Structure of the walls of osseous lacunae during their formation

The osseous lacunae formation in the sponge bone has been studied in the human lumbar vertebrae. Conditionally, this process can be divided into a number of stages. During the first-stage, recesses are formed on the surface of the trabeculae. During the second stage, clearly outlined lacunar edges are formed and mineralization of the fundal collagenous structures is completed. During the third stage, the lacunae are closed. A special attention is paid to changes in the structure and spatial architectonics of the fibrillar components of the ground osseous substance forming the lacunae.     

Morpho-functional correlations of the structure of bone cells and adjoining bone matrix in the developing bone

By means of scanning and transmissive electron microscopy methods structure of the developing bone has been studied. Interconnection of the cell structure and spatial organization of the adjoining matrix has been demonstrated. On the surface of the growing bone not only forming areas have been revealed, where under osteoblasts at various functional states, osteoid layer is determined, but also areas of resorption and completed osteogenesis. This demonstrates an interrupted character of osteogenesis at modelling. At the same time for the remodelling process presence of erosive lacunae is specific; they are filled with a newly deposited collagenous matrix. Therefore, it is possible to suppose that formation of the bone as an organ during the postnatal development includes in itself both mechanisms supporting its form at outgrowth of the osseous matrix volume (modeling) and its continuous rearrangement and adaptation to real conditions of functioning (remodelling).     

Structure of the erosive lacunae on the periosteal and endosteal surfaces of bone

The periostal and endostal surfaces of the femur, ribs and lumbar vertebrae have been investigated in people at the age of 20-90 years. The erosive lacunae on the surface of the bone are revealed as recesses of various form and size. They are usually encountered as groups forming a resorptive focus, or fuse into large zones of resorption. Comparing the data of the light optic investigation and the results of SAM studies of the bone surface, it is possible to distinguish the erosive lacunae with an active process of resorption from the lacunae, where the process proceeds slowly or is not yet fully completed. On the periostal surface the resorptive foci are revealed more often, while on the endostal surface--large zones of resorption are seen. The erosive lacunae are often situated in the ostial parts of the vascular canals. No age dependence is noted in morphological manifestation of the resorption process on the investigated osseous surfaces of a mature person.     

Probable Ankylosaur Ossicles from the Middle Cenomanian Dunvegan Formation of Northwestern Alberta,Canada

A sample of six probable fragmentary ankylosaur ossicles, collected from Cenomanian deposits of the Dunvegan Formation along the Peace River, represent one of the first dinosaurian skeletal fossils reported from pre-Santonian deposits in Alberta. Specimens were identified as ankylosaur by means of a palaeohistological analysis. The primary tissue is composed of zonal interwoven structural fibre bundles with irregularly-shaped lacunae, unlike the elongate lacunae of the secondary lamellar bone. The locality represents the most northerly Cenomanian occurrence of ankylosaur skeletal remains. Further fieldwork in under-examined areas of the province carries potential for additional finds.     

Strain Concentrations Surrounding an Ellipsoid Model of Lacunae and Osteocytes

Direct cell sensing of tissue matrix strains is one possible signaling mechanism for mechanically mediated bone adaptation. We utilized homogenization theory lo estimate bone tissue matrix strains surrounding osteocytes using two sets of models. The first set of models estimated the strain levels surrounding the lacunae and canaliculi, taking into account variations in lamellar properties. The second set estimated strain levels in the osteocyte and the surrounding matrix for different cellular mechanical properties. The results showed that the strain levels found in and surrounding osteocytes, 1700 to 2700 microstrain (denoted as μe; 1 =.0001% strain), were significantly greater than the trabecular tissue level strains of [1325 μe, 287 μe, 87 μe] used for model input. Variation in lamellar properties did not affect strain levels, except at lamellar boundaries. Strain in and surrounding the osteocyte was not significantly affected by cellular stiffness ranging between 28 and 28,000 Pascals (Pa). Strain levels surrounding lacunae and canaliculi were approximately equivalent.     

Strain Concentrations Surrounding an Ellipsoid Model of Lacunae and Osteocytes

Direct cell sensing of tissue matrix strains is one possible signaling mechanism for mechanically mediated bone adaptation. We utilized homogenization theory to estimate bone tissue matrix strains surrounding osteocytes using two sets of models. The first set of models estimated the strain levels surrounding the lacunae and canaliculi, taking into account variations in lamellar properties. The second set estimated strain levels in the osteocyte and the surrounding matrix for different cellular mechanical properties. The results showed that the strain levels found in and surrounding osteocytes, 1700 to 2700 microstrain (denoted as μe; 1 μe =.0001% strain), were significantly greater than the trabecular tissue level strains of {1325 μe, 287 μe, 87 μe} used for model input. Variation in lamellar properties did not affect strain levels, except at lamellar boundaries. Strain in and surrounding the osteocyte was not significantly affected by cellular stiffness ranging between 28 and 28, 000 Pascals (Pa). Strain levels surrounding lacunae and canaliculi were approximately equivalent.     

Histochemical detection of osteocalcin in normal and pathological human bone

We investigated the immunohistochemical localization of osteocalcin in demineralized, paraffin-embedded normal and pathological human bone. Acid decalcification protocols appeared to be more suitable for osteocalcin detection than mild chelating agents. In normal lamellar bone, osteocalcin was detected in osteocytes and along the lamellar bone matrix in fine granular deposits. Under pathological conditions (osteomyelitis, neoplasia), appositional bone showed immunoreactivity in osteoblasts and osteocytes but not in the provisory woven bone matrix. Intense immunoreactivity could be seen at the cell borders of osteoclasts and the bone margins of Howship lacunae. In primary bone-forming tumors, osteocalcin immunoreactivity was detected in osteoblasts and their malignant counterparts. On the basis of these results, we conclude that optimal preservation of osteocalcin is obtained through mild acid decalcifiers. Osteocalcin is deposited in bone matrix, especially that of metabolically inactive bone. In neoplasms, osteocalcin could be a marker of osteoblastic differentiation.     

Osteocyte-osteoclast morphological relationships and the putative role of osteocytes in bone remodeling

An osteocyte lacunae differential count under the light microscope (LM) (1-lacunae with live osteocytes, 2-empty lacunae and lacunae with degenerating osteocytes) was carried out outside the reversal lines of osteonic lamellar bone from various mammals and man to evaluate the possibility of osteocyte survival where osteoclast resorption had occurred. The polarized light microscope (PLM) was used to establish the curvature of bony lamellae outside the convexity of reversal lines: concave lamellae indicate osteocytes reabsorbed on their vascular side where they radiate long vascular dendrites; convex lamellae indicate bone resorption on the osteocyte mineral side, radiating short dendrites. In all samples it was found that: a) about 60% of osteocytes outside the reversal lines were live; b) the percentage of alive osteocytes close to reversal lines is higher when they are attacked on their mineral side. The present data support our view that surviving osteocytes, particularly those attacked from their mineral side, might intervene in the final phase of bone resorption (osteoclast inhibition?). The fact that under the transmission electron microscope (TEM) intercellular contacts were never observed between osteocytes and osteoclasts indicates that if a modulation should occur between these two cellular types it could take place by a paracrine route only. The putative role of the cells of the osteogenic system, particularly osteocytes, in the bone remodeling cycle is also discussed.     

The problem of bone lamellation: An attempt to explain different proposed models

Collagen texture and osteocyte distribution were analyzed in human woven‐ and lamellar‐bone using scanning and transmission electron microscopy. We provide data substantiating the concept that lamellar bone is made up of an alternation of dense‐acellular lamellae and loose‐cellular lamellae, all exhibiting an interwoven texture of collagen fibers. An attempt is also made to explain how the present findings might conform to those of authors whose models propose orderly, geometric arrangements of collagen fibers inside bony lamellae. Such a comparison is possible because the present investigation analyzes split loose lamellae and tangentially‐sectioned dense lamellae. It emerged that only loose lamellae can be dissected, revealing a loose interwoven collagen texture and halved osteocyte lacunae. Dense lamellae cannot be split because of their compactness. The analysis of tangentially sectioned dense lamellae demonstrates that they consist of a network of interwoven collagen fiber bundles. Inside each bundle, collagen fibers run parallel to each other but change direction where they enter adjacent bundles, at angles as described by other authors whose TEM investigations were performed at a much higher magnification than those of the present study. Consequently, what these authors consider to be a lamella are, instead, bundles of collagen fibers inside a lamella. There is discussion of the role played by the manner of osteocyte‐recruitment in the deposition of lamellar‐ and woven‐bone and how the presence of these cells is crucial for collagen spatial arrangement in bone tissues. J. Morphol., 2013. © 2013 Wiley Periodicals, Inc.     

Ossification of the antler in the Lapland reindeer (Rangifer tarandus tarandus)

A histological and histochemical study of biopsy specimens from the Lapland reindeer antler indicated that the intercellular matrix of the cartilage that forms the partitions of longitudinal channels becomes calcified at virtually the initial stage of formation. The lacunae at the peripheries of the cartilaginous partitions are invaded by osteoblasts in a process comparable to endochondral ossification. The very centres of the partitions evidently become directly converted into bone without the presence of e.g. osteoclasts. The osseous partitions are remodelled by osteoclasts. The antler increases in diameter by periosteal apposition.     

Homogenization theory and digital imaging: A basis for studying the mechanics and design principles of bone tissue

Bone tissue is a complex multilevel composite which has the ability to sense ad respond to its mechanical environment. It is believed that bone cells called osteocytes within the bone matrix sense the mechanical environment and determine whether structural alterations are needed. At present it is not known, however, how loads are transferred from the whole bone level to cells. A computational procedure combining representative volume element (RVE) based homogenization theory with digital imaging is proposed to estimate strains at various levels of bone structure. Bone tissue structural organization and RVE based analysis are briefly reviewed. The digital image based computational procedure was applied to estimate strains in individual trabeculae (first-level microstructure). Homogenization analysis of an idealized model was used to estimate strains at one level of bone structure around osteocyte lacunae (second-level trabecular microstructure). The results showed that strain at one level of bone structure is amplified to a broad range at the next microstructural level. In one case, a zeor-level tensile principal strain of 495 muE engendered strains ranging between -1000 and 7000 muE in individual trabeculae (first-level microstructure). Subsequently, a first-level tensile principal strains of 1325 muE within an inidividual trabecula engendered strains ranging between 782 and 2530 muE around osteocyte lacunae. Lacunar orientation was found to influence strains around osteocyte lacunae much more than lacunar ellipticity. In conclusion, the computational procedure combining homogenization theory with digital imaging can proveide estimates of cell level strains within whole bones. Such results may be used to bridge experimental studies of bone adaptation at the whole bone and cell culture level. (c) 1994 John Wiley & Sons, Inc.     

Soldering without transition (osteoassimilation) between the human maxillary bone and a compact dental implant in natural calcite from marine invertebrate

We present evidence for the formation of woven bone between human maxillary lamellar bone (the target site) and a coral implant (Corallium johnsoni Gray). This newly formed bone is characterized by numerous osteocytes located in spherical lacunae and having many ramified processes directed towards the coral; some of these processes continue into the implant surface. Healthy osteocytes were detected within the superficial part of the coral, next to the newly formed bone. Neither osteoclast nor surface of resorption has been noticed. All these observations indicate tight welding or osteoassimilation without any transition between the maxillary bone and the graft. We have obtained analogous results by using grafts of molluscan mother-of-pearl. Our results differ from those reported by other authors, probably due to the compactness of the biomaterial used here.     

The Changing Pore Structure of Aging Human Mandibular Bone1

The spatial structure of human mandibular bone has been studied using microradiography, scanning electron microscopy, and methacrylate replication. Microradiographs have demonstrated lamellar organization and mineralization. Methacrylate replicas have been examined by scanning electron microscopy which revealed the complex structure and inter-connection of the vascular, lacunar, and canalicular spaces. The spatial replicas, representing the pore volume, have been dispersed ultrasonically and separated by sedimentation in a fluid column. The harvested methacrylate replicas of the three types of space have been weighed and knowing the density of methacrylate (1.18g/ml) their volumes determined by calculation. Pore volume increases with age. The vascular space makes the greatest contribution to this increasing porosity with age. Although lacunar volume increases with age, their numbers may fall. Canalicular volume appears to fall with age. This method has provided more information about the contribution the three different spatial compartments make to the increasing porosity of aging bone. There is no difference in the volume of these compartments in alveolar and basal mandibular bone but their distribution indicates that some of the smaller channels are more readily obstructed in alveolar bone.     

Orientation of collagen at the osteocyte lacunae in human secondary osteons

This work characterizes an aspect of human bone micro-structure, pertinent to fracture initiation and arrest. It addresses how the orientation of elementary components proximate to osteocyte lacunae influences secondary osteon micro-biomechanics. New data at the perilacunar region concerning orientation of collagen-apatite, and prior data on collagen orientation outside the perilacunar region, are incorporated in a novel simulation of osteons to investigate how orientation relates to strains and stresses during mechanical testing. The perilacunar region was observed by confocal microscopy within single lamellar specimens, isolated from osteons. The specimens were separated by extinct or bright appearance in transverse section under circularly polarizing light. This is because synchrotron diffraction and confocal microscopy had established that each type, away from the perilacunar region, corresponds to specific dominant collagen orientation (extinct lamellae's dominant collagen forming small angles with the original osteon axis, while the bright lamellae's forms larger angles). Morphometry of serial confocal images of each perilacunar region showed collagen orientation generally following the orientation of canaliculi, circumambiently-perpendicular to the lacuna. The lacunae tilted relative to the lamellar walls were more numerous in extinct than in bright lamella. Their apices were less likely in extinct than bright lamella to show collagen following the canalicular orientation. The simulation of osteocyte lacunae in osteons, under tension or compression loading, supports the hypothesis that collagen orientation affects strains and stresses at the equatorial perilacunar region in conjunction with the presence of the lacuna. We further conjecture that collagen orientation diverts propagation of micro-cracks initiating from apices.     

SHORT COMMUNICATION: A rapid method for the assessment of bone architecture by confocal microscopy

Conventional ways of demonstrating and analysing the components of osseous tissue have always been hampered by the difficulty of physically sectioning bone. In this study, we have used Acridine Orange staining of 100-mu m-thick unembedded bone slices and then assessed the cellular and tissue architecture by confocal microscopy. The result showed the Acridine Orange, by differential staining of the cellular nucleic acids, permits ready assessment of cell shape and cell organization as well as variations in growth patterns. Our studies have provided a new and relatively easy way of assessing the morphology of bone specimens by rendering unnecessary the need for embedding, decalcification and thin sectioning of the osseous tissue. This revised version was published online in November 2006 with corrections to the Cover Date.     

The histological structure of glyptosaurine osteoderms (Squamata: Anguidae), and the problem of osteoderm development in squamates

Glyptosaurinae, a fossil clade of anguid lizards, possess robust osteoderms, with granular ornamentation. In this study, the structural and histological features of these osteoderms were described in order to reconstruct their developmental pattern and further document the degree of homology that could exist between vertebrate integumentary skeletons. Glyptosaurine osteoderms have a diploe architecture and display an unusually complex structure that includes four tissue types: a core of woven‐fibered bone intensely remodeled; a peripheral formation of the same tissue containing dense bundles of long Sharpey fibers; a thick basal layer of lamellar bone; and a superficial layer of a non‐osseous material that belongs to the category of hypermineralized tissues such as ganoine, or enameloid and enamel tissues. The growth pattern of glyptosaurine osteoderms involved appositional processes due to osteoblast activity. In early growth stages, osseous metaplasia might have also been involved, but this possibility is not substantiated by histological observations. The superficial layer of the osteoderms must have resulted from epidermal contribution, a conclusion that would support previous hypotheses on the role of epidermal‐dermal interactions in the formation of squamate osteoderms. J. Morphol., 2010. © 2010 Wiley‐Liss, Inc.     

Expression of versican and ADAMTS1, 4, and 5 during bone development in the rat mandible and hind limb.

Extracellular matrix (ECM) remodeling is achieved by both production and degradation of ECM molecules during bone development. ADAMTS (a disintegrin and metalloprotease with thrombospondin type 1 motifs) constitutes a family of extracellular proteases which are implicated in cleaving the protein versican. The present study was designed to investigate the expression of versican and ADAMTS1, 4, and 5 mRNA during bone development in rat mandibles and hind limbs by RT-PCR and in situ hybridization. Versican was localized by immunohistochemistry. The process of bone development from day 14 postcoitum through week 6 postnatum was divided into the beginning of osteogenesis, woven bone, and lamellar bone stages. Versican protein was abundant in the woven bone matrix, but decreased in the lamellar bone matrix. Versican mRNA was prominent in some osteoblasts with corresponding localization of the cognate protein. The temporal and spatial mRNA expression pattern of ADAMTS1, 4, and 5 was comparable to that of versican. These results suggest that woven bone rich in versican alters into lamellar bone containing little versican during bone development in both mandibles and hind limbs, where some osteoblasts may be involved in production as well as degradation of versican by secreting ADAMTS1, 4, and 5.     

Immunolocalization of collagen types I and III, tenascin, and fibronectin in intramembranous bone.

Structural components of the organic bone matrix were located by immunohistochemical techniques in fresh-frozen sections of normal and dysplastic bone. Fine and coarse birefringent fibers were identified as separate and distinctive features in the extracellular matrix by antibodies raised against human collagen Type III. The glycoprotein tenascin was located on a proportion of the fibers in a characteristic beaded pattern, which was absent in dysplastic bone. The fibers originated in the periosteum or in the fibrous stroma of the marrow cavity and were oriented with regard to both the spatial and the lamellar organization of the bone. The disposition and composition of the fibers suggests that they form a preliminary framework on which intramembranous bone modeling proceeds, and that the specific location of tenascin on the fibers in normal developing membrane bone may be important in determining the alignment of the bone tissue. Epitopes recognized by the collagen Type I and fibronectin antibodies were demonstrated throughout the mineralized matrix, but their incorporation into the collagen "Type III" fibers was evident only outside the mineralized matrix.     

Modeling microdamage behavior of cortical bone

Bone is a complex material which exhibits several hierarchical levels of structural organization. At the submicron-scale, the local tissue porosity gives rise to discontinuities in the bone matrix which have been shown to influence damage behavior. Computational tools to model the damage behavior of bone at different length scales are mostly based on finite element (FE) analysis, with a range of algorithms developed for this purpose. Although the local mechanical behavior of bone tissue is influenced by microstructural features such as bone canals and osteocyte lacunae, they are often not considered in FE damage models due to the high computational cost required to simulate across several length scales, i.e., from the loads applied at the organ level down to the stresses and strains around bone canals and osteocyte lacunae. Hence, the aim of the current study was twofold: First, a multilevel FE framework was developed to compute, starting from the loads applied at the whole bone scale, the local mechanical forces acting at the micrometer and submicrometer level. Second, three simple microdamage simulation procedures based on element removal were developed and applied to bone samples at the submicrometer-scale, where cortical microporosity is included. The present microdamage algorithm produced a qualitatively analogous behavior to previous experimental tests based on stepwise mechanical compression combined with in situ synchrotron radiation computed tomography. Our results demonstrate the feasibility of simulating microdamage at a physiologically relevant scale using an image-based meshing technique and multilevel FE analysis; this allows relating microdamage behavior to intracortical bone microstructure.     

Evidence for the presence of osseous tissue in dogfish vertebrae

Summary The calcified cartilage of the dogfish vertebra has been studied by means of an undecalcified hard tissue method, including microradiography and tetracycline labelling, and electron microscopy. The transversely sectioned vertebra shows a centrum and neural and hemal arches. The mineralized area consists of a narrow but continuous band, which touches the perichondrium, and is formed by chondrocytes that participate in the mineralization of the surrounding matrix. The neural arches appear quite different; the upper parts contain an hypertrophied cartilage and, close to it, an inner zone formed by crescent shaped lamellar bone tissue containing osteoblasts and osteocytes. Tetracycline labelling of these two types of hard tissue reveals a globular calcification with calcospherites and Liesegang rings, at the level of the calcified cartilage, and a strong and linear label of the inner border of the osseous tissue. Transmission electron microscopy shows Type I collagen in the crescent shape area and Type II collagen in calcified cartilage area. The presence of osseous tissue in elasmobranch endoskeleton is discussed in relation to the evolution of the gnathostomes skeleton and the endocrinological control of calcium metabolism.