First Shark from the Late Devonian (Frasnian) Gogo Formation,Western Australia Sheds New Light on the Development of Tessellated Calcified Cartilage

BackgroundLiving gnathostomes (jawed vertebrates) comprise two divisions, Chondrichthyes (cartilaginous fishes, including euchondrichthyans with prismatic calcified cartilage, and extinct stem chondrichthyans) and Osteichthyes (bony fishes including tetrapods). Most of the early chondrichthyan (‘shark’) record is based upon isolated teeth, spines, and scales, with the oldest articulated sharks that exhibit major diagnostic characters of the group—prismatic calcified cartilage and pelvic claspers in males—being from the latest Devonian, c. 360 Mya. This paucity of information about early chondrichthyan anatomy is mainly due to their lack of endoskeletal bone and consequent low preservation potential.Conclusions/SignificanceThe Meckel’s cartilages show a jaw articulation surface dominated by an expansive cotylus, and a small mandibular knob, an unusual condition for chondrichthyans. The scapulocoracoid of the new specimen shows evidence of two pectoral fin basal articulation facets, differing from the standard condition for early gnathostomes which have either one or three articulations. The tooth structure is intermediate between the ‘primitive’ ctenacanthiform and symmoriiform condition, and more derived forms with a euselachian-type base. Of special interest is the highly distinctive type of calcified cartilage forming the endoskeleton, comprising multiple layers of nonprismatic subpolygonal tesserae separated by a cellular matrix, interpreted as a transitional step toward the tessellated prismatic calcified cartilage that is recognized as the main diagnostic character of the chondrichthyans.     

Etude Histologique et Microradiographique du Cartilage Hémal de la Vertebre de la Carpe, Cyprinus carpio L. (Pisces, Teleostei, Cyprinidae)

The abdominal vertebrae of the adult carp retain a bulk of cartilage at the basement of the haemapophyses. This cartilage has two opposite directions of differentiation. There is an enchondral ossification of the hypertrophic calcified cartilage in its distal area whereas its proximal area is calcifying without previous hypertrophy. The calcification of this proximal area (hyaline calcified cartilage) is permanent and shows typical rings and waves of Liesegang. The calcification of the cartilage of the hemapophyses is of a globular type. The hyaline calcified cartilage is not a metaplastic bone. Other studies, specially with electron microscope, will allow us to understand the innermost process of the different stages of calcification in the cartilage of the carp.     

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.     

Histological structure of the cancellous bone layer in Bothriolepis canadensis (Antiarchi, Placodermi)

The Placodermi are extinct basal gnathostomes which had extensive dermal and perichondral bone, but which lacked the endochondral bone which characterizes the more derived bony fishes. Thin sections of bone from a specimen of the antiarch placoderm Bothriolepis canadensis, from the Escuminac Formation (Frasnian, Upper Devonian), Québec, Canada, reveal that part of the cancellous layer in its dermal and endoskeletal bone formed from perichondral bone trabeculae growing around cartilage spheres. The resultant structure mimics that of osteichthyan endochondral bone. The layout and dimensions of this polygonal mosaic patterning of the bone trabeculae and flattened cartilage spheres resemble those of the prismatic layers of calcified cartilage in chondrichthyans. If the lack of endoskeletal bone in chondrichthyans is a derived character, then the structure identified in B. canadensis could represent a 'template' for the formation of prismatic calcified cartilage in the absence of bone.     

Embryonic development of the axial column in the little skate,Leucoraja erinacea

The morphological patterns and molecular mechanisms of vertebral column development are well understood in bony fishes (osteichthyans). However, vertebral column morphology in elasmobranch chondrichthyans (e.g., sharks and skates) differs from that of osteichthyans, and its development has not been extensively studied. Here, we characterize vertebral development in an elasmobranch fish, the little skate, Leucoraja erinacea , using microCT, paraffin histology, and whole‐mount skeletal preparations. Vertebral development begins with the condensation of mesenchyme, first around the notochord, and subsequently around the neural tube and caudal artery and vein. Mesenchyme surrounding the notochord differentiates into a continuous sheath of spindle‐shaped cells, which forms the precursor to the mineralized areolar calcification of the centrum. Mesenchyme around the neural tube and caudal artery/vein becomes united by a population of mesenchymal cells that condenses lateral to the sheath of spindle‐shaped cells, with this mesenchymal complex eventually differentiating into the hyaline cartilage of the future neural arches, hemal arches, and outer centrum. The initially continuous layers of areolar tissue and outer hyaline cartilage eventually subdivide into discrete centra and arches, with the notochord constricted in the center of each vertebra by a late‐forming “inner layer” of hyaline cartilage, and by a ring of areolar calcification located medial to the outer vertebral cartilage. The vertebrae of elasmobranchs are distinct among vertebrates, both in terms of their composition (i.e., with centra consisting of up to three tissues layers—an inner cartilage layer, a calcified areolar ring, and an outer layer of hyaline cartilage), and their mode of development (i.e., the subdivision of arch and outer centrum cartilage from an initially continuous layer of hyaline cartilage). Given the evident variation in patterns of vertebral construction, broad taxon sampling, and comparative developmental analyses are required to understand the diversity of mechanisms at work in the developing axial skeleton of vertebrates. J. Morphol. 278:300–320, 2017. © 2017 Wiley Periodicals, Inc.     

Ultrastructure of calcified cartilage in the endoskeletal tesserae of sharks

The tesserate pattern of endoskeletal calcification has been investigated in jaws, gill arches, vertebral arches and fins of the sharks Carcharhinus menisorrah, Triaenodon obesus and Negaprion brevirostris by techniques of light and electron microscopy. Individual tesserae develop peripherally at the boundary between cartilage and perichondrium. An inner zone, the body, is composed of calcified cartilage containing viable chondrocytes separated by basophilic contour lines which have been called Liesegang waves or rings. The outer zone of tesserae, the cap, is composed of calcified tissue which appears to be produced by perichondrial fibroblasts more directly, i.e., without first differentiating as chondroblasts. Furthermore, the cap zone is penetrated by acidophilic Sharpey fibers of collagen. It is suggested that scleroblasts of the cap zone could be classified as osteoblasts. If so, the cap could be considered a thin veneer of bone atop the calcified cartilage of the body of a tessera. By scanning electron microscopy it was observed that outer and inner surfaces of tesserae differ in appearance. Calcospherites and hydroxyapatite crystals similar to those commonly seen on the surface of bone are present on the outer surface of the tessera adjacent to the perichondrium. On the inner surface adjoining hyaline cartilage, however, calcospherites of variable size are the predominant surface feature. Transmission electron microscopy shows calcification in close association with coarse collagen fibrils on the outer side of a tessera, but such fibrils are absent from the cartilaginous matrix along the under side of tesserae. Calcified cartilage as a tissue type in the endoskeleton of sharks is a primitive vertebrate characteristic. Calcification in the tesserate pattern occurring in modern Chondrichthyes may be derived from an ancestral pattern of a continuous bed of calcified cartilage underlying a layer of perichondral bone, as theorized by Ørvig (1951); or the tesserate pattern in these fish may itself be primitive.     

Perivascular cells in cartilage canals of the developing mouse epiphysis

Morphological variability among perivascular cells adjacent to cartilage matrix during the elongation of canals through both uncalcified and calcified matrix has not been reported. Cartilage canals were located in distal femoral epiphyses of 5- to 7-day-old mice and identified as vascular channels arising from perichondrial surfaces along the condyles and intercondylar fossae. Three stages of canal development were identified based on the length of canals and on characteristics of chondrocytes and matrix surrounding the canals. Superficial canals terminated in uncalcified matrix of resting cartilage; intermediate canals terminated in matrix containing hypertrophic chondrocytes; deep canals terminated in calcified matrix. The ultrastructural morphology of perivascular cells in contact with the matrix varied in the three stages. Cells resembling fibroblasts and vacuolated macrophages were present adjacent to the uncalcified matrix in superficial canals. At the tips of intermediate canals, cells resembling fibroblasts were larger, contained numerous lysosomes and phagolysosomes, and were in intimate contact with the matrix. At the tips of deep canals, chondroclasts with ruffled borders and clear zones contacted the calcified matrix. The results indicate that 1) mouse epiphyses provide a suitable model for studying cartilage-canal perivascular cells, 2) calcification of cartilage matrix occurs along the course of the canal, and 3) the morphology of perivascular cells in contact with the matrix may be determined, in part, by matrix calcification.     

The effect of calcification on the structural mechanics of the costal cartilage

The costal cartilage often undergoes progressive calcification with age. This study sought to investigate the effects of calcification on the structural mechanics of whole costal cartilage segments. Models were developed for five costal cartilage specimens, including representations of the cartilage, the perichondrium, calcification, and segments of the rib and sternum. The material properties of the cartilage were determined through indentation testing; the properties of the perichondrium were determined through optimisation against structural experiments. The calcified regions were then expanded or shrunk to develop five different sensitivity analysis models for each. Increasing the relative volume of calcification from 0% to 24% of the cartilage volume increased the stiffness of the costal cartilage segments by a factor of 2.3–3.8. These results suggest that calcification may have a substantial effect on the stiffness of the costal cartilage which should be considered when modelling the chest, especially if age is a factor.     

Influence of intermittent compressive force on proteoglycan content in calcifying growth plate cartilage in vitro

We investigated the effect of mechanical stimulation by an intermittent compressive force (ICF) on proteoglycan (PG) synthesis and PG structure in calcified and noncalcified cartilage of fetal mouse long bone rudiments. Uncalcified cartilaginous long bone rudiments were cultured for 5 days in the presence of [35S]sulfate and [3H]glucosamine under control conditions (atmospheric pressure) or under the influence of ICF. ICF was generated by intermittently compressing the gas phase above the culture medium (130 mbar, 0.3 Hz). During culture, the center of the rudiments started to calcify. ICF stimulated calcification such that, after 5 days, the diaphysis of calcified cartilage was about two times as long as in the control cultures. At the end of the experiment, the rudiments were divided in a central calcified diaphysis and two noncalcified epiphyses. Diaphysis and epiphyses were pooled separately. PGs were extracted with 4 M guanidinium chloride and isolated by cesium chloride density gradient centrifugation. PGs (predigested with proteinase K or chondroitinase ABC) were characterized for hydrodynamic size of aggregates, monomers, and chondroitin sulfate chains by gel permeation chromatography and for degree of sulfation by ion exchange chromatography on high pressure liquid chromatography columns. ICF increased the amount of incorporated sulfate per tissue volume unit in the noncalcified epiphyses, but decreased this parameter in the calcified diaphysis. However, in both calcified and noncalcified cartilage, ICF increased the degree of sulfation of the chondroitin sulfate chains. No effects were found on the hydrodynamic size of the PG aggregates or monomers, but in the epiphyses ICF increased the size of the chondroitin sulfate chains. No other changes of structural characteristics of the macromolecules were observed. This study demonstrates that ICF generally stimulated the incorporation of [35S]sulfate into chondroitin sulfate chains. We conclude from the lowered [35S]sulfate content in calcified cartilage that ICF reduced the number of chondroitin sulfate chains and probably PGs while accelerating matrix calcification. It seems likely that the two effects are linked, indicating that a reduction of the number of chondroitin sulfate chains is part of the complicated process of cartilage calcification.     

Growth plate abnormalities in a new dwarf mouse model: tich

Growth plate cartilage calcification has been examined in a recently described mouse mutant, tich, which is co-isogenic with the A.TL strain. Long bones were studied from 1-day-old and 1-month-old mice which carried a homozygous recessive gene mutation making them short limbed and dumpy. Specimens were studied by routine histology, scanning electron microscopy and radiography. In 1-day-old tich mice the front of calcified cartilage was recessed behind the advancing periosteum and bone. No similar recess was seen in control mice. At 1 month of age, a number of the long bone growth plates were irregularly thickened, particularly in the central area. This produced a central tongue of non-calcified cartilage (particularly prominent in the proximal tibia) which gave rise to a corresponding pit in the calcified cartilage layer, in macerated specimens. This was accompanied by poor resorption of calcified cartilage. At both ages the presence of the respective defects was radiographically confirmed. At present it is not known whether this is primarily a defect of calcification or resorption but its presence, apparently from a single mutation in a genetically defined mouse strain, makes it a potentially valuable model.     

EVIDENCE FOR CHANGES IN PROTEIN POLYSACCHARIDE ASSOCIATED WITH THE ONSET OF CALCIFICATION IN CARTILAGE

Past work has suggested that protein polysaccharide may play a role in the calcification of cartilage. Recent electron microscopic studies on noncalcified cartilage have indicated that protein polysaccharide in cartilage matrix is represented by granules associated with collagen fibers. The present work has been designed for comparison of the matrix of noncalcified cartilage to that of calcified cartilage, with particular reference to these granules. Small blocks of tibia from 16-day embryos were fixed in cacodylate-buffered glutaraldehyde and postfixed in either phosphate- or Veronal-buffered osmium tetroxide. Special care was taken to maintain the pH above 7.0 at all times. For electron microscopy the tissues were dehydrated, embedded in Epon 812, sectioned, and stained with uranyl acetate or lead citrate. A marked decrease in the size of granules in the matrix of calcified cartilage compared to noncalcified cartilage was noted. Associated with the decrease in the size of granules was a condensation of matrix components and the presence of an amorphous electron-opaque material that was not seen in noncalcified areas. These results are interpreted to represent either a drop in concentration or a change in state of protein polysaccharide with the onset of calcification in cartilage.     

Immunohistochemical investigation on the presence of chondroitin sulfate in calcification nodules of epiphyseal cartilage.

Chondroitin sulfate localization in mouse epiphyseal cartilage was studied using CS-56 monoclonal antibody immunospecific for the glycosaminoglycan portion of the molecule. For light and fluorescence microscopy, decalcified specimens were embedded in paraffin, Lowicryl, or were frozen and cryostat-sectioned, and the antigen-antibody reaction was demonstrated by treating sections with IgM-peroxidase, IgM-alkaline phosphatase, or IgM-fluorescein conjugates. For electron microscopy, decalcified and undecalcified specimens were embedded in Lowicryl; ultrathin sections from undecalcified specimens were decalcified by flotation on EDTA; sections from both types of specimens were treated with IgM-immunogold conjugate for demonstration of CS-56 reaction. Before immunoreaction, part of all decalcified sections were digested with Streptomyces or testicular hyaluronidase. Control sections were treated with either mouse and goat non-immune serum, or mouse monoclonal antiserum to human dendritic reticulum cells. Both light and electron microscopy show CS-56 reaction with cytoplasmic components of maturing and hypertrophic chondrocytes. Under the light microscope, immunoreaction was not visible in calcified matrix, and was visible in uncalcified matrix only after hyaluronidase digestion. Under the electron microscope, it was evident both in uncalcified and calcified matrix, although the latter showed few immunogold particles, usually placed on areas which appeared incompletely calcified. Gold particles were chiefly distributed at the periphery of calcification nodules and fully calcified matrix. These results show that CS-56, besides reacting with cytoplasm of maturing and hypertrophic chondrocytes, binds to crystal ghosts and other components of cartilage matrix, immunoreactivity decreasing as calcification increases. This suggests that chondroitin sulfate molecules are either degraded during calcification, or segregated into macromolecular complexes, or both degraded and segregated. The second possibility is supported by the increase of immunosensitivity induced by hyaluronidase digestion.     

ELECTRON MICROSCOPIC STUDIES OF INDUCED CARTILAGE DEVELOPMENT AND CALCIFICATION

Cultured, human, amniotic cells (FL strain) injected into the thigh muscles of cortisone-conditioned mice proliferated to form discrete colonies which, over a period of 5 days, became invested by numerous fibroblasts. Cartilage cells and matrix appeared within the fibroblastic zones during the succeeding 2–4 days. Cartilage matrix calcified within 12 days following FL-cell injection. Cartilage cells closely resembled fibroblasts from which they appeared to be derived, and were readily distinguished from FL cells by their prominent ergastoplasm and Golgi complexes. Cartilage matrix was composed of a distinctive feltwork of randomly arranged, collagen fibrils (~600 A axial period and ~250 A width) from which small electron-opaque, leaflike matrix particles extended. Matrix calcification occurred with the deposition of radially arranged needle-like structures resembling hydroxyapatite. Dense centers were often identified within these clusters. Examination of heavily calcified areas revealed confluent masses of apatite-like material. In general, the fine structure of induced cartilage formation and calcification resembled that of cartilage development and calcification as previously described in the normal epiphysis.     

Calcification in the bivalve periostracum

The periostracum in certain bivalves is imbedded with calcified, spiculelike structures analogous if not homologous to cuticular spicules found in the Aplacophora and Polyplacophora (chitons). Although rare or absent in most living bivalves, calcified periostracal structures are apparently an ancestral feature in some bivalve groups, i.e. the Mytilacea, Permophoridae, Myoida. and Anomalodesmata. Ancestors of the Bivalvia and Polyplacophora may have been covered with a flexible, spiculestudded cuticle. Shell plates in these two classes may have originated through a modification of the mechanism of spiculelike cuticular calcification. resulting in a primordial shell with simple prismatic structure.     

Distribution and Immunologic Cross Reactivity of a Phosphohydrolytic Activity of Calcifying Cartilage and Metaphyseal Bone

The increased phosphohydrolytic activity found in calcifying cartilage has breen implicated in the process of normal calcification. Part of this multipotential activity was found to be associated with an extracellular vesicle presumed to be the initial side of calcium salt deposition.
The phosphohydrolytic activity of water extracts from calcifying cartilage and metaphyseal bone has been resolved into three enzymatic entities by DEAE-cellulose column chromatography. The activity which was eluted first, phosphatase I (pyrophosphatase I), increases as cartilage differentiates and calcifies. This increase could serve as a marker for cartilage differentiation and/or calcification. Antibodies to this enzyme isolated from calcifying cartilage or metaphyseal bone cross-react suggesting that the enzymes might, at least in part, be similar.
Cartilage and bone also possess an inorganic pyrophosphatase, pyrophosphatase II, eluted second through the DEAE-cellulose column and another phosphatase, phosphatase II, which was eluted last. By enzymatic and immunologic criteria, it appears that bone and cartilage have the same phosphate-releasing activities indicative of tissues with common cellular origin.
The possible transformation of the differentiating chondrocyte into an osteoblast or osteocyte has been postulated as the cellular mechanism whereby calcified cartilage is replaced by bone. The similarity between the phosphatase I found in epiphyseal cartilage and metaphyseal bone suggests that such transformation is quite likely.     

The differentiation and calcification of chondrocytes in primary cell cultures.

The cartilage from a non-immobilized fracture undergoes a series of morphological and biochemical changes resembling the in vivo differentiation and calcification in the epiphyseal plate. The studies reported here demonstrate that a homogeneous population of chondrocytes isolated from fracture callus fibrocartilage undergoes the same changes in vitro. Chondrocyte primary cultures were grown for 28 days during which time the morphological, histological and histochemical properties of the cultures were studied. Demonstrated by various histological procedures, chondrocytes synthesized the characteristic cartilage matrix, and progressively calcified with increased culture age. This system can be used to elucidate the cellular and molecular mechanisms of calcification.     

Growth cartilage calcification and formation of bone trabeculae are late and dissociated events in the endochondral ossification of <Emphasis Type="Italic">Rana catesbeiana</Emphasis>

Endochondral ossification in the growth cartilage of long bones from the bullfrog Rana catesbeiana was examined. In stage-46 tadpoles and 1-year-old animals, the hypertrophic cartilage had a smooth contact with the bone marrow and the matrix showed no calcification or endochondral bone formation. In spite of showing no aspects of calcification, the chondrocytes exhibited alkaline phosphatase activity and some of them died by apoptosis. However, matrix calcification and endochondral ossification were observed in 2-year-old bullfrogs. Calcium deposits appeared as isolated or coalesced spherical structures in the extracellular matrix of hypertrophic cartilage. Bone trabeculae were restricted to the central area at the sites where the hypertrophic cartilage surface was exposed to the bone marrow. Cartilage matrix calcification and the formation of bone trabeculae were not dependent on each other. Osteoclasts were involved in calcified matrix resorption. These results demonstrate that the calcification of hypertrophic cartilage and the deposition of bone trabeculae are late events in R. catesbeiana and do not contribute to the development and growth of long bones in adults. These processes may play a role in reinforcing bony structures as the bullfrog gains weight in adulthood. In addition, the deposition of bone trabeculae is not dependent on cartilage matrix calcification.     

The calcified-noncalcified cartilage interface: the tidemark

Tidemark is an interface which may better be defined by biochemical methods than by morphology. It originates, by chondrocyte activity, between calcified and noncalcified cartilage layers of any kind, hyaline or fibrous, in areas exposed to either loading (joint) or pulling (insertion). In the articular cartilage it appears with skeletal maturation, in other localizations it is age-independent. It should be regarded as a special instance of a broader phenomenon of the calcification/mineralization front. Inside the joint cartilage its changes reflect the slow remodelling of the calcified layer and its inapparent shift towards the surface of the articular cartilage. In the marginal transitional zone of the joint, tidemark smoothly passes into the periosteum. Chondrocytes on both sides of the tidemark are positive for alkaline phosphatase and the positive reaction continuously goes on to the periosteum.     

Chondrocyte apoptosis is not essential for cartilage calcification: evidence from an in vitro avian model

The calcification of cartilage is an essential step in the process of normal bone growth through endochondral ossification. Chondrocyte apoptosis is generally observed prior to the transition of calcified cartilage to bone. There are, however, contradictory reports in the literature as to whether chondrocyte apoptosis is a precursor to cartilage calcification, a co-event, or occurs after calcification. The purpose of this study was to test the hypothesis that chondrocyte apoptosis is not a requirement for initial calcification using a cell culture system that mimics endochondral ossification. Mesenchymal stem cells harvested from Stages 21-23 chick limb buds were plated as micro-mass cultures in the presence of 4 mM inorganic phosphate (mineralizing conditions). The cultures were treated with either an apoptosis inhibitor or stimulator and compared to un-treated controls before the start of calcification on day 7. Inhibition of apoptosis with the caspase inhibitor Z-Val-Ala-Asp (O-Me)-fluoromethylketone (Z-VAD-fmk) caused no decreases in calcification as indicated by radioactive calcium uptake or Fourier transform infrared (FT-IR) analysis of mineral properties. When apoptosis was inhibited, the cultures showed more robust histological features (including more intense staining for proteoglycans, and more intact cells within the nodules as well as along the periphery of the cells as compared to untreated controls), more proliferation as noted by bromo-deoxyuridine (BrdU) labeling, decreases in terminal deoxynucleotidyl transferase (Tdt)-mediated dUTP nick-end labeling (TUNEL) staining, and fewer apoptotic bodies in electron microscopy. Stimulation of apoptosis with 40-120 nM staurosporine prior to the onset of calcification resulted in inhibition of calcium accretion, with the extent of total calcium uptake significantly decreased, the amount of matrix deposition impaired, and the formation of abnormal mineral crystals. These results indicate that chondrocyte apoptosis is not a pre-requisite for calcification in this culture system.