ABSTRACT
Ralstonia
metallidurans CH34, a soil bacterium resistant to a
variety of metals, is known to reduce selenite to
intracellular granules of elemental selenium (Se0). We have
studied the kinetics of selenite (SeIV) and selenate
(SeVI) accumulation and used X-ray absorption spectroscopy
to identify the accumulated form of selenate, as well as possible
chemical intermediates during the transformation of these two
oxyanions. When introduced during the lag phase, the presence of
selenite increased the duration of this phase, as previously
observed. Selenite introduction was followed by a
period of slow uptake, during which the bacteria contained
Se0 and alkyl selenide in equivalent proportions. This
suggests that two reactions with similar kinetics take place:
an assimilatory pathway leading to alkyl selenide and a slow
detoxification pathway leading to Se0. Subsequently,
selenite uptake strongly increased (up to 340 mg Se per g of proteins)
and Se0 was the predominant transformation product,
suggesting an activation of selenite transport and reduction systems
after several hours of contact. Exposure to selenate did not induce an
increase in the lag phase duration, and the bacteria accumulated
approximately 25-fold less Se than when exposed to selenite.
SeIV was detected as a transient species in the first
12 h after selenate introduction, Se0 also
occurred as a minor species, and the major accumulated form was alkyl
selenide. Thus, in the present experimental conditions, selenate mostly
follows an assimilatory pathway and the reduction
pathway is not activated upon selenate exposure. These results show
that R. metallidurans CH34 may be suitable for the
remediation of selenite-, but not selenate-, contaminated
environments.