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The reconstruction of complex political formations in tropical and subtropical environments has long been challenged by the ephemeral nature of archaeological deposits and the detectability of a settlement hierarchy. This paper presents findings from systematic archaeological surveys in the Lake Dian basin in southwest China to evaluate processes of political differentiation during the Bronze Age (ca. BC 900–100) and identified with the protohistoric kingdom of Dian. We discuss the problems of interpreting political consolidation based on mono-centers and ranked site size distributions. Our approach considers the contingent forms that ‘built’ landscapes can take in the humid subtropics in an effort to understand the variable relationship between politics and spatial scale. Combining traditional survey as well as subsurface methods suited for intensively worked paddy landscapes, we discuss the emergence and timing of multiple nucleated settlements as indicative of peer polity dynamics in the basin and examine the formation histories of large shell mound sites to highlight physical modifications that embedded central places during the Bronze Age period. We show that the boundary between on-site and off-site, living and non-living spaces is not solely determined by the availability of prime land but also by spatial conventions with discrete cultural and historical ramifications. By contextualizing macroscale views on complexity with an understanding of local scales of landscape transformation, we provide an alternative to models of pristine state formation based in temperate alluvial environments. [ABSTRACT FROM AUTHOR]

Abstract: The earliest evidence of prehistoric religious practice in China found so far comes from excavations at Beifudi, about 120 km south of Beijing, in the form of votive offerings and porcelain sorcery masks dated to the period 8000–7000 yr BP. These finds are part of a rich Neolithic site located on the second river terrace on the north shore of the Yi River. This paper presents results of pollen analysis of part of a sediment profile from a depression at the edge of first terrace towards second terrace, a few hundred metres away from the main archaeological finds. A sequence of marked changes in environment occurred between 9000 cal yr BP and 6000 cal yr BP, and dating evidence suggests strong associations with the ebb and flow of human activity in the area. The first phase of activity on the site begins at around 8000 cal yr BP, towards the end of a period of relatively dry, cold environmental conditions. Between 7800 cal yr BP and 7400 cal yr BP, the first clear evidence of cereal cultivation appears in the pollen record. Rich archaeological finds occur during the same time period, suggesting local prosperity. This first phase of the Beifudi culture ends at 7300 cal yr BP, when warmer and wetter conditions are inferred and wetland areas expand, reducing the area available for crop cultivation near the site. A return to drier and cooler conditions from 6900 cal yr BP corresponds with the second phase of apparent prosperity in the archaeological record from Beifudi. This phase ends at around 6500 cal yr BP, at the start of another shift towards wetter conditions in the flood plain environment. The pollen record suggests that environmental conditions in the flood plain were a major determinant of human activity at Beifudi in the early-mid Holocene. [Copyright &y& Elsevier]

Abstract: More than 200 bronze objects found in Hanzhong, southwest Shaanxi Province, China, a frontier region of the Shang Kingdom during the Shang dynasty, have been analysed for their composition and microstructure. Forty-three typologically distinct, and probably culturally indigenous, items have been found to be compositionally distinctive as well. This paper presents analytical results of the two types of local Hanzhong bronzes, namely the sickle-shaped and sceptre-shaped objects. Three special alloys, arsenic bronze, antimonial bronze and copper–nickel–arsenic ternary alloy, are particularly emphasized and discussed. The archaeological context of Hanzhong bronzes and their significance for the archaeometallurgy research of the Shang period are discussed as well. [Copyright &y& Elsevier]

Abstract: Shang-dynasty bronzes recovered in the Hanzhong region, Shaanxi province have been receiving considerable research interest since the 1950s due to their strong regional characteristics. This paper presents preliminary analytical results of 16 samples taken from 13 Hanzhong bronze objects, which, for the first time, have revealed their diversity in chemical composition and casting quality. In particular, the finding that some correspondence probably exists between the types of artefact and their materials has significant implications for identifying regional technical characteristics of the Hanzhong bronzes, as well as for exploring the interaction between the metropolitan areas of the Shang Kingdom with the areas beyond its southwestern frontiers. [Copyright &y& Elsevier]

• We review the state of research on human-environment interaction in Holocene China. • We demonstrate the benefits of a multidisciplinary, regionally focused approach. • We conclude datasets must be local and specific, and integrate data on multiple scales. • China is large, well-documented, and critical for understanding social-natural systems. This paper reviews recent archaeological research on human-environment interaction in the Holocene, taking continental China as its geographic focus. As China is large, geographically diverse, and exceptionally archaeologically and historically well-documented, research here provides critical insight into the functioning of social-natural systems. Based on a broad review of the field as well as recent advances and discoveries, the authors reflect on research themes including climate change and adaptive systems theory, spatial and temporal scale, anthropogenic environmental change, risk management and resilience, and integration of subdisciplines. These converge on three overarching conclusions. First, datasets relevant to climate change and ancient human-environment interaction must be as local and specific as possible, as the timing of environmental change differs locally, and the human response is highly dependent on local social and technological conditions. Second, the field still needs more robust theoretical frameworks for analyzing complex social-natural systems, and especially for integrating data on multiple scales. Third, for this work to contribute meaningfully to contemporary climate change research, effective communication of research findings to the public and to scientists in other disciplines should be incorporated into publication plans. [ABSTRACT FROM AUTHOR]

In their paper "The beginning of faience in China: A review and new evidence", Lin et al. (2019) conclude that the Kayue people in Qinghai began making faience with a high potash content during the second half of the second millennium BC, prior to the Zhou people (1046-771BC). Based on a thorough assessment of the archaeological evidence, especially concerning the dates of the Kayue tombs, I conclude there is a lack of solid evidence that these faience beads predate the Western Zhou Dynasty (1046-771BC) so it cannot be inferred that the Zhou people learned production technologies for high potash faience from the Kayue people. A possible faience road for the transfer of production technologies from Xinjiang to Central China is further proposed. In this transfer process, some typology and production technologies for faience beads were adopted by the Western Zhou people, but the glaze recipe of most faience changed greatly in Central China due to adaptation to local resources. • The spread of faience is the earliest case of globalization in ceramic history. • A faience road is proposed between East Xinjiang and Central China during the late Bronze Age/early Iron Age. • Copper has been used as a glaze colorant in China since the introduction of faience. [ABSTRACT FROM AUTHOR]