a biography of the earth Flashcards

1
Q

geologic time scale

A

Epochs
Smallest time blocks
Periods
Made of many epochs
Eras
Made of many periods
Eons
Made of many eras
Largest time blocks

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2
Q

Precambrian eons: hadean

A

youngest to oldest:
Proterozoic
Archean

Hadean birth-4.0Ga(billion yrs.) oldest
Intense meteorite bombardment
Volcanoes: Outgassing creates secondary atmosphere
N2, NH3, CH4, H2O, CO, CO2, & SO2 (the earth has no primary atmosphere, we’re not big enough)
Liquid water collects into early oceans
no life!

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3
Q

precambrian eons; archean

A

Archean 4.0-2.5 million yrs ago
Cooling Earth
Continental crust creation
Plate tectonics!

Life first appears
~3.5 Ga
Chemical evidence of life (see things that are from biologic processes)
Could be as old as 3.8 Ga
~3.2 Ga
Bacterial cell fossils
Blue-green algae

Stromatolites
Pumps free oxygen into the atmosphere
free oxygen is highly flammable

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4
Q

stomatilites

A

evidence in fossilled layer and current microbial mats

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5
Q

precamrbian eons: proterozoic

A

Proterozoic 2.5-.5 billion years ago
“First Life” (named before Archean life was discovered)
2 billion years
Oxygenated atmosphere
90% continental crust present by middle Proterozoic

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6
Q

Proterozoic oxygen

A

Tertiary Atmosphere
Created by LIFE
Rapid rise of free oxygen
Evidence:
Banded Iron Formations
Major source of iron ore today
Reddish when deposited
Indicates free oxygen atmosphere

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7
Q

proterozoic north america

A

United States
Precambrian rocks are covered by sedimentary rocks of the stable platform
Canadian Shield
Precambrian rocks are visible at the surface
Archean interior
Proterozoic arcs and crustal slivers were added through plate tectonics (convergence)

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8
Q

supercontinents cycle

A

Continents periodically collide
May create a “supercontinent”
Continents eventually rift apart
Heat is trapped under the massive supercontinent
Thins and rifts the interior, initiating divergence
Rodinia (snowball earth time)
~1 Ga - ~700 Ma
Gondawana
~550 Ma – 100 Ma
Pangea
300 Ma – 200 Ma

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9
Q

gondwana

A

Not Gondwanaland
Gondwana means “Land of the Gonds”
“Gonds”
Derived from a tribe in India
see screen shot of tan land on blue ocean

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10
Q

Proterozoic life

A

1.0 Ga
Eukaryotic (nucleated) cells
1.0 Ga – 500 Ma
Biological complexity
Ediacaran fauna
Multicellular invertebrates
(Worm- and jellyfish-like)

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11
Q

Phanerozoic

A

Eras
Cenozoic
Mesozoic
Paleozoic
Most recent 541 Ma of Earth history
Hard-shelled organisms debut
(Much nicer for fossilization)

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12
Q

early Paleozoic era

A

Transgressions
Cambrian-Ordovician
Flooded the low-lying interior of North American

Orogenies
First of several Appalachian orogenies begins in the Ordovician

Cambrian Explosion
Marine life thrived in the warm, shallow oceans of the transgressions
Rapid evolutionary diversification

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13
Q

early paleozoic life

A

Cambrian Explosion
Marine life thrived in the warm, shallow oceans of the transgressions
Rapid evolutionary diversification

Ordovician diversity
First vertebrates
Crinoids
Primitive land plants

mass extinction at the end of ordovician
85% of all species gone
Causes:
Sea level drop (regression) & global cooling
Sea level rise & global warming

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14
Q

middle Paleozoic era

A

Silurian and Devonian
Greenhouse warming
Hot!
Transgressions
Orogenies
Second of several Appalachian orogenies begins in the Devonian

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15
Q

middle paleozoic life

A

Rich marine diversity
First animals to walk on land
Amphibians
Walking on legs, breathing with lungs
Tiktaalik (late Devonian)
Lobe-finned fish fossil
Discovered in 1996
Transitional between fish and amphibians

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16
Q

late paleozoic era

A

Carboniferous & Permian
Carboniferous
Split into two periods in North America
Pennsylvanian (younger)
Mississippian (older)

Cooling after mid-Paleozoic greenhouse
Regressions
Thick coals near tropics
Gondwana moves over South Pole
Covered with ice sheets

17
Q

late paleozoic: mississippian limestones

A

Many of the units making up the Utah County Wasatch Front are deposited during this time

18
Q

Pangea paleozoic

A

Gondwana smashes into Laurentia & Baltica
Orogenies
Third and final of several Appalachian orogenies begins in the Late Paleozoic

19
Q

late paleozoic

A

Coal swamps
Giant insects
Diversity of land animal life
More amphibians
First reptiles
FIRST (amniote) EGG

20
Q

permian-triassic extinction event

A

late paleozoic
“The Great Dying”
Up to 85% of all marine species GONE
Up to 70% of all terrestrial vertebrates GONE

21
Q

permian-triassic extinction event: why?

A

WHY?
Flood basalt volcanic eruptions
Siberian Traps
LIP (large igneous provinces)
2 million years of eruptions
4 million km3 of basalt
HUGE amounts of SO2 & CO2
Elevates global temperatures
Acidifying the oceans
Possible:
Meteorite impact
Thermal decomposition of hydrocarbon deposits

22
Q

permian-triassic extinction event leads to:

A

dinosaurs