Early Earth Flashcards

(39 cards)

1
Q

Hadean

A

Huh-dee’-un
up to 4 billion years ago
oldest eon in ages of the earth

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2
Q

Old theory of earth hadean surface

A

lava oceans

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3
Q

New theory of earth hadean surface

A

water, stratovolcanoes, stromatolites

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4
Q

stromatolite

A

sedimentary rocks formed from layers of microbial reefs
oldest dated rocks

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5
Q

Earliest crust

A

komatiites

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6
Q

komatiite

A

ultramafic extrusive igneous rock
forms in extremely hot conditions

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7
Q

how did felsic crust form

A

after some cooling of earth surface
recycling of komatiites due to fractional crystallization

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8
Q

fractional crystallization

A

composition of magma changes as certain elements solidify into minerals (crystallize) in specific temperature ranges
(Fe, Mg crytallize first, carbon and silicon later)

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9
Q

characteristics of zircon

A

durable
chemically inert
persist as detrital (sand) and reincorporated over and over in sedimentary rock

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10
Q

Jack Hills zircon

A

oldest dated zircon ~4.4 Gya, found in conglomerates and metamorphic (so must be recycled) rocks in the Jacks Hills, mountain range in Australia (rocks dated to 3.8Gya)
G= billion

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11
Q

2 pieces of evidence from Jack Hills zircon and what that tells us

A

1) crust existed 4.4 Gya - the zircons had to have come from an older crust and been recycled into these rocks (those rocks likely did not survive Heavy Bombardment of 3.9Gya and were recycled as sedimentary/metamorphic rocks)
2) oxygen isotopes in the zircon suggest liquid water was present at the formation of zircon

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12
Q

What does Jack Hills zircon mean for life on earth?

A

If crust and water was present, the environment was potentially hospitable earlier than previous thought

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13
Q

Did life exist in Hadean?

A

There is no evidence to suggest it

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14
Q

If life existed during Hadean, how could it have survived bombardment?

A

Hydrothermal vents could have provided some
(maybe - its just a thought experiment)

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15
Q

Archean

A

2nd oldest eon
4Gya -> 2.5 Gya (has 4 eras)

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16
Q

Mantle temperature during Archean

A

hotter than any other known eon, believed to not be as hot as Hadean
(no rocks remaining from Hadean to confirm)

17
Q

What makes measuring temperature of mantle difficult?

A

mantle eruptions come from a plume, not the bulk or ambient mantle

18
Q

How can we infer the ambient mantle temperature?

A

empirical evidence links MgO weight % to temperature at time of basalt formation
(still measuring plumes, not ambient mantle, so an inference, not measurable fact)

19
Q

Two theories on regarding HOT Archean CRUST

A

Hot because greater abundance of radioactive species in crust (generating heat as they decay)
1) so hot it was thermally unstable
2) mechanisms in play that provided effective enough cooling to prevent instability

20
Q

Thermal Instabailty

A

Temperatures so hot and variable that it induces rapid changes in pressure and density

21
Q

Rocks that help understand Archean environment

A

Acasta Granitic Gneiss (4.03Gy)
Greenland conglomerate (3.8Gy)
Coonterunah/Warrawoona (Australia) unconformity (3.5Gy)

22
Q

Acasta Granitic Gneiss

A

oldest known exposed rock (most well accepted proposed)

23
Q

What does gneiss tell us about environment?

A

Contain mica = hydrated minerals = liquid water had to be present

24
Q

What does conglomerate tell us about the environment?

A

conglomerate has pebbles with rounded edges = shallow flowing liquid water had to be present on surface to erode weathered rocks

25
What does an unconformity tell us about the environment?
It is subaerial - not sure why this matters
26
How does plate tectonics help life?
provides planetary homeostasis by regulating the environment
27
2 theories about Archean plate tectonics
hotter mantle (evidence from MgO weight % in basalts) 1) plates were smaller and moved faster 2) thicker oceanic crust due to hotter mantle having more melt, would have caused problems for subduction and therefore larger and slower plates
28
Bonninites
extrusive igneous rock containing magnesium and silica, thought to form in the early stages of subduction in volcanic arc systems; Drew's definition = primitive andesite
29
oldest bonninites
2.7 to 2.8, Finland and Canada
30
Ophiolites
rock formed from sequence of formations and deposits on the ocean floor that have been uplifted and exposed in continental crust
31
oldest ophiolite
2.0 Ga, Canada
32
rocks that help define history of plate movement via tectonics
bonninites ophiolites rocks that constrain pressure/temp conditions that are found in subduction zones (blueschist, eclogites)
33
blueschist
formed in subduction zones and indicate high pressure, low temperature (200-500 Celsius, 15-30 km depth)
34
eclogites
formed in subduction zones and indicate high pressure, mid-range temperature (500-1000 Celcius, 30-50 km depth)
35
oldest subduction zone rocks
~ 1 Ga (many locations)
36
Timeline of early earth (9 points)
4.54 Ga - earth formed 4 Ga - Moon forming impact cooling 4.4 Ga water present/crust present? ~4 Ga water/crust exposed? 3.8 Ga water definitely present 3.5 Ga crust definitely exposed ~ 2.8 Ga plate tectonics? 1 Ga, definitely plate tectonics
37
Why is crust important for early life?
provided stable platform, diverse environments, opportunity for heating and cooling
38
why is temperature change important for origin of life?
causes disequilibrium that could encourage specific chemical reactions
39
what are indications that the earth had an environment friendly for life early in its history?
presence of liquid water and crust