K+-induced swelling of vestibular dark cells is dependent on Na+ and Cl? and inhibited by piretanide

1990 ◽  
Vol 416 (3) ◽  
pp. 262-269 ◽  
Author(s):  
Philine Wangemann ◽  
Daniel C. Marcus
1992 ◽  
Vol 262 (6) ◽  
pp. C1423-C1429 ◽  
Author(s):  
D. C. Marcus ◽  
S. Takeuchi ◽  
P. Wangemann

Patch-clamp recordings were made on cell-attached and excised apical membrane from dark cells of the semicircular canal of the gerbil. These cells are thought to secrete K+ and absorb Na+ from the luminal fluid (endolymph). Single-channel events were identified as being equally conductive (27.6 +/- 0.4 pS; n = 48) for K+, Na+, Rb+, Li+, and Cs+ and 1.4 times more permeable to NH4+ but not permeable to Cl-, Ca2+, Ba2+, nor to N-methyl-D-glucamine. The channels displayed linear current-voltage relations that passed nearly through the origin (intercept: -2.6 +/- 0.5 mV; n = 48) when conductive monovalent cations were present on both sides of the membrane in equal concentrations. Channel activity required the presence of Ca2+ at the cytosolic face; there was no activity at less than or equal to 10(-7) M Ca2+ and full activity at greater than or equal to 10(-5) M Ca2+. Cell-attached recordings had a mean reversal voltage of -36.4 +/- 7.9 mV (n = 7), which was interpreted to reflect the intracellular potential of dark cells under the present conditions. We have identified a nonselective cation channel in the apical membrane of vestibular dark cells that might participate in K+ secretion or Na+ absorption under stimulated conditions, but the density appears to be insufficient to fully account for the transepithelial K+ flux.


1996 ◽  
Vol 94 (1-2) ◽  
pp. 94-106 ◽  
Author(s):  
Philine Wangemann ◽  
Jianzhong Liu ◽  
Nobuyuki Shiga

1995 ◽  
Vol 115 (sup519) ◽  
pp. 140-142 ◽  
Author(s):  
Mamoru Fujii ◽  
Yasuo Harada ◽  
Katsuhiro Hirakawa ◽  
Masaya Takumida

1973 ◽  
Vol 82 (1) ◽  
pp. 23-35 ◽  
Author(s):  
David J. Lim

Although mammalian otoconia are known to be composed of calcium carbonate in calcite form, their morphogenesis, maintenance, and fate are not well understood. More information on these problem areas would aid considerably in better understanding various clinical conditions, such as cupulolithiasis and otolith degeneration. This study was intended to clarify the fine morphology of the otolith in normal and adverse conditions in laboratory animals with the use of the scanning and transmission electron microscopes. It was confirmed by this study that the mammalian otoconium is composed of an organic matrix and minerals (calcium carbonate). When the minerals are removed by decalcification, or chelation, a well arranged organic matrix, and even a nucleus, can be found in the crystal. The matrix of the crystal is identical to the gelatin matrix of the otolithic membrane. This finding supports the possibility that a normal protein matrix is a prerequisite for normal otoconia formation, and that the exchange of calcium ions can occur without altering the crystal structure. The vestibular dark cells, which are thought to be endolymph-secreting cells, appear to be capable of removing calcium from the otoconia that are attached to the dark cell surfaces. Although this evidence is only circumstantial, its consistency is impressive. On the basis of the foregoing, it is tempting to speculate that the dark cells participate in the removal of the dislodged otoliths, but further study is required to ascertain this point.


2001 ◽  
Vol 153 (1-2) ◽  
pp. 132-145 ◽  
Author(s):  
Marie-Thérèse Nicolas ◽  
Danielle Demêmes ◽  
Agnès Martin ◽  
Sabina Kupershmidt ◽  
Jacques Barhanin

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