Biomineralization Processes
The large number of different minerals formed by organisms from almost 50 different phyla described in Chapter 2 should in itself discourage anyone from searching for the mechanism of biomineralization. On the other hand, the survey of macromolecules used by many organisms to control mineralization (Chapter 2), even though limited primarily to carbonate- and phosphate-bearing mineralized hard parts, shows that similar and rather unusual acidic glycoproteins and proteoglycans are widely utilized in biomineralization. This raises the possibility that many organisms may have adopted common approaches or strategies for regulating mineral formation. We do not know whether this arose as a result of divergence from a common ancestor or is a product of convergent evolution in which many different phyla independently began utilizing similar macromolecules for controlling mineralization (see Chapter 12). Either way we view the diversity in biomineralization as the product of a very broad and almost continuous spectrum of processes that organisms use to control mineralization. This ranges from no apparent control at one end to, it seems, control over every detail at the other. However, this is achieved by a fairly limited number of different basic processes used in various combinations and ways to produce a unique final product. This last statement is, we readily admit at this point in time, more an act of faith than an established fact. In this chapter we will try to identify and/or speculate about some of these basic processes. We will draw upon material from many different sources, and, in particular, we will refer whenever possible to the more detailed descriptions of mineralization processes given in the chapters that follow. As a consequence, this chapter may also be used by the reader as a guide toward more discriminating reading on selected topics in the remainder of the book. The spectrum of biomineralization processes can in principle be easily divided into cases in which control is exercised in some way over mineralization and those in which it is not. In practice the differentiation is not that simple as all organisms do exercise some control at one level or another, even if it simply involves, for example, removing from the cell some undesirable metabolic end-product or ion that combines with another ion in the external medium and precipitates.