Bone

  • AN71.1 Identify bone under the microscope; classify various types and describe the structure-function correlation of the same.

Introduction

  • Bone is a specialized connective tissue characterized by an extracellular matrix rich in calcium salts.
  • It consists of living cells embedded within a highly mineralized matrix.
  • Matrix mineralization provides bones with strength, rigidity, and resistance to mechanical stress.
  • Bone is a dynamic tissue that continuously undergoes remodeling in response to physical demands and hormonal influences.
  • Bones protect vital organs, provide structural support, and serve as major reservoirs of calcium and phosphate.
  • Bone also contains bone marrow, which is responsible for hematopoiesis (blood cell formation).

General Features of Bone

  • A long bone consists of a central shaft (diaphysis) and two expanded ends (epiphyses).
  • In cross-section, a long bone is composed of the diaphysis, epiphyses, and connective tissue coverings, namely the periosteum externally and endosteum internally.
  • The diaphysis forms a strong tubular structure that encloses the medullary (marrow) cavity.
  • Its wall is primarily made of compact (cortical) bone, which is dense and contains very few visible spaces.
  • The epiphyses contain a thin outer layer of compact bone surrounding an internal network of bony trabeculae.
  • This trabecular framework encloses numerous marrow-filled spaces, giving rise to spongy (cancellous or trabecular) bone.
  • The articular surfaces of the epiphyses are covered by hyaline articular cartilage.
  • This smooth, resilient cartilage reduces friction, absorbs mechanical stress, and facilitates efficient movement at synovial joints.
Figure 6.1: General features of long bone

Covering of Bone

  • Bone surfaces are covered by specialized connective tissue membranes that support growth, repair, and remodeling.
  • The periosteum covers the external surface of bone, except at sites of tendon or ligament attachment and areas covered by articular cartilage.
  • It consists of two layers: an outer fibrous layer and an inner osteogenic (cellular) layer containing osteoprogenitor cells.
  • The endosteum is a thin membrane lining the internal surfaces of bone, including the medullary cavity and trabecular spaces of spongy bone.
  • Unlike the periosteum, the endosteum is composed mainly of a single layer of osteoprogenitor cells.
  • The endosteum is thinner than the periosteum and is the most metabolically active bone lining, playing a key role in bone remodeling and repair.

Composition of Bone Tissue

  • Bone is a specialized type of connective tissue. It consists of three basic components as follows
    1. Cells
    2. Fibers
    3. Ground substance.
Figure 6.2: Composition of bone tissue

Cells of Bone Tissue

  • Bone tissue consists of five types of cells: Osteoprogenitor cells, osteoblasts, osteocytes, bone lining cells, and osteoclasts.
Figure 6.3: Cells of bone

Osteoprogenitor Cells

  • Osteoprogenitor cells are mesenchymal stem cells that serve as precursors of bone-forming cells.
  • They are located in the inner osteogenic layer of the periosteum, endosteum, and along the walls of Haversian and Volkmann’s canals.
  • These cells differentiate into osteoblasts, which synthesize and form new bone tissue.
  • Osteoprogenitor cells are abundant during fetal development and childhood, but their number gradually decreases with age.
  • Bone morphogenetic proteins (BMPs) and insulin-like growth factors (IGFs) promote their differentiation into osteoblasts.
  • Exposure to controlled electromagnetic fields may enhance osteogenic differentiation and support fracture healing.
  • Histologically, they appear as flattened, spindle-shaped cells with elongated or oval nuclei and closely resemble fibroblasts.

Function: They give rise to osteoblasts.

Osteoblasts

  • Osteoblasts are specialized bone-forming cells derived from osteoprogenitor cells.
  • They are typically cuboidal to polygonal in shape and are arranged along surfaces where new bone is being deposited.
  • Histologically, osteoblasts possess an eccentrically placed oval, euchromatic nucleus and a basophilic cytoplasm rich in protein-synthesizing organelles.
  • Ultrastructurally, they contain abundant rough endoplasmic reticulum, Golgi apparatus, and secretory vesicles, reflecting their high synthetic activity.
  • Cytoplasmic processes of adjacent osteoblasts communicate through gap junctions.

Functions of Osteoblasts

  1. Osteoblasts synthesize type I collagen, the principal organic component of bone matrix.
  2. They also produce matrix proteins such as osteocalcin, osteonectin, bone sialoprotein, and proteoglycans.
  3. These cells secrete alkaline phosphatase, an enzyme involved in bone mineralization.
  4. Elevated serum alkaline phosphatase may indicate increased bone formation, although it can also occur in conditions such as pregnancy and liver disease.

Osteocytes

  • Osteocytes are mature bone cells located within small cavities called lacunae in the mineralized bone matrix.
  • They are derived from osteoblasts that become enclosed within the matrix they secrete.
  • During transformation into osteocytes, the cells decrease in size and show reduced synthetic activity with fewer organelles.
  • Osteocytes extend cytoplasmic processes through tiny channels called canaliculi, forming connections with neighboring osteocytes and surface bone cells.
  • This interconnected network facilitates the exchange of nutrients, waste products, and signaling molecules within bone tissue.
  • In routine H&E-stained sections, osteocytes exhibit lightly basophilic or eosinophilic cytoplasm due to limited rough endoplasmic reticulum.
  • During histological preparation, decalcification may cause osteocytes to shrink or disappear from lacunae.
  • The average lifespan of an osteocyte is approximately 10–20 years.

Functions of osteocytes

  1. Osteocytes maintain the structural integrity of bone and play a central role in bone remodeling and mechanosensation.

Osteoclasts

  • Osteoclasts are large, multinucleated cells specialized for bone resorption.
  • They are located on bone surfaces undergoing active remodeling and breakdown.
  • During resorption, osteoclasts create shallow depressions known as Howship’s lacunae (resorption bays).
  • Histologically, they are large cells (approximately 50–150 μm in diameter) with multiple nuclei and abundant eosinophilic cytoplasm.
  • Osteoclasts secrete tartrate-resistant acid phosphatase (TRAP), an important marker of osteoclastic activity.

Functions of Osteoclasts

  1. Their primary function is the degradation and removal of bone matrix.
  2. They release lysosomal enzymes, including cathepsin K and matrix metalloproteinases, which digest the organic matrix.
  3. Osteoclasts also generate an acidic microenvironment that dissolves bone minerals and facilitates resorption.

Bone-lining Cells

  • Bone-lining cells are flattened cells that cover bone surfaces where neither active bone formation nor bone resorption is occurring.
  • They form a continuous, epithelium-like layer on the periosteal and endosteal surfaces and line internal bone channels.
  • These cells are derived from inactive osteoblasts.
  • Bone-lining cells help regulate the exchange of calcium, phosphate, and nutrients between bone tissue and the surrounding environment.
Figure 6.4: Cells of bone and their functional correlation

Bone Matrix

  • Bone matrix is the extracellular material of bone and consists of organic and inorganic components.
  • The organic component is composed of collagen fibers and ground substance, which together provide flexibility and tensile strength.
  • Approximately 90% of the organic matrix is formed by collagen fibers, while the remaining 10% consists of ground substance containing proteoglycans and glycoproteins.
  • The inorganic component is primarily made up of mineral salts, especially hydroxyapatite crystals, which impart hardness and resistance to compression.
  • The combined action of organic and inorganic components gives bone its unique strength and durability.

Classification of Bones

  • Bones can be classified using gross anatomical and histological characteristics.
  • Based on gross (macroscopic) appearance:
    1. Compact bone is dense and lacks visible cavities.
    2. Spongy (cancellous or trabecular) bone contains numerous interconnected spaces, giving it a porous appearance.
  • Based on histological structure:
    1. Woven (immature) bone contains irregularly arranged collagen fibers and is found during fetal development and early fracture repair.
    2. Lamellar (mature) bone contains organized layers (lamellae) of collagen fibers and forms the normal adult skeleton.
  • Bones may also be classified according to shape into long, short, flat, irregular, and other categories in gross anatomy.

Compact Bones

  • Compact bone is a dense type of bone that lacks visible cavities on gross examination.
  • It forms the diaphysis of long bones, the thin outer layer of epiphyses, the outer and inner tables of flat bones, and the external layer of most other bones.
  • In flat bones, the intervening spongy bone is known as the diploë.
  • In living bone, the outer surface is covered by the periosteum, while the inner surface is lined by the endosteum.
  • These coverings are absent in ground sections of dry bone prepared for microscopic study.
  • Microscopically, compact bone is organized into three lamellar patterns:
    1. Haversian (osteonal) lamellae
    2. Interstitial lamellae
    3. Circumferential lamellae (outer and inner)
Figure 6.5: Structure of compact bone

Haversian System of Lamellae

  • The osteon (Haversian system) is the structural and functional unit of compact bone.
  • Each osteon consists of a central Haversian canal surrounded by 4–15 concentric lamellae of mineralized bone matrix.
  • Haversian canals run parallel to the long axis of the bone and, in living tissue, contain blood vessels, nerves, loose connective tissue, and lymphatics.
  • In ground sections of dry bone, these canals may appear empty or contain debris.
  • Small spaces called lacunae are located between adjacent lamellae and house osteocytes.
  • Fine channels known as canaliculi radiate from lacunae and contain osteocyte processes, allowing communication and nutrient transport between cells.
  • Within each lamella, collagen fibers are arranged parallel to one another, while fibers in adjacent lamellae are oriented in different directions, increasing bone strength.
  • Volkmann’s (perforating) canals connect neighboring Haversian canals and transmit blood vessels and nerves from the periosteum into the bone.
  • Unlike Haversian canals, Volkmann’s canals run obliquely or perpendicular to the bone axis and are not surrounded by concentric lamellae.
  • In transverse sections, a Haversian canal appears as a circular or oval central opening encircled by concentric lamellae, whereas Volkmann’s canals appear as transverse or oblique channels connecting adjacent osteons.
  • In longitudinal sections, Haversian canals run parallel to one another, while Volkmann’s canals cross between them.
  • Each osteon is bounded by a distinct cement line, a highly mineralized layer that contains little or no collagen and clearly demarcates the osteon from surrounding bone.
Figure 6.6: Osteocytes in lacunae

Interstitial Lamellae

  • Bone undergoes continuous remodeling, during which old osteons are resorbed and new osteons are formed.
  • Newly formed osteons contain a central Haversian canal surrounded by concentric lamellae.
  • Remnants of partially resorbed older osteons persist between adjacent osteons and are known as interstitial lamellae.
  • Interstitial lamellae contain lacunae with osteocytes and interconnected canaliculi.

Circumferential Lamellae

  • Circumferential lamellae are broad layers of bone matrix that encircle the entire circumference of compact bone.
  • They are of two types:
    • Outer circumferential lamellae, located immediately beneath the periosteum.
    • Inner circumferential lamellae, situated adjacent to the endosteum and surrounding the medullary cavity.

Periosteum

  • The periosteum is a connective tissue membrane covering the external surface of bone, except at articular surfaces.
  • It consists of:
    • An outer fibrous layer rich in collagen fibers.
    • An inner osteogenic layer containing osteoprogenitor cells, especially prominent in growing bone.
  • The periosteum is highly vascular, and its blood vessels communicate with osteonal vessels through Volkmann’s canals.

Endosteum

  • The endosteum is a thin cellular lining covering the internal surfaces of bone, including the medullary cavity, trabecular spaces of spongy bone, and Haversian canals.
  • It is typically a single-cell-thick layer composed of osteoblasts, osteoclasts, bone-lining cells, and osteoprogenitor cells, and plays an important role in bone growth, repair, and remodeling.
Figure 6.7: Transverse section of compact bone/ground bone
Figure 6.8: Longitudinal section of dry, compact bone
Figure 6.9: Detailed structure of osteon at high magnification
Figure 6.10: Histology of compact bone

Spongy Bone

  • Spongy bone, also known as cancellous or trabecular bone, forms the interior of epiphyses of long bones and the core of short, flat, and irregular bones.
  • It is covered externally by a thin layer of compact bone.
  • Grossly, it has a porous appearance due to numerous spaces between interconnected bony plates or rods called trabeculae.
  • Unlike compact bone, trabeculae do not contain Haversian systems (osteons).
  • Osteocytes are located within lacunae in the trabeculae and communicate through fine canaliculi containing their cellular processes.
  • Because trabeculae are thin, nutrients can diffuse directly from adjacent marrow spaces; therefore, a Haversian system is unnecessary.
  • Trabecular surfaces are lined by endosteum and are associated with osteoblasts, osteoclasts, and osteoprogenitor cells, which participate in bone remodeling and repair.
Figure 6.11: Cancellous bone with trabeculae and bone marrow cavities
Figure 6.12: Histology of spongy bone

Formation and Growth of Bone

  • Most bones develop from mesenchymal tissue derived from mesoderm, although much of the facial skeleton receives contributions from neural crest cells.
  • The process of bone formation is called ossification (osteogenesis).
  • Ossification occurs by two principal mechanisms:
    • Intramembranous ossification involves the direct differentiation of mesenchymal cells into bone-forming cells without a cartilage precursor.
    • Bones formed by this process are called membranous bones.
    • Examples include the bones of the cranial vault, much of the mandible, and a major part of the clavicle.
    • Endochondral ossification involves the formation of a hyaline cartilage model that is subsequently replaced by bone.
    • Bones formed through this mechanism are termed cartilaginous bones.
    • Examples include most long bones (except much of the clavicle), the base of the skull, vertebrae, and ribs.
  • Both processes contribute to the development, growth, and remodeling of the skeletal system.

Zones of epiphyseal cartilage

  • The epiphyseal (growth) plate is responsible for longitudinal growth of long bones. It appears during fetal development and remains active until skeletal maturity.
  • During endochondral ossification, vascular endothelial growth factor (VEGF) promotes vascular invasion and replacement of cartilage by bone.
  • The growth plate is divided into distinct zones:
    1. Zone of Reserve Cartilage
      • Contains relatively inactive chondrocytes scattered singly within lacunae.
      • Serves as a reservoir of cartilage cells.
    2. Zone of Proliferation
      • Chondrocytes undergo rapid mitotic division.
      • Cells become more numerous and are arranged in longitudinal columns parallel to the long axis of the bone.
    3. Zone of Hypertrophy
      • Chondrocytes enlarge considerably and develop clear cytoplasm.
      • The columnar arrangement becomes more prominent.
    4. Zone of Calcified Cartilage
      • The cartilage matrix becomes calcified.
      • Chondrocytes undergo apoptosis, leaving a calcified cartilage framework that temporarily supports new bone formation.
    5. Zone of Ossification (Resorption)
      • Blood vessels, osteoprogenitor cells, and osteoblasts invade the calcified cartilage.
      • Osteoblasts deposit bone matrix on remnants of calcified cartilage, forming mixed spicules.
      • These spicules fuse and remodel to form bony trabeculae, contributing to bone elongation and growth.
Figure 6.13: Histology of developing bone
Figure 6.14: Photomicrograph of developing bone

CLINICAL CORRELATION

  • Osteogenesis imperfecta (brittle bone disease) is a genetic disorder caused primarily by defects in type I collagen synthesis. It results in fragile bones, recurrent fractures, blue sclerae, hearing impairment, joint laxity, and short stature.
  • Scurvy, caused by vitamin C deficiency, impairs collagen formation and osteoid production. Spongy bone shows reduced trabeculae, while compact bone develops a thinner cortex.
  • Rickets occurs in children due to vitamin D deficiency or impaired vitamin D metabolism, leading to defective mineralization of growing bones and deformities such as bowing of the legs.
  • Osteomalacia is the adult counterpart of rickets and is characterized by inadequate mineralization of bone matrix, resulting in soft and weak bones.
  • Osteoporosis involves decreased bone mass and deterioration of bone microarchitecture. It is common in older adults, especially postmenopausal women, due to increased bone resorption.
  • Osteoma is a benign bone-forming tumor, whereas osteosarcoma is a malignant tumor of osteoblastic origin with the potential to metastasize.

Important Questions

  • List the cells of bone and their functional correlation.
  • List the cells of bones and their functions.
  • Write a short note on transverse section of compact bone/ground bone.
  • Write a short note on longitudinal section of compact bone or ground bone.
  • Write a short note on zones of epiphyseal cartilage.
  • List the zones of epiphyseal cartilage.

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