2021
DOI: 10.1017/irq.2021.1
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Late Chalcolithic Ceramic Development in Southern Iraqi Kurdistan: The Stratigraphic Sounding at Kani Shaie

Abstract: Kani Shaie is a small archaeological site in the Kurdistan Region of Iraq, centrally located in the Bazian Basin, a narrow valley at the western edge of the Zagros Mountains along the major route between Kirkuk and Sulaymaniyah. Its main mound was inhabited almost continuously from the fifth to the middle of the third millennium, c. 5000–2500 B.C.E. This period of Mesopotamian prehistory, corresponding to the Chalcolithic and Early Bronze Age, witnessed major transformations such as initial urbanism and intens… Show more

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Cited by 5 publications
(9 citation statements)
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“…500 years before the following MM VIb (LC1) levels. Considering the continuity in the pottery assemblages (Renette et al 2021: Figure 17) and lack of clear evidence for a break in the stratigraphic sounding, such a long hiatus seems unlikely and cannot at present be substantiated by this single radiocarbon sample. However, this result can also not be fully rejected considering the unusually high date ranges provided for the Ubaid-LC1 transition by the Surezha project (Stein 2018).…”
Section: Resultsmentioning
confidence: 82%
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“…500 years before the following MM VIb (LC1) levels. Considering the continuity in the pottery assemblages (Renette et al 2021: Figure 17) and lack of clear evidence for a break in the stratigraphic sounding, such a long hiatus seems unlikely and cannot at present be substantiated by this single radiocarbon sample. However, this result can also not be fully rejected considering the unusually high date ranges provided for the Ubaid-LC1 transition by the Surezha project (Stein 2018).…”
Section: Resultsmentioning
confidence: 82%
“…The sequence consists of 12 levels (SS-1-12; mainly defined by the construction of new architecture) that are combined into subphases (MM Va-d and MM VIa-b) based on changes in the ceramic assemblages (Renette et al 2021: Figure 17). Even though our approach to defining these ceramic assemblages prioritized the internal, sitespecific development by identifying vessel shapes and fabrics within the site's ceramic corpus before determining external comparanda, the phasing largely matches the general LC1-5 chronological framework established for northern Mesopotamia, albeit with distinct local characteristics (Renette et al 2021). Subperiods LC3 and LC5 proved to be more difficult to reliably identify based on ceramic parallels due to the absence of specific vessel shapes that have been used to define those periods in northern Mesopotamia (Renette et al Table 1 Kani Shaie Main Mound phasing (B levels are from Area B, which is a 5 × 5 m trench at the top of the southern slope of the mound; SS levels are from the Stratigraphic Sounding, which is a downward continuation of Area B as can be seen in Figure 5).…”
Section: Kani Shaie-stratigraphic Sequencementioning
confidence: 92%
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