We investigated the effects of native ungulates on grassland N cycling
in Yellowstone National Park by examining natural N-15 abundance (del
ta(15)N) of soils and plants inside and outside long-term (32-36 yr) e
xclosures. Across six topographically diverse sites, grazers increased
delta(15)N Of soil (0-20 cm) by 0.7 parts per thousand, which was sub
stantial considering that values for ungrazed soil ranged 2.4 parts pe
r thousand (2.4-4.8 parts per thousand). The magnitude of grazer N-15
enrichment was positively related (r(2) = 0.70) to the intensity of he
rbivore activity during the study, indexed by the amount of dung (g/m(
2)) deposited at the sites. We also found that soil delta(15)N Of ungu
late urine and dung patches was significantly higher than that of cont
rol areas. Grazers probably increased soil delta(15)N by promoting N l
oss from the soil via leaching, ammonia volatilization, and/or denitri
fication. Each of these processes results in the removal of N-15 deple
ted products from the soil and, consequently, N-15 enrichment of the r
emaining soil. In contrast to soil results, grazers reduced plant N-15
by an average of 0.7 parts per thousand, probably due to isotopically
light, soil NO3-(compared to soil NH4+) constituting a more important
N source for plants in grazed grassland relative to those in ungrazed
grassland. These findings indicate that native grazers increased N lo
ss from this north-temperate grassland as a result of accelerated loss
es on urine-and dung-affected microsites and, potentially, from elevat
ed N loss throughout the grazed landscape due to grazers promoting N c
ycling. Furthermore, these results suggest that herbivores increase pl
ant NO3-assimilation, which may positively affect primary productivity
in this grazed ecosystem.