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Center for Nonlinear Dynamics and Department of Physics, The University of Texas, Austin, Texas 78712
Correspondence: Address reprint requests to Anna L. Lin, E-mail: alin{at}phy.duke.edu.
| ABSTRACT |
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| INTRODUCTION |
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Our work is motivated by recent theoretical studies of the Fisher equation, which was generalized to model growth in an inhomogeneous environment under the influence of a convective flow. Those studies indicated a transition from localized populations to delocalized populations that grow everywhere (Nelson and Shnerb, 1998
; Dahmen et al., 2000
; Shnerb, 2001
). Experiments have also been conducted on growth in inhomogeneous environments, but the conditions were too complex to compare with the model studies (Neicu et al., 2000
; Shnerb, 2001
).
We have developed an experimental system for studying bacterial growth in an inhomogeneous environment. Escherichia coli bacteria grow in a long, thin channel with different growth conditions in a small section of it. The position of this different growth region changes in time. We measure the bacterial concentration as a function of space and time in experiments that typically last one week, which is long compared to the half-hour doubling time for the bacteria. The quasi one-dimensional geometry permits comparison with simple one-dimensional models.
The spreading of bacterial colonies measured for certain homogeneous conditions (Shapiro and Dworkin, 1997
; Matsushita et al., 1998
) in a petri dish has been found to be described by the Fisher equation (Fisher, 1937
; Murray, 1989
), which has traveling front solutions that propagate with a velocity
F = 2(Da)1/2, where a and D are, respectively, the growth rate and diffusion coefficient of the bacteria (Shapiro and Dworkin, 1997
; Berg and Purcell, 1977
; Ben-Jacob et al., 1994
). Nelson and co-workers (Nelson and Shnerb, 1998
; Dahmen et al., 2000
) proposed a generalization of the Fisher equation to describe the growth of bacteria in an environment with a localized region of favorable growth conditions (an "oasis") that moves with a constant velocity
:
![]() | (1) |
W/2) is U(x
t) = a, and in the surrounding "desert" (|x| > W/2) the growth rate is U(x
t) =
a, where W is the width of the oasis in a system of length L, as shown in Fig. 1 a. The average growth rate over the full length of the system is
![]() | (2) |
and the average terrain (Eq. 2). Numerical simulations (Dahmen et al., 2000
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exceeding a critical value
c and sufficiently harsh terrains (i.e., for
sufficiently negative), life is not sustainable and the population becomes extinct, approaching zero concentration everywhere.
For |
| <
c, there is a range of values of the terrain
for which the population remains localized, growing in the oasis while decaying exponentially with distance from the oasis. An example of such a localized state is pictured in Fig. 1 b. The population is sustained in the moving oasis but dies out in the desert.
Finally, for a sufficiently rich terrain, the population grows everywhere, for any value of the oasis velocity
. No matter how the population is initially distributed throughout the length of the system, the population becomes delocalized.
The identification of the distinct sustainable localized, delocalized, and extinct states, and the suggestion that there could be well-defined transitions among them, originally resulted from an analysis of a linearized version of Eq. 1, which disregards the biologically important saturation term (Nelson and Shnerb, 1998
; Dahmen et al., 2000
). Transitions between the different regimes can be understood only by including the nonlinear saturation term. We have performed numerical simulations of the full nonlinear equation to compare with the laboratory observations and to study the transitions among the localized, delocalized, and extinct states.
| METHODS |
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The species selected for this study was E. coli RW 120 because, for these bacteria, UV exposure results in cell death rather than mutation (the two mechanisms for repair of DNA are switched off) (Ho et al., 1993
). Thus, as in the model, the population dies out in the desert if it is sufficiently harsh.
The rectangular channel was filled before each experimental run with a define media in a 0.2% agar gel maintained at 37°C; this nutrient level supported steady bacterial growth for at least 1 week. The purpose of the gel was to inhibit uncontrolled convection while allowing diffusion of the bacteria. A 120 cm long mercury lamp positioned 8.5 cm above the cell provided 10 W/m2 UV illumination for the region not shielded by the mask.
Each run was initiated by dragging a needle that had been dipped into bacteria across the gel surface underneath the mask, thus infecting only the oasis region. We waited several hours for the bacteria to reach a saturated concentration cs = a/b in the oasis before starting to move the oasis with a constant velocity
, as in Fig. 1 b. Runs were made for oasis velocities ranging from 1.5 x 105 cm/s, where the oasis moved only 13 cm in an experiment lasting 10 days, to 3.6 x 104 cm/s, where the oasis traversed the 25 cm cell length in 19 h. At high oasis velocities, the original population could not keep up with the moving oasis, and the population decreased and became extinct; we continued to monitor the decline in the original population for several days after the oasis reached the end of the cell. During a weeklong experiment, most of the live bacteria remained close to the (oxygenated) air-gel interface, whereas dead bacteria sunk to the bottom of the channel in
2 days.
The bacterial concentration near the gel surface was determined by measuring the transmission of light through the thin dimension of the cell. The light source was a 4.5 mW diode laser with a 670 nm wavelength and a 1 mm beam diameter. The light source and a detector were mounted on a translation stage with the center of the beam passing through the gel 1 mm below its surface. Each spatial scan of the bacterial concentration took 7 min, a time short compared to the time for the concentration to change significantly; thus the measurements yielded c(x, t) at all positions x and times t for the duration of an experiment (310 days).
Experimental determination of the model parameters
We have measured the parameters in the model: the growth rate a of E. coli in 0.2% agar define media, the growth attenuation coefficient
of the UV light, the diffusion constant D, and the saturation constant b.
The growth rate of RW 120 was determined using a standard dilution plating technique (Runyen-Janecky, 2001, private communication) in which the number of bacteria per unit volume was counted every half hour. The measurements, shown in Fig. 2, yielded a = 4 x 104 s1.
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, we measured the bacterial death rate caused by the UV light and found
= 28; hence
We chose this strong illumination intensity for a first exploration of the experimental phenomena to have good signal/noise. Future studies should develop instrumentation with improved signal/noise to study the interesting behavior of the model for an average terrain near zero. However, even with improved signal/noise, it will not be possible in practice to make extensive explorations of the parameters because of the long timescales of the phenomena.
The diffusion constant D was determined from measurement of the radially averaged front velocity
F of a colony growing in 0.2% agar under homogeneous conditions in a petri dish, assuming that
(Murray, 1993
; van Saarloos, 1987
, 1988
). For bacteria growing in a petri dish with 0.2% agar in define media, we measured
F = 2.4 x 104 cm/s. This result together with the measured value of a yields D = 7 x 105 cm2/s.
A steady-state concentration cs was achieved with point inoculation of bacteria in the oasis and no incubation period for
/
F << 1. A value for the saturation parameter b, 7.93 x 1011 cm/s, was determined from the relationship b = a/cs.
We also conducted some measurements in 0.1% agar Luria Broth media where a and D were larger. These measurements yielded a = 6 x 104 s1,
F = 4.4 x 104 cm/s, and D = 1.6 x 104 cm2/s.
Simulation
We numerically integrated Eq. 1 using the parameter values given in the previous section, except for
, which was scanned over a range of values in the simulations (see Fig. 5). The value of
F used in the simulations was typically
F = 3.38 x 104 cm/s, the average of the values measured in the two different growth media. In the simulation, space was discretized using the method described in Dahmen et al. (2000)
and Franosch and Nelson (2000)
. The resulting N-coupled ordinary differential equations (where the number of grid points N was typically 2032) were integrated in time from an initial condition of a Gaussian concentration profile with 10% noise centered in the favorable growth region (Mann, 2001
). An alternative initial condition, a spatially uniform concentration with the saturation value a/b, also with 10% noise, yielded the same behavior at long times. Both periodic and reflective boundary conditions were found to yield extinct and localized solutions, whereas delocalized solutions were found only with periodic boundary conditions.
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| OBSERVATION OF LOCALIZATION AND EXTINCTION |
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of the oasis. The observations are compared with the numerical simulations in Fig. 3: for large
, the population becomes extinct (left column) and for small
a sustained localized population develops (right column); the figure also shows an example of an intermediate value of
, where the population slowly becomes extinct (middle column). The model captures the observed qualitative dependence on
.
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In the case shown in Fig. 3 a, the bacteria inoculated in the oasis were first allowed to grow for 13 h with the oasis at rest before it began to move at 3.6 x 104 cm/s. The bacteria did not diffuse and grow fast enough to maintain a population within the moving oasis, and the original bacterial colony that was left behind became fully exposed to UV light. The bacteria then died and slowly sunk to the bottom of the channel, out of the field of the measurement of concentration; at 73 h some (presumably dead) bacteria were still present, but the population was declining toward zero. The waviness in the concentration profile is due to the inhomogeneous inoculation of the gel (see t = 3 h).
The development of stable localized populations in a moving oasis is illustrated in the column on the right of Fig. 3. The bacterial colony moves in the same direction as the oasis motion, and at least part of the colony remains in the oasis; bacteria that are left behind in the desert eventually die.
The spatiotemporal behavior of the colony under conditions close to the extinction-localization transition is shown in the middle column of Fig. 3. Close to this transition we observe in the experiment a double-peaked oscillating front, as can be seen in Fig. 4. These oscillations persist for many generations. The parameters in the simulations of the model Eq. 1 have been varied widely, but no oscillations have been found.
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and
/
F. The simulations revealed not only the three distinct states but also information on the transitions among these states: extinction-localization, extinction-delocalization, and localization-delocalization, as shown in Fig. 5. The phase diagram is plotted in parameter ranges near the transitions, whereas the experiments were run at
off the plot. Simulations conducted using experimental parameters show that the phase diagram for those values can be extrapolated from Fig. 5.
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/
F changed in steps as small as 0.0001 and
changed in steps as small as 0.0005. These studies showed that each transition was continuous, as Fig. 6 illustrates. In addition, scans were made for both increasing and decreasing values of the control parameters, and the results were found to be independent of the direction in which the control parameter changed; this absence of hysteresis provides further evidence that the transitions are continuous.
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could be determined for each set of control parameters. These times became very long as a transition was approached, indicating the critical slowing down that is characteristic of supercritical bifurcations (Cross and Hohenberg, 1993
For
large enough, the average terrain experienced by each bacterium was sufficient to support life everywhere; the population, initially limited to the oasis, became delocalized. However, the population remained larger in the oasis region, as Fig. 7 illustrates for a range of increasing oasis velocities.
| DISCUSSION |
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Our study has concerned bacterial populations that initially grew in a stationary oasis that lay within a desert; then the oasis was made to move with a constant velocity. We found that the population could be sustained or could die out, depending on the oasis velocity and the average terrain, which depended on harshness of the desert and the size of the oasis relative to the size of the desert. Results from our numerical simulations of Eq. 1 are in qualitative accord with the laboratory observations, although the model fails to capture the observed double-peaked oscillations found for the spatial distribution of bacteria in the moving oasis. An alternative model might include (in addition to diffusion, convection, and growth) the internal dynamics of various gene expression networks within individual bacteria. Such a model could produce oscillations as the protein levels change in response to environmental stresses. Temporal oscillations of various proteins within cells have been demonstrated in E. coli (Elowitz and Leibler, 2000
). Similar temporal oscillations have been captured in a minimal model based on activator-repressor dynamics (Vilar et al., 2002
).
The analysis of the linearized equations by Dahmen et al. (2000)
revealed a transition between delocalized and mixed steady states for
c = 0.92
F, whereas our numerical analysis of the full nonlinear equations, conducted in the range of biologically relevant parameters, yielded only sustained delocalized states, i.e., nonzero concentration everywhere (see Mann, 2001
).
In conclusion, our numerical simulations of the model yield deeper insights into the mechanisms governing the colony behavior than could be obtained from the experiments alone. In particular, the simulations showed that the transitions between the different states were continuous and nonhysteretic. Further, the simulations yielded a delocalized state, where the bacterial population grew throughout the entire system; this state was not accessible in the experiments.
| ACKNOWLEDGEMENTS |
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This work was supported by the Engineering Research Program of the Office of Basic Energy Sciences of the Department of Energy and the Robert A. Welch Foundation (A.L.L., B.A.M., and H.L.S.), and by the National Institutes of Health and the National Science Foundation (G.T., B.L., and J.K.).
| FOOTNOTES |
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Submitted on October 9, 2003; accepted for publication March 15, 2004.
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