The hallmark of biological mineralization is the precise regulation of
mineral deposition in space and time, The cells which produce mineral
ized tissues are themselves controlled hy developmental programs and h
ormonal signals which result in regulation of gene expression and modu
lation of protein function, These signals are transduced into changes
in enzyme levels and/or activity, Upon activation, cellular enzymes th
en act to synthesize the organic matrix and process it extracellularly
, utilize metabolic energy to transport ions from the blood to the mat
rix, and to initiate the mineralization cascade. The first enzyme acti
vity described in mineralizing tissues was alkaline phosphatase and it
is still the best characterized enzyme in the mineralization process,
Yet, important questions about the role of this protein remain unansw
ered, and it continues to occupy a central focus in mineralized tissue
investigation, Other phosphatases, including protein tyrosine phospha
tases are important in regulating tyrosine kinase mediated signals, In
vestigators have now begun to look closely at several groups of kinase
s which are also important for proper mineralization. As peptide hormo
nes are important modulators of mineralized tissues, protein kinase A
has always been presumed to play a key role in phosphorylating intrace
llular proteins, There is also considerable interest in protein kinase
C, as well as tyrosine kinases in mineralized tissue signal transduct
ion, Another group of kinases important in mineralized tissues are the
enzymes which phosphorylate the matrix phosphoproteins. Of these, cas
ein kinase II appears to be involved in intracellular and extracellula
r protein phosphorylation. Several enzymes present in the pre-minerali
zed matrix are thought to be significant in triggering mineralization.
Alkaline phosphatase may act at this level, but new data also suggest
s that metalloproteases and gelatinases, by modifying or digesting mat
rix components, may be important in the initiation of calcification.