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Radiocarbon-dating an early minting site: the emergence of standardised coinage in China

Published online by Cambridge University Press:  06 August 2021

Hao Zhao*
Affiliation:
School of History, Zhengzhou University, P.R. China
Xiangping Gao
Affiliation:
School of History, Zhengzhou University, P.R. China
Yuchao Jiang
Affiliation:
School of History, Zhengzhou University, P.R. China
Yi Lin
Affiliation:
School of History, Zhengzhou University, P.R. China
Jin Zhu
Affiliation:
School of History, Zhengzhou University, P.R. China
Sicong Ding
Affiliation:
School of History, Zhengzhou University, P.R. China
Lijun Deng
Affiliation:
Modern Analysis and Computer Center of Zhengzhou University, P.R. China
Ji Zhang
Affiliation:
School of Archaeology and Museology, Peking University, P.R. China
*
*Author for correspondence ✉ haozhao@zzu.edu.cn
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Abstract

The origins of metal coinage and the monetisation of ancient economies have long been a research focus in both archaeology and economic history. Recent excavations of an Eastern Zhou period (c. 770–220 BC) bronze foundry at Guanzhuang in Henan Province, China, have yielded clay moulds for casting spade coins. The technical characteristics of the moulds demonstrate that the site functioned as a mint for producing standardised coins. Systematic AMS radiocarbon-dating indicates that well-organised minting developed c. 640–550 BC, making Guanzhuang the world's oldest-known, securely dated minting site. This discovery provides important new data for exploring the origin of monetisation in ancient China.

Information

Type
Research Article
Copyright
Copyright © The Author(s), 2021. Published by Cambridge University Press on behalf of Antiquity Publications Ltd.
Figure 0

Figure 1. Location of Guanzhuang and the political landscape of the Chunqiu period. Guanzhuang is located some 60km to the north-west of the capital of the Zheng State (Xinzheng) and 100km to the east of the royal capital of the Zhou Dynasty. The map shows the primary polities (white pentagons) around the Chinese Central Plains and their capital cities. The major competitors fighting for the hegemony of the Central Plains are marked in red (figure by H. Zhao).

Figure 1

Figure 2. Layout of Guanzhuang and the location of the bronze foundry (figure by H. Zhao).

Figure 2

Figure 3. Spatial distribution of the minting remains in the foundry's excavation area: red dots: deposit with clay moulds; green dots: deposits with fragments of finished spade coins (drone photograph by Z. Qu; figure by H. Zhao).

Figure 3

Figure 4. Spade coin SP-1 and its reconstruction. The outer mould (bottom left) from pit H2032 is also used to reconstruct the spade coin (photograph by H. Zhao).

Figure 4

Figure 5. CT image of coin SP-1. Three parallel striations and the raised rim around the spade are clearly visible. Top right) lateral view of handle, with the clay core still inside the socket of the handle (CT photograph by H. Zhao).

Figure 5

Figure 6. Unused clay cores for casting spade coins and coin SP-2. The letters and schematic diagrams above each core indicate its type of batch mark. The numbers below each core indicate its archaeological context (photograph by H. Zhao).

Figure 6

Table 1. Elemental composition of the spade coins from Guanzhuang and comparative specimens. The composition of coin SP-1 was obtained through electron-probe micro analysis (EPMA), that of coin SP-2 by inductively coupled plasma mass spectrometry (ICP-MS). Comparative data taken from Zhou (2004).

Figure 7

Figure 7. Discarded core heads. The letters and schematic diagrams above each core indicate its type of batch mark. Although some core heads are damaged, their batch marks can still be discerned (photograph by H. Zhao).

Figure 8

Figure 8. A) Diagram showing the assemblage of the outer moulds and core; B) diagram of the casting sequence of a spade coin; C) structure of an almost intact, unused clay core. The core head and body are demarcated by a raised boundary line. CB top thickness = the top thickness of the core body; CB top width = the top width of the core body (photograph and figure by H. Zhao).

Figure 9

Figure 9. Plan and profile of pit H2032 and associated contexts. Deposit units subjected to AMS radiocarbon-dating are marked with stars (figure by H. Zhao).

Figure 10

Figure 10. OxCal plot of the calibrated AMS radiocarbon dates of tested samples. The data are presented according to the stratigraphic sequence (figure by Beta Analytic Inc.; Reimer et al. 2013; Bronk Ramsey 2017).

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