Center
for Environmental Bioinorganic Chemistry
(CEBIC; François
Morel, PI)
Agency: DOE/NSF
Ward Lab Participants: Carrie
Tuit , Amal
Jayakumar
Trace metal limitation
of denitrification :
We have investigated the trace metal limitations and requirements (Mo,
Cd, Fe, Cu) for denitrifying bacteria by quantifying denitrification under
trace-metal clean anoxic conditions, using trilaminate incubation bags.
Several denitrifying strains were found to be unusually resistant to Cd
toxicity. Both Cu and Fe could limit growth and denitrification by denitrifiers,
and Cu in particular led to a terminal accumulation of N2O.
Nitrous oxide reductase is a Cu enzyme and Cu limitation appears to act
directly at this point in the pathway. We hypothesize that Cu limitation
may be involved in controlling the distribution of N2O in the
ocean; regions where N2O accumulates(oxygen minimum zones) are also regions
of very low Cu availability. These observations are unusual and significant
in that copper is more likely to be toxic than limiting for most microoganisms,
and because it may be an example of control of biogeochemical cycles by
metals other than iron. Fieldwork is planned for spring of 2003 in the
Eastern Tropical South Pacific with experiments designed to detect in
situ Cu limitation.
Nitrite reductase
Our research on the biochemistry and molecular biology of denitrification
focuses on nitrite reductase, the enzyme that catalyzes the reduction
of nitrite to nitric oxide (NO). This is a central enzyme in the pathway,
often referred to as the denitrifying enzyme, because it converts fixed
N to gaseous N, which is no longer available to most organisms. The two
forms of dissimilatory (respiratory) nitrite reductase, the cd-NiR (nirS
gene) and Cu-NiR (nirK gene), are distributed across the Bacterial and
Archaeal domains in a great diversity of microorganisms.
a)
Diversity:
We have retrieved nirK and nirS genes from a large number and variety
of microorganisms obtained from marine and sediment environments, from
soils and halobenzoate degrading enrichments, and from uncultivated organisms
using direct cloning. Phylogenetic analysis of the nir genes showed that
with the well known exception of Pseudomonas, both forms of nir are not
found within a single genus. The phylogeny of the nir genes is not congruent
with the 16S rRNA phylogeny of the organisms, indicating widespread horizontal
gene transfer of the components of denitrification. As part of the planned
Arabian Sea program, we will determine the relative abundance and activity
of nirK and nirS genes in the denitrifying assemblage of the oxygen minimum
zone and the role of trace metals in their distribution and activity.
The majority of nirS sequences retrieved from a coastal water column oxygen
minimum zone of the Arabian Sea (the first denitrifier sequences from
a water column environment) were unique; i.e., not closely related to
previously known sequences from sediment environments. We also detected
a possible relationship between diversity and dentrification rates in
this environment.
b) Nitrifying bacteria
Both NiRs are well known in denitrifying bacteria, and the nitric oxide
reductase (NoR, which produces N2O) in denitrifiers has also
been characterized. It is also well known that nitrifying bacteria, obligate
aerobic autotrophs, also produce both NO and N2O under some
conditions, but the enzymology and genetics of these transformations in
nitrifiers was not understood. We discovered a nitrite reductase in nitrifying
bacteria that is homologous with the nirK of denitrifiers. Similarly,
we also recently discovered a norB gene in nitrifiers which is highly
homologous with the norB gene from denitrifiers.
We further investigated
the similarities in the genes between denitrifiers and nitrifiers by determining
the isotopic effects of the enzymes in whole cell and lysate assays. For
the residual nitrite, the isotopic effect is determined by the kind of
NiR present, but is not influenced by whether the process is performed
by a nitrifier or a denitrifier. The isotopic effect must result from
the mode of action of the iron vs. the copper enzyme, and perhaps the
degree of exchange that occurs between the cell and the environment. The
implication is that the significance of isotopic signatures of inorganic
and gaseous nitrogen species in the ocean may be more complicated than
previous suspected, if the effects of nitrification and denitrification
cannot be distinguished. A model is being developed to help sort out the
expected isotopic fractionation in different environmental scenarios.
Assimilatory Nitrate
Reductase:
Our goals in this project were to clone and sequence the nitrate reductase
(nar) genes from several eukaryotic algae and to investigate trace metal
regulation of gene expression. Expression data are to be linked to enzyme
assays on cells grown under varying light and metal conditions, to investigate
Mo cycling in relation to NR regulation. This work has been slowed by
difficulties encountered in cloning the nar gene. We have succeeded in
obtaining the complete gene sequence for nar from Dunaliella, the first
example from a marine alga, and partial gene sequences of nar from several
diatoms. Expression studies to characterize induction of nar have been
carried out in Dunaliella and are planned for the diatoms.
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