Behavior of the contractile vacuole of Tetrahymena pyriformis W: a redescription with comments on the terminology.

The behavior of the contractile vacuole of Tetrahymena pyriformis W has been recorded and analyzed quantitatively by cinephotography. The vacuole fills in a stepwise fashion by the confluence of ampullae which appear regularly at the beginning of systole and whose membranes are continuous with that of the contractile vacuole throughout the cycle. The vacuole may subsequently fill slowly by a means not discernible by light microscopy. The vacuole rounds up at the beginning of systole and shortly thereafter the ampullae reappear around the perimeter of the vacuole. They are expanded by fluid forced into them from the vacuole. Round-up and the mode of growth of the ampullae indicate that the contractile vacuole is truly contractile. Expulsion occurs soon after the appearance of the ampullae and terminates the cycle. Contraction is initiated at regular intervals by a timing mechanism which is independent of the size of the vacuole. Suitable terminology to describe the structure and behavior of the contractile vacuole is discussed.     

Membrane Dynamics of the Contractile Vacuole Complex of Paramecium1

ABSTRACT. Membrane dynamics of the contractile vacuole complex of Paramecium were investigated using conventional electron microscopy of cells so that the vacuoles were serial-sectioned longitudinally and transversely. During systole, vacuolar membrane collapses first into flattened cisternae which undergo further modification into a mass of interconnected small membrane tubules. These tubules retain their connections with the radiating microtubular ribbons; consequently they are found only in the poleward hemisphere. Permanent connections between ampullae and the collapsed vacuole membrane could not be verified nor was a sphincter-like mechanism for closing such a junction observed. Membranes of the ampullae and the collecting canals also collapse to varying extents into arrays of tubules that remain bound to microtubular ribbons during diastole. Thus vacuole, ampullae, and collecting canal membranes all assume tubular forms when internal volume is at a minimum. Having failed to observe a microfilamentous encasement of the vacuole, we suggest that an alternative mechanism for the “contractile” function should be sought. One such is based on fluid volume increase and fluid flow within transiently interconnected tubular membrane systems that cycle between a tubular and a planar membrane form as internal volume is periodically increased and reduced. The driving force for this mechanism might best be sought in the molecular structure of the membranes of the contractile vacuole complex.     

Fine Structure of the Contractile Vacuole Pore in Paramecium*

The pore through which a Paramecium contractile vacuole communicates with the external environment is a 1.2 μm long and 1 μm diameter cylindrical orifice in the pellicle. During diastole, the vacuole:pore junction is closed by a substantial diaphragm which parts to the side at systole. The diaphragm is composed of inner and outer membranes continuous with the vacuole and pore membranes, respectively, and an intervening cytoplasmic layer containing filaments and irregular membranous tubules and vesicles. Microtubules, organized into 2 sets, are an important component of the pore apparatus. One set of ～ 16 microtubules forms an annulus around the pore. These microtubules are organized into a right-handed helix with a pitch of 0.5-0.6 μm, and thus complete slightly more than 2 turns in their course from the level of the diaphragm to the pore outer lip. They appear to be embedded in a layer of dense material immediately adjacent to the pore membrane. The other set consists of 5 or more bands of 10–20 microtubules which radiate in a slight left-handed helix from an insertion at the pore out over the vacuole surface to the ampullae.     

The response of contractile and non-contractile vacuoles of Paramecium calkinsi to widely varying salinities.

Paramecium calkinsi from tidal marshes survive a wide salinity range. Fluid output of contractile vacuoles of these cells decreased as salinity of the medium to which they were acclimated increased, and both pulse rate and vacuole volume were used to regulate output. When cells were first exposed to more dilute medium, contractile vacuoles greatly increased volume so that fluid output increased even though pulse rate decreased. In cells shifted to a more concentrated medium, contractile vacuole output decreased by decreasing pulse rate. The contractile vacuole is surrounded by a set of collecting structures which change form as the salinity changes. Distensible ampullae are found in media of low salinity and collecting canals are found in media of high salinity. When cells are shifted from high salinity to low, the number of ampullae increases and the number of canals decreases. When cells are shifted from low salinity to high, the number of ampullae decreases and the number of canals decreases. Other non-contracting vacuoles also appear in response to a hypoosmotic shock. These include vacuoles within the cell as well as "blisters" on the surface. The number and frequency of blisters increases with the size of the hypoosmotic shock. They detach from cells without resulting in any visible loss of cytoplasm. Non-contractile vacuoles may play a role in sequestering and removing excess water that the contractile vacuoles cannot handle.     

The Response of Contractile and Non-Contractile Vacuoles of Paramecium calkinsi to Widely Varying Salinities

ABSTRACT. Paramecium calkinsi from tidal marshes survive a wide salinity range. Fluid output of contractile vacuoles of these cells decreased as salinity of the medium to which they were acclimated increased, and both pulse rate and vacuole volume were used to regulate output. When cells were first exposed to more dilute medium, contractile vacuoles greatly increased volume so that fluid output increased even though pulse rate decreased. In cells shifted to a more concentrated medium, contractile vacuole output decreased by decreasing pulse rate. The contractile vacuole is surrounded by a set of collecting structures which change form as the salinity changes. Distensible ampullae are found in media of low salinity and collecting canals are found in media of high salinity. When cells are shifted from high salinity to low, the number of ampullae increases and the number of canals decreases. When cells are shifted from low salinity to high, the number of ampullae decreases and the number of canals decreases. Other non-contracting vacuoles also appear in response to a hypoosmotic shock. These include vacuoles within the cell as well as "blisters" on the surface. The number and frequency of blisters increases with the size of the hypoosmotic shock. They detach from cells without resulting in any visible loss of cytoplasm. Non-contractile vacuoles may play a role in sequestering and removing excess water that the contractile vacuoles cannot handle.     

A novel model for fluid secretion by the trypanosomatid contractile vacuole apparatus

We have studied fluid secretion by the contractile vacuole apparatuss of the trypanosomatid flagellate Leptomonas collosoma with thin sections and freeze-fracture replicas of cells stabilized by ultrarapid freezing without prior fixation or cryoprotection. The ultrarapid freezing has revealed membrane specializations related to fluid segregation and transport as well as membrane rearrangements which may accompany water expulsion at systole. This osmoregulatory apparatu consists of the spongiome, the contractile vacuole, and the fluid discharge site. The coated tubules of the spongiome converge on the contractile vacuole from all directions. These 60- to 70-nm tubules contain characteristic double rows of 11-nm intramembrane particles in a helical configuration which fracture predominantly with the E face. Short double rows of similar particles are also frequently found on both faces of the contractile vacuole itself, in addition to many smaller particles on the P face. The spongiome tubules fuse with the vacuole during the filling stage of each cycle and then detach before secretion. The contractile vacuole membrane is permanently attached to the plasma membrane of the flagellar pocket by a dense adhesion plaque. In some ultrarapidly frozen cells, 20- to 40-nm perforations can be visualized within the plaque and the adjacent membranes during the presumptive time of discharge. The formation of the plaque perforations and the membrane channels occurs without fusion of the vacuole and the plasma membrane and does not require extracellular calcium. On the basis of our results, we have developed a model for water secretion which suggests that the adhesion plaque may induce pore formation in the adjoining lipid bilayers, thereby allowing bulk expulsion of the fluid.     

The Role of the Contractile Vacuole in the Osmoregulation of Tetrahymena pyriformis*

The relationship of cell size and contractile vacuole efflux to osmotic stress was studied in Tetrahymena pyriformis strain W, after transfer into fresh solutions iso- or hypoosmotic to the growth medium. Microscopic measurements of the cell and contractile vacuole dimensions, made with an image-sharing ocular at 27 C, allowed the calculation of the cell size and shape and the vacuolar efflux rate which provide a measure of osmoregulation. The contractile vacuole cycles have no homeostatic oscillations. In 0.03–0.10 osmolar solutions, the cell size and shape are constant while the vacuolar efflux rate has an inverse linear dependence upon extracellular osmolarity. Regression analyses indicate that for cells with systole faster than 0.1 sec (the major part of the population), it is only the final diastolic volume of the contractile vacuole that is related to osmotic stress while the frequency of systole is independent of osmotic stress and has a constant period of 7.7 ± 0.2 sec. Therefore, osmotic stress upon Tetrahymena is regulated by a corresponding change in the filling rate of its contractile vacuole to allow an unaltered cell size and shape. Kinetic measurements of vacuoles during diastole fit the model (dV/dt = K_1-K₂A), where (dV/dt) is the vacuolar filling rate and (A) is the vacuolar surface area. This dependence of vacuolar volume upon its surface area may be ascribed either to elastic components of the vacuolar membrane or to an increasing leakiness of this membrane during diastole. Mitochondrial inhibitors were used to observe the energy requirements of vacuolar operation and of intracellular secretion of water.     

An Electron Microscope Study of the Contractile Vacuole in Tokophrya infusionum

Contractile vacuoles are organelles that collect fluid from the cytoplasm and expel it to the outside. After each discharge (systole), they appear again and expand (diastole). They are widely distributed among Protozoa, and have been found also in some fresh water algae, sponges, and recently in some blood cells of the frog, guinea pig, and man. In spite of the extensive work on the contractile vacuole, very little is known concerning its mode of operation. An electron microscope study of a suctorian Tokophrya infusionum provided an opportunity to study thin sections of contractile vacuoles, and in these some structures were found which could be part of a mechanism for the systolic and diastolic motions the organelle displays. In Tokophrya, as in Suctoria and Ciliata in general, the contractile vacuole has a permanent canal connecting it with the outside. The canal appears to have a very elaborate structure and is composed of three parts: (1) a pore; (2) a channel; and (3) a narrow tubule located in a papilla protruding into the cavity of the contractile vacuole. Whereas the pore and channel have fixed dimensions and are permanently widely open, the tubule has a changeable diameter. At diastole it is so narrow (about 25 to 30 mµ in diameter) that it could be regarded as closed, while at systole it is widely open. It is assumed that the change in diameter is due to the contraction of numerous fine fibrils (about 180 A thick) which are radially disposed around the canal in form of a truncated cone, with its tip at the channel, and its base at the vacuolar membrane. It seems most probable that the broadening of the tubule results in discharge of the content of the contractile vacuole. In the vicinity of the very thin limiting vacuolar membrane, small vesicles and canaliculi of the endoplasmic reticulum, very small dense particles, and mitochondria may be found. In addition, rows of closely packed vesicles are present in this region, and in other parts of the cytoplasm. It is suggested that they might represent dictyosome-like bodies, responsible for withdrawing fluids from the cytoplasm and then conveying them to the contractile vacuole, contributing to its expansion at diastole.     

The Contractile Vacuole in Amoeba proteus: Temperature Effects

The influence of temperature on the various aspects of the contractile vacuole cycle of Amoeba proteus has been established. In the upper temperature range (20, 25 and 30 C) an increase in temperature results in shorter vacuolar cycles with greater systolic (final) volumes. The systole is rapid and always complete. At 35 C the vacuole shows the effect of heat stress, cycles are irregular in volume and duration with only partial systoles. In the lower temperature range (15, 10 and 5 C), a new phenomenon has been observed, the plateau. Instead of undergoing systole, after reaching a certain critical volume the vacuole abruptly ceases to grow in size and remains in a state of pause for a well defined period of time, ending at a comparatively slow but complete systole. The duration of this plateau as well as its inception and termination seem quite precisely controlled. Its effect, a decrease in the fluid output by the vacuole, is such as to adjust vacuolar output to near constant Q₁₀ kinetics over our temperature range. This is correlated with a single straight line fit in an Arrhenius plot. Available data do not permit a complete explanation of the nature of the plateau. It could represent a steady state between 2 opposing phenomena: active fluid influx into the vacuole and osmotic losses from the vacuole into the relatively hypertonic cytoplasm.     

Structure and behavior of contractile vacuoles inChlamydomonas reinhardtii

Summary The contractile vacuole (CV) cycle ofChlamydomonas reinhardtii has been investigated by videomicroscopy and electron microscopy. Correlation of the two kinds of observation indicates that the total cycle (15 s under the hypo-osmotic conditions used for videomicroscopy) can be divided into early, middle, and late stages. In the early stage (early diastole, about 3 s long) numerous small vesicles about 70–120 nm in diameter are present. In the middle stage (mid-diastole, about 6 s long), the vesicles appear to fuse with one another to form the contractile vacuole proper. In the late stage (late diastole, also about 6 s long), the CV increases in diameter by the continued fusion of small vesicles with the vacuole, and makes contact with the plasma membrane. The CV then rapidly decreases in size (systole, about 0.2 s). In isosmotic media, CVs do not appear to be functioning; under these conditions, the CV regions contain numerous small vesicles typical of the earliest stage of diastole. Fine structure observations have provided no evidence for a two-component CV system such as has been observed in some other cell types. Electron microscopy of cryofixed and freeze-substituted cells suggests that the irregularity of the profiles of larger vesicles and vacuoles and some other morphological details seen in conventionally fixed cells may be shrinkage artefacts. This study thus defines some of the membrane events in the normal contractile vacuole cycle ofChlamydomonas, and provides a morphological and temporal basis for the study of membrane fusion and fluid transport across membranes in a cell favorable for genetic analysis.Abbrevations CV contractile vacuole - PM plasma membrane     

THE MECHANISM OF THE NEPHRIDIAL APPARATUS OF PARAMECIUM MULTIMICRONUCLEATUM : II. The Filling of the Vesicle by Action of the Ampullae

Our recent analysis of the nephridial apparatus of Paramecium multimicronucleatum by high-speed cinematography (300 fps at X 250) indicates that before the water expulsion vesicle ("contractile vacuole") is completely voided of fluid during expulsion, the ampullae surrounding and confluent with the vesicle swell with fluid entering from their respective nephridial tubules. Once the membranes of the excretory pore at the base of the excretory canal (leading from the vesicle proper to the outside) have constricted and resealed the excretory pore, the up till then constricted injection tubules of the ampullae which conduct fluid to the vesicle open as waves of contraction along the coacervate gel around the ampulla and proceed along each ampulla from distal to proximal end. The coacervate gel around any one ampulla does not necessarily contract in phase with that of any other ampulla. Each ampulla acts independently. The fluid from the ampullae is thus pumped sequentially, but not in predetermined order, into the water expulsion vesicle, refilling and distending it. Our previous studies (Organ et al., 1968a) suggest that an actomyosinoid ATP-using mechanism may be functional in the ampullary contractions.     

Tubular-vesicular transformation in the contractile vacuole system of Dictyostelium

The contractile vacuole complex of Dictyostelium is the paradigm of a membrane system that undergoes tubular-vesicular transitions during its regular cycle of activities. This system acts as an osmoregulatory organelle in freshwater amoebae and protozoa. It collects fluid in a network of tubules and cisternae, and pumps it out of the cell through transient pores in the plasma membrane. Tubules and vacuoles are interconvertible. The tubular channels are associated with the cortical actin network and are capable of moving and fusing. The contractile vacuole complex is separate from vesicles of the endosomal pathway and preserves its identity in a dispersed state during cell division. We outline techniques to visualize the contractile vacuole system by electron and light microscopy. Emphasis is placed on GFP-fusion proteins that allow visualization of the dynamics of the contractile vacuole network in living cells. Proteins that control activities of this specialized organelle in Dictyostelium have been conserved during evolution and also regulate membrane trafficking in man.     

The Permanence of the Infraciliature in Suctoria: An Electronmicroscopic Study of Pattern Formation in Tokophrya infusionum*

SYNOPSIS. The adult Tokophrya infusionum does not possess cilia, but has 20–30 barren basal bodies arranged in 6 short rows adjacent to the contractile vacuole pore. During reproduction, which is by internal budding, the contractile vacuole sinks into the parent along with the invaginating membranes that form the embryo and the wall of the brood pouch. The 6 rows of basal bodies radiate away from the pore and elongate to form 5 long ciliary rows, that encircle the anterior half of the embryo, and 1 short row at the posterior end. The contractile vacuole pore, along with several barren basal bodies, remains in the parent when the embryo is completed. The pore rises to the surface when the embryo is born. New basal bodies are then formed in the parent to replace those which were incorporated into the embryo, and formation of another embryo may begin. The cilia of the embryo are partially resorbed 10 min after the start of metamorphosis, with depolymerization of the ciliary microtubules. Later, the cilia and most of the basal bodies disappear completely, except for a group of barren basal bodies near the embryo's contractile vacuole pore, which form 6 rows and serve as an anlage for the basal bodies and cilia that arise during embryogenesis. There is, therefore, an organized infraciliature in Suctoria throughout their life cycle, and a distinct continuity of basal bodies across the generations.     

The Fine Structure of the Internal Spiral of Kinetosomes in Foettingeria's Tomite,a Unique Storage Depot for Kinetosomes1

ABSTRACT. The fine structure of the tomite of Foettingeria actiniarum (Claparède) was examined and compared with that of other apostome tomites. This stage in the life cycle has a unique configuration of kineties that form a spiral through the cytoplasm in the interior of the body. The structure and behavior of this internal spiral were evaluated as a mechanism for the storage of kinetosomes, an adaptation to the ciliate's two-host life cycle. The spiral is composed of nine ribbons of laterally compressed kinetosomes that are in contact with a thin electron-dense fibril. Paralleling the kineties of the spiral are conspicuous, swollen lamellae of the rough endoplasmic reticulum; these lamellae contain moderately electron-dense material. The spiral is associated with the large contractile vacuole and winds about the macronucleus. The tomite of Foettingeria possesses a single, robust, caudal cilium located in a pit, along with the nozzle-like pore of the contractile vacuole. The walls of the pit contain several trichocysts arranged radially about the caudal cilium and aimed into the pit.     

Involvement of smooth and coated vesicles in the function of the contractile vacuole complex of some cryptophycean flagellates

The contractile vacuole complex of cryptophycean flagellates comprises the contractile vacuole, a pore and a vesicular spongiome. A minority of spongiome vesicles bear a 15-nm coat on the cytoplasmic surface of the membrane. The coat superficially resembles a clathrin coat. The majority of vesicles are smooth surfaced. Both types of vesicles are found at the same time. Smooth vesicles can be seen in profile suggesting vesicle-vesicle and vesicle-vacuole fusion. It is suggested that smooth vesicles are involved in the segregation of fluid from the cytoplasm and in filling the vacuole. Coated elements exist only as independent vesicles and as coated pits in the contractile vacuole membrane. There is no evidence of fusion of coated vesicles. It is suggested that coated vesicles function to retrieve specific membrane components from the contractile vacuole.     

Distribution of alkaline phosphatase in vegetative dictyostelium cells in relation to the contractile vacuole complex

The structure of the contractile vacuole complex of Dictyostelium discoideum has long been a subject of controversy. A model that originated from the work of John Heuser and colleagues described this osmoregulatory organelle as an interconnected array of tubules and cisternae the membranes of which are densely populated with vacuolar proton pumps. A conflicting model described this same organelle as bipartite, consisting of a pump-rich spongiome and a pump-free bladder, the latter membranes being identified by their alkaline phosphatase activity. In the present study we have employed an antiserum specific for Dictyostelium alkaline phosphatase to examine the distribution of this enzyme in vegetative cells. The antiserum labels puncta, probably vesicles, that lie at or near the plasma membrane and are sometimes, but only rarely, enriched near contractile vacuole membranes. We conclude that alkaline phosphatase is not a suitable marker for contractile vacuole membranes. We discuss these results in relation to the two models of contractile vacuole structure and suggest that all data are consistent with the first model.     

Osmoregulatory mutants that affect the function of the contractile vacuole inChlamydomonas reinhardtii

Summary Four independent osmoregulatory mutants,osml, osm3,osm4, and osm7, were isolated on the basis of their requirement for growth medium of high osmotic strength. In normal low-osmoticstrength medium, in contrast to wild-type cells, the mutants grow poorly or not at all; in distilled water mutant cells are immobilized and eventually swell and burst. The mutants were examined by ordinary brightfield and phase-contrast microscopy, videomicroscopy, and electron microscopy. The four mutants showed different defects in the contractile vacuole (CV) cycle. Timing of various stages of the CV cycle showed thatosm1 was affected primarily in the early stage of the cycle when the CV begins to grow,osm3 primarily in midcycle when vacuoles fuse to form the CV proper,osm7 at a late stage of the cycle at docking and fusion of the CV with the plasma membrane, andosm4 during contraction of the CV. At the electron microscopic level, in dilute medium, mutant cells by comparison with wild-type cells had large autophagosomes, swollen mitochondria, and dilated ER cisternae. Although electron microscopy showed general abnormalities of the contractile vacuoles consistent with the videomicroscopic observations of living cells, no obvious vacuole membrane abnormalities were seen which would explain the mutational defects. The mutations help define the separate processes that contribute to the coordinated CV cycle inChlamydomonas, and open the way to eventual isolation of some of the genes responsible for CV function.Abbreviations CV contractile vacuole - TAP Tris-acetate-phosphate medium - TAP+L medium supplemented with lactose - TAP+S medium supplemented with sucrose or other sugar     

THE FINE STRUCTURE OF ACANTHAMOEBA CASTELLANII : I. The Trophozoite

The fine structure of the trophozoite of Acanthamoeba castellanii (Neff strain) has been studied. Locomotor pseudopods, spikelike "acanthopodia," and microprojections from the cell surface are all formed by hyaline cytoplasm, which excludes formed elements of the cell and contains a fine fibrillar material. Golgi complex, smooth and rough forms of endoplasmic reticulum, digestive vacuoles, mitochondria, and the water-expulsion vesicle (contractile vacuole) are described. A canicular system opening into the water-expulsion vesicle contains tubules about 600 A in diameter that are lined with a filamentous material. The tubules are continuous with unlined vesicles or ampullae of larger diameter. Centrioles were not observed, but cytoplasmic microtubules radiate from a dense material similar to centriolar satellites and are frequently centered in the Golgi complex. Cytoplasmic reserve materials include both lipid and glycogen, each of which amounts to about 10% of the dry weight.     

Ultrastructural Aspects of the Somatic Cortex and Contractile Vacuole of the Ciliate,Ichthyophthirius multifiliis Fouquet1

The trophont stage in the life cycle of Ichthyophthirius multifiliis was studied in the electron microscope. Surface ridges contain up to 24 ridge microtubules, disposed as a ribbon. Kinetosomes show the classic morphology of 9 triplets of microtubules. Associated with each kinetosome is a kinetodesmal fibril, originating in proximity to triplets 5, 6, and 7, and having a 30 nm periodicity; 3 to 5 postciliary microtubules, originating between triplets 8 and 9; and up to 3 transverse microtubules, originating at triplet 4, as well as a parasomal sac. Each cell is partially enclosed by a system of 3 “unit” membranes: the outer limiting membrane, and the outer and inner alveolar membranes. The last two membranes define the alveolar sac. Mucocysts, each with a dense core, are present in large numbers. The contractile vacuole system includes the contractile vacuole, associated tubules and vesicles, injection canals, a discharge canal, and a pore. Microtubules abound in the walls of the contractile vacuole, injection and discharge canals, and in the region of the pores, where both ring and radial microtubular arrangements are noted. The ultrastructure suggests that I. multifiliis is more closely related to Tetrahymena pyriformis than to Paramecium aurelia.