Development of calcareous skeletal elements in invertebrates.
Most metazoans require skeletal support systems. While the formation of bones and teeth in vertebrates has been well studied, endo- and exoskeleton development of non-vertebrates, especially calcification during terminal differentiation, has been neglected. Biomineralization of skeletons in invertebrates presents interesting research opportunities. We undertake here to survey some of the better understood examples of skeletal development in selected invertebrates. The differentiation of the skeletal spicules of euechinoid larvae and other non-vertebrate deuterostomes, the shells of molluscs, and the calcification of crustacean carapaces are surveyed. The diversity of these different kinds of animals and our present limited understanding make it difficult to identify unifying themes, but there certainly are unifying questions: How is the mineral precursor secreted? What is the nature of the interaction of mineral with the matrix proteins of the skeleton? Is there any conservation of protein domains in matrix proteins found in skeletal elements from different phyla? Are there common strategies in the development of organs that form mineralized structures?
Wilt
Fred H
FH
Department of Molecular and Cell Biology, University of California, Berkeley, 142 Life Sciences Addition, Berkeley, California 94720-3200, USA. wilt@socrates.berkeley.edu
Killian
Christopher E
CE
Livingston
Brian T
BT
D000818:Animals; D002454:Cell Differentiation / Q000502:physiology*; D016326:Extracellular Matrix Proteins / Q000502:physiology; D007448:Invertebrates / Q000196:embryology* / Q000254:growth & development; D012863:Skeleton
D016326:Extracellular Matrix Proteins