Physiological Diversity and Distributions of Heterotrophic Bacteria in Deep Cretaceous Sediments of the Atlantic Coastal Plain
- 1 February 1991
- journal article
- research article
- Published by American Society for Microbiology in Applied and Environmental Microbiology
- Vol. 57 (2) , 402-411
- https://doi.org/10.1128/aem.57.2.402-411.1991
Abstract
A series of 23 intact core segments was obtained from two distinct deep subsurface geological formations, the Middendorf and the Cape Fear formations, underlying the southeastern coastal plain of South Carolina. The Middendorf formation in this region consists of permeable, saturated, sandy sediments; the Cape Fear formation consists mainly of less permeable sediments. The core segments were separated by vertical distances ranging from several centimeters to 48 m. Aerobic chemoheterotrophic bacteria were enumerated on a dilute medium, and populations ranged from 3.1 to 6.4 log CFU g of sediment-1 in the Middendorf cores and from below detection to 4.3 log CFU g-1 in the Cape Fear cores. A total of 198 morphologically distinct colony types were isolated, purified, and subjected to 108 different physiological measurements. The isolates from the two formations were distinct (i.e., they produced substantially different response patterns to the various physiological measurements), as were those in different core samples from the same formation. Cluster analysis revealed 21 different biotypes based on similarities of 75% or higher in response patterns to 21 physiological assays. One biotype contained 57 (29%) of the subsurface isolates, 10 biotypes contained 5 or more isolates, and the remainder had 4 or fewer. The organic compounds that were most commonly metabolized by the subsurface bacteria included Tween 40 (85%) and β-hydroxybutyric acid (60%). Organic acids, in general, were also commonly metabolized by the subsurface bacteria. Isolates from the Cape Fear core segments were capable of metabolizing a higher percentage of the substrates than were bacteria isolated from the Middendorf formation. Although the heterogeneous distributions of bacteria in deep subsurface sediments may make it difficult to use aquifer microcosms to predict in situ biotransformation rates, the diversity of the physiological properties of these organisms offers promise for in situ remediation of contaminants.Keywords
This publication has 6 references indexed in Scilit:
- Rates of Microbial Metabolism in Deep Coastal Plain AquifersApplied and Environmental Microbiology, 1990
- Comparison of phenotypic diversity and DNA heterogeneity in a population of soil bacteriaApplied and Environmental Microbiology, 1990
- Vertical and Horizontal Variations in the Physiological Diversity of the Aerobic Chemoheterotrophic Bacterial Microflora in Deep Southeast Coastal Plain Subsurface SedimentsApplied and Environmental Microbiology, 1989
- Isolation and characterization of quinoline-degrading bacteria from subsurface sedimentsApplied and Environmental Microbiology, 1989
- Microbial Ecology of the Terrestrial SubsurfaceAdvances in applied microbiology, 1988
- Characterization of Subsurface Bacteria Associated with Two Shallow Aquifers in OklahomaApplied and Environmental Microbiology, 1985