992 resultados para Hebrew imprints
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J.Janathanson
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A.Schorr
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A.Schorr
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Cantor Josef Rosenblatt
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A.Schor
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B.Thomashevsky
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A.Goldfaden
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by S. Schechter
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Vorbesitzer: Hebrew Union College Library, Cincinnati, O.;
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transl. from the original and annotated by M. Friedlander
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133 Briefe zwischen Max Horkheimer und Margot von Mendelssohn; 2 Briefe zwischen Margot von Mendelssohn und Western Defense Command and Fourth Army (San Francisco), 1942; 1 Briefe an die Wartime Civil Control (San Francisco) von Margot von Mendelssohn, 1.12.1942; 1 Brief von Max Horkheimer an die Wartime Civil Control (San Francisco), [1942]; 3 Briefe an das Police Department (West Los Angeles) von Max Horkheimer, 1942; 1 Brief von Margot von Mendelssohn an L. M. Newberry, 03.09.1942; 1 Brief an L. M. Newberry von Max Horkheimer, 31.08.1942; 1 Brief von Max Horkheimer an U. S. Attorney (Los Angeles), 16.06.1942; 1 Brief von der Hebrew Sheltering and Immigrant Aid Society (New York) an Max Horkheimer, 29.10.1941; 1 Brief an das Department of State (Washington D. C.) von F. Pollock, 30.07.1941; 1 Brief von Leo Löwenthal an das Department of State (Washington D. C.), 28.07.1941;
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El judaísmo tardío y posteriormente el cristianismo incursionaron frecuentemente en el célebre pasaje de Éx. 3, 14, entendiéndolo como la revelación del Nombre divino a Moisés. Las respectivas influencias de la ontología griega y de la Septuaginta que traduce el citado texto hebreo por “Yo Soy el que Soy" (ejgwv eijmi oJ w[n), se hicieron presentes en la tradición cristiana desde sus orígenes hasta la Escolástica del siglo XIII. Sea con matices esencialistas o de carácter existencial, el Dios bíblico ha sido comprendido como “Ser" en distintos momentos del cristianismo medieval. Este alejamiento de la intuición bíblica originaria en dirección a una concepción helénica del Ser, produjo notables consecuencias en la imagen de Dios sostenida por los cristianos.
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Based on the study of 10 sediment cores and 40 core-top samples from the South China Sea (SCS) we obtained proxy records of past changes in East Asian monsoon climate on millennial to bidecadal time scales over the last 220,000 years. Climate proxies such as global sea level, estimates of paleotemperature, salinity, and nutrients in surface water, ventilation of deep water, paleowind strength, freshwater lids, fluvial and/or eolian sediment supply, and sediment winnowing on the sea floor were derived from planktonic and benthic stable-isotope records, the distribution of siliciclastic grain sizes, planktonic foraminifera species, and the UK37 biomarker index. Four cores were AMS-14C-dated. Two different regimes of monsoon circulation dominated the SCS over the last two glacial cycles, being linked to the minima and maxima of Northern Hemisphere solar insolation. (1) Glacial stages led to a stable estuarine circulation and a strong O2-minimum layer via a closure of the Borneo sea strait. Strong northeast monsoon and cool surface water occurred during winter, in part fed by an inflow from the north tip of Luzon. In contrast, summer temperatures were as high as during interglacials, hence the seasonality was strong. Low wetness in subtropical South China was opposed to large river input from the emerged Sunda shelf, serving as glacial refuge for tropical forest. (2) Interglacials were marked by a strong inflow of warm water via the Borneo sea strait, intense upwelling southeast of Vietnam and continental wetness in China during summer, weaker northeast monsoon and high sea-surface temperatures during winter, i.e. low seasonality. On top of the long-term variations we found millennial- to centennial-scale cold and dry, warm and humid spells during the Holocene, glacial Terminations I and II, and Stage 3. The spells were coeval with published variations in the Indian monsoon and probably, with the cold Heinrich and warm Dansgaard-Oeschger events recorded in Greenland ice cores, thus suggesting global climatic teleconnections. Holocene oscillations in the runoff from South China centered around periodicities of 775 years, ascribed to subharmonics of the 1500-year cycle in oceanic thermohaline circulation. 102/84-year cycles are tentatively assigned to the Gleissberg period of solar activity. Phase relationships among various monsoon proxies near the onset of Termination IA suggest that summer-monsoon rains and fluvial runoff from South China had already intensified right after the last glacial maximum (LGM) insolation minimum, coeval with the start of Antarctic ice melt, prior to the d18O signals of global sea-level rise. Vice versa, the strength of winter-monsoon winds decreased in short centennial steps only 3000-4000 years later, along with the melt of glacial ice sheets in the Northern Hemisphere.