Imaging of multicellular large-scale rhythmic calcium waves during zebrafish gastrulation.

Oscillations of cytosolic free calcium levels have been shown to influence gene regulation and cell differentiation in a variety of model systems. Intercellular calcium waves thus present a plausible mechanism for coordinating cellular processes during embryogenesis. Herein we report use of aequorin and a photon imaging microscope to directly observe a rhythmic series of intercellular calcium waves that circumnavigate zebrafish embryos over a 10-h period during gastrulation and axial segmentation. These waves first appeared at about 65% epiboly and continued to arise every 5-10 min up to at least the 16-somite stage. The waves originated from loci of high calcium activity bordering the blastoderm margin. Several initiating loci were active early in the wave series, whereas later a dorsal marginal midline locus predominated. On completion of epiboly, the dorsal locus was incorporated into the developing tail bud and continued to generate calcium waves. The locations and timing at which calcium dynamics are most active appear to correspond closely to embryonic cellular and syncytial sites of known morphogenetic importance. The observations suggest that a panembryonic calcium signaling system operating in a clock-like fashion might play a role during vertebrate axial patterning.

Localized calcium transients accompany furrow positioning, propagation, and deepening during the early cleavage period of zebrafish embryos.

Through the injection of f-aequorin (a calcium-specific luminescent reporter) and the use of an imaging photon detector, we see a distinct localized elevation of intracellular calcium that accompanies the appearance of the first furrow arc at the blastodisc surface: the furrow positioning signal. As the leading edges of the arc progress outward toward the margins of the blastodisc, they are accompanied by two subsurface slow calcium waves moving at about 0.2 micron/s: the furrow propagation signal. As these wave fronts approach the edge of the blastodisc, another calcium signal arises in the central region where the positioning signal originally appeared. Like the propagation signal, it extends outward to the margins of the blastodisc, but in this case it also moves downward, accompanying the deepening process that separates the daughter cells: the furrow deepening signal. Both of these furrow deepening progressions move at around 0.1 to 0.2 micron/s. The deepening signal begins to diminish from the center outward, returning to precleavage resting levels on completion of cytokinesis. The signaling sequence is repeated during the second cell division cycle. These localized transients do not require external calcium and they can be dissipated after they have begun by introducing calcium shuttle buffers, resulting in furrow delocalization and regression. They also occur in parthenogenetically activated eggs in which, in an attenuated form, they accompany abortive cleavages.

Analysis of the calcium transient at NEB during the first cell cycle in dividing sea urchin eggs.

Accumulating evidence from several systems suggests that nuclear envelope breakdown (NEB) is triggered by an endogenous transient of free calcium. Using h- and f-semisynthetic aequorins as cytosolic calcium indicators, we have clearly and regularly visualized a single large, global calcium transient just before first NEB in normally developing, monospermic Lytechinus eggs. Although similar transients were not observed at NEB in subsequent cell cycles, microinjection of the calcium buffer BAPTA into one blastomere of the two-celled embryo resulted in the inhibition of NEB. The NEB transient in the first cell cycle was some five-fold smaller than the one associated with egg activation. Our data suggest that this transient takes the form of a calcium wave that spreads inwards from the periphery of the egg toward the nucleus. We confirmed that these NEB transients did not require extracellular Ca2+. In polyspermic eggs, NEB-associated transients were four-fold larger than in monospermic eggs and were periodically repeated. Examination of the distribution of fluorescein-conjugated aequorins with a laser scanning confocal microscope indicated that aequorin both enters the nucleus and is evenly distributed within the cytosol of the egg. The use of h- and f-aequorins did not reveal any NEB transients during subsequent cell cycles, nor did we detect transients associated with other cell cycle events. However, a complex train of calcium transients in the form of both localized pulses and propagated waves was detected from embryos beginning at about the morula-to-blastula transition and continuing through to hatching.

Bicarbonate dependence of ion current in damaged bone.

The aim of this work was to characterize the ion current that enters mouse metatarsal bones following damage to the cortex. We assessed both the spatial distribution of this current and its dependence on the presence of bicarbonate in the medium. We used a voltage-sensitive probe system vibrating in two dimensions and recorded the signal as function of the position of the probe with respect to the site of damage and of ion substitutions in the medium. When the cortex was damaged (50 microm cylindrical hole penetrating into the marrow cavity), we recorded a steady state net inward electrical current directed toward the site of damage. In nonbicarbonate media, the density of the current was maximal near the center of the hole and ranged from 6 to 18 microA/cm2. As the probe was moved off the center of the hole, measured current density decreased in a manner consistent with the hypothesis that the source of the inward current is localized to the hole. After changing bicarbonate concentration in the medium from 0 to 42 mM, the current density nearly doubled, then decayed back to its original level exponentially over 35 minutes. When the diaphysis of living bone was left intact the current density was close to background level either in the presence or absence of bicarbonate in the medium. Damaged dead bone did not drive any current higher than background level. We conclude that the vibrating probe technique is a powerful tool to characterize ion currents in injured bone, helping to understand the physiology of bone-plasma interface and the bone healing processes. The current density transiently doubled upon addition of bicarbonate, indicating that this ion may carry the electrical current in damaged bone, probably by pump-leak mechanisms operating at the bone-plasma interface.