| Atlas | Wheater’s, Skeletal tissues - Bone |
|---|---|
| Text | Ross and Pawlina , Chapter 7 Cartilage and Chapter 8 Bone |
Mature Bone
Intramembranous Bone Formation
Endochondral Bone Formation
There is no single perfect section in which to study bone and its formation. The process involves transitions, and the various stages are simply too many to be encompassed in any one section. Even the many slides available in this session may not have all the structures you need for study, so try to look as many different slides as you can. With the exception of slide #51 and #93, all the slides you study have been decalcified by the action of acid or a chelating agent, so you will be looking at the remaining organic matrix. Bone is difficult to cut in paraffin so there are distortions and differential shrinkages, common events that lead to an almost universal separation of the bone from the periosteum. If you look long enough, however, you’ll find intact areas; these areas are the ones with which to start your study.
Slide 46-HE (embryonic face, H&E) WebScope ImageScope
Slide 46-M (embryonic face, Masson trichrome) WebScope ImageScope
Slide 46-M-N (new scan of slide 46M) WebScope ImageScope
Slide 120 (head, 66mm embryo, H&E) WebScope ImageScope
Slide 120-N (new scan of slide 120) WebScope ImageScope
These sections of human faces exhibits all stages of intramembranous bone formation. Use figures 10.5 and 10.6 in the Wheater’s atlas (pg 190) for cell identification. Wheater’s covers long bone formation exclusively, but some of the images can be useful in membrane bone formation. These frontal sections of a fetal human face are stained with either H&E or H & Masson. You should be able to find:
Slide 115-N (palate, H&E) WebScope ImageScope
Slide 115-M (palate, Masson) WebScope ImageScope (note: this slide is a bit dark; in ImageScope, go to the Image menu, then select Adjustments to adjust the brightness and contast if necessary)
Further stages of developing a compact bone from a spongy one are illustrated in this parasagittal section of the palate. Note the increased numbers of osteocytes, in some places forming one or two rings of an osteon. In the H&E section, the rapidly formed, immature bone (aka “woven” bone) [example] exhibits a greater affinity for hematoxylin and higher cell density compared to mature bone. An outer fibrous layer and loose inner layer of periosteum can be seen. Sharpey’s fibers made primarily of type I collagen spanning the cellular layer of periosteum and inserting into the bone are well illustrated in the both the H&E [example] and Masson-stained [example] sections.
Slide 48 (leg, 154mm embryo, H&E) WebScope ImageScope
Slide 48b (leg, 154mm embryo, Masson) WebScope ImageScope
One slide is stained with H&E, while the other is stained with trichrome. Only long bones grow in length by proliferative activity at the epiphyseal plate and subsequent endochondral ossification. Appositional growth increases their circumference. New bone is laid down around the shaft of a long bone by a mechanism that is essentially the same as that of intramembranous ossification (many authors use this term to describe the process–which can confuse you!). In this cross section of the developing tibial and fibular shafts (two stains again) note particularly the osteoblastic activity, and the forming osteons at the outer edge of the shafts in the H&E [example] and trichrome sections [example] .With the Masson stain you may see collagen fibers [example] running from the fibrous periosteum to the bone –what are they? (hint: refer to slide 115 above) The purple area in the Masson stained section is calcified cartilage - see endochondral section that follows.
Slide 49_20x (humerus, H&E) WebScope ImageScope
Slide 49_40x (humerus, H&E) WebScope ImageScope
There are two different magnifications (20X and 40X) of the epiphysis of a human long bone (those of you with even locker numbers may have a canine specimen on slide #49 that is much better). We require you to recognize 5 zones (W pg 200, 10.21): 1) resting or reserve (R); 2) proliferative (P); 3) hypertrophy (H); 4) calcification (D); and 5) ossification (O). These specimens do not permit an actual distinction between hypertrophic and calcification, but make sure you understand the sequence ! Note the persistence of the cartilage cores well into the marrow cavity (W pg 201, 10.22). Please remember that the zone of hypertrophy is the weakest region of the epiphyseal growth plate. It is here that the process of cartilage calcification is starting and no bone has yet been deposited on its surface. Therefore, it is prone to breakage in children. Also find the secondary center of ossification [example] in slide 49 that is just starting to form in the head of the bone (there are blood vessels present in the cartilage, but it hasn’t yet started to ossify); the primary center of ossification is in the shaft of the bone. Note that hyaline cartilage in the head of the bone, while avascular, certainly contains spaces for traversing large blood vessels indicative of bone formation. An example in which bone can actually be seen in the secondary ossification center may be found in slide 61 in the UCSF collection ImageScope WebScope ImageScope .
Slide 108 (finger, H&E) WebScope ImageScope
Slide 110 (finger, H&E) WebScope ImageScope
Slide 47 (knee, sheep embryo, H&E) WebScope ImageScope
These slides are useful for looking at other examples of endochondral ossification because you can see the entire forming bone and adjacent joint cavities. Look at the cartilage ends (epiphyses) and the forming bony shaft. The phalanges do not develop an epiphyseal plate, but the same process of growth and calcification of cartilage takes place, a process that can be seen more easily in slide #108 [example] than in #110 [example] . Examine the periosteum and forming marrow cavity. Slide #47 [example] of a developing knee joint also illustrates endochondral bone formation quite well. The intense basophilia present in the zone of ossification is likely due to abundant glycosaminoglycans (GAGs) associated with proteins (e.g. ostenectin, osteocalcin, and ostepontin) involved with the early stages of matrix ossification.
Note: this section is repeated from the Cartilage/Mature Bone lab session. However, NOW you know what “interstitial lamellae” are and how they form, so be sure you can identify them.
Slide 50 (compact bone, decalicified, H&E) WebScope ImageScope
Even though this section is distorted, you should be able to find osteons in various stages of development, lacunae, and canaliculi (to see canaliculi you will need to use your microscope and the glass slide from your collection –cut down the light by closing down the iris diaphragm to see them). Incremental deposition similar to that which would be present in inner and outer circumferential lamellae can be seen.
Ground sections:
Slide 51 (cross section) WebScope ImageScope
Slide 93B (cross section) WebScope ImageScope
Slide 93A (long section, thin) WebScope ImageScope
Slide 51 (long section, 20x) WebScope ImageScope
Slide 51L-EX (long section, 40x) WebScope ImageScope
Slide 93C (long section) WebScope ImageScope
There are both longitudinal and cross sections. First, study cross sections (#51, #93B). In these sections, the trapped air bends the light giving a dark image; the mineral and matrix generally transmit the light. You should be able to identify osteons and their subdivisions (as in slide 50), interstitial lamellae, Haversian canals and nutrient canals (Volkmann). Note that the latter canals penetrate osteons without causing new lamellae to be laid down around them. Study the thinnest ground section (#93A) to identify lacunae and canaliculi. (W pg 193, 10.10a; in this figure the tissue is “unstained” but a red dye has been used to illustrate canals, lacunae and canaliculi). Now, look at the longitudinal sections (#51-20x, #51-40x, or #93C) of compact bone and try identifying the various structures mentioned above, especially Haversian and Volkmann’s canals.
This is sometimes called "direct" bone formation because it does not involve cartilage. Hence, chrondocytes would not be found in this section. The term "membrane" is used here because the periosteum around forming bone appears like a membrane. Make sure you know the structural and functional differences between an osteoblast and osteocyte. Observe (and remember) that the bone formation, which occurs from the periosteum of the diaphysis of long bones is identical to the process of intramembranous bone formation. In this unique micrograph, study the differentiation of osteoprogenitor cells to osteoblasts and subsequently to osteocytes. What is osteoid? (BO8) Note the formation of long cell processes as the osteoblast (lower right corner) prepares for the transformation into an osteocyte. Find the cell process, which is already located in a canaliculus.
The calcium crystals of the bone matrix were removed in this preparation by a decalcification process. Note how coarse the collagenous fibrils are and the difficulty in visualizing the periodicity of the fibrils (probably due to the process of mineralization).
Study the transition that occurs in the chondrocytes as they change from very active to hypertrophied and dying. Why do the chondrocytes die?(BO9)
Study the changes that are associated with the removal of the cartilage and the deposition of a bone matrix.
The osteoclast is a very large cell (multinucleated) that sits on the surface of bone matrix. Note the many lysosomes and phagocytic vacuoles. What is the functional significance of these structures?(BO10). Most osteoclasts are thought to arise by fusion of monocyte-macrophages
Note the "inactive" appearance of endosteal cells. The presence of a macrophage in the Haversian canal indicates the potential eroding function of the endosteal lining of the canal. Why are blood vessels so important in bone? (MatureBO2)