Linked from

The 17 pages that link to Permafrost carbon cycle, each with the reason it gives.

• PermafrostRelated: Thaw can expose ancient organic matter to decomposition and greenhouse-gas release.

• Arctic tundraRelated: Tundra thaw can release carbon previously stored in frozen organic matter.

• TundraRelated: Tundra soils hold large carbon stores that can become greenhouse-gas sources as they thaw.

• TaigaRelated: Thaw can expose stored organic matter to decomposition and release greenhouse gases.

• East Siberian SeaRelated: River and coastal inputs make the sea part of a changing Arctic carbon system.

• Subarctic climateRelated: Subarctic permafrost stores organic carbon that may enter the atmosphere as soils warm.

• ThermokarstRelated: Thermokarst exposes previously frozen organic matter to decomposition and greenhouse-gas production.

• BiogeochemistryRelated: Thaw can expose stored organic matter to decomposition, creating uncertain climate feedbacks.

• Forest carbon cycleRelated: Warming in northern forests can thaw permafrost and expose previously frozen carbon to decomposition.

• Organic matterRelated: Frozen organic matter can decompose and release greenhouse gases when thaw exposes it to microbes.

• Lyakhovsky IslandsRelated: Thawing island soils can release stored carbon.

• Bolshoy Lyakhovsky IslandRelated: Thawing island deposits expose ancient carbon to microbial decomposition.

• Tipping points in the climate systemRelated: Thaw can release greenhouse gases that add warming and increase further thaw.

• Gyda PeninsulaRelated: Thawing organic soils can release greenhouse gases from the peninsula’s tundra.

• Lena Delta Wildlife ReserveRelated: Thawing delta soils may change carbon storage and greenhouse-gas emissions.

• Maly Lyakhovsky IslandRelated: Thawing Arctic ground can release carbon from soils across islands like Maly Lyakhovsky.

• New SiberiaRelated: Thawing permafrost in Arctic landscapes may alter greenhouse-gas emissions.