Earth

Formed ~4.5 billion years ago.

Earth’s layers

Cooling dense materials (Fe) sink to middle; low-density minerals crystallized and floated to the surface.

Differentiation into compositional zones or layers

  • Central core: dense and hot
    • Composed of nickel (Ni) and iron (Fe)
  • Mantle: thickest zone and surrounds the core
    • Composed of ultramafic and mafic rocks and magma (fe, Mg, Si)
    • Heat from core escapes by convective circulation
  • Crust: chemically different from core or mantle
    • Two types of crust: Oceanic (mafic) and Crustal (felsic)
    • Water and atmospheric gases interact only with outermost crust

Whole process completed well before 4 billion years ago…

Most Common Chemical Elements in Earth

Earth’s Early Atmosphere

  • The heating and subsequent differentiation of the early earth led to the formation of the atmosphere and oceans
  • Many minerals contained water or gases in their crystals and released them during the heating and melting
  • As the Earth’s surface cooled, the water could condense to form the oceans and gases form the atmosphere
  • Chemically different than today
    • Lacked free oxygen (O2)
    • Dominated by nitrogen (N) and carbon dioxide (CO2)
    • Minor amounts of other gases:
      • Methane (CH4)
      • Ammonia (NH3)
      • Sulfur gases
  • No modern pollution
  • Barren of life because it lacked oxygen

[! Question] So how did the atmosphere fill with oxygen as it is today?

  • Earliest life were anaerobic, surviving off sulfur in an oxygen-free environment
  • Cyanobacteria began using water, CO2, and sunlight in the oceans for energy, producing oxygen as a by-product
    • First organisms (and still only bacteria) to conduct oxygenic photosynthesis

Early Life

Signs of oxygen and early life

Banded Iron Ore

  • Sedimentary rocks of alternating layers of iron oxides and iron-poor chert
  • Evidence of oxygenation of the oceans circa ~2-4 billion years ago

Stromatolites

  • Sedimentary formations created by photosynthetic organisms, like cyanobacteria
  • Peaked in fossil record about 1.25 billions years ago

Look at Earliest Known Life Forms