Palynology and radiocarbon dating on sediment profile PG1756 from Lake Billyakh, NE Siberia, Russia

In this study a radiocarbon-dated pollen record from Lake Billyakh (65°17'N, 126°47'E; 340 m a.s.l.) in the Verkhoyansk Mountains was used to reconstruct vegetation and climate change since about 15 kyr BP (1 kyr=1000 cal. yr). The pollen record and pollen-based biome reconstruction suggest that open cool steppe and grass and sedge tundra communities with Poaceae, Cyperaceae, Artemisia, Chenopodiaceae, Caryophyllaceae and Selaginella rupestris dominated the area from 15 to 13.5 kyr BP. On the other hand, the constant presence of Larix pollen in quantities comparable to today's values points to the constant presence of boreal deciduous conifer trees in the regional vegetation during the last glaciation. A major spread of shrub tundra communities, including birch (Betula sect. Nanae), alder (Duschekia fruticosa) and willow (Salix) species, is dated to 13.5-12.7 kyr BP, indicating a noticeable increase in precipitation toward the end of the last glaciation, particularly during the Allerød Interstadial. Between 12.7 and 11.4 kyr BP pollen percentages of herbaceous taxa rapidly increased, whereas shrub taxa percentages decreased, suggesting strengthening of the steppe communities associated with the relatively cold and dry Younger Dryas Stadial. However, the pollen data in hand indicate that Younger Dryas climate was less severe than the climate during the earlier interval from 15 to 13.5 kyr BP. The onset of the Holocene is marked in the pollen record by the highest values of shrub and lowest values of herbaceous taxa, suggesting a return of warmer and wetter conditions after 11.4 kyr BP. Percentages of tree taxa increase gradually and reach maximum values after 7 kyr BP, reflecting the spread of boreal cold deciduous and taiga forests in the region. An interval between 7 and 2 kyr BP is noticeable for the highest percentages of Scots spine (Pinus subgen. Diploxylon), spruce (Picea) and fir (Abies) pollen, indicating mid-Holocene spread of boreal forest communities in response to climate amelioration and degradation of the permafrost layer.

Notas a una estética del olvido

La literatura no se ha mantenido indiferente respecto de sucesos que han dejado marcas en la historia de las sociedades, particularmente aquellos concebidos como traumáticos. Tradicionalmente, las narraciones suscitadas por ellos se sustentan en el trabajo con la memoria y delinean un sujeto que asume el estatuto de testigo narrador. En este marco, ¿resulta factible pensar relatos que se funden en el olvido? Si así lo fuera, ¿qué tipo de sujeto propondrían? Tales cuestiones invitan a pensar y discutir una estética del olvido. Esta estética torna evidentes las limitaciones del lenguaje para abordarlo como objeto y confieren a quien narra una subjetividad diferenciada del sujeto de la memoria, por la cual no intenta superar aquellas dificultades sino que las asume, las expone y las explora. La estética del olvido propone una lectura alternativa a la que lo opone, sin mayores contemplaciones, a la memoria -antinomia en la que el primero de los términos se reviste una valoración negativa-. De mismo modo que autores como Huyssen (2001) y Ric?ur (2004) rescatan las dimensiones políticas y éticas del olvido como elemento constitutivo de la memoria, es posible distinguir en él cierta fertilidad estética que posibilite el surgimiento de un ars oblivionalis

Notas a una estética del olvido

La literatura no se ha mantenido indiferente respecto de sucesos que han dejado marcas en la historia de las sociedades, particularmente aquellos concebidos como traumáticos. Tradicionalmente, las narraciones suscitadas por ellos se sustentan en el trabajo con la memoria y delinean un sujeto que asume el estatuto de testigo narrador. En este marco, ¿resulta factible pensar relatos que se funden en el olvido? Si así lo fuera, ¿qué tipo de sujeto propondrían? Tales cuestiones invitan a pensar y discutir una estética del olvido. Esta estética torna evidentes las limitaciones del lenguaje para abordarlo como objeto y confieren a quien narra una subjetividad diferenciada del sujeto de la memoria, por la cual no intenta superar aquellas dificultades sino que las asume, las expone y las explora. La estética del olvido propone una lectura alternativa a la que lo opone, sin mayores contemplaciones, a la memoria -antinomia en la que el primero de los términos se reviste una valoración negativa-. De mismo modo que autores como Huyssen (2001) y Ric?ur (2004) rescatan las dimensiones políticas y éticas del olvido como elemento constitutivo de la memoria, es posible distinguir en él cierta fertilidad estética que posibilite el surgimiento de un ars oblivionalis

Notas a una estética del olvido

La literatura no se ha mantenido indiferente respecto de sucesos que han dejado marcas en la historia de las sociedades, particularmente aquellos concebidos como traumáticos. Tradicionalmente, las narraciones suscitadas por ellos se sustentan en el trabajo con la memoria y delinean un sujeto que asume el estatuto de testigo narrador. En este marco, ¿resulta factible pensar relatos que se funden en el olvido? Si así lo fuera, ¿qué tipo de sujeto propondrían? Tales cuestiones invitan a pensar y discutir una estética del olvido. Esta estética torna evidentes las limitaciones del lenguaje para abordarlo como objeto y confieren a quien narra una subjetividad diferenciada del sujeto de la memoria, por la cual no intenta superar aquellas dificultades sino que las asume, las expone y las explora. La estética del olvido propone una lectura alternativa a la que lo opone, sin mayores contemplaciones, a la memoria -antinomia en la que el primero de los términos se reviste una valoración negativa-. De mismo modo que autores como Huyssen (2001) y Ric?ur (2004) rescatan las dimensiones políticas y éticas del olvido como elemento constitutivo de la memoria, es posible distinguir en él cierta fertilidad estética que posibilite el surgimiento de un ars oblivionalis

Palynological and geochemical data of sediment core GeoB3910-2 located offshore Northeast Brazil

High resolution palynological and geochemical data of sediment core GeoB 3910-2 (located offshore Northeast Brazil) spanning the period between 19 600 and 14 500 calibrated year bp (19.6-14.5 ka) show a land-cover change in the catchment area of local rivers in two steps related to changes in precipitation associated with Heinrich Event 1 (H1 stadial). At the end of the last glacial maximum, the landscape in semi-arid Northeast Brazil was dominated by a very dry type of caatinga vegetation, mainly composed of grasslands with some herbs and shrubs. After 18 ka, considerably more humid conditions are suggested by changes in the vegetation and by Corg and C/N data indicative of fluvial erosion. The caatinga became wetter and along lakes and rivers, sedges and gallery forest expanded. The most humid period was recorded between 16.5 and 15 ka, when humid gallery (and floodplain) forest and even small patches of mountainous Atlantic rain forest occurred together with dry forest, the latter being considered as a rather lush type of caatinga vegetation. During this humid phase erosion decreased as less lithogenic material and more organic terrestrial material were deposited on the continental slope of northern Brazil. After 15 ka arid conditions returned. During the humid second phase of the H1 stadial, a rich variety of landscapes existed in Northeast Brazil and during the drier periods small pockets of forest could probably survive in favorable spots, which would have increased the resilience of the forest to climate change.

Pollen distribution in marine sediment samples along the south-western African coast

The distribution of pollen in marine sediments is used to reconstruct pathways of terrigenous input to the oceans and provides a record of vegetation change on adjacent continents. The wind transport routes of aeolian pollen is comprehensively illustrated by clusters of trajectories. Isobaric, 4-day backward trajectories are calculated using the modelled wind-field of ECHAM3, and are clustered on a seasonal basis to estimate the main pathways of aeolian particles to sites of marine cores in the south-eastern Atlantic. Trajectories and clusters based on the modelled wind-field of the Last Glacial Maximum hardly differ from those of the present-day. Trajectory clusters show three regional, and two seasonal patterns, determining the pathways of aeolian pollen transport into the south-eastern Atlantic ocean. Mainly, transport out of the continent occurs during austral fall and winter, when easterly and south-easterly winds prevail. South of 25°S, winds blow mostly from the west and southwest, and aeolian terrestrial input is very low. Generally, a good latitudinal correspondence exists between the distribution patterns of pollen in marine surface sediments and the occurrence of the source plants on the adjacent continent. The northern Angola Basin receives pollen and spores from the Congolian and Zambezian forests mainly through river discharge. The Zambezian vegetation zone is the main source area for wind-blown pollen in sediments of the Angola Basin, while the semi-desert and desert areas are the main sources for pollen in sediments of the Walvis Basin and on the Walvis Ridge. A transect of six marine pollen records along the south-western African coast indicates considerable changes in the vegetation of southern Africa between glacial and interglacial periods. Important changes in the vegetation are the decline of forests in equatorial Africa and the north of southern Africa and a northward shift of winter rain vegetation along the western escarpment.

Pollen analysis and age model of sediment core GIK-15856-2

Pollen and spores from a deep-sea core located west of the Niger Delta record an uninterrupted area of lowland rain forest in West Africa from Guinea to Cameroon during the last Interglacial and the early Holocene. During other periods of the last 150 ka, a savanna corridor between the western - Guinean - and the eastern - Congolian - part of the African lowland rain forest existed. This so-called Dahomey Gap had its largest extension during Glacial Stages 6, 4, 3, and 2. Reduced surface salinity in the eastern Gulf of Guinea as recorded by dinoflagellate cysts indicates sufficient precipitation for extensive forest growth during Stages 5 and 1. The large modern extension of dry forest and savanna in West Africa cannot be solely explained by climatic factors. Mangrove expansion in and west of the Niger Delta was largest during the phases of sea-level rise of Stages 5 and 1. During Stages 6, 4, 3, and 2, shelf areas were exposed and the area of the mangrove swamps was minimal.

On the Closure of the Tame Automorphism Group of Affine Three-Space

We provide explicit families of tame automorphisms of the complex affine three-space which degenerate to wild automorphisms. This shows that the tame subgroup of the group of polynomial automorphisms of C3 is not closed, when the latter is seen as an infinite-dimensional algebraic group.

Results of n-alkane biomarker analyses and paleoclimate reconstruction

The current study presents quantitative reconstructions of tree cover, annual precipitation and mean July temperature derived from the pollen record from Lake Billyakh (65°17'N, 126°47'E, 340 m above sea level) spanning the last ca. 50 kyr. The reconstruction of tree cover suggests presence of woody plants through the entire analyzed time interval, although trees played only a minor role in the vegetation around Lake Billyakh prior to 14 kyr BP (<5%). This result corroborates low percentages of tree pollen and low scores of the cold deciduous forest biome in the PG1755 record from Lake Billyakh. The reconstructed values of the mean temperature of the warmest month ~8-10 °C do not support larch forest or woodland around Lake Billyakh during the coldest phase of the last glacial between ~32 and ~15 kyr BP. However, modern cases from northern Siberia, ca. 750 km north of Lake Billyakh, demonstrate that individual larch plants can grow within shrub and grass tundra landscape in very low mean July temperatures of about 8 °C. This makes plausible our hypothesis that the western and southern foreland of the Verkhoyansk Mountains could provide enough moist and warm microhabitats and allow individual larch specimens to survive climatic extremes of the last glacial. Reconstructed mean values of precipitation are about 270 mm/yr during the last glacial interval. This value is almost 100 mm higher than modern averages reported for the extreme-continental north-eastern Siberia east of Lake Billyakh, where larch-dominated cold deciduous forest grows at present. This suggests that last glacial environments around Lake Billyakh were never too dry for larch to grow and that the summer warmth was the main factor, which limited tree growth during the last glacial interval. The n-alkane analysis of the Siberian plants presented in this study demonstrates rather complex alkane distribution patterns, which challenge the interpretation of the fossil records. In particular, extremely low n-alkane concentrations in the leaves of local coniferous trees and shrubs suggest that their contribution to the litter and therefore to the fossil lake sediments might be not high enough for tracing the Quaternary history of the needleleaved taxa using the n-alkane biomarker method.

Case Study of Applied LIP Approach/Activities in the Philippines The Training Services Enhancement Project for Rural Life Improvement (TSEP-RLI) Experience

TSEP-RLI was a technical cooperation project jointly conducted by GOP thru DA-Agricultural Training Institute (ATI) and GOJ thru JICA aimed at institutionalizing the training program for Rural Life Improvement (RLI) at the (ATI). As expected, farmers, fisherfolk, women, youth and extension agents were provided with efficient and effective training services from ATI leading to the improvement of quality of life in the rural areas through efforts of human resource development. The ATI- Bohol was chosen as the model center where participatory trials and various activities of the project were undertaken for five years. These activities were participatory surveys and data collection of on-farm and off-farm productive activities; planning workshop for RLI; feedbacking of survey results and action plans to the community and the Local Government Units (LGUs), and signing of Memorandum of Agreement between the Project and participating LGUs. The above activities were done to facilitate the planning and development of most effective and necessary rural life improvement activities, to confirm the willingness of the people to support and participate and to formalize the partnership between the Project and the LGUs. Since the concept of rural life covers a vast range of activities, a consensus had been reached that the total aspects of rural life be grasped in three spheres, namely, Production & Livelihood (P/L), Rural Living Condition (RLC) and Community Environment (C/E). The RLI for Ubi (Yam) Growers was one of the pilot activities undertaken in two pilot barangays and the target beneficiaries were members of the Rural Improvement Club (RIC- a group of organized women) with the LGU of the Municipality of Corella as the implementing partner. During the planning workshop, the barangay residents articulated their desire to promote production and processing of ubi (sphere on P/L - as the entry point), lack of nutritious food was one of the identified problem (sphere on RLC- expansion point) and environmental degradation such as deforestation, and soil erosion was another problem articulated by the community people (sphere on C/E- expansion point). Major activities that were undertaken namely, Ubi cooking contest, cooking/processing seminar, training courses on entrepreneurial development, ubi production and storage technology, packaging and product design, human resource development and simplified bookkeeping motivated the beneficiaries as well as developed and enhanced their skills & capabilities while strengthening their associations. Their participation to the 5 ubi festivals and other related activities had brought some impacts on their economic and rural life improvement activities. The seven principles of TSEP-RLI include the participatory process, holistic approach, dialogical approach, bottom -up training needs assessment, demand-driven approach, cost sharing approach and collaborative implementation with other agencies including LGUs and the community.

Criterios para el refuerzo de estructuras metálicas: rehabilitación del 'Circulo de Bellas Artes' y la 'Casa Encendida'

REHABILITACION DEL 'CIRCULO DE BELLAS ARTES' Y LA 'CASA ENCENDIDA'

Estudio del estado de la vegetación de ribera en la España peninsular. Implicaciones de la alteración hidrológica y herramientas para su manejo y gestión

El objetivo general de este trabajo es explorar las potenciales interacciones entre la alteración hidrológica y el estado de la vegetación de ribera en diversas cuencas hidrográficas españolas. La mayor parte del área de estudio está dentro de la región Mediterránea, una región caracterizada por un particular comportamiento climatológico, ecológico y socio-económico. Las cuencas estudiadas son: Guadiana, Guadalquivir, Tajo, y Duero. Para complementar el estudio y comparar resultados con otras regiones climáticas españolas se estudiaron dos Demarcaciones atlánticas: Cantábrico y Miño-Sil. El funcionamiento fluvial, en las áreas mediterráneas, presenta grandes variaciones en el régimen hídrico, siendo uno de los principales controladores de la estructura, composición y distribución de la vegetación de ribera. Para investigar las interacciones mencionadas previamente, se presenta un nuevo índice, Riparian Forest Evaluation (RFV). El objetivo de este índice es valorar el estado de la vegetación de ribera en base a los principales controladores hidro-morfológicos responsables de la dinámica fluvial, y por tanto, relacionados con el desarrollo del corredor ribereño. RFV divide la evaluación del bosque de ribera en cuatro componentes: continuidad longitudinal, transversal, y vertical (dimensiones espaciales), y condiciones del regenerado (dimensión temporal). La clasificación final está basada en las mismas cinco clases fijadas por la Directiva europea Marco del Agua (DMA) (2000/60/CE) para valorar el estado ecológico de las masas de agua. La aplicación de este índice en 187 masas de agua ha mostrado su facilidad de aplicación y su consistencia desde un punto de vista legislativo y técnicocientífico. En paralelo al diseño del índice RFV, se ha desarrollado una nueva herramienta para dar apoyo a la evaluación del bosque de ribera (RFV) y la extracción de variables hidromorfológicas a escala de masa de agua en lugar de a escala local (muestreo de campo local). Se trata de Riparian Characterisation by LiDAR (RiC-DAR), que permite valorar el estado del bosque de ribera de una manera semiautomática, en un modo cuasi-continuo, usando LiDAR de alta resolución. Esto hecho permite mejorar significativamente la calidad y cantidad de información comparado con la toma de datos en campo, lo que permite reducir los recursos, particularmente cuando se trabaja a escala de masas de agua. Una de las potenciales causas de la degradación del bosque de ribera es la alteración hidrológica; así una vez se ha realizado la evaluación del bosque de ribera basada en elementos hidro-morfológicos ligados al régimen hídrico (RFV), se han identificado las potenciales relaciones entre la alteración hidrológica y la degradación de la vegetación riparia. Para ello, se requiere contar con series de aforos fiables y de una duración apropiada. Para satisfacer este requerimiento, se ha creado una nueva herramienta: el Servidor de Datos para el Estudio de la Alteración Hidrológica (SEDAH). Esta herramienta genera datos diarios y mensuales completados para más años, construyendo así bases de datos más aptas para el estudio de la alteración hidrológica. (http://ambiental.cedex.es/Sedah) Haciendo uso de las herramientas y métodos desarrollados previamente, se han calculado diferentes indicadores de alteración hidrológica en 87 masas de agua que han sido analizados conjuntamente con el estado de la vegetación de ribera. Los resultados estadísticos han mostrado relaciones significativas entre ellos: la degradación de la vegetación podría estar fuertemente ligada a la alteración del régimen hídrico en años secos y a las sequías en el entorno mediterráneo. A su vez se ha analizado la relación del estado del bosque de ribera con el estado ecológico basado en la DMA, mostrando una relación no significativa. Esta y otras potenciales relaciones son discutidas a lo largo del documento. Los resultados permiten proponer recomendaciones de gestión de la vegetación de ribera y de manejo del régimen de caudales para masas de agua reguladas. ABSTRACT The general objective of this work is to explore the potential interactions between hydrologic alteration and degradation of the riparian vegetation, mainly focused in the Mediterranean Environment. The majority of the study area is part of the Spanish Mediterranean region, a geographical environment characterized by a singular climatologic, ecological and socio-economical behavior. The basins analysed in this work are: Guadiana, Guadalquivir, Tagus, Douro. In order to complete the results and compare those to other climatic regions in Spain, two Atlantic Districts where selected: Cantábrico and Miño-Sil. The river functioning, in the Mediterranean areas, presents great variations in the flow regimes being one of the main drivers of the riparian vegetation development. To explore the interactions stated above, a new index is presented, Riparian Forest Evaluation (RFV). This index is aimed to assess the status of the riparian vegetation based on the main hydromorphological drivers responsible of the river dynamic, and so, related to the development of the riparian corridor. RFV split the evaluation of the riparian forest into four components: longitudinal continuity, transversal continuity, vertical (structure) continuity and regeneration (temporal) continuity. The final classification is based in the same five classes to those stated in the European Water Frame Work directive to assess the ecological status. The application of this index over 187 water bodies has shown to be easily applicable and consistent from a regulatory perspective. In parallel to the design of RFV, a new tool has been developed to enhance the evaluation of the riparian forest and river morphology (RFV and morphological parameters) at water body scale rather than at local scale, i.e. when field surveyed at different sites. The Riparian Characterisation by LiDAR, RiC-DAR allows to assess the status of the riparian vegetation semi-automatically in a quasi-continuous way using high resolution LiDAR. This improves significantly the quantity and quality of information gathered through field sampling methods, reducing resources when working at larger scales. One of the potential major causes of degradation of the riparian forest is the hydrologic alteration; hence, once the evaluation of the riparian forest is done consistently based on hydro-morphological features linked to the hydrological regime (RVF), this work has identified potential relationships between hydrologic alteration and degradation of riparian vegetation. In order to do this, it is required to count with reliable series of flow records describing both reference and altered regimes. To satisfy this need, a new tool has been created, SEDAH, data server for assessing hydrologic alteration. This tool has completed daily and monthly gaps in the flow series to build up an improved database to assess the hydrologic alteration. This application is available on line (http://ambiental.cedex.es). Making use of the tools and methods developed previously, this work uses these data to work out indicators of hydrologic alteration through 87 water bodies to be analysed against the riparian status. These indicators are statistically analysed exploring significant relationships with the status of riparian vegetation and ecological status, showing some potential significant relationships; hence it seems that the degradation of riparian vegetation, particularly the regeneration, is associated with the alteration of the hydrologic regimen in dry years and draughts in Mediterranean environments. Furthermore, the analysis of the status of the ecological status and the status of the riparian vegetation has shown the lack of significant influence of the riparian vegetation in the final ecological status using the WFD approach applied in Spain. This and other potential relationships are discussed in this work. The results allow giving guidance on the management of both riparian vegetation and environmental flows of water bodies affected by flow regulation.

Wireless Power Transfer: Control para máxima transferencia de potencia con enlace resonante inductivo

Este trabajo forma parte del proyecto “Health aware enhanced range wireless power transfer systems”, conocido por el acrónimo de ETHER. Los grupos investigadores que forman parte de ETHER involucran a dos instituciones, Universidad Politécnica de Cataluña (UPC) y Universidad Politécnica de Madrid (UPM). En este caso, el trabajo ha sido llevado a cabo en el marco del Centro de Electrónica Industrial(CEI) de la UPM. Además, este trabajo es el tercero en una sucesión de estudios realizados por el CEI con el objetivo de lograr implementar un sistema de carga inalámbrica en un marcapasos. Los trabajos previos al desarrollado son los realizados por Miguel Gifford y María Gonzalez. Otros trabajos del CEI han servido de guía. El principal objetivo de la aplicación, es evitar las operaciones que se llevan a cabo actualmente para la sustitución de la batería de los marcapasos implantados en pacientes. Este periodo de sustitución es del orden de cuatro años, lo que depende del tipo de marcapasos y las circunstancias en las que se vea envuelto el paciente. Se pretende lograr la carga del dispositivo causando la menor molestia posible al paciente sin afectar a su salud. El sistema de carga inalámrica o WPT1, está basado en inducción magnética resonante, conocida como RIC2. Esta tecnología se fundamenta en el uso de bobinas acopladas como elemento transmisor de energía. A su vez, la impedancia de estas bobinas, es compensada mediante el uso de condensadores, obteniendo circuitos resonantes. Mediante el uso de RIC se logran mejores características técnicas para la transmisión de energía en el rango medio. Esto permite salvar la distancia entre el elemento generador y la batería del marcapasos, incluso ante la existencia de tejido orgánico entre las dos bobinas. Se han considerado dos posibilidades de configuraci´on del sistema. Dos etapas: se dispone de dos bobinas, emisora y receptora. Esta configuración supone trabajar a altas frecuencias para conseguir transferencia de energías efectivas teniendo en cuenta las especificaciones del marcapasos. Tres etapas: se dispone de tres bobinas, emisora, intermedia y receptora. Se mejora el alcance, permitiendo trabajar a menores frecuencias, pero complicando el control y la implementación del sistema. Sin embargo, el foco de los esfuerzos invertidos en este trabajo, es el estudio del sistema de optimización que se introduce en las configuraciones anteriormente descritas. La optimización se centra en conseguir máxima transferencia de potencia, quedando relegado a un segundo plano el rendimiento. Esto se justifica por las características de la aplicación donde la principal limitación es la viabilidad del sistema. Asímismo, la viabilidad viene impuesta por la potencia que consume el marcapasos y la que es capaz de suministrar el sistema. Este sistema de optimización se basa en la regulación en frecuencia y en la adaptación de la impedancia de carga. Este último método es estudiado, y se basa en lograr una impedancia de carga igual al complejo conjugado de la impedancia de salida, logrando máxima transferencia de potencia. El sistema de optimización hace uso de varias estructuras de control de electrónica de potencia. Inversor: Se sitúa en la etapa emisora y permite controlar la frecuencia de trabajo del sistema. Rectificador activo: Se sitúa en la etapa receptora y controla el desfase entre intensidad y tensión. Convertidor CC-CC: Se sitúa en la etapa receptora, tras el rectificador. Controla la amplitud de la tensión.Mediante el uso conjunto del rectificador y el convertidor es posible controlar la impedancia de la carga. Se ha realizado un análisis teórico para determinar el punto de funcionamiento óptimo del sistema, y posteriormente, se han validado estos resultados mediante simulaciones. Se demuestra que la potencia transferida por el sistema WTP se multiplica por cinco respecto de la solución original, es decir, en ausencia del sistema de optimización. Además se logra mayor robustez, ya que el control activo del sistema proporciona mayor adaptabilidad ante condiciones alejadas de las de diseño. El trabajo realizado se ha prolongado durante un periodo de doscientos días efectivos con una dedicación de 360 horas de trabajo. El coste total asignado al desempeño del trabajo es de 16.678,94 euros.

A genetic selection for Caenorhabditis elegans synaptic transmission mutants.

We have isolated 165 Caenorhabditis elegans mutants, representing 21 genes, that are resistant to inhibitors of cholinesterase (Ric mutants). Since mutations in 20 of the genes appear not to affect acetylcholine reception, we suggest that reduced acetylcholine release contributes to the Ric phenotype of most Ric mutants. Mutations in 15 of the genes lead to defects in a gamma-aminobutyric acid-dependent behavior; these genes are likely to encode proteins with general, rather than cholinergic-specific, roles in synaptic transmission. Ten of the genes have been cloned. Seven encode homologs of proteins that function in the synaptic vesicle cycle: two encode cholinergic-specific proteins, while five encode general presynaptic proteins. Two other Ric genes encode homologs of G-protein signaling molecules. Our assessment of synaptic function in Ric mutants, combined with the homologies of some Ric mutants to presynaptic proteins, suggests that the analysis of Ric genes will continue to yield insights into the regulation and functioning of synapses.