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Fig. 9. Tentative model for intracellular Ca2+ storage and generation of [Ca2+]i signals and cellular responses in progesterone-stimulated human spermatozoa. The initial [Ca2+]i transient that occurs immediately upon application of progesterone is mediated primarily by Ca2+-influx and induces acrosome reaction in a proportion of cells (grey arrow). Ca2+ is removed from the cytoplasm primarily by pumping at the plasma membrane (PMCA and Na+-Ca2+ exchanger, blue). Acrosome reaction may involve mobilisation of Ca2+ stored in the acrosome itself (De Blas et al., 2002; Herrick et al., 2005). Sustained elevation of [Ca2+]i, which follows the transient (or can be induced by a progesterone concentration gradient to simulate approach to the oocyte, a procedure that induces [Ca2+]i oscillations without a preceding [Ca2+]i transient) (Harper et al., 2004), acts on RyRs (red) on a Ca2+ store in the caudal part of the head or midpiece, causing Ca2+-induced Ca2+ release. Cyclic release and re-uptake occur as a result of refilling of this store by bis-phenol-sensitive SPCA1 (green), generating slow [Ca2+]i oscillations at the base of the flagellum and causing alternation of flagellar beat pattern (grey arrow).





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