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Inositol 1,3,4,5-tetrakisphosphate-induced Ca2+ sequestration into bovine adrenal-medullary secretory vesicles.

ABSTRACT: Ins(1,3,4,5)P4 induced a rapid sequestration of Ca2+ into both secretory vesicles and microsomes of bovine adrenal medulla. The Ca(2+)-sequestering role of Ins(1,3,4,5)P4 contrasts with the Ca(2+)-releasing role of Ins(1,4,5)P3 in adrenal-medullary secretory vesicles and microsomes. The Ins(1,3,4,5)P4-induced Ca2+ sequestration into secretory vesicles was not inhibited by heparin (50 micrograms/ml), whereas Ins(1,4,5)P3-induced Ca2+ release was completely inhibited, indicating two different receptors for Ins(1,4,5)P3 and Ins(1,3,4,5)P4. Furthermore, Ins(1,3,4,5)P4 was as effective at 4 degrees C as at 24 degrees C in sequestering Ca2+ into secretory vesicles, implying Ca2+ sequestration through receptor-operated Ca2+ channels or activation of the Ca(2+)-exchange mechanism by Ins(1,3,4,5)P4. The Ca(2+)-sequestering activity of Ins(1,3,4,5)P4 has also been demonstrated with 45Ca2+; 10 microM-Ins(1,3,4,5)P4 induced rapid uptake of 45Ca2+ into secretory vesicles optimized for Ca2+ uptake, whereas 10 microM-Ins(1,4,5)P3 induced 45Ca2+ release from secretory vesicles in similar experiments.

SUBMITTER: Yoo SH

PROVIDER: S-EPMC1151353 | biostudies-other | 1991 Sep

REPOSITORIES: biostudies-other

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Project description:Inositol-polyphosphate-induced Ca2+ mobilization was investigated in saponin-permeabilized SH-SY5Y human neuroblastoma cells. Ins(1,4,5)P3 induced a dose-related release from intracellular Ca2+ stores with an EC50 (concn. giving half-maximal effect) of 0.1 microM and a maximal release of 70%. Ins(1,3,4)P3, DL-Ins(1,4,5,6)P4 and Ins(1,3,4,5,6)P5 did not evoke Ca2+ mobilization in these cells when used at concentrations up to 10 microM. However, Ins(1,3,4,5)P4 was found to release Ca2+ in a dose-related manner, but the response was dependent on the source of Ins(1,3,4,5)P4 used. When commercially available D-Ins(1,3,4,5)P4 was used, the EC50 and maximal response values were 1 microM and 50% respectively, compared with values for chemically synthesized DL-Ins(1,3,4,5)P4 of 2 microM and 25%. The enhanced maximal response of commercial D-Ins(1,3,4,5)P4 was decreased by pretreatment with rat brain crude Ins(1,4,5)P3 3-kinase and was therefore concluded to be indicative of initial Ins(1,4,5)P3 contamination of the Ins(1,3,4,5)P4 preparation. When metabolism of DL-Ins(1,3,4,5)P4 (10 microM) in these cells at 25 degrees C was investigated by h.p.l.c., substantial amounts of Ins(1,4,5)P3 (0.2 microM) and Ins(1,3,4)P3 (0.8 microM) were found to be produced within 3 min. Analysis of DL-Ins(1,3,4,5)P4 incubation with cells at 4 degrees C, however, indicated that metabolism had been arrested ([3H]Ins(1,4,5)P3 detection limits were estimated to be approx. 0.01 microM). When chemically synthesized DL-Ins(1,3,4,5)P4 and incubation conditions of low temperature were used, the Ca2(+)-releasing properties of this compound were established to be 1 microM and 19% for the EC50 and maximal response values respectively. The results obtained strongly suggest that Ins(1,3,4,5)P4 alone has the ability to release intracellular Ca2+. However, in the presence of sub-maximal concentrations of Ins(1,4,5)P3, Ca2+ release appears to be synergistic with Ins(1,3,4,5)P4, but at supramaximal concentrations not even additive effects are observed.

Project description:L1210 lymphoma cells were permeabilized with digitonin, and the ability of Ins(2,4,5)P3 and Ins(1,3,4,5)P4 to mobilize intracellular Ca2+ was studied. At high doses of Ins(2,4,5)P3 Ca2+ was rapidly released from intracellular stores, and prior or subsequent addition of Ins(1,3,4,5)P4 had no discernible effect. However, the Ca2(+)-mobilizing action of low (threshold or just above) concentrations of Ins(2,4,5)P3 was markedly enhanced by Ins(1,3,4,5)P4, which alone caused no mobilization of Ca2+; this phenomenon was shown not to be due to protection of Ins(2,4,5)P3 by the Ins(1,3,4,5)P4 against hydrolysis. The ability of the pre-addition of Ins(1,3,4,5)P4 to enhance subsequent Ins(2,4,5)P3-induced Ca2+ mobilization was always seen whether or not the free Ca2+ concentration was low (pCa = 7) or high (pCa = 6). However, at low Ca2+, Ins(1,3,4,5)P4 could cause a further mobilization if added after the Ins(2,4,5)P3, whereas at higher Ca2+ values Ins(1,3,4,5)P4 was only able to affect Ca2+ if added before Ins(2,4,5)P3. These effects of Ins(1,3,4,5)P4 were not, at the same concentration, mimicked by a random mixture of InsP4 isomers obtained by partial acid hydrolysis of phytic acid, by Ins(1,3,4)P3 or by Ins(1,3,4,5,6)P5, and they were shown not to be due to enzymic generation of Ins(1,4,5)P3 from Ins(1,3,4,5)P4 by (a) the absence of any detectable production of Ins(1,4,5)P3 if radiolabelled Ins(1,3,4,5)P4 was used, or (b) the observation that Ins(1,3,4,5,6)P5 could mimic Ins(1,3,4,5)P4 provided that higher doses were used; this inositol phosphate, when added radiolabelled, yielded only trace quantities of D/L-Ins(1,4,5,6)P4, which itself does not mobilize Ca2+. We interpret these results overall to mean that in these cells there is a small proportion of the Ins(2,4,5)P3-mobilizable Ca2+ pools which can only be mobilized in the presence of Ins(1,3,4,5)P4 [or at the least, Ins(1,3,4,5)P4 can help Ins(2,4,5)P3 to gain access to them]. The significance of this conclusion is discussed in the light of current concepts of the second messenger function of Ins(1,3,4,5)P4.

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Inositol 1,3,4,5-tetrakisphosphate-induced Ca2+ sequestration into bovine adrenal-medullary secretory vesicles.

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