Linked from

The 26 pages that link to Carbon sink, each with the reason it gives.

• Carbon cycleRelated: Net uptake by sinks can lower atmospheric carbon dioxide.

• Amazon rainforestRelated: Amazon forests store carbon, though drought and disturbance can reduce their uptake.

• PeatlandRelated: Undisturbed peatlands can store carbon accumulated over centuries or millennia.

• Carbon dioxide emissionsRelated: Oceans and ecosystems remove part of emitted CO₂ from the atmosphere.

• PeatRelated: Intact peatlands accumulate carbon, though drainage or fire can reverse that balance.

• Permafrost carbon cycleCompared with: Permafrost landscapes can shift from carbon accumulation toward net emissions as they warm.

• TaigaRelated: Taiga forests and soils store large amounts of carbon, though fire and thaw can reverse the balance.

• Kyoto ProtocolRelated: Kyoto accounting rules credited certain land-use activities that remove carbon from the atmosphere.

• Soil carbon sequestrationRelated: Soil is a sink only when its net carbon balance is positive.

• Forest carbon cycleCompared with: A forest is a sink only when its net carbon balance is inward.

• ClearcuttingNarrower topic: Harvesting reduces the carbon held in standing trees and can alter a forest’s sink strength.

• Gran ChacoCompared with: Intact Chaco forests store carbon, while clearing can turn them into net sources of emissions.

• SphagnumRelated: Sphagnum peatlands store carbon when plant production outpaces decomposition.

• BogRelated: Accumulating peat stores carbon that would otherwise return to the atmosphere through decomposition.

• Forest conservationRelated: Growing and intact forests can remove and store atmospheric carbon.

• Raised bogRelated: Growing raised bogs can store carbon in peat, though drainage can reverse that balance.

• RainforestRelated: Living rainforest biomass stores carbon, though disturbance can turn forests into carbon sources.

• Tongass National ForestRelated: Tongass forests store substantial carbon in trees and soils.

• Tropical and subtropical moist broadleaf forestsRelated: Living biomass and soils store carbon, though disturbance can reverse that storage.

• Tropical forest conservationRelated: Keeping forests intact retains stored carbon and supports continued uptake, while disturbance can reverse that role.

• Climate change in BrazilCompared with: Intact Brazilian forests can absorb carbon, but degradation and clearing can reverse that role.

• Great Dismal SwampRelated: Intact peatlands in the swamp can store large quantities of carbon.

• ShrublandRelated: Shrubland plants and soils store carbon, though fires and land-use change can reverse gains.

• Vasyugan SwampRelated: Peat accumulation stores carbon that would otherwise return to the atmosphere through decay.

• Congolian rainforestsRelated: Living trees and soils store carbon, although the balance varies across the region.

• Deforestation and climate changeNarrower topic: Intact forests act as carbon sinks; deforestation weakens that removal.