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Origins

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The Nature Of Science

  • What Is Oceanography?
    • The process of discovering unifying principles in data obtained from the ocean, its associated life forms, and the bordering lands.
    • Science is a systematic process of asking questions about the observable world and then testing the answers to those questions.
  • The Scientific Method
The Nature Of Science | Origins & The Formation Of The Universe | Links | top

Origins & The Formation Of The Universe

  • The Big Bang Theory
  • Galaxies and Stars
    • Galaxy - a huge rotating aggregation of stars, dust, gas and other debris held together by gravity.
    • We live in the Milky Way Galaxy
      • Stars - massive spheres of incandescent gasses.
      • Solar System - The sun together with the planets and other bodies that revolve around it.
      • Solar Nebulas - The diffuse cloud of dust and gas from which the solar system originated
        • Protosun - Tightly condensed knot of material that has not yet attained fusion temperature
        • Planets - A smaller, usually nonluminous body orbiting a star.
        • New planets form from accretion - An increase in the mass of a body by accumulation or clumping of smaller particles.
  • The Earth and the Ocean
    • Formation of the Earth
      • The Earth formed by the accretion of cold particles.
      • The surface was then heated due to meteor impacts
      • This caused the Earth to partially melt & density stratification.
        • Gravity pulled most of the iron to the core
        • Lighter minerals rose towards the surface
      • First surface on the Earth formed ~4.6 billion years ago.
      • A collision with a rocky body about the size of Mars smashed into the Earth
        • Rocky mantle of the object formed a debris ring around the Earth
        • The metallic core merged with the Earth's
        • Radiation from the Sun stripped the outermost layer of gasses (1st atmosphere) from the Earth
      • Gasses trapped within the Earth were released and formed a 2nd atmosphere
      • The volcanic venting of volatile substances (outgassing) condensed into clouds in the cool upper atmosphere
    • Formation of the Oceans
      • After millions of years, the clouds cooled enough to form water droplets.
      • At first, these hot rains were evaporated back into the atmosphere
      • As the Earth cooled, the water collected in basins and dissolve minerals in the rocks.
      • These rains may have lasted as long as 25 million years.
      • Water may have covered the Earth's surface for 200 million years
    • Composition of the Atmosphere
      • The original atmosphere was much different than today's
      • Geochemists believe that the early atmosphere was:
        • Rich in carbon dioxide and water vapor
        • Lesser amounts of carbon monoxide, nitrogen, hydrogen, and hydrogen chloride
        • Trace amounts of ammonia and methane
      • 3.5 billion years ago, the composition began to change to the present composition of mostly nitrogen & oxygen.
      • First due to carbon dioxide dissolving in seawater to form carbonic acid, then combining with crustal rocks
      • 2 billion years ago, the ancestors of green plants began releasing more oxygen into the atmosphere
    • The Origins of Life
      • 1953 - Stanley Miller mixed together water vapor, ammonia, methane and hydrogen and ran an electric spark through the mix for a week.
        • Produced a number of amino acids and other organic compounds.
      • Recent research now suggests that simple organic compounds were brought to Earth on comets, meteors, and asteroids that crashed into the Earth during its birth.
      • So where did life originate?
        • Not completely sure, but evidence suggests that all life originated in the oceans.
          • Biosynthesis - The initial formation of life on Earth
      • The first self-sustaining molecules may have formed deep below the layers of ice near hydrothermal vents.
    • When did life begin?
      • Oldest fossils are cyanobacteria from NW Australia and are 3.4 - 3.5 y.o
      • Stromatolites are colonial structures formed by photosynthesizing cyanobacteria and other microbes

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