Cap is hoof-shaped or triangular, hard and tough, and up to 30–40 x 25x 10 cm. Its surface is more or less smooth, at first orange-yellow with a white margin, later dark reddish to brown and then frequently with an orange margin. The pore surface is pale yellow to leather-brown, 3–4 pores per mm. It grows as thick shelves on live and dead coniferous or deciduous trees. The fruiting body of Fomitopsis pinicola is called the conk. It is a woody, pileate fruiting body with pores lined with basidia on its underside. As in other polypores, the fruiting body is perennial with a new layer of pores produced each year on the bottom of the old pores. The pores are whitish when young and become somewhat brownish in age. This mushroom is inedible due to its woody texture, but it is useful as tinder.
Stem decay characteristics
Most of the stem decay in mature forests that results from this fungus does not interfere with the normal growth and physiological processes of live trees since the vascular system is not affected. It is classified as a brown rot, which primarily degrades cellulose in tree stands. Wood impacted by this fungus may become more brittle and prone to breakage in high winds, and cannot be used for pulp production. This species requires exposed wood of wounds for entry, continuing their decay after the tree dies. The fruiting bodies of the fungus disperse airborne spores, but the actual degradation of the wood is by the threadlike vegetative part of the fungus inside the trees. The fungus can occur anywhere on roots or the stem, but is most common low on the bole, where frequent wounds promote infection.
Ecology
This stem decay fungi is found on live conifer trees in southeast Alaska such as Western hemlock, Mountain hemlock, White spruce, Lutz spruce and Sitka spruce. The tree stem decay is caused by the fungus when it invades and colonizes the wood of living trees and decomposes the wood before the tree is dead. This brown rot fungus degrades only cellulose, leaving the other primary constituents of wood, lignin, as a considerably less dense but fairly stable residual structure that is suitable for excavation by woodpeckers. This fungus is normally found on dead conifers, but can also be observed growing on large stem wounds, broken tops, and dead tissue of live trees. In mature forests, these stem decay fungi cause enormous annual wood volume loss of Alaska’s major tree species. Approximately one-third of the old-growth timber board-foot volume in Southeast Alaska is defective, largely due to decay from this type of fungus. Conversely, there is very little decay in young-growth stands without prevalent wounding from commercial thinning activities, wind damage, or animal feeding. By predisposing large old trees to bole breakage and windthrow, stem decays serve as important small-scale disturbance regimes in these temperate rainforest ecosystems where fire and other large-scale disturbances are uncommon. This stem decay creates canopy gaps, influences stand structure and succession, increases biodiversity, and enhances wildlife habitat. The fungus also performs essential nutrient cycling functions in these forests by decomposing stems, branches, roots, and boles of dead trees. Cavities created by the fungus in standing trees provide crucial habitat for many wildlife species including bears, voles, squirrels, and a number of bird species. The lack of disturbance in these areas and longevity of individual trees allows ample time for this slow-growing decay fungus to cause significant decay. There is a growing interest in acquiring methods to promote earlier development of stem decays in second-growth stands to achieve wildlife and other non-timber objectives.
