THERMAL AND HYDROGEOLOGICAL EVOLUTION OF
TAYLORSVILLE BASIN IN VIRGINIA: IMPLICATIONS FOR
SUBSURFACE GEOMICROBIOLOGY EXPERIMENTS
TSENG, Hsin-Yi, ONSTOTT, T. C., Department of
Geosciences, Princeton University, Princeton, NJ
08544
BURRUSS, R. C., U. S. Geological Survey, Denver, CO
80225
PERSON, M., Department of Geology and Geophysics,
University of Minnesota, Minneapolis, MN 55455
Micro-organisms were extracted from sidewall cores at 2800 m below
land surface in fine-grained sandstone and shale of the Triassic age
Doswell Formation of the Taylorsville Basin in Virginia (Stevens and
Boone, 1993). These micro-organisms containing saline tolerant,
thermophilic, anaerobic metal-reducers and fermenters appear to be
indigenous to the rock strata (McKinley et al., 1993). The observed
physiological traits of these bacteria, including thermophilicity,
salinity tolerance and pH preference, appear to be compatible with
geophysical estimates of current environmental conditions (Boone et
al., 1995). However, the thermal models from analyses of fluid
inclusions (Tseng et al., in press), of vitrinite reflectance, and of
apatite fission tracks, suggest that the strata have been exposed to
temperatures of 160-200°C at ~210 Ma followed by fast cooling and
that the current temperature was not attained until sometime in the
Tertiary. This implies that the bacteria migrated to their current
location. A two-dimensional steady-state fluid flow model indicates
that the present day groundwater flow rates are insufficient to transport
this microbial community from the surface. Instead, it is likely that the
migration of these bacteria is closely linked to the paleo-
hydrogeological evolution of the basin. A two-dimensional transient
fluid flow model suggests that the topographic relief generated at the
beginning of uplifting stage (e.g., 210-190 Ma) could drive
groundwater flow deep into the subsurface and yield the greatest flow
rate of 0.1 m/yr. This groundwater circulation caused fast cooling of
the strata after the thermal maximum, reduced the salinity of water as
recorded in secondary aqueous inclusions, changed hydrocarbon
compositions, and probably introduced bacteria into the microbial
sampling zone.
Boone, D.R., Liu, Y., Zhao, Z., Balkwill, D.L., Drake, G.R., Stevens,
T.O., and Aldrich, H.C., 1995, Bacillus infernus-sp. nov.: an
Fe(III)- and Mn(IV)-reducing anaerobe from the deep terrestrial
subsurface: International Journal of Systematic Bacteriology, v.
45, p. 441-448.
McKinley, J.P., Colwell, F.S., Long, P.E., Phelps, T.J., and Veverka,
C., 1993, The application of perfluorocarbon tracers to
subsurface microbial sampling: Abstract of Second International
Symposium of Subsurface Microbiology, Bath, UK..
Stevens, T.O. and Boone, D.R., 1993, Thermophilic anaerobic bacteria
in 2800-m-deep samples from the terrestrial subsurface:
Abstract of Second International Symposium of Subsurface
Microbiology, Bath, U.K..
Tseng, Hsin-Yi, Onstott, T. C., Burruss, R. C., and Miller, D. S., 1996,
Constraints on the thermal history of Taylorsville Basin, Virginia,
from fluid inclusion and fission track analyses: Implications for
subsurface geomicrobiology experiments: Chemical Geology (in
press).
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