| Literature DB >> 24556576 |
M Dumont1, T Tütken2, A Kostka3, M J Duarte3, S Borodin3.
Abstract
Pigmented tooth enamel occurs in several vertebrate clades, ranging from mammals to fish. Although an iron compound is associated with this orange to red colored pigmentation, its chemical and structural organization within the enamel is unknown. To determine the nature of the iron compound, we investigated heavily pigmented teeth of the northern short-tailed shrew Blarina brevicauda using combined characterization techniques such as scanning and transmission electron microscopy and synchrotron X-ray diffraction. We found that the pigmentation of the enamel with an iron content of around 8wt% results from a close to amorphous magnetite phase deposited around the nm-sized enamel crystals. Furthermore, the influence of the pigmentation on the enamel hardness was determined by nanoindentation measurements. Finally, the biomechanical function and biological context are discussed in light of the obtained results.Entities:
Keywords: Amorphous magnetite; Enamel; Microstructure; Nanoindentation; Pigmentation; Shrew; Tooth; Transmission electron microscopy; X-ray diffraction
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Year: 2014 PMID: 24556576 DOI: 10.1016/j.jsb.2014.02.006
Source DB: PubMed Journal: J Struct Biol ISSN: 1047-8477 Impact factor: 2.867