Chaenactis thompsonii |
Chaenactis artemisiifolia |
|
---|---|---|
Thompson's pincushion |
artemisia leaf chaenactis, white pincushion |
|
Habit | Perennials, 10–30 cm (not or scarcely cespitose, not matted); proximal indument thinning with age, grayish, arachnoid-sericeous to thinly lanuginose. | Plants (15–)25–90(–200) cm. |
Stems | mostly 5–15+, ascending to erect. |
|
Leaves | mostly cauline, 2–5 cm; largest blades ± elliptic, ± plane, 1-pinnately lobed; lobes mostly 2–5 pairs, remote, ± plane. |
basal (withering) and cauline, 3–15(–20) cm; largest blades ± plane, not succulent; primary lobes mostly 5–10 pairs, ultimate lobes ± crowded, antrorse, lanceolate to elliptic, plane. |
Peduncles | ascending to erect, 2–5 cm. |
1.5–6 cm. |
Involucres | ± obconic. |
± hemispheric, mostly 10–15 mm diam. |
Receptacles | paleae 0. |
|
Corollas | 7–9 mm. |
5–7 mm. |
Phyllaries | longest (10–)12–15 mm; outer closely lanuginose, not stipitate-glandular, apices erect, ± rigid. |
longest 7–10(–12) mm, ± densely villous, not or sparsely glandular; apices (all) erect, ± green, acute or scarcely acuminate, not aristate, ± plane. |
Heads | mostly 1–3 per stem. |
|
Cypselae | 7–9 mm (eglandular); pappi: longest scales 3.5–5 mm. |
compressed, 4–7 mm; pappi 0 or coroniform (of ± 10 scales, longest 0.1–0.5 mm). |
2n | = 16. |
|
Chaenactis thompsonii |
Chaenactis artemisiifolia |
|
Phenology | Flowering Jun–Aug. | Flowering Apr–early Jul. |
Habitat | Rocky or gravelly serpentine slopes, scree, talus, openings in or above conifer forests | Dry canyons, open slopes, often over granitoid rocks, locally abundant in chaparral burns or other recovering disturbances |
Elevation | (900–)1200–2200 m ((3000–)3900–7200 ft) | 80–1600 m (300–5200 ft) |
Distribution |
WA
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CA; Mexico (Baja California)
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Discussion | Of conservation concern. Chaenactis thompsonii appears to be sister to C. evermannii; it is known from the mountains of central and northwestern Washington. The similar habits of C. thompsonii and C. ramosa (= C. douglasii var. douglasii) appear to result from convergent evolution in the distinctive habitat of their type localities (Wenatchee Mountains), not from a close genetic relationship as suggested by Cronquist. (Discussion copyrighted by Flora of North America; reprinted with permission.) |
In the flora area, Chaenactis artemisiifolia is known from the Transverse and Peninsular ranges and seaward valleys of southwestern California. It is fire-adapted; its germination is significantly enhanced by exposure to biomass smoke (J. E. Keeley and C. J. Fotheringham 1998). Chaenactis lacera Greene, the eighteenth species of the genus, is known from coastal portions (including islands) of the western Vizcaíno Desert in Baja California and Baja California Sur, Mexico. Forms of C. artemisiifolia sometimes resemble C. lacera in coastal southern California (P. Stockwell 1940), where C. lacera could eventually be introduced. Besides the key characteristics above, C. lacera differs from C. artemisiifolia by its largest leaf blades broadly ± elliptic, 2–3-pinnately lobed, ultimate lobes remote, recurved to retrorse, ± linear, involute (leaf blades appearing ± skeletal). (Discussion copyrighted by Flora of North America; reprinted with permission.) |
Source | FNA vol. 21, p. 407. | FNA vol. 21, p. 402. |
Parent taxa | ||
Sibling taxa | ||
Synonyms | Acarphaea artemisiifolia | |
Name authority | Cronquist: in C. L. Hitchcock et al., Vasc. Pl. Pacif. N.W. 5: 123, fig. [p. 125]. (1955) | (Harvey & A. Gray) A. Gray: Proc. Amer. Acad. Arts 10: 74. (1874) |
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