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Volume 58—1978

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MICROBIAL FORMATION OF CARCINOGENIC DIMETHYLNITROSAMINE

S. K. Pancholy* and M.A.B. Mallik

Langston University, Langston, Oklahoma


*Present address: Box 29, Florida A & M University, Tallahassee, FL 32307.

Microorganisms possessing high nitrate reductase activity generally produce carcinogenic dimethylnitrosamine at neutral pH when incubated with dimethylamine and nitrate. Cell suspensions of several microorganisms enhanced nitrosation of dimethylnitrosamine in the presence of nitrite; however, involvement of an enzyme was not detected.

The formation of nitrosamine in natural ecosystems in the presence of high concentrations of secondary amines and nitrite has been demonstrated by Ayanaba et al. (1) and Pancholy (2). Secondary amines occur widely among plant and animal kingdoms (3), which ultimately find their way into the soil. During decomposition, certain pesticides (e.g. thiram, eptam, and vernam) are known to produce secondary amines (4). There exists the possibility that nitrite concentrations may attain high levels at localized microsites to effect nitrosation of secondary amines.

The occurrence and formation of dimethylnitrosamine (DMNA) has been intensively studied because of its high toxicity, carcinogenicity, high water solubility, and ubiquitous occurrence of the precursor amines (5, 6). Soluble DMNA, synthesized in soil, may leach downward into the natural water table and eventually pose a health hazard to wild animals, livestock, and human beings. Sander (7) first pointed out that bacteria can cause the nitrosation reaction at neutral pH. A microbial contribution in the synthesis of nitrosamines has been shown (8). The present investigation was designed to study the role of microorganisms in the synthesis of DMNA at neutral pH.

MATERIALS AND METHODS

Nitrate-utilizing microorganisms were isolated from six different sources (two soils, lake sediments, sewage, and sheep and cattle feed lots) by using nitrate-agar medium (glucose 2% KNO3 0.2%, K2HPO4 1.06%, KH2PO4 0.53%, MgSO4 0.01%, and agar 1.5%). Eight isolates of bacteria, one actinomycete and four fungi were obtained this way. Two bacteria (DM-A) and (DM-B) that could utilize dimethylamine (DMA) as the sole source of both carbon and nitrogen were isolated from the sewage and sheep feed lot by an enrichment culture technique. One g of soil was introduced into 100 ml of DMA-isolation medium containing dimethylamine hydrochloride (DMAHCl) 0.058%; K2HPO4 1.06%; KH2PO4 0.53%, and MgSO4 0.001%. Duplicate flasks were prepared for each soil. The flasks were incubated at 30 C for 10 days. One to two loopfuls of the enrichment solution were then streaked on an agar plate of the same composition. Representative colonies were purified by repeated streaking on the same medium.

Enterobacter cloacae and E. aerogenes, obtained from North Carolina Biological Supply, and Escherichia coli from the University of Oklahoma microbiology culture collection were also utilized.

In order to get a large quantity of bacterial inoculum, the selected isolates were first streaked on an agar plate of the same composition. Glucose at 0.5% level was added to the DMA-isolation medium. The plates were incubated for 40 hr at 30 C, and the bacterial growth was scraped off and used to inoculate a broth of the same composition.

The flasks were incubated for 40 hr on a shaker. The bacterial cells were harvested by centrifugation at 6000 g for 15 min. The pellets were washed twice with 0.1M phosphate buffer, pH 7.0, and resuspended in an appropriate volume of the same buffer.

Initial inocula of the fungi and the actinomycetes were built up on a nitrate-agar medium, and then they were grown in nitrate-broth at 30 C without shaking for 10 days until the mats covered the surface of broth. After decanting off the fluid the

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fungal mat was washed twice with the phosphate buffer and homogenized, and almost the whole quantity was used as an inoculum. The actinomycete inoculum was prepared in the same way as the bacterial inoculum, starting from the isolation.

Three ml of the bacterial suspension were introduced into 27 ml of nitrosating solution (KNO3 2.5 g, glucose 2.0 g, DMAHCl 0.29 g, and 0.1M phosphate buffer pH 7.0, 100 ml). The control flask received an equal amount of the buffer. The flasks were incubated at room temperature on a rotary shaker at 110 rpm up to 96 hr; nitrite and DMNA were determined quantitatively at 24 hr intervals.

An aliquot of the supernatant from the nitrosating solution was pipeted out for the determination of nitrite content by the colorimetric method of Montgomery and Dymock (9). In the analysis for DMNA the remaining portion of the sample was steam distilled (10) and DMNA measured by the photochemical method of Daiber and Preussman (11).

To determine whether microorganisms can directly enhance nitrosation of DMA in the presence of nitrite, and differ in nitrosating ability, cell suspensions of 16 microorganisms were incubated in the nitrosating solution containing DMAHCl 0.29 g, NaNO2 0.25 g, glucose 0.10 g, and phosphate buffer pH 7.0, 100 ml. The method of inoculation and the incubation conditions were the same as before. In the case of bacteria DMNA was measured at 0, 24, 48, 72, and 96 hr and at intervals of 0, 1, 3, 7, and 10 days in the case of fungi and actinomycetes.

In order to test whether cell-free extract of E. coli could enhance nitrosation, the bacterium was grown for 48 hr on a shaker in a large flask with continuous aeration. The cells were harvested by centrifugation and twice washed with phosphate buffer solution. They were dispensed in four small centrifuge tubes, each containing approximately 2 g of bacterial cells, and after resuspending in 2.5 ml of buffer were exposed to ultrasonic vibration for 10 min each. The cells were centrifuged at 10,000 g for 15 min; the clear supernatant was pooled and divided into 2 equal parts, one of which was kept in a boiling water bath for 20 min. Two ml of this extract were incubated with 8 ml of nitrosating solution. Control flasks received equal amounts of buffer. Analyses were done after 0, 1, 2, and 4 hr of incubation.

RESULTS AND DISCUSSION

Of the 18 microorganisms tested, 11 bacteria, one actinomycete and four fungi produced nitrite from nitrate in levels ranging from 0.3 to 180 mg/ l under the test conditions. Formation of DMNA was recorded in the cultures of five bacteria, one actinomycete, and one fungus (Tables 1 and 2). The organisms yielding high levels of nitrite also produced DMNA. The results are in agreement with those of Hill and Hawksworth (12). Among the microorganisms investigated, E. cloacae had the highest nitrate reductase activity. The yield of both nitrite and DMNA in the cultures of E. cloacae attained maximum at 96 hr (Table 1). The production of nitrite and DMNA with E. aerogenes reached their peaks at 24 and 96 hr respectively; at 96 hr the pH of 4.29 was highly favorable for the nitrosation reaction.

Members of Enterobacteriaceae contain nitrate reductase and may therefore be considered to be potential contributors to nitrosamine formation. Contrary to other reports (1) the strain of E. coli used in this experiment yielded negligible nitrite and no DMNA; this suggests the existence of strain variation in this respect.

DMNA can be nitrosated to some extent even at neutral pH (Tables 3 and 4). Sander (8) obtained similar results working with diphenylamine.

DMNA production in the inoculated flasks containing various microbial cultures was higher than in uninoculated flasks. Among these, the highest yield was obtained in the culture of E. cloacae after 48 hr and 72 hr, after which the amount decreased. The loss of DMNA during the later period of incubation is not understood.

The data presented here indicated that, in addition to altering pH and reducing nitrate, the microorganisms can directly enhance nitrosation under neutral pH in a system containing both DMA and nitrite.

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[Page 100 consists entirely of Table 1, Table 2, Table 3, and Table 4.]

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In the present investigation the cells of E. cloacae incubated with DMA and nitrite produced DMNA, but the cell-free extract failed to enhance the reaction. These results do not agree with those of Ayanaba and Alexander (1).

In conclusion, microorganisms contribute to the nitrosation reaction by reducing nitrate to nitrite, lowering the pH in the system, and possibly creating microsites with high concentrations of precursors by adsorbing nitrite and secondary amines. The occurrence of the nitrosation reaction in natural soil environment appears highly probable from the experimental data available to date.

ACKNOWLEDGMENTS

This research was supported by a research grant from the Cooperative State Research Service, U.S. Department of Agriculture, Washington, D.C.

REFERENCES

1.   A. AYANABA and M. ALEXANDER, App. Microbiol. 23: 862-868 (1973).

2.   S. PANCHOLY, Soil Biol. Biochem. 10: 27-32 (1978).

3.   T. A. SMITH, Biol. Rev. 46: 201-241 (1971).

4.   A. AYANABA, W. VERSTRAETE, and M. ALEXANDER, Soil Sci. Soc. Am. Proc. 37: 565-568 (1973).

5.   W. LIJINSKY and S. EPSTEIN, Nature (Lond.) 225: 21-23 (1970).

6.   P. N. MAGEE, Food Cosmet. Toxicol. 9: 207-218 (1971).

7.   J. SANDER, Hoppe-Seyler's Z. Physiol. Chem. 349: 429-432 (1968).

8.   J. SANDER, Environment and Cancer, Williams and Wilkins Co., Baltimore, 1971.

9.   H. A. C. MONTGOMERY and J. F. DYMOCK, Analyst 86: 414-416 (1961).

10.   D. F. HEATH and J. A. E. JARVIS, Analyst 80: 613-616 (1955).

11.   D. DAIBER and R. PREUSSMAN, Z. Anal. Chem. 206: 344-352 (1964).

12.   M. J. HILL and G. HAWKSWORTH, in P. BOGOVSKI, R. PREUSSMAN and B. A. WALKER (eds), N-Nitroso Compounds, Analysis and Formation, International Agency for Research on Cancer, Lyon, France, 1973.