FGF-23 in bone biology
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- Wesseling-Perry, K. Pediatr Nephrol (2010) 25: 603. doi:10.1007/s00467-009-1384-6
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Recent studies have demonstrated that levels of fibroblast growth factor 23 (FGF-23), a key regulator of phosphorus and vitamin D metabolism, rise dramatically as renal function declines and may play a key initiating role in disordered mineral and bone metabolism in patients with chronic kidney disease (CKD). The physiologic importance of FGF-23 in mineral metabolism was first identified in human genetic and acquired rachitic diseases and further characterized in animal models. FGF-23 and its regulators, including phosphate regulating endopeptidase homolog, dentin matrix 1 (DMP1), and matrix extracellular phosphoglycoprotein, are made primarily in bone, specifically in osteocytes. Dysregulation of these proteins results in osteomalacia, implicating the osteocyte in the regulation of skeletal mineralization. Studies in pediatric patients with CKD, the majority of whom have altered skeletal mineralization in early stages of CKD, have demonstrated that skeletal expression of both FGF-23 and its regulator, DMP1, are increased in early stages of CKD and that expression of these proteins is associated with alterations in skeletal mineralization. Thus, dysregulation of osteocytic proteins occur very early in the course of CKD and appear to be central to altered bone and mineral metabolism in this patient population.
KeywordsChronic kidney diseaseDentin matrix protein 1Fibroblast growth factor 23Matrix extracellular phosphoglycoproteinPhosphate-regulating endopeptidase homologSkeletal mineralization
Abnormalities in mineral and bone metabolism occur early in the course of chronic kidney disease (CKD) and progress as renal function declines . Traditionally, these abnormalities have been ascribed to changes in the parathyroid hormone (PTH) and vitamin D axis, which lead to subsequent alterations in calcium and phosphorus metabolism [1–3]. However, recent studies have revealed that circulating values of fibroblast growth factor 23 (FGF-23), a key regulator of phosphorus and vitamin D metabolism, rise dramatically as renal function declines and may play a key initiating role in the development of abnormal mineral metabolism in patients with CKD .
FGF-23 is made in osteocytes in mineralized bone , and studies of FGF-23 in human on genetic and acquired diseases and those using animal models have demonstrated that both under- and over-expression [6–8] of FGF-23 result in impairments in bone biology. Although the defective skeletal mineralization observed in patients with FGF-23 excess is likely a consequence of low phosphorus and vitamin D values, studies of FGF-23 deficiency in animal models and in cell culture suggest that FGF-23, and the proteins that regulate FGF-23, also have a direct effect on bone . In these models, FGF-23 appears to directly regulate osteoblast differentiation , while a complete lack of the FGF-23 protein impairs skeletal mineralization, despite adequate (even excessive) circulating levels of phosphorus and vitamin D [6, 7]. In addition, recent studies suggest that alterations in skeletal FGF-23 expression also coincide with impairments in skeletal metabolism in the CKD population. Indeed, FGF-23 is up-regulated early in the course of CKD and is associated with skeletal mineralization indices in these individuals . Although the mechanisms by which these effects on bone are mediated are unknown, they may involve a number of proteins that have been shown to regulate both FGF-23 levels and skeletal mineralization [11, 12].
FGF-23 and mineral metabolism: function and regulation
The physiologic importance of FGF-23 was first identified in human genetic and acquired rachitic diseases, such as autosomal dominant hypophosphatemic rickets (ADHR), tumor-induced osteomalacia (TIO), and X-linked hypophosphatemic rickets (XLH) [8, 13–15]. In these conditions, increased levels of the protein are accompanied by impaired tubular phosphate reabsorption, hypophosphatemia, low (or inappropriately normal) levels of 1,25 (OH)2vitamin D, and impaired skeletal mineralization (rickets or osteomalacia) [6, 7, 16–18]. Increased circulating levels of FGF-23 are necessary and sufficient to account for these abnormalities since the infusion of FGF-23 into rats with normal renal function results in renal phosphate wasting and direct suppression of 1α hydroxylase activity  while the inverse phenotype accompanies a complete lack of either functional FGF-23 or its co-receptor, Klotho [6, 7, 19–23]. More recently, FGF-23 has also been shown to regulate PTH metabolism based on observations that it can suppress PTH secretion both in vitro and in vivo [24, 25].
FGF-23 expression is regulated by vitamin D, phosphate and, potentially, PTH. In both animals and humans, the administration of 1,25(OH)2vitamin D increases circulating FGF-23 levels , apparently due to a direct action of vitamin D on FGF-23 via a vitamin D response element located upstream of the FGF-23 promoter . Sustained increases in dietary phosphorus are also associated with increasing FGF-23 levels and declining 1,25(OH)2vitamin D levels [28, 29], while dietary phosphorus restriction reverses these trends [28, 29]. PTH levels may also stimulate FGF-23 expression ; findings in primary hyperparathyroidism , McCune–Albright syndrome , and Jansen’s disease  suggest that osteocytic stimulation by PTH directly increases skeletal FGF-23 release. The mechanism by which phosphate and PTH mediate changes in FGF-23 expression remain unknown and may be either direct effects on FGF-23 gene expression itself or mediated through other potential regulators of FGF-23.
Regulation of FGF-23: effects on bone metabolism and interaction with other skeletal proteins
Although the effects of FGF-23 on mineral metabolism obscure the potential direct effects of the protein on bone biology, a growing compendium of data from animals as well as from genetic and acquired human diseases of FGF-23 deficiency and excess have yielded many insights into the role that both FGF-23 and the factors that regulate FGF-23 play in bone biology. While FGF-23 is expressed in a variety of tissues, the majority of circulating FGF-23 is derived from osteocytes (in high levels) and osteoblasts (in lower levels) . Although Klotho, the obligate co-receptor for the actions of FGF-23 on mineral metabolism, has not been described in skeletal tissue, a number of studies suggest that FGF-23 has a direct effect on bone.
FGF-23 appears to directly inhibit osteoblast maturation and matrix mineralization particularly during embryonic skeletal development . Consistent with an effect of FGF-23 on osteoblast proliferation, FGF-23 expression is much lower in the embryonic skeleton than it is in adult animals  and, indeed, disruption of the Wnt signaling pathway—a pathway responsible for osteoblast proliferation and bone matrix mineralization—has been noted in mice with excess skeletal FGF-23 expression . In mature animals, a complete lack of FGF-23 also results in focal alterations in skeletal mineralization, despite adequate (even excessive) serum phosphate, calcium, and vitamin D levels [6, 7], suggesting a direct role of the protein on maintaining skeletal mineralization at later stages of development.
Several factors have been described which are produced in bone and regulate skeletal FGF-23 expression and which may themselves contribute to the skeletal mineralization process. The genetic condition of XLH (a condition with a phenotype very similar to that of ADHR) and its mouse homolog, the Hyp mouse, are associated with increased FGF-23 levels as a result of defects in the phosphate-regulating endopeptidase homolog (PHEX). PHEX is a cell-surface endopeptidase predominantly located in osteoblasts and osteocytes. Although the exact actions of PHEX in vivo have not yet been completely defined, inactivation of PHEX leads to increased FGF-23 expression by an indirect mechanism. Potential mediators of these increased FGF-23 levels include increased skeletal expression of fibroblast growth factor 1, which has been shown to directly stimulate the FGF-23 promoter , and decreased expression of UDP-N-acetyl-alpha-D-galactosamine polypeptide N-acetylgalactosaminyltransferase 3 (GALNT3), an enzyme essential for the glycosylation (and hence, stabilization) of the FGF-23 protein .
Whether from a direct effect of increased skeletal FGF-23 expression or due to some other factor modulated by the loss of PHEX activity, bone from Hyp mice displays an intrinsic mineralization defect that is not corrected by normalization of circulating calcium and phosphate concentrations; indeed, the selective ablation of PHEX in osteoblasts and osteocytes is sufficient to generate a phenotype of osteomalacia in mice , while the transplantation of Hyp mouse bone into wild-type mice does not reverse the phenotype of the explanted bone . This intrinsic mineralization defect may be due to excessive proteolytic activity in the absence of PHEX; Rowe et al.  have demonstrated that the mineralization defect in the Hyp mouse can be reversed with CA074 and pepstatin—inhibitors of proteolytic activity—without correcting systemic hypophosphatemia. Factors which regulate local pH, such as carbonic anhydrase 12 (Car12), carbonic anhydrase 3 (Car3), and sodium-dependent citrate transporter (Slc13a5) expression, are also dysregulated in Hyp osteoblasts , suggesting that altered local bicarbonate and/or citrate concentrations may also impair mineralization by depriving the osteocyte of citrate necessary for energy metabolism. In addition, intrinsic mineralization inhibitors, including matrix gla protein (MGP) and thrombospondin (Thbs) 4, are increased in Hyp mouse osteocytes and may also contribute to altered skeletal mineralization .
Skeletal mineralization in various forms of hypophosphatemic rickets may also be regulated through interactions with members of the short integrin binding-ligand, N-linked Glycoprotein (SIBLING) family. It has been proposed that PHEX binds to members of the (SIBLING) family, proteins which regulate both FGF-23  and the process of skeletal mineralization . Indeed, PHEX regulates at least two SIBLING proteins, matrix extracellular phospho-glycoprotein (MEPE)  and dentin matrix protein 1 (DMP1), thereby preventing their proteolytic cleavage and the release their active C-terminal peptide [11, 12]. Consistent with these findings, MEPE is increased in XLH patients and in Hyp mice [11, 39], while PHEX inhibits the cleavage of the acidic, serine- and aspartic acid-rich motif (ASARM) peptide, an active peptide which inhibits mineralization, from full-length MEPE . However, as the deletion of MEPE fails to correct the Hyp phenotype , other factors are likely to be involved.
The role of DMP1 in the regulation of FGF-23 and skeletal mineralization may be of even greater importance. In contrast to MEPE, DMP1, or rather the 2 active (N- and C-terminal) fragments of DMP1 generated from its cleavage by such proteinases as bone morphogenic protein 1 (BMP1) , promotes mineral formation . In both humans and animals, DMP1 dysfunction results in increased skeletal and circulating FGF-23 values as well as a diffuse skeletal mineralization defect [33, 42] and disrupted osteocyte structure . Furthermore, the DMP1/FGF-23 double knockout is phenotypically similar to the FGF-23 knockout , suggesting that DMP1 regulates FGF-23 and is located upstream of the FGF-23 molecule.
The effects of FGF-23 on mineral and bone metabolism in CKD
FGF-23 levels rise progressively as renal function declines [4, 44]. Several potential mechanisms for these increasing values have been proposed, including (1) an increased production by bone in response to a decreased capacity for renal phosphate excretion and/or (2) decreased renal clearance of FGF-23. The variety of assays available for detecting FGF-23 complicates this issue; currently, the “intact” molecule may be detected by two assays produced by two different manufacturers: Kainos and Immutopics . A “C-terminal” assay is also available (Immutopics, Los Angeles, CA) that has the potential to measure potentially inactive C-terminal fragments of the molecule . However, in a number of studies, values of FGF-23 by these different assays are well correlated [10, 46], and recent data suggest that the vast majority of circulating FGF-23 in dialysis patients is in the full-length, intact, active form of the molecule . Thus, although these three assays are calibrated differently, all three likely measure full-length, active FGF-23 in circulation.
Regardless of the cause, increased FGF-23 values are found in early stages of CKD—before any abnormalities in serum calcium, phosphorus, or PTH are apparent [4, 48, 49]. Since normal serum phosphate levels are typically maintained until late in the course of CKD , increasing concentrations of FGF-23 appear to represent a compensatory response to maintain normal serum phosphate levels in the face of declining nephron mass. As FGF-23 values are independently associated with decreasing kidney function and low 1,25(OH)2vitamin D levels , the decline in calcitriol levels associated with increasing FGF-23 levels is thought to represent the initial event in the development of secondary hyperparathyroidism.
As in patients with primary excesses in FGF-23 , defective skeletal mineralization is also common in patients with all stages of chronic kidney disease, in whom increased circulating levels of FGF-23 occur in the presence of normal or elevated serum phosphorus values [6, 7]. However, the association between FGF-23 and bone in this population differs greatly from that in the general population. The results of a cross-sectional analysis of 49 pediatric dialysis patients with secondary hyperparathyroidism suggest that high circulating levels of FGF-23 in pediatric dialysis patients are associated with improved indices of skeletal mineralization . Although these results appear to contrast with findings in patients with normal kidney function, they are similar to the mineralization defects found in rodents with a complete lack of FGF-23, despite adequate circulating mineral content [6, 7].
Confirming this association, a study of FGF-23, DMP1, and MEPE expression in bone tissue of 32 pediatric and young adult patients with CKD demonstrated that both FGF-23 and DMP1 expression were up-regulated in trabecular bone in early (stage 2) CKD, while MEPE expression remained unchanged from normal controls. In patients with all stages of CKD, the amount of bone FGF-23 correlated directly with bone DMP1 expression and the expression of each was inversely related to osteoid accumulation. In contrast, MEPE expression was not related to skeletal mineralization, but it was inversely related to bone volume. Although the simultaneous increase in both DMP1 and FGF-23 expression appears to be contrary to previous data suggesting that DMP1 acts to suppress FGF-23 expression, other data have suggested that the over-expression of DMP1 does not suppress FGF-23 expression . Moreover, DMP1 promoter activity increases in response to increasing phosphate concentrations . Thus, it is possible that the simultaneous increase in bone DMP1 and FGF-23 expression reflects the increasing phosphate burden associated with progressive renal failure. Alternatively, increased DMP1 expression may reflect an alteration in protein function in the context of CKD. Although the mechanism by which this might occur is unknown, alterations in DMP1 protein phosphorylation or cleavage  could play a role. Recent data suggest that DMP1 undergoes post-translational cleavage, leaving less than 1% of the protein in the full-length form . The cleavage products appear to have distinct biological functions; in vitro mineralization studies have demonstrated that while the carboxyl-terminal fragment promotes mineralization [41, 53], the full-length DMP1 molecule may inhibit hydroxyapatite formation . Thus, alterations in protein cleavage could have significant ramifications for DMP1 function.
FGF-23 plays a central role in mineral and bone metabolism. This role was initially delineated by the study of genetic and acquired conditions of hypophosphatemic rickets, but the greatest clinical impact of the discovery of FGF-23 may be in the management of CKD patients. FGF-23 and its regulators are made in osteocytes in bone, and in patients with CKD, FGF-23 levels rise as renal function declines, likely due to the decreasing capacity of the damaged kidney to excrete dietary phosphorus loads. Rising FGF-23 levels contribute to the development of secondary hyperparathyroidism and may also be linked to alterations in skeletal mineralization in the CKD population. Thus, through the expression of various proteins crucial to mineral metabolism, osteocytes appear to be endocrine cells with a key role in the regulation of skeletal mineralization. Alterations in osteocyte metabolism occur in very early stages of CKD and likely mediate altered bone and mineral metabolism in patients with even very mild degrees of renal dysfunction.
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