2H stable isotope analysis of human tooth enamel: a new tool for forensic human provenancing?

Stable isotope analysis of biogenic tissues such as tooth enamel and bone mineral has become a well-recognised and increasingly important method for determining the provenance of human remains, and it has been used successfully in bio-archaeological studies as well as forensic investigations. In particular, (18)O and (2)H stable isotope signatures of bone and hair, respectively, are well-established proxies of climate (temperature) and source water and are therefore considered as indicators of geographic life trajectories of animals and humans. While the methodology for (2)H analysis of human hair, fingernails, and bone collagen is currently used to determine human provenance, i.e. geographic origin and identify possible migration patterns, studies involving the analysis of (2)H in tooth enamel appear to be nonexistent in the scientific literature. Ground tooth enamel was analysed by continuous-flow isotope ratio mass spectrometry (IRMS) coupled on-line to a high-temperature conversion elemental analyser (TC/EA). An array of tooth enamel samples from archaeological and modern teeth has been analysed under different experimental conditions, and the results of this proof-of-concept study are presented. While no significant differences in (2)H abundance were noted as a result of H exchange studies or different sample preparation protocols, no significant differences or trends in measured δ(2)H-values were observed either with regard to known differences in geographical provenance. We concluded that the δ(2)H-values obtained from tooth enamel could not be used as proxy for a person's geographical origin during adolescence.

Measurement at the field scale of soil delta13C and delta15N under improved grassland.

Variations in natural abundance of carbon (C) and nitrogen (N) stable isotopes are widely used as tools for many aspects of scientific research. By examining variations in the ratios of heavy to light stable isotopes, information can be obtained as to what physical, chemical and biological processes may be occurring. The spatial heterogeneity of soil delta(15)N- and delta(13)C-values across a range of scales and under different land use have been described by a number of researchers and the natural abundances of the C and N stable isotopes in soils have been found to be correlated with many factors including hydrology, topography, land use, vegetation cover and climate. In this study the Latin square sampling +1 (LSS+1) sampling method was compared with a simple grid sampling approach for delta(13)C and delta(15)N measurement at the field scale. A set of 144 samples was collected and analysed for delta(15)N and delta(13)C from a 12 x 12 grid (in a 1 ha improved grassland field in south-west England). The dimension of each cell of the grid was approximately 11 x 6 m. The 12 x 12 grid was divided into four 6 x 6 grids and the LSS+1 sampling technique was applied to these and the main 12 x 12 grid for a comparison of sample means and variation. The LSS+1 means from the 12 x 12 grid and the four 6 x 6 grids compared well with the overall grid mean because of the low variation within the field. The LSS+1 strategy (13 samples) generated representative samples from the 12 x 12 grid, and hence would be an acceptable method for sampling similar plots for the measurement of mean isotopic composition.

Interactions between thyroid hormone and tryptophan transport in rat liver are modulated by thyroid status.

We have identified both N-ethylmaleimide (NEM)-resistant (system T) and NEM-sensitive (system L1) L-[3H]tryptophan transporters in sinusoidal membrane vesicles (SMVs) from euthyroid, hypothyroid (propylthiouracil-treated), and hyperthyroid [L-3,5,3'-triiodothyronine (L-T3)-injected] rats. L-[125I]T3 associates with SMVs largely by surface binding. Kinetic characteristics of tryptophan uptake and T3 binding (transporter or receptor abundance and substrate affinity) are not significantly affected by thyroid status. T3 and thyroxine (T4) inhibit NEM-resistant tryptophan uptake in SMVs to an extent dependent on the thyroid status of the donor rat, increasing in the order hypothyroid < euthyroid < hyperthyroid; the inhibitor constant for this inhibition (0.3 microM T3) is equal to the dissociation constant for T3 binding. Both T3 binding and T3 inhibition of tryptophan transport in SMVs are markedly reduced by treatments (Triton X-100 or trypsin) that do not significantly affect vesicle integrity or transport of tryptophan and glucose. T3 and/or T4 transport at the liver-plasma interface may be facilitated by direct interactions between hormone receptors and system T transporter proteins. Modulation of such interactions may be important for control of hepatic T4 and/or T3 turnover and aromatic amino acid metabolism during altered thyroid status.

Glucose transport correlates with GLUT2 abundance in rat liver during altered thyroid status.

Glucose transport activity ([3H]D-glucose uptake) in liver sinusoidal membrane vesicles (SMVs) from hyperthyroid rats was significantly higher than that from euthyroid controls (2.1-times increase in V(max) with K(m) unchanged at approximately 18 mM), associated with increased GLUT2 expression. In contrast, glucose transport V(max) into SMVs from hypothyroid rats was reduced to 0.75-times that of euthyroid controls, associated with a reduced GLUT2 abundance. GLUT1 expression in SMVs was unaffected by changes in thyroid status. GLUT2, but not GLUT1 abundance on the blood-facing membrane of liver cells is sensitive to changes in thyroid status and these changes in transporter expression directly correlate (r = 0.96) with altered glucose transport activity.