Sehring IM, Plattner H. Ca2+ oscillations mediated by exogenous GTP in Paramecium cells: assessment of possible Ca2+ sources.
Cell Calcium 2005;
36:409-20. [PMID:
15451624 DOI:
10.1016/j.ceca.2004.04.001]
[Citation(s) in RCA: 11] [Impact Index Per Article: 0.6] [Reference Citation Analysis] [Abstract] [MESH Headings] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Received: 01/23/2004] [Revised: 02/27/2004] [Accepted: 04/05/2004] [Indexed: 11/20/2022]
Abstract
We applied exogenous guanosine trisphosphate, GTP, to Paramecium tetraurelia cells injected with Fura Red for analysing changes of free intracellular Ca(2+) concentrations, [Ca(2+)](i), during periodic back-/forward swimming thus induced. Strain ginA (non-responsive to GTP) shows no Ca(2+) signal upon GTP application. In strain nd6 (normal Ca(2+) signalling) an oscillating [Ca(2+)](i) response with a prominent first peak occurs upon GTP stimulation, but none after mock-stimulation or after 15 min adaptation to GTP. While this is in agreement with previous electrophysiological analyses, we now try to identify more clearly the source(s) of Ca(2+). Stimulation of nd6 cells, after depletion of Ca(2+) from their cortical stores (alveolar sacs), shows the same Ca(2+) oscillation pattern but with reduced amplitudes, and a normal behavioural response is observed. Stimulation with GTP, supplemented with the Ca(2+) chelator BAPTA, results in loss of the first prominent Ca(2+) peak, in reduction of the following Ca(2+) amplitudes, and in the absence of any behavioural response. Both these observations strongly suggest that for the initiation of GTP-mediated back-/forward swimming Ca(2+) from the extracellular medium is needed. For the maintenance of the Ca(2+) oscillations a considerable fraction must come from internal stores, probably other than alveolar sacs, rather likely from the endoplasmic reticulum.
Collapse