INTRODUCTION
In the pelagic ocean, bacterial chemotaxis is considered an important selective advantage to compete for microscale nutrient patches, including marine snow and living organisms (
11). Surfaces of phytoplankton cells represent microenvironments supplying bacteria with essential nutrients and sites for attachment, which greatly increase their capabilities to successfully compete with other microorganisms (
7). Chemotaxis might initiate the interaction of bacterial cells with the phytoplankton organism, as it has been postulated for the paradigm of the so-called phycosphere (
9). Indeed, attraction of marine bacteria to microalgae or their exudates and further bacterial utilization of attracting compounds have been predicted or demonstrated in previous studies (
8,
11,
20,
44,
53,
54,
61). Besides the bacterial growth-promoting effect of phytoplankton exudates, bacteria in turn may support algal growth and reproduction by, e.g., remineralization of nutrients (
15,
44).
Interactions of marine algae and bacteria may be envisioned to be by one of four major types: mutualism, parasitism, commensalism, or competition (
25). These interactions are likely to be transient and highly dependent on micro- and macroecological environmental conditions. Different interaction types may exist simultaneously, and the balance between stimulatory and inhibitory effects ultimately determines the survival of particular organisms (
15). The specific mechanisms by which those organisms interact and how factors such as motility or chemotaxis impact the fate of an interaction are largely unknown. Only a few previous studies have approached this topic by investigating specific interaction pathways. Two of those addressing bacterium-dinoflagellate interactions proposed that bacterial siderophore production may stimulate algal growth in a symbiotic manner (
4,
5). Further, the algicidal activity of a
Pseudoalteromonas sp. strain was suspected to be due to an extracellular serine protease produced by this bacterium (
37). Additionally, bioactive polyunsaturated aldehydes produced by several marine phytoplankton organisms were shown to inhibit the growth of some bacterial strains but to stimulate that of others (
48). A detailed biochemical mechanism for the interaction of
Emiliania huxleyi with a
Roseobacter clade organism,
Phaeobacter gallaeciensis, was demonstrated by elicitation of roseobacticide production via algal aging-derived lignin breakdown products (
51,
52). Those studies not only demonstrated the delicate balance between a symbiotic and parasitic interaction but also prompted the question of how interaction signals are perceived and transduced in either organism.
Despite the individual type of interaction, physical proximity and thus motility are thought to be prerequisites for cellular interactions in aquatic systems (
26). Two independent types of bacterial motility were generally described for the model organism
Pseudomonas aeruginosa, and these are also found in numerous other bacteria and have been shown to be regulated by distinct proteins encoded by different chemotaxis gene clusters (
10,
16–18,
21,
32,
60). Bacterial flagellar movement is controlled via a methylation-dependent histidine-aspartate phosphorelay multienzyme
che system (
59). In contrast, twitching motility describes the bacterial movement on surfaces performed with the help of type IV pili (
29) and mediated by the
chp chemosensory system (
10,
60), which controls the motor complex of the pili, causing extension and retraction of these cellular appendages. In
P. aeruginosa, one of the five described chemotaxis gene clusters, namely, that comprised of the
chp genes, is exclusively responsible for pilus chemotaxis (
10,
16–18,
50,
60). In the present study, we investigated the chemotaxis gene clusters of
Marinobacter adhaerens and the functions of certain individual chemotaxis genes by mutational analysis. This study describes the chemotaxis of a
Marinobacter strain for the first time.
To understand the actual mechanisms by which diatom cells and bacteria interact and influence marine aggregate formation, a bilateral model system was established (
22,
23,
31,
57). The bacterial strain
M. adhaerens HP15 was demonstrated to attach to the diatom
Thalassiosira weissflogii and to induce formation of transparent exopolymeric particles (TEPs) and aggregates in cocultures. Since the bacterium is genetically accessible (
57), specific mechanisms of the interaction can now be studied on a molecular basis. Herein, we describe the chemotactic behavior of
M. adhaerens toward the diatom
T. weissflogii using functional knockouts of the genes coding for central histidine kinases and methyltransferases of two chemotaxis signaling cascades. Thereby, we aim to evaluate the importance of bacterial chemotaxis in alga-bacterium interactions and thus to extend our knowledge of its role in carbon flux and nutrient cycling in marine ecosystems.
DISCUSSION
The phycosphere of a phytoplankton cell is an important area of nutrient uptake for bacteria in the oceans (
24). Various types of interactions between those two groups of organisms might be beneficial or detrimental for one or both partners. To identify genes and gene products which are essential for the interaction, a bilateral model system consisting of the diatom
T. weissflogii and the bacterial strain
M. adhaerens was previously established (
22,
23,
31,
57). This interaction promotes the growth of both the bacterium and the diatom. Moreover,
M. adhaerens attached to the diatom and the coculture resulted in increased TEP synthesis and aggregation of the diatom cells (
22). Processes required for initiation of this interaction might be bacterial motility, chemotaxis, and surface attachment (
15). It was hypothesized that bacterial chemotaxis may be required for diatom-bacterium interaction since
M. adhaerens is highly motile and possesses distinct chemotaxis gene clusters. Importantly,
M. adhaerens was found to be attracted to diatom-derived supplements in soft agar. Migration diameter formation solely due to growth was excluded by a direct comparison of the wild type and chemotaxis-deficient mutants in the same soft agar plate (data not shown). Furthermore, these mutants were not impaired in growth, as validated by liquid culture (data not shown), but nevertheless, they did not form the circle generated by outward-migrating cells. A significant difference between the amount of added cell-free spent diatom supernatant and the diameter of migration of the wild type was observed. Since bacterial attraction to diatom homogenate was less than that to diatom culture or culture supernatant, it is intriguing to speculate that this might be due to yet unknown attracting substances secreted by
T. weissflogii. Alternatively, the less pronounced effects of diatom homogenates might be due to the simultaneous presence of various potentially toxic and thus repelling substances formed during the breakage of diatom cells, as described previously (
48). Testing fractionated cell-derived or supernatant-based attractant-containing solutions might elucidate this type of interaction. In particular, an intense biochemical analysis of the metabolites secreted by the diatom might reveal certain beneficial or detrimental allelochemicals acting toward
M. adhaerens. Since interactions are generally not stable in a changing environment like aquatic systems,
T. weissflogii might produce molecules to attract the bacterium to initiate a symbiosis but might switch to production of deterring substances under specific conditions.
Interestingly,
M. adhaerens does not utilize as the sole carbon source any sugars that had previously been shown to be produced by
T. weissflogii (
3,
31). However, as shown in the same previous study (
31),
M. adhaerens is able to grow on specific amino acids as the sole carbon source. By consuming specific protein or unknown carbohydrate components of diatom exudates,
M. adhaerens might likely modify the chemical structure of the algal exudates, thereby potentially impacting aggregation of diatom cells, e.g., by enzymatic hydrolysis, as proposed previously for phytoplankton-bacterium interaction (
45,
46,
56). To evaluate this hypothesis, time-dependent testing of aggregate formation and TEP synthesis during cocultures in so-called rolling tank experiments (
22) comparing the wild type and the chemotaxis mutants will potentially reveal the actual mechanism of metabolite exchange and/or modification during the diatom-bacterium interaction.
Following the nutrient gradient established during bacterial growth (
41),
chpA and
chpB mutants of
M. adhaerens showed a swimming phenotype indistinguishable from that of the wild type, whereas mutants with defects in
cheA and
cheB showed a clearly decreased migration behavior. These observations indicate that the Chp chemosensory pathway might not be involved in the swimming-mediated chemotaxis of
M. adhaerens. These findings are supported by the proposed twitching motility function of the corresponding genes in
P. aeruginosa (
21,
32,
39,
60). The conditioned agar matrix might require utilization of the flagellum for motility but not that of putative pili by
M. adhaerens. As shown for PAO1, twitching motility mutants can be observed only on very thin agar medium (
19). However, application of this method to demonstrate twitching motility of
M. adhaerens in the current study was not successful (data not shown). Additional analysis tools, such as time-lapse microscopy of flow chambers, are required to fully understand the phenotype of
chp mutants (
35,
40,
43). However, all four chemotaxis-deficient mutants of HP15 showed a decreased ability to attach to an abiotic surface and to diatom cells. The latter finding raises the interesting question of how flagella and putative pili contribute individually to the attachment process, which needs to be addressed in future studies.
Previously, the impact of bacterial chemotaxis on attachment to abiotic surfaces has been described for the environmental organism
Aeromonas spp., the plant pathogen
Agrobacterium tumefaciens, and the soilborne diazotroph
Azospirillum brasilense (
34,
40,
55). For all three organisms, the attachment of chemotaxis-deficient mutants to abiotic surfaces was notably compromised. In
Vibrio cholerae, chemotaxis was proposed to play a stage-specific role in attachment to a polystyrene microtiter dish, since a
cheY3 mutant was deficient in generating a monolayer (
42). In contrast, chemotaxis-deficient mutants of
E. coli appear to form biofilms indistinguishable from the biofilm formed by the wild type (
47). The opportunistic human pathogen
P. aeruginosa has a rather complex chemotaxis system, in which one of the chemotaxis gene clusters exclusively regulates twitching motility (
10,
33). Even though sequence analysis revealed homologies of the twitching motility gene cluster of
P. aeruginosa in the genome of
M. adhaerens, the two bacteria seem to greatly differ in their ability to attach to surfaces and to form biofilms. Although the respective
P. aeruginosa mutants form a more robust biofilm than the wild type (
13),
chp mutants of
M. adhaerens have a significantly decreased ability to attach to an abiotic surface and, hence, to form biofilms. Notably, most of the previously reported studies were based on tests with abiotic surfaces. In contrast, the current study demonstrated a chemotaxis-mediated attachment of a bacterial species to the environmentally relevant biotic surface of marine diatoms.
A somewhat puzzling outcome of the current study was the apparent discrepancy in the total numbers of CFU ml−1 of HP15 wild-type cells determined after the 24-h coincubation with T. weissflogii cells compared to the corresponding total cell numbers at the start of the experiments. Subsequent microscopic analyses, however, revealed that despite thorough vortexing of samples, a significant portion of wild-type cells stayed attached to either diatom cells or alcian blue-stainable aggregates. This suggests a potential limitation of the CFU method used herein and in many other studies. Following sample treatment and dilution plating, any single bacterial colony might thus have originated from multiple diatom-aggregated bacterial cells, thereby falsifying the actual cell numbers and causing a decrease in total cell numbers for the HP15 wild type. This assumption is supported by the converse results for the four tested mutants, for which total cell numbers predominantly derived from free-living, nonattached cells increased over the course of the experiments.
On the one hand, these findings indicate a relatively strong binding of HP15 wild-type cells to biotic surfaces, and on the other hand, these results demonstrate that determinations of the numbers of CFU alone are not sufficient to investigate the interaction of
M. adhaerens and
T. weissflogii. However, concluding from the attachment assay as well as microscopic observations, an interaction pathway between bacteria and diatoms involving bacterial migration toward and attachment to the diatom, followed by a yet unknown sequence of events leading to TEP formation, might be cautiously proposed. TEP formation can in turn be associated with aggregation (
22). A continuation of this study aims to understand which partner in this specific interaction actually secretes and/or modifies the TEP leading to marine snow formation.
In summary, although a wealth of knowledge on mechanisms of chemotaxis in various bacterial species has been acquired
in vitro (
1,
6,
12,
33,
59), the individual effects of bacterial chemotaxis in environmentally relevant habitats are still poorly understood. For the first time and using genetic tools, this study demonstrated a potentially important role of chemotaxis for initiation of phytoplankton-bacterium interactions.
Our future research will focus on the identification of the chemotactic signal(s) of this interaction; the nutrient exchange between
M. adhaerens and
T. weissflogii, including TEP and aggregate formation; and the effects of bacterial chemotaxis on TEP formation by the diatom under various environmental conditions. Consequently, future experiments will elucidate the importance of molecular interaction mechanisms on global processes (
30), particularly on the efficiency of the oceanic carbon pump.