@phdthesis{Cornefert2023,
  author    = {Cornefert, Gabrielle},
  title     = {De/lirios},
  series = {Mimesis},
  volume    = {104},
  journal   = {Mimesis},
  publisher = {De Gruyter},
  address   = {Berlin/Boston},
  isbn      = {978-3-11-099367-7},
  issn      = {0178-7489},
  doi       = {10.1515/9783110980516},
  school      = {Universit{\"a}t Potsdam},
  pages     = {XI, 336},
  year      = {2023},
  abstract  = {En base al concepto de "de/lirio", que articula trastornos en la enunciaci{\´o}n literaria en primera persona, por un lado, con la caracterizaci{\´o}n psicopatol{\´o}gica de este yo enunciativo, por otro lado, el estudio explora las "l{\´i}ricas desviadas" de Mario Levrero y Alberto Laiseca, y muestra como responden productivamente a problem{\´a}ticas est{\´e}ticas, {\´e}ticas y ontol{\´o}gicas propias de la vuelta del milenio, en el R{\´i}o de la Plata y m{\´a}s all{\´a}.},
  language  = {es}
}
@book{Ette2023,
  author    = {Ette, Ottmar},
  title     = {Sin domicilio fijo},
  series = {Colecci{\´o}n iridiscencias},
  journal   = {Colecci{\´o}n iridiscencias},
  publisher = {Ubu ediciones},
  address   = {Olivios, Buenos Aires},
  isbn      = {978-987-8495-25-5},
  pages     = {141},
  year      = {2023},
  language  = {es}
}
@phdthesis{Molina2023,
  author    = {Molina, Gisela},
  title     = {La imagen de religiosidad popular en la narrativa moderna de Tom{\´a}s Carrasquilla},
  doi       = {10.25932/publishup-59785},
  url       = {http://nbn-resolving.de/urn:nbn:de:kobv:517-opus4-597852},
  school      = {Universit{\"a}t Potsdam},
  pages     = {310},
  year      = {2023},
  abstract  = {In der vorliegenden Arbeit soll aufgezeigt werden, daβ die Erz{\"a}hlungen von Tom{\´a}s Carrasquilla Naranjo (1858 - Medell{\´i}n, 1940) einen Wahrheitsgehalt (Benjamin, 2012) in sich bergen, eine tempor{\"a}re konkrete Verwirklichung einer Idee, die sich materialisiert in dem, was ich hier Bild der Volksreligiosit{\"a}t nenne. Das heiβt, das Erz{\"a}hlwerk von Carrasquilla ist wie ein groβes Mosaik konstruiert, in dem das Zusammenf{\"u}gen der verschiedenen und ungleichen Elemente, aus dem es besteht, ein Bild ergibt. Dieses Bild stellt die historische Erfahrung der Moderne in den {\"a}rmeren Bev{\"o}lkerungsschichten dar, ausgehend von der fl{\"u}chtigen Verbindung zwischen veralteten Traditionen und neueren Lebensformen. Weit entfernt von den Konventionen seiner Zeit, wo die Frage nach den Erfahrungen der Moderne groβst{\"a}dtische Gebiete und die Rolle des K{\"u}nstlers beinfluβt, fragt sich Carrasquilla, was in den weiten l{\"a}ndlichen Gebieten oder in den Grenzgebieten zwischen Stadt und Land geschieht, und nach den {\"U}berschneidungen. Die Bewohner dieser Gebiete, denen konzeptionelle Werkzeuge zur Definierung dieser neuen „lebenden Erfahrung", dieser neuen Structures and Feeling, wie Raymond Williams sie nennt, (2019) fehlen, greifen zur{\"u}ck auf das Einzige, was sie kennen, das veraltete, m{\"u}ndlich {\"u}bermittelte Wissen, um sich ihr Hier und Jetzt zu erkl{\"a}ren. In diesem Sinne kann man behaupten, daβ Carrasquilla, indem er dieses Bild der Volksreligiosit{\"a}t benutzt, einen Dialog im literarischen Bereich herstellen wollte, von dem aus er eine differenzierende Idee der Moderne postulierte. Der Autor bekr{\"a}ftigte mehrmals, daβ die Literatur lokale Erfahrungen in den Dialog des Universellen einbeziehen sollte. Ein Beispiel daf{\"u}r ist der Vergleich der Literatur mit dem Planetensystem, denn, wie Carrasquilla meinte, hierarchische Strukturen erscheinen, wenn diejenigen L{\"a}nder, die literarische Modetendenzen produzieren, d.h. die Planeten (Europa), Andere zum Satellitendasein degradieren, d.h. zum Imitieren. Heute kann in dieser an seine Landsleute, die Modernisten aus Antioquia, gerichteten Kritik eine Geltendmachung der Alterit{\"a}t gesehen werden. Obwohl sich die Erfahrungen von denjenigen in den jungen groβst{\"a}dtischen Gebieten, wo G{\"u}ter zum neuen Ersatz von Glauben geworden sind, unterscheiden, wird im vorliegenden Text behauptet, daβ in den weiten Gebieten, die provinziell und weit entfernt vom Kontakt mit anderen Kulturen und anderem Wissen erscheinen, das Bild der Volksreligiosit{\"a}t dieselbe Rolle spielt. Mit anderen Worten, "indem an Dingen ihr Gebrauchswert abstirbt" (Nutzen oder Anbetung), weist die Subjektivit{\"a}t der Person ihnen "Intentionen von Wunsch und Angst" (Benjamin, 2013a). zu und verwandelt sie in Anbetungsobjekte, die bei sich getragen oder gesammelt werden. Auf {\"a}hnliche Weise bediente Carrasquilla sich des gesammelten Restwissens seiner hypothetischen Leserschaft, ein Erbgut verschiedener Kulturbereiche - dank des Kolonisierungsprozesses - sowie der entsprechenden unterschiedlichen Zeiten und Sprachen (Ette, 2019), um es mit den gegenw{\"a}rtigen profanen Erfahrungen zu verbinden. So repr{\"a}sentiert das Werk (Erz{\"a}hlung oder Roman) auf k{\"u}nstlerische Weise „Lebensformen" der {\"a}rmeren Bev{\"o}lkerungsschichten, durch die „auf {\"a}sthetische Weise erlebt" werden kann, wie die Modernit{\"a}t in den marginalisierten Sektoren {\"u}berlebt wird (Ette, 2015). Das heiβt, nur ausgehend vom Veralteten und Ruin{\"o}sen der einst heiligen Volksreligiosit{\"a}t kann die Erfahrung der Moderne, ihr Hier und Jetz erkl{\"a}rt werden.},
  language  = {es}
}
@article{SanchezSanz2023,
  author    = {Sanchez Sanz, Arturo},
  title     = {La her{\´a}ldica amaz{\´o}nica},
  series = {thersites 16},
  volume    = {2023},
  journal   = {thersites 16},
  number    = {16},
  editor    = {Amb{\"u}hl, Annemarie and Carl{\`a}-Uhink, Filippo and Rollinger, Christian and Walde, Christine},
  issn      = {2364-7612},
  doi       = {10.34679/thersites.vol16.202},
  pages     = {1 -- 82},
  year      = {2023},
  abstract  = {Nowadays, we know about 4,475 iconographic representations dedicated to the Amazonian universe in Antiquity. Most of them belong to vase painting pieces (3,448). This current work analyze the Amazonian emblems that appear in a high percentage of these representations (725), together with the few examples associated with other artistic supports. In that way, we will study the chosen designs, which of them achieved greater popularity and the possible reasons why some of them were more popular in certain contexts. According to the results, we can discover that the Amazons present a type of emblem very similar to that used by the hoplites who fought against them in the same representation of the Amazonomachy. It is true that we appreciate a greater interest in certain models within a broad group of options that became traditional for Amazonian representations, but the results of this study suggest that the artists freely chose between them. However, his decision could be influenced by aspects such as the predominant trends in each period, the tastes of the export markets or the influence generated by other types of works (mainly paintings, reliefs or sculptures) whose popularity made them models.},
  language  = {es}
}
@article{UthVanrell2023,
  author    = {Uth, Melanie and Vanrell, Maria del Mar},
  title     = {Multiling{\"u}ismo y turismo},
  series = {Energeia : online journal for linguistics, language philosophy and history of linguistics},
  volume    = {VIII},
  journal   = {Energeia : online journal for linguistics, language philosophy and history of linguistics},
  publisher = {Romanisches Seminar der Universit{\"a}t Z{\"u}rich},
  address   = {Z{\"u}rich},
  issn      = {1869-4233},
  pages     = {104 -- 130},
  year      = {2023},
  abstract  = {El turismo es un fen{\´o}meno territorial de contacto ling{\"u}{\´i}stico-cultural que tiene impactos significativos tanto en las sociedades receptoras como, aunque en menor medida, en las sociedades de origen de los turistas. Adem{\´a}s de las repercusiones territoriales y medioambientales, la pr{\´a}ctica tur{\´i}stica deja su huella en la cultura, la sociodemograf{\´i}a y la identidad de los destinos tur{\´i}sticos. Este trabajo aborda la relaci{\´o}n entre el turismo y el multiling{\"u}ismo, comparando el litoral del estado de Quintana Roo, en la pen{\´i}nsula de Yucat{\´a}n, M{\´e}xico, con la isla de Mallorca. Nuestro objetivo principal es identificar tanto los puntos en com{\´u}n como las diferencias entre las dos regiones en el marco de los aspectos socioling{\"u}{\´i}sticos mencionados anteriormente. Esto nos permitir{\´a} distinguir las din{\´a}micas ling{\"u}{\´i}sticas regionales relacionadas con el turismo, por un lado, de aquellas din{\´a}micas que operan a nivel global o transatl{\´a}ntico, por el otro. De esta manera, esperamos contribuir a un entendimiento m{\´a}s profundo de las din{\´a}micas socioling{\"u}{\´i}sticas caracter{\´i}sticas de cada uno de los dos contextos y establecer las bases para futuros trabajos de tipo emp{\´i}rico.},
  language  = {es}
}
@phdthesis{JimenezAlvaro2023,
  author    = {Jim{\´e}nez {\´A}lvaro, Eliana},
  title     = {An{\´a}lisis neotect{\´o}nico y lito-tefroestratigr{\´a}fico de los grandes movimientos en masa asociados al fallamiento activo de la cuenca intermontana Quito-Guayllabamba, Ecuador},
  doi       = {10.25932/publishup-62220},
  url       = {http://nbn-resolving.de/urn:nbn:de:kobv:517-opus4-622209},
  school      = {Universit{\"a}t Potsdam},
  pages     = {195},
  year      = {2023},
  abstract  = {Within the Quito-Guayllabamba intermontane basin of Ecuador, five unusually large colluvial deposits of ancient landslides have been identified and analyzed in this study. The voluminous rotational MM-5 Guayllabamba landslide is the largest one, with a volume of 1183 million m3. The mega debris-avalanches MM-1 Conocoto, MM-3 Oyacoto, and MM-4 San Francisco were originally triggered by an initial rupture that was associated with a rotational landslide, the corresponding deposits have volumes between 399 to 317 million m3. Finally, the deposit with the smallest volume, the MM-2 Bat{\´a}n rotational landslide and debris fall, has a volume of 8,7 million m3. In this thesis, a detailed study of these large mass movements was carried out using neotectonic and litho-tephrostratigraphic methods to understand the geological and geomorphological boundary conditions that might have been relevant for triggering such mass movements. The neotectonic part of the study was based on the qualitative and quantitative geomorphic analysis of these large mass-movement deposits through the structural characterization of anticlines located east of the Quito sub-basin and their collapsed flanks that constitute the break-off areas. This part of the analysis was furthermore supported by the application of different morphometric indices to reveal tectonically forced landscape evolution processes that may have aided mass-movement generation. The litho-tephrostratigraphic part of the study was based on the analysis of petrographic, geochemical, and geochronological characteristics of soil horizons and intercalated volcanic ashes with the aim to constrain the timing of individual mass-movement events and their potential correlation. The results were integrated into chronostratigraphic schemes using break-off surfaces, cross-cutting and superposition relationships of landslide deposits and subsequently deposited strata to understand the mass movements in the tectonic and temporal context of the intermontane basin setting, as well as to identify the triggering mechanisms for each event. The MM-5 Guayllabamba mass movement is the result of the collapse of the southwestern slope of the Mojanda volcano and was triggered by the interaction of geologic and morphologic conditions approximately 0,81 Ma. The first debris-avalanche episode of the MM-3 Oyacoto and MM-4 San Francisco mass movements could be related to both geological and morphological conditions, given the highly fractured rocks and uplift of the Bellavista-Catequilla anticline that was subsequently incised at the foot of the slope by fluvial erosion. This first episode of collapse most likely occurred around 0,8 Ma. The MM-2 Bat{\´a}n mass movement was possibly also facilitated by a combination of geological and morphological conditions, most likely associated with a reduction in the lithostatic stresses affecting the Chiche and Mach{\´a}ngara formations and an increase of shear stresses during lateral fluvial scouring processes at the flanks of the source areas. This points to a linked process between river erosion and uplift processes associated with the evolution of the El Bat{\´a}n-La Bota anticline that could have occurred between 0,5 and 0,25 Ma. The voluminous MM-1 Conocoto debris avalanche, as well as the second debris avalanche episode that generated the MM-3 Oyacoto and MM-4 San Francisco mass movements, were caused by the gravitational collapse of the Mojanda and Cangahua formations that are characterized by the intercalation of volcanic ashes. The failure of the eastern flank of the anticlines probably was associated with increased available humidity related to regional Holocene climatic variations. The results of paleosol chronology combined with regional chronostratigraphic and paleoclimate data suggests that these debris avalanches were triggered between 5 and 4 ka. Active tectonics has shaped the morphological features of the Quito-Guayllabamba intermontane basin. The triggering of mass movements in this environment is associated with failure of Pleistocene lithologies (lake sediments, alluvial and volcanic deposits) subjected to ongoing deformation processes, seismic activity, and superposed episodes of climate variability. The Metropolitan District of Quito is an integral part of this complex environment and the geological, climatic, and topographic conditions that continue to influence the urban geographic space within this intermontane basin. The city of Quito comprises the area with the largest urban consolidation including the sub-basins of Quito and San Antonio, with a population of 2,872 million inhabitants, reflecting the importance of studying the inherent geological and climatic hazards that this region is confronted with.},
  language  = {es}
}
@phdthesis{QuirogaCarrasco2023,
  author    = {Quiroga Carrasco, Rodrigo Adolfo},
  title     = {Cenozoic style of deformation and spatiotemporal variations of the tectonic stress field in the southern central Andes},
  doi       = {10.25932/publishup-61038},
  url       = {http://nbn-resolving.de/urn:nbn:de:kobv:517-opus4-610387},
  school      = {Universit{\"a}t Potsdam},
  pages     = {228},
  year      = {2023},
  abstract  = {The central Andean plateau is the second largest orogenic plateau in the world and has formed in a non-collisional orogenic system. It extends from southern Peru (15°S) to northern Argentina and Chile (27°30'S) and reaches an average elevation of 4,000 m.a.s.l. South of 24°S, the Andean plateau is called Puna and it is characterized by a system of endorheic basins with thick sequences where clastic and evaporitic strata are preserved. Between 26° and 27°30'S, the Puna terminates in a structurally complex zone which coincides with the transition from a normal subduction zone to a flat subduction ("flat slab") zone, which extends to 33°S. This transition zone also coincides with important morphostructural provinces that, from west to east, correspond to i) the Cordillera Frontal, where the Maricunga Belt is located; ii) the Famatina system; and iv) the north-western, thick-skinned Sierras Pampeanas. Various structural, sedimentological, thermochronological and geochronological studies in this region have documented a complex history of deformation and uplift during successive Cenozoic deformation events. These processes caused the increase of crustal thickness, as well as episodes of diachronic uplift, which attained its present configuration during the late Miocene. Subsequently, the plateau experienced a change in deformation style from contraction to extension and transtension documented by ubiquitous normal faults, earthquakes, and magmatic rocks. However, at the southern edge of the Puna plateau and in the transition to the other morphostructural provinces, the variation of deformation processes and the changes in the tectonic stress field are not fully understood. This location is thus ideally located to evaluate how the tectonic stress field may have evolved and how it may have been affected by the presence/absence of an orogenic plateau, as well as by the existence of inherited structural anisotropies within the different tectonic provinces. This thesis investigates the relationship between shallow crustal deformation and the spatiotemporal evolution of the tectonic stress field in the southern sector of the Andean plateau, during pre-, syn- and post-uplift periods of this plateau. To carry out this research, multiple methodological approaches were chosen that include (U-Pb) radiometric dating; the analysis of mesoscopic faults to obtain stress tensors and the orientation of the principal stress axes; the determination of magnetic susceptibility anisotropy in sedimentary and volcanoclastic rocks to identify shortening directions or directions of sedimentary transport; kinematic modeling to infer deep crustal structures and deformation; and finally, a morphometric analysis to identify geomorphological indicators associated with Quaternary tectonism. Combining the obtained results with data from published studies, this study reveals a complex history of the tectonic stress field that has been characterized by changes in orientation and by vertical permutations of the principal stress axes during each deformation regime over the last ~24 Ma. The evolution of the tectonic stress field can be linked with three orogenic phases at this latitude of the Andean orogen: (1) a first phase with an E-W-oriented compression documented between Eocene and middle Miocene, which coincided with Andean crustal thickening, lateral growth, and topographic uplift; (2) a second phase characterized by a compressive transpressional stress regime, starting at ~11 Ma and ~5 Ma on the western and eastern edge of the Puna plateau, respectively, and a compressive stress regime in the Famatina system and the Sierras Pampeanas, which is interpreted to reflect a transition between Neogene orogenic construction and the maximum accumulation of deformation and topographic uplift of the Puna plateau; and (3) a third phase, when the tectonic regime caused a changeover to a tensional stress state that followed crustal thickening and the maximum uplift of the plateau between ~5-4 Ma; this is especially well expressed in the Puna, in its western border area with the Maricunga-Valle Ancho Belt, and along its eastern border in the transition with the Sierras Pampeanas. The results of the study thus document that the plateau rim experienced a shift from a compressional to a transtensional regime, which differs from the tensional state of stress of the Andean Plateau in the northern sectors for the same period. Similar stress changes have been documented during the construction of the Tibetan plateau, where a predominantly compressional stress regime changed to a transtensional regime, but which was superseded by a purely tensional regime, between 14 and 4 Ma.},
  language  = {es}
}
@book{CurielMartinez2023,
  author    = {Curiel Mart{\´i}nez, Geishel},
  title     = {Rumbo a Venecia},
  editor    = {Ette, Ottmar},
  publisher = {Universit{\"a}tsverlag Potsdam},
  address   = {Potsdam},
  isbn      = {978-3-86956-558-3},
  issn      = {2629-2548},
  doi       = {10.25932/publishup-58696},
  url       = {http://nbn-resolving.de/urn:nbn:de:kobv:517-opus4-586964},
  publisher      = {Universit{\"a}t Potsdam},
  pages     = {212},
  year      = {2023},
  abstract  = {Esta investigaci{\´o}n explora la representaci{\´o}n de viajes a Venecia en la literatura latinoamericana y de lengua alemana del siglo XX. Aplicando planteamientos te{\´o}ricos de literatura de viaje, se descodifica la estructura m{\´i}tica que subyace en la descripci{\´o}n del desplazamiento hacia la ciudad lacustre. El objetivo es exponer los recursos narrativos y estil{\´i}sticos utilizados para entrelazar este recorrido, en su mayor{\´i}a oblicuo, con la emersi{\´o}n gradual del conflicto de los y las protagonistas. Adem{\´a}s, a partir del estudio comparativo de algunos elementos arquitect{\´o}nicos emblem{\´a}ticos como son los palacios, los puentes y, sobre todo, la conformaci{\´o}n laber{\´i}ntica, se muestran las peculiaridades de la representaci{\´o}n de Venecia en obras de Julieta Campos, Alejo Carpentier, Julio Cort{\´a}zar, Hugo von Hofmannsthal, Thomas Mann y Sergio Pitol. Con ello se busca, primeramente, visibilizar el papel de Venecia en la literatura latinoamericana y, segundo, ofrecer nuevas claves de lectura a obras que han sido ampliamente estudiadas, mas no en una confrontaci{\´o}n transareal.},
  language  = {es}
}