Afforestation, forest regeneration and peatland restoration

Ecosystems (Continuity and change) · Climate change · note 5 of 7

Afforestation, forest regeneration and peatland restorationSpec D4.3.8

In short

Afforestation, forest regeneration and restoration of peat-forming wetlands are approaches to carbon sequestration: removing carbon dioxide from the atmosphere and storing it as organic carbon. Scientists debate whether plantations of non-native trees or rewilding with native species is best. Peat forms in waterlogged soils, where decomposition is slow.

Carbon sequestration is the capture of carbon dioxide from the atmosphere and its long-term storage, here as organic carbon in plants and soil.

ApproachWhat it involves
AfforestationPlanting trees on land that has not been forest for a long time
Forest regenerationAllowing or helping forest to regrow on land where it has been cleared
Restoration of peat-forming wetlandsBlocking drains to rewet peatland, so waterlogged conditions return and peat forms again

Peat forms because waterlogged soil is anaerobic and acidic, so decomposers break down dead plant matter very slowly and carbon accumulates. Peat formation naturally occurs in waterlogged soils in temperate and boreal zones, and also very rapidly in some tropical ecosystems.

An active scientific debate
ApproachForAgainst
Plantations of non-native treesFast-growing species can absorb CO₂ quicklyOften monocultures with low biodiversity; harvesting releases stored carbon
Rewilding with native speciesHigher biodiversity; more resilient to pests and climateMay sequester carbon more slowly at first
Exam tip:

When asked to evaluate, weigh both sides: speed of carbon uptake against biodiversity and long-term storage.

Written and checked against the IB Biology HL specification · Updated October 2026

Frequently asked questions

What are positive feedback loops in climate change?

Positive feedback loops are cycles in which warming causes changes that cause more warming. Examples are loss of reflective snow and ice, so more solar radiation is absorbed; thawing permafrost releasing CO₂ and methane; CO₂ released from the deep ocean; and more droughts and forest fires releasing carbon.

How does climate change affect coral reefs?

Climate change threatens coral reefs in two ways. Increased carbon dioxide causes ocean acidification, which suppresses calcification so corals build skeletons more slowly. Higher water temperatures cause coral bleaching, when corals expel their symbiotic algae and may die. Loss of corals causes collapse of the whole reef ecosystem.

Why are species moving to higher altitudes and towards the poles?

Species are moving because warming makes the warm edge of their range too hot, while cooler places further upslope or poleward become suitable. Tropical montane birds in New Guinea have shifted upslope, and some North American trees show contraction at their warm edge and northward spread.

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