Cofilin Activation during Podosome Belt Formation in Osteoclasts

Podosomes are dynamic actin-based structures found constitutively in cells of monocytic origin such as macrophages, dendritic cells and osteoclasts. They have been involved in osteoclast cell adhesion, motility and matrix degradation, and all these functions rely on the ability of podosomes to form supra-molecular structures called podosome belts or sealing zones on mineralized substrates. Podosomes contain two distinct domains, an actin-rich core enriched in actin polymerization regulators, surrounded by a ring of signaling and plaque molecules. The organization of podosome arrays into belts is linked to actin dynamics. Cofilin is an actin-severing protein that is known to regulate cytoskeleton architecture and cell migration. Cofilin is present in lamellipodia and invadopodia where it regulates actin polymerization. In this report, we show that cofilin is a novel component of the podosome belt, the mature osteoclast adhesion structure. Time-course analysis demonstrated that cofilin is activated during primary osteoclast differentiation, at the time of podosome belt assembly. Immunofluorescence studies reveal a localization of active cofilin in the podosome core structure, whereas phosphorylated, inactive cofilin is concentrated in the podosome cloud. Pharmacological studies unraveled the role of a specific cofilin phosphatase to achieve cofilin activation during osteoclast differentiation. We ruled out the implication of PP1/PP2A and PTEN in this process, and rather provided evidence for the involvement of SSH1. In summary, our data involve cofilin as a regulator of podosome organization that is activated during osteoclast differentiation by a RANKL-mediated signaling pathway targeting the SSH1 phosphatase.     

The mineral dissolution function of osteoclasts is dispensable for hypertrophic cartilage degradation during long bone development and growth

During long bone development and post-natal growth, the cartilaginous model of the skeleton is progressively replaced by bone, a process known as endochondral ossification. In the primary spongiosa, osteoclasts degrade the mineralized cartilage produced by hypertrophic chondrocytes to generate cartilage trabeculae that osteoblasts embed in bone matrix. This leads to the formation of the trabecular bone network of the secondary spongiosa that will undergo continuous remodeling. Osteoclasts are specialized in mineralized tissue degradation, with the combined ability to solubilize hydroxyapatite and to degrade extracellular matrix proteins. We reported previously that osteoclasts lacking Dock5 could not degrade bone due to abnormal podosome organization and absence of sealing zone formation. Consequently, adult Dock5^−/− mice have increased trabecular bone mass. We used Dock5^−/− mice to further investigate the different functions of osteoclast during endochondral bone formation. We show that long bones are overall morphologically normal in developing and growing Dock5^−/− mice. We demonstrate that Dock5^−/− mice also have normal hypertrophic cartilage and cartilage trabecular network. Conversely, trabecular bone volume increased progressively in the secondary spongiosa of Dock5^−/− growing mice as compared to Dock5^+/+ animals, even though their osteoclast numbers were the same. In vitro, we show that Dock5^−/− osteoclasts do present acidic compartments at the ventral plasma membrane and produce normal amounts of active MMP9, TRAP and CtsK for matrix protein degradation but they are unable to solubilize minerals. These observations reveal that contrarily to bone resorption, the ability of osteoclasts to dissolve minerals is dispensable for the degradation of mineralized hypertrophic cartilage during endochondral bone formation.     

Podosomes are dispensable for osteoclast differentiation and migration

Podosomes are adhesion structures characteristic of the myeloid cell lineage, encompassing osteoclasts, dendritic cells and macrophages. Podosomes are actin-based structures that are dynamic and capable of self-organization. In particular in the osteoclast, podosomes densely pack into a thick ring called the sealing zone. This adhesion structure is typical of osteoclasts and necessary for the resorption of the bone matrix. We thought to explore in more details the role of podosomes during osteoclast differentiation and migration. To this end, we made from soft to stiff substrates that had not been functionalized with extracellular matrix proteins. Such substrates did not support podosome formation in osteoclasts. With such devices, we could show that integrin activation was sufficient to drive podosome assembly, in a substrate stiffness independent fashion. We additionally report here that osteoclast differentiation is a podosome-independent process. Finally, we show that osteoclasts devoid of podosomes can migrate efficiently. Our study further illustrates the great capacity of myeloid cells to adapt to the different environments they encounter during their life cycle.