Linked from

The 115 pages that link to Carbon cycle, each with the reason it gives.

• Climate changeRelated: Human emissions alter the natural movement of carbon into and out of the atmosphere.

• DeforestationRelated: Removing forests releases stored carbon and reduces future uptake from the atmosphere.

• Carbon dioxideNarrower topic: CO₂ is a major exchangeable form of carbon linking these reservoirs.

• PhotosynthesisNarrower topic: Photosynthesis is a major pathway moving atmospheric carbon dioxide into living matter.

• Greenhouse gas emissionsNarrower topic: It determines how long emitted carbon dioxide remains in the atmosphere.

• WildfireRelated: Wildfires release stored carbon and can alter how much vegetation later absorbs.

• DecompositionRelated: Decomposition transfers carbon from dead organisms into soils and the atmosphere.

• Nutrient cyclingBroader topic: Carbon cycling links ecosystem production and decomposition to atmospheric change.

• AnthropoceneNarrower topic: Fossil-fuel combustion has rapidly shifted carbon from geological stores into the atmosphere and oceans.

• Land-use changeNarrower topic: Changing vegetation and soils alters carbon storage and emissions.

• Climate modelRelated: Carbon-cycle models determine how much emitted carbon dioxide remains in the atmosphere.

• PermianRelated: Carbon release and storage help explain Permian climate change and extinction pressures.

• PlanktonNarrower topic: Photosynthesis and sinking planktonic material move carbon through the ocean and atmosphere.

• Seagrass meadowNarrower topic: Meadow degradation can expose stored sediment carbon to decomposition and release.

• Biogeochemical cycleBroader topic: It links biological carbon storage to atmospheric carbon dioxide and climate.

• PhytoplanktonNarrower topic: Phytoplankton fix dissolved carbon and help move it through ocean ecosystems.

• Chemical weatheringRelated: Silicate weathering consumes carbon dioxide over geological timescales, linking rock reactions to climate.

• Primary productionNarrower topic: Primary production is a major route by which carbon enters living biomass.

• EarthRelated: Carbon exchange links life, oceans, and rocks to atmospheric carbon dioxide.

• Alcoholic fermentationNarrower topic: Fermentation returns sugar-derived carbon to the atmosphere as carbon dioxide.

• DetritivoreRelated: Detritivore processing affects how carbon in dead matter is stored or released.

• Atmosphere of EarthRelated: Carbon exchange regulates atmospheric carbon dioxide over timescales from seasons to geologic ages.

• Carbon dioxide emissionsNarrower topic: It connects emission sources to the sinks and reservoirs that determine atmospheric CO₂ levels.

• Congo BasinNarrower topic: Forest growth and peat accumulation make the basin a major terrestrial carbon store.

• Greenhouse gasRelated: It governs how emissions and natural sinks change atmospheric carbon dioxide concentrations.

• Phosphorus cycleCompared with: Carbon cycles rapidly through the atmosphere, while phosphorus lacks a comparable gaseous route.

• Carbon sinkNarrower topic: It tracks the exchanges that determine whether a system is a net sink or source.

• PeatNarrower topic: Peat accumulation removes carbon from active circulation and stores it in soils.

• Snowball EarthRelated: Its disruption and recovery provide the proposed route from global ice to greenhouse warming.

• Soil food webRelated: Soil consumers influence whether organic carbon is stored, transformed, or released as carbon dioxide.

• MethanogenesisNarrower topic: Methanogenesis converts organic or inorganic carbon into methane.

• CarbonRelated: This cycle tracks carbon between reservoirs and helps explain its environmental effects.

• Conservation of massRelated: Carbon inventories use conservation accounting to track transfers among reservoirs.

• CerradoRelated: Cerrado vegetation and deep roots store carbon, while clearing and fire release it.

• EvergreenRelated: Year-round foliage influences when forests take up and release carbon.

• PaleoceneNarrower topic: Carbon-cycle shifts help explain Paleocene climate and the warming at its end.

• Paleocene–Eocene Thermal MaximumNarrower topic: Its reservoirs and exchanges frame the event’s carbon release and recovery.

• Atmospheric lifetimeNarrower topic: Carbon dioxide’s persistence reflects exchange among reservoirs, not just atmospheric chemical loss.

• Forest degradationRelated: Degraded forests often store less carbon and may release stored carbon through damage or decay.

• CarbonateNarrower topic: Carbonate formation and dissolution transfer carbon between ocean water and solid Earth.

• CharcoalNarrower topic: Charcoal can store biomass carbon in a persistent solid form or release it when burned.

• Bark beetleRelated: Dead trees and altered growth change how affected forests store and release carbon.

• Slash-and-burn agricultureNarrower topic: Burning and regrowth transfer carbon between vegetation and the atmosphere.

• Biological carbon pumpNarrower topic: The pump is one pathway within the global exchange of carbon among reservoirs.

• Carbon-12Related: Carbon-12 traces carbon transfer through reservoirs and biological processes.

• Coastal upwellingRelated: Upwelled water can return dissolved carbon to the surface, affecting air–sea exchange.

• Aerobic respirationRelated: Respiratory carbon dioxide returns oxidized organic carbon to the environment.

• Carboniferous rainforest collapseRelated: Changing plant cover may have altered carbon storage and atmospheric carbon dioxide.

• Earth system scienceBroader topic: Carbon transfers couple ecosystems, oceans, climate, and geological storage.

• Edge effectsRelated: Edges can alter forest growth and decomposition, changing carbon storage and release.