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IMPORTANCE: Hypopigmented mycosis fungoides is a rare variant of mycosis fungoides with limited published clinicohistopathologic data available. OBJECTIVE: To characterize our patient group, to provide additional information and insight into this malignancy. DESIGN: A 16-year retrospective medical records review (from 1992 to 2009) was conducted of patients with a diagnosis of hypopigmented mycosis fungoides. SETTING: All patients were seen in the department of dermatology at Howard University Hospital, an outpatient clinic in an urban academic institution. PARTICIPANTS: The review comprised of 20 patients. Inclusion required presence of hypopigmented skin lesions and a skin biopsy diagnostic for hypopigmented mycosis fungoides. INTERVENTIONS: Treatment modalities, including oral psoralen with UVA, narrow-band UVB and/or topical medications such as nitrogen mustard and topical corticosteroids were employed. RESULTS: Patients ranged from 4 to 57 years old. Fifteen were African American, three African, one Afro-Caribbean and one Hispanic. The interval from disease onset to diagnosis ranged from 7 months to 24 years. Patients presented at Stage 1A or 1B. Treatment included phototherapy and topical medications. In four patients with pre- and post-treatment biopsies, the original histological diagnosis of hypopigmented mycosis fungoides and the subsequent complete resolution were shown. There was no associated mortality in the patients studied. CONCLUSIONS AND RELEVANCE: Hypopigmented mycosis fungoides affected skin of colour patients in this study. This variant differs from classic mycosis fungoides: younger population, slower progression and the majority of patients remaining in Stage I with treatment. We observed that any repigmentation of lesions suggests an effective treatment regimen, complete repigmentation correlates with clinical and histopathologic resolution, and new hypopigmented lesions during remission suggest relapse. A limitation of this study is the small sample size. This is the first study to correlate the histological resolution of hypopigmented mycosis fungoides with clinical repigmentation of lesions.

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Wall thickness, a major determinant of trabecular thickness, falls with age and falls further in osteoporosis. To estimate the importance of defective osteoblast recruitment in the pathogenesis of this defect, we compared various histologic indices of bone formation in iliac bone biopsies in three groups of subjects--healthy premenopausal women, healthy postmenopausal women, and patients with postmenopausal osteoporosis and at least one non-traumatic vertebral compression fracture. Indices that reflect the frequency of activation of bone remodeling and consequent birth rate of new teams of osteoblasts (osteoid surface, mineralizing surface, osteoblast surface, and bone formation rate, all expressed per unit of bone surface) were each higher in healthy subjects who were postmenopausal than in those who were premenopausal, but lower in osteoporotic than in normal postmenopausal women. In each group, the primary surface measurements were significantly correlated with each other, but the correlation was less close in those with osteoporosis. Indices that reflect the average collective performance of individual teams of osteoblasts (mineralizing surface and osteoblast surface per unit of osteoid surface, mineral apposition rate, adjusted apposition rate, and wall thickness) were all lower in postmenopausal than in premenopausal normal subjects, and even lower in those with postmenopausal osteoporosis. The parameters of the regression lines relating bone formation rate to osteoblast surface were essentially the same in each group, indicating that bone formation rate per unit of osteoblast surface was unaffected by age or menopause, and was the same in osteoporosis as in healthy subjects of similar age.(ABSTRACT TRUNCATED AT 250 WORDS)

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We developed staining techniques that permit identification and histomorphometric analysis of microcracks in the human femoral head 1) from thick, ground bone sections (100 microns) by prestaining with the Villanueva mineralized bone stain (MIBS), and 2) from plastic embedded, undecalcified thin bone sections (5-15 microns) by staining in gallocyanin chrome alum-Villanueva blood stain methods. Both methods represent a significant improvement in the stainability of the microcracks, cellular and tissue elements, and the simultaneous assessment of osteoid seams and tetracycline markers by histomorphometry. Shrinkage and other artifacts were minimized, which helped to clarify some of the uncertainties arising from artifacts resulting from some bone staining methods. Histomorphometric analyses of microcracks were conducted on thick, ground sections of subchondral and trabecular bone. Microcracks were more prevalent in the subchondral bone and osteochondral junction than in the more distant trabeculae. We have consistently localized microcrack areas in bone tissues prepared in these ways.

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We measured the individual lengths of fluorescent labels on the three subdivisions of the endosteal envelope in iliac bone biopsy specimens produced by the administration of both oxytetracycline and demethylchlortetracycline. Fifty-one healthy subjects and 53 patients with postmenopausal osteoporosis were labeled in the stated order, and 8 osteopenic patients were labeled in the reverse order. Whatever the order of administration, the demethylchlortetracycline label was longer than the oxytetracycline label. We conclude: (1) the difference in label lengths reflects a difference between the two compounds in some intrinsic property, whether physical, chemical, or pharmacokinetic. (2) If the calculation of extent of mineralizing surface is based on the mean length of the two labels, a suitable correction should be applied to the shorter label; alternatively, the length of the longer label alone should be used. (3) Unlabeled osteoid not due to label escape probably results from slow terminal mineralization after cessation of matrix synthesis during which too few tetracycline molecules are incorporated to exceed the threshold for visible fluorescence, rather than from the temporary interruption of mineralization followed by its resumption.

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A versatile mineralized bone stain (MIBS) for demonstrating osteoid seams and tetracycline fluorescence simultaneously in thin or thick undecalcified sections has been developed. Bone specimens are fixed in 70% ethanol, but 10% buffered formalin is permissible. Depending upon one's preference, these specimens can be left unstained or be prestained before plastic embedding. Osteoid seams are stained green to jade green, or light to dark purple. Mineralized bone matrix is unstained or green. Osteoblast and osteoclast nuclei are light to dark purple, cytoplasm varies from slightly gray to pink. The identification of osteoid seams by this method agrees closely with identification by in vivo tetracycline uptake using the same section from the same biopsy. The method demonstrates halo volumes, an abnormal, lacunar, low density bone around viable osteocytes in purple. This phenomenon is commonly seen in vitamin D-resistant rickets, fluorosis, renal osteodystrophy, hyperparathyroidism, and is sometimes seen in fluoride treated osteoporotic patients. In osteomalacic bone, most osteoid seams are irregularly stained as indicated by the presence of unmineralized osteoid between mineralized lamellae. The method has been used effectively in staining new bone formation in hydroxyapatite implants and bone grafts. Old, unstained, plastic embedded undecalcified sections are stained as well as fresh sections after removal of the coverslip. This stain also promises to be valuable in the study of different metabolic bone diseases from the point of view of remodeling, histomorphometry, and pathology.

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We measured iliac bone formation rates on all surfaces after double tetracycline labeling, serum levels of type 1 procollagen carboxy-terminal extension peptide (pColl-I-C), and serum levels of total alkaline phosphatase activity (TAP) in four normal subjects and in 44 patients with various forms of metabolic bone disease. In three patients with enzymatic evidence of liver disease both biochemical serum markers were disproportionately raised. In a patient with idiopathic axial osteosclerosis serum pColl-I-C was selectively increased by more than ten-fold. In the remaining 44 subjects pColl-I-C and TAP levels correlated significantly with each other (r = 0.70) and both showed the same directional changes and broadly similar correlations with iliac bone formation rate expressed in different ways. In general, pColl-I-C levels correlated better with cancellous bone formation rates and TAP levels cortical bone formation rates. There was a modest improvement in prediction of bone formation rate with multiple regression using both markers. In 15 patients with typical uncomplicated postmenopausal osteoporosis, neither biochemical marker, singly or jointly, correlated significantly with any expression of bone formation rate. Disadvantages to the use of pColl-I-C as a marker include a significant contribution to the serum level from type 1 collagen biosynthesis in tissues other than bone, and (probably) variable metabolic clearance. For both biochemical markers the most consistently high correlations (r = 0.77-0.79) were found with total bone formation rate for the entire biopsy core volume, which is the best estimate available from a biopsy of formation rate at the bone organ level of organization in vivo. The core volume as a referent also allows the amount of bone formed on cortical, endocortical, and cancellous surfaces to be compared. Measurement of serum pColl-I-C levels merits further study as a noninvasive index of bone metabolism. Differences between normal and abnormal subjects in the relationships between a variety of biochemical markers and a variety of histologic indices have the potential for providing insight into the pathogenesis of osteoporosis.

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We present iliac bone histomorphometric data after in vivo double tetracycline labeling and related biochemical data from 14 nonalcoholic men referred for evaluation of symptomatic spinal osteoporosis. Six patients had previously undiagnosed hypogonadism, and 8 had normal gonadal function and no evident etiology for osteoporosis. Bone histomorphometry revealed no differences in structural measurements or resorption indices between the 2 groups. However, compared to reference values for normal postmenopausal women, osteoblast surface, mineralizing surface, and formation rate were normal or modestly increased in the hypogonadal men and significantly reduced in the idiopathic group. There were significant corresponding differences between the 2 groups in the fasting urinary hydroxyproline to creatinine ratio, an index of bone resorption, and serum total alkaline phosphatase, an index of bone formation. Plasma 25-hydroxyvitamin D levels did not differ between the 2 groups and were above 10 ng/mL in all patients. Plasma 1,25-dihydroxyvitamin D [1,25-(OH)2D] levels were normal in the hypogonadal group and significantly reduced in the idiopathic group, but did not correlate with any histological measurements. The formation indices fell substantially in 3 of 4 hypogonadal men after 7-14 months of therapy with testosterone and a calcium supplement. We conclude the following. In vitamin D-replete hypogonadal men with osteoporosis, 1,25-(OH)2D synthesis is normal, and bone remodeling is modestly increased and correctable by hormone replacement therapy, as in normal postmenopausal women. In middle-aged men with idiopathic osteoporosis, there is impairment of 1,25-(OH)2D synthesis and of the recruitment and activity of teams of osteoblasts, as in postmenopausal osteoporosis.

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Two patients, one with myeloma (Patient 1) and the other with probable chronic lymphocytic leukemia (Patient 2), had reduced renal tubular phosphate reabsorption in the absence of hyperparathyroidism together with other features of the Fanconi syndrome, as consequences of the nephropathy associated with light-chain proteinuria. Both patients had hypophosphatemic osteomalacia, demonstrated for the first time in this condition by iliac bone histomorphometry after in vivo double tetracycline labeling, despite absence of bone pain or Looser zones. Neither patient was vitamin D-depleted, but plasma calcitriol level was normal in Patient 1 and low in Patient 2; only the latter patient had severe muscle weakness. Complete histologic correction of osteomalacia was achieved by treatment in accordance with the biochemical defects--oral phosphate therapy alone in Patient 1 and combined with calcitriol in Patient 2. Both patients are now symptom-free, five and three years after the initial diagnosis of bone disease and hematogenous malignancy. Thirteen previous instances of the same form of osteomalacia were reviewed; in most cases, the Fanconi syndrome developed before its probable cause became apparent. The Fanconi syndrome has also been reported in two cases of osteomalacia due to mesenchymal tumor, but not in osteomalacia associated with prostatic carcinoma. Light-chain nephropathy and consequent renal tubular dysfunction appears to be a third form of oncogenous osteomalacia.

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A gallocyanin method for demonstrating cement lines in thin, undecalcified sections of bone has been developed that is compatible with prestaining with osteochrome before plastic embedding. After sectioning at 5 microns on the Jung K heavy duty microtome, the sections are attached to a microslide using Haupt's adhesive mounting medium, placed on a slide warmer at 37 C until completely dry, and deplasticized in xylene at 45 C for 16-24 hr. Sections are stained with 0.15% gallocyanin-5% chrome alum solution for 30 min, followed by staining in buffered Villanueva blood stain for 1-1 1/2 hr, quickly dehydrated, differentiated in equal parts xylene and 100% ethanol, cleared, and mounted in Eukitt's medium. Reversal lines appear as thin, scalloped, blue or purple lines approximately 0.3 micron wide, and arrest lines as thick, homogeneous, straight or evenly curved, dark blue or purple lines approximately 2 microns wide. The method also demonstrates abnormal halo volumes around osteocytes, old and new bone matrix, osteoid seams, and the granular mineralization front at the osteoid-bone interface. It promises to be valuable in the study of age-related bone loss, osteoporosis, and metabolic bone disease.

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We compared indices of three-dimensional microstructure of iliac trabecular bone between 26 patients with vertebral compression fractures due to postmenopausal osteoporosis and 24 control subjects without vertebral fracture, who were matched for age, sex, race, menopausal status, and several densitometric and histologic indices of both cortical and trabecular bone mass. The patients with fracture had a significantly lower mean value (1.03 +/- 0.15 vs. 1.26 +/- 0.26; P less than 0.005) for indirectly calculated mean trabecular plate density, an index of the number and connectivity of structural elements, and as a necessary corollary, a significantly higher mean value for the mean thickness of structural elements. Plate density was more than one standard deviation below the age-adjusted mean value for normal postmenopausal white females in 19 (73%) of the fracture cases and in only 5 (21%) of the nonfracture cases (P less than 0.001). We conclude that the biomechanical competence of trabecular bone is dependent not only on the absolute amount of bone present but also on the trabecular microstructure.

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We examined the relationships between the changes in bone mineral deficit in the radius, determined by single-energy photon absorptiometry at standard proximal and distal sites, and in the ilium, determined by bone histomorphometry, during the treatment of osteomalacia of diverse etiology in 28 patients. In the ilium, relative osteoid volume decreased by 75-80% in both cortical bone (from 6.0% to 1.5%) and trabecular bone (from 30.1% to 6.6%) during a mean treatment duration of 2 yr. There was also a significant fall in iliac cortical porosity from 10.3% to 7.8%. As a result, mineralized bone volume increased by 7.5% in cortical and by 40.1% in trabecular bone; the cortical and trabecular increments were correlated (r = 0.69, P less than 0.001). The properly weighted increase for the entire tissue sample was 18.6%. By contrast, there was no change in bone mineral at either radial site, although there was a 2% increase at both sites when allowance was made for age-related bone loss during treatment. The proximal and distal age-adjusted increments was correlated (r = 0.76, P less than 0.001), but there was no correlation between the changes in any photon absorptiometric and any histomorphometric index. In that iliac cortical bone turnover in normal subjects was 7.2%/yr, we estimated the rate of bone turnover to be less than 2%/yr at both proximal and distal radial sites, including any trabecular bone present at the distal site. Compared to appropriate control subjects, the bone mineral deficits fell during treatment from 19.2% to 17.1% at the proximal radius (greater than 95% cortical bone) and from 20.5% to 18.5% at the distal radius (greater than 75% cortical bone). In the ilium the deficits, assuming attainment of normal values for osteoid volume and cortical porosity, fell from 41.7% to 36.1% in cortical and from 31.5% to 6.3% in trabecular bone, the properly weighted combined deficit falling from 38.6% to 27.7%. The irreversible iliac cortical deficit was entirely due to cortical thinning because of increased net endosteal resorption; the resultant expansion of the marrow cavity offset the modest loss of fractional trabecular mineralized bone. We conclude: in osteomalacia there is a large irreversible and a small reversible bone mineral deficit at both proximal and distal radial sites, in similar proportion to the iliac cortex but of smaller magnitude; the anatomic basis of the irreversible bone mineral deficit at all three sites that persists despite correction of the mineralization defect by appropriate treatment is thinning of cortical bone, most likely owing to prolonged secondary hyperparathyroidism; (c) there is no evidence that the proportion of trabecular bone in the distal radius at any site proximal to the radioulnar joint has any relevance to the interpretation of measurements made at that site; (d) there are at least three functional subdivisions of trabecular bone depending on proximity to hematopoietic marrow, fatty marrow, or synovium; and (e) single photon absorptiometry of the radius is an excellent method for measuring cortical bone mass in the appendicular skeleton, but is of little value for the assessment of changes in trabecular bone status.

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We performed iliac bone histomorphometry after in vivo double tetracycline labeling 3-14 years after intestinal bypass surgery for obesity in 21 patients, selected because of clinical suspicion of metabolic bone disease, and compared the results with those of 40 age-matched normal control subjects. Osteomalacia defined by rigorous kinetic criteria was found in six cases, histologic features of secondary hyperparathyroidism without significantly impaired mineralization in one case, and possible osteomalacia masked by impaired matrix synthesis in one case. In the patients with definite osteomalacia, nonfracture bone pain was more frequent, corrected plasma calcium lower, plasma alkaline phosphatase and magnesium higher, and secondary hyperparathyroidism more severe than in the other patients. In the patients without osteomalacia there was a 24.5% reduction in trabecular bone volume compared to the controls; in contrast to age-related bone loss and post-menopausal osteoporosis, this was due mainly to reduction in the thickness rather than the density of trabecular plates. About two-thirds of the reduction in trabecular thickness was due to reduction in interstitial bone thickness, representing the cumulative effect of increased depth of osteoclastic resorption cavities, probably due in part to secondary hyperparathyroidism. About one-third of the reduction in trabecular thickness was the result of reduced mean wall thickness, representing insufficient osteoblastic matrix synthesis, probably due in part to malabsorption of an unidentified nutrient necessary for normal bone health. Resorption indices were not increased at the time of the biopsy, but there were persistent defects in the recruitment and activity of osteoblasts. Clinically significant bone loss after intestinal shunt surgery, as in several other clinical situations, results from the combined effects of an unsustained increase in bone resorption and a sustained decrease in bone formation.

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We devised a new method for examining the structural changes that occur in trabecular bone in aging and in osteoporosis. With simultaneous measurement of total perimeter and bone area in thin sections, indirect indices of mean trabecular plate thickness (MTPT) and mean trabecular plate density (MTPD) can be derived, such that trabecular bone volume = MTPD X MTPT. MTPD is an index of the probability that a scanning or test line will intersect a structural element of bone, and is the reciprocal of the mean distance between the midpoints of structural elements, multiplied by pi/2. We applied this method to iliac bone samples from 78 normal subjects, 100 patients with vertebral fracture, and 50 patients with hip fracture. The reduction in trabecular bone volume observed in normal subjects with increasing age was mainly due to a reduction in plate density, with no significant decrease in plate thickness. The further reduction in trabecular bone volume observed in patients with osteoporotic vertebral fracture was mainly due to a further reduction in plate density. There was a relatively smaller reduction in plate thickness that was statistically significant in males but not in females. Only in patients with hip fracture did trabecular thinning contribute substantially to the additional loss of trabecular bone in osteoporosis relative to age. These data indicate that age-related bone loss occurs principally by a process that removes entire structural elements of bone; those that remain are more widely separated and some may undergo compensatory thickening, but most slowly become reduced in thickness. We propose that the process of removal is initiated by increased depth of osteoclastic resorption cavities which leads to focal perforation of trabecular plates; this is followed by progressive enlargement of the perforations with conversion of plates to rods. The resulting structural changes are more severe in osteoporotic patients than in normal subjects, but have been completed in most patients before they develop symptoms.

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A modified toluidine blue method for identification of the mineralization front at the zone of demarcation between bone and osteoid in undecalcified, plastic-embedded sections of bone is described. The intensity of staining is increased both by increasing the pH of the solution and by increasing the duration of staining. The method is reproducible, since measurements of the extent of mineralization front on two nonadjacent sections from the same biopsy in 20 cases had a correlation coefficient of 0.98. The identification of the mineralization front by toluidine blue agrees closely with identification by means of in vivo tetracycline uptake, with a correlation coefficient of 0.97 between measurements of its extent using the two methods on adjacent sections from the same biopsy. It is likely that both toluidine blue staining at pH 6.5 and tetracycline uptake depend on some property of the most recently deposited bone mineral. With either method we find low values for the extent of mineralization front as a fraction of osteoid surface in many patients with osteoporosis. The uniformly normal values for this quantity in osteoporosis reported by other investigators may reflect different criteria for distinguishing osteoid-covered from quiescent bone surfaces.

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Disodium hydroxymethanediphosphonic acid was administered subcutaneously (s.c.) to adult beagle dogs for 1 to 2 years at various dose levels to determine its skeletal effects when given chronically. The effects were followed densitometrically, radiographically and by making histomorphometric measurements in sequential rib biopsies. At low doses (0.1 and 0.5 mg/kg/day s.c.) EHDP caused a time-and-dose dependent reduction in the percentage of bone surfaces with active mineralization, a reduction in mineralization rates, a reduction in resorption spaces but no changes in osteoid seam widths. No treatment related bone fractures were noted at the 0.1 mg/kg/day level, while at 0.5 mg/kg/day, fracture incidence appeared slightly increased. At higher doses (2-10 mg/kg/day), there was also a reduction in the number of resorption spaces, but mineralization activity was totally blocked, osteoid seams became thickened and fracture incidence was markedly increased. In one group of animals, EHDP treatment was discontinued after one year of dosage at 5 mg/kg/day given subcutaneously. In these animals, mineralization activity reappeared within 3 months, but osteoid seams remained thickened until 7 months post-treatment. These data indicate that EHDP can have profound effects on bone remodeling in the dog but that these effects are dose-and-time-dependent and they appear to be reversible.

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Nubian bone recovered from an X-group cemetery (A.D. 350 to 550) exhibits a pattern of fluorescence identical to that of modern tetracycline-labeled bone. When it is viewed under ultraviolet light at 490 angstroms, fluorophors are visible as a characteristic yellow-green fluorescence on surfaces that were actively mineralizing at the time of exposure. Contamination of stored grains provided the proper environment for cultivation of tetracycline-producing Streptomycetes. Evidence for exposure to antibiotics in an archeological population is relevant to studies of the evolution of R factors and to the interpretation of health and disease within the population.

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