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Applied and Environmental Microbiology, August 1998, p. 2958-2965, Vol. 64, No. 8
Department of Molecular and Cell Biology,
Received 4 March 1998/Accepted 11 May 1998
A combination of denaturing gradient gel electrophoresis (DGGE) and
oligonucleotide probing was used to investigate the influence of soil
pH on the compositions of natural populations of autotrophic
0099-2240/98/$04.00+0
Copyright © 1998, American Society for Microbiology. All rights reserved.
Analysis of
-Subgroup Proteobacterial Ammonia Oxidizer
Populations in Soil by Denaturing Gradient Gel Electrophoresis Analysis
and Hierarchical Phylogenetic Probing

-subgroup proteobacterial ammonia oxidizers. PCR primers specific to
this group were used to amplify 16S ribosomal DNA (rDNA) from soils
maintained for 36 years at a range of pH values, and PCR products were
analyzed by DGGE. Genus- and cluster-specific probes were designed to
bind to sequences within the region amplified by these primers. A
sequence specific to all
-subgroup ammonia oxidizers could not be
identified, but probes specific for Nitrosospira clusters 1 to 4 and Nitrosomonas clusters 6 and 7 (J. R. Stephen, A. E. McCaig, Z. Smith, J. I. Prosser, and T. M. Embley,
Appl. Environ. Microbiol. 62:4147-4154, 1996) were designed.
Elution profiles of probes against target sequences and closely related nontarget sequences indicated a requirement for high-stringency hybridization conditions to distinguish between different clusters. DGGE banding patterns suggested the presence of
Nitrosomonas cluster 6a and Nitrosospira
clusters 2, 3, and 4 in all soil plots, but results were ambiguous
because of overlapping banding patterns. Unambiguous band
identification of the same clusters was achieved by combined DGGE and
probing of blots with the cluster-specific radiolabelled probes. The
relative intensities of hybridization signals provided information on
the apparent selection of different Nitrosospira genotypes
in samples of soil of different pHs. The signal from the
Nitrosospira cluster 3 probe decreased significantly, relative to an internal control probe, with decreasing soil pH in the
range of 6.6 to 3.9, while Nitrosospira cluster 2 hybridization signals increased with increasing soil acidity. Signals
from Nitrosospira cluster 4 were greatest at pH 5.5, decreasing at lower and higher values, while Nitrosomonas
cluster 6a signals did not vary significantly with pH. These findings
are in agreement with a previous molecular study (J. R. Stephen,
A. E. McCaig, Z. Smith, J. I. Prosser, and T. M. Embley,
Appl. Environ. Microbiol 62:4147-4154, 1996) of the same sites,
which demonstrated the presence of the same four clusters of ammonia
oxidizers and indicated that selection might be occurring for clusters
2 and 3 at acid and neutral pHs, respectively. The two studies used
different sets of PCR primers for amplification of 16S rDNA sequences
from soil, and the similar findings suggest that PCR bias was unlikely
to be a significant factor. The present study demonstrates the value of
DGGE and probing for rapid analysis of natural soil communities of
-subgroup proteobacterial ammonia oxidizers, indicates significant
pH-associated differences in Nitrosospira populations, and
suggests that Nitrosospira cluster 2 may be of significance
for ammonia-oxidizing activity in acid soils.
*
Corresponding author. Mailing address: Department of
Molecular and Cell Biology, University of Aberdeen, Institute of
Medical Sciences, Foresterhill, Aberdeen AB25 2ZD, Scotland, United
Kingdom. Phone: 44 1224 273148. Fax: 44 1224 273144. E-mail:
j.prosser{at}ac.uk.aberdeen.
Present address: Department of Land, Air and Water Resources,
University of California, Davis, CA 95616.
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