967 resultados para ne bis in idem


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Beschrieben von dem Negermissionar N. Clerk, mitgeteilt von J. G. Christaller

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von Dr. G. Hellmann

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Signatur des Originals: S 36/F12039

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Entwürfe für ein Mögliches Forschungsprojekt über Liberlaismus des 19. Jahrhunderts; 1953; 1. Typoskript mit eigenhändigen Korrekturen von Theodor W. Adorno; 7 Blatt; 2. Typoskript mit eigenhändigen Korrekturen von Theodor W. Adorno; 3 Blatt; "Untersuchungn des sozialen Klimas in Stadt- und Landkreisen Hessens"; Entwürfe für ein "Handbuch der Methoden zur Messung des sozialen Klimas", nicht veröffentlicht; 1953; 1. Pollock, Friedrich: "Einführung" zum "Handbuch" a) Typoskript mit eigenhändigen Korrekturen; 8 Blatt; b) Typoskript mit eigenhändigen Korrekturen, 5 Blatt; c) Manuskript, "Vorwort"; 5 Blatt; d) Baumert, Gerhard: Entwurf des "Vorworts"; Typoskript mit handschriftlichen Korrekturen, 2 Blatt; e) Baumert, Gerhard: "Notizen zu Vorwort und Einführung des Handbuchs"; Typoskript, 1 Blatt; 2. Inhaltsverzeichnis zum "Handbuch"; 1 Blatt; 3. Pollock, Friedrich: eigenhändige Notizen zur Einführung; 7 Blatt; 4. Pollock, Friedrich: 1 eigenhändiger Brief mit Unterschrift an Theodor W. Adorno, Santa Monica, 21.09.1953; 1 Blatt; "Betriebsklime. Eine industrie-soziologische Untersuchung aus dem Ruhrgebiet" 1954-1956 veröffentlicht als Band 3 der Frankfurter Beiträge zur Soziologie, Frankfurt 1955; 1. Druckfahnen, mit handschriftlichen Korrekturen; 38 Blatt; 2. Korrektur-Notizen zu den Druckfahnen; 4 Blatt; 3. Adorno, Theodor W. [Mitarbeit]: "Grundreiz [Betriebsumfrage)" a) Typoskript mit handschriftlichen Korrekturen, 4 Blatt; b) Typoskript, 5 Blatt; 4. Adorno, Theodor W.: 1 Brief an Max Horkheimer, ohne Ort, 30.06.1954; 1 Blatt; 5. Fragebogen- Entwurf; Typsokript, 2 Blatt; 6. Fragebogen- Entwurf; Typoskript, 2 Blatt; 7. Adorno, Theodor W.: 1 Brief an Max Horkheimer, ohne Ort, ohne Datum [1954]; 1 Blatt; 8. Dirks, Walter: "Notiz über meine Reise nach Köln, Düsseldorf und Essen", 22.02.1955. Typoskript, 2 Blatt; 9. Becker, Hellmut: "Aktennotiz, Betreff: Ersetzung der Pressekonferenz über die Mannesmann-Studie durch in den nächsten Wochen und Monaten aufeinanderfolgende Artikel qualifizierter Korrespondenten", 15.02.1955. Typoskript, 1 Blatt; 10. Adorno, Theodor W.: 1 Brief an Hermann Winkhaus, Mannesmann AG, ohne Ort, 05.03.1956; 2 Blatt; 11. Winkhaus, Hermann, Mannesmann AG: 1 Breifabschrift an das Institut für Sozialforschung, Düsseldorf, 18.07.1955; 12. Presseveröffentlichungen zur Betriebsklima-Untersuchung; 1 Ordner, 13 Blatt; 13. Zeitschriftenartikel und Abschriften von Artikeln zur Betriebsklima- Untersuchung; mit: Becker, Egon: 2 Briefe mit Unterschrift an Max Horkheimer, Frankfurt, 1955; 1 Brief von Max Horkheimer, Zürich, 25.10.1955; Sardemann, Karl: Interview mit einem Juden über sein Leben 1933 bis circa 1953, insbesondere seine Erlebnisse im Konzentrationslager; 1955; 1. Interview; Typsokript, 38 Blatt; 2. Sardemann, Karl: 1 Brief mit Unterschrift an Max Horkheimer, ohne Ort, 15.12.1955; 1 Blatt; "Altersbild und Altersvorsorge der Arbeiter und Angestellten" veröffentlicht als Sonderheft 1 der Frankfurter Beiträge zur Soziologie, Frankfurt 1958.; Zwischenbericht zum Projekt und Material, 1955; 1. Becker, Egon, u.a.: "Zwischenbericht" 10.03.1953; Typoskript, 9 Blatt; mit einem Brief mit Unterschrift von Egon Becker an Max Horkheimer, ohne Ort, 11.03.1955; 1 Blatt; 2. Fragebogen; als Typoskript vervielfältigt, 16 Blatt; 3. Fragebogen; als Typoskript vervielfältigt, 11 Blatt;

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Critically ill and injured patients require pain relief and sedation to reduce the body's stress response and to facilitate painful diagnostic and therapeutic procedures. Presently, the level of sedation and analgesia is guided by the use of clinical scores which can be unreliable. There is therefore, a need for an objective measure of sedation and analgesia. The Bispectral Index (BIS) and Patient State Index (PSI) were recently introduced into clinical practice as objective measures of the depth of analgesia and sedation. ^ Aim. To compare the different measures of sedation and analgesia (BIS and PSI) to the standard and commonly used modified Ramsay Score (MRS) and determine if the monitors can be used interchangeably. ^ Methods. MRS, BIS and PSI values were obtained in 50 postoperative cardiac surgery patients requiring analgesia and sedation from June to December 2004. The MRS, BIS and PSI values were assessed hourly for up to 6-h by a single observer. ^ The relationship between BIS and PSI values were explored using scatter plots and correlation between MRS, BIS and PSI was determined using Spearman's correlation coefficient. Intra-class correlation (ICC) was used to determine the inter-rater reliability of MRS, BIS and PSI. Kappa statistics was used to further evaluate the agreement between BIS and PSI at light, moderate and deep levels of sedation. ^ Results. There was a positive correlation between BIS and PSI values (Rho = 0.731, p<0.001). Intra-class correlation between BIS and PSI was 0.58, MRS and BIS 0.43 and MRS and PSI 0.27. Using Kappa statistics, agreement between MRS and BIS was 0.35 (95% CI: 0.27–0.43) and for MRS and PSI was 0.21 (95% CI: 0.15–0.28). The kappa statistic for BIS and PSI was 0.45 (95% CI: 0.37–0.52). Receiver operating characteristics (ROC) curves constructed to detect undersedation indicated an area under the curve (AUC) of 0.91 (95% CI = 0.87 to 0.94) for the BIS and 0.84 (95% CI = 0.79 to 0.88) for the PSI. For detection of oversedation, AUC for the BIS was 0.89 (95% CI = 0.84 to 0.92) and 0.80 (95% CI = 0.75 to 0.85) for the PSI. ^ Conclusions. There is a statistically significant positive correlation between the BIS and PSI but poor correlation and poor test agreement between the MRS and BIS as well as MRS and PSI. Both the BIS and PSI demonstrated a high level of prediction for undersedation and oversedation; however, the BIS and PSI can not be considered interchangeable monitors of sedation. ^

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Although the climate development over the Holocene in the Northern Hemisphere is well known, palaeolimnological climate reconstructions reveal spatiotemporal variability in northern Eurasia. Here we present a multi-proxy study from north-eastern Siberia combining sediment geochemistry, and diatom and pollen data from lake-sediment cores covering the last 38,000 cal. years. Our results show major changes in pyrite content and fragilarioid diatom species distributions, indicating prolonged seasonal lake-ice cover between ~13,500 and ~8,900 cal. years BP and possibly during the 8,200 cal. years BP cold event. A pollen-based climate reconstruction generated a mean July temperature of 17.8°C during the Holocene Thermal Maximum (HTM) between ~8,900 and ~4,500 cal. years BP. Naviculoid diatoms appear in the late Holocene indicating a shortening of the seasonal ice cover that continues today. Our results reveal a strong correlation between the applied terrestrial and aquatic indicators and natural seasonal climate dynamics in the Holocene. Planktonic diatoms show a strong response to changes in the lake ecosystem due to recent climate warming in the Anthropocene. We assess other palaeolimnological studies to infer the spatiotemporal pattern of the HTM and affirm that the timing of its onset, a difference of up to 3,000 years from north to south, can be well explained by climatic teleconnections. The westerlies brought cold air to this part of Siberia until the Laurentide ice-sheet vanished 7,000 years ago. The apparent delayed ending of the HTM in the central Siberian record can be ascribed to the exceedance of ecological thresholds trailing behind increases in winter temperatures and decreases in contrast in insolation between seasons during the mid to late Holocene as well as lacking differentiation between summer and winter trends in paleolimnological reconstructions.

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Sediment trap samples from OMEX 2 (49°N, 13°W) provide a continuous record of the seasonal succession of planktonic foraminifera in the midlatitude North Atlantic and reveal a complex relationship between periods of production and specific hydrographic conditions. Neogloboquadrina pachyderma dextral coiling (d.), Globigerina bulloides, and Globorotalia inflata are found in great numbers during both the spring and summer seasons, whereas Globigerina quinqueloba, Globorotalia hirsuta, Globorotalia scitula, and Globigerinita glutinata are associated predominantly with the increase in productivity during the spring bloom. Globigerinella aequilateralis, Orbulina universa, and Globigerinoides sacculifer are restricted to late summer conditions following the establishment of a warm, well-stratified surface ocean. An annually integrated fauna from the sediment trap, comprising ~13,000 individuals, is used to evaluate the accuracy of five faunal-based statistical methods of paleotemperature estimation. All of the temperature reconstruction techniques produce estimates of ~16°C and ~11°C for summer and winter surface temperature, respectively, which are in excellent agreement with regional hydrographic data and suggest that the sediment trap assemblage is well represented in the core top faunas. Analysis of the key species that dominate the OMEX 2 sediment trap fauna, G. bulloides, G. inflata, and N. pachyderma d., based on d18O derived temperatures from North Atlantic core top samples, suggests that seasonal variations in planktonic foraminiferal production are nonuniform across the midlatitudes and that this is likely to complicate reconstructing past seasonal hydrographic dynamics using these taxa.