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GCSE/Combined Science/AQA

C9.1Composition and evolution of the Earth’s atmosphere: early atmosphere, oxygen rise and carbon dioxide fall

Notes

Composition and Evolution of the Earth's Atmosphere (C9.1)

Current composition of the atmosphere

  • Nitrogen (N₂): ~78%
  • Oxygen (O₂): ~21%
  • Argon (Ar): ~1%
  • Carbon dioxide (CO₂): ~0.04% (400 ppm)
  • Water vapour: variable (0–4%)
  • Other noble gases: trace amounts

Early Earth atmosphere

About 4.6 billion years ago, the Earth was newly formed, very hot, with intense volcanic activity.

Early atmosphere contained:

  • Mostly carbon dioxide (CO₂)
  • Water vapour (H₂O)
  • Nitrogen (N₂) — from volcanic outgassing
  • Small amounts of methane (CH₄), ammonia (NH₃), hydrogen sulfide (H₂S)
  • Virtually no oxygen (O₂)

This is similar to the current atmospheres of Mars and Venus (mostly CO₂).

How the atmosphere evolved

Phase 1 — Oceans formed:
As Earth cooled, water vapour condensed → seas formed. CO₂ dissolved into the oceans → reduced atmospheric CO₂. Some CO₂ ended up as carbonate rocks (limestone — CaCO₃).

Phase 2 — Photosynthesis (cyanobacteria, ~3.5 billion years ago):
First photosynthesising organisms (cyanobacteria) produced O₂:
6CO₂ + 6H₂O → C₆H₁₂O₆ + 6O₂
CO₂ removed; O₂ released. Over hundreds of millions of years, O₂ accumulated.

Phase 3 — O₂ reacted with iron:
Initially, O₂ produced was absorbed by iron compounds in oceans (forming iron oxide — "banded iron formations"). Once iron was saturated, O₂ began to accumulate in atmosphere.

Phase 4 — Ozone layer formed:
O₃ (ozone) formed from O₂ in upper atmosphere → absorbed UV radiation → allowed complex life to colonise land.

Phase 5 — Nitrogen accumulated:
N₂ released by volcanic activity and by denitrifying bacteria. N₂ is unreactive → accumulated over billions of years.

Evidence limitations

These events happened billions of years ago. Evidence is indirect and incomplete — rock records, fossil microorganisms, chemical signatures. There is still scientific debate about precise timings and mechanisms.

Common exam errors

  1. Saying the early atmosphere was mainly nitrogen — it was mainly CO₂.
  2. Forgetting that oxygen was produced by photosynthesis (cyanobacteria), not volcanic activity.
  3. Saying CO₂ is currently 21% — that is oxygen; CO₂ is only ~0.04%.

AI-generated · claude-opus-4-7 · v3-deep-combined-science

Practice questions

Try each before peeking at the worked solution.

  1. Question 13 marks

    Current atmospheric composition

    State the approximate percentage of the following gases in today's atmosphere:
    (a) Nitrogen [1]
    (b) Oxygen [1]
    (c) Carbon dioxide [1]

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    AI-generated · claude-opus-4-7 · v3-deep-combined-science

  2. Question 25 marks

    Early atmosphere composition

    (a) Describe the composition of the Earth's early atmosphere about 4.6 billion years ago. [3]
    (b) Explain how the early atmosphere formed. [2]

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    AI-generated · claude-opus-4-7 · v3-deep-combined-science

  3. Question 36 marks

    Oxygen accumulation (6-marker)

    Explain how oxygen came to make up approximately 21% of the Earth's atmosphere today. [6]

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    AI-generated · claude-opus-4-7 · v3-deep-combined-science

  4. Question 42 marks

    CO₂ removal from early atmosphere

    Describe TWO ways in which carbon dioxide was removed from the Earth's early atmosphere. [2]

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    AI-generated · claude-opus-4-7 · v3-deep-combined-science

Flashcards

C9.1 — Composition and evolution of the Earth's atmosphere: early atmosphere, oxygen rise and carbon dioxide fall

8-card SR deck for AQA Combined Science topic C9.1

8 cards · spaced repetition (SM-2)