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Publication : From lysosomes to the plasma membrane: localization of vacuolar-type H+ -ATPase with the a3 isoform during osteoclast differentiation.

First Author  Toyomura T Year  2003
Journal  J Biol Chem Volume  278
Issue  24 Pages  22023-30
PubMed ID  12672822 Mgi Jnum  J:83868
Mgi Id  MGI:2664004 Doi  10.1074/jbc.M302436200
Citation  Toyomura T, et al. (2003) From Lysosomes to the Plasma Membrane: Localization of vacuolar type H+-ATPase with the a3 isoform during osteoclast differentiation. J Biol Chem 278(24):22023-30
abstractText  Osteoclasts generate a massive acid flux to mobilize bone calcium. Local extracellular acidification is carried out by vacuolar type H+-ATPase (V-ATPase) localized in the plasma membrane. We have shown that a3, one of the four subunit a isoforms (a1, a2, a3, and a4), is a component of the plasma membrane V-ATPase (Toyomura, T., Oka, T., Yamaguchi, C., Wada, Y., and Futai, M. (2000) J. Biol. Chem. 275, 8760-8765). To establish the unique localization of V-ATPase, we have used a murine macrophage cell line, RAW 264.7, that can differentiate into multinuclear osteoclast-like cells on stimulation with RANKL (receptor activator of nuclear factor kappaB ligand). The V-ATPase with the a3 isoform was localized to late endosomes and lysosomes, whereas those with the a1 and a2 isoforms were localized to organelles other than lysosomes. After stimulation, the V-ATPase with the a3 isoform was immunochemically colocalized with lysosome marker lamp2 and was detected in acidic organelles. These organelles were also colocalized with microtubules, and the signals of lamp2 and a3 were dispersed by nocodazole, a microtubule depolymerizer. In RAW-derived osteoclasts cultured on mouse skull pieces, the a3 isoform was transported to the plasma membrane facing the bone and accumulated inside podosome rings. These findings indicate that V-ATPases with the a3 isoform localized in late endosomes/lysosomes are transported to the cell periphery during differentiation and finally assembled into the plasma membrane of mature osteoclasts.
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