Dissertations / Theses on the topic 'Atlantic Passage'

Windward Passage, which separates the islands of Cuba and Hispaniola, has been recognized as an important inflow channel to the Caribbean Sea for nearly a century. Despite this fact, few direct measurements of the volume transport through the passage exist. In an effort to gain a more comprehensive understanding of the variability, structure, and mean transport associated with flow through Windward Passage, the University of Miami?s Rosenstiel School of Marine and Atmospheric Science (RSMAS) and the National Oceanic and Atmospheric Administration (NOAA)?s Atlantic Oceanographic and Meteorological Laboratory (AOML) conducted a targeted research study of the passage and surrounding region from October 2003 through February 2005. The project deployed a moored current meter array across the passage and conducted four regional hydrographic surveys. Velocity sections collected across Windward Passage during the four cruises from lowered and hull-mounted acoustic Doppler current profilers show a highly variable field dominated by small-scale eddy features and other areas of locally-intensified flow. However, when integrated horizontally across the passage, the resulting transport-per-unit-depth profiles reveal a remarkably robust vertical shear structure. A net inflow of surface and thermocline waters was observed over the four cruises. Beneath these layers, a persistent outflow of intermediate water was found, intensified along the east side of the passage. Deep inflow, just above the sill depth maximum (1680 m), was observed on cruise #1 and, based on data from the moored current meter record, was determined to be a regular flow feature. Together, project velocity sections and water mass analyses of Windward and surrounding passages suggest that Surface Water (SFC), Subtropical Underwater (SUW), and Central Water (CW) primarily arrive at Windward Passage from the east via the Hispaniola Basin. A majority of SFC and SUW enters the Cayman Basin through Windward Passage, while the arriving CW bifurcates, with slightly more than half bypassing the passage and continuing westward north of Cuba. An intermediate water outflow pathway from the Cayman to the Hispaniola Basin via Windward Passage was also observed. Much of this outflow possessed a salinity signature characteristic of upstream inflow regions immediately to the east and south of the Lesser Antilles. Total Windward Passage transport, calculated from the four ship surveys, was found to be an inflow of 3.0 ±2.8 Sverdrups (1 Sv ≡ 10^6 m^3 s^-1). Data from the 16-month moored current meter array yielded a larger mean inflow of 5.0 ±1.6 Sv. These numbers are lower than previous estimates based on regional passage transport differences, and suggest that more transport may be entering the Florida Current system through passages in the Bahamas (the Northwest Providence and Old Bahama Channels) than previously thought, with proportionately less flow entering the system through the Caribbean Sea.

Hydropower dams block migration routes and disrupt longitudinal connectivity in rivers, thereby posing a threat to migratory fish species. Various fish passage solutions have been implemented to improve connectivity with varying success. A well-functioning passage solution must ensure safe and timely passage routes that are used by a substantial portion of the migrating fish. In this thesis, I report the results from telemetry studies where the behavior and survival of migrating Atlantic salmon spawners, post-spawners and smolts have been evaluated in relation to hydropower dam passage. I evaluate downstream passage performance at dams with no passage solutions in the River Klarälven, and with simple passage solutions in in the Winooski River. In the River Ätran, I study both upstream- and downstream passage performance at a dam with sophisticated passage solutions based on the best available technology. In addition, I have studied the survival and behavior of post-spawners and hatchery-released smolts. A substantial portion of the spawners survived spawning and initiated downstream migration. Most males migrated downstream in autumn following spawning, whereas females tended to stay in the river until spring. For hatchery-reared smolts, early release was associated with faster initiation of migration and higher survival compared to late release. Multiple dam passage resulted in high mortality for both smolts and kelts. For smolts, dam passage, even with simple passage solutions, was associated with substantial delay and mortality. High spill levels were linked to high survival and short delay for downstream migrating salmon. The best available passage solution, which consisted of a nature-like fishway and a low sloping intake rack to guide fish to a bypass, resulted in rapid passage of a large portion of the adult migrants.

This paper explores the history of a group of immigrants that came to the United States from the small rural Austrian region of the Burgenland between World War One and World War Two. By examining several biographical life stories of contemporaries it wants explain why the emigrants decided to leave their country, how they managed their passage, how they assimilated to their adopted‐home, and how they integrated themselves into the new society.

Current conventional weather forecasts are based on high-dimensional numerical models. They are usually only skillful up to a maximum lead time of around 7 days due to the chaotic nature of the climate dynamics and the related exponential growth of model and data initialisation errors. Even the fully detailed medium-range predictions made for instance at the European Centre for Medium-Range Weather Forecasts do not exceed lead times of 14 days, while even longer-range predictions are limited to time-averaged forecast outputs only. Many sectors would profit significantly from accurate forecasts on seasonal time scales without needing the wealth of details a full dynamical model can deliver. In this thesis, we aim to study the potential of a much cheaper data-based statistical approach to provide predictions of comparable or even better skill up to seasonal lead times, using as an examplary forecast target the time until the next occurrence of frost. To this end, we first analyse the properties of the temperature anomaly time series obtained from measured data by subtracting a sinusoidal seasonal cycle, as well as the distribution properties of the first passage times to frost. The possibility of generating additional temperature anomaly data with the same properties by using very simple autoregressive model processes to potentially reduce the statistical fluctuations in our analysis is investigated and ultimately rejected. In a next step, we study the potential for predictability using only conditional first passage time distributions derived from the temperature anomaly time series and confirm a significant dependence of the distributions on the initial conditions. After this preliminary analysis, we issue data-based out-of-sample forecasts for three different prediction targets: The specific date of first frost, the probability of observing frost before summer for forecasts issued in spring, and the full probability distribution of the first passage times to frost. We then study the possibility of improving the forecast quality first by enhancing the stationarity of the temperature anomaly time series and then by adding as an additional input variable the state of the North Atlantic Oscillation on the date the predictions are issued. We are able to obtain significant forecast skill up to seasonal lead times when comparing our results to an unskilled reference forecast. A first comparison between the data-based forecasts and corresponding predictions gathered from a dynamical weather model, necessarily using a lead time of only up to 15 days, shows that our simple statistical schemes are only outperformed (and then only slightly) if further statistical post-processing is applied to the model output<br>Aktuelle Wetterprognosen werden mit Hilfe von hochdimensionalen, numerischen Modellen generiert. Durch die dem Klima zugrunde liegende chaotische Dynamik wachsen Modellfehler und Ungenauigkeiten in der Modellinitialisierung exponentiell an, sodass Vorhersagen mit signifikanter Güte üblicherweise nur für eine Vorlaufzeit von maximal sieben Tagen möglich sind. Selbst die detaillierten Prognosen des Europäischen Zentrums für mittelfristige Wettervorhersagen gehen nicht über eine Vorlaufzeit von 14 Tagen hinaus, während noch längerfristigere Vorhersagen auf zeitgemittelte Größen beschränkt sind. Viele Branchen würden signifikant von akkuraten Vorhersagen auf saisonalen Zeitskalen pro-fitieren, ohne das ganze Ausmaß an Details zu benötigen, das von einem vollständigen dynamischen Modell geliefert werden kann. In dieser Dissertation beabsichtigen wir, am Beispiel einer Vorhersage der Zeitdauer bis zum nächsten Eintreten von Frost zu untersuchen, inwieweit deutlich kostengünstigere, datenbasierte statistische Verfahren Prognosen von gleicher oder sogar besserer Güte auf bis zu saisonalen Zeitskalen liefern können. Dazu analysieren wir zunächst die Eigenschaften der Zeitreihe der Temperaturanomalien, die aus den Messdaten durch das Subtrahieren eines sinusförmigen Jahresganges erhalten werden, sowie die Charakteristiken der Wahrscheinlichkeitsverteilungen der Zeitdauer bis zum nächsten Eintreten von Frost. Die Möglichkeit, durch einen einfachen autoregressiven Modellprozess zusätzliche Datenpunkte gleicher statistischer Eigenschaften wie der Temperaturanomalien zu generieren, um die statistischen Fluktuationen in der Analyse zu reduzieren, wird untersucht und letztendlich verworfen. Im nächsten Schritt analysieren wir das Vorhersagepotential, wenn ausschließlich aus den Temperaturanomalien gewonnene bedingte Wahrscheinlichkeitsverteilungen der Wartezeit bis zum nächsten Frost verwendet werden, und können eine signifikante Abhängigkeit der Verteilungen von den Anfangsbedingungen nachweisen. Nach dieser einleitenden Untersuchung erstellen wir datenbasierte Prognosen für drei verschiedene Vorhersagegrößen: Das konkrete Datum, an dem es das nächste Mal Frost geben wird; die Wahrscheinlichkeit, noch vor dem Sommer Frost zu beobachten, wenn die Vorhersagen im Frühjahr ausgegeben werden; und die volle Wahrscheinlichkeitsverteilung der Zeitdauer bis zum nächsten Eintreten von Frost. Anschließend untersuchen wir die Möglichkeit, die Vorhersagegüte weiter zu erhöhen - zunächst durch eine Verbesserung der Stationarität der Temperaturanomalien und dann durch die zusätzliche Berücksichtigung der Nordatlantischen Oszillation als einer zweiten, den Anfangszustand charakterisierenden Variablen im Vorhersageschema. Wir sind in der Lage, im Vergleich mit einem naiven Referenzvorhersageschema eine signifikante Verbesserung der Vorhersagegüte auch auf saisonalen Zeitskalen zu erreichen. Ein erster Vergleich zwischen den datenbasierten Vorhersagen und entsprechenden, aus den dynamischen Wettermodellen gewonnenen Prognosen, der sich notwendigerweise auf eine Vorlaufzeit der Vorhersagen von lediglich 15 Tagen beschränkt, zeigt, dass letztere unsere simplen statistischen Vorhersageschemata nur schlagen (und zwar knapp), wenn der Modelloutput noch einer statistischen Nachbearbeitung unterzogen wird

Fiskars passager genom vattenkraftverk är förenat med hög dödlighet. För att minska vattenkraftens påverkan på fiskbestånd har olika fiskledare utvecklats. I denna laboratoriestudie utvärderades tre typer av icke-fysiska fiskledare och deras effektivitet i att leda odlade smolt av Atlantlax (Salmo salar L.) till en önskad passage. Målet med denna studie var att undersöka om det var möjligt att leda odlade laxsmolt till en önskad passage med hjälp av bubblor, strobeljus eller en kombination av bubblor och strobeljus. Med relativt enkla medel och låg kostnad konstruerades fiskledare som bestod av en perforerad slang driven av en luftkompressor samt en ljusramp med fyra LED-lampor vilka blinkade simultant med 480 bpm. Fem replikat genomfördes för vardera behandling, bubblor, strobeljus och bubblor/strobeljus, samt sex replikat i kontrollen. Under en timmes behandling fick tio laxsmolt, märkta med PIT-tag, passera en av två antenner, varav den ena var utrustad med en fiskledare, under vandring i nedströms riktning i ett strömakvarium. Denna studie visade att fiskledare av samtliga tre metoder ledde smolt till en önskad passage under behandlingens första femton minuter. Vidare visade fiskledaren bestående av bubblor en fortsatt ledande förmåga över hela behandlingsperioden (60 minuter), medan fiskledarna av strobeljus- och bubbel/strobeljus inte visade en sådan effekt.<br>Passages by fish through hydropower plants are associated with high mortality. In order to reduce the impact of hydropower plants on fish stocks, a variety of fish guiding systems have evolved. In this laboratory study, three types of non-physical fish guiding systems were evaluated by their efficiency in leading cultivated smolt of Atlantic salmon (Salmo salar L.) to a desired passage. This study aimed to answer if it is possible to guide salmon smolt to a desired safe passage by using bubbles, strobe light or a combination of bubbles and strobe light. With relatively simple means and low cost, fish-guides were constructed consisting of a perforated tube driven by an air compressor and a light ramp with four LED lights, which simultaneously flashed at 480 bpm. Five replicates were performed for each treatment; bubbles, strobe light and bubbles / strobe light, as well as six replicates for the controls. During one hour of treatment, ten salmon smolt, marked with PIT tag, could pass one of two antennas, where one had a fish-guide in front of the antenna, while migrating downstream in a stream aquarium. This study showed that fish-guides of all three methods led smolt to a desired passage during the first fifteen minutes of treatment. Furthermore, the bubble method showed a continuous guiding capacity throughout the treatment period (60 minutes), while the strobe light and bubble/strobe light did not show such an effect.

Many passive margins experience pulsed exhumation events late in their history as a result of plate boundary distal geodynamic mechanisms or climatic events. The onset of late Cenozoic glaciation, often associated with enhanced rates of erosion, is one such possible cause of passive margin rejuvenation. However, along passive margins the effectiveness of Plio-Pleistocene glaciers at eroding the landscape may be limited by low tectonic rock uplift rates or as a result of erosionally inefficient cold based continental ice-sheets. In this dissertation the evolution of post-orogenic topography and the effect of glaciations on denuding landscapes along the North Atlantic Passive Margin, in the White Mountains of New Hampshire and the western Scottish Highlands, was investigated. Background exhumation rates averaged over 106-7 yr timescale were determined using apatite (U-Th)/He thermochronology. To resolve whether or not a change in exhumation rate occurred coincident with glaciation these background exhumation rates were compared to magnitudes of erosion averaged over the glacially relevant 103-4 yr timescale using the in situ terrestrial cosmogenic nuclide 10Be. In chapter two, 106-7 yr timescale exhumation and burial histories across the western Scottish Highlands were determined. The results show that post-orogenic burial and exhumation is mostly a result of plate margin distal tectonic and magmatic factors that are variable across short distances (i.e., <100 km). In chapter three, patterns and magnitudes of erosion during glaciation and following deglaciation in the Scottish Highlands were investigated. The results indicate that polythermal glacial erosion denuded low elevation portions of the Scottish Highlands and preserved summits. This produced relief but did not significantly lower the maximum elevation of the landscape. Following deglaciation Scotland's sediment budget remains dominated by glaciogenic sediment. In the fourth chapter, magnitudes of background exhumation in the Presidential and Carter Ranges of the White Mountains, New Hampshire were compared to magnitudes of glacial erosion. The results indicate that most relief was produced prior to glaciation and that background exhumation rates in the Cenozoic are low (<0.01 mm yr-1). In the late-Cenozoic, cold- based glaciation prevented an acceleration of erosion in the White Mountains. The post- glacial sediment budget is made up of dominantly glaciogenic sediment. Overall, the main findings of this dissertation are; (1) post-orogenic burial, exhumation, and relief production are mainly the result of spatially heterogeneous plate margin distal vertical crustal motions; across passive margins covered by large continental ice sheets; (2) cold-based ice limits the magnitudes of late Cenozoic glacial erosion sediment budgets continue to be dominated by glaciogenic sediment, >10 ka after and (3) post-glacial deglaciation.<br>Ph. D.

Thesis (M.S.)--Massachusetts Institute of Technology, Dept. of Earth, Atmospheric, and Planetary Sciences, 1995.<br>Includes bibliographical references (leaves 89-90).<br>by Miles Aaron Sundermeyer.<br>M.S.

Ce mémoire traite de la formation et de l'évolution des bassins de la marge Atlantique argentine. Trois stades de rifting superposés ont été identifiés dans les bassins des Malvinas et de Colorado/Salado. Le premier événement de rifting est associé à la réactivation extensive, durant le Trias tardif, des chevauchements paléozoïques de la phase de Ventania-Cape. Un deuxième stade de rifting (Jurassique inférieur / moyen) a induit les failles contrôlant les principaux dépocentres et intersectant les structures plus anciennes. Finalement, l’extension du Crétacé inférieur liée à l’ouverture de l’Atlantique Sud s’est concentrée en périphérie de la marge continentale actuelle et a abouti à la mise en place de SDRs. L’évolution du bassin Malvinas a été caractérisée d’un point de vue sismique. Des nouveaux âges zircon U-Pb contraignent le rifting au Jurassique. Le nouveau modèle de rupture du Gondwana présenté ici met l'accent sur l'évolution des bassins mésozoïques péri-atlantiques. L’évolution post-rupture de la marge Atlantique argentine a également été étudiée via l’interprétation sismique et la caractérisation stratigraphique. Après la rupture Hauterivien / Barrémien, trois étapes d'évolution de la marge ont été identifiées. Le Crétacé est marqué par la subsidence thermique des principaux dépocentres. La marge devient une plate-forme continentale unique après la transgression régionale Maastrichtienne-Danienne. Le stade d’expansion du Paléogène est caractérisé par un affaissement et un apport sédimentaire centré au nord dans la région de Salado, tandis que le stade d’expansion du Néogène se caractérise par un comportement cylindrique de l’ensemble de la marge et par l’influence notable des courants de contour<br>This work is focused on basin formation and evolution in the Argentinean South Atlantic Margin and the Mesozoic breakup of SW Gondwana. Rifting evolution was studied in the Malvinas and Colorado/Salado basins. Three superimposed rifting events were identified in the latter. The first rifting event is associated with the Late Triassic extensional reactivation of Late Paleozoic thrusts of the Ventania-Cape fold belt. A second and main rifting stage (Early-Middle Jurassic) is related to faults forming the main depocenters and intersecting the older structures. Finally, Early Cretaceous extension linked to the opening of the South Atlantic Ocean focused on the outer continental fringe and produced emplacement of SDRs. The rifting evolution of the Malvinas basin was seismically characterized. New zircon U-Pb ages constrain rifting in the Jurassic. A new model for Gondwana breakup is presented with focus on the evolution of the Mesozoic peri-Atlantic basins. The post-breakup evolution of the Argentinean South Atlantic margin was also studied via seismic interpretation and stratigraphic characterization. Three stages of drift evolution were identified. After the Hauterivian/Barremian breakup, the Cretaceous drift unit is conditioned by the thermal subsidence over the main depocenters. Only after the Maastrichtian-Danian regional transgression, the margin becomes a single continental platform. The Paleogene drift stage is characterized by subsidence and sedimentary input centered in the Salado area, while the Neogene drift stage is characterized by a cylindrical behavior and the remarkable influence of contour currents

A quantitative forward model has been developed to investigate the controls on the deposition, erosion, and preservation of passive rift margin stratigraphy. The model includes thermal subsidence, variable absolute sealevel, flexural isostasy, subaerial and submarine deposition on fluvial and marine equilibrium profiles, and the facility to vary sediment supply through time. Results from the quantitative model can be used to reproduce elements of the sequence stratigraphic depositional model. Conducting sensitivity tests demonstrates that variables such as sediment supply and fluvial profile behaviour are likely to be of equal importance to thermal subsidence and eustasy in passive margin stratigraphy. Sensitivity tests with the quantitative model also demonstrate the problems associated with attempting to use a discretised stratigraphic model to investigate unforced cyclicty resulting from complex interactions in stratigraphic systems. Although the model appears capable of producing such unforced cyclical behaviour, this cyclicity is shown to be due to a numerical instability within the model which occurs with certain initial conditions and assumptions. The applicability of the model to observed stratigraphy is tested by comparing specific model output to patterns of stratigraphy from the North American Atlantic margin. The results from this test demonstrate that although the model is in many respects simplistic when compared to the complexities of natural systems, it is nevertheless capable of reproducing some of the basic elements of the observed stratigraphic patterns.

Young women in Mexico and parts of Central America celebrate their fifteenth birthdays by following a complex rite of initiation, called Quinceañeras, a special ritual developed as a mixed heritage of the native people and their contact with European conquerors. The emerging Latino population in Atlanta celebrates this rite, facing the reality of being a minority racial group, although they maintain the same essence and goal than the celebration than in their country. This research explores this growing population group in Atlanta, in a special and significant cultural occasion, using an ethnographic approach methodology through participant observation and personal journals of the Quinceañeras as way to describe the meaning, implications and issues of this celebration for these girls and their families under a Social Constructionist Model of Ethnicity and Life Course Sociology theoretical framework.

Orientador: Marlies Sazima<br>Tese (doutorado) - Universidade Estadual de Campinas, Instituto de Biologia<br>Made available in DSpace on 2018-08-07T09:26:05Z (GMT). No. of bitstreams: 1 Rocca-de-Andrade_MarciaAlexandra_D.pdf: 8074594 bytes, checksum: 9b23bf58883dbdee47e992b14876d450 (MD5) Previous issue date: 2006<br>Resumo: Beija-flores são considerados os polinizadores vertebrados mais importantes na região Neotropical. Outras aves que visitam flores são geralmente consideradas como parasitas da relação flor-beija-flor, não apresentando o elevado grau de especialização para a nectarivoria como os beija-flores. Apesar de flores ornitófilas serem muito vistosas, apresentando partes florais ou estruturas associadas às flores ou inflorescências muito coloridas, beija-flores também visitam flores não-ornitófilas, as quais na maioria dos casos não são polinizadas durante a tomada de néctar. Durante um estudo de dois anos e três meses sobre a disponibilidade de recurso floral para aves em uma área de Mata Atlântica no sudeste do Brasil, a atividade das aves e a abundância de flores foram estimadas através de transecções lineares e escalando árvores com equipamento de escalada esportiva. O volume de néctar acumulado e a concentração de açúcares foram medidos com o auxílio de micro-seringa e refratômetro manual, respectivamente, a partir de flores ou botões ensacados no dia anterior até o final da manhã seguinte. Espécies de aves foram registradas durante registros visuais e observações focais quando em visita às flores. Sessenta e duas espécies de plantas foram estudadas e beija-flores foram registrados em 95% delas; um número muito pequeno de espécies foi visitado também por outras aves. A maioria das espécies foi de epífitas e as demais foram ervas, lianas ou árvores. Cerca de 68% das espécies foram polinizadas por aves, sendo o restante pilhado. Flores visitadas por beija-flores se distribuíram ao longo do ano, o que deve ser importante para a manutenção de espécies de beija-flores residentes na área, e a maioria deste recurso ocorreu no sub-bosque, apesar de também existir recurso no dossel. Características de néctar foram muito variáveis entre as espécies: as médias de volume acumulado variaram de 1,5 a 220,6 µl e as médias da concentração variaram de 3,1 a 40,9% (Capítulo 1). Dentre as espécies de beija-flores, três pertencem à subfamília Phaethornithinae e dez à Trochilinae. Duas espécies residentes foram observadas ao longo de toda a estratificação vertical da floresta, visitando flores e carregando pólen entre estratos diferentes, enquanto outras espécies ocorreram em apenas um estrato: sub-bosque ou dossel (Capítulo 2). No dossel, duas espécies foram visitadas e polinizadas por outras aves além dos beija-flores, até mesmo por pica-paus (Capítulo 3.1), sendo mais adaptadas à síndrome de ornitofilia por aves que pousam (Capítulo 3.2). Uma das espécies de bromélias (Vriesea rodigasiana) foi estudada acerca de seu principal polinizador com base em freqüência de visitas e carga de pólen germinado por visita (Capítulo 3.3)<br>Abstract: Hummingbirds are considered the most important vertebrate pollinators in the Neotropics. Other flowervisiting birds are often considered as parasites of the flower-hummingbird relationship, not presenting the high degree of specialization for nectarivory as hummingbirds. Although ornithophilous flowers are very showy, displaying colorful floral parts or structures associated with the flowers or inflorescences, hummingbirds also visit non-ornithophilous flowers, which most of the time are not pollinated during nectar probing. In a two years and three months study about floral resource availability for birds in the Atlantic rainforest in South-eastern Brazil, their activities and flower abundance were estimated throughout the studied months and in vertical stratification. Records were made every month, during line transects samplings and accessing canopy with climbing equipment. Accumulated nectar volume and concentration were measured with microliter syringes and a hand-refractometer, respectively, from bagged flowers at the end of the morning. Bird species were registered during sightings and focal observations while visits to flowers. Sixtytwo species of plants were studied and hummingbirds were recorded on 95% of them; a few were also visited by other birds. Most species are epiphytes, and some are shrubs, lianas or trees. About 68% of these species are pollinated by hummingbirds, from the others they steal or rob nectar. Flowers visited by hummingbirds are distributed throughout the year, which is important to support resident species, and most of this resource occurs in the understorey, although there is also resource in the canopy. Nectar features are very variable among species: mean accumulated nectar volume ranging from 1.5 to 220.6 µl, and mean sugar concentration from 3.1 to 40.9% (Chapter 1). Among the hummingbirds, three species belong to the subfamily Phaethornithinae and ten to Trochilinae. Two resident species are recorded all over the vertical stratification, visiting flower species along their vertical distribution, carrying pollen between different strata, while other species only occur in one stratum: understorey or canopy (Chapter 2). In the canopy two species are visited and pollinated by other birds besides hummingbirds, even by woodpeckers (Chapter 3.1), and are more adapted to pollination by perching-birds (Chapter 3.2). One of the bromeliads (Vriesea rodigasiana) was chosen for a study about relative pollinator efficiency, measured by visitation frequency and germinated pollen load per visit (Chapter 3.3)<br>Doutorado<br>Doutor em Biologia Vegetal

White-nose syndrome (WNS) has reduced the abundance of many bat species within the United States' mid-Atlantic region, including the endangered Indiana (Myotis sodalis), threatened Myotis septentrionalis (northern long-eared bat) and other bats of conservation concern, such as Perimyotis subflavus (tri-colored bat), Myotis leibii (eastern small-footed bat) and Myotis lucifugus (little brown bat). Impacts to Eptesicus fuscus (big brown bat) populations have been negative, positive or neutral. Migratory bat species such as Lasiurus borealis (eastern red bat) are not impacted by WNS. To determine changes within the National Park Service National Capital Region bat communities, I surveyed the area with mist netting and active acoustic sampling (2016–2018) and compared findings to pre-WNS (2003–2004) data. I documented a significant reduction in the numbers and distributions of M. lucifugus and P. subflavus, a decrease in the distribution of M. septentrionalis, and an increase in Eptesicus fuscus. Documented M. septentrionalis reproduction suggests that portions of the National Capital Region may be important bat conservation areas. To explore the relationship between bat life history and passive acoustic sampling echolocation call data, as well as to review the sampling effort required to detect the presence of extant species, I used mist-netting captures and acoustic call data collected 2015 – 2018 within the District of Columbia, Maryland, Pennsylvania, Virginia, and West Virginia. Based on locally estimated scatterplot smoothing line calculations, I determined that the highest levels of maternity season acoustic activity for Eptesicus fuscus and Lasiurus borealis corresponded primarily to lactation periods. To determine sampling effort, I developed simulations based on species accumulation curves for individual species within different physiographic regions and land-cover types. I determined that the smallest sampling efforts typically corresponded to sampling additional sites versus sampling the same sites with more nights. Detection effort varied greatly by species, physiographic region and land-cover type. Eptesicus fuscus diet has been well-studied throughout North America with visual identification methods from fecal and stomach content samples. Next-generation sequencing provides large genetic data sets analyses in a cost-effective manner and has been used to identify bat prey items. I collected Eptesicus fuscus fecal samples from mid-Atlantic regions and used next-generation sequencing to identify their prey. I documented high variation between survey areas, but did not note a clear pattern of urbanization or fragmentation impacts upon Insecta diversity. All order-level taxa that I documented had been previously documented in morphological studies; however, I did document new families, genera and species. However, I would suggest caution in using next-generation sequencing technologies as authoritative sources for documenting new diet taxa, as I noted frequent occurrences of confounding environmental DNA within the samples.<br>Doctor of Philosophy<br>White-nose syndrome (WNS) has reduced the abundance of many bat species within the United States' mid-Atlantic region, including the endangered Indiana (Myotis sodalis), threatened Myotis septentrionalis (northern long-eared bat) and other bats of conservation concern, such as the Perimyotis subflavus (tri-colored bat), Myotis leibii (eastern small-footed bat) and Myotis lucifugus (little brown bat). WNS-impacts to Eptesicus fuscus (big brown bat) populations have been negative, positive or neutral. Migratory bat species such as Lasiurus borealis (eastern red bat) are not impacted by WNS. To determine changes within the National Park Service National Capital Region bat communities, I captured bats with mist-netting techniques and recorded bat echolocation calls with active acoustics (20-minute periods; 2016–2018) and compared findings to pre-WNS (2003–2004) data. I documented a significant reduction in the numbers and distributions of M. lucifugus and P. subflavus, a decrease in the distribution of M. septentrionalis, and an increase in Eptesicus fuscus. Documented M. septentrionalis reproduction suggests that portions of the National Capital Region may be important bat conservation areas. To explore the relationship between bat echolocation calls recorded with passive (over-night) acoustic data and bat reproduction trends, as well as the amount of effort required to document bat species, I sampled 849 sites with passive acoustics and 482 sites with mist-netting during 2016 – 2018 within the District of Columbia, Maryland, Pennsylvania, Virginia, and West Virginia. I determined that the highest levels of acoustic activity for Eptesicus fuscus and Lasiurus borealis (eastern red bat) within the maternity season are associated with the period of highest levels of lactation. To determine sampling effort, I used simulations to detect species in different landscape conditions. I determined that sampling additional sites requires less sampling effort than sampling more nights. The amount of effort required to detect each bat species varied, as did the impact of different landscape conditions. Eptesicus fuscus diet has been well-studied throughout North America by identifying insect parts in feces and stomach contents. Next-generation sequencing is a process which produced large amounts of genetic data sets in a cost-effective manner, and it can be used to identify prey within bat feces. I collected Eptesicus fuscus fecal samples from mid-Atlantic regions and used next-generation sequencing to identify potential prey. I determined that bat diet varied greatly based on survey area and number of feces analyzed. At the order-level, I did not document new taxa: however, I did document new families, genera and species. However, I would suggest caution in using next-generation sequencing technologies as authoritative sources for documenting new diet taxa, as many taxa apparent within my samples were subsequently excluded, as the bats may have been incidentally ingested them.

This thesis grapples with questions surrounding representation, mourning, and responsibility in relation to two literary representations of the ZONG massacre of 1781. These texts are M. NourbeSe Philip’s ZONG! and Fred D’Aguiar’s FEEDING THE GHOSTS. The only extant archival document—a record of the insurance dispute which ensued as a consequence of the massacre—does not represent the drowned as victims, nor can it represent the magnitude of the atrocity. As such, this thesis posits that the archival gaps or silences from which the captives’ voices are missing become spaces of possibility for additive representation. This thesis also examines the role voice and sound play in these literary texts and the deconstructive-ethical philosophies of Jean-Luc Nancy and Jacques Derrida. This thesis argues that these texts invoke the sonic materiality of voice in the service of responding to the disremembered dead through mourning and acknowledgment.

The origin of high elevation topography at so-called “passive” continental margins and their interior hinterlands has been an outstanding question in geoscience for decades. An important step towards answering this question is to improve our understanding of the response of the landscape to deformation of the lithosphere over different length scales. During continental rifting, elevated rift flanks may develop as a result of lateral extension of the lithosphere combined with vertical movements of the lithosphere driven by isostasy or convection of buoyant mantle flow. However, mechanisms capable of maintaining rift-related topography over geological timescales or driving post-rift rejuvenation of margin topography remain largely speculative and are strongly dependent on theoretical models. By constraining the timing and magnitude of major erosional events that have occurred across a particular margin using suitable empirical data we can begin to unravel the geomorphic development of the margin and identify the forces driving surface uplift. Apatite fission track (AFT) and apatite (U-Th-Sm)/He (AHe) thermochronometry has the unique ability to deliver these constraints by providing information on the cooling of rocks through temperatures of c. 120 – 40°C as they are exhumed from depth (c. 4 – 6 km) by erosion of overlying rock. Along the western continental margin of South Africa recent insights from thermochronology, structural geology and geomorphology has revealed that the margin may have experienced a more complex post-rift tectonic history than is to be expected for a “passive” margin. In this study, AFT and AHe analysis was performed on samples collected across the high relief escarpment zone along the continental margin (Namaqualand Highlands) and across the continental interior plateau (Bushmanland Plateau) to determine the post-break up cooling history of the continental margin. Sampling was undertaken from a structural perspective by sampling individual fault blocks within the heavily faulted Namaqualand Highlands and by collecting a profile of samples, from the interior plateau, that crosses major structural features at the boundary of the Kaapvaal craton. The approach for AHe analysis was to obtain multiple single grain age measurements (up to 20 grains per sample) for selected samples in order to investigate and exploit the primary causes of natural dispersion of AHe single grain ages and the influence of this dispersion on thermal history modelling. AFT and AHe data from 56 outcrop samples are jointly inverted using a Bayesian transdimensional approach incorporating the compositional influence on fission track annealing and radiation damage enhanced He retention. Two major discrete cooling episodes are recorded in thermal history models at c. 150 – 130 Ma and 110 – 90 Ma, respectively. These cooling episodes are broadly coeval with periods of enhanced deposition in the offshore Orange Basin and are therefore linked to discrete periods of enhanced continental erosion. The first phase of erosion is believed to involve the progressive destruction of syn-rift topography which prevailed across the developing continental margin and inland to the SW boundary of the Kaapvaal craton. The second phase of erosion is proposed to have been induced by regional uplift of southern Africa coupled with localised reactivation of basement structures at the continental margin and craton boundary. A vertical thickness of at least c. 3 – 5 km of material was eroded across the continental margin during the Cretaceous with only minor erosion (typically < 0.5km) occurring during the Cenozoic. There is now considerable support from the low temperature thermochronology record that km-scale denudation has occurred regionally across South Africa during the Mid-Late Cretaceous, long after the end of continental rifting in the South Atlantic. Data from this study reveals a more localised structural component to this regional event and more complexity in the spatial and temporal distribution of denudation during this period. The mechanisms driving this denudation are still uncertain but it is proposed here that regional dynamic uplift of South Africa has occurred due to the presence of an underlying upwelling of buoyant mantle, while in-plane horizontal stresses have triggered reactivation of basement structures. It now seems appropriate to revise the classification of the southwest African continental margin as being “passive” in a tectonic sense and consider the implications this has for our understanding of global plate tectonics.

Cette thèse présente la première étude Source-to-Sink de la marge Atlantique Equatoriale africaine au Méso-Cénozoïque. Nous avons dans un premier temps produit, à partir d'une nouvelle méthode intégrant les limites d'érosion des dépôts préservés dans les bassins et leur extension initiale minimum, une nouvelle reconstruction paléogéographique et structurale couplant pour la première fois le continent ouest africain et l'Atlantique Equatoriale au cours du Méso-Cénozoïque. Ceci nous permet de suivre l'évolution depuis 200 Ma des domaines en érosion (sources) et en sédimentation (puits) à l'échelle continentale. Nous montrons en particulier qu'au Crétacé supérieur la zone correspondait à un grand bassin intracratonique Saharien qui exportaient ses sédiments à la fois vers la Téthys et vers l'Atlantique Equatoriale. La fragmentation de ce bassin a eu lieu à l'Oligocène par le soulèvement du bouclier du Hoggar qui a isolé les petits dépôt-centres résiduels actuels. Le développement de cette topographie particulière est issu de la superposition de différentes longueurs d'onde de déformation à l'échelle continentale combinant les bourrelets marginaux longeant la marge équatoriale et un bombement de type " point chaud ".Nous avons ensuite caractérisé, à partir de l'interprétation des données sismiques et des puits, la segmentation de la marge continentale équatoriale en segments transformants et divergents et l'architecture stratigraphique post-rift du prisme stratigraphique associée au Crétacé Supérieur. Nous montrons que les parties proximales (dépôts de plateforme et pente continentale) des prismes stratigraphiques du Crétacé Supérieur ne sont préservés que le long des segments divergents de la marge, et pas le long des segments transformants. Nous interprétons cette différence de préservation comme résultant de mouvements verticaux post-rift plus importants dans les domaines proximaux des segments transformants empêchant la préservation des termes proximaux des systèmes sédimentaires. La caractérisation des architectures stratigraphiques post-rifts a ensuite permis la quantification des volumes sédimentaires préservés dans ces bassins de marges passives. En parallèle, de nouvelles données de thermochronologie basse-température (AFTA et (U-Th-Sm/He sur apatite) acquises à l'Université de Glasgow sur les échantillons de trois profils perpendiculaires à la marge équatoriale ont permis de quantifier l'histoire de l'érosion et les volumes dénudés sur le domaine continental au cours du Méso-Cénozoïque. Ces données montrent que le seul événement thermique majeur enregistré correspond au refroidissement lié à la dénudation d'une topographie syn-rift le long de la marge. Le bilan d'érosion et d'accumulation montre que les ordres de grandeur des volumes dénudés et accumulés sont comparables à l'échelle de la marge équatoriale au cours du Méso-Cénozoïque. Certaines périodes (Crétacé Supérieur et depuis le Miocène Supérieur), montrent cependant un excès d'accumulation qui pourrait être associé à la remobilisation de sédiments précédemment stockés dans des bassins intracontinentaux ou sur la plateforme de la marge<br>This PhD thesis presents the first source-to-sink study of the African Atlantic Equatorial margin. We established new Meso-Cenozoic paleogeographic and structural reconstructions, integrating the West African sub-continent and the Equatorial Atlantic Ocean, based on a new mapping method defining both erosion limits of preserved deposits and their minimum original extension. We show the evolution over 200 Myrs of the eroding (sources) and accumulating domains (sinks) at continental scale. We demonstrate in particular that during the Cretaceous, a large Saharan intracratonic basin was exporting sediments toward both the Tethys and the future Atlantic Equatorial Ocean. The fragmentation of this basin occurred in the Oligocene, by the growth of the Hoggar swell that isolated the present-day small residual depot-centers. The development of this specific "basin and swell" topography results from the superimposition of various deformation wavelength at continental scale combining a marginal upwarp along the equatorial margin and a hot spot swell. We then characterized, from the interpretation of seismic data and well logs, the segmentation of the Equatorial Atlantic passive margin and the stratigraphic architecture of the post-rift Upper Cretaceous sedimentary wedge. We show that the proximal parts of the Late Cretaceous sedimentary wedge are only preserved along divergent segments of the margin and not along transform segments. We interpret this differential preservation as the result of a greater uplift, during the early post-rift, in the proximal parts of the transform segments preventing the preservation of the proximal terms of the sedimentary systems. The transform segments are associated with narrow necking zone, resulting in greater flexural uplift than divergent segments showing wider necking zones, in particular during the early post-rift. The characterization of the stratigraphic architecture of the post-rift sedimentary wedge then allowed for the quantification of accumulation history in the passive margin basins. New low-temperature thermochronological data (AFTA and Apatite (U-Th-Sm)/He) acquired at the University of Glasgow on the samples of three regional transects perpendicular to the margin allowed for the quantification of the denudation history and eroded volume on the continental domain. These data shows that the major thermal event recorded by those samples is the cooling phase related to the erosion of a rift-related topography along the margin. Erosion and accumulation budgets fall within the same order of magnitude. During some given periods (Late Cretaceous and since the Late Miocene), excess in accumulation may be associated with the reworking of sediments previously stored within intracontinental basins or on the shelf of the margin

The present thesis consists in a real complex case study of halotectonic deformation in the central portion of the Santos Basin passive margin, investigating the complex interactions between deformation and sedimentation and evaluating its impacts on the petroleum systems.Seismic data set and exploration wells were input to the study, which cover an area where halokinetics affect the active petroleum systems. The thickest depocenter of the Santos basin is partially in the study area. The sedimentary infilling history is associated with the Cabo Frio Fault development, linked with a gap of tens of kilometers in the Albian sediments occurrence. Minibasins are under halotectonic compression towards deep waters. The challenges of this work consists in find methods to build and then to restore the structural model in an effective way.Fifteen interpreted horizons were used to build a surface model. Five geological cross-sections were restored and interpolated to get salt and overburden volumes. The restoration successively removes the uppermost layer and decompacts the remaining layers through sedimentary unloading. Restoration also considers the unloading isostatic compensation by flexure of an elastic weak layered lithosphere. The isostasy plays an important role in the tectono-sedimentary control. Its interaction with bathymetry, faults geometry and deposition surface profile constrains the local and regional subsidence. Biostratigraphic data and seismic pattern defined trough time the absolute paleobathymetry.The cross-section restoration has differentiated the major rift phase sequence deformation from three other drift phase sequences above the sal layer.Several 1D geo-histories were reconstructed for different points along the main direction of transport, to control the thickness variations in the 2D sections. 1D and 2D restorations clearly show that salt moves out of the study area and that there is strong coupling between the halotectonic dynamic and the change in the accommodation space.The extrapolation of the restoration results to 3D allows a better compartmentalization between the hemigrabens in the rift phase; highlights the role of structural high in the center of the investigated area and confirms the relation between structural evolution and sedimentation. Two major depocenters were amalgamated by salt deposition over the accentuated relief inherited from the larger vertical tectonic subsidence of the rift phase. The sedimentary infilling reveals the temporal relations of NE-SW and NNW-SSE oriented structures within the higher subsidence compartment in the western sector of the area. Two different ways to restore the sections allowed the uncertainty estimation of the bathymetry and isostatic relationships.The salt layer material conservation assumption, an operational tool, was consistent with the results. The salt volume balance over time showed a good correlation to lateral extension of the continental drift stage.The implications of the restoration scenario on the petroleum systems were only qualitatively interpreted and then compared to the classical backstripping approach. Three main sectors appear: the proximal shelf, the slope and the deepwater sector of the continental rise. The relatively early halotectonics of the proximal sector induces a more fast and short generation whereas, beyond the continental slope region, the petroleum systems is distally more heterogeneous, develops slower, dissipated and differentiated by the halokinesis, with longer refills fronts. The direct impact of salt restoration on the maturity evaluation is actually relatively small, because about 90% of ductile deformation occurred before 65 Ma and a significant part of the generation is ongoing after 65 Ma. On the other hand, the halotectonic restoration is fundamental regarding its impact on the petroleum systems<br>Ce travail étudie la déformation salifère dans la partie centrale du Bassin de Santos sur la marge Atlantique brésilienne et examine l'interaction complexe entre cette déformation et la sédimentation, ainsi que ses effets sur les systèmes pétroliers. Les données sismiques et les puits disponibles couvrent une zone où l'halocinèse affecte les systèmes pétroliers actifs. Le principal dépôt-centre du bassin est partiellement dans la zone d'étude. L'histoire de remplissage sédimentaire est liée au développement de la faille de Cabo Frio, qui induit un absence des sédiments de l'Albien sur des dizaines de kilomètres. Des mini-bassins dus à la compression salifère se produisent dans la partie la plus distale.Il s'agit dans ce travail de trouver une méthode effective de construire et de restaurer le modèle structural. Quinze horizons stratigraphiques ont été interprétés. Cinq coupes géologiques ont été restaurées et interpolées pour analyser l'évolution temporelle des volumes du sel et des unités encaissantes. La restauration enlève successivement la couche la plus récente et décompacte les couches sous-jacentes en fonction de la charge enlevée. La procédure de restauration prend aussi en compte la compensation flexurale d'une lithosphère élastique et peu épaisse. L'isostasie joue un rôle important dans le contrôle tectono-sédimentaire. Son interaction avec la profondeur d'eau, la géométrie des failles et la surface de dépôt contrôle la subsidence locale et régionale. Des données des puits et les facies sismiques aident à calibrer la paléo-profondeur d'eau.La restauration de coupes différencie la déformation verticale de la phase anté sel des trois autres séquences qui ont été déposées au-dessus du sel. Plusieurs reconstructions 1D illustrent différentes situations le long de la direction principale de transport et permettent de contrôler l'épaisseur des coupes restaurées. Les restaurations 1D et 2D ont clairement montré que le sel s'échappe vers l'est au-delà de la région d'étude. La dynamique du sel se corrèle fortement avec l'espace d'accommodation disponible. L'extrapolation de la restauration au domaine 3D a permis de mieux configurer les demi-grabens de la phase rift, a accentué le rôle des hauts structuraux au centre de la zone étudiée et a montré comment les relations structurales contrôlent la sédimentation. Deux dépôt-centres ont été unis par le déposition de sel sur une topographie escarpée héritée du rifting. Le remplissage du compartiment le plus subsident à l'ouest du modèle a permis des interprétations temporelles par rapport aux structures orientées NE-SW et NNW-SSE. Deux façons de restaurer les coupes ont permis d'évaluer l'incertitude sur la paléo-profondeur d'eau et ses relations avec l'isostasie. L'hypothèse d'une préservation volumique du sel s'est avérée cohérente avec les résultats, puisqu'elle a montré une bonne corrélation avec la distension latérale lors de la dérive continentale.Les implications du scénario restauré sur les systèmes pétroliers ont été interprétées qualitativement et comparées ensuite avec l'approche classique de backstripping. Trois secteurs sont distingués : plateforme, pente et l'eau profonde. La tectonique salifère relativement précoce a induit une génération plus rapide et plus courte pour le secteur plus proche tandis que, au-delà de la pente continentale les systèmes pétroliers distaux sont plus hétérogènes avec un développement ralenti, dissipé et différencié par l'halocinèse, avec de recharges sur des temps plus longs. L'impact direct de la restauration de sel sur l'évaluation de la maturité est relativement faible, puisque 90% de la déformation ductile se produit avant 65 Ma et une partie importante de roches mères ont maturé plus tard. Mais la restauration de la tectonique salifère est essentielle par son impact sur le système pétrolier post déformation

This thesis examines the marginal cost of congested travel to a variety of businesses by observing time spent in congestion and estimating excess labor costs based upon the relevant value of time. The fleets in the scoping study represented commercial deliveries of goods and services, government agencies, and transit systems. Observations on limited-access expressways within the 13-county Atlanta metropolitan region were used in the analysis. Vehicles were monitored by using a passive GPS assembly that transmitted speed and location data in real-time to an off-site location. Installation and operation during the observation period required no interaction from the driver. Over 217 hours of good freeway movement during 354 vehicle-days was recorded. Rates of delay, expressed as a unit of lost minutes per mile traveled, were calculated by taking the difference in speeds observed during congestion from an optimal free-flow speed of 45 mph and dividing that by the distance traveled per segment. The difference between the 50th and 95th percentile delay rates was used as the measure for travel unreliability. Daily average values of extra time needed per fleet vehicle to ensure on-time arrivals were derived, and the median buffer across all fleets was 1.65 hours of added time per vehicle. Weekly marginal costs per fleet vehicle were estimated by factoring in the corresponding driver wages or hourly operation costs (for transit fleets). Equivalent toll rates were calculated by multiplying the 95th percentile delay rate by the hourly costs. The equivalent toll per mile traveled was representative of an equal relationship between the marginal costs of congestion experienced and a hypothetical state of free-flow travel (under first-best rules of marginal cost pricing). The median equivalent toll rates across all fleets was $0.43 per mile for weekday mornings, $0.13 per mile for midday weekdays, $0.53 per mile for afternoon weekdays and $0.01 per mile for weekday nights and weekends.

Thesis (PhD)--Stellenbosch University, 2015.<br>ENGLISH ABSTRACT: This study investigates the crustal structure, and assesses the qualitative and quantitative impacts of crust-mantle dynamics on subsidence pattern, past and present-day thermal field and petroleum system evolution at the southern South African continental margin through the application of a multi-disciplinary and multi-scale geo-modelling procedure involving both conceptual and numerical approaches. The modelling procedure becomes particularly important as this margin documents a complex interaction of extension and strike-slip tectonics during its Mesozoic continental rifting processes. Located on the southern shelf of South Africa, the Western Bredasdorp Basin (WBB) constitutes the focus of this study and represents the western section of the larger Bredasdorp sub-basin, which is the westernmost of the southern offshore sub-basins. To understand the margin with respect to its present-day structure, isostatic state and thermal field, a combined approach of isostatic, 3D gravity and 3D thermal modelling was performed by integrating potential field, seismic and well data. Complimenting the resulting configuration and thermal field of the latter by measured present-day temperature, vitrinite reflectance and source potential data, basin-scale burial and thermal history and timing of source rock maturation, petroleum generation, expulsion, migration and accumulation were forwardly simulated using a 3D basin modelling technique. This hierarchical modelling workflow enables geologic assumptions and their associated uncertainties to be well constrained and better quantified, particularly in three dimensions. At present-day, the deep crust of the WBB is characterised by a tripartite density structure (i.e. prerift metasediments underlain by upper and lower crustal domains) depicting a strong thinning that is restricted to a narrow E-W striking zone. The configuration of the radiogenic crystalline crust as well as the conductivity contrasts between the deep crust and the shallow sedimentary cover significantly control the present-day thermal field of the study area. In all respects, this present-day configuration reflects typical characteristics of basin evolution in a strike-slip setting. For instance, the orientations of the deep crust and fault-controlled basin-fill are spatially inconsistent, thereby indicating different extension kinematics typical of transtensional pull-apart mechanisms. As such, syn-rift subsidence is quite rapid and short-lived, and isostatic equilibrium is not achieved, particularly at the Moho level. Accompanied syn-rift rapid subsidence and a heat flow peak led to petroleum preservation in the basin since the Early Cretaceous. Two additional post-rift thermal anomalies related to the Late Cretaceous hotspot mechanism and Miocene margin uplift in Southern Africa succeeded the syn-rift control on maturation. This thermal maturity of the five mature source rocks culminated in four main generation and three main accumulation phases which characterise the total petroleum systems of the WBB. The Campanian, Eocene and Miocene uplift scenarios episodically halted source maturation and caused tertiary migration of previously trapped petroleum. Petroleum loss related to the spill point of each trap configuration additionally occurs during the Late Cretaceous-Paleocene and Oligocene-Early Miocene. The timing and extent of migration dynamics are most sensitive to the geological scenario that combined faulting, intrusive seal bypass system and facies heterogeneity. In fact, for models that do not incorporate facies heterogeneity, predicted past and present-day seafloor leakage of petroleum is largely underestimated. This complex interplay of generation and migration mechanisms has significant implications for charging of petroleum accumulations by multiple source rocks. Due to early maturation and late stage tertiary migration, the syn-rift source rocks particularly Mid Hauterivian and Late Hauterivian source intervals significantly control the extent of petroleum accumulation and loss in the basin. Lastly, the modelled 3D crustal configuration and Mezosoic to Cenozoic thermal regime of the WBB dispute classic uniform lithospheric stretching for the southern South African continental margin. Rather, this PhD thesis confirms that differential thinning of the lithosphere related to a transtensional pull-apart mechanism is the most appropriate for accurately predicting the evolution of basin and petroleum systems of the margin. Also, the presented 3D models currently represent the most advanced insights, and thus have clear implications for assessing associated risks in basin and prospect evaluation of the margin as well as other similar continental margins around the world.<br>AFRIKAANSE OPSOMMING: Hierdie studie ondersoek die korsstruktuur en evalueer die kwalitatiewe en kwantitatiewe impakte van kors-mantel-dinamika op insinkingspatroon, die termiese veld en petroleumstels evolusie aan die suidelike Suid-Afrikaanse kontinentale grens, in die hede en die verlede, deur die toepassing van ’n multidissiplinêre en multiskaal-geomodelleringsprosedure wat beide konseptuele en numeriese benaderings behels. Die modelleringsprosedure veral is belangrik aangesien hierdie kontinentale grens ’n komplekse interaksie van uitbreidings- en strekkingsparallelle tektoniek gedurende die Mesosoïese vastelandskeurprosesse daarvan dokumenteer. Omdat dit op die suidelike platvorm van Suid-Afrika geleë is, maak die Westelike Bredasdorp Kom (WBK) die fokus van hierdie studie uit, en verteenwoordig dit die westelike deel van die groter Bredasdrop-subkom, wat die verste wes is van die suidelike aflandige subkomme. Om die grens met betrekking tot sy huidige struktuur, isostatiese staat en termiese veld te verstaan, is ’n kombinasie benadering bestaande uit isostatiese, 3D-gravitasie- en 3D- termiese modellering gebruik deur potensiëleveld-, seismiese en boorgatdata te integreer Ondersteunend totot die gevolglike konfigurasie en termiese veld van die laasgenoemde deur middel van hedendaagse temperatuur, soos gemeet, vitriniet-refleksiekoëffisiënt en bronpotensiaal data, komskaal-begrawing en termiese geskiedenis en tydsberekening van brongesteentematurasie, is petroleumgenerasie, -uitwerping, -migrasie en -akkumulasie in die toekoms gesimuleer deur gebruik te maak van ’n 3D-kommodelleringstegniek. Hierdie hierargiese modelleringswerkvloei maak dit moontlik om geologiese aannames en hulle geassosieerde onsekerhede goed aan bande te lê en beter te kwantifiseer, veral in drie dimensies. In die hede word die diep kors van die WBK gekarakteriseer deur ’n drieledige digtheidstruktuur (met ander woorde voorrift-metasedimente onderlê deur bo- en benedekors domeine) wat dui op ’n baie wesenlike verdunning, beperk tot ’n dun O-W-strekkingsone. Die konfigurasie van die radiogeniese kristallyne kors, sowel as die konduktiwiteitskontraste tussen die diep kors en die vlak sedimentêre dekking, beheer grotendeels die hedendaagse termiese veld van die studiearea. Hierdie hedendaagse konfigurasie weerspieël in alle opsigte tipiese eienskappe van kom-evolusie in ’n skuifskeur omgewing. Byvoorbeeld, Die oriëntasies van die diep kors en verskuiwingbeheerde komsedimentasie byvoorbeeld is ruimtelik inkonsekwent en dui daardeur op verskillende ekstensiekinematika, tipies van transtensionale tensiemeganisme. As sulks, is sin-rift-versakking taamlik vinnig en kortstondig, en word isostatiese ekwilibrium nie by die Moho-vlak, in die besonder, bereik nie. Samehangende sin-rift vinnige versakking en hittevloeihoogtepunt het gelei tot petroleum behoud in die kom sedert die vroeë Kryt. Twee bykomende post-rift termiese anomalieë wat verband hou met die laat Kryt-“hotspot” meganisme en die Mioseense kontinentale grensopheffing in Suidelike Afrika het die sin-rift-beheer met maturasie opgevolg. Hierdie termiese maturiteit van die vyf gematureerde brongesteentes het in vier hoofgenerasie- en drie hoofakkumulasie fases, wat die totaliteit van die petroleumstelsels van die WBK karakteriseer, gekulmineer. Die Campaniese, Eoseense en Mioseense opheffings senarios het episodies bronmaturasie gestop en tersiêre migrasie van petroleum wat vroeër opgevang was veroorsaak. Addisioneel vind petroleumverlies gekoppel aan die spilpunt van elke opvanggebiedkonfigurasie tydens die laat Kryt-Paleoseen en Oligoseenvroeë Mioseen plaas. Die tydstelling en omvang van migrasiedinamika is die sensitiefste vir die geologiese scenario wat verskuiwing, seëlomseilingstelsel en fasiesheterogeniteit kombineer. Trouens, vir modelle wat nie fasiesheterogeniteit inkorporeer nie, is voorspellings van vroeëre en huidige seebodemlekkasie van petroleum grotendeels onderskattings. Hierdie komplekse wisselwerking van generasie- en migrasiemeganismes het beduidende implikasies vir die laai van petroleumakkumulasies deur veelvoudige brongesteentes. Vanweë vroeë maturasie en laatstadiumtersiêre migrasie, oefen die sin-rift-brongesteentes, veral middel Hauterivium- en laat Hauteriviumbronintervalle, beduidende beheer oor die omvang van petroleumakkumulasie en -verlies in die kom uit. Laastens weerspreek die gemodelleerde 3D-korskonfigurasie en Mesosoïese-tot-Senosoïesetermiese regime van die WBK ’n klassieke uniforme litosferiese rekking vir die suidelike Suid- Afrikaanse kontinentale grens. Inteendeel, hierdie PhD-proefskrif bevestig dat ’n differensiële verdunning van die litosfeer, gekoppel aan ’n transtensiemeganisme, die beste geskik is om ’n akkurate voorspelling oor die evolusie van kom- en petroleumstelsels van die kontinentale grens mee te maak. Verder, verteenwoordig die 3D-modelle, wat hier aangebied word, tans die mees gevorderde insigte, en het hierdie modelle dus duidelike implikasies vir die assessering van verwante risiko’s in kom- en petroleum teikene valuering van die kontinentale grens, so wel as van ander soortgelyke kontinentale grense regoor die wêreld.

Cadre geodynamique de la marge marocaine. Structure et evolution tectonique et sedimentaire de la marge el jadida. Comparaison des resultats avec ceux connus sur la marge nord-ouest africaine jusqu'au plateau de guinee et sur la marge conjuguee de la nouvelle-ecosse, georges bank

CIVINS<br>Approved for public release ; distribution is unlimited<br>This thesis is a geotechnical engineering report which includes a topographical profile at three propitious locations across the American continent for the construction of an interoceanic passage between the Atlantic and Pacific oceans. Surficial soils as well as the general topography of the centerline of the alignments were investigated to the extent possible and an attempt was made to investigate underlying strata. Some information is illustrated graphically to allow an appreciation of the physical irregularities and a rough approximation for the type and extent of excavation required. Although other alternatives exist, this thesis considers only to 3 locations: Mexico, across the Tehuantepec Isthmus, and following the course of the Coatzacoalcos River as closely as possible; Nicaragua, along its border with Costa Rica and using lake Nicaragua and the San Juan River as the main bodies of water; and Colombia, in the vicinity of the Colombia-Panama border using the Atrato River as the main body of water. The majority of the information was gathered from available geological reports and topographic maps. Some of the data for the Nicaraguan and Colombian routes was compared with information published in a study by the Atlantic-Pacific Interoceanic Canal Study Commission (1970). Engineering geology; Site selection; Canals/waterways; Theses.

Current conventional weather forecasts are based on high-dimensional numerical models. They are usually only skillful up to a maximum lead time of around 7 days due to the chaotic nature of the climate dynamics and the related exponential growth of model and data initialisation errors. Even the fully detailed medium-range predictions made for instance at the European Centre for Medium-Range Weather Forecasts do not exceed lead times of 14 days, while even longer-range predictions are limited to time-averaged forecast outputs only. Many sectors would profit significantly from accurate forecasts on seasonal time scales without needing the wealth of details a full dynamical model can deliver. In this thesis, we aim to study the potential of a much cheaper data-based statistical approach to provide predictions of comparable or even better skill up to seasonal lead times, using as an examplary forecast target the time until the next occurrence of frost. To this end, we first analyse the properties of the temperature anomaly time series obtained from measured data by subtracting a sinusoidal seasonal cycle, as well as the distribution properties of the first passage times to frost. The possibility of generating additional temperature anomaly data with the same properties by using very simple autoregressive model processes to potentially reduce the statistical fluctuations in our analysis is investigated and ultimately rejected. In a next step, we study the potential for predictability using only conditional first passage time distributions derived from the temperature anomaly time series and confirm a significant dependence of the distributions on the initial conditions. After this preliminary analysis, we issue data-based out-of-sample forecasts for three different prediction targets: The specific date of first frost, the probability of observing frost before summer for forecasts issued in spring, and the full probability distribution of the first passage times to frost. We then study the possibility of improving the forecast quality first by enhancing the stationarity of the temperature anomaly time series and then by adding as an additional input variable the state of the North Atlantic Oscillation on the date the predictions are issued. We are able to obtain significant forecast skill up to seasonal lead times when comparing our results to an unskilled reference forecast. A first comparison between the data-based forecasts and corresponding predictions gathered from a dynamical weather model, necessarily using a lead time of only up to 15 days, shows that our simple statistical schemes are only outperformed (and then only slightly) if further statistical post-processing is applied to the model output.<br>Aktuelle Wetterprognosen werden mit Hilfe von hochdimensionalen, numerischen Modellen generiert. Durch die dem Klima zugrunde liegende chaotische Dynamik wachsen Modellfehler und Ungenauigkeiten in der Modellinitialisierung exponentiell an, sodass Vorhersagen mit signifikanter Güte üblicherweise nur für eine Vorlaufzeit von maximal sieben Tagen möglich sind. Selbst die detaillierten Prognosen des Europäischen Zentrums für mittelfristige Wettervorhersagen gehen nicht über eine Vorlaufzeit von 14 Tagen hinaus, während noch längerfristigere Vorhersagen auf zeitgemittelte Größen beschränkt sind. Viele Branchen würden signifikant von akkuraten Vorhersagen auf saisonalen Zeitskalen pro-fitieren, ohne das ganze Ausmaß an Details zu benötigen, das von einem vollständigen dynamischen Modell geliefert werden kann. In dieser Dissertation beabsichtigen wir, am Beispiel einer Vorhersage der Zeitdauer bis zum nächsten Eintreten von Frost zu untersuchen, inwieweit deutlich kostengünstigere, datenbasierte statistische Verfahren Prognosen von gleicher oder sogar besserer Güte auf bis zu saisonalen Zeitskalen liefern können. Dazu analysieren wir zunächst die Eigenschaften der Zeitreihe der Temperaturanomalien, die aus den Messdaten durch das Subtrahieren eines sinusförmigen Jahresganges erhalten werden, sowie die Charakteristiken der Wahrscheinlichkeitsverteilungen der Zeitdauer bis zum nächsten Eintreten von Frost. Die Möglichkeit, durch einen einfachen autoregressiven Modellprozess zusätzliche Datenpunkte gleicher statistischer Eigenschaften wie der Temperaturanomalien zu generieren, um die statistischen Fluktuationen in der Analyse zu reduzieren, wird untersucht und letztendlich verworfen. Im nächsten Schritt analysieren wir das Vorhersagepotential, wenn ausschließlich aus den Temperaturanomalien gewonnene bedingte Wahrscheinlichkeitsverteilungen der Wartezeit bis zum nächsten Frost verwendet werden, und können eine signifikante Abhängigkeit der Verteilungen von den Anfangsbedingungen nachweisen. Nach dieser einleitenden Untersuchung erstellen wir datenbasierte Prognosen für drei verschiedene Vorhersagegrößen: Das konkrete Datum, an dem es das nächste Mal Frost geben wird; die Wahrscheinlichkeit, noch vor dem Sommer Frost zu beobachten, wenn die Vorhersagen im Frühjahr ausgegeben werden; und die volle Wahrscheinlichkeitsverteilung der Zeitdauer bis zum nächsten Eintreten von Frost. Anschließend untersuchen wir die Möglichkeit, die Vorhersagegüte weiter zu erhöhen - zunächst durch eine Verbesserung der Stationarität der Temperaturanomalien und dann durch die zusätzliche Berücksichtigung der Nordatlantischen Oszillation als einer zweiten, den Anfangszustand charakterisierenden Variablen im Vorhersageschema. Wir sind in der Lage, im Vergleich mit einem naiven Referenzvorhersageschema eine signifikante Verbesserung der Vorhersagegüte auch auf saisonalen Zeitskalen zu erreichen. Ein erster Vergleich zwischen den datenbasierten Vorhersagen und entsprechenden, aus den dynamischen Wettermodellen gewonnenen Prognosen, der sich notwendigerweise auf eine Vorlaufzeit der Vorhersagen von lediglich 15 Tagen beschränkt, zeigt, dass letztere unsere simplen statistischen Vorhersageschemata nur schlagen (und zwar knapp), wenn der Modelloutput noch einer statistischen Nachbearbeitung unterzogen wird.

Migration results of two multi-channel vertical incidence reflection seismic dataset offshore Virginia are presented. A new velocity model derived from multi-channel and wide-angle reflection/refraction data is developed and fit into regional geology context. The validity and limitation of the new model is discussed by means of ray-tracing travel time forward modeling and 2-D acoustic wave-equation modeling methods. Our new results show that there is a sharp boundary separating normal continental crust from crust produced by the sea-floor spreading process in this region and that the Moho appears to be continuous across the boundary. The zone of so-called "magmatic underplating" proposed previously (Sheridan et al., 1993) may well be magmas produced during the initial stage of sea-floor spreading. There may be some fragments of continental crust entrained in the region immediately seaward of the boundary, but there is no evidence of the existence of large volume of continental crust and we believe the crust in this area is also primarily product of the Mesozoic sea-floor spreading. (Abstract shortened by UMI.)

Tese de doutoramento, Ciências Geofísicas e da Geoinformação (Geofísica), Universidade de Lisboa, Faculdade de Ciências, 2017<br>Twelve combined wide-angle refraction and coincident multi-channel seismic profiles were acquired in the Recˆoncavo, Tucano, Jequitinhonha, Camamú-Almada, Jacuípe, and Sergipe-Alagoas basins, NE Brazil, during the SALSA experiment in 2014. Profiles SL11 (170 km long) and SL12 (180 km long) image the Jequitinhonha basin perpendicularly to the coast, with 15 and 11 four-channel ocean-bottom seismometers, respectively. Forward modelling, combined with pre-stack depth migration to increase the horizontal resolution of the models, resulted in P-wave velocity models that allow the characterisation of the crustal structure and lithospheric mantle of the Jequitinhonha and Camamu-Almada basins. The models are also consistent with the shipboard and satellite gravity anomaly observations. On both profiles, the sedimentary layers reach a thickness of, at least, 3:3 km in the distal basin. The thickness of the sediments increases gradually towards the coast, up to 4:1 km on profile SL11 and up to 6:2 km on SL12. Eight sedimentary mega-sequences are identified and modelled from both OBS and MCS data. Their P-wave seismic propagation velocities increase gradually inside the sedimentary column, although with a slight decrease towards the distal basin, specially on the shallowest layers. Acoustic propagation velocities in the sediments range from 1:8 km=s to 5:2 km=s. These values are confirmed by the RMO analysis of PSDM images. The basement structure has five layers: upper crust, middle crust, lower crust, anomalous velocity zone, and lithospheric mantle. The upper crust has a thickness of 1:0-2:0 km on the distal basin, increasing to 3:7 km on SL11 and 2:9 km on SL12 on the continental slope, with velocities at the top and bottom of the western end from 5:2 km=s to 5:3 km=s that, on profile SL11, decrease to 4:7 km=s and 5:0 km=s at the eastern end. On profile SL11, the middle crust thins from 6:5 km on the continental slope to 1:5 km on the distal basin, with velocities at the top and bottom from 5:6 km=s to 6:1 km=s on the continental slope, and from 5:8 km=s to 6:4 km=s on the distal basin. The thinning is almost symmetrical with respect to the top and base of the layer. On profile SL12, the middle crust has higher propagation velocities, from 6:7 km=s to 7:2 km=s on the continental slope, and from 7:0 km=s to 7:2 km=s on the distal basin, but the relative gradients and thicknesses are similar to those of SL11. The lower crust of SL12 is 5:5 km thick at the western end of the model and completely thins out at 45 km model distance, with velocities at the top and bottom from 7:2 km=s to 7:3 km=s. On profile SL11, the lower crust thins from 8:5 km on the continental slope to 2 km on the distal basin, with velocities at the top and bottom from 6:4 km=s to 6:8 km=s on the distal basin and 6:3 km=s to 6:8 km=s on the continental slope. SL11 has an anomalous velocity zone up to 3 km thick, with velocities at the top and bottom from 7:6 km=s to 8:1 km=s. This feature is not modelled on SL12, but cannot be excluded, given the velocity uncertainty bounds of the model. The lithospheric mantle below the Moho has a velocity of 8:0 km=s to 8:2 km=s. The velocity models indicate two major crustal domains. A thinned continental crust domain, up to 60 km model distance on SL11 and up to 40 km model distance SL12, and a domain where the crust is interpreted as being exhumed lower continental crust. Typical oceanic crust is never imaged. The necking zone is estimated to be 100 km long. Using the results from profiles SL06, SL09 and SL10, that image the Jequitinhonha and Camamu-Almada basins, and the Camamu triple point, the region where the exhumed lower continental crust is found can be extrapolated further north. At the Camamu triple point, well correlated with a gravimetric anomaly high, the upper crust is extremely thinned ,and can be linked to the thinning paroxysm during the opening of the South Atlantic. The VMONTECARLO method was developed to estimate the uncertainty of wideangle seismic refraction models. This method is based on the random exploration of the solution space around the preferred model. It provides upper and lower boundaries for parameter values within which the models have a data fit similar to the preferred model’s. It was successfully applied to models SL11 and SL12, but also to models SB01 and SB02 of the SANBA mission.