Unexpected Nondenitrifier Nitrous Oxide Reductase Gene Diversity And
Unexpected nondenitrifier nitrous oxide reductase gene diversity and abundance in soils Robert A. Sanforda, Darlene D. Wagnerb, Qingzhong Wuc, Joanne C. Chee-Sanfordd, Sara H. Thomasc, Claribel Cruz-Garcíac, Gina Rodríguezc,e, Arturo Massol-Deyáe, Kishore K. Krishnanif, Kirsti M. Ritalahtig,h, Silke Nisseng,h, Konstantinos T. Konstantinidisb,c, and Frank E. Löfflerg,h,i,1 aDepartment of Geology, University of Illinois, Urbana, IL 61801; bSchool of Biology and cSchool of Civil and Environmental Engineering, Georgia Institute of Technology, Atlanta, GA 30332; dUS Department of Agriculture—Agricultural Research Service, Urbana, IL 61801; eDepartment of Biology, University of Puerto Rico, Mayagüez, Puerto Rico 00681; fNational Institute of Abiotic Stress Management, Indian Council of Agricultural Research, Pune 413115, India; gDepartment of Microbiology, University of Tennessee, Knoxville, TN 37996; hBiosciences Division, Oak Ridge National Laboratory, Oak Ridge, TN 37831; and iDepartment of Civil and Environmental Engineering, University of Tennessee, Knoxville, TN 37996 Edited by Edward F. DeLong, Massachusetts Institute of Technology, Cambridge, MA, and approved October 19, 2012 (received for review July 2, 2012) − Agricultural and industrial practices more than doubled the intrin- dissimilatory nitrate reduction to ammonium (DNRA)] (NO3 / fi − + + − sic rate of terrestrial N xation over the past century with drastic NO2 → NH4 ), and nitrosifyers (NH4 → NO2 ) contribute to consequences, including increased atmospheric nitrous oxide (N2O) N2O release (15–21), and additional N2O emissions result from concentrations. N2O is a potent greenhouse gas and contributor to coupled microbial–abiotic processes (chemodenitrification). For ozone layer destruction, and its release from fixed N is almost en- example, ferric iron-reducing bacteria generate ferrous iron, which tirely controlled by microbial activities.
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