973 resultados para 104-1


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Continuous sediment sections spanning the last 2.8 Ma have been studied using stable isotope stratigraphy and sedimentological methods. By using paleomagnetic reversals as a chronostratigraphic tool, climatic and paleoceanographic changes have been placed in a time framework. The results show that the major expansion of the Scandinavian Ice Sheet to the coastal areas occurred in the late Neogene period at about 2.8 Ma. Relatively high-amplitude glacials appeared until about 2 Ma. The period between 2.8 and 1.2 Ma was marked by cold surface water conditions with only weak influx of temperate Atlantic water as compared with late Quaternary interglacials. During this period, climatic variations were smaller in amplitude than in the late Quaternary. The Norwegian Sea was a sink of deep water throughout the studied period but deep water ventilation was reduced and calcite dissolution was high compared with the Holocene. Deep water formed by other processes than today. Between 2 and 1.2 Ma, glaciations in Scandinavia were relatively small. A transition toward larger glacials took place during the period 1.2 to 0.6 Ma, corresponding with warmer interglacials and increasing influx of temperate surface water during interglacials. A strong thermal gradient was present between the Norwegian Sea and the northeastern Atlantic during the Matuyama (2.5-0.7 Ma). This is interpreted as a sign of a more zonal and less meridional climatic system over the region as compared with the present situation. The transition towards more meridionality took place over several hundred thousand yr. Only during the last 0.6 Ma has the oceanographic and climatic system of the Norwegian Sea varied in the manner described from previous studies of the late Quaternary.

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At mid- to high-latitude marine sites, ice-rafted debris (IRD) is commonly recognized as anomalously coarse-grained terrigenous material contained within a fine-grained hemipelagic or pelagic matrix (e.g., Conolly and Ewing, 1970; Ruddiman, 1977, doi:10.1130/0016-7606(1977)88<1813:LQDOIS>2.0.CO;2; Krissek, 1989, doi:10.2973/odp.proc.sr.104.114.1989; Jansen et al., 1990; Bond et al., doi:10.1038/360245a0, 1992; Krissek, 1995, doi:10.2973/odp.proc.sr.145.118.1995). The presence of such ice-rafted material is a valuable indicator of the presence of glacial ice at sea level on an adjacent continent, whereas the composition of the IRD can often be used to identify the location of the source area (e.g., Goldschmidt, 1995, doi:10.1016/0025-3227(95)00098-J). Because the amount of core recovered during Leg 163 was very limited, this shore-based, postcruise study focuses on materials recovered at a nearby site during Leg 152. In particular, this study examines sediments recovered at Site 919; these sediments were described as containing a significant ice-rafted component in the Leg 152 Initial Reports volume (Larsen, Saunders, Clift, et al., 1994, doi:10.2973/odp.proc.ir.152.1994). In this study, the sedimentary section from Site 919 has been examined with the goal of providing a detailed history of glaciations on Greenland and other landmasses adjacent to the Norwegian-Greenland Sea; this history ultimately will be calibrated using an oxygen isotope stratigraphy (Flower, 1998, doi:10.2973/odp.proc.sr.152.219.1998), although that calibration has not been completed at this time. Because ice-core studies of the Greenland Ice Sheet (GIS) have shown that the GIS changed dramatically, and in some cases extremely rapidly, during at least the last interglacial stage (GRIP Members, 1993, doi:10.1038/364203a0), a detailed IRD record from the Southeast Greenland margin should provide insight into the longer term behavior of this sensitive component of the Northern Hemisphere climate system.

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The analysis of 104 core-catcher samples from Site 603 resulted in a continuous palynological record from the middle Miocene to early Pleistocene. Two palynological zones could be established (Zone 2, below 380 m: high Pinus, Quercus, and Carya values; Zone 1, above 380 m: high Pinus, and Sphagnum values). The marine pollen record was found to reflect the history of the vegetation of the eastern United States, the flora from Zone 2 indicating a warmer climate than that from Zone 1, which depicts a climatic cooling trend. The onset of Western Boundary Undercurrent deposition had no noticeable effect on the pollen distribution in the marine sediments.

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Benthic foraminifers have been studied in about 900 samples from Sites 642, 643, and 644 (ODP Leg 104, Voring Plateau), ranging in age from Eocene to Holocene. This sequence has been subdivided into seven assemblage zones. The Eocene to middle Miocene deposits are characterized by an agglutinated fauna. This reflects an environment causing dissolution of calcareous tests rather than the original living fauna. The upper Miocene to middle Pliocene deposits contain a diverse benthic foraminiferal fauna dominated by calcareous forms. The uppermost part of the sediment record, deposited during late Pliocene to Holocene, is characterized by many barren intervals and samples containing shallow-water species as well as ice-rafted material indicating glacial periods. Interglacials are reflected in samples containing a true oceanic foraminifer assemblage and no coarse clastic material.

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The aim of this contribution is to supply summarized information on the distribution and numbers of marine mammals in the Antarctic. In relation to the topic of the workshop the question to be answered is: "Is there spatial or temporal variation in mammalian presence in the Antarctic area that has relevance to the operation of acoustic devices". If acoustic devices have impact on marine mammals, this does not stop at political borders. Nevertheless, since legal implementation of the Antarctic Environmental Protocol was the major stimulus behind the workshop, this contribution was asked to limit itself to the Antarctic Treaty area, that is south of 60°S.

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43. - 62. Sammlung B: "Konzepte als Zugabe zur Festschrift für Friedrich Pollock" [GS 12, S. 250 - 295]. 64 Blatt; 43. "Zum Problem der Bedürfnisse". Typoskript, 6 Blatt; 44. "Dichtung und Moral". Typoskript, 5 Blatt; 45. "Geschichte der amerikanischen Arbeiterschaft". Typoskript, 1 Blatt; 46. "Kein Weg zur Wahrheit". Typoskript, 1 Blatt; 47. "Zur Rechtsphilosophie". Typoskript mit eigenen Korrekturen, 2 Blatt; 48. "Strafgefangene". Typoskript, 1 Blatt; 49. "Jüdischer Charakter". Typoskript, 1 Blatt; 50. "Solidarität". Typoskript, 2 Blatt; 51. "Unmöglichkeit der Dichtung". Typoskript, 1 Blatt; 52. "Theorie des Verbrechers". Typoskript, 14 Blatt; 53. "Erbsünde und Kopula". Typoskript, 2 Blatt; 54. "Feind". Typoskript, 2 Blatt; 55. "Haupt- und Nebensatz". Typoskript, 3 Blatt; 56. "Bewußtsein". Typoskript, 1 Blatt; 57. "Kampf und Gewaltlosigkeit". Typoskript, 6 Blatt; 58. "Umschlag der idealistischen Dialektik". Typoskript, 1 Blatt; 59. "Die Rackets und der Geist". Typoskript, 7 Blatt; 60. "Altmodische Probleme". Typoskript mit eigenen Korrekturen, 2 Blatt; 61. "Physiognomik". Typoskript, 1 Blatt; 62. "Religionspsychologie". Typoskript, 2 Blatt; 63. - 106. Sammlung C: "New Yorker Notizen [I]"; 63. "Dialektik der Aufklärung Nr. 7". Typoskript mit eigenen Korrekturen, 12 Blatt; 64. Aus der "Dialektik der Aufklärung"; Kapitel: "Elemente des Antisemitismus", Abschitt VII:; 64a) Typoskript mit eigenen Korrekturen, 11 Blatt; 64b) Teilstück, Typoskript, 2 Blatt; 64c) Teilstück, Typoskript, 1 Blatt; 64d) Teilstück, Typoskript, 1 Blatt; 65. "Bemerkungen zu These VII" [zu: 64]; Über Antisemitismus und Stalinismus, [von Theodor W. Adorno]. Typoskript, 3 Blatt; 66. "Verwandlung der Idee in Gesinnung":; 66a) Typoskript, 5 Blatt; 66b) Typoskript mit eigenen Korrekturen, 4 Blatt; 66c) Typoskript, 5 Blatt; 67. "Zum Problem der Bedürfnisse". Typoskript mit eigenen Korrekturen, 6 Blatt; 68. "Dichtung und Moral":; 68a) Typoskript, 5 Blatt; 68b) Typoskript mit eigenen Korrekturen, 4 Blatt; 68c) Typoskript mit eigenen Korrekturen, 4 Blatt; 68d) Typoskript mit eigenen Korrekturen, 5 Blatt; 69. "Geschichte der amerikanischen Arbeiterschaft":; 69a) Typoskript, 1 Blatt; 69b) Typoskript; 1 Blatt; 70. "Straftheorie. Zur Rechtsphilosophie":; 70a) Typoskript mit eigenen Korrekturen, 3 Blatt; 70b) Typoskript mit eigenen Korrekturen, 3 Blatt; 70c) Typoskript mit eigenen Korrekturen, 3 Blatt; 70d) Typoskript, 3 Blatt; 71. "Jüdischer Charakter". Typoskript, 1 Blatt; 72. "Solidarität". Typoskript, 2 Blatt; 73. "Theorie des Verbrechens". Typoskript mit eigenen Korrekturen, 17 Blatt; 74. "Erbsünde und Copula":; 74a) Typoskript, 2 Blatt; 74b) Typoskript mit eigenen Korrekturen, 3 Blatt; 75. "Geschichtsphilosophischer Exkurs zur Odysee" [von Theodor W. Adorno ?]. Teilstück, Typoskript, 1 Blatt; 76. "Feind":; 76a) Typoskript, 2 Blatt; 76b) Typoskript, 2 Blatt; 76c) Typoskript, 2 Blatt; 76d) Entwurf, englisch, Typoskript mit eigenen Korrekturen, 2 Blatt; 77. "Haupt- und Nebensatz":; 77a) Typoskript, 2 Blatt; 77b) Typoskript mit eigenen Korrekturen, 2 Blatt; 77c) Typoskript mit eigenen Korrekturen, 2 Blatt; 77d) Typoskript mit eigenen Korrekturen, 3 Blatt; 78. "Bewußtsein":; 78a) Typoskript, 1 Blatt; 78b) Typoskript mit eigenen Korrekturen, 1 Blatt; 79. "Kampf und Gewaltlosigkeit":; 79a) Typoskript, 6 Blatt; 79b) Typoskript, 6 Blatt; 79c) Teilstücke, Typoskript mit eigenen Korrekturen, 6 Blatt; 79d) Typoskript mit eigenen Korrekturen, 5 Blatt; 79e) Typoskript, 5 Blatt; 79f) Teilstück, Typoskript mit eigenen Korrekturen, 2 Blatt; 80. "Die Rackets und der Geist":; 80a) Typoskript mit eigenen Korrekturen, 2 Blatt; 80b) Typoskript mit eigenen Korrekturen, 6 Blatt; 81. "Altmodisches Problem". Typoskript, 2 Blatt; 82. "Physiognomik". Typoskript, 1 Blatt; 83. "Religionspsychologie":; 83a) Typoskript mit eigenen Korrekturen, 2 Blatt; 83b) Typoskript mit eigenen Korrekturen, 2 Blatt; 84. "Leeres Erschrecken":; 84a) Typoskript mit eigenen Korrekturen, 2 Blatt; 84b) Typoskript, 2 Blatt; 84c) Typoskript mit eigenen Korrekturen, 2 Blatt; 85. "Philosophie und Arbeitsteilung":; 85a) Typoskript mit eigenen Korrekturen, 3 Blatt; 85b) Typoskript mit eigenen Korrekturen, 3 Blatt; 85c) Typoskript, 3 Blatt; 85d) Typoskript mit handschriftlichen Korrekturen, 3 Blatt; 86. "Vorrede" zur Dialektik der Aufklärung. Typoskript mit eigenen Korrekturen, 11 Blatt; 87. ["Umschlag der idealistischen Dialektik"] Typoskript, 1 Blatt; 88. Über Erkenntnis und Sprache. Typoskript mit eigenen Korrekturen, 1 Blatt; 89. "Zur Kritik der Geschichtsphilosophie". Typoskript mit eigenen Korrekturen, 3 Blatt; 90. "Mensch und Tier":; 90a) Typoskript mit eigenen und handschriftlichen Korrekturen, 12 Blatt; 90b) Typoskript mit eigenen Korrekturen, 3 Blatt; 90c) Typoskript mit eigenen Korrekturen, 4 Blatt; 90d) Typoskript mit eigenen Korrekturen, 3 Blatt; 90e) Typoskript mit eigenen Korrekturen, 10 Blatt; 91. "Massengesellschaft". Typoskript, 1 Blatt; 92. "Zwei Welten". Typoskript, 2 Blatt; 93. "Zur Theorie der Gespenster":; 93a) Typoskript, 1 Blatt; 93b) Typoskript mit eigenen Korrekturen, 1 Blatt; 94. "Interesse am Körper":; 94a) Typoskript mit eigenen Korrekturen, 6 Blatt; 94b) Typoskript mit eigenen Korrekturen, 7 Blatt; 94c) Typoskript, 2 Blatt; 94d) Typoskript, 6 Blatt; 95. "Unmöglichkeit der Dichtung". Typoskript, 1 Blatt; 96. "Die Einseitigkeit der Negativität":; 96a) Typoskript, 2 Blatt; 96b) Typoskript mit eigenen Korrekturen, 2 Blatt; 96c) Typoskript, 2 Blatt; 97. "Widersprüche":; 97a) Typoskript, 4 Blatt; 97b) Typoskript mit eigenen Korrekturen, 4 Blatt; 98. "Zur Theorie der Dummheit":; 98a) Typoskript, 3 Blatt; 98b) Typoskript mit eigenen Korrekturen, 3 Blatt.; 99. "Gezeichnet". Typoskript, 2 Blatt; 100. "Quand-même":; 100a) Typoskript, 2 Blatt; 100b) Typoskript mit eigenen Korrekturen, 2 Blatt; 101. "Isolierung durch Verkehr":; 101a) Typoskript mit eigenen Korrekturen, 1 Blatt; 101b) Typoskript, 1 Blatt; 102. "Gegen Gescheitheit". Typoskript mit eigenen Korrekturen, 1 Blatt; 103. "Propaganda":; 103a) Typoskript mit eigenen Korrekturen, 2 Blatt; 103b) Typoskript, 2 Blatt; 103c) Typoskript mit eigenen Korrekturen, 2 Blatt; 104. "Der Gedanke". Typoskript mit eigenen Korrekturen, 1 Blatt; 105. Fragment aus der "Dialektik der Aufklärung", Exkurs II. Typoskript mit eigenen Korrekturen, 3 Blatt; 106. Zum Begriff des Individuums bei Leibniz und Hegel [GS 12, S. 314 - 315]. Typoskript mit eigenen Korrekturen, 2 Blatt;

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Thesis (Master's)--University of Washington, 2016-06

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Burn sepsis is a leading cause of mortality and morbidity in patients with major burns. The use of topical anti-microbial agents has helped improve the survival in these patients. There are a number of anti-microbials available, one of which, Silvazine(TM) (1% silver sulphadiazine (SSD) and 0.2% chlorhexidine digluconate), is used only in Australasia. No study, in vitro or clinical, had compared Silvazine(TM) with the new dressing Acticoat(TM). This study compared the anti-microbial activity of Silvazine(TM), Acticoa(TM) and 1% silver sulphadiazine (Flamazine(TM)) against eight common burn wound pathogens. Methods: Each organism was prepared as a suspension. A 10 mul inoculum of the chosen bacterial isolate (representing approximately between 104 and 105 total bacteria) was added to each of four vials, followed by samples of each dressing and a control. The broths were then incubated and 10 mul loops removed at specified intervals and transferred onto Horse Blood Agar. These plates were then incubated for 18 hours and a colony count was performed. Results: The data demonstrates that the combination of 1% SSD and 0.2% chlorhexidine digluconate (Silvazine(TM)) results in the most effective killing of all bacteria. SSD and Acticoat(TM) had similar efficacies against a number of isolates, but Acticoat(TM) seemed only bacteriostatic against E. faecalis and methicillin-resistant Staphylococcus aureus. Viable quantities of Enterobacter cloacae and Proteus mirabilis rei named at 24 h. Conclusion: The combination of 1% SSD and 0.2% chlorhexidine digluconate (Silvazine(TM)) is a more effective anti-microbial against a number of burn wound pathogens in this in vitro study. A clinical study of its in vivo anti-microbial efficacy is required. (C) 2003 Elsevier Ltd and ISBI. All rights reserved.