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Applied and Environmental Microbiology, March 1999, p. 989-994, Vol. 65, No. 3
Division of Engineering and Applied
Sciences1 and Biological
Laboratories,2 Harvard University, Cambridge,
Massachusetts 02138, and Center for Marine Science and
Technology, University of Massachusetts, Dartmouth, North
Dartmouth, Massachusetts 027473
Received 21 August 1998/Accepted 4 December 1998
Nitrogen stable-isotope compositions (
0099-2240/99/$04.00+0
Copyright © 1999, American Society for Microbiology. All rights reserved.
Steady-State Nitrogen Isotope Effects of
N2 and N2O Production in Paracoccus
denitrificans

15N) can help
track denitrification and N2O production in the
environment, as can knowledge of the isotopic discrimination, or
isotope effect, inherent to denitrification. However,
the isotope effects associated with denitrification as a function of
dissolved-oxygen concentration and their influence on
the isotopic composition of N2O are not known. We developed
a simple steady-state reactor to allow the measurement of
denitrification isotope effects in Paracoccus
denitrificans. With [dO2] between 0 and 1.2 µM,
the N stable-isotope effects of NO3
and
N2O reduction were constant at 28.6
± 1.9
and
12.9
± 2.6
, respectively (mean ± standard error,
n = 5). This estimate of the isotope effect of
N2O reduction is the first in an axenic denitrifying
culture and places the
15N of denitrification-produced
N2O midway between those of the nitrogenous oxide
substrates and the product N2 in steady-state systems.
Application of both isotope effects to N2O cycling
studies is discussed.
*
Corresponding author. Mailing address: Department of
Earth and Planetary Sciences, Harvard University, 20 Oxford St.,
Cambridge, MA 02138. Phone: (617) 495-9624. Fax: (617) 495-2768. E-mail: ccb{at}io.harvard.edu.
Present address: School of Biology, Georgia Institute of
Technology, Atlanta, GA 30332.
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