The study of clay tokens in the Ancient Near East has focused, for the most part,
on their role as antecedents to the cuneiform script. Starting with Pierre Amiet
and Maurice Lambert in the 1960s the theory was put forward that tokens, or
calculi, represent an early cognitive attempt at recording. This theory was
taken up by Denise Schmandt-Besserat who studied a large diachronic corpus of
Near Eastern tokens. Since then little has been written except in response to
Schmandt-Besserat's writings. Most discussions of tokens have generally focused
on the time period between the eighth and fourth millennium bc with the
assumption that token use drops off as writing gains ground in administrative
contexts. Now excavations in southeastern Turkey at the site of Ziyaret Tepe
— the Neo-Assyrian provincial capital Tušhan —
have uncovered a corpus of tokens dating to the first millennium bc. This is a
significant new contribution to the documented material. These tokens are found
in association with a range of other artefacts of administrative culture
— tablets, dockets, sealings and weights — in a manner
which indicates that they had cognitive value concurrent with the cuneiform
writing system and suggests that tokens were an important tool in Neo-Assyrian
imperial administration.
A series of pottery samples from the Iranian site Tol-e Kamin, ranging from pre-historical period to the New Elamite, were analyzed in order to study the geochemical variability of the pottery assemblage. A total amount of 168 measurements were obtained using a portable XRF device and were statistically handled. The results could successfully distinguish the geochemical composition of potteries from the chalcolithic to the New Elamite periods in the Kur River Basin. A major shift in the use of different clay sources could be detected since the Proto Elamite period and afterward, in which the carbonated and marl content clays represented by Ca, Ba and Sr shifted to clay sources with a tendency to non-carbonate silty clay Al, Ti, and Fe from a different geological background. The results stress the importance of further provenance studies to address issues of trade and exchange possibilities in southwestern Iran.
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