Efectos de un programa de flexibilidad en el desarrollo de la fuerza muscular en jugadoras de fútbol femenil

Se analizó el impacto de un programa de entrenamiento de flexibilidad sobre el desarrollo de la fuerza muscular en 16 jugadores de futbol con edad de 19.032.7 años. Se entrenó durante 30 días y 5 veces por semanas, donde el grupo "A" realizó entrenamiento de flexibilidad, mientras que "B" el entrenamiento regular. Se midió la flexibilidad, 1RM, salto vertical, peso, talla, circunferencia de pantorrilla y muslo. Los resultados muestran valores para A y B respectivamente, donde el IGF fue de 91.01 18.3 y 111.93 23.5; 78.22 29, y 79.03 29.1. La circunferencia femoral, 48.04 3.6 cms y 49.54 3.4 cms.; 47.56 4.9 y 47.89 5.2. Circunferencia de pantorrilla, 33.83 2.7 cm y 35.21 2.4 cm; 33.83 2 y 33.73 2.8. Fuerza 48.13 7.8 Kg. y 53.38 8.2 Kg.; 52.63 8.6 Kg. y 53.39 9.1 Kg. Potencia anaeróbica, 34.13 2.9 cm. y 36.63 1.7 cm; 38.25 4.7 y 37.06 3.4. Como conclusión se tiene que el uso la flexibilidad impacta de forma positiva en el IGF y por tanto en el desarrollo favorable muscular de jugadoras de fútbol.

Efectos de un programa de flexibilidad en el desarrollo de la fuerza muscular en jugadoras de fútbol femenil

Se analizó el impacto de un programa de entrenamiento de flexibilidad sobre el desarrollo de la fuerza muscular en 16 jugadores de futbol con edad de 19.032.7 años. Se entrenó durante 30 días y 5 veces por semanas, donde el grupo "A" realizó entrenamiento de flexibilidad, mientras que "B" el entrenamiento regular. Se midió la flexibilidad, 1RM, salto vertical, peso, talla, circunferencia de pantorrilla y muslo. Los resultados muestran valores para A y B respectivamente, donde el IGF fue de 91.01 18.3 y 111.93 23.5; 78.22 29, y 79.03 29.1. La circunferencia femoral, 48.04 3.6 cms y 49.54 3.4 cms.; 47.56 4.9 y 47.89 5.2. Circunferencia de pantorrilla, 33.83 2.7 cm y 35.21 2.4 cm; 33.83 2 y 33.73 2.8. Fuerza 48.13 7.8 Kg. y 53.38 8.2 Kg.; 52.63 8.6 Kg. y 53.39 9.1 Kg. Potencia anaeróbica, 34.13 2.9 cm. y 36.63 1.7 cm; 38.25 4.7 y 37.06 3.4. Como conclusión se tiene que el uso la flexibilidad impacta de forma positiva en el IGF y por tanto en el desarrollo favorable muscular de jugadoras de fútbol.

Gene expression and physiological changes of the Antarctic krill Euphausia superba under different hypoxia intensities

Antarctic krill (Euphausia superba) from South Georgia comprise one of the most northern and abundant krill stocks. South Georgia waters are undergoing rapid warming, as a result of climate change, which in turn could alter the oxygen concentration of the water. We investigated gene expression in Antarctic krill related to aerobic metabolism, antioxidant defence, and heat-shock response under severe (2.5% O2 saturation or 0.6 kPa) and threshold (20% O2 saturation or 4 kPa) hypoxia exposure compared to in situ levels (normoxic; 100% O2 saturation or 21 kPa). Biochemical metabolic and oxidative stress indicators complemented the genic expression analysis to detect in vivo signs of stress during the hypoxia treatments. Expression levels of the genes citrate synthase (CS), mitochondrial manganese superoxide dismutase (SODMn-m) and one heat-shock protein isoform (E) were higher in euphausiids incubated 6 h at 20% O2 saturation than in animals exposed to control (normoxic) conditions. All biochemical antioxidant defence parameters remained unchanged among treatments. Levels of lipid peroxidation were raised after 6 h of severe hypoxia. Overall, short-term exposure to hypoxia altered mitochondrial metabolic and antioxidant capacity, but did not induce anaerobic metabolism. Antarctic krill are swarming organisms and may experience short periods of hypoxia when present in dense swarms. A future, warmer Southern ocean, where oxygen saturation levels are decreased, may result in smaller, less dense swarms as they act to avoid greater levels of hypoxia.

Porewater concentrations, pH, single cell number, anaerobic oxidation of methane (AOM) rate, sulfate reduction (SR) rate of samples during METEOR cruise M76/3b at the REGAB cold seep site from the West African margin in 2008

The giant pockmark REGAB (West African margin, 3160 m water depth) is an active methane-emitting cold seep ecosystem, where the energy derived from microbially mediated oxidation of methane supports high biomass and diversity of chemosynthetic communities. Bare sediments interspersed with heterogeneous chemosynthetic assemblages of mytilid mussels, vesicomyid clams and siboglinid tubeworms form a complex seep ecosystem. To better understand if benthic bacterial communities reflect the patchy distribution of chemosynthetic fauna, all major chemosynthetic habitats at REGAB were investigated using an interdisciplinary approach combining porewater geochemistry, in situ quantification of fluxes and consumption of methane, as well bacterial community fingerprinting. This study revealed that sediments populated by different fauna assemblages show distinct biogeochemical activities and are associated with distinct sediment bacterial communities. The methane consumption and methane effluxes ranged over one to two orders of magnitude across habitats, and reached highest values at the mussel habitat, which hosted a different bacterial community compared to the other habitats. Clam assemblages had a profound impact on the sediment geochemistry, but less so on the bacterial community structure. Moreover, all clam assemblages at REGAB were restricted to sediments characterized by complete methane consumption in the seafloor, and intermediate biogeochemical activity. Overall, variations in the sediment geochemistry were reflected in the distribution of both fauna and microbial communities; and were mostly determined by methane flux.

Anaerobic oxidation of methane and sulphate reduction rates, hydrocarbons, sulphate and sulphide concentrations of sediment cores from the Larsen B embayment at the eastern site of the Antarctic Peninsula

First videographic indication of an Antarctic cold seep ecosystem was recently obtained from the collapsed Larsen B ice shelf, western Weddell Sea (Domack et al., 2005). Within the framework of the R/V Polarstern expedition ANTXXIII-8, we revisited this area for geochemical, microbiological and further videographical examinations. During two dives with ROV Cherokee (MARUM, Bremen), several bivalve shell agglomerations of the seep-associated, chemosynthetic clam Calyptogena sp. were found in the trough of the Crane and Evans glacier. The absence of living clam specimens indicates that the flux of sulphide and hence the seepage activity is diminished at present. This impression was further substantiated by our geochemical observations. Concentrations of thermogenic methane were moderately elevated with 2 µM in surface sediments of a clam patch, increasing up to 9 µM at a sediment depth of about 1 m in the bottom sections of the sediment cores. This correlated with a moderate decrease in sulphate from about 28 mM at the surface down to 23.4 mM, an increase in sulphide to up to 1.43 mM and elevated rates of the anaerobic oxidation of methane (AOM) of up to 600 pmol cm**-3 d**-1 at about 1 m below the seafloor. Molecular analyses indicate that methanotrophic archaea related to ANME-3 are the most likely candidates mediating AOM in sediments of the Larsen B seep.

Anaerobic methanotrophic archaea-2 and Desulfosarcina/Desulfococcus group in sediments at different stations

The anaerobic oxidation of methane (AOM) with sulfate as terminal electron acceptor is mediated by consortia of methanotrophic archaea (ANME) and sulfate-reducing bacteria (SRB). In sediment samples from Hydrate Ridge, the Isis Mud Volcano and the Gulf of Mexico, DSS cells accounted for 3-6% of all DAPI-stained single cells. Out of these, 8-17% were labelled with probe SEEP1a-1441. This translated into relative abundances of single SEEP-SRB1a cells of 0.3% to 0.7%. Contrastingly, in a sediment sample from the Gullfaks oil field, DSS cells accounted for 18% and SEEP-SRB1a for 9% of all single cells. This sediment sample also featured an unusually high abundance of single ANME-2 cells and only very few ANME-2/DSS aggregates in comparison with other AOM habitats. Considering also the nature of the sample, it is likely that the high number of single ANME-2 and SEEP-SRB1a cells were an artifact of sample preparation. Here, harsher sonication was required to remove the microorganisms from coarse sand prior to CARD-FISH analysis.

Measuring fixed costs for firms' use of a free trade agreement : threshold regression approach

In this paper, by employing the threshold regression method, we estimate the average tariff equivalent of fixed costs for the use of a free trade agreement (FTA) among all existing FTAs in the world. It is estimated to be 3.2%. This global estimate serves as a reference rate in the evaluation of each FTA’s fixed costs.