Abconterfetung, deß Ehrwürdigen Hocherleuchten Theuren Mann Gottes vnd Teutschen Propheten, Herrn Doctor Martin Luther : Ein Christliches Gebet vor die Jugendt, auff das Evangelische JubelJahr, den 1. vnd 2. Novemb. 1617

Bibliograph. Nachweis: Paas P-308; Straus (1600/1700), Nr. 135

Fürtrefflicher Ritter-Kampf, Der zweyen Neapolitanischen Fürsten D. Francesco Carafa de Noja und D. Guilio Antonio Aquaviva de Aragona : am 5., 15. Novemb. 1673

Bibliograph. Nachweis: VD 17 1:620759R; Drugulin 2845

Warhafftige Abbildung und Beschreibung, Deß grossen und gewaltigen Treffens, welches bey den Chur- Sächsischen Stättlein Lützen, zwischen der Catholischen Liga Generalen Fürst von Friedland, und Graf von Pappenheim, an einem, und der Königl. Majest. in Schweden, auch Hertzog von Weinmar andern theils, den 5. und 6. Novembris deß 1632. Jahrs, vorgangen, kürtzlich beschrieben

Mit Porträtmedaillons von Gustaf Adolf und dem sächsischen Herzog Bernhard

Na 1 Nachlass Max Horkheimer, 655 - Vorträge über Antisemitismus (p. IX 40.1-2-IX 48.1-2)

"Summer institute on Modern European Culture" (1947?); 1. Ankündigung für eine Vorlesungsreihe von Max Horkheimer, Theodor W. Adorno, Leo Löwenthal, Herbert Marcuse, Friedrich Pollock. a) Typoskript mit eigenhändigen Ergänzungen, 20 Blatt b) Typoskript mit handschriftlichen Ergänzungen, 19 Blatt; 2. Herbert Marcuse: "Philosophie allemande et francaise 1871-1933". Typoskript mit eigenhändigen Korrekturen, 18 Blatt; "Tentative Program for the Course of Antisemitism". Vorlesungsankündigung 1948 von Max Horkheimer, Theodor W. Adorno, Friedrich Pollock. Typoskript 2 Blatt; Max Horkheimer: Bericht über die Antisemitismus-Forschungen des Instituts für Sozialforschung (GS 12, S. 165-171). Vortrag gehalten am 16.4.1943, englischer Text. a) Typoskript mit eigenhändigen Korrekturen, 5 Blatt b) Typoskript mit eigenhändigen Korrekturen, 8 Blatt c) Typoskript mit handschriftlichen Korrekturen, 8 Blatt; Max Horkheimer: Bericht über die Antisemitismus-Forschungen des Instituts für Sozialforschung (GS 12, S. 172-183). Vortrag gehalten am 30.4.1943, Temple Israel. a) Typoskript mit eigenhändigen Korrekturen und Ergänzungen, 12 Blatt b) Typoskript mit handschriftlichen Korrekturen, 11 Blatt c) Typoskript mit eigenhändigen Korrekturen, 14 Blatt; Max Horkheimer: Über die Psychologie des Judentums und des Antisemitismus; 1. Vortrag, gehalten am 7.10.1943 im Department of Psychology, UCLA, eigenhändige Notizen, 1 Blatt; 2. Auszüge aus Schriften und Arbeitspapieren von: G.M. Davidson, Salomon Andhil Fineberg, A.R.L. Gurland, Oscar I. Janomsky, Paul W. Massing, Typoskript mit eigenhändigen Ergänzungen, 8 Blatt; Max Horkheimer: Anti-Semitism as a Social Phenomenon (GS 5, S.364-372); 1. Vortrag, gehalten am 17.6.1944 in San Francisco, Psychoanalytic Society, veröffentlicht unter dem Titel 'Sociological Background of the Psychoanalytic Approach". In: Ernst Simmel (ed.), "Anti-Semitism. A Social Disease", New York, 1946, S.1-10. a) Typoskript, 13 Blatt, b) Teilstück, Typoskript, 1 Blatt, c) Teilstück, Typoskript mit eigenhändigen Korrekturen, 2 Blatt d) Typoskript mit handschriftlichen Korrekturen, 9 Blatt; 2. "Notes to the Speech in San Francisco", Notizen, 4 Blatt; 3. eigenhändige Notizen zum Vortrag, 5 Blatt; 4. Rede für Maurice Karpf, Typoskript mit eigenhändigen Korrekturen, 2 Blatt; 5. Theodor W. Adorno: "Mammoth Motives", Notizen zum Verhältnis von Soziologie und Psychologie des Antisemitismus, 3 Blatt; 6. Theodor W. Adorno: "Patterns of Anti-Democratic Propaganda", veröffentlicht in: Ernst Simmel, "Anti-Semitism. A Social Disease", New York, 1946, S.125-137. a) Typoskript, 15 Blatt, b) Typoskript, 14 Blatt;; 7. Einladung, Drucksache, 2 Blatt; 8. Max Horkheimer: 2 Brief an Donald MacFerlane, Pacific Palisades, 22.5.1944, 1 Blatt; Max Horkheimer: Vorträge 1944-45; 1. "Report for the N.C.R.A.C.". Über Forschungsprojekte des American Jewish Committee and des American Jewish Congress, vorgetragen am 14.1.1944, Typoskript, 4 Blatt; 2. Notizen zu 1: Über Kurt Lewin, Typoskript, 3 Blatt; 3. eigenhändige Notizen zu 1., 3 Blatt; 4. Über die europäische Tradition der Arbeiten des Instituts für Sozialforschung. Vortrag, gehalten am 8.12.1944. Eigenhändige Notizen, 1 Blatt; 5. Über psychologische Aspekte der Antisemitismusforschung des Instituts für Sozialforschung. Vortrag, gehalten am 19.4.1945. Eigenhändige Notizen, 2 Blatt; 6. Über sozioökonomische Aspekte des Antisemitismus in Europa und in der Arbeiterschaft der USA. Vortrag, gehalten am 8.6.1945. Psychosomatic Society a) Notizen zum Vortrag, 4 Blatt, b) eigenhändige Notizen, 3 Blatt; 7. Notizen zu 6., Typoskript, 17 Blatt,; 8. Notizen zu 6. "Quotations from Labor Study", Typoskript, 12 Blatt; 9. Über neue Forschungsprojekte des Instituts für Sozialforschung zum Antisemitismus. Vortrag, gehalten am 24.10.1945. Eigenhändige Notizen, 2 Blatt; 10. Über Antisemitismus. Vortrag, gehalten am 3.12.1945. Eigenhändige Notizen, 2 Blatt; 11.-15. Vorträge über Antisemitismus. Datierung unklar (etwa 1945) (u.a. "Mountvernon Speech" und "Breakfast Speech"), 17 Blatt; 16. Über Judentum und Katholizismus in der neueren Geschichte. Eigenhändige Notizen zu einem Vortrag, Datierung unklar, 3 Blatt; 17. Über Vorurteil, Vortrag oder Diskussion in einer Synagoge, Datierung unklar, eigenhändige Notizen, 1 Blatt; Max Horkheimer: Über die Antisemitismus-Forschungen des Instituts für Sozialforschung. Vortrag, gehalten beim U.C.R.A.C.-Meeting, 15.-17.6.1946, Chicago:; 1. eigenhändige Notizen, 13 Blatt; 2. Fragebogen, als Typoskript vervielfältigt, mit eigenhändigen Ergänzungen, 6 Blatt;

Breast cancer risk and heterocyclic amines and effect modification by NAT gene polymorphisms

Breast cancer is the most common cancer in women in the United States and is a leading cause of cancer-related deaths (1). Recently, dietary heterocyclic amines (HCAs) have been proposed to be a risk factor for breast cancer (2). This study uses the data collected for a case-control study conducted at the M.D. Anderson Cancer Center to assess the association between breast cancer risk and HCAs {2-amino-1-methyl-6-phenylimidazole [4,5-b] pyridine (PhIP), 2-amino-3,8-dimethylimidazo [4,5-f] quinoxaline (MeIQx), 2-amino-3,4,8-trimethylimidazo [4,5-f] quinoxaline (DiMeIQx) and mutagenicity of HCAs} and to examine if this association is modified by genetic polymorphisms of N-acetyl transferases (NAT1/NAT2). The NAT1/2 genotype was determined using Taqman technology. HCAs were estimated by using a meat preparation questionnaire on meat type, cooking method, and doneness, combined with a quantitative HCA database. Three hundred and fifty patients with breast cancer attending the Diagnostic Radiology Clinic at M. D. Anderson Cancer Center and fulfilling the eligibility criteria were compared to three hundred and fifty patients attending the same clinic for benign breast lesions to answer these questions. Logistic regression models were used to control for known risk factors and showed no statistically significant association between breast cancer versus benign breast cancer lesions and dietary intake of heterocyclic amines. There was no clear difference in their effect after subgroup analyses in different acetylator strata of NAT1/2 and no statistical interactions were found between NAT1/2 genotypes and HCAs, suggesting no effect modification by NAT1/2 acetylator status. These results suggest the need for further research to analyze if these null associations were because of the benign breast lesions sharing the risk factors with breast cancer or any other factors which haven't been explored yet.^

Ronald E. Heine, Origen. Scholarship in the service of the church, Oxford University Press, Oxford, 2010, pp. 275. ISBN 978-0-19-920907-1.

Fil: Peretó Rivas, Rubén.

Origène, commentaire sur l´épitre aux Romains, tome 1 (Livres I-II). Texte critique établi par C.P. Hammond Bammel. Introduction par Michel Fédou, s.j.. Traduction, notes et index par Luc Brésard, o.c.s.o. (Sources Chrétiennes 532), Cerf, Paris, 2009; 458 pp. ISBN 978-2- 204-09164-0.

Fil: Peretó Rivas, Rubén.

Heavy metal and petroleum product concentrations in waters at the Obskaya 1 drill site

During recent years, the basins of the Kara Sea (Kamennomysskaya, Obskaya, and Chugor'yakhinskaya structures) in the Russian Federation have been considered as promising regions for oil and gas exploration and, simultaneously, as possible paths of relatively cheap pipeline and tanker transportation of hydrocarbons projected for recovery. On the other hand, exploration operations, recovery, and transportation of gas pose a considerable risk of accidents and environmental pollution, which causes a justified concern about the future state of the ecological system of the Gulf of Ob and the adjoining parts of the Kara Sea. Therefore, regular combined environmental investigations (monitoring) are the most important factor for estimating the current state and forecasting the dynamics of the development of estuary systems. The program of investigations (schedule, station network, and measured parameters) is standardized in accordance with the international practice of such work and accounts for the experience of monitoring studies of Russian and foreign researchers. Two measurement sessions were performed during ecological investigations in the region of exploration drilling: at the beginning at final stage of drilling operations and borehole testing; in addition, natural parameters were determined in various parts of the Ob estuary before the beginning of investigations. Hydrophysical and hydrochemical characteristics of the water medium were determined and bottom sediments and water were analyzed for various pollutants (petroleum products, heavy metals, and radionuclides). The forms of heavy-metal occurrence in river and sea waters were determined by the method of continuous multistep filtration, which is based on water component fractionation on membrane filters of various pore sizes. These investigations revealed environmental pollution by chemical substances during the initial stage of drilling operations, when remains of fuels, oils, and solutions could be spilled, and part of the chemical pollutants could enter the environment. Owing to horizontal and vertical turbulent diffusion, wave mixing, and the effect of the general direction of currents in the Ob estuary from south to north, areas are formed with elevated concentrations of the analyzed elements and compounds. However, the concentration levels of chemical pollutants are practically no higher than the maximum admissible concentrations, and their substantial dissipation to the average regional background contents can be expected in the near future. Our investigations allowed us to determine in detail the parameters of anthropogenic pollution in the regions affected by hydrocarbon exploration drilling in the Obskii and Kamennomysskii prospects in the Gulf of Ob and estimate their influence on the ecological state of the basin of the Ob River and the Kara Sea on the whole.

Geochemical analysis of sediments and interstitial water in sediment cores from the North-West African continental margin and from the Central Pacific

A. Continental slope sediments off Spanish-Sahara and Senegal contain up to 4% organic carbon and up to 0.4% total nitrogen. The highest concentrations were found in sediments from water depths between 1000 and 2000 m. The regional and vertical distribution of organic matter differs significantly. Off Spanish-Sahara the organic matter content of sediment deposited during glacial times (Wuerm, Late Riss) is high whereas sediments deposited during interglacial times (Recent, Eem) are low in organic matter. Opposite distribution was found in sediments off Senegal. The sediments contain 30 to 130 ppm of fixed nitrogen. In most sediments this corresponds to 2-8 % of the total nitrogen. Only in sediments deposited during interglacial times off Spanish-Sahara up to 20 % of the total nitrogen is contained as inorganically bound nitrogen. Positive correlations of the fixed nitrogen concentrations to the amounts of clay, alumina, and potassium suggest that it is primarily fixed to illites. The amino acid nitrogen and hexosamine nitrogen account for 17 to 26 % and 1.3 to 2.4 %, respectively of the total nitrogen content of the sediments. The concentrations vary between 200 and 850 ppm amino acid nitrogen and 20 to 70 ppm hexosamine nitrogen, both parallel the fluctiations of organic matter in the sediment. Fulvic acids, humic acids, and the total organic matter of the sediments may be clearly differentiated from one another and their amino acid and hexosamine contents and their amino acid composition: a) Fulvic acids contain only half as much amino acids as humic acids b) The molar amino acid/hexosamine ratios of the fulvic acids are half those of the humic acids and the total organic matter of the sediment c) The amino acid spectra of fulvic acids are characterized by an enrichment of aspartic acid, alanine, and methionine sulfoxide and a depletion of glycine, valine, isoleucine, leucine, tyrosine, phenylalanine, lysine, and arginine compared to the spectra of the humic acids and those of the total organic matter fraction of the sediment. d) The amino acid spectra of the humic acids and those of the total organic matter fraction of the sediments are about the same with the exception that arginine is clearly enriched in the total organic matter. In general, as indicated by the amino compounds humic acids resemble closer the total organic matter composition than the low molecular fulvic acids do. This supports the general idea that during the course of diagenesis in reducing sediments organic matter stabilizes from a fulvic-like structure to humic-like structure and finally to kerogen. The decomposition rates of single aminio acids differ significantly from one another. Generally amino acids which are preferentially contained in humic acids and the total organic matter fraction show a smaller loss with time than those preferably well documented in case of the basic amino acids lysine and arginine which- although thermally unstable- are the most stable amino acids in the sediments. A favoured incorporation of these compounds into high molecular substances as well as into clay minerals may explain their relatively high "stability" in the sediment. The nitrogen loss from the sediments due to the activity of sulphate-reducing bacteria amounts to 20-40 % of the total organic nitrogen now present. At least 40 % of the organic nitrogen which is liberated by sulphate-reducing bacteria can be explained ny decomposition of amino acids alone. B. Deep-sea sediments from the Central Pacific The deep-seas sediments contain 1 to 2 orders of magnitude less organic matter than the continental slope sediments off NW Africa, i.e. 0.04 to 0.3 % organic carbon. The fixed nitrogen content of the deep-sea sediments ranges from 60 to 270 ppm or from 20 to 45 % of the total nitrogen content. While ammonia is the prevailing inorganic nitrogen compound in anoxic pore waters, nitrate predominates in the oxic environment of the deep-sea sediments. Near the sediment/water interface interstital nitrate concentrations of around 30 µg-at. N/l were recorded. These generally increase with sediment depth by 10 to 15 µg-at. NO3- N/l. This suggests the presence of free oxygen and the activity of nitrifying bacteria in the interstitial waters. The ammonia content of the interstitial water of the oxic deep-sea sediments ranges from 2 to 60 µg-at. N/l and thus is several orders of magnitude less than in anoxic sediments. In contrast to recorded nitrate gradients towards the sediments/water interface, there are no ammonia concentration gradients. However, ammonia concentrations appear to be characteristic for certain regional areas. It is suggested that this regional differentiation is caused by ion exchange reactions involving potassium and ammonium ions rather than by different decomposition rates of organic matter. C. C/N ratios All estimated C/N ratios of surface sediments vary between 3 and 9 in the deep-sea and the continental margin, respectively. Whereas the C/N ratios generally increase with depth in the sediment cores off NW Africa they decrease in the deep-sea cores. The lowest values of around 1.3 were found in the deeper sections of the deep-sea cores, the highest of around 10 in the sediments off NW Africa. The wide range of the C/N ratios as well as their opposite behaviour with increasing sediment depth in both the deep-sea and continental margin sediment cores, can be attributed mainly to the combination of the following three factors: 1. Inorganic and organic substances bound within the latticed of clay minerals tend to decrease the C/N ratios. 2. Organic matter not protected by absorption on the clay minerals tends to increase C/N ratios 3. Diagenetic alteration of organic matter by micro-organisms tends to increase C/N ratios through preferential loss of nitrogen The diagenetic changes of the microbially decomposable organic matter results in both oxic and anoxic environments in a preferential loss of nitrogen and hence in higher C/N ratios of the organic fraction. This holds true for most of the continental margin sediments off NW Africa which contain relatively high amounts of organic matter so that factors 2 and 3 predominate there. The relative low C/N ratios of the sediments deposited during interglacial times off Spanish-Sahara, which are low in organic carbon, show the increasing influence of factor 1 - the nitrogen-rich organic substances bound to clay minerals. In the deep-sea sediments from the Central Pacific this factor completely predominates so that the C/N rations of the sediments approach that of the substance absorbed to clay minerals with decreasing organic matter content. In the deeper core sections the unprotected organic matter has been completely destroyed so that the C/N ratios of the total sediments eventually fall into the same range as those of the pure clay mineral fraction.

Fatty acid and stable isotope composition of calanoid copepods in the open eastern Atlantic Ocean during POLARSTERN cruise ANT-XXIX/1

The majority of global ocean production and total export production is attributed to oligotrophic oceanic regions due to their vast regional expanse. However, energy transfers, food-web structures and trophic relationships in these areas remain largely unknown. Regional and vertical inter- and intra-specific differences in trophic interactions and dietary preferences of calanoid copepods were investigated in four different regions in the open eastern Atlantic Ocean (38°N to 21°S) in October/November 2012 using a combination of fatty acid (FA) and stable isotope (SI) analyses. Mean carnivory indices (CI) based on FA trophic markers generally agreed with trophic positions (TP) derived from d15N analysis. Most copepods were classified as omnivorous (CI ~0.5, TP 1.8 to ~2.5) or carnivorous (CI >=0.7, TP >=2.9). Herbivorous copepods showed typical CIs of <=0.3. Geographical differences in d15N values of epi- (200-0 m) to mesopelagic (1000-200 m) copepods reflected corresponding spatial differences in baseline d15N of particulate organic matter from the upper 100 m. In contrast, species restricted to lower meso- and bathypelagic (2000-1000 m) layers did not show this regional trend. FA compositions were species-specific without distinct intra-specific vertical or spatial variations. Differences were only observed in the southernmost region influenced by the highly productive Benguela Current. Apparently, food availability and dietary composition were widely homogeneous throughout the oligotrophic oceanic regions of the tropical and subtropical Atlantic. Four major species clusters were identified by principal component analysis based on FA compositions. Vertically migrating species clustered with epi- to mesopelagic, non-migrating species, of which only Neocalanus gracilis was moderately enriched in lipids with 16% of dry mass (DM) and stored wax esters (WE) with 37% of total lipid (TL). All other species of this cluster had low lipid contents (< 10% DM) without WE. Of these, the tropical epipelagic Undinula vulgaris showed highest portions of bacterial markers. Rhincalanus cornutus, R. nasutus and Calanoides carinatus formed three separate clusters with species-specific lipid profiles, high lipid contents (>=41% DM), mainly accumulated as WE (>=79% TL). C. carinatus and R. nasutus were primarily herbivorous with almost no bacterial input. Despite deviating feeding strategies, R. nasutus clustered with deep-dwelling, carnivorous species, which had high amounts of lipids (>=37% DM) and WE (>=54% TL). Tropical and subtropical calanoid copepods exhibited a wide variety of life strategies, characterized by specialized feeding. This allows them, together with vertical habitat partitioning, to maintain high abundance and diversity in tropical oligotrophic open oceans, where they play an essential role in the energy flux and carbon cycling.