Qin-Qin Lu
University of Cambridge, McDonald Institute for Archaeological Research, Department Member
The Miaodigou culture in central China had far-reaching influence across much of the Late Neolithic China, leading to the formation of some would call 'Early China'. Its exquisitely painted pottery with highly stylized patterns is... more
The Miaodigou culture in central China had far-reaching influence across much of the Late Neolithic China, leading to the formation of some would call 'Early China'. Its exquisitely painted pottery with highly stylized patterns is especially well-known to East Asian archaeologists. The Miaodigou culture is represented by archaeological remains of Phase I (3800-3300 BCE) of the Miaodigou site in present-day Sanmenxia City of Henan Province. While a high level of specialization in pottery production has long been assumed for the Miaodigou site (and the culture as well), it has not been systematically demonstrated and discussed. The present study focuses on the Phase I utilitarian pottery-most of which are plain but some are painted-recently unearthed from the Miaodigou site. By combining archaeological and archaeometric evidence, including chemical compositional analysis (hhXRF) and mineral identification (XRD), we, for the first time, discuss pottery production at the very center of the Miaodigou culture. We reveal an overall compositional uniformity in the Miaodigou utilitarian pottery that largely exists across different pastes, colors, vessel forms, form-deduced functions, stages, and spatial units. Our results attest to the high intensity and technological continuity of pottery production at the Miaodigou site, confirming that the site was a regional production center through much of the Miaodigou culture period. We suggest that the centralized production of pottery had taken place at the Miaodigou site.
Research Interests:
Excavated glass artifacts are usually environmentally impacted, causing spatial inhomogeneity which poses great challenges for accurate and non-destructive chemical characterization. Here, we present our study on accurate characterization... more
Excavated glass artifacts are usually environmentally impacted, causing spatial inhomogeneity which poses great challenges for accurate and non-destructive chemical characterization. Here, we present our study on accurate characterization of archaeological glass with Laser Ablation Inductively Coupled Plasma Mass Spectrometry (LA-ICP-MS), a high-precision and minimally destructive analytic method. Using three corroded glass beads excavated from Guangnan, Yunnan, Southern China as examples, we discuss the issues that may be involved when observing signal curves of highly inhomogeneous archaeological glass, as well as provide chemical characterization for the intact pristine body. Results indicate that these Indo-Pacific monochrome beads are of the potassium silicate glass type and used mineral potash source, and that they contain copper as the colorant. By discussing the breadth and depth types of inhomogeneity and focusing on perturbation endured by major elements, we identify the extent of environmental alteration and describe how different elements and matrices can respond differently to the archaeological environment, leading to various corrosion behaviors. For such samples LA-ICP-MS is shown to be an advantageous tool to provide archaeologically relevant information, or to probe artifact conditions for conservation purposes. A good understanding of sample conditions, and close attention to the experimental and calibration process are required to overcome inhomogeneity when tackling archaeological glass.
Research Interests:
Bioavailable Sr and detrital Nd isotopes are important tools for archaeological provenance. To apply Sr and Nd isotopes for provenance, regional isotope databases and baselines are generally needed. For the vast Silk Road regions of... more
Bioavailable Sr and detrital Nd isotopes are important tools for archaeological provenance. To apply Sr and Nd isotopes for provenance, regional isotope databases and baselines are generally needed. For the vast Silk Road regions of Mesopotamia, Iran, and Central Asia, detailed isotopic distribution patterns essential for determining provenance may not become available in the short term due to the severe deficiency of available data. In the present work, we investigate the geo-environmental factors controlling the Sr and Nd isotopic signatures and use published data from archaeology and Earth sciences, selected by rigorous criteria, to construct the first largescale, semi-quantitative Sr-Nd isotope baseline for these Silk Road regions. Three isotopic zones are proposed for Central Asia: CA-1 (mountains), ε Nd < − 7.5, 87 Sr/ 86 Sr > 0.7095; CA-2 (deserts), ε Nd = − 5 to − 2, 87 Sr/ 86 Sr ~ 0.709; CA-3 (loess), ε Nd = − 5 to − 2, 87 Sr/ 86 Sr > 0.710. General isotopic signatures are suggested for Iran: ε Nd = − 8 to − 4, 87 Sr/ 86 Sr = 0.7075-0.7090. Three isotopic zones are proposed for Mesopotamia: MP-1 (floodplain and foothill), ε Nd = − 6.5 to − 4 (putative extended range MP-1N, ε Nd = − 8 to − 6), 87 Sr/ 86 Sr = 0.7080-0.7085; MP-2 (deserts), ε Nd < − 8, 87 Sr/ 86 Sr > 0.7085; MP-3 (Syrian Euphrates), ε Nd = − 5.5 to − 2, 87 Sr/ 86 Sr = 0.7080-0.7085. Within the limitation of available data, these ranges indicate the overall trend of bioavailable Sr and detrital Nd isotopic signatures for each isotopic zone, which are controlled by their geological context, climate (e.g., precipitation), and various Earth surface processes (e.g., riverine versus aeolian transport). This baseline can be used as an essential guide for geochemical contexts to suggest or verify the provenance of plant-ash glass, serving as part of an integrative Sr-Nd isotopic approach. We illustrate the potential of this approach using two case studies. By investigating the isotopic compositions of Mesopotamian plant-ash glass, we suggest possible northern Mesopotamian origins for plant ash and silica raw materials used for Mesopotamian glass-making. By reassessing medieval plant-ash glass from San Lorenzo, Italy, we propose diverse origins including Central Asia and Mesopotamia. Additionally, as part of this isotopic approach, by examining the Nd isotope mixing lines in the context provided by the Nd isotope baseline, we reveal the occurrence of glass recycling for Islamic plant-ash glass from different production zones in association with a westward spread from Mesopotamia to the Eastern Mediterranean metropolises.
Research Interests:
The phases of a Bose-Einstein condensate (BEC) with light-induced spin-orbit coupling (SOC) are studied within the mean-field approximation. The mixed BEC phase, in which the system condenses in a superposition of two plane wave states,... more
The phases of a Bose-Einstein condensate (BEC) with light-induced spin-orbit coupling (SOC) are studied within the mean-field approximation. The mixed BEC phase, in which the system condenses in a superposition of two plane wave states, is found to be stable for sufficiently small light-atom coupling, becoming unstable in a continuous fashion with increasing light-atom coupling. The structure of the phase diagram at fixed chemical potential for bosons with SOC is shown to imply an unusual density dependence for a trapped mixed BEC phase, with the density of one dressed spin state increasing with increasing radius, providing a unique experimental signature of this state. The collective Bogoliubov sound mode is shown to also provide a signature of the mixed BEC state, vanishing as the boundary to the regime of phase separation is approached.