Scanning electron microscopy of bone: instrument, specimen, and issues

Impaired bone formation in transgenic mice resulting from altered integrin function in osteoblasts

To determine the role of integrins in mature osteoblasts in vivo, we expressed in transgenic mice a dominant-negative integrin subunit (beta1-DN) consisting of the beta1 subunit cytoplasmic and transmembrane domains, driven by the osteoblast-specific osteocalcin promoter. Immature osteoblasts isolated from transgenic animals differentiated normally in vitro until the osteocalcin promoter became active; thereafter they detached from the substratum, suggesting that beta1-DN was impairing adhesion in mature osteoblasts. Transgenic animals had reduced bone mass, with increased cortical porosity in long bones and thinner flat bones in the skull. At 35 days, the rate of bone formation was reduced in cortical bone, and the parietal bones were 45% thinner than in wild-type animals. Active osteoblasts were less polar and had larger areas of cytoplasm with intracellular stores of matrix molecules. Osteocyte lacunae appeared normal around the cell body but did not have normal canilicular structures. At 90 days, the parietal bone of transgenic males was of normal width, suggesting that the original defect in matrix deposition had been repaired or compensated for. In contrast, transgenic females still had decreased bone mass in the parietal bone at 90 days. The decreased bone mass in TG females was accompanied by increased staining for osteoclast activity, suggesting that there was a sex-specific defect in mature animals.

Scanning electron microscopic observations of human dentine after mechanical caries excavation

OBJECTIVES

The structural integrity and surface characteristics of dentine remaining after caries excavation may be relevant to the subsequent bonding of adhesive restorative materials to the prepared cavity. This in vitro investigation aimed to analyse the different surface characteristics of the dentine cavity floor created after preparation using five different mechanical and chemo-mechanical methods of excavation: hand excavation, slow-speed bur, sono-abrasion, air-abrasion and Carisolv gel.

METHODS

Ten cavities were prepared using each excavation method in extracted teeth with occlusal carious lesions. Epoxy resin replicas of the 50 cavities were manufactured from silicone impressions and then analysed using secondary electron scanning electron microscopy (SEM) to ascertain the surface characteristics of the dentine at the cavity floor.

RESULTS AND CONCLUSIONS

Results from the 50 cavities examined suggested that each alternative excavation technique produced a different and characteristic dentine surface. Carisolv gel was the only method examined that consistently removed the smear layer during excavation to leave exposed dentine tubules at the end of cavity preparation.

Structure and mineralisation density of antler and pedicle bone in red deer (Cervus elaphus L.) exposed to different levels of environmental fluoride: a quantitative backscattered electron imaging study

The structure and relative degree of mineralisation of antler and pedicle bone of yearling red deer stags exposed either to low or high levels of environmental fluoride were determined by digital quantitative backscattered electron (BSE) imaging. Bone fluoride content (BFC) in antlers (845 +/- 86 mg F-/kg ash, arithmetic mean +/- S.E.M.) and pedicles (1448 +/- 154 mg F-/kg ash) of deer from a highly fluoride polluted area in North Bohemia (Czech Republic) were significantly higher (P < 0.001) than those of controls from uncontaminated regions in West Germany (antlers: 206 +/- 41, pedicles: 322 +/- 52 mg F-/kg ash). Mean (56.5 +/- 4.5%) and maximum (84.9 +/- 2.1%) mineralised bone area of the control antlers significantly (P < 0.05 and P < 0.001, respectively) exceeded the corresponding values for the N. Bohemian deer (43.3 +/- 1.3 and 73.3 +/- 1.9%, respectively), while the pedicles from the 2 groups did not differ significantly. In the pooled antler samples (n = 18), negative correlations existed between BFC and mean (r(s) = -0.62, P < 0.01) as well as maximum (r(s) = -0.69, P < 0.01) mineralised bone area. Morphological imaging revealed a decreased width and an increased porosity of the antler cortex in the N. Bohemian specimens. Mean (148.5 +/- 1.7) and maximum (154.2 +/- 1.7) BSE-signal intensities (= grey levels; range between a monobrominated (grey level 0) and a monoiodinated (grey level 255) dimethacrylate resin standard) of the antlers from the controls were significantly higher than those of the N. Bohemian deer (140.7 +/- 2.1 and 145.7 +/- 2.2, respectively; P < 0.05 for both comparisons). In the pooled antler samples, negative correlations between BFC and mean (r(s) = -0.51, P < 0.05) as well as maximum (r(s) = -0.52, P < 0.05) BSE-signal intensities were observed. No significant differences in mineralisation density parameters were found for the 2 pedicle samples, and BFC and mineralisation density of the pooled pedicles were uncorrelated. Morphological imaging revealed bone mottling (denoting increased remodelling activity) and frequent occurrence of apparently increased osteocyte lacunae in some of the pedicles from the N. Bohemian deer. It is concluded that the reduced amount of mineralised bone in, and the lower mineralisation density of, the N. Bohemian antlers resulted from a fluoride induced disturbance of bone mineralisation. The rapid growth of antlers leads both to a high mineral demand and a high rate of fluoride uptake during antlerogenesis. This, and the limited lifespan of antlers, which does not allow for a compensation of a delay in the onset or progression of the mineralisation process, renders antler bone particularly susceptible to fluoride. Antlers are therefore considered a useful model for studying fluoride effects on bone formation. Furthermore, analysis of cast antlers enables a noninvasive monitoring of environmental pollution by fluorides.

Influence of topography and specimen preparation on backscattered electron images of bone

Backscattered electron (BSE) images of bone exhibit graylevel contrast between adjacent lamellae. Mathematical models suggest that interlamellar contrast in BSE images is an artifact due to topographic irregularities. However, little experimental evidence has been published to support these models, and it is not clear whether submicron topographical features will alter BSE graylevels. The goal of this study was to determine the effects of topography on BSE image mean graylevels and graylevel histogram widths using conventional specimen preparation techniques. White-light interferometry and quantitative BSE imaging were used to investigate the relationship between the BSE signal and specimen roughness. Backscattered electron image graylevel histogram widths correlated highly with surface roughness in rough preparations of homogeneous materials. The relationship between BSE histogram width and surface roughness was specimen dependent. Specimen topography coincided with the lamellar patterns within the bone tissue. Diamond micromilling reduced average surface roughness when compared with manual polishing techniques but did not significantly affect BSE graylevel histogram width. The study suggests that topography is a confounding factor in quantitative BSE analysis of bone. However, there is little quantitative difference between low-to-moderate magnification BSE images of bone specimens prepared by conventional polishing or diamond micromilling.

Age changes in bone

Changes in bone structure as a function of age have been studied by simple inspection, x-ray imaging, stereo-photography, deep field optical microscopy, circularly polarised light microscopy, and scanning electron microscopy (SEM), including both topographic and compositional backscattered electron (BSE) imaging modes. The study of bone as a three-dimensional object, rather than in thin sections, enables us to envisage modelling and remodelling processes in context. The study of ultra-flat block surfaces permits the acquisition of data from an effectively very thin layer in the block face, and to examine bone as a spectrum of tissue types varying in the degree of mineralisation. Particular attention has been paid in our earlier studies to the iliac crest, lumbar vertebral bodies, femoral mid-shaft, neck and head and parietal and frontal skull bones. Recently, we have compared findings from these sites with observations on the mandible. We conclude, from our new imaging data, that common generalisations about the changes in bone in ageing and osteoporosis are too simplified, and that the mandible differs sufficiently from post-cranial skeletal sites that it would be unwise to extrapolate from findings in the jaw to the circumstances elsewhere.

Osteoconduction in large macroporous hydroxyapatite ceramic implants: evidence for a complementary integration and disintegration mechanism

Large, cylindrical implants of a porous calcium phosphate ceramic ("hydroxyapatite" starting material, HAC) were used to replace far greater than critical-sized sections of the midshaft of sheep tibiae and retrieved at 2 and 9 months; external fixation was used in the first 5 months. Excellent clinical function of these implants was reported in a previous study. The material retrieved was embedded in PMMA, and blocks were sectioned and surfaces were polished and carbon coated prior to study using digital backscattered electron (BSE) imaging. Detailed scanning electron microscopy study of the pattern of osseointegration of the implanted material at early (2 months) and late (9 months) timepoints revealed a previously unrecognized pattern of integration/disintegration of this implant material in tandem with bone growth. We conclude that bone adaptation to the HAC leads to its fracture and that the newly generated surfaces are equally osteoconductive. This leads to a self-propagating, self-annealing system in which defects in the HAC are mended by intercalation of bone.

Comparison of eight histomorphometric methods for measuring trabecular bone architecture by image analysis on histological sections

Osteoporosis is defined as a disease characterized by low bone mass and microarchitectural deterioration of trabecular bone leading to enhanced bone fragility. Various histomorphometric methods have been described to measure bone architecture on histological sections. However, not all of the methods are strictly equivalent and some of them appear able to detect differences earlier in the course of the disease. We have compared 8 histomorphometric methods known to characterize the architecture of trabecular bone in 154 male osteoporotic patients. Measurements were done on transiliac bone biopsies: Trabecular number, thickness, and separation (Tb.N, Tb.Th, Tb.Sp); Trabecular Bone Pattern Factor (TBPf); Euler-Poincare's number (E); Interconnectivity Index (ICI); strut analysis of the trabecular network with the ratio of nodes/free-end (N/F); star volume of the bone marrow (V*m.space) and trabeculae (V*Tb) and the Kolmogorov fractal dimension of the trabecular boundaries (D). Relationships between the various architectural parameters were studied by hierarchical cluster analysis. Linear, hyperbolic, and exponential correlations were found between trabecular bone volume (BV/TV) and architectural parameters. Cluster analysis demonstrates the link between these architectural parameters. ICI, E, and TBPf, which reflect the amount of open/closed marrow cavities clustered together and appeared related to Tb.Sp, V*m.space which are indicators of the mean size of marrow cavities. Tb.Th, V*Tb and N/F flocked together as they reflect the trabecular size. Tb.N and D segregated together and seemed to best describe the trabecular network complexity. These histomorphometric techniques are correlated but correlations may be linear or nonlinear. Several histomorphometric techniques need to be used in parallel to appreciate the pathophysiological mechanisms of osteoporotic states.

Pathology of the distal condyles of the third metacarpal and third metatarsal bones of the horse

This study examined material from Thoroughbred horses, the majority of which had been in race training, for evidence of pathology in the third metacarpal (McIII) and third metatarsal (MtIII) bones which might be related to the occurrence of distal condylar fractures. Whole bone samples were studied and documented by macrophotography prior to macroradiography and computed tomographic (CT) imaging. Microradiographs were made from 100 microm thick mediolateral sections cut perpendicular to the dorsal and palmar/plantar articular surfaces of distal condylar regions of McIII and MtIII. Blocks were prepared for morphological imaging using the backscattered electron mode of scanning electron microscopy (BSE SEM). Linear defects in mineralised articular cartilage and subchondral bone were found in the palmar/plantar aspects of the condylar grooves adjacent to the sagittal ridge. These were closely related to the pattern of densification of the subchondral bone and were associated with intense focal remodelling of the immediately adjacent and subjacent bone. Parasagittal fractures of the condyles originated in similar defects. A unifying hypothesis for the aetiopathogenesis of these fractures is presented.

Correlative light and backscattered electron microscopy of bone--Part I: Specimen preparation methods

A method for preparing nondecalcified bone and tooth specimens for imaging by both light microscopy (LM) and backscattered electron microscopy in the scanning electron microscope (BSE-SEM) is presented. Bone blocks are embedded in a polymethylmethacrylate (PMMA) mixture and mounted on glass slides using components of a light-cured dental adhesive system. This method of slide preparation allows correlative studies to be carried out between different microscopy modes, using the same histologic section. It also represents a large time savings relative to other mounting methods whose media require long cure times.

Impaired osteoclastic bone resorption leads to osteopetrosis in cathepsin-K-deficient mice

Cathepsin K is a recently identified lysosomal cysteine proteinase. It is abundant in osteoclasts, where it is believed to play a vital role in the resorption and remodeling of bone. Pycnodysostosis is a rare inherited osteochondrodysplasia that is caused by mutations of the cathepsin-K gene, characterized by osteosclerosis, short stature, and acroosteolysis of the distal phalanges. With a view to delineating the role of cathepsin K in bone resorption, we generated mice with a targeted disruption of this proteinase. Cathepsin-K-deficient mice survive and are fertile, but display an osteopetrotic phenotype with excessive trabeculation of the bone-marrow space. Cathepsin-K-deficient osteoclasts manifested a modified ultrastructural appearance: their resorptive surface was poorly defined with a broad demineralized matrix fringe containing undigested fine collagen fibrils; their ruffled borders lacked crystal-like inclusions, and they were devoid of collagen-fibril-containing cytoplasmic vacuoles. Assaying the resorptive activity of cathepsin-K-deficient osteoclasts in vitro revealed this function to be severely impaired, which supports the contention that cathepsin K is of major importance in bone remodeling.

Validation of quantitative backscattered electron imaging for the measurement of mineral density distribution in human bone biopsies

The measurement of bone mineral density (BMD) using X-rays is usually employed to monitor the mineral content in a given portion of bone. However, this method cannot differentiate between changes in bone volume or in degree of mineralization of the bone matrix. In contrast to BMD, bone mineral density distribution (BMDD), as measured on bone sections by quantitative backscattered electron imaging (qBEI), is able to distinguish differences in the degree of mineralization. For routine clinical research, we have validated the method of calibration and standardization of the backscattered electron (BE) signal. Carbon and aluminum were used as reference materials for BE gray levels and osteoid and apatite for calcium concentration. Experiments were performed to get knowledge about precision (intraassay variance-instrumental stability and interassay variance-reproducibility) and accuracy (standardization) of this method as well as the biological variance (intraindividual and interindividual) in human bone. On transiliac biopsies or necropsies from 20 individuals having had accidental death (13 females, 7 males, age 30-85 years) BMDD measurements were conducted. The patients' medical history as well as the histomorphology of these bones showed no evidence of metabolic bone disease. For instance, the standard deviations of the weighted mean calcium concentrations were <0.3%, <0.4%, <0.9%, and <2.6% of the mean for the intraassay, interassay, intraindividual, and interindividual variations, respectively. In addition, a mean BMDD histogram for transiliac bone specimens was calculated from the 20 aforementioned individuals. The method used allows detection of the degree of mineralization independently from the actual bone volume, a result that seems to be of special interest in the assessment of the effect of treatments for osteoporosis. The power of this technique is demonstrated by using bone from a patient with a metabolic bone disease. In this case of osteomalacia due to celiac disease, the mean calcium concentration in the bone matrix was reduced by 19.3% as compared with normal.

Errors in quantitative backscattered electron analysis of bone standardized by energy-dispersive x-ray spectrometry

Backscattered electron (BSE) imaging has proven to be a useful method for analyzing the mineral distribution in microscopic regions of bone. However, an accepted method of standardization has not been developed, limiting the utility of BSE imaging for truly quantitative analysis. Previous work has suggested that BSE images can be standardized by energy-dispersive x-ray spectrometry (EDX). Unfortunately, EDX-standardized BSE images tend to underestimate the mineral content of bone when compared with traditional ash measurements. The goal of this study is to investigate the nature of the deficit between EDX-standardized BSE images and ash measurements. A series of analytical standards, ashed bone specimens, and unembedded bone specimens were investigated to determine the source of the deficit previously reported. The primary source of error was found to be inaccurate ZAF corrections to account for the organic phase of the bone matrix. Conductive coatings, methylmethacrylate embedding media, and minor elemental constituents in bone mineral introduced negligible errors. It is suggested that the errors would remain constant and an empirical correction could be used to account for the deficit. However, extensive preliminary testing of the analysis equipment is essential.

Effect of estrogen suppression on the mineralization density of iliac crest biopsies in young women as assessed by backscattered electron imaging

The effects of estrogen suppression on bone mineralization in young women were studied by quantitative backscattered electron (BSE) imaging of transiliac biopsies taken before and after treatment for endometriosis. Treatment (6 months) was with analogs of gonadotrophin releasing hormone (GnRH) given either alone (six paired biopsies), which resulted in a marked reduction in the levels of circulating estrogen, or in conjunction with tibolone, a synthetic steroid with estrogenic, progestrogenic, and androgenic properties (four paired biopsies). Estrogen withdrawal increased (p < 0.01) and concomitant tibolone treatment decreased (p < 0.05) the overall mean bone density. Estrogen withdrawal increased the fraction of bone with a high mineralization density [pretreatment: 0.236+/-0.007; GnRH: 0.279+/-0.009, mean +/- standard error of the mean (SEM); p < 0.01]. The concomitant addition of tibolone reversed these effects and increased the proportion of bone with a low mineralization density (pretreatment: 0.198 +/- 0.005; tibolone: 0.230 +/-0.008, p < 0.01). Using previously published data, the mean bone density was inversely correlated with mean wall thickness in cancellous bone (p = 0.030) and with the percentage of active osteons (p = 0.023) in cortical bone. Although treatment had similar effects on the mean bone mineralization density of cortical and cancellous bone, there were different distributions of mineralization between the two sites, with cancellous bone having more skewed and kurtotic distributions both before and after estrogen withdrawal. This study indicates that a short-term estrogen suppression results in the accumulation of bone with a higher mineralization density. As bone with a high mineral content has a decreased impact resistance, this might increase fracture risk. Understanding the cellular and biochemical mechanisms responsible for the local distribution of bone mineral when estrogen is withdrawn may allow the development of new strategies for maintaining bone quality after menopause.

Mineralisation density of human mandibular bone: quantitative backscattered electron image analysis

This study examined the tissue level mineralisation density distribution in mandibles from 88 adult humans. Mandibles (19-96 y) were sectioned vertically in midline (MID), mental foramen (MF), and third molar (M3) regions. Surgical fragments from M3 were obtained from individuals aged 16-38 y. All specimens were cleaned, embedded in PMMA, micromilled and examined by digital 20 kV backscattered electron (BSE) stereology. Quantitation was based on rescaling image histograms to the signal range between a monobrominated (0) and a monoiodinated (255) dimethacrylate resin standard. Mineralisation density increased with age (r=0.70; P < 0.0001): the mean for 39 individuals aged between 16 and 50 y was significantly lower (P < 0.0001) than for 35 individuals over 51 y (mean (+/-S.E.M.): 158.20 (1.63) and 174.71 (1.27) normalised grey level units respectively). There was good correlation in mean mineralisation density between different sites in the same mandible, but MID was significantly less highly mineralised than the other sites: MID 173.90, MF 177.34, M3 177.11 (P < 0.002 and 0.01 for MF and M3 respectively; paired t test), as was the alveolar bone density when compared with the bone of the inferior cortex (e.g. MID: 171.13 (1.53) and 174.46 (1.14) P < 0.0001). No sex difference was found. Partially dentate mandibles generally had regions of higher mineralisation than fully dentate and edentulous mandibles. The lowest density bone occurred at the alveolar crest anteriorly and superolingually at M3, matching sites of net resorption following tooth loss. Highest densities were found inferolingually at MID, inferiorly at MF and buccally at M3, matching the sites thought to experience the highest functional strains. This stresses the importance that local factors may have in the remodelling of the edentulous mandible. Morphology showed that there is a preponderance of highly mineralised cement lines, and of packets containing dead, mineralised, osteocytes.

Porous channels in the cuticle of the head-arrester system in dragon/damselflies (Insecta:Odonata)

The ultrastructure of the porous channels (PC) of the postcervical sclerite (SPC), which provides additional head fixation to the neck in adult odonates, was studied using TEM and high resolution SEM microscopy. Single chitin-protein microfibrils, about 0.14 micron thick, are arranged into channels with cylinder-like shapes. The axial rod of the chitin fiber (0.04 micron thick) is located in the center of the cylinder. The orientation of the axial rods was three-dimensionally demonstrated after dissolving the protein cover with NaOH. The PCs are arranged vertically to the surface and pass from the epidermal cells through all the cuticular layers to the surface of the cuticle. In the exo- and endocuticle, the PCs are usually oval in cross-section and about 0.3 micron thick. In the endocuticle, the cross-sectional area of the PCs varies widely, from 0.01-0.15 micron2. The shape of the PC is determined by the macromolecular organization of the chitin-protein microfibrils: the long axis of the channel is orientated parallel to the axis of the preferred orientation of the cuticular microfibrils. The microfibrils tend to follow the line of the channel very closely. In fractures orientated perpendicular to the surface, the PC resembles a ribbon-like construction, which was clearly demonstrated by casts. The strongly parallel orientation of PCs in the deep layers of the cuticle changes within the microtrichia (MT), and they begin to be curved. Numerous PCs pass through the microtrichium, and most of them end on its side wall. PCs usually contain channel filaments about 0.09 micron thick. Usually, a single channel contained one filament, but channels located in the deep layers of the endocuticle have from one to five single filaments. The filaments were observed in the intact cuticle and in the cuticle enzymatically treated with chitinase, while in the cuticle treated with NaOH filaments were absent. The porous channel system of the odonate arrester is interpreted as a device transporting adhesive excretions from the epidermal cells to the cuticular surface.

Determining mineral content variations in bone using backscattered electron imaging

The mechanical properties of bones are greatly influenced by the ratio of organic constituents to mineral. Determination of bone mineral content on a macroscopic scale is straightforward, but microscopic variations, which can yield new insights into remodelling activities, mechanical strength, and integrity, are profoundly more difficult to measure. Measurement of microscopic mineral content variations in bone material has traditionally been performed using microradiography. Backscattered electron (BSE) imaging is a technique with significantly better resolution than microradiography with demonstrated consistency, and it does not suffer from projection-effect errors. We report results demonstrating the applicability of quantitative BSE imaging as a tool for measuring microscopic mineral content variations in bones representing a broad range of mineralization. Bones from ten species were analyzed with Fourier-transformed infrared spectroscopy, X-ray diffraction, energy dispersive X-ray spectrometry, ash measurements, and BSE imaging. BSE image intensity (graylevel) had a very strong positive correlation to mineral (ash) content. Compositional and crystallographic variations among bones had negligible influence on backscattered electron graylevels. The present study confirms the use of BSE imaging as a tool to measure the microscopic mineral variability in a broad range of mineralized tissues.

Mineralization of cancellous bone after alendronate and sodium fluoride treatment: a quantitative backscattered electron imaging study on minipig ribs

Fluoride stimulates bone formation, whereas bisphosphonates reduce bone resorption. In clinical trials, both treatments increase bone density, although sodium fluoride (NaF) increases and alendronate (bisphosphonate, ALN) decreases bone turnover. In a comparative study using minipigs an inverse correlation has been reported between bone turnover and elastic modulus. Small-angle X-ray scattering (SAXS) measurements of these bones revealed no structural deterioration of the collagen/mineral composite at the nanometer range for ALN-treated vertebra, whereas a slight increase of the average thickness of the mineral crystals as well as changes of the structure of the collagen/mineral composite were found in the bones of NaF-treated animals. In this study we used quantitative backscattered electron imaging (qBSE) to investigate the cancellous bones from ribs of minipigs treated with vehicle, NaF, or ALN. This method provides information on the local mineral concentration in the micrometer range. Mineralization spectra were obtained from each treatment group, and statistically significant differences between ALN and controls were found for the peak position, the peak height, the peak width, and the average calcium (Ca) concentration of the mineral distribution. The results reveal that the cancellous bone matrix was more uniformly mineralized after ALN treatment. The reduced bone turnover induced by ALN, documented histomorphometrically could be at the origin of this phenomenon. No significant differences were detected between NaF and control. Together with the earlier SAXS data these results may explain in part the increase in bone density and the improvement of biomechanical properties observed after ALN treatment in animals and in osteoporotic patients.

Design of insect unguitractor apparatus

The structure of the unguitractor system of insect legs was studied using scanning and transmission electron microscopy. On the base of serial semithin sections, the 3-D reconstruction of structures of the terminal tarsomere was obtained and the arrangement of different types of cuticle was demonstrated. The membrane connects all structures of the system and divides the terminal parts of the claw flexor muscle into the external (unguitractor plate) (UT) and inner (tendon) ones. Elastic nonlayered cuticle located between the claws and the posterior wall of the terminal tarsomere is interpreted as a claw-returning string. Cuticle surrounding the apodeme of the posterior wall of the terminal tarsomere contains large porous canals. The anterior part of the terminal tarsomere has an invagination that forms a plate facing toward the UT. This plate comprises the UT anteriorly and laterally and contains a microtrichia field (MF) on its distal part. The surface of the UT has a complex microstructure providing fixation to the MF of the corresponding surface of the anterior wall of the terminal tarsomere. Microtrichia of the UT and MF are directed to opposite directions and provide anchorage of the UT whenever the flexor claw muscle contracts. The microsculpture of UT and MF for representatives of Odonata, Coleoptera, Hemiptera, Hymenoptera, and Diptera was compared. It is suggested that small insects, which are able to walk quickly on thin rods, usually have wide microplates on the UT plate to provide quicker fixation-release of the UT in the contact area. Insects using the legs to produce hollows in the soil usually have a large UT with well-developed microtrichia on its surface to produce strong friction forces in the contact area for a long period of time. © 1996 Wiley-Liss, Inc.

Vital confocal microscopy in bone

We wished to exploit confocal microscopy for high spatial and temporal resolution vital microscopy in bone. To this end, we evolved implants with glass windows supported in titanium, which were placed in the medial proximal tibial plateau of the rabbit, and special small, self-focussing objectives (dry 10/0.25, water immersion 20/0.45, and oil immersion 45/0.65 and 120/1.0) which mated and matched to the conical window entrance section of the metal components. At intervals of up to 21 months after implant healing, these lenses were used to study live tissue using two genera of confocal microscope: multiple aperture disc, tandem scanning, microscopes for observation in reflection, and video rate confocal laser scanning microscopes for recording, mainly in the fluorescence mode. The latter allowed the study of a variety of intravenously administered substances, including fluorescein, fluorescein-dextrans, fluorescent microspheres, acridine orange, DASPMI, calcein, and tetracycline. We were able to remove blood, stain cells with fluorescent markers, and replace them into the circulation. Calcein and tetracycline bind to the mineral front in bone: this labelling was studied in progress. We observed that both substances partition and remain for long periods (at least days) in adipocytes. Further characterisation of the system used both confocal fluorescence and scanning electron microscopy methods in the study of retrieved implants. These studies showed that the subimplant cortical bone remodelled to a less compact structure with a rich microvasculature extremely close to bone. The points of attachment of bone to glass were found to involve coarse fibres, with the matrix containing large numbers of large cells: some of this tissue was cartilage and some immature bone. An amorphous, mineralised matrix was in immediate contact with glass. The results provide further confirmation of the general utility of high-scan speed confocal methodology in physiology.