Early Earth: The First Two Billion Years Flashcards

1
Q

How do we know about Earth in the Precambrian?

A

Precambrian rocks are poorly exposed -> eroded or metamorphosed or deeply buried beneath younger rocks
Fossils are seldom found in Precambrian rocks
Long time ago - Does “Uniformitarianism” apply?
87% of Earth history is poorly known – a fragmented record

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2
Q

when was the Hadean?

A

4.55-4.0 Ga

no rocks are preserved from this time

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3
Q

when was the Archean?

A

4.0-2.5 Ga

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4
Q

what are the great precambrian events?

A
  1. 0 Ga - oldest known rocks
  2. 5 Ga - oldest known fossils
  3. 0-1.6 Ga - transition to oxygen atmosphere and approx origin of eukaryotes
  4. 54 Ga (540 Ma) - oldest animal fossils
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5
Q

what happened in the first 50 million years with regards to earths core and layering?

A

Layering requires process of differentiation
Initial heating, partial melting: ‘magma ocean’
Fe metal sinks to form core
Less dense ‘silicate’ melt (Si,O, remaining other elements) forms lighter mantle & crust

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6
Q

Why was early Earth hot?

A

Heat from gravitational contraction
Accretionary heat from asteroid impacts
Radioactive decay

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7
Q

what is a possible explanation for the formation of the moon?

A

(4.5 Ga)

Giant Impact Hypothesis (the Big Splash) -> Theia crashes into earth -> moon forms

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8
Q

what is the evidence for liquid water in the early hadean?

A

Earth’s oldest minerals
Jack Hills, Australia
4.4 billion yr-old zircons
Isotope data
-> Magma in which the zircons formed included melt from crustal material that must have interacted with liquid water
-> Liquid water present during early Hadean

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9
Q

when are the earths oldest preserved rocks from?

A

the Archean

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10
Q

where are precambrian rocks found today?

A

archean rocks: form cores of continents -cratons

- metamorphosed granite, volcanic & sedimentary rocks in ‘belts’

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11
Q

what are the earths oldest rocks?

A

Acasta Gneiss, NWT, Canada
3.962 Ga
Oldest rock age (igneous origin)

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12
Q

what is evidence for liquid water from the Archean?

A
Isua, West Greenland
3.8 Ga
Deformed pillow lavas - Implication?
- subaqueous eruption
- ‘ocean water’ existed
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13
Q

what is the ‘faint young sun’ paradox

A

Early Earth Surface Temperature Should be Freezing (no liquid water)
4.5 Ga:
Sun’s output only 70% that of today (Stellar evolution)
Too cold to maintain a liquid ocean -> refuted by geologic evidence

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14
Q

Why are there so few rocks older than ~3.8 Ga?

A

Late Heavy Bombardment
‘Impact zones’ & impact melt rocks on the Moon
Ages peak at 3.8 Ga
Consequence for Earth’s surface nearby? -> obliterated

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15
Q

what were plate tectonics like in the Archean?

A

Higher internal temperature of the Earth
Faster plate motion?
Many small, mobile plates
Early crust oceanic –continents formed later

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16
Q

what is some evidence for continents in the Archean (4-2.5 Ga)?

A

Oldest rocks (Acasta Gneiss, 3.96 Ga; Isuapillow lavas, 3.8 Ga)
3.46 Ga fossil soil (paleosol): Pilbara region, Australia
Liquid oceans -> warm greenhouse atmosphere
Subaerial weathering, soil formation
Continents above sea level

17
Q

what was the early atmosphere like?

A

Initial H, He lost to space
Volcanic outgassing -> water vapour, CO2, SO2, H2S, CH4.
Meteorites/comets -> water, nitrogen
Convection in core -> magnetic field deflects solar wind, so gases/atmosphere can accumulate
Early atmosphere dense, very hot
Mostly water vapour, CO2, nitrogen
Very little oxygen -> Earth inhospitable to most forms of life as we know it today

18
Q

what are most Archean fossils?

A

stromatolites and single cells

19
Q

what is a stromatolite?

A

dome-like layered structure formed from mat-like colonies (of single-celled cyanobacteria) that trap sediment and calcium carbonate
Oldest stromatolites: 3.5 Ga (W. Australia)

20
Q

where are modern stromatolites found?

A

extreme environments: e.g., high-salinity Shark Bay, Australia

21
Q

what are the archean single-celled micro-organisms?

A

Simplest form of modern carbon-based life
Lack DNA-packaging nuclei
Only life on Earth for next 2 billion years

Infer: Photosynthesis: occurring by 3.0 Ga, possibly as early as 3.5 Ga -> oxygen

22
Q

what is needed for the origins of life?

A

Carbon, Hydrogen, Oxygen, Nitrogen, Phosphorus, Sulfur
Proteins (chains of amino acids): build living materials, catalysts for reactions in organisms
Nucleic acids (DNA, RNA)
Organic phosphorus: transforms light/chemical fuel -> energy
Cell membrane: encloses cell components

23
Q

how were amino acids formed in a simulated early earth atmosphere?

A

Miller and Urey experiment (1950’s):
Formed amino acids (building blocks of life)from: H2, CH4(methane), NH3(ammonia), H2O (steam) gases & sparks (simulated lightning)

24
Q

in what type of environment did early organisms form in?

A

Developed in presence of an oxygen-free atmosphere (anaerobic- no oxygen for respiration)
No oxygen -> no ozone shield(O3) against harmful ultraviolet radiation

25
Q

where did early organisms live?

A

Deep-sea hydrothermal vents
Hyperthermophiles or microbes thrive in seawater hotter than 100 C
Derive energy by chemosynthesis, not by photosynthesis
Hyperthermophiles are Archaea, different from bacteria (also single-celled)
Possible environment for origin of life