843 resultados para Diurnal firefly


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The freezing and desiccation tolerance of 12 Klebsormidium strains, isolated from various habitats (aero-terrestrial, terrestrial, and hydro-terrestrial) from distinct geographical regions (Antarctic - South Shetlands, King George Island, Arctic - Ellesmere Island, Svalbard, Central Europe - Slovakia) were studied. Each strain was exposed to several freezing (-4°C, -40°C, -196°C) and desiccation (+4°C and +20°C) regimes, simulating both natural and semi-natural freeze-thaw and desiccation cycles. The level of resistance (or the survival capacity) was evaluated by chlorophyll a content, viability, and chlorophyll fluorescence evaluations. No statistical differences (Kruskal-Wallis tests) between strains originating from different regions were observed. All strains tested were highly resistant to both freezing and desiccation injuries. Freezing down to -196°C was the most harmful regime for all studied strains. Freezing at -4°C did not influence the survival of studied strains. Further, freezing down to -40°C (at a speed of 4°C/min) was not fatal for most of the strains. RDA analysis showed that certain Antarctic and Arctic strains did not survive desiccation at +4°C; however, freezing at -40°C, as well as desiccation at +20 °C was not fatal to them. On the other hand, other strains from the Antarctic, the Arctic, and Central Europe (Slovakia) survived desiccation at temperatures of +4°C, and freezing down to -40°C. It appears that species of Klebsormidium which occupy an environment where both seasonal and diurnal variations of water availability prevail, are well adapted to freezing and desiccation injuries. Freezing and desiccation tolerance is not species-specific nor is the resilience only found in polar strains as it is also a feature of temperate strains.

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The properties of snow on East Antarctic sea ice off Wilkes Land were examined during the Sea Ice Physics and Ecosystem Experiment (SIPEX) in late winter of 2007, focusing on the interaction with sea ice. This observation includes 11 transect lines for the measurement of ice thickness, freeboard, and snow depth, 50 snow pits on 13 ice floes, and diurnal variation of surface heat flux on three ice floes. The detailed profiling of topography along the transects and the d18O, salinity, and density datasets of snow made it possible to examine the snow-sea-ice interaction quantitatively for the first time in this area. In general, the snow displayed significant heterogeneity in types, thickness (mean: 0.14 +- 0.13 m), and density (325 +- 38 kg/m**3), as reported in other East Antarctic regions. High salinity was confined to the lowest 0.1 m. Salinity and d18O data within this layer revealed that saline water originated from the surface brine of sea ice in 20% of the total sites and from seawater in 80%. From the vertical profiles of snow density, bulk thermal conductivity of snow was estimated as 0.15 W/K/m on average, only half of the value used for numerical sea-ice models. Although the upward heat flux within snow estimated with this value was significantly lower than that within ice, it turned out that a higher value of thermal conductivity (0.3 to 0.4 W/K/m) is preferable for estimating ice growth amount in current numerical models. Diurnal measurements showed that upward conductive heat flux within the snow and net long-wave radiation at the surface seem to play important roles in the formation of snow ice from slush. The detailed surface topography allowed us to compare the air-ice drag coefficients of ice and snow surfaces under neutral conditions, and to examine the possibility of the retrieval of ice thickness distribution from satellite remote sensing. It was found that overall snow cover works to enhance the surface roughness of sea ice rather than moderate it, and increases the drag coefficient by about 10%. As for thickness retrieval, mean ice thickness had a higher correlation with ice surface roughness than mean freeboard or surface elevation, which indicates the potential usefulness of satellite L-band SAR in estimating the ice thickness distribution in the seasonal sea-ice zone.

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El proyecto del presente trabajo consiste en reflexionar sobre la constitución del sujeto ético-político en los Erga de Hesíodo. Trabajaremos desde una propuesta de matriz antropológica, en torno a los consejos de administración familiar que el poeta propone, recurriendo a Jenofonte cuando la comparación sea oportuna. Siguiendo el horizonte semántico del término chresis, indagaremos dos cuestiones fundamentales, la gestión del hogar, a partir de la problematización del matrimonio como cuestión afín, y la gestión de los vínculos personales, que van más allá del oikos, para convocar a otros actores, el hermano, el huésped, el amigo. En ambos niveles, el estrictamente familiar con la presencia del marido y la esposa en el centro de la escena, y el familiar, en sentido más amplio, los tópicos devuelven ciertas preocupaciones y reflexiones en torno a cuestiones que se repiten, el trabajo, la riqueza, la productividad, la prudencia, el honor, la convivencia, la tolerancia. Se plasma un universo antropológico que nos permite relevar, desde los topoi recortados, la pequeña familia intramuros y la gran familia extramuros, la preocupación habitual de la constitución de un sujeto temperante que en Hesíodo cobra distintas aristas. El modelo discursivo obedece a las reglas de formación que reconocemos en los Erga como matriz de discurso: recomendaciones, consejos, exhortaciones, que delinean dos topoi reconocibles, dos categorías de sujetos, dos registros de conductas, dos modelos de instalación en la vida. Hesíodo nos tiene acostumbrados a esos sistemas binarios que, a nuestro juicio, se inscriben en la lógica del linaje. Hombres, valores, conductas de matriz diurna o nocturna, positiva o negativa, luminosa o tenebrosa. La vida familiar y la comunitaria no parece escapar a esta lógica binaria y el corpus de consejos no hace otra cosa que vigorizar con su logos el aspecto diurno de la tensión

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In the framework of the projects DYFAMED and PICASSO, diel variations of particulate dimethylsulfoniopropionate (DMSPp) and of its size fraction higher than 10 µm (DMSPp>10 µm) were studied in surface waters of the central Ligurian Sea in May 1990 and May 1995, and in the harbour of the city of Barcelona (Spain) in July 1998. Time series performed in stratified and nitrate depleted surface waters of the Ligurian Sea revealed that DMSPp>10 µm was undergoing diurnal variations. DMSPp-containing particles in the size range higher than 10 µm also markedly affected the DMSPp-to-chlorophyll (chl) a ratio of surface waters on a daily basis. The ratios were 35% to 72% lower at dawn than at dusk. The fact that the diadinoxanthin (DD)-to-chl a ratio of surface phytoplanktonic populations did not exhibit diurnal cycles suggests that physiological adaptation of cellular DMSP and chl a to the light conditions was not a likely process to account for the diurnal changes of the DMSPp-to-chl a ratio. It is suggested that such diurnal variability resulted from changes in plankton composition due to vertical migrations of DMSP-containing organisms larger than 10 µm. We have demonstrated from samples collected in the harbour of the city of Barcelona that DMSP-containing dinoflagellates are active diel migrants. However, the results obtained in the open sea in May 1990 suggest that dinoflagellates and also ciliates contribute to the pool of DMSPp in the size range larger than 10 µm. The results of May 1995 are ambiguous as to the role of dinoflagellates because, in the absence of specific cell counts, DMSPp>10 µm and the pigment peridinin, which is usually present in dinoflagellates (but peridinin-free dinoflagellates exist) showed very different vertical and temporal patterns.

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To evaluate the mechanical stress on the volcanic edifice that results from lava lake level variations, we deployed a self-recording, differential capacitance (MEMS Inertial Sensor STMicroelectronics LIS3LV02DQ), 3-axis X6-1A accelerometer (Gulf Coast Data Concepts, LLC) at a distance of ~100m from the center of the Nyiragongo lava lake on freshly erupted lava flows. The device range was used in high (12-bit) resolution mode, which corresponds to a sensitivity of about 1 mg. The device was set to high-sensitivity mode with four additional bits to improve resolution, yet with a much lower signal-noise ratio. Once in position, the accelerometer continuously recorded data for three-day periods in June 2010. The system was oriented so that the X- and Y-axes form a plain parallel to the lava lake. During data collection, we did not attempt to calibrate the precision of the angle because relative G-force measurements were required instead of absolute G-force measurements. To distinguish the tiny accelerations caused by temperature differentials of the atmosphere, from the forces caused by magma movements, the temperature of the X6-1A device was continuously recorded. Temperature variations were corrected for by applying a de-correlation method to the recorded signal. Data was collected at 20 Hz, regrouped into batches that cover 1 hour per observation and associated with one averaged temperature measurement. This method was reproducible because diurnal temperature variations were the main cause for heating and cooling.

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Feeding patterns of mass herbivorous copepods in upwelling areas are investigated. Daily rations and aspects of their formation are examined in Calanoides carinatus (Benguela upwelling), Calanus pacificus (off the California coast), and Calanus australis (Peru upwelling). Rations were calculated based on gut plant pigment contents obtained at daily stations using laser spectrofluorometry, experimental data on the rate of gut evacuation and data on the carbon/chlorophyll ratio in phytoplankton and particulate matter at the respective stations. When phytoplankton was abundant, diel feeding rhythms were not pronounced and gut pigment level was high during the entire 24-h period. When phytoplankton biomass was low, distinct feeding rhythms were pronounced with a nocturnal maximum. During active upwelling intensive feeding on phytoplankton supports energy (respiration) and plastic (growth, development, reproduction, accumulation of reserves) metabolism of copepods. When upwelling was inactive, the surface part of the population feeds less actively and is able only partially to cover its energy expenditures. The actively growing and reproducing populations of C. pacificus and C. carinatus may consume close to 20% of primary production, whereas the inactive population of C. australis consumed only 0.2% of primary production when upwelling weakened.

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El proyecto del presente trabajo consiste en reflexionar sobre la constitución del sujeto ético-político en los Erga de Hesíodo. Trabajaremos desde una propuesta de matriz antropológica, en torno a los consejos de administración familiar que el poeta propone, recurriendo a Jenofonte cuando la comparación sea oportuna. Siguiendo el horizonte semántico del término chresis, indagaremos dos cuestiones fundamentales, la gestión del hogar, a partir de la problematización del matrimonio como cuestión afín, y la gestión de los vínculos personales, que van más allá del oikos, para convocar a otros actores, el hermano, el huésped, el amigo. En ambos niveles, el estrictamente familiar con la presencia del marido y la esposa en el centro de la escena, y el familiar, en sentido más amplio, los tópicos devuelven ciertas preocupaciones y reflexiones en torno a cuestiones que se repiten, el trabajo, la riqueza, la productividad, la prudencia, el honor, la convivencia, la tolerancia. Se plasma un universo antropológico que nos permite relevar, desde los topoi recortados, la pequeña familia intramuros y la gran familia extramuros, la preocupación habitual de la constitución de un sujeto temperante que en Hesíodo cobra distintas aristas. El modelo discursivo obedece a las reglas de formación que reconocemos en los Erga como matriz de discurso: recomendaciones, consejos, exhortaciones, que delinean dos topoi reconocibles, dos categorías de sujetos, dos registros de conductas, dos modelos de instalación en la vida. Hesíodo nos tiene acostumbrados a esos sistemas binarios que, a nuestro juicio, se inscriben en la lógica del linaje. Hombres, valores, conductas de matriz diurna o nocturna, positiva o negativa, luminosa o tenebrosa. La vida familiar y la comunitaria no parece escapar a esta lógica binaria y el corpus de consejos no hace otra cosa que vigorizar con su logos el aspecto diurno de la tensión

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El proyecto del presente trabajo consiste en reflexionar sobre la constitución del sujeto ético-político en los Erga de Hesíodo. Trabajaremos desde una propuesta de matriz antropológica, en torno a los consejos de administración familiar que el poeta propone, recurriendo a Jenofonte cuando la comparación sea oportuna. Siguiendo el horizonte semántico del término chresis, indagaremos dos cuestiones fundamentales, la gestión del hogar, a partir de la problematización del matrimonio como cuestión afín, y la gestión de los vínculos personales, que van más allá del oikos, para convocar a otros actores, el hermano, el huésped, el amigo. En ambos niveles, el estrictamente familiar con la presencia del marido y la esposa en el centro de la escena, y el familiar, en sentido más amplio, los tópicos devuelven ciertas preocupaciones y reflexiones en torno a cuestiones que se repiten, el trabajo, la riqueza, la productividad, la prudencia, el honor, la convivencia, la tolerancia. Se plasma un universo antropológico que nos permite relevar, desde los topoi recortados, la pequeña familia intramuros y la gran familia extramuros, la preocupación habitual de la constitución de un sujeto temperante que en Hesíodo cobra distintas aristas. El modelo discursivo obedece a las reglas de formación que reconocemos en los Erga como matriz de discurso: recomendaciones, consejos, exhortaciones, que delinean dos topoi reconocibles, dos categorías de sujetos, dos registros de conductas, dos modelos de instalación en la vida. Hesíodo nos tiene acostumbrados a esos sistemas binarios que, a nuestro juicio, se inscriben en la lógica del linaje. Hombres, valores, conductas de matriz diurna o nocturna, positiva o negativa, luminosa o tenebrosa. La vida familiar y la comunitaria no parece escapar a esta lógica binaria y el corpus de consejos no hace otra cosa que vigorizar con su logos el aspecto diurno de la tensión

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This publication presents results of microbiological and biogeochemical studies in the White Sea. Material was obtained during a series of expeditions in 1999-2002. The studies were carried out in the open part of the White Sea, in the Onega, Dvina and Kandalaksha Bays, as well as in the intertidal zone of the Kandalaksha Bay. Quantitative characteristics of activity of microbial processes in waters and bottom sediments of the White Sea were obtained. The total number of bacteria was equal to 150000-800000 cells/ml, and intensity of dark CO2 assimilation was equal to 0.9-17 µg C/l/day. Bacterial sulfate reduction was equal to 3-150 mg S/m**2/day, and methane formation and oxidation was equal to 13-6840 and 20-14650 µl CH4/m**2/day, respectively. Extremely high values of intensity of all principal microbial processes were found in intertidal sediments rich in organic matter: under decomposing macrophytes, in local pits at the lower intertidal boundary, and in the mouth of a freshwater brook. Average hydrogen sulfide production in highly productive intertidal sediments was 1950-4300 mg S/m**2/day, methane production was 0.5-8.7 ml CH4/m**2/day, and intensity of methane oxidation was up to 17.5 ml CH4/m**2/day. Calculations performed with account for areas occupied by microlandscapes of increased productivity showed that diurnal production of H2S and CH4 per 1 km**2 of the intertidal zone (August) was estimated as 60.8-202 kg S/km**2/day and 192-300 l CH4/km**2/day, respectively.

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Vertical distributions and diel migrations of the main species of micronekton, four euphausiids, one mysid, one decapod and three fishes, were described in detail in the 0-1000 m water column on a fixed station in the Northwestern Mediterranean Sea. The euphausiids Euphausia krohni and Thysanopoda aequalis, the decapod Gennadas elegans and, to a lesser extent, the fish Argyropelecus hemigymnus were shown to perform clear diel vertical migrations. Results of horizontal hauls at a given depth around sunrise and sunset showed a marked diurnal symmetry of the migratory cycles, particularly for E.krohni, T.aequalis and G.elegans. The behaviour of the euphausiid Nematoscelis megalops was more complex: it presented a repetitive bimodal day distribution and only part of its population migrated. As very weak or non-migrators we found the euphausiid Stylocheiron longicorne and the bathypelagic mysid Eucopia unguiculata, for which migration concerned only some of the older individuals. The fishes Cyclothone braueri and Cyclothone pygmaea appeared to be non-migrants. As depth increased, C.braueri was replaced by C.pygmaea, with maximum concentrations at 350-550 and 550-700 m depth, respectively.

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A large population of the colonial pelagic tunicate Pyrosoma atlanticum occurred in April 1991 in offshore waters of the Ligurian Sea (Northwestern Mediterranean). The high numbers of colonies caught allowed their vertical distribution and diel migration in the 0-965 m water column to be described as a function of their size. Daytime depths and amplitudes of the migration were correlated with colony size. The amplitude of the migration ranged from 90 m for 3-mm-length colonies to 760 m for 51-mm-length colonies, with a mean amplitude of 410 m for the whole population, all sizes pooled. The results of horizontal hauls at a given depth around sunrise and sunset showed a marked diurnal symmetry of the migratory cycle relative to noon, and that migration of the population was not cohesive. For example, the larger the colonies, the later after sunset they reached the upper layers during their upward migration.

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High temporal resolution (three hours) records of temperature, wind speed and sea level pressure recorded at Antarctic research station Neumayer (70°S, 8°W) during 1982-2011 are analysed to identify oscillations from daily to intraseasonal timescales. The diurnal cycle dominates the three-hourly time series of temperature during the Antarctic summer and is almost absent during winter. In contrast, the three-hourly time series of wind speed and sea level pressure show a weak diurnal cycle. The dominant pattern of the intraseasonal variability of these quantities, which captures the out-of-phase variation of temperature and wind speed with sea level pressure, shows enhanced variability at timescales of ~ 40 days and ~ 80 days, respectively. Correlation and composite analysis reveal that these oscillations may be related to tropical intraseasonal oscillations via large-scale eastward propagating atmospheric circulation wave-trains. The second pattern of intraseasonal variability, which captures in-phase variations of temperature, wind and sea level pressure, shows enhanced variability at timescales of ~ 35, ~ 60 and ~ 120 days. These oscillations are attributed to the Southern Annular Mode/Antarctic Oscillation (SAM/AAO) which shows enhanced variability at these timescales. We argue that intraseasonal oscillations of tropical climate and SAM/AAO are related to distinct patterns of climate variables measured at Neumayer.