Continental margin architecture : the palynological signature of glacioeustasy /

Palynomorphs from two siliciclastic margins were examined to gain insights into continental margin architecture. Sea level change is thought to be one of the primary controls on continental margin architecture. Because Late Neogene glacioeustasy has been well studied marine sediments deposited during the Late Neogene were examined to test this concept. Cores from the outer shelf and upper slope were taken from the New Jersey margin in the western North Atlantic Ocean and from the Sunda Shelf margin in the South China Sea. Continental margin architecture is often described in a sequence stratigraphic context. One of the main goals of both coring projects was to test the theoretical sequence stratigraphic models developed by a research group at Exxon (e.g. Wilgus et al., 1988). Palynomorphs provide one of the few methods of inferring continental margin architecture in monotonous, siliciclastic marine sediments where calcareous sediments are rare (e.g. New Jersey margin). In this study theoretical models of the palynological signature expected in sediment packages deposited during the various increments of a glacioeustatic cycle were designed. These models were based on the modem palynomorph trends and taphonomic factors thought to control palynomorph distribution. Both terrestrial (pollen and spores) and marine (dinocysts) palynomorphs were examined. The palynological model was then compared with New Jersey margin and Sunda Shelf margin sediments. The predicted palynological trends provided a means of identifying a complete cycle of glacioeustatic change (Oxygen Isotope Stage 5e to present) in the uppermost 80 meters of sediment on the slope at the New Jersey margin. Sediment availability, not sea meters of sediment on the slope at the New Jersey margin. Sediment availability, not sea level change, is thought to be the major factor controlling margin architecture during the late Pleistocene here at the upper slope. This is likely a function of the glacial scouring of the continents which significantly increases sediment availability during glacial stages. The subaerially exposed continental shelf during the lowstand periods would have been subject to significant amounts of erosion fi:om the proglacial rivers flowing fi-om the southern regions of the ice-sheet. The slope site is non-depositional today and was also non-depositional during the last full interglacial period. The palynomorph data obtained fi-om the South China Sea indicate that the major difference between the New Jersey Margin sites and the Sunda Shelf margin sites is the variation in sediment supply and the rate of sediment accumulation. There was significantly less variation in sediment supply between glacial and interglacial periods and less overall sediment accumulation at the Sunda Shelf margin. The data presented here indicate that under certain conditions the theoretical palynological models allow the identification of individual sequence stratigraphic units and therefore, allow inferences regarding continental margin architecture. The major condition required in this approach is that a complete and reliable database of the contemporaneous palynomorphs be available.

Geology of the Gander Group, Gander River Ultramafic Belt and Davidsville Group in the Jonathan's Pond - Weir's Pond Area, northeast Newfoundland /

The study area is situated in NE Newfoundland between Gander Lake and the north coast and on the boundary between the Gander and Botwood tectonostratigraphic zones (Williams et al., 1974). The area is underlain by three NE trending units; the Gander Group, the Gander River Ultramafic Belt (the GRUB) and the Davidsville Group. The easternmost Gander Group consists of a thick, psammitic unit composed predominantly of psammitic schist and a thinner, mixed unit of semipelitic and pelitic schist with minor psammite. The mixed unit may stratigraphically overlie the psammitic unit or be a lateral facies equivalent of the latter. No fossils have been recovered from the Gander Group. The GRUB is a terrain of mafic and ultramafic plutonic rocks with minor pillow lava and plagiogranite. It is interpreted to be a dismembered ophiolite in thrust contact with the Gander Group. The westernmost Davidsville Group consists of a basal conglomerate, believed deposited unconformably upon the GRUB from which it was derived, and an upper unit of greywacke and slate, mostly of turbidite origin, with minor limestone and calcareous sandstone. The limestone, which lies near the base of the unit, contains Upper Llanvirn to Lower Llandeilo fossils. The Gander and Davidsville Groups display distinctly different sedimentological , structural and metamorphic histories. The Gander Group consists of quartz-rich, relatively mature sediment. It has suffered three pre-Llanvirn deformations, of which the main deformation, Dp produced a major, NE-N-facing recumbent anticline in the southern part of the study area. Middle greenschist conditions existed from D^ to D- with growth of metamorphic minerals during each dynamic and static phase. In contrast, the mineralogically immature Davidsville Group sediment contains abundant mafic and ultramafic detritus which is absent from the Gander Group. The Davidsville Group displays the effects of a single penetrative deformation with localized D_ and D_ features, all of which can be shown to postdate D_ in the Gander Group. Rotation of the flat Gander S- into a subvertical orientation near the contact with the GRUB and the Davidsville Group is believed to be a Davidsville D^ feature. Regional metamorphism in the Davidsville Group is lower greenschist with a single growth phase, MS . These sedimentological, structural and metamorphic differences between the Gander and Davidsville Groups persist even where the GRUB is absent and the two units are in contact, indicating that the tectonic histories of the Gander and Davidsville Groups are distinctly different. Structural features in the GRUB, locally the result of multiple deformations, may be the result of Gander and/or Davidsville deformations. Metamorphism is in the greenschist facies. Geochemical analyses of the pillow lava suggest that these rocks were formed in a back-arc basin. Mafic intrusives in the Gander Group appear to be the result of magraatism separate from that producing the pillow lava. The Gander Group is interpreted to be a continental rise prism deposited on the eastern margin of the Late Precambrian-Lower Paleozoic lapetus Ocean. The GRUB, oceanic crust possibly formed in a marginal basin to the west, is believed to have been thrust eastward over the Gander Group, deforming the latter, during the pre-Llanvirnian, possibly Precambrian, Ganderian Orogeny. The Middle Ordovician and younger Davidsville Group was derived from, and deposited unconformably on, this deformed terrain. Deformation of the Davidsville Group occurred during the Middle Devonian Acadian Orogeny.

The New Continental Line Atchison, Topeka and Santa Fe Railroad West and Southwest schedule

The New Continental Line Atchison, Topeka and Santa Fe Railroad West and Southwest schedule. The schedule is slightly torn. This does not affect the text, Sept. 4, 1881.

Geochemistry of Rare Erath Elements and Trace Metals along the Western Continental Shelf of India

Rare earth elements have occupied an important role in marine geochemical research, particularly as used in the format of REE abundance patterns to describe the geochemical pathways in marine sedimentation and authigenesis. This study concentrates on the distribution pattern of Rare earth elements in the sediments, behavior of Eu and Ce with respect to their occurrence in multiple oxidation states. It also concentrate the depth wise variation of sediment REEs from near shore areas (30m) to deeper depths 200m) in the Arabian Sea. It includes the downcore variation of REEs and other trace elements in the sediment cores and a comparison between the REE distributions of Arabian Sea sediment with the sediments of Andaman Sea. The study gives a general introduction regarding the importance of RRE studies, its occurrence and abundance, electronic configuration, lanthanide contraction, oxidations states and REE supply to the ocean, seawater and sediments.

Dynamics of Rifting Along the Southwest Continental margin of India Through Coherence and Process oriented Analysis of Gravity Data

Department of Marine Geology and Geophysics,Cochin University of Science and Technology

Marine Benthos of the Continental Shelf of Southwest and Southeast Coast of India

Department of Marine Biology,Microbiology and Biochemistry,Cochin University of Science and Technology

Geochemistry of transition, non-transition and rare-earth elements in the surficial sediments of continental shelf of Kerala and an annex to the Cochin estuarine system

The metals present in the surface sediments have high demand on a global perspective, and the main reservoir of these elements is believed to be the ocean floor. A lot of studies on metals are going on throughout the world for its quantification and exploitation. Even though, some preliminary attempts have been made in selected areas for the quantitative study of metals in the western continental shelf of India, no comprehensive work has been reported so far. The importance of this study also lies on the fact that there has not been a proper evaluation of the impact of the Great Tsunami of 2004 on the coastal areas of the south India. In View of this, an attempt has been made to address the seasonal distribution, behavior and mechanisms which control the deposition of metals in the sediments of the western continental shelf and Cochin Estuary, an annex to this coastal marine region.Surface sediment samples were collected seasonally from two subenvironemnts of southwest coast of India, (continental shelf of Kerala and Cochin estuarine system), to estimate the seasonal distribution and geochemical behavior of non-transition, transition, rare-earth elements, Th and U. Bottom water samples were also taken from each station, and analysed for temperature, salinity and dissolved oxygen, hence the response of redox sensitive elements to oxygen minimum zone can be addressed. In addition, other sedimentary parameters such as sand, silt, clay fractions, CaCO3 and organic carbon content were also estimated to evaluate the control factors on level of metals present in the sediment. The study used different environmental data analysis techniques to evaluate the distribution and behavior of elements during different seasons. This includes environmental parameters such as elemental normalisation, enrichment factor, element excess, cerium and europium anomalies and authigenic uranium.

Heterotrophic bacteria from the continental slope sediments of arabian sea

The marine environment is indubitably the largest contiguous habitat on Earth. Because of its vast volume and area, the influence of the world ocean on global climate is profound and plays an important role in human welfare and destiny. The marine environment encompasses several habitats, from the sea surface layer down through the bulk water column, which extends >10,000 meters depth, and further down to the habitats on and under the sea floor. Compared to surface habitats, which have relatively high kinetic energy, deep-ocean circulation is very sluggish. By comparison, life in the deep sea is characterized by a relatively constant physical and chemical environment. Deep water occupying the world ocean basin is a potential natural resource based on its properties such as low temperature, high pressure and relatively unexplored properties. So, a judicious assessment of the marine resources and its management are essential to ensure sustainable development of the country’s ocean resources. Marine sediments are complex environments that are affected by both physiological and biological factors, water movements and burrowing animals. They encompass a large extent of aggregates falling from the surface waters. In aquatic ecosystems, the flux of organic matter to the bottom sediments depend on primary productivity at the ocean surface and water depth. Over 50% of the earth’s surface is covered by deep-sea sediments that are primarily formed through the continual deposition of particles from the productive pelagic waters (Vetriani et al., 1999). These aggregates are regarded as ‘hot spots’ of microbial activity in the ocean (Simon et al., 2002). This represents a good nutritional substrate for heterotrophic bacteria and favours bacterial growth

Mineralogical And Sedimentological Studies Of Innershelf And Beach Sediments Along The Coast Between Paravur And Kovalam, South Kerala, India

Continental shelf is of particular significance in marine geology , because it links the two basically different structural zones in the earth's crust; the continents and ocean basins. The shelf area has much wider importance in many fields of activity such as scientific, economic, social, political and strategic. The pace of development has ultimately put pressure on mankind to look for exploitable resources and accessibility to the continental shelf area and beyond. Added to the above, the developmental activities in the coastal area would readily and directly influence the innershelf sediments. This situation demands a thorough geological knowledge of the continental shelf area. Moreover, a successful management of the continental shelf zone requires an optimum data base on the physico-chemical nature of the shelf sediments. Although sedimentological studies were carried out along the western continental shelf of India, a well documented systematic study of the inner shelf off Trivandrum coast is still found to be lacking. Considering the physiographic settings and the vicinity of two renowned placer deposits at Chavara and Manavalakurichi, such a sedimetological inventory has become all the more vital. In view of the above, a research programme has been drawn up to account the salient sedimentological and mineralogical aspects of the innershelf and beach sediments between Paravur and Kovalam, Trivandrum district, Kerala (latitudes 8° 7'00" to 8° 47'45" and longitudes 76°43'00" to 77° 40'45"). The findings are presented in six chapters formatted to address the aim of this research.

Behaviour of REEs in a tropical estuary and adjacent continental shelf of southwest coast of India: Evidence from anomalies

The distribution and accumulation of the rare earth elements (REE) in the sediments of the Cochin Estuary and adjacent continental shelf were investigated. The rare earth elements like La, Ce, Pr, Nd, Sm, Eu, Gd, Tb, Dy, Ho, Er, Tm, Yb, Lu and the heavy metals like Mg, V, Cr, Mn, Fe, Cu, Zn, U, Th were analysed by using standard analytical methods. The Post-Archean Australian Shale composition was used to normalise the rare earth elements. It was found that the sediments were more enriched with the lighter rare earth elements than the heavier ones. The positive correlation between the concentrations of REE, Fe and Mn could explain the precipitation of oxyhydroxides in the study area. The factor analysis and correlation analysis suggest common sources of origin for the REEs. From the Ce-anomalies calculated, it was found that an oxic environment predominates in all stations except the station No. 2. The Eu-anomaly gave an idea that the origin of REEs may be from the feldspar. The parameters like total organic carbon, U/Th ratio, authigenic U, Cu/Zn, V/Cr ratios revealed the oxic environment and thus the depositional behaviour of REEs in the region

El mecanismo de Desarrollo Limpio : oportunidades de Desarrollo Sostenible para Países en Desarrollo en el Protocolo de Kioto. Caso Colombia como posible potencia continental ambiental

El Cambio Climático y los Mecanismos de Desarrollo Limpio (MDL) en Colombia: Con el protocolo de Kyoto nacen los Mecanismos de Desarrollo Limpio, los cuales posibilitan a los países en desarrollo el generar cambios en los modelos de producción de las industrias altamente contaminantes por producciones limpias, obteniendo beneficios adicionales por la comercialización de los títulos de Reducciones Certificadas de las Emisiones (RCE). Nuestro país, tiene un potencial importante para fomentar el desarrollo de proyectos MDL con lo cuál puede aumentar su capacidad de negociación frente a políticas ambientales internacionales, contribuyendo al incremento del comercio exterior colombiano.

Fase Plan Exportador Continental Trade

Por medio de la metodología suministrada por el CIDEM-MALOKA, se ha elaborado un análisis integral de la compañía, junto a la proyección de tres mercados objetivos a los cuales se puede realizar una exportación efectiva, y como resultado de lo anterior, una serie de actividades que la empresa llevara a cabo para la consecución de sus objetivos tanto a corto como a largo plazo. La Metodología de plan exportador desarrollada por el CIDEM Universidad del rosario se constituye en la realización de procesos de consultoria de cada uno de los procesos productivos de la empresa, esto, con el fin de encontrar estrategias de mejoramiento y capacitación para la penetración del mercado internacional. Dicha metodología se desarrolla a partir de los siguientes componentes: Se describe inicialmente un diagnostico empresarial en el que se definen cada una de las debilidades y fortalezas de la empresa, así como las oportunidades explicitas en el entorno con el fin de realizar planes de acción determinados en las áreas de mejoramiento existentes; luego de esto, la empresa recibe consultoria particular en cada una de sus áreas productivas (descritas inicialmente en el diagnostico), de las cuales surgen nuevas estrategias orientadas a la misión y al visión de la misma pero enfocadas al entorno internacional, se describen en esta nueva fase : área productiva y administrativa y luego de mercadeo dirigida a tres países con clientes potenciales para el producto de exportación y por ultimo comercio exterior y plan exportador, en estas ultimas, cuando la empresa se encuentra preparada para penetrar los mercados internacionales, se establecen estrategias dirigidas a países en los que se encuentran los clientes potenciales de la misma con lo que la empresa logra hacer efectiva su estrategia exportadora. A partir de lo anterior, el presente documento servirá a la empresa continental Trade como una herramienta que preparara a la empresa para realizar su proceso de exportación; permitirá entonces al empresario dar cuenta de las debilidades y fortalezas respecto al funcionamiento actual, con el fin de realizar un redireccionamiento estratégico, y consecutivamente a esto, llevar a cabo su primer proyecto exportador.

Declaraci?? final del F??rum Continental sobre Educaci?? : segona cimera dels pobles d'Am??rica (Quebec, 17-18 d'abril de 2001)

Resumen tomado de la revista

Análisis de la influencia de los organismos adscritos a la organización de naciones unidas (UNICEF- ECPAT) en la solución de la problemática de la trata de niños en el sudeste asiático continental. periodo 2000-2010

La trata de niños es un fenómeno cada vez más relevante en el sistema internacional y ha generado importantes esfuerzos de cooperación de agencias internacionales como UNICEF y ECPAT. En ese sentido, ambos organismos han enfocado su actividad en las regiones donde se han registrado los mayores índices de violación de los Derechos Humanos. Este Estudio de Caso se ha centrado en el Sudeste Asiático continental conformado por Tailandia, Laos, Camboya, Vietnam, Singapur, Myanmar y Malasia; con el fin de determinar de qué manera han trabajado ambos organismos en la región y de qué forma han contribuido a la solución de esta problemática por medio de la firma de acuerdos internacionales, implementación de legislación nacional y programas de cooperación. A pesar del trabajo realizado no solo por entidades internacionales sino también por autoridades gubernamentales, no se ha observado una disminución real de las cifras.

La configuración jurídico administrativa de las universidades públicas españolas : su encuadramiento en el marco europeo continental.

Averiguar qué regimen jurídico ha de aplicarse realmente a las universidades públicas cuando la solución no viene dada expresamente por su derecho específico y determinar cuál es su naturaleza jurídica. Investigar cuál es el sistema general de distribución de competencias normativas en materia de enseñanza universitaria y cuál es el sistema particular de distribución de competencias en cada uno de los apartados fundamentales del regimen jurídico de las universidades, especialmente de los recogidos en el articulo 3.2 de la LORU. Investigar el problema de la configuración jurídico-administrativa de las universidades, examinando por periodos históricos los indicadores básicos de dicha configuración en un ente público. Trabajo realizado desde las premisas conceptuales y metodológicas del Derecho administrativo. Se investiga el derecho aplicable y la distribución de competencias normativas entre el Estado, las Comunidades Autónomas y las Universidades públicas, todo ello siguiendo un método analítico. Se indaga la naturaleza jurídica de las universidades públicas. Ello se consigue mediante el estudio de los términos con que se califica a las universidades en los textos normativos, el estudio de los autores y de los pronunciamientos jurisprudenciales. Se hace un análisis histórico, acudiendo a los autores que pueden ofrecer datos sobre los aspectos de la investigación, a los documentos históricos y a las obras doctrinales de cada época. Finalmente, del análisis obtenido en torno a cada uno de los apartados básicos, se obtienen unas conclusiones finales para cada periodo. Desde la perspectiva de la distinción de personas jurídicas públicas en entes fundacionales o institucionales, por un lado, y entes corporativos, por otro, las universidades públicas aparecen con rasgos propios de los entes institucionales, pero también con algunos otros de los corporativos, por lo que el autor considera que estamos ante una nueva categoría mixta respecto de las anteriores. No en vano es ésta también la solución a la que hay que llegar actualmente en Alemania y ésta es también la posible herencia histórica que tienen las universidades españolas actuales, respecto de la posición jurídica de las medievales y de la Edad Moderna, nunca fueron exclusivamente corporaciones, sino fundamentalmente fundaciones reales concejiles o de nobles y prelados, con derechos corporativos. Se puede asumir también que estos entes jurídico-administrativos de naturaleza mixta son, a su vez, administraciones independientes, por contar con un status autónomo frente a la acción del gobierno.