Abstract
Many motile unicellular organisms have evolved specialized behaviors for detecting and responding to environmental cues such as chemical gradients (chemotaxis) and oxygen gradients (aerotaxis). Magnetotaxis is found in magnetotactic bacteria and it is defined as the passive alignment of these cells to the geomagnetic field along with active swimming. Herein we show that Magnetospirillum magneticum (AMB-1) show a unique set of responses that indicates they sense and respond not only to the direction of magnetic fields by aligning and swimming, but also to changes in the magnetic field or magnetic field gradients. We present data showing that AMB-1 cells exhibit sudden motility reversals when we impose them to local magnetic field gradients. Our system employs permalloy (Ni80Fe20) islands to curve and diverge the magnetic field lines emanating from our custom-designed Helmholtz coils in the vicinity of the islands (creating a drop in the field across the islands). The three distinct movements we have observed as they approach the permalloy islands are: unidirectional, single reverse and double reverse. Our findings indicate that these reverse movements occur in response to magnetic field gradients. In addition, using a permanent magnet we found further evidence that supports this claim. Motile AMB-1 cells swim away from the north and south poles of a permanent magnet when the magnet is positioned less than ∼30 mm from the droplet of cells. All together, these results indicate previously unknown response capabilities arising from the magnetic sensing systems of AMB-1 cells. These responses could enable them to cope with magnetic disturbances that could in turn potentially inhibit their efficient search for nutrients.
Introduction
Diverse organisms can sense and respond to the Earth's magnetic field. This ability is dependent upon the intracellular biomineralization of magnetic particles and the formation of organic compartments or vesicles; this magnetic field sensing behavior can be found in a diversity of organisms (Lowenstam, 1981). For example, Gould et al. (1978) discovered that honeybees contain magnetite localized in their abdomen, and Walcott and colleagues (Walcott, 1977; Walcott et al., 1979) discovered magnetite in the head of homing pigeons. Among other eukaryotic organisms in which magnetite has been experimentally found are fish (Mann et al., 1988; Diebel et al., 2000) and termites (Maher 1998). All of these organisms presumably use this mineral as a ‘compass' to sense magnetic fields when navigating and homing.
Certain unicellular microorganisms such as magnetotactic bacteria (MTB) have the ability to synthesize chains of mineral crystals (Ruder et al., 2012), each of which is enveloped by individual lipid bilayers in organelles known as magnetosomes (Frankel et al., 1979). These magnetosome inclusions render these creatures a model organism to study compartmentalization in prokaryotes (Komeili, 2012), and the formation mechanisms of these structurally organized magnetosomes under genetic control have been elucidated (Komeili et al., 2004, 2006; Scheffel et al., 2006). According to previous studies the proposed mechanisms of the assembly of magnetosomes are: (1) the magnetosome compartment invaginates from the inner cell membrane (Komeili et al., 2004); (2) individual magnetosomes are recruited to the actin-like protein, MamK (Komeili et al., 2006; Katzmann et al., 2010) (providing a structural scaffold), where an acidic protein, MamJ (Scheffel et al., 2006), (running along the cell, from pole to pole), attaches them to this cytoskeleton filaments in a beads-on-a-string manner; (3) ferric ions are chelated by siderophores and transported into these cells; and (4) magnetite crystallization ensues within the nucleated vesicles. There is a plethora of information about magnetosomes and the proteins involved in their formation processes. However, there is no study showing evidence of the ability of magnetotactic bacteria to cope with magnetic disturbances or fluctuations (that is, gradients) in their surrounding environments that can misguide them, pull them and inhibit their efficient search for nutrients. Investigation of the swimming behavior in the presence of magnetic field gradients could shed light on a possible defense mechanism that these organisms could have adopted under physiological stress in their natural environment or in the laboratory setting to impart a protection against self-magnetics. In this paper, we have found sudden motility reversals (Figure 1a) exhibited by the Magnetospirillum magneticum (AMB-1) that are related to magnetic field gradients. We proposed that these organisms may utilize these reversals to respond to magnetic disturbances.
Materials and methods
Helmholtz coils
In order to examine the interaction of AMB-1 cells, we custom built a pair of Helmholtz coils that produced an area with a uniform magnetic field (González et al., 2014) . This system consisted of two identical coils separated by the radius of the coils. The radius of the coil was 4.5 inch and the gauge of the magnet wire used was 22 AWG. For this pair of Helmholtz coils, there were 400 turns in each coil, and the windings were stacked in 7 layers. For the U-turn experiments, we used another larger pair of Helmholtz coils with a radius of 13 inch with 150 turns in each coil and the magnet wire gage used was 18 AWG. An Arduino Uno microcontroller was used to rapidly alternate the stimulation between the two coils to do the U-turn experiments. A circuit with a transistor (TIP102) and diode (1N4004) was built to protect the electrical circuitry of the Arduino microcontroller as the maximum current the Arduino can take is ∼30 mA and we needed over 0.1 Å to drive the coils. In the circuitry, we included light-emitting diodes (LEDs) to indicate which coils were operating at each time (Supplementary Figure S1 shows the coil arrangement and the circuit used to control both coils).
Permalloy island fabrication
Permalloy islands (Figures 1b and c) were fabricated and then magnetized using the previously described Helmholtz coils. To visualize the interaction of the AMB-1 cells with these islands, we used a × 63 objective on a modified inverted microscope (Zeiss Anxiovert 200, Göttingen, Germany). The permalloy islands and the microscope slide thickness was <170 μm for visualization. To make the permalloy island master mold, we used an image reversal fabrication process (Long and Newman, 1984). The ensuing master was used as the mold to deposit the metal. In order for the layer of permalloy to be optically transparent, the thickness of the metal needed to be <30 nm. A 25 Å layer of tantalum and a 250 Å thick layer of NiFe were subsequently deposited onto the master mold. The islands were rinsed in fresh acetone and isopropyl alcohol. Detailed information about the set-up and the fabrication of these islands can be found in the study of González et al. (2014).
Analysis of the reversal behavior and direction of swimming
To track the bacteria, we used a MATLAB code written by Wauthier (Wauthier, 2011). The code subtracts the background by determining the most frequent values of a pixel and it tracks the objects by gathering information from different frames using a Kalman filter. After running the run_tracker.m script, we used the extract_trajectories.m script to extract information such as the frame at which the cells were first and last observed, the position and the length of the trajectories and so on. This information was stored in structure (or struct) arrays. Using the MATLAB dot operator, these data were assessed. We used this information and wrote a MATLAB script to determine whether the cells were reversing and to determine the direction the cells were swimming (see script in the Supplementary Information).
Results
Reversal behaviors because of the magnetic islands
Magnetotactic bacteria use their intracellular magnetic chains to align their movement to magnetic field lines, but the ability of these bacteria to switch directions in response to local magnetic field gradients has not been explored. Sudden motility reversals in axial magnetotactic bacteria have been previously observed in response to oxygen gradients in a mechanism known as magneto-aerotaxis, because it is a ‘magnetically assisted aerotaxis' (Frankel et al., 1997). In this study, we imposed sharp concentrated magnetic field gradients using thin film permalloy (Ni80Fe20) island (∼30 nm in height) to concentrate magnetic fields generated through our custom-designed Helmholtz coils that produced a uniform magnetic field (González et al., 2014). We exposed AMB-1 cells to magnetic field gradients as they approached and crossed the star-shaped islands. They experienced a change in the magnetic field from high to low and back to high again. The bacteria were observed to exhibit three distinct behavior modes, unidirectional movement (UM), single-reverse movement (SRM) and double-reverse movement (DRM), as shown in Figure 1a. The UM mode was characterized by continued, straight-line movement with only very slight deviations from the straight path in one direction as the AMB-1 cells moved toward and then across the patterned islands. This group of the AMB-1 cells responded with a UM mode and their movement was not affected by magnetic field gradients. However, another group of the bacteria exhibited a SRM mode, completely reversing their direction of motion as they reached the permalloy island and the associated magnetic field gradients (Figure 1b and Supplementary Movie S1). Other AMB-1 cells exhibited a DRM mode, in which the bacteria switched directions once in the vicinity of the islands, moving in the opposite direction for a short distance and then switching directions a second time to continue in their original direction (Figure 1b and Supplementary Movie S2). A very small fraction of AMB-1 cells exhibited multiple reversals in sequence. These different reversals suggest these bacteria were detecting changes in the magnetic field or the magnetic field gradient.
Using the magnetic islands to create magnetic field gradients, we observed an unprecedented correlation between the magnetic field gradient and the reversing behavior in AMB-1 cells. The number of reversals (SRM and DRM) in the vicinity of the star-shaped island (Figure 2a) increased as we actuated the external field (from Helmholtz coils) from 0 to ∼13 mT. As an important control, we examined the motion of the bacteria when increasing the magnetic field, with no magnetic island present. The bacteria reversed only ∼6% of the time under this condition. At higher fields, 13 mT, 42% of the AMB-1 cells exhibited the DRM or SRM motility mode, with 22% and 20% exhibiting the DRM and the SRM mode, respectively. The higher number of reversals at higher fields was noted to correspond to the location where the magnetic field varied significantly with position (that is, the region with a high magnetic field gradient) (Figures 2b and c; see Supplementary Information for MATLAB script for analysis and quantification of the reversals).
We modeled the magnetic field using the finite element method package called FEMM (Finite Element Method Magnetics; see the Supplementary Information for details). At low fields, lower gradients were found (∼3 mT case; Figure 2c), whereas at higher fields, higher gradients were present (∼13 mT case; Figure 2c). We also examined the region in the vertical direction further away from the island's top tip (shown in Figure 2c with dashed lines in the 3 mT case), which indicated the gradient decreased and the field became more uniform across the island (Figure 2c). It is interesting to note the degree of extension of the magnetic field lobes (showed the contour along which the magnetic field suddenly changes between the different regions) at different field magnitudes as shown in Figure 2c (simulation results). The higher the magnetic field was, the larger the area covered by these lobes. More interesting was the comparison of the 13 mT case with Figure 2b (we plotted the first reversals for the 13 mT case). In Figure 2b, there was an empty region where fewer SRM reversals were observed. This region resembled one of the lobes in the simulation where the magnetic field changed abruptly. We also determined the distribution of AMB-1 cells that exhibited different modes with respect to the speed of the bacteria. The reversing behavior was most often found among AMB-1 cells moving at 0–20 μm s−1 and less frequently for AMB-1 cells moving at higher speeds (see Supplementary Figure S2 in the Supplementary Information). Through simulation of the magnetic islands and comparison with experimental results, we reasoned that the motility reversals must be because of magnetic field gradients.
Swimming patterns of AMB-1 cells because of a permanent magnet
From the observation of the data collected with the magnetic islands and the Helmholtz coils, we speculated that the reversals were because of the magnetic field gradients. To further test our hypothesis, we reasoned that if the reversals are because of the magnetic field gradients then when using a permanent magnet with gradients throughout a larger surface area (that is, a global field), we should expect more reversals in comparison with that of the localized changes as it was in the case of the islands. To address this, we performed experiments using a permanent magnet and recorded whether the cells were swimming to the right or to the left assuming that they would be reversing near the edge as the magnet moved away from the cells (see Figure 3a for a schematic). We characterized the magnetic field gradient produced by the permanent magnet with respect to distance using a gaussmeter (Figure 3b) that was determined from the magnetic field versus distance plot shown in the inset of Figure 3b. We first determined the polarity of an iron permanent magnet (that is, which side of the magnet was north and south) using a compass and then recorded the percentage of the cells swimming away from the north (Figure 3c and Supplementary Movie S3; see Supplementary Table S1 for statistical analysis) and south faces (Figure 3d and Supplementary Movie S4; see Supplementary Table S2 for statistical analysis) of the magnet as we retracted the magnet from the droplet of cells. We imaged the cells at the center of the droplet and found that at 5 and 10 mm, ∼70% of the cells were persistently swimming away from the magnet. This occurred when the north and south faces of the magnet were facing the droplet. At distances of >30 mm, the percentage of cells swimming away from the magnet decreased. This location corresponded to a gradient of ∼0.2 T m−1 (tesla per meter), whereas for the case of the magnetic island, we observed a higher magnetic field gradient of ∼7 T m−1. This suggests that closer to the island the cells experience larger gradients resulting in a direct visualization of the reversals. One point noted is that the 7 T m−1 gradients (at ∼15mm from the island) could be beyond the threshold and a 0.2 T m−1 gradient is close to the threshold that induces this behavior.
Alignment of the bacteria to the Helmholtz coils
In the absence of an external magnetic field, the AMB-1 cells showed no preferred direction of movement in the field of view (Figures 4a and b and Supplementary Movie S5). Upon application of a uniform magnetic field (∼1 mT), the bacteria aligned to the direction of the magnetic field. This alignment alteration was likely because of a force-induced torque that caused the bacteria to rotate (Figures 4a and c and Supplementary Movie S6). In addition, when we increased the magnetic field from 0 to 1.6 mT, the fraction of bacteria aligning their movement to the direction of the magnetic field increased from 0 to ∼90% (Figure 4d). Above 1.1 mT, the fraction of bacteria aligning to the magnetic field did not increase further. In this case, the threshold at ∼1.1 mT may induce a force sufficiently strong so that all of the bacteria can no longer overcome an applied torque on the magnetosome chain (Supplementary Figure S3 shows the transmission electron microscopy images and analysis). The variation in the number of particles within each cell could account for the difference in alignment of the cells to the external magnetic field.
U-turn versus reversals
Comparing the reversal behaviors with that of the U-turn was important to clearly differentiate between the two movements. Previous work has documented U-turn motion (Esquivel and Lins De Barros, 1986) observed when subjecting magnetotactic bacteria to a reversing magnetic field (Frankel, 2003). Our reported reversing behavior in the presence of the induced local magnetic field gradients is very different from these U-turn responses. To examine this further, we built on previous work that analyzed time to reverse, τ, and U-turn width, W, for spirillum organisms (see Supplementary Information). Similar expressions have been developed for a coccus organism (Esquivel and Lins De Barros, 1986) and nonspherical magnetotactic bacteria (Bahaj et al., 1996). These papers predicted that for an AMB-1 cell to make a U-turn that is ∼10 μm in width with an applied field of ∼1 mT, the time to make the U-turn is τ∼0.5 s. We first confirmed these predictions through experiments in which we completely reversed the field and measured the time it took for the bacteria to make a U-turn (Supplementary Figure S4 and Supplementary Movie S7). In contrast, our findings (Figure 1) showed that in the vicinity of high magnetic field gradients, the AMB-1 cells reversed without turning around, suggesting a different mechanism. To reverse direction, the bacteria can change the propulsion from the flagellum on one end of its body to the flagellum on the opposite end (Krieg, 1976; Thar and Fenchel, 2005).
Discussion
Alignment to an external magnetic field
The uniformity of magnetic fields is important when studying magnetotactic bacteria. It is worthwhile to reiterate that Helmholtz coils provide a uniform magnetic field and the introduction of a magnetic material in the pool of these magnetic field lines causes them to warp and penetrate or permeate the magnetic materials such as the permalloy islands. However, a permanent magnet found in nature always produces a magnetic field gradient. Others have observed similar reversal behaviors with different magnetotactic organisms under different conditions. For example, Greenberg reported ‘ping-pong' movements associated with magnetotactic multicellular organisms (Greenberg et al., 2005). Erglis et al. (2007) also observed a ‘back and forth' motion when studying the dynamics of Magnetospirillum gryphiswaldense in a rotating uniform magnetic field. An early study by Spormann and Wolfe (1984) called a observed reversal behavior ‘tactile behavior,' and they demonstrated the maintenance of a band of cells while aligning the cells with a magnet. These results have similar components to our findings with the permanent magnet as at a certain distance, the cells start swimming to the left and to the right at about equal number. Frankel et al. (1997) showed that axial magnetotactic bacteria use the magnetic field lines as an axis and occasionally switch direction as they swim, and they concluded that these bacteria use a temporal sensory mechanism sampling the media and swimming up an oxygen gradient that they called two-way swimming. All of the studies mentioned above used various types of fields from rotating fields to uniform to permanent magnets. The type and nature of the magnetic field applied while doing experiments with MTB is crucial to correctly determine the effect of other environmental cues as these cells sense magnetic field gradients as demonstrated in this study.
Evolutionary implication and the ecology
In the literature, it is hypothesized that magnetosomes impart MTB with an advantage in finding favorable environments in an efficient matter by using a simple route for obtaining nutrients rather than the more widely used, well-known and random walks employed by some other organisms such as Escherichia coli (Berg, 1993). MTBs in the Northern Hemisphere and Southern Hemisphere predominantly swim toward the north and south, respectively (Blakemore, 1975; Blakemore et al., 1980), that helps the cells to swim in a roughly vertical pathway downward toward the oxygen-depleted region near the sediments. However, these observations did not explain the benefit of alignment and the predominance of magnetotactic bacteria in the oxic–anoxic transition zone, which forms from an inverse double gradient of oxygen (O2) from above and sulfide (S2−) from below. This zone is scant in oxygen and sulfide concentrations (Simmons et al., 2004). Moreover, south-seeking cells were once found in the Northern Hemisphere (Simmons et al., 2006), conflicting with previous studies. Our study attempts to explain these discrepancies and indicates that determining the uniformity of the magnetic field is extremely important before drawing conclusions as MTB may respond to magnetic field gradients. The magneto-aerotaxis theory emerged to explain the predominance of MTB in the oxic–anoxic transition zone. The theory suggests that these organisms swim to find comfortable oxygen gradient using the Earth's magnetic field as an axis as in a ‘magnetically assisted aerotaxis' (Frankel et al., 1997). The magneto-aerotaxis theory provides a more reasonable explanation, but the system could be more complex than this as these organisms may be sensing magnetic field gradients.
Despite all of the studies involving MTB organisms, the sensing mechanism and the connection of the magnetosome structures to the flagella motor are largely unknown. One possible aspect of this unknown magnetosome–flagella system is a possible mechanism developed by these organisms to cope with self-magnetics against magnetic fluctuations in their environments. For example, if a MTB is in the vicinity of a large volume of magnetite, it could be immobilized because of its magnetic body. There is a report on the dynamics of the MTB populations found in chemically stratified water column presumably because of water column chemistry that moves the oxic–anoxic transition zone throughout the seasons, and at some point it gets much closer to the sediments (Simmons et al., 2007). Taking this into account along with the abundance of MTB and the accumulation and preservation of these in the sediments, termed magnetofossils, Kopp and Kirschvink (2008) could indicate an important role in the selection of bacteria with the ability to keep a distance from magnetic sediments that could immobilize them. The disintegration of the organic constituents is likely occurring and the sediments could contain clumps and agglomeration of magnetic specimens (Simmons et al., 2007; Kopp and Kirschvink, 2008). This may present a threat to these organisms. In addition, studies have shown the preservation of magnetofossils with only minimal extensive dissolution effect of Deep Sea Drilling Projects (Vali and Kirschvink, 1989), which aids in the conservation of the magnetic properties.
Furthermore, during the Paleocene–Eocene Thermal Maximum time interval, with abundant bacterial magnetofossils, Schumann et al. (2008) found a giant spearhead-like shape up to 4 μm long and that most likely derived from eukaryotes (because of their large size). Magnetofossils usually appear in aggregates of several dozen particles (Petersen et al., 1986; Stolz et al., 1986), increasing the volume of the magnetic material and thus the magnetic field emanating from these species. These kinds of magnetofossils could contribute to the development of MTB mechanism to cope with self-magnetics and to dodge magnetic attractive forces by swimming away from magnetic debris. For these cells, having a magnetic body could be a burden under the presence of any magnetic material. The AMB-1 cells could be displaying this intrinsic property through the abrupt changes in direction previously observed.
MCP and the flagella motor
In addition, the reversal behaviors could involved a more complex magnetoreception mechanism (Kirschvink et al., 2001). For example, this microorganism has a significant number of expressed methyl-accepting chemotaxis proteins (MCPs) (Fukuda et al., 2006) that are not thoroughly understood in terms of their interactions with the magnetosome chain. Philippe and Wu (2010) suggested a chemotaxis-like magnetotaxis model that may be related to the switching behavior observed in this study. MCP Amb0994 is one of the two MCPs found within the magnetosome island (MAI) that harbors proteins known to be involved in magnetosome formation and biomineralization (Murat et al., 2010). The theory is that the magnetosome chain could be affected by MCP Amb0994, but the mechanism has yet to be elucidated. In this model, when a magnetic torque is imposed on the MamK, which is a cytoskeleton protein involved in giving the magnetosome chain its structural scaffold (Komeili et al., 2006; Pradel et al., 2006; Scheffel et al., 2006), it presumably interacts with a MCP, Amb0994 (which lacks a periplasmic sensing domain; presumably receiving an internal signal) (Philippe and Wu, 2010). This MCP protein in turn could be relaying a signal to the flagella motor switch protein, FliM, through an unknown mechanism or through a CheA–CheY signal transduction system (Falke and Hazelbauer, 2001; West and Stock, 2001; Victor, 2004, Wadhams and Armitage, 2004), presumably slowing down the bacteria. The bacteria showing SRM and DRM are slower than the ones showing UM, and protein Amb0994 and other associate genes (Greene et al., 2012) could be responsible for these reversals as this protein localizes at the poles near the flagella motor. Amb0994 could be implicated in the sudden reversal behavior responses that we have observed in AMB-1 cells in the presence of magnetic field gradients.
Temporal versus spatial sensing in AMB-1 cells
Cells detect gradients through two types of mechanisms: temporal and spatial. It is widely known that small bacteria usually employ a temporal sensing mechanism to sense changes in the environment by sampling the concentration and integrating the signal over time because of the limitation in their size (Macnab and Koshland, 1972). However, bacteria can also employ a spatial sensing mechanism (Dusenbery, 1998; Thar and Kühl, 2003; Hu et al., 2010; Lower et al., 2010). In a spatial detection mechanism, a cell compares the difference between different receptors and instantly makes a decision based on these various inputs. We propose the AMB-1 cells perform reversals by employing a spatial detection mechanism to instantly sense magnetic field gradients. This could be best explained through changes in the curvature of the field lines as shown in Figure 5. Hu et al. (2010) argue that receptor coupling can improve sensing of a gradient in bacteria by spatial sensing. In addition, Dusenbery (1998) argues that when steep gradients occur, spatial sensing is favorable over temporal sensing. The changing magnetic fields can exert a bending force on the magnetosome chains (Figure 5) that can be in turn transferred through a coupling protein. The MamK could be acting as a coupling protein as it forms long filaments along the length of the cells body between the two cell poles of the AMB-1 cells. MamK could be interacting with MCP Amb0994 at the poles to allow a fast relay of the magnetic signal between the head and the tail and establish a communication between the two flagella motors. The Helmholtz coils produce straight lines and as these approach the islands they tend to bend toward the island (as shown in the simulation of Figure 2). These bending of the field lines could be causing the cells to sense different curvature of the field lines at the head and at the tail of their long bodies. This difference in the field could be torqueing the cells and relaying this signal to the MCP Amb0994. This could be related to the sensing of magnetic field line angles proposed by Zhu et al. (2014) as they proposed a similar model.
Conclusions
In this study, we found that AMB-1 cells posses the ability to sense magnetic field gradients and respond to them by reversing direction. We investigated this sensing capability by exposing the AMB-1 cells to magnetic field gradients from magnetic islands and Helmholtz coils. Motile AMB-1 cells swim away from the north and south poles of a permanent magnet, which also indicate sensing of magnetic field gradients. Our results indicate that the magnetic field sensing mechanisms of these organisms may be even more sophisticated than previously realized, and the system provides these AMB-1 cells a pivotal capability that we call protection against self-magnetics.
Acknowledgments
We acknowledge Joseph Suhan for his help in acquiring TEM images. We also thank Sara Majetich for her valuable discussion about the manuscript. This work was supported in part by the Office of Naval Research (N000140910215), the Sloan Foundation, the Air Force Office of Scientific Research (FA9550-13-1-01-08) as well as a National Science Foundation Graduate Research Fellowship under Grant No. 0946825 to LMG. In addition, we want to acknowledge the National Science Foundation with Grant No. CMMI-1100430, CMMI-1160840 and CPS-1135850.
The authors declare no conflict of interest.
Footnotes
Supplementary Information accompanies this paper on The ISME Journal website (http://www.nature.com/ismej)
Supplementary Material
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