Naslov
Molluscan Shell Proteins: Primary Structure, Origin, and Evolution

Autori
Marin, Frederic ; Luquet, Gilles ; Marie, Benjamin ; Medakovic, Davorin

Vrsta, podvrsta i kategorija rada
Poglavlja u knjigama, pregledni

Knjiga
Current Topics in Developmental Biology

Urednik/ci
Schatten, P. Gerald

Izdavač
Elsevier

Grad
Pittsburgh (PA)

Godina
2007

Raspon stranica
209-276

ISBN
9780123739148

Ključne riječi
biomineralization, biomaterials, biomedical, evolution, proteins, shell

Sažetak
In the last few years, the field of molluscan biomineralization has known a tremendous mutation, regarding fundamental concepts on iomineralization regulation as well as regarding the methods of investigation. The most recent advances deal more particularly with the structure of shell biominerals at nanoscale and the identification of an increasing number of shellmatrix protein components. Although the matrix is quantitatively a minor constituent in the shell of mollusks (less than 5% w/w), it is, however, the major component that controls diffrent aspects of the shell formation processes: synthesis of transient amorphous minerals and evolution to crystalline phases, choice of the calcium carbonate polymorph (calcite vs aragonite), organization of crystallites in complex shell textures (microstructures). Until recently, the classical paradigm in molluscan shell biomineralization was to consider that the control of shell synthesis was performed primarily by two antagonistic mechanisms: crystal nucleation and growth inhibition. New concepts and emerging models try now to translate a more complex reality, which is remarkably illustrated by the wide variety of shell proteins, characterized since the mid-1990s, and described in this chapter. These proteins cover a broad spectrum of pI, from very acidic to very basic. The primary structure of a number of them is composed of different modules, suggesting that these proteins are multifunctional. Some of them exhibit enzymatic activities. Others may be involved in cell signaling. The oldness of shell proteins is discussed, in relation with the Cambrian appearance of the mollusks as a mineralizing phylum and with the Phanerozoic evolution of this group. Nowadays, the extracellular calcifying shell matrix appears as a whole integrated system, which regulates protein-mineral and protein-protein interactions as well as feedback interactions between the biominerals and the calcifying epithelium that synthesized them. Consequently, the molluscan shell matrixmay be a source of bioactive molecules that would ofer interesting perspectives in biomaterials and biomedical fields.

Izvorni jezik
Engleski

Znanstvena područja
Geologija, Biologija, Temeljne medicinske znanosti

Napomena
Financial Support: EGIDE, Programme d'Action Integree, Cogito 09084XG

POVEZANOST RADA