The composition and structure of the semiarid or desert grasslands of south
western North America have changed over the past 150 y. Brushy or woody spe
cies in these communities have increased in density and cover. This increas
e in density of woody species is called brush encroachment because most of
these species have been present in these communities at lower densities for
thousands of years. The brushy or woody species were not introduced from o
ther continents or from great distances. They are indigenous species that h
ave increased in density or cover because of changes in local abiotic or bi
otic conditions. The brushy and woody plants are not the cause of these cha
nges, but their increase is the result of other factors. The causes of chan
ges that have led to the present woody-brushy composition of these semiarid
grasslands has been difficult to determine. Warming of the climate seems t
o be a background condition, but the driving force seems to be chronic, hig
h levels of herbivory by domestic animals. This herbivory has reduced the a
boveground grass biomass, leading to the reduction of fine fuel and a conco
mitant reduction or complete elimination of grassland fires. This combinati
on of factors favors the encroachment, establishment, survival and growth o
f woody plants. Less competition from grasses, dispersal of seeds of woody
plants by domestic animals, and changes in rodent, lagomorph, and insect po
pulations seem to modify the rate of change. Elevated levels of atmospheric
CO2 are not necessary to explain shrub encroachment in these semiarid gras
slands. The direction of future change is difficult to predict. The density
of brushy and woody plants will probably increase as will the stature and
number of species. However, if soil nutrients increase, woody legumes may b
e replaced by other brushy or woody species. Reversing the changes that hav
e been going on for 150 y will be a difficult, long-term, and perhaps impos
sible, task.