Physiological effects of mechanical pain stimulation at the lower back measured by functional near-infrared spectroscopy and capnography

The aim was to investigate the effect of mechanical pain stimulation at the lower back on hemodynamic and oxygenation changes in the prefrontal cortex (PFC) assessed by functional near-infrared spectroscopy (fNIRS) and on the partial pressure of end-tidal carbon dioxide ( PetCO 2) measured by capnography. 13 healthy subjects underwent three measurements (M) during pain stimulation using pressure pain threshold (PPT) at three locations, i.e., the processus spinosus at the level of L4 (M1) and the lumbar paravertebral muscles at the level of L1 on the left (M2) and the right (M3) side. Results showed that only in the M2 condition the pain stimulation elicited characteristic patterns consisting of (1) a fNIRS-derived decrease in oxy- and total hemoglobin concentration and tissue oxygen saturation, an increase in deoxy-hemoglobin concentration, (2) a decrease in the PetCO 2 response and (3) a decrease in coherence between fNIRS parameters and PetCO 2 responses in the respiratory frequency band (0.2-0.5 Hz). We discuss the comparison between M2 vs. M1 and M3, suggesting that the non-significant findings in the two latter measurements were most likely subject to effects of the different stimulated tissues, the stimulated locations and the stimulation order. We highlight that PetCO 2 is a crucial parameter for proper interpretation of fNIRS data in experimental protocols involving pain stimulation. Together, our data suggest that the combined fNIRS-capnography approach has potential for further development as pain monitoring method, such as for evaluating clinical pain treatment.

Relation between acid back -diffusion and luminal surface hydrophobicity in canine gastric mucosa: Effects of salicylate and prostaglandin

The stomach is thought to be protected from luminal acid by a gastric mucosal barrier that restricts the diffusion of acid into tissue. This study tested the hypothesis that the hydrophobic luminal surface of canine gastric mucosa incubated in Ussing chambers, impedes the back-diffusion of luminal acid into the tissue. Isolated sheets of mucosa were treated with cimetidine to inhibit spontaneous acid secretion, and incubated under conditions that prevented significant secretion of luminal bicarbonate. By measuring acid loss from the luminal compartment using the pH-stat technique, acid back-diffusion was continuously monitored; potential difference (PD) was measured as an index of tissue viability. Tissue luminal surface hydrophobicity was estimated by contact angle analysis at the end of each experiment. Addition of 16,16-dimethyl prostaglandin E$\sb2$ to the nutrient compartment enhanced luminal surface hydrophobicity, but did not reduce acid back-diffusion in tissues that maintained a constant PD. 10 mM salicylate at pH 4.00 in the luminal compartment reduced surface hydrophobicity, but this decrease did not occur if 1 ug/ml prostaglandin was present in the nutrient solution. Despite possessing relatively hydrophilic and relatively hydrophobic surface properties, respectively, acid back-diffusion in the absence of salicylate was not significantly different between these two groups. Neither group maintained a PD after incubation with salicylate. Lastly, radiolabelled salicylate was used to calculate the free (non-salicylate associated) acid loss in tissues incubated with salicylate and/or prostaglandin. No significant correlation was found between free acid back-diffusion and luminal surface hydrophobicity. These data do not support the hypothesis that acid back-diffusion in impeded by the hydrophobic surface presented by isolated canine gastric mucosa. ^

Propagación de Lecanophora heterophylla : especie nativa con potencial ornamental

En este trabajo se presentan estudios de germinación y propagación in vitro de L. heterophylla, nativa con potencial ornamental. Se evaluó el efecto del momento y lugar de recolección sobre la germinación. Se recolectaron semillas en plena floración y al final de la misma, en dos localidades de la provincia de Mendoza: Gualtallary y Chacras de Coria. Las pruebas de germinación se realizaron en estufa a 20 °C. Las semillas provenientes de Gualtallary germinaron en mayor proporción que las de Chacras de Coria: en ambas localidades la máxima germinación se obtuvo en la recolección de plena floración. Para establecer un protocolo de micropropagación se realizaron dos ensayos de introducción y uno de multiplicación. En la introducción se evaluó el medio de cultivo MS entero o ½ de macronutrientes, en combinación con BA y AIB. En la multiplicación se evaluaron los medios MS ½ o ¼ de macronutrientes con 20 o 40 g.L-1 de sacarosa. No se encontraron diferencias en la sobrevivencia, el BA incrementó significativamente la proliferación de brotes. El mejor medio de multiplicación fue MS ¼ adicionado de 20 g.L-1 de sacarosa.

Geochemistry of lavas from the Lau-Tonga arc and back-arc system

Detailed comparison of mineralogy, and major and trace geochemistry are presented for the modern Lau Basin spreading centers, the Sites 834-839 lavas, the modern Tonga-Kermadec arc volcanics, the northern Tongan boninites, and the Lau Ridge volcanics. The data clearly confirm the variations from near normal mid-ocean-ridge basalt (N-MORB) chemistries (e.g., Site 834, Central Lau Spreading Center) to strongly arc-like (e.g., Site 839, Valu Fa), the latter closely comparable to the modern arc volcanoes. Sites 835 and 836 and the East Lau Spreading Center represent transitional chemistries. Bulk compositions range from andesitic to basaltic, but lavas from Sites 834 and 836 and the Central Lau Spreading Center extend toward more silica-undersaturated compositions. The Valu Fa and modern Tonga-Kermadec arc lavas, in contrast, are dominated by basaltic andesites. The phenocryst and groundmass mineralogies show the strong arc-like affinities of the Site 839 lavas, which are also characterized by the existence of very magnesian olivines (up to Fo90-92) and Cr-rich spinels in Units 3 and 6, and highly anorthitic plagioclases in Units 2 and 9. The regional patterns of mineralogical and geochemical variations are interpreted in terms of two competing processes affecting the inferred magma sources: (1) mantle depletion processes, caused by previous melt extractions linked to backarc magmatism, and (2) enrichment in large-ion-lithophile elements, caused by a subduction contribution. A general trend of increasing depletion is inferred both eastward across the Lau Basin toward the modern arc, and northward along the Tongan (and Kermadec) Arc. Numerical modeling suggests that multistage magma extraction can explain the low abundances (relative to N-MORB) of elements such as Nb, Ta, and Ti, known to be characteristic of island arc magmas. It is further suggested that a subduction jump following prolonged slab rollback could account for the initiation of the Lau Basin opening, plausibly allowing a later influx of new mantle, as required by the recognition of a two-stage opening of the Lau Basin.

Lagrangian back-tracing results for Kohnen station; output of time dependent numerical experiment with a 3D nested Antarctic ice sheet model

A nested ice flow model was developed for eastern Dronning Maud Land to assist with the dating and interpretation of the EDML deep ice core. The model consists of a high-resolution higher-order ice dynamic flow model that was nested into a comprehensive 3-D thermomechanical model of the whole Antarctic ice sheet. As the drill site is on a flank position the calculations specifically take into account the effects of horizontal advection as deeper ice in the core originated from higher inland. First the regional velocity field and ice sheet geometry is obtained from a forward experiment over the last 8 glacial cycles. The result is subsequently employed in a Lagrangian backtracing algorithm to provide particle paths back to their time and place of deposition. The procedure directly yields the depth-age distribution, surface conditions at particle origin, and a suite of relevant parameters such as initial annual layer thickness. This paper discusses the method and the main results of the experiment, including the ice core chronology, the non-climatic corrections needed to extract the climatic part of the signal, and the thinning function. The focus is on the upper 89% of the ice core (appr. 170 kyears) as the dating below that is increasingly less robust owing to the unknown value of the geothermal heat flux. It is found that the temperature biases resulting from variations of surface elevation are up to half of the magnitude of the climatic changes themselves.

Isotopic composition of rocks from the Lau/Tonga back-arc basin, data of DSDP Leg 21 and ODP Legs 91 an 135

New trace element, Sr-, Nd-, Pb- and Hf isotope data provide insights into the evolution of the Tonga-Lau Basin subduction system. The involvement of two separate mantle domains, namely Pacific MORB mantle in the pre-rift and early stages of back-arc basin formation, and Indian MORB mantle in the later stages, is confirmed by these results. Contrary to models proposed in recent studies on the basis of Pb isotope and other compositional data, this change in mantle wedge character best explains the shift in the isotopic composition, particularly 143Nd/144Nd ratios, of modern Tofua Arc magmas relative to all other arc products from this region. Nevertheless, significant changes in the slab-derived flux during the evolution of the arc system are also required to explain second order variations in magma chemistry. In this region, the slab-derived flux is dominated by fluid; however, these fluids carry Pb with sediment-influenced isotopic signatures, indicating that their source is not restricted to the subducting altered mafic oceanic crust. This has been the case from the earliest magmatic activity in the arc (Eocene) until the present time, with the exception of two periods of magmatic activity recorded in samples from the Lau Islands. Both the Lau Volcanic Group, and Korobasaga Volcanic Group lavas preserve trace element and isotope evidence for a contribution from subducted sediment that was not transported as a fluid, but possibly in the form of a melt. This component shares similarities with that influencing the chemistry of the northern Tofua Arc magmas, suggesting some caution may be required in the adoption of constraints for the latter dependent upon the involvement of sediments from the Louisville Ridge. A key outcome of this study is to demonstrate that the models proposed to explain subduction zone magmatism cannot afford to ignore the small but important contributions made by the mantle wedge to the incompatible trace element inventory of arc magmas.

Pollen and macrofossils profiles and age determination from the Pittsburg Basin in the lowlands of south-central Illinois

Pollen and macrofossil evidence for the nature of the vegetation during glacial and interglacial periods in the regions south of the Wisconsinan ice margin is still very scarce. Modern opinions concerning these problems are therefore predominantly derived from geological evidence only or are extrapolated from pollen studies of late Wisconsinan deposits. Now for the first time pollen and macrofossil analyses are available from south-central Illinois covering the Holocene, the entire Wisconsinan, and most probably also Sangamonian and late Illinoian time. The cores studied came from three lakes, which originated as kettle holes in glacial drift of Illinoian age near Vandalia, Fayette County. The Wisconsinan ice sheet approached the sites from the the north to within about 60 km distance only. One of the profiles (Pittsburg Basin) probably reaches back to the late Illinoian (zone 1), which was characterized by forests with much Picea. Zone 2, most likely of Sangamonian age, represents a period of species-rich deciduous forests, which must have been similar to the ones that thrive today south and southeast of the prairie peninsula. During the entire Wisconsinan (14C dates ranging from 38,000 to 21,000 BP) thermophilous deciduous trees like Quercus, Carya, and Ulmus occurred in the region, although temporarily accompanied by tree genera with a more northerly modern distribution, such as Picea, which entered and then left south-central Illinois during the Woodfordian. Thus it is evident that arctic climatic conditions did not prevail in the lowlands of south-central Illinois (about 38°30' lat) during the Wisconsinan, even at the time of the maximum glaciation, the Woodfordian. The Wisconsinan was, however, not a period of continuous forest. The pollen assemblages of zone 3 (Altonian) indicate prairie with stands of trees, and in zone 4 the relatively abundant Artemisia pollen indicates the existence of open vegetation and stands of deciduous trees, Picea, and Pinus. True tundra may have existed north of the sites, but if so its pollen rain apparently is marked by pollen from nearby stands of trees. After the disappearance of Pinus and Picea at about 14,000 BP (estimated!), there developed a mosaic of prairies and stands of Quercus, Carya, and other deciduous tree genera (zone 5). This type of vegetation persisted until it was destroyed by cultivation during the 19th and 20th century. Major vegetational changes are not indicated in the pollen diagram for the late Wisconsinan and the Holocene. The dating of zones 1 and 2 is problematical because the sediments are beyond the14C range and because of the lack of stratigraphic evidence. The zones dated as Illinoian and Sangamonian could also represent just a Wisconsinan stadial and interstadial. This possibility, however, seems to be contradicted by the late glacial and interglacial character of the forest vegetation of that time.

Prototipo de e-store para un ecosistema y un framework de provisión de servicios

El trabajo realizado se encuentra enmarcado dentro del proyecto de I+D+I del 7o programa marco de la Comisión Europea Fi-WARE: The future Internet core platform que forma parte de la iniciativa Future Internet PPP. En concreto, se ha desarrollado la especificación de un Generic Enabler con funcionalidad de tienda virtual que de soporte a la publicación y adquisición o subscripción de aplicaciones y servicios dentro del denominado Business Framework Ecosystem (BFE), además de una implementación de referencia de este Generic Enabler (GE) que ha sido utilizada para la realización de una prueba de concepto con el objetivo de comprobar la adecuación del comportamiento de la especificación dentro del BFE. La primera tarea realizada ha consistido en un estudio de otras stores (o tiendas digitales) existentes, mirando aspectos tales como la funcionalidad proporcionada, la información mostrada de los distintos productos ofrecidos o la organización de la interfaz de usuario y la metáfora visual. Este estudio ha tenido como objetivo establecer un punto de partida desde el que empezar a analizar las distintas funcionalidades que deberá proveer el sistema.Utilizando como base el estudio anterior y las necesidades concretas de la plataforma Fi-WARE se paso a la educación de los requisitos generales del sistema en los cuales se especifica a grandes rasgos la funcionalidad que debe proveer esta tienda digital así como algunos aspectos concretos de la experiencia de usuario. Una vez definida la funcionalidad de la store se ha abordado el diseño del sistema. Para realizar este diseño se ha trabajado en dos tareas principales: La primera de estas tareas ha consistido en realizar el diseño de la arquitectura del Store GE, en el que se especifican todos los módulos que debe contener el sistema para poder satisfacer los requisitos, así como las distintas conexiones del Store GE con otros componentes del proyecto Fi-Ware y de sus interrelaciones con el resto de componentes de dicho proyecto. Esto ofrece una visión global de la ubicación del Store GE dentro de la arquitectura general del proyecto Fi-Ware. La segunda tarea ha consistido en el desarrollo de la especicación abierta (Open specication) del Store GE. Esta tarea es probablemente la más relevante de cara a cumplir con los objetivos del proyecto Fi-Ware, ya que Fi-Ware se propone como objetivo principal proporcionar las especificaciones de una plataforma tecnológica abierta para la Internet del futuro, formada por un conjunto de componentes (denominados Generic Enablers), entre los que se encuentra el Store GE. En este documento ha quedado descrito con todo detalle en que consiste el Store GE y cuales son sus APIs, sobre las que se construirán las aplicaciones de la futura Internet basadas en Fi-Ware, de manera que sea posible que cualquier empresa pueda realizar una implementación diferente a la que se está desarrollando en este proyecto (si bien ésta será su implementación de referencia). Para esta Open specication se han desarrollado un modelo de gestión de usuarios y roles, un modelo de datos, diagramas de interacción que definen todas las posibles comunicaciones de la store con otros Generic Enablers del proyecto Fi-Ware, la definición del ciclo de vida de una oferta y las APIs REST del Store GE, incluyendo el contenido de las peticiones y los tipos MIME soportados. En este punto se pudo comenzar a trabajar en la implementación de referencia del Store GE. La primera tarea ha consistido en realizar la integración con el Marketplace GE, otro de los Generic Enablers del proyecto Fi-Ware, para ello se definieron unos requisitos específicos y se realizó un diseño de bajo nivel de este móodulo seguido de la propia implementación y un conjunto exhaustivo de pruebas unitarias para comprobar su correcto funcionamiento. A continuación se pasó a realizar la integracióon con el Repository GE siguiendo los mismos pasos que con la integración con el Marketplace GE. La siguiente tarea realizada ha consistido en la realización de los móodulos necesarios para permitir crear nuevas ofertas en la implementación de referencia de Store GE incluyendo nuevamente una fase de educación de requisitos específicos, un diseño de bajo nivel, la propia implementación y una serie de pruebas unitarias. Una vez implementada la creación de nuevas ofertas, se pasó a la realización de la funcionalidad necesaria para la recuperación y visualizacion de estas ofertas así como a la realización del soporte necesario para el registro de recursos y para la vinculación de estos a determinadas ofertas, siguiendo nuevamente la metodología antes mencionada. Finalmente se ha dado el soporte para la publicación y la adquisición de ofertas. En este caso la adquisición de ofertas se ha realizado tan solo en la parte servidora de la aplicación y no se ha llegado a dar soporte a esta funcionalidad en la interfaz Web al no ser necesaria para la realización de la prueba de concepto prevista. No obstante esta funcionalidad será implementada junto con otras funcionalidades como el soporte de características sociales, ya fuera del ámbito de este Trabajo de fin de grado. Como paso previo a la realización de la prueba de concepto se ha trabajado en la plataforma Wirecloud, que es una implementación de referencia del denominado Application Mashup GE, modicando su funcionalidad para integrarla con la API de compras realizada dentro de la implementación de referencia del Store GE. La úultima tarea realizada para este Trabajo de fin de grado ha consistido por fin en la realización de la prueba de concepto del Store GE integrando su implementación de referencia con las del resto de Generic Enablers, lo cual ha permitido comprobar así el fucionamiento de la arquitectura y modelo propuestos.