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The 149 pages that link to Carbon dioxide, each with the reason it gives.

• CombustionRelated: Complete combustion of carbon-containing fuels commonly releases it.

• PhotosynthesisRelated: Photosynthesis incorporates carbon dioxide into organic molecules.

• OxygenRelated: It is a major product of oxygen-consuming metabolism and combustion, but is not itself molecular oxygen.

• Marine snowRelated: Respiration and decomposition of sinking organic matter return carbon as dissolved carbon dioxide.

• SpeleothemRelated: Carbon dioxide loss from cave water can trigger calcium carbonate precipitation.

• Carbonic acidRelated: Dissolved carbon dioxide is the precursor in the reversible reaction that forms carbonic acid.

• MesozoicRelated: Volcanism and other carbon-cycle changes influenced Mesozoic greenhouse conditions.

• Melting pointRelated: At atmospheric pressure, solid carbon dioxide sublimes instead of melting.

• Alcoholic fermentationRelated: Its release can raise bread dough and carbonate some fermented drinks.

• Carbon footprintRelated: It is the reference gas for expressing most footprint totals.

• Fossil fuelRelated: Complete combustion of fossil fuels releases carbon dioxide from geologic carbon stores.

• Deccan TrapsRelated: Deccan emissions could have driven warming during the eruptions.

• Global warmingRelated: Its persistent accumulation is the largest driver of human-caused warming.

• Cutaneous respirationRelated: Cutaneous exchange removes this metabolic waste gas from the body.

• OligoceneRelated: Changes in atmospheric carbon dioxide are central to explaining long-term Oligocene cooling.

• StomataRelated: Stomata provide the main pathway for atmospheric carbon dioxide to enter leaves.

• Sodium hydroxideRelated: It reacts with sodium hydroxide to form carbonate or bicarbonate, affecting storage and solutions.

• AlkalinityRelated: Dissolved carbon dioxide shifts carbonate speciation and changes pH without necessarily changing total alkalinity.

• CarbonRelated: This atmospheric carbon compound links fossil-fuel use to climate warming.

• ChemosynthesisRelated: It supplies the carbon that chemosynthetic pathways incorporate into organic matter.

• Sodium bicarbonateRelated: Its formation creates bubbles that expand baked mixtures and drive other bicarbonate reactions.

• Paleocene–Eocene Thermal MaximumRelated: Its rise contributed to warming and drove carbon into the ocean.

• Tracheal systemRelated: The tracheal network provides a route for carbon dioxide to leave tissues.

• GasolineRelated: Burning gasoline releases carbon dioxide from its carbon content.

• Late TriassicRelated: Volcanic carbon dioxide likely contributed to Late Triassic warming and ocean stress.

• Exoplanet atmosphereRelated: Its spectral bands can trace atmospheric chemistry and thermal structure on distant planets.

• Flood basaltRelated: Volcanic release can contribute to prolonged warming as flood-basalt activity continues.

• CarbonateRelated: Dissolved CO₂ feeds the aqueous reactions that form bicarbonate and carbonate.

• Svante ArrheniusRelated: His climate calculations examined how changing atmospheric carbon dioxide alters heat retention.

• DecarboxylationRelated: It is the usual gaseous product when a carboxyl group is removed.

• Permafrost carbon cycleRelated: Aerobic decomposition of thawed organic matter releases this long-lived greenhouse gas.

• John TyndallRelated: His experiments demonstrated that this atmospheric gas absorbs radiant heat.

• Grignard reactionRelated: Reaction with a Grignard reagent followed by acid workup produces a carboxylic acid.

• StalactiteRelated: Its escape from dripping water helps trigger calcium carbonate deposition.

• PropaneRelated: Complete combustion of propane releases carbon dioxide as a principal product.

• TravertineRelated: CO₂ loss from spring water can trigger calcium carbonate precipitation.

• Volcanic gas monitoringRelated: Its early exsolution can signal deep magma even when sulfur dioxide remains trapped.

• BiogasRelated: It commonly makes up a substantial share of raw biogas.

• Carbonate mineralRelated: Changes in dissolved CO₂ alter water acidity and carbonate mineral stability.

• Direct reduced ironRelated: The reducing agent and energy source shape the carbon dioxide emissions of DRI production.

• Leavening agentRelated: It is the main gas that chemical and biological leavening agents produce in dough.

• Natural gas processingRelated: Excess carbon dioxide lowers heating value and can create corrosion risks when water is present.

• PhotorespirationRelated: A low carbon dioxide concentration relative to oxygen makes RuBisCO more likely to initiate photorespiration.

• Baking sodaRelated: This gas forms bubbles that expand baked mixtures.

• Controlled-atmosphere storageRelated: Elevated carbon dioxide can suppress some spoilage processes but can injure sensitive produce.

• Grignard reagentRelated: Grignard reagents add to carbon dioxide to form magnesium carboxylates.

• Hall–Héroult processRelated: It forms when oxygen released from alumina reacts with the carbon anodes.

• Lake KivuRelated: Dissolved carbon dioxide contributes to the pressure and chemistry of Kivu’s deep water.

• Silicate weatheringRelated: Dissolved CO₂ forms carbonic acid and supplies carbon to the weathering pathway.

• StalagmiteRelated: Carbon dioxide loss from dripping water helps trigger calcium carbonate precipitation.