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Journal of Bacteriology, March 2006, p. 2275-2279, Vol. 188, No. 6
0021-9193/06/$08.00+0 doi:10.1128/JB.188.6.2275-2279.2006
Copyright © 2006, American Society for Microbiology. All Rights Reserved.
Global Gene Expression Analysis of Iron-Inducible Genes in Magnetospirillum magneticum AMB-1
Takeyuki Suzuki,
Yoshiko Okamura,
Ronie J. Calugay,
Haruko Takeyama, and
Tadashi Matsunaga*
Department of Biotechnology, Tokyo University of Agriculture and Technology, Koganei, Tokyo, Japan
Received 20 September 2005/
Accepted 5 December 2005

ABSTRACT
Iron uptake systems were identified by global expression profiling
of
Magnetospirillum magneticum AMB-1.
feo,
tpd, and
ftr, which
encode ferrous iron transporters, were up-regulated under iron-rich
conditions. The concomitant rapid iron uptake and magnetite
formation suggest that these uptake systems serve as iron supply
lines for magnetosome synthesis.

TEXT
Iron is crucial in microbial metabolism. It exists in two redox
states: the reduced Fe
2+ soluble ferrous state and the oxidized
Fe
3+ ferric form, which is extremely insoluble (
1). In magnetotactic
bacteria, the formation of highly organized membrane-bound intracellular
magnetites (Fe
3O
4) or greigites (Fe
3S
4) requires the acquisition
of a large amount of iron several orders of magnitude greater
than that required by
Escherichia coli (
5). Because of the large
amount of iron to be transported, complex iron uptake systems
that differ from known transport mechanisms in other microorganisms
are expected to be operating in magnetotactic bacteria. Exceptional
progress has been made in the isolation and characterization
of functional genes and proteins involved in magnetosome synthesis
(
2,
11,
13,
21,
24), but at present, specific iron transport
systems remain unidentified in magnetotactic bacteria.
Here we report the identification of iron uptake systems by global expression profiling of the magnetotactic bacterium Magnetospirillum magneticum AMB-1 grown under iron-rich and iron-deficient conditions. Our results indicate that despite the unusual high-iron requirement of M. magneticum AMB-1, it utilizes robust but simple iron uptake systems similar to those of other gram-negative bacteria. This robust ferrous iron uptake suggests a significant contribution to magnetite synthesis. This study is the first to identify specific iron uptake systems in the complex iron metabolism of magnetotactic bacteria. The data presented here may facilitate future studies on the mechanism of magnetosome formation.
To monitor iron uptake and magnetite formation, M. magneticum AMB-1 (ATCC 700264) was grown at 25°C under microaerobic conditions by sparging argon gas for 10 min into 500 ml of MSGM medium as previously described (5), with various iron concentrations of 0.1 to 300 µM. All iron measurements were performed by atomic absorbance spectrophotometry. Extracellular iron concentrations were measured at different time points in cell-free culture supernatants. For intracellular iron measurements, cells were disrupted by lysozyme treatment (20) and ultracentrifuged at 100,000 x g to separate the insoluble (magnetites) and soluble iron fractions.
Iron was rapidly taken up in iron-rich cultures, and a corresponding increase of intracellular iron was observed within 10 min (Fig. 1A). Up to 70% of the initial iron concentration of the medium was taken up, and intracellular iron increased to 5,000 nmol/109 cells after 60 min. Insoluble iron in the cytoplasm, which mostly included magnetites, also increased within 10 min (Fig. 1B). These data indicate that the external iron was rapidly assimilated and formed into magnetite. Such rapid magnetite formation has also been observed in M. gryphiswaldense (26). Transmission electron microscopy confirmed the absence of magnetosomes in cells grown in 0.1 µM iron.
To relate the robust iron uptake to the corresponding gene expressions
of
M. magneticum AMB-1 cultured under different iron conditions,
transcription profiles were obtained by standard DNA microarray
(
8,
18,
19). The sequence of each of the 4,492 genes obtained
from
M. magneticum AMB-1 (
15), representing

99% of the total
protein-coding capacity of the whole genome sequence, was determined
and synthesized from the 60-mer region of minimal homology to
other open reading frames analyzed with the BLAST program. The
amino-activated oligonucleotides (40 pmol) were imprinted onto
glass slides (TaKaRa-Hubble Slide Glass; TaKaRa Bio Inc., Shiga,
Japan). Total RNA was extracted by the hot phenol acid method
(
10) and purified with an RNeasy Mini kit (QIAGEN, Hilden, Germany).
The threshold value was determined by using RNA extracted from
the strain AMB-1 cultures with various iron concentrations.
Five micrograms of purified RNA was reverse transcribed with
an RNA fluorescence labeling kit (TaKaRa Bio Inc.) by using
random 6-mer primers and the fluorochromes Cy3 dUTP (for mRNA
of cells grown with 20 to 300 µM iron) and Cy5 dUTP (for
mRNA of cells grown with 0.1 µM iron). Cy3- and Cy5-labeled
cDNAs were hybridized with oligonucleotides onto glass slides.
The signal value of each spot was determined by the following
formula: (signal of each spot background)/sum of all
the signal values from the 4,492 AMB-1 genes. The Cy3/Cy5 fluorescence
ratio was plotted, and the distribution was determined. Most
genes exhibited signals with ratios ranging from 0.7 to 1.5;
hence, up-regulated genes were defined by a signal ratio of
greater than 1.5 and down-regulated genes were defined by a
signal ratio of less than 0.7. Relative gene expression is presented
as the
n-fold change in the fluorescence intensity of cDNA synthesized
from total RNA derived from cells grown under several iron conditions
(magnetosome-forming condition: cultures with a 20 to 300 µM
initial iron concentration) compared to that of the reference
condition (non-magnetosome-forming condition: culture with a
0.1 µM initial iron concentration).
Global gene expression profiling of M. magneticum AMB-1 yielded five gene expression profile patterns (genes which have no uniform ratio were not categorized). Figure 2 shows the patterns categorized as types A, B, C, D, and E. Type A (384 genes) shows a pattern of genes consistently up-regulated in cells grown at initial iron concentrations of 20 to 300 µM with signal ratios 1.7-fold higher than genes from the iron-limiting condition (0.1 µM iron). Type B (230 genes) genes were consistently down-regulated in cells grown at iron concentrations of 20 to 300 µM with signal ratios less than 0.7-fold lower than genes in the cells grown at the low iron concentration. Type C genes (33 genes) were down-regulated above a 100 µM initial iron concentration, while type D genes (80 genes) were up-regulated above a 100 to 150 µM initial iron concentration. Type E genes (357 genes) were neither up-regulated nor down-regulated by any initial iron concentration, indicating that these genes are not responsive to the iron concentration. Figure 2 shows a partial list of genes.
Interestingly, two distinct patterns were observed in relation
to iron uptake and magnetosome synthesis. High-affinity ferrous
iron transport genes were up-regulated in magnetosome-forming
cells grown under iron-rich conditions, and ferric iron transport
genes were down-regulated under these conditions (Table
1).
The
ftr,
tpd, and
feo genes are known to be expressed under
low-oxygen conditions when ferrous iron remains stable and predominates
over ferric iron (
1,
7,
9,
12,
14). In this study, these gene
expressions are consistent with the microaerobic culture conditions
in which the cells were grown. This codependence of high iron
assimilation and microaerobic conditions for magnetosome synthesis
to occur is in agreement with earlier findings on
M. magnetotacticum (
5) and
M. gryphiswaldense (
26,
27). On the other hand, ferric
iron transport genes, which include
fepA,
tonB,
exbB, and
exbD (
1), were down-regulated under iron-rich conditions. This trend
is consistent with the mode of ferric iron uptake in other bacteria.
Two copies,
cirA, encoding a ferric-siderophore outer membrane
receptor, and
fepC, encoding an inner membrane ferric-siderophore
transporter (
1), however, were up-regulated under high-iron
conditions. In
M. magnetotacticum MS-1, more siderophores were
produced under iron-rich conditions than under iron-limited
conditions (
25). In
M. magneticum AMB-1, we have shown that
the initial high concentration of iron is rapidly assimilated
from the medium within only 4 h after inoculation, reaching
levels comparable to those of iron-deficient cultures, thereby
triggering siderophore excretion (
6). Microorganisms require
a minimum effective iron concentration of

0.01 µM for
growth but

1.0 µM for optimal growth (
22). This range
is much higher in magnetotactic bacteria, at least 6 µM
(
6), because of their high iron requirement for magnetosome
synthesis. Ferric siderophores may not be directly involved
in magnetosome synthesis but may contribute in ensuring that
the high iron supply demanded by magnetotactic bacteria is acquired.
View this table:
[in this window]
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TABLE 1. Expression of genes involved in ferrous and ferric ion transport and nitrogen respiration in M. magneticum AMB-1 at various initial iron concentrations
|
Additionally, higher transcript levels of nitrate reductase
(amb2686, amb2687, amb2690) and ferric reductase (amb3335) genes
were obtained under iron-rich, magnetosome-forming conditions.
In
M. magnetotacticum, ferric reductase was apparently required
for magnetite production (
23). We have previously reported that
when
M. magneticum AMB-1 utilizes nitrate as its sole nitrogen
source, magnetites are produced, with ferric iron serving as
the terminal electron acceptor (
16,
17). Iron reduction and
magnetosome formation with respiratory nitrate reduction were
inhibited by dicumarol, an inhibitor of quinone (
17), indicating
that iron reduction is coupled with respiratory nitrate reduction
during magnetosome synthesis.
In order for magnetosome production to proceed in magnetotactic bacteria, two main precise physiological conditions are required: (i) a narrow range of low oxygen concentrations and (i) an extraordinary amount of iron to be assimilated. Although these have been clearly demonstrated by several groups (3-5, 26), these findings must be augmented with specific iron transport systems to further elucidate the unique process of magnetosome synthesis.
Nucleotide sequence accession number.
The microarray data and nucleotide sequence information obtained in this study were submitted to the National Center for Biotechnology Information GEO database and assigned accession no. GSE3914.

ACKNOWLEDGMENTS
This work was funded in part by Grant-in-Aid for Specially Promoted
Research 13002005 from the Ministry of Education, Science, Sports
and Culture of Japan.

FOOTNOTES
* Corresponding author. Mailing address: Department of Biotechnology, Tokyo University of Agriculture and Technology, 2-24-16 Naka-cho, Koganei, Tokyo, Japan 184-8588. Phone: 81-42-388-7020. Fax: 81-42-385-7713. E-mail:
tmatsuna{at}cc.tuat.ac.jp.


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Journal of Bacteriology, March 2006, p. 2275-2279, Vol. 188, No. 6
0021-9193/06/$08.00+0 doi:10.1128/JB.188.6.2275-2279.2006
Copyright © 2006, American Society for Microbiology. All Rights Reserved.
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