Proterozoic (midterm 2) Flashcards

1
Q

What time frame was the Proterozoic Eon?

A

2.5 Ga - 542 Ma

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2
Q

What are some characteristics of the rocks/fossils in the Proterozoic Eon?

A
  • many Proterozoic rocks are exposed and not metamorphosed
  • proterozoic fossils are uncommon
  • fewer greenstone belts and granite-gneiss complexes
  • passive continental margins
  • many banded iron formations
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3
Q

List some differences between Archean and Proterozoic plate tectonics

A

Archean:
- “Archean-style” tectonics - unstable
- metamorphosed and complexly deformed rocks
- fast crustal movement
- rare sedimentary rocks (minor component in GSB and GGC) - most rocks are igneous
- high rate of volcanism

Proterozoic:
- “modern-style” plate tectonics - stable permanent crust
- many undeformed and unmetamorphosed rock successions
- slower crustal movement
- widespread sedimentary assemblages
- lower rate of volcanism

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4
Q

What are some characteristics of plate tectonics specific to Proterozoic time?

A
  • commonly separated from Archean rocks by an unconformity
  • abundant stromatolites
  • quartzite-carbonate-shale assemblages
  • fluvial sands, continental red beds
  • deep marine sediments
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5
Q

What is Laurentia? What areas does it make up?

A

Early continent that makes up the core of North America
- also makes up parts of Greenland, Scotland, and possibly Baltic Shield and Scandinavia
- lots of exposures in North America

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6
Q

What is basement rock?

A

Crystalline (igneous and metamorphic) rocks that lie beneath sedimentary rocks, mostly all Archean and Proterozoic

Underneath all the younger sedimentary rocks on top

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7
Q

What is an orogen?

A

A part of Earth’s crust that was or is being deformed during an orogeny (mountain building event) > can form belts

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8
Q

When/where did the growth of Laurentia begin?

A

2-1.8 billion years ago

(in the Paleoproterozoic era - 2.5-1.6 Ga)

Most of it started from the Wopmay orogen
(Archean cratons coming together at orogens - grows along its southern and eastern margins)

*beginning of the north american continent

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9
Q

List the steps of the Wilson Cycle

A
  1. Uplift
  2. Divergence (spreading - creates an ocean basin)
  3. Passive continental margin (no significant plate bounday/tectonics)
  4. Convergence (subduction)
  5. Convergence (collision) and uplift
  6. Convergence and uplift
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10
Q

What is the Wilson Cycle?

A

A model that describes the opening and closing of ocean basins and the subduction and divergence of tectonic plates during the assembly and disassembly of supercontinents

*check textbook definition about this perhaps

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11
Q

Which parts of Laurentia showed up 1.8-1.6 billion years ago (in the Paleoproterozoic)

A

Yavapai province
Mazatzal province

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11
Q

Which parts of Laurentia showed up 1.3-1 billion years ago (in the Mesoproterozoic)

A

Grenville province
Granite-Rhyolite province
Llano province

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12
Q

What is the significance of the rocks of the Grenville orogeny? (when did they occur, where are they exposed, what did they maybe result in?)

A

Grenville Orogeny occurred on the eastern boundary of Laurentia from 1-1.3 Ga

Grenville rocks (metamorphic) exposed in the modern northern Appalachian Mountains, eastern Canada, Greenland, and Scandinavia

Grenville belt may have resulted in the closure of an ocean basin (end of a Wilson cycle) that assembed the supercontinent Rodinia, which persisted into the Neoproterozoic

At the end of the Grenville Orogeny?? - about 75% of present-day North America existed

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13
Q

In the Wilson cycle, there is a change from _______-_______ compact to _______-______ compact

A

continent-ocean

continent-continent

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14
Q

What timeframe does the Rodinia supercontinent span?

A

1 Ga - 542 Ma

middle to end of Proterozoic eon
(actually broke up around 750 Ma)

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15
Q

What are continents?

A
  • formed by cratons
  • has a shield and platform
  • not just land above sea level, edges can be submerged
  • granitic crust, thicker than ocean crust
16
Q

What are supercontinents?

A

Two or more continents that have joined
- all or most of Earth’s land mass > except oceanic islands
ex. Pangea (300-200 Ma)
- older supercontinents existed

17
Q

Modern-style plate tectonics were occurring by the ___________

A

Paleoproterozoic

18
Q

What are Ophiolites? What is the ideal ophiolite sequence?

A

Ophiolites are one feature used to recognize ancient convergent plate boundaries (Neoarchean & Paleoproterozoic)
> during subduction, pieces of oceanic lithosphere accrete onto the edge of the continent

Ideal Sequence:
- deep-sea sediments (sandstone, black shale, chert)
- oceanic crust (pillow lava and sheet lava, sheeted dikes, massive gabbro, layered gabbro)
- upper mantle peridotite

19
Q

What is one of the oldest known complete ophiolites?

A

The Jormua Mafic-Ultramfic Complex Finland
1.96 Ga

20
Q

What are the Proterozoic Supercontinents?
What are the two POSSIBLE Archean supercontinents?

A

Nuna 1.8 Ga (Paleoproterozoic)
Rodinia 1.3-1 Ga (Mesoproterozoic)

Possible Archean Supercontinents:
Vaalbara 3.1 Ga
Kenorland 2.7 Ga
- would’ve been small; accretion and underplating just beginning

21
Q

What is the supercontinent cycle?

A

Assembly, fragmentation, reassembly

22
Q

Explain the Supercontinent Rodinia and what happened to it

A

Rodinia is the oldest documented supercontinent
- assembled 1-1.3 Ga and began fragmenting about 750 Ma
- continental rifting (divergent plate boundary)

Separate pieces of Rodinia reassembled into the supercontinent Pannotia about 650 Ma > Pannotia fragmented about 550 Ma

23
Q

What is the most recent glaciation event in Earth’s history

When were there glaciation events before this?

A

Pleistocene (ice age) spanning from 2.6 Ma - 11,700 years ago
(repeated glacial periods - ice sheets covered a large part of North America 5 different times during this period)

Paleozoic glaciers (after proterozoic)
Proterozoic glaciation

*overall very few widespread glaciation events in Earth’s history

24
Q

What is the evidence for glaciation events?

A
  • Tillite
  • Varves
  • Striated, polished bedrock
  • extensive geographic distribution
25
Q

Describe the Neoproterozoic glaciers - what theory did this lead to?

A

Neoproterozoic (final era of the proterozoic eon) glaciers : 900-600 mya

  • on all continents except Antarctica > Tillites and varved mudstones
  • episodic, not continuous
  • most extensive in Earth’s history

*if there were widespread glacial deposits everywhere did glaciers cover all the land? were seas frozen? snowball earth?

26
Q

What would some of the triggers be of a snowball earth?

A
  • the near equatorial location of most continents
  • high rates of weathering > consumed CO2 in atmosphere leads to glaciers
  • glaciers reflect solar radiation > leads to more glaciers

*look over diagram/steps in pictures

27
Q

How would the snowball earth have ended?

A
  • volcanoes adding CH4 & CO2 to atmosphere > warms atmosphere (greenhouse gas effect)
  • movement of continents to higher latitudes > slowed weathering rates
28
Q

What are theories for how life would’ve survived through a snowball earth?

A
  • it was thin glacial ice?
  • hydrothermal vents?
  • slushy with some open water?

*the retreat of glaciers was one of the causes of the explosion of life that followed

29
Q

Explain the general forms of life that existed during the Proterozoic

A
  • abundant bacteria and archaea
  • cyanobacteria become more abundant (widespread stromatolites)
  • appearance of eukaryotes > sexual reproduction speeds up evolution
30
Q

What are the subgroups of prokaryotic and eukaryotic cells

A

Prokaryotic:
- Monera
- Archaea

Eukaryotic:
- Protista
- Fungi
- Plantae
- Animalia

31
Q

What is Symbiosis and Endosymbiosis? When is this thought to have happened?

A

1.5 Ga (but there is no fossil evidence for this)

Symbiosis: Relationship between 2+ organisms where both benefit, sometimes to the point where they cannot live separately

Endosymbiosis: One symbiont lives within another

32
Q

What is the oldest known eukaryote?

A

The Bangiomorpha
- sexually reproducing red algae
- Somerset Island, Canada

1.2 Ga

33
Q

What are multi-celled organisms and their advantages? When are they thought to have started existing?

A

Organisms that have cells performing specialized tasks (ex. reproduction and respiration)

Advantages: Larger size, efficiency, longer life

They existed in Neoproterozoic, likely earlier
- no fossil record for how they came to exist
- colonial organisms likely intermediate step

34
Q

What were the Edicaran Fauna?

A

Edicaran Fauna is the name that we give collectively to fossils of this type found in this time period (635-545 Ma)

The first animals
- soft bodied
- widespread (found in every continent except antarctica), but fossils not common

First evidence in the fossil record of hard parts being found - no skeletons yet but they had Chitinous carapace (similar to insect exoskeleton)
- some have spots/small areas of calcium-carbonate (CaCO3, limestone)
- environment = form in shallow seas
- first evidence of simple ecological interactions (This evidence is why we see a shift between this time period and the next - start seeing organisms with these types of skeletons)

35
Q

The Ediacaran Environment is thought to represent what 3 modern groups?

A

Phylum Cnidaria
- jellyfish and sea pens

Phylum Annelida
- Segmented worms

Phylum Arthropoda
- primitive versions of insects, spiders, crabs and others
- very limited hard parts

36
Q

In the Proterozoic context, what are dikes?

A

Sheet-like intrusions of magma that cut through existing rock layers

37
Q

What is the basic difference between prokaryotes and eurkaryotes?

A

Prokaryotes: single celled, fairly simple, reproduce asexually

Eukaryotes: a bunch of other internal structures, reproduce sexually, increases evolution because of genetic variation