Affiliation:
1. Center for Earth and Planetary Physics, Division of Applied Sciences, Harvard University, Cambridge, Massachusetts 02138
2. Woods Hole Oceanographic Institution Woods Hole, Massachusetts 02543
Abstract
Pure cultures of the marine ammonium-oxidizing bacterium
Nitrosomonas
sp. were grown in the laboratory at oxygen partial pressures between 0.005 and 0.2 atm (0.18 to 7 mg/liter). Low oxygen conditions induced a marked decrease in the rate for production of NO
2
-
, from 3.6 × 10
−10
to 0.5 × 10
−10
mmol of NO
2
-
per cell per day. In contrast, evolution of N
2
O increased from 1 × 10
−12
to 4.3 × 10
−12
mmol of N per cell per day. The yield of N
2
O relative to NO
2
-
increased from 0.3% to nearly 10% (moles of N in N
2
O per mole of NO
2
-
) as the oxygen level was reduced, although bacterial growth rates changed by less than 30%. Nitrifying bacteria from the genera
Nitrosomonas, Nitrosolobus, Nitrosospira
, and
Nitrosococcus
exhibited similar yields of N
2
O at atmospheric oxygen levels. Nitrite-oxidizing bacteria (
Nitrobacter
sp.) and the dinoflagellate
Exuviaella
sp. did not produce detectable quantities of N
2
O during growth. The results support the view that nitrification is an important source of N
2
O in the environment.
Publisher
American Society for Microbiology
Subject
Ecology,Applied Microbiology and Biotechnology,Food Science,Biotechnology
Cited by
723 articles.
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