Assessing the biology of fossil vertebrates through bone histology

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dc.contributor.author Chinsamy, Anusuya
dc.date.accessioned 2015-01-11T08:01:14Z
dc.date.available 2015-01-11T08:01:14Z
dc.date.issued 1997
dc.identifier.citation None en_ZA
dc.identifier.issn 0078-8554
dc.identifier.uri http://hdl.handle.net/10539/16394
dc.description Main article en_ZA
dc.description.abstract Soon after death and burial of an animal, the organic components of bone generally decay. The closely associated inorganic components (mainly apatite) are more resilient and even after millions of years of burial, preserve the spatial organisation of the collagen fibres and hence the structure of the bone. In the past fossil bone histology has been the subject of substantial research. Such studies have included a wide array of extinct vertebrates including fishes, amphibians, pelycosaurs, therapsids, ichthyosaurs, pterosaurs, and dinosaurs. The relative rate ofbone formation is indicated by the texture of the fibrillar matrix, while the overall nature of the primary compact bone provides a direct assessment of whether bone deposition was continuous or interrupted. The amount of secondary bone formation depicts the extent of primary bone resorption and subsequent redeposition. In addition, the internal organisation of bone indicates remodelling and relocation processes of growth, including functional adaptations of the bone morphology. Thus, osteohistology reflects ontogeny, growth dynamics, biomechanical adaptations, as well as various events that punctuate the life history of an animal. en_ZA
dc.description.sponsorship the Foundation for Research and Development (SA), and by the National Science Foundation (USA). en_ZA
dc.language.iso en en_ZA
dc.publisher Bernard Price Institute for Palaeontological Research en_ZA
dc.relation.ispartofseries None;
dc.subject Bone histology, bone microstructure, osteohistology, vertebrates, fossils. en_ZA
dc.title Assessing the biology of fossil vertebrates through bone histology en_ZA
dc.type Article en_ZA


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