Zacharias Frankel's principieller Standpunkt in der Reformfrage des Judenthums bis zum Zusammentritt der ersten Rabbiner-Versammlung in Braunschweig im Jahre 1844

Vortrag geh. ... von M. Krakauer

Ausstellung von jüdischen Bauten und Kultus-Gegenständen für Synagoge und Haus in Abbildungen und Originalen : 3. Mai bis 2. August 1908

veranst. von der Gesellschaft zur Erforschung jüdischer Kunstdenkmäler e.V. zu Frankfurt am Main

Geschichte des Volkes Israel von Anbeginn bis zur Eroberung Masada's im Jahre 72 nach Christus : in zwei Theilen

von Ferdinand Hitzig

Studien zur Geschichte der wirtschaftlichen und sozialen Verhältnisse im israelisch-jüdischen Reiche : von der Einwanderung in Kanaan bis zum babylonischen Exil

von M. Lurje

Geschichte Ezra's und der Heiligherrschaft in Israel bis Christus

Diese Ausg. ist im Freimann-Kat. nicht enthalten

Auswahl historischer Stücke aus hebräischen Schriftstellern vom zweiten Jahrhundert bis auf die Gegenwart : für Theologen und Historiker, so wie zum Gebrauch in höheren jüdischen Lehranstalten ; mit vokalisirtem Texte, deutscher Übers. u. Anm.

[Verf.: Josef Zedner]

A chrysophyte-based quantitative reconstruction of winter severity from varved lake sediments in NE Poland during the past millennium and its relationship to natural climate variability

Chrysophyte cysts are recognized as powerful proxies of cold-season temperatures. In this paper we use the relationship between chrysophyte assemblages and the number of days below 4 °C (DB4 °C) in the epilimnion of a lake in northern Poland to develop a transfer function and to reconstruct winter severity in Poland for the last millennium. DB4 °C is a climate variable related to the length of the winter. Multivariate ordination techniques were used to study the distribution of chrysophytes from sediment traps of 37 low-land lakes distributed along a variety of environmental and climatic gradients in northern Poland. Of all the environmental variables measured, stepwise variable selection and individual Redundancy analyses (RDA) identified DB4 °C as the most important variable for chrysophytes, explaining a portion of variance independent of variables related to water chemistry (conductivity, chlorides, K, sulfates), which were also important. A quantitative transfer function was created to estimate DB4 °C from sedimentary assemblages using partial least square regression (PLS). The two-component model (PLS-2) had a coefficient of determination of View the MathML sourceRcross2 = 0.58, with root mean squared error of prediction (RMSEP, based on leave-one-out) of 3.41 days. The resulting transfer function was applied to an annually-varved sediment core from Lake Żabińskie, providing a new sub-decadal quantitative reconstruction of DB4 °C with high chronological accuracy for the period AD 1000–2010. During Medieval Times (AD 1180–1440) winters were generally shorter (warmer) except for a decade with very long and severe winters around AD 1260–1270 (following the AD 1258 volcanic eruption). The 16th and 17th centuries and the beginning of the 19th century experienced very long severe winters. Comparison with other European cold-season reconstructions and atmospheric indices for this region indicates that large parts of the winter variability (reconstructed DB4 °C) is due to the interplay between the oscillations of the zonal flow controlled by the North Atlantic Oscillation (NAO) and the influence of continental anticyclonic systems (Siberian High, East Atlantic/Western Russia pattern). Differences with other European records are attributed to geographic climatological differences between Poland and Western Europe (Low Countries, Alps). Striking correspondence between the combined volcanic and solar forcing and the DB4 °C reconstruction prior to the 20th century suggests that winter climate in Poland responds mostly to natural forced variability (volcanic and solar) and the influence of unforced variability is low.

Beiträge zur neueren jüdischen Wirtschaftsgeschichte : die Juden in Halberstadt u. Umgebung bis zur Emanzipation

von Max Köhler

Local formation of varved sediments in a karstic collapse depression of Lake Banyoles (NE Spain)

Banyoles is the largest and deepest lake of karstic-tectonic origin in the Iberian Peninsula. The lake comprises several circular sub-basins characteri- zed by different oxygenation conditions at their hypolimnions. The multiproxy analysis of a > 5 m long sediment core combined with high resolution seis- mic stratigraphy (3.5 kHz pinger and multi-frequency Chirp surveys), allow a precise reconstruction of the evolution of a karstic depression (named B3) until present times. Local meromictic conditions in this sub-basin have been conducive to deposition and preservation of ca. 85 cm of varved sediments since the late 19th century. The onset of these conditions is likely related to lake waters eutrophication caused by increasing farming activities in the wa- tershed. Increasing clastic input and organic productivity during the second half of the 20th century have also been recorded within the laminated sedi- ments, revealing an intensification of human impact and warmer water tem- peratures.

Die Staats- und Privat-Lotterie- oder Prämien-Anleihen in übersichtlicher Zusammenstellung : mit den Verlosungsplänen und den bis auf die neueste Zeit geordneten Verzeichnissen der gezogenen Serien oder Lose; ein unentbehrliches Hülfsbuch ...

von H. Marcus

Die Millionärs-Wirthschaft auf dem Frankfurter Rathhause : ein Rückblick für die Stadtverordnetenwahlen auf der städtischen Verwaltung in den Jahren 1900 bis 1904

von O. Zielowski

Verbindungen von Juden in Deutschland mit denen in Babylonien und Palästina während des Mittelalters bis zum ersten Kreuzzuge

Aaron Freimann

Geschichte der hebräischen Typographie in Polen : ihre Entstehung im Jahre 1534 und Entwicklung bis zur Gegenwart nach archivalischen und historischen Quellen ; nebst Nachtrag zum bibliographischen Lexikon "Bet eked sepharim"/ bearb. von B. Friedberg

Nebent.: Histoire de la typographie hébraïque in Pologne