European Policy and the Regions: A Review and Analysis of Tensions

This article explores a series of tensions inherent in the series of European policies that are designed to improve the competitiveness of regions in the face of globalization. Its focus is the co-existence of interventionist policies intended to overcome problems of lagging regions such as cohesion policies and those, for example competition policy which are designed to remove barriers to market integration and that are anti-interventionist. Moreover, the changing relationship between the European Union (EU), member states and the regions and problems of how regions are defined complicate policy implementation. To review these issues, the article adopts an agent-centred approach to understanding economic behaviour in the face of globalization in particular geographical and sectoral contexts. This methodology is used to highlight five sources of tension relating to the reality of the experience of globalization. These are illustrated by evidence from a recently completed EU Fifth Framework Programme study of regional adjustment strategies and technological change in five European countries.     

INNER-CITY REAL ESTATE ACTIVITY IN MONTREAL: INSTITUTIONAL CHARACTERISTICS OF DECLINE

Inner-city housing decline is reviewed in terms of neo-classical and Marxist theory. The latter is tested in two empirical studies. First, housing transactions in an inner-city district of Montreal are compared with the city as a whole for 1966-1974. Second, three contrasting sub-markets are compared with respect to mortgage arrangements and property tax for the years 1966 and 1974. It is concluded that Marxist theory provides a valuable interpretation of inner-city decline which is complementary to neo-classical analysis. However, the variables explored give only partial insight into the Marxist perspective.
Les raisons pour la détérioration du marché immobilier des quartiers populaires sont considérées des points de vue néo-classique et marxiste. La théorie marxiste est vérifiée en deux analyses empiriques. d'abordabord il y a un examen des transactions dans le secteur de l'habitation d'abordun quartier populaire de Montréal par rapport aux transactions dans le reste de la ville pendant les années 1966-1974. Deuxièmement, les hypothèques et la taxe foncière sont compareées dans trois sous-marchés en 1966 et en 1974. l'étude conclut que la théorie marxiste ajoute un aperçu complémentaire à l'analyse néoclassique dans l'explication du déclin des quartiers populaires. Toutefois les variables utilisées dans cette étude ne donnent qu'une connaissance partielle de la perspective marxiste.     

NEW EVIDENCE FOR IRON AGE BURIAL AND PROPITIATION PRACTICES IN SOUTHERN BRITAIN

It has been 30 years since the first scheme that categorized fragmentary Iron Age human remains in southern Britain ( Wilson 1981 ), and nearly 20 years since Cunliffe's paper ‘Pits, Preconceptions and Propitiation’ was published ( Cunliffe 1992 ). This study integrates the osteological, forensic and field evidence to identify archaeological signatures from three interrelated areas. The results show different depositional trends for five sites in Hampshire, and that the hillforts studied – Danebury (Hampshire) and Maiden Castle (Dorset) – demonstrate yet another pattern. Three main depositional practices were observed; intentional exposure, propitiatory deposits, and intentional practices, in which the body was kept whole in death, ran in parallel with each another.     

Constraining the rate and extent of mantle serpentinization from seismic and petrological data: implications for chemosynthesis and tectonic processes

We used seismic velocity as a proxy for serpentinization of the mantle, which occurred beneath thinned but laterally continuous continental crust during continental break up, prior to opening of the Atlantic Ocean. The serpentinized sub‐continental mantle is now exhumed, beneath the Iberia Abyssal Plain and was accessed by scientific drilling on Ocean Drilling Program legs 149 and 173. Chromatographic modelling of kinetically limited transport of the serpentinization front yields a front displacement of 2197 ± 89 m, a time‐integrated fluid flux of 1098 ± 45 m³ m^?2 and a Damköhler number of 6.0 ± 0.2. Whether either surface reaction or chemical transport limit the rate of reaction, we calculate timescales for serpentinization of approximately 10⁵–10⁶ years. This yields time‐average fluid flux rates for H₂O, entering and reacting with the mantle, of 60–600 mol m^?2 a^?1 and for CH₄, produced as a by‐product of oxidation of Fe⁺⁺ to magnetite and exiting the mantle, of 0.55–5.5 mol m^?2 a^?1. This equates to a CH₄‐flux of 0.18–1.8 Tg a^?1 for coeval serpentinization of the mantle that was exhumed west of Iberia. This represents 0.03–0.3% of the present‐day annual CH₄‐flux from all sources and a higher fraction of pre‐anthropogenic (lower) CH₄ levels. CH₄ released by serpentinization at or beneath the seafloor could provide substrate for biological chemosynthesis and/or promote gas‐hydrate formation. Finally, noting its volumetric extent and rapidity (<10⁶ years), we interpret serpentinization to be a reckonable component of tectonic processes, contributing both diapiric and expansional forces and helping to ‘lubricate’ extensional processes. Given its anisotropic permeability, actively deforming serpentinite might impede melt migration which may be of interest, given the apparent lack of melt in some rifted margins.     

Spatial coupling between spilitization and carbonation of basaltic sills in SW Scottish Highlands: evidence of a mineralogical control of metamorphic fluid flow

In a geochemical and petrological analysis of overprinting episodes of fluid–rock interaction in a well‐studied metabasaltic sill in the SW Scottish Highlands, we show that syn‐deformational access of metamorphic fluids and consequent fluid–rock interaction is at least in part controlled by preexisting mineralogical variations. Lithological and structural channelling of metamorphic fluids along the axis of the Ardrishaig Anticline, SW Scottish Highlands, caused carbonation of metabasaltic sills hosted by metasedimentary rocks of the Argyll Group in the Dalradian Supergroup. Analysis of chemical and mineralogical variability across a metabasaltic sill at Port Cill Maluaig shows that carbonation at greenschist to epidote–amphibolites facies conditions caused by infiltration of H₂O‐CO₂ fluids was controlled by mineralogical variations, which were present before carbonation occurred. This variability probably reflects chemical and mineralogical changes imparted on the sill during premetamorphic spilitization. Calculation of precarbonation mineral modes reveals heterogeneous spatial distributions of epidote, amphibole, chlorite and epidote. This reflects both premetamorphic spilitization and prograde greenschist facies metamorphism prior to fluid flow. Spilitization caused albitization of primary plagioclase and spatially heterogeneous growth of epidote ± calcic amphibole ± chlorite ± quartz ± calcite. Greenschist facies metamorphism caused breakdown of primary pyroxene and continued, but spatially more homogeneous, growth of amphibole + chlorite ± quartz. These processes formed diffuse epidote‐rich patches or semi‐continuous layers. These might represent precursors of epidote segregations, which are better developed elsewhere in the SW Scottish Highlands. Chemical and field analyses of epidote reveal the evidence of local volume fluctuations associated with these concentrations of epidote. Transient permeability enhancement associated with these changes may have permitted higher fluid fluxes and therefore more extensive carbonation. This deflected metamorphic fluid such that its flow direction became more layer parallel, limiting propagation of the reaction front into the sill interior.     

Australia's Indigenous Carbon Economy: A National Snapshot

Many Indigenous communities in Australia are well situated to provide greenhouse gas abatement and carbon sequestration benefits, but little is known about the factors affecting the capability of Australia's Indigenous organisations to participate in climate change mitigation strategies. This paper provides a ‘snapshot’ summary of certain aspects of Australia's Indigenous organisations' participation in carbon offset schemes. The snapshot provides insight into the degree to which Indigenous organisations are aware of carbon market opportunities in Australia, the level that these Indigenous organisations participate in or engage with carbon‐based economic enterprises, and the key pathways through which Indigenous carbon market opportunities are pursued. Analysis of data collected from a national survey conducted between 2011 and 2012 show that most obstacles to Indigenous participation in carbon offset schemes relate to land tenure arrangements; geographic and biophysical factors; low levels of requisite technical, human and financial resources; and appropriate recognition of Indigenous knowledge and cultural responsibilities. The snapshot also highlights the value of supporting regionally specific capacity‐building strategies to enable Indigenous people to participate in emerging carbon offset activities and the generation of associated ecosystem services. Cultural, socio‐economic or demographic factors that are also likely to influence the ability of many Indigenous communities to participate in carbon market opportunities are identified as important areas for further research.     

Heading west? Georgia's Euro‐Atlantic path

Events in Ukraine in 2014 are likely to transform the presence and role of western institutions such as NATO in the post‐Soviet area. The crisis has starkly revealed the limits of their influence within Russia's ‘zone of privileged interest’, as well as the lack of internal unity within these organizations vis‐à‐vis relations with Moscow and future engagement with the area. This will have long‐term implications for the South Caucasus state of Georgia, whose desire for integration into the Euro‐Atlantic community remains a key priority for its foreign and security policy‐makers. This article examines the main motivators behind Georgia's Euro‐Atlantic path and its foreign policy stance, which has remained unchanged for over a decade despite intense pressure from Russia. It focuses on two aspects of Georgia's desire for integration with European and Euro‐Atlantic structures: its desire for security and the belief that only a western alignment can guarantee its future development, and the notion of Georgia's ‘European’ identity. The notion of ‘returning’ to Europe and the West has become a common theme in Georgian political and popular discourse, reflecting the belief of many in the country that they are ‘European’. This article explores this national strategic narrative and argues that the prevailing belief in a European identity facilitates, rather than supersedes, the central role of national interests in Georgian foreign policy.     

The timescale and mechanisms of fault sealing and water‐rock interaction after an earthquake

Hydrogeochemical monitoring of a basalt‐hosted aquifer, which contains Ice Age meteoric water and is situated at 1220 m below sea level in the Tjörnes Fracture Zone, northern Iceland, has been ongoing since July 2002. Based on hydrogeochemical changes following an earthquake of magnitude (M_w) 5.8 on 16 September 2002, we constrained the timescales of post‐seismic fault sealing and water–rock interaction. We interpret that the earthquake ruptured a hydrological barrier, permitting a rapid influx of chemically and isotopically distinct Ice Age meteoric water from a second aquifer. During the two subsequent years, we monitored a chemical and isotopic recovery towards pre‐earthquake aquifer compositions, which we interpret to have been mainly facilitated by fault‐sealing processes. This recovery was interrupted in November 2004 by a second rupturing event, which was probably induced by two minor earthquakes and which reopened the pathway to the second aquifer. We conclude that the timescale of fault sealing was approximately 2 years and that the approach to isotopic equilibrium (from global meteoric water line) was approximately 18% after >10⁴ years.     

Isotopic and petrological evidence of fluid–rock interaction at a Tethyan ocean–continent transition in the Alps: implications for tectonic processes and carbon transfer during early ocean formation

We report overprinting stable isotope evidence of fluid–rock interaction below two detachment faults along which mantle rocks were exhumed to the seafloor, between the respective landward and seaward limits of oceanic and continental crust, at a Tethyan ocean–continent transition (OCT). This OCT, which is presently exposed in the Tasna nappe (south‐eastern Switzerland) is considered an on‐land analogue of the well‐studied Iberian OCT. We compare our results with the fault architecture (fault core–damage zone–protolith) described by Caine et al. [Geology (1996) Vol. 24, pp. 1025–1028]. We confirm the existence of a sharp boundary between the fault core and damage zone based on isotopic data, but the boundary between the damage zone and protolith is gradational. We identify evidence for: (1) pervasive isotopic modification to 8.4 ± 0.1‰ which accompanied or post‐dated serpentinization of these mantle rocks at an estimated temperature of 67–109°C, (2) either (i) partial isolation of some highly strained regions [fault core(s) and mylonite] from this pervasive isotopic modification, because of permeability reduction (Caine et al.) or (ii) subsequent isotopic modification caused by structurally channelled flow of warm fluids within these highly strained regions, because of permeability enhancement, and (3) isotopic modification, which is associated with extensive calcification at T = 54–100°C, primarily beneath the younger of the two detachment faults and post‐dating initial serpentinization. By comparing the volumetric extent of calcification with an experimentally verified model for calcite precipitation in veins, we conclude that calcification could have occurred in response to seawater infiltration, with a calculated flux rate of 0.1–0.2 m year^?1 and a minimum duration of 0.2–4.0 × 10⁴ years. The associated time‐averaged uptake flux of carbon during this period was 8–120 mol m^?2 year^?1. By comparison with the estimated area of exhumed mantle rocks at the Iberian OCT, we calculate a maximum annual uptake flux for carbon of 2–30 Tg year^?1. This is an order of magnitude greater than that for carbon exchange at the mid‐ocean ridges and 0.1–1.4% of the global oceanic uptake flux for carbon.