Linked from

The 16 pages that link to Oxygen minimum zone, each with the reason it gives.

• Permian–Triassic extinction eventRelated: Its ancient expansion may have brought toxic, oxygen-poor waters into shallow habitats.

• FossilizationRelated: Low oxygen can slow decay and improve the chances of preservation.

• UpwellingRelated: Upwelling can bring oxygen-poor waters toward the surface and affect coastal habitats.

• ThermoclineRelated: A strong thermocline can restrict ventilation and help maintain low-oxygen waters below it.

• Deep-sea ecologyRelated: Low-oxygen layers impose distinct constraints on deep-water communities.

• Deep seaRelated: Low-oxygen layers create distinct constraints for animals living at depth.

• Benguela CurrentRelated: Low-oxygen waters affect Benguela habitats and may expand or shift with changing conditions.

• Bathyal zoneRelated: Where it intersects bathyal depths, low oxygen limits which organisms can persist.

• Deep-sea benthosRelated: Low oxygen near some deep seafloors filters which animals can live there.

• External gillsRelated: Low oxygen availability can constrain animals that depend on water passing over gill surfaces.

• Marine benthic zoneRelated: Low oxygen in overlying water can restrict benthic animals and reshape seabed communities.

• RicefishRelated: Ricefish adaptations to oxygen-poor water are studied in relation to such low-oxygen conditions.

• Chilean SeaRelated: A pronounced oxygen minimum zone occurs off northern and central Chile.