo
Precambrian,
Australia

12. Banded Iron Formations Created
iron dissolves in anaerobic water
when iron bonds to O2 it becomes solid
the solid sinks to the ocean floor is deposited in layers
Layers of oxidized iron are red

13. Why are BIFs Banded? When runoff added more Fe to the water the entire process stared over again.

14. What Likely Happened O2 made by cyanobacteria at ocean surface
O2 toxic to them
but not if the O2 was removed by bonding with iron (Fe)
Oceans contained dissolved iron

15. BIFs began forming 3.5 bya = 1st free O2
ended about 1.8 bya = constant free O2

16. The Proterozoic Eon: 2.5 - .54 billion years ago major geologic changes
Earths crust fuse into large continents
End of BIFs……
Oxygen resistant Cyanobacteria (early proterozoic)
Diversification of bacteria
First Eukaryotes appear ( protists)
Ediacaran fauna appear (soft invertebrates)

17. Phanerozioc Eon 540 million years ago -present
540 mya = .54 bya
Began with the Cambrian explosion of
multicellular animal species and
complex land plants