Situating Justice in the Environment: The Case of BHP at the Ok Tedi Copper Mine

The rubric of sustainable development has now gained wide theoretical and political acceptance in the global community. However, after the Rio Declaration, each nation must now confront the specific question of how to decide between those industries and activities that are sustainable and those that are not when conflicting social and ecological interests are at stake. Any fundamental change to resource allocation will have social distributional consequences, and the issue of justice therefore becomes a critical element of any sustainability formulation. This paper contributes to this debate by exploring the potential for a politically grounded theory of justice in and to the environment. More specifically, we argue for a situated analysis that nevertheless retains the postulate of a neo-Kantian universal ethic as the foundation for global institutions that could integrate and safeguard the principles of justice and ecological responsibility underpinning most notions of sustainability. We show this by locating the question of justice in a particular conflict of interest, that between the Australian mining giant Broken Hill Proprietary, Ltd., and the traditional landowners of an area on the Ok Tedi river in Papua New Guinea.     

From Propaganda to ‘Information’: Reforming Government Communications in Britain

Since the 1980s, several studies of post-war British propaganda have been published. While many of these have focused on developments abroad, some have explored domestic work carried out under the auspices of the Central Office of Information. Established in 1946, the Central Office of Information provided a range of services to government departments, including advertising and public opinion polling, but it was just part of a wider system of official communications that has tended to attract less attention in the historiography. Reorganised by Clement Attlee’s post-war Labour governments, this system was presented to the public as a means of disseminating impartial and apparently non-controversial ‘facts’ about government policy. Few commentators today accept that justification, but little is known about why it emerged after the Second World War or what impact it had on existing communications machinery. Taking a broad view of the subject that considers the inter-war and wartime antecedents to the post-war communications system, this paper seeks to fill in some of the gaps that have emerged in the literature. Focusing on shifts in official nomenclature and departmental practice, it explores the relationship propaganda shared to government policy and its broader legacy in the twentieth century.     

British and Irish Conflict Regulation from Sunningdale to Belfast Part I: Tracing the Status of Contesting Sovereigns, 1968–1974

Abstract. This article, which is presented in two parts, analyses the changing conceptions of the status of the two sovereigns (the United Kingdom and the Irish Republic) whose competing claims to sovereignty over Northern Ireland has been the ultimate cause of conflict. In Part I (presented here) I adapt Ian Lustick's theory of state contraction and expansion to the British-Irish relationship as it affected the negotiation of the Sunningdale Power-sharing Agreement of 1973–1974. I argue that the failure to address the competing claims to sovereignty limited the possibilities of achieving and maintaining the consent of sufficient proportions of each ethno-national community. Part I of the article (forthcoming) will extend the analysis to explain the relative equalisation of sovereignty status between Britain and Ireland and presents a modification of a ‘liberal intergovernmentalist’ explanation of the evolution of the Anglo-Irish Agreement (1985) and Belfast Agreement (1998).     

Recovering a ‘Subjugated History’: Disability and the Institution in the Industrial City

The paper explores physically disabled people’s experiences of institutions in the industrial city, focusing on the case of nineteenth-century Melbourne. Here ‘institutions’ refers to the panoply of public, semi-public, private and charitable places that were established in industrial cities to house, and frequently confine, a diverse estate of poor, ill, elderly, disabled and otherwise socially dependent persons. The aim of this paper is to retrace the institutional experiences of disabled people in nineteenth-century Melbourne, with a view to explaining the role of the institution within a broader ‘social space of disability’in the industrial city. In particular, the analysis seeks to identify the type of institutions that disabled people were admitted to, including places of confinement such as gaols. The paper also explores how disabled people coped with the ‘duty to attend the asylum‘ (after Foucault) that weighed heavily on socially marginalised people in the industrial city.     

Infiltration of basinal fluids into high-grade basement, South Norway: sources and behaviour of waters and brines

Quartz veins hosted by the high‐grade crystalline rocks of the Modum complex, Southern Norway, formed when basinal fluids from an overlying Palaeozoic foreland basin infiltrated the basement at temperatures of c. 220°C (higher in the southernmost part of the area). This infiltration resulted in the formation of veins containing both two‐phase and halite‐bearing aqueous fluid inclusions, sometimes with bitumen and hydrocarbon inclusions. Microthermometric results demonstrate a very wide range of salinities of aqueous fluids preserved in these veins, ranging from c. 0 to 40 wt% NaCl equivalent. The range in homogenization temperatures is also very large (99–322°C for the entire dataset) and shows little or no correlation with salinity. A combination of aqueous fluid microthermometry, halogen geochemistry and oxygen isotope studies suggest that fluids from a range of separate aquifers were responsible for the quartz growth, but all have chemistries comparable to sedimentary formation waters. The bulk of the quartz grew from relatively low δ¹⁸O fluids derived directly from the basin or equilibrated in the upper part of the basement (T < 200°C). Nevertheless, some fluids acquired higher salinities due to deep wall‐rock hydration reactions leading to salt saturation at high temperatures (>300°C). The range in fluid inclusion homogenization temperatures and densities, combined with estimates of the ambient temperature of the basement rocks suggests that at different times veins acted as conduits for influx of both hotter and colder fluids, as well as experiencing fluctuations in fluid pressure. This is interpreted to reflect episodic flow linked to seismicity, with hotter dry basement rocks acting as a sink for cooler fluids from the overlying basin, while detailed flow paths reflected local effects of opening and closing of individual fractures as well as reaction with wall rocks. Thermal considerations suggest that the duration of some flow events was very short, possibly in the order of days. As a result of the complex pattern of fracturing and flow in the Modum basement, it was possible for shallow fluids to penetrate basement rocks at significantly higher temperatures, and this demonstrates the potential for hydrolytic weakening of continental crust by sedimentary fluids.     

Oxygen isotope seasonality in a temperate estuarine shell midden: a case study from CA-ALA-17 on the San Francisco Bay,California

Seasonality determination using stable oxygen isotope (δ¹⁸O) analyses in archaeological mollusk shell has been largely limited to aquatic settings where one of the two factors that control shell δ¹⁸O – water δ¹⁸O (or salinity) and temperature – is assumed to be constant. Open coastal marine environments reflect the former situation, and tropical estuaries constitute the latter. In an effort to expand stable isotope seasonality to an ecological setting where neither variable remains constant, we present a model of annual shell δ¹⁸O cycle of aragonite deposition derived from instrumental data on salinity and temperature from San Francisco Bay, California. The predicted range of modeled shell δ¹⁸O is consistent with observed δ¹⁸O values in prehistoric and modern shells when local conditions are considered. Measurements of δ¹⁸O taken at 0 mm and 2 mm from the terminal growth margin were made on 36 archaeological specimens of Macoma nasuta from a late Holocene hunter-gatherer site CA-ALA-17, and season of collection was inferred using the shell δ¹⁸O model. We conclude that shellfish exploitation occurred through the year with the exception of fall, which may indicate scheduling conflicts with acorn harvesting or other seasonally abundant resources elsewhere. The model supports the feasibility of stable isotope seasonality studies in temperate estuaries, provided that instrumental records are available to quantify the relevant water conditions at appropriate spatial and temporal scales.