Handschriften, Einbände, Formschnitte und Kupferstiche des 15. Jahrhunderts, Druckwerke und Einblattdrucke des 15. bis 20. Jahrhunderts

Stadtbibliothek Frankfurt am Main. [Bearb. ... Emil Sarnow]

Impact of weight loss on survival after chemoradiation for locally advanced head and neck cancer: secondary results of a randomized phase III trial (SAKK 10/94).

BACKGROUND To analyze the impact of weight loss before and during chemoradiation on survival outcomes in patients with locally advanced head and neck cancer. METHODS From 07/1994-07/2000 a total of 224 patients with squamous cell carcinoma of the head and neck were randomized to either hyperfractionated radiation therapy alone or the same radiation therapy combined with two cycles of concomitant cisplatin. The primary endpoint was time to any treatment failure (TTF); secondary endpoints were locoregional recurrence-free survival (LRRFS), distant metastasis-free survival (DMFS) and overall survival (OS). Patient weight was measured 6 months before treatment, at treatment start and treatment end. RESULTS The proportion of patients with >5% weight loss was 32% before, and 51% during treatment, and the proportion of patients with >10% weight loss was 12% before, and 17% during treatment. After a median follow-up of 9.5 years (range, 0.1 - 15.4 years) weight loss before treatment was associated with decreased TTF, LRRFS, DMFS, cancer specific survival and OS in a multivariable analysis. However, weight loss during treatment was not associated with survival outcomes. CONCLUSIONS Weight loss before and during chemoradiation was commonly observed. Weight loss before but not during treatment was associated with worse survival.

Emergence of acquired HIV-1 drug resistance has almost been stopped in Switzerland - a 15 year prospective cohort analysis

BACKGROUND  Drug resistance is a major barrier to successful antiretroviral treatment (ART). Therefore, it is important to monitor time trends at a population level. METHODS  We included 11,084 ART-experienced patients from the Swiss HIV Cohort Study (SHCS) between 1999 and 2013. The SHCS is highly representative and includes 72% of patients receiving ART in Switzerland. Drug resistance was defined as the presence of at least one major mutation in a genotypic resistance test. To estimate the prevalence of drug resistance, data for patients with no resistance test was imputed based on patient's risk of harboring drug resistant viruses. RESULTS  The emergence of new drug resistance mutations declined dramatically from 401 to 23 patients between 1999 and 2013. The upper estimated prevalence limit of drug resistance among ART-experienced patients decreased from 57.0% in 1999 to 37.1% in 2013. The prevalence of three-class resistance decreased from 9.0% to 4.4% and was always <0.4% for patients who initiated ART after 2006. Most patients actively participating in the SHCS in 2013 with drug resistant viruses initiated ART before 1999 (59.8%). Nevertheless, in 2013, 94.5% of patients who initiated ART before 1999 had good remaining treatment options based on Stanford algorithm. CONCLUSION  HIV-1 drug resistance among ART-experienced patients in Switzerland is a well-controlled relic from the pre-combination ART era. Emergence of drug resistance can be virtually stopped with new potent therapies and close monitoring.

Na 1 Nachlass Max Horkheimer, 688 - "Fortune Polls on Antisemitism" (p. IX 153.1-18)

"Fortune Polls on Antisemitism" (1947) (veröffentlicht unter dem Titel "Fortune Survey Analyzed by AJC Consultant to Appraise Results", in: News Letter, American Jewish Committee, Dezember 1947, S. 4):; 1. Max Horkheimer: Über Fortune Polls, a) Typoskript, 3 Blatt, b) Typoskript, 3 Blatt, c) Typoskript mit eigenhändigen Korrekturen, 3 Blatt, d) Typoskript, 3 Blatt; 2. Max Horkheimer: Über Fortune Polls und die Gefahren eines neuen Antisemitismus (Vortragsskript?), Typoskript und Manuskript, 4 Blatt; 3. Theodor W. Adorno (?): "Some Results of Adult Project". Typoskript mit eigenhändigen Korrekturen, 2 Blatt; 4. "Education Counteracts Prejudice" Auszug aus "Antisemitism among American Labor". Typoskript, 1 Blatt; 5. "Discord versus Harmony", Excerpt from: The Annals of the American Academy of Political and Social Science, March 1946, Typoskript, 1 Blatt; 6. Theodor W. Adorno: "Memorandum, Subject: Poll Controversy", 24.4.1948; 7. Leo Löwenthal: "Memorandum on Fortune Poll" und "Supplementary Memorandum on Fortune Poll", 8.10.1947. Typoskripte mit eigenhändigen Ergänzungen, 4 Blatt; 8. "Massing's Comment" (8.10.1947). Typoskript, 2 Blatt; 9. "Excerpts from Fortune Magazine 'The Fortune Survey': Racial and Religious Intolerance". Typoskript, 3 Blatt, a) "Summary of 'Fortune Survey' on Antisemitism in U.S. (Fortune, April, 1939)", Typoskript, 2 Blatt; 10. Leo Löwenthal: 1 Brief mit Unterschrift an Max Horkheimer, New York, 4.10.1947, 1 Blatt; 11. Exzerpt der Umfrage-Materialien der Opinion Research Corporation, Typoskripte, 61 Blatt; 12. Zahlenmaterial zu den Umfragen, 16 Blatt; Office of War Information, Bureau of Intelligence: Berichte über Antisemitismus: 13. "Attitudes toward Jews in the United States", 27.10.1942, a) als Typoskript vervielfältigt, 22 Blatt, b) Typoskript, 35 Blatt; 14. "Political Anti-Semitism: A Study of Indoctrination" (27.10.1942), a) als Typoskript vervielfältigt, 18 Blatt, b) Typoskript, 26 Blatt; 15. "Anti-Semitism - a Symptom of Disaffection" (8.10.1942), a) als Typoskript vervielfältigt, 8 Blatt, b) Typoskript, 12 Blatt; 16. Samuel H. Flowerman und Marie Jahoda: "Polls on Anti-Semitism. How much do they tell us?", Sonderdruck, 4 Blatt; 17. Fragebogen, Drucksachen, 4 Blatt; 18. Zeitungausschnitte aus: The Fortune Survey, 9 Blatt;

Physical oceanography from the TRACTOR project

Primary Objectives - Describe and quantify the present strength and variability of the circulation and oceanic processes of the Nordic Seas regions using primarily observations of the long term spread of a tracer purposefully released into the Greenland Sea Gyre in 1996. - Improve our understanding of ocean processes critical to the thermaholine circulation in the Nordic Seas regions so as to be able to predict how this region may respond to climate change. - Assess the role of mixing and ageing of water masses on the carbon transport and the role of the thermohaline circulation in carbon storage using water transports and mixing coefficients derived from the tracer distribution. Specific Objectives Perform annual hydrographic, chemical and SF6 tracer surveys into the Nordic regions in order to: - Measure lateral and diapycnal mixing rates in the Greenland Sea Gyre and in the surrounding regions. - Document the depth and rates of convective mixing in the Greenland Sea using the SF6 and the water masses characteristics. - Measure the transit time and transport of water from the Greenland Sea to surrounding seas and outflows. Document processes of water mass transformation and entrainment occurring to water emanating from the central Greenland Sea. - Measure diapycnal mixing rates in the bottom and margins of the Greenland Sea basin using the SF6 signal observed there. Quantify the potential role of bottom boundary-layer mixing in the ventilation of the Greenland Sea Deep Water in absence of deep convection. Monitor the variability of the entrainment of water from the Greenland Sea using time series auto-sampler moorings at strategic positions i.e., sill of the Denmark Strait, Labrador Sea, Jan Mayen fracture zone and Fram Strait. Relate the observed variability of the tracer signal in the outflows to convection events in the Greenland Sea and local wind stress events. Obtain a better description of deepwater overflow and entrainment processes in the Denmark Strait and Faeroe Bank Channel overflows and use these to improve modelling of deepwater overflows. Monitor the tracer invasion into the North Atlantic using opportunistic SF6 measurements from other cruises: we anticipate that a number of oceanographic cruises will take place in the north-east Atlantic and the Labrador Sea. It should be possible to get samples from some cruises for SF6 measurements. Use process models to describe the spread of the tracer to achieve better parameterisation for three-dimensional models. One reason that these are so resistant to prediction is that our best ocean models are as yet some distance from being good enough, to predict climate and climate change.

Stable isotope analysis and temperature reconstruction data from DSDP Hole 94-609B and ODP Hole 162-984B

The Greenland ice sheet is accepted as a key factor controlling the Quaternary glacial scenario. However, the origin and mechanisms of major Arctic glaciation starting at 3.15 Ma and culminating at 2.74 Ma are still controversial. For this phase of intense cooling Ravelo et al. proposed a complex gradual forcing mechanism. In contrast, our new submillennial-scale paleoceanographic records from the Pliocene North Atlantic suggest a far more precise timing and forcing for the initiation of northern hemisphere glaciation (NHG), since it was linked to a 2-3 °C surface water warming during warm stages from 2.95 to 2.82 Ma. These records support previous models, claiming that the final closure of the Panama Isthmus (3.0- ~2.5 Ma induced an increased poleward salt and heat transport. Associated strengthening of North Atlantic Thermohaline Circulation and in turn, an intensified moisture supply to northern high latitudes resulted in the build-up of NHG, finally culminating in the great, irreversible climate crash at marine isotope stage G6 (2.74 Ma). In summary, there was a two-step threshold mechanism that marked the onset of NHG with glacial-to-interglacial cycles quasi-persistent until today.

Granulometry of two sediment cores from Maxwell Bay, South Shetland Islands, West Antarctica

The climate evolution of the South Shetland Islands during the last c. 2000 years is inferred from the multiproxy analyses of a long (928 cm) sediment core retrieved from Maxwell Bay off King George Island. The vertical sediment flux at the core location is controlled by summer melting processes that cause sediment-laden meltwater plumes to form. These leave a characteristic signature in the sediments of NE Maxwell Bay. We use this signature to distinguish summer and winter-dominated periods. During the Medieval Warm Period, sediments are generally finer which indicates summer-type conditions. In contrast, during the Little Ice Age (LIA) sediments are generally coarser and are indicative of winter-dominated conditions. Comparison with Northern and Southern Hemisphere, Antarctic, and global temperature reconstructions reveals that the mean grain-size curve from Maxwell Bay closely resembles the curve of the global temperature reconstruction. We show that the medieval warming occurred earlier in the Southern than in the Northern Hemisphere, which might indicate that the warming was driven by processes occurring in the south. The beginning of the LIA appears to be almost synchronous in both hemispheres. The warming after the LIA closely resembles the Northern Hemisphere record which might indicate this phase of cooling was driven by processes occurring in the north. Although the recent rapid regional warming is clearly visible, the Maxwell Bay record does not show the dominance of summer-type sediments until the 1970s. Continued warming in this area will likely affect the marine ecosystem through meltwater induced turbidity of the surface waters as well as an extension of the vegetation period due to the predicted decrease of sea ice in this area.