A View of Earth`s Past
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Transcript A View of Earth`s Past
A view of Earth’s Past
Objectives:
Summarize how evolution is related to geologic
change.
Interpret a geologic time scale.
Arizona State Standard:
Strand 6: Concept 3:
P04: Interpret a geologic time scale
P06: Investigate theories of how life originated on Earth.
P07: Describe how life on Earth has influenced the
evolution of Earth’s system.
P08: Sequence major events in Earth’s evolution.
Geologic Time
PO 8: Sequence major events in the
Earth’s evolution using relative and
absolute data (e.g., mass extinctions,
ice ages).
PO 4: Interpret a geologic time scale
The geologic Column
A time line of
Earth’s history
Ordered rock
layers based on
relative age
Distinguishable by
type of rock and
fossils.
Think back, what
is relative age?
Relative age is the
age of an object in
relation to the ages
of other objects
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Why did many
scientist have to
work together to
develop the
geologic column?
Explain why
constructing
geologic columns
is useful to Earth
scientist.
Scientist worked together because different
rocks occur in different parts of the world.
A geologic column is useful because it
shows the relative ages of rocks and fossils
How can scientist use the
geologic column to determine
the absolute age of earth’s
major events?
Ice ages
Mass extinctions
Organisms explosions
o Ice cores
trap gasses
that tell about
past climates
and changes
in the
environment.
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o Radiometric
dating can be
used to
determine the
absolute age
of fossils and
the
surrounding
rock
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Divisions of Geologic Time
Marked by major changes in Earth’s
surface, climate, and type of organisms.
Divided into smaller units characterized
by type of fossil.
Units of Geologic Time
Eons: Largest Unit of geologic time.
Most are in Pre-Cambrian time.
Eras: Divided into smaller Units.
Paleozoic
Mesozoic
Cenozoic
Periods: Eras are divided into smaller units of time
characterized by fossil type.
There are 11 periods.
Epochs: Divided into smaller units called ages
Precambrian time & The Paleozoic Era.
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Precambrian Time
Began with the formation of Earth
Makes up 88% of Earth’s History
Difficult to interpret due to
deformation caused by tectonic
activity.
Fossils are rare
No hard parts to preserve.
Stromatolites formed by blue green
algae.
Form in warm, shallow waters.
The Paleozoic Era
Includes:
Cambrian Period:
First Vertebrates
Ordovician Period:
Oxygen rich atmosphere
Silurian Period:
First Land Plants
Devonian Period:
First amphibians appear
Carboniferous Period:
First Reptiles
Permian:
Pangea is complete
Mass Extinction from environmental
changes.
The Mesozoic Era: Age Of Reptiles
Triassic Period:
Pangea begins to break
apart, and first mammals
begin to appear.
Jurassic Period:
First primitive birds.
Cretaceous Period:
First Flowering Plants
The last dinosaurs
become extinct.
Meteorite Impact: Impact
hypothesis.
The Cenozoic Era:
Age of Mammals
Tertiary Period: Modern Mammals
Quaternary Period: First Hominids
The Cenozoic Era:
Age of Mammals
Tertiary Period: Modern Mammals
Whales
Carnivores
Hoofed Animals
Primates
First grasses appear
India collides with Asia.
Antarctica drifts over the south pole.
Quaternary Period: First Hominids
Modern ice age begins
Modern Humans appear
Evolution
P06: Investigate theories of how life
originated on Earth.
PO7:Describe how life on Earth has
influenced the evolution
of Earth’s systems
The gradual development of new
organisms from preexisting organisms.
Evolution occurs from natural selection
Models of evolution include:
High Temperature
Low Oxygen
Clay Catalyst
High Temperature
Earth’s surface temperature was extremely
hot and the atmosphere was noxious.
The air contained CH, NH, and H
Outgassing from the molten rock produced
an enormous amount of water vapor.
Eventually forming a cloud layer that covered
the entire planet.
Violent storms fueled with lightening sparking
followed
Earth’s ancient atmosphere, combined
with the intense electrical storms, was
essential for the production of the
molecules that cells need to survive.
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Low Oxygen
First unicellular life appears in the
Precambrian time when oxygen was not
present in the atmosphere.
Organisms that thrived in this
atmosphere were anaerobic--does not
require free oxygen.
Clay Catalyst
Clay served as a storage for amino
acids to join together.
Water is absorbed between platelets in
clay.
Clay dries with proteins inside, then
when moist again the proteins will
return.
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How has life on Earth
influenced the evolution of
Earth’s systems?
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