939 resultados para 133-818
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comp. ... von Adolph Schönfeld
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comp. von A. Schönfeld
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Vorbesitzer: Abraham Merzbacher
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Vorbesitzer: Bartholomaeusstift Frankfurt am Main
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u.a.: Parerga und Paralipomena; Tierethik; Anschaffung von Schopenhauers Veröffentlichungen in die Bibliothek Wiesbaden;
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Vorbesitzer: Dominikanerkloster Frankfurt am Main
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Stoltze: Biographie, Carl Rößler, Johannes Proelß, Verlag Keller
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Briefwechsel und Beilagen zwischen Max Horkheimer, Theodor W. Adorno und Gretel Adorno, 1942 - 1944; 1 Brief von Friedrich Pollock an Theodor W. Adorno, 1942; 1 Brief von Theodor W. Adorno an Friedrich Pollock, 1944; 1 Brief von Else Frenkel-Brunswick an Theodor W. Adorno, 1944; 1 Brief von Max Horkheimer an das American Jewish Commitee, 1944; Briefwechsel und Beilagen zwischen Gretel Adorno, Theodor W. Adorno und Frederick Wild, 1942 - 1944; 1 Brief von Gretel Adorno an Leo Löwenthal, 1944; 1 Brief von Monroe E. Deutsch an Theodor W. Adorno, 1944; Briefwechsel zwischen Theodor W. Adorno und Margot von Mendelssohn, 1942 - 1943; 1 Brief von der Bank of America in Los Angeles an Frederick Wild, 1942;
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Vorbesitzer: Freiherren von Holzhausen
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Vorbesitzer: Negus Hezkejas; Eduard Rüppell
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Vorbesitzer: Michael Paul Baumhauer (Schenkungsvermerk im Vorderdeckel)
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Vorbesitzer: Bernhard Waldschmidt
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Geochemical and mineralogical proxies for paleoenvironmental conditions have the underlying assumption that climate variations have an impact on terrestrial weathering conditions. Varying properties of terrigenous sediments deposited at sea are therefore often interpreted in terms of paleoenvironmental change. Also in gravity core GeoB9307-3 (18° 33.99' S, 37° 22.89' E), located off the Zambezi River, environmental changes during Heinrich Stadial 1 (HS 1) and the Younger Dryas (YD) are accompanied by changing properties of the terrigenous sediment fraction. Our study focuses on the relationship of variability in the hydrological system and changes in the magnetic properties, major element geochemistry and granulometry of the sediments. We propose that changes in bulk sedimentary properties concur with environmental change, although not as a direct response of climate driven pedogenic processes. Spatial varying rainfall intensities on a sub-basin scale modify sediment export from different parts of the Zambezi River basin. During humid phases, such as HS 1 and the YD, sediment was mainly exported from the coastal areas, while during more arid phases sediments mirror the hinterland soil and lithological properties and are likely derived from the northern Shire sub-basin. We propose that a de-coupling of sedimentological and organic signals with variable discharge and erosional activity can occur.