A two-year study of the decomposition of alpine avens (Acomastylis ros
sii) foliage in alpine tundra of the Front Range of Colorado demonstra
ted a strong landscape-mediated effect on decay rates. Litter on sites
with intermediate amounts of snowpack decayed more rapidly than Litte
r on sites with larger or smaller amounts of snow. Annual decay consta
nts (k-values) of this foliage ranged from -0.33 in dry tundra to -0.5
2 in moist tundra to -0.47 in the wettest habitat. No site differences
in mass loss of litter were detected until late winter-early spring o
f the first year of decomposition, when significantly faster decomposi
tion was observed for litter beneath the snowpack. In spite of obvious
landscape-related patterns in rates of litter decomposition, total mi
croarthropod densities in the top 5 cm of soil did not differ among ha
bitats. However, the relative abundance of the oribatid and prostigmat
id mites did vary significantly across the landscape in relation to th
e moisture gradient. Oribatid mites comprised a greater proportion of
total mites in wetter areas. Microarthropod densities and composition,
as well as patterns of decomposition, were compared with previous alp
ine, as well as arctic tundra, studies. The effects of soil invertebra
tes on decomposition rates in the alpine were evaluated with a mushroo
m litterbag decomposition experiment. Naphthalene was used to exclude
fauna from a subset of litterbags placed in mesic and xeric habitats.
Mushrooms without naphthalene additions decayed significantly faster i
n the me sic sites. Densities of invertebrates were also greater on mu
shrooms in these mesic sites. Mushrooms placed in xeric sites generall
y lacked fauna. Thus, both the activities and the composition of the d
etritus-based food web appear to change substantially across the moist
ure gradient found in alpine tundra.