B4.1.5—Coral reef formation conditions
Coral reef formation depends on warm, shallow, clear, sunlit, saline water and is limited by temperature, light, pH and carbon dioxide.
- Syllabus
- First assessment 2025
- Objective
- B4.1.5
- Level
- HL
Coral reef formation depends on warm, shallow, clear, sunlit, saline water and is limited by temperature, light, pH and carbon dioxide.

Coverage 2016–2016 · Updated 15 Jul 2026
Coral reef formation requires warm, shallow, clear, well-lit marine conditions that support photosynthetic symbionts and calcium-carbonate skeletons.
Light reaches shallow water for symbiotic algae, while suitable temperature, salinity and carbonate chemistry support coral metabolism and calcification. A severe change in one condition can limit reef growth.
Evaluate a reef site by checking: light; temperature; salinity; water clarity; carbonate supply; and disturbance.
A warm, clear tropical shelf can support reef-building corals, whereas deep turbid water limits light even if temperature is suitable.
‘Tropical’ alone does not guarantee a reef; local depth, sediment, nutrients and chemistry also matter.
This objective is assessed through structured response, commonly using Outline / Describe / State.
Outline / Describe / State
Build the answer around this relationship: Reef-building corals need light because their zooxanthellae photosynthesise.
Saying higher temperature alone proves coral decline without acknowledging correlation limits.
Representative question
Outline one way in which reef-building corals are affected by increasing atmospheric carbon dioxide.
Alternative 1
a. corals have parts/shells/«exo»skeleton made of calcium carbonate
b. calcium carbonate «shells» dissolve in acid conditions
c. acid/high CO2 conditions reduces availability of calcium carbonate «for forming shells» OR negatively affects enzymes involved in calcification
Alternative 2
d. CO2 is «significant» greenhouse gas causing rise in ocean temperatures
e. higher ocean temperatures/acidification leads to rejection of zooxanthellae OR higher ocean temperatures/acidification leads to coral bleaching
2 max
A strong answer defines the place as a habitat or microhabitat, names the abiotic factor, and shows how it limits distribution through a tolerance range. Named examples then secure the marks: coral reefs require specific light, temperature, salinity, pH, and clear shallow water; biomes are predicted from temperature, rainfall, and insolation; desert and rainforest organisms show adaptations matched to their environmental pressures.