Lord Nathaniel Rothschild : der heutige Chef der Londoner Firma

Aus: Thorner Presse ; 1903, 20. Sept.

Führer durch die neuere jüdische Literatur : [1828-1928]; Jubiläumskatalog XXI der Firma M. W. Kaufmann

M. W. Kaufmann

Mitschreiben an der digitalen Welt

Wer Computerprogramme schreiben kann, gestaltet die digitale Welt mit – alle anderen sind abhaengige Konsumenten. Deshalb sollten am besten schon Kinder die Kulturtechnik des Programmierens lernen. Entscheidend ist ausserdem, dass wir ueberhaupt mitschreiben duerfen – dafuer setzen sich die verschiedenen «Open»-Bewegungen ein.

Verlags-Signet [Illustration] : (der Firma S. Calvary & Co. zum 50jährigen Jubiläum - Mai 1902 - von ihrem Personal gewidmet)

Hermann Struck

Zur Geschichte der Firma J. Kauffmann Frankfurt am Main : Eine kulturhistorische Skizze

Oscar Lehmann

Samuel Jacobs : Aus: Als die Firma verkrachte [1929]

Nathan Asch

Na 1 Nachlass Max Horkheimer, 50 - Korrespondenzen u.a. an die Firma A. L. Stamm & Co (p. I 23, 190-421)

9 Briefe und Beilage zwischen Alfred Sohn-Rethel und Max Horkheimer, 1936-1940 sowie Briefwechsel mit Joan M. Levi; 6 Briefe zwischen Joan M. Levi und Max Horkheimer, 1940; 1 Brief von Max Horkheimer an Assistac Westcent, 25.06.1937; 1 Brief von John MacMurray an Walter Adams, 19.05.1937; 1 Brief von Walter Adams an Theodor W. Adorno, 01.06.1937; 2 Briefe zwischen Charles Somlo & Co und Max Horkheimer, 06.06.1939, 12.09.139; 1 Brief von Martin Sommerfeld an Max Horkheimer, 29.05.1934; 3 Briefe von Josef Sondek an Max Horkheimer, 1937, 1942; 3 Briefe zwischen Elsa Sontheimer, Max Sontheimer und Max Horkheimer, Februar 1940, 07.03.1940; 1 Drucksache von der The Southard School an Max Horkheimer; 1 Brief von der Soziologischen Verlagsanstalt an Gertrud Janosi, 20.07.1931; 9 Briefe zwsichen Maurice J. Speiser und Max Horkheimer, 1936-1948; 2 Briefe zwischen de Spengler und Max Horkheimer, 30.11.1936, 27.01.1937; 5 Briefe zwischen Sterling D. Spero und Max Horkheimer, 1936-1937; 1 Lebenslauf von Herbert Spielberg; 1 Brief und 2 Beilagen von René A. Spitz an Max Horkheimer, 23.06.1938; 2 Briefe von Elsa Spriesterbach an Max Horkheimer, Juli 1949; 1 Brief von Ida M. Stadie an Max Horkheimer, 21.05.1937; 20 Rechnungen von A. L. Stamm & Co an Max Horkheimer, 1938-1939; 1 Brief von Rose Horkheimer an A. L. Stamm und Co, 28.09.1938; 1 Betriebsanleitung und 1 Auslieferugnsschein für Max Horkheimer vom Standard Air Conditioning, 03.03.1936; 1 Brief von Max Horkheimer an Standard Air Conditioning, 28.03.1936; 5 Briefe zwischen Taylor Starck und Max Horkheimer, 1943; 8 Briefe zwischen Hans Staudinger und Max Horkheimer, 1937, 1943; 1 Briefauszug und Beilage von Paul Stefan, 1940 sowie Briefwechsel mit Samuel R. Wachtell; 1 Brief von Samuel R. Wachtell an Gertrude Blitz, 23.10.1940; 3 Briefe zwischen Leo Löwenthal und Samuel R. Wachtell, September 1940, 23.10.1940; 1 Brief von Loe Löwenthal an Hermann Kesten, 01.10.1940; 7 Briefe und Beilage zwischen George Stefansky und Max Horkheimer, 1939-1940; 2 Briefe zwischen dem Refugee Section of the American Friends Service Committee und Max Horkheimer, 16.05.1940, 28.05.1940; 3 Briefe zwischen dem Institute of International Education und Max Horkheimer, 09.04.1940, April 1940; 1 Brief von Max Horkheimer an Friess, 01.03.1940; 1 Brief vom Institute of Sociology Malvern und Max Horkheimer, 31.01.1940; 3 Briefe zwischen Stein und Max Horkheimer, 30.11.1934, 1936, 1937; 7 Briefe von Estell A. Stein an Max Horkheimer, 1929, 1937; 1 Brief von Franz Stein an Max Horkheimer; 1 Brief von Friedrich Pollock an Gertrude R. Stein, 22.03.1939; 1 Brief von Leo Stein an Max Horkheimer, 25.07.1944; 1 Brief von Max Horkheimer an Emilia Steinacher, 20.07.1937; 4 Briefe zwischen Friedrich Steinfeld und Max Horkheimer, 1941, 1945; 1 Brief und Beilage von Eugene G. Steinhof an Max Horkheimer; 3 Briefe zwischen Ernst Steinitz und Max Horkheimer, 25.04.1938, April 1938; 2 Briefe zwischen Theodor Steltzer und Eric E. Warburg, 07.03.1948; 4 Brief zwischen Hermine Sterler und Max Horkheimer, 11.09.1939, 1939, 1941; 4 Briefe zwischen Alfred K. Stern und Max Horkheimer, 1938, 1940 sowie 1 Brief und 1 Beilage von Max Gottschalk; 1 Brief von Max Gottschalk an Max Horkheimer; 2 Briefe und 1 Beilage zwischen Erich Stern und Max Horkheimer, 26.02.1937, 17.03.1937; 2 Briefe und Beilage von Eugene I. Stern an Max Horkheimer, 1938; 2 Briefe zwischen Joseph M. Weidberg und Max Horkheimer, 15.07.1938, 29.07.1938; 1 Brief von Max Horkheimer an das Cooperative Bureau for Teachers, 03.02.1938; 12 Briefe zwischen Günther Stern und Max Horkheimer, 1936, 1938 sowie Briefwechsel mit John Guggenheim Memorial Foundation; 3 Briefe und 1 Beilage zwischen der John Simon Guggenheim Memorial Foundation und Max Horkheimer, 1937; 1 Brief vom Social Research Quarterly an Max Horkheimer, 03.01.1937; 3 Briefe zwischen Hugo Stern und Max Horkheimer, 06.12.1937, Dezember 1937;

Chlorophyll a concentration and zooplankton abundance and biomass below melting sea ice in the Amundsen Gulf

Early summer in the Arctic with extensive ice melt and break-up represents a dramatic change for sympagic-pelagic fauna below seasonal sea ice. As part of the International Polar Year-Circumpolar Flaw Lead system study (IPY-CFL), this investigation quantified zooplankton in the meltwater layer below landfast ice and remaining ice fauna below melting ice during June (2008) in Franklin Bay and Darnley Bay, Amundsen Gulf, Canada. The ice was in a state of advanced melt, with fully developed melt ponds. Intense melting resulted in a 0.3- to 0.5-m-thick meltwater layer below the ice, with a strong halocline to the Arctic water below. Zooplankton under the ice, in and below the meltwater layer, was sampled by SCUBA divers. Dense concentrations (max. 1,400 ind./m**3) of Calanus glacialis were associated with the meltwater layer, with dominant copepodid stages CIV and CV and high abundance of nauplii. Less abundant species included Pseudocalanus spp., Oithona similis and C. hyperboreus. The copepods were likely feeding on phytoplankton (0.5-2.3 mg Chl-a/m**3) in the meltwater layer. Ice amphipods were present at low abundance (<10 ind./m**2) and wet biomass (<0.2 g/m**2). Onisimus glacialis and Apherusa glacialis made up 64 and 51% of the total ice faunal abundance in Darnley Bay and Franklin Bay, respectively. During early summer, the autochthonous ice fauna becomes gradually replaced by allochthonous zooplankton, with an abundance boom near the meltwater layer. The ice amphipod bust occurs during late stages of melting and break-up, when their sympagic habitat is diminished then lost.

Absolute and relative abundances of zooplankton taxa in Kongsfjorden during 2002

Seasonal changes in the zooplankton composition of the glacially influenced Kongsfjorden, Svalbard (79°N, 12°E), and its adjacent shelf were studied in 2002. Samples were collected in the spring, summer and autumn in stratified hauls (according to hydrographic characteristics), by means of a 0.180-mm Multi Plankton Sampler. A strong front between the open sea and the fjord waters was observed during the spring, preventing water mass exchange, but was not observed later in the season. The considerable seasonal changes in zooplankton abundance were related to the seasonal variation in hydrographical regime. The total zooplankton abundance during the spring (40-2010 individuals/m**3) was much lower than in the summer and autumn (410-10,560 individuals/m**3). The main factors shaping the zooplankton community in the fjord include: the presence of a local front, advection, the flow pattern and the decreasing depth of the basin in the inner fjord. Presumably these factors regulate the gross pattern of zooplankton density and distribution, and override the importance of biological processes. This study increased our understanding of seasonal processes in fjords, particularly with regard to the strong seasonal variability in the Arctic.

Historia de empresas : PINDAPOY S.A., una firma que lideró la citricultura nacional

Fil: Palacios, Paula. Universidad Nacional de La Plata. Facultad de Humanidades y Ciencias de la Educación; Argentina.

Zooplankton and seston in the White Sea and its chemical composition

A technique of zooplankton net sampling at night in the Kandalaksha and Dvinskii Bays and during the full tide in the Onezhskii Bay of the White Sea allowed us to obtain "clean" samples without considerable admixtures of terrigenous particulates. Absence of elements-indicators of the terrigenous particulates (Al, Ti, and Zr) in the EDX spectra allows to conclude that ash composition of tested samples is defined by constitutional elements comprising organic matter and integument (chitin, shells) of plankton organisms. A quantitative assessment of accumulation of ca. 40 chemical elements by zooplankton based on a complex of modern physical methods of analysis is presented. Values of the coefficient of the biological accumulation of the elements (Kb) calculated for organic matter and the enrichment factors (EF) relative to Clarke concentrations in shale are in general determined by mobility of the chemical elements in aqueous solution, which is confirmed by calculated chemical speciation of the elements in the inorganic subsystem of surface waters of Onezhskii Bay.