‘YAMPIL INSPIRATIONS’: A STUDY OF THE DNIESTER CULTURAL CONTACT AREA AT THE FRONTIER OF PONTIC AND BALTIC DRAINAGE BASINS

The article presents the present state of research on the general issue of the dniester region of cultural contacts between communities settling the Baltic and Pontic drainage basins . Some five domains of research shall be brought to discussion in which it is possible to see fresh opportunities for archaeological study, on the basis of ‘Yampil studies’ on dniester-Podolia (forest-steppe) barrow-culture ceremonial centres from the latter half of the 4th millennium and first half of the 3rd millennium BC . This relates to the peoples of the Eneolithic and the Early Bronze age . in terms of topogenesis, embracing the Pontic-Tripolye, Yamnaya and Catacomb cultures, as well as Globular amphora and Corded ware in central prehistoric Europe .

The Ponto-Caspian basin as a final trap for southeastern Scandinavian Ice-Sheet meltwater

This paper provides new data on the evolution of the Caspian Sea and Black Sea from the Last Glacial Maximum until ca. 12 cal kyr BP. We present new analyses (clay mineralogy, grain-size, Nd isotopes and pollen) applied to sediments from the river terraces in the lower Volga, from the middle Caspian Sea and from the western part of the Black Sea. The results show that during the last deglaciation, the Ponto-Caspian basin collected meltwater and fine-grained sediment from the southern margin of the Scandinavian Ice Sheet (SIS) via the Dniepr and Volga Rivers. It induced the deposition of characteristic red-brownish/chocolate-coloured illite-rich sediments (Red Layers in the Black Sea and Chocolate Clays in the Caspian Sea) that originated from the Baltic Shield area according to Nd data. This general evolution, common to both seas was nevertheless differentiated over time due to the specificities of their catchment areas and due to the movement of the southern margin of the SIS. Our results indicate that in the eastern part of the East European Plain, the meltwater from the SIS margin supplied the Caspian Sea during the deglaciation until ∼13.8 cal kyr BP, and possibly from the LGM. That led to the Early Khvalynian transgressive stage(s) and Chocolate Clays deposition in the now-emerged northern flat part of the Caspian Sea (river terraces in the modern lower Volga) and in its middle basin. In the western part of the East European Plain, our results confirm the release of meltwater from the SIS margin into the Black Sea that occurred between 17.2 and 15.7 cal kyr BP, as previously proposed. Indeed, recent findings concerning the evolution of the southern margin of the SIS and the Black Sea, show that during the last deglaciation, occurred a westward release of meltwater into the North Atlantic (between ca. 20 and 16.7 cal kyr BP), and a southward one into the Black Sea (between 17.2 and 15.7 cal kyr BP). After the Red Layers/Chocolate Clays deposition in both seas and until 12 cal kyr BP, smectite became the dominant clay mineral. The East European Plain is clearly identified as the source for smectite in the Caspian Sea sediments. In the Black Sea, smectite originated either from the East European Plain or from the Danube River catchment. Previous studies consider smectite as being only of Anatolian origin. However, our results highlight both, the European source for smectite and the impact of this source on the depositional environment of the Black Sea during considered period.

Someone Else's Textbooks: German Education 1945-2014

In the 20th century, German education repeatedly transformed as the occupying Americans, Soviets, and western-dominated reunification governments used their control of the German secondary education system to create new definitions of what it meant to be German. In each case, the dominant political force established the paradigm for a new generation of Germans. The victors altered the German education system to ensure that their versions of history would be the prevailing narrative. In the American Occupation Zones from 1945-1949, this meant democratic initiatives; for the Soviet Zone in those same years, Marxist-Leninist pedagogy; and for the Bundesrepublik after reunification, integrated East and West German narratives. In practice, this meant succeeding generations of German students learned very different versions of history depending on the temporal and geographic space they inhabited, as each new prevailing regime supplanted the previous version of “Germanness” with its own.

Convolution of Orbital Measures on Symmetric Spaces of type Cp and Dp

International audience

Introduccion - Simulando con OMNET: selección de la herramienta y su utilización

La diferenciación y el soporte en calidad de servicio es utilizada en muchas arquitecturas de red, técnicas y frameworks, tales como IP, con los esquemas de DiffServ e IntServ, redes NGN, GMPLS (Generalized Multiprotocol Label Switching) y redes ópticas, entre otras. Actualmente, la calidad de servicio no es solo una cuestión técnica, sino que se ha convertido en un producto que puede ser visto desde numerosas perspectivas, en las que los clientes, cada día, demandan más servicios, de mayor calidad. Por lo tanto, los proveedores deben mejorar sus implementaciones para permanecer en este reñido mercado (Piotr, Stankiewicz, Cholda, & Jajszczyk, 2011). En este contexto, las redes actuales deben garantizar la calidad en los servicios sin importar el incremento paulatino de usuarios y dispositivos de interconectividad. La mejor manera de hacerlo no es necesariamente invirtiendo en la infraestructura más moderna que soporte técnicas para este fin. Existen mecanismos que se pueden aplicar sobre infraestructuras de red actuales, las cuales ayudan a manejar el tráfico de manera adecuada, de tal manera que los parámetros de calidad de servicio se mantengan dentro de los límites permisibles establecidos por la Recomendación Y.1541 (UIT, 2011a).

The real effects of banking supervision:evidence from enforcement actions

We present a novel way to examine macro-financial linkages by focusing on the real effects of bank supervisors’ enforcement actions. Exploiting plausibly exogenous variation in supervisory monitoring intensity, we show that enforcement actions in single-market banks trigger temporarily large adverse effects for the macroeconomy by reducing personal income growth, the number of establishments, and increasing unemployment. These effects are related to contractions in bank lending and liquidity creation, and are more pronounced when we consider enforcement actions on both single-market and multi-market banks, and in counties with fewer banks and greater external financial dependence.

Teknova: Calciner Problem

Expressing the properties of the exit material as a function of the potential difference and mass flux (scraping rate) and solving the mechanical problem in order to obtain a velocity field to be fed into multi-physics numerical platforms.

Improved model of an electric calciner for carbon materials

Teknova have 2D steady-state models of the calciner but wish, in the long term, to have a 3D model that can also cover unsteady conditions, and can can model the loss of axisymmetry that someties occurs. Teknova also wish to understand the processes happening around the tip of the upper electrode, in particular the formation of a lip on it and the the shape of the empty region below it. The Study Group proposed potential models for the degree of graphitization, and for the granular flow. Also the Study Group considered the upper electrode in detail. The proposed model for the lip formation is by sublimation of carbon from the hottest parts of the furnace with redeposition in the region around the electrode, which may stick particles onto the electrode surface. In this model the region below the electrode would be a void, roughly a vertex-down conical cavity. The electric field near the lower rim of the electrode will then have a singularity and so the most intense heating of the charge will be around the rim. We conjecture that the reason why the lower electrode lasts so much longer than the upper is that it is not adjacent to a cavity like this, and therefore does not have a singularity in the field.