In the human T-lymphocyte cell lines Jurkat and HPB.ALL and the human monocytoid cell line U937, Ins(1,3,4,5)P4 triggers a dose-dependent release of Ca2+ from crude microsomal preparations, with a half-maximal effective concentration (EC50) of 1.2-2.3 microM. Similar results were obtained with enriched vesicular plasma membranes from U937 cells. However, in permeabilized preparations of the same cell types only Ins(1,4,5)P3 was able to release Ca2+ from intracellular stores, with EC50 values in the range 0.11-0.84 microM. In crude microsomes the effects of Ins(1,3,4,5)P4 and Ins(2,4,5)P3, a non-metabolizable InsP3 isomer, occurred independently of each other, indicating subpopulations of Ins(1,3,4,5)P4- and Ins(1,4,5)P3-sensitive vesicles. The Ins(1,3,4,5)P4 preparation used for the Ca(2+)-release experiments contains neither Ca2+ nor contaminating Ins(1,4,5)P3 and was not metabolized to Ins(1,4,5)P3 during the Ca(2+)-release experiments. We conclude that Ins(1,3,4,5)P4 independently of Ins(1,4,5)P3 induces a Ca2+ flux via a membrane compartment, most likely the plasma membrane, that is functionally destroyed during the permeabilization of the cells.
No takes yet. Share an insight, caveat, or question.
Guse et al. (1992) studied this question.
Synapse has enriched 3 closely related papers on similar clinical questions. Consider them for comparative context: