Palabras pronunciadas por el Catedrático de la Universidad Politécnica de Madrid Profesor Dr. D. José Antonio Martín Pereda en el acto de investidura de Doctor "Honoris Causa" del Profesor Dr. William A. Gambling

El autor reflexiona sobre la trayectoria investigadora y académica del Dr. William A. Gambling, destacado científico dedicado al campo de las Comunicaciones Ópticas.

Predicción espacio-temporal de la irradiancia solar global a corto plazo en España mediante geoestadística y redes neuronales artificiales

El enriquecimiento del conocimiento sobre la Irradiancia Solar (IS) a nivel de superficie terrestre, así como su predicción, cobran gran interés para las Energías Renovables (ER) - Energía Solar (ES)-, y para distintas aplicaciones industriales o ecológicas. En el ámbito de las ER, el uso óptimo de la ES implica contar con datos de la IS en superficie que ayuden tanto, en la selección de emplazamientos para instalaciones de ES, como en su etapa de diseño (dimensionar la producción) y, finalmente, en su explotación. En este último caso, la observación y la predicción es útil para el mercado energético, la planificación y gestión de la energía (generadoras y operadoras del sistema eléctrico), especialmente en los nuevos contextos de las redes inteligentes de transporte. A pesar de la importancia estratégica de contar con datos de la IS, especialmente los observados por sensores de IS en superficie (los que mejor captan esta variable), estos no siempre están disponibles para los lugares de interés ni con la resolución espacial y temporal deseada. Esta limitación se une a la necesidad de disponer de predicciones a corto plazo de la IS que ayuden a la planificación y gestión de la energía. Se ha indagado y caracterizado las Redes de Estaciones Meteorológicas (REM) existentes en España que publican en internet sus observaciones, focalizando en la IS. Se han identificado 24 REM (16 gubernamentales y 8 redes voluntarios) que aglutinan 3492 estaciones, convirtiéndose éstas en las fuentes de datos meteorológicos utilizados en la tesis. Se han investigado cinco técnicas de estimación espacial de la IS en intervalos de 15 minutos para el territorio peninsular (3 técnicas geoestadísticas, una determinística y el método HelioSat2 basado en imágenes satelitales) con distintas configuraciones espaciales. Cuando el área de estudio tiene una adecuada densidad de observaciones, el mejor método identificado para estimar la IS es el Kriging con Regresión usando variables auxiliares -una de ellas la IS estimada a partir de imágenes satelitales-. De este modo es posible estimar espacialmente la IS más allá de los 25 km identificados en la bibliografía. En caso contrario, se corrobora la idoneidad de utilizar estimaciones a partir de sensores remotos cuando la densidad de observaciones no es adecuada. Se ha experimentado con el modelado de Redes Neuronales Artificiales (RNA) para la predicción a corto plazo de la IS utilizando observaciones próximas (componentes espaciales) en sus entradas y, los resultados son prometedores. Así los niveles de errores disminuyen bajo las siguientes condiciones: (1) cuando el horizonte temporal de predicción es inferior o igual a 3 horas, las estaciones vecinas que se incluyen en el modelo deben encentrarse a una distancia máxima aproximada de 55 km. Esto permite concluir que las RNA son capaces de aprender cómo afectan las condiciones meteorológicas vecinas a la predicción de la IS. ABSTRACT ABSTRACT The enrichment of knowledge about the Solar Irradiance (SI) at Earth's surface and its prediction, have a high interest for Renewable Energy (RE) - Solar Energy (SE) - and for various industrial and environmental applications. In the field of the RE, the optimal use of the SE involves having SI surface to help in the selection of sites for facilities ES, in the design stage (sizing energy production), and finally on their production. In the latter case, the observation and prediction is useful for the market, planning and management of the energy (generators and electrical system operators), especially in new contexts of smart transport networks (smartgrid). Despite the strategic importance of SI data, especially those observed by sensors of SI at surface (the ones that best measure this environmental variable), these are not always available to the sights and the spatial and temporal resolution desired. This limitation is bound to the need for short-term predictions of the SI to help planning and energy management. It has been investigated and characterized existing Networks of Weather Stations (NWS) in Spain that share its observations online, focusing on SI. 24 NWS have been identified (16 government and 8 volunteer networks) that implies 3492 stations, turning it into the sources of meteorological data used in the thesis. We have investigated five technical of spatial estimation of SI in 15 minutes to the mainland (3 geostatistical techniques and HelioSat2 a deterministic method based on satellite images) with different spatial configurations. When the study area has an adequate density of observations we identified the best method to estimate the SI is the regression kriging with auxiliary variables (one of them is the SI estimated from satellite images. Thus it is possible to spatially estimate the SI beyond the 25 km identified in the literature. Otherwise, when the density of observations is inadequate the appropriateness is using the estimates values from remote sensing. It has been experimented with Artificial Neural Networks (ANN) modeling for predicting the short-term future of the SI using observations from neighbor’s weather stations (spatial components) in their inputs, and the results are promising. The error levels decrease under the following conditions: (1) when the prediction horizon is less or equal than 3 hours the best models are the ones that include data from the neighboring stations (at a maximum distance of 55 km). It is concluded that the ANN is able to learn how weather conditions affect neighboring prediction of IS at such Spatio-temporal horizons.

An Implemented of a Real-Time Experimental Setup for Robotic Teleoperation System

The development of this work presents the implementation of an experimental platform, which will permit to investigate on a methodology for the design and analysis of a teleoperated system, considering the delay in the communication channel. The project has been developed in partnership with the laboratory of Automatic and Robotics of the Universidad Politécnica de Madrid and the Laboratory at the Centro de Tecnologías Avanzadas de Manufactura at the Pontificia Universidad Católica del Perú. The mechanical structure of the arm that is located in the remote side has been built and the electric servomechanism has been mounted to control their movement. The experimental test of the Teleoperation system has been developed. The PC104 card commands the power interface and sensors of the DC motor of each articulation of the arm. Has developed the drives for the management of the operations of the master and the slave: send/reception of position, speed, acceleration and current data through a CAN network. The programs for the interconnection through a LAN network, between the Windows Operating System and the Real-time Operating System (QNX), has been developed. The utility of the developed platform (hardware and software) has been demonstrated.

Control of a Teleoperation System by State Convergence with Variable Time Delay

In this paper, we propose a novel control scheme for bilateral teleoperation of n degree-of-freedom (DOF) nonlinear robotic systems with time-varying communication delay. We consider that the human operator contains a constant force on the local manipulator. The local and remote manipulators are coupled using state convergence control scheme. By choosing a Lyapunov-Krasovskii functional, we show that the local-remote teleoperation system is asymptotically stable. It is also shown that, in the case of reliable communication protocols, the proposed scheme guarantees that the remote manipulator tracks the delayed trajectory of the local manipulator. The time delay of communication channel is assumed to be unknown and randomly time varying, but the upper bounds of the delay interval and the derivative of the delay are assumed to be known.

Estratos arquitectónicos : conceptos, lógicas, sinopsis

La presente tesis doctoral se centra en la investigación del "estrato arquitectónico", manejando conceptos, lógicas y sinopsis como puntos organizativos, enlazados y superpuestos, que den paso a un marco propositivo que pueda ser simultáneamente articulado e independiente. Una situación que, ante nuevos desafíos, pretende ir más allá de una estricta definición de estrato o de su noción preconcebida descrita desde la superposición de diversos materiales. Todo ello a fin de revelar los diferentes perfiles del estrato y de la estratificación. Para ello, se abre y amplía el campo de estudio proyectual/procesual desdibujando los límites entre disciplinas –geología, filosofía, tecnología, arquitectura–. Y al mismo tiempo, se construye una cartografía del estrato arquitectónico asociada: a una taxonomía descriptora, a nuevas formulaciones, a pensamientos de personajes reconocibles y/o rescatados –como Rowe/Slutzky, Smithson, Parent/Virilio, Koolhaas, MVRDV, etc.–, y, por último, a nuevas lógicas proyectuales y operativas referidas al estrato, que fusionan conocimientos complejos. Unos contenidos que habitualmente no se presentan en investigaciones doctorales tradicionales –lo que permite afrontar nuevos cambios metodológicos, e imprimir un punto de partida para el desarrollo de futuras investigaciones o de otros posibles caminos emergentes–. Así, el discurso se impregna de nuevos referentes teóricos dentro de una misma mitología común (la del estrato). Un tema abordado con claves híbridas, es decir, con estudios selectivos y escritos coleccionados –analizados a partir de antecedentes encontrados y consolidados–, combinados con interpretaciones subyacentes en la arquitectura contemporánea –que pueden todavía encontrarse en fase experimental–. Una investigación que muestra la adaptación, la evolución y el cambio de la definición de "estrato arquitectónico", así como de su apariencia, utilización y aplicación a lo largo del tiempo, consecuencia de las nuevas necesidades y/o de las nuevas bases ideológicas ocasionadas por nuevos descubrimientos. Estratos arquitectónicos que dotan al espacio de profundidad –desde la bidimensionalidad– mediante la superposición de planos paralelos hacia la construcción de una nueva experiencia de estratificación fenomenológica. Estratos que generan estímulos y cambian su materialidad –de opacos a (en)tramados– creando apariencias y produciendo diversos efectos, para posteriormente exfoliarse y convertirse en estratos habitables. Estratos capturadores del espacio-tiempo, o de las dinámicas internas. Llegando incluso, con un último giro, a la era digital, donde el estrato informacional –que continua siendo independiente, autónomo y diverso, y que puede ser modificado, manipulado, suprimido o activable sin alterar el conjunto–, propicia obtener sistemas flexibles, relacionales, capaces de mutar o adaptarse, asociados a distintos niveles de organización dispositiva, que impulsan acciones y hacen emerger lógicas proyectuales. Estratos que surgen de forma elaborada o espontánea en el territorio urbano o natural (ciudad sobre ciudad, suelo sobre suelo), que se aplican extendiendo e hibridando el territorio (paisajes operativos), que son replanteados artificialmente como mecanismos edificatorios según las exigencias existentes (estratos programáticos, capas especializadas), y que se implantan como capas/layers en los programas informáticos utilizados como herramientas de diseño (multicapas, sistemas de intercambio informacional). Un trabajo que se estructura de manera multicapa lo que permite recorrer la tesis como un mapa de secuencias, saltar entre estratos de información, o seleccionar lecturas según intereses de pensamiento o acción arquitectónica. En consecuencia, una investigación sobre el "estrato arquitectónico" que conecta diversas disciplinas, que recopila distintos posicionamientos teórico/prácticos –lo que implica la introducción de parámetros y datos vivos–, y afronta un posicionamiento estratégico que vuelve a poner en valor el estrato arquitectónico –partiendo de estrategias formales que se han transformado en estrategias experimentales/operativas (a medida que el entorno se ha ido complejizando), siguiendo una estrategia conceptual e intelectual contemporánea, propia y específica–. ABSTRACT This PhD thesis is based on the research of "architectural stratum" using concepts, logical and synopsis as organizational, linked and overlapping points, which give way to a proactive framework that can be articulated and independent simultaneously. A situation that, faced with new challenges, aims to go beyond a strict definition of stratum or their preconceived notion described from the superposition of different materials. All this in order to reveal the different profiles of stratum and stratification. To do this, it opens and widens the field of project/process study, blurring the boundaries between disciplines –geology, philosophy, technology, architecture–. And, at the same time, a cartography of the architectural stratum is constructed, that associates with: descriptor taxonomy, new formulations, thoughts of recognizable and/or rescued characters, –as Rowe/Slutzky, Smithson, Parent/Virilio, Koolhaas, MVRDV, etc.–, and finally, a new project and operational logics referred to stratum, which merge complex knowledge. A content not usually presented in traditional doctoral research –which can face new methodological changes, and creates a starting point for future research or other possible emerging paths–. Thus, the work is imbued with new theoretical framework within a common mythology (stratum’s myth). An issue addressed with hybrid keys, that is, with selective studies and collected writings –analyzed starting from found and consolidated backgrounds–, combined with underlying performances on contemporary architecture –which can still be in experimental phase–. A research that shows adaptation, evolution and change of the definition of "architectural stratum", as well as their appearance, use and application throughout time, result of the new requirements and/or the new ideological foundations caused by new discoveries. Architectural strata that give depth to space –from two-dimensionality– by overlapping parallel planes towards the construction of a new experience of phenomenological stratification. Strata that generate stimuli and change their materiality –from opaque to lattice– creating appearances and producing various effects, for later exfoliating and becoming habitable strata. Strata that capture space-time or internal dynamics. Even reaching, with a final twist, the digital age, where the informational stratum –which remains independent, autonomous and diverse, and can be modified, manipulated, deleted or activated without altering the whole–, contribute to obtaining flexible, relational systems, able to mutate or adapt, associated with different levels of regulatory organization, that drive actions and make emerge project logics. Strata that arise elaborately or spontaneously in urban or natural territory (city upon city, floor upon floor), which apply expanding and hybridizing the territory (operational landscapes), which are artificially restated as building mechanisms according to existing requirements (strata program, specialized layers), which are implemented as layers in the software used as design tools (multilayer, systems of informational interchange). A work that is structured in a multi-layered way, which allows explore the thesis as a sequence map, jump between layers of information, or select readings according to an interest in thought or architectural action. Therefore, an investigation into the "architectural stratum" that connects different disciplines, which collects different theoretical/practical positions –which implies the introduction of live parameters and data– and faces a strategic positioning returning to value the architectural stratum –based on formal strategies that have become experimental/operational strategies (as the environment has become more complex), following a conceptual, intellectual, contemporary, own specific strategy–.

Análisis y modelado de las oscilaciones biológicas

Desde el descubrimiento de los ritmos ultradianos (Halberg 1967) en el estudio de las etapas de sueño humano (Dement y Kleitman, 1957) , muchos investigadores han dado cuenta de la existencia de estas oscilaciones en varias funciones de conducta, emocionales o fisiológicas. Si anteriormente predominó la idea de que los ritmos ultradianos tenían lugar únicamente durante el sueño, el descubrimiento de las oscilaciones en estado insomne (Weltzman et al, 1.970) y su persistencia en diferentes funciones bajo el efecto de inhibición de la droga (estados REM, Baekeland, 1967), han demostrado que persiste el mismo ciclo en el sueño que en estado insomne (Kleitman, 1969) que conduce y controla simultáneamente diferentes parámetros biológicos. Basado en este principio y a partir de nuestras estimaciones estadísticas de oscilaciones en el rango de 70-250 minutos de periodo en la actividad locomotora de diferentes especies; un mecanismo básico de desencadenamiento de los ritmos ultradianos por sincronizantes externos y su sincronización coherente con las oscilaciones circadianas (a través de acoplamientos mutuos o jerárquicos); presentamos un modelo matemático que simula el sistema oscilatorio de comportamiento ultradiano-circadiano producido por una secuencia bien definida luz-oscuridad. El modelo se basa en una topología de círculo límite (representada en un espacio bidimensional de estados) con control paramétrico producido por las transiciones luz—oscuridad y viceversa, siendo el efecto paramétrico dependiente de la fase endógena del sistema cuando se aplica las transiciones.

Disfacilitation and active inhibition in the neocortex during the natural sleep-wake cycle: An intracellular study

Earlier extracellular recordings during natural sleep have shown that, during slow-wave sleep (SWS), neocortical neurons display long-lasting periods of silence, whereas they are tonically active and discharge at higher rates during waking and sleep with rapid eye movements (REMs). We analyzed the nature of long-lasting periods of neuronal silence in SWS and the changes in firing rates related to ocular movements during REM sleep and waking using intracellular recordings from electrophysiologically identified neocortical neurons in nonanesthetized and nonparalyzed cats. We found that the silent periods during SWS are associated with neuronal hyperpolarizations, which are due to a mixture of K+ currents and disfacilitation processes. Conventional fast-spiking neurons (presumably local inhibitory interneurons) increased their firing rates during REMs and eye movements in waking. During REMs, the firing rates of regular-spiking neurons from associative areas decreased and intracellular traces revealed numerous, short-lasting, low-amplitude inhibitory postsynaptic potentials (IPSPs), that were reversed after intracellular chloride infusion. In awake cats, regular-spiking neurons could either increase or decrease their firing rates during eye movements. The short-lasting IPSPs associated with eye movements were still present in waking; they preceded the spikes and affected their timing. We propose that there are two different forms of firing rate control: disfacilitation induces long-lasting periods of silence that occur spontaneously during SWS, whereas active inhibition, consisting of low-amplitude, short-lasting IPSPs, is prevalent during REMs and precisely controls the timing of action potentials in waking.

Sleep modifies retinal ganglion cell responses in the normal rat

Recordings were obtained from the visual system of rats as they cycled normally between waking (W), slow-wave sleep (SWS), and rapid eye movement (REM) sleep. Responses to flashes delivered by a light-emitting diode attached permanently to the skull were recorded through electrodes implanted on the cornea, in the chiasm, and on the cortex. The chiasm response reveals the temporal order in which the activated ganglion cell population exits the eyeball; as reported, this triphasic event is invariably short in latency (5–10 ms) and around 300 ms in duration, called the histogram. Here we describe the differences in the histograms recorded during W, SWS, and REM. SWS histograms are always larger than W histograms, and an REM histogram can resemble either. In other words, the optic nerve response to a given stimulus is labile; its configuration depends on whether the rat is asleep or awake. We link this physiological information with the anatomical fact that the brain dorsal raphe region, which is known to have a sleep regulatory role, sends fibers to the rat retina and receives fibers from it. At the cortical electrode, the visual cortical response amplitudes also vary, being largest during SWS. This well known phenomenon often is explained by changes taking place at the thalamic level. However, in the rat, the labile cortical response covaries with the labile optic nerve response, which suggests the cortical response enhancement during SWS is determined more by what happens in the retina than by what happens in the thalamus.

Diazepam-induced changes in sleep: Role of the α1 GABAA receptor subtype

Ligands acting at the benzodiazepine (BZ) site of γ-aminobutyric acid type A (GABAA) receptors currently are the most widely used hypnotics. BZs such as diazepam (Dz) potentiate GABAA receptor activation. To determine the GABAA receptor subtypes that mediate the hypnotic action of Dz wild-type mice and mice that harbor Dz-insensitive α1 GABAA receptors [α1 (H101R) mice] were compared. Sleep latency and the amount of sleep after Dz treatment were not affected by the point mutation. An initial reduction of rapid eye movement (REM) sleep also occurred equally in both genotypes. Furthermore, the Dz-induced changes in the sleep and waking electroencephalogram (EEG) spectra, the increase in power density above 21 Hz in non-REM sleep and waking, and the suppression of slow-wave activity (SWA; EEG power in the 0.75- to 4.0-Hz band) in non-REM sleep were present in both genotypes. Surprisingly, these effects were even more pronounced in α1(H101R) mice and sleep continuity was enhanced by Dz only in the mutants. Interestingly, Dz did not affect the initial surge of SWA at the transitions to sleep, indicating that the SWA-generating mechanisms are not impaired by the BZ. We conclude that the REM sleep inhibiting action of Dz and its effect on the EEG spectra in sleep and waking are mediated by GABAA receptors other than α1, i.e., α2, α3, or α5 GABAA receptors. Because α1 GABAA receptors mediate the sedative action of Dz, our results provide evidence that the hypnotic effect of Dz and its EEG “fingerprint” can be dissociated from its sedative action.

Composition of bottom sediments from the anoxic Mogil'noe Lake, Kil'din Island (Barents Sea)

In summer 2006 integrated geological, geochemical, hydrological, and hydrochemical studies were carried out in the relict anoxic Mogil'noe Lake (down to 16 m depths) located in the Kil'din Island in the Barents Sea. Chemical and grain size compositions of bottom sediments from the lake (permanently anoxic basin) and from the Baltic Sea deeps (periodically anoxic basins) were compared. Vertical location of the hydrogen sulfide layer boundary in the lake (9-11 m depths) was practically the same from 1974 up to now. Concentrations of suspended matter in the lake in June and July 2006 appeared to be close to its summer concentrations in seawater of the open Baltic Sea. Muds from the Mogil'noe Lake compared to those of the Baltic Sea deeps are characterized by fluid and flake consistency and by pronounced admixtures of sandy and silty fractions (probably of eolic origin). Lacustrine mud contains much plant remains; iron sulfides and vivianite were also found. Concentrations of 22 elements determined in lacustrine bottom sediments were of the same levels as those found here 33 years ago. Concentrations also appeared to be close to those in corresponding grain size types of bottom sediments in the Baltic Sea. Low C_org/N values (aver. 5.0) in muds of the Mogil'noe Lake compared to ones for muds of the Baltic Sea deeps (aver. 10) evidence considerable planktogenic component in organic matter composition of the lacustrine muds. No indications were reveled for anthropogenic contaminations of the lacustrine bottom sediments with toxic metals.

Rock magnetic records and geochemical methods of sediment cores off NW Africa

Two gravity cores retrieved off NW Africa at the border of arid and subtropical environments (GeoB 13602-1 and GeoB 13601-4) were analyzed to extract records of Late Quaternary climate change and sediment export. We apply End Member (EM) unmixing to 350 acquisition curves of isothermal remanent magnetization (IRM). Our approach enables to discriminate rock magnetic signatures of aeolian and fluvial material, to determine biomineralization and reductive diagenesis. Based on the occurrence of pedogenically formed magnetic minerals in the fluvial and aeolian EMs, we can infer that goethite formed in favor to hematite in more humid climate zones. The diagenetic EM dominates in the lower parts of the cores and within a thin near-surface layer probably representing the modern Fe**2+/Fe**3+ redox boundary. Up to 60% of the IRM signal is allocated to a biogenic EM underlining the importance of bacterial magnetite even in siliciclastic sediments. Magnetosomes are found well preserved over most of the record, indicating suboxic conditions. Temporal variations of the aeolian and fluvial EMs appear to faithfully reproduce and support trends of dry and humid conditions on the continent. The proportion of aeolian to fluvial material was dramatically higher during Heinrich Stadials, especially during Heinrich Stadial 1. Dust export from the Arabian-Asian corridor appears to vary contemporaneous to increased dust fluxes on the continental margin of NW Africa emphasizing that melt-water discharge in the North Atlantic had an enormous impact on atmospheric dynamics.

Mineral and foraminifer composition of sediments across the Paleocene/Eocene Thermal Maximum from ODP Leg 198 sites

The Paleocene/Eocene Thermal Maximum (PETM) was a transient interval of global warming ~55 m.y. ago associated with transformation of ecosystems and changes in carbon cycling. The event was caused by the input of massive amounts of CO2 or CH4 to the ocean-atmosphere system. Rapid shoaling of the lysocline and calcite compensation depth (CCD) is a predicted response of CO2 or CH4 input; however, the extent of this shoaling is poorly constrained. Investigation of Ocean Drilling Program (ODP) Sites 1209-1212 at Shatsky Rise, which lies along a depth transect, suggests a minimum lysocline shoaling of ~500 m in the tropical Pacific Ocean during the PETM. The sites also show evidence of CaCO3 dissolution within the sediment column, carbonate "burn-down" below the level of the carbon isotope excursion, and a predicted response to a rapid change in deepwater carbonate saturation. Close examination of several foraminiferal preservation proxies (i.e., fragmentation, benthic/planktonic foraminiferal ratios, coarse fraction, and CaCO3 content) and observations of foraminifers reveal that increased fragmentation levels most reliably predict intervals with visually impoverished foraminiferal preservation as a result of dissolution. Low CaCO3 content and high benthic/planktonic ratios also mirror intervals of poorest preservation.

Grain counts and relative abundances of volcaniclastic sands and sandstones of ODP Leg 180 sites

Modal analysis of middle Miocene to Pleistocene volcaniclastic sands and sandstones recovered from Sites 1108, 1109, 1118, 1112, 1115, 1116, and 1114 within the Woodlark Basin during Leg 180 of the Ocean Drilling Program indicates a complex source history for sand-sized detritus deposited within the basin. Volcaniclastic detritus (i.e., feldspar, ferromagnesian minerals, and volcanic rock fragments) varies substantially throughout the Woodlark Basin. Miocene sandstones of the inferred Trobriand forearc succession contain mafic and subordinate silicic volcanic grains, probably derived from the contemporary Trobriand arc. During the late Miocene, the Trobriand outerarc/forearc (including Paleogene ophiolitic rocks) was subaerially exposed and eroded, yielding sandstones of dominantly mafic composition. Rift-related extension during the late Miocene-late Pliocene led to a transition from terrestrial to neritic and finally bathyal deposition. The sandstones deposited during this period are composed dominantly of silicic volcanic detritus, probably derived from the Amphlett Islands and surrounding areas where volcanic rocks of Pliocene-Pleistocene age occur. During this time terrigenous and metamorphic detritus derived from the Papua New Guinea mainland reached the single turbiditic Woodlark rift basin (or several subbasins) as fine-grained sediments. At Sites 1108, 1109, 1118, 1116, and 1114, serpentinite and metamorphic grains (schist and gneiss) appear as detritus in sandstones younger than ~3 Ma. This is thought to reflect a major pulse of rifting that resulted in the deepening of the Woodlark rift basin and the prevention of terrigenous and metamorphic detritus from reaching the northern rift margin (Site 1115). The Paleogene Papuan ophiolite belt and the Owen Stanley metamorphics were unroofed as the southern margin of the rift was exhumed (e.g., Moresby Seamount) and, in places, subaerially exposed (e.g., D'Entrecasteaux Islands and onshore Cape Vogel Basin), resulting in new and more proximal sources of metamorphic, igneous, and ophiolitic detritus. Continued emergence of the Moresby Seamount during the late Pliocene-early Pleistocene bounded by a major inclined fault scarp yielded talus deposits of similar composition to the above sandstones. Upper Pliocene-Pleistocene sandstones were deposited at bathyal depths by turbidity currents and as subordinate air-fall ash. Silicic glassy (high-K calc-alkaline) volcanic fragments, probably derived from volcanic centers located in Dawson and Moresby Straits, dominated these sandstones.

Elementa recentioris philosophiae : Volumen primum [-alterum] ... ad usum scholaris juventus ... /

El V.1 se divide en cinco partes: Historiae philosophiae epitome. - Elementorum recentioris philosophiae pars I. Elementa logices. - Elementorum recentioris philosophiae pars altera. Elementa methaphysices. - Elementorum recentioris philosophiae pars III. Ethices elementa. - Elementorum geometriae, quae ad rem physicam plurimum adtinet, epitome.

Observationes philologico-exegeticae in quinque Mosis libros aliosque libros historicos Veteris Testamenti : quibus praesertim verus & analogus temporum & modorum usus variis in lociis indagatur ... /

Mode of access: Internet.