User:KDS4444/Mire

A mire, sometimes called a peatland (in North America), is a wetland terrain dominated by living, peat-forming plants, although for botanists and ecologists the term peatland is technically a more universal term for any terrain dominated by peat to a depth of 30-40cm, even if it has been completely drained (i.e., a peatland can be dry, but a mire by definition is still wet). Fens and bogs are both types of mires, bogs being situated higher than the surrounding landscape on a domed-shaped landform and obtaining most of their water from rainfall (i.e., are ombrotrophic) while fens are located on slopes, flats, or depressions and get theirs from both rainfall as well as groundwater. Also, while a bog is always acidic and nutrient-poor, a fen may be either acidic or alkaline, and either nutrient-poor or nutrient-rich. A mire is distinguished from a swamp by its lack of a forest canopy (though some bogs may support limited tree or bush growth, mires are dominated by grass and mosses), and from a marsh by its water nutrients and distribution (marshes are characterized by nutrient-rich stagnant or slow-moving waters; mire waters are located mostly below the soil surface level) as well as its plant life (marsh plants are generally submerged or floating-leaved; those in a mire are not).

The reliance on rainwater for moisture means that mires are usually deficient in both oxygen and phosphorus though they my vary widely with regard to nitrogen. . These things mean that mires are a kind of "...living relic... [A] living skin on an ancient body" in which successive layers of regular plant growth and decay are preserved stratigraphically with a quality of preservation unknown in other wetland environments.