Umm an‐Nar burial 401 at Bat,Oman: architecture and finds

The archaeological site at Bat has an important status with regard to research on the Umm an‐Nar culture. Investigations began there in 1972 and were revived in 2004, when the excavation of tomb 401 was begun. This paper presents the complete corpus of grave‐goods. Despite all the disturbances within the find layers, when comparing the two chambers it is possible to observe some indications of the different burial cycles and detect distinguishing characteristics. Taking into account the divergent earlier and later ceramic styles, burial use must be proposed between 2400 and 2200 BC. This date accords with observations of the architectural details of tomb 401 and with the sequence of tomb construction types in the Bat region. This paper is dedicated to the memory of professor Gerd Weisgerber.     

Kusanagi Tsuyoshi x Chonangang: Transcending Japanese/Korean Ethnic Boundaries in Japanese Popular Culture

In the last ten years or so, interest among the Japanese in their Korean neighbour has increased significantly. Yet, before the Korean Wave hit Japan in the early 2000s, Kusanagi Tsuyoshi, member of popular Japanese boy-band SMAP, had already débuted and gained popularity as Chonangang, his Korean alter-self. From releasing a Korean pop-music single to interviewing South Korean Presidents on Japanese national television, it is undeniable that Kusanagi (and Chonangang) has brought Korea closer to the hearts of the Japanese. In this paper, I argue that Kusanagi's performances of and as Chonangang create a polyglotic, hybrid identity that functions as a “third space” through which notions of an underlying, essential Japanese (and Korean) identity can be destabilised. Beyond mere entertainment, Kusanagi's adoption of an identity position that is neither Japanese nor Korean, yet also both Japanese and Korean, enables the articulation of difference and hybridity which, I contend, has direct relevance to Japan–Korea and Japanese–resident Korean relations.     

HMQS Mosquito: the rediscovery and identification of Queensland's first warship

In 2009, the remnants of Her Majesty's Queensland Ship Mosquito, a 2nd‐class torpedo‐boat built in 1883, were relocated. Purchased by the colonial government of Australia in response to heightened tensions between Great Britain and Imperial Russia, Mosquito was assigned to Queensland's capital, Brisbane, where it had a largely uneventful career. Following removal from active duty it was stripped and abandoned on the foreshore of a tributary of the Brisbane River. This paper discusses Mosquito's historical background, and chronicles the rediscovery of the vessel, and the archaeological investigation and identification of its remains. © 2010 The Author     

The Mesolithic Maritime Landscape on the North Coast of Ireland

A combination of reconstruction of the former coastline and field survey of previously unrecorded sites provides the basis for the study of the maritime landscape and maritime activities around Portrush on the north coast of Ireland during the Mesolithic period. Movements in relative sea‐level and geological events indicate significant change in environment and availability of resources, particularly flint, for the coastal community. Evidence suggests that most Early Mesolithic material, deposited close to the then shoreline, is presently under water. Remnants of the Late Mesolithic are fast disappearing as coastal erosion continues. © 2010 The Author     

Money talks: banknote iconography and symbolic constructions of Scotland

ABSTRACT. It has become common for scholars of nations and nationalism to use banknotes, coins and postage stamps as passing examples of everyday objects expressive of nationalism. Until recently, however, it has been less common for these objects to form the focus of empirical enquiries that substantiate their contribution to the creation and transmission of national symbolism. This article addresses this lacuna through an empirical investigation of over 300 years of Scottish banknote iconography. In their symbolic content, banknotes are shown to be amenable to the service of both national and non‐national political agendas. To explain this phenomenon, we advance three interrelated arguments. First, we contend that variations in banknote iconography reflect the different political contexts in which notes were produced and the distinctive loyalties and customer constituencies of the banks that issue them. Second, we argue that changes in banknote imagery reflect changes in the scale of their circulation. Third, we argue that Scottish banknotes have always included iconography that constructs the image of the bank and advertises its reliability, often through association with national images. The article concludes by addressing Scotland's place in wider understandings of the iconographic power of banknotes.     

The politics of recognition: symbols,nation building and rival nationalisms

ABSTRACT. Ceremonial initiatives linked to nation‐building projects are highly visible in multiethnic states, where governments seem to have adopted a Durkheimian approach in which ceremonies contribute to the strengthening of communities. However, national ceremonies are not invented or exported to other nations easily, as seen when outlining the pattern of a successful national day. A unifying narrative (sometimes the historical genesis) is significant in the establishment of successful national days, as is the nature of the national day design. The celebrations of the constitution in Norway – and the 77 year struggle to get the Norwegian flag officially recognised – became part of resisting the enforced union with Sweden (1814–1905). Therefore, the growth of Norwegian nationalism must be understood in the context of rival nationalisms in Scandinavia. However, Constitution Day (17 May) has remained a powerful component of Norwegian nationalism long since the constitution ceased to be threatened because of its incorporation in primary and secondary school curricula and, more recently, within the debate on multiculturalism.     

Origin of palaeo‐waters in the Ordovician carbonates in Tahe oilfield,Tarim Basin: constraints from fluid inclusions and Sr,C and O isotopes

Petrographic features, isotopes, and trace elements were determined, and fluid inclusions were analyzed on fracture‐filling, karst‐filling and interparticle calcite cement from the Ordovician carbonates in Tahe oilfield, Tarim basin, NW China. The aim was to assess the origin and evolution of palaeo‐waters in the carbonates. The initial water was seawater diluted by meteoric water, as indicated by bright cathodoluminescence (CL) in low‐temperature calcite. The palaeoseawater was further buried to temperatures from 57 to 110°C, nonluminescent calcite precipitated during the Silurian to middle Devonian. Infiltration of meteoric water of late Devonian age into the carbonate rocks was recorded in the first generation of fracture‐ and karst‐filling dull red CL calcite with temperatures from <50°C to 83°C, low salinities (<9.0 wt%), high Mn contents and high ⁸⁶Sr/⁸⁷Sr ratios from 0.7090 to 0.7099. During the early Permian, ⁸⁷Sr‐rich hydrothermal water may have entered the carbonate rocks, from which precipitated a second generation of fracture‐filling and interparticle calcite and barite cements with salinities greater than 22.4 wt%, and temperatures from 120°C to 180°C. The hydrothermal water may have collected isotopically light CO₂ (possibly of TSR‐origin) during upward migration, resulting in hydrothermal calcite and the present‐day oilfield water having δ¹³C values from ?4.3 to ?13.8‰ and showing negative relationships of ⁸⁷Sr/⁸⁶Sr ratios to δ¹³C and δ¹⁸O values. However, higher temperatures (up to 187°C) and much lower salinities (down to 0.5 wt%) measured from some karst‐filling, giant, nonluminescent calcite crystals may suggest that hydrothermal water was deeply recycled, reduced (Fe‐bearing) meteoric water heated in deeper strata, or water generated from TSR during hydrothermal water activity. Mixing of hydrothermal and local basinal water (or diagenetically altered connate water) with meteoric waters of late Permian age and/or later may have resulted in large variations in salinity of the present oilfield waters with the lowest salinity formation waters in the palaeohighs.     

CHEMISTRY VERSUS DATA DISPERSION: IS THERE A BETTER WAY TO ASSESS AND INTERPRET ARCHAEOMETRIC DATA?

Given the common use of chemical concentration data to define ceramic groups that aid in the exploration of ancient technology, trade and provenance, it is important to reflect on how we collectively establish and define both chemical groups and outliers. In this paper, we argue that commonly used data analysis procedures, such as principal component analysis and centred log‐ratio principal component analysis favoured in the examination of ceramic chemical data, although rapid and easy, may overlook existing chemical groups and outliers, especially when the ratio of non‐diagnostic to diagnostic elements is high. To evaluate whether geochemistry is more important than data dispersion in data assessment, we re‐examine chemical concentration data from previously published ceramic, clay and daub samples from the lower Ohio River Valley. We begin by briefly discussing steps we took to ensure that the data set reflects geochemical differences, rather than analytical or data transfer errors. Next, we use bivariate plots, as well as PCA and CLR–PCA, to examine different versions of our altered data, using varying numbers of element combinations. We propose that the careful examination of bivariate plots is critical in establishing the elements that should be included in PCA and other multivariate analyses.     

ARTIFICIAL OR NATURAL ORIGIN OF HEMATITE‐BASED RED PIGMENTS IN ARCHAEOLOGICAL CONTEXTS: THE CASE OF RIPARO DALMERI (TRENTO,ITALY)

This study concerns those crystallographic and microstructural features that can provide indications on the actual origin of red pigments based on hematite (Fe₂O₃). The main features of natural and artificial hematite are recalled and used to discuss the results obtained from the characterization of red‐ochre samples coming from the Palaeolithic site of Riparo Dalmeri, a rock‐shelter located in northeastern Italy, dated to 13 000 cal. bp , and notorious for the presence, among the other finds, of red‐painted calcareous stones. Painting and the treatment of leather and hides obtained from the intensive hunting activity were the main uses of the hematite‐based red‐ochres at Riparo Dalmeri. It turns out that hematite was mostly obtained from the thermal treatment of goethite, which, unlike hematite, was and still is widely available in the neighbourhood of the site.