Geology Test 3 Flashcards

0
Q

Archean Eon

A

• Greenstone belts
• First evidence of life
• Chemical evidence

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1
Q

Hadean Eon

A

• Differentiation
• Origin of continental crust

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2
Q

Precambrian

A

Earth’s earliest time is referred
• Corresponding to all time prior to the Cambrian period (which contain conspicuous fossils).
• ~90% of geologic time.
• Rocks have fossils….just inconspicuous.
• Less than 20% of rocks at Earth’s surface are of Precambrian age.
Contains Hadean: 4.6-3.8 billion years ago
• Archean: 3.8-2.5 billion years ago
And Proterozoic eons

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3
Q

Hadean eon

A

In the Precambrian era
earliest interval of geologic time:
• Key points?
• Earth acquired it’s basic configuration
(mantle and crust surrounding the core).
• Insignificant amount of continental crust in
existence.
• Very few rocks of Hadean-Eon age exist today.

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4
Q

Archean eon

A

Second level in the Precambrian
second oldest interval of geologic time:
• Key points?
• First time when substantial continental
crust was formed.
• High heat flow from Earth’s interior was much greater than today….so continents remained small because they were constantly rifting apart.

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5
Q

Cratons

A

Precambrian rock:
large stable interior parts of continents that haven’t undergone substantial tectonic deformation in a long time.
• Edges of continents are sites of active orogeny

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6
Q

Precambrian Shield

A

Precambrian rock:
parts of the craton that are of Precambrian age.
• Canadian Shield is largest; exposed by erosion during recent glaciations
• Mostly Ig/Met; some have Sed rocks providing details about paleo-ecosystems.

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7
Q

Hadean Eon

A

• Early Earth was very hot due to:
• Impacts from asteroids and meteorites
• Radioactive decay
• Initial molten Earth was generally a homogeneously-mixed molten mass.

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8
Q

Atmosphere of hadeon eon

A

• Water vapor
• Hydrogen, carbon monoxide, carbon dioxide, nitrogen
• Methane (CH4) and ammonia (NH3)
• Little oxygen gas (O2)

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9
Q

What started first small
continental crust.

A

A much hotter early Earth melted subducted slabs of basalt to form
magma rich in Na (called granitoid; because richer in Na, not in K). Felsic crust formed by partial melting of oceanic lithosphere.
• Partial melting processes creates felsic magmas.
These felsic granitoids formed the nuclei of it
Tho Don’t have actual continental crustal rocks from Hadean.

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10
Q

Greenstone Belts

A

Part of Archean eon
Rock type
broad regions of elongate, stratified bodies consisting of high-grade metamorphic (felsic) rocks
• Have a distinct green color from metamorphic mineral, chlorite
• Formed by squeezing forearc basin sediments, deformed oceanic crust, and arc volcanics between margins of small protocontinents

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11
Q

2 major rock types of Archean eon

A

Greenstone belts

Banded iron formations

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12
Q

Banded Iron Formations (BIF)

A

• Typical of Archean sedimentary rocks
• Composed of alternations of iron-oxide-rich layers interbedded with chert layers:
• Chert + Fe-rich: precipitated from sea water
• Silica was more concentrated in ocean because this is before diatoms.
• Bacteria may have aided in precipitation of Fe
• The precipitation of iron does not occur in the oceans today.

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13
Q

Life first appeared on Earth sometime after…

A

4.5 Ga

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14
Q

Evidence for Archean Life:

Stromatolites

A

Still created today in association with Cyanobacteria (prokaryotic).
• Earliest known fossil life.

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15
Q

Evidence for Archean Life:

Biomarkers

A

Photosynthesis at 3.7 Ga
• Small carbon particles in deep-water black shales and turbidites
• Carbon is so isotopically light (C12), researchers believe it must be from photosynthesis by an unknown primitive life form (~3.7Ga).

16
Q

Evidence for Archean Life:

oldest fossilized organism

A

prokaryotic life form found in Archean rock (~ 3.5 Ga).
• Intertwined filaments on pillow lavas
• Similar prokaryotes found today associated with pillow basalts

17
Q

Evidence for Archean Life:

Steranes

A

compounds produced by eukaryotes
• Discovered in Archean rocks 2.7 Ga BP
• Suggests eukaryotes were present by end of Archean

18
Q

Basis of life

Building blocks of proteins are amino acids. • Amino acids (20) made of:

A

Carbon
• Hydrogen • Oxygen
• Nitrogen

19
Q

Life on Earth likely originated at:

A

MOR
No oxidation problem.
• Archean life originated in a warm environment isolated from Earth’s atmospherewarm area adjacent to MOR likely.
• Super-heated water circulating, rising as large vents.
• Known to inhabit these areas today.

20
Q

Today (and probably in the past) these organisms perform:

A

chemosynthesis.
= harness energy of naturally occurring chemical reactions
They consume the chemical compounds and employ enzymes to speed up the chemical reaction, which release the energy that organisms use for their metabolism.

21
Q

Hadean overview

A

Earth differentiated
• Moon formed.
• Partial melting of subducted lithosphere when deep Earth was
much hotter lead to development of continental crust.
• High heat rates meant high tectonic plate movements, preventing the formation of large continents.

22
Q

Archean overview

A

Greenstone belts and BIF
• Larger continents formed as heat dropped within Earth.
• Appearance of life (likely at MOR)
• Oxygen proliferation

23
Q

The fossil record is the basis for the division of the Proterozoic Eon into 3 eras:

A
  1. Neoproterozoic: 1 - 0.54 billion years ago
  2. Mesoproterozoic: 1.6 – 1 billion years ago 1. Paleoproterozoic: 2.5 – 1.6 billion years ago
24
Q

Orogen

A

eroded, deformed remains of what was a mountain (orogenic event).
• Consists of deformed rocks, since leveled by erosion.
• Distinct features (W-E):
Igneous Intrusion Metamorphic belt Fold and thrust belt Undeformed zone

25
Q

Formation of larger cratons began in the late Archean
• Proterozoic: what formed now??

A

cratons start exhibiting modern-style orogeny • Found in
Canada.

26
Q

Mitochondrion

A

Site of respiration (energy from food)
• Animal-like protists

27
Q

Chloroplast

A

Site of photosynthesis
• Animal-like protists – consumed and
retained the cyanobacteria – became
a chloroplast
• First plant-like protists (producer)
evolved from an animal-like protist
(consumer)
• From these two protists: multicellular
animals and plants evolved.