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Method of micro-sampling human dentine collagen for stable isotope analysis
Authors:Mandi J Curtis  Julia Beaumont  Fadil Elamin  Andrew S Wilson  Hannah E C Koon
Institution:1. School of Archaeological and Forensic Sciences, University of Bradford, Bradford, UK;2. Institute of Dentistry, Bart's and The London School of Medicine and Dentistry, Queen Mary University of London, London, UK

Khartoum Centre for Research and Medical Training, Khartoum, Sudan

Abstract:

Rationale

Sampling of dentine for stable carbon (δ13C) and nitrogen (δ15N) isotope ratios in the direction of tooth growth allows the study of temporal changes to the diet and physiological stress of an individual during tooth formation. Current methods of sampling permanent teeth using 1 mm increments provide temporal resolution of 6–9 months at best depending on the tooth chosen. Although this gives sufficient sample sizes for reliable analysis by mass spectrometry, sectioning the dentine across the incremental structures results in a rolling average of the isotope ratios. A novel method of incremental dentine collagen sampling has been developed to decrease the collagen increment size to 0.35 mm along the incremental structures, thus reducing averaging and improving the temporal resolution of short-term changes within the δ13C and δ15N values.

Methods

This study presents data for a MicroMill-assisted sampling method that allows for sampling at 0.35 mm width × 1 mm depth increments following the incremental growth pattern of dentine. A NewWave MicroMill was used to sample the demineralised dentine section of modern donated human third molars from Sudan and compared to data from the same teeth using the 1 mm incremental sectioning method 2 established by Beaumont et al.

Results

The δ13C and δ15N isotopic data showed an increased temporal resolution, with each increment providing data for 2–4 months of dentine formation.

Conclusions

The data show the potential of this method for studying dietary reconstruction, nutritional stress, and physiological change with greater temporal resolution potentially to seasonal level and with less attenuation of the δ13C and δ15N values than was previously possible from human dentine.
Keywords:
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