Geologic Time Scale
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Transcript Geologic Time Scale
Journal #4 – Geologic Time
1. What types of information is included on
the geologic time scale?
2. What is the difference between an Era and
an Epoch?
3. According to the geologic time scale, how
has life on Earth changed since the
beginning of time?
Objective: Understanding the events of
Earth’s past and how they are organized
into a chart.
Geologic Time
Organic Evolution
The change in life-forms through time
Species
A group of organisms that normally
reproduce only with themselves
Species
2 Different Species Breed
Offspring unable to reproduce
Adaptation
Adaptation
The ability to change to survive
Ex. Light colored peppered moths
camouflaged on light tree bark; pollution
causes them to change to darker colors to
survive
Ex. Galapagos finches and their beaks
Natural Selection
Natural Selection
Organisms with traits that are suited to a
certain environment have a better chance
of surviving and reproducing
1836 by Charles Darwin
Evolution
Main Causes of Evolution
Changes to the environment
Caused by plate tectonics
Competition with others for resources
Endangered vs. Extinct
Endangered
When only a small number of members
are living
Extinct
When none of its members are living
Extinction
Human Contribution to Extinction
Destruction of habitats
Competition for same food supply
Overhunting
Geologic Time
Geologic Time Scale
A record of Earth’s history that shows
events of life, earth processes, time units
and ages
Divided into smaller units based on
Types of life-forms living at that time
Geologic events occurring at that time
Geologic Time
Eras
• Largest
• Based on lifeforms and fossil
evidence
Periods
• Divide Eras
• Based on lifeforms and
geologic events
Epochs
• Smallest
• Divide Periods
Geologic Time
Precambrian
Longest geologic time unit in Earth’s
history
Began: 4600 million years ago (4.6 billion
years)
Ended: 540 million years ago
Precambrian
Precambrian Fossils
Limited
Rocks deeply buried or eroded
Rocks have been changed by heat and pressure
Early organisms were soft-bodied
Early organisms were small and single-celled
Cyanobacteria
Cyanobacteria
Bacteria and algae combine and
photosynthesize to form stromatolites
Appeared: 3.5 billion years ago
Take in CO2, Release O2
Cyanobacteria
Cyanobacteria
Importance: changed Earth’s atmosphere
by adding free oxygen to the air
Formed the ozone layer protecting organisms
from UV light
Single-celled organisms evolved into
complex organisms
Invertebrate
Invertebrate
Animal without a backbone
Appeared: end of the Precambrian
Ex. Jellyfish, sponges, worms
Paleozoic Era
Paleozoic Era
“Ancient Life”
Beginning marked by the development of
hard parts
Began: 540 million years ago
Ended: 245 million years ago
Paleozoic Era
Paleozoic Era
Abundant Life: ocean dwelling marine
organisms
Caused by warm, shallow seas covering most
of earth
Appeared: Cambrian Period
Ex. Trilobites, brachiopods, cephalopods,
crinoids
Paleozoic Era Animals
Vertebrate
Animals with a backbone
Appeared: Ordovician Period
Ex. Jawless fish, bony fishes, reptiles,
mammals
Paleozoic Era Animals
Amphibian
Vertebrates that live on land by must
return to water to reproduce (lay eggs)
Appeared: Devonian Period
Ex. Frogs, salamanders
Paleozoic Era Animals
Reptiles
Vertebrates that live entirely on land; eggs
have leathery or mineralized covering
Appeared: Late Carboniferous
(Pennsylvanian Period)
Ex. Tortoises, snakes, lizards, crocodiles
Paleozoic Era Plants
Ferns, Palms, Ginkgos, Pines
Appeared: Devonian Period
Paleozoic Era Plants
Gymnosperms
“naked seed plant”; no fruit covering their
seeds
Appeared: Carboniferous Period
Ex. Eastern White Pine
Paleozoic Era
Appalachian Mountains
Formed at the end of the Paleozoic
What marked the end of the Paleozoic?
Largest mass extinction in Earth’s history
Formation of Pangaea
Mesozoic Era
Mesozoic Era
“Middle Life”
“Age of the Dinosaurs”
Began: 245 million years ago
Ended: 66 million years ago
Mesozoic Era
Pangaea
All Continents
Laurasia
North America,
Europe, Asia,
Greenland
Gondwanaland
South America,
Africa, Antarctica,
India, Australia
Mesozoic Era Animals
Small Dinosaurs
Appeared: Triassic Period
Evidence of being Warm-Blooded
Tracks (trace fossils) indicate fast motion
Traveled in herds and nurtured young
Bone structure resembles other warm-blooded
animals
Mesozoic Era Animals
Mammals
Appeared: Triassic Period
Traits Allowing Survival
Hair or Fur
Warm Blooded
Produce Milk to Feed Young
Mesozoic Era Animals
Birds
Appeared: Jurassic Period
Ex. Archaeopteryx had wings and feathers like
a bird, teeth, claws and tail like a dinosaur
Mesozoic Era Plants
Angiosperms
Flowering plants
Produce seeds with a hard outer covering
and/or fruit
Appeared: Early Cretaceous Period
Ex. Fruits, vegetables, flowers, flowering
trees
Mesozoic Era
What marked the end of the Mesozoic Era?
Break up of Pangaea
Seas drained from lands
Extensive volcanism
Extinction of the dinosaurs
Cenozoic Era
Cenozoic Era
“Recent Life”
Age of the Mammals
Begin: 66 million years ago
Current Time
Cenozoic Era
Alps in Europe
Form from the collision between African
and Eurasian Plates
Cenozoic Era
The Himalaya Mountains
Formed from the collision between the
Indian and Eurasian Plates
Cenozoic Era Animals
Placental Mammals
Nourish their young internally from a
placenta
Offspring born live and independent
First Appeared: Cretaceous Period
Ex. Rodents, bats, dogs, cats, cows,
humans
Cenozoic Era Animals
Marsupials
Offspring are born immature
Must complete development in a pouch
First Appeared: Cretaceous Period
Ex. Kangaroo, koala, wombat, opossum
Australia has the greats population of
marsupials
Cenozoic Era Animals
Monotremes
Egg-laying mammals
Ex. Platypus
Homo Sapiens
Homo Sapiens
500,000 years ago
Homo Sapiens
Homo Sapiens
Neanderthalensis
Sapiens
250,000 years ago
100,000 years ago
Humans
Humans
Dominant life form for the past 10,000
years
Started agriculture, domestication of animals,
cities, writing