Climate change during the last 2.5 million years is characterised by glacial-interglacial cycles of fluctuating sea level and temperature increasing in magnitude and duration towards the present day. The central North Sea preserves these glacial-interglacial cycles in an expanded sedimentary sequence creating a high resolution palaeo-climatic record. Basin-wide, low-resolution 3D seismic data, covering more than 80,000 km2 of the central North Sea, is combined with high-resolution, broadband 3D seismic, regional 2D seismic and local ultra-high resolution seismic from the Dogger Bank windfarm development zone in order to investigate in full the sedimentary sequence. The evolution of the basin is analysed along with the preserved geomorphological landforms in order to build a framework for the development of the North Sea and its changing palaeo-environments from the inception of the Quaternary (2.58 Ma) until the extensive glacial unconformity formed during the Elsterian (0.48 Ma).At the onset of the Quaternary the structure of the North Sea was that of an elongate marine basin, rapidly infilled from the south by continued progradation of the large clinoformal deposits of the southern North Sea deltaic system. The basin rapidly decreased in extent and depth however it was not until around 1.1 Ma that the broad, shallow shelf of the present day was fully established. A revision of the current seismic stratigraphy is proposed, identifying four new Members within the Aberdeen Ground Formation taking into account the development of the basin through time. Powerful downslope gravity currents dominated the basin during much of the early Quaternary, although a well-established, anti-clockwise tidal gyre acted to gently modify the gravity currents. Iceberg scouring was nearly continual from the onset of the Quaternary until grounded ice sheets began to penetrate into the basin from 1.7 Ma, more than half a million years before any previous estimates. Effects of confluence of the British and Fennoscandian ice sheets are observed from 1.3 Ma. The tunnel valleys of the Dogger Bank represent a continuation of the North Sea tunnel valley network, interacting with both older glaciotectonic thrusting and younger glaciotectonic folded deformation.

O interesse no uso de técnicas de aquisição de dados 3D em vídeos interativos e sistemas de videoconferência imersiva aumentou significativamente nos últimos anos. A disponibilidade de sensores de profundidade baseados em luz estruturada no varejo apresenta uma série de novas oportunidades em sistemas de teleconferência, entretenimento e e-learning. No entanto, problemas de oclusão frequentemente ocorrem quando é utilizado um único sensor ou técnicas de reconstrução 2,5D. Outras técnicas de interação e aplicações de teleconferências podem exigir uma reconstrução mais completa do usuário. Uma possível solução para isso implica na utilização de múltiplos dispositivos simultaneamente, o que traz novos desafios relacionados ao processo de calibração de câmaras e a aferição do aumento da superfície capturada quando é adicionado um novo sensor. Neste trabalho é apresentada a proposta VMD (Video-avatar from Multiple Depth maps), uma arquitetura de sistema que trata esses dois problemas. Com a finalidade de validar a viabilidade dessa proposta, três experimentos foram feitos resultando em uma análise qualitativa e quantitativa a fim de encontrar uma configuração adequada de múltiplos sensores de profundidade. / The interest in the use of 3D data acquisition techniques in video based interaction and immersive videoconferencing systems has noticeably increased in recent years. The availability of structured light 3D sensors as off-the-shelf hardware presents a series of new opportunities in teleconferences, entertainment and e-learning. However, occlusion issues often occur when it is used a single sensor or 2,5D reconstruction techniques. Other interaction techniques and teleconferencing applications may require a more complete reconstruction of the user. One possible solution to this involves the use of multiple devices simultaneously, which may bring new challenges related to the calibration process of cameras and measurement of the increase in covered area when it is added a new sensor. In this work we present VMD (Video-avatar from Multiple Depth maps), a system architecture that addresses this two issues. In order to validate the feasibility of this proposal, three experiments were performed resulting in a qualitative and quantitative analysis with the purpose of finding a suitable setup with multiple depth sensors.

O interesse no uso de técnicas de aquisição de dados 3D em vídeos interativos e sistemas de videoconferência imersiva aumentou significativamente nos últimos anos. A disponibilidade de sensores de profundidade baseados em luz estruturada no varejo apresenta uma série de novas oportunidades em sistemas de teleconferência, entretenimento e e-learning. No entanto, problemas de oclusão frequentemente ocorrem quando é utilizado um único sensor ou técnicas de reconstrução 2,5D. Outras técnicas de interação e aplicações de teleconferências podem exigir uma reconstrução mais completa do usuário. Uma possível solução para isso implica na utilização de múltiplos dispositivos simultaneamente, o que traz novos desafios relacionados ao processo de calibração de câmaras e a aferição do aumento da superfície capturada quando é adicionado um novo sensor. Neste trabalho é apresentada a proposta VMD (Video-avatar from Multiple Depth maps), uma arquitetura de sistema que trata esses dois problemas. Com a finalidade de validar a viabilidade dessa proposta, três experimentos foram feitos resultando em uma análise qualitativa e quantitativa a fim de encontrar uma configuração adequada de múltiplos sensores de profundidade. / The interest in the use of 3D data acquisition techniques in video based interaction and immersive videoconferencing systems has noticeably increased in recent years. The availability of structured light 3D sensors as off-the-shelf hardware presents a series of new opportunities in teleconferences, entertainment and e-learning. However, occlusion issues often occur when it is used a single sensor or 2,5D reconstruction techniques. Other interaction techniques and teleconferencing applications may require a more complete reconstruction of the user. One possible solution to this involves the use of multiple devices simultaneously, which may bring new challenges related to the calibration process of cameras and measurement of the increase in covered area when it is added a new sensor. In this work we present VMD (Video-avatar from Multiple Depth maps), a system architecture that addresses this two issues. In order to validate the feasibility of this proposal, three experiments were performed resulting in a qualitative and quantitative analysis with the purpose of finding a suitable setup with multiple depth sensors.

Reconstruction studies of seasonal rainfall utilizing stable isotope based proxy approach suffer from the limitations of time resolutions. Conventional methods and archives limit the achievable resolution to annual scales. However, high resolution reconstruction (seasonal to sub-weekly scale) can be achieved in proxy records where growth rates are high enough to leave spatial signatures in an organically or inorganically deposited layer such as growth bands. In this study, aragonitic skeleton of the gastropod Lissachatina fulica (Bowdich, Giant African Land Snails) is investigated with an aim to achieve sub-weekly scale reconstruction of the Indian monsoon rainfall. These terrestrial gastropods are native of Africa and highly invasive. Their evolution in the geological time period dates back to the Pliocene and is presently distributed across the tropical belt. They exhibit a high growth rate in the presence of water and high relative humidity in the environment. As a result, they are ideally suited for the task of palaeo seasonality reconstruction. The isotopic patterns recorded in their growth bands reveal composition of environmental water at seasonal time scales. In vitro studies were carried out on L. fulica to estimate their growth rates and growth responses to changes in the physical conditions within the culture chamber. The Indian monsoon rainfall exhibits characteristic dry spells that are generally sandwiched between periods of active phases of high rainfall during the South West monsoon season. These dry spells are typically characterized by rainfall with low intensity. Isotope fingerprinting of the rain water at daily time resolution, covering the years of 2007-10 exhibited distinct isotopic ratios for the dry and wet spells. Dry spells were clearly demarcated in the record with isotopically enriched signature. In addition, the study indentified the role of three distinct moisture sources on δ18O of rain water at Bangalore, India. The variability in the oxygen isotopic composition of the Indian monsoon rainfall is predominantly controlled by this source moisture variability at inter annual time scales, while temperature and amount of rainfall tend to dominate the variability in the precipitation isotopes at seasonal and weekly scales. Simultaneous isotopic analyses of both rainwater and shell carbonates growth bands were undertaken to understand their relationship to aid in high resolution reconstruction. Carbonate found in the growth bands of the gastropods, which is precipitated under equilibrium condition from rainwater, preserves the signature of rainfall. This provides an opportunity to reconstruct rainfall parameters (i.e. amount and moisture sources) knowing the variability in shell carbonates. Stable isotopic ratios measured across the growth bands of live shell specimens collected from the southern and eastern Indian regions (Bangalore and Kolkata, respectively) were compared with the rainfall isotope ratios at these two locations; signature of dry spells were clearly identified from the study of isotopic composition in the growth bands of the gastropod specimens. The approach was also extended to older samples from historical archives from eastern Indian region (Kolkata, East India). Individual specimens belonging to the same species of gastropod, which were collected during the monsoon season of the year 1918 were used for reconstructing the seasonal pattern in monsoon rainfall over the region. The record of variation in the isotopic composition seen in the shell was compared with the rainfall data from Indian Metrological Division observatory at Kolkata station. The year 1918 was characterized as a major drought year and the signature of dry period was seen preserved in the specimen. The work under taken in this thesis will widen the scope of seasonality reconstruction using terrestrial shell fossils from palaeo records, which have been rarely investigated in paleoclimate studies from the perspective of understanding the seasonal precipitation variability.

Reconstruction studies of seasonal rainfall utilizing stable isotope based proxy approach suffer from the limitations of time resolutions. Conventional methods and archives limit the achievable resolution to annual scales. However, high resolution reconstruction (seasonal to sub-weekly scale) can be achieved in proxy records where growth rates are high enough to leave spatial signatures in an organically or inorganically deposited layer such as growth bands. In this study, aragonitic skeleton of the gastropod Lissachatina fulica (Bowdich, Giant African Land Snails) is investigated with an aim to achieve sub-weekly scale reconstruction of the Indian monsoon rainfall. These terrestrial gastropods are native of Africa and highly invasive. Their evolution in the geological time period dates back to the Pliocene and is presently distributed across the tropical belt. They exhibit a high growth rate in the presence of water and high relative humidity in the environment. As a result, they are ideally suited for the task of palaeo seasonality reconstruction. The isotopic patterns recorded in their growth bands reveal composition of environmental water at seasonal time scales. In vitro studies were carried out on L. fulica to estimate their growth rates and growth responses to changes in the physical conditions within the culture chamber. The Indian monsoon rainfall exhibits characteristic dry spells that are generally sandwiched between periods of active phases of high rainfall during the South West monsoon season. These dry spells are typically characterized by rainfall with low intensity. Isotope fingerprinting of the rain water at daily time resolution, covering the years of 2007-10 exhibited distinct isotopic ratios for the dry and wet spells. Dry spells were clearly demarcated in the record with isotopically enriched signature. In addition, the study indentified the role of three distinct moisture sources on δ18O of rain water at Bangalore, India. The variability in the oxygen isotopic composition of the Indian monsoon rainfall is predominantly controlled by this source moisture variability at inter annual time scales, while temperature and amount of rainfall tend to dominate the variability in the precipitation isotopes at seasonal and weekly scales. Simultaneous isotopic analyses of both rainwater and shell carbonates growth bands were undertaken to understand their relationship to aid in high resolution reconstruction. Carbonate found in the growth bands of the gastropods, which is precipitated under equilibrium condition from rainwater, preserves the signature of rainfall. This provides an opportunity to reconstruct rainfall parameters (i.e. amount and moisture sources) knowing the variability in shell carbonates. Stable isotopic ratios measured across the growth bands of live shell specimens collected from the southern and eastern Indian regions (Bangalore and Kolkata, respectively) were compared with the rainfall isotope ratios at these two locations; signature of dry spells were clearly identified from the study of isotopic composition in the growth bands of the gastropod specimens. The approach was also extended to older samples from historical archives from eastern Indian region (Kolkata, East India). Individual specimens belonging to the same species of gastropod, which were collected during the monsoon season of the year 1918 were used for reconstructing the seasonal pattern in monsoon rainfall over the region. The record of variation in the isotopic composition seen in the shell was compared with the rainfall data from Indian Metrological Division observatory at Kolkata station. The year 1918 was characterized as a major drought year and the signature of dry period was seen preserved in the specimen. The work under taken in this thesis will widen the scope of seasonality reconstruction using terrestrial shell fossils from palaeo records, which have been rarely investigated in paleoclimate studies from the perspective of understanding the seasonal precipitation variability.