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Potential importance of bacteria and fungi in nitrate assimilation in soil
Soil microorganisms can use a wide range of N compounds but are thought to prefer NH 4 +. Nevertheless, 15N isotope dilution studies have shown that microbial immobilization of NO 3 − can be an important process in many soils, particularly relatively undisturbed soils. Our objective was to develop a...
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Published in: | Soil biology & biochemistry 2007-07, Vol.39 (7), p.1737-1743 |
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Main Authors: | , |
Format: | Article |
Language: | English |
Subjects: | |
Citations: | Items that this one cites Items that cite this one |
Online Access: | Get full text |
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Summary: | Soil microorganisms can use a wide range of N compounds but are thought to prefer NH
4
+. Nevertheless,
15N isotope dilution studies have shown that microbial immobilization of NO
3
− can be an important process in many soils, particularly relatively undisturbed soils. Our objective was to develop a method for measuring NO
3
− immobilization potential so that the relative contributions of bacteria and fungi could be determined. We modified and optimized a soil slurry method that included amendments of KNO
3, glucose, and methionine sulfoximine (an inhibitor of N assimilation) in the presence of two protein synthesis inhibitors: chloramphenicol, which inhibits bacteria, or cycloheximide, which inhibits fungi. By adding
15N-labeled KNO
3, we were able to measure gross rates of NO
3
− production (i.e., gross nitrification) and consumption (i.e., gross NO
3
− immobilization). We found that bacteria, not fungi, had the greatest potential for assimilating, or immobilizing, NO
3
− in these soils. This is consistent with their growth habit and distribution in the heterogeneous soil matrix. |
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ISSN: | 0038-0717 1879-3428 |
DOI: | 10.1016/j.soilbio.2007.01.033 |