Linked from

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

• Red Sea coral reefsRelated: Reduced carbonate availability can make reef framework formation more difficult.

• Sagami BayRelated: It poses a broader chemical stress to shell-forming organisms in the bay.

• ShellfishRelated: Lower carbonate availability can make shell formation more difficult for some shellfish.

• South Pacific OceanRelated: The South Pacific absorbs carbon dioxide, changing conditions for marine organisms.

• Anthropogenic climate changeRelated: Human carbon dioxide emissions alter the ocean as well as the atmosphere.

• Arctic biodiversityRelated: It can challenge organisms that build shells or skeletons in Arctic waters.

• Carbon isotope excursionRelated: Acidification can accompany carbon release, but its geological evidence is indirect.

• Great AccelerationRelated: Rising emissions associated with the acceleration have altered ocean chemistry.

• Human impact on the environmentRelated: Carbon dioxide emissions alter seawater chemistry as well as the climate.

• OceanRelated: It shows how ocean chemistry responds to human-caused carbon emissions.

• Ocean conservationRelated: It threatens organisms that build shells or skeletons and requires emissions reductions.

• Phoenix IslandsRelated: More acidic seawater can make it harder for corals to build reef skeletons.

• Polar ecosystemRelated: It adds chemical stress to polar marine organisms as waters absorb carbon dioxide.

• Tide poolRelated: Acidification can challenge organisms that build calcium-carbonate shells or skeletons.

• Volcanic outgassingRelated: Geological carbon emissions can contribute to ocean acidification when atmospheric carbon dioxide rises.

• Caribbean coral reefsRelated: Lower carbonate availability can make it harder for reef corals to build skeletons.

• Climate systemRelated: It shows how atmospheric carbon changes ocean chemistry as well as temperature.

• Gulf of AlaskaRelated: Cold North Pacific waters can absorb carbon dioxide readily, challenging shell-forming organisms in the gulf.

• Luzon StraitRelated: Changing water exchange can influence how carbon-rich waters move through this marine corridor.

• Marine microbiologyRelated: Its effects on microbial physiology and biogeochemical activity remain an active research area.

• NeustonRelated: Changing carbonate chemistry can affect calcifying organisms among surface communities.

• Phoenix Islands Protected AreaRelated: Climate-driven chemistry changes threaten coral ecosystems even where fishing is restricted.

• Photic zoneRelated: Its effects on plankton and ecosystems can alter production within illuminated waters.

• RhizariaRelated: Acidification can make it harder for shell-forming foraminifera to build and maintain calcium carbonate tests.

• Sargasso SeaRelated: Changing ocean chemistry can affect the organisms and food webs sustained by this habitat.

• Shellfish aquacultureRelated: Lower carbonate availability can impair shell formation, especially during early life stages.

• AnthozoaRelated: Acidification makes it harder for many stony corals to build calcium carbonate skeletons.

• DecapodRelated: Researchers investigate how changing carbonate chemistry affects decapod shells and early development.

• HalobatesRelated: Changing ocean chemistry may alter the surface ecosystem in which Halobates feeds and reproduces.

• Mozambique ChannelRelated: Its effects on reefs and shell-forming organisms are a growing concern in channel waters.

• Alexander ArchipelagoRelated: It threatens shell-forming organisms and marine food webs around these islands.

• Geochemical cycleRelated: This change follows carbon transfer from the atmosphere into ocean reservoirs.

• HaptophyteRelated: Changing carbonate chemistry affects calcifying haptophytes and their coccolith production.

• Methane clathrateRelated: Methane oxidation in seawater can produce carbon dioxide and locally contribute to acidification.

• SnailRelated: Changing seawater chemistry can make shell formation harder for marine snails.

• Leafy seadragonRelated: Its ecological effects could alter food webs and habitat conditions in coastal waters.

• Ocean sunfishRelated: Its ecosystem effects could change food webs supporting gelatinous prey.

• Coral Sea IslandsRelated: It can make it harder for reef-building organisms to form skeletons.

• Extinction eventRelated: Rapid acidification can impair organisms that build shells or skeletons from carbonate minerals.

• Gulf of MaineRelated: Acidification affects shell-forming organisms that support gulf food webs and fisheries.

• Marine lifeRelated: Changing carbonate chemistry makes shell and skeleton formation harder for some organisms.

• Pelagic sedimentRelated: Acidification can reduce carbonate preservation in pelagic sediments.

• Sea surface microlayerRelated: Its effects on microlayer organisms and surface reactions are not fully characterized.

• SeabedRelated: Acidification can affect seabed organisms that build calcium-carbonate shells or skeletons.

• Terrestrial crabRelated: Marine larval stages may face chemical changes even when adults spend most of their lives on land.

• Calcium cycleRelated: Lower carbonate availability can hinder calcium-carbonate formation and increase shell dissolution.

• Climate variability and changeRelated: The same emissions driving warming also change ocean chemistry.

• Clione limacinaRelated: Changes in carbonate chemistry threaten the shelled pteropods that Clione eats.

• Coastal fishRelated: Changing carbonate chemistry can affect coastal food webs and fish development.

• Crested penguinRelated: It can affect marine food webs that sustain penguin prey.