Hineh mah-tov u-mah-naʿim : Psalm 133 ; für Männerchor, Harmonium- und Pianoforte-Begleitung

componirt von Ed. Birnbaum

Bundeslied : [nach Psalm 133] ; für israelitische Cantoren

comp. ... von Adolph Schönfeld

Bundeslied : [nach Psalm 133]

comp. von A. Schönfeld

Ms. hebr. oct. 133 - [Sammelband in 6 Teilen: Handschriftenkonvolut]

Vorbesitzer: Abraham Merzbacher

Ms. Barth. 133 - Medizinische Sammelhandschrift

Vorbesitzer: Bartholomaeusstift Frankfurt am Main

Na 50 Nachlass Arthur Schopenhauer - 'Schopenhauer-Archiv', 812 - Erfahrungsbericht über naturwissenschaftliche Experimente

u.a. Verbrennungen als Folge eines Unfalls; Europareisen; Konfirmation; Fahrt nach Montpellier;

Na 50 Nachlass Arthur Schopenhauer - 'Schopenhauer-Archiv', 133 - Mitteilung über die Predigt zur Tierethik

u.a.: Parerga und Paralipomena; Tierethik; Anschaffung von Schopenhauers Veröffentlichungen in die Bibliothek Wiesbaden;

Ms. Praed. 133 - Sermones de sanctis

Vorbesitzer: Dominikanerkloster Frankfurt am Main

Ms.Ff.F.Stoltze 3. 133 - Brief von Otto Hörth an Lyda Stoltze

Stoltze: Biographie, Carl Rößler, Johannes Proelß, Verlag Keller

Na 1 Nachlass Max Horkheimer, 504 - Korrespondenzen mit Theodor W. Adorno (p. VI 1B, 133 - 295)

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;

Ms. lat. oct. 133 - Psalterium non feriatum

Vorbesitzer: Freiherren von Holzhausen

Ms. or. 133 - Theologische Sammelhandschrift

Vorbesitzer: Negus Hezkejas; Eduard Rüppell

Inc. fol. 133 (Ausst. 172) - [Sammelband in 3 Teilen: Konvolut aus Inkunabeln]

Vorbesitzer: Michael Paul Baumhauer (Schenkungsvermerk im Vorderdeckel)

Ms. lat. qu. 133 - Quaestiones philosophicae

Vorbesitzer: Bernhard Waldschmidt

Granulometry of two sediment cores from Maxwell Bay, South Shetland Islands, West Antarctica

The climate evolution of the South Shetland Islands during the last c. 2000 years is inferred from the multiproxy analyses of a long (928 cm) sediment core retrieved from Maxwell Bay off King George Island. The vertical sediment flux at the core location is controlled by summer melting processes that cause sediment-laden meltwater plumes to form. These leave a characteristic signature in the sediments of NE Maxwell Bay. We use this signature to distinguish summer and winter-dominated periods. During the Medieval Warm Period, sediments are generally finer which indicates summer-type conditions. In contrast, during the Little Ice Age (LIA) sediments are generally coarser and are indicative of winter-dominated conditions. Comparison with Northern and Southern Hemisphere, Antarctic, and global temperature reconstructions reveals that the mean grain-size curve from Maxwell Bay closely resembles the curve of the global temperature reconstruction. We show that the medieval warming occurred earlier in the Southern than in the Northern Hemisphere, which might indicate that the warming was driven by processes occurring in the south. The beginning of the LIA appears to be almost synchronous in both hemispheres. The warming after the LIA closely resembles the Northern Hemisphere record which might indicate this phase of cooling was driven by processes occurring in the north. Although the recent rapid regional warming is clearly visible, the Maxwell Bay record does not show the dominance of summer-type sediments until the 1970s. Continued warming in this area will likely affect the marine ecosystem through meltwater induced turbidity of the surface waters as well as an extension of the vegetation period due to the predicted decrease of sea ice in this area.