Linked from

The 10 pages that link to Anoxia, each with the reason it gives.

• PeatlandRelated: Saturated soils restrict oxygen and slow the decay of plant remains.

• Lake TanganyikaRelated: Deep water below the oxygenated upper layer is largely anoxic.

• Meromictic lakeRelated: The monimolimnion commonly becomes anoxic when it lacks exchange with surface waters.

• SphagnumRelated: Waterlogged peat restricts oxygen, slowing the decay of dead Sphagnum.

• AnaerobicRelated: It names a strict oxygen-free condition in which anaerobic processes may occur.

• Late Ordovician mass extinctionRelated: Oxygen-poor marine waters contributed to losses during the extinction’s later phase.

• Triassic–Jurassic extinctionRelated: Oxygen-poor marine waters likely intensified ecological stress during the extinction.