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Topography and climate: Black greasewood thrives in many areas and plant associations from Mexico to Canada, but prefers the cold deserts north of 37o latitude [116]. Throughout its range, black greasewood grows from 500 to 8,000 feet (152-2,438 m) in elevation [78,112,116]. It is found at low to middle elevations in the intermountain region (1,000-8,000 feet) [16,18,85,107], as well as subalpine to alpine sites [83].
Annual temperatures in the shadscale zone where black greasewood is often dominant may range from a maximum of 110 oF (43 oC) to a minimum of -30 oF (-34 oC). Daily temperature fluctuations may be 21 oF in January and 56 oF during summer months [11,52]. Black greasewood grows in areas receiving 3 to 20 inches (76-508 mm) of annual precipitation [11,52,107,112]. Precipitation is unevenly distributed, with most falling during 2 periods: March through May and July through August. Summer precipitation is often in the form of cloudbursts: quick, high volume showers that provide limited available water for plants due to high runoff and evaporation in high summer temperatures [52].
Black greasewood occupies sites ranging from wetlands to deserts and open to wooded areas [83]. In the Intermountain area, it is often confined to alkali soils on alluvial areas, floodplains, dry washes, and gullies where soil moisture is high. Black greasewood often dominates desert areas where runoff waters have accumulated [18,47,76,78,84,93,103]. In the northern Great Plains, black greasewood is common on bottomland flats, adjacent gentle slopes, and stream bottoms [9,66,134].
Soils: Soils supporting black greasewood include silt-clays, clay-loams, silt-loams, or deep fine sand-loams [47,76,93,134]. Black greasewood may grow on sandy soil in the northeastern part of its range, but it is most commonly associated with heavy textured soils of high salt content (0.05-1.6%) [15,16,48,48,78,85,116,131]. Black greasewood is halophytic [20,37,48] and often associated with saline [8,16,21,36,76,78,93] and alkaline soils [21,36,78] that may have a pH of 6.2 to 9.8 [8,36,47,76,131]. Donovan and Richards [39] found that black greasewood is more stress tolerant than rubber rabbitbrush, growing better on sites high in sodium and boron. Black greasewood frequently occurs in nearly pure stands in saline conditions [15,16,48,78]. Black greasewood is not, however, an infallible indicator of high soil salt content; it also grows well on nonsaline soils [27,48,128].
On black greasewood sites, surface soil may be rich in sodium and other cations, especially immediately beneath greasewood shrubs where localized recycling occurs [71,103]. Black greasewood accumulates sodium in its leaves and creates a salt-enriched microenvironment under its canopy due to leaching of salt from shed leaves [40,114]. Soils are likely alkali-sodic in the upper stratum immediately under the plant crown, and either saline or alkali-sodic between plants and in the strata below a depth of 9 to 12 inches (23-30 cm) [47]. The accumulation of osmotically active salts facilitates black greasewood's tolerance of very saline sites. Higher leaf ion concentration can maintain lower osmotic potentials and thus maintain water uptake [40]. In one Washington study, sodium content of black greasewood leaves steadily increased from about 45 mg/g of dry matter in late April to 118 mg/g in early November [114]. Black greasewood can accumulate large amounts of leaf sodium over a range of sites from non-saline to highly saline, contributing to its success over salinity gradients. It is also able to maintain adequate uptake of N, P, K, Ca, and Mg under variable substrate combinations of nutrients and sodium [41].
The following table presents mean values (n=10) for various soil characteristics from 4 depths in a Utah black greasewood community [64]:
Soil depth 0-6 inches (0-15 cm) 6-18 inches (15-46 cm) 18-36 inches (46-91 cm) 36-60 inches (91-152 cm) pH 8.2 8.7 8.4 8.2 total soluble salts (%) 0.29 0.82 1.03 1.19 lime (%) 13 19 19 14 permeability (in./hr) 0.25 0.12 0.16 0.31 sodium (ppm) 580 1,865 2,355 2,946 calcium (ppm) 63 88 237 1,003 magnesium (ppm) 20 47 80 166 potassium (ppm) 158 118 90 118 chloride (ppm) 788 2,425 2,894 3,557 sulfate (ppm) 140 1,323 1,412 4,244 carbonate (ppm) 0 0 1 0 bicarbonate (ppm) 587 697 546 432
Average soil nutrient contents from additional black greasewood communities in Utah are higher [24]:
percent nitrogen 0.13 phosphorus (ppm) 18.6 calcium (ppm) 9062.30 magnesium (ppm) 607.80 sodium (ppm) 1031.20 percent sodium saturation 8.64 potassium (ppm) 921.00 iron (ppm) 5.80 manganese (ppm) 8.70 zinc (ppm) 1.70 copper (ppm) 2.20
In addition to salt tolerance, black greasewood is also drought tolerant [78]. However, it may respond to severe drought with leaf drop, reduced canopy size, or increased mortality [40]. Black greasewood is intolerant of strongly acid soils [112].
Water relations: Black greasewood is phreatophytic [40,48], and its distribution is well correlated with the distribution of groundwater [103]. It is also believed to be related to the amount of exchangeable sodium and the percent of water retained at field capacity [116,131]. Black greasewood stands develop best where moisture is readily available, either from surface or subsurface runoff [27]. It is commonly found on floodplains that are either subject to periodic flooding, have a high water table at least part of the year, or have a water table less than 34 feet (10.5 m) deep [15,16,20,48,48,71,78,85]. A study of an expanding lake in Oregon found that black greasewood tolerated flooding for 40 days before negative effects were apparent. Water tables within 9.8 to 11.8 inches (25-30 cm) of the surface had no effect on black greasewood [62]. Another study, conducted in California, found that black greasewood did not survive 6 months of continuous flooding [67,68].