996 resultados para 205-1


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Mode of access: Internet.

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Microfilm. Ann Arbor, Mich., University Microfilms [n.d.] (American culture series, Reel 205.1)

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This paper focuses on Belarus in order to find explanation as to why could Lukashenko remain the authoritarian leader of Belarus, while in Ukraine the position of the political elite had proved less stable and collapsed in 2004. We seek to determine whether the internal factors (macroeconomic conditions, standard of living, the oppressive nature of the political system) play a significant role in the operation of the domino effect. This article emphasises the determining role of immanent internal factors, thus the political stability in Belarus can be explained by the role of the suppressing political regime, the hindrance of democratic rights and the relatively good living conditions that followed the transformational recession. Whilst in Ukraine, the markedly different circumstances brought forth the success of the Orange Revolution.

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We analyzed hydrographic data from the northwestern Weddell Sea continental shelf of the three austral winters 1989, 1997, and 2006 and two summers following the last winter cruise. During summer a thermal front exists at ~64° S separating cold southern waters from warm northern waters that have similar characteristics as the deep waters of the central basin of the Bransfield Strait. In winter, the whole continental shelf exhibits southern characteristics with high Neon (Ne) concentrations, indicating a significant input of glacial melt water. The comparison of the winter data from the shallow shelf off the tip of the Antarctic Peninsula, spanning a period of 17 yr, shows a salinity decrease of 0.09 for the whole water column, which has a residence time of <1 yr. We interpret this freshening as being caused by a combination of reduced salt input due to a southward sea ice retreat and higher precipitation during the late 20th century on the western Weddell Sea continental shelf. However, less salinification might also result from a delicate interplay between enhanced salt input due to sea ice formation in coastal areas formerly occupied by Larsen A and B ice shelves and increased Larsen C ice loss.

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Based on a well-established stratigraphic framework and 47 AMS-14C dated sediment cores, the distribution of facies types on the NW Iberian margin is analysed in response to the last deglacial sea-level rise, thus providing a case study on the sedimentary evolution of a high-energy, low-accumulation shelf system. Altogether, four main types of sedimentary facies are defined. (1) A gravel-dominated facies occurs mostly as time-transgressive ravinement beds, which initially developed as shoreface and storm deposits in shallow waters on the outer shelf during the last sea-level lowstand; (2) A widespread, time-transgressive mixed siliceous/biogenic-carbonaceous sand facies indicates areas of moderate hydrodynamic regimes, high contribution of reworked shelf material, and fluvial supply to the shelf; (3) A glaucony-containing sand facies in a stationary position on the outer shelf formed mostly during the last-glacial sea-level rise by reworking of older deposits as well as authigenic mineral formation; and (4) A mud facies is mostly restricted to confined Holocene fine-grained depocentres, which are located in mid-shelf position. The observed spatial and temporal distribution of these facies types on the high-energy, low-accumulation NW Iberian shelf was essentially controlled by the local interplay of sediment supply, shelf morphology, and strength of the hydrodynamic system. These patterns are in contrast to high-accumulation systems where extensive sediment supply is the dominant factor on the facies distribution. This study emphasises the importance of large-scale erosion and material recycling on the sedimentary buildup during the deglacial drowning of the shelf. The presence of a homogenous and up to 15-m thick transgressive cover above a lag horizon contradicts the common assumption of sparse and laterally confined sediment accumulation on high-energy shelf systems during deglacial sea-level rise. In contrast to this extensive sand cover, laterally very confined and maximal 4-m thin mud depocentres developed during the Holocene sea-level highstand. This restricted formation of fine-grained depocentres was related to the combination of: (1) frequently occurring high-energy hydrodynamic conditions; (2) low overall terrigenous input by the adjacent rivers; and (3) the large distance of the Galicia Mud Belt to its main sediment supplier.

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The chemical composition of surface associated metabolites of two Fucus species (Fucus vesiculosus and Fucus serratus) was analysed by means of gas chromatography-mass spectrometry (GC-MS) to describe temporal patterns in chemical surface composition. Method: The two perennial brown macroalgae F. vesiculosus and F. serratus were sampled monthly at Bülk, outer Kiel Fjord, Germany (54°27'21 N / 10°11'57 E) over an entire year (August 2012 - July 2013). Per month and species six non-fertile Fucus individuals were collected from mixed stands at a depth of 0.5 m under mid water level. For surface extraction approx. 50 g of the upper 5-10 cm apical thalli tips were cut off per species. The surface extraction of Fucus was performed according to the protocol of de Nys and co-workers (1998) with minor modifications (see Rickert et al. 2015). GC/EI-MS measurements were performed with a Waters GCT premier (Waters, Manchester, UK) coupled to an Agilent 6890N GC equipped with a DB-5 ms 30 m column (0.25 mm internal diameter, 0.25 mM film thickness, Agilent, USA). The inlet temperature was maintained at 250°C and samples were injected in split 10 mode. He carrier gas flow was adjusted to 1 ml min-1. Alkanes were used for referencing of retention times. For further details (GC-MS sample preparation and analysis) see the related publication (Rickert et al. submitted to PLOS ONE).

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Two complementary de facto standards for the publication of electronic documents are HTML on theWorldWideWeb and Adobe s PDF (Portable Document Format) language for use with Acrobat viewers. Both these formats provide support for hypertext features to be embedded within documents. We present a method, which allows links and other hypertext material to be kept in an abstract form in separate link databases. The links can then be interpreted or compiled at any stage and applied, in the correct format to some specific representation such as HTML or PDF. This approach is of great value in keeping hyperlinks relevant, up-to-date and in a form which is independent of the finally delivered electronic document format. Four models are discussed for allowing publishers to insert links into documents at a late stage. The techniques discussed have been implemented using a combination of Acrobat plug-ins, Web servers and Web browsers.

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1 Brief von Max Horkheimer an Abel, 16.03.1936; 3 Briefe zwischen Hubert Abrahamsohn und Max Horkheimer, 1935-1936, 21.12.1936; 2 Briefe zwischen Emanuel Adler und Max Horkheimer, 12.04.1946, 26.04.1946; 2 Briefe zwischen Max Adler und Max Horkheimer, 16.03.1935, 29.03.1935; 1 Brief von Eva Ahamson an Max Horkheimer, 01.11.1944; 2 Briefe der Aircraft Warning Service Brentwood an Max Horkheimer, Mai 1942; 6 Briefe zwischen Librairie Félix Alcan und Max Horkheimer, 1935, 18.12.1935; 11 Briefe zwischen Franz Alexander und Max Horkheimer, 1938-1940; 2 Briefe zwischen der American Historical Review New York und Max Horkheimer, 01.04.1941, 07.04.1941; 1 Brief von Paul Reiwald an Max Horkheimer, 18.10.1940; 2 Briefe zwischen Helen Manice Alexander und Max Horkheimer, 1936; 2 Briefe zwischen Bernardine Allen und Max Horkheimer, 17.06.1938, 24.06.1938; 1 Brief der Alumni Federation of Columbia University an Max Horkheimer, 21.07.1942; 1 Brief der American Friends Service Comittee an Max Horkheimer, 10.12.1940; 3 Briefe zwischen der American Academy of Political and Social Science Philadelphia und Max Horkheimer, 1939,1940, 16.01.1939; 1 Brief der American Automobile Association Washington an Max Horkheimer, 22.03.1938; 1 Brief der American Association for the Advancement of Science Washington an Max Horkheimer, 16.08.1937; 2 Briefe von Max Horkheimer an den American Consulate General Berlin, 1939; 1 Brief von Max Horkheimer an den American Consulate General Havana, 03.03.1941; 4 Briefe von Max Horkheimer an den American Consul London, 1939-1941; 2 Briefe von Max Horkheimer an den American Consulate General Stuttgart, 1939-1941; 1 Brief von Max Horkheimer an den American Consul Zürich, 1939; 1 Brief von Friedrich Pollock an den American Council of Learned Society, Washington, 27.06.1941; 2 Briefe von Max Horkheimer an die American Friends of German Freedom New York, 1941; 4 Briefe der American Historical Association Washington an Max Horkheimer, 1937-1938; 1 Brief von Max Horkheimer an den American Red Cross Westwood Office, 21.06.1943; 18 Briefe zwschen der American Society for the Prevention of Cruelty to Animals New York und Max Horkheimer, 1936-1941; 1 Brief von Max Horkheimer an die American Women's Volunteer Service Pacific Palisades, 27.07.1942; 23 Briefe zwischen Eugene Anderson und Max Horkheimer, 1937-1941; 2 Briefe zwischen Norah Andreae und Max Horkheimer, 27.10.1944, 09.09.1946; 1 Brief von Rosa Nebel-Schenk, 04.03.1946; 1 Brief von der National Catholic Welfare Conference, 14.08.1944; 12 Briefe zwischen Werner Andreae und Max Horkheimer, 1945-1954; 1 Brief von Julius Marx an Werner Andreae, 10.05.1946, 11.05.1950; 2 Briefe von Josef Messinger an Werner Andreae, 23.10.1946, ohne Datum; 3 Briefe zwischen dem Advokatenbüro Hodler und Max Horkheimer, 1946, 09.05.1946;

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veröffentlicht in: Schopenhauer, Arthur : Arthur Schopenhauers sämtliche Werke - München : Piper - Bd. 14 : Der Briefwechsel Arthur Schopenhauers ; 1 (1799 - 1849), Nr. 270