Materialities of Nostalgia at the Old Homestead

This paper reflects on processes of memory- and history-making at the Elihu Akin House, a historic site in a New England coastal village. Since the late 18th century, the house has been a place of dwelling and deliberate recollection. Recent archaeological excavations, a 1922 silent movie, and an Akin son’s 1778 letter represent multiple media, periods, and perspectives, for which the house serves as a touchstone. These three occasions comprise an archive of nostalgia. Remembrance is repeatedly filtered through and entangled with in-process experiences. The material and emotional are mutually constituted as the house is reinvested with significance. Understanding these processes has implications as the site is developed into a heritage center striving to present not only local and regional history, but also the methods and challenges of heritage management.     

A Comparative Study of the Aquaculture Innovation Systems in Quebec's Coastal Region and Norway

This paper examines the actors and activities and the institutional–spatial dynamics that characterize innovation and knowledge processes within the aquaculture industry and its support organizations in the coastal region of Quebec, Canada. It aims to identify the main features and components of such support organizations and their roles in entrepreneurial and knowledge processes. Comparing this Canadian case with the more developed Norwegian innovation system in aquaculture, the paper concludes that the market possibilities for the products of aquaculture are almost the same in Norway and Quebec. However, it is the policy and institutional settings, as well as the historical trajectories of the respective innovation systems, which seem to explain the growth of the aquaculture industry in Norway and its less successful development in Quebec. The paper also investigates the conditions and institutional arrangements that may stimulate the building and development of a more mature aquaculture innovation system support in Quebec's coastal region.     

‘They never pass me the ball’: exposing ableism through the leisure experiences of disabled children,young people and their families

In this paper, we explore the participation of disabled children, young people and their families in leisure activities. Drawing on the accounts of disabled children, young people, and their parents and careers, we reflect on the leisure spaces that they access and record some of their experiences within them. Using the concept of ‘ableism’ [Campbell, F. K. 2009. Contours of Ableism. Basingstoke: Palgrave Macmillan] we interrogate the data gathered as part of a two-year project funded by the Economic and Social Research Council Does Every Child Matter, post-Blair? The interconnections of disabled childhoods' (RES-062-23-1138). By doing so we identify some of the inherent and embedded discriminations in favour of those children and young people who are perceived to be ‘able’ that simultaneously work to exclude the young ‘kinds of people’ [Hacking, I. 2007. “Kinds of People: Moving Targets.” Proceedings of the British Academy 151: 285–318] categorised as ‘disabled’ and their families from leisure facilities and opportunities. We suggest that currently, disabled families and children occupy a mix of ‘mainstream’, ‘segregated’ and ‘separate’ leisure spaces. We discuss the impact of occupying these spaces and ask what the experiences of accessing leisure by disabled children, young people and their families reveal about the processes and practices of ableism.     

Origin of palaeofluids in a normal fault setting in the Aegean region

The province of Burdur (SW Turkey) is seismically an active region. A structural, geochronological, petrographical, geochemical and fluid inclusion study of extension veins and fault‐related calcite precipitates has been undertaken to reconstruct the palaeofluid flow pattern in this normal fault setting in the Aegean region. A palaeostress analysis and U/Th dating of the precipitates reveals the neotectonic significance of the sampled calcites. Fluid inclusion microthermometry of calcites‐filling extension veins shows final melting temperatures (T_m ice) of 0°C. This indicates pure water, most likely of meteoric origin. The oxygen isotope values (?9.8‰ to ?6.5‰ VPDB) and the carbon isotopic composition (?10.4‰ to ?2.9‰ VPDB) of these calcites also show a near‐surface meteoric origin of the fluid responsible for precipitation. The microstructural characteristics of fault‐related calcites indicate that calcite precipitation was linked with fault activity. Final melting temperature of fault‐related calcites ranges between 0 and ?1.9°C. The oxygen isotope values show a broad range between ?15.0‰ and ?2.2‰ VPDB. Several of these calcites have a δ¹⁸O composition that is higher or lower than the oxygen isotopic composition of meteoric calcites in the area (i.e. between ?10‰ and ?6‰ VPDB). The δ¹³C composition largely falls within the range of the host limestones and reflects a rock‐buffered system. Microthermometry and stable isotopic study indicate a meteoric origin of the fluids with some degree of water–rock interaction or mixing with another fluid. Temperatures deduced from microthermometry and stable isotope analyses indicate precipitation temperatures around 50°C. These higher temperatures and the evidence for water–rock interaction indicate a flow path long enough to equilibrate with the host–rock limestone and to increase the temperature. The combined study of extension vein‐ and fault‐related calcite precipitates enables determining the origin of the fluids responsible for precipitation in a normal fault setting. Meteoric water infiltrated in the limestones to a depth of at least 1 km and underwent water–rock interaction or mixing with a residual fluid. This fluid was, moreover, tapped during fault activity. The extension veins, on the contrary, were passively filled with calcites precipitating from the downwards‐migrating meteoric water.