Made available in DSpace on 2014-06-11T19:27:16Z (GMT). No. of bitstreams: 0 Previous issue date: 2010-10-07Bitstream added on 2014-06-13T19:55:40Z : No. of bitstreams: 1 medeiros_mab_me_jabo.pdf: 498854 bytes, checksum: 73074b86ac0db45184c33210013d1ef4 (MD5) / Coordenação de Aperfeiçoamento de Pessoal de Nível Superior (CAPES) / O estudo teve por objetivo determinar a prevalência da brucelose bovina entre fornecedores de leite de um laticínio situado no Município de Itirapuã, Estado de São Paulo, analisar fatores de risco eventualmente associados à ocorrência de brucelose nos rebanhos estudados e analisar o desempenho de testes sorológicos para detectar a infecção. De uma população de 942 bovinos adultos distribuídos em 55 rebanhos, situados nos municípios de Itirapuã e de Patrocínio Paulista, foi obtida uma amostra voluntária composta por 813 animais, distribuídos em 37 rebanhos cujos proprietários aceitaram participar do estudo. Foi aplicado um questionário, para a obtenção de informações sobre fatores que pudessem estar associados às taxas de prevalência. Foram colhidas amostras de soro sanguíneo de todos animais, as quais foram submetidas ao teste do antígeno acidificado tamponado (AAT), e as amostras positivas nesse teste foram submetidas à reação de fixação de complemento (RFC). Foram obtidas amostras de leite do conjunto de cada rebanho participante do estudo, que foram examinadas pelo teste do anel do leite (TAL). Das 813 amostras de soro sanguíneo colhidas, 26 (3,2%) resultaram positivas na aplicação em série dos testes de triagem (AAT) e confirmatório (RFC), e das 37 propriedades estudadas, 12 (32,4%) apresentaram pelo menos um animal positivo. Os fatores que se mostraram associados à ocorrência de brucelose foram número de animais no rebanho, não utilização da vacina B19 e compra frequente de animais. Não se observou boa concordância entre o TAL, que apontou resultado positivo em quatro (10,8%) dos 37 rebanhos, e os testes sorológicos individuais na detecção de rebanhos infectados / The aim of this investigation was to verify the prevalence of bovine brucellosis among milk suppliers of a dairy industry located in the municipality of Itirapuã, state of São Paulo, Brazil, analyze risk factors eventually associated with the occurrence of brucellosis among the herds involved in the study, and compare the performance of serological tests in detecting infected herds. From a population of 942 adult cattle in 55 herds, in the municipalities of Itirapuã and Patrocínio Paulista, a voluntary sample of 813 animals was obtained in 37 herds whose owners agreed in participating in the study. A questionnaire about risk factors that could be associated to the prevalence rates was applied. Serum samples of all the 813 animals were collected and tested by the rose Bengal plate test (RBPT); positive samples were then tested by the complement fixation test (CFT). Milk samples were taken from each can at the industry and tested by the milk ring test (MRT). Of the 813 serum samples, 26 (3.2) tested positive in the serial application of RBPT and CFT, and of the 37 herds, 12 (32.4%) had at least one positive animal. Factors that showed association with the prevalence rate were number of animals in the herd, lack of vaccination with strain 19 and frequent introduction of animals. The agreement between individual serological tests and MRT to detect infected herds was not good, since MRT showed positive results in only four (10.8%) of the 37 herds

No description available.

The Seven Years’ War and the resulting Treaty of Paris of 1763 represent a watershed in British domestic and imperial histories. Not only did the war result in Britain acquiring vast new territories and rights in North America and South Asia, but it also saddled Britain with a national debt of over £140,000,000. The challenge for British politicians in the post-1763 era was not only finding a balance between the need to secure territorial gains while searching for a means to reduce costs and raise revenues to pay down the debt, but rather to do so without infringing on the constitutional rights of colonists and chartered companies. The political ramifications of the Treaty of Paris were equally important. Disputes over the terms of the Peace tore apart the Newcastle-Pitt coalition, resulting in the dissolution of the Whig Broadbottom. With the Duke of Newcastle and his allies in opposition alongside William Pitt, the political situation was thrown into turmoil. Although the confused state of politics in the short-term undoubtedly resulted in an opposition which acted, as Namier suggested, on the basis of self-interest rather than on principles, it can also be said to have provided the matrix within which historians can observe the genesis of new policies of domestic and imperial governance. It was precisely the lack of ideological identification in politics at the accession of George III that allowed British political ideologies in the age of the American Revolution to so quickly develop alongside the formulation and implementation of, as well as in the opposition responses to, the new challenges facing British parliamentarians in the governance of the Empire. This work therefore traces the development of distinct imperial ideologies among British politicians as they emerged in response to the various imperial crises of the 1760s and 1770s. Additionally, it will be shown that the new and unprecedented crises in both American and Indian affairs were brought about primarily as a means of obtaining revenues for the Treasury. The interrelated nature of the imperial problems in the east and the west, as well as the attempts of British politicians to resolve them, will be examined primarily through the policies made surrounding the article of tea.

Present study deals with training and development strategies in IT service industry in Kolkata region. This study highlighted present trends and common practices in training and development activities in specific and in human resources management in general. InfoTech sector is a thrust area of economic development in developing economies, like in India. Government and private joint initiatives make this sector a sunshine industry sector. Potentials of human resources explore in the professionally managed IT service companies. The training and development activities strengthen capabilities of IT service companies and help them to achieve excellence. Present study evaluated the heart of this knowledge industry, which centered on knowledge workers. Present study briefly elaborated the training and development practices of two top-ranked companies in Kolkata and found some unique modes of delivery of training. This study also pointed out that companies placed in higher value-chain have long-term vision as compared to ones in lower in value-chain.

Le Golfe du Bengale (GdB), dans l'océan indien Nord, est sous l'influence d'intenses vents de mousson, qui se renversent saisonnièrement. Les fortes pluies et les apports fluviaux associés à la mousson de Sud-Ouest font du GdB l'une des régions les moins salées des océans tropicaux. La forte stratification haline proche de la surface qui en découle contribue à limiter le mélange vertical, ce qui maintient des températures de surface élevées et favorise la convection atmosphérique et les pluies. Cette stratification en sel a ainsi des implications profondes sur les échanges air-mer et sur le climat des pays riverains. L'objectif de ma thèse est d'améliorer la description de la variabilité de la salinité de surface (SSS) du GdB, et de comprendre ses mécanismes aux échelles de temps saisonnières à interannuelles. Les climatologies existantes ont permis de mettre en évidence un cycle saisonnier marqué de la SSS, avec un dessalement intense de la partie Nord du bassin pendant l'automne, suivi par une expansion de ces eaux dessalées le long du bord Ouest du bassin. Cette langue dessalée s'érode finalement pendant l'hiver, pour revenir à son extension minimale au printemps. Cependant, la rareté des observations in-situ de SSS ne permet d'observer les fluctuations interannuelles autour de ce cycle saisonnier que de manière parcellaire dans le GdB. Le développement récent de la télédétection spatiale de la SSS (missions SMOS et AQUARIUS) a ouvert de nouvelles opportunités à cet égard. Cette technologie reste toutefois délicate dans le cas d'un bassin de petite taille tel que le GdB, du fait des contaminations éventuelles du signal de SSS par les interférences radio et par les sources d'origine continentale. Une validation systématique des produits satellites par comparaison à un jeu de données in-situ exhaustif montre qu'Aquarius capture de façon réaliste les évolutions saisonnières et interannuelles de la SSS partout dans le GdB. A l'inverse, SMOS ne parvient pas à restituer une salinité meilleure que les climatologies existantes. / Located in the Northern Indian Ocean, the Bay of Bengal (BoB) is forced by intense seasonally reversing monsoon winds. Heavy rainfall and strong river runoffs associated with the southwest monsoon makes the bay one of the freshest regions in the tropical ocean. This surface fresh water flux induces strong near surface salinity stratification, which reduces vertical mixing and maintains high sea surface temperatures and deep atmospheric convection and rainfall. This intense near surface haline stratification has therefore profound implications on the air-sea exchanges, and on the climate of the neighboring countries. The goal of my thesis is to improve the description of the Sea surface salinity (SSS) variability in the BoB and to understand the oceanic and atmospheric processes driving this variability at seasonal and interannual timescales. Existing climatologies reveal a marked seasonal cycle of SSS with an intense freshening of the northern part of the basin during fall that subsequently spreads along the western boundary. This fresh pool finally erodes during winter, to reach its minimal extent in spring. The paucity of in-situ SSS observations however prevented to monitor the interannual fluctuations around this seasonal picture with a good spatial coverage. The recent development of SSS remote-sensing capabilities (with SMOS and AQUARIUS satellites) may help with that regard. However this is particularly challenging for a small semi-enclosed basin such as the Bay of Bengal, because of the potential contamination of the SSS signal by radio frequency interferences and land effects in the near coastal environment. A thorough validation of these satellite products to an exhaustive gridded in-situ dataset shows that Aquarius reasonably captures the large-scale observed seasonal and interannual SSS evolution everywhere in the BoB while SMOS does not perform better than existing climatologies, advocating for improvements of its SSS retrieval algorithm there.

The early history of Arakan has been generally considered to be that of a province of eastern India, and hence its study has been neglected by both Indian and Southeast Asian historians. This dissertation seeks to examine the dynamics of the history from the beginnings of urbanization until the rise of the Burmese empire which subsequently dominated Arakanese culture. The first chapter deals with the geographical and ethnolinguistic background to the development of the earliest cities. In the second, all the inscriptions of the period, in Sanskrit, Pali and Pyu are catalogued and edited. The inscriptions issued by the kings establish a chronology for the period and illustrate the nature of the cult surrounding the institution of kingship, while copper-plate and votive inscriptions elucidate the nature of state organisation and the popular religion. Chapter Three deals with the coinage which emerged following the development of a centralised economy, and discusses the impetus for this and the role of the king on whom the prosperity of the country depended. A comparison with similar coin types in Southeast Asia is made and the catalogue includes all the coins yet discovered. The sites of the most important monuments are discussed in Chapter Four, which catalogues all the architectural and sculptural remains. A comparative analysis of the Buddhist and Hindu images and of the minor arts reveals, to a greater extent that do the inscriptions, the nature of contact with India and the rest of Southeast Asia. The conclusion deals with the political and cultural history which thus emerges, examining in detail the rationale behind the development of the concept of divine kingship in Arakan.

Recent years witnessed a vast advent of stalagmites as palaeoclimate archives. The multitude of geochemical and physical proxies and a promise of a precise and accurate age model greatly appeal to palaeoclimatologists. Although substantial progress was made in speleothem-based palaeoclimate research and despite high-resolution records from low-latitudinal regions, proving that palaeo-environmental changes can be archived on sub-annual to millennial time scales our comprehension of climate dynamics is still fragmentary. This is in particular true for the summer monsoon system on the Indian subcontinent. The Indian summer monsoon (ISM) is an integral part of the intertropical convergence zone (ITCZ). As this rainfall belt migrates northward during boreal summer, it brings monsoonal rainfall. ISM strength depends however on a variety of factors, including snow cover in Central Asia and oceanic conditions in the Indic and Pacific. Presently, many of the factors influencing the ISM are known, though their exact forcing mechanism and mutual relations remain ambiguous. Attempts to make an accurate prediction of rainfall intensity and frequency and drought recurrence, which is extremely important for South Asian countries, resemble a puzzle game; all interaction need to fall into the right place to obtain a complete picture. My thesis aims to create a faithful picture of climate change in India, covering the last 11,000 ka. NE India represents a key region for the Bay of Bengal (BoB) branch of the ISM, as it is here where the monsoon splits into a northwestward and a northeastward directed arm. The Meghalaya Plateau is the first barrier for northward moving air masses and receives excessive summer rainfall, while the winter season is very dry. The proximity of Meghalaya to the Tibetan Plateau on the one hand and the BoB on the other hand make the study area a key location for investigating the interaction between different forcings that governs the ISM. A basis for the interpretation of palaeoclimate records, and a first important outcome of my thesis is a conceptual model which explains the observed pattern of seasonal changes in stable isotopes (d18O and d2H) in rainfall. I show that although in tropical and subtropical regions the amount effect is commonly called to explain strongly depleted isotope values during enhanced rainfall, alone it cannot account for observed rainwater isotope variability in Meghalaya. Monitoring of rainwater isotopes shows no expected negative correlation between precipitation amount and d18O of rainfall. In turn I find evidence that the runoff from high elevations carries an inherited isotopic signature into the BoB, where during the ISM season the freshwater builds a strongly depleted plume on top of the marine water. The vapor originating from this plume is likely to memorize' and transmit further very negative d18O values. The lack of data does not allow for quantication of this plume effect' on isotopes in rainfall over Meghalaya but I suggest that it varies on seasonal to millennial timescales, depending on the runoff amount and source characteristics. The focal point of my thesis is the extraction of climatic signals archived in stalagmites from NE India. High uranium concentration in the stalagmites ensured excellent age control required for successful high-resolution climate reconstructions. Stable isotope (d18O and d13C) and grey-scale data allow unprecedented insights into millennial to seasonal dynamics of the summer and winter monsoon in NE India. ISM strength (i. e. rainfall amount) is recorded in changes in d18Ostalagmites. The d13C signal, reflecting drip rate changes, renders a powerful proxy for dry season conditions, and shows similarities to temperature-related changes on the Tibetan Plateau. A sub-annual grey-scale profile supports a concept of lower drip rate and slower stalagmite growth during dry conditions. During the Holocene, ISM followed a millennial-scale decrease of insolation, with decadal to centennial failures resulting from atmospheric changes. The period of maximum rainfall and enhanced seasonality corresponds to the Holocene Thermal Optimum observed in Europe. After a phase of rather stable conditions, 4.5 kyr ago, the strengthening ENSO system dominated the ISM. Strong El Nino events weakened the ISM, especially when in concert with positive Indian Ocean dipole events. The strongest droughts of the last 11 kyr are recorded during the past 2 kyr. Using the advantage of a well-dated stalagmite record at hand I tested the application of laser ablation-inductively coupled plasma-mass spectrometry (LA-ICP-MS) to detect sub-annual to sub-decadal changes in element concentrations in stalagmites. The development of a large ablation cell allows for ablating sample slabs of up to 22 cm total length. Each analyzed element is a potential proxy for different climatic parameters. Combining my previous results with the LAICP- MS-generated data shows that element concentration depends not only on rainfall amount and associated leaching from the soil. Additional factors, like biological activity and hydrogeochemical conditions in the soil and vadose zone can eventually affect the element content in drip water and in stalagmites. I present a theoretical conceptual model for my study site to explain how climatic signals can be transmitted and archived in stalagmite carbonate. Further, I establish a first 1500 year long element record, reconstructing rainfall variability. Additionally, I hypothesize that volcanic eruptions, producing large amounts of sulfuric acid, can influence soil acidity and hence element mobilization. / Stalagmiten erfuhren in den letzten Jahren vermehrt Aufmerksamkeit als bedeutende Paläoklima- Archive. Paläoklimatologen sind beeindruckt von der grossen Zahl geochemischer und physikalischer Indikatoren (Proxies) und der Möglichkeit, präzise absolute Altersmodelle zu erstellen. Doch obwohl substantielle Fortschritte in der speleothem-basierten Klimaforschung gemacht wurden, und trotz hochaufgelöster Archive aus niederen Breiten, welche zeigen, das Umweltveränderungen auf Zeitskalen von Jahren bis Jahrtausenden archiviert und rekonstruiert werden können, bleibt unser Verständnis der Klimadynamik fragmentarisch. Ganz besonders gilt dies für den Indischen Sommermonsun (ISM) auf dem Indischen Subkontinent. Der ISM ist heute als ein integraler Bestandteil der intertropischen Konvergenzzone verstanden. Sobald dieser Regengürtel während des borealen Sommer nordwärts migriert kann der ISM seine feuchten Luftmassen auf dem Asiatischen Festland entladen. Dabei hängt die Stärke des ISM von einer Vielzahl von Faktoren ab. Zu diesen gehören die Schneedicke in Zentralasien im vorhergehenden Winter und ozeanische Bedingungen im Indischen und Pazifschen Ozean. Heute sind viele dieser Faktoren bekannt. Trotzdem bleiben deren Mechanismen und internen Verbindungen weiterhin mysteriös. Versuche, korrekte Vorhersagen zu Niederschlagsintensität und Häufigkeit oder zu Dürreereignissen zu erstellen ähneln einem Puzzle. All die verschiedenen Interaktionen müssen an die richtige Stelle gelegt werden, um ein sinnvolles Bild entstehen zu lassen. Meine Dissertation versucht, ein vertrauenswürdiges Bild des sich wandelnden Holozänen Klimas in Indien zu erstellen. NE Indien ist eine Schlüsselregion für den östlichen Arm des ISM, da sich hier der ISM in zwei Arme aufteilt, einen nordwestwärts und einen nordostwärts gerichteten. Das Meghalaya Plateau ist das erste Hindernis für die sich nordwärts bewegenden Luftmassen und erhält entsprechend exzessive Niederschläge während des Sommers. Die winterliche Jahreszeit dagegen ist sehr trocken. Die Nähe zum Tibetplateau einerseits und der Bucht von Bengalen andererseits determinieren die Schlüsselposition dieser Region für das Studium der Interaktionen der den ISM beeinflussenden Kräfte. Ein Fundament für die Interpretation der Paläoklimarecords und ein erstes wichtiges Ergebnis meiner Arbeit ist ein konzeptuelles Modell, welches die beobachteten saisonalen Veränderungen stabiler Isotope (d18O und d2H) im Niederschlag erklärt. Ich zeige, das obwohl in tropischen und subtropischen Regionen meist der amount effect zur Erklärung stark negativer Isotopenwerte während starker Niederschläge herangezogen wird, dieser allein nicht ausreicht, um die Isotopenvariabilität im Niederschlag Meghalaya's zu erklären. Die Langzeitbeobachtung der Regenwasserisotopie zeigt keine negative Korrelation zwischen Niederschlagsmenge und d18O. Es finden sich Hinweise, das der Abfluss aus den Hochgebirgsregionen Tibets und des Himalaya eine Isotopensignatur an das Oberflächenwasser der Bucht von Bengalen vererbt. Dort bildet sich aus isotopisch stark abgereicherten Wässern während des ISM eine Süsswasserlinse aus. Es ist wahrscheinlich, das Wasserdampf, der aus dieser Linse stammt, ein Isotopensignal aufgeprägt bekommt, welches abgereichertes d18O weitertransportiert. Der Mangel an Daten lässt es bisher leider nicht zu, quantitative Aussagen über den Einfluss dieses plume effect' auf Niederschläge in Meghalaya zu treffen. Es lässt sich allerdings vermuten, das dieser Einfluss auf saisonalen wie auch auf langen Zeitskalen variabel ist, abhängig vom Abfluss und der Quellencharacteristik. Der Fokus meiner Arbeit liegt in der Herauslösung klimatischer Signale aus nordostindischen Stalagmiten. Hohe Urankonzentrationen in diesen Stalagmiten erlaubt eine exzellente Alterskontrolle, die für hochauflösende Klimarekonstruktionen unerlässlich ist. Die stabilen Isotope (d18O und d13C), sowie Grauwertdaten, erlauben einmalige Einblicke in die Dynamik des Sommer und auch des Wintermonsun in NE Indien. Die ISM Stärke (d. h. Niederschlagsmenge) wird in Veränderungen in den d18Ostalagmites reflektiert. Das d13C Signal, welches Tropfratenänderungen speichert, dient als potenter Indikator für winterliche Trockenheitsbedingungen. Es zeigt Ähnlichkeit zu temperaturabhängigen Veränderungen auf dem Tibetplateau. Das sub-annuell aufgelöste Grauwertprofil stärkt das Konzept, das verminderte Tropfraten und langsameres Stalagmitenwachstum eine Folge von Trockenheit sind. Während des Holozäns folgte der ISM der jahrtausendelangen Verringerung der Insolation. Es finden sich aber ebenso rapide Anomalien, die aus atmosphärischen Veränderungen resultieren. Die Phase des höchsten Niederschlages und erhöhter Saisonalität korrespondiert mit dem Holozänen Thermalen Maximum. Nach einer Phase einigermassen stabilen Bedingungen begann vor ca. 4500 Jahren ENSO einen zunehmenden Einfluss auf den ISM auszuüben. Starke El Nino Ereignisse schwächen den ISM, besonders wenn diese zeitgleich mit positiven Indian Ocean Dipole Ereignissen auftreten. Die stärksten Dürren des gesamten Holozäns traten in den letzten 2000 Jahren auf. Um zusätzliche Informationen aus den hervorragenden Proben zu gewinnen nutzte ich die Vorteile der laser ablation inductively coupled plasma mass spectrometry (LA-ICP-MS). Diese erlaubt die Detektion sub-annueller bis sub-dekadischer Elementkonzentrationsveränderungen in Stalagmiten. Mittels einer neu entwickelten Ablationszelle konnten Proben von maximal 22 cm Länge untersucht werden. Jedes analysierte Element ist ein potentieller Träger einer Klimainformation. Die Kombination der früheren Ergebnisse mit denen der LA-IPC-MS zeigt, das die Elementkonzentrationen nicht nur von Niederschlagsveränderungen und assoziiertem Auswaschen aus dem Boden abhängen. Zusätzlich können auch die biologische Aktivität und hydrogeochemische Bedingungen in der vadosen Zone Einfluss auf die Elementzusammensetzung im Tropfwasser und in den Stalagmiten haben. Darum entwickelte ich ein theoretisches Modell für meinen Standort, um zu klären, wie Klimasignale von der Atmosphäre in die Höhle transportiert werden können. Ein anschliessend rekonstruierter 1500 Jahre langer Proxyrecord zeigt Niederschlagsvariabilität an. Zudem besteht die Möglichkeit, das Vulkaneruptionen, welche grosse Mengen an Schwefelsäure produzieren, eine Bodenversauerung verursachen und damit die Elementmobilisierung verstärken können.

NJ, Univ., Dep. of Economics, Diss.--Princeton, 2004. / Kopie, ersch. im Verl. UMI, Ann Arbor, Mich. - Enth. 3 Beitr.

A bacia de Bengala, localizada a Nordeste da Índia tem uma história evolutiva extraordinária, diretamente controlada bela fragmentação do Gondwana. O início da formação desta bacia é considerada como sendo relacionada ao final do evento da quebra, datado em 126 Ma quando a Índia separou do continente Antártico e da Austrália. Desde então, a placa continental Indiana viajou do pólo sul a uma velocidade muito rápida (16 cm/a) chocando-se com o hemisfério norte e fundindo-se com a Placa Eurasiana. Durante a viagem passou por cima de um hot spot, onde hoje estão localizadas as ilhas Seicheles, resultando em um dos maiores derrames de lava basáltica do mundo, conhecido como Deccan Trap. Na região onde a bacia de Bengala foi formada, não houve aporte significativo de sedimentos siliciclásticos, resultando na deposição de uma espessa plataforma carbonática do Cretáceo tardio ao Eoceno. Após este período, devido a colisão com algumas microplacas e a amalgamação com a Placa Eurasiana, um grande volume sedimentar siliciclástico foi introduzido para a bacia, associado também ao soerguimento da cadeia de montanhas dos Himalaias. Atualmente, a Bacia de Bengala possui mais de 25 km de sedimentos, coletados neste depocentro principal. Nesta dissertação foram aplicados conceitos básicos de sismoestratigrafia na interpretação de algumas linhas regionais. As linhas sísmicas utilizadas foram adquiridas recentemente por programa sísmico especial, o qual permitiu o imageamento sísmico a mais de 35km dentro da litosfera (crosta continental e transicional). O dado permitiu interpretar eventos tectônicos, como a presença dos Seawards Dipping Reflectors (SDR) na crosta transicional, coberto por sedimentos da Bacia de Bengala. Além da interpretação sísmica amarrada a alguns poços de controle, o programa de modelagem sedimentar Beicip Franlab Dionisos, foi utilizado para modelar a história de preenchimento da bacia para um período de 5,2 Ma. O nível relativo do nível do mar e a taxa de aporte sedimentar foram os pontos chaves considerados no modelo. Através da utilização dos dados sísmicos, foi possível reconhecer dez quebras de plataformas principais, as quais foram utilizadas no modelo, amarrados aos seus respectivos tempos geológico, provenientes dos dados dos poços do Plioceno ao Holoceno. O resultado do modelo mostrou que a primeira metade modelada pode ser considerada como um sistema deposicional retrogradacional, com algum picos transgressivos. Este sistema muda drasticamente para um sistema progradacional, o qual atuou até o Holoceno. A seção modelada também mostra que no período considerado o total de volume depositado foi em torno de 2,1 x 106 km3, equivalente a 9,41 x 1014 km3/Ma. / The Bengal Basin in Northeast India has a remarkable evolution history directly controled by the Gondwana fragmentation. The Beginning of this basin is considered related to the final break up event, dated as 126 Ma when India finally became separeted from Antarctica and Australia Continents. Since then, the India Continental Plate traveled from the South pole at very fast rate (16 cm/y) reaching the nortern hemisphere and merging with Eurasia Plate. During the travel it passed over a hot spot, located where is today Seychelles Island, resulting in one of the biggest basalt leakage, know as Deccan Trap. In the area where the Bengal Basin was formed during the travel there wasnt any supply of siliciclastics, resulting in the deposition of a very thick section of carbonate platforms from Late Cretaceous to Eocene. After this period, due to the collision with same microplates and the amalgamation with Eurasia Plate a huge siliciclastic supply was introduced in the basin, associated with rising of the Himalayas Mountains. Therefore, the Belgal Basin today has more than 25 km of sediments, collected in its main depocenter. In this dissertation it was applied to the basic concepts of seismostratigraphy in the interpretation of some regional lines. These seismic lines were acquired recently by a special survey program that allowed having good quality data until more than 35 km in the lithosphere (continental and transitional crust). The data permitted to interpret tectonic events such as the presence of Seawards Dipping Reflectors (SDR) in the transitional crust, covered by the Bengal Basin sediments. Besides the seismic interpretation tied to some well data, it was used in the dissertation a Beicip Franlab Software, known as Dionisos, to model and develop a basin fill history. The eustatic relative sea level flutuations and sediment rate of sediment influx are the key points to be considered in the model. Using the seismic data it was possible to recognize ten main platform breakes than were used in the model, tied to a geological time frame provided by the well data interpretation, from Pliocene to Holocene. The output of the model shown that a first half of the considered time predominated a major retrogradational system, with some minor trangression peaks. This changed to a very strong progradational system that is acting until the Holocene. The section modeled also shows a total of sediments deposited in the period considered was about 2,1 x106 km3 equivalent to a 9,41 x 1014 km3/Ma.

Fondé en 1955 par un fonctionnaire bengali, Ananda Marga, « la voie de la félicité », est une secte hindoue qui s’est donné un mode d’organisation à échelle planétaire et s’implique dans des activités missionnaires dans un grand nombre de pays. Dans le paysage religieux de l’Inde contemporaine, elle se distingue par les violences dont ses disciples ont été accusés. L’enquête ethnographique menée en son sein, l’analyse de sa littérature interne et le recueil de témoignages d’anciens disciples montrent que ces violences s’expliquent par les aspirations politiques de son fondateur et de ses membres ainsi que par l’instabilité de son assise économique. Mais pas uniquement. Elles visent également une mutation radicale de la personne du disciple et une transformation profonde la société, deux processus intimement liés. En se soumettant volontairement à des violences psychologiques et physiques, le disciple entend se soustraire aux limitations de l’existence ordinaire. S’il se libère ainsi du monde, c’est pour mieux agir dans le monde au service exclusif de son Gourou et de sa mission. Dotés d’une telle finalité, les actes de violence extrême apparaissent comme les expressions d’une ardeur dévotionnelle poussée à son paroxysme. Cette conception singulière de l’ascétisme prend source dans la culture tantrique bengalie, laquelle tient la force pour une manifestation de l’Énergie divine (śakti) et le Maître pour une divinité incarnée / Founded in 1955 by a Bengali civil servant, Ananda Marga, the "way of bliss", is a Hindu sect with worldwide organization and involved in missionary activities in a great number of countries. In the religious landscape of contemporary India, it is distinctively characterized by the violence for which its followers have been accused. The ethnographical research carried out among this sect, combined with the analysis of its internal literature and the collection of testimonies of former disciples shows that this violence can be explained by the political aspirations of its founder and its members as well as by instability of its economic base. But it can also be explained by two interrelated processes: the profound change in the person of the disciples and a radical transformation of the society. By submitting himself voluntarily to psychological and physical violence, a disciple tries to go over the limitations of ordinary existence. However, he frees himself from this world so that he can be in exclusive service to his Guru and his mission in this world. With such a purpose, acts of extreme violence appear as expressions of devotional fervour pushed to its climax. The source of this peculiar conception of asceticism can be traced in Bengali tantric culture, for which the force represents a manifestation of divine energy (śakti) and the Guru represents an incarnate deity