Diplodia pinea (Desm.) Kickx y Fusarium circinatum Niremberg & O'Donell, principales hongos de chancro de las masas forestales de Pinus radiata D. Don del País Vasco

228 p.

Histogénèse et structure de la glande hermaphrodite d'Helix pomatia (Linn.)

(PDF contains 267 pages)

Desarrollo de una aplicación para una red de sensores inalámbricos (WSN) mediante Contiki

Durante los últimos años hemos venido observando la tendencia a incorporar capacidad de proce- samiento y comunicación a dispositivos que hasta entonces se utilizaban de modo independiente. La evolución de los móviles a smartphones es un claro ejemplo de dicha tendencia, aunque también cabe mencionar otros ejemplos, como es el caso de los denominados hogares inteligentes, en los que elementos del hogar se encuentran interconectados y pueden actuar de modo conjunto. Esta ten- dencia no se limita a sistemas independientes, sino que propone interconectar todos los elementos disponibles para conformar la denominada Internet de los Objetos/Cosas o Internet of Things, IoT. Una de las mayores dificultades que se presenta en estos sistemas es que las características de es- tos nuevos dispositivos inteligentes, en general limitados en términos de cómputo, almacenamiento, autonomía o comunicación, queda a menudo lejos de los equipos informáticos tradicionales. Esta cuestión, junto con la ausencia de estándares para gestionar estos dispositivos, constituye un impor- tante problema a abordar. Considerando este marco, en este proyecto se ha desarrollado una aplicación orientada a este tipo de dispositivos. Más concretamente, la aplicación tiene como soporte una red de sensores inalámbricos, WSN, con el objetivo de realizar seguimiento de individuos. Cabe destacar que el desarrollo de la aplicación se ha realizado utilizando Contiki OS, sistema ope- rativo diseñado especialmente para dispositivos con características limitadas como los presentados anteriormente y firme candidato a convertirse en estándar.

Soporte a la explotación de datos y gestión de una red de sensores

El seguimiento de distintas especies de animales contribuye en gran medida a su estudio y, por tanto, a su conservación y control. Los avances tecnológicos de los últimos años han facilitado las posibilidades de seguimiento con la creación de distintos dispositivos que permiten conocer los movimientos de la especie que se desea estudiar. Uno de los sistemas más utilizados consiste en la utilización de dispositivos GPS incorporados al espécimen sobre el que se realiza el seguimiento y cuya señal es recogida por satélites que se encargan de almacenar y posteriormente reenviar la información para su almacenamiento y procesamiento en el laboratorio. El principal problema de este sistema es su elevado coste. Existen alternativas que no presentan un coste tal alto, tales como el uso de módulos basados en telefonía móvil. Sin embargo, tienen limitaciones de cobertura, por lo que no es aplicable en todos los ámbitos. Este proyecto forma parte de una propuesta que ofrece realizar seguimiento de ejemplares de una especie de ave, la gaviota Patiamarilla, en Gipuzkoa mediante la utilización de una red de sensores y que tiene varias ventajas frente a las opciones presentadas anteriormente. En este proyecto en concreto se ha diseñado e implementado el módulo que permite recoger la información obtenida por el conjunto de sensores (cada ejemplar lleva incorporado un sensor que permite registrar su posición) y enviarla a un servidor centralizado para su posterior consulta y análisis. Adicionalmente, también se permite consultar el último estado registrado de cada dispositivo de seguimiento, además de contemplar la posibilidad de actualizar su software.

^(18)O/^(16)O and D/H studies on the interactions between heated meteoric ground waters and igneous intrusions: Western San Juan Mountains, Colorado and the Isle of Skye, Scotland

Detailed oxygen, hydrogen and carbon isotope studies have been carried out on igneous and metamorphic rocks of the Stony Mountain complex, Colorado, and the Isle of Skye, Scotland, in order to better understand the problems of hydrothermal meteoric water-rock interaction.

The Tertiary Stony Mountain stock (~1.3 km in diameter), is composed of an outer diorite, a main mass of biotite gabbro, and an inner diorite. The entire complex and most of the surrounding country rocks have experienced various degrees of ¹⁸O depletion (up to 10 per mil) due to interaction with heated meteoric waters. The inner diorite apparently formed from a low-¹⁸O magma with δ¹⁸O ≃ +2.5, but most of the isotopic effects are a result of exchange between H₂O and solidified igneous rocks. The low-¹⁸O inner diorite magma was probably produced by massive assimilation and/or melting of hydrothermally altered country rocks. The δ¹⁸O values of the rocks generally increase with increasing grain size, except that quartz typically has δ¹⁸O = +6 to +8, and is more resistant to hydrothermal exchange than any other mineral studied. Based on atom % oxygen, the outer diorites, gabbros, and volcanic rocks exhibit integrated water/rock ratios of 0.3 ± 0.2, 0.15 ± 0.1, and 0.2 ± 0.1, respectively. Locally, water/rock ratios attain values greater than 1.0. Hydrogen isotopic analyses of sericites, chlorites, biotites, and amphiboles range from -117 to -150. δD in biotites varies inversely with Fe/Fe+Mg, as predicted by Suzuoki and Epstein (1974), and positively with elevation, over a range of 600 m. The calculated δD of the mid-to-late-Tertiary meteoric waters is about -100. Carbonate δ¹³C values average -5.5 (PDB), within the generally accepted range for deep-seated carbon.

Almost all the rocks within 4 km of the central Tertiary intrusive complex of Skye are depleted in ¹⁸O. Whole-rock δ¹⁸O values of basalts (-7. 1 to +8.4), Mesozoic shales (-0.6 to + 12.4), and Precambrian sandstones (-6.2 to + 10.8) systematically decrease inward towards the center of the complex. The Cuillin gabbro may have formed from a ¹⁸O-depleted magma (depleted by about 2 per mil); δ¹⁸O of plagioclase (-7.1 to + 2.5) and pyroxene (-0.5 to + 3.2) decrease outward toward the margins of the pluton. The Red Hills epigranite plutons have δ¹⁸O quartz (-2.7 to + 7.6) and feldspar (-6.7 to + 6.0) that suggest about 3/4 of the exchange took place at subsolidus temperatures; profound disequilibrium quartz-feldspar fractionations (up to 12) are characteristic. The early epigranites were intruded as low-¹⁸O melts (depletions of up to 3 per mil) with δ¹⁸O of the primary, igneous quartz decreasing progressively with time. The Southern Porphyritic Epigranite was apparently intruded as a low-¹⁸O magma with δ¹⁸O ≃ -2.6. A good correlation exists between grain size and δ¹⁸O for the unique, high-¹⁸O Beinn an Dubhaich granite which intrudes limestone having a δ¹⁸O range of +0.5 to +20.8, and δ¹³C of -4.9 to -1.0. The δD values of sericites (-104 to -107), and amphiboles, chlorites, and biotites (-105 to -128) from the igneous rocks , indicate that Eocene surface waters at Skye had δD ≃ -90. The average water/rock ratio for the Skye hydrothermal system is approximately one; at least 2000 km³ of heated meteoric waters were cycled through these rocks.

Thus these detailed isotopic studies of two widely separated areas indicate that (1) ¹⁸O-depleted magmas are commonly produced in volcanic terranes invaded by epizonal intrusions; (2) most of the ¹⁸O-depletion in such areas are a result of subsolidus exchange (particularly of feldspars); however correlation of δ¹⁸O with grain size is generally preserved only for systems that have undergone relatively minor meteoric hydrothermal exchange; (3) feldspar and calcite are the minerals mos t susceptible to oxygen isotopic exchange, whereas quartz is very resistant to oxygen isotope exchange; biotite, magnetite, and pyroxene have intermediate susceptibilities; and (4) basaltic country rocks are much more permeable to the hydrothermal convective system than shale, sandstone, or the crystalline basement complex.

Studies directed toward the synthesis of palau'amine and axinellamines A-D

The use of spiro [2.4]hepta-4,6-diene-1-methanol 7 as a general precursor for the synthesis of highly functionalized cyclopentyl rings is described. Diene 7 was converted to its silyl protected 4-nitrile derivative 24 in 46% overall yield. The cyclopropyl ring of 24 reacted with soft carbanionic nucleophiles to give ring opened homo-conjugate addition products 25a-h in 76-97% yield without loss of optical purity. The addition products could be further manipulated by selective mono-hydrogenation to give 1,2 substituted cyclopentenes 26a-e in 85-96% yield.

Diene 7 was used as a starting material for studies directed toward the synthesis of the stereochemically dense chloro-cyclopentyl core of palau'amine 1. Two advanced intermediates 50 and 72 were synthesized. Attempts to effect intramolecular chlorine transfer with 50 were unsuccessful. Attempted intramolecular chlorine transfer with 72 led, instead, to an oxygenated species resulting from oxygen radical trapping.

The enantioselective synthesis of the stereochemically dense chloro-cyclopenty l core of axinellamines A-D 2-5 starting from 7 is also described. The core is synthesized in 4.6% yield over 24 steps. Nakamura's radical dehalogenative hydroxylation is applied for the first time to a cyclopropyl carbonyl iodide to give the ring-opened product in 86% yield. Bolm's meso-anhydride desymmetrization is used to introduce asymmetry in a norbornene intermediate. The final step is a diastereoselective intermolecular chlorination using Barton's methodology to achieve chlorine transfer in 76% yield.