The European Impact on State–Religion Relations in Turkey: Political Islam,Alevis and Non-Muslim Minorities

Since Turkey's application for membership of the European Union (EU) in 1987, the EU has itself been a structural component of Turkey's political transformation. The European impact intensified after Turkey was granted the status of an official candidate at the EU's Helsinki Summit in 1999. Since then, Turkey has issued a series of reform packages with the aim of starting accession negotiations, which began in October 2005. These reforms have initiated a democratic regime that is structurally different from its predecessors in terms of its definition of political community, national identity and the territorial structure of the state. Among many other aspects of the current political transformation such as the resolution of the Kurdish problem and administrative reform, this article concentrates on how the European impact, which I label Europeanisation, has influenced state–religion relations in Turkey. Europeanisation has three major mechanisms that influence actors, institutions, ideas and interests in varying ways: institutional compliance, changing opportunity structures, and the framing of domestic beliefs and expectations. The article concentrates on how these mechanisms operate in the creation of a new regulatory framework of religion in Turkey.     

Diffuse hydrothermal methane output and evidence of methanotrophic activity within the soils at Sousaki (Greece)

Methane soil flux measurements have been made in 38 sites at the geothermal system of Sousaki (Greece) with the closed chamber method. Fluxes range from ?47.6 to 29 150 mg m^?2 day^?1, and the diffuse CH₄ output of the system has been estimated at 19 t a^?1. Contemporaneous CO₂ flux measurements showed a moderate positive correlation between CO₂ and CH₄ fluxes. Comparison of the CO₂/CH₄ soil flux ratios with the CO₂/CH₄ ratio of the gases of the main gas manifestations provided evidence for methanotrophic activity within the soil. Laboratory CH₄ consumption experiments confirmed the presence of methanotrophic microorganisms in soil samples collected at Sousaki. Consumption was generally in the range from ?4.9 to ?38.9 pmolCH₄ h^?1 g^?1 but could sometimes reach extremely high values (?33 000 pmolCH₄ h^?1 g^?1). These results are consistent with recent studies on other geothermal systems that revealed the existence of thermoacidophilic bacteria exerting methanotrophic activity in hot, acid soils, thereby reducing methane emissions to the atmosphere.     

TRANSPORT AND SUBSISTENCE PATTERNS AT THE TRANSITION TO PASTORALISM,KOOBI FORA,KENYA

The Turkana Basin in Kenya has an extensive record of Holocene activities relating to mobility and economy of foraging and herding communities. Obsidian is only known from a few key localities in northern Kenya. As such, the use of obsidian as a toolstone material, commonly used during the mid‐Holocene, provides one way to trace exchange, interaction and population movements during the transition to pastoralism. We employ X‐ray fluorescence to characterize obsidian artefacts from four Pastoral Neolithic assemblages. Data reveal a highly mobile and diversified population that used watercraft to access and transport obsidian resources. Specifically, the use of the North Island obsidian source in Lake Turkana indicates that boat use was significant during this transitional period. The incorporation of watercraft transport and aquatic resources in our analyses of Pastoral Neolithic sites affords a greater understanding of subsistence, mobility and economy in this important period in East African prehistory.     

What Does the Somali Experience Teach Us about the Social Contract and the State?

Since 1991 the international system has struggled and failed to recreate a state on the territory of the former Somalia. Proto‐state systems have been formed by Somalis themselves in Somaliland and Puntland and alternative forms of governance and order exist in other parts of Somalia, but none enjoys international recognition. The polities of Somalia offer important lessons concerning our general theories about social contract, the role that states play in creating wealth, indigenous systems of governance, and the failure of existing international approaches to state reconstruction. Contemporary Somali politics is re‐explored here to extract these lessons. The article explores the assumptions embedded in the works of the classic Western social contract theorists in the light of Somali experience in order to show that the underlying conceptual structure of international state reconstruction work needs to be rethought. We conclude that it frequently is better to allow for bottom‐up, organic, disjointed negotiation of indigenous governance solutions (even though they probably will not conform to Western ideas of liberal democracy) than for the international system to impose top‐down answers. The former more closely tracks the history of state formation in Europe and the latter is troubled by the inconsistent and not necessarily benign interests of the international actors involved. Indigenous, local political systems are changed by the stresses of violent conflict, so prompt action to employ them in a post‐conflict situation is indicated.     

Frozen Film and FOSDIC Forms: Restoring the 1960 U.S. Census of Population and Housing

In this article, the authors describe a collaboration of the Minnesota Population Center (MPC), the U.S. Census Bureau, and the National Archives and Records Administration to restore the lost data from the 1960 Census. The data survived on refrigerated microfilm in a cave in Lenexa, Kansas. The MPC is now converting the data to usable form. Once the restored data are processed, the authors intend to develop three new data sources based on the 1960 census. These data will replace the most inadequate sample in the series of public-use census microdata spanning the years from 1850 to 2000, extend the chronological scope of the public census summary files, and provide a powerful new resource for the Census Bureau and its Research Data Centers.     

An archaeologically validated protocol for computing obsidian hydration rates from laboratory data

This paper reports the computation of hydration rate for Topaz Mountain obsidian from laboratory data, and a comparison with archaeological data from a well-dated site, Camels Back Cave, in western Utah. Topaz Mountain obsidian is found to be slow-hydrating, with a rate of 0.071 ± 0.021 μ/yr^½ at an effective hydration temperature of 16.01 °C. This rate agrees with a rate developed from archaeological data from Camels Back Cave within ∼6%. Activation energy of Topaz Mountain obsidian is 10370 ± 544 K, and its diffusion constant is (1.87 ± 9.13) × 10¹³ μ²/yr, both of which are independent of temperature. Its intra-source variability in hydration rate is very low (CV < 0.01), implying a low variability in intrinsic water. We present a model of chemical erosion which shows why earlier laboratory-determined rates were incorrect, and discuss the implications of our findings on the determination of experimentally derived rates in obsidian hydration dating.     

The Scaling of Sustainable Urban Form: A Case of Scale-related Issues and Sustainable Planning in Malmö, Sweden

In this article, I investigate “spatial scale” as an aspect that needs to be more carefully addressed in the discussion and planning of “sustainable urban forms”. Focusing on the Malmö–Lund region in Sweden, I discuss problems of scale as related to the new take on sustainability in Malmö planning documents, especially the update of the Malmö comprehensive plan from 2005. The article is divided into three sections. First, I discuss the concept and problem of spatial scale, contextualizing it in theory as well as in recent discussions on urban transformations. Second, I briefly discuss the discourse of sustainable urban forms, pointing out some scale-related issues that need to be more carefully addressed. In the third and main section of the article, I investigate plans and projects for urban development in Malmö, focusing and elaborating on spatial scale and discussing the findings in terms of three kinds of scale stabilization: in terms of territory, size and hierarchy. The article concludes with a call for further work for the possibilities of a more dynamic and multi-scalar approach in urban planning.