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.

• 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.

• 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.

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

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

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

• 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.

• 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.

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

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

• 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.

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

• DetritusRelated: Detritus stores organic carbon temporarily and releases it through decomposition.

• Sulfur cycleRelated: Sulfur and carbon cycles interact through biological production, sediment burial, and atmospheric chemistry.

• AragoniteRelated: Aragonite stores carbon in shells, reefs, and marine sediments.

• Soil microbiologyRelated: Microbial decomposition determines how much soil carbon returns to the atmosphere or remains stored.

• Carbonate mineralRelated: Carbonate formation stores carbon in long-lived sedimentary minerals.

• DecomposerRelated: Decomposition returns organic carbon to soil and releases some as carbon dioxide.

• Early JurassicRelated: Carbon-isotope changes help track major Early Jurassic environmental disruptions.

• CoccolithophoreRelated: Coccolithophore photosynthesis and calcification move carbon through different ocean pools.

• Large igneous provinceRelated: Province-related carbon emissions can rapidly perturb this cycle and drive climate change.

• Social cost of carbonRelated: It determines how much of an emitted tonne remains in the atmosphere and for how long.

• Tropical deforestationRelated: Forest removal releases stored carbon and weakens a major pathway for atmospheric carbon uptake.

• Land coverRelated: Cover types differ in how much carbon they store and exchange with the atmosphere.

• PlantRelated: Plant photosynthesis removes atmospheric carbon dioxide, while decay and fires return carbon.

• Forest diebackRelated: Dead trees and reduced growth alter carbon storage and emissions from forests.

• Siberian TrapsRelated: Volcanic and thermogenic carbon inputs disrupted this cycle during the extinction interval.

• Anoxygenic photosynthesisRelated: Anoxygenic phototrophs can fix carbon and influence local carbon flows.

• Arctic methane emissionsRelated: Arctic methane emissions transfer carbon from ecosystems and geological stores into the atmosphere.

• ProterozoicRelated: Changes in carbon burial and weathering helped drive Proterozoic climate and oxygen levels.

• Biomass burningRelated: Burning rapidly transfers carbon stored in vegetation into the atmosphere.

• DeadwoodRelated: As wood decomposes, deadwood releases stored carbon and transfers it through the forest.

• Tropical rainforest climateRelated: Rainforests store carbon in vegetation and soils while exchanging carbon dioxide with the atmosphere.

• Earth scienceRelated: Carbon exchange connects climate, life, oceans, and long-term geology.

• Mesopelagic fishRelated: Their vertical movements can transport carbon from surface waters into the ocean interior.

• PaleoenvironmentRelated: Ancient carbon records reveal exchanges between environmental reservoirs over time.

• NeoproterozoicRelated: Carbon-isotope shifts in Neoproterozoic rocks help track its changing ocean chemistry.

• Tropical AmericasRelated: Tropical forests store and exchange large quantities of carbon.