Establishing the Prehistoric Cultural Sequence for the Lopburi Region, Central Thailand

This study comprises the first archaeologically-defined chronological and cultural sequence for central Thailand. Based on collaborative research between the Thai–Italian Lopburi Regional Archaeological Project and the Thai–American Thailand Archaeometallurgy Project, the results of excavations at seven pre- and protohistoric sites that witnessed three millennia of local cultural development, from the early second millennium BC onward, are synthesized herein. This study fills a significant gap in Thailand’s prehistory, also identifying important cultural interactions ranging into southern China and Vietnam that led to the formation during the second millennium BC of a ‘Southeast Asian Interaction Sphere’. This interaction sphere, at the close of the second millennium BC, facilitated the transmission of the knowledge of copper-base metallurgy from southern China into Thailand, where it reached the communities of the Lopburi Region who took advantage of their ore-rich environment. At the end of the first millennium BC, strong South Asian contacts emerge in Southeast Asia. Among this study’s salient contributions is the characterization of these critical prehistoric antecedents, which culminated in a process of localization of exogenous elements, usually termed ‘Indianization’. The impact of this dynamic process was initially felt in central Thailand in the late first millennium BC, leading over time to the rise there, by the mid first millennium AD, of one of Southeast Asia’s first ‘state-like’ entities.     

Seismic vulnerability assessment of historical centers at urban scale

Seismic prevention and mitigation of historical centers have gained a central position within earthquake engineering topics, particularly in areas such as Italy, Greece, and Portugal. Many historical towns in these countries have been strongly damaged, due to the high quantity of old buildings and urban structures and infrastructures. In this article, these aspects are described, modeled, and investigated in terms of structural safety, the goal being the set-up of a comprehensive strategy for seismic prevention and mitigation of a whole historical center. The proposed approach is based on two relevant parts: the first is an urban risk assessment, the second is a prioritization of retrofitting interventions so as to optimally increase urban safety.

The effectiveness of the proposed methodology is shown with reference to a complex case study, the historical center of “Montebello di Bertona”. It is initially modeled as a series/parallel system and then studied by applying seismic reliability methods. Seismic retrofitting interventions are finally prioritized.     

The Origins of the Bronze Age of Southeast Asia

White and Hamilton (J World Prehist 22: 357–97, 2009) have proposed a model for the origin of the Southeast Asian Bronze Age founded on seven AMS radiocarbon determinations from the Northeast Thai site of Ban Chiang, which would date the initial Bronze Age there to about 2000 BC. Since this date is too early for the derivation of a bronze industry from the documented exchange that linked Southeast Asia with Chinese states during the 2nd millennium BC, they have identified the Seima-Turbino 3rd millennium BC forest-steppe technology of the area between the Urals and the Altai as the source of the Southeast Asian Bronze Age. We challenge this model by presenting a new chronological framework for Ban Chiang, which supports our model that the knowledge of bronze metallurgy reached Southeast Asia only in the late 2nd millennium BC, through contact with the states of the Yellow and Yangtze valleys.     

Minero-petrographic characterization of fine ware from Cales (South Italy)

79 samples of black glazed pottery, Terra sigillata, fine common ware, and production indicators were recovered in the archaeological site of Cales and investigated via a multi-analytical program (polarized light microscopy, thermal analyses, XRPD, XRF, FESEM, FESEM-EDS). Among the materials, finds of important production indicators, represented by welded pieces of black glazed pottery and spacers, attest a local production. Polarized light microscopy shows that the inclusions consist of feldspar, quartz, mica, calcite, and lithic fragments of both volcanic and sedimentary nature. Additional information about the mineralogical assemblage comes from the XRPD that revealed the presence of neoformed Ca-silicates, indicating equivalent firing temperatures ranging from 750 to 1050°C. All the samples show a Ca-rich character and an extreme compositional homogeneity, including the production indicators. The comparison with some Ca-rich Campanian clay raw materials shows a greater affinity with the Mio-Pliocene marine clay sediments of the Apennine sector, which include local clays. This allowed us to formulate the first hypotheses about clay sources used to produce fine pottery during the third century BCE to the early imperial period in Cales.