Assessing natural variation and the effects of charring, burial and pre-treatment on the stable carbon and nitrogen isotope values of archaeobotanical cereals and pulses
Assessing natural variation and the effects of charring, burial and pre-treatment on the stable carbon and nitrogen isotope values of archaeobotanical cereals and pulses
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DOI:
10.1016/j.jas.2013.01.032
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发表时间:
2013-12-01
影响因子:
2.8
通讯作者:
Heaton, T. H. E.
中科院分区:
文献类型:
--
作者:
Fraser, R. A.;Bogaard, A.;Heaton, T. H. E.
The aim of this study is to assess the potential of charred archaeobotanical cereal grain and pulse seed delta C-13 and delta N-15 values to provide evidence of crop growing conditions and as a potential component of palaeodietary studies. In order to reliably interpret archaeobotanical delta C-13 and delta N-15 values it is necessary to take into account the impact of charring, burial and laboratory pre-treatment procedures. We examine the effects of charring and burial on bulk delta C-13, delta N-15, %C, %N and C:N ratios in modern cereal and pulse material, and of cleaning by acid base acid (ABA) pre-treatment on modern and archaeobotanical charred material. Our study utilised bulk grain and seed samples to help account for within-ear/pod and between-plant variability in delta C-13 and delta N-15 values. Heating at relatively low temperatures and for prolonged times (230 degrees C for up to 24 h) is conducive to the formation of well preserved, undistorted charred cereal grain and pulse seed. Heating for 24 h has a systematic and predictable effect on delta N-15 values, with increases of around 1 parts per thousand on average in cereal grains and pulse seeds, and no consistent impact on delta C-13 values. Increases in delta N-15 are likely due to the loss of lighter N-14 via N-containing volatiles. Burial (for up to 2 years) and ABA pre-treatment have no significant effects on delta C-13 or delta N-15 values. After pre-treatment, however, the %C and %N contents of the archaeobotanical material more closely resembles that of the modern charred grains and seeds, suggesting that archaeobotanical remains accumulate non-structural material during burial but retain their original carbon and nitrogen content. Therefore %C, %N contents and C:N ratios can provide useful criteria for assessing archaeobotanical preservation. (C) 2013 Elsevier Ltd. All rights reserved.