Die Feste des Herrn : israelitische Predigten für alle Festtage des Jahres, gehalten in dem neuen Tempel zu Hamburg

von E. Kley

Die göttliche Erziehung in unserm Leben : Predigt über 5 Mos. 8, 5, am 12. Juni 1841 (23. Sivan 5601), als am Sabbath nach der Grundsteinlegung zum neuen, von Herrn Salomon Heine zum Gedaechtnisse seiner Gattin, der sel. Frau Betty Heine, gestifteten israelitischen Krankenhause ; gehalten im Neuen Israelitischen Tempel zu Hamburg

von N. Frankfurter

Der Hamburger Tempel : zum 70jährigen Denktage seiner Begründung (18. October 1818) ; Zwei Kanzelreden gehalten im Israelitischen Tempel zu Hamburg am 20. October und 3. November 1888 ; nebst Beigabe der früher erschienenen Rede über Gotthold Salomon

von David Leimdörfer

Ordnung der öffentlichen Andacht für die Sabbath- und Festtage des ganzen Jahres : nach dem Gebrauche des Neuen-Tempel-Vereins in Hamburg

hrsg. von S. I. Fränkel und M. I. Bresselau

Der Kaiser - in der Bibel : Kriegspredigt 1916 ; Zur Feier des Geburtstages Sr. Majestät Kaiser Wilhelms II. ; 27. Jan. 1916, gehalten im Israelitischen Tempel zu Hamburg

von D. Leimdörfer

Der Brand von Hamburg vom 5. bis 8. Mai 1842 : Schilderung der Feuersbrunst ; mit den nöthigen historischen, topographischen und statistischen Nachweisungen über die vernichteten Straßen u. Staatsgebäude

von G. W. Mit einem Plane von Hamburg, ... so wie auch 13 ... Ansichten der wichtigsten Häuser, Kirchen und Stadtteile, als das Rathaus, ... und einer Hauptansicht von Hamburg vom Jungfernstieg ...

Jüdisches Gemeindeblatt für das Gebiet der Hansestadt Hamburg

Online-Ressource

Nib Sefataim : dreißig Predigten gehalten während des jüdischen Kalenderjahres 5629, im israelitischen Tempel zu Hamburg

von Dr. H. Jonas

"Fremd bin ich bei Euch und heimisch, gebt mir Besitz, meinen Todten zu begraben." : Predigt am Sabbath: חיי שרה [Ḥaye Śarah] im neuen Isr. Tempel in Hamburg

von Schwabacher

Sammlung der neuesten Predigten gehalten in dem neuen Israelitischen Tempel zu Hamburg : Predigten in dem neuen Israelitischen Tempel [Erstes Heft ; Zweites Heft]

gehalten von Eduard Kley. Hrsg. von Ed. Kley und G. Salomon

Hamburgisches Kochbuch oder vollständige Anweisung zum Kochen, insonderheit für Hausfrauen in Hamburg und Niedersachsen

verf. von einigen Frauenzimmern in Hamburg

Compilation of Thunnus thynnus (bluefin tuna) catche in the Northeast Atlantic Ocean 1906-1949

The data have been extracted and compiled from various sources but mainly from the ICES data base. The ICES data are from catch databases downloaded from the ICES website on 2014-01-14. These data are resolved by ICES area, country and year. During inspection of these data, it was noted that Norwegian data for years before 1950 had not been entered into the catch database on the ICES website. ICES has been notified of this omission by B. R. MacKenzie. The Norwegian data from ICES Bulletins. Statistiques has been added. Additional historical bluefin tuna catch data from other fishery reports and sources have been included in the data file for years preceding those when countries started reported their landings officially to ICES. These additional data have been reported in the literature previously (MacKenzie and Myers 2007, Fisheries Research).

Biogenic and mineral composition and foraminiferal stratigraphy of sediment cores obtained in northern Germany

The Ratekau boring ended in clays of the so-called Asterigerina-Zone; these clays have shallow-water features in the uppermost samples. The clays are overlain by deep-water clays with pteropods; this formation is split into two parts by a shallow-water deposit. The fossiliferous series ends upward in sandy deposits with shallow-water fossils. The question is raised whether the two deep-water deposits might correspond to the Lower Doberg Beds (Eochattian) and the Upper Doberg Beds (Neochattian) at the Doberg hill, closer to the rim of the basin. All fossiliferous samples from this boring are thought to be of Late Oligocene age; the boundary towards the Middle Oligocene, however, could not be ascertained. The Vaale boring ended in rather typical Septaria clay of the Middle Oligocene. This clay is capped by some metres of unfossiliferous glauconite clays, which in turn are overlain by silts and silty clays with planktonic fossils identical to those found at Dingden locality. These deposits are tentatively dated as Early Miocene. The next higher series of samples consists of sands and clays deposited in shallower waters. They contain a rich fauna of benthic molluscs, which, according to the current notion in stratigraphy, would have a Reinbek Age. In addition, they contain a set of planktonic fossils which differs from the 'Lower Miocene' assemblages. These sands and clays are overlain by a thick series of marine sands very poor in fossils. Finally, four metres of clay with foraminifera, having Younger Miocene affinities, form the top of the fossiliferous sequence. The borings at Wulksfelde and Langenhorn were not far apart and their sediments are easily correlated. Both wells start below in continental 'Lignite Sands' and contain overlying shallow water sands and clays. These yielded Hemmoor benthic mollusca, supposed to indicate Lower Miocene in the relevant literature; however, we encountered their planktonic foraminifera in the uppermost Miocene as well. The same planktonic species were found in all samples of both borings. These deposits under discussion furthermore contain a particular pteropod species. They are overlain by a thick series of gypsiferous clays, with scarce fossils. The uppermost fossiliferous clays (probably Langenfelde Age) contain another pteropod species, not met with in other samples. The discrepancies between the plankton zonation and the traditional subdivision according to benthic molluscs in the borings of Vaale, Wulksfelde and Langenhorn (and in samples from Twistringen, Dingden and Antwerp localities as well) renders the time-stratigraphic value of the denominations Reinbek and Hemmoor rather doubtful. The samples of the Westerland boring can be placed in the Gram and Sylt stages of local chronostratigraphy on the strength of the Astarte series established by HINSCH. The Gram samples contain a typical pteropod species; both groups of samples contain the same planktonic foraminifera as the borings Wulksfelde and Langenhorn. Our material did not bring the problem of the Miocene-Pliocene boundary in this region any closer to a solution. In conclusion, it can be claimed that this investigation provides strong arguments that the usual recognition of Hemmoor and Reinbek does not correspond to well-defined chronostratigraphical units. A better chronostratigraphic subdivision has to be based on the examination of many more samples, and on a better understanding of the paleoecology of the fossils involved.