Physaria hitchcockii subsp. hitchcockii |
Physaria hitchcockii subsp. confluens |
|
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Habit | Plants forming tufts; caudex not elongated, not elastic. | Plants forming soft mats; caudex elongated, elastic (creeping). |
Basal leaves | petiole differentiated from blade (sometimes weakly); blade oblanceolate to obovate. |
petiole differentiated from blade (sometimes weakly); blade oblanceolate to obovate. |
Fruits | 2.6–3.8 mm wide. |
1.7–3 mm wide. |
Anthers | 1.4–1.8(–2) mm. |
1–1.5 mm. |
Physaria hitchcockii subsp. hitchcockii |
Physaria hitchcockii subsp. confluens |
|
Phenology | Flowering Jun–Jul. | Flowering Jun–Jul. |
Habitat | Gravelly or rocky limestone at or above timberline | Gravelly or rocky limestone |
Elevation | 2300-3500 m (7500-11500 ft) | 2300-3500 m (7500-11500 ft) |
Distribution |
NV; UT |
NV |
Discussion | It is possible that populations of subsp. hitchcockii on the Table Cliff Plateau, Utah, are consubspecific with the nearby subsp. rubicundula. The leaf blades are indistinguishable from the material from Nevada and the plants do not form elongated, elastic caudices. Subspecies hitchcockii is found in the Sheep Range and Spring Mountains (Charleston Mountain), Nevada, and on the Table Cliff Plateau, Utah, where it is limited to the white member of the limestone Wasatch (Claron) Formation. (Discussion copyrighted by Flora of North America; reprinted with permission.) |
Subspecies confluens is found at or above timberline in the Grant, Quinn Canyon, and Schell Creek ranges. (Discussion copyrighted by Flora of North America; reprinted with permission.) |
Source | FNA vol. 7, p. 643. | FNA vol. 7, p. 643. |
Parent taxa | ||
Sibling taxa | ||
Synonyms | Lesquerella hitchcockii subsp. confluens, Lesquerella confluens | |
Name authority | unknown | (Maguire & A. H. Holmgren) O’Kane: Novon 17: 380. (2007) |
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