Submitted by Maicon Juliano Schmidt (maicons) on 2015-03-24T19:11:22Z No. of bitstreams: 1 Carlos Hiroshi Nitta.pdf: 684742 bytes, checksum: 0857f27947f3270ae0fa6aba1e59c2da (MD5) / Made available in DSpace on 2015-03-24T19:11:22Z (GMT). No. of bitstreams: 1 Carlos Hiroshi Nitta.pdf: 684742 bytes, checksum: 0857f27947f3270ae0fa6aba1e59c2da (MD5) Previous issue date: 2008-01-31 / Nenhuma / Os tatus (Cingulata: Dasypodidae), apesar da diversidade de espécies, 21 espécies, e ampla distribuição, da Argentina até a metade sul dos EUA, passando pela América Central, as informações sobre a utilização dos ambientes por estes animais é escassa. A escavação e utilização de buracos no solo é uma característica ecológica relevante para o grupo, podendo estas estruturas serem consideradas indicadores conspícuos da presença desses animais. No presente estudo investiguei a densidade, direção, morfometria e microhabitat das tocas, em diferentes tipos de formação vegetal. O trabalho foi desenvolvido durante 13 meses (Out/06 a Nov/07) no Parque Estadual de Itapuã, na Grande Porto Alegre, RS, Brasil. O tatu-galinha (Dasypus novemcinctus) parece ser a espécie mais abundante neste local, onde ainda ocorre ao menos uma outra espécie, tatu-de-rabo-mole-grande (Cabassous tatouay). As características físicas e ambientais de 72 tocas, no campo (n = 31), mata (n = 22) e Restinga (n = 19), encontradas foram analisadas. A densidade de tocas não variou significativamente entre estes ambientes. Embora o tatu-galinha seja apontado como uma espécie de áreas florestadas no presente estudo, as áreas abertas foram utilizadas com a mesma intensidade que mata e restinga. Dentre as variáveis ambientais o número de árvores e porcentagem de cobertura de solo por arbustos tiveram influência no número de tocas encontradas em mata. A direção das tocas foram predominantemente sul nas áreas de floresta (mata e restinga) e significativamente diferentes das áreas de campo (campoXmata p = 0,002; campoXrestinga p = 0,001). Sugerindo que esta espécie possa mudar o comportamento e aumentar o nicho na ausência ou relaxamento de predadores e competidores. / Armadillos ( Cingulata : Dasypodidae ), despite the diversity of species , 21 species , and wide distribution , from Argentina to the southern half of the United States through Central America, information on the use of animals in these environments is scarce. The excavation and using holes in the ground is an important ecological nature of the group, these structures may be considered conspicuous indicators of the presence of these animals. In the present study I have investigated the density, direction, morphometric and microhabitat of the burrows in different types of plant formation. The study was conducted during 13 months (Oct/06 to Nov/07) in Itapuã State Park, in Porto Alegre , RS , Brazil . The nine-banded armadillo (Dasypus novemcinctus) seems to be the most abundant species at this site, which is still at least one other species, the greater naked-tailed armadillo (Cabassous tatouay). The physical and environmental characteristics of 72 holes, fields (n = 31), forest (n = 22) and Restinga (n = 19), found were analyzed. The density of burrows did not vary significantly between these environments. Although the nine-banded is touted as a kind of wooded areas in the present study, the open areas were used with the same intensity that forest and dunes. Among the environmental variables the number of trees and percentage of ground cover shrubs influenced the number of burrows found in the woods. The direction of the burrows were predominantly southern areas of forest (forest and Restinga) and significantly different from field areas (fieldXforest p = 0.002; fieldXrestinga p = 0.001). Suggesting that this species can change behavior and increase the niche or relaxation in the absence of predators and competitors.

No description available.

Dur At Talah sedimentary sequence, located at the southern side of the Sirt Basin in central Libya, is composed of 150 m thick of mainly siliciclastic rocks. The importance of this sequence is linked to the importance of the Sirt Basin as one of large hydrocarbon reservoirs in Libya. The sequence is also an excellent site for vertebrate fossils of Late Eocene, the age of the sequence. Previous studies, though very limited compared to the importance of this area, are focused on its paleontological content. Sedimentology received only scant attention before this project. This thesis is an outcrop based study in which the focus is given to the sedimentary and biogenic (trace fossils) structures, aiming at defining and interpreting depositional facies which building up the sequence. The study is mainly based on field data which are analyzed on the light of related published literature and on the comparison with modern sedimentary environments. Results of facies analysis have led to splitting the entire sequence into three genetically related intervals. The oldest, we called the New Idam Unit (around 80m), is composed of very fine sandstones to mudstones. New Idam Unit is unconformably overlain by the Sarir Unit (around 50m), composed of medium grained cross bedded sandstones (the lower 25-30 m) changes up to very coarse and microconglomeratic sandstone (the upper 20-30 m). Thus, the Sarir Unit is split into the lower Sarir Subunit and upper Sarir subunit. The New Idam Unit presents both classical and unusual sedimentary and biogenic indicators that attribute this unit to estuarine depositional environment. It starts with outer estuarine (the lower 35 m) and ends up with inner estuarine (the upper 45 m). Maximum flooding surface is located in between. Above this surface the fluvial indicators increase and tidal indicators decrease, thus providing clue for basinward (North) migration of the shoreline. The lower Sarir subunit which was previously interpreted as fluvial deposits, preserves multi-scale sedimentary structures that undoubtedly belong to tidal processes. This is especially evidenced at the lower part of the lower Sarir Subunit (LLS). Fluvial indications over dominates the tidal ones in the upper part of the lower Sarir (ULS). Due to this configuration the whole lower Sarir subunit is interpreted as shallow marine, deltaic, depositional system, occurred during sea level ¨normal¨ regression. This time, maximum flooding surface is located between the LLS and ULS. The lower Sarir subunit is terminated by subaerial unconformity, with evidences of subaerial exposure preserved at the top of the ULS. These are intruded by the upper Sarir subunit which presents clear evidences of strictly fluvial environment of deposition. The deposits of the upper Sarir subunit record the low stand system tract part of the Dur At Talah sequence. In addition to the outlined results, the sequential pattern of the depositional events is suggested for the entire sequence of Dur At Talah. This study provides a valuable information regarding the depositional and sequential aspects of the Sirt Basin during the late Eocene, it also provide an unique case study for the better understanding of the shallow marine tidal deposits.

Research Doctorate - Doctor of Philosophy (PhD) / The aim of the thesis is to use computational stylistics, and in particular the methods pioneered by John Burrows, to explore aspects of the nineteenth-century periodical genre. Published for the most part anonymously, periodical articles were written by an extraordinary range of authors on an incredible variety of topics. The standard of writing in the thousands of articles appearing in the ‘higher’ or ‘literary’ journals has generally been agreed by scholars to be ‘remarkably good’. Beginning in 1802 and flourishing for most of the century, this outstanding genre of writing had all but disappeared by the beginning of the twentieth century. The text collection for the thesis consists of almost two million words by twenty-two authors. My study employs a variety of statistical tests on these texts to examine the effect of such factors as anonymity, commonality, authorial individuality, gender, house-style, text-type and chronology on the periodicals. I begin by taking a broad view of the field: first allowing the articles to ‘speak for themselves’ and to exhibit their commonalities and individual differences; then exploring the significance of both the intra-generic focus of the article – the stance taken in a particular article – and the author’s own idiosyncratic preferences in determining the incidence of function words in these articles. The interplay between these two factors provided an explanation as to why the articles of some authors invariably grouped together while those of other authors displayed marked variability. The use of lists of authorial ‘marker words’ – those words used relatively more or relatively less frequently by individual authors – showed that one can think of this large group of mostly anonymous periodical articles as a set of authorial oeuvres. I also look at the frequently made assertion that authors adapted their writing to the ‘house style’ of particular journals, and come to the conclusion that it does not significantly affect the deeper level of style revealed by function word usage. I then examine the question of whether or not there are differences between men’s and women’s usages of function words, coming to the conclusion that, although differences can be seen to exist, it is not at present possible to come up with sets of ‘marker words’ that reveal gender in the way that is possible with authorship. I use ‘marker words’ to identify the characteristics of one major author, George Eliot, and to show how she modified her stylistic practices when she moved from the periodical essay to fiction. I demonstrate how the techniques of computational stylistics can be used to check the legitimacy of some of the attributions made in the Wellesley Index, and I attribute one much-discussed anonymous group of articles on ‘the woman question’ to Robert Cecil 3rd Marquess of Salisbury and Prime Minister of England.

The European Bee-eater (Merops apiaster) is species of open landscapes with solitary trees with expressive and unmistakable colour. The origin is in North Africa and southern Europe, in the Czech republic is found in southern Moravia. The expansion of this kind is shifting to the north due to changes in landscape. For European bee-eater is typical of nesting burrows in the sand wall. The aim of this thesis was to describe the biology of African species of the genus Merops, to assess the situation of nature conditions for the kind of Merops apiaster, to describe the breeding of this species in captivity and to evaluate the success existing rearings in selected breeding institutions. In this thesis was described the breeding of European Bee-eater in Vienna Zoo, Dresden Zoo and Frankfurt Zoo, the breeding of Northern Carmine Bee-eater (Merops nubicus) in Zoo in Plzeň and the breeding of White-fronted Bee-eater (Merops bullocoides) in Vienna Zoo. Farther was described the breeding of all three species in private breeding of Mr. Drozdek in the Český Rudolec.

La compréhension des processus contrôlant le fonctionnement des mangroves est capitale au vu des services socio-économiques/écosystémiques rendus par ces écosystèmes et des menaces qu’ils subissent. En Guyane Française, les mangroves se développent rapidement en réponse aux contraintes sédimentaires récurrentes induites naturellement par les apports sédimentaires amazoniens. Cette thèse étudie la structure et la composition de trois classes de taille de communautés benthique (méso, macro, mégafaune), et les activités de bioturbation associées (remaniement sédimentaire biologique : RS, terriers) dans les jeunes stades de mangrove. 51 taxons de méso-macrofaune et 12 espèces de crabes (mégafaune) ont été identifiés. Bien que la biodiversité benthique soit spécifique à l'âge de la mangrove, des taxons tolèrent les modifications brusques du milieu, et cette persistance maintient des fonctions clés du remaniement sédimentaire tout au long du développement des mangroves. L’intensité du RS varie le long de ce gradient (21-146 g PS.m-2.cycle tidal-1). Si les crabes dominent le RS, cette thèse souligne la contribution effective de la méso-macrofaune aux transports particulaires. Les communautés benthiques montrent des capacités de bioturbation adaptées aux instabilités récurrentes du littoral. Les variations du RS au cours du temps pourraient indiquer l’état fonctionnel des mangroves. Cette étude conclut que l’hétérogénéité morpho-sédimentaire au sein des jeunes stades de mangroves influence la structuration spatiale des crabes, le remaniement sédimentaire qu’ils induisent, et la morphologie des terriers. Les microhabitats devraient être considérés lors de l'évaluation du rôle fonctionnel de la faune benthique des mangroves. / Understanding the processes that control mangroves functioning is essential regarding the socioeconomic/ecosystemic services these ecosystems provide and the increasing threats they suffer. In French Guiana, mangroves grow rapidly in response to natural sedimentary perturbations caused by sediment inputs from the Amazon River. This thesis characterizes the structure and the composition of benthic fauna communities (three size classes: meso-, macro- and megafauna) and the associated bioturbation activities (biological sediment reworking: SR, burrows) in mangrove early growth stages. 51 meso- macrofaunal taxa and 12 crab (megafauna) species were identified.Despite a mangrove age specific biodiversity, some taxa tolerate abrupt environmental changes, and such persistence maintains key sediment reworking functions along mangrove development.The SR intensity varies along this gradient from 21 to 146 g DW.m-2.tidal cycle-1. Burrower crabs dominate the SR but this thesis also outlines the non-negligible contribution of smaller-sized (meso- and macrofauna) organisms to particulate transport. Benthic communities’ bioturbation capacities are adapted to recurrent environmental instabilities. Changes of the biologicallyinduced SR may be used as a proxy of the functional status of mangrove ecosystems. This study concludes that morpho-sedimentary heterogeneity of early-growth mangrove stages influences crab spatial structuration, the crab-induced sediment reworking and burrow shapes. Thus, microhabitat specificities should be considered when evaluating the role of benthic fauna in mangroves ecosystem functioning.

La séquence sédimentaire du Dur At-Talah, située dans la partie sud du bassin de Syrte au centre de la Libye, est composée de 150 m d'épaisseur de roches principalement siliciclastiques (grès, siltites et argiles). L'importance de cette séquence est liée en partie à l'importance du bassin de Sirt qui est un des plus grands réservoirs d'hydrocarbures de Libye. La séquence est également un des plus important site de fossiles de vertébrés de l’Eocène supérieur, l'âge de la séquence. Les études antérieures, bien que très limitées par rapport à l'importance de cette zone, se sont concentrées principalement sur le contenu paléontologique de la séquence. L’étude sédimentologique n’avait été jusqu’à ce jour que très peu abordée. Cette thèse est un travail basé sur l’examen des affleurements et où l'accent est mis sur les structures sédimentaires et biogéniques (traces fossiles), visant à définir et à interpréter les faciès sédimentaires qui ont construit la séquence du Dur At Talah. L’ étude de la séquence a conduit à diviser la totalité de l’affleurement en trois intervalles génétiquement liés. Le plus ancien que nous avons appelé la « New Idam Unit » (environ 80 m d’épaisseur), est composé de grès très fins, de siltites et d’argiles. Cette unité (New Idam Unit) est recouverte en discordance par la « Sarir Unit » (environ 50 m d’épaisseur), composée de grès fins à moyens à faisceaux de litages entrecroisées dans sa partie inférieure (environ 25-30 m d’épaisseur) et de grès grossiers à microconglomératiques dans sa partie supérieure (environ 20-30 m d’épaisseur). La « Sarir Unit » est ainsi divisée en « Sarir inférieur » et « Sarir supérieur ». La « New Idam Unit » présente des dépôts qui sont attribués à un milieu main estuarien. La série débute par des dépôts d’environ 35 m d’épaisseur typiques d’un estuaire externe. Les 45 mètres qui lui font suite passent progressivement à des dépôts tidaux caractéristiques d’un estuaire interne. La Surface d'inondation maximale se situe entre les deux intervalles. Au-dessus de cette surface les indicateurs fluviaux augmentent et les indicateurs de marées diminuent progressivement, offrant ainsi un indice pour la migration de la rive de rivage vers le bassin (vers le Nord). La sous-unité du Sarir inférieur qui avait été interprétée avant ce travail comme dépôts fluviatiles, préserve pourtant des structures sédimentaires multi-échelles qui sont le résultat incontestable de processus de marée. Ceci est particulièrement évident dans la partie inférieure de l’unité « Sarir inférieur » (la Lower Lower Sarir Unit ; LLS). Dans la partie supérieure de l’unité Sarir inférieur (Upper Lower Sarir; ULS), les indicateurs de dynamique fluviale dominent largement sur ceux de la marée. Le Sarir inférieur est donc interprété comme un système deltaique mis en place lors d’une régression normale. Cette fois-ci, la surface maximale d'inondation se situe entre le LLS et ULS. Le « Upper Lower Sarir » (ULS) se terminée par une discordance subaérienne, avec de nombreuses traces d’émersion conservées au sommet de l'ULS. Celles-ci sont recoupées par le « Upper Sarir » qui montre des marqueurs fiables d'environnement de dépôt strictement fluvials. Les dépôts du « Upper Sarir » enregistre la séquence de bas niveau marin. Cette étude fournit des informations précieuses concernant le dépôt des séquences dans le bassin de Syrte au cours de la fin de l'Éocène. Elle fournit également une étude originale sur la dynamique tidale dans des milieux marins margino-littoraux. / Dur At Talah sedimentary sequence, located at the southern side of the Sirt Basin in central Libya, is composed of 150 m thick of mainly siliciclastic rocks. The importance of this sequence is linked to the importance of the Sirt Basin as one of large hydrocarbon reservoirs in Libya. The sequence is also an excellent site for vertebrate fossils of Late Eocene, the age of the sequence. Previous studies, though very limited compared to the importance of this area, are focused on its paleontological content. Sedimentology received only scant attention before this project. This thesis is an outcrop based study in which the focus is given to the sedimentary and biogenic (trace fossils) structures, aiming at defining and interpreting depositional facies which building up the sequence. The study is mainly based on field data which are analyzed on the light of related published literature and on the comparison with modern sedimentary environments. Results of facies analysis have led to splitting the entire sequence into three genetically related intervals. The oldest, we called the New Idam Unit (around 80m), is composed of very fine sandstones to mudstones. New Idam Unit is unconformably overlain by the Sarir Unit (around 50m), composed of medium grained cross bedded sandstones (the lower 25-30 m) changes up to very coarse and microconglomeratic sandstone (the upper 20-30 m). Thus, the Sarir Unit is split into the lower Sarir Subunit and upper Sarir subunit. The New Idam Unit presents both classical and unusual sedimentary and biogenic indicators that attribute this unit to estuarine depositional environment. It starts with outer estuarine (the lower 35 m) and ends up with inner estuarine (the upper 45 m). Maximum flooding surface is located in between. Above this surface the fluvial indicators increase and tidal indicators decrease, thus providing clue for basinward (North) migration of the shoreline. The lower Sarir subunit which was previously interpreted as fluvial deposits, preserves multi-scale sedimentary structures that undoubtedly belong to tidal processes. This is especially evidenced at the lower part of the lower Sarir Subunit (LLS). Fluvial indications over dominates the tidal ones in the upper part of the lower Sarir (ULS). Due to this configuration the whole lower Sarir subunit is interpreted as shallow marine, deltaic, depositional system, occurred during sea level ¨normal¨ regression. This time, maximum flooding surface is located between the LLS and ULS. The lower Sarir subunit is terminated by subaerial unconformity, with evidences of subaerial exposure preserved at the top of the ULS. These are intruded by the upper Sarir subunit which presents clear evidences of strictly fluvial environment of deposition. The deposits of the upper Sarir subunit record the low stand system tract part of the Dur At Talah sequence. In addition to the outlined results, the sequential pattern of the depositional events is suggested for the entire sequence of Dur At Talah. This study provides a valuable information regarding the depositional and sequential aspects of the Sirt Basin during the late Eocene, it also provide an unique case study for the better understanding of the shallow marine tidal deposits.

This thesis describes Burrow-Wheeler compression algorithm. It focuses on each part of Burrow-Wheeler algorithm, most of all on and entropic coders. In section are described methods like move to front, inverse frequences, interval coding, etc. Among the described entropy coders are Huffman, arithmetic and Rice-Golomg coders. In conclusion there is testing of described methods of global structure transformation and entropic coders. Best combinations are compared with the most common compress algorithm.