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The Actin‐Binding Protein Cofilin and Its Interaction With Cortactin Are Required for Podosome Patterning in Osteoclasts and Bone Resorption In Vivo and In Vitro
Author(s) -
Zalli Detina,
Neff Lynn,
Nagano Kenichi,
Shin Nah Young,
Witke Walter,
Gori Francesca,
Baron Roland
Publication year - 2016
Publication title -
journal of bone and mineral research
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 1.882
H-Index - 241
eISSN - 1523-4681
pISSN - 0884-0431
DOI - 10.1002/jbmr.2851
Subject(s) - podosome , cofilin , cortactin , microbiology and biotechnology , bone resorption , chemistry , actin , cytoskeleton , actin cytoskeleton , biology , biochemistry , cell , genetics
The adhesion of osteoclasts (OCs) to bone and bone resorption require the assembly of specific F‐actin adhesion structures, the podosomes, and their dense packing into a sealing zone. The OC‐specific formation of the sealing zone requires the interaction of microtubule (MT) + ends with podosomes. Here, we deleted cofilin, a cortactin (CTTN)‐ and actin‐binding protein highly expressed in OCs, to determine if it acts downstream of the MT‐CTTN axis to regulate actin polymerization in podosomes. Conditional deletion of cofilin in OCs in mice, driven by the cathepsin K promoter (Ctsk‐Cre), impaired bone resorption in vivo, increasing bone density. In vitro, OCs were not able to organize podosomes into peripheral belts. The MT network was disorganized, MT stability was decreased, and cell migration impaired. Active cofilin stabilizes MTs and allows podosome belt formation, whereas MT disruption deactivates cofilin via phosphorylation. Cofilin interacts with CTTN in podosomes and phosphorylation of either protein disrupts this interaction, which is critical for belt stabilization and for the maintenance of MT dynamic instability. Accordingly, active cofilin was required to rescue the OC cytoskeletal phenotype in vitro. These findings suggest that the patterning of podosomes into a sealing zone involves the dynamic interaction between cofilin, CTTN, and the MTs + ends. This interaction is critical for the functional organization of OCs and for bone resorption. © 2016 American Society for Bone and Mineral Research.

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