Stable Isotope and Radiocarbon Analysis for Diet, Climate and Mobility Reconstruction in Agras (Early Iron Age) and Edessa (Roman Age), Northern Greece

被引:2
作者
Dotsika, Elissavet [1 ]
Tassi, Maria [1 ]
Karalis, Petros [1 ]
Chrysostomou, Anastasia [2 ]
Michael, Dimitra Ermioni [1 ]
Poutouki, Anastasia Elektra [1 ]
Theodorakopoulou, Katerina [3 ]
Diamantopoulos, Georgios [1 ]
机构
[1] NCSR Demokritos, Inst Nanosci & Nanotechnol, Stable Isotope Unit, Patriarchou Gregoriou End & Neapoleos St, Aghia Paraskevi 15341, Greece
[2] Minist Culture, Mpoumpoulinas 20-22 Str, Athens 10682, Greece
[3] Natl & Kapodistrian Univ Athens, Dept Geol & Geoenvironm, Athens 15784, Greece
来源
APPLIED SCIENCES-BASEL | 2022年 / 12卷 / 01期
关键词
stable isotopes; bone collagen; bone apatite; palaeodiet; palaeoclimate; C-13; N-15; O-18; mobility; OXYGEN ISOTOPES; BONE-COLLAGEN; CARBON ISOTOPES; BIOGEOCHEMISTRY C-13; NITROGEN ISOTOPES; SOUTHERN ONTARIO; TROPHIC LEVEL; BRONZE-AGE; PHOSPHATE; FRACTIONATION;
D O I
10.3390/app12010498
中图分类号
O6 [化学];
学科分类号
0703 ;
摘要
In this article we present an isotopic analysis of human bone collagen (delta C-13(col), and delta N-15(col)) and bone apatite (delta C-13) for diet reconstruction, as well as delta O-18(ap) of human bone apatite for climate reconstruction, using samples from Northern Greece. Radiocarbon dating analysis was conducted on three of the Agras samples and the results (from 1000 to 800 BC) correspond to the Early Iron Age. Isotopic values for delta C-13(col) range from -20.5 parts per thousand to -16 parts per thousand and for delta N-15(col) from 6 parts per thousand to 11.1 parts per thousand-a strong indication of a C3-based diet, with contributions by C4 and freshwater fish elements. The results were compared to the ones from Roman Edessa, and Alexandreia (a contemporary city near Edessa), as well as to other Early Iron sites in Greece and wider Europe. In general, the results from Agras are in good agreement with the results from Northern Greece, with the exception of the Makriyalos site, and are quite close to those of Croatia's and Hungary's sites. Additionally, from the delta O-18(ap) results we calculated the oxygen isotopic composition of consumed water for Agras (from -9.6 parts per thousand to -10.9 parts per thousand) and for Roman Edessa (from -9.6 parts per thousand to -11.2 parts per thousand) for the palaeoclimate and palaeomobility reconstruction.
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