Dl. Haldeman et Ps. Amy, BACTERIAL HETEROGENEITY IN DEEP SUBSURFACE TUNNELS AT RAINIER MESA, NEVADA TEST SITE, Microbial ecology, 25(2), 1993, pp. 183-194
To characterize the deep subsurface environment of Rainier Mesa, Nevad
a Test Site, rock samples were taken from tunnels U 12b, U 12g, U 12p,
and U 12n, which varied in depth from 50 m to 450 m and in gravimetri
c moisture content from 4% to 27%. Values for total count, viable coun
t, biomass, Simpson diversity, equitability, similarity coefficient, a
nd number of distinct colony types indicated microbiological variabili
ty between samples. Viable counts ranged from less than 1 x 10(1) to 2
.4 x 10(5) CFU g dry wt-1 of rock. Direct counts and enumeration based
on phospholipid determination indicated larger numbers of cells g dry
wt-1 of rock than viable counts. Simpson diversity indices, equitabil
ity, and numbers of distinct colony types varied from 3.00 to 8.05, 0.
21 to 0.89, and 7 to 19, respectively, and indicated heterogeneity bet
ween samples. Each distinct morphotype was purified and characterized.
Gram reaction, morphology, metal and antibiotic resistances, and meta
bolic activities of each isolate confirmed spatial variability among m
icrobiota isolated from different locations. Most probable numbers of
nitrifying, sulfur oxidizing, and sulfur-reducing bacteria were below
the limit of detection in all samples, while the numbers of nitrogen f
ixing bacteria ranged from below the level of detection to 7.8 x 10(2)
cells g dry wt-1 of rock sample, and the numbers of dentrifying bacte
ria ranged from below the level of detection to greater than 1.6 x 10(
3) cells g dry wt-1 of rock sample.