The eighteenth-century natural philosopher Mikhail Vasil'evich Lomonosov (1711-1765) has long been represented by Russian writers and scholars as an encyclopedic figure who not only pioneered the dissemination of a scientific ethos in Russia, but whose own innumerable contributions to science make him eminently worthy of inclusion in a pantheon among the greatest scientific minds. A robust mythology extolling Lomonosov's role in Russian science and culture formed in the years immediately following his death, and would increase in vigor while adapting to changing historical circumstances until well into the twentieth century. This dissertation explores the evolution of Lomonosov's imposing stature in Russian thought from the middle of the eighteenth century to the first decades of the Soviet period. It reveals much about the intersection in Russian culture of changing attitudes towards the meaning and significance of science, as well as about the rise of a Russian national identity of which Lomonosov became an outstanding symbol. / The processes by which myths can be used to create and shape historical memory are highlighted throughout this inquiry. At first, Lomonosov was depicted very generally as the pioneering Russian natural philosopher; later his contributions, still broadly framed, were conflated with select institutional agendas; finally historians of various disciplines appropriated his life in order to reinforce their own professional strategies. Even as the myth of Lomonosov grew more elaborate, however, it was the inspiring idea of Lomonosov's heroic determination to propagate science, culture, and education within Russia and his successful struggles against myriad obstacles to achieve this end that remained the primary and enduring biographical element. It is this image with which my study is principally concerned.

Thesis (Ph. D.)--University of Wisconsin--Madison, 1963. / Typescript. Vita. eContent provider-neutral record in process. Description based on print version record. Includes bibliographical references (leaves 170-177).

No description available.

Diss.--Lett.--Tübingen--Univ., Neuphilologischen Fakultät, 1998. / Bibliogr. p. 178-185. Notes bibliogr.

During the first half of the XVIIIth century in Russia, deep social and cultural changes led to a chaotic linguistic situation. The Russian scholar Michail Lomonosov played a key role in the grammatical and lexical organization of the Russian literary language around the middle of the century. His contributions are reviewed and their importance analyzed in the present thesis. / Chapter One provides an analysis of the linguistic situation during the first half of the XVIIIth century. The role and the functions of different linguistic elements are examined, including West European lexical borrowings, the native Russian, the Church Slavonic, and their mutual interactions. / Chapters two and three analyze M. Lomonosov's role in the standardization of Russian grammar and vocabulary by examining his two major philological works: the "Rossiaeiskaeiia Grammatika" and the article "Predislovie o polbze knig tserkovnikh v rossiiskom yazike." / Although Lomonosov's merit is widely acknowledged among scholars, the importance of his stylistic theory has been challenged lately. In Chapter Four, Lomonosov's linguistic contributions to the development of the modern Russian literary language are weighed and assessed against these critical arguments.

No description available.

No description available.

O presente trabalho se propõe a esboçar a primeira apresentação em língua portuguesa de uma das mais importantes figuras do pensamento, letras e educação da Rússia, absolutamente central em seu desenvolvimento técnico, científico e literário, Mikhail Vassílievitch Lomonóssov. Nele, juntamente com uma introdução provendo uma contextualização geral do século XVIII russo, seguida de um panorama biográfico do polímata centrado em sua produção literária e findada em um relato sobre sua contribuição para a formação da língua russa moderna, são apresentadas as traduções integrais de quatro obras suas na área das letras, duas das quais poemas longos acrescidos de comentários, bem como outras traduções secundárias ilustrativas da primeira parte. / The goal of the present work is to provide a sketch presenting for the first time in Portuguese language one of the most important individuals in Russian thought, language and education, who played a fundamental role in the technological, scientific and literary development of the country, Mikhail Vasilievitch Lomonosov. Here, along with an introduction containing a general outline of 18th century Russia, followed by a biographical overview of the polymath and ending in an account of his main contributions to the shaping of the modern Russian language, four full translations of his works in the realm of letters are presented, two of which duly commented long poems, as well as minor secondary translations, illustrating the first part.

O presente trabalho se propõe a esboçar a primeira apresentação em língua portuguesa de uma das mais importantes figuras do pensamento, letras e educação da Rússia, absolutamente central em seu desenvolvimento técnico, científico e literário, Mikhail Vassílievitch Lomonóssov. Nele, juntamente com uma introdução provendo uma contextualização geral do século XVIII russo, seguida de um panorama biográfico do polímata centrado em sua produção literária e findada em um relato sobre sua contribuição para a formação da língua russa moderna, são apresentadas as traduções integrais de quatro obras suas na área das letras, duas das quais poemas longos acrescidos de comentários, bem como outras traduções secundárias ilustrativas da primeira parte. / The goal of the present work is to provide a sketch presenting for the first time in Portuguese language one of the most important individuals in Russian thought, language and education, who played a fundamental role in the technological, scientific and literary development of the country, Mikhail Vasilievitch Lomonosov. Here, along with an introduction containing a general outline of 18th century Russia, followed by a biographical overview of the polymath and ending in an account of his main contributions to the shaping of the modern Russian language, four full translations of his works in the realm of letters are presented, two of which duly commented long poems, as well as minor secondary translations, illustrating the first part.

Abstract In this Ph.D. thesis sediment cores from the central Arctic Ocean, southwestern Barents Sea and sediment exposures from the Kola Peninsula were investigated in order to reveal interactions between the late middle Pleistocene and late Pleistocene Arctic ice sheets, between Marine Isotope Stages 6 and 1 (MIS 6 and MIS 1). One of the main objectives of this work is to establish provenance areas for the sediments studied in the central Arctic, the southwestern (SW) Barents Sea and the Kola Peninsula, their transport mechanisms and through that their relationship to glaciations in the Arctic and to development in the Kola Peninsula during the late middle and late Pleistocene. Mineralogical and geochemical data from the core 96/12-1pc on the Lomonosov Ridge, central Arctic Ocean was studied to evaluate ice transport from circum-Arctic ice sheets and variability in sediment drainage systems associated with their decay. SW Barents Sea sediments contain important information on Late Glacial and Holocene sediment provenance characteristics in relation to ice flow patterns and ice rafting from different regional sectors. The studied SW Barents Sea sediment cores show that sediments were most likely derived from a combination of far-field Fennoscandian sources, local subcropping Mesozoic strata below the seafloor and sea ice transport. The investigation carried out on the Kola Peninsula indicates that the Eemian (MIS 5e) marine environment in the White Sea Basin and onshore coastal areas gradually changed into a glaciolacustrine environment during MIS 5d to MIS 5a. Subsequently, the Scandinavian Ice Sheet (SIS) covered the Kola Peninsula, most probably during MIS 4. The final deglaciation of the SIS on the Kola Peninsula took place, however, during the late Weichselian (MIS 2) between 16–12 ka. / Tiivistelmä Tässä väitöstutkimuksessa tutkittiin sedimenttikairanäytteitä keskeiseltä Jäämereltä ja Lounais-Barentsinmereltä sekä tarkasteltiin sedimenttiseurantoja Kuolan niemimaalla tarkoituksena selvittää myöhäisen keskipleistoseeni- ja myöhäispleistoseeniajan Arktisten jääkenttien keskinäiset vuorovaikutukset erityisesti merellisten isotooppivaiheiden 6 ja 1 (MIS 6 ja MIS 1) välillä. Tämän työn yhtenä päätavoitteena on määritellä sedimenttien lähdealueet keskeisellä Arktiksella, lounaisella Barentsinmerellä ja Kuolan niemimaalla, sedimenttien kuljetusmekanismit ja näiden perusteella riippuvuudet Arktisiin jäätiköihin ja Kuolan niemimaalla tapahtuneeseen myöhäiskeski- ja myöhäispleistoseenin kehitykseen. Mineraloginen ja geokemiallinen tieto Lomonosovin harjanteen kairauksesta 96/12-1pc, keskeisellä Jäämerellä on perusta arvioitaessa jääkuljetusmekanismeja ympäröiviltä sirkum-Arktisilta jäätiköiltä ja arvioitaessa valuma-alueiden osuutta suhteessa näiden jäätiköiden häviämiseen. Lounaisen Barentsinmeren sedimentit sisältävät tärkeätä tietoja viimeisen jäätiköitymisen loppuvaiheen ja holoseeni-ajan sedimenttien lähdealueista ja suhteista jäävirtauksiin ja jääkuljetukseen eri aluesektoreilta. Tutkitut Lounais-Barentsinmeren sedimentit osoittavat, että sedimentit olivat todennäköisimmin peräisin suhteellisen kaukaisilta Fennoscandian lähdealueilta, paikallisista mesotsoosista merenpohjan kerrostumista ja merijään kuljettamasta materiaalista. Kuolan niemimaalla tehty tutkimus osoittaa, että Eem-kauden (MIS 5e) meriympäristö Vienanmeren altaassa ja rannikkoalueilla vähitellen muuttui glaciolakustriseksi ympäristöksi MIS 5d:n ja MIS 5a:n välisenä aikana. Sen jälkeen Skandinavian jääkenttä (SIS) peitti Kuolan niemimaan, todennäköisimmin koko MIS:n 4 ajanjakson. SIS:n lopullinen deglasiaatio alkoi Kuolan niemimaalla kuitenkin myöhäisen Veiksel-jääkauden (MIS 2) aikana noin 16–12 ka sitten.