We revisited 68 plots of forest vegetation in the San Bernardino Mount
ains that had been quantitatively described in 1929-1935 from the Cali
fornia Vegetation Type Map (VTM) Survey. By using the same sampling me
thods, we documented changes-over approximately 60 years and during a
period of fire suppression management-in tree density by both species
and size class. In general we found increasing stand densities, a tran
sformation from old-growth age structure to young growth, and a compos
itional shift from Pinus ponderosa and P. jeffreyi to Abies concolor a
nd Calocedrus decurrens. Density of trees of more than 12 cm diameter
at breast height (dbb) increased by 79%, including three to ten-fold i
ncreases in the youngest cohorts 12-66 cm dbh. The magnitude of change
depended upon initial forest composition and local annual precipitati
on. Monotypic stands of P. jeffreyi or those initially dominated by Ab
ies concolor showed the least change in species composition; the most
xeric stands of P. jeffreyi showed the least gain in density and mesic
mixed P. ponderosa stands showed the most dramatic change in composit
ion and density. We compared these data to records of past and present
forests in the Sierra Nevada and found parallel trends but magnified
by the increased precipitation of the Sierra Nevada. We also compared
VTM data from the San Bernar dino Mountains to mixed conifer forests i
n the Sierra San Pedro Martir of Baja California. These Mexican sites
and forests are ecologically similar to those in California but they s
till experience unmanaged fire regimes. Californian forests of 60 year
s ago are remarkably similar to modern forests in the Sierra San Pedro
Martir. Thus, we conclude that forest changes in the San Bernardino M
ountains are primarily due to lengthening fire intervals. Forest chang
es as a result of fire suppression have important conservation consequ
ences for bird species diversity in general and for Spotted Owl and Ne
otropical migrants in particular.