Douglas fir (Fd) - Pseudotsuga menziesii
|
Page Index
External Links Other external information on Douglas fir
|
BC Distribution of Douglas fir (Fd)
![]() |
An old cohort of common douglas on a moist, rich site in the CWH zone in Coquitlam River valley
|
| Description |
Common douglas is one of the most important and valuable timber species of Western North America, as well as many other temperate forest regions in which it has been successfully introduced. It is a medium- to large-sized (reaching nearly 100 m in height), evergreen conifer, and at maturity has a moderately dense, conical crown with long branches, and deeply furrowed, dark reddish-brown bark with irregular, broad ridges.
|
|
Geographic Range
|
Geographic element: Western North American/Pacific and Cordilleran Distribution in Western North America: central and south in the Pacific region; central and south in the Cordilleran region |
Ecological Amplitudes
|
Climatic amplitude: (subalpine boreal) - montane boreal - (semiarid) - cool and warm temperate - cool (and warm) mesothermal Orographic amplitude: submontane - montane - (subalpine) Occurrence in biogeoclimatic zones: (lower southern MH), (lower southern ESSF), MS, southern SBS, (SBPS), (BG), (PP), IDF, southern ICH, CDF, southern CWH Edaphic Amplitude Range of soil moisture regimes: very dry - moderately dry - slightly dry - fresh - moist - very moist Range of soil nutrient regimes: (very poor) - poor - medium - rich - very rich It has been experimentally found that common douglas grows poorly where it is dependent only on NH4-N for its nitrogen supply, but grows best in soils that are rich in NO3-N (Garm 1958, Krajina 1969). Nitrate-poor soils are indicated by Mor humus formation and the presence of oxylophytic plants, while nitrate-rich soils are indicated by Moder and Mull humus formation and the presence of nitrophytic plants (nitrate accumulators) which have easily detectable nitrates, especially in their leaves: such as Sambucus racemosa L., Rubus spectabilis Pursh, R. parviflorus Nutt., Ribes bracteosum Dougl. ex. Hook., R. lacustre (Pers.) Poir, Adenocaulon bicolor Hook., Asarum caudatum Lindl., Athyrium filix-femina (L.) Roth, Bromus vulgaris (Hook.) Shear, Cardamine breweri S. Wats., Carex deweyana Schwein., C. hendersonii Bailey, Cinna latifolia (Trev. ex. Goepp.) Griseb, Claytonia sibirica (L.), Dicentra formosa (Andr.) Walp., Galium triflorum Michx., Geum macrophyllum Willd., Melica subulata (Griseb.) Scribn., Mitella ovalis Greene, Oenanthe sarmentosa K. Presl ex. DC., Osmorhiza chilensis Hook. & Arn., Stachys cooleyae Heller, S. mexicana, Stellaria crispa Cham. & Schlecht., Tellima grandiflora (Pursh) Dougl. ex. Lindl., Tiarella laciniata Hook., T. trifoliata L., Tolmiea menziesii (Pursh) Torr. and Gray, and Urtica dioica (L.). However, in addition to nitrates, some ammonium compounds are beneficial for common douglas as they are necessary for phosphorus to be in soluble form. Calcium deficiency is manifested in calcium-dieback of roots. However, common douglas may survive more easily than other species because it can develop new roots when older ones die. |
| Root System Characteristics | Common douglas is a deep-rooting species; however, as in many other tree species, its root morphology varies according to the nature of the soil. In deep, well-drained soils, taproots may grow up to 50% of their final depth in 3 to 5 years. Plate-like root systems develop when it grows in shallow soils or with a high water table. Fine roots are concentrated in the upper 20 cm of soil. Roots of common douglas are associated with both ecto- and endo-mycorrhizae. | ||||||||||||||||||||||||||||||||||||||||||
| Tolerances |
|
||||||||||||||||||||||||||||||||||||||||||
| top | |||||||||||||||||||||||||||||||||||||||||||
| Damaging Agents |
|
||||||||||||||||||||||||||||||||||||||||||
| Associated tree species and successional role | In British Columbia, common douglas grows in pure even-aged (usually after wildfires), uneven-aged stands, or in a great variety of mixed-species stands. It is often a pioneer species (primary succession) on colluvial sites, and is present in early, mid-, and late stages of secondary succession. It is a major or minor component in old-growth forests in boreal, cool temperate, and cool mesothermal climates. | ||||||||||||||||||||||||||||||||||||||||||
|
|||||||||||||||||||||||||||||||||||||||||||
| top | |||||||||||||||||||||||||||||||||||||||||||
| Silvical Characteristics |
|
Genetics and Notes
| Genetics |
Common douglas has two widely recognized varieties: menziesii, the green or coastal variety, and glauca, the blue or interior variety. Intravariety breeding is fairly frequent but not easily detectable morphologically. The interior variety grows more slowly than the coastal variety, both in the interior and along the coast; but the coastal variety does not survive or grows poorly in cool temperate climates. Common douglas has one of the broadest latitudinal range of any North American conifer. Thus clinal patterns of variation in growth and phenological traits have been observed over latitudinal, as well as longitudinal, and elevational transects. |
| Notes |
Common douglas is a very productive and desirable species considering its easy regeneration and good growth which remains fairly constant for a long time. More detailed silvics information is given by: Hermann, R.K. and D.P. Lavender. 1990. Pseudotsuga menziesii. Pp. 527-540 in R.M. Burns and B.H. Honkala (technical coordinators) Silvics of North America, Vol. 1. Agri. Handbook 654, USDA For. Serv., Washington, D.C. Oliver, C.D., D.P. Hanley, and J.A. Johnson. (editors) 1986. Douglas-fir: Stand management for the future. Institute of Forest Resources, Contribution No. 55, University of Washington, Seattle, Washington. 388 pp. |
