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The Geological Time Scale

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The Geological Time Scale 8-2.4 Recognize the relationship among the units era, epoch, and period into which the geologic time scale is divided. – PowerPoint PPT presentation

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Title: The Geological Time Scale


1
The Geological Time Scale
8-2.4 Recognize the relationship among the
unitsera, epoch, and periodinto which the
geologic time scale is divided. 8-2.5 Illustrate
the vast diversity of life that has been present
on Earth over time by using the geologic time
scale. 8-2.2 Summarize how scientists study
Earths past environment and diverse life-forms
by examining different types of fossils
(including molds, casts, petrified fossils,
preserved and carbonized remains of plants and
animals, and trace fossils). 8-2.3 Explain how
Earths history has been influenced by
catastrophes (including the impact of an asteroid
or comet, climatic changes, and volcanic
activity) that have affected the conditions on
Earth and the diversity of its life-forms.
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What is the Earths time scale?
  • The Geological time scale is a record of the life
    forms and geological events in Earths history.
  • Scientists developed the time scale by studying
    rock layers and fossils world wide.
  • Radioactive dating helped determine the absolute
    divisions in the time scale.

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Divisions of Geologic Time
  • Eras are subdivided into periods...periods are
    subdivided into epochs.

Era
Period
Epoch
E P EP
8
Divisions of Geologic Time
  • Geological time begins with Precambrian Time.
    Precambrian time covers approximately 88 of
    Earths history.

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FOUR Eras
  • PRE-CAMBRIAN 88 of earths history
  • Paleozoic (ancient life)
  • 544 million years agolasted 300 million yrs
  • Mesozoic (middle life)
  • 245 million years agolasted 180 million yrs
  • Cenozoic (recent life)
  • 65 million years agocontinues through present day

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Today
  • Today we are in the Holocene Epoch of the
    Quaternary Period of the Cenozoic Era.

Which unit is the largest? Which unit is the
smallest?
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Paleozoic Era (Ancient Life)
  • The Cambrian period is the 1st period of the
    Paleozoic Era. Age of the Trilobites
  • Explosion of life in the oceans began during this
    era.
  • Most of the continents were covered in warm,
    shallow seas.
  • Invertebrates were dominate - Trilobites
  • Fish emerged during this time
  • Fish led to the arrival of amphibians
  • The end of the Paleozoic era is called the Age
    of Amphibians
  • Early land plants including mosses, ferns and
    cone-bearing plants.
  • The early coal forming forests were also formed
    during this time.

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Paleozoic Era
  • Much of the limestone quarried for building and
    industrial purposes, as well as the coal deposits
    of western Europe and the eastern United States,
    were formed during the Paleozoic.
  • The Cambrian (beginning) opened with the breakup
    of the world-continent Rodinia and closed with
    the formation of Pangaea, as the Earth's
    continents came together once again.
  • This event is thought to have caused the climate
    changes that led to mass extinction event.
  • The Appalachian mountains were formed during this
    time.

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Paleozoic Era
  • At the end of the Paleozoic, the largest mass
    extinction in history wiped out approximately 90
    of all marine animal species and 70 of land
    animals.
  • Possible causes of this Mass Extinction Event
  • Lowering of sea levels when the continents were
    rejoined as Pangaea (convergent boundary)
  • Increased volcanic activity (ash and dust)
  • Climate changes cooler climate

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Trilobites
  • Lived in Earths ancient seas
  • Extinct before the dinosaurs came into existence
  • Cambrian Period is know as the Age of the
    Trilobites (put in on table)

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Brachiopods
  • Marine animals that resemble clams.

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Early Fish
Early fish did not have jaws. Some species of
sharks were in existence at this time.
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Fields Frilled Shark that was found in Japan in
January 2007. This shark was considered a
living fossil
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Frilled Shark that was found in Japan in January
2007. This shark was considered a living fossil
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Early Land Plants
Mosses
Cone bearing plants
Ferns
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Mesozoic Era Middle Life
  • At the beginning of this era the continents were
    joined as Pangaea.
  • Pangaea broke up around the middle of this era.
  • Reptiles became the most abundant animals because
    of their ability to adapt to the drier climate of
    the Mesozoic Era.
  • Skin maintains body fluids
  • Embryos live in shells

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Mesozoic Era
  • Dinosaurs were also very active in this era.
  • First small dinosaurs appeared in the Triassic
    Period.
  • Larger and more abundant dinosaurs appeared in
    the Jurassic Period.
  • Small mammals and birds also appeared during this
    era.
  • The mammals were small, warm-blooded animals.
    Hair covering their bodies.
  • These characteristics help them survive in
    changing environments.

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Mesozoic Era
  • The main plant life of this time were Gymnosperms
    or plants that produce seeds, but no flowers.
  • Pine Trees
  • Flowering plants appeared during the END of this
    era.

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Mesozoic Era
  • This era ended with a mass extinction event about
    65 million years ago.
  • Many groups of animals, including the dinosaurs
    disappeared suddenly at this time.
  • Many scientists believe that this event was
    caused by a comet or asteroid colliding with the
    Earth.

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Crater sites on Earth
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Mesozoic Era Mass Extinction Event
  • Asteroid or Comet collides with Earth.
  • Huge cloud of smoke and dust fills the air
  • Blocks out sunlight
  • Plants die
  • Animals that eat plants die
  • Animals that eat plant-eaters die.
  • However, not all forms of life died during this
    event. Many animals that you see today are
    descendants from the survivors of this extinction
    event.

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Dinosaurs
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Mesozoic Reptiles
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Mesozoic Mammals
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Mesozoic Plants
Flowering plants evolved towards the end of the
Mesozoic Era.
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Cenozoic Era Recent Life
  • Began about 65 million years ago and continues
    today!!!!!
  • Climate was warm and mild.
  • Marine animals such as whales and dolphins
    evolved.
  • Mammals began to increase and evolve adaptations
    that allowed them to live in many different
    environments land, air and the sea.
  • Grasses increased and provided a food source for
    grazing animals
  • Many mountain ranges formed during the Cenozoic
    Era
  • Alps in Europe and Himalayas in India Rocky
    Mountains in the USA

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Cenozoic Era
  • Growth of these mountains may have helped to cool
    down the climate
  • Ice Ages occurred late in the Cenozoic Era
    (Quaternary Period).
  • As the climate changed, the animals had to adapt
    to the rise and fall of the oceans caused by
    melting glaciers.
  • This era is sometimes called the Age of Mammals

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Cenozoic Era
  • Marine animal examples
  • Algae, Mollusks, Fish and Mammals
  • Land animal examples
  • Bats, Cats, Dogs, Cattle and Humans
  • Humans are thought to have appeared around 3.5
    million years ago (during the most recent period
    Quaternary).
  • Flowering plants were now the most common plant
    life.

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Cenozoic Mammals
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Flowering Plants were common during the Cenozoic
Era
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