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alpine cliff fern, alpine woodsia, northern cliff fern, woodsie alpine

Plummer's cliff fern, Plummer's woodsia

Stems

compact, erect to ascending, with cluster of persistent petiole bases of ± equal length;

scales uniformly brown, lanceolate.

compact, erect to ascending, with a few 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.

Leaves

2.5–20 × 0.5–2.5 cm.

5–25 × 1.5–6 cm.

Petiole

reddish brown or dark purple when mature, articulate above base at swollen node, relatively brittle and easily shattered.

reddish brown to dark purple when mature, not articulate above base, somewhat pliable and resistant to shattering.

Blade

linear to narrowly lanceolate, usually pinnate-pinnatifid proximally, lacking glands, never viscid;

rachis with widely scattered hairs and scales.

lanceolate to ovate, usually 2-pinnate proximally, densely glandular, often somewhat viscid;

most glandular hairs with thick stalks and distinctly bulbous tips;

rachis with abundant glandular hairs and a few narrow scales.

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 5–11 pairs of pinnules;

abaxial and adaxial surfaces glandular, lacking nonglandular hairs or scales.

Indusia

of narrow, hairlike segments, these uniseriate throughout, composed of cells many times longer than wide, usually surpassing mature sporangia.

of relatively broad segments;

segments multiseriate for most of length, often divided and uniseriate distally, composed of ± isodiametric cells, often surpassing mature sporangia.

Spores

averaging 46–53 µm.

averaging 44–50 µm. 2n = 152.

Pinnules

entire or broadly crenate;

margins nonlustrous, thin, with occasional isolated cilia, lacking translucent projections.

dentate, often shallowly lobed;

margins nonlustrous, thin, densely glandular, lacking cilia but with occasional 1–2-celled translucent projections.

Vein

tips often enlarged to form whitish hydathodes visible adaxially.

tips slightly (if at all) enlarged, barely visible adaxially.

Woodsia alpina

Woodsia plummerae

Phenology Sporulating summer–early fall. Sporulating late spring–fall.
Habitat Crevices and ledges on cliffs (occasionally on rocky slopes), mostly slaty and calcareous rocks Cliffs and rocky slopes, usually on granite or volcanic substrates
Elevation 0–1500 m (0–4900 ft) 700–3100 m (2300–10200 ft)
Distribution
from FNA
AK; ME; MI; MN; NH; NY; VT; BC; MB; NB; NF; NS; NT; ON; QC; SK; YT; Greenland; n Eurasia
[BONAP county map]
from FNA
AZ; CA; CO; NM; OK; TX; n Mexico
[WildflowerSearch map]
[BONAP county map]
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.)

The origin and phylogenetic affinities of the tetraploid Woodsia plummerae have not been established with certainty. The hypothesis that it arose as a hybrid between the Mexican species W. mollis (Kaulfuss) J. Smith and W. mexicana Fée (D. F. M. Brown 1964; D. B. Lellinger 1985) seems untenable in light of recent chromosome studies indicating that the latter species is also tetraploid (M. D. Windham 1993). On the basis of sporophyte morphology and spore ornamentation, W. plummerae appears most closely related to the W. mexicana complex and W. oregana. In fact, W. oregana can be difficult to separate from W. plummerae in western New Mexico and northern Arizona. Intermediate plants occurring in this region may represent stable allotetraploids resulting from hybridization between the diploid progenitors of W. plummerae and W. oregana subsp. cathcartiana. Considering the available evidence, populations of W. plummerae in the United States probably originated through autopolyploidy from a recently discovered, but as yet unnamed, Mexican diploid of similar morphology. Woodsia plummerae occasionally hybridizes with W. phillipsii to produce sterile, morphologically intermediate triploids.

(Discussion copyrighted by Flora of North America; reprinted with permission.)

Source FNA vol. 2. FNA vol. 2.
Parent taxa Dryopteridaceae > Woodsia Dryopteridaceae > Woodsia
Sibling taxa
W. cochisensis, W. glabella, W. ilvensis, W. neomexicana, W. obtusa, W. oregana, W. phillipsii, W. plummerae, W. scopulina
W. alpina, W. cochisensis, W. glabella, W. ilvensis, W. neomexicana, W. obtusa, W. oregana, W. phillipsii, W. scopulina
Synonyms Acrostichum alpinum, W. alpina var. bellii, W. bellii, W. hyperborea, W. ilvensis var. alpina W. obtusa var. glandulosa, W. obtusa var. plummerae, W. pusilla var. glandulosa
Name authority (Bolton) Gray: Nat. Arr. Brit. Pl. 2: 17. (1822) Lemmon: Bot. Gaz. 7: 6. (1882)
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