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The 173 pages that link to Ocean acidification, each with the reason it gives.

• Climate changeRelated: It is a direct consequence of rising atmospheric carbon dioxide, alongside warming.

• Coral reefRelated: Lower carbonate availability can make skeleton formation harder for reef-building organisms.

• Carbon dioxideRelated: Dissolved CO₂ changes seawater chemistry and reduces carbonate availability for shell-building organisms.

• pHRelated: Ocean pH tracks a major consequence of carbon dioxide entering seawater.

• SolubilityRelated: Changing seawater chemistry alters the solubility and stability of calcium carbonate minerals.

• Carbon cycleRelated: Dissolved carbon dioxide changes seawater chemistry and challenges organisms that build carbonate structures.

• Mediterranean SeaRelated: It threatens organisms that build shells or skeletons in Mediterranean waters.

• Coral bleachingRelated: This separate climate stressor can weaken reef-building alongside bleaching-related heat damage.

• Marine food webRelated: Acidification can affect organisms whose roles support or connect marine food webs.

• Calcium carbonateRelated: Lower pH reduces carbonate availability and can hinder calcium carbonate formation.

• Permian–Triassic extinction eventRelated: Volcanic carbon emissions likely lowered ocean pH and stressed marine life.

• Marine pollutionRelated: Carbon dioxide pollution changes seawater chemistry, although this process differs from waste contamination.

• Marine snowRelated: Changing carbonate chemistry may affect calcifying organisms that contribute particles to marine snow.

• Volcanic gasRelated: Volcanic carbon dioxide can acidify nearby waters, though its effects vary with scale and setting.

• Ocean deoxygenationCompared with: It is a separate ocean stressor that often occurs alongside deoxygenation and interacts with its effects.

• Intertidal zoneRelated: Acidification can hinder shell formation in intertidal mollusks and other calcifying organisms.

• PlanktonRelated: Changing carbonate chemistry can affect plankton that build shells or skeletons from calcium carbonate.

• ZooplanktonRelated: Acidification can affect calcifying zooplankton, including pteropods, and alter food-web interactions.

• Pelagic zoneRelated: Acidification alters conditions for organisms throughout the pelagic water column.

• Acid rainCompared with: It is a distinct acidification problem driven chiefly by carbon dioxide, not acid rain.

• Biogeochemical cycleRelated: It is a chemical consequence of the ocean's role in the carbon cycle.

• Marine biodiversityRelated: Acidification alters conditions for marine organisms, especially those that build shells or skeletons.

• Carbonic acidRelated: Absorbed carbon dioxide forms carbonic acid and shifts seawater carbonate equilibria.

• PhytoplanktonRelated: Acidification can alter growth and shell formation in some phytoplankton groups.

• Antarctic krillRelated: Acidification may threaten krill larvae, whose development depends on carbonate chemistry.

• Marine ecosystemRelated: Changing carbonate chemistry affects organisms that build shells and skeletons.

• Mesopelagic zoneRelated: Carbonate chemistry changes with depth, affecting organisms that pass through this layer.

• UpwellingRelated: Deep water often contains accumulated carbon dioxide, so its upwelling can lower coastal pH.

• Great Barrier ReefRelated: Acidification makes it harder for reef organisms to build calcium-carbonate structures.

• Kelp forestRelated: Changing seawater chemistry may affect kelp and the organisms around it.

• CrabRelated: Changing carbonate chemistry can make shell formation harder for crabs.

• Carbon dioxide emissionsRelated: A substantial share of emitted CO₂ enters the ocean and alters its chemistry.

• CnidariaRelated: Its effects on coral calcification vary across species and environmental conditions.

• Greenhouse gasRelated: Carbon dioxide affects oceans chemically as well as by trapping heat in the atmosphere.

• Carbon sinkRelated: Ocean uptake slows atmospheric accumulation while changing seawater chemistry.

• Ocean heat contentRelated: It is a parallel consequence of carbon emissions, though it arises from carbon chemistry rather than heat storage.

• SeafoodRelated: Acidification can impair shell formation and affect seafood-producing ecosystems.

• Ocean currentRelated: Currents redistribute dissolved carbon and influence how quickly acidification spreads through ocean waters.

• Ekman transportRelated: Upwelling can bring carbon-rich deep water to the surface, affecting local carbonate chemistry.

• Marine sedimentRelated: Changing seawater chemistry affects carbonate dissolution and preservation in marine deposits.

• AlkalinityRelated: Seawater alkalinity affects its capacity to buffer added carbon dioxide and acidity.

• Arctic sea ice declineRelated: Sea ice changes interact with regional ocean conditions, while carbon dioxide uptake drives acidification.

• CarbonRelated: Dissolved carbon dioxide alters seawater chemistry and threatens organisms that build shells.

• Ocean gyreRelated: Gyre circulation affects how carbon-rich surface waters are transported and mixed.

• OceanographyRelated: Its effects on marine organisms and ecosystems remain an active research focus.

• Sea surface temperatureCompared with: It is a separate stressor from warming, though both affect marine organisms and often co-occur.

• HydroxideRelated: Added acidity consumes carbonate and lowers seawater hydroxide concentrations.

• Ocean stratificationRelated: Stratification influences how carbon-rich surface water and deeper water are exchanged.

• Paleocene–Eocene Thermal MaximumRelated: Rapid carbon input lowered ocean pH and impaired carbonate-producing organisms.

• Late TriassicRelated: Carbon release near the boundary disrupted marine carbonate formation.