Soil Biology & Biochemistry Citation Classic XVI

Soil Biology & Biochemistry Citation Classic XVI Soil Biology and Biochemistry 123 (2018) A1–A2 Contents lists available at ScienceDirect Soil Biology and Biochemistry journal homepage: www.elsevier.com/locate/soilbio Citation Classic Richard G. Burns Faculty of Science, Health, Education and Engineering, The University of the Sunshine Coast, Maroochydore, Queensland 4556, Australia To those of us from an earlier generation the microbial nitrogen subsequently in soils and is now considered, at least under some con- cycle was a simple, elegant and apparently logical sequence of events. It ditions, to be a major contributor to atmospheric nitrous oxide – one of involved a large number of bacteria and fungi that released ammonium the three most potent greenhouse gases with regard to climate change from the degradation of plant, animal and microbial organic matter and and stratospheric ozone depletion. Currently, microbial denitrifiers are two small groups of collaborative aerobic bacteria, the first of which under close examination by many, including the authors of this most oxidized the ammonia to nitrite and then passed it on to the second recent Citation Classic. Exciting advances are being made using stable which oxidized the nitrite to nitrate. This sometimes prompted a debate isotope and isotopomer methods and molecular and modelling ap- about whether nitrate generation http://www.deepdyve.com/assets/images/DeepDyve-Logo-lg.png Soil Biology and Biochemistry Elsevier

Soil Biology & Biochemistry Citation Classic XVI

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Publisher
Elsevier
Copyright
Copyright © 2018 Elsevier Ltd
ISSN
0038-0717
D.O.I.
10.1016/j.soilbio.2018.03.019
Publisher site
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Abstract

Soil Biology and Biochemistry 123 (2018) A1–A2 Contents lists available at ScienceDirect Soil Biology and Biochemistry journal homepage: www.elsevier.com/locate/soilbio Citation Classic Richard G. Burns Faculty of Science, Health, Education and Engineering, The University of the Sunshine Coast, Maroochydore, Queensland 4556, Australia To those of us from an earlier generation the microbial nitrogen subsequently in soils and is now considered, at least under some con- cycle was a simple, elegant and apparently logical sequence of events. It ditions, to be a major contributor to atmospheric nitrous oxide – one of involved a large number of bacteria and fungi that released ammonium the three most potent greenhouse gases with regard to climate change from the degradation of plant, animal and microbial organic matter and and stratospheric ozone depletion. Currently, microbial denitrifiers are two small groups of collaborative aerobic bacteria, the first of which under close examination by many, including the authors of this most oxidized the ammonia to nitrite and then passed it on to the second recent Citation Classic. Exciting advances are being made using stable which oxidized the nitrite to nitrate. This sometimes prompted a debate isotope and isotopomer methods and molecular and modelling ap- about whether nitrate generation

Journal

Soil Biology and BiochemistryElsevier

Published: Aug 1, 2018

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