O. Hojberg et al., Oxygen-sensing reporter strain of Pseudomonas fluorescens for monitoring the distribution of low-oxygen habitats in soil, APPL ENVIR, 65(9), 1999, pp. 4085-4093
The root colonizing bacterium Pseudomonas fluorescens CHA0 was used to cons
truct an oxygen-responsive biosensor. An anaerobically inducible promoter o
f Pseudomonas aeruginosa, which depends on the FNR (fumarate and nitrate re
ductase regulation)-like transcriptional regulator ANR (anaerobic regulatio
n of arginine deiminase and nitrate reductase pathways), was fused to the s
tructural lacZ gene of Escherichia coil. By inserting the reporter fusion i
nto the chromosomal attTn7 site of P. fluorescens CHA0 by using a mini-Tn7
transposon, the reporter strain, CHA900, was obtained. Grown in glutamate-y
east extract medium in an oxystat at defined oxygen levels, the biosensor C
HA900 responded to a decrease in oxygen concentration from 210 x 10(2) Pa t
o 2 x 10(2) Pa of O-2 by a nearly 100-fold increase in beta-galactosidase a
ctivity. Half-maximal induction of the reporter occurred at about 5 x 10(2)
Pa. This dose response closely resembles that found for E. coil promoters
which are activated by the FNR protein. In a carbon-free buffer or in bulk
soil, the biosensor CHA900 still responded to a decrease in oxygen concentr
ation, although here induction was about 10 times lower and the low oxygen
response was gradually lost within 3 days. Introduced into a barley-soil mi
crocosm, the biosensor could report decreasing oxygen concentrations in the
rhizosphere for a 6 day period. When the water content in the microcosm wa
s raised from 60% to 85% of field capacity, expression of the reporter gene
was elevated about twofold above a basal level after 2 days of incubation,
suggesting that a water content of 85% caused mild anoxia. Increased compa
ction of the soil was shown to have a faster and more dramatic effect on th
e expression of the oxygen reporter than soil water content alone, indicati
ng that factors other than the water-filled pore space influenced the oxyge
n status of the soil. These experiments illustrate the utility of the biose
nsor for detecting low oxygen concentrations in the rhizosphere and other s
oil habitats.