You are not currently logged in.
Access JSTOR through your library or other institution:
If You Use a Screen ReaderThis content is available through Read Online (Free) program, which relies on page scans. Since scans are not currently available to screen readers, please contact JSTOR User Support for access. We'll provide a PDF copy for your screen reader.
Climates and Vegetation Pattern across the Mojave/Great Basin Desert Transition of Southern Nevada
Janice C. Beatley
The American Midland Naturalist
Vol. 93, No. 1 (Jan., 1975), pp. 53-70
Published by: The University of Notre Dame
Stable URL: http://www.jstor.org/stable/2424105
Page Count: 18
You can always find the topics here!Topics: Vegetation, Deserts, Species, Climate models, Rain, Desert soils, Shrubs, Playas, Drainage basins, Lowlands
Were these topics helpful?See something inaccurate? Let us know!
Select the topics that are inaccurate.
Since scans are not currently available to screen readers, please contact JSTOR User Support for access. We'll provide a PDF copy for your screen reader.
Preview not available
Plant communities of the transition between the Mojave and Great Basin deserts of southern Nevada are under the primary control of climatic variables. Rainfall increases and temperature decreases according to large increments of increase in elevation of the drainage basins from S to N. Within the basins, the climates and vegetation pattern are primarily under the control of patterns of air circulation and nocturnal cold air accumulations and secondarily, of edaphic factors. Minimum temperature and maximum mean rainfall tolerances of Mojave Desert Larrea (creosote bush) communities are exceeded across this transition as, apparently, are the mean maximum temperature and minimum rainfall tolerances of the Great Basin Artemisia (sagebrush) communities. In those communities which characterize the transition (Coleogyne, Grayia-Lycium andersonii, Lycium pallidum-Grayia, Lycium shockleyi), the Mojave and Great Basin temperature and rainfall regimes occur in various definable combinations. Only Atriplex confertifolia (shadscale) communities cannot be so defined; these occur along topographic gradients in both Mojave and Great Basin Desert climates. Contrasts in temperature regimes and their effects on vegetation in the lowlands of closed basins are illustrated by air temperature and plant data from two adjacent sites, with only 1.5 m elevation difference, near the playa of Frenchman Flat. All relationships are inferred from data collected during 10 years on a network of study sites on the Nevada Test Site of central-southern Nevada, whose drainage basins encompass the transition from the Mojave to the Great Basin Desert.
The American Midland Naturalist © 1975 The University of Notre Dame