Am. Derry et al., Functional diversity and community structure of micro-organisms in three arctic soils as determined by sole-carbon-source-utilization, BIODIVERS C, 8(2), 1999, pp. 205-221
Functional diversities of micro-organisms in arctic soils at three incubati
on temperatures were assessed using sole-carbon-source-utilization (SCSU).
Soil samples were collected from an area of anthropogenic fertilization (mi
xed Dorset/Thule/Historic site), an area of animal enrichment (bird rock pe
rches), and unaltered tundra (raised beach; control soil site). The micro-o
rganisms were extracted from the soil samples and inoculated into Gram-nega
tive (GN) Biolog plates incubated at 30 degrees C, 10 degrees C, and 4 degr
ees C. Calculations of the Shannon index, substrate utilization richness, S
hannon evenness, and the Jaccard coefficient of similarity were based upon
substrate utilization on the Biolog plates. Principal component analysis di
stinguished microbial communities in enriched soils from unenriched soils.
At 10 degrees C and 4 degrees C, Shannon indices of enriched soil microbial
communities (10 degrees C: soils influenced by wild animals = 4.28, soils
influenced by human activities = 4.20; 4 degrees C: soils influenced by wil
d animals = 4.15, soils influenced by human activities=4.03) were significa
ntly higher than unenriched soil microbial communities (10 degrees C: 3.66;
4 degrees C: 3.38). Substrate utilization richness and evenness displayed
similar trends. Although Jaccard coefficients showed uniformity across the
different soil samples, cluster analysis supported patterns demonstrated by
PCA. Lower temperatures (4 degrees C and 10 degrees C) yielded greater res
olution between soil microbial communities than 30 degrees C based on Biolo
g colour development patterns.