The aim of this study is to elucidate and reconstruct paleo diets using the carbon and nitrogen isotope ratios (δ
13C and δ
15N) of
charred residue on earthenware pots. It is necessary to consider whether there are any significant differences in the δ
13C and δ
15N
values of modern foods between before and after cooking. In this study, we investigated the changes occurring during the boiling
of foods (sea bream, coho salmon, hard-shell clam, wakame, rice, and millet) in the earthenware pot. In addition, we examined the
fluctuations in δ
13C and δ
15N values in the charred residue. We defined the cases where δ
13C and δ
15N values varied by more than 1.0
‰ and 3.0 ‰, respectively, as “varied”. The δ
13C “variation” was small within 1.0 ‰ except sea bream which indicated decreases
of 1.4-1.8 ‰. The change in δ
15N values was less than 3.0 ‰ in all charred residue samples. The δ
13C and δ
15N values were likely
to be almost maintained during boiling. This result suggested that δ
13C and δ
15N values of charred residue depended on the food
group, such as fish, shellfish, seaweed, and C
3 and C
4 plants. Thus, we may discriminate the food groups of charred residues using
their δ
13C and δ
15N values.
View full abstract