Describe the proportions of gases in the modern atmosphere.
Around 80% of N2.
20% of O2.
Small quantities of CO2, H2O, and noble gases.
Describe the Earth’s early atmosphere and how it was formed.
The Earth was hot when it was formed.
There was significant volcanic activity.
Gases have been released from these volcanoes.
These gases included CO2, N2, CH4, NH3, H2O.
How did the amount of oxygen in the atmosphere increase?
Algae and plants produced the atmospheric O by photosynthesis, which can be represented by the equation: 6CO2 + 6H2O → C6H12O6 + 6O2.
As the amount of gradually O2 increased, there were more plants that produced more oxygen.
How did the amount of oxygen in the atmosphere decrease?
Some CO2 was dissolved in the oceans, where it reacted with metal ions to form insoluble carbonates, such as CaCO3, or was taken in by animals to become a part of skeleton. When the animal dies, this becomes a sedimentary rock.
Some CO2 was used in photosynthesis to make oxygen.