A first meeting place: John Webber’s An Interview Between Captain Cook and the Natives (January 1777)

On 26 January 1777, on the first stage of his third voyage to the Pacific, James Cook anchored in Adventure Bay on what is now called Bruny Island, Tasmania. Cook encountered the local Nuonenne people on two occasions, the second of which was recorded in an unfinished drawing (possibly done on the spot) by the expedition’s artist, John Webber. Comments in their journals from officers and sailors on board Cook’s ships indicate that the European perceptions and representations of Aboriginal people were initially mediated by the explorers’ stereotypical understanding of other races. However, through a close reading of a number of structural features of Webber’s composition – symmetry, resemblances in opposition, chiasmus, a figure who acts as a spectatorial stand-in, spatialisation – it is argued that Webber’s drawing recognises the Aboriginal people encountered by the British as individuals, attends to the dramaturgy of the encounter, and is marked in various ways by a powerful and grounded indigenous agency. It is proposed that anthropologist Marshall Sahlins’ paradoxical aphorism ‘structure of the conjuncture’ might be used to illuminate and designate the particular quality of events, the ‘indigenous countersigns’, depicted by Webber in this drawing.     

Suffolk Place,Southwark, London: a Tudor palace and its terracotta architectural decoration

Suffolk Place (c. 1518–22), Southwark, was the London residence of Charles Brandon, Duke of Suffolk. This majestic palace is visible in the foreground of Wyngaerde’s London panorama (c. 1544), from which it can be inferred that it possessed a double courtyard plan. The southern and eastern ranges of the outer courtyard of Suffolk Place were apparently adorned with architectural terracottas at both entablature and parapet level. As the palace was demolished in 1557–58, the finds of ex-situ terracottas are a key source of information concerning the decorative scheme of this vanished palace. Petrological study and other research indicates that the terracottas were locally manufactured, implying the existence of a London-area workshop.     

Sex work and exclusion in the tourist districts of Salvador,Brazil

Salvador, capital of the state of Bahia, in the Northeastern region of Brazil, is composed of racialized, gendered, and sexualized spaces in which certain people are welcome, while others are marginalized and excluded. Praça da Sé, in the Centro Histórico, is a major site of both the local commercial sex industry and the tourist industry in Salvador. With their public visibility in sites heavily frequented by tourists, sex workers in Salvador reveal how sexuality is public, politically contested, economically charged, and, most significantly, racialized. If, as Tom Boellstorff argues, ‘globalization resignifies the meaning of place rather than making place irrelevant’ (2007, 23), how does one then study racialized sexualities in the context of the globalized tourism industry? How do class, space, and race influence practices of sex work and sex tourism in Salvador? This article offers a critical analysis of racialized sexualities in the study of the sexual economies of tourism in Salvador. I conceptualize Salvador as a ‘site of desire’ (Manderson and Jolly 1997) where issues of socioeconomic inequality, racism, and sexism coexist alongside celebratory affirmations of Afro-Brazilian cultural production in Salvador. This article explores how the touristic cityscape of Salvador is divided into carefully demarcated zones where class and race are crucial factors in determining who ‘belongs’ and who is ‘out of place.’     

Iron isotope analysis of red and black pigments on pottery in Nasca,Peru

The Nasca culture of the south coast of Peru developed during the first millennium ad and is known internationally for its elaborately decorated polychrome pots. Despite decades of iconographic analysis, little is known about the more technological aspects of Nasca pigment production and application. We present results from a pilot study on iron isotopes as a potential line of inquiry into the differences between red and black pigments in Nasca pigments. As well, we conduct a small firing experiment to examine potential changes in isotope composition. Our analyses show three significant results. First, firing does not change the isotopic ratios of Fe in pigments. Second, red and black pigments show differences in their iron isotope composition, which relate to differences in the minerals used to make the different colors. Third, naturally available hematite samples show greater isotopic variation than pigment samples, suggesting that people selected a limited range of iron oxides to produce pigments.     

Baseline data for Andean paleomobility research: a radiogenic strontium isotope study of modern Peruvian agricultural soils

While the use of radiogenic strontium isotope values to examine paleomobility is increasingly common in the Andes, and beyond, many questions about baseline variability remain. To better understand baseline radiogenic strontium isotope compositions in the Andes, we present new ⁸⁷Sr/⁸⁶Sr values from Peruvian soil samples. Modern soil samples were collected from agricultural fields from the following areas in central and southern Peru: Arequipa, Atico, Camaná, Chala, Cusco, Ica, Ilo, Lima, Mejía, Moquegua, Nazca, Ocoña, Palpa, Pisco, Puno, Tacna, and Yauca. Samples were partially dissolved to better approximate the bioavailable strontium. Radiogenic strontium isotope values from the partially dissolved soil samples range from ⁸⁷Sr/⁸⁶Sr?=?0.70202 to 0.71894 and, for all soil samples, have a mean of ⁸⁷Sr/⁸⁶Sr?=?0.70773?±?0.00166 (1σ, n?=?114). In general, the ⁸⁷Sr/⁸⁶Sr values measured for soil samples collected from modern agricultural fields reflect the expected ⁸⁷Sr/⁸⁶Sr values based on bedrock geology. Comparing our new soil data with published radiogenic strontium isotope data for bedrock, soil, water, and faunal samples provides constraints on the regions in the Andes that can, and cannot, be distinguished through radiogenic strontium isotope analysis.