The carbon cycle, carbon sinks and combustion

Ecosystems (Interaction and interdependence) · Transfers of energy and matter · note 7 of 9

The carbon cycle, carbon sinks and combustionSpec C4.2.17, C4.2.18, C4.2.19

In short

Carbon is recycled in ecosystems by photosynthesis, feeding and respiration. An ecosystem is a carbon sink if photosynthesis exceeds respiration, giving a net uptake of carbon dioxide, and a carbon source if respiration exceeds photosynthesis. Combustion of biomass, peat, coal, oil and natural gas releases carbon dioxide; human activities have greatly increased combustion rates.

Carbon cycle diagrams

  • Photosynthesis: autotrophs fix CO₂ from the air (or dissolved in water) into carbon compounds.
  • Feeding: carbon compounds pass to consumers when they eat.
  • Death and egestion: carbon compounds in dead organisms and faeces pass to decomposers.
  • Respiration: producers, consumers and decomposers oxidise carbon compounds, releasing CO₂.
  • Combustion: burning biomass and fossil fuels releases CO₂.
Carbon cycle: carbon dioxide in the air is taken in by plants in photosynthesis; plants pass carbon to animals by feeding; plants, animals and decomposers release carbon dioxide by respiration; death and waste pass carbon to dead plants and animals, which decomposers break down; some dead material forms fossil fuels (coal, oil and natural gas) over millions of years, which release carbon dioxide by combustion. (opens full size in a new tab)
The carbon cycle. Each arrow is a process; each box is a store of carbon. Biomass and peat can also burn, releasing CO₂.

Sinks and sources

If photosynthesis exceeds respiration, an ecosystem has a net uptake of CO₂ and is a carbon sink (a growing forest, an expanding peat bog). If respiration exceeds photosynthesis, there is a net release of CO₂ and it is a carbon source (a drained peatland where peat now decomposes).

Combustion

Carbon stores that release CO₂ when burned
StoreHow and when it formed
Biomass (wood, crops)Recent: from photosynthesis over years to centuries
PeatPartly decomposed plant matter in waterlogged, acidic, anaerobic bogs, building up over thousands of years
CoalBuried plant remains compressed over hundreds of millions of years, much of it from the Carboniferous period
Oil and natural gasRemains of marine plankton buried in sediments and transformed by heat and pressure over millions of years

Combustion sometimes happens naturally, for example when lightning strikes start forest or peat fires, but human activities have greatly increased combustion rates, through burning fossil fuels and clearing forests by fire.

Written and checked against the IB Biology HL specification · Updated October 2026

Frequently asked questions

Why is energy lost between trophic levels?

Energy is lost between trophic levels because not all of an organism is eaten, not all food eaten is digested, and much of the absorbed energy is converted to heat in cell respiration. Heat is lost to the environment. Typically only about 10% of the energy passes to the next level, which limits food chain length.

What is the difference between an autotroph and a heterotroph?

An autotroph uses an external energy source, light or oxidation reactions, to synthesise carbon compounds from simple inorganic substances such as carbon dioxide. A heterotroph uses carbon compounds obtained from other organisms, digesting and assimilating them to build the carbon compounds it needs. Both release energy by cell respiration.

Why can matter be recycled in ecosystems but energy cannot?

Matter is recycled because atoms are conserved: decomposers break down dead organic matter and release elements in inorganic forms that producers reuse. Energy cannot be recycled because it is eventually converted to heat by cell respiration, and organisms cannot convert heat back into chemical energy. New energy must keep arriving as sunlight.

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