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Stable isotopic evidence for land use patterns in the Middle Euphrates Valley, Syria
Author(s) -
Sołtysiak Arkadiusz,
Schutkowski Holger
Publication year - 2018
Publication title -
american journal of physical anthropology
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 1.146
H-Index - 119
eISSN - 1096-8644
pISSN - 0002-9483
DOI - 10.1002/ajpa.23480
Subject(s) - bronze age , subsistence agriculture , δ34s , period (music) , residence , δ13c , geography , mass migration , isotope analysis , archaeology , ancient history , stable isotope ratio , demography , history , agriculture , geology , immigration , paleontology , art , quantum mechanics , sociology , oceanography , aesthetics , quartz , physics , fluid inclusions
Objectives Stable carbon and nitrogen isotope ratios (δ 13 C and δ 15 N) were used to reconstruct the history of subsistence strategies in the middle Euphrates valley, NE Syria, in six temporal subsets dating from the Early Bronze Age (c. 2300 BCE) to the Modern period (19th/20th century CE). The study aims to demonstrate that changes in political and social organization over time, for which the archaeological record suggests different goals of land use and modes of production, register through dietary patterns that are reflected in isotopic data. Materials and methods 173 dentin samples were taken from human individuals buried at three sites (Tell Ashara, Tell Masaikh and Gebel Mashtale) together with 15 animal bone samples. Distribution of the δ 13 C and δ 15 N values in collagen was interpreted in diachronic perspective, and with regard to lifetime shifts between childhood and adolescence. Results Diachronically, isotope signatures indicate a clear decrease in δ 15 N values accompanied by a small shift in δ 13 C values between the Old Babylonian (c. 1800–1600 BCE) and the Neo‐Assyrian (c. 850–600 BCE) subsets. A major shift in δ 13 C values occurred between the Early Islamic (c. 600–1200 CE) and Modern (c. 1800–1950) periods. Ontogenetic changes only occur in a few individuals, but these suggest change of residence between childhood and adolescence. Discussion The depletion in 15 N from the Neo‐Assyrian period onwards is best explained in terms of a shift from intensive to extensive farming, triggered by the fall of regional city‐states after the Old Babylonian period and the formation of large supra‐regional polities in the Neo‐Assyrian period and later. The enrichment in 13 C during the Modern period was most likely the effect of more widely utilizing the dry steppes, abundant in C 4 plants, as pasture.