FROM THE BIG BANG TO THE PRESENT:
EVOLUTION OF THE UNIVERSE AND EARTH

 

Universe 13 – 16 Billion Years old

 

Big Bang – Time Begins.

 

Formation of 1st generation stars and galaxies

6,000,000,000 years after big bang

(7 to 10 billion years before present)

 

 

 

 

Formation of the Sun

5,000,000,000 years ago

 

Solar system ~4.5 billion years old?

Condensed from gas/dust clouds (nebula) left over from supernovas of 1st generation stars –NEBULAR HYPOTHESIS

 

 

 

 

 

Formation of our solar system

 

Formed from accretion of many smaller boulder-to-mountain-to continent sized objects, under the influence of gravity.

 

Summary Image

 

 

Details of Process

 

Formation of Accretion Disk

Different Materials for Inner and Outer Planets

 

 

 

Condensation of Materials vs. Distance from Sun

 

 

 

 

Accretion of Planetesimals

 

 

 

4.6 – 3.5 Billion years before present

 

Earth Melted - Heat Sources:

(1) residual heat of formation - gravitational compression

(2) impacts from planetesimals,

(3) internal radioactivity

(4) friction and angular momentum - conversion to heat

 

 

 

 

 

 

 

 

Examples of Cratering

 

 

 

 

 

 

Differentiation occurred- producing the core/mantle/crust structure

 

An atmosphere formed from outgassing of volcanoes: carbon dioxide, nitrogen, water, etc.

 

 

 

 

 

 

Cooling of crust permitted oceans to form

 

Continental land masses formed

from lighter rocks (e.g,, granite)

 

Plate tectonics started, driven by interior heat

 

Life originated in early oceans.

 

 

NEXT 3.5 BILLION YEARS:

 

Continents drift across globe, floating on and powered by mantle convection currents.
Continents collide, mountains are built, they erode and continental drift continues
.
EPISODES OF MOUNTAIN BUILDING ACCELERATE REMOVAL OF CO2 FROM ATMOSPHERE
as erosion of lofty mountains increases and limestone (primarily CaCO3) is buried in the sea.
At the same time volcanic activity increases the level of CO2.

 

Living organisms changed the atmosphere
Green plants evolve and photosynthesis removes C02from the atmosphere.
Blue Green Algae were first about 3.5 BYBP then
multi-cellular eukaryotes about 2.5 BYBP.
RESULT: CO2 LEVEL FALLING, O2LEVEL RISING.

Cambrian Explosion, vast increase in the number of organisms with hard parts
especially CaCO3 (calcium carbonate) shells.
RESULT: ACCELERATION OF REMOVAL OF CO2.

 

Geologic cycle established—erosion by water, wind, and ice, new crust formed by volcanic activity.


NOW: Once again life is modifying the atmosphere on a global scale
Since the beginning of the Industrial Revolution CO2 levels have doubled because of human activity.
Stratospheric Ozone is being depleted by chloroflourocarbons.

On a local and regional scale, acid enhanced rainfall is
having a devastating effect on soil and vegetation health. .