|Foliage and cones|
(Mill.) Britton, Sterns & Poggenburg
Picea mariana (black spruce) is a North American species of spruce tree in the pine family. It is widespread across Canada, found in all 10 provinces and all 3 Arctic territories. Its range extends into northern parts of the United States: in Alaska, the Great Lakes region, and the Northeast. It is a frequent part of the biome known as taiga or boreal forest.
Picea mariana is a slow-growing, small upright evergreen coniferous tree (rarely a shrub), having a straight trunk with little taper, a scruffy habit, and a narrow, pointed crown of short, compact, drooping branches with upturned tips. Through much of its range it averages 5–15 m tall with a trunk 15–50 cm diameter at maturity, though occasional specimens can reach 30 m tall and 60 cm diameter. The bark is thin, scaly, and grayish brown. The leaves are needle-like, 6–15 mm long, stiff, four-sided, dark bluish green on the upper sides, paler glaucous green below. The cones are the smallest of all of the spruces, 1.5–4 cm long and 1–2 cm broad, spindle-shaped to nearly round, dark purple ripening red-brown, produced in dense clusters in the upper crown, opening at maturity but persisting for several years.
It differs from P. glauca in having a dense cover of small hairs on the bark of young branch tips, an often darker reddish-brown bark, shorter needles, smaller and rounder cones, and a preference for wetter lowland areas. Numerous differences in details of its needle and pollen morphology also exist but require careful microscopic examination to detect. From true firs, such as Abies balsamea (Balsam Fir), it differs in having pendulous cones, persistent woody leaf-bases, and four-angled needles, arranged all round the shoots.
Due to the large difference between heartwood and sapwood moisture content, it is easy to distinguish these two wood characteristics in ultrasound images, which are widely used as a nondestructive technique to assess the internal condition of the tree and avoid useless log breakdown.
Older taxonomic synonyms include Abies mariana, Picea brevifolia, Picea nigra.
Growth varies with site quality. In swamp and muskeg it shows progressively slower growth rates from the edges toward the centre. The roots are shallow and wide spreading, resulting in susceptibility to windthrow. In the northern part of its range, ice pruned asymmetric black spruce are often seen with diminished foliage on the windward side. Tilted trees colloquially called "drunken trees" are associated with thawing of permafrost.
In the southern portion of its range it is found primarily on wet organic soils, but farther north its abundance on uplands increases. In the Great Lakes States it is most abundant in peat bogs and swamps, also on transitional sites between peatlands and uplands. In these areas it is rare on uplands, except in isolated areas of northern Minnesota and the Upper Peninsula of Michigan.
Most stands are even-aged due to frequent fire intervals in black spruce forests. It commonly grows in pure stands on organic soils and in mixed stands on mineral soils. It is tolerant of nutrient-poor soils, and is commonly found on poorly drained acidic peatlands. It is considered a climax species over most of its range; however, some ecologists question whether black spruce forests truly attain climax because fires usually occur at 50 to 150 year intervals, while "stable" conditions may not be attained for several hundred years.
The frequent fire return interval, a natural fire ecology, perpetuates numerous successional communities. Throughout boreal North America, Betula papyrifera (Paper Birch) and Populus tremuloides (Aspen|Quaking Aspen) are successional hardwoods that frequently invade burns in black spruce. Black spruce typically seeds in promptly after fire, and with the continued absence of fire, will eventually dominate the hardwoods.
It is a pioneer that invades the sedge mat in filled-lake bogs, though often preceded slightly by Larix laricina (Tamarack), with which it may in time form a stable forest cover in swamps. However, as the peat soil is gradually elevated by the accumulation of organic matter, and the fertility of the site improves, Balsam Fir and Thuja occidentalis (Eastern Arborvitae) will eventually replace black spruce and tamarack.
The larvae of the spruce budworm moth cause defoliation which will lead to death if it occurs several years in a row, though black spruce is less susceptible than white spruce or balsam fir. Trees most at risk are those growing with balsam fir and white spruce.
Uses and symbolism
The timber is of low value due to the small size of the trees, but it is an important source of pulpwood and the primary source of it in Canada. Fast-food chopsticks are often made from black spruce.
|Wikimedia Commons has media related to:|
- The Plant List Picea mariana (Mill.) Britton, Sterns & Poggenb.
- Farjon, A. (1990). Pinaceae. Drawings and Descriptions of the Genera. Koeltz Scientific Books ISBN 3-87429-298-3.
- Rushforth, K. (1987). Conifers. Helm ISBN 0-7470-2801-X.
- Gymnosperm Database: Picea mariana
- Flora of North America: Picea mariana
- Biota of North America Program 2014 state-level distribution map
- Wei, Q.; Chui, Y. H.; Leblon, B.; Zhang, S. Y. (2009). "Identification of selected internal wood characteristics in computed tomography images of black spruce: A comparison study". Journal of Wood Science 55 (3): 175. doi:10.1007/s10086-008-1013-1.
- C. Michael Hogan, Black Spruce: Picea mariana, GlobalTwitcher.com, ed. Nicklas Stromberg, November, 2008
- Kokelj, S.V.; Burn, C.R. (2003). "'Drunken forest' and near-surface ground ice in Mackenzie Delta, Northwest Territories, Canada". In Marcia Phillips, Sarah Springman, Lukas Arenson. Proceedings of the 8th Int'l Conf. on Permafrost (PDF). Rotterdam: A.A. Balkema. ISBN 9058095827. Retrieved 2 April 2013.
- "Picea mariana 'Nana' AGM". Royal Horticultural Society. Retrieved 14 February 2013.
- Powers, R.F.; Adams, M.B.; Joslin, J.D.; Fisk, J.N. (2005). "Non-Boreal Coniferous Forests of North America". In Andersson, F. Coniferous Forests (1st ed.). Amsterdam [u.a].: Elsevier. p. 271. ISBN 9780444816276.