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Ignition Learning — Activity Sheet

The carbon cycle & Earth's spheres

Science · Year 9

Name: ______________________Date: ____________

Carbon continuously moves between Earth's major spheres — the atmosphere (air), biosphere (living things), hydrosphere (water) and geosphere (rock and soil) — in an ongoing cycle. Photosynthesis pulls carbon dioxide from the atmosphere into plants (biosphere) as they build sugars using sunlight. Respiration releases carbon dioxide back into the atmosphere as living things break down those sugars for energy. Combustion (burning fuels, whether wood or fossil fuels) rapidly releases carbon stored in the biosphere or geosphere back into the atmosphere. These processes normally balance over long timescales, but human activity — especially burning fossil fuels, which releases carbon stored underground for millions of years — has significantly increased the rate of carbon entering the atmosphere.

Example

A tree absorbs atmospheric CO₂ through photosynthesis, storing carbon in its wood (biosphere) for decades. When the tree eventually decomposes or is burned, that stored carbon releases back into the atmosphere — but burning coal (formed from ancient plant matter in the geosphere over millions of years) releases carbon that had been locked away for a vastly longer timescale, adding it to the atmosphere much faster than natural cycles remove it.

Key terms

Carbon cycle:
The continuous movement of carbon between Earth's atmosphere, biosphere, hydrosphere and geosphere.
Combustion:
The rapid burning of a fuel, releasing stored carbon as carbon dioxide.

Questions

  1. 1. The carbon cycle describes carbon moving between:

    • Earth's major spheres
    • Only the atmosphere, nowhere else
    • Nothing, carbon never moves
    • Only human-made objects
  2. 2. Photosynthesis pulls carbon dioxide:

    • From the atmosphere into plants
    • Only out of water
    • From rocks directly into animals
    • Nowhere, it has no effect on carbon
  3. 3. Respiration releases carbon dioxide:

    • Back into the atmosphere
    • Only into rocks
    • Only into water
    • Nowhere at all
  4. 4. Combustion (burning fuel):

    • Rapidly releases stored carbon into the atmosphere
    • Removes carbon from the atmosphere
    • Has no connection to the carbon cycle
    • Only happens underwater
  5. 5. The biosphere refers to:

    • Living things
    • Only the atmosphere
    • Only rocks and soil
    • Only water
  6. 6. The geosphere refers to:

    • Rock and soil
    • Only living things
    • Only air
    • Only water
  7. 7. Fossil fuels store carbon that was:

    • Locked away for millions of years
    • Added to the ground yesterday
    • Never part of the carbon cycle
    • Always in the atmosphere
  8. 8. Why does burning fossil fuels add carbon to the atmosphere faster than it can be naturally removed?

    • It releases carbon that took millions of years to accumulate, all at a much faster rate than natural processes reabsorb it
    • Burning fossil fuels removes carbon from the atmosphere, not adds it
    • Fossil fuels contain no carbon at all
    • Natural processes always remove carbon from the atmosphere instantly regardless of how fast it is released
  9. 9. Why are photosynthesis and respiration often described as roughly balancing each other in a stable ecosystem?

    • Photosynthesis removes CO2 from the atmosphere while respiration returns it, keeping levels relatively stable over time
    • Photosynthesis and respiration always move carbon in the exact same direction
    • These two processes have no meaningful relationship to each other
    • Respiration always removes far more carbon from the atmosphere than photosynthesis can add
  10. 10. Why might a growing forest be considered a "carbon sink," temporarily storing more carbon than it releases?

    • Trees continuously absorb and store carbon in their growing wood faster than it is released through respiration or decomposition
    • Forests never actually absorb or store any carbon
    • A growing forest always releases more carbon than it absorbs
    • Carbon storage has no connection to how quickly a forest is growing
  11. 11. Why does the ocean (part of the hydrosphere) play a significant role in the carbon cycle, beyond just being a body of water?

    • Oceans absorb and store large amounts of atmospheric carbon dioxide, acting as another major carbon reservoir
    • Oceans have no connection to the carbon cycle at all
    • Only land-based spheres are ever involved in moving carbon around the planet
    • Water is incapable of storing or exchanging carbon dioxide with the atmosphere
  12. 12. Why might deforestation affect the carbon cycle in two separate, compounding ways?

    • It reduces the number of trees able to absorb CO2, AND often involves burning that releases stored carbon back into the atmosphere
    • Deforestation has no effect on the carbon cycle whatsoever
    • Cutting down trees always removes carbon from the atmosphere with no other effect
    • Only one of these two effects could ever occur from deforestation, never both together
  13. 13. Why might scientists model the carbon cycle as interactions between spheres, rather than describing carbon movement without this framework?

    • It helps clarify exactly which parts of the Earth system are gaining or losing carbon, and how processes connect across them
    • Modelling carbon movement using Earth's spheres provides no additional scientific clarity
    • Carbon never actually moves between different parts of the Earth system
    • The concept of Earth's spheres has no genuine connection to the carbon cycle
  14. 14. Why might the timescale of carbon cycling through the atmosphere-biosphere loop (photosynthesis/respiration, often years) differ dramatically from the timescale of carbon locked in the geosphere (fossil fuels, millions of years)?

    • Different carbon reservoirs and pathways operate at vastly different natural speeds, from rapid biological exchange to extremely slow geological processes
    • All carbon cycling processes, regardless of which spheres are involved, occur at an identical speed
    • Fossil fuel formation and photosynthesis operate on the exact same natural timescale
    • Timescale has no bearing on understanding how the carbon cycle functions
  15. 15. Why might human combustion of fossil fuels be described as "unlocking" carbon that was previously outside the active, fast-moving parts of the carbon cycle?

    • Fossil fuels represent carbon that had been removed from active atmosphere-biosphere exchange for a very long geological time before being burned
    • Fossil fuels have always been part of the fast-moving atmosphere-biosphere carbon exchange
    • Burning fossil fuels has no effect on which parts of the carbon cycle are active
    • Carbon in fossil fuels was never originally part of the carbon cycle at all
  16. 16. Why might understanding the carbon cycle help explain why planting new trees is often suggested as one, but not the only, solution to rising atmospheric carbon dioxide?

    • While trees can absorb and store carbon, the scale and speed of human fossil fuel combustion may exceed what forest growth alone can offset
    • Planting trees always immediately and completely solves any rise in atmospheric carbon
    • Trees have no actual role in absorbing or storing atmospheric carbon
    • The rate of carbon released by burning fossil fuels has no bearing on how effective tree planting can be as a solution
  17. 17. A wetland is drained and converted to farmland, releasing large amounts of stored carbon that had built up in the waterlogged soil over centuries. Which spheres are directly involved in this carbon release?

    • The geosphere (soil) releasing carbon into the atmosphere
    • Only the hydrosphere, since wetlands involve water
    • No spheres are involved, since farmland has no connection to carbon storage
    • Only the biosphere, since farmland involves crops
  18. 18. Why might scientists studying the carbon cycle need long-term data spanning decades or centuries, rather than just a single year of measurements?

    • Natural fluctuations occur over short periods, so long-term data helps distinguish a genuine underlying trend from normal year-to-year variation
    • A single year of data always provides a completely accurate picture of long-term carbon cycle trends
    • Carbon cycle processes never show any variation from year to year
    • Long-term data collection provides no additional insight beyond a single year of measurement
  19. 19. Why might ocean acidification (a hydrosphere effect) be considered a consequence of the same processes driving atmospheric carbon dioxide increases?

    • As oceans absorb more atmospheric CO2, chemical reactions in the water increase acidity, linking atmospheric and hydrosphere changes
    • Ocean acidity has no connection whatsoever to atmospheric carbon dioxide levels
    • Only the atmosphere is ever affected by changes in global carbon levels
    • Oceans are entirely unable to absorb any carbon dioxide from the atmosphere
  20. 20. Why might restoring a wetland (rather than only planting trees) sometimes be proposed as an additional strategy for managing atmospheric carbon?

    • Different ecosystems store carbon through different processes and timescales, so multiple restoration strategies can each contribute in their own way
    • Wetlands have no capacity to store or affect carbon compared to forests
    • Only tree planting can ever have any meaningful effect on atmospheric carbon
    • Ecosystem restoration strategies are always completely interchangeable with identical effects
  21. 21. Understanding the carbon cycle and Earth's spheres mainly helps you to:

    • Explain how carbon moves between and is stored within different parts of the Earth system
    • Assume carbon never moves or changes location on Earth
    • Ignore the connection between human activity and atmospheric carbon levels
    • Treat all of Earth's spheres as completely unconnected to each other

Answer key (parent copy)

  1. 1. Earth's major spheres
  2. 2. From the atmosphere into plants
  3. 3. Back into the atmosphere
  4. 4. Rapidly releases stored carbon into the atmosphere
  5. 5. Living things
  6. 6. Rock and soil
  7. 7. Locked away for millions of years
  8. 8. It releases carbon that took millions of years to accumulate, all at a much faster rate than natural processes reabsorb it
  9. 9. Photosynthesis removes CO2 from the atmosphere while respiration returns it, keeping levels relatively stable over time
  10. 10. Trees continuously absorb and store carbon in their growing wood faster than it is released through respiration or decomposition
  11. 11. Oceans absorb and store large amounts of atmospheric carbon dioxide, acting as another major carbon reservoir
  12. 12. It reduces the number of trees able to absorb CO2, AND often involves burning that releases stored carbon back into the atmosphere
  13. 13. It helps clarify exactly which parts of the Earth system are gaining or losing carbon, and how processes connect across them
  14. 14. Different carbon reservoirs and pathways operate at vastly different natural speeds, from rapid biological exchange to extremely slow geological processes
  15. 15. Fossil fuels represent carbon that had been removed from active atmosphere-biosphere exchange for a very long geological time before being burned
  16. 16. While trees can absorb and store carbon, the scale and speed of human fossil fuel combustion may exceed what forest growth alone can offset
  17. 17. The geosphere (soil) releasing carbon into the atmosphere
  18. 18. Natural fluctuations occur over short periods, so long-term data helps distinguish a genuine underlying trend from normal year-to-year variation
  19. 19. As oceans absorb more atmospheric CO2, chemical reactions in the water increase acidity, linking atmospheric and hydrosphere changes
  20. 20. Different ecosystems store carbon through different processes and timescales, so multiple restoration strategies can each contribute in their own way
  21. 21. Explain how carbon moves between and is stored within different parts of the Earth system