Coral bleaching happens when corals lose the algae that live inside their tissues, often because ocean temperatures stay too high for too long. This cheat sheet helps students connect climate change, water quality, disease, and human activities to reef health. It also gives a clear reference for the warning signs scientists use to measure whether a reef ecosystem is stable or declining.
The core idea is that corals depend on a symbiotic relationship with zooxanthellae, which provide much of the coral’s energy through photosynthesis. When stress increases, corals may expel these algae and turn white, which can lead to starvation or death if stressful conditions continue. Reef health is measured using indicators such as live coral cover, bleaching percentage, species diversity, water temperature, pH, turbidity, and nutrient levels.
Key Facts
- Coral bleaching occurs when stressed coral polyps expel zooxanthellae, causing the coral skeleton to show through the clear tissue.
- The basic stress relationship is higher temperature + longer exposure = greater bleaching risk.
- Corals can recover from bleaching if temperatures return to normal and the coral regains zooxanthellae before starvation or disease occurs.
- Percent bleached coral can be calculated as percent bleached = bleached coral area / total coral area x 100.
- Percent live coral cover can be calculated as percent live cover = live coral area / total reef survey area x 100.
- Ocean acidification lowers seawater pH and reduces carbonate ion availability, making it harder for corals to build calcium carbonate skeletons.
- Major reef stressors include marine heat waves, pollution, sediment runoff, overfishing, disease, coastal development, and physical damage.
- Healthy reefs usually have high live coral cover, high biodiversity, clear water, balanced fish populations, and low disease or algae overgrowth.
Vocabulary
- Coral bleaching
- A stress response in which corals lose their symbiotic algae and appear white or pale.
- Zooxanthellae
- Photosynthetic algae that live inside coral tissues and provide food energy to the coral.
- Symbiosis
- A close relationship between two organisms, such as coral and zooxanthellae, where both can benefit.
- Ocean acidification
- The decrease in ocean pH caused mainly by the absorption of carbon dioxide from the atmosphere.
- Live coral cover
- The percentage of a reef surface that is covered by living coral tissue.
- Reef resilience
- The ability of a coral reef to resist damage, recover after stress, and continue functioning as an ecosystem.
Common Mistakes to Avoid
- Thinking bleached coral is always dead is wrong because bleached coral is stressed but may recover if conditions improve soon enough.
- Blaming only warm water for reef decline is wrong because pollution, sediment, disease, overfishing, and acidification can also weaken reefs.
- Confusing coral with rock is wrong because coral reefs are built by living animals that secrete calcium carbonate skeletons.
- Using percent bleached = total coral area / bleached area x 100 is wrong because the bleached area must be divided by the total coral area.
- Assuming clear water always means a healthy reef is wrong because temperature stress, low biodiversity, or disease can still harm a reef even when visibility is good.
Practice Questions
- 1 A reef survey finds 18 square meters of bleached coral out of 60 square meters of total coral. What is the percent bleached coral?
- 2 A transect covers 80 square meters of reef, and 44 square meters are covered by living coral. Calculate the percent live coral cover.
- 3 During a heat wave, reef water temperature stays 2 degrees Celsius above the usual summer maximum for three weeks. Explain how this could affect coral and zooxanthellae.
- 4 A reef has moderate bleaching but high fish diversity, low pollution, and nearby protected areas. Explain why this reef may have a better chance of recovery than a reef with heavy runoff and overfishing.