origin of earth Flashcards

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1
Q

eons

A

largest time division

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2
Q

Eons determined by

A

major changes in the Earth

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3
Q

Most recent Eon started with

A

started with the proliferation of multicellular animals = Phanerozoic Eon

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4
Q

what Three Eons make up what was previously know as the Precambrian Period

A

1) Proterozoic (most recent)
2) Archean
3) Hadean

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5
Q

hadean eon started

A

4.5 billion years ago

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6
Q

during the hadean eon

A

Earth & planets formed from dust and gasses surrounding the sun
Electromagnetic forces & Gravity gathers dust into large lumps, called planetisimals
collisions between lumps made lots of heat, made earth molten
Steam atmosphere formed
temperature of earth cooled and first rocks formed

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7
Q

Heavy elements in planets suggest

A

dust/gas from supernova

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8
Q

how do other solar systems form

A

They form in diffuse nebulae

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9
Q

planetisimals

A

Electromagnetic forces & Gravity gathers dust into large lumps

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10
Q

how did the steam atmosphere form from hadean eon

A

from light elements & water vapor from comet

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11
Q

oldest earth rock

A

3.8 billion years old

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12
Q

oldest meteorites and lunar rocks

A

4.5 billion years old

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13
Q

what destroyed all Earth rocks older than 3.8 by

A

erosion and plate tectonics

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14
Q

the Archean eon start and end

A

3.8 (oldest rocks) - 2.5 bya first life

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15
Q

Archean eon

A

Began with formation of solid rock
Volcanoes added heavier gasses to atmosphere (CO2, N2)
Water condensed
oceans formed
First life appeared on Earth (most primitive, most archaic)

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16
Q

Archean atmosphere

A

(CO2, H2O, N2- still in modern atmo)
(CO, H2S, HCl- rare in modern)
no free oxygen or ozone

17
Q

oldest fossil

A

3.5 byo

18
Q

life must have evolved before there was

A

free oxygen because oxygen breaks down macromolecules, and if they couldn’t form, neither could living cells

19
Q

BIFS

A

banded iron formation

20
Q

BIFS time line (start, peak, end)

A

began forming about 3.5 bya = 1st free O2
reached peak about 2.5 bya
deposition ended about 1.8 bya

21
Q

early Archean sediment

A

dark colored, unoxidized, deposited before free oxygen

22
Q

oxidized (rusted) sediment appears in the

A

Proterozoic Eon

23
Q

what was Indirect (non-fossil) evidence for the presence of

Cyanobacteria – 3.5 bya

A

Banded iron formation

24
Q

BIFS created

A

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

25
Q

what likely happened to form BIFS

A

O2 made by cyanobacteria at ocean surface
Toxic O2 removed by iron until iron runs out
Then O2 builds up & kills off most cyanobacteria
O2 levels drop
Unoxidized dark sediments deposited

26
Q

Why are BIFs Banded?

A

When runoff added more Fe to the water the entire process stared over again. Iron has to move back in and cyanobacteria have to grow back

27
Q

Proterozoic eon time

A

2.5-.54 billion years ago

28
Q

what happened in Proterozoic

A

end of BIFS (consistent free oxygen)
Cyanobacteria resistant to oxygen poisoning by 1.8 billion years ago (early proterozoic)
Spontaneous formation of new cells no longer possible (because of free oxygen)
Diversification of bacteria
First Eukaryotes appear ( protists)
Ediacaran fauna appear (soft invertebrates)

29
Q

Phanerozoic eon time

A

.54 bya- present

30
Q

Phanerozoic eon

A

Began with the Cambrian explosion of multicellular animal species and complex land plants