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Journal of Bacteriology, May 2004, p. 2897-2899, Vol. 186, No. 9
0021-9193/04/$08.00+0 DOI: 10.1128/JB.186.9.2897-2899.2004
Copyright © 2004, American Society for Microbiology. All Rights Reserved.
Preferential Reduction of Fe(III) over Fumarate by Geobacter sulfurreducens
Abraham Esteve-Núñez,1* Cinthia Núñez,1,2 and Derek R. Lovley1
Department of Microbiology, University of Massachusetts, Amherst, Massachusetts 01003,1
Departamento de Microbiología Molecular, Instituto de Biotecnología, Universidad Nacional Autónoma de México, Cuernavaca, Morelos 62251, México2
Received 23 October 2003/
Accepted 16 January 2004

ABSTRACT
The presence of Fe(III), but not that of Fe(II), resulted in
ca. 20-fold-lower levels of mRNA for fumarate reductase, inhibiting
fumarate reduction and favoring utilization of fumarate as an
electron donor in chemostat cultures of
Geobacter sulfurreducens,
despite the fact that growth yield with fumarate was 3-fold
higher than with Fe(III).

INTRODUCTION
The study of Fe(III) reduction has been greatly facilitated
by the finding that microorganisms in the family
Geobacteraceae are the predominant Fe(III)-reducing microorganisms in a diversity
of subsurface environments (
1,
3,
6,
11) and the fact that
Geobacteraceae similar to those that predominate in these environments can
be recovered in pure culture.
Geobacter sulfurreducens, which
commonly serves as the model organism for the
Geobacteraceae in subsurface environments, can use both Fe(III) and fumarate
as an electron acceptor (
2). Understanding the relative utilization
of Fe(III) and fumarate as electron acceptors could aid in developing
strategies to best promote the growth of
Geobacter species for
bioremediation applications, such as the reductive precipitation
of uranium from contaminated groundwater (
1). In previously
studied microorganisms, the regulation of electron acceptor
utilization favors the reduction of the electron acceptor that
can yield the most energy to support cell growth (
5,
7,
8,
12).
However, it is not clear whether the same trend applies to microorganisms
in subsurface environments.

Inhibition of fumarate respiration in the presence of Fe(III).
In order to evaluate potential controls on fumarate and Fe(III)
respiration,
G. sulfurreducens was grown in continuous culture
(A. Esteve-Núñez, M. Rothermich, M. Sharma, and
D. R. Lovley, submitted for publication) with the electron donor,
acetate (5.5 mM), which limited growth at a dilution rate of
0.05 h
1. This culture condition was designed to simulate
the most prevalent conditions in anoxic soils and subsurface
environments, in which acetate is the key electron donor for
Fe(III) reduction (
10). When fumarate (30 mM) was provided as
the electron acceptor, there was a steady-state accumulation
of succinate resulting from fumarate reduction (Fig.
1). The
steady-state biomass was 45.5 ± 5 (mean ± standard
deviation of results from three replicate experiments) mg of
protein per liter. When cultures were grown with the same acetate
input, but with 60 mM Fe(III) citrate as the electron acceptor,
the culture density was 15.5 ± 3 mg of protein per liter.
Thus, fumarate reduction provided significantly more energy
to support growth than Fe(III) reduction.
In order to examine the interaction between fumarate and Fe(III)
reduction, Fe(III) citrate (10 mM) was added to steady-state
cultures of cells growing with fumarate as the electron acceptor
(Fig.
1). There was an immediate decrease in succinate concentration
concurrent with an accumulation of Fe(II) resulting from Fe(III)
reduction. The inhibition of fumarate reduction was associated
with a dramatic decline in levels of mRNA for the fumarate reductase
operon,
frdCAB (Fig.
1), measured by Northern analysis (the
probe was generated with PCR using the primers frdCfor [5'-GTTCGGTATCCAGCTGAG-3']
and frdCrev [5'-CTTTCAGAATGCCGGTGACG-3']). Six hours after the
addition of Fe(III), the mRNA levels for
frdCAB were 17-fold
lower than in cells not exposed to Fe(III) (Fig.
1). Furthermore,
at this time fumarate reductase-specific activity in the membrane
fraction of Fe(III)-amended cultures was fourfold lower than
in unamended cultures (13 ± 1 versus 52 ± 4 nmol
min
1 mg of protein
1). Once the Fe(III) was completely
reduced to Fe(II), the level of mRNA for the fumarate reductase
genes returned to the level detected prior to the addition of
Fe(III), even though there was still a significant quantity
of Fe(II) in the culture (Fig.
1). The finding that the expression
of the fumarate reductase was down-regulated in the presence
of Fe(III), but not Fe(II), represents a novel instance in which
discrimination between iron redox states seems essential for
regulating processes that might have an impact on the pathway
for electron transfer.
In order to determine whether Fe(III) had a similar effect on fumarate respiration over longer periods of time in which G. sulfurreducens would have time to adapt to the simultaneous presence of high quantities of Fe(III) and fumarate, G. sulfurreducens was grown in continuous culture with acetate as the electron donor and the limiting growth substrate, with both fumarate (35 mM) and Fe(III) (70 mM) as potential electron acceptors (Fig. 2). As was observed in the short-term studies, fumarate reduction was inhibited and levels of fumarate reductase mRNA were lower in the presence of Fe(III) and fumarate than in control cultures growing on fumarate alone. The steady-state biomass concentration in the presence of both fumarate and Fe(III) was slightly higher than that with Fe(III) alone but significantly lower than when fumarate was the sole electron acceptor.
During bacterial growth on fumarate, the succinate that is produced
from fumarate reduction is not oxidized in the tricarboxylic
acid cycle (
4), but it is possible that in the presence of Fe(III),
small amounts of fumarate were used as an electron donor or
carbon source in a pathway in which fumarate was converted to
acetyl coenzyme A via malate and pyruvate with the formation
of formate (Fig.
3A). In the presence of Fe(III), high concentrations
of malate accumulated, and there was an increased rate of formate
production (Fig.
3B). The high levels of malate indicated that
conversion of malate to pyruvate might be the limiting step
in fumarate utilization. Once Fe(III) was depleted and fumarate
reduction resumed, malate accumulation and formate production
stopped (Fig.
3B).

Implications.
The respiration in
G. sulfurreducens is clearly not optimized
for maximal growth when high concentrations of fumarate as well
as Fe(III) are available. However, the down-regulation of fumarate
respiration in the presence of Fe(III) may represent an effective
adaptation to conditions found in most subsurface environments.
Generally, the scarcity of readily metabolizable organic matter
severely limits microbial growth in the subsurface. In contrast,
Fe(III) is often the most abundant electron acceptor available
for microbial respiration (
9). Therefore, in typical anoxic
subsurface environments in which
Geobacter species predominate,
if any fumarate becomes available it may be more beneficial
to funnel it toward catabolic reactions rather than to use it
as an electron acceptor. Thus, although the regulation of respiration
in
G. sulfurreducens does not fit the paradigm that the most
energetically favorable electron acceptors are reduced first,
this finding may represent the most adaptive response to the
environmental conditions that
Geobacter species typically encounter.

ACKNOWLEDGMENTS
This research was funded by the Genomes to Life Program, U.S.
Department of Energy (grant DE-FC02-02ER63446). A.E.-N. was
the recipient of a postdoctoral fellowship from the Secretaría
de Estado de Educación y Universidades (Madrid, Spain),
cofunded by the European Social Fund. In addition, C.N. was
the recipient of a DGAPA/UNAM postdoctoral fellowship.

FOOTNOTES
* Corresponding author. Mailing address: University of Massachusetts, Dept. of Microbiology, Morrill Science Center IVN, Amherst, MA 01003. Phone: (413) 545-9782. Fax: (413) 545-1578. E-mail:
aesteve{at}microbio.umass.edu.


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Journal of Bacteriology, May 2004, p. 2897-2899, Vol. 186, No. 9
0021-9193/04/$08.00+0 DOI: 10.1128/JB.186.9.2897-2899.2004
Copyright © 2004, American Society for Microbiology. All Rights Reserved.
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