More info for the terms: constancy, cover, frequency, litter, presence, xeric
Throughout its range, Hood's phlox occupies dry, open, rocky, gravelly, or sandy sites [4,41,62,67,68,72,95].
Specific characteristics are described for several areas where Hood's phlox is common. Near Saskatoon, Saskatchewan, Hood's phlox importance values were greatest on the upper and middle positions on eastern to southern slopes. From May to September soil temperatures on upper and middle southern slopes averaged 81 °F (27 °C), and average soil moisture content was 7.9% and 5.3%, respectively. Hood's phlox importance changed dramatically with relatively minor changes in aspect and position [12].
In Eagle, Alaska, Hood's phlox occurred in fringed sagebrush (Artemisia frigida)/bluebunch wheatgrass steppe vegetation but not in forested vegetation dominated by quaking aspen (Populus tremuloides), balsam poplar (P. balsamifera), and white spruce (Picea glauca). Environmental conditions were different in the 2 habitats. Soil moisture was lower and soil temperature was higher in steppe vegetation than in the forests. Steppe vegetation received 93.9% full sun and forests received 57%. Litter cover was 5% in steppe vegetation and 79% in forests [139].
Hood's phlox was common on glacial moraines in northwestern Montana's Upper Blackfoot Valley and reached its greatest frequency on the upper part of southern slopes. Summer soil moisture content averaged 11% on upper slopes, less than that of lower slope positions. Temperatures were higher and temperature fluctuations were greatest on southern slopes [16].
Hood's phlox is most typical in sagebrush habitats. Characteristics of some of these habitats are summarized below.
Rangeland cover type Elevation
(feet) Annual precipitation/climate Soils Black sagebrush
(A. nova) middle elevations 8-12 inches, most common coarse textured, dry soils [128] Low sagebrush
(A. arbuscula) 3,000-9,000 8-16 inches shallow soils; normally 12-20 inches to clay or bedrock [129] Stiff sagebrush
(A. rigida) 700-4,000 8-16 inches shallow soils; typically < 9.8 inches to basalt [130] Threetip sagebrush 4,000-9,000 12-16 inches; cool, moderately moist sites intermediate between big sagebrush and low and black sagebrush types [127] Wyoming big sagebrush ---- 7-12 inches; ~40% in growing season moderate to fairly shallow, low in organic matter, stony, often over hardpan or parent material [126]
Climate: Hood's phlox primarily occupies sites with continental climates. Conditions are typically dry, and a wide range of temperatures are possible. In North Dakota, Hood's phlox occurs in the west where arid conditions prevail [109]. Parker [95] reports that Hood's phlox occupies sites that receive 15 to 20 inches (380-510 mm) of annual precipitation. However, Hood's phlox occurs in steppe vegetation in Eagle, Alaska, where annual precipitation averages 12.1 inches (308 mm) and average January and July temperatures are -9.4 °F (-23 °C) and 59 °F (15 °C), respectively [139]. In areas near Saskatoon, Saskatchewan, where Hood's phlox occurs, snow is typical from November to March and contributes 30% to the total annual precipitation. Summer temperatures over 100 °F (38 °C) and winter lows of -40 °F (-40 °C) have been recorded for this area [12]. In the Laramie Basin of Wyoming, precipitation averages 11.2 inches (284 mm), and January and July temperatures average 22.4 °F (-5.3 °C) and 64 °F (17.8 °C) [49]. Hood's phlox is sparsely distributed on the Dickinson Experimental Station in southwestern North Dakota, where winters are long and cold, and summers are short and hot. Based on a 70-year record, annual precipitation averaged 15.5 inches (394 mm), and June temperatures averaged 61.4 °F (16.3 °C) [54].
A number of studies indicate that Hood's phlox is restricted to sites with early snow melt. Hood's phlox was rarer on sites with late snow melt dates than on sites with early melting dates on the Bangtail Mesa near Bozeman, Montana [136]. Hood's phlox was common (presence 56%) on sites with a snow melt date of 15 May in southwestern Montana; Hood's phlox presence decreased as snow cover remained longer. Presence was 27% on sites with a 1 June melt date, and Hood's phlox was absent from sites with melt date of 15 June or later [90]. In central Wyoming's Owl Creek range, Hood's phlox was present on windblown sites in threetip sagebrush-dominated sites but was absent from sites where deep snow drifts were common [50].
Elevation: Hood's phlox is common at middle and high elevations throughout its range. Narrower elevational ranges by state and variety are provided below:
State/region Variety, if applicable Elevation in feet Arizona 4,000 [72] California P. h. ssp. canescens 4,500-8,900 [61,94] P. h. ssp. lantana 4,000-6,000 [94] P. h. ssp. muscoides 4,600-8,900 [61] New Mexico P. h. ssp. canescens 5,000-7,000 [88] Nevada 4,500-8,000 P. h. ssp. lantana 6,500-8,000 P. h. ssp. muscoides 5,600-8,000 [71] Uinta Basin, Utah 4,800-8,400 P. h. ssp. muscoides ~7,100 [55] Utah 4,000-6,700 [95] P. h. ssp. canescens 4,790-10,700 P. h. ssp. muscoides 4,590-6,910 [138]
Soils: Hood's phlox persists on a variety of soil types; however, it commonly occurs on dry, coarse textured soils. In the northern Great Plains and in Utah, Hood's phlox occurs on gravelly, rocky, or sandy soils [57,95]. In grasslands of southwestern Saskatchewan, Hood's phlox was most closely associated with clay and loam soils and was present on fine sandy loams, loams, and clay loams [64]. In steppe vegetation of central Montana, Hood's phlox cover and constancy were "consistently" higher on fine-textured soils, and Hood's phlox showed little preference for position along a gradient of 0.4 to 4 inches (1-10 cm) of water storage capacity [59]. Hood's phlox was most common on windward exposures where soil moisture was lowest in sagebrush steppe vegetation at Wyoming's Stratton Sagebrush Hydrology Study Area [24]. In Utah, Hood's phlox coverage was significantly greater (p≤0.01) on crest than mid-slope or base sites. Crest sites were the most xeric and had the shallowest soils, which averaged 8 inches (20 cm) deep. Clay content was significantly lower and sand and exposed rock were significantly greater on crest than mid-slope or base positions [21].