1000 resultados para 74-525_Site
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Boletim elaborado pela Assessoria de Comunicação e Imprensa da Reitoria da UNESP
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Revista elaborada pela Assessoria de Comunicação e Imprensa da Reitoria da UNESP
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The 1970s are in the limelight of a growing historiographic attention, partly due to the recent opening of new archival resources. 1973, in particular, has a special interest in the historian’s eyes, as many are the events that happened that year: to name but a few, the Chilean coup, the October War, the ensuing oil crisis, the Vietnamese peace treaty. So it is may be not entirely surprising that not much attention has been paid to the Year of Europe, a nebulous American initiative destined to sum up to nothing practical - as Kissinger himself put it, it was destined to be the Year that never Was.1 It is my opinion, however, that its failure should not conceal its historical interest. Even though transatlantic relations have sometimes been seen as an uninterrupted history of crisis,2 in 1973 they reached what could then be considered as their unprecedented nadir. I believe that a thorough analysis of the events that during that year found the US increasingly at odds with the countries of Western Europe is worth carrying out not only to cast a new light on the dynamics of transatlantic relations but also to deepen our comprehension of the internal dynamics of the actors involved, mainly the Nixon administration and a unifying Europe. The Nixon administration had not carefully planned what the initiative actually should have amounted to, and its official announcement appears to have been one of Kissinger’s coups de theatre. Yet the Year of Europe responded to the vital priority of revitalising the relations with Western Europe, crucial ally, for too long neglected. But 1973 did not end with the solemn renewal of the Atlantic Declaration that Kissinger had sought. On the contrary, it saw, for the first time, the countries of the newly enlarged EC engaged in a real, if short-lived, solidarity on foreign policy, which highlighted the Nixon administration’s contradictions regarding European integration. Those, in addition to the numerous tensions that already strained transatlantic relations, gave birth to a downward spiral of incomprehensions and misperceptions, which the unexpected deflagration of the October war seriously worsened. However, even though the tensions did not disappear, the European front soon started to disintegrate, mainly under the strains imposed by the oil crisis. Significant changes in the leadership of the main European countries helped to get the tones back to normal. During the course of 1974-5, the substantial failure of the Euro-Arab dialogue, the Gymlich compromise, frequent and serene bilateral meetings bear witness that the worst was over.
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Zwischen April und Juni 1994 wurden in dem kleinen zentralafrikanischen Land Ruanda ca. 800.000 Menschen ermordet worden. Die Mehrzahl der Opfer waren Tutsi, aber auch viele Hutu verloren ihr Leben. Nahezu jede internationale und nationale Organisation versagte im Angesicht des Ausmaßes der Tragödie. Auch die in Ruanda sehr einflussreiche katholische Kirche konnte oder wollte die Massaker nicht beenden. Einzig die in der ruandischen Geschichte bis zum Genozid immer marginalisierten Muslime verweigerten in der Mehrzahl eine Teilnahme an den Massakern. Warum es zu diesem Verhalten kam, steht als Ausgangsfrage zu Beginn der Untersuchung. Im Folgenden gliedert sich die Arbeit in drei Teile – Geschichte des Islam bis 1994, Verhalten der Muslime im Völkermord von 1994 und die Veränderungen in den zehn Jahren nach dem Genozid. Die Arbeit, welche sich auf die Ergebnisse einer zweimonatigen Feldforschung und einige ältere Arbeiten zum Thema stützt, macht deutlich, dass die Geschichte der ruandischen Muslime bis 1994 durch eine kontinuierliche Marginalisierung gekennzeichnet war. Als nach dem Völkermord das außergewöhnliche Verhalten der ruandischen Muslime langsam deutlich wurde, änderte sich bei vielen Menschen und auch bei offiziellen Stellen auch die Einstellung gegenüber Muslimen.
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Abstract. The 74 (75) ka Toba eruption in Sumatra, Indonesia, is considered to be one of the largest volcanic events during the Quaternary. Tephra from the Toba eruption has been found in many terrestrial and marine sedimentary deposits, and acidity peaks related to the eruption have been used to synchronize ice core records from Greenland and Antarctica. Seismic profiles and sedimentological data from Lake Prespa on the Balkan Peninsula, SE Europe, indicate a lake level lowstand at 73.6±7.7 ka based on ESR dating of shells. Tephrostratigraphy, radiocarbon dating and tuning of the total organic carbon content with the NGRIP isotope record, corroborate that the lake level lowstand was a short-term event superimposed on the general cooling trend at the end of MIS 5, most likely at the onset of the Greenland Stadial GS- 20. Acknowledging that tectonic events or karst processes could have triggered this lake level lowstand, the chronological correspondence between the lowstand and the Toba eruption is intriguing. Therefore a Toba-driven short-term shift to aridity in the Balkan region, leading to lake level changes and triggering spatial expansion events in one of the lake’s most abundant benthic species, the carino mussel Dreissena presbensis, cannot be excluded.
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The Toba eruption that occurred some 74 ka ago in Sumatra, Indonesia, is among the largest volcanic events on Earth over the last 2 million years. Tephra from this eruption has been spread over vast areas in Asia, where it constitutes a major time marker close to the Marine Isotope Stage 4/5 boundary. As yet, no tephra associated with Toba has been identified in Greenland or Antarctic ice cores. Based on new accurate dating of Toba tephra and on accurately dated European stalagmites, the Toba event is known to occur between the onsets of Greenland interstadials (GI) 19 and 20. Furthermore, the existing linking of Greenland and Antarctic ice cores by gas records and by the bipolar seesaw hypothesis suggests that the Antarctic counterpart is situated between Antarctic Isotope Maxima (AIM) 19 and 20. In this work we suggest a direct synchronization of Greenland (NGRIP) and Antarctic (EDML) ice cores at the Toba eruption based on matching of a pattern of bipolar volcanic spikes. Annual layer counting between volcanic spikes in both cores allows for a unique match. We first demonstrate this bipolar matching technique at the already synchronized Laschamp geomagnetic excursion (41 ka BP) before we apply it to the suggested Toba interval. The Toba synchronization pattern covers some 2000 yr in GI-20 and AIM-19/20 and includes nine acidity peaks that are recognized in both ice cores. The suggested bipolar Toba synchronization has decadal precision. It thus allows a determination of the exact phasing of inter-hemispheric climate in a time interval of poorly constrained ice core records, and it allows for a discussion of the climatic impact of the Toba eruption in a global perspective. The bipolar linking gives no support for a long-term global cooling caused by the Toba eruption as Antarctica experiences a major warming shortly after the event. Furthermore, our bipolar match provides a way to place palaeo-environmental records other than ice cores into a precise climatic context.
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composé par M. Henkel