The Earth's Atmosphere

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1
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What was the atmosphere of the earth like when it was formed 4.6 billion years ago?

Intense volcanic activity releases:

  • Mainly CO2

  • Water vapour (condenses - oceans)

  • Small amount of methane +ammonia

2
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How did the atmosphere of the earth change 3 billion years ago?

Green plants & algae evolve and:

  • CO2 reduced - plants take it in and give O2 out.

  • Microorganisms that can’t tolerate O2 are killed off.

  • C from CO2 locked in sedimentary rocks formed from shells + skeletons of marine organisms

  • Other gases react with O2 ,release N

  • N produced by bacteria removing nitrates from decaying plant material

3
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How has the atmosphere of the earth changed now?

  • 20% oxygen and 80% nitrogen

  • Carbon dioxide decreased alot.

4
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Why have the levels of oxygen increased over time?

  • Algae and plants started to photosynthesise 2.7 billion years ago

  • Plants evolved ,O2 levels increased.

  • Eventually O2 levels increased enough to allow animals to evolve.

5
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How have plants and algae caused the levels of carbon dioxide to decrease over time?

Plants and algae evolved, using more carbon dioxide during photosynthesis.

6
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How has carbon caused the levels of carbon dioxide to decrease over time?

Carbon becomes locked up in sedimentary (limestone) rocks and fossil fuels. (coal, crude oil, natural gas)

7
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What is limestone?

Contains calcium carbonate, formed from shells and skeleton of sea creatures.

8
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What is coal?

Sedimentary rock formed from plant deposits that were buried + compressed over million of years.

9
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How has sea water caused the levels of carbon dioxide to decrease over time?

Carbon dioxide and sea water react to produce:

  • Insoluble carbonates that are deposited as sediment

  • Soluble hydrogen carbonates

10
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Why is carbon dioxide a risk for marine life?

Too much carbon dioxide dissolving in oceans can harm sea life, such as coral reefs.