903 resultados para Long-distance Migration


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• Background and Aims The uptake, translocation and redistribution of the heavy metals zinc, manganese, nickel, cobalt and cadmium are relevant for plant nutrition as well as for the quality of harvested plant products. The long-distance transport of these heavy metals within the root system and the release to the shoot in young wheat (Triticum aestivum ‘Arina’) plants were investigated. • Methods After the application of 65Zn, 54Mn, 63Ni, 57Co and 109Cd for 24 h to one seminal root (the other seminal roots being excised) of 54-h-old wheat seedlings, the labelled plants were incubated for several days in hydroponic culture on a medium without radionuclides. • Key Results The content of 65Zn decreased quickly in the labelled part of the root. After the transfer of 65Zn from the roots to the shoot, a further redistribution in the phloem from older to younger leaves was observed. In contrast to 65Zn, 109Cd was released more slowly from the roots to the leaves and was subsequently redistributed in the phloem to the youngest leaves only at trace levels. The content of 63Ni decreased quickly in the labelled part of the root, moving to the newly formed parts of the root system and also accumulating transiently in the expanding leaves. The 54Mn content decreased quickly in the labelled part of the root and increased simultaneously in leaf 1. A strong retention in the labelled part of the root was observed after supplying 57Co. • Conclusions The dynamics of redistribution of 65Zn, 54Mn, 63Ni, 57Co and 109Cd differed considerably. The rapid redistribution of 63Ni from older to younger leaves throughout the experiment indicated a high mobility in the phloem, while 54Mn was mobile only in the xylem and 57Co was retained in the labelled root without being loaded into the xylem.

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Lake sediments and pollen, spores and algae from the high-elevation endorheic Laguna Miscanti (22°45′S, 67°45′W, 4140 m a.s.l., 13.5 km2 water surface, 10 m deep) in the Atacama Desert of northern Chile provide information about abrupt and high amplitude changes in effective moisture. Although the lack of terrestrial organic macrofossils and the presence of a significant 14C reservoir effect make radiocarbon dating of lake sediments very difficult, we propose the following palaeoenvironmental history. An initial shallow freshwater lake (ca. 22,000 14C years BP) disappeared during the extremely dry conditions of the Last Glacial Maximum (LGM; 18,000 14C years BP). That section is devoid of pollen. The late-glacial lake transgression started around 12,000 14C years BP, peaked in two phases between ca. 11,000 and <9000 14C years BP, and terminated around 8000 14C years BP. Effective moisture increased more than three times compared to modern conditions (∼200 mm precipitation), and a relatively dense terrestrial vegetation was established. Very shallow hypersaline lacustrine conditions prevailed during the mid-Holocene until ca. 3600 14C years BP. However, numerous drying and wetting cycles suggest frequent changes in moisture, maybe even individual storms during the mid-Holocene. After several humid spells, modern conditions were reached at ca. 3000 14C years BP. Comparison between limnogeological data and pollen of terrestrial plants suggest century-scale response lags. Relatively constant concentrations of long-distance transported pollen from lowlands east of the Andes suggest similar atmospheric circulation patterns (mainly tropical summer rainfall) throughout the entire period of time. These findings compare favorably with other regional paleoenvironmental data.

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Despite the many technological innovations that had for some time contributed to a significant reduction of global travel times, intercontinental ship passages in the late nineteenth century were no quick affair. Depending on the route, such journeys could last between a few weeks and several months. During this time, crew and passengers shared the narrow space of the ship—largely isolated from the rest of the world and basically suspended between origin and destination. On many long-distance steamers, the production and consumption of ship newspapers became one possible means of whiling away the time in transit for the passengers. In this article, we seek to demonstrate how these extraordinary publications can serve as lenses not only on shipboard life but actually on historical actors of globalisation in a more general context. First, we seek to highlight why and how ship newspapers played an important role in the shaping of the peculiar social space of the passenger ship. We will then give a brief overview of the context in which these newspapers were produced and what kind of news they contained. In a third step, we will introduce two brief examples of topics discussed in ship newspapers and outline possible fields of research on which ship newspapers will be able to shed new light.

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Abstract. We resumed mowing in two plots of ca. 100 m2 in an abandoned meadow dominated by Brachypodium pinnatum on the slope of Monte Generoso (Switzerland). We monitored species composition and hay yield using point quadrats and biomass samples. Species frequencies changed little during 10 yr (1988–1997) while hay yields showed large fluctuations according to mean relative humidity in April-June. We performed a seed-addition experiment to test whether the establishment of meadow species is limited by lack of diaspores or favourable microsites for germination and recruitment from the seed bank. We sowed ca. 12 000 seeds of 12 species originating from a nearby meadow individually in plots of a 4 × 6 unbalanced Latin square with four treatments, burning, mowing, mowing and removal of a layer of decayed organic matter, and a control. We monitored the fate of seedling individuals for 24 months. Seedlings of all species were established and survived for 12 months, 10 species survived during at least 24 months, some reached a reproductive stage. Species responded to different qualities of microsites provided by the different treatments thus required different regeneration niches. Spontaneous long-distance immigration was insignificant. We conclude that the former species composition of abandoned meadows cannot easily be restored by mowing alone because many plant species of meadows do not have persistent seed banks and immigration over distances of more than 25 m and successful establishment is very unlikely.

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Although long distance running clearly has benefits--as witnessed by its popularity--it also has risks of injury and death. Little is known, however, about the prevalence of potentially dangerous training habits in long distance runners, although anecdotal information suggests that many runners have erroneous beliefs about risks and benefits of marathon running. We conducted a cross-sectional survey to estimate the prevalence of 19 potentially dangerous training habits (risky behaviors) among marathon runners. A 66-item self-administered questionnaire was mailed to a stratified random sample of runners who finished of the 1992 Houston-Tenneco Marathon and were 21-71 years of age. Responses were obtained from 508 runners (83%) with approximately equal representation in four age-gender groups: men $<$40 years, men $\ge$40 years, women $<$40 years, and women $\ge$40 years.^ Prevalences of risky behaviors were high. 50% or more ran in dangerously hot and humid conditions, did not cool down or stretch after running, did not wear proper running gear, or ran when injured or ill; 25-49% did not warm up, ran on dangerous surfaces, did not drink sufficient water during training, increased weekly mileage too quickly, and ran during lightning storms; 10-24% ran daily, ran in areas with high pollution, ran in the same direction as traffic, did hard runs frequently, ran more than 60 miles per week, or ran against the advice of a physician.^ Positive associations were found between the practice of risky behaviors and self-reported prevalence of musculoskeletal injuries, heat-related injuries, noncompliance with recommendations for preventive health examinations, and noncompliance with positive health habits.^ These results indicate that many marathon runners engage in training habits that may increase risk of substantial injury or illness. Further studies are needed to explore the association of risky training behaviors on the incidence of injuries, and to determine reasons for noncompliance with recommendations from sports medicine specialists. ^

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Carbon isotope measurements were made on bulk sediments from the well preserved calcareous sequences recovered at ODP Sites 689 and 690 on the Maud Rise, Weddell Sea, Antarctica. The very positive delta13C values that characterize the late Paleocene and the rapid trend toward lighter values in the early Eocene established in other sites are clearly recorded here and may be of value for long-distance stratigraphic correlation. However, values in the late Eocene are significantly more positive than have been reported from other areas. The general pattern of the records from Sites 689 and 690 is sufficiently unlike those previously reported from lower latitudes that we suggest that carbon isotope data should be used only with considerable caution for correlating sequences from such high latitudes with lower latitude records.

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Innerdalen was once a mountain valley (ca. 780 m a.s.l.) with birch forests, bogs and several summer farms. Today it is a 6.5 km**2 artifical lake. In 1980 and 1981 archaeological and palynological investigations were carried out due to the hydroelectric power plans. Radiocarbon dated pollen diagrams from 9 different localities in Innerdalen provide information on a mountain environment which has been exploited to varying degrees by human groups for thousands of years. In the Birch Zone, ca. 9500-8500 years B.P., the deglaciated surface is vegetated by the normal sequence of pioneering species, first show-bed communities, then shrub/dwarf-shrub communities, and finally a birch forest community. In the Pine Zone, ca. 8500-7500 years B.P., the mixed Birch-Pine forest which prevailed at the end of the Birch Zone is replaced by a dense pine forest. The tree limit was higher than it is today. In the Alder Zone, ca. 7500-4000 years B.P., the newly arrived alder gradually succeeded pine, particularily on good soils. This alder forest has a modem analog in the pre-alpine gray alder forests in Norway. In the last part of the Alder Zone, ca. 6000-4000 years B.P., elm and hazel are nominally present on particularily rich soils, marking the edaphic and climatic optimum in Innerdalen. During this time the first evidence of human impact on the vegetation is apparent in the pollen diagrams. At both Sætersetra in the south of the valley and Liabekken in the north, forest clearance and the development of grazed grass meadows is documented, and human impact continues until the present. The Herb Zone, ca. 4000 years B.P. to 1600 A.D., is characterized by the rapid decline of alder. The forest is increasingly open, and bog formation is initiated. The sub-alpine belt of birch forest is established, probably due to the shift to a cooler, moister climate. Human activity can also have influenced the vegetational changes, although at 4 of the localities human activity also is first apparent after the alder decline. Some localities show measurably less human impact on the vegetation ca. 2600-2000 years B.P. Grazing intensity increases ca. 2000 years B.P. At the end of the Herb Zone rye and barley pollen is registered at Sætersetra and Flonan, indicating contact between the grazing activities of Innerdal and grain cultivation activities outside the valley. The Spruce Zone, ca. 1600 A.D. to the present, does not begin synchronously since the presence of long-distance transported spruce pollen at a locality is entirely dependent on the density of the vegetation ie. degree of human impact. The youngest spruce rise is ca. 1500 A.D. at Røstvangen, when summerfarming is initiated. Summerfarming activities in Innerdal produce an increasingly open landscape. Rye and barley pollen at several localities may indicate limited local cultivation, but is more likely long-distance transport via humans and domesticated animals from cultivated areas outside Innerdalen.

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El presente trabajo propone explorar el modo cómo la literatura inglesa se apropia de la figura del héroe ático por antonomasia, Teseo, prefiriendo a las historias relacionadas con la aventura aquellas que lo muestran como figura garante del orden y de la sabiduría. Proponemos rastrear el modo cómo el héroe es presentado en el "Cuento del caballero" de los Canterbury Tales, representando no sólo el discurso patriarcal sino y, al mismo tiempo, quien desata las contiendas y quien las re-ordena. En este sentido, la figura del cuento- épico en el sentido bajtiniano del término- testimonia el discurso del orden, donde el varón es el eje vertebrador de la sociedad civil y familiar. Shakespeare, que había tomado contacto con las fuentes clásicas y medievales-tanto italianas como inglesas- incorpora en su Sueño de una noche de verano a un nuevo Teseo, que no sólo discurre acerca de la imaginación sino que también retoma la idea de orden a partir de la proclama de que es necesario someter las trampas de la imaginación a la prueba de la "fría razón". A partir de estos dos ejemplos, trataremos de reflexionar el modo cómo la literatura inglesa se apropió de estos mitos clásicos

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El presente trabajo pretende continuar la línea general inaugurada por Krivochen y Luder (2012) en el desarrollo de herramientas formales para el estudio de las lenguas clásicas, en particular la lengua latina. Tales herramientas, desarrolladas a partir de métodos axiomático-formales, son puestas a prueba con los datos concretos y nos ayudan a comprender mejor no solamente el funcionamiento de una lengua como sistema sino el sustrato cognitivo-biológico que posibilita el desarrollo de tal sistema. Nuestro foco en este trabajo será la noción de "localidad" en las derivaciones sintácticas, que ha sido el centro de gran parte de los estudios de orientación chomskyana durante la última década. Basándonos en problemas concretos que aparecen en la consideración de ejemplos atestiguados en los textos, proporcionaremos una explicación alternativa a la ortodoxia chomskyana. El objetivo es proveer al lector de una serie de herramientas teóricas explícitas que pueda utilizar en el análisis de la localidad en la lengua latina

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El presente trabajo pretende continuar la línea general inaugurada por Krivochen y Luder (2012) en el desarrollo de herramientas formales para el estudio de las lenguas clásicas, en particular la lengua latina. Tales herramientas, desarrolladas a partir de métodos axiomático-formales, son puestas a prueba con los datos concretos y nos ayudan a comprender mejor no solamente el funcionamiento de una lengua como sistema sino el sustrato cognitivo-biológico que posibilita el desarrollo de tal sistema. Nuestro foco en este trabajo será la noción de "localidad" en las derivaciones sintácticas, que ha sido el centro de gran parte de los estudios de orientación chomskyana durante la última década. Basándonos en problemas concretos que aparecen en la consideración de ejemplos atestiguados en los textos, proporcionaremos una explicación alternativa a la ortodoxia chomskyana. El objetivo es proveer al lector de una serie de herramientas teóricas explícitas que pueda utilizar en el análisis de la localidad en la lengua latina

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El presente trabajo propone explorar el modo cómo la literatura inglesa se apropia de la figura del héroe ático por antonomasia, Teseo, prefiriendo a las historias relacionadas con la aventura aquellas que lo muestran como figura garante del orden y de la sabiduría. Proponemos rastrear el modo cómo el héroe es presentado en el "Cuento del caballero" de los Canterbury Tales, representando no sólo el discurso patriarcal sino y, al mismo tiempo, quien desata las contiendas y quien las re-ordena. En este sentido, la figura del cuento- épico en el sentido bajtiniano del término- testimonia el discurso del orden, donde el varón es el eje vertebrador de la sociedad civil y familiar. Shakespeare, que había tomado contacto con las fuentes clásicas y medievales-tanto italianas como inglesas- incorpora en su Sueño de una noche de verano a un nuevo Teseo, que no sólo discurre acerca de la imaginación sino que también retoma la idea de orden a partir de la proclama de que es necesario someter las trampas de la imaginación a la prueba de la "fría razón". A partir de estos dos ejemplos, trataremos de reflexionar el modo cómo la literatura inglesa se apropió de estos mitos clásicos

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El presente trabajo propone explorar el modo cómo la literatura inglesa se apropia de la figura del héroe ático por antonomasia, Teseo, prefiriendo a las historias relacionadas con la aventura aquellas que lo muestran como figura garante del orden y de la sabiduría. Proponemos rastrear el modo cómo el héroe es presentado en el "Cuento del caballero" de los Canterbury Tales, representando no sólo el discurso patriarcal sino y, al mismo tiempo, quien desata las contiendas y quien las re-ordena. En este sentido, la figura del cuento- épico en el sentido bajtiniano del término- testimonia el discurso del orden, donde el varón es el eje vertebrador de la sociedad civil y familiar. Shakespeare, que había tomado contacto con las fuentes clásicas y medievales-tanto italianas como inglesas- incorpora en su Sueño de una noche de verano a un nuevo Teseo, que no sólo discurre acerca de la imaginación sino que también retoma la idea de orden a partir de la proclama de que es necesario someter las trampas de la imaginación a la prueba de la "fría razón". A partir de estos dos ejemplos, trataremos de reflexionar el modo cómo la literatura inglesa se apropió de estos mitos clásicos

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El presente trabajo pretende continuar la línea general inaugurada por Krivochen y Luder (2012) en el desarrollo de herramientas formales para el estudio de las lenguas clásicas, en particular la lengua latina. Tales herramientas, desarrolladas a partir de métodos axiomático-formales, son puestas a prueba con los datos concretos y nos ayudan a comprender mejor no solamente el funcionamiento de una lengua como sistema sino el sustrato cognitivo-biológico que posibilita el desarrollo de tal sistema. Nuestro foco en este trabajo será la noción de "localidad" en las derivaciones sintácticas, que ha sido el centro de gran parte de los estudios de orientación chomskyana durante la última década. Basándonos en problemas concretos que aparecen en la consideración de ejemplos atestiguados en los textos, proporcionaremos una explicación alternativa a la ortodoxia chomskyana. El objetivo es proveer al lector de una serie de herramientas teóricas explícitas que pueda utilizar en el análisis de la localidad en la lengua latina

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Palynological investigation of a 410 cm long core section from Tso Kar (33°10'N, 78°E, 4527 m a.s.l.), an alpine lake situated in the arid Ladakh area of NW India at the limit of the present-day Indian summer monsoon, was performed in order to reconstruct post-glacial regional vegetation and climate dynamics. The area was covered with alpine desert vegetation from ca. 15.2 to 14 kyr BP (1 kyr=1000 cal. years), reflecting dry and cold conditions. High influx values of long-distance transported Pinus sylvestris type pollen suggest prevailing air flow from the west and northwest. The spread of alpine meadow communities and local aquatic vegetation is a weak sign of climate amelioration after ca. 14 kyr BP. Pollen data (e.g. influx values of Pinus roxburghii type and Quercus) suggest that this was due to a strengthening of the summer monsoon and the reduced activity of westerly winds. The further spread of Artemisia and species-rich meadows occurred in response to improved moisture conditions between ca. 12.9 and 12.5 kyr BP. The subsequent change towards drier desert-steppe vegetation likely indicates more frequent westerly disturbances and associated snowfalls, which favoured the persistence of alpine meadows on edaphically moist sites. The spread of Chenopodiaceae-dominated vegetation associated with an extremely weak monsoon occurred at ca. 12.2-11.8 kyr BP during the Younger Dryas interstadial. A major increase in humidity is inferred from the development of Artemisia-dominated steppe and wet alpine meadows with Gentianaceae after the late glacial/early Holocene transition in response to the strengthening of the summer monsoon. Monsoonal influence reached maximum activity in the Tso Kar region between ca. 10.9 and 9.2 kyr BP. The subsequent development of the alpine meadow, steppe and desert-steppe vegetation points to a moderate reduction in the moisture supply, which can be linked to the weaker summer monsoon and the accompanying enhancement of the winter westerly flow from ca. 9.2 to 4.8 kyr BP. The highest water levels of Tso Kar around 8 kyr BP probably reflect combined effect of both monsoonal and westerly influence in the region. An abrupt shift towards aridity in the Tso Kar region occurred after ca. 4.8 kyr BP, as evidenced by an expansion of Chenopodiaceae-dominated desert-steppe. Low pollen influx values registered ca. 2.8-1.3 kyr BP suggest scarce vegetation cover and unfavourable growing conditions likely associated with a further weakening of the Indian Monsoon.

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Thirteen sediment samples, including calcareous ooze, sandy clay, volcanic sand, gravel, and volcanic breccia, from Ocean Drilling Program (ODP) Sites 732B, 734B, 734G and Conrad Cruise 27-9, Station 17, were examined. Contents of major and trace elements were determined using XRF or ICP (on samples <0.5 g). Determinations of rare earth elements (REE) were performed using ICP-MS. Mineralogy was determined using XRD. On the basis of the samples studied, the sediments accumulating in the Atlantis II Fracture Zone are characterized by generally high MgO, Cr, and Ni contents compared with other deep-sea sediments. A variety of sources are reflected in the mineralogy and geochemistry of these sediments. Serpentine, brucite, magnetite, and high MgO, Cr, and Ni contents indicate derivation from ultramafic basement. The occurrence of albite, analcime, primary mafic minerals, and smectite/chlorite in some samples, coupled with high SiO2, Al2O3, TiO2, Fe2O3, V, and Y indicate contribution from basaltic basement. A third major sediment source is characterized as biogenic material and is reflected primarily in the presence of carbonate minerals, and high CaO, Sr, Pb, and Zn in certain samples. Kaolinite, illite, quartz, and some chlorite are most likely derived from continental areas or other parts of the ocean by long-distance sediment transport in surface or other ocean currents. Proportions of source materials in the sediments reflect the thickness of the sediment cover, slope of the seafloor, and the nature of and proximity to basement lithologies. REE values are low compared to other deep-sea sediments and indicate no evidence of hydrothermal activity in the Atlantis II Fracture Zone sediments. This is supported by major- and trace-element data.