Earth - PowerPoint PPT Presentation

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Earth

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Earth s History – PowerPoint PPT presentation

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Title: Earth


1
Earths History
2
Origin of the Earth
  • Nebular Hypothesis
  • Bodies of our solar system condensed from an
    enormous cloud
  • Cloud began contracting, spinning, and flattening
  • Earth
  • Density sorted material and eventually, gases
    escaped from the interior to form an atmosphere

3
Earths Atmosphere Evolves
  • Outgassing
  • Gases that are in molten rock are gradually
    released
  • Water vapor condensed to form clouds
  • Rain cooled Earths crust until the rains slowly
    filled low areas, forming the oceans
  • Reduced CO2 because it became trapped in water
  • Plants evolved and released oxygen

4
Precambrian Time
  • 4.6 billion to 570 million years ago
  • Precambrian Rocks
  • Shields
  • Areas shaped like shields that have been
    extensively eroded to reveal Precambrian rock
  • Mostly deformed metamorphic rock
  • Ore deposits

5
Precambrian Time
  • Precambrian Fossils
  • Stromatolites
  • Calcium carbonate deposited by algae
  • Indirect evidence of algae
  • Tiny organisms
  • Life 3.5 billion years ago
  • Most preserved in chert, a hard, dense chemical
    sedimentary rock
  • Prokaryotes found (blue-green algae bacteria)
  • Southern Africa3.1 billion years
  • Lake Superior1.7 billion years

6
Precambrian Time
  • Eukaryotes found (green algae)
  • Bitter Springs, Australia1 billion years
  • Plant fossils date from the middle Precambrian
  • Trace fossils of animals
  • Trails and worm holes
  • Fossil impressions
  • Animal fossils date from the late Precambrian
  • Diverse and multicelled organisms exist by the
    close of the Precambrian

7
Paleozoic EraLife Explodes
  • 570-245 million years ago
  • Hard parts appeared on organisms
  • Early Paleozoic History
  • Mountain building affected eastern North
    Americalong since eroded

8
Paleozoic EraLife Explodes
  • Early Paleozoic Life Age of Invertebrates
  • Restricted to seas
  • Cambrian
  • Trilobites
  • Mud-burrowing scavengers
  • More than 600 genera
  • Ordovicianshallow seas
  • Organisms with hard parts
  • Brachiopods
  • Adults attached to the sea floor, larvae
    free-swimming
  • Cephalopods
  • Mobile, highly developed mollusks predators

9
Paleozoic EraLife Explodes
  • Late Paleozoic History
  • Devonian, Mississippian, Pennsylvanian, and
    Permian periods
  • Pangaea
  • Extreme seasons that caused one of the most
    dramatic biological declines in history

10
Paleozoic EraLife Explodes
  • Late Paleozoic Life
  • Land plants developed
  • Fishes continued to adapt
  • Devonian period Age of Fishes
  • Lobe-finned fish evolved into amphibians
  • Insects
  • Extensive coal swamps develop

11
Paleozoic Extinction
  • Climates changed because of the formation of
    Pangaea
  • 75 of amphibians disappeared
  • Up to 95 of marine life disappeared
  • 1 of 5 mass extinctions
  • Cause is uncertain

12
Mesozoic EraAge of the Dinosaurs
  • 245 to 66 million years ago
  • Mesozoic History
  • Much of worlds land above sea level
  • Breakup of Pangaea
  • Mountains of western North America begin forming

13
Mesozoic EraAge of the Dinosaurs
  • Mesozoic Life
  • Survivors of the great Paleozoic extinction
  • Gymnosperms became dominant
  • Reptiles adapt to dry climate
  • Reptiles have shell-covered eggs that can be laid
    on the land
  • One group of reptiles led to the birds
  • Many reptile groups and other animal groups
    became extinct at the close of the Mesozoic

14
Cenozoic EraAge of Mammals
  • 66 million years ago to present
  • North America
  • Most was above sea level
  • Mountain building, volcanism, and earthquakes in
    the West
  • In the East stable with abundant marine
    sedimentation eroded Appalachians were raised by
    isostatic adjustments

15
Cenozoic EraAge of Mammals
  • Western North America
  • Rivers erode and form gorges (Grand Canyon)
  • Volcanic activity common
  • Coast ranges form
  • Sierra Nevada become fault-block mountains

16
Cenozoic EraAge of Mammals
  • Cenozoic life
  • Mammals replace reptiles as dominant land animals
  • Angiosperms dominate the plant world
  • Mammals evolve after the reptilian extinctions of
    the Mesozoic
  • Marsupials
  • Placentals

17
Cenozoic EraAge of Mammals
  • Mammals diversify rapidly and some groups become
    very large
  • Hornless rhinocerosnearly 16 feet high
  • Many large animals became extinct
  • Humans evolve
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