H. Ludemann et al., Spatial changes in the bacterial community structure along a vertical oxygen gradient in flooded paddy soil cores, APPL ENVIR, 66(2), 2000, pp. 754-762
Molecular ecology techniques were applied to assess changes in the bacteria
l community structure along a vertical oxygen gradient in flooded paddy soi
l cores. Microsensor measurements showed that oxygen was depleted from 140
mu M at the floodwater/soil interface to nondetectable amounts at a depth o
f approximately 2.0 mm and below. Bacterial 16S rRNA gene (rDNA)-based comm
unity fingerprint patterns were obtained from 200-mu m-thick soil slices of
both the oxic and anoxic zones by using the T-RFLP (terminal restriction f
ragment length polymorphism) technique. The fingerprints revealed a tremend
ous shift in the community patterns in correlation to the oxygen depletion
measured with depth. 16S rDNA clone sequences recovered from the oxic or an
oxic zone directly corresponded to those terminal restriction fragments whi
ch were highly characteristic of the respective zone. Comparative sequence
analysis of these clones identified members of the alpha and beta subclasse
s of Proteobacteria as the abundant populations in the oxic zone. In contra
st, members of clostridial cluster I were determined to be the predominant
bacterial group in the oxygen-depleted soil. The extraction of total RNA fo
llowed by reverse transcription-PCR of the bacterial 16S rRNA and T-RFLP an
alysis resulted for both oxic and anoxic zones of flooded soil cores in com
munity fingerprint patterns similar to those obtained by the rDNA-based ana
lysis. This finding suggests that the microbial groups detected on the rDNA
level are the metabolically active populations within the oxic and anoxic
soil slices examined.