Some natural ecosystems near industrialized and agricultural areas receive
atmospheric nitrogen inputs that are an order of magnitude greater than tho
se presumed for preindustrial rimes. Because nitrogen (N) often limits micr
obial growth on dead vegetation, increased N input can be expected to affec
t the ecosystem process of decomposition. We found that extracellular enzym
e responses of a forest-floor microbial community to chronically applied aq
ueous NH4NO3 can explain both increased and decreased litter decomposition
rates caused by added N. Microbes responded to N by increasing cellulase ac
tivity in decaying leaf litter of flowering dogwood, red maple, and red oak
, but in high-lignin oak litter, the activity of lignin-degrading phenol ox
idase declined substantially. We believe this is the first report of reduce
d ligninolytic enzyme activity caused by chronic N addition in an ecosystem
. This result provides evidence that ligninolytic enzyme suppression can be
an important mechanism explaining decreased decay rates of plant matter se
en in this and other N-addition experiments. Since lignin and cellulose are
the two most abundant organic resources on earth, these altered enzyme res
ponses signal that atmospheric N deposition may be affecting the global car
bon cycle by influencing the activities of microbes and their carbon-acquir
ing enzymes-especially the unique ligninolytic enzymes produced by white-ro
t fungi-over broad geographic areas.