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Effect of Charring on Rice Grain Morphology and Carbon Isotopic Composition


Affiliations
1 Indian Institute of Science Education and Research Kolkata, Mohanpur 741 246, India
2 Divecha Centre for Climate Change, Indian Institute of Science, Bengaluru 560 012, India
 

Rice cultivation over Asia has several thousand years of history. Adequate water availability is a prime factor for the cultivation of rice in this region. The remains of rice at the archaeological sites, therefore, provide an indirect clue on rainfall in this region. The stable isotopic compositions in remains of rice grains allow estimation of rainfall condition during rice cultivation. Often, such remains found at the archaeological sites suffer from the process of charring, which is likely to modify the original isotopic signature. Here, we performed charring experiments on rice grains at two different temperatures, i.e. 230°C and 250°C and documented the changes in the morphology and carbon isotopic composition (δ13C). A noticeable morphological shift was registered in the samples with progressive duration and temperature of charring. Further, cellulose was extracted and analysed for δ13C. Our results showed that the shift in δ13C observed for charred rice was relatively lower as compared to that observed in other cereals.

Keywords

Charring, Palaeoclimate Proxy, Rice, Stable Carbon Isotope.
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  • Effect of Charring on Rice Grain Morphology and Carbon Isotopic Composition

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Authors

Arpita Biswas
Indian Institute of Science Education and Research Kolkata, Mohanpur 741 246, India
Ritika Kaushal
Divecha Centre for Climate Change, Indian Institute of Science, Bengaluru 560 012, India
Prosenjit Ghosh
Divecha Centre for Climate Change, Indian Institute of Science, Bengaluru 560 012, India

Abstract


Rice cultivation over Asia has several thousand years of history. Adequate water availability is a prime factor for the cultivation of rice in this region. The remains of rice at the archaeological sites, therefore, provide an indirect clue on rainfall in this region. The stable isotopic compositions in remains of rice grains allow estimation of rainfall condition during rice cultivation. Often, such remains found at the archaeological sites suffer from the process of charring, which is likely to modify the original isotopic signature. Here, we performed charring experiments on rice grains at two different temperatures, i.e. 230°C and 250°C and documented the changes in the morphology and carbon isotopic composition (δ13C). A noticeable morphological shift was registered in the samples with progressive duration and temperature of charring. Further, cellulose was extracted and analysed for δ13C. Our results showed that the shift in δ13C observed for charred rice was relatively lower as compared to that observed in other cereals.

Keywords


Charring, Palaeoclimate Proxy, Rice, Stable Carbon Isotope.

References





DOI: https://doi.org/10.18520/cs%2Fv118%2Fi7%2F1052-1059