IB ESS HL Topic 4 — Aquatic Food Production Paper 1 & 2 Core idea ~10 min read

Warming Seas and Ocean Acidification

Quotas, mesh sizes and marine parks can all be enforced. Neither warming nor acidification can. Both come from the same cause — extra carbon dioxide in the atmosphere — and both are already reshaping the systems that aquatic food production depends on.

📘 What you need to know

Two problems, one cause

Extra CO2 in the atmosphere does two separate things to the ocean. It traps heat, warming the water. And it dissolves into seawater, where it forms carbonic acid and lowers the pH. Students often merge these; keep them apart and your answers get sharper immediately.

Keep these separate more CO2 → warmer water  •  more CO2 → lower pH

What warming does

Coral bleaching, step by step

Corals live with tiny algae inside their tissues. The algae photosynthesise and feed the coral; the coral gives them shelter. Heat and acidity break that partnership.

How a coral bleaches Bleaching is not death, but it is the step before it 1 HEALTHY Algae live inside the coral tissue and feed it Coral is coloured 2 STRESSED Heat and acidity make the coral expel its algae Food supply is lost 3 BLEACHED White skeleton remains Recovery is possible Death if stress persists A bleached coral is starving, not dead Repeated events give it no time to recover between them
The distinction in stage 3 matters. Coral can regain its algae if conditions improve quickly, which is why the frequency of bleaching events matters as much as their severity.

What acidification does to shell builders

Case study: the Great Barrier Reef

Off Queensland, Australia, the Great Barrier Reef is the world’s largest coral reef system and supports both tourism and fishing. It is also the clearest illustration of what these two pressures do together.

🧩 What is happening, and what it costs

  1. Repeated bleaching. Back-to-back events in 2016 and 2017 affected around two-thirds of the reef.
  2. Rising sea temperatures. Even small increases are enough to trigger bleaching, so events are becoming more frequent.
  3. Acidification. Weakens the coral structure itself, making it more likely to erode or break.
  4. Biodiversity. Reefs support enormous numbers of species; losing coral removes both habitat and food.
  5. Fishing. Commercial and recreational fisheries lose stock, and local fishers lose income.
  6. Tourism. Millions of visitors come for vibrant reef; bleached reef draws fewer, and snorkelling and diving revenue falls.
  7. Coastal protection. Reefs buffer storm surge and waves. Weakened reef means Queensland coastal communities face higher flood and property damage risk.
One damaged reef, five sets of consequences Ecological, economic and social, all at once REEF DAMAGE bleaching and erosion BIODIVERSITY LOSS habitat and food sources gone FISHING INDUSTRY fewer fish, lost livelihoods TOURISM diving revenue falls COASTAL PROTECTION less buffering of storms FOOD WEB DISRUPTION predator-prey links altered Reef loss is an economic event as well as an ecological one Tourism, fishing and flood protection are all reef services
Grouping the consequences this way makes essays easy to structure: two ecological branches, two economic, one that is both.
Every impact here is an ecosystem service being lost. Naming them as services — provisioning (fish), cultural (tourism), regulating (coastal protection) — connects this page straight to the systems parts of the course.

Worked examples

WORKED EXAMPLE 1

Scale of the 2016–17 bleaching

The Great Barrier Reef covers roughly 344 000 km2. If back-to-back bleaching affected about two-thirds of it, estimate the area affected.

Step 1: convert the fraction two-thirds = 0.667, or about 67% Step 2: apply it to the area 344 000 × 0.667 = 229 000 km2 Roughly 230 000 km2 affected for context, that is larger than the United Kingdom — comparisons like this earn credit in extended answers
WORKED EXAMPLE 2

Explain how rising CO2 causes coral bleaching [4]

Cover both mechanisms.

Link 1 Rising atmospheric CO2 traps heat, so sea temperature rises Link 2 CO2 also dissolves in seawater, forming carbonic acid and lowering pH Link 3 Both stresses cause the coral to expel the algae living in its tissues Link 4 Without the algae the coral loses its colour and its main food supply Prolonged stress kills the coral the two-mechanism structure is the point — an answer about heat alone caps at half marks
WORKED EXAMPLE 3

Why are oyster farms struggling? [3]

Explain using acidification.

Link 1 More dissolved CO2 makes seawater less alkaline, reducing available carbonate ions Link 2 Oysters build shells from calcium carbonate, so shell formation slows and shells weaken Link 3 Larvae in particular fail to survive, so harvests fall Reduced yields for growers in acidifying waters the Pacific Northwest is the named example to reach for here

💡 Exam tip

⚠ Common mix-up

Up next: Nutrients and Productivity in the Oceans — the first HL section, on why some seas are crowded with life and others are close to empty.

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