A procedure for estimating Bacillus cereus spores in soil and stream-sediment samples — A potential exploration technique
Journal of Geochemical Exploration
By: J.R. Watterson
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Abstract
The presence of bacterial spores of the Bacillus cereus group in soils and stream sediments appears to be a sensitive indicator of several types of concealed mineral deposits, including vein-type gold deposits. The B. cereus assay is rapid, inexpensive, and inherently reproducible. The test, currently under investigation for its potential in mineral exploration, is recommended for use on a research basis.
Among the aerobic spore-forming bacilli, only B. cereus and closely related strains produce an opaque zone in egg-yolk emulsion agar. This characteristic, also known as the Nagler of lecitho-vitellin reaction, has long been used to rapidly indentify and estimate presumptive B. cereus. The test is here adapted to permit rapid estimation of B. cereus spores in soil and stream-sediment samples. Relative standard deviation was 10.3% on counts obtained from two 40-replicate pour-plate determinations. As many as 40 samples per day can be processed. Enough procedural detail is included to permit investigation of the test in conventional geochemical laboratories using standard microbiological safety precautions.
Suggested Citation
Watterson, J., 1985, A procedure for estimating Bacillus cereus spores in soil and stream-sediment samples — A potential exploration technique: Journal of Geochemical Exploration, v. 23, no. 3, p. 243-252, https://doi.org/10.1016/0375-6742(85)90028-7.
| Publication type | Article |
|---|---|
| Publication Subtype | Journal Article |
| Title | A procedure for estimating Bacillus cereus spores in soil and stream-sediment samples — A potential exploration technique |
| Series title | Journal of Geochemical Exploration |
| DOI | 10.1016/0375-6742(85)90028-7 |
| Volume | 23 |
| Issue | 3 |
| Year Published | 1985 |
| Language | English |
| Publisher | Elsevier |
| Description | 10 p. |
| First page | 243 |
| Last page | 252 |