Linked from

The 26 pages that link to Peat, each with the reason it gives.

• BryophyteRelated: Peat forms largely from Sphagnum and other plants, storing carbon in bryophyte-rich wetlands.

• Carboniferous rainforest collapseRelated: Peat formation depended on the wet environments that contracted during the collapse.

• MossRelated: Dead moss, particularly Sphagnum, is a major source of peat.

• Salt marshRelated: Roots and plant remains add organic material that can build marsh elevation.

• BogRelated: Slow decomposition lets plant remains build into the deep deposits characteristic of bogs.

• MarshRelated: Some marshes accumulate peat where plant production exceeds decomposition.

• Coal forestRelated: Peat is the precursor material from which coal can develop after burial and alteration.

• CyperaceaeRelated: Sedge-dominated wetlands can contribute plant matter to peat accumulation and carbon storage.

• Scotch whiskyRelated: Burning peat to dry malt can give Scotch whisky smoky aromas.

• Hudson Bay LowlandsRelated: Slow decomposition allows thick peat deposits to build across the lowlands.

• Great Dismal SwampRelated: Its deposits store carbon and form the swamp’s deep, combustible soils.

• MoorlandRelated: Peat soils form beneath many wet moors and store large amounts of carbon.

• Picea marianaRelated: Black spruce peatlands store carbon in slowly decomposing organic soils.

• Vasyugan SwampRelated: Centuries of peat accumulation built the swamp’s thick organic deposits.