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Summary.The contractile vacuole (CV) cycle of Chlamydomonas 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 of Chlamydornonas, 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.
Summary.The contractile vacuole (CV) cycle of Chlamydomonas 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 of Chlamydornonas, 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.
The pressure response of (plant) cells to osmotic challenges depends on the reflection coefficient, sigma, of osmotically active solutes; it is less than predicted by the van't Hoff equation if sigma < 1. In Valonia utricularis, sigma is significantly reduced by internal (and, to a lesser extent, by external) unstirred layers, protecting the cytoplasm against vacuolar osmotic fluctuations. As shown by scanning and transmission electron microscopy, diffusion-restricted spaces are formed by innumerable small vacuoles that are interconnected with each other and with the central vacuole. They are embedded in networks of cytoplasmic strands connecting and encircling the organelles. Unstirred layers are also created in the central vacuole by an extensive network of acid mucopolysaccharide filaments (visualized by alcian blue staining). Mucopolysaccharides apparently also affect steady-state turgor by reducing the water activity. When the effective vacuolar osmotic pressure was adjusted to that of the bath by perfusion with an artificial vacuolar sap (AVS), an "offset turgor pressure" of 17 +/- 5 kPa was recorded. Consistent with the ultrastructural data, sigma values less than unity were calculated from the pressure response upon vacuolar addition of KCl or sucrose by perfusion (sigma(iKCl) = 0.63 +/- 0.13; sigma(isuc) = 0.58 +/- 0.17). Dilution of AVS yielded slightly higher sigma(iKCl) values (0.73 +/- 0.35). External addition to the artificial sea water (ASW) indicated that sigma(e) > sigma(i) for these osmotica. However, even in this case, sigma(esuc) (0.86 +/- 0.09) and sigma(ePEG) (0.58 +/- 0.08) were significantly less than sigma(eNaCl) (0.94 +/- 0.05) and sigma(eKCl) (0.91 +/- 0.13), presumably due to unstirred layers within the 4 micro m thick cell wall. Consistent with the low sigma values, a partial replacement of NaCl by osmotically equivalent amounts of sucrose (ASW(suc)), PEG and dextran, respectively, as well as replacement of Cl(-) by the large anion MES(-) induced an 'anomalous' hyposmotic turgor pressure response followed by the usual backregulation of pressure. After a 2-day preincubation in ASW(suc), significantly lower sigma(e) values were obtained both hyperosmotically (sigma(eNaCl) = 0.78 +/- 0.14; sigma(esuc) = 0.72 +/- 0.15) and hyposmotically (sigma(eNaCl) = 0.70 +/- 0.17; sigma(esuc) = 0.63 +/- 0.09), probably due to long-term effects on membrane structure to be elucidated yet. The freshwater alga Chara corallina lacked these apparently closely related structural and biophysical features of Valonia.
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