Evolution of Earth's atmosphere
I can describe how Earth’s atmosphere developed over billions of years.
- Year 11
- OCR
Evolution of Earth's atmosphere
I can describe how Earth’s atmosphere developed over billions of years.
Lesson details
Key learning points
- Early volcanic activity is thought to have made an atmosphere of carbon dioxide and nitrogen billions of years ago.
- Carbon dioxide can dissolve in oceans and form carbonates that, over millions of years, can form sedimentary rock.
- The amount of carbon dioxide was reduced by the formation of sedimentary rocks and photosynthesis by algae and plants.
- Algae and plants produced the oxygen that is now in the atmosphere by photosynthesis.
- Phytoplankton in the oceans are responsible for roughly half of all oxygen production that takes place today.
Keywords
Algae - A diverse range of unicellular or multicellular organisms that can photosynthesise.
Phytoplankton - A group of microscopic algae, usually found floating in the upper part of the ocean.
Photosynthesis - A process in which energy from sunlight converts carbon dioxide and water into glucose and oxygen.
Carbon sink - A process or system that takes more carbon from the atmosphere than it releases.
Sedimentary rock - Rock formed when particles settle on Earth’s surface and then become cemented together.
Common misconception
Earth's atmosphere has always contained oxygen. The atmosphere's composition is static and unchanging.
Clarify the development of oxygen through photosynthesis. Describe how atmospheric composition has evolved over time due to geological and biological processes.
Equipment
Licence
Prior knowledge starter quiz
6 Questions
Q1.Earth's atmosphere comprises approximately 21% of which gas?
Q2.What is the percentage of carbon dioxide in Earth's atmosphere?
Q3.How old is Earth thought to be?
Q4.The atmosphere on Earth has been in roughly the same proportions for how many million years?
Q5.What name is given to the layer of gas that surrounds a planet?
Q6.What is the name of this process?
