Studies in temperate grassland ecosystems have shown that differences in co
mposition of C-3 and C-4 plant functional types can have important influenc
es on ecosystem pools and processes. We used a plant community dynamics mod
el (STEPPE) linked to a biogeochemical cycling model (CENTURY) to determine
how ecosystem properties in shortgrass steppe are influenced by plant func
tional type composition. Because of phenological differences between C-3 an
d C-4 plants, we additionally simulated the effects of precipitation season
ality on plant communities and examined how C-3 and C-4 composition interac
ts with precipitation to affect ecosystems. The model output suggests that
differences in C-3 and C-4 composition can lead to differences in soil orga
nic carbon (C) and nitrogen (N) within 1000 simulation years. Soil organic
C and N (g C and N m(-2) to 0.2-m depth) were least in a 100% C-3 community
compared with a 100% C-3 community and a mixed C-3-C-4 community. A change
in the time of maxi-mum precipitation from summer to spring in a simulated
shortgrass steppe slightly favored C-3 plants over C-4 plants. The proport
ion of total net primary production accounted for by C-3 plants increased f
rom 21% to 25% after 200 years, when 90 mm of precipitation was switched fr
om summer to spring. Soil organic matter (SOM) was relatively stable in the
C-4-dominated communities with respect to changes in precipitation seasona
lity, whereas SOM in the C-3 community was sensitive to precipitation seaso
nality changes. These results suggest an important interaction between plan
t community composition and precipitation seasonality on SOM, with phenolog
y playing a key role.