Laser-scanning confocal microscopy was used in conjunction with a high
ly fluorescent Ca2+ indicator fluo-3 to visualize real-time alteration
s in the intracellular Ca2+ concentration ([Ca2+](i)) in individual li
ving Jurkat T-cells during the first minutes of activation by phytohae
magglutinin (PHA) at the physiological temperature (37 degrees C). Wit
h a delay of 30-120 s, PHA induced a strong [Ca2+](i) peak in the micr
omolar range (1-3 mu M). The rise in [Ca2+](i) lasted for 1-2 minutes,
and was followed by a sustained plateau of elevated [Ca2(+)](i) in th
e 0.2-0.5 mu M range. Some cells (10-20%) responded with additional as
ynchronous 0.5-1.5 mu M peaks during the plateau phase. These oscillat
ions continued for 10-20 minutes. The spans of the peaks ranged from 3
0 to 100 s, intervals between peaks varied from 60 to 300 s. It was sh
own that the initial [Ca2+](i) peak was associated with Ca2+ mobilisat
ion from internal sources, whereas the plateau was maintained by an in
flux of Ca2+ from external medium. In K+-rich medium or in the presenc
e of quinine, a K+ channel blocker, no secondary response to PHA-activ
ation characterised by an elevated plateau was observed. The data sugg
est that the Ca2+ influx was dependent on the membrane potential and/o
r the extracellular K+-concentration. Optical sectioning showed that t
he intracellular Ca2+ distributed almost homogeneously throughout the
cell volume both in control and in PHA-stimulated cells including thos
e exhibiting Ca2+ oscillations. This suggests that Ca2+ signals are lo
calized not only in cytoplasm at the cell plasma membrane but can be a
lso transferred directly into the nucleus.