995 resultados para Schliemann, Heinrich


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H.Stahl was the last president of the Jewish Community in Berlin. He is seated in a chair with wooden arm supports. He seems a small man, an impression emphasized by a large expanse of plain, tan background. The facial expression is tense, with deeply furrowed brows.

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Passports for Heinrich and Regina Lichtenstein

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A new concept for resource oriented federal research within the competence of the German Ministry of Food, Agriculture and Consumer Protection was implemented in 2008. The Johann Heinrich von Thünen-Institute, Federal Research Institute for Rural Areas, Forestry and Fisheries is one of 4 newly established large scale federal research institutions. It comprises the former Federal Research Centre for Fisheries, the Federal Research Centre for Forestry and Forest Products and large parts of the Federal Agricultural Research Centre. The institute is named after Johann Heinrich von Thünen, a famous national economist and social reformer of the 19th century. He developed the first serious treatment of spatial economics (the so-called Thünen rings) and the basics of the theory of the natural pay.

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Planktonic foraminiferal faunas, oxygen isotope and modern analog technique sea surface temperature records were obtained in piston core DGKS9603 (28degrees08.869'N, 127degrees16.238'E, water depth 1100 in) collected from the middle Okinawa Trough. During the last glaciation, four cold events were identified and correlate Heinrich events (HE) H2-5 of the last 45 ka. During the last deglaciation, core DGKS9603 has begun to be influenced by the Kuroshio since about 16 cal ka BP. Three weakenings of this warm current occurred at about 2.8-5.3, 11.4 and 15.5 cal ka BP respectively. Among the three fluctuations, the oldest one is synchronous with HE1 and could be a response to the strong cooling observed in the North Atlantic Ocean. The fluctuation occurring at about 11.4 cal ka ago corresponds to the Younger Dryas within the age error bars. Our observations provide new evidence that the HEs documented from Greenland and the northern North Atlantic had a global climatic impact. Changes in the intensity of the East Asian monsoon could be the main mechanism responsible for the paleoccanographic variations observed in the Okinawa Trough. (C) 2001 Elsevier Science B.V. All rights reserved.

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Cooling and sinking of dense saline water in the Norwegian–Greenland Sea is essential for the formation of North Atlantic Deep Water. The convection in the Norwegian–Greenland Sea allows for a northward flow of warm surface water and southward transport of cold saline water. This circulation system is highly sensitive to climate change and has been shown to operate in different modes. In ice cores the last glacial period is characterized by millennial-scale Dansgaard–Oeschger (D–O) events of warm interstadials and cold stadials. Similar millennial-scale variability (linked to D–O events) is evident from oceanic cores, suggesting a strong coupling of the atmospheric and oceanic circulations system. Particularly long-lasting cold stadials correlate with North Atlantic Heinrich events, where icebergs released from the continents caused a spread of meltwater over the northern North Atlantic and Nordic seas. The meltwater layer is believed to have caused a stop or near-stop in the deep convection, leading to cold climate. The spreading of meltwater and changes in oceanic circulation have a large influence on the carbon exchange between atmosphere and the deep ocean and lead to profound changes in the 14C activity of the surface ocean. Here we demonstrate marine 14C reservoir ages (R) of up to c. 2000 years for Heinrich event H4. Our R estimates are based on a new method for age model construction using identified tephra layers and tie-points based on abrupt interstadial warmings.

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O casal de suíços, Heinrich (1795–1866) e Cécile Däniker-Haller (1816–1887), com seus filhos, viveu no Rio de Janeiro entre 1828 e 1852. Comerciantes prósperos, cosmopolitas e melômanos, deixaram grande quantidade de informações sobre suas atividades de música em ambiente doméstico daquele período, mas também depois de terem voltado a se estabelecer na Suíça. O Genealogisches Archiv der Helene und Cécile Rübel Familienstiftung (FA HCR), na cidade de Zurique, documenta a história desta família. As informações registradas pelo casal estudado, principalmente em forma de cartas e diários, permitem-nos conhecer e analisar a prática musical em ambiente doméstico das famílias estrangeiras no Rio de Janeiro, e demonstrar quais eram os repertórios por eles utilizados. Entre as conclusões tiradas, inclui-se o fato de que o romantismo alemão teria feito sua entrada no ambiente musical brasileiro através dos salões musicais das famílias estrangeiras, exatamente como foi o caso em outras cidades do mundo não germânico. Nos documentos deixados pela família Däniker-Haller encontram-se os mais antigos testemunhos até hoje encontrados da execução de Lieder de Schubert em ambiente doméstico no Rio de Janeiro. Por outro lado, a prática da Hausmusik na cidade de Zurique vem descrita e comparada àquela carioca. A análise destes relatos também nos permite descrever a diferença que havia entre os eventos musicais em ambiente doméstico íntimo e informal, e os "salões musicais", onde diletantes se produziam em esfera semi-pública previamente preparados e ensaiados, e a marcante diferença no repertório destes dois tipos de eventos sociais.

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Référence bibliographique : Rol, 59545

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Màster Oficial en Construcció i Representació d'Identitats Culturals (CRIC), Curs 2008-2009, Director: Dr. Robert Caner

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