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We examined the pattern of inorganic orthophosphate (PPi) ion distribution in dividing cells of Zea mays root-tips. Unfixed and paraformaldehyde- or glutaraldehyde-vapor fixed tissues were immersed in lead acetate, glutaraldehyde, and cacodylate buffer to capture PPi as insoluble orthophosphate lead hydroxyapatite. Excess lead ions were removed with sodium citrate, then permeabilized in ammonia. Precipitates were stained with potassium sulfide, washed with distilled water and squashed in a drop of glycerin. The accumulation of PPi ions was cyclic in the cytoplasm during mitosis and they surrounded all chromosomes during metaphase and anaphase. Partition between dividing cells started with a high concentration of PPi ions at sites where plasma membrane and cell walls formed. Small daughter cells and those in G1 phase had PPi concentrated in the nucleolus, with lower levels elsewhere in the nucleus. Later in the cell cycle, there were greater amounts of PPi ions associated with condensed chromatin in larger nuclei. In Xenopus laevis oocytes, PPi was concentrated in the nucleus, mainly in the active central core of multiple nucleoli. These results and others indicate that compartmentalization of PPi occurs in the intact cell and correlates with the rate of transcription in distinct functional domains within the nucleus.

Potassium pyroantimonate, when used as fixative (saturated or half-saturated, without addition of any conventional fixative) has been demonstrated to produce intracellular precipitates of the insoluble salts of calcium, magnesium, and sodium and to preserve the general cell morphology. In both animal and plant tissues, the electron-opaque antimonate precipitates were found deposited in the nucleus-as well as within the nucleolus-and in the cytoplasm, largely at the site of the ribonucleoprotein particles; the condensed chromatin appeared relatively free of precipitates. The inorganic cations are probably in a loosely bound state since they are not retained by conventional fixatives. The implications of this inorganic cation distribution in the intact cell are discussed in connection with their anionic counterparts, i.e., complexing of cations by fixed anionic charges and the coexistence of a large pool of inorganic orthophosphate anions in the nucleus and nucleolus.

Lead acetate treatment of unfixed cells immobilizes the intracellular water-soluble, inorganic orthophosphate ions as microcrystalline lead hydroxyapatite precipitates (see reference 1). These precipitates have been analyzed with the electron microprobe. A much higher concentration of phosphorus has been found in the nucleoli of maize root tip cells fixed in lead acetate-glutaraldehyde (organic phosphorus plus inorganic orthophosphate), as compared to the nucleoli of roots fixed in glutaraldehyde alone (organic phosphorus). The concentration of the inorganic orthophosphate pool in these nucleoli is three to five times as high as the concentration of the macromolecular organic phosphate. Since nearly all of the latter is in RNA, the concentration of inorganic phosphate in the nucleolus is calculated to be roughly 0.5-0.8 M. About 30%-and up to 50%-of the total cellular inorganic phosphate is accumulated in the nucleolus since the mean concentration per cell is about 10(-2)M. In the extranucleolar part of the nucleus the mean concentration was estimated by densitometry to be roughly six times less than in the nucleolus ( 0.1 M), and appears more concentrated in the nucleoplasm than in the condensed chromatin. While there is no direct evidence for the concentration in the cytoplasm, it certainly must be much lower than the mean cellular level (i.e., < 10(-2)M) since the nucleus is about 10% of the total cell volume. The implications of this compartmentation in the intact cell are discussed in connection with (A) the availability of orthophosphate ions for the cytoplasm in those processes in which these ions affect the rate of enzymatic reactions, and (B) protein nucleic acid interactions within the nucleus and nucleolus.

Earlier reports indicated the presence of significant amounts of inorganic salts in the nucleus. In the present study the possibility that this might be related to the transcription process was tested on seminiferous epithelium of the adult mouse, using potassium pyroantimonate as a fixative. The results indicated that a correlation exists between the inorganic cations comprising the pyroantimonate-precipitable fraction and the RNA synthetic activity. During meiotic prophase an accumulation of cation-antimonate precipitates occurs dispersed through the middle pachytene nuclei, the stage in which RNA synthesis reaches a maximum. At other stages (zygotene to diplotene), where RNA synthesis falls to a low level, that pattern is not seen; cation-antimonate deposits are restricted to a few masses in areas apparently free of chromatin. The condensed sex chromosomes, the heterochromatin of the "basal knobs," the axial elements, and the synaptonemal complexes are devoid of antimonate deposits during the meiotic prophase. The Sertoli cells, active in RNA synthesis in both nucleoplasm and nucleolus, show cation-antimonate deposits at these sites. In the nucleoplasm some "patches" of precipitates appear coincident with clusters of interchromatin granules; in the nucleolus the inorganic cations are mainly located in the fibrillar and/or amorphous areas, whereas relatively few are shown by the granular component. The condensed chromatin bodies associated with the nucleolus were always free of antimonate precipitates. It is suggested that the observed sites of inorganic cation accumulation within the nucleus may at least partially indicate the presence of RNA polymerases, the activity of which is dependent on divalent cations.