Abstract
Bacteria in nature encounter substrates at widely varying concentrations, yet studies of bacterial 30
physiology have focused more on nutrient type than concentration, partly due to challenges in
maintaining low concentrations. We developed a Millifluidic Continuous Culture Device
(MCCD) to culture bacteria under precisely controlled nutrient conditions, including very low
concentrations, in a manner suitable for proteomic analysis. Using the MCCD, we cultured
Escherichia coli with a mixture of amino acids as the sole carbon source at three concentrations 35
supporting growth rates spanning a fivefold range. Surprisingly, at the lowest concentration, cells
exhibited proteomic signatures of iron shortage despite constant iron levels across conditions.
Uptake of labeled iron-histidine and iron-cysteine complexes demonstrated that amino-acid-
bound iron is bioavailable to E. coli. These findings reveal a previously unknown mechanism of
bacterial iron acquisition that emerged under the flow imposed by the MCCD, which diluted the 40
siderophore pool and reduced their efficacy. This work highlights the importance of studying
bacterial physiology under low nutrient concentrations and demonstrates how physical
conditions, such as flow, shape microbial nutrient acquisition strategies.
.CC-BY-NC-ND 4.0 International licenseavailable under a
(which was not certified by peer review) is the author/funder, who has granted bioRxiv a license to display the preprint in perpetuity. It is made
The copyright holder for this preprintthis version posted January 16, 2025. ; https://doi.org/10.1101/2025.01.15.633289doi: bioRxiv preprint
2
Main Text
Bacteria constitute one of the largest biomass fractions on the planet (1), contribute to host health
and disease (2), and play essential roles in biogeochemical cycles (3). In environments ranging
from the gut to the ocean, bacteria often encounter low concentrations of diverse nutrients that
limit their growth (4–9). Understanding bacterial growth under nutrient-limited conditions is 5
challenging for multiple reasons. First, mimicking such conditions in the laboratory for extended
periods is difficult: although chemostats are commonly used to study low-nutrient regimes, the
use of low dilution rates can lead to inhomogeneities in nutrient distribution (10). Second, the
interplay between multiple nutrient shortages can trigger complex physiological responses: the
uptake of one nutrient may rely on the availability of another, creating a dependency in nutrient 10
acquisition.
Proteomics has emerged as a valuable approach for mechanistically understanding bacterial
physiological responses to environmental change (11–15) and diagnosing resource shortages, as
one can infer underlying stressors from observed protein abundances (16). While microfluidic
approaches have enabled the study of bacterial physiology under low nutrient conditions (17), 15
these methods typically yield insufficient biomass for proteomic analysis. Consequently, studies
on bacterial physiology have primarily relied on bulk cultures with saturating nutrient
concentrations and have mainly investigated how different nutrient types affect bacterial growth
rates and physiological states (12, 18–25). To address this limitation, we developed a novel
cultivation method that allows proteomic investigation of bacterial populations grown under a 20
broad range of nutrient concentrations.
Here, we introduce the Millifluidic Continuous Culture Device (MCCD), which enables the
cultivation of bacterial populations under constant nutrient conditions. Using the MCCD, we
analyzed the proteome of Escherichia coli grown under different concentrations of a nutrient
mixture containing amino acids, nucleobases, and vitamins. Our analysis revealed broad 25
proteomic shifts across nutrient concentrations, including a reduction in amino acid biosynthesis
enzymes at higher nutrient concentrations. This finding contrasts with results from studies
conducted under saturating conditions that varied only the organic carbon source.
Unexpectedly, despite varying only carbon substrate concentrations, in the low nutrient condition
cells displayed a proteomic signature indicative of iron shortage. Based on these findings and on 30
the results of a chemical equilibrium model, we propose that amino acids form complexes with
iron that are bioavailable to the bacteria, so that the low abundance of amino acids in the low
nutrient concentration resulted in iron limitation. This hypothesis was confirmed by uptake
experiments with 57Fe, demonstrating that E. coli can acquire iron when it is complexed with
cysteine or histidine and thus revealing a previously unrecognized role for amino acids in 35
facilitating iron uptake. Given the pervasive scarcity of iron across microbial habitats, our
findings suggest that the role of free amino acids in iron uptake may be pervasive in microbial
ecology.
A novel device to cultivate cells for proteomics at low nutrient concentrations
We developed the Millifluidic Continuous Culture Device (MCCD), a device that enables the 40
cultivation of bacterial populations under approximately constant nutrient conditions, even at low
concentrations, by maintaining continuous fluid flow. The MCCD supports the accumulation of
sufficient bacterial biomass for proteomic analysis, providing a new approach to study bacterial
physiological responses to nutrient stress. Additionally, the presence of continuous flow mimics
the dynamic conditions encountered in many natural microbial habitats. The device delivers a 45
.CC-BY-NC-ND 4.0 International licenseavailable under a
(which was not certified by peer review) is the author/funder, who has granted bioRxiv a license to display the preprint in perpetuity. It is made
The copyright holder for this preprintthis version posted January 16, 2025. ; https://doi.org/10.1101/2025.01.15.633289doi: bioRxiv preprint
3
steady supply of fresh medium to bacterial cells growing within a Sterivex filter (Fig. 1A). The
0.45-µm pore size filter contained within a 2.5-mL cylinder (Fig. 1A, dotted inset) permits the
flow of nutrients (2 mL/min) while retaining cells, facilitating biomass accumulation for
downstream analyses.
We grew E. coli in a MOPS-based medium (26) with three concentrations of a rich-defined 5
medium (RDM) supplement to impose carbon limitation and support distinct physiological
states: "High" for rapid growth, "Medium" for intermediate growth, and "Low" for slow growth.
The supplement, containing 20 amino acids, four nucleobases, and vitamins, was proportionally
diluted across the conditions to maintain relative concentration ratios (table S1). Using the
MCCD, we observed exponential growth in all conditions (fig. S1), with growth rates of 0.18 ± 10
0.002 h⁻¹, 0.64 ± 0.06 h⁻¹, and 0.88 ± 0.03 h⁻¹ in the Low, Medium, and High conditions,
respectively (Fig. 1B). The MCCD sustained exponential growth for at least three doublings in
each condition. Since protein half-lives are governed by cell division (27), we assumed that this
timescale was sufficient for the proteome to adjust to the nutrient environment.
We performed experiments and simulations to characterize the nutrient environment experienced 15
by cells in the MCCD. Scanning electron microscopy (SEM) of the bacterial population on the
filter confirmed that cells were distributed across the membrane surface in layers that were three
cells thick or less when the population inside the Sterivex reached approximately 109 cells (Fig.
1C, fig. S2). This spatial distribution ensures minimal nutrient concentration decrease between
the bottom and top layers of cells (Supplementary Text 1). Numerical simulations of the flow 20
field in the filter revealed uniform flow velocity across the membrane surface (fig. S3A) and
indicated that the pressure experienced by the bacteria due to the flowing medium was small (6.4
kPa; fig. S3B) (28). Finally, metabolomic analysis of the medium flowing in and out of the filters
housing the bacterial population showed that, for the nutrients detectable by mass spectrometry,
consumption reached up to 40% in the High condition (fig. S4), though complete nutrient 25
exhaustion was not observed. In the Medium and Low conditions, nutrient concentrations were
below the detection limit at inflow, preventing an assessment of their consumption. Together,
these data indicate that the MCCD is suitable for exposing a bacterial population to
approximately homogeneous and constant nutrient conditions.
Evidence of a non-carbon nutrient shortage in the Low condition despite lowest carbon 30
concentration
To determine the relative protein abundances in E. coli cells cultured in each of the three nutrient
concentrations, we performed liquid chromatography tandem mass spectrometry on each of four
replicate samples, for each concentration. From the mass spectrometry data, we identified 1,441
proteins that account for 32% of the predicted protein-encoding genes in E. coli NCM3722 (Data 35
S1, table S2). We report protein abundances as normalized spectral counts to account for
variation in total spectral counts across samples, thus allowing comparison of relative protein
abundances between samples. To ensure our analysis was robust to biological noise, we focused
further analysis on a subset of 861 proteins that exceeded an abundance threshold (Materials and
Methods). We report the abundances of these 861 proteins as percentages of total spectral counts 40
throughout the figures and text.
To identify the biological processes with higher or lower protein abundances in each nutrient
concentration as indicative of physiological responses, we used the EcoCyc database (29) to
group the 861 proteins into functional protein groups (table S3). This analysis identified 52
functional groups, with 33 showing significant differences between nutrient concentrations (p < 45
.CC-BY-NC-ND 4.0 International licenseavailable under a
(which was not certified by peer review) is the author/funder, who has granted bioRxiv a license to display the preprint in perpetuity. It is made
The copyright holder for this preprintthis version posted January 16, 2025. ; https://doi.org/10.1101/2025.01.15.633289doi: bioRxiv preprint
4
0.05, Kruskal-Wallis test) (Fig. 2, fig. S5). We focused on these 33 functional protein groups
(representing 627 proteins) for the remainder of the study. We conducted a comparative analysis
of the Low and Medium conditions relative to the High condition, which was the least limiting
for bacterial growth.
Hierarchical clustering of the functional protein groups revealed distinct abundance patterns 5
across nutrient concentrations (Fig. 2). From these patterns, three main clusters emerged: protein
groups that increased in abundance with higher nutrient concentration (Fig. 2, purple cluster),
those that decreased (Fig. 2, green cluster), and those that peaked in the Medium concentration
(Fig. 2, orange cluster). Most protein groups that increased in abundance with higher nutrient
concentration (purple cluster) are associated with the demands of rapidly growing cells, such as 10
translation, protein folding, and fatty acid biosynthesis. This cluster also included
gluconeogenesis and TCA cycle enzymes, reflecting the use of amino acids as the carbon source
in our experiments (30). Amino acids are catabolized to pyruvate and TCA cycle intermediates,
which feed into the TCA cycle and gluconeogenesis pathways (25). The higher abundance of
these enzymes indicates greater amino acid availability in this condition. 15
Conversely, some groups that increased in abundance with lower nutrient concentration (green
cluster in Fig. 2) are part of the general stress response triggered by nutrient limitation to protect
cells from stresses (31). These include osmoregulation, oxidative stress, and membrane integrity.
Proteins in the σS regulon are known to become more abundant at slower growth rates (22, 31).
Our observation of increased stress response proteins in the Low and Medium conditions aligns 20
with this, confirming that the modulation of σS levels is consistent with the slower growth rates
observed in these conditions. We also observed an increase in amino acid and nucleotide
biosynthesis groups with lower nutrient concentrations. This contrasts with studies of E. coli’s
growth rate with saturating concentrations of different carbon sources, where amino acid and
nucleotide biosynthesis enzymes are positively correlated with growth rate (22, 25, 32). The 25
opposite trend in our study, where we varied carbon concentration instead, likely reflects a
decreased biosynthetic requirement for amino acids and nucleotides in the Medium and High
conditions, as these are provided in the culture medium.
Unexpectedly, protein groups whose relative abundance peaked in the Medium condition
included those known to increase in response to carbon limitation, such as carbon catabolism 30
(31, 32), nucleotide degradation (33–37), and protein degradation (38–40) (orange cluster in Fig.
2; Fig. 3A-C). This was surprising since carbon concentrations were lowest in the Low
condition, where we expected the highest abundance of these protein groups. To investigate
whether this “concave expression profile” (highest abundance in the Medium condition) was
present at the individual protein level, we classified each protein according to its expression 35
profile: increasing abundance with higher nutrient concentration, increasing abundance with
lower nutrient concentration, or highest abundance in the Medium concentration (see Materials
and Methods and fig. S6 for classification details). Over 50% of proteins in these groups
displayed the concave expression profile (Fig. 3D-F; table S4). This unexpected pattern suggests
that cells in the Low condition, despite having the lowest carbon concentration, may have 40
experienced a shortage of another nutrient.
Further support for the idea of a nutrient shortage other than carbon was observed in the
abundance of enzymes involved in glycogen biosynthesis, which peaked in the Low condition
(“Synthesis of storage compounds” in the green cluster in Fig. 2 and Fig. 3G-I). In E. coli,
glycogen is synthesized when there is sufficient carbon but growth is constrained by the lack of 45
another essential nutrient (5, 41, 42). The increased abundance of two key enzymes in the
.CC-BY-NC-ND 4.0 International licenseavailable under a
(which was not certified by peer review) is the author/funder, who has granted bioRxiv a license to display the preprint in perpetuity. It is made
The copyright holder for this preprintthis version posted January 16, 2025. ; https://doi.org/10.1101/2025.01.15.633289doi: bioRxiv preprint
5
glycogen biosynthesis pathway in the Low condition (Fig. 3H,I), especially GlgC – the first rate-
limiting enzyme – suggests that the observed response in the Low condition was not solely
driven by carbon scarcity.
Evidence for iron shortage in the Low condition
Our analysis revealed three lines of evidence of iron scarcity in the Low condition, based on the 5
expression patterns of the iron acquisition protein FepA, Isc system proteins, and TCA cycle
enzymes (Fig. 4A). First, FepA was 4.4 times more abundant in the Low condition compared to
the Medium condition and 3.6 times more abundant than in the High condition (Fig. 4B). FepA
is an outer membrane transporter induced under low-iron conditions, responsible for transporting
enterobactin—a siderophore secreted by the cell to capture ferric iron with high affinity—into 10
the periplasm (43, 44). Given that the ferric uptake regulator (Fur) represses fepA transcription
when iron concentrations are sufficient (43, 44), the elevated abundance of FepA in the Low
condition indicates iron availability was insufficient, triggering upregulation of this iron
acquisition pathway.
Second, we found that IscU, a component of the Isc system, was least abundant in the Low 15
condition, with a 35% decrease relative to the High condition (Fig. 4C). IscS showed a similar
trend, though this was not strictly significant (Kruskal-Wallis test, p = 0.063, fig. S7). These
observations are consistent with iron scarcity, as the Isc system, a multiprotein complex that
assembles iron-sulfur clusters and transfers them to proteins for catalytic function and structural
stability (Fig. 4A) (45), is known to be repressed under iron scarcity (46). In E. coli, 20
downregulation of Isc proteins is part of the iron-sparing response, which conserves iron for
critical functions by reducing the expression of iron-rich proteins when iron is scarce (47).
Third, in the Low condition we observed increased abundances of certain TCA cycle enzymes
known to retain activity under iron scarcity (48–50). Fumarase A (FumA) and Fumarase C
(FumC), which catalyze the same reaction, showed opposing expression patterns: FumA was 25
least abundant in the Low condition, whereas FumC was most abundant (Fig. 4G,H). A similar
trend was observed with the aconitase isozymes: Aconitase B (AcnB) was most abundant in the
High condition, followed by the Medium condition, whereas Aconitase A (AcnA) was less
abundant in the Low and Medium conditions (Fig. 4E,F). These expression patterns align with
the iron dependency of these enzymes. FumC remains active under iron scarcity because, unlike 30
FumA, it lacks an iron-sulfur cluster (48, 49). Similarly, while both AcnA and AcnB have iron-
sulfur clusters, AcnA is known to be more stable under low iron conditions, whereas the exposed
cluster in AcnB is prone to dissociation (50). The concurrent upregulation of FumC and AcnA,
alongside the downregulation of FumA and AcnB, reflects a signature iron-sparing response in
E. coli (Fig. 4D) (46, 51). Together, the simplest explanation for the proteome profile in the Low 35
condition is that the cells in the Low condition experienced iron scarcity.
Iron-amino-acid complexes as bioavailable iron sources
The scarcity of iron in the Low condition is surprising, given that the same amount of iron (0.01
mM iron sulfate) and tricine (4 mM) was present in all nutrient conditions (Materials and
Methods, (26)). We hypothesized that amino acid concentrations influenced iron availability due 40
to the formation of iron-amino-acid complexes. The solubility of iron is strongly influenced by
its redox state: ferrous iron (Fe(II)) is soluble, but in oxic environments it rapidly oxidizes to
ferric iron (Fe(III)), which precipitates as nearly insoluble hydroxides (occurring at
concentrations around 0.5 nM in natural waters (52)). However, iron can form complexes with
organic compounds, including certain amino acids (53–57), which, when bound as Fe(II), 45
.CC-BY-NC-ND 4.0 International licenseavailable under a
(which was not certified by peer review) is the author/funder, who has granted bioRxiv a license to display the preprint in perpetuity. It is made
The copyright holder for this preprintthis version posted January 16, 2025. ; https://doi.org/10.1101/2025.01.15.633289doi: bioRxiv preprint
6
prevent its oxidation and maintain a soluble Fe(II) pool. In the medium we used tricine, which
serves to prevent the oxidation of Fe(II) and keep it in solution (26). However, while tricine
concentrations were constant across conditions, amino acid concentrations varied. Thus,
differences in the pool of available Fe(II) complexes were likely driven by variations in amino
acid concentrations. 5
To investigate the speciation of Fe(II), we used MINEQL+ 5.0 (58, 59) to construct a chemical
equilibrium model and calculate the concentrations of Fe(II) complexes in each condition.
Specifically, we examined two fractions of the ferrous iron pool: Fe(II)', representing Fe(II)
bound to inorganic compounds and the divalent cation species (with Fe2+ constituting
approximately 98% of Fe(II)’; supplementary table S6), and Fe(II)L, representing Fe(II) bound 10
to organic ligands, including iron-amino-acid complexes. The model used the concentrations of
19 amino acids (asparagine was excluded due to the lack of stability constants), tricine, and
inorganic salts for each nutrient condition, based on the defined composition of the medium.
Stability constants for amino acids were obtained from the MINEQL+ database (54, 55). To our
knowledge, stability constants for tricine have not been reported. Therefore, we substituted 15
bicine in the model due to its structural similarity to tricine. A ligand exchange experiment
confirmed comparable stability constants for bicine and tricine (Fig. S8), supporting the validity
of this substitution. We set the total amount of iron as Fe(II), assuming minimal oxidation to
Fe(III) based on oxidation rate estimates (Supplementary Text 2). Our results showed that Fe(II)-
bicine, which accounted for the majority (95.8–98.7%) of the Fe(II) pool, and Fe(II)’ remained 20
nearly constant across the Low, Medium, and High conditions (Fig. 5A). This near-constancy
indicates that tricine-bound Fe(II) and inorganic Fe(II) species were not responsible for the
reduced iron availability observed in the Low condition.
In contrast, the model predicted that the Low condition had substantially lower concentrations of
Fe(II) complexed with amino acids (Fig. 5A). The concentration of the Fe(II)-cysteine complex, 25
the most abundant Fe(II)-amino-acid complex, was two orders of magnitude lower in the Low
condition (0.006 µM) than in the High condition (0.297 µM). Similarly, Fe(II)-histidine and
Fe(II)-serine, the next most abundant complexes, also showed concentrations two orders of
magnitude lower in the Low condition compared to the High condition (Fig. 5A, table S6).
Though Fe(II)' is considered to be a highly bioavailable form of iron (60), our proteomic and 30
modeling data indicate that the iron shortage arose from the lower concentrations of iron-amino-
acid complexes in the Low condition. Overall, our modeling results suggest that iron-amino-acid
complexes serve as important bioavailable iron sources for E. coli and their scarcity in the Low
condition led to iron scarcity.
Cysteine- and histidine-iron complexes are bioavailable iron sources for E. coli 35
To test whether iron-amino-acid complexes serve as bioavailable iron sources for E. coli, we
conducted iron uptake experiments using the rare 57Fe isotope, which constitutes only 2% of
naturally occurring iron. Complexes of 57Fe-Cysteine (57Fe-Cys) and 57Fe-Histidine (57Fe-His)
were prepared by mixing 57Fe with cysteine or histidine at a 1:10 molar ratio and spiked into
actively growing cultures in the MCCD at three timepoints, spaced 30 minutes apart. Controls 40
included (1) a “dead cells” control with glutaraldehyde-killed cells (1.5% final concentration)
spiked with the 57Fe -Cys complex, (2) a non-bioavailable control with an 57Fe -EDTA complex,
and (3) no iron complex addition. At each timepoint, cell pellets were harvested, and intracellular
iron (56Fe and 57Fe isotopes) concentrations were quantified using inductively coupled plasma
mass spectrometry (ICP-MS). 45
.CC-BY-NC-ND 4.0 International licenseavailable under a
(which was not certified by peer review) is the author/funder, who has granted bioRxiv a license to display the preprint in perpetuity. It is made
The copyright holder for this preprintthis version posted January 16, 2025. ; https://doi.org/10.1101/2025.01.15.633289doi: bioRxiv preprint
7
The results showed that 57Fe -amino-acid complexes were bioavailable to E. coli. To account for
biomass differences, 57Fe concentrations were normalized to phosphorus levels ([57Fe]/[P]),
assuming proportionality between phosphorus content and cell growth (18, 61). A linear
regression analysis revealed that the slopes of [57Fe]/[P] for the 57Fe -Cys and 57Fe -His
treatments were 36 and 27 µM M-1min-1, respectively. In contrast, the 57Fe-EDTA and dead-cells 5
control had slopes of 5 and 1 µM M-1min-1 (Fig. 5B). These results indicate that 57Fe
accumulation in the 57Fe -Cys and 57Fe -His treatments was active and mediated by amino acid
complexation. The unchanged [57Fe]/[P] levels in the dead-cell control confirmed that uptake of
iron-amino-acid complexes was not passive, and the unchanged levels in the 57Fe-EDTA control,
acting as the non-bioavailable control, demonstrated that iron uptake was not driven by non-10
specific chelation.
To further examine the preferential uptake of ⁵⁷Fe from amino acid complexes, we compared the
rates of iron uptake for ⁵⁷Fe, enriched with pre-formed iron-amino-acid complexes, and the most
naturally abundant isotope ⁵⁶Fe, predominantly bound to tricine (Fig. 5A). Therefore, comparing
the ratio of the uptake of the two iron isotopes reflects differences in uptake efficiency due to 15
complexation of iron with AA. We used an ordinary least squares (OLS) linear model to analyze
the time-course measurements of intracellular 56Fe and 57Fe concentrations for each treatment,
revealing that the uptake rate of 57Fe was 3.8 times higher than that of 56Fe in the 57Fe-Cys
treatment and 5.8 times higher in the 57Fe-His treatment (p < 0.05, two-tailed t-test, Fig. S9A,B).
These results indicate that the complexation of iron with cysteine or histidine facilitates iron 20
uptake.
References
1. Y. M. Bar-On, R. Phillips, R. Milo, The biomass distribution on Earth. Proc Natl Acad Sci U S A
115, 6506–6511 (2018). 15
2. K. Hou, Z. X. Wu, X. Y. Chen, J. Q. Wang, D. Zhang, C. Xiao, D. Zhu, J. B. Koya, L. Wei, J. Li, Z.
S. Chen, Microbiota in health and diseases. Signal Transduct Target Ther 7 (2022).
3. P. G. Falkowski, T. Fenchel, E. F. Delong, The Microbial Engines That Drive Earth’s
Biogeochemical Cycles. Science (1979) 320, 1034–1039 (2008).
4. T. Egli, “The ecological and physiological significance of the growth of heterotrophic 20
microorganisms with mixtures of substrates” in Advances in Microbial Ecology (1995)vol. 14, pp.
305–386.
5. T. Conway, P. S. Cohen, Commensal and Pathogenic Escherichia coli Metabolism in the Gut.
Microbiol Spectr 3 (2015).
6. S. Doranga, T. Conway, K. A. Krogfelt, P. S. Cohen, Nutrition of Escherichia coli within the 25
intestinal microbiome. EcoSal Plus, eesp-0006 (2024).
7. U. Muenster, Concentrations and fluxes of organic carbon substrates in the aquatic environment.
Antonie Van Leeuwenhoek 63, 243–274 (1993).
8. A. L. Koch, Oligotrophs versus copiotrophs. BioEssays 23, 657–661 (2001).
9. C. M. Moore, M. M. Mills, K. R. Arrigo, I. Berman-Frank, L. Bopp, P. W. Boyd, E. D. Galbraith, R. 30
J. Geider, C. Guieu, S. L. Jaccard, T. D. Jickells, J. La Roche, T. M. Lenton, N. M. Mahowald, E.
Marañón, I. Marinov, J. K. Moore, T. Nakatsuka, A. Oschlies, M. A. Saito, T. F. Thingstad, A.
Tsuda, O. Ulloa, Processes and patterns of oceanic nutrient limitation. Nat Geosci 6, 701–710
(2013).
10. G. S. Hansford, A. E. Humphrey, The effect of equipment scale and degree of mixing on continuous 35
fermentation yield at low dilution rates. Biotechnol Bioeng 8, 85–96 (1966).
11. M. S. Guo, C. A. Gross, Stress-induced remodeling of the bacterial proteome. Current Biology 24,
R424–R434 (2014).
12. A. Schmidt, K. Kochanowski, S. Vedelaar, E. Ahrné, B. Volkmer, L. Callipo, K. Knoops, M. Bauer,
R. Aebersold, M. Heinemann, The quantitative and condition-dependent Escherichia coli proteome. 40
Nat Biotechnol 34, 104–110 (2016).
13. A. Mateus, J. Hevler, J. Bobonis, N. Kurzawa, M. Shah, K. Mitosch, C. V. Goemans, D. Helm, F.
Stein, A. Typas, M. M. Savitski, The functional proteome landscape of Escherichia coli. Nature 588,
473–478 (2020).
14. C. Wu, M. Mori, M. Abele, A. Banaei-Esfahani, Z. Zhang, H. Okano, R. Aebersold, C. Ludwig, T. 45
Hwa, Enzyme expression kinetics by Escherichia coli during transition from rich to minimal media
depends on proteome reserves. Nat Microbiol 8, 347–359 (2023).
15. M. Mori, S. Schink, D. W. Erickson, U. Gerland, T. Hwa, Quantifying the benefit of a proteome
reserve in fluctuating environments. Nat Commun 8, 1225 (2017).
16. N. G. Walworth, M. A. Saito, M. D. Lee, M. R. McIlvin, D. M. Moran, R. M. Kellogg, F. X. Fu, D. 50
A. Hutchins, E. A. Webb, Why Environmental Biomarkers Work: Transcriptome–Proteome
Correlations and Modeling of Multistressor Experiments in the Marine Bacterium Trichodesmium. J
Proteome Res 21, 77–89 (2022).
.CC-BY-NC-ND 4.0 International licenseavailable under a
(which was not certified by peer review) is the author/funder, who has granted bioRxiv a license to display the preprint in perpetuity. It is made
The copyright holder for this preprintthis version posted January 16, 2025. ; https://doi.org/10.1101/2025.01.15.633289doi: bioRxiv preprint
10
17. J. Nguyen, V. Fernandez, S. Pontrelli, U. Sauer, M. Ackermann, R. Stocker, A distinct growth
physiology enhances bacterial growth under rapid nutrient fluctuations. Nat Commun 12 (2021).
18. M. Schaechter, O. Maaloe, N. O. Kjeldgaard, Dependency on Medium and Temperature of Cel Size
and Chemical Composition during Balanced Growth of Salmonella typhimurium. Microbiology (N
Y) 19, 592–606 (1958). 5
19. F. C. Neidhardt, B. Magasanik, Studies on the role of ribonucleic acid in the growth of bacteria.
Biochim Biophys Acta 42, 99–116 (1960).
20. M. Scott, C. W. Gunderson, E. M. Mateescu, Z. Zhang, T. Hwa, Interdependence of cell growth and
gene expression: origins and consequences. Science (1979) 330, 1099–1102 (2010).
21. M. U. Caglar, J. R. Houser, C. S. Barnhart, D. R. Boutz, S. M. Carroll, A. Dasgupta, W. F. Lenoir, 10
B. L. Smith, V. Sridhara, D. K. Sydykova, D. Vander Wood, C. J. Marx, E. M. Marcotte, J. E.
Barrick, C. O. Wilke, The E. coli molecular phenotype under different growth conditions. Sci Rep 7
(2017).
22. M. Mori, Z. Zhang, A. Banaei‐Esfahani, J. Lalanne, H. Okano, B. C. Collins, A. Schmidt, O. T.
Schubert, D. Lee, G. Li, R. Aebersold, T. Hwa, C. Ludwig, From coarse to fine: the absolute 15
Escherichia coli proteome under diverse growth conditions . Mol Syst Biol 17 (2021).
23. C. You, H. Okano, S. Hui, Z. Zhang, M. Kim, C. W. Gunderson, Y. P. Wang, P. Lenz, D. Yan, T.
Hwa, Coordination of bacterial proteome with metabolism by cyclic AMP signalling. Nature 500,
301–306 (2013).
24. Z. Li, M. Nimtz, U. Rinas, The metabolic potential of Escherichia coli BL21 in defined and rich 20
medium. Microb Cell Fact 13 (2014).
25. S. Hui, J. M. Silverman, S. S. Chen, D. W. Erickson, M. Basan, J. Wang, T. Hwa, J. R. Williamson,
Quantitative proteomic analysis reveals a simple strategy of global resource allocation in bacteria.
Mol Syst Biol 11 (2015).
26. F. C. Neidhardt, P. L. Bloch, D. F. Smith, Culture Medium for Enterobacteria. J Bacteriol 119, 736–25
747 (1974).
27. M. Shamir, Y. Bar-On, R. Phillips, R. Milo, SnapShot: Timescales in Cell Biology. Cell 164, 1302–
1302 (2016).
28. A. Guyet, M. Dade-Robertson, A. Wipat, J. Casement, W. Smith, H. Mitrani, M. Zhang, Mild
hydrostatic pressure triggers oxidative responses in Escherichia coli. PLoS One 13 (2018). 30
29. I. M. Keseler, S. Gama-Castro, A. Mackie, R. Billington, C. Bonavides-Martínez, R. Caspi, A.
Kothari, M. Krummenacker, P. E. Midford, L. Muñiz-Rascado, W. K. Ong, S. Paley, A. Santos-
Zavaleta, P. Subhraveti, V. H. Tierrafría, A. J. Wolfe, J. Collado-Vides, I. T. Paulsen, P. D. Karp,
The EcoCyc Database in 2021. Front Microbiol 12 (2021).
30. L. Reitzer, Catabolism of Amino Acids and Related Compounds. EcoSal Plus 1 (2005). 35
31. R. Hengge, Stationary-Phase Gene Regulation in Escherichia coli §. EcoSal Plus 4, 10–1128 (2011).
32. M. Scott, T. Hwa, Shaping bacterial gene expression by physiological and proteome allocation
constraints. Nat Rev Microbiol 21, 327–342 (2022).
33. Y. E. Zhang, R. L. Bærentsen, T. Fuhrer, U. Sauer, K. Gerdes, D. E. Brodersen, (p)ppGpp Regulates
a Bacterial Nucleosidase by an Allosteric Two-Domain Switch. Mol Cell 74, 1239-1249.e4 (2019). 40
34. K. Nath, A. L. Koch, Protein Degradation in Escherichia coli. Journal of Biological Chemistry 246,
6956–6967 (1971).
35. K. F. Jensen, G. Dandanell, B. Hove-Jensen, M. Willemoës, Nucleotides, Nucleosides, and
Nucleobases. EcoSal Plus 3 (2008).
36. R. Kaplan, L. Cohen, E. Yagil, Acid-Soluble Degradation Products of Ribonucleic Acid in 45
Escherichia coli and the Role of Nucleotidases in Their Catabolism. J Bacteriol 124, 1159–1164
(1975).
37. L. Cohen, R. Kaplan, Accumulation of Nucleotides by Starved Escherichia coli Cells as a Probe for
the Involvement of Ribonucleases in Ribonucleic Acid Degradation. J Bacteriol 129, 651–657
(1977). 50
38. D. Weichart, N. Querfurth, M. Dreger, R. Hengge-Aronis, Global role for ClpP-containing proteases
in stationary-phase adaptation of Escherichia coli. J Bacteriol 185, 115–125 (2003).
39. C. A. Reeve, A. T. Bockman, A. Matin, Role of Protein Degradation in the Survival of Carbon-
Starved Escherichia coli and Salmonella typhimurium. J Bacteriol 157, 758–763 (1984).
40. D. Pletzer, T. M. Blimkie, H. Wolfmeier, Y. Li, A. Baghela, A. H. Y Lee, R. Falsafi, R. E. W 55
Hancock, C. D. Pletzer, L. Ahy, H. Rew, The Stringent Stress Response Controls Proteases and
.CC-BY-NC-ND 4.0 International licenseavailable under a
(which was not certified by peer review) is the author/funder, who has granted bioRxiv a license to display the preprint in perpetuity. It is made
The copyright holder for this preprintthis version posted January 16, 2025. ; https://doi.org/10.1101/2025.01.15.633289doi: bioRxiv preprint
11
Global Regulators under Optimal Growth Conditions in Pseudomonas aeruginosa. mSystems 5, 10–
1128 (2020).
41. J. Preiss, T. Romeo, Molecular Biology and Regulatory Aspects of Glycogen Biosynthesis in
Bacteria. Prog Nucleic Acid Res Mol Biol 47, 299–329 (1994).
42. S. A. Jones, M. Jorgensen, F. Z. Chowdhury, R. Rodgers, J. Hartline, M. P. Leatham, C. Struve, K. 5
A. Krogfelt, P. S. Cohen, T. Conway, Glycogen and maltose utilization by Escherichia coli
O157:H7 in the mouse intestine. Infect Immun 76, 2531–2540 (2008).
43. M. Sandy, A. Butler, Microbial iron acquisition: Marine and terrestrial siderophores. Chem Rev 109,
4580–4595 (2009).
44. S. C. Andrews, A. K. Robinson, F. Rodríguez-Quiñones, Bacterial iron homeostasis. FEMS 10
Microbiol Rev 27, 215–237 (2003).
45. J. A. Imlay, The molecular mechanisms and physiological consequences of oxidative stress: Lessons
from a model bacterium. Nat Rev Microbiol 11, 443–454 (2013).
46. E. Massé, M. Arguin, Ironing out the problem: New mechanisms of iron homeostasis. Trends
Biochem Sci 30, 462–468 (2005). 15
47. A. Gaballa, H. Antelmann, C. Aguilar, S. K. Khakh, K.-B. Song, G. T. Smaldone, J. D. Helmann,
The Bacillus subtilis iron-sparing response is mediated by a Fur-regulated small RNA and three
small, basic proteins. Proceedings of the National Academy of Sciences 105, 11927–11932 (2008).
48. D. H. Flint, M. H. Emptage, J. R. Guest, Fumarase A from Escherichia coli: Purification and
Characterization as an Iron-Sulfur Cluster Containing Enzyme. Biochemistry 31, 10331–10337 20
(1992).
49. S. I. Liochev, I. Fridovich, FumaraseC, the stable fumarase of Escherichia coli, is controlled by the
soxRS regulon. Proceedings of the National Academy of Sciences 89, 5892–5896 (1992).
50. S. Varghese, Y. Tang, J. A. Imlay, Contrasting sensitivities of Escherichia coli aconitases A and B
to oxidation and iron depletion. J Bacteriol 185, 221–230 (2003). 25
51. E. Massé, S. Gottesman, A small RNA regulates the expression of genes involved in iron
metabolism in Escherichia coli. Proceedings of the National Academy of Sciences 99, 4620–4625
(2002).
52. K. Kuma, J. Nishioka, K. Matsunaga, Controls on iron(III) hydroxide solubility in seawater: The
influence of pH and natural organic chelators. Limnol Oceanogr 41, 396–407 (1996). 30
53. D. B. Sabine, Metallo-Amino Acid Complexes III. iron Complexes. Microchemical Journal 24,
475–478 (1979).
54. A. E. Martell, R. M. Smith, Critical Stability Constants: Vol. 1 Amino Acids (Plenum Press, New
York, 1974)vol. 1.
55. L. G. Sillén, A. E. Martell, Stability of Metal-Ion Complexes. Special Pub. No. 25 (The Chemical 35
Society, London, 1971).
56. K. Severin, R. Bergs, W. Beck, Bioorganometallic chemistry-transition metal complexes with α-
amino acids and peptides. Angewandte Chemie 37, 1634–1654 (1998).
57. B. W. Fitzsimmons, A. Hume, L. F. Larkworthy, M. H. Turnbull, A. Yavari, The Preparation and
Characterisation of Some Complexes of Iron(II) with Amino Acids. Inorganica Chim Acta 106, 40
109–114 (1985).
58. J. C. Westall, J. L. Zachary, F. M. M. Morel, “MINEQL: A computer program for the calculation of
chemical equilibrium composition of aqueous systems” (Cambridge, 1976).
59. W. D. Schecher, D. McAvoy, MINEQL+: A Chemical Equilibrium Modeling System.
Environmental Research Software 5.0 [Preprint] (1998). 45
60. F. M. M. Morel, A. B. Kustka, Y. Shaked, The role of unchelated Fe in the iron nutrition of
phytoplankton. Limnol Oceanogr 53, 400–404 (2008).
61. J. B. Cotner, W. Makino, B. A. Biddanda, Temperature affects stoichiometry and biochemical
composition of Escherichia coli. Microb Ecol 52, 26–33 (2006).
62. K. G. Wooldridge, P. H. Williams, Iron uptake mechanisms of pathogenic bacteria. FEMS Microbiol 50
Rev 12, 325–348 (1993).
63. C. K. Y. Lau, K. D. Krewulak, H. J. Vogel, Bacterial ferrous iron transport: The Feo system. FEMS
Microbiol Rev 40, 273–298 (2016).
64. C. Völker, D. A. Wolf-Gladrow, A. Gladrow, Physical limits on iron uptake mediated by
siderophores or surface reductases. Mar Chem 65, 227–244 (1999). 55
65. J. Kramer, Ö. Özkaya, R. Kümmerli, Bacterial siderophores in community and host interactions. Nat
Rev Microbiol 18, 152–163 (2020).
.CC-BY-NC-ND 4.0 International licenseavailable under a
(which was not certified by peer review) is the author/funder, who has granted bioRxiv a license to display the preprint in perpetuity. It is made
The copyright holder for this preprintthis version posted January 16, 2025. ; https://doi.org/10.1101/2025.01.15.633289doi: bioRxiv preprint
12
66. O. X. Cordero, L. A. Ventouras, E. F. DeLong, M. F. Polz, Public good dynamics drive evolution of
iron acquisition strategies in natural bacterioplankton populations. Proceedings of the National
Academy of Sciences 109, 20059–20064 (2012).
67. R. Kümmerli, A. S. Griffin, S. A. West, A. Buckling, F. Harrison, Viscous medium promotes
cooperation in the pathogenic bacterium Pseudomonas aeruginosa. Proceedings of the Royal Society 5
B: Biological Sciences 276, 3531–3538 (2009).
68. G. E. Leventhal, M. Ackermann, K. T. Schiessl, Why microbes secrete molecules to modify their
environment: The case of iron-chelating siderophores. J R Soc Interface 16 (2019).
69. R. M. Boiteau, D. R. Mende, N. J. Hawco, M. R. McIlvin, J. N. Fitzsimmons, M. A. Saito, P. N.
Sedwick, E. F. Delong, D. J. Repeta, Siderophore-based microbial adaptations to iron scarcity across 10
the eastern Pacific Ocean. Proceedings of the National Academy of Sciences 113, 14237–14242
(2016).
70. E. L. Rue, K. W. Bruland, Complexation of iron(III) by natural organic ligands in the Central North
Pacific as determined by a new competitive ligand equilibration/adsorptive cathodic stripping
voltammetric method. Mar Chem 50, 117–138 (1995). 15
71. P. W. Boyd, M. J. Ellwood, The biogeochemical cycle of iron in the ocean. Nat Geosci 3, 675–682
(2010).
72. C. S. Hassler, V. Schoemann, C. M. Nichols, E. C. V. Butler, P. W. Boyd, Saccharides enhance iron
bioavailability to southern ocean phytoplankton. Proceedings of the National Academy of Sciences
108, 1076–1081 (2011). 20
73. P. T. Chivers, E. L. Benanti, V. Heil-Chapdelaine, J. S. Iwig, J. L. Rowe, Identification of Ni-(l-
His)2 as a substrate for NikABCDE-dependent nickel uptake in Escherichia coli. Metallomics 4,
1043–1050 (2012).
74. H. Lebrette, E. Borezée-Durant, L. Martin, P. Richaud, E. Boeri Erba, C. Cavazza, Novel insights
into nickel import in Staphylococcus aureus: The positive role of free histidine and structural 25
characterization of a new thiazolidine-type nickel chelator. Metallomics 7, 613–621 (2015).
75. K. D. Fine, C. A. S. Ana, J. L. Porter, J. S. Fordtran, Effect of changing intestinal flow rate on a
measurement of intestinal permeability. Gastroenterology 108, 983–989 (1995).
76. J. Cremer, M. Arnoldini, T. Hwa, Effect of water flow and chemical environment on microbiota
growth and composition in the human colon. Proc Natl Acad Sci U S A 114, 6438–6443 (2017). 30
77. Y. Seyoum, K. Baye, C. Humblot, Iron homeostasis in host and gut bacteria–a complex
interrelationship. Gut Microbes 13, 1–19 (2021).
78. D. J. Sexton, M. Schuster, Nutrient limitation determines the fitness of cheaters in bacterial
siderophore cooperation. Nat Commun 8 (2017).
79. A. E. Shea, V. S. Forsyth, J. A. Stocki, T. J. Mitchell, A. E. Frick-Cheng, S. N. Smith, S. L. Hardy, 35
H. L. T. Mobley, Emerging roles for ABC transporters as virulence factors in uropathogenic
Escherichia coli. Proc Natl Acad Sci U S A 121 (2024).
80. A. Tagliabue, A. R. Bowie, P. W. Boyd, K. N. Buck, K. S. Johnson, M. A. Saito, The integral role
of iron in ocean biogeochemistry. Nature 543, 51–59 (2017).
81. R. G. Keil, D. L. Kirchman, Utilization of dissolved protein and amino acids in the northern 40
Sargasso Sea. Aquatic Microbial Ecology 18, 293–300 (1999).
82. D. L. Kirchman, “The Contribution of Monomers and Other Low-Molecular Weight Compounds to
the Flux of Dissolved Organic Material in Aquatic Ecosystems” in Aquatic Ecosystems (Academic
Press, 2003).
83. R. G. Keil, D. L. Kirchman, Dissolved combined amino acids: Chemical form and utilization by 45
marine bacteria. Limnol Oceanogr 38, 1256–1270 (1993).
84. R. R. Malmstrom, R. P. Kiene, M. T. Cottrell, D. L. Kirchman, Contribution of SAR11 bacteria to
dissolved dimethylsulfoniopropionate and amino acid uptake in the North Atlantic Ocean. Appl
Environ Microbiol 70, 4129–4135 (2004).
85. B. E. Clifton, U. Alcolombri, G. I. Uechi, C. J. Jackson, P. Laurino, The ultra-high affinity transport 50
proteins of ubiquitous marine bacteria. Nature, doi: 10.1038/s41586-024-07924-w (2024).
.CC-BY-NC-ND 4.0 International licenseavailable under a
(which was not certified by peer review) is the author/funder, who has granted bioRxiv a license to display the preprint in perpetuity. It is made
The copyright holder for this preprintthis version posted January 16, 2025. ; https://doi.org/10.1101/2025.01.15.633289doi: bioRxiv preprint
13
Acknowledgments: We thank Martin Ackermann, Julia Vorholt, current and former members of
the Stocker group, and members of the PriME collaboration for their helpful discussions. We are
grateful to Suckjoon Jun for generously providing the NCM3722 strain of E. coli used in this
study. We thank Miriam Lucas from ScopeM for processing samples for SEM and acquiring
SEM images, as well as ScopeM for their support and technical assistance. We also thank 5
Russell Naisbit for his critical reading, which greatly improved this manuscript, and
acknowledge the use of ChatGPT-4o for grammar correction and phrasing enhancements.
Funding:
Gordon and Betty Moore Foundation Symbiosis in Aquatic Systems Initiative Investigator
Award GBMF9197 (RS) 10
Simons Foundation through the Principles of Microbial Ecosystems (PriME) collaboration grant
542395FY22 (RS, TH)
Swiss National Science Foundation grant 205321_207488 (RS)
NSF Postdoctoral Research Fellowships in Biology Program for support under Grant
No.2109890 (JN) 15
Author contributions:
Conceptualization: JLG, RS, MS, JN
Methodology: JLG, RS, MS, JN, UA, ZL
Investigation: JLG, MRM, IS, DMM, SP, JJM
Visualization: JLG, IS, JJM 20
Funding acquisition: RS, MS
Project administration: JLG
Supervision: RS, MS
Writing – original draft: JLG
Writing – review & editing: JLG, JN, JMK, UA, TH, MS, RS, and all other co-authors 25
Competing interests: Authors declare that they have no competing interests.
Data and materials availability: All data and code will be available upon publication.
Supplementary Materials