IB Biology SL D4.3 Climate change Questions

Practise IB Biology SL D4.3 by linking greenhouse gases to warming, feedback loops and biological impacts across ecosystems.

48 questions in this syllabus scope, with question parts counted together.

Syllabus
First assessment 2025
Course
Biology SL
Level
SL

Exam analysis

SL · 2010–2025
Papers with this topic45 / 141in the analysed sample
Latest appearanceNovember 2025
Tagged question parts54
Paper types5

Most tested objectives

  1. D4.3.1—Anthropogenic causes23 papers
  2. D4.3.8—Carbon sequestration approaches7 papers
  3. D4.3.4—Polar habitat changes5 papers
  4. D4.3.6—Range shifts5 papers
  5. D4.3.7—Coral reef threats5 papers

Common question formats

  • Comparison
  • Data analysis
  • Definition or recall
  • Diagram interpretation
  • Evaluation
  • Extended response
  • Graph interpretation
  • Process explanation
  • Structured response

Recent exam appearances

November 2025Paper 2 SL · TZ3Q5(d)[ 2 ]
November 2025Paper 1A SL · TZ3Q15, 29[ 2 ]
November 2025Paper 1A SL · TZ1Q30[ 1 ]

141 papers analysed · Tagging incomplete

Exam points

  • Explain how fossil fuels, cement, deforestation and livestock add greenhouse gases and intensify warming.
  • Explain ice-albedo and permafrost greenhouse-gas positive feedback that amplifies warming.
  • Explain how warming, drought, fire, pests and competition can drive boreal-forest decline and habitat loss.
  • Explain how polar ice loss changes habitat, migration, competition, food webs and species survival.
  • Interpret climate-induced range shifts and their effects on competition, predation, prey availability and survival.
  • Explain coral bleaching, acidification, reduced calcification and their consequences for reef biodiversity.
  • Identify how deforestation, afforestation and peatland conditions change carbon sequestration and storage.

Exam points

  • Explain how human activities raise atmospheric CO₂ or methane, using fossil-fuel combustion, deforestation, cattle farming or land-use change as examples.
  • Explain how increased anthropogenic greenhouse gases retain outgoing long-wave radiation and raise global temperature.

Question 1

[Maximum number: 1]

The graph shows the correlation between atmospheric carbon dioxide concentration and global temperature anomalies (deviations from mean global temperatures) since the industrial revolution to the year 2017.

Figure for Question 1 — IB Biology SL
Figure for Question 1 — IB Biology SL

Which statement explains the correlation between atmospheric carbon dioxide concentration and temperature shown in the graph?

A

Carbon dioxide heats up the surface of the Earth.

B

More short wave radiation bounces back to space, causing warmer seasons.

C

Less long wave radiation can escape the atmosphere, heating up the Earth.

D

Less radiation is emitted by the Earth's surface, increasing seasonal fluctuations.

Exam points

  • Explain how loss of snow or polar ice lowers albedo, increases absorbed radiation and amplifies warming.
  • Explain how warming of permafrost or ice can release methane or carbon dioxide, increasing greenhouse trapping in a positive loop.

Question 1

[Maximum number: 1]

What results from global warming?

A

An increase in absorption of solar radiation decreases poleward shift of temperate species.

B

Release of carbon dioxide from the deep ocean causes decreased rates of decomposition.

C

Release of methane from melting permafrost causes a decrease in absorption of solar radiation.

D

Loss of snow and ice causes an increase in absorption of solar radiation.

Exam points

  • Explain how warming can increase transpiration and drought stress, leading to water shortage and greater wildfire risk in boreal forests.
  • Explain how climate change can increase pests and disease, shift competition and species ranges, and cause habitat loss and faster decomposition in boreal forests.

Question 1

[Maximum number: 2]

Boreal forests stretch across Canada, Russia and Scandinavia. This northern ecosystem accounts for 29 % of the world's forest areas. The long, cold winters favour tall evergreen trees with either needles or scale-like leaves. These trees are wind-pollinated and their seeds are not enclosed in a fruit. The photograph shows a typical boreal forest in winter.

Figure for Question 1 — IB Biology SL

An increase in global temperatures poses a critical threat to boreal forests. Explain the consequences of climate change to this northern ecosystem.

Exam points

  • Explain how warming melts landfast or sea ice and reduces breeding, feeding and resting habitat for polar organisms.
  • Explain how ice loss changes habitat space and can drive migration, competition or shifts in prey and food-web relationships.
  • Outline consequences for polar organisms, including reduced survival, extinction or expansion of temperate species.

Question 1

[Maximum number: 2]

Outline two possible consequences of global warming for organisms living in arctic ecosystems.

No public sample questions are available for this syllabus point yet.

Exam points

  • Use warming and distribution data to predict poleward shifts in species ranges.
  • Explain how range shifts can alter populations and species interactions through competition, predation and food-web changes.

Question 1

[Maximum number: 1]

The data shows how the hardiness zones in part of North America are predicted to change over the next 25 years. A hardiness zone is an area that has a certain average annual minimum temperature, a factor relevant to the survival of many plants. The lower the number, the more cold

resistant the plants must be.

Figure for Question 1 — IB Biology SL

What is a likely consequence of this change for tree species?

A

Tree species will spread northwards as climate changes.

B

Tree species that are not cold-resistant will decline.

C

There will be no change in the distribution of the tree species.

D

Tree species that currently live in the north will outcompete other tree species.

Exam points

  • Explain how warming disrupts coral–zooxanthellae mutualism, reducing photosynthesis and causing bleaching, starvation or coral death.
  • Explain how ocean acidification lowers carbonate availability or calcification, damaging coral skeletons and reef habitat.
  • Link bleaching and acidification to coral-reef biodiversity decline and ecosystem consequences.

Question 1

[Maximum number: 2]

A study was done on the effect of heat stress on species of coral and their relationship with zooxanthellae algae.

The graphs show the effects of heat stress on the rates of photosynthesis in zooxanthellae and respiration of both organisms.

Global warming increases sea temperatures. Coral bleaching occurs at sea water temperatures above 33∘C33^{\circ} \mathrm{C}. Using the data in the graphs, explain the reasons for coral bleaching.

Exam points

  • Describe how dead plant material forms peat in waterlogged, acidic and anaerobic conditions where decomposition is incomplete.
  • Explain how reforestation stores atmospheric carbon and identify deforestation as an action that decreases carbon sequestration.

Question 1

[Maximum number: 1]

Which action will decrease carbon sequestration?

A

Afforestation

B

Primary production

C

Deforestation

D

Rewetting peatlands

Question 1

[Maximum number: 4]

Boreal forests stretch across Canada, Russia and Scandinavia. This northern ecosystem accounts for 29 % of the world's forest areas. The long, cold winters favour tall evergreen trees with either needles or scale-like leaves. These trees are wind-pollinated and their seeds are not enclosed in a fruit. The photograph shows a typical boreal forest in winter.

Figure for Question 1 — IB Biology SL

Question (a)

(a)

In some areas there are gaps in the boreal forest where trees fail to grow and peat tends to accumulate. Suggest reasons for this.

[ 2 ]

Question (b)

(b)

An increase in global temperatures poses a critical threat to boreal forests. Explain the consequences of climate change to this northern ecosystem.

[ 2 ]
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