Woodsia alpina |
Woodsia obtusa |
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alpine cliff fern, alpine woodsia, northern cliff fern, woodsie alpine |
blunt-lobe woodsia, blunt-lobed cliff fern, bluntlobe cliff fern, woodsie à lobes arrondis |
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Stems | compact, erect to ascending, with cluster of persistent petiole bases of ± equal length; scales uniformly brown, lanceolate. |
compact to creeping, erect to horizontal, with few to many persistent petiole bases of unequal lengths; scales often uniformly brown but at least some bicolored with dark central stripe and pale brown margins, narrowly lanceolate. |
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Leaves | 2.5–20 × 0.5–2.5 cm. |
8–60 × 2.5–12 cm. |
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Petiole | reddish brown or dark purple when mature, articulate above base at swollen node, relatively brittle and easily shattered. |
light brown or straw-colored when mature, occasionally darker at very base, not articulate above base, relatively brittle and easily shattered. |
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Blade | linear to narrowly lanceolate, usually pinnate-pinnatifid proximally, lacking glands, never viscid; rachis with widely scattered hairs and scales. |
lanceolate to ovate, 2-pinnate to 2-pinnate-pinnatifid proximally, moderately glandular, rarely somewhat viscid; many glandular hairs with thick stalks and distinctly bulbous tips; rachis with glandular hairs and scattered, often hairlike scales. |
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Pinnae | ovate-lanceolate to deltate, longer than wide, abruptly tapered to a rounded or broadly acute apex; largest pinnae with 1–3 pairs of pinnules; abaxial surface with isolated hairs and linear scales, adaxial surface glabrous. |
ovate-deltate to elliptic, longer than wide, abruptly tapered to a rounded or broadly acute apex, occasionally attenuate; largest pinnae with 5–14 pairs of pinnules; abaxial and adaxial surfaces glandular, lacking nonglandular hairs or scales. |
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Indusia | of narrow, hairlike segments, these uniseriate throughout, composed of cells many times longer than wide, usually surpassing mature sporangia. |
of relatively broad, nonfilamentous segments, these multiseriate throughout, composed of ± isodiametric cells, entire or glandular along distal edge, concealed by or slightly surpassing mature sporangia. |
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Spores | averaging 46–53 µm. |
averaging 35–47 µm. |
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Pinnules | entire or broadly crenate; margins nonlustrous, thin, with occasional isolated cilia, lacking translucent projections. |
dentate, sometimes deeply lobed; margins nonlustrous, thin, with occasional glands, lacking cilia or translucent projections. |
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Vein | tips often enlarged to form whitish hydathodes visible adaxially. |
tips usually enlarged to form whitish hydathodes visible adaxially. |
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Woodsia alpina |
Woodsia obtusa |
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Phenology | Sporulating summer–early fall. | |||||
Habitat | Crevices and ledges on cliffs (occasionally on rocky slopes), mostly slaty and calcareous rocks | |||||
Elevation | 0–1500 m (0–4900 ft) | |||||
Distribution |
AK; ME; MI; MN; NH; NY; VT; BC; MB; NB; NF; NS; NT; ON; QC; SK; YT; Greenland; n Eurasia |
AL; AR; CT; DE; FL; GA; IA; IL; IN; KS; KY; LA; MA; MD; ME; MI; MN; MO; MS; NC; NE; NH; NJ; NY; OH; OK; PA; RI; SC; TN; TX; VA; VT; WI; WV; ON; QC; only in the flora
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Discussion | Isozyme studies confirm the longstanding hypothesis that Woodsia alpina is an allotetraploid derived from hybridization between W. glabella and W. ilvensis (see reticulogram). Considerable disagreement exists concerning the chromosome number of W. alpina, but 2n = 160 seems most likely, given the numbers reported for the two parental species. Hybrids between W. alpina and W. ilvensis have been reported from both Europe and North America. These morphologically intermediate triploids with malformed spores have been called W. × gracilis (Lawson) Butters. (Discussion copyrighted by Flora of North America; reprinted with permission.) |
Woodsia obtusa comprises two cytotypes that are treated here as subspecies because they show subtle morphologic and ecological distinctions and tend to have different distributions. Tetraploid populations (subsp. obtusa) are found throughout the eastern flora, commonly occurring on limestone. The diploid (subsp. occidentalis) is found near the western edge of the species range, usually on sandstone and granitic substrates. Isozyme studies suggest that subsp. obtusa may have been derived from subsp. occidentalis through autopolyploidy (M. D. Windham 1993). The westernmost collections of Woodsia obtusa (all subsp. occidentalis) come from the Wichita Mountains of Oklahoma and the Edwards Plateau of Texas. Reports of this species from the trans-Pecos region of western Texas are apparently based on misidentifications. Subspecies 2. (Discussion copyrighted by Flora of North America; reprinted with permission.) |
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Key |
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Source | FNA vol. 2. | FNA vol. 2. | ||||
Parent taxa | ||||||
Sibling taxa | ||||||
Subordinate taxa | ||||||
Synonyms | Acrostichum alpinum, W. alpina var. bellii, W. bellii, W. hyperborea, W. ilvensis var. alpina | Aspidium obtusum, W. perriniana | ||||
Name authority | (Bolton) Gray: Nat. Arr. Brit. Pl. 2: 17. (1822) | (Swartz) Torrey: New York State, Rep. Geol. Surv. 195. (1840) | ||||
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