NDLI: Rates of Microbial Metabolism in Deep Coastal Plain Aquifers

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Simple, Sensitive Zymogram Technique for Detection of Xylanase Activity in Polyacrylamide Gels

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Pyrolytic Methylation-Gas Chromatography of Whole Bacterial Cells for Rapid Profiling of Cellular Fatty Acids

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Fermentation studies of the secretion of Serratia marcescens nuclease by Escherichia coli.

Purification and Characterization of a Tripeptidase from Lactococcus lactis subsp. cremoris Wg2

Assessment of the endo-1,4-beta-glucanase components of Ruminococcus flavefaciens FD-1.

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Rates of Microbial Metabolism in Deep Coastal Plain Aquifers

Modeling of the Bacterial Growth Curve

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Nickel accumulation and storage in Bradyrhizobium japonicum.

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Combination of 16S rRNA-targeted oligonucleotide probes with flow cytometry for analyzing mixed microbial populations.

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Comparative Studies of Delignification Caused by Ganoderma Species †

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Stability of antibiotics under growth conditions for thermophilic anaerobes.

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Rates of Microbial Metabolism in Deep Coastal Plain Aquifers

Content Provider	PubMed Central
Author	Chapelle, Francis H. Lovley, Derek R.
Abstract	Rates of microbial metabolism in deep anaerobic aquifers of the Atlantic coastal plain of South Carolina were investigated by both microbiological and geochemical techniques. Rates of [2-14C]acetate and [U-14C]glucose oxidation as well as geochemical evidence indicated that metabolic rates were faster in the sandy sediments composing the aquifers than in the clayey sediments of the confining layers. In the sandy aquifer sediments, estimates of the rates of CO2 production (millimoles of CO2 per liter per year) based on the oxidation of [2-14C] acetate were 9.4 × 10−3 to 2.4 × 10−1 for the Black Creek aquifer, 1.1 × 10−2 for the Middendorf aquifer, and <7 × 10−5 for the Cape Fear aquifer. These estimates were at least 2 orders of magnitude lower than previously published estimates that were based on the accumulation of CO2 in laboratory incubations of similar deep subsurface sediments. In contrast, geochemical modeling of groundwater chemistry changes along aquifer flowpaths gave rate estimates that ranged from 10−4 to 10−6 mmol of CO2 per liter per year. The age of these sediments (ca. 80 million years) and their organic carbon content suggest that average rates of CO2 production could have been no more than 10−4 mmol per liter per year. Thus, laboratory incubations may greatly overestimate the in situ rates of microbial metabolism in deep subsurface environments. This has important implications for the use of laboratory incubations in attempts to estimate biorestoration capacities of deep aquifers. The rate estimates from geochemical modeling indicate that deep aquifers are among the most oligotrophic aquatic environments in which there is ongoing microbial metabolism.
Starting Page	1865
File Format	PDF
ISSN	10985336
e-ISSN	10985336
Journal	Applied and Environmental Microbiology
Issue Number	6
Volume Number	56
Language	English
Publisher Date	1990-06-01
Access Restriction	Open
Subject Keyword	Research in Higher Education
Content Type	Text
Resource Type	Article
Subject	Ecology Food Science Applied Microbiology and Biotechnology Biotechnology

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