Nanoscale visualization of a fibrillar array in the cell wall of filamentous cyanobacteria and its implications for gliding motility

Many filamentous cyanobacteria are motile by gliding, which requires attachment to a surface. There are two main theories to explain the mechanism of gliding. According to the first, the filament is pushed forward by small waves that pass along the cell surface. In the second, gliding is powered by the extrusion of slime through pores surrounding each cell septum. We have previously shown that the cell walls of several motile cyanobacteria possess an array of parallel fibrils between the peptidoglycan and the outer membrane and have speculated that the function of this array may be to generate surface waves to power gliding. Here, we report on a study of the cell surface topography of two morphologically different filamentous cyanobacteria, using field emission gun scanning electron microscopy (FEGSEM) and atomic force microscopy (AFM). FEGSEM and AFM images of Oscillatoria sp. strain A2 confirmed the presence of an array of fibrils, visible as parallel corrugations on the cell surface. These corrugations were also visualized by AFM scanning of fully hydrated filaments under liquid; this has not been achieved before for filamentous bacteria. FEGSEM images of Nostoc punctiforme revealed a highly convoluted, not parallel, fibrillar array. We conclude that an array of parallel fibrils, beneath the outer membrane of Oscillatoria, may function in the generation of thrust in gliding motility. The array of convoluted fibrils in N. punctiforme may have an alternative function, perhaps connected with the increase in outer membrane surface area resulting from the presence of the fibrils.     

A MOLECULAR MOTOR FOR GLIDING MOTILITY IN CYANOBACTERIA

Motile microorganisms either swim, by using flagella or glide over surfaces by mechanisms that are poorly understood. In cyanobacteria, gliding motility appears as a relatively slow and smooth surface-associated translocation in the direction of the long axis of the filaments at rates up to a few micrometers a second. Many filamentous species translocate in a highly coordinated manner. Translational movements are usually accompanied by revolutions around the long axis of the filament. While moving, the cyanobacteria secrete slime which is left behind as a twisted and collapsed thin tube. The observation of the slime secretion process shows that the mucilage is formed as fine bands that emerge in close proximity to the cells cross walls. Ultrastructural studies have revealed that the cyanobacteria possess at their cross walls complex, pore-like organelles, which might be involved in slime secretion. As each cell possess two different sets of pores pointing in opposite direction, the coordinated activity of these structures could explain how the filament can reverse the direction of locomotion. Furthermore, ultrastructural studies have shown that rotating cyanobacteria possess cell surfaces formed by parallel, helically arranged surface fibrils. As the arrangement of these fibrils corresponds with the path of the filaments during locomotion, it might be imaginable that these fibrils serve as screw thread guiding the rotation of the filaments, with the necessary thrust for locomotion being derived from the secretion of slime using the pores at the cross walls.     

Gliding motility in cyanobacteria: observations and possible explanations

Cyanobacteria are a morphologically diverse group of phototrophic prokaryotes that are capable of a peculiar type of motility characterized as gliding. Gliding motility requires contact with a solid surface and occurs in a direction parallel to the long axis of the cell or filament. Although the mechanistic basis for gliding motility in cyanobacteria has not been established, recent ultrastructural work has helped to identify characteristic structural features that may play a role in this type of locomotion. Among these features are the distinct cell surfaces formed by specifically arranged protein fibrils and organelle-like structures, which may be involved in the secretion of mucilage during locomotion. The possible role of these ultrastructural features, as well as consequences for understanding the molecular basis of gliding motility in cyanobacteria, are the topic of this review.     

GLIDING MOTILITY IN THE BLUE-GREEN ALGA OSCILLATORIA PRINCEPS1

Gliding is an active movement displayed by a microorganism in contact with a solid substrate where there is no evidence of a motility organelle or of a conformational change in the organism. Gliding may be accompanied by rotations, reversals, flectional activity, and mucilage sheath production, as well as linear translation. Previous explanations of the mechanism responsible did not consider all these aspects of behavior. The gliding behavior and ultrastructure of the blue-green alga Oscillatoria princeps Vaucher were examined. O. princeps has a maximum observed gliding rate of 11.1 μm/sec. The trichomes can glide in either longitudinal direction following rapid and occasionally frequent reversals. Right-handed trichome rotation was always observed, which means that any surface point on these trichomes traces a 60-deg right-handed helix. A mucilage sheath envelopes the moving trichomes. The rate of gliding was reduced by viscous substrates, extreme pH, lysozyme, DNP, and cyanide, while sustained darkness had no inhibitory effect. Ultrastructurally, the cell wall is composed of an L-1 layer which is 10 nm thick and often ill-defined. The L-2 layer which is outside this is 200 nm thick and participates in septum formation. The L-3 layer is outside the L-2 and is continuous over the trichome surface. The L-4 “membrane” lies outside the L-3 layer. Grazing surface sections and freeze-etch replicas show a parallel and tight array of 6–9 nm wide continuous fibrils in the cell wall on the surface of the distinctive L-2 layer. Isolated wall fragments were tightly coiled inside out with the fibrils on the inside. The angle of orientation for the fibrils was to the right in a helix with a pitch of 60 deg. O. animalis, a blue-green alga with a movement tracing a left-handed helix, showed a similar array of fibrils oriented in a left-handed helix with a pitch of 60 deg. It is proposed that gliding is produced by unidirectional waves of bending in the fibrils which, act against the sheath or substrate, tints displacing the trichome.     

ELECTRON MICROSCOPIC STUDIES ON THE INDIRECT FLIGHT MUSCLES OF DROSOPHILA MELANOGASTER : I. Structure of the Myofibrils

The myofibrils in Drosophila have thick and thin types of myofilaments arranged in the hexagonal pattern described for Calliphora by Huxley and Hanson (15). The thick filaments, along most of their length in the A band, seem to be binary in structure, consisting of a dense cortex and a lighter medulla. In the H zone, however, they show more uniform density; lateral projections (bridges) also appear to be absent in this region. The M band has a varying number of granules (probably of glycogen) distributed between the myofilaments. The myofilaments on reaching the Z region appear to change their hexagonal arrangement and become connected to one another by Z filaments. The regular arrangement of the filaments found in most regions of the fibrils is not seen in the terminal sarcomeres of some flight muscles; the two types of filaments appear to be intermingled in an irregular pattern in these parts of the fibrils. The attachment of myofibrils to the cuticle through the epidermal cells is described.     

Oscillin, an extracellular, Ca2+-binding glycoprotein essential for the gliding motility of cyanobacteria

Electron microscopic studies have demonstrated that various gliding filamentous cyanobacteria have trichome surfaces with a common structural organization. They contain an S-layer attached to the outer membrane and an array of parallel fibrils on top of the S-layer. In all species studied, the helical arrangement of these fibrils corresponds to the sense of rotation of the organism during the gliding movement. We have investigated the surface fibrils of Phormidium uncinatum using electron microscopic, spectroscopic and biochemical techniques. The fibrils consist of a single rod-shaped protein, which we refer to as oscillin. Oscillin is a 646 amino acid residue protein ( M _r 65 807; pI 3.63) and appears to be glycosylated. Sequence analysis reveals a two-domain structure: a 554 residue domain contains 46 repeats of a Ca²⁺-binding motif; it is followed by a 92 residue C-terminal domain, which might mediate its export. Filaments that do not express oscillin lose their ability to move. Homology studies suggest that similar proteins play comparable roles in other motile cyanobacteria. The structure of oscillin appears to favour a passive role in gliding.     

The fine structure of Herpetosiphon,and a note on the taxonomy of the genus

The fine structure of the Gram-negative filamentous gliding bacterium, Herpetosiphon is described. The outer membrane of the cell envelope could not be resolved as a separate structure, probably because it is fused with the underlying dense (peptidoglycan) layer. There was an additional wall layer outside this membrane-peptidoglycan complex, but a sheath in the classical sense, as postulated in the definition of the genus, was lacking. On the cell surface a loose network of fibrils could be seen. Inside the cells 3 types of intracytoplasmic membranes were discernible: a) true mesosomes near cross walls; b) a system of coarser membranes which was not connected with the septa and formed networks or tubular complexes; c) degenerated septa within bulbs. the bulbs are swollen sections of filaments, occurred mainly in ageing cultures, and are probably a degeneration phenomenon. The filaments contained necridia, i.e. dead and empty cells, across which breaks may occur so that empty cell wall cylinders remain attached to the ends of the daughter filaments, falsely suggesting the presence of a sheath. The taxonomy of Herpetosiphon is discussed in detail: The organism has been described before as Flexibacter giganteus. It is proposed to abandon the species H. aurantiacus in favor of H. giganteus, but to retain the genus Herpetosiphon. An improved definition of the genus is given.     

Fibrillar Array in the Cell Wall of a Gliding Filamentous Cyanobacterium

The cell walls of a number of filamentous, gliding cyanobacteria of the genus Oscillatoria were examined by transmission electron microscopy of ultrathin sections, of freeze-etched replicas, and of whole cells crushed between glass slides and negatively stained. All three techniques revealed the presence of a highly ordered array of parallel fibrils, seen in transverse sections to be situated between the peptidoglycan and the outer membrane. Approximately 200 individual fibrils, each 25 to 30 nm in width, form a parallel, helical array that completely surrounds each cyanobacterial filament, running at an angle of 25 to 30° to its long axis. This highly regular arrangement of the fibrillar layer may imply some underlying symmetry responsible for its organization. A possible source of such symmetry would be the peptidoglycan, and some form of interaction between this layer and the fibrils might provide the necessary scaffolding for the fibrillar array. In crushed, negatively stained samples of fresh cells, individual fibrils were seen outside the filament, released from the cell wall. These released fibrils were of the same width as those observed in situ but were in short lengths, mostly of 100 to 200 nm, and were invariably bent, sometimes even into U shapes, implying great flexibility. Negative staining of released fibrils showed no evidence that they were hollow tubes but did give some indication of a substructure, implying that they were composed of many subunits. The function of this fibrillar array is unknown, although its position in the cell wall, as well as the correspondence between the angle of the fibrils with respect to the long axis of the filament and the rotation of the filament during gliding, may imply an involvement in gliding motility.     

Envelope structure of four gliding filamentous cyanobacteria.

The cell walls of four gliding filamentous Oscillatoriaceae species comprising three different genera were studied by freeze substitution, freeze fracturing, and negative staining. In all species, the multilayered gram-negative cell wall is covered with a complex external double layer. The first layer is a tetragonal crystalline S-layer anchored on the outer membrane. The second array is formed by parallel, helically arranged surface fibrils with diameters of 8 to 12 nm. These fibrils have a serrated appearance in cross sections. In all cases, the orientation of the surface fibrils correlates with the sense of revolution of the filaments during gliding, i.e., clockwise in both Phormidium strains and counterclockwise in Oscillatoria princeps and Lyngbya aeruginosa. The lack of longitudinal corrugations or contractions of the surface fibrils and the identical appearances of motile and nonmotile filaments suggest that this structure plays a passive screw thread role in gliding. It is hypothesized that the necessary propulsive force is generated by shear forces between the surface fibrils and the continuing flow of secreted extracellular slime. Furthermore, the so-called junctional pores seem to be the extrusion sites of the slime. In motile cells, these pores exhibit a different staining behavior than that seen in nonmotile ones. In the former, the channels of the pores are filled with electron-dense material, whereas in the latter, the channels appear comparatively empty, highly contrasting the peptidoglycan. Finally, the presence of regular surface structures in other gliding prokaryotes is considered an indication that comparable structures are general features of the cell walls of gliding microbes.     

Soil stabilization by a prokaryotic desert crust: Implications for Precambrian land biota

A cyanophyte dominated mat, desert crust, forms the ground cover in areas measuring hundreds of square meters in Utah and smaller patches in Colorado. The algal mat shows stromatolitic features such as sediment trapping and accretion, a convoluted surface, and polygonal cracking. Sand and clay particles are immobilized by a dense network of filaments of the two dominating cyanophyte species,Microcoleus vaginatus andM. chthonoplastes, which secrete sheaths to which particles adhere. These microorganisms can tolerate long periods of desiccation and are capable of instant reactivation and migration following wetting. Migration occurs in two events: 1. immediately following wetting of dry mat, trichomes are mechanically expelled from the sheath as it swells during rehydration, and 2. subsequently, trichomes begin a self-propelled gliding motility which is accompanied by further production of sheath. The maximum distance traveled on solid agar by trichomes ofMicrocoleus vaginatus during a 12 hour period of light was 4.8 cm. This corresponds to approximately 500 times the length of the fastest trichome, and provides a measure of the potential for spreading of the mat in nature via the motility of the trichomes.Dehydration resistence of the sheath modifies the extracellular environment of the trichomes and enables their transition to dormancy. Following prolonged wetting and evaporative drying of the mat in the laboratory, a smooth wafer-like crust is formed by the sheaths ofMicrocleus trichomes that have migrated to the surface. Calcium carbonate precipitates among the algal filaments under experimental conditions, indicating a potential for mat lithification and fossilization in the form of a caliche crust. It is suggested that limestones containing tubular microfossils may, in part, be of such an origin.The formation of mature Precambrian soils may be attributable to soil accretion, stabilization, and biogenic modification by blue-green algal land mats similar to desert crust.     

Soil stabilization by a prokaryotic desert crust: implications for Precambrian land biota.

A cyanophyte dominated mat, desert crust, forms the ground cover in areas measuring hundreds of square meters in Utah and smaller patches in Colorado. The algal mat shows stromatolitic features such as sediment trapping and accretion, a convoluted surface, and polygonal cracking. Sand and clay particles are immobilized by a dense network of filaments of the two dominating cyanophyte species, Microcoleus vaginatus and M. chthonoplastes, which secrete sheaths to which particles adhere. These microorganisms can tolerate long periods of desiccation and are capable of instant reactivation and migration following wetting. Migration occurs in two events: 1. immediately following wetting of dry mat, trichomes are mechanically expelled from the sheath as it swells during rehydration, and 2. subsequently, trichomes begin a self-propelled gliding motility which is accompanied by further production of sheath. The maximum distance traveled on solid agar by trichomes of Microcoleus vaginatus during a 12 hour period of light was 4.8 cm. This corresponds to approximately 500 times the length of the fastest trichome, and provides a measure of the potential for spreading of the mat in nature via the motility of the trichomes. Dehydration resistence of the sheath modifies the extracellular environment of the trichomes and enables their transition to dormancy. Following prolonged wetting and evaporative drying of the mat in the laboratory, a smooth wafer-like crust is formed by the sheaths of Microcleus trichomes that have migrated to the surface. Calcium carbonate precipitates among the algal filaments under experimental conditions, indicating a potential for mat lithification and fossilization in the form of a caliche crust. It is suggested that limestones containing tubular microfossils may, in part, be of such an origin. The formation of mature Precambrian soils may be attributable to soil accretion, stabilization, and biogenic modification by blue-green algal land mats similar to desert crust.     

Characterization of gliding motility in Flexibacter polymorphus

Motility of the marine gliding bacterium Flexibacter polymorphus was studied by using microcinematographic techniques. Following adhesion to a glass surface, multicellular filaments and individual cells usually began to glide within a few seconds at a speed of approximately 12 micron per second (at 23 degrees C). Adhesion to the glass surface was evidently mediated by multitudes of extremely fine extracellular fibrils. Gliding velocity was independent of filament length but directly related to electron-transport activity and substratum temperature in the range 3-35 degrees C. The rate of gliding was inversely related to medium viscosity, suggesting that the locomotor apparatus functions at constant torque. Forward motion was occasionally interrupted by direction reversals, somersaults (observed primarily in single cells of short filaments), or spinning of filaments tethered by one pole. The frequency of direction reversal was found to be an inverse function of filament length. Translational motility was invariably accompanied by sinistral revolution about the longitudinal axis of a filament. The sense and pitch of revolution were constant among filaments of different length. Polystyrene microspheres or India ink particles adsorbed to gliding cells were actively displaced in either direction, their movement tracing either a regular zigzag or helical path along the filament surface. Because microspheres were also observed to move on nonmotile filaments, particle translocation was evidently not obligatorily linked to gliding locomotion. Multiple particles adsorbed to a single filament often moved independently. The data are consistent with a motility mechanism involving limited motion in numerous mechanically independent (yet functionally coordinated) domains on the cell surface.     

Intercellular power transmission along trichomes of cyanobacteria

An attempt at demonstrating lateral power transmission over millimeter distances along a coupling membrane has been undertaken. Trichomes of the multicellular filamentous cyanobacteria Phormidium uncinatum were illuminated with a very narrow light beam forming a light spot that covered only 4–5% of a 1–2 mm long cyanobacterial trichome. Such illumination was found to support motility (gliding along agar surface) of the trichome under conditions when the light was the only energy source. It was also shown that illumination with the light spot caused rotation of rings of slime (accompanying the operation of the ‘motors’ responsible for the motility of cyanobacteria) not only in the illuminated, but also in the distal, nonilluminated part of the trichome. Electric potential transmission along trichomes was revealed by means of the extracellular electrode technique. The light spot was found to induce generation of an electric potential difference between two electrodes in the dark region of the trichomes, which were placed at different distances from the illuminated end. Cutting the trichomes between the light spot and the closest ‘dark’ electrode abolished this effect. Valinomycin + K⁺ and carbonyl cyanide p-trifluoromethoxyphenylhydrazone affected the potential difference formation between two ‘dark’ electrodes much stronger than that between a light and a dark electrode. All the light spot-induced effects develop in the seconds time scale. Both the amplitudes and the kinetics of the potential difference measured with four electrodes placed along the trichome prove to be in good agreement with the theoretical curves computed on the basis of the electric cable equation. It is concluded that transcellular power transmission in the form of Δψ takes place along trichomes of cyanobacteria. This confirms the hypothesis about the biological function of Δψ as a transportable form of energy.     

Some Observations on the Fine Structure of the Giant Nerve Fibers of the Earthworm, Eisenia foetida

Sectioned dorsal giant fibers of the earthworm Eisenia foetida have been studied with the electron microscope. The giant axon is surrounded by a Schwannian sheath in which the lamellae are arranged spirally. They can be traced from the outer surface of the Schwann cell to the axon-Schwann membranes. Irregularities in the spiral arrangement are frequently observed. Desmosome-like attachment areas occur on the giant fiber nerve sheath. These structures appear to be arranged bilaterally in columns which are oriented slightly obliquely to the long axis of the giant fiber and aligned linearly from the axon to the periphery of the sheath. At these sites they bind together apposing portions of Schwann cell membrane comprising the sheath. Longitudinal or oblique sections of the nerve sheath attachment areas are reminiscent of the Schmidt-Lantermann clefts of vertebrate peripheral nerve. Septa of the giant fibers have been examined. They are symmetrical or non-polarized and consist of the two plasma membranes of adjacent nerve units. Characteristic vesicular and tubular structures are associated with both cytoplasmic surfaces of these septa.     

Inducible defence against a ciliate grazer Pseudomicrothorax dubius,in two strains of Phormidium (cyanobacteria)

Experiments were done with two strain of filamentous, mat-forming Phormidium and their ciliate grazer Pseudomicrothorax dubius, to explain why the ciliates remain hungry in an apparent surplus of food, except for the first 24 hours after feeding. Under grazing pressure, both strains of cyanobacteria showed statistically significant increases in the number of filaments terminating in an empty sheath, compared to the control. Direct observations revealed that the mechanism behind this effect was active withdrawal of the trichomes inside the sheaths when disturbed by grazers. As P. dubius is unable to ingest trichomes with such endings, we conclude that cyanobacteria are not limited to chemical means of defence against grazers but can also defend themselves by means of movement and changes in filament morphology. This is apparently the first report on behavioural defence observed in cyanobacteria.     

Fine Structure of Spirochaeta stenostrepta, a Free-living, Anaerobic Spirochete

The fine structure of Spirochaeta stenostrepta strain Z1, a free-living anaerobic spirochete, was studied by electron microscopy. The organism possessed a coiled protoplasmic cylinder, an axial filament inserted subterminally, and a loosely fitting sheath which enclosed both the protoplasmic cylinder and the axial filament. The axial filament consisted of two fibrils partially overlapping in a 1-2-1 arrangement. The axial fibrils appeared to possess a sheath surrounding an inner core. Both inner core and sheath were apparently enclosed in a cross-striated tubular structure, which was itself surrounded by an outer sheath. The axial filament exhibited a basal hook. A disc- or mushroom-shaped structure, possibly consisting in part of cytoplasmic membrane, was observed at the insertion end of isolated filaments. The protoplasmic cylinder had a distinctive surface structure consisting of an array of tightly packed, longitudinally arranged helices measuring 2.0 to 2.5 nm in diameter. This layer of helices lay below the outer cell sheath and the axial filament. Ballistic disintegration loosened the helical array, causing individual helices or segments of helices to become separated from the cell. The function of this layer of helices is still obscure.     

The junctional pore complex and the propulsion of bacterial cells

Gliding motility is defined as translocation in the direction of the long axis of the bacterium while in contact with a surface. This definition leaves unspecified any mechanism and, indeed, it appears that there is more than one physiological system underlying the same type of motion. Currently, two distinct mechanisms have been discovered in myxobacteria. One requires the extension, attachment, and retraction of type IV pili to pull the cell forwards. Recent experimental evidence suggests that a second mechanism for gliding motility involves the extrusion of slime from an organelle called the 'junctional pore complex'. This review discusses the role of slime extrusion and the junctional pore complex in the gliding motility of both cyanobacteria and myxobacteria.     

Organic structures of the hypercalcified peritubular matrix in horse dentine.

EDTA-insoluble organic structures of the hypercalcified peritubular matrix (PM) in horse dentine were observed by scanning electron microscopy. The PM was enveloped in double cylindrical structures composed of fibrillar sheaths in the inner and outer peripheries. Between the outer fibrillar sheath and intrinsic fibrils of the intertubular matrix, a calcified cementing membrane existed. Within the PM, warped cone-shaped structures of fibrillar sheaths, overlapping at intervals of 4-6 microns and semiconcentrically surrounding the dentinal tubule, extended from the inner fibrillar towards the outer fibrillar sheath. The cone-shaped fibrillar sheaths following the inner and outer fibrillar sheaths were identified as the incremental lines of the PM. Most of these fibrils may be collagen although it could not be confirmed, whereas non-collagenous organic materials in the lateral branches of the dentinal tubule are radially arranged in the PM. These EDTA-insoluble structures were three-dimensionally illustrated using an image-analysing system.     

Hormogonia in two nostocalean cyanophytes (cyanobacteria) from the genera Hapalosiphon and Fischerella

The formation of hormogonia in the nostocalean cyanophytes/cyanobacteria Hapalosiphon fontinalis (C. Agardh) Bornet and Fischerella sp. was studied in natural populations collected from the Klin peatbog, northern Slovakia. Hormogonia were produced terminally in lateral branches of filaments (both species), or also directly on the main branches (Fischerella sp.). In contrast to vegetative filaments, hormogonia were not ramified, lacked heterocytes, were embedded in mucilaginous envelopes, were able to move, and their cells contained aerotopes. They were released by gliding through an opening in the sheath at the end of lateral branches of filaments. Released hormogonia of H. fontinalis were solitary or agglomerated into common fascicles morphologically resembling planktic colonies of Aphanizomenon flos-aquae (L.) Ralfs ex Bornet et Flahault or Dolichospermum affine (Lemmermann) Wacklin, Hoffmann et Komárek (syn. Anabaena affinis Lemmermann). Occasionally, lateral or sessile Nostochopsis-like heterocytes and apical spherical monocytes were formed on the main filaments. Hormogonia of Fischerella sp. were formed not only in apical part of lateral trichomes, but also directly on the main trichomes. Their cells were markedly larger than the vegetative cells and possessed well-developed aerotopes. Released hormogonia remained solitary, and were not agglomerated into fascicles. Apical hormogonia were released by gliding through an opening in the sheath at the end of lateral branches of filaments, and basal hormogonia were released by breaking off the main axis. In contrast to filaments of H. fontinalis which were very common and represented the dominant species of the cyanophyte communities in the locality, filaments of Fischerella sp. were observed only in one sample and for a limited period. This is the first record of a representative of the genus Fischerella in Slovakia.