Estudios acerca de ametralladoras /

Mode of access: Internet.

Das Becken der Aïno und der Japaner,

Detached from the Mittheilungen aus dem Medicin. Facultat der Kaiserlich-Japanischen Universitat zu Tokio, Bd. 4.

Toledo, locus terribilis. Iglesia y milagro en el De viris illustribus de Ildefonso de Toledo

A mediados del siglo VII, el obispo Ildefonso de Toledo (657-667) elaboró su propio catálogo de hombres ilustres, continuando una tradición cuyos orígenes cristianos se remontaban a Jerónimo en el siglo IV. Sin embargo, en lugar de reproducir los modelos de sus antecesores cristianos, entre los que se incluyen además a Genadio de Marsella e Isidoro de Sevilla, el De viris illustribus de Ildefonso incorporaba cambios significativos en el género. Este artículo estudia el tópico del milagro en el opúsculo toledano con el objetivo de indagar qué tipo de relación estableció la Iglesia visigoda de la segunda mitad del siglo VII con este tipo de fenómenos y qué estrategias elaboró en función de él.

A vueltas con la naturaleza del cambio fonético-fonológico: los casos de Nj y Lj

Las etapas del cambio fonético-fonológico han sido descritas desde hace décadas, especialmente desde un punto de vista articulatorio y casi siempre partiendo de los testimonios escritos de que se podía disponer. No obstante, recientemente han ido surgiendo nuevas teorías que defienden que el cambio puede ser explicado a través del estudio de la variación y los procesos fonéticos propios del habla actual, puesto que ambos están relacionados con fenómenos de hipo (e hiper) articulación y, a la postre, de coarticulación. Una de ellas es la Fonología Evolutiva (Blevins 2004), aun cuando no ofrece una explicación satisfactoria para la difusión del cambio. En este estudio, se ha recurrido a estas teorías para esclarecer las causas de la evolución de dos contextos de yod segunda: /nj/ y /lj/, que llevaron a la fonologización de // y //, en un primer estadio de la historia del español.

Manual: Crianza y manejo de codornices

La codorniz común ( Coturnix coturnix ) , es un ave migratoria de Asia, África y Europa. Las espec ies más importantes son la codorniz europea o Coturnix coturnix coturnix y la codorniz asiática o japonesa Coturnix coturnix japónica , u na subespecie que comúnmente emigraba entre Europa y Asia , eventualmente domesticada en China. Durante muchos años , est as aves fueron consideras únicamente de carácter ornamental , aprecia das también por el canto característico del macho. La codorniz doméstica fue llevada alrededor del siglo XI desde China a Japón , a través de Corea , y fue domesticada en el lejano oriente y no en oriente m edio co mo argumenta n algunos autores ( T imy , 2009). Si bien la codorniz europea emigraba al sur a través del mar Mediterráneo, al encontrarse exhausta por el vuelo, probablemente haya sido fácilmente cazada o capturada. Un indicio de esto e s que los escritos bíblicos y egipcios que mencionan estas aves no indican que fueran criadas en cautiverio. Los primeros registros escritos sobre la domesticación de la codorniz en Japón , datan del siglo XII. Estas aves fueron inicialmente criadas por su canto, hecho que cambió después de la noticia de que el e mperador de Japón se había curado de tuberculosis gracias a una dieta a base de carne de codorniz. Esto inició la producción masiva de carne y huevos de codorniz en la última parte del siglo XIX. P or el año 1910, en Japón, la codorniz era utilizada no sólo por su carne y huevos , sino también por su canto . 4 Entre los años de 1910 y 1940 , la población de codorni z japónica se incrementó rápidamente en Japón, especialmente en las localidades de Tokio , M ishima, Nagoya, Gifu y Toyohashi. Este período es coincidente con el de la expansión imperial de Japón, por lo que la codorniz japonesa fue establecida en otros países como Corea, China y Taiwán, para hacerlo más tarde en todo el s udeste asiático. La sube specie domesticada, Coturnix coturnix jap ó nica , es llamada codorniz japonesa , pero también se la conoce por otros nombres: codorniz común, codorniz oriental, codorniz asiática, codorniz faraona, codorniz pecho rojo, codorniz real y codorniz real japonesa ( T imy , 2009 ) . Por otro lado, e xisten tres grandes rutas migratorias de las codornices desde el continente af ricano hasta las zonas europeas: La primera ruta abarca desde las costas occidentales de Á frica, M arruecos , Australia y Argelia hacia la península ibérica , y desde esta pasa a Francia e Inglaterra, países escandinavos y parte de Europa central. Una segunda ruta parte de zonas de Argelia oriental, L ibia y Túnez , dirigiéndose a través de Italia a Europa central a las zonas del Danubio y Rusia. La terce ra ruta va desde Egipto hacia Grecia y Europa oriental (Quintana , 2008 ). La llegada a Europa de las codornices tiene lugar durante el final de la primavera y regresan a África , durante el otoño

Geophysics: Principles, applications and emerging technologies

This book presents research in the field of Geophysics, particularly referring to principles, applications and emerging technologies. Table of Contents: Preface pp. i-xxi Environmental Geophysics: Techniques, advantages and limitations (Pantelis Soupios and Eleni Kokinou, Department of Environmental and Natural Resources Engineering, Technological Educational Institute of Crete, Dynamics of the Ocean Floor, Helmholtz Centre for Ocean Research Kiel, Geomar)pp i-xxi Application of Innovative Geophysical Techniques in Coastal Areas (V. Di Fiore, M. Punzo, D. Tarallo, and G. Cavuoto, Institute for Marine Coastal Environment, National Research Council, Naples)pp. i-xxi Marine Geophysics of the Naples Bay (Southern Tyrrhenian sea, Italy): Principles, Applications and Emerging Technologies (Gemma Aiello and Ennio Marsella, Institute for Marine Coastal Environment, National Research Council, Naples)pp. i-xxi Oceanic Oscillation Phenomena: Relation to Synchronization and Stochastic Resonance (Shinya Shimokawa and Tomonori Matsuura, National Research Institute for Earth Science and Disaster Prevention, Univ. of Toyama)pp. i-xxi Assessment of ocean variability in the Sicily Channel from a numerical three-dimensional model using EOFs decomposition (R. Sorgente, A. Olita, A.F. Drago, A. Ribotti, L. Fazioli, and C. Tedesco, Institute for Marine Coastal Environment, National Research Council, Oristano)pp. i-xxi Monitoring Test of Crack Opening in Volcanic Tuff (Coroglio Cliff. Italy) Using Distributed Optical Fiber Sensor (A. Minardo, A. Coscetta, M. Caccavale, G. Esposito, F. Matano, M. Sacchi, R. Somma, G. Zeni, and L. Zeni, Department of Industrial and Information Eng., Second University of Naples Aversa, Institute for Marine Coastal Environment, National Research Council Naples, National Institute for Geophysics and Volcanology, Osservatorio Vesuviano Naples, Institute for Electromagnetic Sensing of the Environment, National Research Council Naples)pp. i-xxi

New morpho-bathymetric and tectono-stratigraphic data on Naples and Salerno gulfs (southern tyrrhenian sea, Italy) derived from bathymetric and seismic data analysis and integrated geological interpretation

New morpho-bathymetric and tectono-stratigraphic data on Naples and Salerno Gulfs, derived from bathymetric and seismic data analysis and integrated geologic interpretation are here presented. The CUBE(Combined Uncertainty Bathymetric Estimator) method has been applied to complex morphologies, such as the Capri continental slope and the related geological structures occurring in the Salerno Gulf.The bathymetric data analysis has been carried out for marine geological maps of the whole Campania continental margin at scales ranging from 1:25.000 to 1:10.000, including focused examples in Naples and Salerno Gulfs, Naples harbour, Capri and Ischia Islands and Salerno Valley. Seismic data analysis has allowed for the correlation of main morpho-structural lineaments recognized at a regional scale through multichannel profiles with morphological features cropping out at the sea bottom, evident from bathymetry.Main fault systems in the area have been represented on a tectonic sketch map, including the master fault located northwards to the Salerno Valley half graben. Some normal faults parallel to the master fault have been interpreted from the slope map derived from bathymetric data. A complex system of antithetic faults bound two morpho-structural highs located 20km to the south of the Capri Island. Some hints of compressional reactivation of normal faults in an extensional setting involving the whole Campania continental margin have been shown from seismic interpretation.

The Southern Ischia canyon system: examples of deep sea depositional systems on the continental slope off Campania (Italy)

The Southern Ischia canyon system has been investigated in detail through Multibeam bathymetry and Sparker seismic data and has been put in the geological framework of the deep sea depositional systems off the Campania region. The geological and geomorphological characteristics of the canyon system have been also compared with the characters of the Mediterranean submarine canyons and with the deep sea depositional systems of the Tyrrhenian sea. The Southern Ischia canyon system engraves a narrow continental shelf from Punta Imperatore to Punta San Pancrazio, being limited southwestwards from the relict volcanic edifice of the Ischia Bank. It consists of twenty-two drainage axes, whose planimetric trending has been reconstructed in a sketch morphological map realized through the geological interpretation of Multibeam bathymetry. While the eastern boundary of the canyon system is controlled by extensional tectonics, being limited by a NE-SW trending (anti-Apenninic) normal fault, its western boundary is controlled by volcanism, due to the growth of the Ischia volcanic bank. Submarine gravitational instabilities also acted in relationships to the canyon system, allowing for the individuation of large-scale creeping at the sea bottom and hummocky deposits already interpreted as debris avalanche deposits. Quaternary marine seismic sequences have been reconstructed through a densely spaced seismic grid recorded through a Sparker multitip seismic source, allowing for a detailed observation of steep erosional slopes occurring on the southern flank of the island and related deep sea depositional systems. Important implications of this study will regard the coastal monitoring and beach nourishment of the southern flank of the island, being involved by a strong erosion of marine and coastal systems.

Interactions between Late Quaternary volcanic and sedimentary processes in the Naples Bay, Southern Tyrrhenian sea

The interactions between Late Quaternary volcanic and sedimentary processes in the Naples Bay, Southern Tyrrhenian sea, are here discussed through the results of the marine geological survey at the scale 1:25.000. The example of the geological map n. 465 “Isola di Procida”, herein presented, has put in evidence the stratigraphy of marine Quaternary deposits and related volcanic seismic units. The volcanic deposits cropping out in the Procida island have been explained as the result of eruptions of local eruptive centres. The geological survey carried out onshore indicates the occurrence of several pyroclastic units linked to the eruptive activity of the Ischian and Phlegrean volcanic complexes, interstratified with the products erupted by local volcanic centres. The occurrence in the pyroclastic sequences of Ischia and Procida islands of several marker horizons and their stratigraphic correlations have allowed to reconstruct the volcanological evolution of the two islands and the interactions with sedimentary processes at the scale of the whole Tyrrhenian margin. Four geological maps at the scale 1:25.000 covering the whole Naples Bay have been reconstructed based on the interpretation of marine geological and geophysical data. The stratigraphic relationships between the seismic units and the eruptive deposits have testified the activity of several monogenetic volcanic centers, whose products are interstratified with marine and continental deposits of the Late Quaternary depositional sequence.

Magnetic Theory and Applications in the Naples Bay (Southern Tyrrhenian Sea, Italy): Magnetic Anomaly Fields and Relationships with Morpho-Structural Lineaments

Magnetic theory and application to a complex volcanic area located in Southern Italy are here discussed showing the example of the Gulf of Naples, located at Southern Italy Tyrrhenian margin. A magnetic anomaly map of the Gulf of Naples has been constructed aimed at highlighting new knowledge on geophysics and volcanology of this area of the Eastern Tyrrhenian margin, characterized by a complex geophysical setting, strongly depending on sea bottom topography. The theoretical aspects of marine magnetometry and multibeam bathymetry have been discussed. Magnetic data processing included the correction of the data for the diurnal variation, the correction of the data for the offset and the leveling of the data as a function of the correction at the cross-points of the navigation lines. Multibeam and single-beam bathymetric data processing has been considered. Magnetic anomaly fields in the Naples Bay have been discussed through a detailed geological interpretation and correlated with main morpho-structural features recognized through morphobathymetric interpretation. Details of magnetic anomalies have been selected, represented and correlated with significant seismic profiles, recorded on the same navigation lines of magnetometry. They include the continental shelf offshore the Somma-Vesuvius volcanic complex, the outer shelf of the Gulf of Pozzuoli offshore the Phlegrean Fields volcanic complex, the relict volcanic banks of Pentapalummo, Nisida and Miseno, the Gaia volcanic bank on the Naples slope, the western slope of the Dohrn canyon, the Magnaghi canyon’s head and the magnetic anomalies among the Ischia and Procida islands.

Geological Evolution of Coastal and Marine Environments off the Campania Continental Shelf Through Marine Geological Mapping - The Example of the Cilento Promontory

The geological evolution of coastal and marine environments offshore the Cilento Promontory through marine geological mapping is discussed here. The marine geological map n. 502 “Agropoli,” located offshore the Cilento Promontory (southern Italy), is described and put in regional geologic setting. The study area covers water depths ranging between 30 and 200 m isobaths. The geologic map has been constructed in the frame of a research program financed by the National Geological Survey of Italy (CARG Project), finalized to the construction of an up-to-date cartography of the Campania region. Geological and geophysical data on the continental shelf and slope offshore the southern Campania region have been acquired in an area bounded northward by the Gulf of Salerno and southward by the Gulf of Policastro. A high-resolution multibeam bathymetry has permitted the construction of a digital elevation model (DEM). Sidescan sonar profiles have also been collected and interpreted, and their merging with bathymetric data has allowed for the realization of the base for the marine geologic cartography. The calibration of geophysical data has been attempted through sea-bottom samples. The morpho-structures and the seismic sequences overlying the outcrops of acoustic basement reported in the cartographic representation have been studied in detail using single-channel seismics. The interpretation of seismic profiles has been a support for the reconstruction of the stratigraphic and structural setting of the Quaternary continental shelf successions and the outcrops of rocky acoustic basement in correspondence to the Licosa Cape morphostructural high. These areas result from the seaward prolongation of the stratigraphic and structural units, widely cropping out in the surrounding emerged sector of the Cilento Promontory. The cartographic approach is based on the recognition of laterally coeval depositional systems, interpreted in the frame of system tracts of the Late Quaternary depositional sequence.

Computational approaches to emotional decision making

Findings on the role that emotion plays in human behavior have transformed Artificial Intelligence computations. Modern research explores how to simulate more intelligent and flexible systems. Several studies focus on the role that emotion has in order to establish values for alternative decision and decision outcomes. For instance, Busemeyer et al. (2007) argued that emotional state affects the subjectivity value of alternative choice. However, emotional concepts in these theories are generally not defined formally and it is difficult to describe in systematic detail how processes work. In this sense, structures and processes cannot be explicitly implemented. Some attempts have been incorporated into larger computational systems that try to model how emotion affects human mental processes and behavior (Becker-Asano & Wachsmuth, 2008; Marinier, Laird & Lewis, 2009; Marsella & Gratch, 2009; Parkinson, 2009; Sander, Grandjean & Scherer, 2005). As we will see, some tutoring systems have explored this potential to inform user models. Likewise, dialogue systems, mixed-initiative planning systems, or systems that learn from observation could also benefit from such an approach (Dickinson, Brew & Meurers, 2013; Jurafsky & Martin, 2009). That is, considering emotion as interaction can be relevant in order to explain the dynamic role it plays in action and cognition (see Boehner et al., 2007).

Características y perfil microbiológico de pacientes con colecistitis moderada y severa en Mederi de 2014 a 2016

Introducción: Las guías de Tokyo de 2013 lograron un consenso respecto al manejo antibiótico de la infección biliar. Sus recomendaciones están sustentadas en estudios internacionales de la epidemiología bacteriana, pero también recalcan la importancia de conocer la microbiología local para ajustar las guías de manejo. Materiales y métodos: Se diseñó un estudio descriptivo tipo serie de casos de pacientes tratados por colecistitis aguda moderada y severa en Méderi Hospital Universitario Mayor (HUM), describiendo los aislamientos microbiológicos y perfiles de resistencia de los cultivos de bilis tomados durante la cirugía. Resultados: Se analizaron 131 pacientes con una edad promedio de 63 años, la mayoría sin comorbilidades médicas. Se encontró un 48% de positividad en los cultivos, predominantemente enterobacterias siendo la más frecuente Escherichia coli, seguida de especies de Klebsiella y de Enterococcus. Los perfiles de resistencia evidenciaron un 93% de multisensibilidad antibiótica y se aislaron 4 microorganismos multirresistentes. No se encontraron diferencias en comorbilidades, alteraciones paraclínicas, presencia de síndrome biliar obstrutivo, pancreatitis o instrumentación previa de la vía biliar entre los pacientes con cultivo positivo y negativo. Conclusiones: Los resultados concuerdan con los reportes internacionales en cuanto a la flora bacteriana aislada, pero los perfiles de resistencia evidenciados en esta serie son diferentes a los que sustentan las guías de manejo de Tokio revisadas en 2013. Este hallazgo obliga a ajustar las guías de manejo institucionales con base en la epidemiología local.

El rol de los actores subnacionales en la construcción de la política exterior de Japón. Estudio de caso: La disputa territorial por las islas Senkaku/Diaoyu entre Japón y China (2001-2014)

El presente estudio de caso tiene como objetivo analizar la influencia de la gobernación de Tokio en la formulación de la política exterior de Japón durante la disputa territorial por las islas Senkaku/Diaoyu. Para ello, se identifican los puntos más relevantes de la política exterior de seguridad de Japón después de la Segunda Guerra Mundial. Se hace un énfasis en la política bilateral de seguridad sino-japonesa, con el fin de ubicar el conflicto territorial por las islas Senkaku/Diaoyu como un punto importante en la agenda internacional de seguridad de ambos países. Se estudia y analiza el concepto de paradiplomacia; articulado, a su vez, por los conceptos de identidad y rol en política exterior de la perspectiva teórica del Constructivismo de las Relaciones Internacionales, para así analizar la influencia de Tokio en el manejo de la política exterior de Japón en el marco del conflicto territorial por las islas Senkaku/Diaoyu.