We examined soil microarthropod populations inhabiting a clay-silt soil of a tabosa grass (Hilaria mutica) swale in southern New Mexico. Maximum population densities of soil microarthropods occurred in September (48,400.m-2) and lowest densities were in July (1,250-m 2). These densities were 50% lower than those reported for well-drained soils on the upper parts of the same watershed. Prostigmatid mites made up 67% and cryptostigmatid mites, 26%, of the total microarthropod population. The ratio between prostigmatid and cryptostigmatid mites, approximately 4:1, was consistent throughout the year. Overall densities of microarthropod groups were correlated with soil moisture but many individual taxa were not. The most numerous and frequently occurring taxa [nanorchestid, tydeid and bdellid mites (Prostigmata); Aphelacarus sp. and Cosmochthonius sp. (Cryptostigmata)] are common in all Chihuahuan desert habitats examined to date and are common in other North American desert areas. INTRODUCTION Microarthropods constitute a numerically important component of the soil fauna. Microarthropods play an active role in breakdown of dead plant parts (Santos and Whitford, 1981), in vertical transport of organic material through the soil profile, in humus formation, and they may also increase microbial activity by disseminating fungal spores (Wallwork, 1970). Santos et al. (1978) and Franco et al. (1979) found that, in two North American desert areas, the microarthropod fauna was dominated by prostigmatid mites rather than the oribatid mites that feed on dead plant material in more mesic environments. Loots and Ryke (1967) working in different South African biotopes found that the soil moisture content was not always the most important factor determining the composition of the soil rnicroarthropod fauna. They found a significant correlation between the ratio of oribatei/trombidiformes (= prostigmata) and the percentage of organic matter in different soils. Montane piedmonts, bajadas, in the desert Southwest of North America, drain onto clay basins or flats which form from the deposition of fine particles. The clay and swales are characterized by poor drainage and poor percolation. Following rains, they may be inundated for varying periods. Clay pans may be unvegetated or have sparse shrub and grass cover. Swales are characterized by a dense cover of tabosa grass, Hilaria mutica. Litter accumulation constitutes an important storage reservoir in desert ecosystems and may affect soil water, which is generally thought to affect the density of soil fauna. Because of the soil characteristics of swales, i.e., poor drainage, low infiltration and percolation, high soil water content and relatively high vegetative cover, we hypothesized that the soil fauna would differ in taxonomic composition and exhibit less seasonal change in population size than microarthropod populations in better-drained desert soils. We further hypothesized that the population densities would be higher and numbers of taxa would be lower than those found in erosional soils. Whitford et al. (1981) used simulated rainfall in comparison to natural rainfall to follow the responses of a number of taxa as the soils dried. They found marked shifts in 1Present address: Department of Biology, Bar-Ilan University, Ramat Gan, Israel. 2Address reprint requests to: W.G. Whitford, Department of Biology, New Mexico State University, Las Cruces 88003.