Creative industries in a European Capital of Culture

This article examines the articulation of the benefits associated with staging the European Capital of Culture (ECoC) in Liverpool, England in 2008. It is argued that relevant policy documents, and policy discourses more generally, propose a strong influential role for the operations of the ECoC upon the creative industries. Such a strong relationship, however, is difficult to evidence either at a discursive level or from the attitudes expressed by those working within the creative industries locally. The idea that the ECoC can promote broadly ‘creative’ activity is thus posited as being merely one aspect of the ECoC’s major goal of attempted city rebranding, rather than anything more substantive; nevertheless the articulation of ‘success’ of the ECoC in this regard seems entrenched.     

Reflections of a London-Irish musician: an interview with Cáit O'Riordan

The second-generation Irish have played a major role in the history of popular music in Britain. The significance of Irish ethnicity in the lives and work of these musicians has recently been addressed. However, scant attention has been paid to issues of gender amongst this generation of musicians, and the role of female musicians has been largely overlooked. This essay seeks to address this issue, via an interview with Cáit O'Riordan, the former bass guitarist (and occasional vocalist) in The Pogues. The article suggests that the voice of O'Riordan might serve as a useful starting point in addressing the role of female musicians amongst the Irish diaspora in Britain.     

The International Lenin School: A Response to Cohen and Morgan

This paper challenges the methods and conclusions of an articleon British students at the International Lenin School by GidonCohen and Kevin Morgan published in a recent issue of TwentiethCentury British History. It questions their model of relationsbetween the Comintern and its national affiliates, and theirassertion of the prominence and total nature of the Lenin Schoolas a control mechanism of the former over the latter. Afterdemonstrating the inadequacy of their data and methodology,it indicates significant deficiencies and omissions in theirhandling of qualitative evidence relevant to the influence ofthe school on its students. It concludes by showing that theauthors underestimate the scale and duration of the impact ofthe school's graduates upon the apparatus of the Communist Partyof Great Britain.     

Conservation Narratives in Costa Rica: Conflict and Co‐existence

This article examines narratives about nature conservation in Costa Rica, specifically those related to wildlife and biodiversity, and their evolution with the growth of tourism and bioprospecting industries. It outlines a traditional conservation narrative and two streams of an emerging counter‐narrative, and discusses problems and prospects for each in contemporary Costa Rica. The use of narrative and counter‐narrative follows Roe (1991, 1995), Fairhead and Leach (1995), and Leach and Mearns (1996). The article focuses particularly on the ways in which the narratives are increasingly drawing on, informing, and sometimes conflicting with one another; it is based on the author’s research undertaken in various protected areas in Costa Rica since 1994 and on research published by others.     

Ancient hydrocarbon seeps from the Mesozoic convergent margin of California: carbonate geochemistry, fluids and palaeoenvironments

More than a dozen hydrocarbon seep‐carbonate occurrences in late Jurassic to late Cretaceous forearc and accretionary prism strata, western California, accumulated in turbidite/fault‐hosted or serpentine diapir‐related settings. Three sites, Paskenta, Cold Fork of Cottonwood Creek and Wilbur Springs, were analyzed for their petrographic, geochemical and palaeoecological attributes, and each showed a three‐stage development that recorded the evolution of fluids through reducing–oxidizing–reducing conditions. The first stage constituted diffusive, reduced fluid seepage (CH₄, H₂S) through seafloor sediments, as indicated by Fe‐rich detrital micrite, corroded surfaces encrusted with framboidal pyrite, anhedral yellow calcite and negative cement stable isotopic signatures (δ¹³C as low as ?35.5‰ PDB; δ¹⁸O as low as ?10.8‰ PDB). Mega‐invertebrates, adapted to reduced conditions and/or bacterial chemosymbiosis, colonized the sites during this earliest period of fluid seepage. A second, early stage of centralized venting at the seafloor followed, which was coincident with hydrocarbon migration, as evidenced by nonluminescent fibrous cements with δ¹³C values as low as ?43.7‰ PDB, elevated δ¹⁸O (up to +2.3‰ PDB), petroleum inclusions, marine borings and lack of pyrite. Throughout these early phases of hydrocarbon seepage, microbial sediments were preserved as layered and clotted, nondetrital micrites. A final late‐stage of development marked a return to reducing conditions during burial diagenesis, as implied by pore‐associated Mn‐rich cement phases with bright cathodoluminescent patterns, and negative δ¹⁸O signatures (as low as ?14‰ PDB). These recurring patterns among sites highlight similarities in the hydrogeological evolution of the Mesozoic convergent margin of California, which influenced local geochemical conditions and organism responses. A comparison of stable carbon and oxygen isotopic data for 33 globally distributed seep‐carbonates, ranging in age from Devonian to Recent, delineated three groupings that reflect variable fluid input, different tectono‐sedimentary regimes and time–temperature‐dependent burial diagenesis.     

Vegetation history at the multi-period prehistoric complex at Ballynahatty,Co. Down,Northern Ireland

Palaeoecological methods can provide an environmental context for archaeological sites, enabling the nature of past human activity to be explored from an indirect but alternative perspective. Through a palynological study of a small fen peatland located within the catchment of a multi-period prehistoric complex at Ballynahatty, Co. Down, Northern Ireland, we reconstruct the vegetation history of the area during the early prehistoric period. The pollen record reveals tentative evidence for Mesolithic activity in the area at 6410–6220 cal BC, with woodland disturbance identified during the Mesolithic–Neolithic transitional period ca. 4430–3890 cal BC. A more significant impact on the landscape is observed in the Early Neolithic from 3950 to 3700 cal BC, with an opening up of the forest and the establishment of a mixed agricultural economy. This activity precedes and continues to be evident through the Mid-Neolithic during which megalithic tombs and related burial sites were constructed at Ballynahatty. Due to chronological uncertainties and a possible hiatus in peat accumulation in the fen, the contemporary environment of the Ballynahatty timber circle complex (constructed and used ca. 3080–2490 cal BC) and henge (dating to the third millennium cal BC) cannot certainly be established. Nevertheless, the pollen record suggests that the landscape remained open through to the Bronze Age, implying a long continuity of human activity in the area. These findings support the idea that the Ballynahatty prehistoric complex was the product of a gradual and repeated restructuring of the ritual and ceremonial landscape whose significance continued to be recognised throughout the early prehistoric period.