Pinus attenuata |
Pinus taeda |
|
---|---|---|
knobcone pine |
loblolly pine |
|
Habit | Shrubs or trees to 24m; trunk to 0.8m diam., usually straight; crown mostly narrowly to broadly conic. | Trees to 46m; trunk to 1.6m diam., usually straight, without adventitious shoots; crown broadly conic to rounded. |
Bark | purple-brown to dark brown, shallowly and narrowly fissured, with irregular, flat, loose-scaly plates, on upper sections of trunk nearly smooth. |
red-brown, forming square or irregularly rectangular, scaly plates, resin pockets absent. |
Branches | ascending; twigs slender, red-brown. |
spreading-ascending; twigs moderately slender (to ca. 1cm thick), orangish to yellow-brown, aging darker brown, rough. |
Buds | ovoid to ovoid-cylindric, dark red-brown, aging darker, ca. 1.5cm, resinous; scale margins fringed, apex attenuate. |
lance-cylindric, pale red-brown, 1–1.2(–2)cm, mostly less than 1cm broad, slightly resinous; scale margins white-fringed, apex acuminate. |
Leaves | 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. |
2–3 per fascicle, ascending to spreading, persisting 3 years, (10–)12–18(–23)cm × 1–2mm, straight, slightly twisted, pliant, deep yellow-green, all surfaces with narrow stomatal lines, margins finely serrulate, apex acute to abruptly conic-subulate; sheath 1–2.5cm, base persistent. |
Pollen cones | ellipsoid-cylindric, 10–15mm, orange-brown. |
cylindric, 20–40mm, yellow to yellow-brown. |
Seed(s) | 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. |
cones maturing in 2 years, shedding seeds soon thereafter, not persistent, solitary or in small clusters, nearly terminal, symmetric, lanceoloid before opening, narrowly ovoid when open, 6–12cm, mostly dull yellow-brown, sessile to nearly sessile, scales without dark border on adaxial surface distally; apophyses dull, slightly thickened, variously raised (more so toward cone base), rhombic, strongly transversely keeled; umbo central, recurved, stoutly pyramidal, tapering to stout-based, sharp prickle. |
2n | =24. |
=24. |
Pinus attenuata |
Pinus taeda |
|
Habitat | Fire successional on dry slopes and foothills of Sierra Nevada and the Cascade and Coast ranges | Mesic lowlands and swamp borders to dry uplands |
Elevation | 300–1200m (1000–3900ft) | 0–700m (0–2300ft) |
Distribution |
CA; OR; Mexico in Baja California
|
AL; AR; DE; FL; GA; KY; LA; MD; MS; NC; NJ; OK; SC; TN; TX; VA
|
Discussion | 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.) |
Originally most races of Pinus taeda were in the lowlands. Following disturbance of the natural vegetation after settlement by Europeans, the species spread to fine-textured, fallow, upland soils, where it now occurs intermixed with P. echinata and P. virginiana. In the Southeast P. taeda is commonly used in plantation forestry, along with P. elliottii and P. echinata. Pinus taeda frequently forms hybrids with P. echinata and P. palustris (P. × sondereggeri H.H. Chapman). Commercially, it is a valuable pulpwood and timber species. (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. tuberculata | |
Name authority | Lemmon: Mining Sci. Press 64: 45. (1892) | Linnaeus: Sp. Pl. 2: 1000. (1753) |
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