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- W2600182213 abstract "A number of recent studies dealing with palaeoclimate and environmental reconstruction include the measurement of oxygen isotope composition of mammalian teeth. Some of them analyse a temporal sequence of the changes recorded in bioapatite from enamel layers representing the whole period of tooth development. Enamel samples display large intra-tooth δ 18 O variations that may reflect a seasonal fluctuation in the δ 18 O of local palaeoclimate parameters. The present paper provides an effective analytical protocol for sequential δ 18 O analysis of human teeth using SHRIMP IIe/MC ion microprobe. It is possible to follow the inner enamel layer along enamel-dentine junction on a high spatial scale in a range about 0.02 mm of spot diameter and 0.12–0.14 mm of the distance between spots. Using the methodology described herein, we can achieve an external precision for δ 18 O analysis <0.2‰ (1σ). The number of 60 to 90 single analyses covering the enamel layer between the incisal and apical ends is enough to obtain temporal resolution of less than one month and to document precisely seasonal fluctuation caused by local environmental and climate factors. The methodology of δ 18 O in situ measurements has been tested on human teeth from Tell Majnuna, a 4th millennium BCE cemetery in Northern Mesopotamia, which is a relatively arid area with high seasonal differences in precipitation and temperature. Observed pattern of δ 18 O variations is consistent with expected seasonal fluctuations, although the overall effect is blurred by some inertia in the enamel maturation." @default.
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- W2600182213 date "2017-01-01" @default.
- W2600182213 modified "2023-10-05" @default.
- W2600182213 title "Reconstructing seasonality using d18O in incremental layers of human enamel: a test of the analytical protocol developed for SHRIMP IIe/MC ion microprobe" @default.
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- W2600182213 doi "https://doi.org/10.7306/gq.1354" @default.
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