Pinus strobus |
Pinus attenuata |
|
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eastern white pine, northern white pine, pin blanc, soft pine, Weymouth pine, white pine |
knobcone pine |
|
Habit | Trees to 67m; trunk to 1.8m diam., straight; crown conic, becoming rounded to flattened. | Shrubs or trees to 24m; trunk to 0.8m diam., usually straight; crown mostly narrowly to broadly conic. |
Bark | gray-brown, deeply furrowed, with long, irregularly rectangular, scaly plates. |
purple-brown to dark brown, shallowly and narrowly fissured, with irregular, flat, loose-scaly plates, on upper sections of trunk nearly smooth. |
Branches | whorled, spreading-upswept; twigs slender, pale red-brown, glabrous or pale puberulent, aging gray, ±smooth. |
ascending; twigs slender, red-brown. |
Buds | ovoid-cylindric, light red-brown, 0.4–0.5cm, slightly resinous. |
ovoid to ovoid-cylindric, dark red-brown, aging darker, ca. 1.5cm, resinous; scale margins fringed, apex attenuate. |
Leaves | 5 per fascicle, spreading to ascending, persisting 2–3 years, 6–10cm × 0.7–1mm, straight, slightly twisted, pliant, deep green to blue-green, pale stomatal lines evident only on adaxial surfaces, margins finely serrulate, apex abruptly acute to short-acuminate; sheath 1–1.5cm, shed early. |
3 per fascicle, spreading or ascending, persisting 4–5 years, (8–)9–15(–20)cm × (1–)1.3–1.8mm, straight or slightly curved, twisted, yellow-green, all surfaces with fine stomatal lines, margins serrulate, apex abruptly conic-subulate; sheath (1–)1.5–2cm, base persistent. |
Pollen cones | ellipsoid, 10–15mm, yellow. |
ellipsoid-cylindric, 10–15mm, orange-brown. |
Seed(s) | cones maturing in 2 years, shedding seeds and falling soon thereafter, clustered, pendent, symmetric, cylindric to lance-cylindric or ellipsoid-cylindric before opening, ellipsoid-cylindric to cylindric or lance-cylindric when open, (7–)8–20cm, gray-brown to pale brown, with purple or gray tints, stalks 2–3cm; apophyses slightly raised, resinous at tip; umbo terminal, low. |
cones maturing in 2 years, serotinous, long-persistent, remaining closed for 20 years or more, or opening on burning, in whorls, hard and heavy, very asymmetric, lanceoloid before opening, ovoid-cylindric when open, 8–15cm, yellow- or pale red-brown, stalks to 1cm; apophyses toward outside base increasingly elongate, mammillate or raised-angled-conic, downcurved near base, scarcely raised on branchlet side, rhombic; umbo central, low-pyramidal, sharp, upcurved. |
2n | =24. |
=24. |
Pinus strobus |
Pinus attenuata |
|
Habitat | Mesic to dry sites | Fire successional on dry slopes and foothills of Sierra Nevada and the Cascade and Coast ranges |
Elevation | 0–1500m (0–4900ft) | 300–1200m (1000–3900ft) |
Distribution |
CT; DE; GA; IA; IL; IN; KY; MA; MD; ME; MI; MN; NC; NH; NJ; NY; OH; PA; RI; SC; TN; VA; VT; WI; WV; MB; NB; NF; NS; ON; PE; QC; SPM; Mexico; Central America in Guatemala
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CA; OR; Mexico in Baja California
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Discussion | Pinus strobus is an important timber tree; because of extensive lumbering, few uncut stands remain. It was once prized as a source for ship masts, and large tracts of it were reserved for the Royal Navy during colonial times. Pinus strobus var. chiapensis appears to be as Martínez saw it: a clinal variant that, compared to the type variety, has finer leaves, different resin canal distribution, and heavier cones when cones of similar sizes are compared. Eastern white pine (Pinus strobus) is the provincial tree of Ontario and the state tree of Maine and Michigan. (Discussion copyrighted by Flora of North America; reprinted with permission.) |
Pinus attenuata, mostly a chaparral species, bears cones at an early age. Its seed crops are heavy, and a hot fire permits the seeds to be released. It forms hybrids with P. muricata and P. radiata. (Discussion copyrighted by Flora of North America; reprinted with permission.) |
Source | FNA vol. 2. | FNA vol. 2. |
Parent taxa | Pinaceae > Pinus | Pinaceae > Pinus |
Sibling taxa | ||
Synonyms | P. chiapensis, P. strobus var. chiapensis, Strobus strobus | P. tuberculata |
Name authority | Linnaeus: Sp. Pl. 2: 1001. (1753) | Lemmon: Mining Sci. Press 64: 45. (1892) |
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