We examined the content and isotopic composition of nitrogen within so
ils of a juniper woodland and found that a cryptobiotic crust composed
of cyanobacteria, lichens, and mosses was the predominant source of n
itrogen for this ecosystem. Disturbance of the crust has resulted in c
onsiderable spatial variability in soil nitrogen content and isotopic
composition; inter-canopy soils were significantly depleted in nitroge
n and had greater abundance of N-15 compared to intra-canopy soils. Va
riations in the N-15/N-14 ratio for inter- and intra-canopy locations
followed similar Rayleigh distillation curves, indicating that the gre
ater N-15/N-14 ratios for inter-canopy soils were due to relatively gr
eater net nitrogen loss. Coverage of cryptobiotic crusts has been redu
ced by anthropogenic activities during the past century, and our resul
ts suggest that destruction of the cryptobiotic crust may ultimately r
esult in ecosystem degradation through elimination of the predominant
source of nitrogen input.