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Biophys J, November 2002, p. 2502-2510, Vol. 83, No. 5

and
Departments of *Surgery,
Biomedical Engineering, and
Mechanical Engineering and Materials Science, Duke
University Medical Center, Durham, North Carolina 27710 USA
Loading of the spine alters the osmotic environment in
the intervertebral disk (IVD) as interstitial water is expressed from the tissue. Cells from the three zones of the IVD, the anulus fibrosus
(AF), transition zone (TZ), and nucleus pulposus (NP), respond to
osmotic stress with altered biosynthesis through a pathway that may
involve calcium (Ca2+) as a second messenger. We examined
the hypothesis that IVD cells respond to hyperosmotic stress by
increasing the concentration of intracellular calcium
([Ca2+]i) through a mechanism involving
F-actin. In response to hyperosmotic stress, control cells from all
zones decreased in volume and cells from the AF and TZ exhibited
[Ca2+]i transients, while cells from the NP
did not. Extracellular Ca2+ was necessary to initiate
[Ca2+]i transients. Stabilization of F-actin
with phalloidin prevented the Ca2+ response in AF and TZ
cells and decreased the rate of volume change in cells from all zones,
coupled with an increase in the elastic moduli and apparent viscosity.
Conversely, actin breakdown with cytochalasin D facilitated
Ca2+ signaling while decreasing the elastic moduli and
apparent viscosity for NP cells. These results suggest that
hyperosmotic stress induces volume change in IVD cells and may initiate
[Ca2+]i transients through an actin-dependent mechanism.
Biophys J, November 2002, p. 2502-2510, Vol. 83, No. 5
© 2002 by the Biophysical Society 0006-3495/02/11/2502/09 $2.00
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