Associations
provided by BioImages, the virtual fieldguide, UK
Foodplant / sap sucker
hypophyllous Adelges cooleyi sucks sap of live branch of Pseudotsuga menziesii
Remarks: season: summer
In Great Britain and/or Ireland:
Plant / epiphyte
fruitbody of Antrodia xantha grows on stump of Pseudotsuga menziesii
Foodplant / saprobe
fruitbody of Armillaria gallica is saprobic on dead wood of Pseudotsuga menziesii
Other: minor host/prey
Foodplant / pathogen
Armillaria mellea s.l. infects and damages Pseudotsuga menziesii
Foodplant / parasite
punctiform colony of Bactrodesmium dematiaceous anamorph of Bactrodesmium obliquum var. suttonii parasitises live bark of Pseudotsuga menziesii
Foodplant / saprobe
fruitbody of Baeospora myosura is saprobic on decayed, often partly buried cone of Pseudotsuga menziesii
Foodplant / saprobe
fruitbody of Bjerkandera fumosa is saprobic on decayed wood of Pseudotsuga menziesii
Remarks: Other: uncertain
Other: minor host/prey
Plant / associate
fruitbody of Buchwaldoboletus lignicola is associated with rotting wood of Pseudotsuga menziesii
Other: major host/prey
Foodplant / saprobe
stipitate, solitary or gregarious apothecium of Ciboria rufofusca is saprobic on fallen, rotting, stromatised cone scale of Pseudotsuga menziesii
Foodplant / saprobe
Foveostroma anamorph of Dermea balsamea is saprobic on dead branch of Pseudotsuga menziesii
Foodplant / saprobe
erumpent pycnidium of Phomopsis coelomycetous anamorph of Diaporthe eres is saprobic on dead cone of Pseudotsuga menziesii
Other: minor host/prey
Foodplant / saprobe
fruitbody of Ganoderma lucidum is saprobic on dead stump of Pseudotsuga menziesii
Other: minor host/prey
Foodplant / saprobe
fruitbody of Gloeophyllum sepiarium is saprobic on dead, fallen, decayed log (large) of Pseudotsuga menziesii
Other: major host/prey
Foodplant / mycorrhiza / ectomycorrhiza
fruitbody of Gomphidius glutinosus is ectomycorrhizal with live root of Pseudotsuga menziesii
Foodplant / pathogen
Brunchorstia anamorph of Gremmeniella abietina infects and damages live twig of Pseudotsuga menziesii
Other: minor host/prey
Foodplant / saprobe
fruitbody of Hemimycena lactea is saprobic on dead debris of Pseudotsuga menziesii
Foodplant / mycorrhiza / ectomycorrhiza
fruitbody of Hygrophorus lucorum is ectomycorrhizal with live root of Pseudotsuga menziesii
Remarks: Other: uncertain
Other: minor host/prey
Foodplant / saprobe
fruitbody of Hypholoma lateritium is saprobic on dead, decayed wood of Pseudotsuga menziesii
Other: minor host/prey
Foodplant / mycorrhiza / ectomycorrhiza
fruitbody of Inocybe subcarpta is ectomycorrhizal with live root of Pseudotsuga menziesii
Remarks: Other: uncertain
Other: major host/prey
Foodplant / saprobe
fruitbody of Ischnoderma benzoinum is saprobic on dead, fallen trunk (large) of Pseudotsuga menziesii
Foodplant / saprobe
apothecium of Lachnellula calyciformis is saprobic on dead twig of Pseudotsuga menziesii
Remarks: season: 12-4
Foodplant / saprobe
fruitbody of Laetiporus sulphureus is saprobic on trunk of old tree of Pseudotsuga menziesii
Other: unusual host/prey
Plant / associate
Laricobius erichsoni is associated with Pseudotsuga menziesii
Foodplant / saprobe
fruitbody of Lepiota perplexa is saprobic on soil of tree of Pseudotsuga menziesii
Other: unusual host/prey
Foodplant / sap sucker
nymph of Leptoglossus occidentalis sucks sap of unripe seed of Pseudotsuga menziesii
Remarks: season: 5-8
Other: major host/prey
Foodplant / saprobe
fruitbody of Leucogyrophana sororia is saprobic on dead, very decayed, brown rotted bark of Pseudotsuga menziesii
Plant / associate
fruitbody of Limacella delicata var. vinosorubescens is associated with Pseudotsuga menziesii
Other: unusual host/prey
Foodplant / saprobe
fruitbody of Marasmiellus ramealis is saprobic on dead, fallen, decayed brash of Pseudotsuga menziesii
Other: major host/prey
Foodplant / parasite
amphigenous, subepidermal pycnium of Melampsora laricis-populina parasitises live leaf of Pseudotsuga menziesii
Remarks: season: 5-6
Other: uncertain
Foodplant / saprobe
stromatic, in large groups perithecium of Nectria fuckeliana is saprobic on dead branch of Pseudotsuga menziesii
Remarks: season: 3-8
Other: minor host/prey
Foodplant / saprobe
in small groups, erumpent on thin stroma perithecium of Nectria pinea is saprobic on dead branch of Pseudotsuga menziesii
Remarks: season: 9-5
Other: minor host/prey
Foodplant / saprobe
erumpent, solitary or clustered apothecium of Pezicula livida is saprobic on dead, fallen cone of Pseudotsuga menziesii
Remarks: season: 1-12
Other: minor host/prey
Foodplant / saprobe
immersed, partially erumpent pycnidium of Phomopsis coelomycetous anamorph of Phacidiopycnis pseudotsugae is saprobic on dead trunk of Pseudotsuga menziesii
Foodplant / parasite
hypophyllous, superficial pseudothecium of Phaeocryptopus gaeumannii parasitises live leaf of Pseudotsuga menziesii
Remarks: season: 6-7
Foodplant / pathogen
fruitbody of Phaeolus schweinitzii infects and damages live root of mature tree of Pseudotsuga menziesii
Other: minor host/prey
Foodplant / saprobe
fruitbody of Phanerochaete radicata is saprobic on dead, decayed wood of Pseudotsuga menziesii
Other: major host/prey
Foodplant / saprobe
fruitbody of Phellinus ferreus is saprobic on dead, fallen trunk of Pseudotsuga menziesii
Other: unusual host/prey
Foodplant / saprobe
fruitbody of Pleurocybella porrigens is saprobic on dead, decayed wood of Pseudotsuga menziesii
Other: minor host/prey
Foodplant / mycorrhiza / ectomycorrhiza
fruitbody of Porphyrellus porphyrosporus is ectomycorrhizal with live root of Pseudotsuga menziesii
Remarks: Other: uncertain
Other: unusual host/prey
Foodplant / saprobe
fruitbody of Postia placenta is saprobic on dead, decayed wood of Pseudotsuga menziesii
Other: minor host/prey
Foodplant / saprobe
fruitbody of Postia sericeomollis is saprobic on dead, decayed trunk (large) of Pseudotsuga menziesii
Other: minor host/prey
Foodplant / saprobe
fruitbody of Postia stiptica is saprobic on dead, decayed log (large) cut end of Pseudotsuga menziesii
Other: major host/prey
Foodplant / saprobe
fruitbody of Resinicium bicolor is saprobic on dead, decayed wood of Pseudotsuga menziesii
Other: major host/prey
Foodplant / parasite
in rows, subepidermal, opening by epidermis folding back apothecium of Rhabdocline pseudotsugae parasitises live leaf of Pseudotsuga menziesii
Remarks: season: 5-7
Foodplant / mycorrhiza / ectomycorrhiza
subhypogeous fruitbody of Rhizopogon villosulus is ectomycorrhizal with live root of Pseudotsuga menziesii
Remarks: Other: uncertain
Other: major host/prey
Foodplant / mycorrhiza / ectomycorrhiza
hypogeous fruitbody of Rhizopogon vinicolor is ectomycorrhizal with live root of Pseudotsuga menziesii
Remarks: Other: uncertain
Foodplant / saprobe
superficial, clustered, hypophyllous pycnidium of Rhizosphaera coelomycetous anamorph of Rhizosphaera kalkhoffii is saprobic on dead needle of Pseudotsuga menziesii
Remarks: season: late winter to early spring
Foodplant / mycorrhiza / ectomycorrhiza
fruitbody of Russula albonigra is ectomycorrhizal with live root of Pseudotsuga menziesii
Remarks: Other: uncertain
Other: minor host/prey
Foodplant / mycorrhiza / ectomycorrhiza
fruitbody of Russula delica is ectomycorrhizal with live root of Pseudotsuga menziesii
Remarks: Other: uncertain
Other: minor host/prey
Foodplant / saprobe
conidioma of Pycnidiella coelomycetous anamorph of Sarea resinae is saprobic on resinous exudate of Pseudotsuga menziesii
Remarks: season: 1-12
Other: minor host/prey
Foodplant / saprobe
fruitbody of Serpula himantioides is saprobic on dead, decayed wood of Pseudotsuga menziesii
Other: major host/prey
Foodplant / saprobe
conidioma of Sirococcus coelomycetous anamorph of Sirococcus conigenus is saprobic on fallen cone of Pseudotsuga menziesii
Other: minor host/prey
Foodplant / saprobe
effuse colony of Spadicoides dematiaceous anamorph of Spadicoides atra is saprobic on dead wood of Pseudotsuga menziesii
Foodplant / saprobe
fruitbody of Sparassis crispa is saprobic on dead root of Pseudotsuga menziesii
Other: minor host/prey
Foodplant / pathogen
erumpent pycnidium of Sphaeropsis coelomycetous anamorph of Sphaeropsis sapinea infects and damages live twig of Pseudotsuga menziesii
Remarks: season: 10-4
Other: minor host/prey
Foodplant / saprobe
immersed, becoming erumpeny conidioma of Strasseria coelomycetous anamorph of Strasseria geniculata is saprobic on dead twig of Pseudotsuga menziesii
Remarks: season: 1-5
Other: minor host/prey
Foodplant / saprobe
long-rooted fruitbody of Strobilurus esculentus is saprobic on buried, partially decayed cone of Pseudotsuga menziesii
Remarks: season: spring
Other: unusual host/prey
Foodplant / mycorrhiza / ectomycorrhiza
fruitbody of Suillus lakei is ectomycorrhizal with live root of Pseudotsuga menziesii
Plant / associate
fruitbody of Tephrocybe cessans is associated with Pseudotsuga menziesii
Foodplant / saprobe
effuse colony of Thysanophora dematiaceous anamorph of Thysanophora penicillioides is saprobic on dead, rotting, fallen needle of Pseudotsuga menziesii
Other: minor host/prey
Foodplant / saprobe
erumpent coelomycetous anamorph of Tryblidiopsis pinastri is saprobic on dead, attached twig of Pseudotsuga menziesii
Remarks: season: 1-4
Comments
provided by eFloras
Pseudotsuga menziesii is a most important timber tree, valued in both the Old and New worlds. The two intergrading varieties are sympatric in southern British Columbia and northeastern Washington.
Douglas-fir ( Pseudotsuga menziesii ) is the state tree of Oregon.
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Description
provided by eFloras
Trees to 100 m tall; trunk to 4 m d.b.h. in native range; bark dark gray-brown or blackish green, smooth, with resin blisters, aging rough and scaly with deep longitudinal fissures; branchlets initially light yellow, becoming red-brown when dry, slightly pubescent. Leaves dark green adaxially, linear, 1.5-3 cm × 1-2 mm, stomatal bands 2, abaxial, white, apex obtuse or acuminate. Seed cones brown, glossy, ellipsoid-ovoid, ca. 8 × 3.5-4 cm. Seed scales ± rhombic, 2-2.5 × 2-2.5 cm, as long as or longer than wide. Bracts exserted, longer than seed scales, cusp straight or reflexed, 6-10 mm, tapering at apex, lateral lobes wide and short, denticulate at margin.
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Description
provided by eFloras
Trees to 90(--100)m; trunk to 4.4m diam.; crown narrow to broadly conic, flattened in age. Twigs slender, pubescent, becoming glabrous with age. Leaves 15--30(--40) × 1--1.5mm, yellow-green to dark or bluish green, apex obtuse to acute. Pollen cones yellow-red. Seed cones 4--10 × 3--3.5cm. Seeds 5--6mm, wing longer than seed body.
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Habitat & Distribution
provided by eFloras
Cultivated. Beijing Shi, Jiangxi (Lu Shan) [native to W Canada, Mexico, W United States]
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Synonym
provided by eFloras
Abies menziesii Mirbel, Mem. Mus. Hist. Nat. 13: 70. 1825; Abies taxifolia Lambert (1803), not Salisbury (1796); Pinus douglasii Sabine ex D. Don; Pseudotsuga douglasii (Sabine ex D. Don) Carriere; P. taxifolia (Lambert) Britton.
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Synonym
provided by eFloras
Abies menziesii Mirbel, Mém. Mus. Hist. Nat. 13: 63, 70. 1825; A. mucronata Rafinesque; A. taxifolia Poiret 1805, not Desfontaines 1804; Pinus taxifolia Lambert 1803, not Salisbury 1796; Pseudotsuga douglasii (Lindley) Carrière; P. mucronata (Rafinesque) Sudworth; P. taxifolia (Lambert) Britton
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Associated Forest Cover
provided by Silvics of North America
Periodic recurrence of catastrophic wildfires created vast, almost pure
stands of coastal Douglas-fir throughout its range north of the Umpqua
River in Oregon. Although logging has mainly eliminated the original
old-growth forest, clearcutting combined with slash burning has helped
maintain Douglas-fir as the major component in second-growth stands. Where
regeneration of Douglas-fir was only partially successful or failed, red
alder (Alnus rubra) has become an associate of Douglas-fir or has
replaced it altogether.
Rocky Mountain Douglas-fir grows in extensive pure stands, uneven- and
even-aged, in southern Idaho and northern Utah and in western Montana as a
broad belt between ponderosa pine and spruce-fir zones. At high elevations
or northerly latitudes, more cold-tolerant mountain hemlock (Tsuga
mertensiana), whitebark pine (Pinus albicaulis), true firs
(Abies spp.), Engelmann spruce (Picea engelmannii),
western white pine (Pinus monticola), and lodgepole pine (Pinus
contorta) gradually replace Douglas-fir. Douglas-fir yields to
ponderosa pine (P. ponderosa), incense-cedar (Libocedrus
decurrens), Oregon white oak Quercus garryana), California
black oak (Q. kelloggii), canyon live oak (Q. chrysolepis),
and interior live oak (Q. wislizeni) on droughty sites, and to
western redcedar (Thuja plicata), maples (Acer spp.),
red alder, black cottonwood (Populus trichocarpa), and other
broad-leaved species on poorly drained sites.
Toward the fog belt of the Pacific coast, Douglas-fir gives way to Sitka
spruce (Picea sitchensis), western hemlock (Tsuga
heterophylla), and western redcedar. The variety menziesii is a major
component of four forest cover types (20): Pacific Douglas-Fir (Society of
American Foresters Type 229), Douglas-Fir-Western Hemlock (Type 230), Port
Orford-Cedar (Type 231), and Pacific Ponderosa Pine-Douglas-Fir (Type
244). It is a minor component of the following types:
221 Red Alder
223 Sitka Spruce
224 Western Hemlock
225 Western Hemlock-Sitka Spruce
226 Coastal True Fir-Hemlock
227 Western Redcedar-Western Hemlock
228 Western Redcedar
232 Redwood
233 Oregon White Oak
234 Douglas-Fir-Tanoak-Pacific Madrone
The variety glauca is a principal species in three forest cover
types: Interior Douglas-Fir (Type 210), Western Larch (Type 212), and
Grand Fir (Type 213). It is a minor species in five types: Engelmann
Spruce-Subalpine Fir (Type 206), White Fir (Type 211), Western White Pine
(Type 215), Aspen (Type 217), and Lodgepole Pine (Type 218).
Wherever Douglas-fir grows in mixture with other species, the proportion
may vary greatly, depending on aspect, elevation, kind of soil, and the
past history of an area, especially as it relates to fire. This is
particularly true of the mixed conifer stands in the southern Rocky
Mountains where Douglas-fir is associated with ponderosa pine,
southwestern white pine (Pinus strobiformis), corkbark fir (Abies
lasiocarpa var. arizonica), white fir (Abies concolor),
blue spruce (Picea pungens), Engelmann spruce, and aspen (Populus
spp.).
The most important shrubs associated with coastal Douglas-fir (21)
through its central and northern range are vine maple (Acer
circinatum), salal (Gaultheria shallon), Pacific rhododendron
(Rhododendron macrophyllum), Oregongrape (Berberis nervosa),
red huckleberry (Vaccinium parvifolium), and salmonberry (Rubus
spectabilis). Toward the drier southern end of its range, common shrub
associates are California hazel (Corylus cornuta var. californica),
oceanspray (Holodiscus discolor), creeping snowberry (Symphoricarpos
mollis), western poison-oak (Toxicodendron diversilobum), ceanothus
(Ceanothus spp.), and manzanita (Arctostaphylos spp.).
Principal understory species associated with variety glauca differ
within its range (3). In the northern part, they are common snowberry (Symphoricarpos
albus), white spirea (Spirea betulifolia), ninebark (Physocarpus
malvaceus), and pachistima (Pachistima myrsinites). In the
central part, they are true mountain-mahogany (Cercocarpus montanus),
squaw currant (Ribes cereum), chokeberry (Prunus
virginiana), big sagebrush (Artemisia tridentata), western
serviceberry (Amelanchier alnifolia), and bush rockspirea (Holodiscus
dumosus); in the southern part they are New Mexico locust (Robinia
neomexicana), Rocky Mountain maple (Acer glabrum), and
oceanspray (3).
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Climate
provided by Silvics of North America
Douglas-fir grows under a wide variety of climatic conditions (table 1).
The coastal region of the Pacific Northwest has a maritime climate
characterized by mild, wet winters and cool, relatively dry summers, a
long frost-free season, and narrow diurnal fluctuations of temperature (6°
to 8° C; 43° to 46° F). Precipitation, mostly as rain, is
concentrated in the winter months. Climate in the Cascade Range and Sierra
Nevada tends to be more severe.
Table 1- Climatic data for five regional subdivisions of
the range of Douglas-fir (6,62)
Mean temperature
Mean precipitation
Region
July
January
Frost-free period
Annual
Snow fall
°C
°C
days
mm
cm
Pacific Northwest
Coastal
20 to 27
-2 to 3
195 to 260
760 to 3400
0 to 60
Cascades and
Sierra Nevada
22 to 30
-9 to 3
80 to 180
610 to 3050
10 to 300
Rocky Mountains
Northern
14 to 20
-7 to 3
60 to 120
560 to 1020
40 to 580
Central
14 to 21
-9 to -6
65 to 130
360 to 610
50 to 460
Southern
7 to 11
0 to 2
50 to 110
410 to 760
180 to 300
°F
°F
days
in
in
Pacific Northwest
Coastal
68 to 81
28 to 37
195 to 260
34 to 134
0 to 24
Cascades and
Sierra Nevada
72 to 86
15 to 28
80 to 180
24 to 120
4 to 120
Rocky Mountains
Northern
57 to 68
19 to 28
60 to 120
22 to 40
16 to 320
Central
57 to 70
16 to 22
65 to 130
14 to 24
20 to 180
Southern
45 to 52
32 to 36
50 to 110
16 to 30
70 to 120
Altitude has a significant effect on local climate. In general,
temperature decreases and precipitation increases with increasing
elevation on both western and eastern slopes of the mountains. Winters are
colder, frost-free seasons are shorter, and diurnal fluctuations of
temperature are larger (10° to 16° C; 50° to 61° F).
Much of the precipitation is snow. In the northern Rocky Mountains,
Douglas-fir grows in a climate with a marked maritime influence. Mild
continental climate prevails in all seasons, except midsummer.
Precipitation is evenly distributed throughout the year, except for a dry
period in July and August. In the central Rocky Mountains, the climate is
continental. Winters are long and severe; summers are hot and in some
parts of the region, very dry. Annual precipitation, higher on the western
sides of the mountains, is mainly snow. Rainfall patterns for the southern
Rocky Mountains generally show low winter precipitation east of the
Continental Divide but high precipitation during the growing season. West
of the Continental Divide, the rainfall is more evenly divided between
winter and summer. Frost may occur in any month in the northern part of
the range. Length of frost-free periods, however, varies within the
central and southern Rocky Mountain regions, even at the same elevations.
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Damaging Agents
provided by Silvics of North America
From seed to maturity, Douglas-fir is subject
to serious damage from a variety of agents. Douglas-fir is host to
hundreds of fungi, but relatively few of these cause serious problems.
Various species of Pythium, Rhizoctonia, Phytophthora, Fusarium, and
Botrytis may cause significant losses of seedlings in nurseries
(58,60), whereas Rhizina undulata, shoestring root rot (Armillaria
mellea), and laminated root rot (Phellinus weirii) have caused
significant damage in plantations. In fact, the latter two fungi represent
a serious threat to management of young-growth stands of Douglas-fir,
especially west of the summit of the Cascades. Trees die or are so
weakened that they are blown over. Effective control measures are not
available. Of the many heart rot fungi (more than 300) attacking
Douglas-fir, the most damaging and widespread is red ring rot (Phellinus
pini). Knots and scars resulting from fire, lightning, and falling
trees are the main courts of infection. Losses from this heart rot far
exceed those from any other decay. Other important heart rot fungi in the
Pacific Northwest are Fomitopsis officinalis, F. cajanderi, and
Phaeolus schweinitzii (28). In the Southwest, Echinodontium
tinctorium, Fomitopsis cajanderi, and F. pinicola are
important.
Several needle diseases occur on Douglas-fir. The most conspicuous, a
needlecast, is caused by Rhabdocline pseudotsugae. It is mainly a
disease of younger trees, reaching damaging proportions only after
prolonged periods of rain while the new needles are appearing. The
interior variety is particularly susceptible to the disease but is less
often exposed to long periods of rain during the spring growth period.
The most damaging stem disease of Douglas-fir is Arceuthobium
douglasii. This dwarf mistletoe occurs throughout most of the range of
Douglas-fir (26).
Over 60 species of insects are indigenous to Douglas-fir cones, but only
a few species damage a significant proportion of the seed crop. Damage by
insects is frequently more pronounced during the years of light or medium
seed crops that may follow good or heavy crops.
The most destructive insects include: (a) the Douglas-fir seed chalcid
(Megastigmus spermotrophus), which matures in the developing seed
and gives no external sign of its presence; (b) the Douglas-fir cone moth
(Barbara colfaxiana) and the fir cone worm (Dioryctria
abietivorella) whose larvae bore indiscriminately through the
developing cones and may leave external particles of frass; and (c) the
Douglas-fir cone gall midge (Contarinia oregonensis) and cone
scale midge (C. washingtonensis), which destroy some seed but
prevent harvest of many more by causing galls that prevent normal opening
of cones. The Douglas-fir cone moth is perhaps a more serious pest in the
drier, interior portions of the Douglas-fir range and the Contarinia
spp.in the wetter regions. Any of these insects, however, may
effectively destroy a cone crop in a given location (27).
Insects are generally not a severe problem for Douglas-fir regeneration,
although both the strawberry root weevil (Otiorhynchus oratus) and
cranberry girdler (Chrysoteuchia topiaria) may cause significant
damage to seedlings in nurseries; damage to plantations by rain beetles
(Pleocoma spp.) and weevils (Steremnius carinatus)- the
latter particularly damaging to container-grown-plants-has been reported.
The Douglas-fir tussock moth (Orgyia pseudotsugata) and the
western spruce budworm (Choristoneura fumiferana) are the most
important insect enemies of Douglas-fir. Both insects attack trees of all
ages at periodic intervals throughout the range of interior Douglas-fir,
often resulting in severe defoliation of stands. The Douglas-fir beetle
(Dendroctonus pseudotsugae) is a destructive insect pest in
old-growth stands of coastal and interior Douglas-fir. Its impact is
diminishing, however, with the change to second-growth management and
rotations of less than 100 years (24).
Consumption of Douglas-fir seeds by small forest mammals such as
white-footed deer mice, creeping voles, chipmunks, and shrews, and birds
such as juncos, varied thrush, blue and ruffed grouse, and song sparrows
further reduces seed quantity. A single deer mouse may devour 350
Douglas-fir seeds in a single night. Mouse populations of 7 to 12/ha (3 to
5/acre) are not uncommon. Most seedfall occurs at least 150 days before
the germination period, so this single rodent species has the capacity to
destroy the great majority of natural seedfall. Spot seeding studies in
the Western United States have clearly demonstrated that forest mammals
destroy virtually all unprotected seed.
Browsing and clipping by hares, brush rabbits, mountain beaver, pocket
gophers, deer, and elk often injure seedlings and saplings. Recent reports
have indicated that such damage in western Oregon and Washington may
strongly affect seedling survival in many plantations (7,61). In drier
areas, domestic livestock have caused considerable damage to variety glauca
plantations by grazing and trampling seedlings. In pole-sized timber,
bears sometimes deform and even kill young trees by stripping off the bark
and cambium.
High winds following heavy rains occasionally cause heavy losses from
blowdown in the Pacific Northwest. Heavy snow and ice storms periodically
break the tops of scattered trees in dense young stands. Crown fires, when
they occur, destroy stands of all ages. The thick bark of older
Douglas-firs, however, makes them fairly resistant to ground fires.
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Flowering and Fruiting
provided by Silvics of North America
Douglas-fir is monoecious; trees
commonly begin to produce strobili at 12 to 15 years of age, although
observations of younger seedlings bearing ovulate strobili have been
reported.
Primordia of both pollen and seed cone buds are present when the
vegetative bud breaks in the spring of the year before the cone crop. But
neither can be distinguished from primordia of vegetative buds for the
first 10 weeks of their existence. By mid-June, histochemical differences
separate the pollen cone primordia, which are usually clustered near the
base of the extending shoot, from the seed cone primordia, which are borne
singly near the acropetal end of the shoot, and from the vegetative bud
primordia (5). These three primordia may be microscopically identified in
mid-July; by September, the egg-shaped pollen cone buds are easily
distinguished by the naked eye from the darker vegetative buds and the
larger seed cone buds.
The size of the cone crop is determined by the number of primordia that
differentiate and develop into buds, not by the number formed. Poor cone
crops, then, reflect a high abortion rate of primordia the preceding year.
Large numbers of pollen or seed cone buds in the fall merely indicate the
potential for a heavy cone crop the following year. Damaging frost during
cone anthesis or depredations by insects may destroy most of the cones and
seeds before they mature (19).
Male strobili are about 2 cm (0.8 in) long and range from yellow to deep
red. Female strobili are about 3 cm (1.2 in) long and range from deep
green to deep red (45). They have large trident bracts and are receptive
to pollination soon after emergence.
Anthesis and pollination of variety menziesii occur during March
and April in the warmer part of the range and as late as May or early June
in the colder areas. At low and middle elevations, Douglas-fir cones
mature and seeds ripen from mid-August in southern Oregon to mid-September
in northern Washington and southern British Columbia. Mature cones are 8
to 10 cm (3 to 4 in) long. The bracts turn brown when seeds are mature
(45). Seedfall occurs soon after cone maturity with, generally, two-thirds
of the total crop on the ground by the end of October. The remaining seeds
fall during winter and spring months. In British Columbia, seedfall starts
later and lasts longer-less than half the seeds fall by late October and
more than one-third fall after March 1. In general, Douglas-fir seedfall
in the fog belt of western North America is more protracted than in the
drier areas east of the summit of the Coast Ranges.
The phenology of flowering is similar for variety glauca; early
flowering occurs in mid-April to early May in Colorado and as late as
early May to late June in northern Idaho. Cone ripening varies from late
July at the lower elevations (about 850 m or 2,800 ft) in Montana to
mid-August in northern Idaho. Seed dispersal of glauca begins in
mid-August in central Oregon and occurs as late as mid-September at higher
elevations (about 1710 m or 5,600 ft) in Montana (45).
Seed quality varies during the seedfall period. It is high in the fall
but declines rapidly during winter and spring. This pattern probably
reflects the fact that cone scales in the center of the cone, where the
highest quality seed are borne, open early and scales at the tip and base
of the cone, which bear generally poorly formed seeds, open late.
Both cones and seeds vary greatly in size; the smaller seeds (about
132,000/kg or 60,000/lb) occur on trees in British Columbia and the larger
seeds (about 51,000/kg or 23,000/lb), on trees in California. Seeds of
variety glauca are slightly heavier and more triangular in shape
than seeds of menziesii. Size is determined before fertilization,
so there is no correlation between weight of seed and genetic vigor,
although seedlings germinated from heavier seeds may be slightly larger
the first few months of growth than those grown from lighter seeds.
Because the range in seed size from any one tree is relatively small,
however, fractionation of seed lots to segregate the heavier seed may
reduce the genetic variation and actually eliminate traits from certain
populations.
Douglas-fir seed crops occur at irregular intervals- one heavy and one
medium crop every 7 years on the average; however, even during heavy seed
years, only about 25 percent of the trees produce an appreciable number of
cones (34). Trees 200 to 300 years old produce the greatest number of
cones. For example, a stand of old-growth Douglas-fir may produce 20 to 30
times the number of cones per hectare that a second-growth stand 50 to 100
years old produces.
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Genetics
provided by Silvics of North America
The genus Pseudotsuga includes two species (P. menziesii
and P. macrocarpa) indigenous to North America and five
species native to Asia. All except P. menziesii have a karyotype
of 2N=24, the number of chromosomes characteristic of Pinaceae. But the
Douglas-fir karyotype is 2N=26, a probable reason for the general failure
of hybridization trials with this species (56).
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Growth and Yield
provided by Silvics of North America
Natural stands of coastal Douglas-fir normally
start with more than 2,500 trees per hectare (1,000/acre). Planted stands
generally have between 750 and 1,500/ha (300 and 600/acre) at the
beginning (9). Annual height increment is relatively slow the first 5
years but then begins to accelerate. Coastal Douglas-fir attains the
largest height increments between 20 and 30 years of age but retains the
ability to maintain a fairly rapid rate of height growth over a long
period. Douglas-fir in high-elevation forests of the Oregon-Washington
Cascade Range can continue height growth at a substantial rate for more
than 200 years (15). Height growth of Douglas-fir on dry sites at mid-site
indices in the Cascade Range of western Oregon is similar to that of
upper-slope Douglas-fir in the Washington and Oregon Cascade Range. At
higher site indices, however, height growth on dry sites is initially
faster but slower later in life; at lower site indices, it is initially
slower but faster later in life (40).
On a medium site (III) at low elevations, height growth, which averages
61 cm (24 in) annually at age 30, continues at a rate of 15 cm (6 in) per
year at age 100, and 9 cm (3.6 in) at age 120 (18,39). Trees 150 to 180 cm
(60 to 72 in) in diameter and 76 m (250 ft) in height are common in
old-growth forests (22). The tallest tree on record, found near Little
Rock, WA, was 100.5 m (330 ft) tall and had a diameter of 182 cm (71.6
in). Coastal Douglas-fir is very long lived; ages in excess of 500 years
are not uncommon and some have exceeded 1,000 years. The oldest
Douglas-fir of which there is an authentic record stood about 48 km (30
mi) east of Mount Vernon, WA. It was slightly more than 1,400 years old
when cut (39).
Information about yields of coastal Douglas-fir under intensive
management for an entire rotation is still limited. It is therefore
necessary to rely either on estimates based on yields from unmanaged
stands, or on yields from intensively managed stands in regions where
Douglas-fir has been introduced as an exotic (12), or on growth models
(16). If measured in cubic volume of wood produced, range in productivity
between the best and poorest sites is more than 250 percent. Depending on
site quality, mean annual net increments at age 50 vary from 3.7 to 13.4 m³/ha
(53 to 191 ft³/acre) in unmanaged stands (39). Estimates of gross
yields may increase these values as much as 80 percent, depending on
mensurational techniques and assumptions. Comparisons of gross yields from
unmanaged stands with those from managed stands of the same site indexes
in Europe and New Zealand suggest that yields in managed stands will be
considerably higher than would be indicated by estimates based on yields
in unmanaged stands. Presumably, managed stands of coastal Douglas-fir can
produce mean annual increments of 7 m³/ha (100 ft³/acre) on poor
sites and exceed 28 m³/ha (400 ft³/acre) on the highest sites
under rotations between 50 and 80 years (55). Although information on
productivity of Douglas-fir in terms of total biomass production is still
limited, indications are that it may reach 1000 t/ha (447 tons/acre) on
high sites (22).
The interior variety of Douglas-fir does not attain the growth rates,
dimensions, or age of the coastal variety. Site class for Rocky Mountain
Douglas-fir is usually IV or V (site index 24 to 37 m or 80 to 120 ft at
age 100) when compared with the growth of this species in the Pacific
Northwest (1,43). On low sites, growth is sometimes so slow that trees do
not reach saw-log size before old age and decadence overtake them.
Interior Douglas-fir reaches an average height of 30 to 37 m (100 to 120
ft) with a d.b.h. between 38 and 102 cm (15 and 40 in) in 200 to 300
years. On the best sites, dominant trees may attain a height of 49 m (160
ft) and a d.b.h. of 152 cm (60 in) (23). Diameter growth becomes extremely
slow and height growth practically ceases after age 200. Interior
Douglas-fir, however, appears capable of response to release by
accelerated diameter growth at any size or age (35). The interior variety
is not as long lived as the coastal variety and rarely lives more than 400
years, although more than 700 annual rings have been counted on stumps
(23).
Gross volume yields for Douglas-fir east of the Cascades in Oregon and
Washington range from 311 m³/ha (4,442 ft³/acre) for site index
15.2 m or 50 ft (at age 50) to 1523 m³/ha (21,759 ft³/acre) for
site index 33.5 m (110 ft) (14). In the northern Rocky Mountains,
estimates of yield capabilities of habitat types where Douglas-fir is
climax range from about 1.4 to 7 m³/ha (20 to 100 ft³/acre) per
year to more than 9.8 m³/ha (140 ft³/acre) per year in some of
the more moist habitat types where Douglas-fir is seral (46).
Information on yields of Douglas-fir in the southern Rocky Mountain
region is scant. In New Mexico, a virgin stand of Douglas-fir (61 percent)
and associated species averaged 182 m³/ha (13,000 fbm/acre).
Occasionally, stands yield as high as 840 m³/ha (60,000 fbm/acre).
Annual growth rates from 2.0 to 3.9 m³/ha (140 to 280 fbm/acre) after
partial cutting have been reported in New Mexico (17).
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Reaction to Competition
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Except in its youth, when it is
reasonably tolerant of shade, coastal Douglas-fir is classed as
intermediate in overall shade tolerance, below most of its common
associates in tolerance to shade (42). Of these associates, ponderosa
pine, Jeffrey pine (Pinus jeffreyi), incense-cedar, noble fir (Abies
procera), and red alder are more demanding of light. In its interior
range, Douglas-fir ranks intermediate in tolerance among its associates,
being more tolerant than western larch, ponderosa pine, lodgepole pine,
southwestern white pine, and aspen (23).
The coastal variety is a seral species, except on extremely dry sites in
southwestern Oregon and northern California. In its interior range,
Douglas-fir is both a climax and a seral species. In the northern Rocky
Mountains, it replaces ponderosa pine, lodgepole pine, and western larch
above the ponderosa pine belt, and in turn is replaced by western
redcedar, western hemlock, Engelmann spruce, grand fir, and subalpine fir
on cooler and wetter sites. In the southern Rocky Mountains, Douglas-fir
is a climax species in several habitat types of mixed conifer forest and a
seral species in the spruce-fir forests (4).
The natural occurrence of Douglas-fir in extensive stands is mainly a
consequence of forest fires. The species' rapid growth and longevity, the
thick corky bark of its lower boles and main roots, combined with its
capacity to form adventitious roots, are the main adaptations that have
enabled Douglas-fir to survive less fire-resistant associates and to
remain a dominant element in western forests. Without fire or other
drastic disturbance, Douglas-fir would gradually be replaced throughout
much of its range by the more tolerant hemlock, cedar, and true fir.
Old-growth forests of Douglas-fir tend to show wide ranges in age
structure-rather than being even-aged- which indicates that Douglas-fir
was not established over short periods after major fires or other
disturbances (22).
Stands of vigorous Douglas-fir can be successfully regenerated by any of
the even-aged methods. Clear cutting in combination with planting is the
most widely used method. In stands infected with dwarf mistletoe (Arceuthobium
spp.), clearcutting is the best alternative for eliminating
the disease. If clearcutting on good sites results in establishment of red
alder, Douglas-fir is at a severe disadvantage. Alder has very rapid
juvenile growth on high sites and can easily over top and suppress
Douglas-fir. If Douglas-fir is released in time, however, its subsequent
development will actually benefit from the nitrogen fixed by red alder.
Nitrogen is the only nutrient in forest soils of the Pacific Northwest
(41) and Intermountain Northwest (44) that has been shown to be limiting
to growth of Douglas-fir.
Because of its ability to tolerate shade in the seedling stage, the
shelterwood system is a feasible alternative to clearcutting in coastal
stands (64). Shelterwood cutting has been practiced only on a limited
scale in the Pacific Northwest, however, where the large dimensions of
old-growth timber, danger of blowdown to the residual stand, and
probability of brush encroachment limit its use. In the Rocky Mountains,
shelterwood cutting has been more commonly applied and with good results
(50). Where interior Douglas-fir is climax, the true selection method can
be used. It is unsuitable for coastal Douglas-fir.
Although Douglas-fir may be regenerated either naturally or artificially
from seed, the erratic spacing characteristic of many naturally
regenerated stands and the general lack of reliability of this system have
resulted in legislation (Forestry Practices Acts) in Washington, Oregon,
and California that virtually mandates artificial regeneration. And,
because direct seeding also produces variable results, the regeneration
system uses 2-year-old bare root seedlings, 3-year-old transplants,
year-old container-grown seedlings, or 2-year-old transplants that were
grown the first year in containers (9). Such planting stock may be
affected by agents discussed here under the heading "Damaging Agents"
or may suffer mortality from a lack of vigor occasioned by improper
production and harvest practices, from poor planting practices, and from
frost damage incurred either in nursery beds or after planting (13).
When Douglas-fir develops in a closed stand, the lower limbs die rapidly
as they are increasingly subjected to overhead shade. Nevertheless,
natural pruning is exceedingly slow because even small dead limbs resist
decay and persist for a very long period. On the average, Douglas-fir is
not clear to a height of 5 m (17 ft) until 77 years old, and to 10 m (33
ft) until 107 years. Obviously, natural pruning will not produce clear
butt logs in rotations of less than 150 years. Artificial pruning will
greatly reduce the time required to produce clear lumber but may result in
severe grain distortion and brittle grain structure around pruning wounds
(10).
Seedlings and saplings of Douglas-fir respond satisfactorily to release
from competing brush or overstory trees if they have not been suppressed
too severely or too long. Trees of pole and small sawtimber size in
general respond very well to thinning. Trees that have developed in a
closed stand, however, are poorly adapted to radical release, such as that
occasioned by very heavy thinning. When exposed, the long slender holes
with short crowns are highly susceptible to damage from snowbreak,
windfall, and sunscald. Sudden and drastic release of young Douglas-fir
may cause a sharp temporary reduction in height growth (57). Application
of a nitrogen fertilizer in combination with thinning gives better growth
responses in Douglas-fir than either fertilizer or thinning alone (41).
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Rooting Habit
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Although Douglas-fir is potentially a
deep-rooting species, its root morphology varies according to the nature
of the soil. In the absence of obstructions, Douglas-fir initially forms a
tap root that grows rapidly during the first few years. In deep soils (69
to 135 cm, 27 to 53 in), it was found that tap roots grew to about 50
percent of their final depth in 3 to 5 years, and to 90 percent in 6 to 8
years; however, boulders or bedrock close to the soil surface result in
quick proliferation of the original tap root. Platelike root systems
develop when Douglas-fir grows in shallow soils or soils with a high water
table. Main lateral branches develop during the first or second growing
season as branches of the tap root. These structural roots tend to grow
obliquely into deeper soil layers and contribute to anchoring a tree. The
majority of roots in the surface soil are long rope-like laterals of
secondary and tertiary origin. Fine roots, those less than 0.5 cm (0.2 in)
in diameter, develop mostly from smaller lateral roots and are
concentrated in the upper 20 cm (8 in) of soil (29). Fine roots have a
short life-span, ranging in general from a few days to several weeks.
Cyclic death and replacement of fine roots changes seasonally, reflecting
changes in environmental conditions (51).
Size of the root system appears to be related to size of the crown
rather than the bole. In British Columbia, ratios of root spread to crown
width averaged 1.1 for open- and 0.9 for forest-grown Douglas-fir, but
greater lateral spread has been observed on poorly drained sand and sandy
gravel soils. The radial symmetry of root systems seems to be readily
distorted by slope, proximity to other trees, and presence of old roots.
Observations in the Pacific Northwest and the Rocky Mountains indicate
that roots of Douglas-fir extend farther downslope than upslope.
The proportion of root biomass decreases with age and may vary from 50
percent at age 21 to less than 20 percent in stands older than 100 years
(29). Root grafting is very common in stands of Douglas-fir, often leading
to a system of interconnected roots in older stands (36).
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Seed Production and Dissemination
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Major deterrents to natural
regeneration of Douglas-fir include limited seed supply; consumption of
seed by insects, animals, and birds; competing plant species; and
unfavorable environments. Although reports of fully stocked stands
resulting from seedfall from sources 1 to 2 km (0.6 to 1.2 mi) distant are
not rare, the great majority of Douglas-fir seeds fall within 100 m (330
ft) of a seed tree or stand edge (18).
Data describing the quantities of seeds that may fall vary widely, but
most years are characterized by less than 2.2 kg/ha (2 lb/acre), of which
no more than 40 percent is sound. Years with poor seed crops generally
have a lower percentage of viable seeds, perhaps because the low incidence
of fruiting trees may favor a higher level of selfing (25).
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Seedling Development
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Douglas-fir germination is epigeal. Seed
germinates in mid-March to early April in the warmer portions of the range
and as late as mid-May in the cooler areas. Seedling growth the first year
is indeterminate but relatively slow and limited generally by moisture,
which triggers initiation of dormancy in midsummer. The dormant period
normally extends from midsummer until April or May of the following year
(37). Douglas-fir can produce lammas shoots, but this habit is confined to
either the more moist portion of the range or to years with abnormally
heavy summer rainfall. This habit is probably most pronounced in the
southern Rockies, where the summer period is characterized by irregular,
heavy rainstorms. In any event, the great majority of the annual shoot
growth occurs during the initial flush. First-year seedlings on better
sites in the Pacific Northwest may develop shoots 6 to 9 cm (2.5 to 3.5
in) long. Growth in subsequent years is determinate and gradually
accelerates so that when saplings are 8 to 10 years old, terminal growth
may consistently exceed 1 m (3.3 ft) per year on the more productive
sites.
Seedlings of the variety menziesii normally survive best when
the seed germinates on moist mineral soil, but menziesii will tolerate
a light litter layer. Seedlings do not survive well, however, on heavy
accumulations of organic debris. In contrast, seedlings of the variety
glauca are favored by a duff layer, especially in the larch
forests of northwestern Montana (53).
First-year seedlings survive and grow best under light shade, especially
on southerly exposures, but older seedlings require full sunlight.
Particularly in the fog belt, competing vegetation such as alder, maple,
salmonberry, and thimbleberry (Rubus parviflorus) limits
Douglas-fir regeneration by creating intolerable levels of shade; plants
such as grasses, manzanita, ceanothus, and oak compete strongly for
available moisture; and plants such as bracken (Pteridium aquilinum)
and vetch (Vicia spp.) smother small seedlings with
leaves and other debris. Successful regeneration of variety menziesii
often depends on weed control in the commercial range of Douglas-fir
because many associated plant species have growth rates much greater than
that of juvenile Douglas-fir (8). For this reason, regeneration may be
more reliable after a wildfire, which destroys the reservoir of potential
competitive species, than after a harvest operation, which leaves areas
well suited to the rapid proliferation of the herbaceous and woody
competitors of Douglas-fir.
In the Rocky Mountains, competing vegetation may promote the
establishment of variety glauca seedlings by reducing temperature stress
and may inhibit seedling growth by competing strongly for moisture. The
latter effect is most pronounced in the southern portions of glauca's
range.
Microsites with adverse moisture and temperature conditions frequently
limit establishment of both menziesii and glauca seedlings on southerly
aspects (32). Soil surface temperatures in excess of 65° C (149°
F) are prevalent in the southern Cascade Range and Siskiyou Mountains and
are common in the Cascades even as far north as Mount Rainier. Prolonged
droughts, which may extend from May through September, are frequent in
southern Oregon and northern California, and low annual precipitation and
high evaporation stress greatly limit the distribution of glauca in the
Rocky Mountains.
Like nearly all perennial woody plants, Douglas-fir is dependent on a
mycorrhizal relationship for efficient uptake of mineral nutrients and
water. Approximately 2,000 species of fungi have been identified as
potential symbionts with Douglas-fir, and both ectomycorrhizal and
ectendomycorrhizal structures have been observed on this species (59).
Occasionally, nursery practices result in seedlings with few mycorrhizae,
but no deficiencies in mycorrhizal infection have been reported for
natural seedlings.
Historically, large burned or cleared areas in the range of variety
menziesii, such as those on Vancouver Island (52), have naturally seeded
into nearly pure stands of Douglas-fir. On mesic to moist sites this
process may occur over a relatively short period, perhaps 10 to 15 years.
On drier sites, such regeneration may be quite protracted and require a
hundred or more years. Stocking of harvested areas has been extremely
variable during the past 30 years, and large tracts in the drier or cooler
portions of the range are covered by brush species such as manzanita,
ceanothus, salmonberry, salal, or lower value hardwoods, such as alder,
maple, and oak.
Regeneration of variety glauca in the Rocky Mountains has also been
variable. In general, glauca may be considered a seral species in moist
habitats and a climax component in the warmer, drier areas. Regeneration
is favored where Douglas-fir is seral, especially in northern Idaho and
western Montana where a strong maritime influence modifies the generally
continental climate that prevails in the central and southerly Rocky
Mountains. In contrast, regeneration of Douglas-fir is poor where the
species has attained climax status (49).
From 1950 until about 1970, large areas of cutover and burned-over
forest land in the Pacific Northwest were aerially seeded. Direct seeding
suffers from the same deficiencies as natural regeneration, however; that
is, stands produced are often uneven in stocking and require interplanting
or pre-commercial thinning, and animals destroy a large proportion of the
seeds. With the advent of greatly increased forest nursery capacity,
direct seeding is much less common (13,54).
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Soils and Topography
provided by Silvics of North America
The variety menziesii of Douglas-fir reaches its best growth on
well-aerated, deep soils with a pH range from 5 to 6. It will not thrive
on poorly drained or compacted soils. Soils in the coastal belt of
northern California, Oregon, and Washington originated chiefly from marine
sandstones and shales with scattered igneous intrusions. These rocks have
weathered deeply to fine-textured, well-drained soils under the mild,
humid climate of the coast. Surface soils are generally acid, high in
organic matter and total nitrogen, and low in base saturation. Soils in
the Puget Sound area and in southwestern British Columbia are almost
entirely of glacial origin. Soils farther inland within the range of the
variety menziesii are derived from a wide variety of parent
materials. These include metamorphosed sedimentary material in the
northern Cascades and igneous rocks and formations of volcanic origin in
the southern Cascades.
Depth of soils ranges from very shallow on steep slopes and ridgetops to
deep in deposits of volcanic origin and residual and colluvial materials.
Texture varies from gravelly sands to clays. Surface soils are in general
moderately acid. Their organic matter content varies from moderate in the
Cascade Range to high in portions of the Coast Range and Olympic
Peninsula. Total nitrogen content varies considerably but is usually low
in soils of glacial origin. Great soil groups characteristic of the range
of coastal Douglas-fir include Haplohumults (Reddish Brown Lateritics) of
the order Ultisols, Dystrochrepts (Brown Lateritics), Haplumbrepts (Sols
Bruns Acides) of the order Inceptisols, Haplorthods (Western Brown Forest
soils) of the order Spodosols, Xerumbrepts (Brown Podzolic soils), and
Vitrandepts (Regosols) (63).
Soils within the range of Rocky Mountain Douglas-fir originated also
from a considerable array of parent materials. In south-central British
Columbia, eastern Washington, and northern Idaho, soils vary from basaltic
talus to deep loess with volcanic ash to thin residual soil over granitic
or sedimentary rocks. They are mostly Vitrandepts and Xerochrepts. Parent
materials in Montana and Wyoming consist of both igneous and sedimentary
rocks, and locally of glacial moraines. Soils derived from noncalcareous
substrates are variable in texture but consistently gravelly and acidic. A
significant portion of the sedimentary rocks is limestone, which gives
rise to neutral or alkaline soils ranging in texture from gravelly loams
to gravelly silts. Limestones often weather into soils that are
excessively well drained. Soils are Cryoboralfs of the order Alfisols, and
Cryandepts and Cryochrepts of the order Inceptisols. Soils in the central
and southern Rocky Mountains are very complex. They developed from glacial
deposits, crystalline granitic rocks, conglomerates, sandstones, and, in
the Southwest, limestones. These soils are Alfisols (Gray Wooded soils),
Mollisols (Brown Forest soils), Spodosols (Brown Podzolic soils, Podzols),
and Entisols (2,46).
Altitudinal distribution of both varieties of Douglas-fir (menziesii
and glauca) increases from north to south, reflecting the
effect of climate on distribution of the species. The principal limiting
factors are temperature in the north of the range and moisture in the
south. Consequently, Douglas-fir is found mainly on southerly slopes in
the northern part of its range, and on northerly exposures in the southern
part. At high elevations in the southern Rocky Mountains, however,
Douglas-fir grows on the sunny slopes and dry rock exposures (56).
Generally, the variety glauca grows at considerably higher
altitudes than the coastal variety of comparable latitude. Altitudinal
limit for Douglas-fir in central British Columbia is about 760 m (2,500
ft) but rises to 1250 m (4,100 ft) on Vancouver Island. In Washington and
Oregon, the species generally occurs from sea level to 1520 m (5,000 ft),
although locally it may occur higher. In the southern Oregon Cascades and
in the Sierra Nevada, the altitudinal range is between 610 and 1830 m
(2,000 and 6,000 ft). In river valleys and canyon bottoms, the species may
occasionally occur at elevations of 240 to 270 m (800 to 900 ft). Near the
southern limit of its range in the Sierra Nevada, the species grows to
elevations of 2300 m (7,500 ft). The inland variety grows at elevations
from 550 to 2440 m (1,800 to 8,000 ft) in the northern part of its range.
In the central Rocky Mountains, Douglas-fir grows mostly at elevations
between 1830 and 2590 m (6,000 and 8,000 ft), and in the southern Rocky
Mountains, between 2440 and 2900 m (8,000 and 9,500 ft). In some
localities in southern and central Arizona, Douglas-fir may be found as
low as 1550 m (5,100 ft) in canyon bottoms. The highest elevation at which
Douglas-fir grows in the Rocky Mountains is 3260 m (10,700 ft) on the
crest of Mount Graham in southeastern Arizona.
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Special Uses
provided by Silvics of North America
Douglas-fir is grown as a Christmas tree on rotations ranging from 4 to
7 years. Trees are sheared each year to obtain a pyramid-shaped crown.
Attempts to grow Douglas-fir as a Christmas tree in North America outside
its native range have failed. Coastal Douglas-fir is usually killed by
frost, and the interior variety suffers too much from the needle cast
disease Phaeocryptopus gaeumanni.
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Vegetative Reproduction
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Douglas-fir does not naturally
reproduce vegetatively. Substantial research to develop cuttings as a
regeneration procedure has demonstrated that reliable rooting of cuttings
is limited to material collected from trees less than 10 years old, or
from trees that have been subjected to repeated shearing to regenerate
material with a juvenile habit. A second major impediment to the use of
cuttings as a regeneration technique for this species is that most such
material has a period of plagiotropic growth, which may be lengthy, before
the erect habit is assumed.
Research with tissue culture techniques has demonstrated substantial
promise, but widespread use of this technique in reforestation of the
Douglas-fir region is, at best, a future possibility.
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Brief Summary
provided by Silvics of North America
Pinaceae -- Pine family
Richard K. Hermann and Denis P. Lavender
Douglas-fir (Pseudotsuga menziesii), also called red-fir,
Oregon-pine, Douglas-spruce, and piño Oregon (Spanish), is one of
the world's most important and valuable timber trees. It has been a major
component of the forests of western North America since the
mid-Pleistocene (30). Although the fossil record indicates that the native
range of Douglas-fir has never extended beyond western North America, the
species has been successfully introduced in the last 100 years into many
regions of the temperate forest zone (31). Two varieties of the species
are recognized: P. menziesii (Mirb.) Franco var. menziesii,
called coast Douglas-fir, and P. menziesii var. glauca (Beissn.)
Franco, called Rocky Mountain or blue Douglas-fir.
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Distribution
provided by Silvics of North America
The latitudinal range of Douglas-fir is the greatest of any commercial
conifer of western North America. Its native range, extending from
latitude 19° to 55° N., resembles an inverted V with uneven
sides. From the apex in central British Columbia, the shorter arm extends
south along the Pacific Coast Ranges for about 2200 km (1,367 mi) to
latitude 34° 44' N., representing the range of the typical coastal or
green variety, menziesii; the longer arm stretches along the Rocky
Mountains into the mountains of central Mexico over a distance of nearly
4500 km (2,796 mi), comprising the range of the other recognized variety,
glauca- Rocky Mountain or blue. Nearly pure stands of Douglas-fir
continue south from their northern limit on Vancouver Island through
western Washington, Oregon, and the Klamath and Coast Ranges of northern
California as far as the Santa Cruz Mountains. In the Sierra Nevada,
Douglas-fir is a common part of the mixed conifer forest as far south as
the Yosemite region. The range of Douglas-fir is fairly continuous through
northern Idaho, western Montana, and northwestern Wyoming. Several
outliers are present in Alberta and the eastern-central parts of Montana
and Wyoming, the largest being in the Bighorn Mountains of Wyoming. In
northeastern Oregon, and from southern Idaho south through the mountains
of Utah, Nevada, Colorado, New Mexico, Arizona, extreme western Texas, and
northern Mexico, the distribution becomes discontinuous.
- The native range of Douglas-fir.
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Physical Description
provided by USDA PLANTS text
Tree, Evergreen, Monoecious, Habit erect, Trees without or rarely having knees, Tree with bark rough or scaly, Young shoots 3-dimensional, Buds not resinous, Leaves needle-like, Leaves alternate, Needle-like leaf margins entire (use magnification), Leaf apex acute, Leaf apex obtuse, Leaves < 5 cm long, Leaves < 10 cm long, Leaves yellow-green above, Leaves yellow-green below, Leaves blue-green, Leaves not blue-green, Scale leaf glands not ruptured, Needle-like leaves flat, Needle-like leaves not twisted, Needle-like leaf habit erect, Needle-like leaf habit drooping, Needle-like leaves per fascicle mostly 1, Needle-like leaf sheath early deciduous, Needle-like leaf sheath persistent, Twigs pubescent, Twigs not viscid, Twigs with peg-like projections or large fascicles after needles fall, Berry-like cones orange, Woody seed cones > 5 cm long, Bracts of seed cone exerted, Bracts of seed cone included, Seeds tan, Seeds brown, Seeds winged, Seeds unequally winged, Seed wings prominent, Seed wings equal to or broader than body.
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- Steffi Ickert-Bond
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- Damon Little
Douglas fir
provided by wikipedia EN
The Douglas fir (Pseudotsuga menziesii)[3] is an evergreen conifer species in the pine family, Pinaceae. It is native to western North America and is also known as Douglas-fir,[4] Douglas spruce,[5] Oregon pine,[6] and Columbian pine.[7] There are three varieties: coast Douglas-fir (P. menziesii var. menziesii), Rocky Mountain Douglas-fir (P. menziesii var. glauca) and Mexican Douglas-fir (P. menziesii var. lindleyana).[8]
Despite its common names, it is not a true fir (genus Abies), spruce (genus Picea), or pine (genus Pinus). It is also not a hemlock; the genus name Pseudotsuga means "false hemlock".
Description
Douglas-firs are medium-size to extremely large evergreen trees, 20–100 metres (70–330 feet) tall (although only Pseudotsuga menziesii var. menziesii, common name coast Douglas-firs, reach heights near 100 m)[9] and commonly reach 2.4 m (8 ft) in diameter,[10] although trees with diameters of almost 5 metres (16 feet) exist.[11] The largest coast Douglas-firs regularly live over 500 years, with the oldest specimens living for over 1,300 years.[12] Rocky Mountain Douglas-firs, found further to the east,[13] are less long-lived, usually not exceeding 400 years in age.[14]
There are records of former coast Douglas-firs exceeding 120 metres (390 feet)[15][16] in height, which if alive today would make it the tallest tree species on Earth. Some particular specimens that exceeded 400 feet tall were the Lynn Valley Tree and the Nooksack Giant.
The leaves are flat, soft, linear needles 2–4 centimetres (3⁄4–1+1⁄2 in) long, generally resembling those of the firs, occurring singly rather than in fascicles; they completely encircle the branches, which can be useful in recognizing the species. As the trees grow taller in denser forest, they lose their lower branches, such that the foliage may start as high as 34 m (110 ft) off the ground.[17] Douglas-firs in environments with more light may have branches much closer to the ground.
The bark on young trees is thin, smooth, grey, and contains numerous resin blisters. On mature trees, usually exceeding 80 years, it is very thick and corky, growing up to 36 cm (14 in) thick with distinctive, deep vertical fissures caused by growth. Layers of darker brown bark are interspersed with layers of lighter colored, corky material.[18] This thickness makes the Douglas-fir perhaps the most fire-resistant tree native to the Pacific Northwest.[19]
The female cones are pendulous, with persistent scales, unlike those of true firs. They have distinctive long, trifid (three-pointed) bracts which protrude prominently above each scale and are said to resemble the back half of a mouse, with two feet and a tail.[20] The cones are tan when mature, measuring 6–10 cm (2+1⁄2–4 in) long for coastal Douglas-firs and a couple of centimetres shorter inland.[13]
The massive mega-genome of Douglas fir was sequenced in 2017 by the large PineRefSeq consortium, revealing a specialized photosynthetic apparatus in the light-harvesting complex genes.[21]
Taxonomy
The common name honors David Douglas, a Scottish botanist and collector who first reported the extraordinary nature and potential of the species. The common name is misleading since it is not a true fir, i.e., not a member of the genus Abies. For this reason, the name is often written as Douglas-fir (a name also used for the genus Pseudotsuga as a whole).[22][13]
The specific epithet menziesii is after Archibald Menzies, a Scottish physician and rival naturalist to David Douglas. Menzies first documented the tree on Vancouver Island in 1791. Colloquially, the species is also known simply as Doug fir[7] or Douglas pine[7] (although the latter common name may also refer to Pinus douglasiana).[23] Other names for this tree have included Oregon pine,[6] British Columbian pine,[7] Puget Sound pine,[7] Douglas spruce,[7] false hemlock,[6] red fir,[6] or red pine[6] (although again red pine may refer to a different tree species, Pinus resinosa, and red fir may refer to Abies magnifica).[24]
One Coast Salish name for the tree, used in the Halkomelem language, is lá:yelhp.[25] In the Lushootseed language, the tree is called čəbidac.[26]
Distribution
Pseudotsuga menziesii var. menziesii, the coast Douglas-fir, grows in the coastal regions from west-central British Columbia southward to central California. In Oregon and Washington, its range is continuous from the eastern edge of the Cascades west to the Pacific Coast Ranges and Pacific Ocean. In California, it is found in the Klamath and California Coast Ranges as far south as the Santa Lucia Range, with a small stand as far south as the Purisima Hills in Santa Barbara County.[27][28] One of the last remaining old growth stands of conifers is in the Mattole Watershed, and is under threat of logging.[29][30] In the Sierra Nevada, it ranges as far south as the Yosemite region. It occurs from sea level along the coast to elevations of 1,500 m (4,900 ft) or higher, and inland in some cases up to 2,100 m (6,900 ft).[13]
Another variety exists further inland, Pseudotsuga menziesii var. glauca, the Rocky Mountain Douglas-fir or interior Douglas-fir. Interior Douglas-fir intergrades with coast Douglas-fir in the Cascades of northern Washington and southern British Columbia, and from there ranges northward to central British Columbia and southeastward to the Mexican border, becoming increasingly disjunct as latitude decreases and altitude increases. Mexican Douglas-fir (P. lindleyana), which ranges as far south as Oaxaca, is often considered a variety of P. menziesii.
Fossils (wood, pollen) of Pseudotsuga are recorded from the Miocene and Pliocene of Europe (Siebengebirge, Gleiwitz, Austria).[31]
It is also naturalised throughout Europe,[32] Argentina and Chile (called Pino Oregón). In New Zealand it is considered to be an invasive species, called a wilding conifer, and is subject to control measures. But is also one of the most common lumber trees used in forestry alongside Radiata pine with large plantations throughout the country. The species was introduced in the 1900s for its wood.[33][34]
Ecology
Preferred sites
Douglas-fir prefers acidic or neutral soils.[35] However, it exhibits considerable morphological plasticity, and on drier sites P. menziesii var. menziesii will generate deeper taproots. Pseudotsuga menziesii var. glauca exhibits even greater plasticity, occurring in stands of interior temperate rainforest in British Columbia, as well as at the edge of semi-arid sagebrush steppe throughout much of its range, where it generates even deeper taproots still.
The coast Douglas-fir variety is the dominant tree west of the Cascade Mountains in the Pacific Northwest. It occurs in nearly all forest types and competes well on most parent materials, aspects, and slopes. Adapted to a more moist, mild climate than the interior subspecies, it grows larger and faster than Rocky Mountain Douglas-fir. Associated trees include western hemlock, Sitka spruce, sugar pine, western white pine, ponderosa pine, grand fir, coast redwood, western redcedar, California incense-cedar, Lawson's cypress, tanoak, bigleaf maple and several others. Pure stands are also common, particularly north of the Umpqua River in Oregon. It is most dominant in areas with a more frequent fire regime that suppresses less fire-resistant conifers.[18]
Use by animals
A
snag provides nest cavities for birds.
Douglas-fir seeds are an extremely important food source for small mammals such as moles, shrews, and chipmunks, which consume an estimated 65% of each annual seed crop. The Douglas squirrel harvests and hoards great quantities of Douglas-fir cones, and also consumes mature pollen cones, the inner bark, terminal shoots, and developing young needles.[12]
Mature or "old-growth" Douglas-fir forest is the primary habitat of the red tree vole (Arborimus longicaudus) and the spotted owl (Strix occidentalis). Home range requirements for breeding pairs of spotted owls are at least 400 hectares (4.0 km2; 990 acres) of old growth. Red tree voles may also be found in immature forests if Douglas-fir is a significant component. The red vole nests almost exclusively in the foliage of the trees, typically 2–50 metres (5–165 ft) above the ground, and its diet consists chiefly of Douglas-fir needles.[12]
Douglas-fir needles are generally poor browse for ungulates, although in the winter when other food sources are lacking it can become important, and black-tailed deer browse new seedlings and saplings in spring and summer. The spring diet of the blue grouse features Douglas-fir needles prominently.[12]
The leaves are also used by the woolly conifer aphid Adelges cooleyi; this 0.5 mm-long sap-sucking insect is conspicuous on the undersides of the leaves by the small white "fluff spots" of protective wax that it produces. It is often present in large numbers, and can cause the foliage to turn yellowish from the damage it causes. Exceptionally, trees may be partially defoliated by it, but the damage is rarely this severe. Among Lepidoptera, apart from some that feed on Pseudotsuga in general, the gelechiid moths Chionodes abella and C. periculella as well as the cone scale-eating tortrix moth Cydia illutana have been recorded specifically on P. menziesii.
The inner bark is the primary winter food for the North American porcupine.[12]
Poriol is a flavanone, a type of flavonoid, produced by P. menziesii in reaction to infection by Poria weirii.[36]
Value to other plants
A parasitic plant which uses P. menziesii is the Douglas-fir dwarf mistletoe (Arceuthobium douglasii). Epiphytes such as crustose lichens and mosses are common sights on Douglas-firs.[18] As it is only moderately shade tolerant,[13] undisturbed Douglas-fir stands in humid areas will eventually give way to later successional, more shade-tolerant associates such as the western redcedar and western hemlock—though this process may take a thousand years or more.[12] It is more shade tolerant than some associated fire-dependent species, such as western larch and ponderosa pine, and often replaces these species further inland.[13]
Diseases and insects
Fungal diseases such as laminated root rot and shoestring root-rot can cause significant damage, and in plantation settings dominated by Douglas-fir monocultures may cause extreme damage to vast swathes of trees.[12] Interplanting with resistant or nonhost species such as western redcedar and beaked hazelnut[37] can reduce this risk. Other threats to Douglas-fir include red ring rot and the Douglas-fir beetle.[12]
Uses
A 9-ft log, scaling over 7,000
board-ft of timber, c. 1937
Many different Native American groups used the bark, resin, and pine needles to make herbal treatments for various diseases.[38] British Columbia's Bella Coola tribe mixed the resin with dogfish oil for many medicinal applications.[13] Some tribes used the foliage as a hygienic freshener in sweat baths, and the leaves were used as a coffee substitute.[13] Native Hawaiians built waʻa kaulua (double-hulled canoes) from coast Douglas-fir logs that had drifted ashore.[39] The wood has historically been favored as firewood, especially from the coastal variety.[13] In addition early settlers used Douglas fir for all forms of building construction, including floors, beams, and fine carving. Even today much of the Northwest chain saw art is completed on Douglas fir logs. The structures built from fir have lasted 150 years and more.
The species is extensively used in forestry management as a plantation tree for softwood timber. Douglas-fir is one of the world's best timber-producing species and yields more timber than any other species in North America, making the forestlands of western Oregon, Washington, and British Columbia the most productive on the continent. In 2011, Douglas-fir represented 34.2% of US lumber exports, to a total of 1.053 billion board-feet.[40][12] Douglas fir timber is used for timber frame construction and timber trusses using traditional joinery, veneer, and flooring due to its strength, hardness and durability.[41] As of 2012, the only wooden ships still currently in use by the U.S. Navy are Avenger-class minesweepers, made of Douglas-fir.[42]
Douglas fir sees wide use in heavy timber structures, as its wood is strong, available in a number of specifications including kiln dried and grade stamped, and can be supplied in very long lengths to 60 feet. West coast mills are sophisticated in their processing of timbers, making lead times predictable and availability reliable. Paints adhere well to Douglas fir. Stains perform well on Douglas fir timbers with the mild caution that the natural color of this species varies and care must be taken to ensure uniformity of color. Pitch pockets that may ooze resin can be present in timbers that have not been kiln dried. Because of the timber sizes available, stamped timber grading, and relatively short lead times, Douglas fir sees wide use in both public and residential projects.
The species has ornamental value in large parks and gardens.[43] It has been commonly used as a Christmas tree since the 1920s, and the trees are typically grown on plantations.[44]
The buds have been used to flavor eau de vie, a clear, colorless fruit brandy.[45] Douglas-fir pine leaves can be used to make pine needle tea.[46] They possess a tangy citrus flavor and may serve in some recipes as a wild substitute for rosemary.[47]
See also
References
-
^ Farjon, A. (2013). "Pseudotsuga menziesii". IUCN Red List of Threatened Species. 2013: e.T42429A2979531. doi:10.2305/IUCN.UK.2013-1.RLTS.T42429A2979531.en. Retrieved 19 November 2021.
-
^ "Taxonomy - GRIN-Global Web v 1.10.5.0". npgsweb.ars-grin.gov. Retrieved 24 September 2019.
-
^ "Pseudotsuga menziesii ". Calflora. Berkeley, California: The Calflora Database.
-
^ Lipscomb, Barney (1993). "Pseudotsuga menziesii". In Flora of North America Editorial Committee (ed.). Flora of North America North of Mexico (FNA). Vol. 2. New York and Oxford. Retrieved 2018-11-07 – via eFloras.org, Missouri Botanical Garden, St. Louis, MO & Harvard University Herbaria, Cambridge, MA.
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^ "Douglas Fir".
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^ a b c d e "Pseudotsuga menziesii var. menziesii ". Calflora. Berkeley, California: The Calflora Database.
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^ a b c d e f Wilson, Donald A. (2008-01-28). Forensic procedures for boundary and title investigation. John Wiley & Sons. ISBN 9780470113691.
-
^ USDA, NRCS (n.d.). "Pseudotsuga menziesii". The PLANTS Database (plants.usda.gov). Greensboro, North Carolina: National Plant Data Team. Retrieved 2018-11-07.
-
^ Carder, Al (1995). Forest Giants of the World Past and Present. pp. 3–4.
-
^ Brockman, C. Frank (1968). "Pseudotsuga menziesii". Trees of North America: A Guide to Field Identification. New York: Golden Press. pp. 44–45. ISBN 0-307-13658-2.
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^ "World's Largest Douglas-fir Tree - the Red Creek Fir!". 8 June 2011.
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^ a b c d e f g h i Van Pelt, Robert (2007). "Identifying Mature and Old Forests In Western Washington" (PDF) (pdf). Washington State Department of Natural Resources. Archived (PDF) from the original on 11 November 2020. Retrieved 1 September 2021.
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^ a b c d e f g h i Arno, Stephen F.; Hammerly, Ramona P. (2020) [1977]. Northwest Trees: Identifying & Understanding the Region's Native Trees (field guide ed.). Seattle: Mountaineers Books. pp. 101–110. ISBN 978-1-68051-329-5. OCLC 1141235469.
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^ "Douglas Fir: Pseudotsuga menziesii". National Wildlife Federation. Retrieved 1 September 2021.
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^ "Tallest Douglas Fir in America". 12 November 2012.
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^ "Giant logged long ago but not forgotten". 4 September 2011.
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^ Russell, Tony; Cutler, Catherine; Walters, Martin (2014). "Pseudotsuga menziesii". The Illustrated Encyclopedia of Trees of the World. London: Anness Publishing Ltd. p. 120. ISBN 978-1-4351-5597-8.
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^ a b c "Pseudotsuga menziesii var. menziesii". www.fs.fed.us. Retrieved 2021-05-11.
-
^ Van Pelt, Robert (2007). "Identifying Mature and Old Forests In Western Washington" (PDF) (pdf). Washington State Department of Natural Resources. Archived (PDF) from the original on 11 November 2020. Retrieved 11 May 2021.
-
^ "U.S. Fish and Wildlife Service, Open Spaces Blog". www.fws.gov. Retrieved 2021-05-12.
-
^ Neale DB (2017). "The Douglas-Fir Genome Sequence Reveals Specialization of the Photosynthetic Apparatus in Pinaceae". G3: Genes, Genomes, Genetics. 7 (9): 3157–3167. doi:10.1534/g3.117.300078. PMC 5592940. PMID 28751502.
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^ "Douglas-fir (Pseudotsuga)". Common Trees of the Pacific Northwest. Oregon State University. Archived from the original on 2012-12-19. Retrieved 2022-02-13.
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^ Farjon, A. (2013). "Pinus douglasiana". IUCN Red List of Threatened Species. 2013: e.T42357A2974933. doi:10.2305/IUCN.UK.2013-1.RLTS.T42357A2974933.en. Retrieved 19 November 2021.
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^ USDA, NRCS (n.d.). "Pinus resinosa". The PLANTS Database (plants.usda.gov). Greensboro, North Carolina: National Plant Data Team. Retrieved 2018-11-07.
-
^ Galloway, Brent Douglas. Dictionary of Upriver Halkomelem. Vol. I. p. 213.
-
^ "čəbidac". Lushootseed: the language of Puget Sound. March 18, 2017.
-
^ Griffin, James R. (September 1964). "A New Douglas-Fir Locality in Southern California". Forest Science: 317–319. Retrieved December 31, 2010.
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^ Griffin, James R.; Critchfield, William B. (1976). The Distribution of Forest Trees in California USDA Forest Service Research Paper PSW – 82/1972 (PDF). Berkeley, California: USDA Forest Service. p. 114. Retrieved 2015-05-03.
-
^ "Douglas Fir, Then and Now | The Seattle Times". archive.seattletimes.com.
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^ "Tensions Rise In the Battle To Save Old Trees". Cal Alumni Association. September 1, 2018.
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^ R. K. Hermann (October 1985). The Genus Pseudotsuga : Ancestral History and Past Distribution (Special Publication 2b). Forest Research Laboratory, College of Forestry, Oregon State University. pp. 23–24.
-
^ "Distribution of Douglas-fir". Royal Botanical Garden Edinburgh.
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^ "Weed Information Sheet". Weedbusters. Retrieved 2021-05-12.
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^ "Douglas-fir". www.nzfoa.org.nz.
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^ "Douglas-fir Tree on the Tree Guide". arborday.org.
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^ Barton GM (1972). "New C-methylflavanones from Douglas-fir". Phytochemistry. 11 (1): 426–429. doi:10.1016/S0031-9422(00)90036-0.
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^ "Corylus cornuta". www.fs.fed.us. Retrieved 2021-05-12.
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^ "Douglas Fir" (PDF). Retrieved 2020-02-21.
-
^ "Pseudotsuga menziesii var. menziesii ". The Gymnosperm Database. Retrieved March 17, 2013. This was the preferred species for Hawaiian war canoes. The Hawaiians, of course, did not log the trees; they had to rely on driftwood.
-
^ Curtis, Robert; Carey, Andrew (1996). Timber Supply in the Pacific Northwest (PDF). USDA Forest Service.
-
^ "Douglas-Fir". Wood Database. Retrieved August 15, 2018.
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^ Tarantola, Andrew (23 May 2012). "The Navy's Wooden Avengers Are Real-Life Mine Sweepers". Gizmodo. wooden hulls—typically oak, Douglas-fir, or Nootka Cypress—coated in glass-reinforced plastic
-
^ "Pseudotsuga menziesii ". Royal Horticultural Society. Archived from the original on 2013-11-09. Retrieved 2012-07-14.
-
^ "Douglas-Fir". National Christmas Tree Association. Archived from the original on 2020-08-03. Retrieved 2022-02-10.
-
^ Asimov, Eric (August 15, 2007). "An Orchard in a Bottle, at 80 Proof". The New York Times. Retrieved February 1, 2009.
-
^ "Foraging for Pine Needles (and other conifer needles)". Grow Forage Cook Ferment. December 23, 2015.
-
^ Boyd, Sabra (November 27, 2020). "As a homeless teen, I foraged for wild food to survive. The lessons still shape my cooking". The Washington Post. Archived from the original on November 27, 2020. Retrieved December 1, 2020.
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Douglas fir: Brief Summary
provided by wikipedia EN
The Douglas fir (Pseudotsuga menziesii) is an evergreen conifer species in the pine family, Pinaceae. It is native to western North America and is also known as Douglas-fir, Douglas spruce, Oregon pine, and Columbian pine. There are three varieties: coast Douglas-fir (P. menziesii var. menziesii), Rocky Mountain Douglas-fir (P. menziesii var. glauca) and Mexican Douglas-fir (P. menziesii var. lindleyana).
Despite its common names, it is not a true fir (genus Abies), spruce (genus Picea), or pine (genus Pinus). It is also not a hemlock; the genus name Pseudotsuga means "false hemlock".
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