C4.2 Transfers of energy and matter. Practice questions with markscheme.
83 original IB-style questions on C4.2, written from the 2025 guide: 38 multiple-choice, 31 short-answer, 7 data-based, 3 extended-response parts, 3 drawing, 1 labelling. This subtopic has no additional higher level content, so the 22-mark practice paper below serves SL and HL alike. Hand one out as a class quiz or homework, or sit it yourself and mark against the scheme. Print it, project it, or build a fresh one on the same topic.
What the guide asks for
22 statements at SL and HL.
- C4.2.1SL / HL Ecosystems as open systems in which both energy and matter can enter and exit
- C4.2.2SL / HL Sunlight as the principal source of energy that sustains most ecosystems
- C4.2.3SL / HL Flow of chemical energy through food chains
- C4.2.4SL / HL Construction of food chains and food webs to represent feeding relationships in a community
- C4.2.5SL / HL Supply of energy to decomposers as carbon compounds in organic matter coming from dead organisms
- C4.2.6SL / HL Autotrophs as organisms that use external energy sources to synthesize carbon compounds from simple inorganic substances
- C4.2.7SL / HL Use of light as the external energy source in photoautotrophs and oxidation reactions as the energy source in chemoautotrophs
- C4.2.8SL / HL Heterotrophs as organisms that use carbon compounds obtained from other organisms to synthesize the carbon compounds that they require
- C4.2.9SL / HL Release of energy in both autotrophs and heterotrophs by oxidation of carbon compounds in cell respiration
- C4.2.10SL / HL Classification of organisms into trophic levels
- C4.2.11SL / HL Construction of energy pyramids
- C4.2.12SL / HL Reductions in energy availability at each successive stage in food chains due to large energy losses between trophic levels
- C4.2.13SL / HL Heat loss to the environment in both autotrophs and heterotrophs due to conversion of chemical energy to heat in cell respiration
- C4.2.14SL / HL Restrictions on the number of trophic levels in ecosystems due to energy losses
- C4.2.15SL / HL Primary production as accumulation of carbon compounds in biomass by autotrophs
- C4.2.16SL / HL Secondary production as accumulation of carbon compounds in biomass by heterotrophs
- C4.2.17SL / HL Constructing carbon cycle diagrams
- C4.2.18SL / HL Ecosystems as carbon sinks and carbon sources
- C4.2.19SL / HL Release of carbon dioxide into the atmosphere during combustion of biomass, peat, coal, oil and natural gas
- C4.2.20SL / HL Analysis of the Keeling Curve in terms of photosynthesis, respiration and combustion
- C4.2.21SL / HL Dependence of aerobic respiration on atmospheric oxygen produced by photosynthesis, and of photosynthesis on atmospheric carbon dioxide produced by respiration
- C4.2.22SL / HL Recycling of all chemical elements required by living organisms in ecosystems
In the bank for C4.2
- 38 multiple-choice
- 31 short-answer
- 7 data-based
- 3 extended-response parts
- 3 drawing
- 1 labelling
- 0 higher level only
Every question is original and tagged to a guide statement. See the whole bank →
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The practice paper
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The food web shows feeding relationships in a freshwater pond. Which statement about the stickleback is correct?
- It is a secondary consumer in every food chain.
- It occupies the second and third trophic levels.
- It occupies the third and fourth trophic levels.
- It is a tertiary consumer in every food chain.
The diagram shows a food web in a forest stream. Dead leaves fall into the stream from trees on the banks and are partly broken down by bacteria and fungi before caddisfly larvae eat them.
Atmospheric CO₂ has been measured continuously at the Mauna Loa observatory, Hawaii, since the 1950s. Within each year the concentration oscillates, falling through the northern-hemisphere summer and rising through winter; the size of this annual swing is the seasonal amplitude. The table shows two related datasets: the mean CO₂ concentration and seasonal amplitude for each decade, alongside the global mean temperature anomaly (the difference from the 20th-century average temperature) for the same decade.
| Decade | Mean CO₂ concentration / ppm | Seasonal amplitude / ppm | Global temperature anomaly / °C |
|---|---|---|---|
| 1970s | 328 | 5.0 | 0.00 |
| 1980s | 345 | 5.3 | +0.18 |
| 1990s | 360 | 5.5 | +0.32 |
| 2000s | 379 | 5.9 | +0.51 |
| 2010s | 401 | 6.2 | +0.72 |
Outline the processes that transfer carbon between organisms and the atmosphere in the carbon cycle.
Original practice questions © Biology by Bradford · CC BY-NC-SA 4.0 · Not affiliated with or endorsed by the International Baccalaureate Organization.
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One mark per point; / separates alternative wording within a point, OR separates alternative answers, words in brackets are not required, underlined words are essential. OWTTE = or words to that effect.
- C: eating water fleas (primary consumers) makes the stickleback a secondary consumer (third trophic level), while eating diving beetle larvae (secondary consumers) makes it a tertiary consumer (fourth level);
- (a) [1]
- secondary consumer / third trophic level;
- (b) [2]
- the leaves are dead organic matter, not living organisms that fix energy;
- the energy in them was captured by photosynthesis in the trees (the producers) outside the stream, OWTTE;
- (c) [2]
- they feed on dead organic matter from every trophic level, so cannot be placed at one level in a chain;
- they release the energy in dead matter (as heat by respiration) rather than passing it on to a consumer / they recycle nutrients rather than energy, OWTTE;
- (a) [2]
- (401 − 328) ÷ 4 (decades);
- = 18.25 ≈ 18 ppm per decade;
Accept 18–18.3. Award ECF for correct method.
- (b) [2]
- (strong) positive correlation: temperature anomaly rises as CO₂ rises;
- across the whole period / consistently in every decade (about +0.1 °C per ~10 ppm), OWTTE;
- (c) [2 max]
- the long-term trend: the mean rose by 73 ppm, over ten times the seasonal amplitude (5.0 to 6.2 ppm);
- the annual oscillation cancels out within each year: the summer drawdown by photosynthesis is matched by the winter release by respiration/decomposition, so it causes no net change;
- (so) the rise comes from an additional net input of CO₂, (mainly) from combustion (of fossil fuels), OWTTE;
- (d) [2]
- higher CO₂ (and a longer/warmer growing season) increases summer photosynthesis / plant growth;
- (so) the summer drawdown (and matching winter release) both become larger, OWTTE;
- (e) [2 max]
- no, correlation does not (by itself) establish causation;
- a third factor could (in principle) drive both / the direction of causation is not shown by the correlation;
Beyond this subtopic. Award if given; the marks above can be earned without it.
- D4.3.1 (however) the known greenhouse mechanism plus experimental/physical evidence supports causation, the data are consistent with it, OWTTE;
- (f) [2 max]
- it was taken up by carbon sinks;
- (by) ecosystems in which photosynthesis exceeds respiration (e.g. growing or regrowing forests), giving a net uptake of CO₂;
- CO₂ dissolved in the oceans / was fixed by marine producers (phytoplankton), OWTTE;
Content pivot.
- photosynthesis fixes CO₂ (from air/water) into carbon compounds in producers;
- feeding passes carbon compounds along food chains;
- cell respiration (by all organisms) returns CO₂ to the atmosphere;
- decomposition: saprotrophs respire carbon from dead matter, releasing CO₂;
- combustion of biomass/fossil fuels releases CO₂;
- (some carbon is stored long-term in) fossil fuels / peat / carbonate rocks (removed from circulation), OWTTE;
More in Theme C · Interaction and interdependence
- C1.1 Enzymes and metabolism 67
- C1.2 Cell respiration 69
- C1.3 Photosynthesis 68
- C2.1 Chemical signalling 68
- C2.2 Neural signalling 67
- C3.1 Integration of body systems 74
- C3.2 Defence against disease 65
- C4.1 Populations and communities 67
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