Please use this identifier to cite or link to this item: http://hdl.handle.net/1893/25085
Appears in Collections:Biological and Environmental Sciences Journal Articles
Peer Review Status: Refereed
Title: Contrasts between organic participation in apatite biomineralization in brachiopod shell and vertebrate bone identified by nuclear magnetic resonance spectroscopy
Authors: Neary, Marianne T
Reid, David G
Mason, Michael J
Friscic, Tomislav
Duer, Melinda J
Cusack, Maggie
Contact Email: maggie.cusack@stir.ac.uk
Keywords: Lingula anatina
Discinisca tenuis
francolite
hydroxyapatite
fluoroapatite
bone
Issue Date: 6-Feb-2011
Citation: Neary MT, Reid DG, Mason MJ, Friscic T, Duer MJ & Cusack M (2011) Contrasts between organic participation in apatite biomineralization in brachiopod shell and vertebrate bone identified by nuclear magnetic resonance spectroscopy, Journal of the Royal Society Interface, 8 (55), pp. 282-288.
Abstract: Unusually for invertebrates, linguliform brachiopods employ calcium phosphate mineral in hard tissue formation, in common with the evolutionarily distant vertebrates. Using solid-state nuclear magnetic resonance spectroscopy (SSNMR) and X-ray powder diffraction, we compare the organic constitution, crystallinity and organic matrix-mineral interface of phosphatic brachiopod shells with those of vertebrate bone. In particular, the organic-mineral interfaces crucial for the stability and properties of biomineral were probed with SSNMR rotational echo double resonance (REDOR). Lingula anatina and Discinisca tenuis shell materials yield strikingly dissimilar SSNMR spectra, arguing for quite different organic constitutions. However, their fluoroapatite-like mineral is highly crystalline, unlike the poorly ordered hydroxyapatite of bone. Neither shell material shows 13C{ 31P} REDOR effects, excluding strong physico-chemical interactions between mineral and organic matrix, unlike bone in which glycosaminoglycans and proteins are composited with mineral at sub-nanometre length scales. Differences between organic matrix of shell material from L. anatina and D. tenuis, and bone reflect evolutionary pressures from contrasting habitats and structural purposes. The absence of organic-mineral intermolecular associations in brachiopod shell argues that biomineralization follows different mechanistic pathways to bone; their details hold clues to the molecular structural evolution of phosphatic biominerals, and may provide insights into novel composite design. © 2010 The Royal Society.
DOI Link: http://dx.doi.org/10.1098/rsif.2010.0238
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