Osteoblasts(from theGreekcombining forms for "bone",ὀστέο-,osteo-and βλαστάνω,blastanō"germinate" ) arecellswith a singlenucleusthat synthesizebone.However, in the process ofbone formation,osteoblasts function in groups of connected cells. Individual cells cannot make bone. A group of organized osteoblasts together with the bone made by a unit of cells is usually called theosteon.
Osteoblast | |
---|---|
Details | |
Location | Bone |
Function | Formation ofbone tissue |
Identifiers | |
Greek | osteoblastus |
MeSH | D010006 |
TH | H2.00.03.7.00002 |
FMA | 66780 |
Anatomical terms of microanatomy |
Osteoblasts are specialized, terminally differentiated products ofmesenchymal stem cells.[1]They synthesize dense, crosslinkedcollagenand specialized proteins in much smaller quantities, includingosteocalcinandosteopontin,which compose the organic matrix of bone.
In organized groups of disconnected cells, osteoblasts producehydroxyapatite,thebone mineral,that is deposited in a highly regulated manner, into the inorganic matrix forming a strong and densemineralized tissue,the mineralized matrix. The mineralizedskeletonis the main support for the bodies of air breathingvertebrates.It is also an important store of minerals for physiologicalhomeostasisincluding bothacid-base balanceandcalciumorphosphatemaintenance.[2][3]
Bone structure
editTheskeletonis a large organ that isformed and degradedthroughout life in the air-breathing vertebrates. The skeleton, often referred to as the skeletal system, is important both as a supporting structure and for maintenance of calcium, phosphate, andacid-base statusin the whole organism.[4]The functional part of bone, thebone matrix,is entirely extracellular. The bone matrix consists ofproteinandmineral.The protein forms theorganic matrix.It is synthesized and then the mineral is added. The vast majority of the organic matrix iscollagen,which providestensile strength.The matrix is mineralized by deposition of hydroxyapatite (alternative name, hydroxylapatite). This mineral is hard, and providescompressive strength.Thus, the collagen and mineral together are acomposite materialwith excellent tensile and compressive strength, which can bend under a strain and recover its shape without damage. This is calledelastic deformation.Forces that exceed the capacity of bone to behave elastically may cause failure, typicallybone fractures.[citation needed]
Bone remodeling
editBone is a dynamic tissue that is constantly beingreshaped by osteoblasts,which produce and secrete matrix proteins and transport mineral into the matrix, andosteoclasts,which break down the tissues.
Osteoblasts
editOsteoblasts are the major cellular component of bone. Osteoblasts arise frommesenchymal stem cells(MSC). MSC give rise to osteoblasts,adipocytes,andmyocytesamong other cell types. Osteoblast quantity is understood to be inversely proportional to that of marrow adipocytes which comprisemarrow adipose tissue (MAT).Osteoblasts are found in large numbers in theperiosteum,the thin connective tissue layer on the outside surface of bones, and in theendosteum.
Normally, almost all of the bone matrix, in the air breathingvertebrates,is mineralized by the osteoblasts. Before the organic matrix is mineralized, it is called theosteoid.Osteoblasts buried in the matrix are calledosteocytes.During bone formation, the surface layer of osteoblasts consists of cuboidal cells, calledactive osteoblasts.When the bone-forming unit is not actively synthesizing bone, the surface osteoblasts are flattened and are calledinactive osteoblasts.Osteocytes remain alive and are connected by cell processes to a surface layer of osteoblasts. Osteocytes have important functions in skeletal maintenance.
Osteoclasts
editOsteoclasts are multinucleated cells that derive from hematopoietic progenitors in the bone marrow which also give rise to monocytes in peripheral blood.[5]Osteoclasts break down bone tissue, and along with osteoblasts and osteocytes form the structural components of bone. In the hollow within bones are many other cell types of thebone marrow.Components that are essential for osteoblast bone formation include mesenchymal stem cells (osteoblast precursor) andblood vesselsthat supply oxygen and nutrients for bone formation. Bone is a highly vascular tissue, and active formation of blood vessel cells, also from mesenchymal stem cells, is essential to support the metabolic activity of bone. The balance of bone formation andbone resorptiontends to be negative with age, particularly in post-menopausal women,[6]often leading to a loss of bone serious enough to cause fractures, which is calledosteoporosis.
Osteogenesis
editBone is formed by one of two processes:endochondral ossificationorintramembranous ossification.Endochondral ossification is the process of forming bone from cartilage and this is the usual method. This form ofbone developmentis the more complex form: it follows the formation of a first skeleton ofcartilagemade bychondrocytes,which is then removed and replaced by bone, made by osteoblasts. Intramembranous ossification is the direct ossification ofmesenchymeas happens during the formation of themembrane bonesof the skull and others.[7]
During osteoblastdifferentiation,the developing progenitor cellsexpress the regulatorytranscription factorCbfa1/Runx2.A second required transcription factor isSp7 transcription factor.[8]Osteochondroprogenitor cellsdifferentiate under the influence ofgrowth factors,although isolated mesenchymal stem cells in tissue culture may also form osteoblasts under permissive conditions that includevitamin Cand substrates foralkaline phosphatase,a keyenzymethat provides high concentrations of phosphate at the mineral deposition site.[1]
Bone morphogenetic proteins
editKey growth factors in endochondral skeletal differentiation includebone morphogenetic proteins(BMPs) that determine to a major extent where chondrocyte differentiation occurs and where spaces are left between bones. The system of cartilage replacement by bone has a complex regulatory system.BMP2also regulates early skeletal patterning.Transforming growth factor beta(TGF-β), is part of a superfamily of proteins that include BMPs, which possess common signaling elements in theTGF beta signaling pathway.TGF-β is particularly important incartilagedifferentiation, which generally precedes bone formation for endochondral ossification. An additional family of essential regulatory factors is thefibroblast growth factors(FGFs) that determine where skeletal elements occur in relation to the skin
Steroid and protein hormones
editMany other regulatory systems are involved in the transition of cartilage to bone and in bone maintenance. A particularly important bone-targeted hormonal regulator isparathyroid hormone(PTH). Parathyroid hormone is a protein made by theparathyroidgland under the control of serum calcium activity.[3]PTH also has important systemic functions, including to keep serum calcium concentrations nearly constant regardless of calcium intake. Increasing dietary calcium results in minor increases in blood calcium. However, this is not a significant mechanism supporting osteoblast bone formation, except in the condition of low dietary calcium; further, abnormally high dietary calcium raises the risk of serious health consequences not directly related to bone mass includingheart attackandstroke.[9]Intermittent PTH stimulation increases osteoblast activity, although PTH is bifunctional and mediates bone matrix degradation at higher concentrations.
The skeleton is also modified for reproduction and in response to nutritional and otherhormonestresses; it responds tosteroids,includingestrogenandglucocorticoids,which are important in reproduction and energy metabolism regulation. Bone turnover involves major expenditures of energy for synthesis and degradation, involving many additional signals includingpituitaryhormones. Two of these areadrenocorticotropic hormone(ACTH)[10]andfollicle stimulating hormone.[11]The physiological role for responses to these, and several otherglycoproteinhormones, is not fully understood, although it is likely that ACTH is bifunctional, like PTH, supporting bone formation with periodic spikes of ACTH, but causing bone destruction in large concentrations. In mice, mutations that reduce the efficiency of ACTH-induced glucocorticoid production in the adrenals cause the skeleton to become dense (osteoscleroticbone).[12][13]
Organization and ultrastructure
editIn well-preserved bone studied at high magnification viaelectron microscopy,individual osteoblasts are shown to be connected bytight junctions,which preventextracellular fluidpassage and thus create a bone compartment separate from the general extracellular fluid.[14]The osteoblasts are also connected bygap junctions,small pores that connect osteoblasts, allowing the cells in one cohort to function as a unit.[15]The gap junctions also connect deeper layers of cells to the surface layer (osteocyteswhen surrounded by bone). This was demonstrated directly by injecting lowmolecular weightfluorescent dyesinto osteoblasts and showing that the dye diffused to surrounding and deeper cells in the bone-forming unit.[16]Bone is composed of many of these units, which are separated by impermeable zones with no cellular connections, called cement lines.
Collagen and accessory proteins
editAlmost all of the organic (non-mineral) component of bone is densecollagentype I,[17]which forms dense crosslinked ropes that give bone its tensile strength. By mechanisms still unclear, osteoblasts secrete layers of oriented collagen, with the layers parallel to the long axis of the bone alternating with layers at right angles to the long axis of the bone every fewmicrometers.Defects in collagen type I cause the commonest inherited disorder of bone, calledosteogenesis imperfecta.[18]
Minor, but important, amounts of small proteins, includingosteocalcinandosteopontin,are secreted in bone's organic matrix.[19]Osteocalcin is not expressed at significant concentrations except in bone, and thus osteocalcin is a specific marker for bone matrix synthesis.[20]These proteins link organic and mineral component of bone matrix.[21]The proteins are necessary for maximal matrix strength due to their intermediate localization between mineral and collagen.
However, in mice where expression of osteocalcin or osteopontin was eliminated by targeted disruption of the respective genes (knockout mice), accumulation of mineral was not notably affected, indicating that organization of matrix is not significantly related to mineral transport.[22][23]
Bone versus cartilage
editThe primitive skeleton iscartilage,a solid avascular (without blood vessels) tissue in which individual cartilage-matrix secreting cells, orchondrocytes,occur. Chondrocytes do not have intercellular connections and are not coordinated in units. Cartilage is composed of a network ofcollagentype II held in tension by water-absorbing proteins, hydrophilicproteoglycans.[24]This is the adult skeleton incartilaginous fishessuch assharks.It develops as the initial skeleton in more advancedclassesof animals.
In air-breathing vertebrates, cartilage is replaced by cellular bone. A transitional tissue is mineralizedcartilage.Cartilage mineralizes by massive expression of phosphate-producing enzymes, which cause high local concentrations of calcium and phosphate that precipitate.[24]This mineralized cartilage is not dense or strong. In the air breathing vertebrates it is used as a scaffold for formation of cellular bone made by osteoblasts, and then it is removed byosteoclasts,which specialize in degrading mineralized tissue.
Osteoblasts produce an advanced type of bone matrix consisting of dense, irregular crystals ofhydroxyapatite,packed around the collagen ropes.[25]This is a strong composite material that allows the skeleton to be shaped mainly as hollow tubes. Reducing the long bones to tubes reduces weight while maintaining strength.
Mineralization of bone
editThe mechanisms of mineralization are not fully understood. Fluorescent, low-molecular weight compounds such astetracyclineorcalceinbind strongly to bone mineral, when administered for short periods. They then accumulate in narrow bands in the new bone.[26]These bands run across the contiguous group of bone-forming osteoblasts. They occur at a narrow (sub-micrometer) mineralization front. Most bone surfaces express no new bone formation, no tetracycline uptake and no mineral formation. This strongly suggests that facilitated oractive transport,coordinated across the bone-forming group, is involved in bone formation, and that only cell-mediated mineral formation occurs. That is, dietary calcium does not create mineral by mass action.
The mechanism of mineral formation in bone is clearly distinct from thephylogeneticallyolder process by which cartilage is mineralized: tetracycline does not label mineralized cartilage at narrow bands or in specific sites, but diffusely, in keeping with a passive mineralization mechanism.[25]
Osteoblasts separate bone from the extracellular fluid by tight junctions[14]by regulated transport. Unlike in cartilage,phosphateandcalciumcannot move in or out by passive diffusion, because thetight osteoblast junctionsisolate the bone formation space. Calcium is transported across osteoblasts byfacilitated transport(that is, by passive transporters, which do not pump calcium against a gradient).[25]In contrast, phosphate is actively produced by a combination of secretion of phosphate-containing compounds, includingATP,and byphosphatasesthat cleave phosphate to create a high phosphate concentration at the mineralization front.Alkaline phosphataseis a membrane-anchored protein that is a characteristic marker expressed in large amounts at the apical (secretory) face of active osteoblasts.
At least one more regulated transport process is involved. Thestoichiometryof bone mineral basically is that ofhydroxyapatiteprecipitating from phosphate, calcium, and water at a slightly alkalinepH:[27]
- 6 HPO2−4+ 2 H2O + 10 Ca2+⇌ Ca10(PO4)6(OH)2+ 8 H+
In a closed system as mineral precipitates, acid accumulates, rapidly lowering thepHand stopping further precipitation. Cartilage presents no barrier to diffusion and acid therefore diffuses away, allowing precipitation to continue. In the osteon, where matrix is separated from extracellular fluid by tight junctions, this cannot occur. In the controlled, sealed compartment, removing H+drives precipitation under a wide variety of extracellular conditions, as long as calcium and phosphate are available in the matrix compartment.[28]The mechanism by which acid transits the barrier layer remains uncertain. Osteoblasts have capacity for Na+/H+exchange via the redundant Na/H exchangers, NHE1 and NHE6.[29]This H+exchange is a major element in acid removal, although the mechanism by which H+is transported from the matrix space into the barrier osteoblast is not known.
In bone removal, a reverse transport mechanism uses acid delivered to the mineralized matrix to drive hydroxyapatite into solution.[30]
Osteocyte feedback
editFeedback from physical activity maintains bone mass, while feedback from osteocytes limits the size of the bone-forming unit.[31][32][33]An important additional mechanism is secretion by osteocytes, buried in the matrix, ofsclerostin,a protein that inhibits a pathway that maintains osteoblast activity. Thus, when the osteon reaches a limiting size, it deactivates bone synthesis.[34]
Morphology and histological staining
editHematoxylin and eosinstaining (H&E) shows that the cytoplasm of active osteoblasts is slightlybasophilicdue to the substantial presence ofrough endoplasmic reticulum.The active osteoblast produces substantial collagen type I. About 10% of the bone matrix is collagen with the balance mineral.[27]The osteoblast's nucleus is spherical and large. An active osteoblast is characterized morphologically by a prominentGolgi apparatusthat appears histologically as a clear zone adjacent to the nucleus. The products of the cell are mostly for transport into the osteoid, the non-mineralized matrix. Active osteoblasts can be labeled by antibodies toType-I collagen,or using naphthol phosphate and thediazoniumdye fast blue to demonstrate alkaline phosphataseenzymeactivity directly.
-
Osteoblast (Wright Giemsa stain, 100x)
-
Light micrographofdecalcifiedcancellous bone displaying osteoblasts actively synthesizing osteoid, containing two osteocytes.
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Light micrographof undecalcified tissue displaying osteoblasts actively synthesizing osteoid (center).
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Light micrographof undecalcified tissue displaying osteoblasts actively synthesizing rudimentary bone tissue (center).
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Osteoblasts lining bone (H&E stain).
Isolation of Osteoblasts
edit- The first isolation technique by microdissection method was originally described by Fell et al.[35]using chick limb bones which were separated into periosteum and remaining parts. She obtained cells which possessed osteogenic characteristics from cultured tissue using chick limb bones which were separated into periosteum and remaining parts. She obtained cells which possessed osteogenic characteristics from cultured tissue.
- Enzymatic digestion is one of the most advanced techniques for isolating bone cell populations and obtaining osteoblasts. Peck et al. (1964)[36]described the original method that is now often used by many researchers.
- In 1974 Jones et al.[37]found that osteoblasts moved laterally in vivo and in vitro under different experimental conditions and described the migration method in detail. The osteoblasts were, however, contaminated by cells migrating from the vascular openings, which might include endothelial cells and fibroblasts.
See also
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Further reading
edit- William F. Neumanand Margaret W. Neuman. (1958). The Chemical Dynamics of Bone Mineral. Chicago: The University of Chicago Press.ISBN0-226-57512-8.
- Netter, Frank H.(1987).Musculoskeletal system: anatomy, physiology, and metabolic disorders.Summit, New Jersey: Ciba-Geigy CorporationISBN0-914168-88-6.