Ultrastructure of quick-frozen and freeze-substituted chick osteoclasts

Three-dimensional morphology of the Golgi apparatus in osteoclasts: NADPase and arylsulfatase cytochemistry, and scanning electron microscopy using osmium maceration

This study was designed to observe osteoclasts in the rat femora by light and electron microscopic cytochemistry for nicotinamide adenine dinucleotide phosphatase (NADPase) and arylsulfatase, and scanning electron microscopy using osmium maceration to assess the three-dimensional morphology of the Golgi apparatus in osteoclasts. The Golgi apparatus showed strong NADPase activity and surrounded each nucleus with the cis-side facing the nucleus. The Golgi apparatus could be often traced for a length of 20 μm or longer. Observations of serial semi-thin sections confirmed that a single line of reaction products (=lead precipitates) intervened somewhere between any two neighboring nuclei. The nuclear membrane showed strong arylsulfatase activity as well as rough endoplasmic reticulum and lysosomes. Scanning electron microscopy showed that the Golgi apparatus covered the nucleus in a porous sheet-like configuration. Under magnification, the cis-most saccule showed a sieve-like configuration with fine fenestrations. The saccules decreased fenestration numbers toward the trans-side and displayed a more plate-like appearance. The above findings indicate the following. (1) The Golgi saccules of osteoclasts have a three-dimensional structure comparable with that generally seen in other cell types. (2) The Golgi apparatus forms a porous multi-spherical structure around nuclei. Within the structure, in most cases a Golgi stack partitions the room into several compartments in each of which a nucleus fits. (3) The nuclear membrane synthesizes some kinds of proteins more stably and sufficiently than the rough endoplasmic reticulum. Consequently, the Golgi apparatus accumulates around nuclei with the cis-side facing the nucleus.

Scattered podosomes and podosomes associated with the sealing zone architecture in cultured osteoclasts revealed by cell shearing, quick freezing, and platinum-replica electron microscopy

Osteoclasts (OCs) can adhere to a variety of substrate surfaces by highly dynamic actin-based cytoskeletal structures termed podosomes. This tight attachment is established by a sealing zone (SZ), which is made of interconnected individual podosomes. Compared with scattered podosomes in various cell types, the architecture of the SZ is still unclear. Especially, ultrastructural studies on the details of the cytoskeletal structure of an OC have been challenging, because the high density of filaments in their podosomes obscure visualization of individual filaments. Therefore, to study this organization in more exact detail, we employed shearing open combined with replica electron microscopy. The present study provides several new details of the podosome and SZ structure, which were previously unrecognized: (a) the SZ consists of recognizable podosomes with a dense actin network of interpodosomal regions characterized by multiple layers of crossing, branching and anastomosing actin filament networks; (b) the Arp2/3 complex is distributed throughout the actin network of podosomes and SZ, indicating that actin polymerization is concentrated at these regions; (c) a close spatial relationship between the podosome and the dorsal membrane; and (d) a network of membranous organelles in close proximity to the podosomes in the SZ. Taken together, the present study reveals that a more complicated interpodosomal actin network among neighboring individual podosomes, which is more complicated than previously thought, appears to form the SZ. Indeed, individual podosomes are not an isolated structural unit from other organelles; and, in turn, their dynamism might affect the surrounding interpodosomal cytoskeletons, membranous organelles, and plasma membrane.

Visualization of structural organization of ventral membranes of sheared-open resorbing osteoclasts attached to apatite pellets

Osteoclasts are highly polarized cells from both morphological and functional points of view. Using quick-freeze, rotary-replication methods combined with cell-shearing, we clarified the variability of cytoplasmic surface of the polarized membranes of osteoclasts seeded on apatite. As to the organization of actin filaments and clathrin sheets, we confirmed almost the same ventral membrane specializations of osteoclasts on apatite as seen on glass plates. The organized actin filaments and membrane-associated particles supported the ruffled border membranes. Inside the actin sealing zone, membrane specializations were not always occupied with the ruffled border but also with other types of membranes. Some osteoclasts formed an actin ring but lacked the ruffled border projections. We report a unique and distinctive membrane modification of apatite-attached osteoclasts, i.e., the presence of dense aggregates of membrane-associated particles and related structures not found in the osteoclasts seeded on glass plates. Actin filament polarity in the podosomes was determined by decoration with myosin S1. The actin filament polarity within podosome appears to be oriented predominantly with its barbed ends toward the core, whereas the interconnecting F-actin appears to be mixed oriented. Two different types of clathrin plaques displayed different distributions: clathrin-dependent endocytosis was observed in the ruffled border regions, whereas flat clathrin sheets were found in the leading edge of lamellipodia and near podosomes. The clathrin sheets adhered to the apatite surface tightly on the ventral membranes overlaying the resorption lacunae. All these membrane specializations as mentioned above may indicate the functional variability of osteoclasts seeded on apatite.

The resorptive apparatus of osteoclasts supports lysosomotropism and increases potency of basic versus non-basic inhibitors of cathepsin K

In mice and humans, the effect of genetic deficiency of cathepsin K (catK) is impaired bone resorption, or osteopetrosis. Inhibition of catK is therefore a promising strategy for the treatment of osteoporosis. The enzyme acts in an acid environment. This provides a further potential opportunity: if the inhibitor is basic it is more likely to accumulate in membrane-bound acidic compartments (lysosomotropism), so minimizing off-target effects. However, the resorptive hemivacuole is not membrane-bound, and so might not retain lysosomotropic compounds. We therefore elected to determine whether the osteoclastic resorptive apparatus supports such accumulation. First, we attempted to compare the persistence of a lysosomotropic dye in the hemivacuole versus intracellular vesicles. To our surprise the dye could not be detected in the ruffled border region by confocal microscopy. We found that this could be explained by the tight packing of the folds of the ruffled border, and their close apposition to the bone surface. We also found that the dye persisted similarly in resorbing osteoclasts and macrophages, consistent with the notion that resorbing osteoclasts support lysosomotropism. Next, we compared the ability of basic and non-basic inhibitors of catK to suppress bone resorption by human osteoclasts. We found that basic compounds were considerably more potent than non-basic compounds at suppression of osteoclastic resorption than would be anticipated from their potency as enzyme inhibitors. Also consistent with osteoclastic lysosomotropism, basic inhibitors suppressed resorption for substantially longer than a non-basic inhibitor after washout from cell cultures. Furthermore, selectivity of basic inhibitors for inhibition of catK versus other cathepsins persisted: concentrations that inhibited catK in osteoclasts had no detectable effect on cathepsin S (catS) in a cell-based assay. This data is consistent with accumulation and enrichment of such basic inhibitors in the resorptive apparatus of the osteoclast, allowing for prolonged efficacy at the intended site of action. Our results suggest a major advantage for lysosomotropic compounds as inhibitors of bone resorption by osteoclasts in osteoporosis and other diseases caused by excessive osteoclastic activity.

The relationship between calcium accumulation in osteoclast mitochondrial granules and bone resorption

In the process of bone resorption, calcium is considered to be transported within vesicles in osteoclasts and eventually released. We studied the ultramicromorphology of calcium (Ca) transport in osteoclasts by preparing samples of osteoclasts collected from rat femurs in which calcium was maximally preserved and subjected them to high-pressure quick-freezing and freeze-substitution. We then examined the localization of calcium by Electron Energy Loss Spectroscopy (EELS). The structures of cell membranes were preserved, suggesting the suitability of this high-pressure quick-freezing and freeze-substitution technique. Osteoclast mitochondria adjacent to the ruffled border were rich in mitochondrial granules and contained a large amount of Ca. In contrast, mitochondria in the basolateral region contained few granules. Moreover, by an osteoclast-culturing experiment, differences in the morphology of mitochondrial granules were noted between culturing on a dentin slice and that on a gold plate, i.e., few mitochondrial granules were noted in osteoclasts cultured on a non-dentin plate. These findings suggest an association between the morphology of mitochondrial granules in osteoclasts and bone resorption as well as a new transport route for Ca resorbed by osteoclasts. We propose that Ca accumulates in mitochondria granules to prevent increased Ca concentration in cytoplasm of osteoclasts during bone resorption.