The small mammal communities in four major plant associations were examined in the Whirlwind Valley, Eureka and Lander Counties, Nevada. All associations have been extensively grazed by livestock. Live trapping plots were placed and sampled seasonally in each habitat. Dipodomys microps and Perognathus parvus were the primary species within the big sagebrush and shadscale associations. In the greasewood association, P. maniculatus and Eutamias minimus were primary species. Microtus montanus, Reithrodontomys megalotis, Sorex vagrans, and Thomomys talpoides formed the small mammal community in the marsh-meadow association. Density was low on all plots, not exceeding a total of 13 individuals/ha. Grazing pressure probably accounts for the low habitat quality which did not support more than 0.6 kg/ ha biomass in shadscale and big sagebrush-shadscale, whereas less than 0.3 kg/ha was supported on each of the remaining habitats. Mammal species diversity was highest in greasewood and the ecotonal plot which corresponded to the habitats with the greatest plant diversity, cover, and vertical structure. The composition of small mammal communities changes from east to west in the Great Basin Desert of Nevada (Hall, 1946). The western edge of Nevada contains components of the southern Nevada Mohave Desert fauna that is lacking in the remainder of the northern part of the state. Detailed population studies which relate the temporal and spatial properties of small mammal community structure have not been conducted in northeastern Nevada. The high elevation, cold Great Basin Desert encompasses the intermontane region of Nevada, California, Utah, Idaho, Oregon, Washington, Montana, and Wyoming. In addition to the expected rigors of desert existence, small mammals must also cope with winters marked by intense cold. Inasmuch as this desert region consists of such a massive area, there are considerable variations in habitat mosaic and concomitant structural differences within respective small mammal communities. The shrub-steppe of south central Washington represents a six-species system of small mammals with 99% of the community represented by Perognathus parvus and Peromyscus maniculatus (O'Farrell et al., 1975). The Great Basin scrub of eastern California had a seven-species system with virtually all of the individuals belonging to Dipodomys microps, D. merriami, and Perognathus longimembris (Kenagy, 1973). Several habitat types were examined in Idaho and the composite community consisted of five species (Larrison and Johnson, 1973). A total of 12 species was documented for a sagebrush community in west-central Nevada (O'Farrell, 1974). Measures of seasonal population fluctuations are presented for all of these studies. The purpose of this study was to provide a baseline description of existing faunal conditions in the Whirlwind Valley in northern Nevada as a part of an environmental assessment of the Geysers Geothermal Resource Area. A thorough seasonal examination took place in all the major habitat types within this valley. T E S TH ESTERN NATURALIST 31(1):23-32 MARCH 31, 1986 This content downloaded from 157.55.39.192 on Wed, 24 Aug 2016 05:56:20 UTC All use subject to http://about.jstor.org/terms The Southwestern Naturalist STUDY AREA-The Whirlwind Valley is located about 80 km west of Elko, in portions of Lander and Eureka Counties, Nevada. The valley is formed by a bifurcation of the northern end of the Shoshone Range, bordered on the northwest by the Argenta Rim and on the southeast by the Malpais. Plant associations were mapped using aerial photographs and extensive ground truthing and designated by the nomenclature of Cronquist et al. (1972). Species identification follows Cronquist et al. (1972, 1977) and Holmgren (1942). Four major plant associations were found: big sagebrush, shadscale, greasewood, and marsh-meadow. The big sagebrush association occupied the upper elevations (1525 to 2205 m), including the Malpais with its steep northern slope. Soil tended to be rocky (17% ground cover). Dominant perennial species consisted of Artemisia tridentata, Poa nevadensis, Gutierrezia sarothrae, Grayia spinosa and Sitanion hystrix, in decreasing order of importance. Abundant annuals were Microsteris gracilis (30.2/m2) and Bromus tectorum (3.5/m2). Aerial perennial cover was 29% and mean height was 25.2 cm + 5.0 (1 S.E.). Perennial species richness was 18, diversity (H') 1.82, and evenness (V') 0.63. The shadscale association occurred adjacent to and interdigitated with big sagebrush (1463 to 1525 m) throughout most of the valley floor and gentler slopes. Soil tended to be less rocky (10% ground cover) and more saline than at the higher elevations. Dominant perennials were Atriplex confertifolia, Artemisia spinescens, Grayia spinosa, and Poa nevadensis. Annuals were dominated by Lepidium perfoliatum (49.2/m2), Microsteris gracilis (23.0/m2), and Bromus tectorum (14.9/ m2). Aerial perennial cover was 24% and mean height was 21.1 cm ± 6.2. Perennial species richness was 9, diversity 1.48, and evenness 0.67. The greasewood association occupied the lowest elevations (1402 to 1463 m) and the most saline soils. The soil surface predominantly was a salty crust devoid of rock. Dominant perennials were Sarcobatus vermiculatus, Suaeda fruticosa, Distichlis stricta, Chrysothamnus parryi, and Atriplex lentiformis. The primary annual was Atriplex pusilla (8.4/m2). Aerial perennial cover was 45% and mean height was 41.9 cm ± 12.7. Perennial species richness was 10, diversity 1.70, and evenness 0.74. The marsh-meadow association was a relatively small, discrete patch found in the runoff areas from the geothermal pools. This area was limited to seepage zones where water was readily available (1402 to 1463 m). Predominant perennial species were Distichlis stricta, Juncus balticus, Carex spp., Scirpus nevadensis, and Solidago spectabilis. Vegetative cover, excluding litter, was 70%. Climatic records taken during this study show some differences when compared to long term trends (Table 1). Mean temperature extremes differed slightly for most months although mean minimum values were generally higher than long term values from August 1982 through January 1983. Rainfall in 1982 was 5.3 cm greater than the 11 year mean. Large quantities of rain in March and September coupled with warm temperatures provided suitable conditions for germination and growth of annual vegetation. Data on livestock use in the Whirlwind Valley is generic at best. Bureau of Land Management (BLM) data is given in animal unit months (AUM); one animal unit (1 cow, 455 kg, plus a calf