Human muscle net K(+) release during exercise is unaffected by elevated anaerobic metabolism, but reduced after prolonged acclimatization to 4,100 m

[EN] It was investigated whether skeletal muscle K(+) release is linked to the degree of anaerobic energy production. Six subjects performed an incremental bicycle exercise test in normoxic and hypoxic conditions prior to and after 2 and 8 wk of acclimatization to 4,100 m. The highest workload completed by all subjects in all trials was 260 W. With acute hypoxic exposure prior to acclimatization, venous plasma [K(+)] was lower (P < 0.05) in normoxia (4.9 +/- 0.1 mM) than hypoxia (5.2 +/- 0.2 mM) at 260 W, but similar at exhaustion, which occurred at 400 +/- 9 W and 307 +/- 7 W (P < 0.05), respectively. At the same absolute exercise intensity, leg net K(+) release was unaffected by hypoxic exposure independent of acclimatization. After 8 wk of acclimatization, no difference existed in venous plasma [K(+)] between the normoxic and hypoxic trial, either at submaximal intensities or at exhaustion (360 +/- 14 W vs. 313 +/- 8 W; P < 0.05). At the same absolute exercise intensity, leg net K(+) release was less (P < 0.001) than prior to acclimatization and reached negative values in both hypoxic and normoxic conditions after acclimatization. Moreover, the reduction in plasma volume during exercise relative to rest was less (P < 0.01) in normoxic than hypoxic conditions, irrespective of the degree of acclimatization (at 260 W prior to acclimatization: -4.9 +/- 0.8% in normoxia and -10.0 +/- 0.4% in hypoxia). It is concluded that leg net K(+) release is unrelated to anaerobic energy production and that acclimatization reduces leg net K(+) release during exercise.

Regional differences in modelled net production and shallow remineralization in the North Atlantic subtropical gyre

[EN] We used 5-yr concomitant data of tracer distribution from the BATS (Bermuda Time-series Study) and ESTOC (European Station for Time-Series in the Ocean, Canary Islands) sites to build a 1-D tracer model conservation including horizontal advection, and then compute net production and shallow remineralization rates for both sites. Our main goal was to verify if differences in these rates are consistent with the lower export rates of particulate organic carbon observed at ESTOC. Net production rates computed below the mixed layer to 110m from April to December for oxygen, dissolved inorganic carbon and nitrate at BATS (1.34±0.79 molO2 m?2, ?1.73±0.52 molCm?2 and ?125±36 mmolNm?2) were slightly higher for oxygen and carbon compared to ESTOC (1.03±0.62 molO2 m?2, ?1.42±0.30 molCm?2 and ?213±56 mmolNm?2), although the differences were not statistically significant. Shallow remineralization rates between 110 and 250m computed at ESTOC (?3.9±1.0 molO2 m?2, 1.53±0.43 molCm?2 and 38±155 mmolNm?2) were statistically higher for oxygen compared to BATS (?1.81±0.37 molO2 m?2, 1.52± 0.30 molCm?2 and 147±43 mmolNm?2). The lateral advective flux divergence of tracers, which was more significant at ESTOC, was responsible for the differences in estimated oxygen remineralization rates between both stations. According to these results, the differences in net production and shallow remineralization cannot fully explain the differences in the flux of sinking organic matter observed between both stations, suggesting an additional consumption of nonsinking organic matter at ESTOC.

Gestor web de recursos geoespaciales con tecnología Openlayers

[ES] El objetivo de este Trabajo Final de Grado (TFG) es la creación de un prototipo de aplicación web para la gestión de recursos geoespaciales. Esta propuesta surgió a partir de la necesidad de disponer de una herramienta que no tuviera que ser instalada en un dispositivo, sino servida por un servidor web, permitiendo su acceso desde cualquier parte y dispositivo. El resultado fue el Gestor Web de Recursos Geoespaciales con Tecnología OpenLayers, una aplicación que combina diversas herramientas (OpenLayers, GeoServer, PostgreSQL, jQuery…) – todas ellas basadas en Software Libre – para cumplir funcionalidades como la creación de primitivas vectoriales sobre un mapa, gestión y visualización de la información asociada, edición de estilos, modificación de coordenadas, etc. siendo todas éstas funcionalidades características de un Sistema de Información Geográfica (SIG) y ofreciendo una interfaz de uso cómoda y eficaz, que abstraiga al usuario de detalles internos y complejos. El material desarrollado dispone del potencial necesario para convertirse en una solución a las necesidades de gestión de información geoespacial de la ULPGC, especialmente en el campus de Tafira, sobre el que se ha ejemplificado su uso. Además, a diferencia de las herramientas ofertadas por empresas como Google o Microsoft, esta aplicación está por completo bajo una licencia GNU GPL v3, lo que permite que se pueda indagar dentro de su código, mejorarlo y añadir funcionalidades a cualquier persona interesada.

Teoría celular de los sistemas IPO-NET

Director de tesis: Antonio Ocón Carreras. Programa de doctorado: Tecnologías de la información y sus aplicaciones