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Sphagnum is a genus of approximately 380 accepted species [2] [3] of mosses, commonly known as sphagnum moss, also bog moss and quacker moss (although that term is also sometimes used for peat). Accumulations of Sphagnum can store water, since both living and dead plants can hold large quantities of water inside their cells; plants may hold 16 ...
Sphagnum fimbriatum, the fringed bogmoss, [3] is a peat moss found in temperate regions worldwide, from the Arctic to New Zealand and along the Andes. William Wilson formally described the species in 1846. Plants measure up to 10 cm (4 in) tall, varying from slender to moderately robust forms.
Sphagnum angustifolium, the fine bogmoss, [2] is a species of peat moss with a Holarctic distribution. A member of the S. recurvum species complex within Sphagnum section Cuspidata, it is a relatively small, green to yellowish moss that grows in wet, moderately nutrient-rich mires, typically forming carpets or growing intermixed with other peat moss species.
[1] [2] Sphagnum moss, also called peat moss, is one of the most common components in peat, although many other plants can contribute. The biological features of sphagnum mosses act to create a habitat aiding peat formation, a phenomenon termed 'habitat manipulation'. [3] Soils consisting primarily of peat are known as histosols.
Sphagnum moss affects the chemistry of nearby water, which becomes highly acidic relative to a more natural environment (a pH of roughly 3.3–4.5). The concentration of dissolved minerals also tends to be low. Dying moss forms layers of sediment and releases sugars and humic acids that consume oxygen. Since the surface of the water is covered ...
Sphagnum fuscum prefers older, drier bogs to inhabit and will formulate hummocks in such conditions. In bogs dominated by black spruce, S. fuscum will form extensive ground cover. On average, S. fuscum inhabits more acidic soils with pH ranging from 3.6-7.5, and is also able to colonize at high elevations. The moss is circumpolar. [3]
Sphagnum moss affects the chemistry of nearby water, which becomes highly acidic (a pH of roughly 3.3 to 4.5) relative to a more ordinary environment. The concentration of dissolved minerals also tends to be low. Dying moss forms layers of sediment and releases sugars and humic acids which consume oxygen.
Sphagnum rubellum, commonly known as the red peat moss, [1] is a species of peat moss in the family Sphagnaceae. It forms low, reddish cushions in wet areas like bogs and poor fens across North America and Eurasia, particularly in regions with oceanic climates. The species can vary in colour from green to pink or deep crimson, and grows up to ...
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