Processes and patterns of migration on a global scale have changed in profound ways during the last two decades (Smith and King, 2012). In the European context, this is exemplified by transformations to the traditional mobility patterns from East to West Europe (Koser and Lutz, 1998), with migrants more likely to be involved in temporary circular and transnational mobility (Favell, 2008). Since the end of the Second World War, historical and political events in Europe have facilitated the mobility of ethnic Germans from Eastern Europe to Germany. Subsequently, the fall of the Iron Curtain has permitted unrestrained East-West movements, which resulted in mass migrations towards the West and diaspora fragments in the East. However, after settlement in the West, ethnic Germans have also been absorbed within wider temporary and transnational movements (Koser, 2007). Within this context, this thesis examines the post-migratory lives of three generations of Transylvanian Saxons in Germany by exploring the cultural, social, economic and political dimensions of this community. This thesis aims to contribute to on-going academic debates about diasporas by explicitly responding to Hoerder s (2002) call for more studies on ethnic German diasporas. It shows that Transylvanian Saxons, who relocated to the ancestral homeland, do not disrupt identities and lives forged in diaspora, but rather, they negotiate complex identities and belongings in relation to both home and homeland . It reveals a double diaspora and the necessity to perceive identity and diaspora as dynamic processes and constantly evolving in relation to time, space and place. This double diasporic allegiance in the case of the Transylvanian Saxons suggests interrogating the formation of a return diaspora and its importance for processes of international migration.

In response to shifting borders and radical changes in political and economic regimes, a great number of Hungarian Romanians left their homeland in the last century. Drawing on ethnographic fieldwork in a Hungarian village in Romania, in this thesis I argue that the growing uncertainty in villagers’ working lives, a result of the high unemployment accompanying post-socialist transformation, and ethnic and class based disadvantage in Romania, impels them to engage in pluriactivity in their livelihood strategies. This includes circular labour migration in Hungary and other European Union states. Economic inequalities within the expanded EU create an ethnically segmented labour market, in which working class Transylvanian Hungarians become associated with certain types of work, in this case, temporary and often undocumented jobs in the least desirable sectors of the economy.

Current Cultural Situation of Transylvanian Saxons in Romania PhDr. Tomáš Drs Abstract The thesis deals with the current situation of the Transylvanian Saxons in Romania. Based on multiple field visits, it describes and analyzes the problems related to reconstructing the ethnic identity of the community, noting the minority's transnational situation and exploring the generational relations, the minority's position in the ethnically different environment or its political and revitalization activities. The thesis also attemps to reconstruct the actual historical development, looks into how memory is socially conditioned memory and lays out biographies of individual characters. Methodologically, the thesis draws upon the tradition of ethnographic research, working with theoretical concepts of ethnicity (Eriksen, Anderson), transnationalism (Werbner, Szaló) or memory studies (Halbwachs, Assmann, Nora). The aim of the thesis is to introduce the Transylvanian Saxons and other groups commonly referred to as Romanian Germans in the Czech environment. It lays out the history of Transylvanian Saxons, describes their negotiations with the state and the framing of their minority identity. Also, it seeks to answer whether the end of the numerically smaller ethnic minority of Transylvanian Saxons is inevitable and how...

This thesis is an exploration of liberalism in Romania and in anthropology. Liberalism is frequently represented in contemporary anthropology as a hegemonic technocratic practice, rationalist ideology and hypocritically exclusionary politics. I challenge this representation through an ethnography of a British-Romanian rural revitalisation and conservation programme in the Saxon villages region of southern Transylvania, Romania, and the vernacular liberalism of the cosmopolitan youth who have taken this project up. Douglas Holmes has asserted that in the European Union (EU) in the twenty-first century, communities and people are experimenting with new identity projects that fuse the liberal and illiberal in innovative ways. I trace how the rural revitalisation programme brought together romantic, "integralist" visions of the Saxon villages with the EU's liberal technologies of governance to create a set of projects the value of which could be translated between diverse sets of actors, from British tourists through European bureaucrats and Transylvanian farmers. This provided local youth with the possibility of making a life in their home region in a context of significant economic decline and massive emigration. The seemingly disparate liberal and romantic elements, initially brought together in a transnational context, were "domesticated" by Transylvanian liberals as complementary resources that could be mobilised to combat entrenched problems of Romanian society and modernity, as liberals saw it, notably the failure of the state to provide key services and the stagnation of the public sphere. The state's failures had led liberals to abandon it is a source of hope, turning instead to voluntary action, which made the dilemmas of how to mobilise engaged publics all the more crucial. Village liberals' attempts to foster such publics frequently ended up reproducing their own marginality, however. Against conventional representations of liberalism, I argue that its technocratic pretensions can be an object of hope in a milieu where expertise is perceived to be absent as much as an institutional hegemony. I further conclude that the multiple ways in which the liberal and the romantic are combined challenges dominant images of liberal ideology and practice as purely abstract and formal.

Ce travail retrace l’évolution varisque des Massifs d’Almǎj (Roumanie), de Deli Jovan (Serbie) et de la Stara Planina Occidentale (Bulgarie), à travers une étude pétrostructurale effectuée sur les différentes unités lithologiques de la Nappe alpine du Danubien supérieur. Cette nappe possède la particularité de contenir un marqueur de convergence de toute première importance sous la forme de 4 massifs ophiolitiques démembrés lors de l’orogenèse alpine :Tisoviţa Iuţi (TI, Roumanie), Deli Jovan (DJ, Serbie), Zaglavak (Z, Serbie) et Tcherni Vrah (TV, Bulgarie). Les études pétrologiques de terrain effectuées dans ces trois pays ont permis de confirmer la continuité entre ces 4 massifs, qui, séparément, comprennent chacun une portion de croûte océanique différente (TI :section mantélique et cumulats inférieurs, DJ :cumulats inférieurs et supérieurs, Z :cumulats supérieurs, TV :cumulats supérieurs et section effusive), mais considérés ensemble, forment une pile ophiolitique classique complète. De nouvelles datations par la méthode 147Sm-143Nd confirment un âge d’accrétion pour cette croûte océanique au Dévonien inférieur (~ 400 Ma). Cependant, l’essentiel de ce mémoire concerne les Monts Almǎj, notamment les roches encaissantes du massif de Tisoviţa Iuţi. La partie sud de ce massif ophiolitique représente la section inférieure d’une croûte océanique classique, alors que sa partie orientale est caractérisée par des roches de la croûte océanique supérieure, fortement déformées et transformées (métagabbros à zoïsite et fuchsite). Ces roches font partie de la Zone Mylonitique de Corbu (CMZ), qui comporte également des métasédiments à Gt ± St ± And et des serpentinites. Les conditions PT de formation de ces métagabbros, datés à 380-360 Ma par la méthode 40Ar-39Ar, ont été estimées à des températures comprises entre 450°C et 300°C. Leur contexte de formation peut être assimilé à une semelle ophiolitique ‘froide’, développée lors d’une obduction intra-océanique initiée probablement le long d’une faille transformante. Si le pic de métamorphisme des roches de Corbu a été estimé à 585°C/ 5.5 kbar, leur exhumation pourrait s’effectuer au sein d’un anticlinal en régime transpressif sénestre, en relation avec la formation de la CMZ, interprétée comme une ancienne zone plissée qui évolue en zone de cisaillement sénestre. Au Carbonifère, le granite syntectonique de Cherbelezu se met en place le long de la CMZ et enregistre les dernières phases de cette déformation lors de son refroidissement. Les études préliminaires sur les roches encaissantes des massifs ophiolitiques en Serbie et Bulgarie permettent de préciser une vergence d’obduction du lambeau ophiolitique vers le paléo-NW et d’établir un modèle de reconstitution paléogéodynamique au Varisque pour l’ensemble de la région étudiée./ This study provides new information on the Variscan evolution of the Almǎj Mountains (Romania), Deli Jovan Massif (Serbia) and Western Stara Planina (Bulgaria), throughout a petrostructural investigation conducted on the various lithological units of the Upper Danubian Alpine Nappe. This nappe displays an important convergence tectonic marker in the form of four ophiolitic massifs dismembered during the Alpine orogeny: Tisoviţa Iuţi (TI, Romania), Deli Jovan (DJ, Serbia), Zaglavak (Z, Serbia) and Tcherni Vrah (TV, Bulgaria). Our petrological studies in these three countries have confirmed the continuity between these four massifs, each of which showing, separately, a different portion of the oceanic crust (TI: mantle section and lower cumulates, DJ: lower and upper cumulates, Z: upper cumulates, TV: upper cumulates and effusive section), but taken together, forming a complete classical ophiolitic pile. New dating using the 147Sm-143Nd method has confirmed an accretion age for this oceanic crust at around 400 Ma (Early Devonian). However, the main part of this study has been focused in the Almǎj Mountains, particularly the Tisoviţa Iuţi ophiolitic massif and its enclosing rocks. The Southern part of this ophiolitic massif represents the lower section of a classical oceanic crust whereas its eastern part is characterized by upper crustal oceanic rocks that are highly deformed and transformed (zoïsite and fuchsite-bearing metagabbros). These rocks belong to the Corbu Mylonitic zone (CMZ), which also comprises Gt ± St ± And metasediments and serpentinites. Temperature estimates for the formation of the metagabbros are bracketed between 450°C and 300°C and these rocks have been dated at 380-360 Ma using the 40Ar-39Ar method on fuchiste. The geodynamic context for their formation can be viewed as a ‘cold’ ophiolitic sole, developed during an intra-oceanic obduction probably initiated along transform fault. If the metamorphic peak for the Corbu rocks has been estimated at 585°C/5.5kbar, their rapid exhumation could be realized via an anticline under a transpressive sinistral regime, connected with the formation of the CMZ that is interpreted as an ancient fold zone evolving in a sinistral shear zone. Finally, the Carboniferous syntectonic Cherbelezu granite intrudes along the CMZ and records the final stages of this deformation during its cooling. Preliminary investigations on the enclosing rocks of the ophiolitic massifs in Serbia and Bulgaria allow us to define a top to the NW obduction vergence for the ophiolite and to propose a paleogeodynamic reconstitution model for the Carpathian/Balkans terrains in the Variscan times. / Doctorat en Sciences / info:eu-repo/semantics/nonPublished