IB Biology SL Topic 3 — Adapting to the Environment Paper 1 & 2 Core idea ~12 min read

Abiotic Factors: Marine & Terrestrial

Look at a world map of coral reefs and the pattern is almost suspiciously neat: a band around the tropics, hugging the coasts, and nothing anywhere else. That map is a range of tolerance drawn on a globe.

📚 What you need to know

A coral is two organisms, not one

This is the fact that makes the rest of the page make sense. A coral polyp is a small animal, related to sea anemones. Living inside its tissues are enormous numbers of single-celled algae called zooxanthellae.

Each partner gives the other something it cannot get alone. The polyp provides a safe place to live and protection from being eaten. The algae photosynthesise and pass on carbon compounds such as carbohydrates, which supply most of the polyp’s energy.

The partnership that builds a reef An animal and an alga, each supplying what the other cannot make shelter and protection sugars made by photosynthesis coral polyp (an animal) sits in a hard calcium carbonate cup zooxanthellae (algae) live inside the polyp tissueThe algae need light, so the coral needs light too. That single fact explains most of the limits on where reefs can grow.
Layer upon layer of calcium carbonate, laid down by thousands of polyps over thousands of years, is what becomes the hard structure of a reef.
Keep the partnership in your head as you read the rest of this page. Almost every limiting factor traces back to it: the algae need light, the polyp needs carbonate, and both need the right temperature.

Why reefs sit where they do

Coral has a narrow range of tolerance for several factors at once, and the reef can only form where all of them are satisfied. That intersection is a thin band around the tropics.

Water depth

Corals only grow at shallow depths, because light has to reach the zooxanthellae in strong enough amounts for them to photosynthesise. Water absorbs light quickly, so below a certain depth there is not enough energy to keep the partnership going.

Light runs out with depth, and so does the reef Depths here are approximate — the shape of the limit is what matters reef-building corals grow here below roughly 25 m there is too little light the algae cannot photosynthesise enough to support the polyp0 m 20 m 40 m 60 mAnything that blocks light does the same job as extra depth. Sediment washed off the land and water pollution both cut light and stop reef growth.
Notice the yellow light rays getting shorter as you move into deeper water. That fading is what sets the depth limit.

The other four factors

FactorEffect on reef formation
pHThe hard skeleton is calcium carbonate, which dissolves if the water is too acidic. Corals also need carbonate ions to build it, and those become scarce at low pH
SalinityCorals are marine animals and need salty water, roughly 32 to 42 parts per thousand. Fresh water running off the land dilutes the sea and limits growth
Water clarityLight must be able to pass through. Sediment from land run-off and pollution make the water cloudy and cut light to the algae
TemperatureCorals tolerate roughly 20 to 28 °C and grow best above about 23 °C. Sustained high temperatures make polyps expel their algae, causing bleaching
Water depthOnly shallow water lets enough light through for the zooxanthellae to photosynthesise

Ocean acidification, step by step

This is the chain examiners like, because it links chemistry to a living consequence. Take it one arrow at a time.

Why more carbon dioxide means less reef Four steps, and every arrow is a “therefore” More carbon dioxide in the atmosphere It dissolves in the sea and lowers the pH Hydrogen ions bind to carbonate ions Less carbonate left to build the reef with Acid does not only dissolve the reef. It removes the raw material. Burning fossil fuels raises atmospheric carbon dioxide, which lowers ocean pH.
Both halves score marks: carbonate becomes less available to build with, and existing calcium carbonate dissolves faster at low pH.

🤔 What actually happens in coral bleaching

Corals can cope with short spells of warmer water. What they cannot cope with is sustained high temperature. When the sea stays too warm, the polyps expel the zooxanthellae living in their tissues.

The algae were providing the colour, so the coral turns white — hence “bleaching”. More importantly, the algae were also providing most of the polyp’s food. A bleached coral is not dead yet, but it is starving. If conditions improve quickly it can take the algae back; if they do not, it dies.

Do not confuse bleaching with death. Bleaching is the loss of the algal partner. Death follows only if the coral is not recolonised in time. Saying “the coral dies immediately” loses the mark.

The same logic on land

Coral reefs are the marine example, but the reasoning is identical for terrestrial habitats. A species is found where its tolerance ranges for every relevant factor overlap, and nowhere else.

On land the leading factors are usually temperature and rainfall, because between them they decide what kind of vegetation can grow. That is the whole basis of the next page.

Worked examples

WORKED EXAMPLE

Explain why reef-building corals are only found in shallow water. [3 marks]

Step 1: name the partner that needs the light Coral polyps contain zooxanthellae, algae that carry out photosynthesis. Step 2: what depth does to light Light is absorbed as it passes through water, so intensity falls as depth increases. Step 3: the consequence for the coral too little light → less photosynthesis → fewer carbon compounds passed to the polyp Without that supply the polyp cannot grow or secrete calcium carbonate, so no reef forms. The algae need light, so the coral needs shallow water The mark is lost by writing “corals need light”. Corals do not photosynthesise; their algae do.
WORKED EXAMPLE

Sea temperatures at a reef stay 3 °C above normal for several weeks. Explain the likely effect on the coral. [3 marks]

Step 1: relate to the range of tolerance Corals tolerate roughly 20 to 28 °C. A sustained rise takes conditions above the upper limit of that range. Step 2: the response The polyps expel their zooxanthellae, so the coral loses its colour and appears white. This is coral bleaching. Step 3: why it matters The algae supplied most of the polyp’s carbon compounds, so without them the coral is starved of energy and will die if the algae are not regained. Bleaching, then starvation and death if conditions do not improve
WORKED EXAMPLE

A river carrying soil and fertiliser enters the sea beside a reef. Suggest two reasons why coral growth falls near the river mouth. [4 marks]

Reason 1: water clarity Sediment carried by the river makes the water cloudy, so less light reaches the zooxanthellae and photosynthesis is reduced. Reason 2: salinity Fresh water from the river dilutes the sea water, lowering the salinity below the range corals can tolerate. Reduced clarity cuts light; reduced salinity falls outside the tolerance range A third valid answer would be nutrients from fertiliser feeding algal growth that shades the coral.

💡 Exam tip

⚠ Common mix-up

Up next: Biomes — scaling the same idea up to whole continents, and why two unrelated plants on opposite sides of the world end up looking almost identical.

Want this explained one-to-one?

Book a free session with an experienced IB Biology tutor and get your trickiest topics made simple.

Book a Free Session →