989 resultados para 130-803A


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BACKGROUND: Microsomal transfer protein inhibitors (MTPi) have the potential to be used as a drug to lower plasma lipids, mainly plasma triglycerides (TG). However, studies with animal models have indicated that MTPi treatment results in the accumulation of hepatic TG. The purpose of this study was to evaluate whether JTT-130, a unique MTPi, targeted to the intestine, would effectively reduce plasma lipids without inducing a fatty liver. METHODS: Male guinea pigs (n = 10 per group) were used for this experiment. Initially all guinea pigs were fed a hypercholesterolemic diet containing 0.08 g/100 g dietary cholesterol for 3 wk. After this period, animals were randomly assigned to diets containing 0 (control), 0.0005 or 0.0015 g/100 g of MTPi for 4 wk. A diet containing 0.05 g/100 g of atorvastatin, an HMG-CoA reductase inhibitor was used as the positive control. At the end of the 7th week, guinea pigs were sacrificed to assess drug effects on plasma and hepatic lipids, composition of LDL and VLDL, hepatic cholesterol and lipoprotein metabolism. RESULTS: Plasma LDL cholesterol and TG were 25 and 30% lower in guinea pigs treated with MTPi compared to controls (P < 0.05). Atorvastatin had the most pronounced hypolipidemic effects with a 35% reduction in LDL cholesterol and 40% reduction in TG. JTT-130 did not induce hepatic lipid accumulation compared to controls. Cholesteryl ester transfer protein (CETP) activity was reduced in a dose dependent manner by increasing doses of MTPi and guinea pigs treated with atorvastatin had the lowest CETP activity (P < 0.01). In addition the number of molecules of cholesteryl ester in LDL and LDL diameter were lower in guinea pigs treated with atorvastatin. In contrast, hepatic enzymes involved in maintaining cholesterol homeostasis were not affected by drug treatment. CONCLUSION: These results suggest that JTT-130 could have potential clinical applications due to its plasma lipid lowering effects with no alterations in hepatic lipid concentrations.

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Vorbesitzer: Bartholomaeusstift Frankfurt am Main

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33 Briefe zwischen Julius S. Bach und Max Horkheimer, 1937-1941; 1 Brief von Julius S. Bach an Mary von Meldelsohn, 28.08.1940; 24 Briefe zwischen Richard Bach und Max Horkheimer, 1938-1940; 1 Abschrift eines Briefes von Oscar W. Gross an Emil de Leuw, 1938; 1 Brief von A. Bailer an Mr. Iggersheimer, 01.05.1940; 1 Brief von Max Horkheimer an Bailliere, Tindall & Cox London, 05.07.1949; 1 Brief von Beatrix Baird an Max Horkheimer; 5 Briefe zwischen Leonard Balet und Max Horkheimer, 1938-1949; 2 Briefe zwischen John Simon Guggenheim Memorial Foundation New York und Max Horkheimer, 22.11.1948, 05.01.1949; 1 Brief von W. H. de Graaff, Ladislaus Bálint an Max Horkheimer, 11.05.1938; 6 Briefe zwischen Bank of Manhattan Company New York und Max Horkheimer, 1934-1935; 6 Briefe zwischen Ladislaus Bálint und Max Horkheimer, 1934-1935; 2 Briefe zwischen der Bank of the Manhatten Company in New York und Max Horkheimer, 14./15.11.1934; 5 Briefe zwischen der Bankers Trust Company und Max Horkheimer, 1934; 1 Brief von R. Bárány an Max Horkheimer, 05.05.1933; 5 Briefe zwischen Hans Baron und Max Horkheimer, 1936; 3 Briefe zwischen Salo W. Baron und Max Horkheimer, 1941-1942, 16.04.1940; 1 Brief zwischen A. Barratt Brown und Max Horkheimer, 01.10.1936;

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2 Briefe zwischen Marga Wadsack und Max Horkheimer, 24.08.1937, 29.08.1937; 1 Brief von Gloria H. Wagner an Max Horkheimer, 27.12.1948; 1 Brief von Herta Wagner an Leo Löwenthal, 05.06.1936; 3 Brief und 1 Beilage zwischen Herta Wagner, 12.03.1936, 1936; 8 Brief zwischen Katja Walch-Lux und Max Horkheimer, 1934-1938; 2 Brief zwischen K. Walcher und Max Horkheimer, 07.08.1936, 04.09.1936 sowie Bemerkungen zum Brief von Max Horkheimer; 2 Briefe zwischen Morris Waldman und Max Horkheimer, 17.04.1940, 11.05.1940; 6 Briefe zwischen Sidney Wallach und Max Horkheimer, 1940; 2 Briefe von Max Horkheimer an Waldman; 2 Briefe von Max Horkheimer an Landau; 1 Brief Max Horkheimer an Warburg; 1 Brief von Hans Wallenberg an Leo Löwenthal, 06.05.1940; 1 Brief von Willard W. Waller an Franz Neumann, 28.04.1941; 2 Briefe und 1 Beilage zwischen Hans Waloschek und Max Horkheimer, 04.08.1938, 31.08.1938; 4 Briefe und 2 Beilagen zwischen Emil J. Walter und Max Horkheimer, 1937, 1938; 5 Briefe und 1 Beilage zwischen Hilde Walter und Max Horkheimer, 1937, 1945; 1 Brief von Rose Walter an Max Horkheimer, 16.11.1938; 2 Briefe zwischen Yu-Chuan Wang und Max Horkheimer, 12.10.1936, 09.12.1936; 1 Brief von Rike Wankmüller-Freyh an Max Horkheimer, 06.07.1949; 1 Brief von Ilse Bach an Heinz Wartenberg, 11.11.1940; 1 Brief von Heinz Wartenberg an Richard Bach, 07.02.1941; 1 Brief von Max Horkheimer an Heinz Wartenberg, 11.03.1941; 1 Brief von Richard Bach an Max Horkheimer; 1 Brief von Franz und Hilde Wasem an Max Horkheimer, 16.02.1949; 5 Briefe zwischen Goodwin Watson und Franz Neumann, 1941; 11 Briefe und Notizen zwischen Julien Wavrinek und Max Horkheimer, 1938-1940; 1 Brief von Max Horkheimer an M. Bruhat; 2 Briefe von Max Horkheimer an Walter Benjamin, 03.05.1940;

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1 Brief von Max Horkheimer an Pierre van Paassen, 31.01.1944; 1 Brief von Max Horkheimer an Frederick M. Padelford, 25.03.1941; 1 Exposé und Beilage von Karl O. Paetel sowie sowie Briefwechsel mit Karl A. Wittfogel; 2 Briefe zwischen Karl A. Wittfogel und Margot von Mendelssohn, 01.06.1941, 04.06.1941; 2 Briefe von Max Horkheimer an D. D. Paige, August 1944; 2 Briefe zwischen Maria Pape und Max Horkheimer, 23.07.1949, 29.07.1949; 1 Brief von Fritz Pappenheim an Max Horkheimer, 11.03.1939; 2 Briefe zwischen Claire Patek-Hohenadl und Max Horkheimer, 18.02.1945, 02.03.1945; 4 Briefe zwischen Wilhelm Pauck und Max Horkheimer, 1938; 2 Briefe von Max Horkheimer an Thomas Peardon, September 1941; 2 Briefe zwischen Christine Peck und Max Horkheimer, 01.02.1944, 16.02.1944; 2 Briefe zwischen Alexander H. Pekelis und Max Horkheimer, 20.10.1941, 29.10.1941; 4 Briefe zwischen Pendle Hill Wallingford und Max Horkheimer, 21.05.1940, 1940; 1 Einladung von The People Lobby an Max Horkheimer, April 1937; 1 Brief von Franz L. Neumann an Selig Perlman, 08.10.1941; 2 Briefe zwischen Florence Pfleger und Max Horkheimer, 30.10.1944, 06.11.1944; 2 Briefe zwischen The Philharmonic-Symphony Society of New York und Max Horkheimer, 11.06.1936, 22.06.1936; 2 Briefe zwischen Philosophical Library New York und Max Horkheimer, 09.09.1941; 2 Briefe von Max Horkheimer an Donald A. Piatt, Oktober 1940; 1 Brief von Max Horkheimer an Alfred Pinkus, 27.08.1942; 20 Briefe und Beilage zwischen Kurt Pinthus und Max Horkheimer, 1940-1942; 1 Brief von Friedrich Pollock an das American Consul General Berlin, 20.05.1941; 1 Brief von Friedrich Pollock an den National Refugee Service New York, 30.04.1941; 4 Briefe zwischen The Emergency Committee in Aid of Displaced Foreign Scholars, New York und Friedrich Pollock, 27.09.1940-1941; 1 Brief von Max Horkheimer an John Simon Guggeheim von der Memorial Foundation, 08.11.1940; 3 Brief zwischen Robert Plank und Max Horkheimer, 12.07.1944, 1944; 4 Briefe und 1 Beilage zwischen Richard S. Plant und Max Horkheimer, Januar 1939; 2 Briefe zwischen Caroline S. Platt und Max Horkheimer, 06.05.1942, 08.05.1942; 1 Brief und 2 Beilagen vom Pledge for Peace Committee New York an Max Horkheimer, 10.04.1944; 1 Brief vom Popular Publications, Inc. New York an Mein, 23.10.1939; 2 Briefe von Else Heim an die Popular Publikations, Inc. New York, 1939; 1 Brief und 1 Beilage von Frederick Pollock an Leonard Powers, 03.06.1941; 2 Briefe zwischen S. Pressburger udn Max Horkheimer, 18.06.1939, 05.07.1939; 2 Briefe zwsichen dem Preston Hotel, Swampscott und Max Horkheimer, 28.04.1937, 08.05.1937; 1 Brief von Lucio José F. Weil an das Preston Hotel, Swampscott, 25.06.1936; 5 Briefe zwischen F. V. Preve und Max Horkheimer, 1937; 4 Briefe zwischen Rena Proulx und Max Horkheimer, 1934, 1937; 2 Briefe zwischen dem Psychatry Journal of the Biology and the Pathology of Interpersonal Relations Washington und Max Horkheimer, 21.08.1939, 11.09.1939;

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u.a.: Empfehlung zur Veröffentlichung der Schopenhauerschen Fragmente zur Geschichte der Philosophie; Trendelenburg; Friedrich Schleiermacher;

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Vorbesitzer: Dominikanerkloster Frankfurt am Main

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Texte für die Frankfurter Latern, Prozeß (Delbrück)

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Vorbesitzer: P.O.D.; M.A.; Courtois Curé de Cauvigny; Freiherrl. Carl von Rothschild'sche Bibliothek Frankfurt am Main

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This dataset characterizes the evolution of western African precipitation indicated by marine sediment geochemical records in comparison to transient simulations using CCSM3 global climate model throughout the Last Interglacial (130-115 ka). It contains (1) defined tie-points (age models), newly published stable isotopes of benthic foraminifera and Al/Si log-ratios of eight marine sediment cores from the western African margin and (2) annual and seasonal rainfall anomalies (relative to pre-industrial values) for six characteristic latitudinal bands in western Africa simulated by CCSM3 (two transient simulations: one non-accelerated and one accelerated experiment).

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The Neogene biostratigraphy presented here is based on the study of 230 samples through 737 m of pelagic sediment in Hole 806B. Sediment accumulation is interrupted only once in the uppermost lower Miocene (Zone N6), apparently coincident with a widespread deep-sea hiatus. Preservation of planktonic foraminifers through the section ranges from good to moderately poor. One hundred and ten species of planktonic foraminifers were identified; taxonomic notes on most species are included. All of the standard low-latitude Neogene foraminiferal zones are delineated, with the exceptions of Zones N8 and N9 because of a high first occurrence of Orbulina, and Zones N18 and N19 because of a high first occurrence of Sphaeroidinella dehiscens. Good agreement exists between the published account of the variation in planktonic foraminiferal species richness and the rates of diversification and turnover, and measurements of these evolutionary indexes in the record of Hole 806B. The global pattern of change in tropical/transitional species richness is paralleled in Hole 806B, with departures caused by either ecological conditions peculiar to the western equatorial Pacific or by inexactness in the estimation of million-year intervals in Hole 806B. Temporal changes in the relative abundance of taxa in the sediment assemblages, considered in light of their depth habitats, reveal a detailed picture of historical change in the structure of the upper water column over the Ontong Java Plateau. The dominance of surface dwellers (Paragloborotalia kugleri, P. mayeri, Dentoglobigerina altispira, Globigerinita glutinata, and Globigerinoides spp.) throughout the lower and middle Miocene is replaced by a more equitable distribution of surface (D. altispira and Globigerinoides spp.), intermediate (Globorotalia menardii plexus), and deep (Streptochilus spp.) dwellers in the late Miocene, following the closing of the Indo-Pacific Seaway and the initiation of large-scale glaciation in the Antarctic. The shoaling of the thermocline along the equator engendered by these climatic and tectonic events persisted through the Pliocene, when initial increases in the abundance of a new set of shallow, intermediate, and deep dwelling species of planktonic foraminifers coincide with the closing of the Panamanian Seaway.

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We present the first continuous records from 0 to 5 Ma (in 0.333 m.y. integrated time steps) of paired boron/calcium (B/Ca) ratios and boron isotopes (d11B) in the planktonic foraminifera Globogerinoides sacculifer (without sacc) from a site in the western equatorial Pacific Ocean (Ocean Drilling Program Site 806). These measurements, the first made in conjunction with calcification temperature (magnesium/calcium ratios) and average shell mass measurements, indicate that pH is not the sole environmental variable controlling B in planktonic foraminiferal calcite. Our data are consistent with calcification temperature exerting a primary control on B concentration and isotopic composition in planktonic foraminifera. If so, calcification temperature must be taken into account if pH for past oceans and atmospheric pCO2 are to be estimated from B isotope measurements in foraminiferal calcite. Doing so will substantially increase the uncertainty of pH estimates. Although this work was designed as a temporal study, its results define new aspects of calibrating the d11B paleo-pH tracer.