Abstract
Many textbooks, symposium publications and even edited papers in leading journals present denitrification as the only dissimilatory pathway for bacterial NO −3 reduction. In fact, the rapid, dissimilatory reduction to NH +4 by fermentative bacteria was documented many years ago (see, for example, Woods, 1938). As the limited literature on NO −3 dissimilation to NH +4 published before 1988 has recently been reviewed extensively (Cole, 1988; 1989), this article will focus on recent developments which confirm or conflict with the previous conclusions. Although the practical importance of denitrification by essentially respiratory bacteria is beyond doubt, Figure 1 presents it — possibly for the first time — in the context of the emerging diversity of enzymes which have evolved to dissimilate NO −3 and NO −2 in different bacterial groups.
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Cole, J.A. (1990). Physiology, Biochemistry and Genetics of Nitrate Dissimilation to Ammonia. In: Revsbech, N.P., Sørensen, J. (eds) Denitrification in Soil and Sediment. Federation of European Microbiological Societies Symposium Series, vol 56. Springer, Boston, MA. https://doi.org/10.1007/978-1-4757-9969-9_4
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