L. Ranjard et al., RESPONSE OF SOIL BACTERIA TO HG(II) IN RELATION TO SOIL CHARACTERISTICS AND CELL LOCATION, FEMS microbiology, ecology, 24(4), 1997, pp. 321-331
The response of indigenous bacterial communities to the addition of in
organic mercury (50 mu M of Hg(II)) was compared over a 30 day period
in four soils of contrasting properties. Hg(II) impact was estimated b
y following population dynamics of viable heterotrophic bacteria (VH)
and mercury resistant bacteria (Hg-R) by indirect enumeration in unfra
ctionated soil and in the inner and outer parts of soil aggregates obt
ained by successive washings. Numbers of VH bacteria in unfractionated
soils were not affected by mercury in any of the studied soils, where
as an increase in resistant bacteria was observed in all of them. The
lag phase before the increase of Hg-R bacteria and the magnitude of th
e enrichment could be related to soil organic matter and clay contents
suggesting that these factors govern mercury bioavailability. In frac
tionated soil, the increase of resistant populations was more pronounc
ed in the outer part (rep resenting mainly bacteria in macropores) tha
n in the inner part of soil aggregates. This difference in response wa
s clearer in soils with well developed aggregates. Qualitative analysi
s revealed that exposure to Hg caused a large increase in the proporti
on of Gram-negative strains among Hg-R bacteria in both soil parts.