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Geologic Time

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Earth's history on the geologic time ... Eryops is much larger than the frogs and toads of the 20th century. ... Volcanoes are active in the American West. ... – PowerPoint PPT presentation

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Title: Geologic Time


1
Geologic Time
  • P. Lobosco

2
The Geologic Time Scale
  • Earths history on the geologic time scale is
    divided into four geologic eras Precambrian
    Era, Paleozoic Era, Mesozoic Era and Cenozoic
    Era. Eras are broken down into smaller divisions
    called periods. The Earth formed 4.6 billion
    years ago.

3
Precambrian Era
  • The Precambrian Era is the longest era. It
    lasted about 4 billion years or 87 of the
    Earths history. Life exists only in the sea.

4
Life in the Precambrian Era
  • Just beneath the seas surface there bacteria
    clumped together in a tangled mat of threadlike
    fibers. Plants related to modern seaweed are
    also in the seas. They use chemicals from the
    water and energy from the sun to make their own
    food. In the process they produce oxygen. By
    the end of the Precambrian Era, animals such as
    jellyfish, worms, corals and sponges have
    appeared in the seas.

5
Paleozoic Era
  • The Paleozoic Era lasted about 345 million years.
    In the Paleozoic Era, life comes ashore.

6
Life in the Paleozoic Era
  • Life is abundant in the seas, including
    trilobites, brachiopods, and fish. The land is
    no longer lifeless. Forests of ferns and cycads
    grow. Amphibians now appear. Late in the period
    reptiles appear.

7
Trilobite
  • The trilobite is an important index fossil for
    this era since they both evolve and become
    extinct in this era. They have large heads,
    thorny spines and body divisions.

8
Brachiopods
  • Parts of the ocean floor contain lampshade-
    shaped shells. The shells have two parts that
    close to cover and protect the soft animal
    within. These animals are brachiopods.

9
Fish
  • Fish are the first vertebrates, or animals with
    backbones. The Devonian Period is often called
    the Age of the Fishes.

10
Life on Land in the Paleozoic Era
  • Life on land now includes forests of ferns and
    cycads. Amphibians appear. By the end of the
    Paleozoic Era the Amphibians are reduced and new
    animals, reptiles appear on land.

11
Amphibians
  • Amphibians, such as Eryops, are the first land
    vertebrates. They spend their early lives in
    water and move to land. Eryops is much larger
    than the frogs and toads of the 20th century. It
    is 2 meters long with a large head and a thick
    clumsy body. It searches the forest for
    king-sized roaches. It must keep its skin moist
    so it cannot move far from water.

12
Reptiles
  • By the end of the era, amphibians have been
    reduced since there is a drought and the climate
    has cooled. Mountains are rising and all the
    landmasses are joined together. The reptiles
    appear. Their tough skin is protected by scales
    or plates. Unlike amphibians, they do not lose
    water through their skins. Their eggs have thick
    shells so they do not dry out.

13
Mesozoic Era
  • The Mesozoic Era lasted about 160 million years.
    The Mesozoic Era is a period of many changes.
    Pangaea begins to break apart. The expansion
    along the ocean floor causes the continents to
    gradually spread apart. Mountain ranges, such as
    he Sierra Nevadas and the Rockies were formed.
    The Mesozoic is divided into three periods,
    Triassic, Jurassic and Cretaceous.

14
The Triassic Period
  • The drought that began in the Paleozoic Era has
    not ended. It is even hotter. North and South
    America have begun to separate from Africa. A
    narrow sea forms that will become the North
    Atlantic Ocean. Sea creatures that are reptiles,
    have fingerlike projections, and lungs have
    returned to the sea. Mammals appear. The first
    dinosaurs appear.

15
The Jurassic Period
  • The Age of Dinosaurs has begun. Volcanoes are
    active in the American West. The mountains of
    the Sierra Nevada and the Rockies are still
    rising. The southern continents are beginning to
    separate. Conifers make up the forest. The
    first bird, Archaeopteryx, appears.

16
The Cretaceous Period
  • The Cretaceous Period is a time of flooding of
    the continents. The continents continue to move
    apart. By the end of the period the continents
    are almost in their present condition except
    North America and Europe are still joined.
    Dinosaurs rule the world but by the end of the
    period all of the dinosaurs and sea living
    reptiles will have died. Sea levels drop and
    rivers dry up.
  • Flowering plants appear.

17
Cenozoic Era
  • The Cenozoic Era, our present era, has only
    lasted about 65 million years. The Cenozoic Era
    is divided into two periods, the Tertiary Period
    and the Quaternary Period. Great sheets of ice
    will sweep across the land.

18
The Tertiary Period
  • The Uintatherium was one of the largest mammals
    ever. It existed with the ancestor to the
    rhinoceros. The first humanlike creatures begin
    to walk upright on the African Plains. The
    remains of a small adult female from this period,
    about 1 meter tall, is discovered in 1977. She
    is named Lucy.

19
The Quaternary Period
  • The climate turns sharply colder. Four ice ages
    occur. Large parts of Europe, North America and
    South America are covered in sheets of ice. The
    Ice age ends about 11,000 years ago. AS the
    world warms, farming becomes widespread and
    modern civilization begins.

20
Evolution
  • The world evolution comes from Latin and means an
    unfolding or opening out. A scientific
    translation is descent with modification.
    Evolution can be defined as a change in a species
    over time. A species is a group of organisms
    that share similar characteristics and that can
    interbreed with one another to produce fertile
    offspring.

21
Mutations
  • A change in a gene will produce a change in the
    offspring of an organisms. A change in a gene is
    called a mutation. Usually a mutation produces an
    organism that cannot survive. A change that
    increase the chance of survival is called an
    adaptation. The development of a new species can
    result in the extinction of another.

22
The Fossil Record
  • The fossil record indicates that species have
    evolved over time. For example, the discovery of
    the skull of a mammal similar to a whale in 1983
    with a structure for hearing that could not have
    worked underwater led scientists to infer that at
    one point the whale lived on land.

23
Mass Extinction
  • During 1640 and 1859 species began to disappear
    at the rate of one every five years. Between
    1850 and 1900 the rate increased to one lost
    every nine months. At the current rate
    scientists estimate that 1/5 of the species in
    the rainforest will be gone in 50 years.

24
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