Pollen records and lithology of profiles from Lobsigensee, Switzerland

Lobsigensee is a small kettle hole lake 15 km north-west of Bern on the Swiss Plateau, at an altitude of 514 m asl. Its surface is 2ha today, its maximum depth 2.7 m; it has no inlet and the overflow functions mainly during snow melting. The area was covered by Rhone ice during the Last Glaciation (map in Fig.2). Local geology, climate and vegetation are summarized in Figure 3A-C, the history of settlement in Figures 5-7. In order to reconstruct the vegetational and environmental history of the lake and its surroundings pollen analysis and other bio- and isotope stratigraphies were applied to twelve profiles cored across the basin with modified Livingstone corers (Fig.3 D). (1) The standard diagram: The central core LQ-90 is described as the standard pollen diagram (Chapter 3) with 10 local pollen assemblage zones of the Late-Glacial (local PAZ Ll to Ll0, from about 16'000(7) to 10'000 years BP) and 20 PAZ of the Holocene (local PAZ L11 to L30), see Figs. 8-10 and 20-24. Local PAZ L 1 to L3 are in the Late-Glacial clay and record the vegetational development after the ice retreat: L1 shows very low pollen concentration and high Pinus percentages due to long-distance transport and reworking; the latter mechanism is corroborated by the findings of thermophilous and pre-Quaternary taxa. Local PAZ L2 has a high di versi ty of non-arboreal pollen (NAP) and reflects the Late-Glacial steppe rich in heliophilous species. Local PAZ L3 is similar but additionally rich in Betula nana and Sal1x, thus reflecting a "shrub tundra". The PAZ L1 to L3 belong to the Oldest Dryas biozone. Local PAZ L4 to L 10 are found in the gyttja of the profundal or in the lake marl of the littoral and record the Late-Glacial forests. L4 is the shrub phase of reforestation with very high Junlperus and rapidly increasing Betula percentages. L5 is the PAZ with a first, L7 with a second dominance of tree-birches, separated by L6 showing a depression in the Betula curve. L4 to L7 can be assigned to the Balling biozone. Possible correlation of the Betula depression to the Older Dryas biozone is discussed. In local PAZ L8 Plnus immigrates and expands. L9 shows a facies difference in that Plnus dominates over Betula in littoral but not in profundal spectra. L8 and L9 belong to the Allerod biozone. In its youngest part the volcanic ash from Laach/Eifel is regularly found (11,000 BP). The local PAZ Ll0 corresponds to the Younger Dryas blozone. The merely slight increase of the NAP indicates that the pine forests of the lowland were not strongly affected by a cooler climate. In order to evaluate the significance of the littoral accumulation of coniferous pollen the littoral profile LQ-150 is compared to the profundal. Radiocarbon stratigraphies derived from different materials are presented in Figures 13 and 14 and in Tables 2 and 3. The hard-water errors in the gyttja samples and the carbonate samples are similar. The samples of terrestrial plant macrofossils are not affected by hard-water errors. Two plateaux of constant age appear in the age-depth relationship; their consequence for biostratigraphy as well as pollen concentration and influx diagrams are discussed. Radiocarbon ages of the Late-Glacial pollen zones are shown in Table 10. The Holocene vegetational history is recorded in the local PAZ L 11 to L30. After a Preboreal (PAZ L11) dominated by pine and birch the expansions of Corylus, Ulmus and Quercus are very rapid. Among these taxa Corylus dominates dur ing the Boreal (PAZ L 12 and L 1 3), whereas the components of the mixed oak forest dominate in the Older Atlantic (PAZ L14 to L16). In the Younger Atlantic (PAZ L 17 to L 19) Fagus and Alnus play an increasing, the mixed oak forest a decreasing role. During the period of local PAZ L19 Neolithic settlers lived on the shore of Lobsigensee. During the Subboreal (PAZ L20 and L21) and the Older Subatlantic (L22 to L25) strong fluctuations of Fagus and often antagonistic peaks of NAP, Alnus, Betula and Corylus can be interpreted as signs of human impact on vegetation. L23 is characterized not only by high values of NAP (especially apophytes and anthropochorous species) but also by the appearance of Juglans, Castanea and Secale which point to the Roman colonization of the area. For a certain period during the Younger Subatlantic (PAZ L26 to L30) the lake was used for retting hemp (Cannabis). Later the dominance of Quercus pollen indicates the importance of wood pastures. The youngest sediments reflect the wide-spread agricultural grass lands and the plantation of Pinus and Picea. Radiocarbon dates for the Holocene are given in Figure 23 and Table 4, the extrapolated ages of the Holocene pollen zones in Table 15. (2) The cross sections: Figures 25 and 26 give a summary of the litho- and palynostratigraphy of the two cross sections. Based on 11 Late-Glacial and 9 Holocene pollen diagrams (in addition to the standard ones), the consistency of the criteria for the definition of the pollen zones is examined in Tables 7 and 8 for the Late-Glacial and in Tables 11 to 14 for the Holocene. Sediment thicknesses across the basin for each pollen zone are presented in these tables as well as in Figures 43 to 45 for the Late-Glacial and in Figures 59 to 65 for the Holocene. Sediment focusing can explain differences between the gyttja cores of the profundal. Focusing is more than compensated for through "stretching" by carbonate precipitation on the littoral terrace. Pollen influx to the cross section are discussed (Chapters 4.1.5. and 4.2.3.). (3) The regional pollen zones: Based on some selected sites between Lake Geneva and Lake Constance regional pollen zones are proposed (Table 16, 17 and 19). (4) Paleoecology: Climatic change in the Late-Glacial can be inferred from Coleoptera, Trichoptera, Chironomidae and d18O of carbonates: a distinct warming is recorded around 12' 600 BP and around 10' 000 BP. The Younger Dryas biozone (10'700-10'000 BP) was the only cooling found in the Late-Glacial. The Betula depression often correlated wi th the Older Dryas biozone was possibl not colder but dryer than the previous period. During the Holocene the lowland site is not very sensitive to the minor climatic changes. Table 22 summarizes climatic and trophic changes before 8'000 BP as deduced from various biostratigraphies studied by a number of authors. Ostracods, Chironomids and fossil pigments indicate that anoxic conditions prevailed during the BoIling (possibly meromixis). Changes in the lake level are illustrated in Figure 74. A first lake-level lowering occurred in the early Holocene (10'000 to 9'000 BP), a second during the Atlantic (about 6'800 to 5'200 BP). The first "shrinking" of the lake volume resulted in a eutrophication recorded by laminations in the profundal and by pigments of Cyanophyceae. The second fall in water level corresponds to an increase of Nymphaeaceae. Human impact can be inferred in three ways: eutrophication of the lake (since the Neolithic), changes of terrestrial vegetation by deforestations (cyclicity of Fagus, see Figures 78 to 80), and enhanced erosion (increasing sedimentation rates by inwashed clay, particularly since the Roman Colonization, see Figures 49 and 81). Summary: This paper was planned as the final report on Lobsigensee. However, a number of issues are not answered but can only be asked more precisely, for example: (1) For the two periods with the highest rates of change, Le. the Bolling and the Preboreal biozones, pollen influx may reflect vegetation dynamics. Detailed investigations of these periods in annually laminated sediments are planned. (2) Biostratigraphies other than palynostratigraphy are needed to estimate the degree of linkage or independence in the development of terrestrial and lacustrine ecosystems. Often our sampling intervals were not identical, thus influencing our temporal resolution. (3) 6180- and 14C-stratigraPhies with high resolution will elucidate the leads and lags of these dynamic periods. Plateaux of constant age in the age-depth relationship have a strong bearing on both biological and geophysical understanding of Late-Glacial and early Holocene developments. (4) Numerical methods applied to the pollen diagrams of the cross section will help to quantify the significance of similari ties and dissimilarities across a single basin (with Prof. Birks). (5) Numerical methods applied to different sites on the Swiss Plateau and on the transect across the Alps will be helpful in evaluating the influence of different environmental factors (with Prof. Birks). (6) A new map 1: 1000 with 50cm-contour lines prov ided by Prof. Zurbuchen will be combined with a grid of cores sampling the transition from lake marl to peat enabling us to calculate paleo-volumes of the lake. This is interesting for the two "shrinking periods" (in Fig. 74A numbers 2-6 and 7-10), both accompanied by eutrophication. The pal eo-volume during the Neoli thic set tlement of the Cortaillod culture linked wi th an est l.mate of trophic change derived from diatoms (Prof. Smol in prep.) could possibly give an indication of the size of the human population of this period. (7) For the period with the antagonism between Fagus peaks and ABC-peaks close collaboration between palynologists, geochemists and archeologists should enable us to determine the influence of prehistoric and historic people on vegetation (collaboration with Prof. Stockli and Prof. Herzig). (8) The core LL-75 taken with a "cold letter box" will be analysed for major and trace elements by Dr. Sturm for 210pb and 137Cs by Prof.von Gunten and for pollen. We will see if our local PAZ L30 really corresponds to the surface sediment and if the small seepage lake reflects modern pollution.

Pollen record from Muggesfelder See and Plussee in Germany

A basaltic tephra layer consisting of brownish-olive glass shards. and about 0.2 mm thick. was found in cores from four lakes in northwest Germany. According to pollen analysis it was deposited during the early Boreal period (corresponding to about 8700 BP). The petrographic properties. the geochemical composition and the age agree with those of the Saksunarvatn tephra. which was first found on the Faroe Islands. The position of the tephra layer in the pollen stratigraphy and in the absolute time-scale is discussed. Procedures for locating the tephra in other cores are suggested.

Agaete revisited: new data on the Gran Canaria tsunamiites.

The tsunami deposits of the valley of Agaete (Pérez-Torrado et al., 2006), north-western Gran Canaria, attributed to the Guimar flank collapse in Tenerife, have been revisited and new data are presented here. Besides the occurrences reported by Pérez-Torrado et al. (2006) a new outcrop was found and named “La Ruina” (at 28º 05’ 47,41” N; 15º 41’ 52,04” W; 71 m asl). The above-mentioned authors suggested the possibility that more than one marine conglomerate deposit could be present in the outcrops of “Llanos de Turmán” and “Berrazales”. At “La Gasolinera” and “La Aldea 1” the conglomerates are formed by a single layer representing one depositional event; at “La Aldea 2”, the conglomerates are composed of two layers directly contacting with each other, but evidence of a time hiatus between them was not found. Although the hypothesis of stacking of two depositional units within the same episode versus deposition of two distinct layers in different time-moments is debatable at the present state of knowledge, the first possibility is favoured. The field evidence at “Llanos de Turman” and “Berrazales” unquestionably shows that terrestrial sediments (colluvia; paleosols) are present and separate two marine conglomerate deposits, indicating that at least two distinct tsunami inundations are needed to explain the stratigraphy. However, at the new “La Ruina” outcrop, besides the two deposits mentioned above, a third and older marine conglomerate was found, clearly separated in time from the ones cited above. The existence of marine conglomerates emplaced in different moments is evidenced by the occurrence of intercalated paleosols, colluvia and other subaerial materials, implying significant time intervals between the emplacement of marine conglomeratic layers. A number of gastropod operculae from the tsunamiites were sent for U-Th dating to try to further constrain the age span of these deposits. The field evidence presented above shows that the emplacement of the deposits is related to, at least, three tsunami events. The lateral correlation between different outcrops is difficult due to variable number of deposits in each outcrop, lateral discontinuity and variability, and to compositional and textural similarity between distinct tsunami sediments. The occurrence of three Pleistocene tsunami deposits in the same area points to a relatively high frequency of tsunamis (generated by landslides, surface rupturing earthquakes, fast entry of voluminous volcanic deposits into the sea or large submarine eruptions). It is possible that this recurrence of tsunami inundations may reflect multiple-phased landslides responsible for the mega-landslide scars prominent in the geomorphology of the neighbouring island of Tenerife. This is a contribution from project “Estabilidad de los edificios volcánicos en Canarias: análisis de los factores geológicos, geomecánicos y paleoclimáticos. Aplicación a los flancos N y S de la isla de Tenerife” financed by MCT, Spain.

Estrategias visuales y motrices de los porteros expertos de fútbol sala en tareas de intercepción bajo presión temporal y espacial

En los últimos años, la investigación se ha preocupado crecientemente sobre la anticipación visual de los deportistas en deportes de intercepción (e.g.,Van der Kamp, Rivas, Van Doorn y Savelsbergh, 2008). Estos trabajos han mostrado de forma consistente que el rendimiento de los deportistas está regulado por tres factores que interactúan. El primero, la estructura y la dinámica de la tarea estipulan los márgenes espaciales y temporales en los que actuar (e.g., Vilar, Araújo, Davids, Correia y Esteves, 2012). También, cómo los deportistas extraen y utilizan la información disponible del entorno sobre la que guiar su conducta (e.g., Savelsbergh, Williams, Van der Kamp y Ward, 2002). Y el tercero se refiere a su anticipación y tiempos de movimiento (e.g., Dicks, Davids y Button, 2010b). El objetivo del estudio fue evaluar la evolución de las estrategias visuales y motrices cuando se manipulan las demandas espacio-temporales así como la fiabilidad de la información. Para ello, se examinaron doce porteros expertos de fútbol sala in situ mientras recibían tiros de penalti en cuatro condiciones que diferían en cuanto a distancia de disparo (penaltis desde 6 m vs. dobles penaltis desde 10m) y a la estrategia de engaño del oponente (tiros normales vs. tiros conengaño). Se grabó el rendimiento y sus tiempos de movimiento utilizando una cámara de alta velocidad (120fps) y se registró su mirada mientras intentaban interceptar los disparos empleando el sistema portátil de seguimiento de la mirada ASL MobileEye. Se analizaron las medidas derivadas de los análisis de los vídeos a través de una prueba de ANOVA (Friedman o Medidas Repetidas) y se hizo un análisis discriminante para extraer las variables del rendimiento: gol vs. parada. Los porteros pararon más tiros (61% vs. 23%), obtuvieron valores de rendimiento más altos ( 4.1 vs. 2.1 sobre 5), y acertaron el lado más frecuentemente (97% vs. 53%) en los tiros de dobles penaltis comparado con los tiros de penalti. El engaño tuvo un efecto nulo en el rendimiento de los porteros, excepto para el número de correcciones entre dobles penaltis, donde corrigieron su movimiento inicial de parada hacia el otro lado en un 23% de los tiros con engaño por un 12% en los tiros normales. Los participantes iniciaron su acción de parada antes en los penaltis comparado con los dobles penalti, no encontrándose ningún efecto de la estrategia de engaño en los tiempos de movimiento. Esas diferencias entre distancias fueron notables en las medidas del tronco y de los pies (339 y 330 ms respectivamente), los cuales pasaron de valores negativos(movimiento antes del golpeo) en los penaltis, a valores positivos (movimiento después del golpeo) en los dobles penaltis. Sin embargo, los tiempos de los brazos se mantuvieron cercanos a los 200 ms en ambos tiros de penaltis y de dobles penaltis (23 ms de diferencia media). El análisis de los patrones visuales reveló una remarcable variabilidad, tanto entre participantes como intra participantes, aunque emergió un patrón general. Los porteros tendieron a mirar hacia el cuerpo del tirador (sobre todo la cabeza) durante el comienzo de la carrera de aproximación y después, según avanzaba el jugador hacia el balón apartaban su mirada del jugador y la dirigían hacia el balón (o zona entre el balón y la pierna de apoyo). Los porteros miraron durante más tiempo al cuerpo y cambiaron de foco hacia el balón más tarde en los tiros de penalti con respecto a los tiros de doble penal ti. Así pues, este cambio de foco visual corporal hacia el balón pareció estar relacionado con los determinantes espacio-temporales (i.e., 6 vs. 10 m] más que con las estrategias de engaño del tirador o con el tiempo de inicio de los participantes. Tanto los tiros de penalti (6 m] como los de doble penalti (10 m) fueron menos veloces en los tiros con engaño en comparación con los tiros normales .. El análisis discriminante encontró que la distancia horizontal al centro (balón situado más cerca del portero) fue crucial para parar el doble penalti, siendo menos importante para el caso de los penaltis; viceversa sucedió con el tiempo de visión en los primeros momentos de vuelo del balón, resultando más predictivo de la parada en el caso de los penaltis que el de los dobles penaltis. Los resultados sugieren el uso de diferentes estrategias viso-motoras en función de la distancia de disparo. En los tiros de doble penalti (desde 10 m], los participantes esperaron a ver la información del balón (obteniendo información del golpeo y del vuelo) para coordinar sus acciones en función de esa información más fiable (Diaz, Fajen y Phillips, 2012). Así, comenzaron su acción de parada sobre los 200 ms después del golpeo, lo que les permitió moverse de forma constante hacia el mismo lado del balón, pero les dejó sin tiempo suficiente para alcanzar el balón en los casos en los que éste fue relativamente ajustado al palo. Por el contrario, en los tiros de penalti [desde 6 m], los porteros generalmente empezaron a moverse antes del golpeo, para aumentar su margen temporal de acción y así aumentar sus opciones de llegar a los balones escorados(en caso de haber acertado el lado). Esto les obligó a basar sus acciones en información temprana menos predictiva [más tiempo de visión en el cuerpo y cambio de foco más tardío) lo que les provocó un detrimento en el rendimiento. Por ejemplo, en los tiros de penalti los porteros acertaron el lado en sólo en la mitad de los casos. Así, en los penaltis los porteros se movieron hacia nno de los lados (i.e., derecha o izquierda) independientemente de la dirección final de tiro, mientras que en los dobles se encontró una relación de dependencia entre la trayectoria de los tiros y la dirección de la acción de parada (Kuhn, 1988). Por otra parte, los tiempos de inicio del movimiento del tronco y de los pies en los dobles fueron relativamente similares, mientras que en los tiros de penalti la diferencia entre participantes aumentó. Esto podría indicar que la variabilidad en el tiempo de inicio de la parada entre participantes podría verse influenciada por las demandas espacio-temporales. Por último, las intenciones de engaño de los tiradores afectaron su capacidad de tiro (más despacio) pero no provocaron ningún efecto observable en el rendimiento, tiempo de movimiento o patrones visuales de los porteros. La presentación aleatoria de los tiros en cuanto a estrategia podría haber impedido que los porteros establecieran relaciones entre las variables ópticas tempranas (i.e., información del cuerpo del tirador) y la dirección final de tiro (pero ver Dicks, Button y Davids, 2010a).

Análisis del comportamiento visual de taekwondistas de diferente nivel de pericia

El propósito de este estudio fue analizar y comparar el comportamiento visual de taekwondistas de diferente nivel de pericia (17 expertos, 7 experimentados y 9 novatos) ante una situación de combate simulada en laboratorio. Se empleó el pupilómetro Mobile Eye ASL para registrar la mirada mientras visionaban acciones de ataque grabadas y presentadas a tamaño real. Los resultados mostraron que mientras que los taekwondistas novatos mostraron un mayor número de fijaciones de menor duración en zonas corporales como la cabeza o piernas del oponente a medida que aumentaban el nivel de pericia (experimentados y expertos)el comportamiento visual se caracterizó por un menor número de fijaciones pero de mayor duración en la zona del torso del oponente. Los taekwondistas expertos mostraron una estrategia visual muy diferenciada basada en un pivote visual y una estabilización de la mirada, quite eye, antes de la toma de decisiones.

La mirada de los porteros de fútbol-sala ante diferentes tipo de respuesta motriz.

En este estudio se exploró y analizó el comportamiento visual de un grupo de porteros expertos de fútbol sala con el objetivo de comprobar cómo el tipo de respuesta motriz solicitada influía en su comportamiento visual. Participaron 4 porteros a los que se les presentó un total de 48 clips de vídeo en una pantalla a tamaño real, bajo dos condiciones de respuesta: con movimiento de parada y sin movimiento de parada. Se registró su mirada con el pupilómetro ASL Mobile Eye durante dos condiciones de tiro de penalti. Se analizó la mirada en el intervalo de -250 a 205 ms en torno al disparo. Los resultados mostraron que cuando respondían con la acción habitual de parada, solo se encontraron fijaciones en la mitad de los casos, estas fijaciones eran de corta duración y localizadas principalmente en la zona del suelo justo enfrente del balón. Por el contrario, cuando se mantenían en posición estática, su mirada se dirigía hacia la zona entre el balón y la pierna de apoyo, empleando fijaciones de una duración más larga. Se puede concluir que el comportamiento visual fue diferente entre las dos condiciones como resultado de la adaptación a las demandas espacio-temporales específicas de cada condición, ya que el grado de movimiento en la respuesta solicitada tuvo influencia en el comportamiento visual asociado.

Membrane Systems Working with the PFactor: Best Strategy to Solve Complex Problems.

A membrane system is a massive parallel system, which is inspired by the living cells when processing information. As a part of unconventional computing, membrane systems are proven to be effective in solving complex problems. A new factor is introduced. This factor can decide whether a technique is worthwhile being used or not. The use of this factor provides the best chances for selecting the strategy for the rules application phase. Referring to the “best” is in reference to the one that reduces execution time within the membrane system. A pre-analysis of the membrane system determines the P-factor, which in return advises the optimal strategy to use. In particular, this paper compares the use of two strategies based on the P-factor and provides results upon the application of them. The paper concludes that the P-factor is an effective indicator for choosing the right strategy to implement the rules application phase in membrane systems.

Climate and grazing control nurse effects in an Ecuadorian dry shrubby community

Positive plant interactions have strong effects on plant diversity at several spatial scales, expanding species distribution under stressful conditions. We evaluated the joint effect of climate and grazing on the nurse effect of Croton wagneri, by monitoring several community attributes at two spatial scales: microhabitat and plant community. Two very close locations that only differed in grazing intensity were surveyed in an Ecuadorian dry scrub ecosystem. At each location, two 30 × 30-m plots were established at four altitudinal levels (1500, 2630, 1959 and 2100 m asl) and 40 microsites were surveyed in each plot. Croton wagneri acted as community hubs, increasing species richness and plant cover at both scales. Beneath nurses mean richness and cover values were 3.4 and 21.9%, and in open areas 2.3 and 4.5%, respectively. Magnitude of nurse effect was dependent on climate and grazing conditions. In ungrazed locations, cover increased and diversity reduced with altitude, while grazed locations showed the opposite trend. In ungrazed plots the interactions shifted from positive to negative with altitude, in grazed locations interactions remained positive. We conclude that the nurse effect is a key mechanism regulating community properties not only at microsite but also at the entire community scale.

Caracterización morfofisiológica de semillas de especies leñosas distribuidas en dos zonas secas presentes en el Sur del Ecuador

Sudamérica es una de las zonas con mayor cantidad de bosque seco tropical a nivel mundial. No obstante, estos bosques han sido poco conocidos y la mayoría de estudios han estado orientados hacia los bosques húmedos tropicales. Los bosques secos se han reducido drásticamente y siguen muy amenazados, corriendo el riesgo de desaparecer en los próximos años. Por ello, es fundamental, generar investigación aplicada para la conservación inmediata de los ecosistemas secos tropicales. En Ecuador, la situación no es diferente y las zonas secas catalogadas como biodiversas están en constante amenaza. Los pocos estudios realizados en Ecuador sobre zonas secas, han permitido mejorar nuestro conocimiento referente a la diversidad y abundancia de las especies, relaciones planta-planta y síndromes de dispersión. No existen estudios sobre caracteres morfológicos en frutos y semillas de las especies leñosas de bosque seco. Sin embargo, nuestra comprensión de la dinámica y estructura de las comunidades ecológicas de zonas secas poco estudiadas, puede mejorar rápidamente mediante el estudio y enfoque de rasgos morfofisiológicos funcionales. El objetivo general del presente estudio fue aportar al conocimiento de la ecología y biología de semillas de zonas secas tropicales mediante el análisis y evaluación de rasgos morfofisiológicos de frutos y semillas de una comunidad de especies leñosas. El estudio se realizó en una zona de bosque y matorral seco, ubicados al sur occidente del Ecuador, a una altitud comprendida entre los 250 a 1 200 m s.n.m. caracterizada por una marcada estacionalidad ambiental, con lluvias desde diciembre a abril y una estación seca de mayo a noviembre. Precipitación media anual de 500 mm con una temperatura media anual de 20° a 26 °C. La zona de estudio forma parte de la región Tumbesina compartida entre el sur del Ecuador y el norte del Perú con gran diversidad de especies vegetales endémicas. Para el estudio se colectaron frutos con semillas maduras previamente a su dispersión de entre ocho y diez individuos de 80 especies entre árboles y arbustos más representativos de los bosques secos ecuatorianos. De los frutos colectados se utilizó una muestra al azar de 50 frutos y semillas por especie para los diferentes análisis. Se midió y evaluó 18 rasgos morfológicos y fisiológicos cuantitativos y cualitativos de frutos, semillas y de la especie. Se realizaron diferentes análisis de asociación y correlación entre los rasgos evaluados, con cinco variables ambientales registradas de las 109 parcelas establecidas en el área de estudio, además analizamos el tipo de dormición y comparamos la respuesta germinativa a la deshidratación relacionada con dos comunidades secas, matorral y bosque seco. Los resultados mostraron que las especies presentan gran heterogeneidad en rasgos continuos de las semillas. La variabilidad fue más evidente en rasgos como tamaño, volumen, masa y número de semillas por fruto. Sin embargo, una alta proporción de las especies tiende a producir una semilla por fruto. Además, la mayoría de las especies de bosque seco se caracterizan por no poseer algún tipo de apéndices o areola en sus semillas, forma ovalada y sin endospermo. La reserva nutritiva de las semillas se encuentra especialmente en los cotiledones de los embriones. Se encontraron seis tipos diferentes de embriones y la mayoría de las especies presentó embriones gruesos e invertidos. La dispersión de semillas está dominada por zoocoria en un 38 %, con relación a anemocoria (22 %) y autocoria (19 %). Sin embargo, encontramos que el 70 % de las especies posee frutos secos. Los análisis de dormición en las semillas de bosque seco, mostraron que el 60 % de las especies de bosque seco presentaron semillas con algún tipo de latencia, menor a la encontrada en especies de bosque deciduo tropical y sabanas, sin embargo, la dormición de las especies de bosque seco fue mayor al porcentaje de especies con dormición de bosque semiperenne y selva lluviosa tropical. La dormición física constituyó el 35 % de las especies de bosque seco, seguido del 12 % con dormición fisiológica, mientras que solamente una especie tuvo dormición morfológica. Encontramos que la dormición de las semillas de las especies en estudio se relaciona significativamente con el tipo y función del embrión y con el endospermo. Existieron relaciones significativas entre los rasgos morfológicos de los frutos, semillas, embriones y atributos de los individuos de 46 especies, aunque en algunos casos con coeficientes de correlación bajos. Hubo pocas relaciones entre los rasgo morfológicos de las semillas con las variables ambientales registradas. Solamente el tipo de testa y la presencia de apéndices en las semillas mostraron relación con el pH y la temperatura media del suelo. No obstante usando el modelo fouth corner-RLQ, no se encontraron asociaciones claras ni significativas entre rasgos morfológicos de semillas y frutos con variables ambientales. Al medir el efecto de la deshidratación en las semillas de los dos hábitats secos tropicales: bosque y matorral seco, los resultados determinaron que tanto las semillas de las especies leñosas de ambientes más áridos (matorral seco) están en gran medida pre-adaptadas a la desecación que las especies de ambientes menos áridos (bosque seco). Los tratamientos de deshidratación ejercieron un efecto negativo en los porcentajes de germinación en todas las especies, excepto para C. platanifolia. Los resultados más sorprendentes se registraron para Senna alata que mostró germinación extremadamente baja o incluso sin germinación a contenidos de humedad de la semillas de 0,10 g H2O g de peso seco. Las curvas de germinación difirieron significativamente entre los tratamientos de deshidratación en cada especie. Aportar al conocimiento la fisiología de la deshidratación y los límites de tolerancia de las semillas de bosque y matorral seco ayudará a entender mejor el papel de este rasgo en la ecología de las semillas y dinámica de las comunidades áridas tropicales. El estudio demostró, que la adaptación ecológica de las semillas de las especies leñosas de bosque seco a factores ambientales extremos, puede verse reflejada en una red de interacciones y correlaciones complejas entre los propios rasgos morfológicos y fisiológicos continuos y cuantitativos, sobre todo en rasgos internos de las semillas, quienes ejercerían una mayor influencia en toda la red de interacciones. Si bien, los rasgos de las semillas no mostraron fuertes relaciones con las variables ambientales, posiblemente las asociaciones presentes entre rasgos morfológicos pudiesen predecir en cambio interacciones entre especies y comportamientos y procesos relacionados con la tolerancia a la deshidratación y dormición de las semillas. ABSTRACT South America is one of the areas with the largest number of tropical dry forest in the world. However, these forests have been poorly understood and most studies have been directed to tropical rainforests. Dry forests have been drastically reduced and are very threatened, risking desaparecerer in the next years. It is therefore essential, generate applied research for conservation of tropical dry ecosystems. In Ecuador the situation is no different and dry areas classified as biodiverse are under constant threat. The few studies made in Ecuador on drylands have improved our knowledge concerning the diversity and abundance of species, plant-plant relationships and dispersion syndromes. Morphological studies on fruits and seeds of woody dry forest species do not exist. However, our understanding of the dynamics and structure of ecological communities dryland little studied, may improve quickly through the study and functional approach morphophysiological traits. The overall objective of this study was to contribute to the knowledge of the ecology and biology of tropical dry seeds through analysis and evaluation of morphophysiological traits of fruits and seeds of a community of woody species. The study was conducted in an area of dry scrub forest, located at the southwest of Ecuador, at an altitude between 250 to 1200 m asl. Environmental characterized by a marked seasonality, with rainfall from December to April and a dry season from May to November. Annual rainfall of 500 mm with an average annual temperature of 20° to 26 °C. The study area is part of the shared Tumbesina region between southern Ecuador and northern Peru with a great diversity of endemic plant species. For the study, we collected fruit and seed madure of eight and ten individuos of 80 species of trees and shrub most representated of the Ecuador dry forest. We selected a sample of 50 fruits and seeds for different analysis. We measure and evaluate 18 morphological and physiological traits of fruits, seeds and species. We perform analysis and correlation between traits associated with five environmental variables taken from the 109 plots established in the study area also analyze and compare the germination response to dehydration related to two dry communities, scrub and dry forest. The results showed that the species have great heterogeneity in continuous seed traits. Variability was more evident in features such as size, volume, mass, and number of seeds per fruit. However, a high proportion of species tends to produce a seed per fruit. In addition, most of the species of dry forest is characterized by not having some sort of ppendices or areola in its seeds, oval form and without endosperm. The nutrient reserves of seeds are especially in the cotyledons of the embryos. Six different embryos were found and most of the species presented thick and inverted embryos. Seed dispersal zoochory is dominated by 38 %, relative to anemochory (22 %) and autochory (19 %). However, we found that 70 % of the species has dried fruits. The analysis of dormancy from tropical dry forest, showed that 60 % of species showed seed dormancy, down from species found in tropical deciduous forest and savanna, however dormancy dry forest species was higher than the percentage of forest species dormancy semi-evergreen and tropical rain forest. Physical dormancy corresponds to 35 % of species, followed by 12 % with physiological dormancy, while only one species had morphological dormancy. We found that dormancy of the seeds was significantly related to the type and function of the embryo and the endospemo. There were significant relationships between morphological traits of fruits, seeds, embryos and attributes of individuals of 46 species, although in some cases with low correlation coefficients. There was little relationship between the morphologic traits of the seeds with the registered environmental variables. Only the type of tesla and the presence of appendages on the seeds showed relation to pH and the mean soil temperature. However, using the fourth corner-RLQ model, neither clear nor significant between morphological traits of seeds and fruits associations with environmental variables were found. The effect of dehydration on seeds of two tropical dry forest habitats was evident in dry scrub. The results determined that both the seeds of woody species forest and dry scrub are pre-adapted to drier conditions. Dehydration treatments exerted a negative effect on germination percentage in all species, except for C. platanifolia. However, all species germinated in treatments of extreme dryness, but in low percentages. The most striking results were recorded for Senna alata showed no germination when its moisture content was 0.10 g H2O g dry weight. Germination curves differ significantly between the treatments of dehydration in each species. Contribute to the knowledge of physiology and dehydration tolerance limits seeds dry scrub forest and help you better understand the role of this trait in seed ecology and dynamics of tropical arid communities. The study showed that the ecological adaptation of seeds of woody species of dry forest to extreme environmental factors may be reflected in a complex web of interactions and correlations between morphological and physiological traits continuous and quantitative themselves, especially in internal seed traits, who exerted a major influence on the entire network of interactions. While the seed traits showed strong relationships with environmental variables possibly present associations between morphological traits could predict interactions between species and change behaviors related to desiccation tolerance and seed dormancy processes.

Human argininosuccinate lyase: A structural basis for intragenic complementation

Intragenic complementation has been observed at the argininosuccinate lyase (ASL) locus. Intragenic complementation is a phenomenon that occurs when a multimeric protein is formed from subunits produced by different mutant alleles of a gene. The resulting hybrid protein exhibits enzymatic activity that is greater than that found in the oligomeric proteins produced by each mutant allele alone. The mutations involved in the most successful complementation event observed in ASL deficiency were found to be an aspartate to glycine mutation at codon 87 of one allele (D87G) coupled with a glutamine to arginine mutation at codon 286 of the other (Q286R). To understand the structural basis of the Q286R:D87G intragenic complementation event at the ASL locus, we have determined the x-ray crystal structure of recombinant human ASL at 4.0 Å resolution. The structure has been refined to an R factor of 18.8%. Two monomers related by a noncrystallographic 2-fold axis comprise the asymmetric unit, and a crystallographic 2-fold axis of space group P3121 completes the tetramer. Each of the four active sites is composed of residues from three monomers. Structural mapping of the Q286R and D87G mutations indicate that both are near the active site and each is contributed by a different monomer. Thus when mutant monomers combine randomly such that one active site contains both mutations, it is required by molecular symmetry that another active site exists with no mutations. These “native” active sites give rise to the observed partial recovery of enzymatic activity.

Cerebral organization for language in deaf and hearing subjects: Biological constraints and effects of experience

Cerebral organization during sentence processing in English and in American Sign Language (ASL) was characterized by employing functional magnetic resonance imaging (fMRI) at 4 T. Effects of deafness, age of language acquisition, and bilingualism were assessed by comparing results from (i) normally hearing, monolingual, native speakers of English, (ii) congenitally, genetically deaf, native signers of ASL who learned English late and through the visual modality, and (iii) normally hearing bilinguals who were native signers of ASL and speakers of English. All groups, hearing and deaf, processing their native language, English or ASL, displayed strong and repeated activation within classical language areas of the left hemisphere. Deaf subjects reading English did not display activation in these regions. These results suggest that the early acquisition of a natural language is important in the expression of the strong bias for these areas to mediate language, independently of the form of the language. In addition, native signers, hearing and deaf, displayed extensive activation of homologous areas within the right hemisphere, indicating that the specific processing requirements of the language also in part determine the organization of the language systems of the brain.

Nuevos enfoques teóricos en lingüística aplicada: el estudio de la motivación en el aprendizaje de ELE en Grecia

El estudio de las variables individuales es una de las líneas de investigación principales en el ámbito de adquisición de segundas lenguas (ASL, en adelante). Hasta la fecha, se han llevado a cabo estudios entre diferentes variables individuales del aprendiz de lenguas (sexo, edad, aptitud o motivación, entre otras) y el éxito de los resultados de aprendizaje. Todos estos se han realizado en diferentes países y con aprendices de inglés, francés, alemán y español en enseñanzas regladas y no regladas. Sin embargo, mientras las investigaciones sobre la motivación en el aprendizaje de inglés como lengua extranjera han recibido la mayor atención, las que se han realizado sobre la relación de la variable motivación y aprendizaje de español han ido haciéndose paulatinamente un hueco. En este sentido, nuestro artículo es una pequeña aportación a todas estas investigaciones –a algunas de las que haremos mención más adelante– que estudian la motivación y su relación con el aprendizaje de español en contextos de lengua extranjera, revisando los modelos teóricos más recientes sobre la motivación en ASL y analizando su futura aplicación al contexto griego.

Pollen profiles from a Late Palaeolithic site in the community of Bad Buchau-Kappel, Baden-Wuerttemberg, Germany

Excavations were carried out in a Late Palaeolithic site in the community of Bad Buchau-Kappel between 2003 and 2007. Archaeological investigations covered a total of more than 200 m**2. This site is the product of what likely were multiple occupations that occurred during the Late Glacial on the Federsee shore in this location. The site is situated on a mineral ridge that projected into the former Late Glacial lake Federsee. This beach ridge consists of deposits of fine to coarse gravel and sand and was surrounded by open water, except for a connection to the solid shore on the south. A lagoon lay between the hook-shaped ridge and the shore of the Federsee. This exposed location provided optimal access to the water of the lake. In addition, the small lagoon may have served as a natural harbor for landing boats or canoes. Sedimentological and palynological investigations document the dynamic history of the location between 14,500 and 11,600 years before present (cal BP). Evidence of the deposition of sands, gravels and muds since the Bølling Interstadial is provided by stratigraphic and palynological analyses. The major occupation occurred in the second half of the Younger Dryas period. Most of the finds were located on or in the sediments of the ridge; fewer finds occurred in the surrounding mud, which was also deposited during the Younger Dryas. Direct dates on some bone fragments, however, demonstrate that intermittent sporadic occupations also took place during the two millennia of the Meiendorf, Bølling, and Allerød Interstadials. These bones were reworked during the Younger Dryas and redeposited in the mud. A 14C date from one bone of 11,600 years ago (cal BP) places the Late Palaeolithic occupation of the ridge at the very end of the Younger Dryas, which is in agreement with stratigraphic observations. Stone artifacts, numbering 3,281, comprise the majority of finds from the site. These include typical artifacts of the Late Palaeolithic, such as backed points, short scrapers, and small burins. There are no bipointes or Malaurie-Points, which is in accord with the absolute date of the occupation. A majority of the artifacts are made from a brown chert that is obtainable a few kilometers north of the site in sediments of the Graupensandrinne. Other raw materials include red and green radiolarite that occur in the fluvioglacial gravels of Oberschwaben, as well as quartzite and lydite. The only non-local material present is a few artifacts of tabular chert from the region near Kelheim in Bavaria. A unique find consists of two fragments of a double-barbed harpoon made of red deer antler, which was found in the Younger Dryas mud. It is likely, but not certain, that this find belongs to the same assemblage as the numerous stone artifacts. Although not numerous, animal bones were also found in the excavations. Most of them lay in sediments of the Younger Dryas, but several 14C dates place some of these bones in earlier periods, including the Meiendorf, Bølling, and Allerød Interstadials. These bones were reworked by water and redeposited in mud sediments during the Younger Dryas. As a result, it is difficult to attribute individual bones to particular chronological positions without exact dates. Species that could be identified include wild horse (Equus spec.), moose or elk (Alces alces), red deer (Cervus elaphus), roe deer (Capreolus capreolus), aurochs or bison (Bos spec.), wild boar (Sus scrofa), as well as birds and fish, including pike (Esox Lucius).

Identification of superior energy-absorbing materials for school bus interiors: Volume I - summary report. Final report.

National Highway Traffic Safety Administration, Washington, D.C.