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Sphagnum Bog

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sphagnum bog [′sfag·nəm ′bäg]
(ecology)
A bog composed principally of mosses of the genusSphagnum(Sphagnales) but also of other plants, especially acid-tolerant species, which tend to form peat.

Sphagnum Bog 

a marsh generally located at the head of a lake and thickly covered with mosses of the genus Sphagnum, which form peat. Sphagnum bogs are often convex, because the sphagnum moss grows more abundantly in the center of the bog, where the mineral content of the water is lower. Sphagnum bogs predominate in temperate latitudes of the forest and forest-tundra zones.



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Stratigraphy: Found at the interface between fen peat and Sphagnum bog peat, always associated with Calliergon trifarium but in lesser quantity.
Palaeoecological evidence shows that in some extremely mineral-rich fens, the open mat is invaded simultaneously by trees and Sphagnum hummocks such that an open Sphagnum bog never develops (Swinehart & Parker 2000).
 
 
 
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