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The ecology and physiology of anaerobic bacteria isolated from Tay Estuary sediments

Published online by Cambridge University Press:  05 December 2011

S. M. Keith ,
Moya A. Russ ,
G. T. Macfarlane  and
R. A. Herbert
S. M. Keith
Affiliation:
Department of Biological Sciences, University of Dundee, Dundee DD1 4HN, U.K.
Moya A. Russ
Affiliation:
Department of Biological Sciences, University of Dundee, Dundee DD1 4HN, U.K.
G. T. Macfarlane
Affiliation:
Department of Biological Sciences, University of Dundee, Dundee DD1 4HN, U.K.
R. A. Herbert
Affiliation:
Department of Biological Sciences, University of Dundee, Dundee DD1 4HN, U.K.
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Synopsis

The spatial distribution of different physiological groups of bacteria (nitrifying bacteria, nitrate respiring bacteria, clostridia, phototrophic bacteria, sulphate reducing bacteria and methanogens) has been determined in the surface sediments of Kingoodie Bay in the Tay Estuary. The overall distribution of the different microbial populations is largely dependent upon the presence or absence of O2, i.e. populations of obligate aerobes were greater at the surface where O2 was present, but with increasing depth and hence anoxia were successively displaced by populations of facultative and then strictly anaerobic bacteria. Thus, maximum rates of nitrification, an oxygen dependent process, were recorded in the 0–10 mm depth horizon (098 μg of N per g dry weight of sediment per day) while nitrate respiration rates were maximal in the 10–20 mm horizon (2.92 μg N per g dry weight of sediment per day). Dissimilatory sulphate reduction at 20–30 mm depth (102.1 n mol SO42 reduced g dry weight sediment -1.d -1). Methanogenesis was similarly recorded at all depths investigated but higher rates were recorded at 40–50 mm depth (22.64 n mol CH4 produced g dry weight sediment -1.d -1). These data are discussed in relation to the physico-chemical factors which arc generated in these estuarine sediments and which not only govern the spatial organisation of individual microbial populations but also modulate their metabolic activities.

Type
Research Article
Information
Proceedings of the Royal Society of Edinburgh, Section B: Biological Sciences , Volume 92 , Issue 3-4: The Environment of the Tay Estuary , 1987 , pp. 323 - 333
Copyright
Copyright © Royal Society of Edinburgh 1987

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References

Billen, G. 1982. Modelling the processes of organic matter degradation. In Sediment Microbiology, Special Publications of the Society for General Microbiology, eds Nedwell, D. B. and Brown, C. M., pp. 15–52. London: Academic Press.Google Scholar
Brown, C. M., Macdonald-Brown, D. S. & Meers, J. L. 1974. Physiological aspects of microbial inorganic nitrogen metabolism. Advances in Microbial Physiology 11, 1–52.CrossRefGoogle Scholar
Buchanan, R. E. & Gibbons, N. E. 1974. Sergey's Manual of Determinative Bacteriology, 8th edn. Baltimore: Williams and Wilkins Company.Google Scholar
Caskey, W. H. & Tiedje, J. M. 1980. The reduction of nitrate to ammonium by a Clostridium sp. isolated from soil. Journal of General Microbiology 119, 217–223.Google ScholarPubMed
Cowan, S. T. & Steel, K. J. 1981. Identification of medical bacteria. London: Cambridge University Press.Google Scholar
Dunn, G. M., Herbert, R. A. & Brown, C. M. 1979. Influence of oxygen tension on nitrate reduction by a Klebsiella sp. growing in chemostat culture. Journal of General Microbiology 112, 379–383.CrossRefGoogle ScholarPubMed
Dunn, G. M., Wardell, J. M., Herbert, R. A. & Brown, C M. 1980. Enrichment, enumeration and characterisation of nitrate reducing bacteria present in sediments of the River Tay Estuary. Proceedings of the Royal Society of Edinburgh 78B, 47–56.Google Scholar
Hasan, S. M. & Hall, J. B. 1975. The physiological significance of nitrate reduction in Clostridium perfringens. Journal of General Microbiology 87, 120–128.CrossRefGoogle ScholarPubMed
Herbert, R. A. 1975. A preliminary investigation of the effects of salinity on the bacterial flora of the Tay Estuary. Proceedings of the Royal Society of Edinburgh 75B, 137–144.Google Scholar
Jones, J. G. 1982. Activities of aerobic and anaerobic bacteria in lake sediments and their effect on the water column. In Sediment Microbiology, Special Publications of the Society for General Microbiology, eds Nedwell, D. B. & Brown, C. M., pp. 107–143. London: Academic Press.Google Scholar
Jorgensen, B. B. 1977. Bacterial sulphate reduction within reduced microniches of oxidised marine sediments. Marine Biology 41, 7–17.Google Scholar
Jorgensen, B. B. 1980. Mineralisation and the bacterial cycling of carbon, nitrogen and sulphur in marine sediments. In Contemporary Microbial Ecology, eds Ellwood, D.C, Hedger, J. N., Latham, M. J., Lynch, J. M. & Slater, J. H., pp. 239–251. London: Academic Press.Google Scholar
Keith, S. M. & Herbert, R. A. 1983. Dissimilatory nitrate reduction by a strain of Desulfovibrio desulfuricans. FEMS Microbiology Letters 18, 55–59.Google Scholar
Keith, S. M., Herbert, R. A. & Harfoot, 1982a. Isolation of new types of sulphate reducing bacteria from estuarine and marine sediments using chemostat enrichments. Journal of Applied Bacteriology 53, 29–33.Google Scholar
Keith, S. M., Macfarlane, G. T. & Herbert, R. A. 1982b. Dissimilatory nitrate reduction by a strain of Closlridium hutyricum isolated from estuarine sediments. Archives of Microbiology 132, 62–66.Google Scholar
Kessel, J. F. 1982. The relationships between redox potential and denitrification in water-sediment systems. Water Research 12, 285–290.Google Scholar
Macfarlane, G. T. & Herbert, R. A. 1982. Nitrate dissimilation by Vibrio spp. isolated from estuarine sediments. Journal of General Microbiology 128, 2463–2468.Google Scholar
Macfarlane, G. T. & Herbert, R. A. 1984. Dissimilatory nitrate reduction and nitrification in estuarine sediments. Journal of General Microbiology 130, 2301–2308.Google Scholar
Macfarlane, G. T., Russ, Moya A., Keith, S. M. & Herbert, R. A. 1984. Similation of microbial processes in estuarine sediments using gel stabilised systems. Journal of General Microbiology 130, 2927–2933.Google Scholar
Mechalas, B. J. 1974. Pathways and environmental requirements for biogenic gas production in the oceans. In Natural Gases in Marine Sediments, ed. Kaplan, I. R., pp. 12–25. New York: Plenum Press.Google Scholar
Sorensen, J., Jorgensen, B. B. & Revsbech, N. P. 1979. A comparison of oxygen, nitrate and sulphate respiration in coastal marine sediments. Microbial Ecology 5, 105–115.Google Scholar
Thauer, R. K., Jungermann, K. & Decker, K. 1977. Energy conservation in chemotrophic anaerobic bacteria. Bacteriological Reviews 41, 100–180.Google Scholar