The similarities and differences in the structures of the nifH gene pools o
f six different soils (Montrond, LCSA-p, Vernon, Dombes, LCSA-c, and Thysse
Kaymor) and five soil fractions extracted from LCSA-c were studied. Bacter
ial DNA was directly extracted from the soils, and a region of the nifH gen
e was amplified by PCR and analyzed by restriction. Soils were selected on
the basis of differences in soil management, plant cover, and major physico
chemical propel ties. Microenvironments differed on the basis of the sizes
of the constituent particles and the organic carbon and clay contents. Rest
riction profiles were subjected to principal-component analysis. We showed
that the composition of the diazotrophic communities varied both on a large
scale (among sells) and on a microscale (among microenvironments in LCSA-c
soil). Soil management seemed to be the major parameter influencing differ
ences in the nifH gene pool structure among soils by controlling inorganic
nitrogen content and its variation. However, physicochemical parameters (te
xture and total C and N contents) were found to correlate with differences
among nifH gene pools on a microscale. We hypothesize that the observed nif
H genetic structures resulted from the adaptation to fluctuating conditions
(cultivated soil, forest soil, coarse fractions) or constant conditions (p
ermanent pasture soil, fine fractions). We attempted to identify a specific
band within the profile of the clay fraction by cloning and sequencing it
and comparing it with the gene databases. Unexpectedly, the nifH sequences
of the dominant bacteria were most similar to sequences of unidentified mar
ine eubacteria.