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

• Wetland drainageRelated: Oxidation of drained peat releases carbon dioxide into the atmosphere.

• Aluminium smeltingRelated: Conventional carbon anodes generate carbon dioxide as alumina releases oxygen during reduction.

• Central Atlantic Magmatic ProvinceRelated: CAMP eruptions may have raised atmospheric carbon dioxide and driven warming.

• Atmosphere of MarsRelated: It makes up about 95 percent of Mars’s atmosphere.

• Faint young Sun paradoxRelated: Higher atmospheric concentrations could have compensated for the young Sun’s weaker output.

• KimberliteRelated: Its abundance helps distinguish kimberlite magmas and contributes to explosive ascent.

• Permafrost carbon feedbackRelated: Decomposition in oxygen-rich thawed soils releases this major greenhouse gas.

• Potassium carbonateRelated: Acids release carbon dioxide when they react with potassium carbonate.

• RuBisCORelated: It is the substrate RuBisCO incorporates into ribulose bisphosphate.

• Barium carbonateRelated: Acids release this gas when they react with barium carbonate.

• Bohr effectRelated: Rising carbon dioxide contributes to the conditions that lower hemoglobin’s oxygen affinity.

• Fossil fuel power stationRelated: Fuel combustion releases carbon dioxide, a principal driver of the station’s climate impact.

• HyperventilationRelated: Exhaling carbon dioxide faster than metabolism produces it lowers arterial levels.

• Malolactic fermentationRelated: Its release accompanies conversion of malic acid to lactic acid.

• Power-to-XRelated: Carbon-based synthetic fuels require a carbon source, often captured carbon dioxide.

• Vehicle emissionsRelated: Burning vehicle fuel releases carbon dioxide, linking transport to climate change.

• YedomaRelated: Microbial decomposition of thawed yedoma organic matter can release carbon dioxide.

• Anthropogenic climate changeRelated: Fossil-fuel use is the largest human source of this persistent warming influence.

• AutotrophRelated: It is the principal carbon input for many autotrophic pathways.

• HighballRelated: Opening and pouring release carbon dioxide, affecting a highball’s fizz.

• Volcanic outgassingRelated: It is a major volcanic gas and an important long-lived atmospheric greenhouse gas.

• Water–gas shift reactionRelated: It is the carbon-containing product formed from carbon monoxide and steam.

• Antarctic glaciationRelated: Declining atmospheric carbon dioxide contributed to the cooling that enabled major Antarctic ice growth.

• Gin and tonicRelated: Its release from tonic water creates the drink’s fizz and gradually reduces effervescence.

• Huronian glaciationRelated: Its concentration could have moderated or ended prolonged cooling through volcanic emissions and weathering feedbacks.

• Magnesium carbonateRelated: It escapes as gas during the thermal decomposition of magnesium carbonate.

• Atmosphere of VenusRelated: It makes up about 96.5% of Venus’s atmosphere and drives strong heat retention.

• BiotinRelated: Biotin-dependent enzymes transfer carbon dioxide to substrates during carboxylation.

• Copper(II) carbonateRelated: It is released when copper carbonate decomposes thermally.

• Lithium oxideRelated: It reacts with lithium oxide to form lithium carbonate.

• Mineral waterRelated: Natural or added carbon dioxide can make mineral water effervescent and alter acidity.

• Carbon-dioxide laserRelated: Its vibrational transitions provide the laser’s infrared gain.

• Marinoan glaciationRelated: Volcanic emissions could accumulate while ice limited silicate weathering, helping drive deglaciation.

• Potassium superoxideRelated: KO₂ consumes carbon dioxide while producing oxygen, a useful property in breathing systems.

• Respiratory rateRelated: Rising carbon dioxide is a major chemical signal that can increase breathing frequency.

• Ammonium carbonateRelated: It is released alongside ammonia when ammonium carbonate decomposes.

• Cameroon LineRelated: Magmatic carbon dioxide can dissolve in deep volcanic lakes and contribute to limnic eruptions.

• Manganese(II) carbonateRelated: Carbon dioxide is released when manganese carbonate reacts with acids or decomposes.

• Sodium peroxideRelated: Sodium peroxide absorbs this gas while releasing oxygen, enabling use in closed environments.

• Stone ForestRelated: Carbon dioxide in rainwater helps dissolve the limestone.

• Strecker degradationRelated: It is the gaseous product corresponding to the amino acid’s lost carboxyl carbon.

• SyngasRelated: It often accompanies syngas and can be recycled or removed during processing.

• Biological carbon fixationRelated: It is the principal inorganic carbon substrate fixed by many organisms.

• Dieng PlateauRelated: Dense volcanic emissions can collect in low places and cause suffocation.

• John Scott HaldaneRelated: His research examined its role in regulating breathing and blood acidity.

• Blood–air barrierRelated: Carbon dioxide diffuses in the opposite direction, from blood toward alveolar air.

• Calcium bicarbonateRelated: Dissolved carbon dioxide drives the formation of bicarbonate-bearing water.

• Double bond ruleRelated: It offers a familiar second-period example of stable multiple bonding.

• Flammulina filiformisRelated: Elevated carbon dioxide in cultivation encourages long, slender mushroom stems.

• K2-18bRelated: Its detection in K2-18b’s atmosphere helped constrain atmospheric models and the planet’s possible climate.