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  2. Peatland - Wikipedia

    en.wikipedia.org/wiki/Peatland

    A peatland is a type of wetland whose soils consist of organic matter from decaying plants, forming layers of peat. Peatlands arise because of incomplete decomposition of organic matter, usually litter from vegetation, due to water-logging and subsequent anoxia . [ 1 ]

  3. Peat - Wikipedia

    en.wikipedia.org/wiki/Peat

    The peatland ecosystem covers 3.7 million square kilometres (1.4 million square miles) [12] and is the most efficient carbon sink on the planet, [2] [13] because peatland plants capture carbon dioxide (CO 2) naturally released from the peat, maintaining an equilibrium.

  4. Muskeg - Wikipedia

    en.wikipedia.org/wiki/Muskeg

    Muskeg is approximately synonymous with bog or peatland, and is a standard term in Canada and Alaska. The term became common in these areas because it is of Cree origin; maskek (ᒪᐢᑫᐠ) meaning "low-lying marsh". [1]

  5. Fen - Wikipedia

    en.wikipedia.org/wiki/Fen

    In peatlands, including fens, primary production by plants is greater than decomposition, which results in the accumulation of organic matter as peat. Resident mosses usually carry out decomposition within the fen, and temperate fens are often driven by plant roots' decomposition. [20] These peat stores sequester an enormous amount of carbon. [19]

  6. Bog - Wikipedia

    en.wikipedia.org/wiki/Bog

    The gradual accumulation of decayed plant material in a bog functions as a carbon sink. [4] [5] Bogs occur where the water at the ground surface is acidic and low in nutrients. A bog usually is found at a freshwater soft spongy ground that is made up of decayed plant matter which is known as peat.

  7. Peat swamp forest - Wikipedia

    en.wikipedia.org/wiki/Peat_swamp_forest

    They are a kind of peatland, which store and accumulate vast amounts of carbon as soil organic matter—much more than forests on mineral soil (i.e. non-peatland) contain. Peat formation is a natural carbon sink ; because the decomposition of the organic matter is slower than its production rate, the surplus accumulates as peat.

  8. Sphagnum - Wikipedia

    en.wikipedia.org/wiki/Sphagnum

    These peat accumulations then provide habitat for a wide array of peatland plants, including sedges and ericaceous shrubs, as well as orchids and carnivorous plants. [7] [8] Sphagnum and the peat formed from it do not decay readily because of the phenolic compounds embedded in the moss's cell walls.

  9. Fen-meadow - Wikipedia

    en.wikipedia.org/wiki/Fen-meadow

    A fen-meadow is a type of peatland, common in North America and Europe, ... including plant associations such as Juncus subnodulosus-Cirsium palustre, ...

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