@misc{Entrich2013,
  author    = {Entrich, Steve R.},
  title     = {Education and equal opportunity in Japan. Asia Pacific Studies, v. 4.},
  series = {Pacific affairs},
  volume    = {86},
  journal   = {Pacific affairs},
  number    = {2},
  publisher = {University of British Columbia},
  address   = {Vancouver},
  issn      = {0030-851X},
  pages     = {411 -- 413},
  year      = {2013},
  language  = {en}
}
@misc{Fischer2013,
  author    = {Fischer, Stefanie},
  title     = {Doron Rabinovici, Eichmann's Jews - the jewish administration of holocaust Vienna 1938-1945},
  series = {East European Jewish affairs},
  volume    = {43},
  journal   = {East European Jewish affairs},
  number    = {3},
  publisher = {Routledge, Taylor \& Francis Group},
  address   = {Abingdon},
  issn      = {1350-1674},
  doi       = {10.1080/13501674.2013.872438},
  pages     = {354 -- 357},
  year      = {2013},
  language  = {en}
}
@misc{Sorge2013,
  author    = {Sorge, Arndt},
  title     = {Disintegrating Democracy at Work: Labor Unions and the Future of Good Jobs in the Service Economy},
  series = {British journal of industrial relations : an international journal of employment relations},
  volume    = {51},
  journal   = {British journal of industrial relations : an international journal of employment relations},
  number    = {1},
  publisher = {Wiley-Blackwell},
  address   = {Hoboken},
  issn      = {0007-1080},
  doi       = {10.1177/0094306113514539i},
  pages     = {2},
  year      = {2013},
  language  = {en}
}
@misc{DittmannThuenemannFewerNeilan2013,
  author    = {Dittmann-Th{\"u}nemann, Elke and Fewer, David P. and Neilan, Brett A.},
  title     = {Cyanobacterial toxins biosynthetic routes and evolutionary roots},
  series = {FEMS microbiology reviews},
  volume    = {37},
  journal   = {FEMS microbiology reviews},
  number    = {1},
  publisher = {Wiley-Blackwell},
  address   = {Hoboken},
  issn      = {0168-6445},
  doi       = {10.1111/j.1574-6976.2012.12000.x},
  pages     = {23 -- 43},
  year      = {2013},
  abstract  = {Cyanobacteria produce an unparalleled variety of toxins that can cause severe health problems or even death in humans, and wild or domestic animals. In the last decade, biosynthetic pathways have been assigned to the majority of the known toxin families. This review summarizes current knowledge about the enzymatic basis for the production of the hepatotoxins microcystin and nodularin, the cytotoxin cylindrospermopsin, the neurotoxins anatoxin and saxitoxin, and the dermatotoxin lyngbyatoxin. Elucidation of the biosynthetic pathways of the toxins has paved the way for the development of molecular techniques for the detection and quantification of the producing cyanobacteria in different environments. Phylogenetic analyses of related clusters from a large number of strains has also allowed for the reconstruction of the evolutionary scenarios that have led to the emergence, diversification, and loss of such gene clusters in different strains and genera of cyanobacteria. Advances in the understanding of toxin biosynthesis and evolution have provided new methods for drinking-water quality control and may inspire the development of techniques for the management of bloom formation in the future.},
  language  = {en}
}
@misc{Haussig2013,
  author    = {Haußig, Hans-Michael},
  title     = {Ben-Yehuda, N., Theocratic democracy, the social construction of religious and secular extremism; Univ. Press, Oxford, 2010},
  issn      = {1614-6492},
  year      = {2013},
  language  = {en}
}
@misc{JolivetFaccennaHuetetal.2013,
  author    = {Jolivet, Laurent and Faccenna, Claudio and Huet, Benjamin and Labrousse, Loic and Le Pourhiet, Laetitia and Lacombe, Olivier and Lecomte, Emmanuel and Burov, Evguenii and Denele, Yoann and Brun, Jean-Pierre and Philippon, Melody and Paul, Anne and Salaue, Gwenaelle and Karabulut, Hayrullah and Piromallo, Claudia and Monie, Patrick and Gueydan, Frederic and Okay, Aral I. and Oberh{\"a}nsli, Roland and Pourteau, Amaury and Augier, Romain and Gadenne, Leslie and Driussi, Olivier},
  title     = {Aegean tectonics strain localisation, slab tearing and trench retreat},
  series = {Tectonophysics : international journal of geotectonics and the geology and physics of the interior of the earth},
  volume    = {597},
  journal   = {Tectonophysics : international journal of geotectonics and the geology and physics of the interior of the earth},
  publisher = {Elsevier},
  address   = {Amsterdam},
  issn      = {0040-1951},
  doi       = {10.1016/j.tecto.2012.06.011},
  pages     = {1 -- 33},
  year      = {2013},
  abstract  = {We review the geodynamic evolution of the Aegean-Anatolia region and discuss strain localisation there over geological times. From Late Eocene to Present, crustal deformation in the Aegean backarc has localised progressively during slab retreat. Extension started with the formation of the Rhodope Metamorphic Core Complex (Eocene) and migrated to the Cyclades and the northern Menderes Massif (Oligocene and Miocene), accommodated by crustal-scale detachments and a first series of core complexes (MCCs). Extension then localised in Western Turkey, the Corinth Rift and the external Hellenic arc after Messinian times, while the North Anatolian Fault penetrated the Aegean Sea. Through time the direction and style of extension have not changed significantly except in terms of localisation. The contributions of progressive slab retreat and tearing, basal drag, extrusion tectonics and tectonic inheritance are discussed and we favour a model (I) where slab retreat is the main driving engine, (2) successive slab tearing episodes are the main causes of this stepwise strain localisation and (3) the inherited heterogeneity of the crust is a major factor for localising detachments. The continental crust has an inherited strong heterogeneity and crustal-scale contacts such as major thrust planes act as weak zones or as zones of contrast of resistance and viscosity that can localise later deformation. The dynamics of slabs at depth and the asthenospheric flow due to slab retreat also have influence strain localisation in the upper plate. Successive slab ruptures from the Middle Miocene to the late Miocene have isolated a narrow strip of lithosphere, still attached to the African lithosphere below Crete. The formation of the North Anatolian Fault is partly a consequence of this evolution. The extrusion of Anatolia and the Aegean extension are partly driven from below (asthenospheric flow) and from above (extrusion of a lid of rigid crust).},
  language  = {en}
}