Caffeine-Induced Ca²⁺ Transients and Exocytosis in Paramecium Cells. A Correlated Ca²⁺ Imaging and Quenched-Flow/Freeze-Fracture Analysis

Abstract.

Caffeine causes a [Ca²⁺] _i increase in the cortex of Paramecium cells, followed by spillover with considerable attenuation, into central cell regions. From [Ca²⁺]^rest _i ∼50 to 80 nm, [Ca²⁺]^act _i rises within ≤3 sec to 500 (trichocyst-free strain tl) or 220 nm (nondischarge strain nd9–28°C) in the cortex. Rapid confocal analysis of wildtype cells (7S) showed only a 2-fold cortical increase within 2 sec, accompanied by trichocyst exocytosis and a central Ca²⁺ spread during the subsequent ≥2 sec. Chelation of Ca²⁺ _o considerably attenuated [Ca²⁺] _i increase. Therefore, caffeine may primarily mobilize cortical Ca²⁺ pools, superimposed by Ca²⁺ influx and spillover (particularly in tl cells with empty trichocyst docking sites). In nd cells, caffeine caused trichocyst contents to decondense internally (Ca²⁺-dependent stretching, normally occurring only after membrane fusion). With 7S cells this usually occurred only to a small extent, but with increasing frequency as [Ca²⁺] _i signals were reduced by [Ca²⁺] _o chelation. In this case, quenched-flow and ultrathin section or freeze-fracture analysis revealed dispersal of membrane components (without fusion) subsequent to internal contents decondensation, opposite to normal membrane fusion when a full [Ca²⁺] _i signal was generated by caffeine stimulation (with Ca²⁺ _i and Ca²⁺ _o available). We conclude the following. (i) Caffeine can mobilize Ca²⁺ from cortical stores independent of the presence of Ca²⁺ _o . (ii) To yield adequate signals for normal exocytosis, Ca²⁺ release and Ca²⁺ influx both have to occur during caffeine stimulation. (iii) Insufficient [Ca²⁺] _i increase entails caffeine-mediated access of Ca²⁺ to the secretory contents, thus causing their decondensation before membrane fusion can occur. (iv) Trichocyst decondensation in turn gives a signal for an unusual dissociation of docking/fusion components at the cell membrane. These observations imply different threshold [Ca²⁺] _i -values for membrane fusion and contents discharge.